Untitled

第 3 卷第 1 期 

古生物学文摘 ( 网络版 ) 

目录 

2007 年 3 月 

古生物学 

综论 …………………………(1) 

遗迹化石 ……………………(6) 

分子古生物学 ………………(9) 

古生态学 ……………………(11) 

微体古生物学 

综论 ………………………….(13) 

孢粉 ………………………….(13) 

疑源类 ……………………….(32) 

牙形石 ……………………….(44) 

古植物学 

藻类 …………………………(34) 

被子植物 ……………………(35) 

古无脊椎动物学 

综论 ………………………….(35) 

原生动物 …………………….(36) 

古杯、多孔及腔肠物 ……….(42) 

苔藓动物 …………………….(44) 

腕足动物 …………………….(45) 

软体动物 …………………….(47) 

节肢动物 …………………….(74) 

棘皮动物 …………………….(87) 

笔石动物 …………………….(92) 

分类位置不明 ……………….(93) 

古脊椎动物学 

综论 ………………………….(94) 

鱼类 ………………………….(96) 

两栖类 ……………………….(101) 

爬行类 ……………………….(102) 

鸟类 ………………………….(115) 

哺乳类 ……………………….(117) 

古人类学 

古人类学 …………………….(126) 

历史地质学、地层学 

综论 ………………………….(130) 

古地理学、古气候学 ……….(132) 

古生界 ……………………….(138) 

中生界 ……………………….(155) 

新生界 ……………………….(134)

第 3 卷第 1 期 

古生物学文摘 ( 网络版 ) 

2007 年 3 月 

古生物学 

综论 

2007010001 

真核生物厌氧生活方式的多复式起源 = 

Multiple secondary origins of the anaerobic 

lifestyle in eukaryotes. ( 英文 ). Embley T M. 

Philosophical Transactions of the Royal Society 

B: Biological Sciences, 2006, 361(1470): 

1055-1067 

Classical ideas for early eukaryotic evolution 

often posited a period of anaerobic evolution 

producing a nucleated phagocytic cell 

to engulf the mitochondrial endosymbiont, 

whose presence allowed the host to colonize 

emerging aerobic environments. This idea was 

given credence by the existence of contemporary 

anaerobic eukaryotes that were thought to 

primitively lack mitochondria, thus providing 

examples of the type of host cell needed. 

However, the groups key to this hypothesis 

have now been shown to contain previously 

overlooked mitochondrial homologues called 

hydrogenosomes or mitosomes; organelles 

that share common ancestry with mitochondria 

but which do not carry out aerobic respiration. 

Mapping these data on the unfolding 

eukaryotic tree reveals that secondary adaptation 

to anaerobic habitats is a reoccurring 

theme among eukaryotes. The apparent ubiquity 

of mitochondrial homologues bears testament 

to the importance of the mitochondrial 

endosymbiosis, perhaps as a founding event, 

in eukaryotic evolution. Comparative study of 

different mitochondrial homologues is needed 

to determine their fundamental importance for 

contemporary eukaryotic cells. 

2007010002 

生物进化研究的回顾与展望 = Reviews and 

prospectives on the studies of biological evolution. 

( 中文 ). 郝家胜 . 微体古生物学 

报 , 2003, 20(3): 325-332 

生物进化是自然科学的永恒之迷。随 

着历史的发展和科学的进步 , 生物进化思想 

从早期的萌芽 , 到自然选择学说、新达尔文 

主义 , 从现代综合理论 , 到分子进化的中性 

学说 , 再到新灾变论和点断平衡论等。当前 , 

由于生物学各分支学科的飞速发展 , 它们就 

各自的研究对象在宏观和微观上不断地拓 

展和深入 , 并在不同的层次上形成了广泛的 

交叉、渗透和融合 , 现代的进化生物学研究 

从宏观的表型到微观的分子 , 从群体遗传改 

变的微进化到成种事件以及地史上生物类 

群谱系演化的宏进化 , 从直接的化石证据到 

基于形态性状、分子证据和环境变迁的综 

合推理 , 从基于遗传基础的比较基因组学到 

演化机理的进化发育生物学等。可以预见 , 

在新的世纪里 , 在哲学和具体方法论 ( 如系 

统论、控制论和信息论 ) 的指导下 , 在生命 

科学、其他自然科学乃至社会科学工作者 

的通力合作下 , 综合遗传、发育和进化等研 

究领域的各种理论成果 , 生物进化理论即将 

出现也一定会出现的一个新的大综合和新 

的大统一。 

2007010003 

阿根廷内乌肯盆地下白垩统 Agrio 组 

Pilmatue 段大化石的埋葬、均时效应及横 

向搬运 = Taphonomy, time-averaging and 

lateral transport of the macrofossils of the 

Pilmatue Member of the Agrio Formation, 

Lower Cretaceous, Neuquen Basin, Argentina. 

( 其他 ). Lazo D G. Ameghiniana, 2006, 43(2): 

311-326 

A taphonomic and sedimentary facies 

analysis of the Pilmatue Member of the Agrio 

Formation in central Neuquen basin is presented 

to determine the time-averaging and 

degree of lateral transport of its macrofauna. 

The Pilmatue Member is characterized by 

abundant fossil concentrations dominated by 

benthic organisms such as corals, serpulids, 

bivalves and gastropods. Stratigraphic occurrence 

of benthic elements was accurately 

dated by a refined ammonite zonation of the 

Agrio Formation. Three sections were studied 

between Chos Malal and Zapala (Neuquen) 

situated on a north-south line of 44.2 km. Five 

litofacies and nine taphofacies were defined. 

The depositonal system is interpreted as a 

storm influenced homoclinal shoreface to 

shelf environment. Taphonomic analysis 

showed that most macrofaunistic associations 

are autochthonous or slightly parautochthonous 

with no significant lateral transport. Census, 

within-habitat time-averaged and environmentally 

condensed assemblages were 

identified. Time scales of fossil accumulation 

span from days-years up to 0.5 My. Nearshore 

assemblages are less time-averaged than shelf 

assemblages as in modern settings. 

2

2007010004 

华南早 — 中奥陶世腕足动物群落生态多样 

性演变 = Beta-diversity fluctuations in Early- 

Mid Ordovician brachiopod communities of 

South China. ( 英文 ). Zhan Renbin; Jin Jisuo; 

Rong Jiayu. Geological Journal, 2006, 

41(3/4): 271-288 

Lower to Middle Ordovician transitional 

strata (Acrograptus filiformis Biozone to Exigraptus 

clavus Biozone) of the Upper Yangtze 

Platform contain rich and diverse brachiopods, 

particularly in the Daguanshan Formation of 

Sichuan Province, the Meitan Formation of 

Guizhou Province, and the Yingpan Formation 

of Houping, Chongqing City. On the basis 

of multivariate analyses of 207 samples (about 

15 000 brachiopod specimens) and 61 species 

from these strata, 23 brachiopod-dominated 

communities and associations are delineated 

through six graptolitic biozones (Acrograptusfiliformis 

to Exigraptus clavus biozones). The 

disparity of brachiopod associations or betadiversity, 

as measured by the number of contemporaneous 

associations across variable 

ecological settings, was low in the A. filiformis 

Biozone and increased through the 

overlying graptolitic biozones to reach an 

acme in the Azygograptus suecisus and Expansograptus 

hirundo biozones, where as 

many as nine different brachiopod associations 

thrived in mid-shelf and also established 

in inner- and outer-shelf environments. Despite 

a sharp increase in a-diversity within the 

Didymograptellus eobifidus Biozone, betadiversity 

remained relatively low, with only 

three distinct brachiopod communities. The 

diversity of brachiopod associations suffered 

an abrupt drop in the E. clavus Biozone, as a 

result of a major faunal turnover event, with 

only a single Metorthis Community present in 

an upper mid-shelf setting. Temporally, 

brachiopod associations appear to be most 

stable in mid-shelf settings, with the 

Paralenorthis, Sinorthis, Desmorthis, and 

Euorthisina communities having a relatively 

high a-diversity and lasting through two to 

five graptolitic biozones. In both species composition 

and temporal duration, the brachiopod 

associations at the shallow- (BA1 to upper 

BA2) and deep-shelf (BA4) settings are unstable, 

characterized by low a-diversity and 

rapid vertical changes. This study implies that, 

during the Early and Mid Ordovician, 

brachiopod communities already attained a 

high level of organization in mid-shelf settings, 

but remained poorly established in high-stress 

environments of very shallow or very deep 

shelf settings 

2007010005 

生物群的起源和辐射 : 来自中国的实证第 

一集的前言 = Originations and Radiations in 

the Biota of China - Part 1 - Preface. ( 英文 ). 

Rong Jiayu; Somerville I. Geological Journal, 

2006, 41(3/4): 255-258 

2007010006 

热河生物群的演化辐射 : 年代学和生态学 

前景 = Evolutionary radiation of the Jehol 

Biota: chronological and ecological perspectives. 

( 英文 ). Zhou Zhonghe. Geological 

Journal, 2006, 41(3/4): 377-393 

The Jehol Biota, preserved in the lacustrine 

sediments of Liaoning Province, northeast 

China, has provided a new window for 

understanding Early Cretaceous terrestrial 

ecosystems. Based on recent geochronological 

and biostratigraphic studies of the fossilbearing 

deposits, a preliminary temporal 

framework has been established and suggests 

that the Jehol Biota had lasted for at least I I 

Ma during the late Early Cretaceous (131-120 

Ma). The development of the Jehol Biota can 

be divided into three major phases, with the 

most significant biological radiations occurring 

in the second phase between the Barremian 

and Aptian (approximately 125 Ma). 

Thanks to a diverse forest environment, major 

vertebrate groups, i.e. pterosaurs, dinosaurs, 

birds and mammals, in the Jehol Biota are 

characterized by a remarkably high percentage 

of arboreal and herbivorous forms. In addition 

to strong phylogenetic and morphological differentiation 

and high taxonomic diversity, the 

Jehol Biota is also characterized by significant 

dietary differentiation and biological interactions, 

i.e. competition and co-evolution between 

various animal groups, in an environment 

shaped by tectonic activities and palaeoclimatic 

changes both at a global and local 

scale. 

2007010007 

法国东南部 La 'Mede' 地区上白垩统桑托阶 

琥珀 = Presence of amber in the Upper Cretaceous 

(Santonian) of La 'Mede' (Martigues, 

southeastern France). IRTF characterization. 

( 法文 ). Guiliano M; Mille G; Onoratini G; 

Simon P. Comptes Rendus Palevol, 2006, 5(7): 

851-858 

Nodules of fossil resin, associated with 

lignitized woods, have been found, next to the 

3

pond of Berre, not far from Martigues, in the 

area of La Mede in clayey and sandy lagunobrackish 

fort-nations of Santonian age. A 

FTIR study, using attenuated total reflexion 

with a diamond crystal, as well as the comparison 

with ambers and a copal of reference 

and with the FTIR data of the literature, has 

shown that this resin has a lesser maturity than 

Cretaceous ambers rather comparable to Baltic 

ambers of the Tertiary. This low maturity is 

confirmed by the analysis of the associated 

lignitized woods. However, the chemical 

structure of the amber of La Mede appears 

very different from that of Baltic ambers. 

2007010008 

演化的过去与将来 : 斯蒂芬 . 古尔德演化理 

论构架的简介和部分要点 = Evolution's past 

and future: an introduction and partial precis 

to Stephen Jay Gould's The Structure of Evolutionary 

Theory. ( 英文 ). Padian K. Comptes 

Rendus Palevol, 2003, 2(6-7): 335-352 

In The Structure of Evolutionary Theory, 

his last and largest book on evolution, Stephen 

Jay Gould conceives of the structure of evolutionary 

theory since Darwin as comprising 

three major propositions. First, natural selection 

is the most important direction-giving 

force in evolution. Second, it operates at the 

level of the individual organism. Third, selection 

can be extrapolated smoothly from its 

actions on individuals in living species 

throughout geologic time, to produce the 

gradual divergence of species and adaptations 

that characterizes the history of life. Challenges 

to each of these major propositions, 

according to Gould, can be of three kinds of 

severity. The most severe challenges, if true, 

would nullify one of the major propositions 

entirely, thus destroying the integration of the 

theory (and perhaps the logic and support of 

its other propositions). Other, less severe challenges 

would revise, modify, and expand the 

content and scope of one or another of the 

propositions, but not destroy any of them or 

the theory in toto. Still other, even less severe 

challenges add to what is known and extend 

the scope and possibilities of the theory, but 

do not call for a revision in its fundamental 

structure. Gould acknowledges that the theory 

has withstood all presumptive challenges that 

would destroy it, and has accommodated those 

that simply extend and add to it. His principal 

concern is with those challenges that would 

revise the theory substantially: for example, if 

processes other than natural selection were of 

great importance in evolution; if selection 

acted in important ways at the level of species 

and clades, and (or) at the level of the genes, 

alleles, and chromosomes; and if the extrapolation 

of what is known from living populations 

could not by itself explain many patterns 

of large-scale evolution seen in the fossil record. 

He thinks that, both through the history 

of evolution since Darwin and in the present 

day, challenges that substantially revise these 

basic propositions are valid, and that the theory 

needs to integrate them in order to retain 

the explanatory power that it has had for many 

decades. 

2007010009 

赝品及其使用 = Forgeries and use of forgery.. 

( 法文 ). Debrenne F. Comptes Rendus 

Palevol, 2003, 2(6-7): 361-372 

Gould's observations on the falsified fossils 

of Morocco are completed by Cambrian 

and Mesozoic examples. The methods of falsification 

are briefly described. Gould has compared 

this mystification to the Beringer 

"Lugensteine" of the XVIIIth century. Was the 

Piltdown Man half human and half-ape Was 

Teilhard de Chardin an accomplice in this 

hoax European Paleozoic fossils were said to 

have been fraudulently introduced in Deprat's 

field localities. Accused and later rehabilitated, 

the question of the real origin of the fossils is 

still open: who is guilty Gupta has conceived 

an improbable Himalayan geology, with fossils 

of other countries, determined with confidence 

by specialists. Frontals, wearing spiral 

horns of an unknown bovid, Pseudonovibos, 

were in fact falsified horns of ordinary domestic 

bos (Indochina). The mediatic series about 

Archaeoraptor the first flying dinosaur, ended 

when it was recognised that the specimen is a 

composite, a chimera between a carnivorous 

dinosaur and Cretaceous bird. 

2007010010 

种演化中的连续性对非连续性、线性对非 

线性 = Continuity versus discontinuity, linear 

versus nonlinear in species evolution. ( 法文 ). 

Chaline J. Comptes Rendus Palevol, 2003, 

2(6-7): 413-421 

Species evolution is a topic where concepts 

of continuity and discontinuity have 

been opposed for two centuries. What is the 

situation today in biological evolution The 

statistical distribution of appearances and disappearances 

among rodent species follows 

power laws, suggesting nonlinearity and fractal 

structures. Thus, the domain of living beings 

seems to be extended, through critical 

4

physical phenomena, to the analysis of linear 

versus nonlinear biological phenomena. These 

observations are consistent with the new scale 

relativity theory of Nottale, which predicts 

many domains of resolution in nature separated 

by scale dependence or scale independence. 

Despite some scale-dependence particular 

to various levels of biological organization, 

the fact that they are also characterized by 

scale-independence suggests that they could 

be described by new fundamental laws revealing 

their potentially fractal and irreversible 

character. In the proximity of the critical time, 

specific to each system, the system becomes 

unstable and fractal, and shows precursor 

events at an accelerated rate leading up to the 

critical time. After the critical time, the system 

shows replicate events, in a decelerating manner. 

The discontinuous appearance of a number 

of clades follows a log-periodic law with a 

middle scale report of 1.73. This law, first 

applied to earthquakes, stock market crashes, 

demography, and physical turbulences, and 

now also being applied with success to macroevolutionary 

patterns, seems to have a certain 

universality. 

2007010011 

关于宏演化的论争 = The macroevolutionary 

debate. ( 法文 ). Neige P. Comptes Rendus 

Palevol, 2003, 2(6-7): 423-433 

Several historical as well as more recent 

aspects of macroevolutionary theory are discussed, 

in connection with a research program 

initiated by several working groups over the 

last ten years: it consists in dividing the taxonomic 

(diversity) and morphologic (disparity) 

components of biodiversity when studying its 

fluctuations through time. Studies have frequently 

shown a dissociation between the two 

metrics through the history of clades. Comparing 

diversity and disparity is a productive approach, 

which is leading to an exploration of 

large-scale biodiversity fluctuations in terms 

of both patterns and processes. 

2007010012 

从宇宙微观演化到概括性理论 : 斯蒂芬 . 古 

尔德与陆地蜗牛及其演化 = From an evolutionary 

microcosm to general theory: Land 

snails, Steve Gould and evolution. ( 法文 ). 

Tillier S. Comptes Rendus Palevol, 2003, 2(6- 

7): 435-453 

From 1962 to the end of his career, 

Stephen Jay Gould has studied the land snails 

of the genera Poecilozonites and then Cerion. 

Snails have provided him material to develop 

his morphometric methods, to analyze shell 

growth, and may have been at the origin of his 

work on ontogeny and phylogeny. Their variation, 

which he interpreted in terms of adaptation 

until the beginning of the 1980s, has been 

later reanalyzed by him in terms of nonadaptive 

evolution and contingency. Growth 

and variation of the shell allowed Gould to 

define constraint and canalisation in evolution. 

In their taxonomic work, Gould and Woodruff 

have practiced a definition of biological species 

as the group of populations allowing 

maximal congruence of their morphological 

characters, genetic characters and geographic 

distribution, of which potential interfecundity 

is necessary, but not sufficient. 

2007010013 

斯蒂芬 J. 古尔德 : 原核生物及其在地质时 

期的演化 = Stephen Jay Gould, the prokaryotes 

and their evolution in a geological context. 

( 英文 ). Westall F. Comptes Rendus 

Palevol, 2003, 2(6-7): 485-501 

Stephen Jay Gould (Full. House, Harmony 

Books, New York, 1996) emphasised 

the importance of the bacterial (prokaryote) 

world right from the beginnings of the history 

of life, up to the present day and, even into the 

future. Moreover, he suggested that the various 

forms of life on the planet today represent 

a diversification, or increase in complexity, 

from these simple organisms, rather than a 

directed evolution towards complexity. On the 

scale of evolution, the oldest fossils, dating 

back to almost 3.5 billion years ago, comprise 

simple unicellular organisms, i.e. prokaryotes 

that occur adjacent to the left wall of complexity. 

As far as can be ascertained from the fossil 

record, this early life had already exploited 

all the possible ramifications of diversification 

within an anaerobic environment and within 

the habitats available on the early Earth. Further 

evolution from this stage involved the 

development of organisms undertaking oxygenic 

photosynthesis that opportunistically 

invaded the newly formed, sunlight-bathed, 

shallow water continental platforms 

2007010014 

由曲颈龟类检验柯普法则 : 现生种的体形 

大小反映物种体形渐大的趋势吗 = 

Cope's rule in cryptodiran turtles: do the body 

sizes of extant species reflect a trend of 

phyletic size increase. ( 英文 ). Moen D S. 

Journal of Evolutionary Biology, 2006, 19(4): 

1210-1221 

5

Cope's rule of phyletic size increase is 

questioned as a general pattern of body size 

evolution. Most studies of Cope's rule have 

examined trends in the paleontological record. 

However, neontological approaches are now 

possible due to the development of modelbased 

comparative methods, as well as the 

availability of an abundance of phylogenetic 

data. I examined whether the phylogenetic 

distribution of body sizes in extant cryptodiran 

turtles is consistent with Cope's rule. To do 

this, I examined body size evolution in each of 

six major clades of cryptodiran turtles and also 

across the whole tree of cryptodirans (n = 201 

taxa). Extant cryptodiran turtles do not appear 

to follow Cope's rule, as no clade showed a 

significant phyletic body size trend. Previous 

analyses in other extant vertebrates have also 

found no evidence for phyletic size increase, 

which is in contrast to the paleontological data 

that support the rule in a number of extinct 

vertebrate taxa. 

2007010015 

模糊集理论对特提斯西部 Nummulites millecaput 

种统计评价的应用 = Application of 

the fuzzy set theory to the biometric evaluation 

of the species Nummulites millecaput in 

the western part of the Tethys.. ( 法文 ). Bardossy 

G; Kecskemeti T; Fodor J. Comptes 

Rendus Palevol, 2003, 2(5): 317-324 

Application of the fuzzy set theory to the 

biometric evaluation of the species Nummulites 

millecaput in the western part of the 

Tethys. The goal of this paper is to demonstrate 

the ability of the fuzzy-set theory to 

contribute to the evaluation of paleontological 

problems. As an example, the species Nummulites 

millecaput, Boubee has been chosen. One 

hundred specimens of this species, collected 

from four localities (Arrimblar, Adelholzen, 

Dudar, and Mount-Kotuc) have been prepared 

(equatorial sections) for the biometric measurement 

of the external and internal characteristics. 

First a traditional statistical evaluation 

was performed. followed by the construction 

of membership functions, the latter ones expressing 

in the best way the transitions from 

one locality to the other. The results of this 

evaluation confirmed that from Aquitaine 

(France) to Armenia, the same species - 

Nummulites millecaput - was distributed during 

the Eocene. 

遗迹化石 

2007010016 

阿根廷丘布特圣豪尔赫湾 Sarmiento 组和 

Chenque 组之间界线舌形菌迹遗迹相变异 

= Variability of the Glossifuncites ichnofacies 

at the boundary between the Sarmiento Formation 

(middle Eocene-early Miocene) and 

Chenque Formation (early Miocene) in San 

Jorge Gulf, Chubut, Argentina. ( 其他 ). Carmona 

N B; Ponce J J; Mangano M G; Buatois 

L A. Ameghiniana, 2006, 43(2): 413-425 

This study focuses on the ichnologic and 

stratigraphic characteristics of the boundary 

surface between the Sarmiento (middle Eocene- 

early Miocene) and Chenque Formations 

(early Miocene). The analyzed outcrops 

are, located near Comodoro Rivadavia city, 

Chubut Province, Patagonia, Argentina. The 

studied boundary represents a co-planar surface 

of low-stand erosion and transgressive 

erosion that produced exhumation of deposits 

belonging to the Sarmiento Formation, allowing 

the development of the Glossifungites 

ichnofacies. This ichnofacies is characteristic 

of stiff and dewatered sediments (firmgrounds) 

and comprises a particular suite of substratecontrolled 

trace fossils. In the studied outcrops 

(Astra, bahia Solano and Infiernillo), this 

boundary surface was colonized by decapod 

crustaceans that constructed galleries (Thalassinoides 

isp.) and bivalves that constructed 

dwelling structures (Gastrochaenolites ornatus). 

Although in all these localities the ichnotaxonomic 

composition does not show significant 

variations, important paleoecological differences 

between the trace fossil suites preserved 

in each outcrop can be inferred. Recent 

assemblages that colonize firm-ground surfaces 

seem to be controlled by three main parameters: 

sediment texture, substrate firmness 

and bathymetry. In the Miocene examples, the 

observed variability of the Glossifungites 

ichnofacies was probably controlled by the 

firmness of the surface. exhumed during the 

Leonense transgression. Analysis of the ichnologic 

content, truncation of trace fossils, 

and the relationship between biogenic structures 

suggests a complex history for this erosive 

surface, involving successive events of 

ravinement erosion and benthic colonization. 

2007010017 

三叶虫油栉虫科 — 鹿藻迹 : 生物成因的造 

迹者 , 来自阿根廷东科迪勒拉寒武 - 奥陶纪 

的实例研究 = Olenidae (Trilobita)- 

Rusophycus isp.: producer organism - resulting 

ichnofossil. Cases for the analysis in the 

Cambro-Ordovician of the Argentine Eastern 

6

Cordillera. ( 法文 ). Acenolaza G F. 

Ameghiniana, 2003, 40(4): 573-583 

Co-occurrence of Rusophycus isp. A. and 

the olenid Angelina hyeronimi (Kayser) from 

the Cambro-Ordovician beds of the Casa Colorada 

Formation is shown and analyzed. In 

addition, Rusophycus polonica is described 

from the Upper Tremadoc Coquena Formation, 

displaying some distinctive cephalic morphological 

characters of trilobites. Paleoenvironmental 

considerations are also presented on 

the basis of the distribution of ichnoassociations 

within the different lithofacies of northwestern 

Argentina, supporting a relatively 

shallow water setting for the Cambro- 

Orclovician transition. The dominance of elements 

that characterize the Cruziana and Skolithos 

"inchnofacies" support this panorama. 

Finally, a preliminary attempt to relate the 

stratigraphical distribution of Critziana and 

Ritsophycus with different trilobite families is 

presented for the region. 

2007010018 

阿根廷 Calingasta-Uspallata 盆地 Hoyada 

Verde 组遗迹化石属 Psammichnites = The 

Ichnogenus Psammichnites Torell, 1870 in the 

Hoyada Verde Formation, Upper Carboniferous 

of the Calingasta-Uspallata Basin. ( 法文 ). 

Mangano M G; Buatois L A; Limarino C O; 

Tripaldi A; Caselli A. Ameghiniana, 2003, 

40(4): 601-608 

The ichnogenus Psammichnites Torell is 

documented in the Hoyada Verde Formation, 

Carboniferous, Calingasta-Uspallata Basin. 

Two ichnospecies are described and illustrated, 

P. implexus and P. plummeri. In previous 

studies, these structures were erroneously referred 

to as Stibphyllochorda, Helminthoida 

and HeInfinthorhaphe. The presence of 

Psammichnites provides unequivocal ichnologic 

evidence of marine conditions, as also 

indicated by the abundant marine body fossils 

preserved in the succession. 

2007010019 

阿根廷 Sistema de Famatina 地区苏里组火 

山碎屑地层中的遗迹化石 Arachnostega 

gastrochaenae = Arachnostega gastrochaenae 

Bertling (trace fossil) in the volcaniclastic sequences 

of the Suri Formation, Sistema de 

Famatina, Argentina. ( 其他 ). Acenolaza G F; 

Gutierrez-Marco J C; Peralta S. 

Ameghiniana, 2003, 40(3): 315-322 

The occurrence of Arachnostega gastrochaenae 

Bertling on internal moulds of Lower 

Paleozoic mollusks, brachiopods and trilobites 

is reported. The material was found in volcaniclastic 

sediments of the Arenig Suri Formation, 

cropping out in the Sierra de Narvaez, 

Catamarca Province (northwestern Argentina). 

The ichnospecies displays a burrow network 

characterized by a branching pattern with 

variable diameter and slightly irregular internal 

walls. The ichnogenus was originally described 

from Jurassic reefs and modern sediments 

of northern Germany. In South America, 

Arachnostega had only been mentioned in 

Argentina and Uruguay, recorded from Jurassic 

and probably Carboniferous-Permian strata 

respectively. With this new locality, we present 

the oldest record of Arachnostega (Lower 

Ordovician). Paleoecologic interpretations are 

done by means of the particular sedimentologic 

setting of the Suri Formation. Additional 

occurrences of the ichnogenus in bivalve 

and trilobite moulds from Ordovician 

sequences in Europe (Spain, France and the 

Czech Republic), and Devonian strata of La 

Paz (Bolivia) are also mentioned. 

2007010020 

阿根廷圣胡安省 Huerta de Huachi 地区 

Orchesteropus atavus 标准地点的遗迹学和 

古环境特征 = Ichnologic and paleoenvironmental 

characterization of the Orchesteropus 

atavus Frenguelli type locality, Huerta de 

Huachi, San Juan province, Argentina.. ( 其他 ). 

Buatois L A; Mangano M G. 

Ameghiniana, 2003, 40(1): 53-70 

The ichnofossil Orchesteropus atavius 

Frenguelli is only known from the Carboniferous 

of Argentina. Originally described from 

the locality of Huerta de Huachi, near Jachal, 

San Juan Province, no detailed information on 

the associated ichnofauna and sedimentary 

facies was available. Orchesteropus atavus 

occurs in parallel laminated mudstones accumulated 

from suspension fallout, but interbedded 

with dilute turbidites. Orchesteropus atavus 

is associated with simple grazing trails 

(Cochlichnus anguieus Hitchcock, Gordia 

marina Emmons, Helminthoidichnites tenuis 

Fitch, Helminthopsis tenids Ksiazkiewicz, 

Mermia carickensis Smith), feeding traces 

(Circulichnis montanus Vyalov, Treptichnus 

bifurcus Miller), resting traces (Rusophycus 

isp.), other arthropod trackways (Diplichnites 

gouldi Gevers, Maculichna carboniferus 

(Pazos), Umfolozia isp.), and fish trails (Undichna 

britannica Higgs, Undichna isp.). 

Dominance of superficial trails rather than 

infaunal traces, preservation of delicate traces 

7

in the absence of bioturbation, presence of 

plurispecific rather than monospecific suites, 

relatively high ichnodiversity, presence of 

ichnotaxa common in continental settings, and 

absence of ichnotaxa indicative of marine influence 

collectively argue for subaqueous 

deposition under freshwater conditions. Palynomorphs 

from the trace fossil-bearing beds 

are terrestrially derived with no marine representatives 

associated. The analyzed ichnofauna 

is remarkably different from brackish 

water trace fossil assemblages described from 

late Paleozoic marginal marine environments 

of Laurasia and Gondwana. Integration of ichnologic 

data with stratigraphic, sedimentologic, 

and palynologic information suggests 

deposition in fjord settings. 

2007010021 

阿根廷西北部 Puncoviscana 遗迹动物群 : 

前寒武纪 — 寒武纪过渡期的深海集群及古 

环境与古生态系统重建 = The Puncoviscana 

ichnofauna of northwest Argentina: The colonization 

of the deep sea and reconstruction of 

paleoenvironments and paleoecosystems of 

the Precambrian-Cambrian transition.. ( 其他 ). 

Buatois L A; Mangano M G. 

Ameghiniana, 2003, 40(1): 103-117 

The paleoecological, paleoenvironmental 

and evolutionary significance of the Puncoviscana 

ichnofauna is re-evaluated in the light of 

new ideas regarding the anactualistic nature of 

Precambrian-Cambrian ecosystems and the 

role of microbial communities in ecologic 

structure. The ichnofauna includes a wide variety 

of ichnotaxa, such as Circulichnis, Cochlichnus, 

Helminthopsis, Helminthoidichnites, 

Nereites, Oldhamia, Palaeophycus and Treptichnus, 

as well as several types of arthropod 

trackways. Structures considered in previous 

studies as graphoglyptids (Agrichnia), such as 

Protopaleodictyon and Squamodictyon, are 

reinterpreted here as wrinkle marks. Current 

depositional models for the Puncoviscana 

Formation envisage accumulation from turbidity 

currents in submarine fans. However, preliminary 

sedimentologic studies suggest a 

more complex paleoenvironmental situation, 

including not only deep-marine, flysch-type 

deposits, but also shallow-water settings affected 

by wave action. Within this framework, 

the Oldhamia association is interpreted as 

formed in deep water, while the Nereites association 

corresponds to shallow-marine environments. 

Nearly all the ichnofossils are oriented 

parallel to the bedding plane, displaying 

restriction to two-dimensional biotopes,and 

therefore they do not disturb the primary 

sedimentary fabric. Bedding plane trace fossils 

mostly reflect very shallow grazing by 

mobile, bilaterian metazoans. The only exception 

is Treptichnus, which represents a shallow 

infaunal, three-dimensional burrow system 

that records a feeding strategy of underground 

mining. Its presence reveals an early 

attempt of colonization of the infaunal ecospace 

during the early Phanerozoic. The Puncoviscana 

ichnofauna reflects, at least in part, 

lifestyles related to microbial mats that protected 

the sediment from erosion. The presence 

of wrinkled surfaces and palimpsest ripples 

suggests that stabilization by microbial 

binding was a major factor in Neoproterozoic 

to Early Cambrian ecosystems. Close association 

of the ichnogenus Oldhamia with these 

structures supports Seilacher's hypothesis that 

this icnotaxon records a feeding strategy of 

undermat mining. Grazing trails commonly 

are associated to microbial mats also. Behavioral 

patterns represented by several Oldhamia 

ichnospecies in deep Lower Cambrian deposits 

reflects that feeding strategies associated 

with microbial mats persisted in the deep sea 

after the agronomic revolution. This fact suggests 

a gradual closure of a taphonomic window 

during the Proterozoic-Cambrian transition 

and is consistent with the recognition of 

Ediacara-type body fossils in Cambrian strata. 

Presence of guided meanders (Nereites saltensis) 

in Cambrian shallow-water environments 

is consistent with the onshore-offshore model. 

Integration of ichnologic and isotopic data 

suggests a Vendian to Nemakit-Daldynian age 

for the Puncoviscana Formation. 

2007010022 

澳大利亚早侏罗世粪便化石及其古生物学 

意义 = Early Triassic coprolites from Australia 

and their palaeobiological significance. ( 英 

文 ). Northwood C. Palaeontology, 2005, 

48(1): 49-68 

Coprolites from the Arcadia Formation, 

Queensland, Australia, were studied in conjunction 

with the vertebrate fossil assemblages 

from two localities to maximize our understanding 

of the palaeoecology of these Early 

Triassic deposits. Criteria used by other researchers 

to identify the producers of coprolites 

were found to be of little value in the Arcadia 

Formation specimens. Using a combination 

of shape, biostratigraphic distribution, 

size and included remains some of the coprolites 

are attributed to basal archosauromorphs 

and fish whereas others could not be identified. 

8

Perhaps the most important attribute of the 

Arcadia coprolites is that they preserved rare 

organisms such as cyanobacteria, insects and 

other arthropods, and a diversity of fish. Estimates 

of the number of actinopterygians and 

dipnoans preserved in coprolites significantly 

increased relative abundance estimates based 

on skeletal elements alone. Although coprolites 

are an important source of palaeobiological 

information, this information is limited by 

our poor understanding of the taphonomic 

processes involved in the fossilization of faecal 

matter and by the near impossibility of 

assigning coprolites to specific producers. 

2007010023 

受古氧化和沉积控制的深海遗迹化石 : 波兰 

喀尔巴阡 Silesian 单元下白垩统暗复理石 

沉积作为例证 = Deep-sea trace fossils controlled 

by palaeo-oxygenation and deposition: 

an example from the Lower Cretaceous dark 

flysch deposits of the Silesian Unit, Carpathians, 

Poland. ( 英文 ). Uchman A. Fossils and 

Strata, 2004, (51): 39-57 

The associations differ from those of the 

Upper Cretaceous and Tertiary flysch deposits. 

The trace fossil association of the Upper Cieszyn 

Shale belongs to the Nereites ichnofacies, 

but the associations of the jother two 

units do not; therein the trace fossil diversity 

is distinctly lower, and graphoglyptids or horizontal 

meandering pascichnia are absent or 

very rare. These trace fossil associations supposedly 

changed as a result of general evolutionary 

processes that influenced deep-sea 

trace makers after the Early Cretaceous, and 

which intensified the aforementioned difference. 

2007010024 

显生宙早期潮间带生态系统重建 : 阿根廷西 

北部寒武纪 Campanario 组的遗迹学 = Reconstructing 

Early Phanerozoic intertidal ecosystems: 

ichnology of the Cambrian Campanario 

Formation in northwest Argentina. ( 英 

文 ). Mangano M G; Buatois L A. Fossils and 

Strata, 2004, (51): 17-38 

Campanario Formation is the middle unit 

of the upper Lower to Middle Cambrian 

Meson Group of northwest Argentina. This 

formation is interpreted as having accumulated 

in macrotidal shallow-marine environments 

with extensive tidal-flat areas flanked 

seawards by subtidal sandbar complexes. 

Shallow subtidal and intertidal sand-flat deposits 

are dominated by vertical domicitles of 

suspension feeders and passive predators of 

the Skolithos ichnofacies (Skolithos, Arenicolites, 

Diplocraterion). 

2007010025 

元古代末期 - 寒武纪早期生态系统 : 阿根廷 

西北部 Puncoviscana 组的遗迹学 = Terminal 

Proterozoic-Early Cambrian ecosystems: 

ichnology of the Puncoviscana Formation, 

northwest Argentina. ( 英文 ). Buatois L A; 

Mangano M G. Fossils and Strata, 2004, (51): 

1-16 

The Puncoviscana Formation consists of 

a thick, folded and slightly metamorphosed 

succession of sandstones, mudstones and conglomerates 

of terminal Proterozoic to earliest 

Cambrian age, representing the metasedimentary 

basement of northwest Argentina. The 

Puncoviscana ichnofauna is recorded in lowermost 

Cambrian strata and includes a wide 

variety of ichnotaxa, such as Archaeonassa 

fossulata, Circulichnis montanus, Cochlichnus 

anguineus.... Structures considered in previous 

studies as wrinkle marks and elephant skin 

textures. Vertical dwelling structures are absent. 

Nearly all the ichnolossils in the association 

are oriented paralled to the bedding plane, 

displaying restriction to two-dimensional biotopes, 

and therefore they do not disturb the 

primary sedimentary fabric. 

分子古生物学 

2007010026 

由线粒体基因变异推得的地中海鳐鱼动物 

群中新世至上新世快速扩散与演化 = Rapid 

Miocene–Pliocene dispersal and evolution of 

Mediterranean rajid fauna as inferred by mitochondrial 

gene variation. ( 英文 ). Valecchi E 

et al. Journal of Evolutionary Biology, 2005, 

18(): 436-446 

Rajidae (colloquially known as skates 

and rays) experienced multiple and parallel 

adaptive radiations allowing high species diversity 

and great differ-ences of species composition 

between regional faunas. Nevertheless, 

they show considerable conservation of 

bio-ecological, morphological and reproductive 

traits. The evolutionary history and 

dispersal of North-east Atlantic and Mediterranean 

rajid fauna were investigated throughout 

the sequence analysis of the control region 

and 16S rDNA mitochondrial genes. Molecular 

estimates of divergence times indicated 

recent origin and rapid dispersal of the present 

species. Compared with the ancient origin of 

the family (Late Cretaceous), the present spe- 

9

cies diversity arose in a relatively narrow 

time-window (12 Myr) from Middle Miocene 

to Early Pleistocene, likely by speciation 

processes related to dramatic geological and 

climatic events in the Mediterranean. Nucleotide 

substitution rates and phylogenetic relationships 

indicated Mediterranean endemic 

skates derived from sister species with wider 

distribution during Late Pliocene–Pleistocene. 

Skate phylogeny and system-atics obtained 

using mitochondrial gene variation were 

largely consistent with those based on morpho-anatomical 

data. 

2007010027 

陆生软体动物 (Gastropoda, Pulmonata, 

Arionidae)mtDNA 的高度分异 : 加速进 

化 , 异域趋异和二次接触 = Extreme 

mtDNA divergences in a terrestrial slug (Gastropoda, 

Pulmonata, Arionidae): accelerated 

evolution, allopatric divergence and secondary 

contact.. ( 英文 ). Princeel J; Jordaens K; 

Backeljau T. Journal of Evolutionary Biology, 

2005, 18(5): 1264-1258 

Extremely high levels of intraspecific 

mtDNA differences in pulmonate gastropods 

have been reported repeatedly and several hypotheses 

to explain them have been postulated. 

We studied the phylogeny and phylogeography 

of 51 populations (n = 843) of the highly 

polymorphic terrestrial slug Arion subfuscus 

(Draparnaud, 1805) across its native distribution 

range in Western Europe. By combining 

the analysis of single stranded conformation 

polymorphisms (SSCP) and nucleotide sequencing, 

we obtained individual sequence 

data for a fragment of the mitochondrial 16S 

rDNA and a fragment of the nuclear ITS1. 

Additionally, five polymorphic allozyme loci 

were scored. Based on the 16S rDNA phylogeny, 

five monophyletic haplotype groups with 

sequence divergences of 9–21% were found. 

Despite this deep mitochondrial divergence, 

the haplotype groups were not monophyletic 

for the nuclear ITS1 fragment and haplotype 

group-specific allozyme alleles were not 

found. Although there is evidence for an accelerated 

mtDNA clock, the divergence among 

the haplotype groups is older than the Pleistocene 

and their current allopatric ranges probably 

reflect allopatric divergence and glacial 

survival in separate refugia from which different 

post-glacial colonization routes were established. 

A range-overlap of two mtDNA 

groups (S1 and S2, 21% sequence divergence) 

stretched from Central France and Belgium up 

to the North of the British Isles. The nuclear 

data suggest that this secondary contact resulted 

in hybridization between the allopatrically 

diverged groups. Therefore, it seems that, 

at least for two of the groups, the deep 

mtDNA divergence was only partially accompanied 

by the formation of reproductive isolation. 

2007010028 

狸藻属植物的系统发生和高替代速率世系 

trnK 内含子的分子演化 = Phylogenetics of 

Utricularia (Lentibulariaceae) and molecular 

evolution of the trnK intron in a lineage with 

high substitutional rates. ( 英文 ). Müller K; 

Borsch T. Plant Systematics and Evolution, 

2005, 250(1-2): 39-67 

The bladderworts (Utricularia, Lentibulariaceae) 

are the most diverse carnivorous 

plant genus, with a nearly worldwide distribution. 

In the present study, chloroplast DNA 

sequences of the trnK intron were used to reconstruct 

phylogenetic relationships within the 

genus. Parsimony, likelihood, and Bayesian 

analyses resulted in highly congruent and 

well-resolved trees. The phylogenetic signal 

provided by the noncoding trnK intron partition 

of the dataset is similar to that of the 

matK coding region, although the latter is 

twice as long. Within matK, indels appeared in 

multiples of three except very close to the 3 

end of the gene. Substitutions were found to 

result in or eliminate stop codons, thus creating 

a length variable gene end. Indels in both 

trnK and matK exhibit low degrees of homoplasy, 

irrespective of their size. A tree based 

on indels alone is largely congruent to the substitution-based 

trees but less resolved. Three 

major clades found within Utricularia are 

classified as subgen. Utricularia, subgen. Bivalvia, 

and subgen. Polypompholyx. The immediate 

common ancestor of Utricularia is 

suggested to have been a terrestrial plant 

whereas epiphytic and aquatic habits evolved 

later in terminal clades. 

2007010029 

在星际气体中观察到的生命前分子 = The 

prebiotic molecules observed in the interstellar 

gas. ( 英文 ). Thaddeus P. Philosophical 

Transactions of the Royal Society B: Biological 

Sciences, 2006, 361(1474): prebiotic, interstellar 

molecules, radio astronomy 

Over 130 molecules have been identified 

in the interstellar gas and circumstellar shells, 

the largest among them is a carbon chain with 

13 atoms and molecular weight of 147 (twice 

10

that of the simplest amino acid glycine). The 

high reliability of astronomical identifications, 

as well as the fairly accurate quantitative 

analysis which can often be achieved, is emphasized. 

Glycine itself has been claimed, but 

a recent analysis indicates that few, if any, of 

the astronomical radio lines attributed to glycine 

are actually from that molecule. Polycyclic 

aromatic hydrocarbons (PAHs) have 

long been proposed as the source of the unidentified 

infrared bands between 3 and 16μm, 

but no single PAH has been identified in space, 

partly because PAHs generally have weak or 

non-existent radio spectra. A remarkable exception 

is the non-planar corannulene molecule 

(C 20 H 10 ) that has a strong radio spectrum; 

in the rich molecular cloud TMC-1, it is found 

that less than 10 −5 of the carbon is contained 

in this molecule, suggesting that PAHs are not 

the dominant large molecules in the interstellar 

gas, as has been claimed. Owing to inherent 

spectroscopic limitations, determining the 

structures of the large molecules in space may 

require capture of the dust grains, which are 

continually entering the outer Solar System. 

2007010030 

环境因素、花粉 / 胚珠比及种子库的持续性 

对植物分子进化速率的影响 = The influence 

of environmental factors, the pollen : ovule 

ratio and seed bank persistence on molecular 

evolutionary rates in plants. ( 英文 ). Whittle C 

A. Journal of Evolutionary Biology, 2006, 

19(1): 302-308 

One of the main goals of molecular evolutionary 

biology is to determine the factors 

that influence the evolutionary rate of selectively 

neutral DNA, but much remains unknown, 

especially for plants. Key factors that 

could alter the mutation rate include environmental 

tolerances (because they reflect a 

plants vulnerability to changes in habitat), the 

pollen : ovule ratio (as it is associated with the 

number of mitotic divisions) and seed longevity 

(because this influences the number of generations 

per unit time in plants). This is the 

first study to demonstrate that seed bank persistence 

and drought tolerance are positively 

associated with molecular evolutionary rates 

in plants and that pollen : ovule ratio, shade 

tolerance and salinity tolerance have no detectable 

relationship. The implications of the 

findings to our understanding of the impact of 

environmental agents, the number of cell divisions 

and cell aging on neutral DNA sequence 

evolution are discussed. 

古生态学 

2007010031 

阿根廷布宜诺斯艾利斯 Laguna Hinojales 

地区全新世水生孢型体 ( 藻类和疑源 

类 ): 古生态解释 = Holocene aquatic palynomorphs 

(algae and acritarchs) from Laguna 

Hinojales (Buenos Aires, Argentina): paleoecological 

interpretation. ( 其他 ). Borel C 

M; Guerstein G R; Prieto A R. 

Ameghiniana, 2003, 40(4): 531-544 

Holocene palynological samples from the 

Laguna Hinojales (37similar to 34' S; 

57degrees 27' W), southeastern Buenos Aires 

province, contain algae (Chlorophyta, Cyanophyta 

and Dinoflagellata) and acritarchs. The 

chlorophycean algae consist of cenobia of Pediastrum 

musterii Tell and Mataloni, P. boryantim 

(Turpin) Meneghini, and Scenedesmus 

sp., colonies of Botryococois braunii Mitzing, 

zygospores of Debarya madrasensis lyengar, 

Motigeotia laetenvirens (Braun) Wittrock, 

Moitgeotia sp., Zygnenia sp. and Spirogyra 

spp., and spores of Desmidiaceae. Cyanophycean 

sheets and akinetes of Gloeotrichia sp. 

are well preserved. The assemblages also contain 

freshwater dinoflagellates, represented by 

a peridinioid genus. Among the acritarchs, 

Cobricosphaeridium spp. reach highest percentages 

in the lowermost part of the core, 

where possibly freshwater algal spores are 

also present. These palynomorphs, produced 

by organisms from plankton and benthic 

communities, are used as indicators of nutrient, 

depth and salinity changes. Variable size and 

salinity of the water body are inferred from 

fluctuating frequencies of algae and acritarchs 

between ca. 4,500 - 2,100 C-14 yr B.P. From 

2,100 C-14 yr B.P, algal assemblages indicate 

a freshening of the water and a gradual transition 

to favourable trophic conditions in the 

shallow lake. Higher values of Pediastrum 

spp., Scenedesmus sp., and Zygnemataceae, 

along with low frequencies of Botryococcus 

braunii reflect elevated nutrient levels in a 

relatively shallow lake. The improvement of 

climatic conditions, especially an increase in 

average temperature, probably was responsible 

for the expansion of aquatic plants and 

natural eutrophication of the water environment. 

After 400 14C yr B.P. the spectrum 

suggests a shallow eutrophic lake. However, 

alternating intervals, less favourable for algae, 

reflect a reduction in the water body size, possibly 

related to periods of lower precipitation. 

11

2007010032 

日本西部沿岸沉积物中有毒 Gymnodinium 

catenatum Graham (Gymnodiniales, Dinophyceae) 

的出现 = Recent occurrence of toxic 

Gymnodinium catenatum Graham (Gymnodiniales, 

Dinophyceae) in coastal sediments of 

West Japan. ( 英文 ). Matsuoka K; Fujii 

R;Hayashi M; Wang Zhaohui. Paleontological 

Research, 2006, 10(2): 117-125 

In Japan, a paralytic shellfish poison 

(PSP) event caused by Gymnodinium catenatum 

Graham, a naked, colonial and PSP 

dinoflagellate, was first reported from Senzaki 

Bay, western part of the Sea of Japan in 1986. 

Since then, the geographical distribution of 

this species seems to have expanded through 

West Japan. To clarify the possibility of its 

migration being due to anthropogenic agency 

the historical occurrence of G. catenatum in 

Japanese coastal waters was examined; core 

sediments that preserve an historical record of 

this species were collected from several coastal 

areas where it had been observed. From the 

cores collected from Imari Bay, smaller spherical 

cysts ornamented with fine reticulated 

structure and with epicystal archeopyle are 

found which are probably different from Gymnodinium 

nolleri. Low cyst concentrations of G. 

catenatum in these cores may have resulted 

from such a characteristic physiological feature 

as chain formation of its vegetative form. The 

earliest occurrence of this species was recorded 

in sediment of Omura Bay dated to ca. 

1700 A.D. This fact strongly suggests that the 

occurrence of G. catenatum in Japan is natural 

and that it has not been artificially introduced 

from different areas. 

2007010033 

日本西南部大阪湾的底栖有孔虫组合 : 过 

去 50 年来的动物群变迁 = benthic foraminiferal 

assemblages in Osaka Bay, southwestern 

Japan: faunal changes over the last 50 

years. ( 英文 ). Tsujimoto A; Nomura R; Yasuhara 

M; Yoshikawa S. Paleontological Research, 

2006, 10(2): 141-161 

Live benthic foraminiferal assemblages 

from surface sediment in Osaka Bay collected 

in 1999 were analyzed to characterize the distribution 

of the modern foraminiferal assemblages. 

Foraminiferal assemblages were compared 

with those of previous studies to document 

environmental changes in Osaka Bay 

over the past 50 years. 

Sixty-one species of foraminifera belonging 

to 37 genera were recognized from the 

1999 surface sediment samples. An agglutinated 

assemblage containing Trochammina 

hadai and Eggerella advena is dominant in the 

inner part of the bay and is related to eutrophication. 

The foraminiferal assemblage in areas 

deeper than about 20 m is composed of 

Eggerella advena, Ammonia beccarii forma A, 

and Pseudorotalia gaimardii. This assemblage 

may be influenced by the large clockwise 

Okinose Circulation Current which extends 

throughout the western bay. 

Foraminiferal assemblages in Osaka Bay 

have changed dramatically during the last 50 

years. The Trochammina hadai-Eggerella 

advena assemblage became established in the 

inner part of the bay, reflecting eutrophication 

that progressed from the 1960s through the 

1970s. This assemblage became dominant in 

1983, and typically dominated the inner part 

of the bay. From 1983 to 1999, however, the 

abundance of taxa belonging to this assemblage 

decreased greatly following implementation 

of 1973 Osaka City bylaws that restricted 

wastewater discharge. Changes in 

benthic assemblages such as the decrease of 

Ammonia beccarii forma A and increase of 

Eggerella advena have occurred in response 

to decreased incidence of red tides, and floral 

change in the species that cause these tides. 

The results of this study demonstrate that the 

abundance and distribution of benthic foraminifers 

in Osaka Bay are intimately related 

to environmental changes related to the urbanization 

of coastal areas. 

2007010034 

分布区扩大过程中远距离种子传播对基因 

多样性的显著影响 = Contrasting effects of 

long distance seed dispersal on genetic diversity 

during range expansion. ( 英文 ). Bialozyt 

R; Ziegenhagen B; Petit R J. Journal of Evolutionary 

Biology, 2006, 19(1): 12 -20 

Currently many attempts are made to reconstruct 

the colonization history of plant species 

after the last ice age. A surprising finding 

is that during the colonization phase genetic 

diversity did not decrease as much as expected. 

In this paper we examine whether long distance 

seed dispersal events could play a role in 

the unexpected maintenance of genetic diversity 

during range expansion. This study is 

based on simulations carried out with a maternally 

inherited haploid locus using a cellular 

automaton. The simulations reveal a close relationship 

between the frequency of long distance 

seed dispersal events and the amount of 

genetic diversity preserved during colonization. 

In particular, when the colonized region 

12

is narrow, a complete loss of genetic diversity 

results from the occurrence of very rare long 

distance dispersal (LDD) events. We call this 

phenomenon the 'embolism effect'. However, 

slightly higher rates of LDD events reverse 

this effect, up to the point that diversity is better 

preserved than in a pure diffusion model. 

This phenomenon is linked to the reorganization 

of the genetic structure during colonization 

and is called the 'reshuffling effect'. 

微体古生物学 

综论 

2007010035 

南极乔治王岛冰川漂砾中的寒武纪微体化 

石 = Cambrian microfossils from glacial erratics 

of King George Island, Antarctica. ( 英文 ). 

Wrona R. Acta palaeontologica Polonica, 

2004, 49(1): 13-56 

Limestone erratics in the Early Miocene 

glacio-marine Cape Melville Formation of 

King George Island, Antarctica, have yielded 

Early and Middle Cambrian small skeletal 

fossils (SSF) accompanied by calcified cyanobacteria, 

archaeocyath and spiculate sponges, 

trilobites and echinoderms. The SSF assemblage 

comprises disarticulated sclerites of 

chancelloriids, halkieriids, tommotiids, lapworthellids, 

palaeoscolecids, hyolithelminths, 

lingulate brachiopods, helcionelloid molluscs, 

hyoliths, and bradoriids. All 24 described species 

are common to Antarctica and Australia. 

Most are recorded here from Antarctica for the 

first time, including Shetlandia multiplicata 

gen. et sp. nov. and two new species Byronia 

bifida and Hadimopanella staurata. The 

lithological and fossil contents of the boulders 

are almost identical with autochthonous assemblages 

from the Shackleton Limestone in 

the Argentina Range and Transantarctic 

Mountains. Cambrian outcrops around the 

Weddell Sea are a plausible source of the erratics. 

The fauna is closely similar to that from 

the uppermost Botomian Wilkawillina Limestone 

in the Flinders Ranges and Parara Limestone 

on Yorke Peninsula, and Toyonian Wirrealpa 

and Aroona Creek Limestones in the 

Flinders Ranges, as well as the Ramsay Limestone 

on Yorke Peninsula, all in the Arrowie 

and Stansbury Basins of South Australia. 

These very similar faunal and facies successions 

for Antarctica and Australia strongly 

support their common biotic and sedimentary 

evolution on the same margin of a greater 

Gondwana supercontinent throughout the 

Early Cambrian. 

2007010036 

华南新元古代可能源于动物的球形微体化 

石 -- 硅化和磷酸盐化的 Tianzhushania = 

Silicified and phosphatized Tianzhushania, 

spheroidal microfossils of possible animal 

origin from the Neoproterozoic of south 

China.. ( 英文 ). Yin-Chongyu; Bengtson S; 

Yue-Zhao. Acta palaeontologica Polonica, 

2004, 49(1): 1-12 

Comparative study of microfossils from 

two kinds of sediments: chert intercalations 

(studied in thin section) and phosphorite/phosphatic 

carbonate (in thin section 

and maceration), from the upper Neoproterozoic 

Doushantuo phosphorites in the Weng'an 

area, Guizhou Province, South China, shows 

that the phosphatized Megasphaera ornata 

and the chert-preserved Tianzhushania tuberifera 

should be regarded as representing 

the same taxon preserved by different mineralization 

processes. In phosphatized specimens 

the outer wall is often peeled off, exposing 

the ornamented middle wall. Some phosphatized 

specimens isolated from the rock 

matrix and specimens seen in thin sections of 

phosphorites show a partly preserved outer 

wall with spines, which can be compared to 

the thin-sectioned specimens from the chert 

beds. The small pits usually seen on the surface 

of the ornamented middle wall of phosphatized 

specimens correspond to the attachment 

spots of the spines in the outer wall. The 

presence of a spiny outer wall is a characteristic 

of Tianzhushania Yin and Li, 1978. 

Tianzhushania ornata (Xiao and Knoll, 2000) 

comb. nov. is here proposed as the valid name 

for the species. The proposed resting-egg nature 

of T. ornata, mainly based on the ornament 

type of the middle wall, cannot be excluded. 

The presence of a spiny outer wall, 

however, suggests that it is a pelagic rather 

than a benthic form. 

孢粉 

2007010037 

北极巴罗地区 300 年以来的孢粉记录及其 

气候变化 = Pollen record and climatic change 

in Barrow, alaska during the past 300 years. 

( 中文 ). 李春海 ; 唐领余 ; 童国榜 ; 张青松 ; 王国 . 

微体古生物学报 , 2004, 21(1): 53-57 

根据北极巴罗地区 Elson 泻湖 300 年以 

来的孢粉记录 , 揭示出小冰期以来的该地 

区植被的生态变化和气候变化 , 相对温暖 

期分别出现在公元 1720 年、1800 年、1922 

年、1953 年和 1992 年以后 , 结果和其他研 

究成果是比较一致的。孢粉总浓度的变化 

13

和生态变化相对应 , 孢粉总浓度可以作为 

北极巴罗地区温度变化替代性指标。温度 

升降是北极地区植被覆盖率变化的主要原 

因。20 世纪人类已经对北极地区植被产生 

重要影响。 

2007010038 

英国威尔士西南部下老红砂岩淡水西组早 

泥盆世洛霍考夫期微植物群 = An Early Devonian 

(Lochkovian) microflora from the 

Freshwater West Formation, Lower Old Red 

Sandstone, southwest Wales. ( 英文 ). Higgs K 

T. Geological Journal, 2004, 39(3/4): 359-374 

The Lower Old Red Sandstone deposits 

occurring to the south of the Ritec Fault on the 

Pembroke Peninsula in southwest Wales are 

very poorly age-constrained. Two moderately 

well-preserved spore assemblages have been 

recovered from the Freshwater West Formation, 

locally the highest division of the Milford 

Haven Group. These assemblages contain 

both cryptospores and trilete spores, with the 

latter group being dominant. They essentially 

represent a single microflora which is assigned 

to the middle part of the Emphanisporites 

micrornatus-Streelispora newportensis 

(MN) Spore Zone and is considered to be of 

Early Devonian (mid-Lochkovian) age. A new 

cryptospore species Qualisaspora sinuata and 

a new trilete spore species Dictyotriletes williamsii 

are described. The microflora is correlated 

with similar assemblages from the Dittonian 

of the main Anglo-Welsh Basin. Locally, 

the new biostratigraphic data constrain the age 

of the rich ichnofauna of the Freshwater West 

Formation and also date the influx of coarse 

clastic sediments into the basin following the 

sedimentary quiescence represented by the 

underlying Chapel Point Calcrete 

2007010039 

西伯利亚西部侏罗纪植物微体化石的热变 

质作用 = Thermal alteration of Jurassic volga 

plant microfossiles of westhern Siberia. ( 中 

文 ). Lidiya V R; Tatiana N S. 古生物学 

报 , 2003, 42(1): 8-12 

研究了西伯利亚西部几个地点钻孔侏 

罗纪岩芯样中的植物微体化石。在有关组 

合中 ,Lycopodium sp., Coniopteris spp. 和 

Gleicheniidites sp. 的孢子少 ,Klukiasporites 

sp. 极少 ; 代表性花为有 Pinus exilioides, P. 

disulgaus, Sciadopites sp. 和 Classopollis; 微 

体浮游植物占优势 , 例如 Crassisphaera sp., 

Tasmanites sp., Pterospermopsis eurypteris. P. 

harti 和 Cymatiosphaera sp. 颇丰富 , 有时出 

现 Pareodinia sp. 和 Trichodinium sp.。虽然 

各个组合中孢子、花粉、微体浮游植物在 

含量上有变化 , 但总的组成在西伯利亚西 

部不同地区尚稳定 , 此等微化石的颜色或 

有变化 , 它们 ( 特别是微体浮游植物 ) 可 

用来检测沉积有机质受热变质的成熟度级 

别。 

2007010040 

杜鹃花科吊钟花属花粉形态及其分类学意 

义 = Pollen morphology of Enkianthus (Ericaceae) 

and its taxonomic significance. ( 英文 ). 

Ahmed G S; Hideki T. Grana, 2006, 45(3): 

161-174 

Pollen morphology of ten Enkianthus 

species was examined using light (LM) and 

scanning electron microscopy (SEM) and previous 

infrageneric classification of Enkianthus 

was discussed in the light of the palynological 

characters obtained in this study. The pollen 

grains are monads, oblate spheroidal to prolate 

in shape and 3 ‐ to 5‐colpor(oid)ate. Exine 

sculpture varies from granulate to coarsely 

rugulate‐psilate with faint to distinct minute 

granules in SEM. Infraspecific geographical 

differences in palynological characters were 

found in E. deflexus. The species of Enkianthus 

are clearly differentiated into two pollen 

morphological groups that correspond to the 

sections Enkiantella + Meisteria and Andromedina 

+ Enkianthus , respectively. The 

members of the sections Enkiantella and 

Meisteria have pollen grains typically with 

three apertures, prolate spheroidal to prolate, 

ratio of colpus length to polar axis (L/P) 0.69- 

0.84, relatively thinner exine and exine sculpturing 

tendency to granulate, character states 

that are probably plesiomorphic in this genus. 

The members of the sections Andromedina 

and Enkianthus have more derived pollen 

grains with four to five apertures, commonly 

oblate spheroidal, L/P 0.56-0.63, relatively 

thicker exine and exine sculpturing tendency 

to coarsely rugulate‐psilate. It seems to be 

difficult to differentiate between sections of 

the same group on the basis of palynological 

characters only. Adding the palynological 

characters to the infrageneric framework of 

Anderberg indicates an evolutionary trend in 

exine sculpture within Enkianthus from finely 

verrucate‐rugulate through coarsely rugulate 

to coarsely rugulate‐psilate. A dichotomous 

key for Enkianthus was prepared based on the 

palynological characters. 

14

2007010041 

西班牙和意大利气候变化对悬铃木传粉的 

影响 = The influence of climate changes in 

Platanus spp. pollination in Spain and Italy. 

( 英文 ). Emma T; F Javier R‐R; Rosanna C; 

Victoria J; Giuseppe F. Grana, 2006, 45(3): 

222-229 

There is evidence of a significant increase 

in air temperature in the northern hemisphere 

over recent decades, with consequent 

changes for anemophilous pollen. In this work 

we present the effects of climatic change on 

Platanus spp. pollination in different areas of 

Italy and Spain, characterized by different 

climates. In particular, the historical series of 

pollen monitoring and meteorological data of 

two Italian stations, Perugia (1982 - 2003) and 

Torino (1985 - 2003), and two Spanish stations, 

Santiago de Compostela (1992 - 2003) 

and Vigo (1994 - 2003), were analysed. The 

changes recorded in all stations included the 

timing and behaviour of pollen release. However, 

no or minimal influence on the total pollen 

emission was found. Research has linked 

the changes in phenological events to an increase 

in temperature, moreover in this study 

temperature changes are believed to be mainly 

responsible for the variations recorded in the 

pollen season of Platanus . A previous start of 

pollination (−0.66; −1.21; days/year) is reported 

in both Italian stations where the temperatures 

have significantly increased and a 

delay of 0.2 - 0.8 days/year in Spanish stations 

where a different trend of temperature is recorded. 

Other important data is given regarding 

the type of discharge of pollen grains during 

the pollen season. Pollination curves are 

examined by two statistical shape parameters 

(kurtosis and skewness) which show that pollen 

release is more gradual with higher temperatures 

or faster under colder conditions. A 

regression analysis links the atmospheric pollen 

presence to mean air temperature. 

2007010042 

苏格兰海湖 ( 峡湾 ) 流域及表层沉积物的 

表土花粉 = Modern pollen from the catchment 

and surficial sediments of a Scottish sea 

loch (fjord). ( 英文 ). Peter C; William A; 

Sarah D. Grana, 2006, 45(3): 230-238 

Modern pollen was extracted both from 

moss polster samples collected from a range 

of sites across the land surface of the Loch 

Sunart catchment, north‐west Scotland and 

from a number of marine sediment‐water 

interface sites in the sea loch. Comparisons 

between the pollen results and the major vegetation 

types growing in the catchment area 

revealed that in general the moss polsters contained 

a localised picture of the vegetation 

whilst the sea loch sediments varied much less 

from sample to sample and better represented 

a regional picture of the vegetation. It was 

anticipated that the pollen in the sea loch samples 

would be in a much poorer state of preservation 

because of the many pathways 

through which it travels in order to become 

incorporated into the sediments of the loch. 

However, this proved not to be the case and 

the study demonstrates that marine sediments 

of the kind found in Loch Sunart have the potential 

to provide a new source of Holocene 

vegetation data which is as good as the freshwater 

lake sediments that have been preferentially 

sampled in the past. 

2007010043 

“ 指示曲线 ” 及其在恢复陆相古环境中的应 

用 = “Index curve”,its application in terrestrial 

paleoenvironment interpretation. ( 中文 ). 刘耕 

武 . 微体古生物学报 , 2003, 20(4): 439-443 

在一定条件下 , 选择一些能够反映一定 

古环境的指示性化石类型 , 对其百分含量经 

过简单的算术运算 , 就可以绘制出一条能够 

反映一定环境变化的曲线 , 即指示曲线。它 

的优点是直接利用资料、计算方法简单 , 因 

此在制作曲线时减少了可能形成新的误差 

的因素。结果直观、可靠 , 能够比较准确地 

进行半定量的环境解释。它的缺点是应用 

范围局限 , 只有在满足沉积连续 , 化石丰富 

和足够的采样精度的条件下、选择出正确 

的指示分子 , 得出的结论才是可靠的。 

2007010044 

阿根廷凤尾蕨科孢子形态和孢子壁超微结 

构 = Spore morphology and sporoderm ultrastructure 

in Adiantopsis Fée (Pteridaceae‐ 

Pteridophyta) from Argentina. ( 英文 ). 

Raquel P; Gabriela G; Marta M. Grana, 2006, 

45(2): 101-108 

The aim of this study is to analyse, describe 

and compare the spores of the two Adiantopsis 

species that grow in Argentina, A. 

chlorophylla (Sw.) Fée and A. radiata (L.) Fée. 

The study used herbarium material observed 

with light microscopy (LM), scanning electron 

microscopes (SEM) and transmission electron 

microscopes (TEM). The spores of both species 

are trilete with an echinate surface. The 

exospore is smooth, two‐layered in section; 

both layers with different thickness and contrast. 

Depending on the plane of sectioning, 

15

channels are seen running through the exospore 

and in the apertural region. The perispore 

strongly contrasted when seen with TEM, 

is two‐layered and bears ornamentation. The 

two layers have different thickness and structure. 

The inner layer P1 is the thickest layer 

and has three strata, which form the sculptural 

elements. The outer layer P2 covers all the 

surfaces of P1. Two levels of ornamentation 

are clearly distinguished: a basal level composed 

of fused ridges, and an upper level 

composed of echinae. The spores of A. 

chlorophylla are triangular‐globose in polar 

view, with convex sides, 25 - 50 µm in equatorial 

diameter and have more ornamental 

processes per surface unit than the spores of A. 

radiata. The spores of A. radiata are triangular 

in polar view and 30 - 40 µm in equatorial 

diameter. Size and ornamentation help to establish 

differences at species level, and together 

with the exomorphological characteristics 

of the sporophyte, contribute to the systematics 

of this genus. 

2007010045 

希腊空气致敏真菌孢子和气象因子关系的 

预报可行性分析 = Airborne allergenic fungal 

spores and meteorological factors in Greece: 

Forecasting possibilities. ( 英文 ). Athanasios 

D; Dimitrios G. Grana, 2006, 45(2): 122-129 

Specific airborne fungal spore types trigger 

respiratory allergy symptoms in sensitive 

individuals. Aiming to reduce the risk for allergic 

patients, we constructed predictive 

models for the fungal spore circulation in 

Thessaloniki, Greece. Monthly and daily autoregressive 

forecasting models were developed 

(Dynamic Regression) for the airborne spore 

concentrations of Alternaria and Cladosporium 

, the most abundant fungal taxa in the 

area. The forecast horizons were respectively 

12 months and one week. The accuracy of 

each predictive model was tested by means of 

six statistical criteria. Special attention was 

paid to the lag effect of all factors, both meteorological 

and fungal spore records. Aerobiological 

sampling was conducted over 1996- 

2002, using a Burkard trap. Records of 18 meteorological 

parameters were used for the 

same period. Residual analyses tested the adequacy 

of the models. Monthly forecasting 

models were highly significant, with adjusted 

R 2 = 0.68 for Alternaria , and 0.81 for 

Cladosporium . The respective values of adjusted 

R 2 for the daily models were 0.62 and 

0.70. Cladosporium spore counts were consistently 

influenced by solar radiation, whereas 

Alternaria was influenced by air temperature 

(mean and minimum). For monthly forecasts, 

records of the preceding month, and the 12 

month spore record was significant for Alternaria 

, whereas for Cladosporium , the lags 

were 12 and 24 months. With the daily models, 

the respective required periods were mainly 

the preceding one to two weeks and the last 

two years for both fungal taxa, in addition to a 

one‐year lag in the case of Cladosporium . 

Daily models could be further improved by 

co‐estimating interdiurnal variability and 

fungal spore sources. 

2007010046 

克罗地亚萨格勒布市 2002-2005 年间空气 

中的禾本科花粉 = Poaceae pollen in the atmosphere 

of Zagreb (Croatia), 2002 - 2005. 

( 英文 ). Renata P; Lidija S; Josip Č; Ivana H; 

Predrag H. Grana, 2006, 45(2): 130-136 

Pollen of grasses (Poaceae) is one of the 

most important airborne allergen sources 

worldwide. The aim of the study was to determine 

diurnal, day‐to‐day, weekly, 

monthly and annual pollen variation, and the 

effect of selected meteorological parameters 

on atmospheric pollen concentrations in Zagreb. 

A preliminary study was carried out during 

four seasons (2002 - 2005), using a 

7‐day VPPS 2000 Hirst volumetric pollen 

trap. Total annual grass pollen concentrations 

in Zagreb were constant (2 673 - 3 074 p.g.m 

−3 ), with a relative drop in 2004 (1 196 p.g.m 

−3 ). The beginning of the grass pollen season 

is usually observed when the average daily 

temperature exceeds 13.5°C (max. daily temp. 

19.5°C), without precipitation. In all four 

study years the absolute peak of concentrations 

occurs in the second half of May. The 

length of pollen season during the study period 

was 157 - 173 days. A high variability 

was observed in the maximal concentration 

and in the number of days when grass pollen 

concentration exceeded the threshold value of 

30 p.g.m −3 (9 - 40 days). Statistically significant 

correlations were found between airborne 

grass pollen concentrations and air temperature, 

level of precipitation and relative humidity. 

2007010047 

西班牙加那利群岛耶罗岛不同蜂蜜中的花 

粉和感官特征 = Pollen and sensorial characterization 

of different honeys from El Hierro 

(Canary Islands). ( 英文 ). Irene L‐S R; Car- 

men G F. Grana, 2006, 45(2): 146-159 

16

The pollen content of 31 honey samples 

from 19 different apiaries of El Hierro (Canary 

Islands) were subject to qualitative and 

quantitative melissopalynological analysis. 

The quantitative analysis demonstrated that 

13% of the honey belonged to Maurizio Class 

I ( Erica arborea L.), two of Chamaecytisus 

proliferus (L. f.) Link‐type (“tagasaste”), one 

of Fabaceae (Genisteae sp.) and one of Lamiaceae 

Origanum vulgare L. ssp. virens 

(Hoffmanns. & Link) Ietsw. ‐type (thyme: 

Micromeria hyssopifolia Webb & Berthel.). 

Honeydew elements were practically absent. 

Sixty‐nine pollen types were identified be- 

longing to 42 families. The number of pollen 

types range between 18 and 39 (mean of 

27.42). Foeniculum vulgare Mill. ‐type pol- 

len is present in all the samples. Galactites 

tomentosa Moench‐type, Echium plantagi- 

neum L., Echium L. sp., Bituminaria bituminosa 

(L.) C. H. Stirt., Chamaecytisus proliferus 

‐type and Origanum vulgare ssp. 

virens ‐type pollen were found in 96.8% of 

the samples. The sensorial analysis indicated 

that honey types are generally of good quality, 

because 62% were evaluated as very high 

(16%), high (23%), and good (23%). 

2007010048 

夹竹桃科山橙属 (Melodinus) 单体和四合 

体花粉 = Pollen of Melodinus (Apocynaceae): 

Monads and tetrads. ( 英文 ). Erik A. van de 

Ven; Raymond W. J. M. van der Ham. 

Grana, 2006, 45(1): 1 - 8 

Melodinus pollen has been studied by 

light, scanning electron and transmission electron 

microscopy. The pollen grains are usually 

colporate, medium-sized monads, and their 

shape varies from suboblate to oblate spheroidal. 

They are mostly 3-aperturate, while four 

species have pollen with both three and four 

apertures, and one species has exclusively 4- 

aperturate pollen. The ecto- and endoapertures 

show large size ranges. Melodinus coriaceus 

has its pollen in tetrahedral tetrads, while M. 

orientalis is polymorphic as to dispersal unit 

(mostly tetrads, sometimes monads). The 

monotypic genus Craspidospermum, which is 

the closest known relative of Melodinus, has 

its pollen also in tetrads, but these are very 

different (non-tetrahedral, irregularly pantoporate). 

On the basis of pollen morphology, it is 

hypothesised that tetrads evolved independently 

in Melodinus and Craspidospermum。 

2007010049 

日本缩叶藓属 (Ptychomitrium) 四种苔藓 

孢子的超微结构 = Ultrastructure of the spore 

in four Japanese species of Ptychomitrium 

Fürnr. (Musci). ( 英文 ). Belén E; Tomio Y; 

Hironori D. Grana, 2006, 45(1): 61-70 

The ultrastructure of the mature spore in 

four Japanese species of the acrocarpous moss 

genus Ptychomitrium is presented. In all species 

the spores have a similar pattern: there is 

no recognisable aperture nor sporoderm polarity, 

exine and perine are poorly developed, 

cytoplasm only occasionally shows polarity, 

and plastids have a well developed inner 

membrane system. The presence of frequent 

intine protrusions is a remarkable feature of 

this genus. A multilaminar structure of the 

exine, already observed in Grimmia , occurs 

also in these species although here it is less 

pronounced. The significance of these features 

is discussed within these species, as well as in 

comparison to other taxa, especially the genus 

Grimmia . 

2007010050 

尼日利亚恩苏卡 (Nsukka) 地区的空气孢 

粉 = Airborne pollen grains in Nsukka, Nigeria. 

( 英文 ). Reginald Chukwuemeka N. 

Grana, 2006, 45(1): 73-80 

A study of the airborne pollen grains in 

Nsukka, Nigeria, has been carried out at two 

different sampling heights (1.8 m and 15 m) 

from February 1993 to January 1994. Twentysix 

plant families (40 genera) were identified 

at the lower sampling height, whilst thirtyeight 

families (58 genera) were identified at 

the height of 15 m. A total of nine and eighteen 

fern spore types were observed at 1.80 m 

and 15 m, respectively. The quantitative results 

indicate that the number of pollen observed 

at 15 m sampling height was statistically 

different (Casuarina equisetifolia, 

Milicia excelsa, Elaeis guineensis, Celtis integrifolia, 

Alchornea cordifolia , Amaranthaceae/Chenopodiaceae, 

Combretaceae/Melastomataceae, 

Nephrolepis biserrata, 

Thelypteris totta, and Dryopteris spp. 

2007010051 

基于分子和形态系统发育分析推论被子植 

物花粉早期演化 = Early evolution of angiosperm 

pollen as inferred from molecular and 

morphological phylogenetic analyses. ( 英文 ). 

James D. Grana, 2005, 44(4): 227-251 

Phylogenetic analyses of molecular and 

morphological data, revised in this study, shed 

17

light on long-standing controversies on the 

early evolution of angiosperm pollen. Although 

relationships between angiosperms and 

other seed plants remain uncertain, the robust 

rooting of the angiosperms among the 

“ANITA” groups ( Amborella , Nymphaeales, 

Illiciales, Trimenia , and Austrobaileya ) clarifies 

their original pollen morphology. Contrary 

to the view that the first angiosperms had 

boat-shaped monosulcate pollen with granular 

or atectate exine structure, the ANITA rooting 

implies that globose monosulcate pollen with 

more or less columellar structure and a continuous 

tectum was ancestral and a foveolatereticulate 

tectum arose soon after. The oldest 

recognized Cretaceous angiosperm pollen may 

represent the latter grade of evolution. Structure 

described as granular evolved independently 

from columellar within Nymphaeales, 

Magnoliales, and Laurales. In Magnoliales, 

columellar Myristicaceae and Magnoliaceae 

diverge below Degeneria , Galbulimima , 

Eupomatia , and Annonaceae, which shifted to 

granular structure. Granular monosulcate pollen 

was ancestral in Annonaceae but gave rise 

to columellar monosulcates and permanent 

tetrads. In Laurales, reduction and granularization 

culminated in the fragile exines of Lauraceae. 

Although absence of a distinctly staining 

endexine in Magnoliales has been considered 

evidence that the laminated endexine of 

gymnosperms was lost before the origin of 

angiosperms, presence of a thin endexine now 

appears to be ancestral. These results refute 

the view that granular structure supports a 

relationship between angiosperms and 

Gnetales, Bennettitales, and Pentoxylon . Relationships 

with groups with alveolar exines 

(e.g., Caytonia , glossopterids) and/or reticulate-columellar 

Triassic Crinopolles pollen 

now seem equally likely. 

2007010052 

阿根廷朱布特省 Andean Patagonia 地区的 

蜂蜜花粉的特征 = Palynological characterization 

of honeys from the Andean Patagonia 

(Chubut, Argentina). ( 英文 ). Forcone A; Ayestarán 

G; Kutschker A; García J. Grana, 2005, 

44(3): 202-208 

The pollen content of 58 honey samples 

of Apis mellifera L. from the Andean region 

of Chubut (Argentinian Patagonia) was analyzed. 

The samples were provided by beekeepers 

between 1999 and 2004. Eighty-eight 

pollen types were identified, 30 of them are 

not reported in Argentinian honeys. Identified 

types belong to 47 families, of which the most 

diverse were Asteraceae (15 pollen types), 

Fabaceae (13 pollen types), and Rosaceae 

(four pollen types). From the samples analyzed, 

47% were monofloral and corresponded 

to the following taxa: Trifolium spp. (16%), 

Rosaceae (10%), Aristotelia chilensis (Molina) 

Stuntz (7%), Discaria-Colletia (5%), Escallonia 

spp. (3%), Schinus patagonica (Phil.) I. 

M. Johnst. (2%), Phacelia secunda J. F. Gmel. 

(2%), Myrtaceae (2%). The results of this 

study show a high level of utilization of native 

flora by Apis mellifera . Four new types of 

monofloral honey were recognized: Aristotelia 

chilensis , Discaria-Colletia , Phacelia 

secunda , and Schinus patagonica . The high 

representation of native flora distinguishes 

these honeys geographically. 

2007010053 

印度马哈拉施特拉邦地区的蜂蜜花粉 = 

Pollen of Apis honey from Maharashtra. ( 英 

文 ). Bhusari N V; Mate D M; Makde K H. 

Grana, 2005, 44(3): 216-224 

Melissopalynological investigations are 

important in establishing an apiary industry. 

Pollen analyses of the nectar sources of Apis 

florea Fabr. from the Saoner region indicate 

the importance of this region for commercial 

bee keeping enterprises. Twenty seven samples 

were collected during winter season in the 

months of October 1997 to January 1998 and 

November 1998 to January 1999. In addition, 

245 pollen loads were analyzed from 19 honey 

combs collected from the same region. Pollen 

grains were identified from reference slides. 

Of the 27 honey samples, 17 samples were 

unifloral and ten multifloral. A total of 39 pollen 

types were classified into 21 families. In 

the analyses of the 245 pollen loads Lagascea 

mollis Cav. was dominant in 57 pollen loads 

and Parthenium hysterophorus L. in 55 pollen 

loads. Weeds such as Parthenium hysterophorus 

, Sphaeranthus indicus L., Lagascea mollis 

, Bidens pilosa L. and Justicia procumbens 

L. were the common sources of nectar and 

pollen for Apis florea in the region. Agricultural 

tracts of the Saoner region in the Nagpur 

District have a good potential for sustaining 

beekeeping ventures because of the diversity 

of nectar and pollen taxa. 

2007010054 

凤梨科 (Bromeliaceae) 小孢子和花药的 

发育 = Microsporogenesis and anther development 

in Bromeliaceae. ( 英文 ). Sajo M G; 

Furness C; Prychid C; Rudall P. Grana, 2005, 

44(2): 65-74 

18

Bromeliaceae possess several features of 

pollen and anther wall development that are 

plesiomorphic for Poales, consistent with their 

putatively basal or near-basal placement in 

this order. For example, successive microsporogenesis 

and the monocotyledonous type 

of anther wall formation are both plesiomorphic 

features that occur commonly in other 

Poales, with a few notable exceptions, notably 

the simultaneous type of microsporogenesis in 

Rapateaceae. The intermediate type of 

tapetum development in Bromeliaceae was 

probably derived secondarily from a secretory 

type, which occurs in most other Poales except 

Typhaceae. 

2007010055 

菊科帚菊木族 (Mutisieae) 中罕见的三沟 

花粉 = The unusual occurrence of tricolpate 

pollen within Mutisieae (Asteraceae). ( 英文 ). 

Tellería M C; Katinas L. Grana, 2005, 44(2): 

91-97 

The monotypic genus Hecastocleis and 

species of Ainsliaea DC. (Asteraceae, Mutisieae) 

have tricolpate pollen, which is unusual 

in Asteraceae. The pollen morphology 

of H. shockleyi and species of Ainsliaea were 

studied with light microscope and scanning 

electron microscope. Pollen of H. shockleyi 

and some species of Ainsliaea have tricolpate 

aperture but differ in size and exine features. 

The pollen of Ainsliaea is bigger than that of 

Hecastocleis , and has more conspicuous microspines, 

a Mutisia - or an Ainsliaea - exine 

type, and is slightly thickened at the poles. 

The pollen of H. shockleyi is scabratemicroechinate 

with small puncta, and has the 

Mutisia -exine type, which is regularly thickened 

over the complete grain. The occurrence 

of tricolpate pollen supports previous studies 

that Hecastocleis and Ainsliaea stand apart 

from other genera of Mutisieae, but the occurrence 

of Mutisia -exine type does not suggest 

complete independence of the tribe. 

2007010056 

油橄榄 (Olea europaea) 花粉产量和果实产 

量之间的关系 = Relationship between pollen 

emission and fruit production in olive ( Olea 

europaea L.). ( 英文 ). Orlandi F; Romano B; 

Fornaciari M. Grana, 2005, 44(2): 98-103 

Aerobiological data of pollen emission 

concentrations is used to predict fruit production. 

The principal aim of this work was to 

study the relationship between pollen emission 

patterns, emission homogeneity and fruit production 

in olive ( Olea europaea L.). Data of 

daily pollen concentrations in the atmosphere 

during the flowering period, collected over a 

20-year period in Perugia (Central Italy), and 

the corresponding fruit production data were 

analysed. Correlation and regression analyses 

on the partial pollen amounts (subdivisions of 

the whole flowering period), their statistical 

variability (expressed as coefficients of variation 

of the daily pollen concentration), and the 

production values in the different years demonstrate 

that pollen emission, during the seven 

to ten day period immediately preceding the 

maximum pollen emission day, appears to be 

most closely related to fruit production. Moreover, 

the pollen emission homogeneity (minimal 

variability in daily pollen concentrations) 

during the “critical” flowering period is very 

important for fertilization. 

2007010057 

卡塔赫纳地区预报日产花粉浓度的多元回 

归模型 = Multiple regression models for predicting 

total daily pollen concentration in 

Cartagena. ( 英文 ). Angosto J M; Moreno- 

Grau S; Bayo J; Elvira-Rendueles B. 

Grana, 2005, 44(2): 108-114 

The use of meteorological autocorrelation 

variables and pollen concentrations from 

previous days, coupled with classification of 

meteorological data according to multivariate 

analysis techniques, is shown to improve the 

predictive power of multiple regression models 

for daily pollen forecasts. This paper presents 

an investigation of the meteorological 

and autocorrelation variables which influence 

pollen counts in Cartagena, from 1995 to 1999, 

as a basis for the development of predictive 

models. The analysis of total pollen concentrations, 

and especially Chenopodiaceae- 

Amaranthaceae, was determined. Initially, 

forecasting models for total pollen counts 

were developed, using data from 1995 to 1998, 

and autocorrelation and meteorological variables. 

Secondly, predictive models were developed 

for different meteorological situations, 

which improved the results by decreasing the 

number of predictive parameters. Finally, data 

from 1999 were used to validate the predictive 

models. 

2007010058 

阿根廷 Caldén 区南部西方蜜蜂 (Apis mellifera 

L.) 所采集花粉的植物源及其蛋白质 

含量 = Pollen collected by honey bees ( Apis 

mellifera L.) from south of Caldén district 

(Argentina): botanical origin and protein con- 

19

tent. ( 英文 ). Andrada A C; Tellería M C. 

Grana, 2005, 44(2): 115-122 

In the south of the Caldén district (Phytogeographical 

province of Espinal, Argentina) 

the availability of flowering along with the 

botanical origin and protein content of pollen 

harvested by honey bees, was studied. During 

two apiculture periods (from end August to 

early January) pollen loads were collected 

every fortnight using pollen traps. A total of 

637.96 g of pollen loads was analysed. From 

139 species recorded, only 29 were visited by 

honey bees. In terms of biomass the contribution 

of exotic plants was high at the end of the 

winter (Brassicaceae and Erodium cicutarium 

); during this period of pollen shortage, 

honey bees collected spores of Puccinia interveniens 

. During the spring, the native plants 

( Condalia microphylla , Chuquiraga erinacea , 

Discaria americana , Grindelia tehuelches , 

Larrea divaricata , Prosopis sp., Prosopidastrum 

globosum and Vicia pampicola ) were 

utilised. Those pollen types of high protein 

level were collected most intensively. 

2007010059 

印度那格浦尔市粮店中的气传青霉菌属 

(Penicillium) 孢子 = Airborne Penicillium 

in the grain shops of Nagpur (India). ( 英文 ). 

Sawane A M; Saoji A A. Grana, 2005, 44(2): 

123-128 

The airborne Penicillium spp. and total 

airborne fungal spore concentration was investigated 

in the grain shops of Nagpur city, India, 

using a volumetric Hi-Air sampler system 

Mark II (Hi Media Laboratories Ltd., India). 

The mycotoxins were analysed from the Penicillium 

isolates obtained from the seeds by 

thin layer chromatography. The mean concentration 

of the total fungi isolated from different 

grain shops ranged from 7.8×10 2 to 

1.1×10 3 CFU/m 3 . The mean concentration 

of Penicillium isolated from the air of grain 

shops ranged from 8.6×10 1 CFU/m 3 (10.8%) 

to 1.7×10 2 CFU/m 3 (19.9%). Among the 13 

species of Penicillium which were isolated, P. 

citrinum Thom was the most prevalent species 

(24.2%), followed by P. oxalicum Currie & 

Thom (16.5), P. digitatum Saccardo (8.9%), P. 

janthinellum Biourge (8.7%), P. funiculosum 

Thom (8.3%), P. chrysogenum Thom (6.4%), 

P. purpurogenum Stoll (6.2%), P. brevicompactum 

Dierckx (4.8%), P. frequentans Westling 

(4.2%), P. italicum Wehmer (3.8%), P. 

rubrum Stoll (3.4%), P. expansum Link (2.9%) 

and P. cyclopium Westling (1.6%). Penicillium 

species were also isolated from seeds 

such as wheat, maize, soybean, and groundnut. 

The mycotoxins roquefortin C, citrinin, rubratoxin 

B, cyclopiazonic acid, verrucosidin, mitorubrinic 

acid and two unknown metabolites 

were isolated from Penicillium isolates. 

2007010060 

Basmati 栽培籼稻 (Oryza sativa race Indica) 

花粉外壁表面的超微结构 = Pollen morphology 

of Basmati cultivars (Oryza sativa 

race Indica) - exine surface ultrastructure. ( 英 

文 ). Kalyani D; Mithilesh C. Grana, 2004, 

43(2): 89-93 

Pollen morphological studies using LM 

and SEM have been carried out on six cultivars 

of Basmati - a variety of cultivated species 

Oryza sativa race Indica. SEM study at a 

magnification of ×20,000 revealed distinct 

variations in pollen exine surface patterns, in 

relation to the arrangements of fine surface 

excrescences (spinules or granules) and their 

clustering patterns forming small areas or insulae. 

Three distinctly different insular patterns 

occur in cultivars Basmati-370, Karnal 

local and Type-9. Cultivar Bakul Joha is characterized 

by free spinules. Mixed type i.e. 

both free and fused excrescences were observed 

in cultivars Bengali Joha and Bhog 

Maniki but they can be differentiated on the 

basis of the dimensions of the excrescences. 

2007010061 

西班牙西北部 Vigo 地区橄榄树气传花粉对 

预报花粉季节开始和日常浓度的研究 = 

Airborne olive pollen in Vigo (Northwest 

Spain): a survey to forecast the onset and daily 

concentrations of the pollen season. ( 英文 ). F 

Javier R-R; Nuria D; Victoria J. Grana, 2004, 

43(2): 101-110 

Temperature is one of the main factors 

affecting the start of flowering in tree species 

that flower at the beginning of spring. Knowledge 

of the chilling and heat needs required by 

plants to overcome the period of dormancy 

enables us to determine the onset of pollination, 

which is of great importance to allergy 

sufferers. This study attempted to obtain behaviour 

models with a view to determining 

both the onset of the olive pollen season and 

daily pollen concentrations during the pollination 

period in Vigo. Monitoring was carried 

out using a Lanzoni VPPS 2000 pollen trap, 

from 1995 to 2002 inclusive. 

20

2007010062 

沙特阿拉伯一沙漠环境乡村的空气灵芝担 

孢子研究 = Airborne Ganoderma basidiospores 

in a country with desert environment. 

( 英文 ). Syed M H; Abdulrahman A-F; Fatima 

K; Sultan A-S. Grana, 2004, 43(2): 111-115 

Aerobiological studies to identify Ganoderma 

basidiospores were conducted using 

Burkard Volumetric 7-Day Recording Sampler 

(Burkard Manufacturing Co. Ltd., England) 

at three separate cities in Saudi Arabia. 

At one site, Jizan, close to the coast of Red 

Sea, up to 17% of all basidiospores counted 

were identified as Ganoderma spp. while less 

than 1% Ganoderma spp. were identified at 

the two non-coastal sites. A clear seasonal 

pattern from late autumn to early summer (October-March) 

with a peak in December was 

recorded at Jizan and the maximum concentration 

of Ganoderma basidiospores reached 

1.9×10 3 m -3 in December followed by 1.2×10 3 

m -3 in January. The diurnal pattern of Ganoderma 

spore concentrations, when averaged 

over the year had late-evening maxima (a nocturnal 

pattern). However, other sites that 

showed low concentrations of Ganoderma 

basidiospores did not exhibit any peak or a 

high maximal level. The study demonstrates 

that even in a desert environment, airborne 

activities of Ganoderma basidiospores can be 

recorded. The impact of Ganoderma on asthmatic 

patients, particularly in such environments, 

needs to be investigated. 

2007010063 

希腊不同单花种蜂蜜的孢粉学特征 = Palynological 

characteristics of different unifloral 

honeys from Greece. ( 英文 ). Angeliki T; 

Maria P-K; Olga S. Grana, 2004, 43(2): 122- 

128 

Three hundred and twenty-nine Greek 

honey samples of different botanical and geographical 

origin were collected and examined 

by organoleptic evaluation, melissopalynological 

analysis, measurement of electrical 

conductivity and colour. The results showed 

that 208 samples were unifloral with 178 of 

them representing the main types of unifloral 

honey produced in Greece; that is fir, pine, 

chestnut, cotton, orange and thyme honey. All 

honeys had the sensory characteristics typical 

of their origin and complied with the electrical 

conductivity standards set by Council Directive 

2001/110/EC. 

2007010064 

阿根廷布宜诺斯艾利斯布兰卡港湾 del 

Medio 水道全新世孢粉 = Palynology from 

the Holocene of Canal del Medio, Bahia 

Blanca estuary, Buenos Aires, Argentina. ( 其 

他 ). Borel C M; Gomez E A. 

Ameghiniana, 2006, 43(2): 399-412 

Holocene palynological samples from the 

Canal del Medio (38 degrees 49 degrees S; 62 

degrees 17' W), Bahia Blanca inner estuary, 

south of Buenos Aires province, contain pollen, 

spores, remains of algae (Dinoflagellata, 

Chlorophyta and Cyanophyta) and acritarchs. 

The pollen spectra are dominated by Chenopodiineae 

and Poaceae, along with Asteraceae 

and Ephedra. The dinophycean algae are represented 

by cysts of estuarine dinoflagellates 

of the order Gonyaulacales (Operculodinium 

centrocarpum (Deflandre and Cookson) Wall, 

Spiniferites bulloideus (Deflandre and Cookson) 

Sarjeant, S. sp. cf. S. pachydermis (Rossignol) 

Reid, S. bentorii (Rossignol) Wall and 

Dale and S. ramosus (Ehrenberg) Loeblich 

and Loeblich). The chlorophycean algae consist 

of cenobia of Pediastrum boryanum 

(Turpin) Meneghini and colonies of Botryococcus 

braunii Kutzing. The assemblages also 

contain sheets of Gloeotrichia sp. The acritarchs 

are represented by Micrhystridium sp., 

Cymatiosphaera sp., Halodinium minus Bujak, 

Acritarch sp. F, Acritarch sp. G and Acritarch 

sp. H. Three palynological zones are distinguished 

in the sequence. The lowermost zone, 

dated in 3,500 C-14 yr B.P., represents an ancient 

tidal plain in close relation with a channel 

of turbid water and variable energy. The 

intermediate zone suggests better conditions 

for the development of autotrophic dinoflagellates, 

in a restricted estuarine environment. 

For the top zone, the low frequencies of dinocysts 

and acritarchs indicate similar conditions 

to those currently present in the inner Bahia 

Blanca estuary. Along the profile, the pollen 

reflects the development in the surrounding 

areas of halophytic communities, with the 

presence of xerophytic woodland. The characteristics 

of these deposits indicate that ca. 

3,500 C-14 yr B.P., the mean sea level was 

located at a similar position than the current 

one. 

2007010065 

被子植物三沟 - 三孔沟花粉内折的主要模 

式 = Principal modes of infoldings in tricolp(or)ate 

Angiosperm pollen. ( 英文 ). Hei- 

21

demarie H; Michael H. Grana, 2004, 43(1): 1- 

14 

Angiosperm pollen grains can absorb or 

release water quickly. The respective degree 

of hydration has great influence upon the actual 

pollen grain shape and is, to a certain extent, 

reversible (harmomegathic effect). In the 

hydrated condition the majority of pollen 

grains are usually spherical, but in the dry 

condition they are infolded in a highly variable 

manner. This paper demonstrates many 

kinds of infolding within dicotyledonous tricolp(or)ate 

pollen from several angiosperm 

families. In most cases the foldings are directionally 

oriented, but it is only possible to predict 

the final form in dry condition to a limited 

degree. 

2007010066 

洋二仙草科根乃拉草属 (Gunnera) 的花 

粉形态新认识 = New insights into the pollen 

morphology of the genus Gunnera (Gunneraceae). 

( 英文 ). Livia W; Joseph P; Elisabeth 

G. Grana, 2004, 43(1): 15-21 

Pollen grains from ten species of Gunnera, 

chosen to represent the six different 

subgenera in the genus, were examined using 

light and scanning electron microscopy. The 

aim of the study was to explore characters that 

have the potential to define different types of 

pollen within Gunnera and to study the evolution 

of these characters in light of the phylogeny 

of the genus. According to our results, 

there are three main types of pollen in the examined 

species of Gunnera. Type 1, unique 

for the South American species G. herteri 

(subgenus Ostenigunnera), is characterised by 

an imperfect reticulum with sinuous undulating-creasted 

muri. A reticulum with equidimensional 

polygonal lumina is typical for the 

plesiomorphic type of pollen (type 2) present 

in subgenera Gunnera, Misandra and Panke. 

Lastly, pollen grains of subgenera Pseudogunnera 

and Milligania are characterised by 

a reticulum with lumina of variable shape and 

size (type 3). In G. macrophylla (subgenus 

Pseudogunnera), the lumina in the apocolpia 

are of a different shape and size from the 

lumina in the mesocolpia (type 3a), while in G. 

dentata, G. monoica and G. cordifolia (subgenus 

Milligania), the lumina are identical in the 

apocolpium and the mesocolpium (type 3b). 

2007010067 

地中海四种栎属植物的花粉生物学 = Pollen 

biology in four Mediterranean Quercus species. 

( 英文 ). María Teresa G-C; Pablo H; 

Herminia G-M; Eugenio D; Carmen G. 

Grana, 2004, 43(1): 22-30 

Potential pollen production, viability and 

germination were studied in the most important 

species of Quercus in the mountains of 

Córdoba to determine the contribution of each 

species to the total amount of airborne pollen. 

The results were compared over two consecutive 

years with different rainfall patterns. The 

viability of pollen grains was determined at 

anther opening, and during the pollination 

period, in order to determine potential pollination 

capacity. Results indicated that there were 

differences in the number of pollen grains 

produced by stamen in the four species. 

Equally, there were differences in the number 

of flowers among the species, being Q. suber 

the species with higher number of catkins 

groups and flowers per individual tree. Total 

pollen production per tree can be summarized 

in the following proportion: 1: 3: 3: 6 (Q. coccifera, 

Q. ilex ssp. ballota, Q. faginea and Q. 

suber). Potential pollen viability was estimated 

using the Fluorochromatic Reaction 

(FCR) and a germination assay. The results 

have shown that Quercus potential pollen viability 

is high and declines slowly with time. 

Q. coccifera was the species with the highest 

percentage of germination, with Q. suber being 

the lowest. 

2007010068 

西班牙东北部加泰罗尼亚省 (Catalonia) 犹 

大墙草 (Parietaria judaica L.) 生物气候学 

及其花粉产量 = Phenology and pollen production 

of Parietaria judaica L. in Catalonia 

(NE Spain). ( 英文 ). Roser G; Jordina B. 

Grana, 2004, 43(1): 57-64 

Variability of phenology and pollen production 

of three geographically distant (20-60 

km) populations of Parietaria judaica L. in 

Catalonia (Spain) was analysed together with 

their relationships to airborne pollen dynamic 

curves. Parietaria judaica L. is a perennial 

herb, with individual plants consisting of 

many shoots emerging from a common rootstock, 

most of them flowering copiously in 

Spring. Flowers are hermaphrodite or female, 

and pollination is anemophilous. From November 

1999 to October 2000 pollen production 

was estimated from periodical records in 

three permanent plots per zone. Moreover, 

records of airborne Urticaceae pollen were 

obtained daily by means of Hirst spore traps 

operating in each zone. 

22

2007010069 

阿根廷圣胡安省 Volcan 山脉泥盆纪 

Chigua 组和石炭纪 Maliman 组孢粉第一 

部分 : 古微浮游植物、无壁腔光滑和具纹 

饰孢子 = Palynology of the Chigua (Devonian) 

and Maliman (Carboniferous) formations 

in the Volcan Range, San Juan Province, 

Argentina. Part 1. Paleomicroplankton and 

acavate smooth and ornamented spores. ( 英 

文 ). Amenabar C R; Di Pasquo M; Carrizo H 

A; Azcuy C L. Ameghiniana, 2006, 43(2): 

339-375 

Palynological analysis of the Chigua and 

Maliman formations of Devonian and Early 

Carboniferous age respectively, cropping out 

in the Rio Blanco Basin, northwestern Argentina, 

has yielded diverse paleomicroplanktonspore 

assemblages. In this first part, 35 species 

of paleomicroplankton and 68 species of acavate 

spores from both formations are illustrated. 

Two new species are proposed: Apiculiretusispora 

laxa from the Devonian, and 

Aistulatisporites malimanensis from the Early 

Carboniferous. Two new combinations are 

proposed: the spore species Apiculatisporis 

castanea (Butterworth and Williams) nov. 

comb., and the paleomicroplankton species, 

Dictyotidium munificum (Wicander and Wood) 

nov. comb., based on the discussion of the 

main characters of the genera Dictyotidium, 

Muraticavea, Polyedryxium and Cymatiosphaera. 

The genus Quadrisporites Hennelly 

ex Potonie and Lele is emended. Twelve 

species are first recorded in the Devonian of 

South America, such as Pulvinosphaeridium 

trifidum Kiryanov, Dictyotidium granulatum 

Playford in Playford and Dring, Dictyotidium 

venulosum (Playford) Colbath, Orygmahapsis 

pachydemia Colbath, Polyedryxiton leptum 

Turner, Leiotriletes trivialis Naumova, Granulatisporites 

muninensis Allen, Dibolisporites 

varius Tiwari and Schaarschmidt. Other spore 

species are first recorded in the Lower Carboniferous 

of South America, amongst them 

are cited Grantilatisporites triconvexus Staplin, 

Pustidatisporites papillosus (Knox) Potonite 

and Kremp, Verrucosisporites microtuberosus 

(Loose) Smith and Butterworth, 

Dibolisporites medaensis (Playford) Playford, 

Anapiculatisporites ampullaceus (Hacquebard) 

Playford, Lophotriletes severus Playford and 

Satterthwait, Raistrickia gemmifera Playford 

and Satterthwait and Convolutispora tuberculata 

(Waltz) Hoffmeister, Staplin and Malloy. 

Previous worldwide geographic and stratigraphic 

records of the species studied herein 

are charted, while those corresponding to 

South America are cited in the text. 

2007010070 

阿根廷科尔多瓦下二叠统 Tasa Cuna 组孢 

粉 : 系统分类和生物地层意义 = Palynology 

of the Tasa Cuna Formation (Lower Permian), 

Cordoba, Argentina: Systematics and biostratigraphic 

considerations. ( 其他 ). Balarino 

M L; Gutierrez P R. Ameghiniana, 2006, 

43(2): 437-460 

A palynological association belonging to 

the Tasa Cuna Formation, northwest of Cordoba 

Province, Paganzo Basin, is described. 

This assemblage is referred to the Pakhapites 

fusus-Vittatina subsaccata Biozone, Early 

Permian, and it is correlated with the Cristatisporites 

Biozone, Chacoparana Basin. The 

ocurrences of Striatopodocarpites communis 

(Wilson) Hart, Vittatina sp. cf. V. fasciolata 

(Balme and Hennelly) Bharadwaj, V. subsaccata 

Samoilovich emend. Jansonius, Vittatina 

sp. cf. V. vittifera (Luber) Samoilovich, Hamiapollenites 

sp. cf. H. bullaeformis 

(Samoilovich) Jansonius, H.fusiformis 

Marques-Toigo emend. Archangelsky and 

Gamerro, Pakhapites fusus (Bose and Kar) 

Menendez, Lunatisporites sp. cf. L. variesectus 

Archangelsky and Gamerro, and Scheuringipollenites 

medius (Burjack) Dias-Fabricio, 

support the inclusion of this palynological 

association in the Early Permian. Some species 

such as Hamiapollenites sp. cf. H. bullaeformis 

(Samoilovich) Jansonius, Striatopodocarpites 

sp. cf. S. crassits Singh, S. sp. cf. S. 

rants (Bharadwaj and Salujha) Balme, S. 

communis (Wilson) Hart, and Protohaploxypinus 

hagii Foster, are identified in Argentina 

for the first time. This assemblage would represent 

a community related to lacustrine paleoenvironment 

characterized by abundant 

Lycophytes and influenced by a gymnospermic 

community (particularly Coniferales 

and Cordaitales) that, in spite of having mesoxerophytic 

requirements, would have been 

developed close to a fresh water body, where 

the assemblage was deposited. 

2007010071 

阿根廷巴塔哥尼亚北部早侏罗世 Nestares 

组的孢粉地层和古环境 : 第一部分陆相种 

= Palynostratigraphy and paleoenvironments 

of Early Jurassic strata (Nestares Formation) 

in northern Patagonia, Argentina. Part 1. Terrestrial 

species. ( 英文 ). Zavattieri A M; 

23

Volkheimer W. Ameghiniana, 2003, 40(4): 

545-558 

A palynologic analysis is presented of the 

Early Jurassic Nestares Formation at its type 

locality, on both sides of the Limay river, 

Alicura dam, at Neuquen and Rio Negro provinces 

boundary, northern Patagonia, Argentina. 

In this first part the terrestrial species (spores 

and pollen grains) of the microflora are listed, 

illustrated and, in some cases, commented on. 

The geologic context is reviewed and different 

paleoenvironmental interpretations, one as a 

paralic sequence and another as an anastomosing 

fluvial system, both based on earlier sedimentologic 

studies, are considered. The microflora 

is compared with the known record of 

the megaflora and the botanical affinities of 

the components of the microflora are proposed. 

Thirty nine of the species of miospores illustrated 

and listed are recorded for the first time 

in the Early Jurassic of Argentina. The terrestrial 

taxonomic diversity is represented by 48 

species of Bryophyte/Pteridophyte spores and 

23 species of Gymnospermous pollen grains, 

versus five species of Pteridophytes and 17 

Gymnosperm species known from the the 

megaflora; thus the microfloristic biodiversity 

record is larger than the megafloristic one. 

2007010072 

智利第十区 Calafquen 湖 Licen Ray 地区 

上三叠统 Panguipulli 组微体植物群 = Microflora 

of the Panguipulli Formation (Upper 

Triassic) at Licen Ray, Lake Calafquen, 10th 

Region, Chile. ( 法文 ). Zavattieri A M; Herbst 

R; Bravo J M. Ameghiniana, 2003, 40(4): 

585-600 

Triassic continental sedimentary sequences 

from several localities of central 

Chile were sampled for palynological study A 

moderately well preserved continental assemblage 

in one sample from Panguipulli Formation, 

at Lican Ray, north of Lake Calafquen 

(39degrees 30' S - 72degrees 12' W), 

10degrees Region of Chile is recorded. The 

sequence represents a deltaic-lacustrine environment 

of deposition. The Panguipulli assemblage 

is composed of 17 species of bryophytic 

and pteridophytic spores assigned to 

the genera Apiculatisporis, Aratrisporites, 

Baculatisporites, Cacheutasporites, Calamospora, 

Deltoidospora, Dictyophyllidites, 

Gleicheniidites, Neoraistrickia, Osmundacidites, 

Punctatisporites and Rogalskaisporites 

representing almost 17% of the total assemblage. 

Diverse gimnospermous pollen grains 

dominate the microflora with 81.9% including 

26 species of the genera Accinctisporites, 

Alisporites, Chordasporites, Cuneatisporites, 

Cycadopites, Equisetosporites, Falcisporites, 

Goubinispora, Inaperturopollenites, Klausipollenites, 

Lunatisporites, Minutosaccus, 

Platysaccus, Podocarpidites, Protodiploxypinus, 

Sulcatisporites, Sulcosaccispora and 

Vesicaspora. The microflora is associated 

with a megaflora composed of species of the 

genera Dicroidium, Cladophlebis, Gleichenites, 

Linguifolium, Pseudoctenis and 

Sphenobaiera, among others. This microfloristic 

assemblage differs partially from the 

only other Triassic microflora previously recorded 

in Chile from the Llafquentue-Huimpil 

Formation. Comparison with Argentine and 

other Gondwanic microfloras, favours an early 

Late Triassic age for the Paguipulli Formation 

which corresponds to the Ipswich Microflora 

of the gondwanic microfloristic provinces. 

Therefore, the Panguipulli microflora represents 

floral communities of temperate to 

warm-temperate climate, highly seasonal, 

points to a local and moistly environment. 

2007010073 

巴西圣保罗巴拉那盆地 Itaporanga 地区上 

石炭统 Itarare 亚群孢粉第一部分孢子和 

古浮游植物系统分类 = Palynology from the 

Upper Carboniferous Itarare Subgroup at Itaporanga, 

Parana Basin, Sao Paulo, Brasil. Part 

one: spores and palaeophytoplankton systematics. 

( 其他 ). Di Pasquo M; Azcuy C L; 

Souza P A. Ameghiniana, 2003, 40(3): 277- 

296 

Four palyniferous core levels from the 

IG-01 borehole at Itaporanga were analysed. 

This section belongs to the middle-upper part 

of the Itarare Subgroup. The systematic analysis 

of 33 miospore species identified comprise: 

Thirty trilete spores and three paleophytoplankton 

species including Deusilites 

tenuistriatus Gutierrez et al., Botryococcus 

braunii Kutzing and Brazilea scissa (Balme 

and Hennelly) Foster. A new spore species, 

Apiculatisporis variornatus, is described. 

Seven species of spores are identified for the 

first time in the Parana Basin: Retusotriletes 

aufractus Menendez and Azcuy Cyclogranisporites 

firmus Jones and Truswell, Apiculatasporites 

parviapiculatus Azcuy, Dibolisporites 

disfacies Jones and Truswell, Convolutispora 

muriornata Menendez, Cristatisporites 

stellatus (Azcuy) Gutierrez and Limarino 

and Kraeuselisporites volkheimerii Azcuy. 

The diagnosis of the genus Velamisporites 

Bharadwaj and Venkatachala is extended and 

24

one species is newly combined: Velamisporites 

australiensis (Playford and Helby). 

2007010074 

巴西圣保罗巴拉那盆地 Itaporanga 地区上 

石炭统 Itarare 亚群孢粉第二部分 : 花粉 

系统分类、古环境和地层意义 = Palynology 

from the Upper Carboniferous Itarare Subgroup 

at Itaporanga, Parana Basin, Sao Paulo 

State, Brazil. Part two: Pollen systematics and 

palaeoenvironmental and stratigraphic significance. 

( 其他 ). Di Pasquo M; Azcuy C 

L;Souza P A. Ameghiniana, 2003, 40(3): 297- 

313 

Systematic descriptions of 25 pollen 

grains from four core levels of the IG-01 

borehole are presented to complete the whole 

assemblage with those described in part one. 

This section belongs to the middle-upper part 

of the Itarare Subgroup. The species included 

herein comprise: seventeen monosaccate pollen 

(one striate), six bisaccate pollen (two striate), 

one praecolpate pollen and one colpate. 

Circumplicatipollis plicatus Ottone and Azcuy 

is identified for the first time in the Parana 

Basin. Previous paleontological information 

from this well including marine bivalves and 

brachiopods, is taken into account together 

with the palynological composition, botanical 

affinities, palynofacies and lithology, and a 

hypothesis of the palaeoenvironment / paleoclimatic 

conditions of depocentre is proposed. 

Initial estuarine conditions are registered at 

the 76 m level. A restricted coastal lagoon 

with a seasonal temperate climate corresponds 

to the 54 m level. The last episode, interpreted 

as a low energy and normal salinity shelf setting, 

is recognized at the 37 m and 36,5 m levels. 

Therefore, a relative rise in sea-level in 

this middle-upper section of the Itarare Subgroup 

is recognizable, and may correlate with 

glacial retreat. The palynological assemblage 

is datable as very Late Carboniferous based on 

previous records of selected miospore species. 

2007010075 

大戟科叶下珠亚科自饭树亚族 

(Flueggeinae) 的花粉形态 = Pollen morphology 

of the Flueggeinae (Euphorbiaceae, 

Phyllanthoideae). ( 英文 ). Vernie S; Raymond 

V D H. Grana, 2003, 42(4): 193-219 

A total of 129 species from the subtribe 

Flueggeinae of the tribe Phyllantheae (Euphorbiaceae, 

Phyllanthoideae) were investigated 

using light and scanning electron microscopy, 

and 10 species using transmission 

electron microscopy, in order to evaluate the 

relationships between the eight constituent 

genera: Breynia, Flueggea, Glochidion, Margaritaria, 

Phyllanthus, Reverchonia, 

Richeriella, and Sauropus. Of these genera, 

Flueggea, Margaritaria and Richeriella share 

pollen with a prolate spheroidal meridional 

outline and a 3-colporate aperture system. Pollen 

of Reverchonia is also 3-colporate, but 

differs from that of the Flueggea alliance by 

its clearly prolate shape, tilioid ornamentation 

and absence of costae endopori. Breynia and 

Sauropus have 4-12 and 3-16-colporate pollen, 

respectively, with diploporate colpi. Two pollen 

types are recognised in Breynia, and four 

in Sauropus, one of which supports the recognition 

of Sect. Hemisauropus. Glochidion pollen 

is 3-6-colporate, and similar to that of 

Breynia in having reticulate sculpture with Y- 

shaped sexine structures, but it has monoporate 

colpi. Of the genus Phyllanthus, only species 

with pollen with diploporate colpi have 

been studied. Seven types are described. Diploporate 

Phyllanthus pollen can be distinguished 

from that of Breynia and Sauropus by 

its distinct colpus margins consisting of parallel 

muri. Colpal irregularities and endoaperture 

configurations in the subtribe are discussed, 

and pollen morphological trends are 

hypothesised. Placed in the successiform aperture 

series, the Flueggea alliance and Reverchonia 

form a basal group. Glochidion is considered 

intermediate, giving rise to the 

Breynia-Sauropus group. The relationship 

with Phyllanthus remains unclear. 

2007010076 

西班牙南部不同地点空气中油橄榄 (Olea 

europaea L.) 花粉分析 = Aerobiological 

analysis of Olea europaea L. pollen in different 

localities of southern Spain. ( 英文 ). 

Francisca A; Maria D M T; Carmen G; Luis R; 

Silvia S; Consuelo D d l G. Grana, 2003, 

42(4): 234-243 

Pollen from olive trees (Olea europaea 

L.) is one of the main airborne allergens of the 

Mediterranean region. We have performed a 

comparative analysis of the behaviour of Olea 

pollen in the atmosphere at different localities 

in southern Spain with different biogeographic 

and climatic characteristics. Sampling over 

several years with Burkard or Lanzoni volumetric 

collectors was performed in the four 

cities of Córdoba, Jaén, Málaga and Granada. 

The pollen season spans primarily April to 

June, with the heaviest concentrations in May 

and peak days registering: 3890 grains/m 3 

25

(Córdoba), 6730 grains/m 3 (Jaén), 2819 

grains/m 3 (Málaga), and 1884 grains/m 3 (Granada). 

These quantities make these cities 

prime centres of seasonal allergic rhinitis and 

bronchial asthma. The main pollen season was 

defined taking the days registering 95% of the 

total annual pollen, and by studying the fluctuations 

between years and seasons in terms of 

Olea pollen at the different sampling points. 

Correlation analysis showed that the pollen 

concentrations on the preceding days, as well 

as the average accumulated temperature, were 

the parameters that invariably had significant 

correlation indices at all sampling points. In 

addition, the forecast models indicated that 

these two variables, together with others, predicted 

a high percentage (up to 80% in Jaén) 

of the seasonality of this pollen observed in 

the atmosphere of the different localities studied. 

2007010077 

气温对欧洲南部栎属植物花粉传粉起始日 

期的影响 = The influence of air temperature 

on the starting date of Quercus pollination in 

the South of Europe. ( 英文 ). F. Javier R-R; 

Giuseppe F; Victoria J. Grana, 2003, 42(3): 

145-152 

In order to overcome the dormancy period 

Perugia requires 1110 Chilling Hours 

(CH)-884 Growth Degree-Days (GDD°C) and 

Vigo 709 CH-861 GDD°C. With the Ashcroft 

method Perugia needs 1075 CH-1000 GDD°C 

and Vigo 625 CH-1512 GDD°C. Heat accumulation 

from the end of winter dormancy to 

the onset of pollination, showed the highest 

significance when mean temperature in Perugia 

and maximum temperature in Vigo were 

used. Every year we have found that the 

colder station needed a lower heat accumulation: 

Perugia required a higher quantity of 

chilling and heat than Vigo. However, the correlation 

detected between temperature and 

flowering was, on average, less significant 

that those found in the same regions for other 

arboreal taxa that present winter pollination 

(e.g. Corylus, Alnus). This preliminary study 

suggests that there is an effect of air temperature 

on Quercus pollination, but other environmental 

factors, such as photoperiod, hours 

of light, rainfall, relative humidity, may be of 

great influence in determining the onset of 

pollination in plants with a spring flowering. 

2007010078 

禾本科植物花粉的产量 = Pollen production 

in the Poaceae family. ( 英文 ). José P-B; Pablo 

H; Eugenio D; Carmen G. Grana, 2003, 42(3): 

153-159 

Total pollen production per inflorescence 

was studied in the most important species of 

the Poaceae family in the city of Córdoba in 

order to further our knowledge of the partial 

contribution of each species of this family to 

the total amount of pollen released into the 

atmosphere. 

The contribution of grasses in a given 

area was estimated by counting the number of 

inflorescences in an area of one square meter. 

Four different representative areas of the city 

were selected. The number of pollen grains 

per anther and flowers per inflorescence was 

also estimated in order to obtain total pollen 

production per inflorescence. Pollen production 

per inflorescence ranged from 14,500 to 

more than 22,000,000 pollen grains, the 

amount being clearly higher in the perennial 

species. Pollen production per square meter 

was higher in the mountains near the city and 

lower in areas of abandoned crops. Only a few 

species are responsible for the majority of pollen 

produced. A phenological study is necessary 

in order to determine the temporal distribution 

of this pollen production and subsequent 

shedding. 

2007010079 

阿根廷马德普拉塔市空气花粉日间变化比 

较 = Comparison of diurnal variation of airborne 

pollen in Mar del Plata (Argentina). ( 英 

文 ). Claudio P; JesÚs G; Marta P. 

Grana, 2003, 42(3): 161-167 

Intradiurnal variation of arboreal pollen 

(AP) in Mar del Plata city is compared during 

three non - consecutive years of survey and 

described in relation to the associated weather. 

The daily pattern of pollen abundance has a 

maximum between 10:00 and 12:00 h, while a 

minimum occurs at 18:00 h. The first two 

years of survey showed homogeneous daily 

trends, but in 1995 the maximum and minimum 

concentrations were delayed because of 

the change in position of the collecting station. 

Arboreal pollen spectrum presented qualitative 

and quantitative changes in the three years 

analysed. Results indicate optimal conditions 

for diurnal dispersion of arboreal pollen are 

high temperatures and low relative humidity. 

Also interaction between source position and 

wind direction has important effects on the 

timing of the peaks of some pollen types. 

26

2007010080 

印度德里市空气花粉浓度的变化 = Changes 

in airborne pollen concentrations in Delhi, 

India. ( 英文 ). Terlika P; Pushpa D; Anand S. 

Grana, 2003, 42(3): 168-177 

In order to find the qualitative and quantitative 

changes in airborne pollen concentrations 

in Delhi metropolis area an aerobiological 

survey was undertaken from September 

1990 to August 1997. Air samples were collected 

daily using a Rotorod Aeroallergen 

Sampler at 10 m above the ground level. 

Ninety-four pollen types were recorded and 

the major contributors include Morus, Cannabis, 

Chenopod/Amaranth, Prosopis, Artemisia, 

and Eucalyptus. Ten pollen types contributed 

90% of the total pollen load. Two major pollen 

seasons were recorded each year (February-April 

and September-November), although 

pollen grains in low frequency were 

recorded throughout the whole year. A significant 

reduction in pollen concentration was 

observed in subsequent years. The number of 

Morus, Cannabis, Prosopis, and Artemisia 

pollen decreased considerably while the number 

of Ricinus communis pollen did not show 

any considerable change during the study period. 

It is suggested that the reduction in pollen 

numbers from 1990 to 1997 in Delhi is due 

to massive clearing of vegetation for developmental 

activities of the city. 

2007010081 

澳大利亚、葡萄牙和西班牙不同桉树蜂蜜 

中的花粉差别 = Palynological differences in 

the pollen content of Eucalyptus honey from 

Australia, Portugal and Spain. ( 英文 ). José M; 

María C S; María J A. Grana, 2003, 42(3): 

183-190 

A melissopalynological study was carried 

out on 75 samples of Eucalyptus honey from 

different countries (22 from Australia, 13 from 

Portugal and 40 from Northwest Spain), in 

which a total of 145 different pollen types 

were identified. Of such, only Eucalyptus, 

Acacia, Brassica, Echium, Ligustrum, Plantago, 

Rumex, Taraxacum, Trifolium and Vicia 

pollen are present in the honeys from all three 

countries. 

Among the most abundant pollen types in 

Australian honeys, those belonging to the following 

families stand out: Myrtaceae (Angophora 

and Melaleuca), Fabaceae, Asteraceae, 

Proteaceae and Euphorbiaceae, along with 

Raphanus, Echium and Citrus. 

In the Portuguese honeys, the presence of 

Fabaceae, Rosaceae and Cistaceae stands out, 

with Castanea and Erica as secondary pollen 

types, while Fabaceae, Asteraceae, Boraginaceae, 

Cistaceae and Scrophulariaceae are the 

families with the highest quantity of pollen 

types in the samples from Spain. In the latter, 

the most important secondary pollen types are: 

Castanea, Cytisus, Erica, Lotus, Salix and Rubus. 

2007010082 

马达加斯加盆地下赛诺曼统 (Lower 

Cenomanian) 被子植物花粉超微结构的研 

究 = The ultrastructure of angiosperm pollen 

from the Lower Cenomanian of the Morondova 

Basin, Madagascar. ( 英文 ). Michael Z. 

Grana, 2003, 42(1): 20-32 

Samples collected from Cretaceous 

sediments of the Morondova Basin, southwest 

Madagascar yielded a palynoflora composed 

of spores of ferns and fern allies, pollen of 

gymnosperms and angiosperms, and dinoflagellates. 

In addition, a diverse fauna of ammonites 

was recovered along with the microflora. 

The species of dinoflagellates and ammonites 

suggest an Early Cenomanian age. Ninety-two 

percent of the microflora is comprised of fern 

spores and gymnosperm pollen. Approximately 

twenty species of angiosperm pollen 

comprise 3.6% of the flora, a majority of 

which are monosulcate and disulcate, including 

Clavatipollenites, Retimonocolpites, and 

Liliacidites. Single occurrences of tricolpates 

and tricolporates are also recorded. The low 

abundance of angiosperms, and the taxonomic 

position of the angiosperm pollen are more 

reminiscent of Lower Cretaceous palynofloras 

from the Barremian-Albian. The low abundance 

of angiosperms and high diversity relative 

to the ferns and gymnosperms suggest 

that angiosperms arrived on Madagascar by 

long distance dispersal. 

2007010083 

花粉细胞学研究和花粉活力的评价 - 以琉 

璃苣 (Borago officinalis L.) 体内和体外试验 

为例 = Study of pollen cytology and evaluation 

of pollen viability using in vivo and in 

vitro test, in borage (Borago officinalis L.). 

( 英文 ). Celia M; Elena F; JosÉ A. 

Grana, 2003, 42(1): 33-37 

Borage (Borago officinalis L.) pollen 

grains have been ratified as trincellular. The 

tetrazolium test is a reliable method to evaluate 

pollen viability in borage. A satisfactory 

medium for pollen germination and pollen 

tube growth was achieved in a liquid medium 

27

supplemented with 200 g/l of sucrose, 100 

ppm of H 3 BO 3 and 300 ppm of 

Ca(NO 3 ) 2 .4H 2 O at pH 7 and 18°C. The pollen 

tube pathway after effective pollination is described. 

The importance of temperature in 

borage pollen biology is proved. 

2007010084 

表面活性剂对孢粉外壁纹饰形成作用的模 

拟 = A model for the role of surfactants in the 

assembly of exine sculpture. ( 英文 ). Alan H; 

Peter G; Susannah M; Robert M. Grana, 2003, 

42(1): 38-42 

The surface coatings of spores and pollen 

often show complex species or genus specific 

patterning and for which there is no obvious 

explanation in terms of evolutionary advantage. 

It has previously been suggested that 

these patterns are the product of a selfassembly 

process used by plants in spore and 

pollen wall development and are a consequence 

of the physical and chemical behaviour 

of the components and their interactions. 

Experiments have shown that comparable patterning 

and structure can be achieved by selfassembly 

of analogous components but the 

range of patterning obtainable was restricted. 

The introduction of specific surfactants into 

the reaction has now broadened the range of 

patterns that can be derived by this method 

and supports the view that surfactants must be 

important in the development of the naturally 

occurring patterns. 

2007010085 

太阳光对真菌链格孢属 (Alternaria) 过敏原 

孢子释放的影响 = The effect of sunlight on 

allergen release from spores of the fungus Alternaria. 

( 英文 ). Teresa M ;O'meara T; Euan T. 

Grana, 2003, 42(1): 43-46 

Airborne fungal spores are known carriers 

of allergen. Correlations between spore 

counts and allergen concentrations are poor. It 

is known that germination increases allergen 

release, implicating spore viability as a determinant 

of allergen release. During aerial dispersal, 

spores can be exposed to prolonged 

periods of ultraviolet (UV) light which can 

reduce viability of spores. We examined the 

relation between spore viability and allergen 

release in two experiments: firstly spores from 

culture were treated with a UV wavelength of 

254 nm (not present in sunlight reaching the 

earth's surface) or autoclaved, and secondly, 

spores were exposed to simulated sunlight 

over three days. In both studies viability was 

measured (by germination on agar and by 

metabolic activity with nitro-blue tetrazolium 

vital stain) and allergen release by the Halogen 

immunoassay. The UV light reduced the 

proportion of spores able to germinate but did 

not affect metabolic activity or allergen release. 

Autoclaving reduced the proportion of 

spores releasing allergen by half (p

the Tarija Basin, Salta Province, Argentina.. 

( 其他 ). Di Pasquo M. Ameghiniana, 2003, 

40(1): 3-32 

The recognition of 165 indigenous species 

and their stratigraphic range in the 

Machareti and Mandiyuti Groups from Tarija 

Basin (northern Argentina and southern Bolivia) 

is used to propose a biostratigraphic 

scheme composed of a Superzone named 

Kraeuselisporites volkheimerii- Circumplicatipollis 

plicatus, which is divided into five 

First Appearance Interval Palynozones. The 

first three oldest zones, called Crassispora 

kosankei - Cystoptychus azcuyi, Raistrickia 

radiosa - Apiculatasporites spinulistratus and 

Dictyotriletes bireticulatus - Cristatisporites 

chacoparanensis, are attributed to an earlymiddle 

Late Carboniferous age, while the 

other two, named Granulatisporites micronodosus 

- Reticulatisporites reticulatus and 

Marsupipollenites triradiatus - Lundbladispora 

braziliensis, are referable to the late Late 

Carboniferous. The age is based on the biostratigraphic 

range of several key-species and 

the location of each palynozone within the 

lithostratigraphic succession. The abundant 

presence of species in common with other 

palynofloras from the Late Carboniferous of 

South America, especially from Argentina and 

Brazil, also supports this age. Regarding the 

154 reworked species recognized, they confirm 

the deposition of Uppermost Devonian 

and Lower Carboniferous strata at the Argentinean 

part of the basin, which would have 

belonged to the Oriental Protocordilleran and 

Michicola Arc. Both cordilleras were the 

western and south-eastern boundaries of the 

Tarija Basin during the Late Carboniferous. 

2007010088 

阿根廷圣克鲁斯省 Austral 盆地下白垩统 

Kachaike 组孢粉第一部分光滑和具环带 

孢子 = Palynology of the Kachaike Formation, 

Lower Cretaceous of the Austral Basin, Santa 

Cruz province, I. Smooth and cingulate 

spores.. ( 其他 ). Archangelsky A; Llorens M. 

Ameghiniana, 2003, 40(1): 71-80 

Smooth and cingulate disperse spores 

from the Kachaike Formation, Lower Cretaceous 

from Santa Cruz province are described 

sistematically. Deltoidospora inconspicua, 

Contignisporites burgeri and C. glebulentus 

are mentioned for the first time for Argentina. 

The following species are mentioned for the 

first time for the Kachaike Formation: Cyathidites 

patagonicus, C. cf. C. punctatus, 

Deltoidospora australis, Concavisporites cf. C. 

semiangulatus, Todisporites minor, Leiotriletes 

cf. L. regularis, Cyatheacidites tectifera 

and Aequitriradites baculatus. 

2007010089 

南美苔草科花粉 :1. 河苔草属 (Apinagia 

Tul.) = Palynology of South American Podostemaceae: 

I. Apinagia Tul.. ( 英文 ). Passarelli 

L; Girarde S B; Tur N M. Grana, 2002, 

41(1): 10-15 

Pollen structure of three species of Apinagia 

(Podostemaceae) that grow in the Paranean 

Province, South America, are described. 

The pollen grains are isopolar, tricolpate, 

spheroidal to subprolate, with microechinate 

sculpture. The ornamental processes are of 

different size. The colpus membrane has similar 

ornamentation as the non-apertural wall 

but larger. Ultrastructural studies of the wall 

demonstrated that the ectexine is composed of 

a tectum, a granular infratectum formed by 

cylindrical elements, similar to rounded cords 

of different diameter and a basal layer. The 

general morphology and exine ultrastructure 

are similar to that of other taxa of Podostemaceae 

(Marathrum, Mourera, Podostemum, 

Tristicha). These are the first palynological 

descriptions of Apinagia, using transmission 

electron microscopes (TEM). Pollen quantity 

per anther is also reported for the first time. 

2007010090 

毛茛科铁筷子属 (Helleborus) 花粉散发时细 

胞质碳水含量变化 = Changes in cytoplasmic 

carbohydrate content during Helleborus pollen 

presentation. ( 英文 ). Vesprini J L; Nepi M; 

Cresti L; Guarnieri M; Pacini E. Grana, 2002, 

41(1): 16-20 

Pollen grains of Helleborus foetidus and 

H. bocconei were exposed to low temperature 

treatments to simulate the natural events in 

pollen presentation of these two winter flowering 

species and to analyze the pollen carbohydrate 

content (glucose, fructose, sucrose and 

starch). In both species, cytoplasmic polysaccharides, 

monosaccharides and sucrose were 

found, while only Helleborus foetidus contained 

starch. Polysaccharide, sucrose and 

monosaccharide content varied as low temperature 

exposure time varied, a decrease in 

temperature decreases polysaccharide content 

and increases sucrose and monosaccharides. 

The relative quantities of the various types of 

carbohydrates were not affected by variations 

in the naturally occurring thermal cycles. 

Treatments did not greatly affect pollen viability. 

29

2007010091 

裸子植物萌发花粉细胞壁成分的免疫化学 

和细胞化学检测 = Immunochemical and cytochemical 

detection of wall components of 

germinated pollen of gymnosperms. ( 英文 ). 

Yatomi R; Nakamura S; Nakamura N. 

Grana, 2002, 41(1): 21-28 

To elucidate wall construction of gymnosperm 

pollen, we studied the distributions of 

cell wall constituents in the germinated pollen 

of 14 species of gymnosperms in 8 genera and 

6 families cytochemically with 4 staining dyes 

for polysaccharides, and immunochemically 

with 4 monoclonal antibodies for polysaccharides 

and 2 monoclonal antibodies for arabinogalactan 

proteins (AGPs). All intines and 

tube walls of the pollen examined contained 

AGPs and cellulose. Although having small 

differences, pollen of the Podocarpaceae, 

Pinaceae, Taxodiaceae, and Cupressaceae 

(Coniferales) had a similar composition of 

wall constituents: much AGPs occurred in 

both the intine and the tube wall, pectins were 

rare in the tube wall. On the other hand, in 

Cycas revoluta pollen, pectins were abundant 

and in Ginkgo biloba, -(1,3)(1,4)-glucan was 

abundant in both the intine and the tube wall. 

The occurrence of -1, 3-glucan in the intines 

was common to six Pinus species, but its occurrence 

in the tube wall differed among them. 

None of the gymnosperm pollen tubes examined 

had tube walls similar to those of angiosperm 

pollen, which consist of two layers, a 

pectic outer layer and a callosic inner layer. 

These results suggest that wall formation in 

gymnosperm pollen tubes is remarkably different 

from that of angiosperm pollen tubes 

and the composition of the wall constitutes 

may reflect a taxonomic relationship among 

gymnosperms. 

2007010092 

喜马拉雅长叶松 (Pinus roxburghii) 的花 

粉产量变异、花粉 / 胚珠比率及性选择 = 

Pollen productivity variations. Pollen-ovule 

ratio and sexual selection in Pinus roxburghii. 

( 英文 ). Khanduri V P; Sharma C M. 

Grana, 2002, 41(1): 29-38 

Total pollen production, pollen-ovule ratio 

and the production of male-female strobili 

were recorded in Pinus roxburghii at two different 

altitudes during two successive years. 

The values of total pollen production per tree 

and per hectare varied between 1953.56 to 

2727.16 × 109 and 2.91 to 4.26 × 1014 (in 

1999) at the lower altitude and 1247.5 to 

1673.5 × 109 and 2.24 × 1014 (in 1998) and 

1599.89 to 2038.96 × 109 and 3.18 × 1014 (in 

1999) at the higher altitude. The pollen-ovule 

ratio in P. roxburghii has indicated the 

xenogamous type of breeding system The 

production of male and female cones per tree 

and per hectare ranged from 21.7 ± 0.34 to 

33.6 ± 0.71 × 103 and 55.16 ± 24.08 to 220.85 

± 87.75 per tree and 32.55 to 70.56 × 105 and 

2.76 to 26.50 × 103 per hectare respectively. 

However the production of female cones per 

100 male cones oscillated between 0.25 to 

0.66, which suggested the intense male competition 

among trees to pollinate their 

neighbours. 

A linear correlation was recorded between 

diameter and extent of the tree crown to 

the total production of strobili groups/strobili 

clusters, strobili, microsporophylls and pollen 

grains per individual tree. The ratio between 

the number of strobili per strobili group and 

the number of strobili groups per tree showed 

an inverse relationship; thus, the individuals 

with most strobili groups have the strobili 

groups with the least strobili and vice-versa. 

This ratio was also shown between the number 

of pollen grains per strobilus and the number 

of strobili per tree, as well as the number of 

pollen grains per strobili group and the number 

of strobili groups per tree. 

2007010093 

铁刀木 (Cassia siamea) 花粉致敏蛋白的 

鉴定分析 = Identification of the allergenic 

proteins of Cassia siamea pollen. ( 英文 ). Parui 

S; Mondal A K; Mandal S. Grana, 2002, 

41(1): 39-43 

Total soluble proteins from the pollen of 

Cassia siamea Lamk. were extracted and subjected 

to 80% ammonium sulphate precipitation. 

The total protein was then separated on a 

12% SDS-Polyacrylamide gel which revealed 

11 bands between molecular weight range of 

45 kDa and 181kDa with another band having 

molecular weight less than 29kDa. Each band 

was recovered from the gel by electroelution 

and sent for skin tests. CS4 (97kDa). CS7 

(63kDa), CS9 (53 kDa) and CS10 (45kDa) 

were the major allergenic components while 

CS2 (148kDa), CS3 (116kDa), CS6 (75kDa) 

and CS8 (60kDa) also induced reactivity in 

some patients. Immunodiffusion analysis with 

pooled sera of patients sensitive to the total 

extract confirmed the allergenicity of the 

bands. 

30

2007010094 

西班牙加那利群岛拉帕尔玛岛 (La 

Palma) 不同单种花蜜的孢粉谱 = Pollen 

spectra of different unifloral honeys from La 

Palma (Canary Islands, Spain). ( 英文 ). La- 

Serna Ramos I; Méndez Pérez B; Ferreras C G. 

Grana, 2002, 41(1): 48-57 

The pollen content of twenty-four unifloral 

honey samples from twelve different apiaries 

in La Palma (Canary Islands) was subjected 

to qualitative and quantitative melissopalynological 

analysis. The quantitative 

analysis showed that 4% of the honey belonged 

to Maurizio"s Class I, 8% to Class II, 

58% to Class III, 17% to Class IV and 13% to 

Class V. According to the qualitative analysis, 

eight honeys were typified as unifloral of Castanea 

sativa, five of Carlina salicifolia, three 

of Echium brevirame, three of Reseda luteola, 

two of Erica arborea, two of Lotus hillebrandii 

and one of Lamiaceae Origanum vulgare ssp. 

virens-type. 

No honeydew elements were found. 62 pollen 

types were identified belonging to 42 different 

families. There is no pollen type common to 

all samples but Foeniculum vulgare-type is 

present in 22 of the samples (91.7%) and the 

combination Cistus sp., Erica arborea, Aspalthium 

bituminosum, Origanum vulgare ssp. 

virens-type and Rumex sp. in 21 (87.5%). 

The organoleptic analysis indicated that they 

are of good quality. 

2007010095 

阿根廷 Caldeń 区南部的蜜源植物 = Botanical 

origin of honey from south of Caldeń 

district (Argentina). ( 英文 ). Andrada A C; 

Tellería M C. Grana, 2002, 41(1): 58-62 

We performed palynological analysis of 

75 honey samples from the south of Caldén 

district, which is the part of the phytogeographical 

province del Espinal. Prosopis 

caldenia, "caldén" (Fabaceae) is the dominant 

arboreal species in this region. 79 pollen types 

that belong to 36 plant families were identified. 

Honeydew elements are absent or present in 

negligible amounts. Native flora is intensely 

utilized. Main nectar sources that characterize 

monofloral honey samples, are these natives 

Condalia microphylla (Rhamnaceae), Prosopis 

sp. and Vicia sp. (Fabaceae), Larrea divaricata 

(Zygophyllaceae) and Brassicaceae, 

which are foreign to the area. The pollen from 

these plants along with the pollen of Trichocline 

sp. (Asteraceae) and Prosopidastrum 

globosum (Fabaceae), Schinus fasciculatus 

(Anacardiaceae), Astereae and Lycium 

sp.(Solanaceae), 

Caldén. 

characterize honey from 

2007010096 

阿根廷拉里奥前科迪耶拉中新世 Cerro 

Morado 组下段首次孢粉记录 = First palynological 

record for the lower member of 

Cerro Morado Formation (Miocene), La Rioja 

Precordillera.. ( 其他 ). Barreda V; Limarino C; 

Fauque L; Tripaldi A; Net L. 

Ameghiniana, 2003, 40(1): 81-87 

The finding of palynological remains in 

the lower member of the Cerro Morado Formation 

is reported for the first time. The fossiliferous 

levels are located at the headwaters 

of the Guandacol river in southwestern La 

Rioja Province. In this area the Cerro Morado 

Formation has been divided into two members. 

The lower member, composed of sandstones, 

mudstones and scarse conglomerates and 

limestones, contains the palynological remains. 

described in this paper. The palynological assemblages 

are not diverse, they are poorly 

preserved and dominated by aquatic elements 

mainly related to colonial green algae (Pediastrum 

spp., Botryococcus sp.) and dinoflagellates. 

Spore-pollen assemblages consist of 

aquatic herbs of Restionaceae (Milfordia sp.) 

and Malvaceae (Baumannipollis chubutensis 

Barreda, Baumannipollis sp., Malvacipolloides 

comodoroensis Barreda). Typical lake 

shore vegetation consisted of members of 

Ephedraceae [Equisetosporites claricristatus 

(Shakmundes) Barreda, E. notensis (Cookson) 

Romero, E. lusaticus (Krutzsch) Barreda] and 

scarse Chenopodiaceae (Chenopodipollis 

chenopodiaceoides (Martin) Truswell). Pollen 

grains related to Podocarpaceae (Podocarpidites 

marwickii Couper, P. elegans Romero) 

and Fagaceae (Nothofagidites acromegacanthus 

Menendez and Caccavari, N. americanus 

Zamaloa, N. saraensis Menendez and Caccavari) 

are also present, although in low percentages. 

The known stratigraphic ranges of 

the recognized species, and the similarities of 

these assemblages to others previously described 

from Argentina, point to an Early to 

Middle Miocene age for this unit. Finally, 

sedimentological and palynological. evidences 

suggest the development of a large and perennial 

water body during the time of deposition 

of the lower member of Cerro Morado Formation. 

2007010097 

西藏纳木错末次盛冰期以来的古植被、古 

气候和湖面变化 = Paleovegeta- 

31

tion,paleoclimate and lake-level change since 

the last glacial maximum in Nam Co,Tibet. 

( 中文 ). 吴中海 ; 赵希涛 ; 吴珍汉 ; 周春景 ; 严富 

华 ; 朱大岗 . 地质通报 , 2003, 22(11-12): 928- 

935 

西藏纳木错湖相沉积的 U 系、 14 C 年龄 

和孢粉分析结果表明 , 纳木错沿岸的拔湖约 

1.5~8.3m 和 8.3~15.6m 的 T 1 和 T 2 分别形成 

于末次盛冰期以来约 (11.81±0.10) ~ 

(4.22±0.09)kaB.P. 期间和 (28.2±2.8)kaB.P. 左 

右。该套湖相层的孢粉组合、地层和湖岸 

堤的分布表明 , 在末次盛冰期期间 , 纳木错湖 

面主要波动于拔湖 12~20m 之间 , 但湖面最 

低可达拔湖约 8m。区域植被主要为以蒿和 

莎草科为主、含松和桦的草原。在约 

11.8~4.2kaB.P. 期间 , 湖面波动于拔湖 2~ 

9m 之间 , 区域气候整体较为暖湿。其中全新 

世大暖期出现在约 8.4~4.2kaB.P. 期间 , 气候 

温暖湿润 , 区域出现针叶林或针阔叶混交林 , 

气温可能比现今高约 5 ℃ , 降水量可能比现 

今多 100~200mm, 湖面扩张并升高 , 最高可 

达拔湖约 10m。 

2007010098 

当代和化石孢粉中具环状口器型花粉的超 

微结构和多样性 = Ultrastructure and diversity 

of recent and fossil zona-aperturate pollen 

grains. ( 英文 ). Hesse M; Zetter R. Plant Systematics 

and Evolution, 2006, 255(3-4): 145- 

176 

A survey of recent and fossil zonaaperturate 

pollen grains within the angiosperms 

was undertaken. Zona-aperturate pollen 

(with complete ring-like apertures) has 

been evolved independently in several genera 

of basal angiosperm families (Nymphaeaceae, 

Eupomatiaceae, Annonaceae, Monimiaceae, 

Atherospermataceae) and monocots (Araceae, 

Iridaceae, Laxmanniaceae, Arecaceae, and 

Rapateaceae). The special case of the eudicot 

Limnanthes (Limnanthaceae) is discussed. 

New examples of recent and fossil fully 

zonate pollen are presented; a noteworthy new 

example are Scrophulariaceae, with Pedicularis; 

our fossil examples show affinities either 

to Nymphaeaceae, or Araceae, or Iridaceae, 

or cannot be related to an extant taxon. 

The zona-aperturate pollen grains differ in 

ornamentation and stratification mostly in the 

respect of the aperture areas, but sometimes 

also outside the aperture. The question of polarity 

is settled only for some taxa because of 

the frequent lack of tetrad observations. A 

ring-like aperture may divide the pollen grains 

in symmetric halves, or if running asymmetrically, 

divides the pollen grain in two more or 

less unequal halves; the presence of clearly 

unequal halves gives a strong argument to 

assume an equatorial ring in such cases where 

tetrad configurations were not available. The 

zona-aperturate condition may be a functional 

benefit in wet environments: while in dry pollen 

the apertural ring is completely closed, in 

wet or very moist realm it expands greatly, 

and the pollen tube can be formed quickly and 

everywhere in this area. 

2007010099 

菝葜属植物花粉形态的系统分类学意义 = 

The systematic value of pollen morphology in 

Smilacaceae. ( 英文 ). Chen S C; Zhang X P; 

Ni S F; Fu C X; Cameron K M. Plant Systematics 

and Evolution, 2006, 259(1): 19-37 

Smilacaceae are a small family of dioecious, 

mostly climbing, net-veined monocotyledons 

with a cosmopolitan distribution. 

Relatively little is known about the variation 

of pollen morphology within the family. For 

this reason, and to investigate the systematic 

value of palynology in Smilacaceae, pollen 

from 125 species of Smilax, Heterosmilax, 

and Ripogonum was examined using light and 

scanning electron microscopy. Ten of these 

were examined further by transmission electron 

microscopy. Four distinct pollen types 

grouped into two major pollen classes were 

distinguished: Class 1, represented by the pollen 

of all Smilax and Heterosmilax species, is 

mostly spheroidal, inaperturate, and spinulate 

or microspinulate, with a thin, fragile exine of 

varied sculpturing; three pollen types are represented 

within this class. Class 2 is found 

only in Ripogonum and contains a single pollen 

type with prolate, monosulcate, reticulately-sculptured 

pollen. The unique pollen 

morphology of Ripogonum supports its removal 

from Smilacaceae. In contrast, the 

characteristics of Heterosmilax pollen intergrade 

with those seen in Smilax, suggesting 

that the former might be better reduced to 

synonymy with the latter. A key to the identification 

of these pollen types is presented 

along with a discussion of geographic and 

possible evolutionary trends among them. 

牙形石 

2007010100 

四川盐边地区志留纪牙形石生物地层及年 

代地层 = Silurian conodont succession and 

chronostratigraphy of the Baizitian region in 

32

Yanbian, Panzhihua, Sichuan. ( 中文 ). 金淳泰 ; 

钱泳蓁 ; 王吉礼 . 地层学杂志 , 2005, 29(3): 

281-294 2 图版 . 

首次提供了四川盐边地区从下志留统 

至下泥盆统连续的志留系年代地层系统的 

实际证据和原始材料 , 由上而下建立 8 个牙 

形石带 ,2 个牙形石组合带和 1 个笔石带 , 以 

此为依据建立了攀枝花阶、永兴阶、箐河 

阶、叉河阶、透底河阶和支六阶 , 分别归入 

下泥盆统、顶志留统、上志留统、中志留 

统和下志留统 , 为我国志留系安康阶以上地 

层的建阶研究工作提供了实际的基础资 

料。四川盐边地区志留系龙马溪组为笔石 

相地层 , 其上全为碳酸盐岩相 , 其中牙形石发 

育良好 , 形成连续完整的牙形石带序列 , 这对 

我国和更大的范围壳相志留系年代地层系 

统对比提供了非常有价值的资料。 

2007010101 

鲁西地区寒武纪原始真原始真牙形石分类 

学探讨 = A taxanomic study on primitive euconodonts. 

( 中文 ). 武桂春 ; 姚建新 ; 纪占胜 . 

地质学报 , 2004, 78(3): 289-295 1 图版 . 

鲁西地区晚寒武世地层发育 , 产有数 

量丰富、分异度大的原始真牙形石分子 , 

经笔者研究 , 建立了 2 新属、2 新种及 2 未 

定种 Camconodontus rotundatus gen et 

sp . nov., Camconodontus sp., Laiwunodus 

lateronodus gen et sp. nov., Laiwunodus sp.; 

对 Dasytodus 属进行了补充修订 , 建立了 1 

新种 Dasytodus posteronodus sp.nov.。这 

些属种的建立丰富了对已有原始真牙形石 

概念的认识。基于内部构造的观察 , 对原 

始真牙形石及部分易混淆的副牙形石进行 

正确的分类。以此为基础 , 分析、总结了 

这些分子外部形态上的差异 , 选用的分类 

原则和标准是从一般到特殊、特征明显程 

度逐渐降低 , 划分出了三类原始真牙形石 

和一类副牙形石 , 这在很大程度上简化了 

早期真牙形石分类研究的复杂性 , 为早期 

真牙形石的深入研究奠定了基础。 

2007010102 

湖北宜昌夏口剖面二叠纪 - 三叠纪界线的牙 

形石带及其与全球层型剖面和 PTB 点位对 

比 = Conodont zonation across the Permian- 

Triassic boundary at the Xiakou section, Yichang 

city, Hubei Province and its correlation 

with the Global Stratotype Section and Point 

of the PTB. ( 英文 ). Wang G Q, Xia W C. Canadian 

Journal of Earth Sciences, 2004, 41(3): 

323-330 

Xiakou section is situated north of the 

central Yangtze platform with successive Late 

Permian to Early Triassic strata, thicker than 

the Global Stratotype Section and Point 

(GSSP) of the Permian-Triassic boundary 

(PTB). We recognized three conodont zones 

across the PTB in this section by highprecision 

biostratigraphy. They are the 

Hindeodus latidentatus - Clarkina meishanensis 

Zone, Hindeodus parvus Zone, and Isarcicella 

isarcica Zone in ascending order, 

which correspond well with the GSSP. The 

present biostratigraphic work on Xiakou section 

certainly confirmed the conodont zonation 

through the PTB at the GSSP and also 

testified to the correctness of the PTB demarcation 

in Xiakou section. Based on this precise 

demarcation of the PTB, the appearance of a 

clay layer, bed ZSJI266, just beneath the PTB 

should be an important advantage over the 

GSSP, because this clay layer approaches to 

the PTB much in contrast with those two clay 

layers, bed 26 and bed 28, in the GSSP. 

Therefore, the radiometric isotopic dating in 

bed ZSJI266 at Xiakou section should give a 

more accurate age for the PTB. 

2007010103 

我国北方石炭 - 二叠系牙形刺序列再认识 = 

Review of Carboniferous-Permian conodont 

biostratigraphy in North China. ( 中文 ). 王志 

浩 ; 祁玉平 . 微体古生物学报 , 2003, 20(3): 

225-243 1 图版 . 

文中根据当前比较统一的牙形刺分带 

原则 , 对我国北方石炭一二叠系的牙形刺 

序列进行了研究和重新定义。我国北方地 

区石炭一二叠系的牙形刺带或组合带由上 

而下可综合如下 :Sweetognatkus whitei, 

S.tnornatus, Streptognathodus barskovi, 

S.isolatus,S.elegantulus-S.oppletus, 

Idiognathodus magnificus-Neognathodus 

roundyi , Idiognathodus delicatus- 

Neognatkodus bothrops,Idiognathoides corrugatus-I 

. stnuatus , Declinognathodus 

noduliferus , Gnathodus bilineatus bollandensis 

和 Gnathodus bilineatus bilineatus 带或 

组合带。本文同时介绍了牙形刺带和组合 

带在我国北方的分布、时代及其对比。 

2007010104 

永德梯子坡剖面丁家寨组发现早二叠世牙 

形石 = The discovery of early Permiaen 

conodont in Dingjiazhai Formation of Tizipo 

33

section,Yongde. ( 中文 ). 赵成峰 . 云南地 

质 , 2003, 22(2): 196-199 

测制永德县梯子坡剖面时 , 首次于丁家 

寨组顶部灰色亮晶生物碎屑灰岩层中发现 

丰富的早二叠世牙形石。根据牙形石组合 , 

提出丁家寨组上部 ( 至少顶部 ) 存在下二叠统 

沉积。 

2007010105 

澳大利亚新南威尔士中西部 Barnby Hills 

页岩中构造灰岩地块普里多利期牙形类动 

物群 = Pridoli conodont fauna from tectonically 

emplaced limestone blocks within the 

Barnby Hills Shale, central western New 

South Wales. ( 英文 ). Farrell J R. Alcheringa, 

2006, 30(2): 233-249 

Conodont faunas recovered from isolated 

limestone outcrops within the Barnby Hills 

Shale, between Larras Lee and Eurimbla, New 

South Wales, are shown to be of Late Silurian 

(eosteinhornensis Zone) age and are coeval 

with the lower sequence of the Camelford 

Limestone at Wellington. These isolated outcrops 

have been interpreted as having a tectonic 

origin due to their position adjacent to 

the Curra Creek Thrust and the age discrepancy 

between them and the surrounding Barnby 

Hills Shale sediments. 

古植物学 

藻类 

2007010106 

晚 Callovian- 早 Oxfordian 期降温引起的钙 

质微化石变化 = Calcareous nannofossil 

changes during the late Callovian–early Oxfordian 

cooling phase. ( 英文 ). Tremolada 

F;Erba E;Schootbrugge B;Mattioli E. Marine 

Micropaleontology, 2006, 59(3-4): 197-209 

Calcareous nannofossil quantitative and 

biostratigraphic analyses integrated with carbon 

and oxygen stable isotopes were carried 

out on the core ANDRA (Agence Nationale 

pour la gestion des Déchets Radio-Actifs— 

FRANCE) HTM 102 across the Callovian/Oxfordian 

boundary drilled at Cirfontaines-en-Ornois, 

Départment de Haute-Marne, 

eastern France. Calcareous nannofossil assemblages 

at the Callovian–Oxfordian transition 

are dominated by the genus Watznaueria. 

An increase in abundance of Biscutum spp. 

and A-group, which consists of Axopodorhabdus 

spp. (A. atavus, A. rahla, and A. cylindratus), 

Podorhabdus grassei, Octopodorhabdus 

decussatus, Hexapodorhabdus cuvillieri (family 

Axopodorhabdaceae), and Triscutum spp., 

correlates with a significant positive excursion 

in δ 18 O suggesting that these groups were 

probably adapted to cooler surface waters. A 

positive increase in δ 13 C values is coupled 

with high abundances of eutrophic taxa such 

as Zeughrabdotus erectus, Biscutum spp., and 

small-sized Watznaueria britannica, and a 

decrease in abundance of the big and oligotrophic 

taxa Schizosphaerella punctulata and 

Watznaueria manivitae. Climate cooling 

across the Callovian/Oxfordian boundary 

probably triggered a breakdown in stratification 

of surface waters leading to more intense 

nutrient recycling and higher primary productivity 

that favoured the shift in abundance of 

small-sized eutrophic taxa in the East Paris 

Basin. 

2007010107 

植物分类学在化石珊瑚藻 ( 珊瑚藻目 , 红藻 

门 ) 中的应用 = Application of botanical taxonomy 

to fossil coralline algae (Corallinales,Rhodophyta). 

( 英文 ). Braga J C. 微体古生 

物学报 , 2003, 20(1): 47-56 

最近有人认为将化石藻类的分类归入 

现生藻类分类单元有利于珊瑚藻作为古环 

境的标志 , 便于理解该类群的演化。然 

而 , 这样分类可能很难 , 因为并不是所有 

现生藻类分类特征都能在化石种中保存下 

来。Sporolithacea 科的钙化部分 ( 独立或者 

聚集的孢子囊群 ) 的出现 , 可以把它们与这 

个类群的另一个现生科 Corallinaceae 区别 

开 , 这个科在生殖窠中产生孢子囊。节片 

的有无 , 丝间细胞的联系类型 , 生殖窠中 

孢子囊释放的数目都是用来划分 

Coral1inaceae 科的亚科的标准 , 在化石样 

品中也可以用合适的条件进行观察。在大 

多数情况下 , 对现生珊瑚藻类属的划分特 

征可以在化石藻类中鉴别出来 , 但在几种 

现生珊瑚藻没有钙化的生殖结构或发育特 

征。因此 , 它们生殖结构无法与相应的化 

石藻类进行对比 , 也不能进行化石藻类的 

分类。近年来的趋势认为生殖结构和发育 

特征是对现生珊瑚藻进行分类的优先鉴定 

标准 , 然而 , 某些特征的稳定性在属的划 

分上仍然存在争论。在许多情况下 , 现生 

藻类的分类标准特征都不能在化石中保 

存 , 对古生物化石的分类标准的最佳选择 

是在化石藻类中选择辅助的 , 并且可以识 

别的其它鉴定特征 , 或者应用非正式的比 

现生藻类代表定义更宽的属名 . 

34

2007010108 

分布于亚北极地带北太平洋及白令海区的 

海生硅藻 Neodenticula seminae 壳形态的 

空间变异性 = Spatial variability in valve 

morphology of Neodenticula seminae, an oceanic 

diatom in the subarctic North Pacific and 

the Bering Sea. ( 英文 ). Shimada C; Tanimura 

Y. Paleontological Research, 2006, 10(1): 79- 

89 

To gain basic insights into the marine pelagic 

diatom species Neodenticula seminae, 

and particularly the relationships between 

morphology, evolution and environment, we 

conducted a scanning electron microscopic 

image analysis using modern specimens collected 

in the subarctic North Pacific and Bering 

Sea during the summers of 1955 and 

1996-2003. We recognized an apparent intraspecific 

variability between two biogeographic 

provinces in terms of morphology: (1) the 

Oyashio Region (in the northwestern margin 

of the Pacific Ocean) and (2) other oceanic 

regions. This variability may reflect spatial 

variation in the availability of nutrients such 

as silicate. Specimens from the Oyashio morphological 

province had thinly silicified 

valves, whereas those from the other oceanic 

provinces were extraordinarily rich in heavily 

silicified valves. 

被子植物 

2007010109 

辽西侏罗纪木化石 Sahnioxylon( 萨尼木 

属 ) 及其系统学意义 = Jurassic fossil wood 

of Sahnioxylon from western Liaoning, China 

and special references to its systematic affinity. 

( 中文 ). 郑少林 ; 李勇 ; 张武 ; 王永栋 ; 杨小菊 ; 李 

楠 ; 傅小平 . 世界地质 , 2005, 24(3): 209-218 

Sahnioxylon rajmahalense( 拉杰马哈尔萨 

尼木 ) 在中国是首次报道 . 标本产于辽宁北 

票长皋乡喇嘛营和巴图营乡油房附近中体 

罗统髫髻山组 . 文中对 Sahnioxylon 与 

Phoroxylon( 贼木 ) 和 Paradoxoxylon ( 奇 

木 ) 的关系做了讨论 , 将 Sahnioxylon andrewsii( 

安德鲁斯萨尼木 ) 从 Sahnioxylon 

中分出 , 另立一个新属 Boseoxylon( 鲍斯木 

属 ); 并认为 Sahnioxylon, 既不是本内苏铁类 

也不是真正被子植物的木材 , 它最有可能是 

晚古生代一种特殊的木材 Guizhouoxylon 

( 贵州木 ) 经过晚三叠世的 Paradoxoxylon 

向现存无导管的被子植物演化的一个中间 

环节 , 为一种无导管的被子植物的先驱类型 . 

2007010110 

分子及迁徙 : 十字花科植物的生物地理研 

究 = Molecules and migration: biogeographical 

studies in cruciferous plants. ( 英文 ). Koch 

M A; Kiefer C. Plant Systematics and Evolution, 

2006, 259(2-4): 121-142 

In the past two decades our understanding 

of plant biogeography has been improved 

substantially by the introduction of various 

molecular marker systems. Especially within 

the angiosperms, maternally inherited chloroplast 

DNA based data sets have elucidated not 

only genetic relatedness but also geographic 

structuring of genetic variation. These findings 

were based on the observation that DNA 

molecules might mutate during migration, 

which consequently found its manifestation in 

the term phylogeography introduced in the 

late 80s by John Avise. 

However, other markers such as codominantly 

inherited allozymes were used before 

the advent of DNA techniques and were used 

in theoretical population genetic studies. In 

actual phylogeographic studies, highly variable 

markers, such as AFLPs (amplified fragment 

length polymorphisms), were needed to 

unravel recent species histories (e.g. pleistocenic 

differentiation). The levels of molecular 

variation at such markers are closer to that of 

allelic variation measured with allozymes. 

Hence, an increasing number of studies have 

relied on highly polypmorphic markers, such 

as DNA microsatellite loci. 

Herein, we try to present an overview on 

the various biogeographic and phylogeographic 

studies using various molecular 

(including isozyme) markers and methodological 

approaches to analyse them, concentrating 

on studies done with representatives of 

the Brassicaceae family. 

古无脊椎动物学 

综论 

2007010111 

贵州关岭生物群研究的进展和存在问题 ( 代 

序 ) = Study of the Guanling biota in 

Guizhou:progress and problems. ( 中文 ). 汪啸 

风 ; 陈孝红 ; 陈立德 ; 王传尚 . 地质通报 , 2003, 

22(4): 221-227 1 图版 . 

德国被誉为三叠系的故乡 , 因为三叠系 

这个术语来自德国的日尔曼盆地 , 其中三叠 

统壳灰岩素有化石库之称。然而 , 关岭生物 

群的发现和在生物群的时代、组合特征、 

产出层位、分布以及形成环境等方面研究 

的进展表明 : 关岭生物群堪称世界上独一无 

35

二的化石库或化石矿床 , 其化石保存之完 

美、类型之多样、数量之多 , 远远优于德国 

的壳灰岩。对这个珍稀生物群的综合研究 

不仅为创新海生爬行动物、海百合和软骨 

鱼等化石的分类、演化、古生态和古生物 

地理分区的理论提供了丰富的素材 , 而且对 

于解决与此有关的重大问题、建立中国甚 

至全球拉丁阶和卡尼阶界线层型剖面、发 

展生物超常规保存及埋藏环境理论和重建 

“ 三叠纪公园 ” 均具有重要意义。 

2007010112 

河北阳原槽村剖面一孢粉组合特征及古气 

候意义 = Characteristics of a sporo-pollen 

assemblage in the section of Caocun,Yangyuan, 

Hebei, and its paleoclimatic 

significance. ( 中文 ). 王燕 ; 王书兵 ; 蒋复初 ; 

童国榜 ; 赵志中 ;. 地质通报 , 2003, 22(9): 

665-669 

阳原槽村剖面的孢粉分析表明 , 阳原盆 

地晚更新世晚期以来的气候环境经历了温 

凉偏干 — 温暖稍湿 — 温凉偏干 — 冷凉偏干 

等 4 个演化阶段 , 植被亦相应地经历了疏林 

草原 — 森林草原 — 疏林草原 — 森林草原等 4 

个演化过程。但总的说来 , 阳原盆地的植被 

自始至终都是以藜、蒿等草本植物占重要 

地位 , 气候总体表现为凉偏干。 

原生动物 

2007010113 

藏南定日县贡扎上白垩统浮游有孔虫生物 

地层新资料 = New biostratigraphic materials 

of planktic foraminifera of the Upper Cretaceous 

from Gongza, Dingri, southern Tibet, 

China. ( 中文 ). 石和 ; 李国忠 ; 赵鹏肖 ; 李祥辉 ; 

赵兵 . 成都理工大学学报 , 2006, 33(2): 134- 

140 

报道了西藏南部定日的上白垩统浮游 

有孔虫生物地层新资料 , 在厚 291m 的贡扎 

剖面中共采集了 699 个有孔虫样品 , 平均 

的样品间距约 40cm, 每两个样品间的间距 

代表约 50 000a 的时间间隔。根据获得的有 

孔虫化石及其在地层中的分布 , 识别出和 

建立了剖面的 12 个浮游有孔虫化石带 , 较 

为准确地确定了相邻化石带的界线 , 在此 

基础上对剖面进行了年代地层的划分。 

2007010114 

土耳其 Sinop 盆地晚白垩世大洋红层中的 

放射虫 = Radiolarians from Upper Cretaceous 

oceanic red beds in Sinop basin, northern 

Turkey. ( 中文 ). 罗辉 . 地学前缘 , 2005, 

12(2): 45-50 1 图版 . 

在土耳其北部 Sinop 盆地 Kayadibi 剖面 

上发育了一套以红色灰岩及红色硅质岩为 

特征的 , 被称之为 Kapanbo(g)azi 组的远洋或 

半远洋环境下的海相红色沉积 . 其中的硅质 

岩里产丰富且保存完好的放射虫化石 . 其放 

射虫组合以 Crucella cachensis, Alievum superbum, 

Patellula verteoensis, Patellula 

ecliptica, Dictyomitra multicostata, Pseudodictyomitra 

pseudomacrocephala, Halesium 

triacanthum, Pessagnobrachia fabianii, Pseudoaulophacus 

putahensis 和 Paronaella 

communis 等属种同时出现为特征 , 可以与北 

美、西特提斯及俄罗斯等地建立的 Alievum 

superbum 放射虫带对比 , 时代为土仑期 . 

2007010115 

东西特提斯晚白垩世深水底栖有孔虫生物 

相和岩相 = Late Cretaceous deep-water benthic 

foraminiferal biofacies and lithofacies of 

the western and eastern Tethys. ( 英文 ). Wolfgang 

Kuhnt; Ann Holbourn. 地学前缘 , 2005, 

12(2): 81-103 6 图版 . 

白垩纪深水古海洋学研究仍处于早期 

发展阶段 , 一方面是由于来自钙质底栖有 

孔虫的稳定同位素和地球化学数据的缺 

乏 , 其原因在于白垩纪高碳酸盐补偿深 

度 ; 另一方面在于深水有机质胶结有孔虫 

示踪古海洋还没有充分发展起来。深海环 

境深水胶结有孔虫的分布主要取决于碳酸 

盐可利用状况、原始生产的输入通量、深 

水交换、环境波动 ( 深海洋流、浊流和快速 

沉积事件 ) 和底层沉积类型 , 因此对于重建 

深海环境具有非常巨大的潜力。东、西特 

提斯 Campanian—Maastrichtian 深水底栖有 

孔虫组合的统计分析揭示出 6 个生物相 , 

代表着明显不同的沉积环境。包括 : 深海 

红色泥岩与矮小深海生物组合 ( 生物相 1); 

红色深海泥灰岩 (“Couches Rouges” 相 ), 含 

钙质胶结有孔虫组合 ( 生物相 3); 深水远洋 

灰岩 (“Scaglia Roossa” 相 ) , 含易碎的 

Rhizammina 组合 ( 生物相 2); 绿色 - 灰色半远 

洋泥灰岩 , 含适应高输出通量生物组合 ( 生 

物相 4) ; 半远洋泥岩和粉砂岩 , 含 

Aschemocella—Nothia 组合 ( 生物相 5); 陆源 

浊积层序 , 含 “ 复理石型 ”Rhabdammina 组合 

( 生物相 6)。Campanian—Maastrichtian 红色 

氧化深水环境动物组合与现今深海类似 , 

而白垩纪贫氧深海环境胶结组合在现今无 

法找到相类似物。随着古生态信息的增加 

和数据库的扩展 , 深水胶结有孔虫有望成 

36

为揭示古海洋条件的重要工具 , 尤其是对 

于非均变的白垩纪深海沉积的形成而言 , 

比如深海黑色页岩和广泛分布的大洋红 

层。 

2007010116 

日本 Kyushu 西部 Kurosegawa 地体 

Tanoura 组外来灰岩中的安尼西阶有孔虫 

化石 = Anisian foraminifers from allochthonous 

limestones of the Tanoura formation 

(Kurosegawa Terrane, West Kyushu, Japan). 

( 中文 ). Kobayashi G; Martini R; Zaninetti L. 

Geobios, 2005, 38(6): 751-763 

Thirty-five species belonging to 21 genera 

of foraminifers are distinguished from allochthonous 

limestone blocks contained 

within the autochthonous mudstones and 

sandstones of the Carnian Tanoura Formation, 

Kurosegawa Terrane of West Kyushu (SW 

Japan). These blocks are considered to be Anisian 

in age, based on the occurrence of two 

foraminifers widely distributed in the Anisian 

of the Tethyan Realm, Pilammina densa and 

Meandrospira dinarica; they are associated 

with Involutinid-like forms, such as Triadodiscus 

and Aulotortus, and with other foraminifers. 

The allochthonous limestones are 

mostly composed of oolites, abundant bioclasts 

and detrital quartz grains. They are 

thought to have been redeposited during the 

Carnian on the shelf slope of the South Kitakami-Kurosegawa 

Old Land. Palaeogeographically, 

this terrane was part of the 

North Gondwana margin, then isolated eastwards 

before its Early Cretaceous amalgamation 

with South China. Three foraminiferal 

species, Triadodiscus eomesozoicus (Oberhauser), 

Triadodiscus tanourensis, n. sp., and 

Triadodiscus sp. are described from the Anisian 

allochthonous blocks. 

2007010117 

评浮游有孔虫壳体方解石 δ18O 数据对重 

建晚中新世海水表面温度的作用 = Evaluating 

the efficacy of planktonic foraminifer calcite 

δ18O data for sea surface temperature 

reconstruction for the Late Miocene. ( 英文 ). 

Williams M; Haywood A M; Taylor S P; Valdes 

P J; Sellwood B W; Hillenbran C-D. Geobios, 

2005, 38(6): 843-863 

This study examines the efficacy of published 

δ 18 O data from the calcite of Late Miocene 

surface dwelling planktonic foraminifer 

shells, for sea surface temperature estimates 

for the pre-Quaternary. The data are from 33 

Late Miocene (Messinian) marine sites from a 

modern latitudinal gradient of 64°N to 48°S. 

They give estimates of SSTs in the tropics/subtropics 

(to 30°N and S) that are mostly 

cooler than present. Possible causes of this 

temperature discrepancy are ecological factors 

(e.g. calcification of shells at levels below the 

ocean mixed layer), taphonomic effects (e.g. 

diagenesis or dissolution), inaccurate estimation 

of Late Miocene seawater oxygen isotope 

composition, or a real Late Miocene cool climate. 

The scale of apparent cooling in the 

tropics suggests that the SST signal of the foraminifer 

calcite has been reset, at least in part, 

by early diagenetic calcite with higher δ 18 O, 

formed in the foraminifer shells in cool sea 

bottom pore waters, probably coupled with the 

effects of calcite formed below the mixed 

layer during the life of the foraminifera. This 

hypothesis is supported by the markedly 

cooler SST estimates from low latitudes—in 

some cases more than 9 °C cooler than present—where 

the gradients of temperature and 

the δ 18 O composition of seawater between sea 

surface and sea bottom are most marked, and 

where ocean surface stratification is high. At 

higher latitudes, particularly N and S of 30°, 

the temperature signal is still cooler, though 

maximum temperature estimates overlap with 

modern SSTs N and S of 40°. Comparison of 

SST estimates for the Late Miocene from alkenone 

unsaturation analysis from the eastern 

tropical Atlantic at Ocean Drilling Program 

(ODP) Site 958—which suggest a warmer sea 

surface by 2–4 °C, with estimates from oxygen 

isotopes at Deep Sea Drilling Project 

(DSDP) Site 366 and ODP Site 959, indicating 

cooler than present SSTs, also suggest a 

significant impact on the δ 18 O signal. Nevertheless, 

much of the original SST variation is 

clearly preserved in the primary calcite 

formed in the mixed layer, and records secular 

and temporal oceanographic changes at the 

sea surface, such as movement of the Antarctic 

Polar Front in the Southern Ocean. Cooler 

SSTs in the tropics and sub-tropics are also 

consistent with the Late Miocene latitude reduction 

in the coral reef belt and with interrupted 

reef growth on the Queensland Plateau 

of eastern Australia, though it is not possible 

to quantify absolute SSTs with the existing 

oxygen isotope data. Reconstruction of an 

accurate global SST dataset for Neogene timeslices 

from the existing published DSDP/ODP 

isotope data, for use in general circulation 

models, may require a detailed re-assessment 

of taphonomy at many sites. 

37

2007010118 

土耳其麦斯特里希特阶 orbitoidal 有孔虫独 

特的形态结构 = Unusual forms of orbitoidal 

foraminifera in the Maastrichtian of Turkey. 

( 英文 ). Görmüs M; Meriç E. Cretaceous Research, 

2000, 21(6): 801-812 

Maastrichtian orbitoidal foraminifera in 

Turkey show a variety of unusual features. 

They include remarkable specimens of their 

reproductive life cycle, lateral chambers 

within the embryo, teratological individuals 

(polyvalence), microboring activity within 

tests, equatorial chamber growth, and conical 

forms. These features provide evidence for 

Maastrichtian orbitoidal foraminiferal systematics, 

biological life cycle, palaeoecological 

conditions and fossilization. The growth of 

lateral and equatorial chambers is thought to 

have been controlled largely by genetic characteristics. 

Microboring activity is the result of 

their fossilization and life relationships with 

other micro-organisms such as Talpinella 

conicularia. Conical forms and polyvalence 

are thought to be related to sedimentological 

characteristics of the palaeoenvironment, such 

as currents. Abnormal growth of the equatorial 

chambers is accepted as one of the main distinguishing 

features of Orbitoides gruenbachensis. 

2007010119 

东北大西洋末次冰期至今深水有孔虫属 

Uvigerina 种的分布规律 = Late Glacial to 

Recent distribution pattern of deep-water 

Uvigerina species in the north-eastern Atlantic. 

( 英文 ). Schönfeld J; Altenbach A V. Marine 

Micropaleontology, 2005, 57(1-2): 1-24 

Phases with massive abundances of 

Uvigerina species recorded in North Atlantic 

deep-sea cores were previously attributed to 

water mass properties or to extended high 

productivity during the last Glacial. We investigated 

the Uvigerina distribution in 53 sediment 

cores and 555 surface samples from the 

north-eastern Atlantic ranging from 30° to 

70°N and 1 to 4410 m water depth. Our results 

showed that Uvigerina pigmea dominated in 

late Pleistocene assemblages whereas 

Uvigerina peregrina and Uvigerina peregrina 

parva were common during the Holocene. 

Uvigerina pigmea lives today in the Gulf of 

Guinea and South Atlantic only (9°N to 17°S), 

but was present up to 54°N during the Last 

Glacial Maximum. The species retreated 

north- and southwards during Termination I 

and disappeared in the north-eastern Atlantic 

off northern Portugal 6100 years ago. 

Uvigerina peregrina and U. peregrina parva 

spread out from isolated occurrences along the 

continental slope off western Iberia at the onset 

of Termination I. Uvigerina peregrina exhibited 

Recent abundance maxima at Goban 

Spur, Plateau des Landes, and the Iberian 

Margin. These areas are subjected to strong 

lateral advection by downslope transport and 

sediment focusing. The actual flux rate of particulate 

organic matter is locally raised by a 

factor of 4 to 5. Comparable flux rates were 

otherwise recorded at U. peregrina maxima 

under the NW-African coastal upwelling regime. 

The Recent distribution of U. pigmea 

and evidence from sediment cores show an 

organic carbon flux of 3.5 g C m − 2 yr − 1 as 

minimum for a sustainable population of this 

species. Alkenone, pigment and planktonic 

foraminiferal records from cores MD952039 

and MD952040 revealed that a spring bloom 

dominated productivity dynamics and a balanced 

food particle composition of haptophyteae 

algae and diatoms were limiting environmental 

factors for U. pigmea during the 

Pleistocene. A widespread change from glacial 

to modern productivity characteristics 

during the last Deglaciation may have triggered 

the early Holocene disappearance of U. 

pigmea from the north-eastern Atlantic. 

2007010120 

Gargano 北部 ( 意大利南部阿普利亚地 

区 ) 早白垩世钙质超微化石和浮游有孔虫 

= Early Cretaceous nannofossils and planktonic 

foraminifera from northern Gargano 

(Apulia, southern Italy). ( 英文 ). Cobianchi M; 

Luciani V; Bosellini A. Cretaceous Research, 

1997, 18(2): 249-293 

The study of two Lower Cretaceous 

stratigraphic sections from northern Gargano, 

Apulia, southern Italy, has shown that the 

classic succession of the Umbria-Marche Basin, 

central Italy, can be extended to the south 

as far as the Gargano Promontory. Here, the 

Cretaceous basinal succession consists of 

three formations: the Maiolica, the Scisti a 

Fucoidi and the Scaglia. Near the margin of 

the platform, the Mattinata Formation with 

frequent gravity-displaced deposits, laterally 

substitutes the Maiolica Formation. According 

to our integrated biostratigraphic data, and in 

agreement with the classic chronostratigraphic 

schemes proposed from the Umbria-Marche 

Basin, the Scisti a Fucoidi of northern Gargano 

correlates with the late part of the early 

Aptian (C. litterariusZonep. p., L. cabriZone) 

to the late Albian (lower part of theP. 

38

achlyostaurionZone andB. breggiensisZone,T. 

praeticinensisSubzone). The occurrence of 

two anoxic episodes, which can be correlated 

with the ‘Urbino level’ and ‘Amadeus segment’ 

of the Umbria-Marche Basin, also 

strongly supports the proposed correlation of 

the two basins. 

2007010121 

关于 Hantken (1868, 1875) 描述的小有孔虫 

种的修订和分布的资料第一部分 : Textulariidae 

科和 Miliolidae 科 = Data to revision 

and distribution of small foraminifera species 

described by Hantken (1868, 1875) Part I, 

Textulariidae and Miliolidae. ( 英文 ). Horvath 

M. Fragmenta Palaeontologica Hungarica, 

2002, (20): 25-42 

Only 40 original specimens of Hantken's 

species remained in Hungarian collections. 

Recently, I have studied 13 species described 

by Hantken. In this work the systematic position, 

diagnosis, stratigraphical range and scanning 

electron microscope photos of these species 

are given. These species belong to the 

Textulariidae and Miliolidae. 

2007010122 

匈牙利古近纪盆地底栖有孔虫五新种 = 

Five new species of benthic Foraminifera 

from the Hungarian Palaeogene Basin. ( 英文 ). 

Ozsvart P. Fragmenta Palaeontologica Hungarica, 

2003, (21): 1-4 

Five new Eocene species of benthic Foraminifera 

are described from 3 boreholes and 

from the classical Upper Eocene section of 

Matyas-hegy, Budapest, Hungary. The new 

species are Textularia tuberosus, Pyrgo mcrostriatus, 

Lagena clava, Epistomaroides costatus 

and Gyroidinoides koestheri. 

2007010123 

关于 Hantken (1868, 1875) 描述的小有孔虫 

种的修订和分布的资料第二部分 : 

Nodosariidae 科和 Vaginulinidae 科 = Data 

to revision and distribution of small Foraminifera 

species described by Hantken 

(1868, 1875) Part II. Nodosariidae and Vaginulinidae. 

( 英文 ). Horvath M. Fragmenta Palaeontologica 

Hungarica, 2003, (21): 5-32 

In this part, the systematic position, dignosis, 

stratigrphical range and scanning electron 

microscope photos of 50 species, designated 

by Hantken, are given. These species 

belong to the Nodosariidae (Dentalina bacilloides, 

D. crassa, D. budensis, D. acuminata, 

D. contorta, D. guembeli, D. semilaevis, 

Grigelis coarctata, Laevidentalina intermedia, 

L. debilis, L. budensis...) 

2007010124 

匈牙利 Transdanubia 地区 Bakony 山脉始 

新世大有孔虫的古群落研究 = Palaeocommunity 

studies on Eocene larger Foraminifera 

of the Bakony Mountains (Transdanubia, 

Hungary). ( 英文 ). Kecskemeti T. Fragmenta 

Palaeontologica Hungarica, 2003, (21): 33-41 

Two of the palaeocommunities are Lutetian, 

two others are Bartonian and one is 

Priabonian. Their reconstruction below is presenting 

the composition, the dominant population, 

the density, the diversity and also the 

relation of nummulits to the most important 

other large foraminifers. Tracing of the 

changes in the palaeocommunides received a 

special respect. From the factors inducing the 

changes, those are dicussed which are connected 

to tectonism, global sea-level changes, 

climate, and water chemistry. Formation of 

the so-called "monospecific" faunas and the 

possible influence of ontogenetic and phylogenetic 

factors, independent from the environment 

are also discussed. 

2007010125 

法国比利牛斯 - 大西洋省 Tardets 地区的古 

新世角砾岩中的浮游有孔虫 = The planktonic 

Foraminifera from the Palaeocene breccias 

of the Tardets area ('Zone des Chainons 

Bearnais', Pyrenees-Atlantiques, France).. ( 法 

文 ). Fondecave-Wallez M J; Peybernes B; 

Combes P J. Comptes Rendus Palevol, 2006, 

5(7): 859-866 

Palaeocene marine breccias, the so-called 

'Etchebar/Bosmendiette breccias', from the 

area of Tardets (Zone des Chainons Bearnais, 

Pyrenees-Atlantiques, France) are interpreted 

as gravitational deposits (debris-flow) overlying 

a folded Jurassic and Early Cretaceous 

carbonate substrate and overlain, in turn, by 

the karstified rims of palaeocanyons, which, 

on the axis of the future range, were excavated 

during the "Laramide" orogenic phase at the 

end of the Cretaceous and the beginning of the 

Palaeocene. We clarify the cartographic, 

sedimentologic and petrographic characteristics 

of these breccias in this paper. 

Early/Middle Palaeocene (Late Danian-Early 

Selandian, P I c-P3 zonal interval) pelagic 

assemblages of 'Globigerinacea' are identified 

from new thin-section samples in their argillaccous 

carbonate rnatrix as well as within 

interbedded hemipelagites. These breccias are 

39

now well known and well dated along the 

Pyrenees from the 'Corbieres' (to the cast) to 

the Marble Thrust Sheet (to the west). The 

hypothesis of their diapiric origin founded on 

their supposed Aptian age must be consequently 

definitely rejected. 

2007010126 

西班牙南部下上新统 Sclerozoan 类有孔虫 

的生物侵蚀结构 : 海洋硬基底群落古生态 

学实证 = Bioerosive structures of Sclerozoan 

Foraminifera from the lower Pliocene of 

southern Spain: a contribution to the palaeoecology 

of marine hard substrate communities. 

( 英文 ). Santos A; Mayoral E. Palaeontology, 

2006, 49(4): 719-732 

A palaeoecological study of sclerozoan 

foraminifera of the families Saccamminidae 

(aff. Sagenina), Lituolidae (Placopsilina), 

Cibicididae (Cibicides, Dyocibicides, Cibicidella) 

and Planorbulinidae (Planorbulina 

and Planorbulinella) that colonized epifaunal 

bivalves (ostreids and pectinids) during the 

early Pliocene in southern Spain has led to the 

recognition of two new boring ichnogenera: 

Camarichnus ichnogen. nov., with two ichnospecies, 

C. subrectangularis ichnosp. nov. and 

C. arcuatus ichnosp. nov., and Canalichnus 

ichnogen. nov., with one ichnospecies, 

C. tenuis ichnosp. nov. The first two ichnospecies 

were produced by adnate lituolids and 

cibicidids, the last by saccamminids. Their 

recognition is very important when quantifying 

populations of these organisms. Colonisation 

took place after death of the host bivalves, 

when they acted as very stable substrates 

whose topography probably controlled the 

initial settlement pattern of the foraminifera. 

The colonisation sequence started with the 

foraminifera (lituolids-saccamminidscibicidids-planorbulinids) 

and was followed 

by vermetid gastropods, serpulids, spirorbids, 

cheilostome bryozoans and/or ostreids. Preferred 

orientations and overgrowth relationships 

between cheilostome bryozoans and serpulids 

have been detected in this material. 

2007010127 

北太平洋地区副热带环流中有孔虫 

Globigerinoides ruber (white) 两种生态型 

的稳定同位素组成 = Stable isotopic composition 

of two morphotypes of Globigerinoides 

ruber (white) in the subtropical gyre in the 

North Pacific. ( 英文 ). Kawahata Hodaka. Paleontological 

Research, 2005, 9(1): 27-35 

Globigerinoides ruber has recently received 

much attention for paleoceanography in the 

subtropical and tropical ocean. G. ruber has 

two morphotypes (G. ruber s.s. and G. ruber 

s.l.) which dwell at the surface layer and at 

deeper depth in the surface water, respectively. 

In order to establish a proxy for the quantitative 

reconstruction of sea surface temperature, 

oxygen and carbon isotopes were analyzed in 

G. ruber collected at 30°N, 175°E in the Pacific. 

Based upon the fluxes of foraminifers 

and organic matter (OM), the entire duration 

of the sediment trap experiment was divided 

into two periods: Period 6A (May to December) 

characterized by low fluxes of organic 

matter and foraminifers under a stratified condition 

of the surface ocean, and 6B (January to 

April) characterized by high fluxes of OM and 

foraminifers under a well developed deepmixing 

layer. With respect to seasonal variability, 

δÔ values of both G. ruber s.s. 

and G. ruber s.l. decreased in summer with a 

minimum around September-October and increased 

in winter and spring, which was also 

the case with their δ^C values. The mean 

difference of δÔ values between both 

morphotypes was 0.25‰ in August-October, 

corresponding to a 1 ℃ difference in water 

temperature. Consistency with field observation 

confirms that G. ruber s.s. and G. ruber s.l. 

dwell at the surface and at 30-50m water 

depth, respectively. In contrast, the difference 

in δÔ and δ^C values between the 

two morphotypes was not significant in early 

April due to deep-mixing. Together with foraminiferal 

assemblage, δÔ values of 

the two morphotypes of G. ruber can be a 

good proxy for quantitative reconstruction of 

vertical seawater temperature in the surface 

ocean. 

2007010128 

沿东经 175° 北太平洋表层沉积物中放射虫 

的分布 = Distribution of radiolarians in North 

Pacific surface sediments along the 175°E 

meridian. ( 英文 ). Motoyama Isao; Nishimura 

Akira. Paleontological Research, 2005, 9(2): 

95-117 

To characterize the biogeography of individual 

radiolarian taxa in relation to latitudinal 

climatic variation across the subtropical to 

subarctic zones, we investigated the spatial 

distribution of radiolarians in surface sediments 

along a 175°E traverse from 19°N to 

48°N in the North Pacific Ocean. Census survey 

and statistical classification of taxa enabled 

us to recognize distinct radiolarian as- 

40

semblages. Most characteristic taxa analyzed 

had restricted biogeographic ranges along the 

north-south traverse; the biogeographic ranges 

and abundance patterns related well to the 

modern oceanography of the upper layer. Water 

masses (subtropical, transitional, and subarctic 

zones) were characterized by abundance 

of certain taxa, and oceanic fronts (Kuroshio 

Extension, Kuroshio Bifurcation, and 

Subarctic Fronts) coincided with limits of species' 

biogeographic ranges and abrupt changes 

of frequency of some taxa. These results offer 

promise for paleoceanographic interpretations 

of sedimentary records that will enhance the 

value of individual radiolarian species as keys 

to past water masses and hydrographic 

boundaries in the North Pacific. 

2007010129 

日本海表层沉积物中的浮游有孔虫 : 它们 

的地理分布及与表层水团的关系 = Japan 

Sea planktic foraminifera in surface sediments 

: geographical distribution and relationships 

to surface water mass. ( 英文 ). Hanako D; 

Motoyoshi O. Paleontological Research, 2005, 

9(3): 255-270 

Modern planktic foraminifera in 51 surface 

sediments from the Japan Sea, a marginal 

sea of the western North Pacific, were studied 

to reveal the relationships between geographical 

distribution and surface water masses in 

the Japan Sea. Twenty-four species belonging 

to 10 genera were identified, of which nine 

species, namely Neogloboquadrina incompta, 

Neogloboquadrina pachyderma, Globigerina 

quinqueloba, Globigerina bulloides, Globigerinoides 

ruber, Neogloboquadrina dutertrei, 

Pulleniatina obliquiloculata, Globigerinoides 

tenellus, and Globigerinita glutinata are predominant. 

We recognized four geographical 

distribution patterns of these dominant species 

that are related to hydrographic conditions in 

the Japan Sea. The transitional water formed 

by the mixture between the warm Tsushima 

Current and cold waters in the Japan Sea is 

optimal for N. incompta, while the distribution 

of N. pachyderma is matched with cold water 

in the northern Japan Sea. Globigerina quinqueloba 

and G. bulloides appear to be associated 

with less saline, nutrient-rich river water 

from the Changjiang (Yangtze River), and G. 

ruber, N. dutertrei, P. obliquiloculata, G. tenellus, 

and G. glutinata can be regarded as indicators 

of Tsushima Current water. 

2007010130 

日本枥木县 Kuzu 地区 Izuru 组及 

Nabeyama 组的中二叠世有孔虫 —— 第一 

部分 : 希瓦格蜓类、新希瓦格蜓类和费伯 

克蜓类 = Middle Permian foraminifers of the 

Izuru and Nabeyama Formations in the Kuzu 

area, Tochigi Prefecture, Japan Part 1. Schwagerinid, 

neoschwagerinid, and verbeekinid 

fusulinoideans. ( 英文 ). Kobayashi F. Paleontological 

Research, 2006, 10(1): 37-59 

The Middle Permian Izuru and Nabeyama 

Formations in the Kuzu area, Tochigi 

Prefecture are composed of thick basaltic 

rocks and fossiliferous partly dolomitized 

limestone. Fusulinoidean biostratigraphy is 

first established in these two formations, and 

the stratigraphic distribution of the 30 species 

of fusulinoideans distinguished from 70 localities 

is shown. The Izuru and Nabeyama Formations 

are biostratigraphically subdivided 

into the lower Parafusulina nakamigawai, the 

middle Parafusulina yabei, and the upper 

Parafusulina tochigiensis zones. The first 

zone is correlated to the Parafusulina nakamigawai 

Zone of the basal part of the Akasaka 

Limestone. The middle part of the third zone 

corresponds to the upper part of the 

Neoschwagerina craticulifera Zone to the 

lower part of the Neoschwagerina margaritae 

Zone of the Akasaka Limestone based on the 

occurrence of Gifuella amicula. More precise 

correlation of the Parafusulina yabei and 

Parafusulina tochigiensis zones will be possible 

when biostratigraphic zonation by schwagerinids 

is made clear in relation to the stratigraphic 

range of neoschwagerinids in Middle 

Permian limestones of the Jurassic terrane of 

Japan. Seven species of Parafusulina including 

two new species, P. shimotsukensis and P. 

tochigiensis, and Pseudodoliolina ozawai and 

Gifuella gifuensis are described and discussed 

herein. 

2007010131 

日本中部 Kuzu 地区 Izuru 组及 Nabeyama 

组的中二叠世有孔虫 —— 第二部分 : 舒伯 

特蜓类、小泽蜓类和非蜓有孔虫 = Middle 

Permian foraminifers of the Izuru and Nabeyama 

Formations in the Kuzu area, Central 

Japan Part 2. Schubertellid and ozawainellid 

fusulinoideans, and non-fusulinoidean foraminifers. 

( 英文 ). Kobayashi F. Paleontological 

Research, 2006, 10(1): 61-77 

Middle Permian Izuru and Nabeyama 

Formations in the Kuzu area, central Japan are 

divisible into three zones based on the strati- 

41

graphic distribution of larger fusulinoideans: 

the lower Parafusulina nakamigawai Zone, 

the middle Parafusulina yabei Zone, and the 

upper Parafusulina tochigiensis Zone. Although 

schubertellid and ozawainellid fusulinoideans 

and non-fusulinoidean foraminifers 

are accessary in comparison with dominant 

schwagerinid fusulinoideans, 56 species assignable 

to 25 genera and a few more indeterminate 

genera are distinguished in these 

three zones. Their taxonomic diversity is very 

low in the lower zone, and becomes higher in 

the middle zone and highest in the upper zone. 

The difference of their variety well agrees 

with lithologic change of limestone in these 

three zones. There are no remarkable differences 

in the faunal composition of schuberteUid 

and ozawainellid fusulinoideans and 

non-fusulinoidean foraminifers between the 

Izuru and Nabeyama Formations and other 

contemporaneous limestones of Japan. The 

similar faunal composition of these groups 

shows a striking contrast to the provinciality 

of the schwagerinids and neoschwagerinids of 

the Izuru and Nabeyama Formations. Six species 

of schubertellid fusulinoideans newly 

proposed herein are systematically described 

and discussed. They are Schuberetellal 

karasawensis, Schubertella minutisphaera, 

Codonofusiella ashioensis, Codonofusiella 

elongata, Codonofusiella nabeyamensis, and 

Dunbarula oviformis. 

古杯、多孔及腔肠动物 

2007010132 

对一些二叠纪三叠纪房室海绵属种的分类 

厘订 = Treatments of some thalamid sponge 

taxa of Permian and Triassic. ( 中文 ). 吴亚生 ; 

范嘉松 . 古生物学报 , 2004, 43(4): 602-608 1 

图版 . 

Ott(196 7) 归入 Cryptocoelia zitteli 的材 

料在房室充填物类型方面与 Cryptocoelia 

zitteli 的模式标本完全不同 , 但又不能归入其 

它属 , 故建立新属 Vermicoelia 。 Senowbari 

Daryan(1990 ) 归入 Cryptocelia siciliana 的材 

料与该属的定义差别很大 , 应改归入 

Guangxispongia Wu。Senowbari -Daryan 和 

Rigby(1988) 归入 Crystothalamia ramosa 的材 

料与该属模式种的水沟系类型不同 , 应改归 

入 Imbricatocoelia 中。 Rigby ,Fan 和 

Zhang(1989) 归入其新种的 

Glomocystospongia gracilis 的材料之一部分 

( 图版 19, 图 5 ) 应改归入 Waagen 和 

Wentzel(1887) 建立的之中 , 即为 Carterina 

gracilis(Rigby ,FanetZhang)。 

2007010133 

贵州台江凯里生物群中遗迹化石 (Gordia) 

与水母状化石 (Pararotadiscus) 的关系及其 

意义 = Relationship between trace fossil gordia 

and medusiform fossils pararotadiscus 

from the Kaili Biota, Taijiang, Guizhou, and 

its significance. ( 中文 ). 王约 ; 赵元龙 ; 林日白 ; 

王萍丽 . 地质论评 , 2004, 50(2): 113-119 

贵州台江凯里生物群中的遗迹化石 

Gordia marina Emmons 常被保存在水母状 

化石 Pararotadiscus guizhouensis Zhao and 

Zhu 盘体的上下 , 构成凯里生物群生态特色 

之一 . 笔者认为 ,G. marina 可能系蠕形类造迹 

动物在层面或近层面觅食或吞食富含有机 

物的沉积物所形成 . 生活于清澈陆棚环境一 

定水域的 P. guizhouensis, 由于突发性快速沉 

积事件的发生 , 改变了海水的物化条件 , 而被 

" 毒死 ", 并随沉积物安静地沉落于弱氧化 - 还 

原环境的海底 . 在较为缓慢的腐烂过程中 , 营 

食沉积物的 G. marina 造迹生物觅食于 P. 

guizhouensis 盘体上下富含有机物的沉积物 

中 . 随着沉积物的增厚 ,P. guizhouensis 生物 

尸体周围的微环境还原性增强 , 腐烂过程很 

快被终止 ,P. guizhouensis 生物软体得以保存 , 

浅层或层面觅食性造迹生物亦随即离去 , 留 

下其生活活动的潜穴 . 同时通过研究 , 还认为 

G. molassica(Heer) 与 G. marina 为同义名 , 可 

能为 G. marina 造迹生物的幼体 . 

2007010134 

华南下 / 中奥陶统界线附近笔石相的分异与 

全球下 / 中奥陶统界线生物标志的选择 = 

The differentiation of graptolite biofacies 

across the Lower/Middle Ordovician boundary 

in South China and the selection of biomarker 

for global Lower/Middle Ordovician 

boundary. ( 中文 ). 王传尚 ; 汪啸风 ; 陈孝红 ; 李 

志宏 . 现代地质 , 2004, 18(1): 89-95 

通过对宜昌黄花场 ( 扬子地台中部 ) 大湾 

组剖面和重庆城口 ( 扬子地台北部 ) 的湄潭抖 

组剖面笔石动物群特征的分析 , 结合江西崇 

义地区 ( 盆地相 )、江南过渡带笔石动物群的 

研究成果 , 讨论了华南下 / 中奥陶统界线附近 

笔石相分异的现象 , 并探讨了下 / 中奥陶统界 

线附近笔石动物和牙形石的相互关系 . 认为 

宜昌黄花场剖面完全具备建立全球下 / 中奥 

陶统界线层型剖面和点 (GSSP) 的条件 , 牙形 

石 B. triangularis 的首次出现 (FAD) 是良好的 

界线生物标志 . 

42

2007010135 

贵州早、中寒武世斗篷海绵科 (Choiidae) 

的发现 = Discovery of the Early and Middle 

Cambrian Choiidae from Guizhou, SW China. 

( 中文 ). 杨兴莲 ; 赵元龙 ; 吴维义 . 微体古生物 

学报 , 2003, 20(3): 286-295 2 图版 . 

本文描述了贵州遵义下寒武统牛蹄塘 

组生物群和台江中寒武世凯里生物群中保 

存完整的斗篷海绵科 (Choiidae) 中斗篷海绵 

(Choia) 和小斗篷海绵 (Choiaella) 化石标本。 

共计 2 属 2 种 2 未定种 :Choia Zunyiensis 

sp. DOV.,Choia sp.,Choiaella ovata 

sp.nov. 和 Choiaella sp.。Choia 分布很 

广 , 在我国下寒武统澄江生物群及北美中 

寒武统的四大生物群中均有产出。 

Choiaella 原仅产于我国澄江生物群。凯里 

生物群中 Choiaella 的发现使其时代上延至 

中寒武世。贵州早、中寒武世斗篷海绵科 

的发现及研究为海绵动物的早期演化及古 

地理学等方面的研究提供了重要的新材 

料。 

2007010136 

华南石炭纪与二叠纪四射珊瑚多样性模式 

= Diversity patterns of carboniferous and 

Permian rugose corals in South China. ( 英文 ). 

Wang Xiangdong; Wang Xiaojuan; Zhang 

Feng; Zhang Hua. Geological Journal, 2006, 

41(3/4): 329-343 

The diversity and changing patterns of 

rugose corals in the Carboniferous and Permian 

of South China are analysed by statistical 

analyses of 45 families, 284 genera, and 

1979 species from 14 consecutive time intervals. 

The ancestors of Carboniferous rugose 

corals originated early and underwent preliminary 

radiation in the late Famennian, but were 

eliminated by the Hangenberg global regressive 

event, which marks the Devonian- 

Carboniferous boundary. Radiation of typical 

Carboniferous rugose corals began in the late 

Tournaisian, when they were represented by 

an abundance of columellate taxa such as 

Kueichouphyllum and a significant diversification 

of Keyserlingophyllum. A decrease in the 

diversity of rugose genera occurred in the Serpukhovian, 

followed by a change in the composition 

of the rugose coral assemblages at the 

Mid-Carboniferous Serpukhovian-Bashkirian 

boundary, where large dissepimented taxa 

with complex axial structures disappeared. In 

the Bashkirian the Serpukhovian taxa were 

replaced by compound rugosan taxa of the 

Geyerophyllidae, Kepingophyllidae and Waagenophyllidae. 

This compositional change was 

associated with a global regressive event, recognized 

in South China by the absence of upper 

Serpukhovian strata in many places and by 

several erosional surfaces in carbonate sequences 

in the Lower Yangtze region. This 

regressive event was probably caused by an 

episode of glaciation in Gondwana. Subsequent 

transgression occurred in South China 

during the early Bashkirian, where a wide, 

uniform shallow-water platform developed in 

South China, on which were deposited tidalflat 

dolostone and pure limestone containing 

compound rugose corals. Another change in 

the rugose coral assemblages, at the Sakmarian-Artinskian 

boundary, resulted in the 

absence from the Artinskian of representatives 

of typical Pennsylvanian and Early Permian 

families such as the Bothrophyllidae, Lithostrotionidae, 

Cyathopsidae, and Petalaxidae. 

Families uniquely typical of the Permian, 

characterized by Waagenophyllidae and Kepingophyllidae, 

dominate post-Sakmarian strata. 

This faunal change may be related to a major, 

worldwide regression, recognized at the end of 

the Sakmarian. Extinction of rugose corals at 

the end of the Permian occurred in two phases 

in South China. The first phase occurred at the 

end of the Capitanian and eliminated 47% of 

the families and 45% of the genera. Extrusion 

of the Omeishan Basalt, which is widely distributed 

in the western part of South China, 

and/or a global regression at the end of the 

Guadalupian could be the principal causes of 

this first phase of mass extinction. The second 

phase, which occurred at the end of the 

Changhsingian and is the largest extinction 

event in Earth's history, eliminated all remaining 

rugose corals. 

2007010137 

古生代层孔虫及群体珊瑚的分类及带内的 

控制 = Classification and controls of internal 

banding in Palaeozoic stromatoporoids and 

colonial corals. ( 英文 ). Young G A; Kershaw 

S. Palaeontology, 2005, 48(3): 623-651 

Palaeozoic corals and stromatoporoids 

exhibit a variety of internal banding phenomena, 

many of which have been commonly interpreted 

as annual growth bands. We evaluate 

bands through analysis of colonial corals and 

stromatoporoids from three stratigraphic intervals: 

Upper Ordovician of Manitoba Canada, 

and Llandovery–Wenlock and Ludlow of 

Gotland, Sweden. Banding features are divided 

into four categories: (1) absence of 

banding; (2) density banding formed by variation 

in density or form of elements; (3) 

43

growth-interruption banding indicating growth 

cessation and regeneration; and (4) postmortem 

banding caused by compaction or 

diagenesis. For discrimination of band types, 

it is essential to examine internal structures 

and skeletal margins in thin sections or acetate 

peels. Species vary considerably in degree and 

type of banding; each has a distinct pattern of 

variation. We propose criteria to determine if 

banding is consistent with seasonally induced 

growth variation: (1) consistency in band 

character and thickness; (2) continuity of 

skeletal growth; (3) marginal features; and (4) 

evidence of diagenetic alteration. Density 

bands in tabulate and rugose corals probably 

represent annual growth variations, but results 

for stromatoporoids are more ambiguous; although 

stromatoporoids commonly show 

banding, unequivocal density banding is 

poorly developed and growth interruption 

generated most stromatoporoid banding. 

Cerioid rugose and tabulate corals possess the 

thickest density bands; the thinnest bands are 

in stromatoporoids and heliolitid tabulates. 

苔藓动物 

2007010138 

外寄生在季节性基质的苔藓虫的冷水碳酸 

岩生产 = Cool-water carbonate production 

from epizoic Bryozoans on ephemeral substrates. 

( 英文 ). Hageman S J; James N P; 

Bone Y. Palaios, 2000, 15(1): 33-48 

Bryozoan skeletons are a dominant constituent 

of cool-water carbonate sediments in 

the Cenozoic of southern Australia. The primary 

substrate on much of the modern continental 

shelf is loose sediment that is reworked 

intermittently to 200+ m water depth by storm 

waves. Availability of stable substrate is a limiting 

factor in the modern distribution of bryozoans 

in this setting. As a result, a significant 

proportion of the sedimentologically important 

modern bryozoans (30–250 m water depth) 

live attached to sessile, benthic invertebrate 

hosts that possess organic or spicular skeletons. 

Hosts such as hydroids, ascidian tunicates, 

sponges, soft worm tubes, octocorals, and 

other lightly-calcified and articulated bryozoans 

provide ephemeral substrates; after 

death, host skeletons disarticulate and decay, 

leaving little or no body fossil record. 

The calcareous sediments produced by 

these epizoic bryozoans from ephemeral substrates 

result in loose particles that rarely preserve 

substratal relationships, but potentially 

retain diagnostic basal attachment morphologies. 

Although the best known examples of 

epizoic carbonate production on ephemeral 

substrates are from the southern Australian 

margin, this may be an important phenomenon 

both globally and in the fossil record. Bryozoan 

sediment production from epizoans on 

ephemeral substrates would seem, however, to 

have a scant record prior to 

2007010139 

东波罗的海中奥陶统两个神秘的苔藓虫属 

= Two Enigmatic Bryozoans from the middle 

Ordovician of the East Baltic. ( 英文 ). Pushkin 

V I; Popov L E. Palaeontology, 2005, 48(5): 

1065-1074 

Two rare, poorly known bryozoan genera 

from the Middle Ordovician (Volkhovian– 

Lasnamägian) of the St Petersburg Region, 

north-west Russia, are revised and redescribed 

based on new finds. Hexaporites fungiformis 

Eichwald, 1860 is redefined as the type species 

of the genus, which is shown to be one of 

the earliest representatives of the suborder 

Halloporina. The bryozoan nature of the 

specimen described and illustrated by Eichwald 

as Nebulipora ovulum is confirmed after 

re-study of a single preserved specimen. However, 

the original concept of this binomen was 

more likely to have been based on a Silurian 

heliolitide coral. Therefore, the name Eichwaldipora 

ovulum gen. et sp. nov. is introduced. 

2007010140 

基于 Frederick M'Coy(1844) 最初描述的爱 

尔兰苔藓虫种确立的窗格苔藓虫属 = Fenestrate 

Bryozoan genera based on species 

from Ireland originally described by Frederick 

M'Coy in 1844. ( 英文 ). Wyse Jackson P N; 

McKinney F K; Bancroft A J. Palaeontology, 

2006, 49(4): 741-767 

A large number of fenestrate bryozoan 

species were named in 'A Synopsis of the 

Characters of the Carboniferous Limestone 

Fossils of Ireland' by Frederick M'Coy (1844). 

At the same time, M'Coy named the bryozoan 

genera Ichthyorachis, Ptylopora and Polypora, 

each of which by monotypy or by subsequent 

designation was based on new species within 

that work. Subsequently, d' Orbigny (1849) 

named Fenestrellina with the type species 

Fenestella crassa M'Coy, 1844 as type species; 

Miller (1961) named Parafenestella with the 

type species Fenestella formosa M'Coy, 1844 

as type species; and Wyse Jackson (1988) 

named Baculopora with the type species Vincularia 

megastoma M'Coy, 1844. We redescribe 

here in more detail than previously 

44

the fenestrate type species originally published 

in M'Coy (1844), provide diagnoses of the 

genera, and compare the nineteenth century 

genera with more recently named genera that 

have been discriminated specifically from 

them. 

腕足动物 

2007010141 

澳大利亚新南威尔士亚斯晚志留世扭月贝 

腕足动物 = Late Silurian strophomenate 

brachiopods from Yass, New South Wales. 

( 英文 ). Strusz D L. Alcheringa, 2003, 27(1/2): 

1-35 

The Yass Syncline succession, of possibly 

late Wenlock and certainly Late Silurian to 

earliest Devonian age, has yielded eleven species 

and subspecies described here, belonging 

to the Superfamilies Strophomenoidea, Plectambonitoidea, 

Chonetoidea and Chilidiopsoidea. 

The scope of the chilidiopsine genus 

Morinorhynchus is discussed, Two species, 

Leptaena compitalis and P (Plectodonta) 

psygmata, are new. Three species, Desistrophia 

papilio, Epelidoaegiria minuta chilidifera 

and Morinorhynchus oepiki, were originally 

described from the late Wenlock to early 

Ludlow of Canberra. Leptaena compitalis is 

also recorded from the Ludlow of Molong in 

central N.S.W. The 17 species originally assigned 

to Stropheodonta by Mitchell are fully 

revised: two are unusable. the others are now 

reduced to four: M. (Mesoleptostrophia) 

quadrata, Mesopholidostrophia bendeninensis, 

Epelidoaegiria minuta minuta, and P. (Plectodonta) 

bipartita. The greatest species diversity 

is in the lower Ludfordian Black Bog Shale 

none of the species originally described from 

Canberra extends above that level. The fauna 

of the upper Ludfordian Rainbow Hill Member 

(basal Rosebank Shale) is also diverse. 

Only two species are common to those two 

units, reflecting environmental differences. 

One of them (Strophochonetes kemezysi) extends 

into the Pridoli, where it is Joined by P 

(Plectodonta) bipartita. No brachiopod species 

is known from the basal Devonian at the 

top of the Yass sequence. 

2007010142 

南美洲一个新的石炭纪腕足动物属 = A new 

Carboniferous brachiopod genus from South 

America. ( 英文 ). Cisterna G A; Isaacson P E. 

Alcheringa, 2003, 27(1/2): 63-73 

Azurduya gen. nov. (Brachiopoda: Camarotoechiidae) 

is described from Early Carboniferous 

sequences in the Argentine Precordillera 

and northern Chile. Marine assemblages 

and the palynoflora associated with this genus 

suggest a Tournaisian age. The type species 

Azurduya chavelensis (Amos, 1958) is reviewed 

and redescribed from material from 

the type locality. Additional material from 

equivalent localities in the Rio Blanco Basin 

(La Rioja and San Juan provinces, Argentine 

Precordilera)has been used to understand ontogenetic 

changes as well intraspecific variation. 

Azurduya cingolanii sp. nov. is proposed. 

2007010143 

阿根廷圣胡安前科迪耶拉 Villicun 山脉 La 

Pola 组早卡拉道克阶腕足动物 = Early 

Caradoc brachiopods from the La Pola Formation, 

Sierra de Villicun, Precordillera of San 

Juan (Argentina).. ( 其他 ). Benedetto J L. 

Ameghiniana, 2003, 40(1): 33-52 

The La Pola Formation consists of debris 

flow deposits with several shell beds near the 

top containing brachiopods and bryozoans. 

Associated graptolites suggest an Early Caradoc 

age (C. bicornis Zone or slightly younger). 

The brachiopod fauna includes the orthides 

Glyptorthis sp., Dinorthis polaensis n. sp., 

Dinorthis cf. flabellulum (J. de C. Sowerby) 

and Onniella inversa n. sp., the triplesiid Bicuspina 

sp., the clitambonitid Atelelasma sp., 

the plectambonitoideans Anchoramena 

cristata Benedetto, Aporthophyla sp., Sowerbyella 

cf. multipartita Williams, Anoptambonites 

villicumensis n. sp., the strophomenoidean 

Glyptomena cf. sculpturata 

Cooper, and the rhynchonellide Rostricellula 

robusta n. sp. Four of the eleven genera recorded 

in the La Pola Formation are also 

known from the coeval Las Plantas Formation 

cropping out in northern Precordillera. The La 

Pola brachiopod assemblage shows closest 

paleobiogeographical affinities with the 

Scoto-Appalachian faunas and lacks typical 

Gondwanan taxa. Some Mediterranean genera, 

however, have been recorded in boulders from 

the overlying Hirnantian glacial diamictite as 

well as in the coeval Las Plantas Formation. 

2007010144 

华南地区石炭纪至三叠纪腕足动物多样性 

模式 = Brachiopod diversity patterns from 

Carboniferous to triassic in South China. ( 英 

文 ). Shen Shuzhong; Zhang Hua; Li Wenzhong; 

Mu Lin; Xie Junfang. Geological 

Journal, 2006, 41(3/4): 345-361 

45

It has long been recognized that the trend 

of marine diversity from the Carboniferous to 

the Triassic includes an approximately 100- 

myr-long stable biodiversity stage ranging 

from the Late Carboniferous to the late Middle 

Permian, the most severe end-Permian mass 

extinction in the Phanerozoic (pre-Lopingian 

crisis and end-Changhsingian mass extinction 

together), a bleak stage in the Early Triassic 

and a rapid recovery stage in the Middle Triassic. 

However, little attention has been paid 

to smaller diversity fluctuations among relatively 

stable stages in the Carboniferous and 

Permian. Here, we establish a database of the 

brachiopod fossil records from the Carboniferous 

to Triassic in South China, including 

104 families, 373 genera, 2081 species recorded 

by 7948 occurrences with relatively 

detailed biostratigraphic controls. Analyses 

based on the raw taxonomic richness at familial, 

generic and specific levels, proportional 

and total extinction/origination/turnover rates, 

and rarefaction analyses for 21 different intervals 

from the Carboniferous to Triassic reveal 

that the brachiopod diversity trends can be 

generally divided into two distinctly different 

stages. Brachiopods were highly diversified 

during the Carboniferous and Permian Periods, 

whereas they were dramatically reduced in 

diversity after the end-Changhsingian mass 

extinction. Brachiopods were abundant during 

the Early Carboniferous Tournaisian and 

Visean, and were characterized by many genera 

extending from the Late Devonian. This 

was followed by a significant simple diversity 

decline in the Serpukhovian Stage. The Early 

Permian (either in Sakmarian or Artinskian) 

diversity decline previously perceived by coral 

and fusulinid workers is indicated by the raw 

generic and familial richness, and taxonomic 

richness per million years. However, it is not 

expressed by the rarefied brachiopod trajectory, 

which is probably affected by sampling 

effect or taxonomic selectivity. Brachiopods 

apparently declined from Capitanian to Early 

Wuchiapingian. Thus, the brachiopod diversity 

trajectory from Pennsylvanian Bashkirian 

to Late Guadalupian Capitanian generally 

characterises a long stable stage. Brachiopods 

are extremely abundant in the Late Wuchiapingian 

and Changhsingian in view of raw 

taxonomic richness, but a rarefied trajectory 

reveals a flat step following the pre-Lopingian 

(end-Guadalupian) crisis until the end- 

Changhsingian mass extinction. Therefore, the 

previously widely perceived Lopingian radiation 

after the pre-Lopingian crisis appears to 

be at least partly over-stated. Brachiopods 

experienced a long bleak stage in the Early 

Triassic, followed by a rapid recovery in the 

Anisian, and reached their acme in the Norian, 

but never recovered to such a flourishing degree 

during the Carboniferous and Permian 

Periods. Brachiopods were eliminated in 

South China by the end-Triassic withdrawal of 

the sea from this region. 

2007010145 

华南早石炭世一新的卫星长身贝腕足类 = 

A new Early Carboniferous micro-productid 

brachiopod from South China. ( 英文 ). 

Balinski A J; Sun Yuanlin. Palaeontology, 

2005, 48(3): 447-454 

We describe Muhuarina haeretica gen. et 

sp. nov. from a recently discovered silicified 

brachiopod fauna from the Lower Carboniferous 

of South China. This new microproductid 

appears to be the oldest representative of the 

highly differentiated, mainly Permian, aulostegoid 

family Cooperinidae. The internal 

structure of the dorsal valve of M. haeretica is 

dominated by strongly developed, pronounced 

subperipheral ridges, which suggest support 

for a simple schizolophe type of lophophore. 

Brachial ridges, as in other productides, most 

probably represent an attachment area of the 

lophophore to the dorsal epithelium. An attempt 

to homologize subperipheral and brachial 

ridges among Cooperinidae is presented. 

2007010146 

东波罗的海奥陶纪 ARENIG–CARADOC 

期小准共凸贝类腕足动物 = Ordovician 

(Arenig–Caradoc) syntrophiidine brachiopods 

from the east Baltic Region. ( 英文 ). Popov L 

E; Egerquist E V A; Zuykov M A. 

Palaeontology, 2005, 48(4): 739-761 

Syntrophiidine brachiopods are a rare and 

poorly known component of Ordovician Baltoscandian 

faunas. They appear in the East 

Baltic in the Billingenian (lower Arenig) as 

part of the earliest known benthic assemblages 

dominated by elements of the Palaeozoic Evolutionary 

Fauna. These faunal assemblages 

usually include bryozoans, ostracodes, and the 

earliest known porambonitoids, strophomenides 

and endopunctate orthides, such 

as Idiostrophia and Orthidium, which later 

became characteristic of the Whiterockian 

brachiopod assemblages in Laurentia, but by 

that time had disappeared from Baltica. The 

superfamily Syntrophioidea reappears in Baltoscandia 

in the mid Caradoc. In contrast, Porambonitoidea 

remained the integral part of 

46

the Baltoscandian brachiopod associations 

through the Ordovician. Porambonites, herein 

redefined on the basis of restudy of the type 

species P. intermedius, includes only smooth 

porambonitoids; taxa with the distinctive ornament 

of radiating rows of pits first appeared 

in the group in the mid Arenig. The taxa Eoporambonites 

gen. nov., Tetralobula peregrina 

sp. nov., Idiostrophia prima sp. nov. and 

Idiostrophia tenuicostata sp. nov. are erected. 

2007010147 

华南贵阳中奥陶统达瑞威尔阶 Kuniutan 组 

硅化小嘴贝型腕足类 = Silicified rhynchonelliform 

brachiopods from the Kuniutan 

Formation (Darriwilian: Middle Ordovician), 

Guiyang, South China. ( 英文 ). Rong Jiayu; 

Harper D; Zhan Renbin; Huang Youzhuang; 

Cheng Jinhui. Palaeontology, 2005, 48(6): 

1211-1240 

A silicified brachiopod fauna from the 

Middle Ordovician Kuniutan Formation 

(lower–middle Darriwilian, i.e. uppermost 

Arenig to lower Llanvirn) at Wudang, Guiyang, 

central Guizhou, South China, includes 

abundant specimens of Yangtzeella, Orthambonites 

and Leptellina together with common 

Parisorthis, Saucrorthis, rare Anomalorthis, 

Hemipronites, Leptestia and, significantly, 

Aporthophyla; associated are rare trilobites, 

gastropods, crinoids and nautiloids. The Yangtzeella 

kueiyangensis-Orthambonites delicata 

Association is defined for this shallow-water, 

Benthic Assemblage 3, association. This first 

record of Aporthophyla in South China may 

indicate a link between South China and the 

Toquima-Table Head Province, where the 

Aporthophyla fauna is more typically developed. 

However, this association is significantly 

different from the latter in having three 

endemic genera, Yangtzeella, Saucrorthis and 

Parisorthis, rare numbers of Aporthophyla 

and Anomalorthis, and the absence of many 

other typical elements of the Aporthophyla 

fauna. The occurrence of Orthambonites, 

Hemipronites and Leptestia suggests some 

relationships between South China and the 

Baltic Platform during the Mid Ordovician. 

The various brachiopod associations bearing 

Aporthophyla may be quite different in nature, 

composition and diversity, and may possess 

different background palaeobiogeographical 

signatures. The assemblages containing 

Aporthophyla in South China, Qaidam, Malaysia, 

Australia and possibly Tibet are clearly 

different biogeographically from those associated 

with the Toquima-Table Head and the 

Celtic provinces. Two new species, Aporthophyla 

sinensis sp. nov. and Leptellina orientalis 

sp. nov. are described. 

2007010148 

英格兰科茨沃尔德中侏罗统一新 

LACAZELLIN THECIDEOID 腕足动物 = 

A new Lacazellin thecideoid brachiopod from 

the Middle Jurassic of the Cotswolds, England. 

( 英文 ). Baker P. Palaeontology, 2005, 48(6): 

1311-1319 

Restudy of the thecideoid fauna from organo-detrital 

residues of Aalenian age from 

two Cotswold localities revealed the presence 

of a rare form assignable to the Lacazellinae. 

Its morphology and shell microstructure enabled 

it to be identified as the earliest clear 

representative of the subfamily and the possession 

of ramuli, jugal pillar, reniform brachial 

lobes and partially suppressed fibrous 

secondary shell layer indicate proximity to the 

rootstock of the Lacazella Munier-Chalmers 

line of descent in a position possibly ancestral 

to Praelacazella Smirnova. In the absence of 

near stratigraphical or geographical relatives 

the Aalenian specimens are assigned to Protolacazella 

scripta gen. et sp. nov. The suppression 

of fibrous secondary shell in P. scripta 

mirrors the phylogenetic suppression of the 

secretion of fibrous secondary shell in the Lacazellinae 

as a whole and may provide an insight 

into the mechanism by which it was 

achieved. 

软体动物 

2007010149 

中国湘南早侏罗世双壳类壳体内的遗迹化 

石 —— 兼论遗迹化石属 Talpina 

Hagenow,1840 = An Early Jurassic Talpinadominated 

assemblage of borings in bivalveshells 

from southern Hunan, China, with remarks 

on the ichnogenus Talpina Hagenow, 

1840. ( 中文 ). Stiller F. 古生物学报 , 2005, 

44(3): 396-411 2 图版 . 

论文描述的双壳类壳体内的钻孔遗迹 

组合发现于湖南省东南部宜章县下坪附近 

的心田门组上部 ( 早侏罗世 , 早辛涅缪尔期 ) 

浅海沉积地层中。这个遗迹化石群中 , 帚虫 

类动物制造的钻孔 Talpina hunanensis ichnosp.nov.( 

新遗迹化石种 ) 明显地占据了大部 

分 , 偶尔共生的其它钻孔包括 :Rogerella ichnosp.( 

蔓足亚纲尖胸类的遗迹 ) 、 

Calcideletrix ichnosp.( 可能是藻类的遗迹 )、 

藻或菌造的遗迹 ( 暂定为 

"Mycelites"ichnosp.)、以及一种可能被海绵 

47

动物制造的未定钻孔。生物侵蚀者侵害了 

海底上较大的双壳类壳体。钻孔保存为天 

然印模 ( 石核 ), 它们是文石质壳体溶解后留 

下的空间中的充填物。此外 , 文中还讨论了 

遗迹化石属 Talpina Hagenow,1840, 尤其讨论 

了有关遗迹种颇为复杂的鉴别问题 , 同时校 

正了该遗迹属的属征。 

2007010150 

藏南定日剖面晚白垩世菊石和叠瓦蛤类的 

首次发现 : 生物地层和古环境意义 = First 

ammonite and inoceramid data from the Upper 

Cretaceous of the Tingri section in SE- 

Tibet: biostratigraphical and palaeoenvironmental 

implications. ( 英文 ). Lehmann J; 

Wendler I; Wendler J; Willems H; Xiumian H. 

地学前缘 , 2005, 12(2): 105-112 1 图版 . 

藏南定日遮普惹山剖面主要是 Albian 晚 

期到古近纪海相沉积 ,Willems 等 (1996) 对岩 

石地层和沉积微相进行了详细研究 , 并通过 

浮游有孔虫研究建立生物地层格架 . 在与岗 

巴地区地层对比基础上 , 该剖面被认为是整 

个藏南地区白垩纪 - 古近纪海相地层的标准 

剖面 .2004 年我们与中国、德国同行一道对 

该剖面上白垩统地层进行再考察 , 重点对无 

脊椎动物化石样品进行采集和研究 . 与西藏 

大多数白垩纪剖面一样 , 尽管沉积环境为陆 

棚环境 , 该剖面以前却几乎没有菊石和叠瓦 

蛤类化石的报道 , 而同样环境下的世界其他 

地区剖面含有大量的菊石和叠瓦蛤类化石 . 

藏南定日剖面重新调查后发现了少量的菊 

石和叠瓦蛤类化石 . 化石数量少一方面是由 

于灰泥质灰岩和泥灰质灰岩内化石保存状 

况差 , 另一方面采样条件也不理想 . 还有 , 当时 

的环境条件可能不利于大多数无脊椎动物 

类群的生存 , 这一点或许从大量存在于岗巴 

群上部的小个体双壳类碎片可以得到证实 . 

尽管获得的化石分散并且保存差 , 本次研究 

仍获得了一些有价值的生物地层数据 . 岗巴 

群上部发现的化石 Calycoceras, 指示其时代 

为 Cenomanian 晚期 , 随后出现不能鉴定的 

desmoceratids 类的幼体 . 之上 , 菊石 Forresteria 

sp. 的发现表明岗巴群顶部地层属于 

Coniacian 下部 , 这被同一地层内发现的其他 

化石所支持 , 包括 Inoceramus (Cremnoceramus)waltersdorfensis 

hannovrensis. Anagaudryceras 

是一个发现于遮普惹山北或遮 

普惹山坡组的菊石 , 相当于 Santonian - 

Maastrichtian 时期地层 . 

2007010151 

罗马尼亚 Transylvanian 盆地 Buituri 产地 

带有表栖动物群的中中新世腹足类壳体 = 

A middle Miocene gastropod shell with epifauna 

from the locality Buituri (Transylvanian 

Basin, Romania). ( 英文 ). Hladilova S; 

Zagorsek K; Ziegler V. Fragmenta Palaeontologica 

Hungarica, 2004, 22(): 99-105 

Abundant epifauna (bivalves, bryozoans, 

sessile worms), settled on gastropod shell 

(Cerithium crenatum ) , was studied from the 

Badenian locality of Buituri. Several epifaunal 

attachment phases were recognized passing 

off partly either during the life of the gastropod 

or at the time when its empty shell was 

approximately in the same position as during 

its lifetime, partly after the death of the gastropod 

when its shell was turned over from the 

life position. Mutual interactions among various 

representatives of sessile benthos colonizing 

the shell were described and interpreted. 

2007010152 

菊石推进运动的起源 = The origin of ammonoid 

locomotion. ( 英文 ). Klug C; Korn D. 

Acta palaeontologica Polonica, 2004, 49(2): 

235-242 

Evolution of the coiled ammonoid conch 

from the uncoiled bactritid conch was probably 

coupled with changes in manoeuvrability 

and swimming velocity. The gradual tranformation 

of uncoiled to coiled ammonoid 

conchs has essential functional consequences. 

The radical change in conch geometry during 

phylogeny but also in ontogeny of early ammonoids 

implies a shift of the aperture from 

an original roughly downward, via a downward 

oblique and an upward oblique to an 

upward orientation, presuming a neutrally 

buoyant condition of the ammonoid animal. 

Similar trends were reconstructed for the three 

main ammonoid lineages in the Middle Devonian, 

the agoniatitid, the anarcestid, and the 

tornoceratid lineages. This allowed an increase 

in manoeuvrability and in the maximum 

horizontal swimming speed. 

2007010153 

中三叠世鹦鹉螺 Germanonautilus 的软体 

组织附着构造和埋藏 = Soft-tissue attachment 

structures and taphonomy of the Middle 

Triassic nautiloid Germanonautilus. ( 英文 ). 

Klug C; Lehmkuhl A. Acta palaeontologica 

Polonica, 2004, 49(2): 243-258 

The attachment structures of the cephalic 

retractor muscle and of the dorsal and the pos- 

48

terior mantle, some with tracking bands, were 

seen in several specimens. The shape and proportions 

of these soft-tissue attachment structures 

resemble those of Recent Nautilus macromphalus 

and indicate similar soft part anatomy. 

A broad range of animals (fish, decapods, 

ophiurans, crinoids, brachiopods, bryozoans, 

bivalves, Spirorbis, foraminiferans) lived in 

and on these compraratively large secondary 

hardground. 

2007010154 

阿根廷中、西部下白垩统 bakevelliid 双壳 

类分类、沉积相关系及其化石古生物学 = 

Taxonomy, facies relationships and palaeobiology 

of bakevelliid bivalves from the Lower 

Cretaceous of west-central Argentina. ( 英文 ). 

Lazo D G. Cretaceous Research, 2003, 24(6): 

765-788 

Cretaceous bakevelliids in Argentina are 

restricted to the Lower Cretaceous. They are 

recorded in shallow marine deposits in two 

Mesozoic basins located in the Andes foothills 

in Patagonia. In the Austral Basin (44°–55°S) 

there is only one genus, Gervillella, represented 

by a single specimen from the Barremian. 

In the Neuquén Basin (30°–40°S) two 

genera, Gervillaria and Gervillella, occur, 

ranging from the Berriasian to the Lower Barremian. 

In the Pilmatué Member of the Agrio 

Formation two species are identified: Gervillaria 

alatior (Imlay) and Gervillella aviculoides 

(J. Sowerby). The former is also recorded 

in Mexico while the latter is more 

widespread, occurring in Europe, Asia, and 

Africa. In the Bajada del Agrio section they 

come from eight tabular shell beds located 

near and on top of shallowing-upwards cycles. 

They were abundant only in four of these levels. 

These shell beds are interpreted as having 

been deposited in the mid-ramp (middle of 

cycles), and upper mid-ramp (top of cycles). A 

functional analysis of shells revealed two life 

habits: epibyssate and endobyssate. 

2007010155 

尼日利亚土伦阶 ( 白垩纪 ) 菊石壳变异的 

形态测量分析 = Morphometric analysis of 

variability in the shell of some Nigerian Turonian 

(Cretaceous) ammonites. ( 英文 ). Reyment 

R A. Cretaceous Research, 2003, 24(6): 

789-803 

An appraisal of studies concerned with 

vascoceratids of the Nigerian Cenomanian– 

Turonian transitional beds, using methods of 

standard multivariate statistical analysis and 

geometric morphometrics, supports the hypothesis 

that at least one species of the Tunisian 

genus Thomasites entered the Nigerian 

realm via the trans-Saharan seaway some time 

in the late Cenomanian. The special suite of 

fluctuating ecological chemical and physical 

factors that pertained in the long, narrow and 

shallow epicontinental sea, with ‘Caspian Sea 

type‘ episodes, favoured ecogenetic consequences 

leading to the appearance of two 

highly variable species of Thomasites, one of 

which is referred to a sub-genus, Bauchioceras; 

both species have a similar norm of 

reaction. Bauchioceras bears a superficial relationship 

to Pseudotissotia, but the two have 

a different ontogeny, are geometric morphometrically 

distinct and lack a proven evolutionary 

connexion. 

2007010156 

中欧马斯特里赫特晚期和丹尼最早期的船 

菊石 : 系统分类 , 演化和灭绝 = Late Maastrichtian 

and earliest Danian scaphitid ammonites 

from central Europe: Taxonomy, evolution, 

and extinction. ( 英文 ). Machalski M. 

Acta palaeontologica Polonica, 2005, 50(4): 

653-696 

In total, thirteen scaphitid taxa are recognised. 

Sexual dimorphism is demonstrated for 

several species. The extinction pattern of 

European scaphitids is difficult to assess for 

methodological reasons. The available data 

indicate, however, that the Hoploscaphites 

constrictus lineage survived unaffected until 

the very end of the Cretaceous and even 

crossed the Cretaceous - Paleogene boundary. 

The successive members of the Hoploscaphites 

constrictus lineage, i. e., Hoploscaphites 

livivensis subsp. nov., H. c. crassus, and H. c. 

johnjagti subsp. nov. are useful for subdivision 

of upper Maastrichtian deposits. 

2007010157 

几个古生代翁戎螺腹足类的壳型和损伤修 

复 = Repaired injuries and shell form in some 

Palaeozoic pleurotomarioid gastropods. ( 英 

文 ). Lindstrom A; Peel J S. Acta palaeontologica 

Polonica, 2005, 50(4): 697-704 

Study of six Palaeozoic pleurotomarioid 

gastropod species with repaired shell injuries 

shows that repaired injuries are dependent on 

both the nature of the selenizone and shell 

form. The species can be divided onto three 

morphological group and show a variety of 

selenizones with different degrees of prominence. 

Turbiniform shells show more repaired 

injuries than planispiral forms, indicating that 

49

species in the former group more often survive 

predatoty attack. The sudied material is too 

sparse for meaningful statistical analysis, but 

individual case studies suggest that the combined 

influence of shell form and the nature of 

the selenizone can make the interpretation 

complex. 

2007010158 

阿根廷 Neuquén 盆地下白垩统菊石 : 欧特 

里夫阶属 Holcoptychites = Lower Cretaceous 

ammonites from the Neuquén Basin, 

Argentina: the Hauterivian genus Holcoptychites. 

( 英文 ). Aguirre-Urreta M B; Rawson 

P F. Cretaceous Research, 2003, 24(5): 589- 

613 

Holcoptychites is known only from the 

Neuquén Basin, Argentina, but appears close 

to the more widespread genera Jeanthieuloyites 

and Spitidiscus. Thus it is placed in the 

subfamily Spitidiscinae (Family Holcodiscidae). 

Previously described Holcoptychites 

species are revised and their taxonomy clarified, 

while one new species is left under open 

nomenclature. The sequence of forms allows 

two subzones to be recognized. These are correlated 

provisionally with the lowest Hauterivian 

Acanthodiscus radiatus Zone of the 

Mediterranean region. 

2007010159 

阿根廷 Neuquén 和 Austral 盆地白垩纪鹦 

鹉螺属 Cymatoceras = The nautiloid genus 

Cymatoceras from the Cretaceous of the Neuquén 

and Austral basins, Argentina. ( 英文 ). 

Cichowolski M. Cretaceous Research, 2003, 

24(4): 375-390 

Until now, Cretaceous nautiloids from 

Argentina have been studied only briefly. 

Here Cymatoceras is described in detail, based 

on specimens found in the Neuquén and Austral 

basins, located in west-central and southern 

Argentina, respectively. Those from the 

Neuquén Basin are of Valanginian–Barremian 

age and belong to a single species, Cymatoceras 

perstriatum (Steuer). Those from the 

Austral Basin range in age from Hauterivian 

to Campanian and represent the first record of 

Cymatoceras from this region. It is represented 

by a new species, Cymatoceras patagonicum 

from the Turonian, and by isolated 

specimens, which are assigned to this genus in 

open nomenclature, owing to their poor preservation 

state; their ages range from Early 

Hauterivian to Early Campanian. 

2007010160 

Prionocyclus germari, 一个印度中部 Bagh 

层的新的晚土伦期标志化石 = Prionocyclus 

germari, a Late Turonian marker fossil from 

the Bagh Beds of central India. ( 英文 ). Kennedy 

W J; Phansalkar V G; Walaszczyk I. 

Cretaceous Research, 2003, 24(4): 433-438 

A specimen of the Late Turonian marker 

ammonite Prionocyclus germari (Reuss, 1845) 

is recorded from the upper Nodular Limestone 

of the Bagh Beds sequence of the Hatni River 

section near Kukshi, Madhya Pradesh Province, 

India. A reappraisal of previous ammonite 

and inoceramid records from the sequence 

shows that these are all compatible with a Late 

Turonian date for the upper Nodular Limestone. 

The higher parts of the Bagh Beds are 

thus securely dated as Late Turonian to Coniacian 

on ammonite and inoceramid evidence. 

2007010161 

基于新材料的 Umzamba 组腹足动物群的 

新的分类学数据 = New taxonomic data for 

the gastropod fauna of the Umzamba Formation 

(Santonian–Campanian, South Africa) 

based on newly collected material. ( 英文 ). 

Kiel S; Bandel K. Cretaceous Research, 2003, 

24(4): 449-475 

From the type section of the Umzamba 

Formation in the Eastern Cape Province of 

South Africa 37 gastropod species are described; 

11 of these are new species, five are 

described in open nomenclature. Two new 

genera are introduced: Schizofusus gen. nov. 

(higher Caenogastropoda) for a shell resembling 

Schizobasis but having a rounded basal 

slope and a straight siphonal canal of moderate 

length, and Muteluma gen. nov. (Turridae) 

for a high-spired, fusiform shell with convex 

and rounded whorls, and a shallow anal sinus 

on the flank of the whorls. The presence of the 

turritellid Spirocolpus in the Umzamba Formation 

suggests a Late Cretaceous Southern 

Hemisphere origin for that group of turritellids 

with a very deep sinus in their growth lines. 

The protoconch of Blackdownia acuticarinata 

is documented and resembles that of the 

Capulidae rather than the Muricidae, where 

Blackdownia had previously been placed. 

Also in shape of the teleoconch, the genus 

resembles the capulid Trichotropis and is, 

therefore, transferred to the Capulidae. The 

type species of the monotypic Pirula (Protopirula) 

is identified as a juvenile cypraeid; 

Protopirula is, therefore, considered synonym 

with Cypraea. The new species are Solariella 

griesbachi, Iravadia (Pseudonoba) ponderi, 

50

Gyrodes (Dockeryella) renniei, Gyrodes (Sohlella) 

woodsi, Blackdownia kollmanni, ‘Calyptraea’ 

primogenita, Galeodea (Taieria) klingeri, 

Trophon umzambiensis, Muteluma convexa, 

Paleopsephaea compacta, Boltenella 

africana, and Schizofusus transkeiensis. 

2007010162 

Jamaica 马斯特里赫特阶 Titanosarcolites 

灰岩厚壳蛤类 Chiapasella 的生物地层和分 

类 = Biostratigraphy and taxonomy of the rudist 

Chiapasella in the Titanosarcolites Limestones 

(Maastrichtian) of Jamaica. ( 英文 ). 

Mitchell S F; Gunter G C. Cretaceous Research, 

2002, 23(4): 473-487 

The taxonomy of the radiolitid rudist 

Chiapasella Müllerried from theTitanosarcolites 

Limestones of Jamaica is revised based 

on the bed-by-bed collection of specimens 

from the Central and Maldon inliers. Two species 

are recognised: Chiapasella radiolitiformis 

Trechmann and C. trechmanni sp. 

nov.C. radiolitiformis is characterised by usually 

one or more costae (two or more infolds) 

in the interband, by the relatively narrow ventral 

band Vb, and by a costal ornamentation of 

strong growth lines and subsidiary vertical 

striations. C. trechmanni is characterised by 

the usual presence of no costae (one infold) in 

the interband, by the relatively wide Vb, and 

by a costal ornamentation dominated by vertical 

striations rather than horizontal growth 

lines. Two zones are recognised in theTitanosarcolites 

Limestones, a lower zone with C. 

radiolitiformis (B and Middle C Beds of the 

Central Inlier) and an upper zone with C. 

trechmanni (D and lower F Beds of the Central 

Inlier; Maldon Limestone, Popkin Shales 

and Vaughansfield Limestone of the Maldon 

Inlier). 

2007010163 

法国东南部 Verrucosum 亚带箭石的灭绝 

和复苏特征 = Extinction and renewal patterns 

among Tethyan belemnites in the Verrucosum 

Subzone (Valanginian) of southeast 

France. ( 英文 ). Janssen N M M; Clément A. 


Significantly higher extinction compared 

to the normal background extinction is noted 

among Tethyan belemnites in the ‘Horizon à 

Neocomiensis’ (the upper part of the Verrucosum 

Subzone). Several genera and species of 

belemnites disappear at the base of this deposit. 

Certain morphological forms are no 

longer found, i.e., species with conical rostra 

and relatively deep alveolae. According to our 

stratigraphical data this extinction event is 

linked to sequence boundary Va 4 (type-1 sequence). 

Of general interest is the appearance 

of the Boreal belemnite Hibolithes 

cf.jaculoides Swinnerton, 1936 after the extinction 

event. One new genus, Mirabelobelus, 

and two new species, M. blainvillei and M. 

orbignyi, are described based on ‘Belemnites 

bicanaliculatus’ de Blainville, 1827. 

2007010164 

土耳其黑海西部 Zonguldak 地区晚阿普第 

期厚壳蛤动物群 ( 分类、生物地层、古环 

境及生物古地理 ) = Late Aptian rudist faunas 

from the Zonguldak region, western Black 

Sea, Turkey (taxonomy, biostratigraphy, palaeoenvironment 

and palaeobiogeography). 

( 英文 ). Masse J P; Fenerci-Masse M; Özer S. 


In the western Black Sea region of Turkey 

(Zonguldak area), Late Aptian rudistbearing 

carbonates (the Cengellidere Formation) 

yielded the following fauna: Toucasia gr. 

carinata - lonsdalei,Pseudotoucasia catalaunica 

, Polyconites verneuili, Horiopleura 

almerae, Eoradiolites plicatus and Eoradiolites 

sp. This assemblage dates the Gargasian 

and has a broad Mediterranean palaeobiogeographical 

significance. Because typical 

African elements are lacking, it is ascribed to 

the European Province, in agreement with 

palaeotectonic regional reconstructions. The 

rudist communities thrived on a mixed, carbonate-siliciclastic, 

coastal ramp facing a basin 

corresponding to the modern Black Sea. 

This mode of occurrence contrasts with the 

classical Urgonian-type flat, platform settings 

of wide extent. 

2007010165 

法国西南部 Charente-Maritime 下白垩统 

琥珀中一个蝼蛄新属新种 ( 昆虫纲 : 直翅 

目 : 蝼姑科 ) = A new genus and species of 

fossil mole cricket in the Lower Cretaceous 

amber of Charente-Maritime, SW France (Insecta: 

Orthoptera: Gryllotalpidae). ( 英文 ). 

Perrichot V; Néraudeau D; Azar D; Menier J J; 

Nel A. Cretaceous Research, 2002, 23(3): 

307-314 

A new deposit of Lower Cretaceous amber, 

found in Charente-Maritime, SW France, 

has yielded an important entomofauna with 

numerous characteristic moist ground arthropods. 

We describe a new genus and species of 

51

mole cricket,Marchandia magnifica gen. et sp. 

nov., in an exceptional state of preservation. 

2007010166 

藏南喜马拉雅地区晚侏罗世 - 早白垩世双壳 

类雏蛤动物群 = The Late Jurassic and Early 

Cretaceous bivalve buchia fauna of Himalaya 

region, South Tibet. ( 中文 ). 夏遵义 ; 白志强 . 

古生物学报 , 2005, 44(4): 494-504 2 图版 . 

藏南喜马拉雅地区晚侏罗世地层中雏 

蛤化石丰富 , 其它化石仅有少量箭石和菊 

石 , 而且属种单一 , 多为地方种 , 无法进 

一步划分和对比 , 因此 , 雏蛤属 

(Buchia) 的组合特征具有重要的地质意 

义。结合菊石 Uhligites 和 Substeuraces, 作 

者在藏南喜马拉雅地区上侏罗统中识别 

出 :1)Buchia concentrica- 

Buchia spitiensis;2)Buchia mosquensis- 

Buchia rugosa;3)Buchia blanfordiana- 

Buchia piochii 等 3 个雏蛤动物组合 ; 在下 

白垩统中识别出 Buchia subokensis 雏蛤动物 

组合 , 其中 ,Buchia mosquensis- 

Buchia rugosa 组合为证明拉弄拉地区存在 

晚侏罗世晚基末利期至早提塘期地层提供 

了新的证据 , 并与斯匹提地区、北美等地 

区进行了动物群和地层的对比 , 初步探讨 

了本区雏蛤动物群在生物地层方面的研究 

价值。 

2007010167 

台湾南投县中寮乡中新统鹦鹉螺动物群 = 

Studies on the Miocene nautiloid fauna from 

Chunglioshiang, Nantou prefecture, taiwan. 

( 中文 ). 陶锡珍 ; 胡忠恒 . 古生物学报 , 2005, 

44(4): 567-583 4 图版 . 

鹦鹉螺动物群产于台湾南投县中寮乡 

大坑溪谷源头 , 化石埋藏于中部中新世石 

门层。石门层主要为青灰色厚层中至细粒 

砂岩 , 夹有深灰色页岩及砂页岩薄互层 , 

岩层含石灰质 , 致密坚硬 , 主要含鹦鹉 

螺、腹足类、双壳类 , 其它则有螃蟹、藤 

壶、海胆、鲨鱼牙齿、鱼类、腕足类 , 以 

及小化石等。化石种类多且含量丰富 , 自 

成一个完整的动物群落 , 尤以鹦鹉螺及翁 

戎螺为其特产 , 可称为一个特殊而独立的 

化石生物群 , 特命名为鹦鹉螺动物群。 

2007010168 

日本手取群研究的新进展 = New advance in 

researching on the Tetori Group of Japan. ( 中 

文 ). 陈金华 ; 小松俊文 . 古生物学报 , 2005, 

44(4): 627-635 

介绍日本中生代晚期手取群研究的最 

新进展 , 并简要评述与中国的对比。手取 

群从下到上分为九头龙亚群、石微白亚 

群、赤岩亚群。庄川地区九头龙亚群御手 

洗组新发现菊石 , 属 Tithonian-Berriasian 

期 , 改变了以往 Callovian 期的传统意见。 

石微白亚群发现菊石 , 属 Late Hauterivian- 

Early Barremian 期 ; 亚群上部发现海相双壳 

类 , 属 Hauterivian 期 , 半咸水相和淡水双壳 

类也与外带 Hauterivian 期的对比 ; 绝对年龄 

测定为 135±7Ma 和 128±8Ma , 分别属 

Hauterivian 早期和 Barremian 早期 , 其中 

135Ma 被普遍接受 ; 植物群反映的古气候 

特征与俄罗斯东部 Valanginian-Hauterivian 

期温湿化一致。石微白亚群的时代综合为 

Valanginian-Hauterivian 期。赤岩亚群的 

Trigonioides ( Wakinoa ) tetoriensis 也发现 

于外带 , 时代属 latest Hauterivian-Early Barremian 

期 ; 绝对年龄测定数据不稳定 , 自 

127±8Ma ( Barremian 中期 ) 至 106±7Ma 

( Albian 中期 )。对亚群的 Nippononaia 

ryosekiana 作了修订 , 认为应属 N. linhaiensis 

, 与浙江馆头组的同种 , 比濑林组 

(Lower Aptian) 的 N.ryosekiana 原始 , 故 

时代早于 Aptian 期。赤岩亚群的时代综合为 

Barremian 期 , 但不排除上延的可能。区域 

对比结果认为 , 中国东北龙爪沟群及绥滨 

地区的相当地层可与九头龙亚群和石微白 

亚群对比 ; 馆头组、下城子组可与赤岩亚 

群对比 ; 热河群上部沙海组 - 阜新组煤系地 

层可与石微白亚群对比 ; 并对义县组的时 

代提出了看法。 

2007010169 

阿尔卑斯下白垩统 ( 北部 Calcareous 

Alps, 上奥地利 ) 巴列姆阶原位口盖 = In 

situ finds of aptychi in the Barremian of the 

Alpine Lower Cretaceous (Northern Calcareous 

Alps, Upper Austria). ( 英文 ). Lukeneder 

A; Tanabe K. Cretaceous Research, 2002, 

23(1): 15-24 

Lower Barremian deposits (KB1-B) of 

Upper Austria yield some extraordinarily preserved 

ammonoids withLamellaptychus -type 

lower jaws in their body chambers. The ammonoids 

with in situ lower jaws are referable 

toKarsteniceras ternbergense sp. nov. This 

new occurrence was detected during palaeoecological 

and sedimentological studies at 

an outcrop in the Ternberg Nappe in Upper 

Austria. The jaw apparatuses are found in situ 

or in an isolated condition but are associated 

with a mass-occurrence of the genus Karsten- 

52

iceras, which contributes 91% of the total 

ammonite fauna. Most of the lower jaws are 

flattened, but their characteristic mode of occurrence 

with conchs of the Tethyan ammonoidKarsteniceras 

allows their use as indicators 

of palaeobiogeography, palaeobathymetry and 

palaeoecology. 

2007010170 

西印度 Kutch 贝利阿斯期 ( 早白垩世 ) 

pleurotomariid 类 ( 腹足纲 ) 的两个新种和 

最大的 Bathrotomaria = Two new pleurotomariid 

(Gastropoda) species, including the 

largest Bathrotomaria, from the Berriasian 

(Early Cretaceous) of Kutch, western India. 

( 英文 ). Das S S. Cretaceous Research, 2002, 

23(1): 99-109 

The Mesozoic pleurotomariids have a 

wide biogeographic distribution in shallow 

seas. Cenozoic pleurotomariids, however, are 

biogeographically more restricted and are occupants 

of deep-sea rocky substrates. This 

radical ecological shift is also reflected in 

shell morphology and the Mesozoic and Cenozoic 

forms have long been recognized as 

different genera. Attempts to synonymize the 

Tertiary and Recent forms with the Mesozoic 

genus Pleurotomaria Defrance, 1826 have 

been based on a few homeomorphic characters. 

Pleurotomaria sensu stricto became extinct 

during the Early Cretaceous. Recent molecular 

data are consistent with living forms belonging 

to a single clade, Perotrochus Fischer, 

1885, with extant species having diverged 

after the Eocene. Hence Pleurotomaria, is reevaluated 

here as an essentially Mesozoic genus 

and thus is disqualified from the status of 

a living fossil. It shows wide interspecific diversity, 

which has prompted workers to subdivide 

the genus into several subgenera. A new 

subgenus, Indomaria is described, its type 

species, P. (I.) umiensis sp. nov. being from a 

Lower Cretaceous deposit in western India. In 

addition, one new species of the related genus 

Bathrotomaria Cox, 1956, i.e., B. brihattama 

sp. nov., believed to be largest, is also described 

from the same horizon and locality. 

2007010171 

埃及西奈山西部 Wadi Sudr 地区科尼亚克 

阶 - 桑托阶 Matulla 组 Plicatulid 双壳类 = 

Plicatulid bivalves from the Coniacian– 

Santonian Matulla Formation, Wadi Sudr, 

western Sinai, Egypt. ( 英文 ). El-Hedeny M M; 

Aal A A A; Maree M; Seeling J. Cretaceous 

Research, 2001, 22(3): 295-308 

The Coniacian–Santonian Matulla Formation, 

Wadi Sudr, Egypt contains an assemblage 

of the marine shallow-water bivalve 

Plicatula. A total of ten species of this genus 

are described of which four are new: Plicatula 

sinaiensis, P. sinnbishris, P. somarisensis and 

P. sudrensis. In addition, one further possible 

new species from the same strata is mentioned. 

All species are of Tethyan character and are 

true representatives of Plicatula and not of the 

closely related genus Harpax, which is associated 

with high-latitude and cool-water regions. 

Plicatulids characterize the shallower marine 

biofacies in the Coniacian of Wadi Sudr and 

reflect the principal shallowing events during 

the Late Cretaceous in the region. 

2007010172 

南部高纬度地区晚白垩纪菊石生物地理格 

局 : 南极的 Kossmaticeratidae 科 = Patterns 

of Late Cretaceous ammonite biogeography in 

southern high latitudes: the family Kossmaticeratidae 

in Antarctica. ( 英文 ). Olivero E 

B; Medina F A. Cretaceous Research, 2000, 

21(2-3): 269-279 

A refined biostratigraphy of the Antarctic 

kossmaticeratids from the James Ross Basin is 

contrasted against other Upper Cretaceous 

sections around southern Gondwana to inspect 

for possible biogeographic patterns. In the 3- 

km-thick Marambio Group two major unconformities 

are recognized at the base of the upper 

Campanian and Maastrichtian, respectively. 

The unconformities divide the succession 

into a Santonian–lower Campanian Sequence 

(NS); an upper Campanian–lower 

Maastrichtian Sequence (NGS); and a Maastrichtian–Danian 

Sequence (MGS). Natalites 

in the NS;Neograhamites - Gunnarites in the 

NGS; and Maorites - Grossouvrites in the 

MGS are the most abundant kossmaticeratid 

ammonites, represented in parts by hundreds 

or thousands of specimens. Comparison of the 

Antarctic fauna with that of eastern South Africa, 

Madagascar, southern India, Australia, 

New Zealand and southern South America 

suggests three diversification phases for the 

Kossmaticeratinae and Brahmaitinae, occurring 

in different places at different times in 

southern Gondwana. Early diversification of 

the Kossmaticeratinae started in the Santonian 

of eastern Gondwana and continued into the 

early Campanian of southern high latitudes. 

Five kossmaticeratid genera, including the 

relatively long-ranging Maorites and Grossouvrites, 

and a low-endemic ammonite fauna 

are recorded. The NS/NGS unconformity 

53

marks a major faunal change and the early 

disappearance in Antarctica of several mollusc 

groups that are known to range into the Maastrichtian 

in lower latitudes. Within the NGS, a 

new late Campanian–early Maastrichtian diversification 

phase took place in southern high 

latitudes and five Kossmaticeratinae, mostly 

endemic to the Weddellian Province, were 

added. Finally, the Maastrichtian NGS/MGS 

unconformity marks a drastic reduction of 

Weddellian Kossmaticeratinae, with only 

Grossouvrites and Maorites reaching the topmost 

Maastrichtian in Antarctica. By contrast, 

the Maastrichtian of eastern Gondwana saw a 

final diversification phase, with three new 

Brahmaitinae (present also in the Northern 

Hemisphere) and the persistence of five Campanian–early 

Maastrichtian Weddellian Kossmaticeratinae. 

The pattern of successive low 

endemism in the early Campanian NS, earlier 

exclusion of lower latitude Maastrichtian 

groups and higher endemism in the late Campanian–Maastrichtian 

NGS, and drastic diversity 

decrease in the Maastrichtian MGS, is 

consistent with known calcareous microfossil 

biogeography and long-term cooling in southern 

high latitudes. During the final Maastrichtian 

diversification, the kossmaticeratids 

spread toward lower latitudes as a stenothermal 

group of ammonites moving toward their 

preferred seawater temperature. 

2007010173 

巴西 Sergipe 盆地塞诺曼期的牡蛎 = Cenomanian 

oysters from the Sergipe Basin, Brazil. 

( 英文 ). Seeling J; Bengtson P. Cretaceous 

Research, 1999, 20(6): 747-765 

Cenomanian (mid Cretaceous) oysters 

from the Sergipe Basin in northeastern Brazil 

are described, with revisions of previously 

described forms. Nine genera and subgenera, 

including eleven species, are distinguished: 

Rastellum diluvianum (Linné, 1767), Amphidonte 

(Ceratostreon) reticulata (Reuss, 1846), 

A. (Ceratostreon) flabellata (Goldfuss, 1833), 

Exogyra (Costagyra) olisiponensis Sharpe, 

1850, Ilymatogyra (Afrogyra) africana (Lamarck, 

1801), Rhynchostreon (Rhynchostreon)mermeti 

(Coquand, 1862), R. 

(Laevigyra) obliquatum (Pulteney, 1813), R. 

(Laevigyra) sp., Pycnodonte (Phygraea) 

vesiculosa (J. Sowerby, 1823), Curvostrea 

rouvillei (Coquand, 1862) and Ambigostrea sp. 

No undoubted Turonian oysters are known 

from Sergipe, althoughR. (R.) mermeti possibly 

straddles the Cenomanian–Turonian 

boundary. This is in sharp contrast with the 

situation in the more northerly Brazilian basins, 

from where several Turonian but no 

Cenomanian forms have been described. 

Well-preserved material from Sergipe confirms 

the close relationship between Exogyra 

(Costagyra) Vialov andVultogryphaea Vialov. 

The palaeobiogeographical affinity of the oyster 

fauna is typically Tethyan with many taxa 

that are known particularly from the southern 

Tethys. The inferred palaeoenvironment as 

implied by the oysters is that of a shallow 

shelf. 

2007010174 

西非 Iullemmeden 盆地晚白垩纪菊石属 

Libycocerasin 及其古地理学意义 = The 

Late Cretaceous ammonite genus Libycoceras 

in the Iullemmeden Basin (West Africa) and 

its palaeogeographical significance. ( 英文 ). 

Zaborski P M; Morris N J. Cretaceous Research, 

1999, 20(1): 63-79 

The ammonite species Libycoceras 

crossense Zaborski occurs in the Late Campanian 

part of the Nkporo Shale of southern 

Nigeria and in the (mid to Late) Maastrichtian 

Farin Doutchi and Dukamaje formations 

of the Iullemmeden Basin in western 

Niger and north-western Nigeria. After an 

interval during which Libycoceraswas able to 

migrate between southern Nigeria and the 

western Chad Basin, northern and southern 

populations of L. crossensebecame isolated 

from one another during the Late Campanian 

by closure of the connecting route through the 

Benue Trough.Libycocerasevolved rapidly in 

southern Nigeria but disappeared from the 

region early in the Maastrichtian. The northern 

population of L. crossense persisted, being 

introduced into the Iullemmeden Basin during 

a gradual westerly shift of marine environments. 

During the later part of the Maastrichtian 

a regression brought about the disappearance 

of the species here. A subsequent 

Maastrichtian transgressive pulse introduced L. 

ismaelisinto the Iullemmeden Basin from the 

north, through a seaway located to the west of 

the Adrar des Iforas. 

2007010175 

内蒙古宁城道虎沟地区中侏罗世非海相双 

壳类 Ferganoconcha = Non-marine ferganoconcha 

(bivalvia) from the Middle Jurassic 

in daohugou area, ningcheng county, Inner 

Mongolia, China. ( 中文 ). 姜宝玉 . 古生物学 

报 , 2006, 45(2): 259-264 

54

Ferganoconcha 是广泛分布于我国北 

部、中亚、西伯利亚和乌拉尔地区下、中 

侏罗统的一类非海相双壳类。 

Ferganoconchasibirica 的产出表明道虎沟地 

区道虎沟层与辽西地区的海房沟组和冀北 

地区的九龙山组层位相当 , 时代介于早侏 

罗世晚期至中侏罗世之间。结合昆虫和叶 

肢介化石反映的时代 , 认为道虎沟层的时 

代可能为中侏罗世早一中期。综合近年来 

在 Ferganoconchidae 的分类方面取得的进 

展 , 对 F.sibirica 进行了重新厘定。 

2007010176 

加拿大洛基山脉南部侏罗纪 Fernie 组新的 

具生物地层意义的菊石化石 = New, biostratigraphically 

significant ammonites from 

the Jurassic Fernie Formation, southern Canadian 

Rocky Mountains. ( 英文 ). Hall R L. Canadian 


555-570 

Jurassic ammonites described here for the 

first time come from numerous localities in 

the Fernie Formation in the Foothills and 

Front Ranges of the Rocky Mountains of 

north- and south-eastern British Columbia and 

central- and south-western Alberta, and provide 

useful new age data for several members 

of the formation. The occurrence of Orthodactylites 

sp. in the uppermost beds of the Red 

Deer Member indicates this unit extends upwards 

into the basal Toarcian, which will be 

helpful in the search for carbon-isotope excursions 

associated with the early Toarcian anoxic 

event. The presence of Hettangian and 

lower Pliensbachian strata in outcrop of the 

Gordondale Member is confirmed. Diversity 

of the ammonite fauna in the Grey Beds is 

enlarged by the presence of Kepplerites - 

Cadomites and Choffatia spp. These faunas 

also provide biostratigraphic constraints for 

carbon- and oxygen-isotope trends and U-Pb 

ages recently recorded from the Highwood 

Member and Grey Beds exposed in Bighorn 

Creek and its eastern tributary, and in Fording 

River. The first occurrence of Zemistephanus 

richardsoni from cratonic rocks, recorded here, 

suggests close proximity of the allochthonous 

terranes Wrangellia and Stikinia, the only 

other areas from which this species is known, 

to the northwest North American craton by 

early Bajocian time. One new species, Cardioceras 

(Sub vertebriceras) ferniensis, is described. 

2007010177 

西班牙东南部坎帕阶和马斯特里赫特阶的 

菊石 = Campanian and Maastrichtian ammonites 

from southeast Spain. ( 英文 ). Martínez R. 


The Campanian and Maastrichtian ammonite 

fauna from the Internal Prebetic (Betic 

Range), Alicante province, southeast Spain, is 

systematically described and figured for the 

first time. The species identified are Brahmaites 

(Anabrahmaites) vishnu, Pseudokossmaticeras 

brandti, Pachydiscus (Pachydiscus) 

colligatus, P. (P.) neubergicus, P. (P.) gollevillensis 

and Hoplitoplacenticeras rejaudryi. 

2007010178 

南极最年轻的 inoceramid 双壳类 = The last 

inoceramid bivalves in Antarctica. ( 英文 ). 

Crame J A; Luther A. Cretaceous Research, 

1997, 18(2): 179-195 

The last inoceramid bivalves in Antarctica 

are no younger than mid- to late Campanian 

in age. They occur within the Herbert 

Sound and Rabot Point members of the Santa 

Marta Formation, which is the lowermost of 

four component formations within the Late 

Cretaceous-earliest Tertiary Marambio Group, 

James Ross Basin. These inoceramids comprise 

an unusual giant form which is assigned 

herein toAntarcticeramus rabotensisgen. et sp. 

nov. Moderately inequivalve and gryphaeoid 

in form,Antarcticeranusis characterized by a 

larger and more inflated right valve with a 

rounded-trapeziform to obliquely elongated 

outline. Almost all right valves have a sharply 

defined, shelf-like anterior margin. The left 

valve is less obviously obliquely elongated 

and only weakly inflated. Ornament appears to 

have consisted of low, commarginal folds. 

There are indications of a possible phylogenetic 

connection between Antarcticeramusand 

SphenoceramusJ. Böhm, 1915. Antarcticeramus 

rabotensisgen. et sp. nov. is extremely 

abundant at certain levels within the Rabot 

Point Member. It can be demonstrated that the 

majority of these specimens occur in life position 

and show a preferred orientation with 

respect to a horizontal substrate. This is taken 

as evidence of a positive response to prevailing 

water currents (rheotaxis), perhaps to enhance 

the process of filter feeding. Associated 

sparse macrofossils and abundant trace fossils 

indicate aerobic bottom conditions at midshelf 

depths. 

It is postulated that the evolution of giant 

size was primarily an antipredatory device. 

However, just as large, benthic predators were 

radiating in the latest Cretaceous, seawater 

55

temperatures in the southern high latitudes 

were beginning to fall. In the end, secretion of 

such large calcitic shells may have become 

physiologically impractical. 

2007010179 

早白垩纪粘合扇贝 = Early Cretaceous cementing 

pectinid bivalves. ( 英文 ). Harper E 

M; Radley J D; Palmer T J. Cretaceous Research, 

1996, 17(1): 135-150 

Large thick-shelled cementing pectinids, 

variously described as Prohinnites, are conspicuous, 

if not abundant, epifaunal bivalves 

in shallow marine facies deposited in a range 

of Tethyan and Southern Temperate locations 

during the Early Cretaceous. The relationships 

between these bivalves and Jurassic members 

of the genus Eopecten, some individuals of 

which were able to cement to hard substrata, 

have previously been unclear. The recent discovery 

of well preserved specimens of Prohinnites 

in the Aptian Perna Beds Member of 

the Isle of Wight has allowed a re-examination 

of Early Cretaceous cementing pectinids and 

description of their morphology and shell microstructure. 

Comparisons with Middle and 

Upper Jurassic cementing Eopecten have 

shown that the Cretaceous Prohinnitesare 

closely but not directly related. It is probable 

that these taxa represent multiple evolution of 

the cemented habit from a well pre-adapted 

Eopecten-group of byssally attached pectinids. 

2007010180 

印度西部大陆架翼足目表层沉积物的分布 

模式 = Distribution patterns of recent pteropods 

in surface sediments of the western continental 

shelf of India. ( 英文 ). Singh A D; 

Nisha N R; Joydas T V. Journal of Micropalaeontology, 

2006, 24(part 1): 39-54 

This paper is the first contribution to the 

knowledge of pteropods in surficial sediments 

of the entire western continental shelf of India. 

Both qualitative and quantitative analyses of 

pteropod assemblages were carried out on 50 

coarse fractions (> 125 mu m) of topmost portions 

of grab samples recovered along 12 transects 

covering the inner shelf to the upper 

slope (30-200 m water depths). The distribution 

of eight significant species was mapped. 

The resultant maps were correlated with the 

bathymetric, hydrographic and aragonite preservation 

conditions in the investigated area. 

This study reveals a bathymetric control over 

the distribution of Limacina inflata, Creseis 

acicula and Creseis chierchiae across the shelf. 

Furthermore, a marked difference in vertical 

salinity gradient from south to north along the 

shelf appears to have a profound influence on 

the abundance of these species. The pteropod 

shells in sediments of the northern offshore 

region with anoxic bottom conditions are generally 

well preserved, unlike the southern region, 

where oxygen concentration of the bottom 

water is relatively high enough to cause 

dissolution or even elimination of many shells 

of the most susceptible pteropods like C. 

acicula and C. chierchiae. The variation in the 

intensity of the oxygen minimum zone along 

the western continental shelf of India has significant 

influence upon the distribution pattern 

of Clio convexa. 

2007010181 

阿根廷丘布特巴塔哥尼亚石炭纪和二叠纪 

双壳类 : 第二部分 : 马雷蛤科、 

polidevciidae、肌束蛤科和迭瓦蛤科 = Carboniferous 

and Permian bivalves from Patagonia 

(Chubut, Argentina). Part II: Families 

malletidae, polidevciidae, myalinidae and 

inoceramidae. ( 英文 ). Pagani M A. 

Ameghiniana, 2004, 41(4): 271-288 

A thorough systematic analysis is performed 

on the bivalve fauna of the Upper Paleozoic 

of the Tepuel-Genoa Basin (Chubut 

province, Argentina). This second part comprises 

the Families Malletidae (part), 

Polidevciidae, Myalinidae and Inoceramidae. 

Abundant well preserved specimens allowed 

the recognition of two new species: Phestia 

regularis nov. sp. and Phestin sabattinae nov. 

sp. Two new records of Quadratonucula sp. 

and Atomodesma (Intomodesma) sp. are included 

too. On the basis of new material from 

the Tepuel-Genoa Basin, the diagnoses of 

Quadratonucula argentinensis Gonzalez, 

Quadratonucula parva Gonzalez, Phestia 

tepuelensis Gonzalez, Phestia sp. II, Phestia sp. 

III, and Naiadites teckaensis Gonzalez are 

emended. In addition, the descriptions of these 

previously known species are supplemented 

by new information and their geographical 

ranges are expanded. 

2007010182 

巴哈马 San Salvador 岛晚更新世礁相软体 

动物群的稳定性 = Stability of Late Pleistocene 

reef mollusks from San Salvador Island, 

Bahamas. ( 英文 ). Gardiner L. Palaios, 2001, 

16(4): 372–386 

Stability of Cenozoic reefs has been 

documented previously by assessing stability 

of coral assemblages; however, the stability of 

56

other components of reef communities, such 

as mollusks, is unknown. To investigate 

whether reef mollusks form stable associations 

of species, mollusks from a reef decimated by 

brief sea-level fall within the Sangamon interglacial 

were compared to those of the reef that 

reassembled when sea level returned (after 

1100–1500 years) at Cockburn Town, San 

Salvador Island, Bahamas. Additionally, to 

investigate whether mollusks within reefs 

were unique to that environment, assemblages 

from fossil reefs were compared to the assemblage 

of the adjacent subtidal carbonate-sand 

facies. 

A total of 54 species and 4832 individuals 

were observed within twenty-one quadrats 

of both reefs and the subtidal sand. Taphonomic 

alteration was documented to determine 

if taphonomic histories were similar. 

Taxonomic composition of assemblages was 

compared with Detrended Correspondence 

Analysis. To test whether reef mollusk assemblages 

were distinctive and recurring, 

MANOVA tests were performed on transformed 

data with rare taxa excluded. Two null 

hypotheses were evaluated: (1) H o : there is no 

difference in mollusks from different reef 

building episodes, suggesting stability; and, to 

test if assemblages from reefs are unique, (2) 

H o : there is no difference in mollusks from 

reefs and subtidal sands. 

Reef mollusk assemblages from different 

periods of reef building were not significantly 

different. Additionally, reef mollusks formed 

unique assemblages that were distinct from 

those of adjacent subtidal sand areas. Taphonomic 

differences between deposits were 

minor. Reef mollusks followed the same pattern 

of stability that has been documented for 

coral assemblages over longer time intervals. 

Therefore, despite community reassembly 

during the late Pleistocene, mollusks associated 

with the reef communities show evidence 

of stability. 

2007010183 

阿根廷早侏罗世双壳类 Kalentera 及其古 

生物地理意义 = Early Jurassic Kalentera 

(Bivalvia) from Argentina and its palaeobiogeographical 

significance. ( 英文 ). Damborenea 

S E. Ameghiniana, 2004, 41(2): 185-198 

The Triassic-Early Jurassic genus Kalentera 

belongs to a bivalve group which was 

diverse and widely distributed during Late 

Palaeozoic times (family Kalenteridae). The 

family survived the Permo-Triassic crisis but 

only represented by a few genera, and Kalentera 

lingered into the Jurassic to become extinct 

at the end of the Early Jurassic (Toarcian). 

A new species of Kalentera from latest 

Sinemurian - early Pliensbachian deposits of 

Mendoza and Neuquen provinces is described 

herein. The species is restricted to siltstones 

and fine-grained sandstones. These substrate 

conditions seem to have been the main limiting 

factor to their distribution. These conditions 

agree with the occurrences of species of 

this genus in New Zealand, Nevada and Chile. 

Shell morphology suggests that Kalentera species 

were semi-infaunal or superficial infaunal. 

At Las Chilcas, Mendoza, the locality which 

yielded most of the specimens, the species is 

associated to other superficial infaunal bivalves 

(such as Grammatodon and Palaeonucula), 

to epifaunal bivalves (Otapiria, limoids 

and pectinoids) and to ammonoids. Kalentera 

was regarded as endemic to the Maorian Province, 

and indeed the genus was restricted to 

that biochore during the Late Triassic. From 

the Triassic/Jurassic boundary onwards, the 

distribution of the genus is clearly bipolar, 

being apparently absent from Tethys. Kalentera 

is characteristic to the austral biochore as 

recognized on the bases of bivalve distribution 

during the Early Jurassic. The new species 

from the Neuquen Basin has a stratigraphical 

range restricted to the Otapiria neuquensis 

bivalve Assemblage Zone, and to the Miltoceras 

and Dubariceras Zones of the local biostratigraphic 

scale. 

2007010184 

阿根廷丘比特巴塔哥尼亚石炭纪和二叠纪 

双壳类。第一部分 : 介绍、栗石蛤科和马 

雷蛤科 = Carboniferous and Permian bivalves 

from Patagonia (Chubut, Argentina). Part I: 

Introduction, families Nuculidae and Malletidae. 

( 其他 ). Pagani M A. Ameghiniana, 2004, 

41(2): 225-244 

A thorough systematic analysis on the 

bivalve fauna of the Upper Paleozoic of the 

Tepuel-Genoa basin (Chubut province, Argentina) 

is performed. This first part comprises 

the families Nuculidae and Malletidae. (in 

part); based on abundant well preserved 

specimens. Seven species were regonized, of 

which two are new: Nucidopsis (Nuculopsis) 

teckaensis nov. sp. and Palaeoneilo gonzalezi 

nov. sp. Two new records, of Nuculopsis (Nuculopsis) 

sp. and Palaeoneilo sp. are also included. 

On the basis of new material from the 

Tepuel-Genoa Basin, the diagnoses of Nuculopsis 

(Nuculopsis) patagoniensis Gonzalez 

and Nuculopsis (Nuculanella) camachoi Gon- 

57

zalez are emended and the description of Palaeoneilo 

amosi Gonzalez is supplemented by 

new information, and their geographical 

ranges are expanded. 

2007010185 

阿根廷圣胡安埃拉杜拉河 Tupe 组二叠纪双 

壳类 = Permian bivalves from the Tupe Formation 

in the Herradura Creek, San Juan 

Province. ( 法文 ). Sterren A F. 

Ameghiniana, 2004, 41(1): 57-74 

A taxonomic analysis of bivalves from 

the Tupe Formation in the La Herradura Creek, 

located on the western flank of Perico Hill, 

about 20 km northeast of Jachal, San Juan 

province is carried out. Nine species are described 

and figured: Nuculavus levatiformis 

(Walcott), Phestia sp. aff. P. bellistriata (Stevens), 

Modiolus (Modiolus) sp., Septimyalina 

sp., Palaeolima retifera (Shumard), Aviculopecten 

sp., Streblocbondria sp., Schizodus 

sp., and Pleurophorella sp. An Early Permian 

age is suggested for the studied bivalves 

in view of their occurrence along with 

brachiopods belonging to the Tivertonia 

jachalensis-Streptorhynchus inaequiornatus 

Zone. Some genera with tethyan affinities are 

recognized among the bivalves present in this 

biozone. These genera suggest relatively 

higher temperatures than those previously inferred 

for the region at that time. The paleogeographic 

context is analyzed, and the possible 

influential factors upon the faunal composition 

are briefly discussed. 

2007010186 

华南地区奥陶纪头足类生物相及其分区 = 

Ordovician cephalopoda biofacies and their 

provincialization in the South China. ( 中文 ). 

肖传桃 ; 龚文平 ; 罗顺社 ; 何幼斌 ; 李艺斌 . 沉积 

学报 , 2006, 24(2): 242-250 

在研究华南地区奥陶纪头足类生态特 

征基础上 , 根据头足类的生态类型及其保 

存条件等特征 , 识别出 18 个头足类生物 

相 , 即开阔台地 Proterocameroceras 生物 

相 , 局限台地 Pseudoectenolites- 

Xiadongoceras 生物相 , 开阔台地 

Retroclitendoceras-Pararetroclitendoceras 生 

物相 , 开阔台地 Pronajaceras- 

Mamagouceras 生物相 , 陆棚斜坡 - 盆地 

Cyclostomiceras-Bactroceras 生物相 , 开阔 

台地 Cameroceras-Cyrtovaginoceras 生物 

相 , 开阔台地 Coreanoceras-Manchuroceras 

生物相 , 陆棚斜坡 - 盆地 Kaipingoceras- 

Kyminoceras 生物相 , 内陆棚 Bathmoceras- 

Protocycloceras 生物相 , 中部陆棚 

Dideroceras-Ancistroceras 生物相 , 深水陆 

棚 Lituites-Cyclolituites 生物相 , 滞流盆地 

Lituites-Trilaclnoceras 生物相 , 深水盆地 

Paraendoceras-Sactorthoceras , 深水陆棚 

Sinoceras-Michelinoceras-Disoceras 生物 

相 , 深水陆棚 Beloitoceras-Jiangshanoceras 

生物相 , 深水陆棚 - 盆地 Eurasiaticoceras 生 

物相 , 浅海陆棚 - 斜坡 Jiangxweras- 

Yushanoceras 生物相 , 深水盆地 

Michelinoceras 生物相 , 并阐述各生物相的 

组成、生态特征及其生态环境。根据头足 

类生物相在时间和空间上的组合规律 , 划 

分出 3 个头足类生物相区 , 即扬子生物相 

区、黔东 - 湘西生物相区 ( 过渡型生物相 

区 ) 和湘中 - 浙西生物相医 , 并讨论了各生 

物相区在不同时期内头足类生态类型和生 

物相分异特征、海平面升降、环境演变特 

征以及其与油气的关系。认为在低海平面 

或海平面下降阶段中生物相分异明显 , 丽 

在高海平面阶段中则分异较小。 

2007010187 

昆明地区早寒武世关山动物群研究新进展 

= New advances in the study of the Early 

Cambrian Guanshan fauna in the Kunming 

area, Yunnan,China. ( 中文 ). 李勇 ; 陈良忠 ; 罗 

惠麟 ; 傅晓平 ; 胡世学 ; 尤霆 ; 刘琦 . 地质通 

报 , 2006, 25(3): 415-418 

总结了昆明地区关山动物群自 1999 年 

命名以来开展的研究工作和取得的新进 

展。简要叙述了关山动物群的研究概况、 

地层位置、生物群组合特征和关山动物群 

的研究意义。在关山动物群中首次发现了 

古虫动物门的 Vetulicola ganggtoucunenisis 

Luo,Fu et Hu, 吐卓虫 Tuzoia sp.nov., 

古蠕虫 Palaeoscolex sp . nov ., 腕足类 

Heliomedusa sp.nov. 及三叶形虫、海绵 

动物新属种。指出关山动物群是一个由多 

门类软躯体后生动物化石组成的伯吉斯页 

岩型的动物群 , 时代介于澄江动物群与凯 

里动物群 ( 或伯吉斯页岩动物群 ) 之间 , 

起到了承前启后的作用 , 在寒武纪生命大 

爆发和寒武纪早期生物演化的研究中有重 

要意义。 

2007010188 

青藏高原兴措湖腹足类壳体同位素组成特 

征与环境意义 = Environmental signals deduced 

from the shells of freshwater snails 

Xingcuo Lake in the Tibetan Plateau, China. 

58

( 中文 ). 吴敬禄 ;Andreas Lucke; 李世杰 ; 王苏 

民 . 古生物学报 , 2003, 42(2): 292-296 

通过对青藏高原东部兴措湖腹足类 

Gyraulus sibirica 壳体同位素的分析 , 并与 

器测气象资料的相关研究 , 建立兴措湖同 

位素记录与对应的降水和气温间的函数关 

系。对区内 200 年来的温度序列进行定量 

恢复 , 结果表明 , 青藏高原东部兴措湖地 

区腹足类生物壳体主要在温季生长 , 它所 

记录的是温季而不是全年的气候环境信 

息 ;Gyraulus sibirica 壳体 δ 18 O 指标与温季 

滑动平均温度明显为正相关系 , 相关系数 

为 0.89;δ 13 C 指标与温季的降水量呈正相 

关系 , 相关系数 0.71; 近 200 年来研究区 

温度变化有 3 个明显的阶段 , 其中 20 世纪 

初的低温期温度比目前平均低 3.7℃。 

2007010189 

长江源区晚三叠世伟齿蛤科 ( 双壳类 ) 一 

新属 —Quemocuomegalodon = A new genus 

Quemocuomegalodon of megalodontidae from 

the Upper Triassic in the Source area of the 

Yangtze River, western China. ( 中文 ). 姚华舟 ; 

沙金庚 ; 段其发 ; 牛志军 ; 曾波夫 ; 张仁杰 . 古生 

物学报 , 2003, 42(3): 393-407 4 图版 . 

记述青海唐古拉山北坡雀莫错附近晚 

三叠世甲丕拉组灰岩中的一类铰齿构造特 

殊的伟齿蛤类化石 , 建立新属 

Quemocuomegalodon gen. nov . 及 

Q . orientus gen . et sp . nov . 和 

Q.longitatus gen.et sp. nov.2 新种 , 并简述 

伟齿蛤类的生活习性。 

2007010190 

中生代海相双壳类 ( 软体动物 ) 的漂浮与 

假漂浮 = Plankton and pseudoplankton of the 

marine Mesozoic bivalves. ( 中文 ). 沙金庚 . 古 

生物学报 , 2003, 42(3): 408-416 

中生代很多海相足丝固着和粘结固着 

的表栖双壳类有着广泛的、甚至全球的地 

理分布 , 有些种能够穿越赤道 , 跨越特提 

斯海 , 进行南、北高纬度生物群的交流 , 

有些种能够由东向西横渡浩瀚的古太平洋 

进行扩散 , 因为这些双壳类幼虫期的浮游 

异养型幼虫能营漂浮生活 , 而幼虫期后的 

个体又能挂系或粘结在其它漂浮或移动的 

物体上进行假漂浮迁移。 

2007010191 

早寒武世梅树村期软舌螺壳孔沟系统的初 

步研究 = Preliminary research on tubular pore 

system of Early Cambrian Meishucunian Hyolith 

conch. ( 中文 ). 冯伟民 . 古生物学报 , 2003, 

42(4): 585-589 1 图版 . 

对滇东会泽雨碌、寻甸摆宰早寒武世 

梅树村期软舌螺壳质微细结构的研究表 

明 , 软舌螺壳的孔沟系统十分发育 , 壳的 

外层由分叉与合并呈纵向排列的长纤束组 

成 , 内层由横向分布的粒束组成。在外层 

纤束之间和纤束内分布有大量的三角形或 

长椭圆形的孔洞 , 这些孔洞的长轴平行于 

壳的生长方向 ; 在内层粒束之间或粒束内 

有横向分布的长沟。内外层的沟孔可以相 

通。在一些软舌螺纵向和横向的切片中 , 

均发现早期磷酸岩化作用中已被磷质颗粒 

充填的孔沟形态 , 这些孔沟分布相当密 

集 , 基本垂直壳面 , 几乎通达壳壁的顶 

底。多孔性的壳既反映了软舌螺对其特殊 

的生理和生态功能的要求 , 也反映了早期 

带壳动物的原始性和它们在早期生物矿化 

作用中的特殊地位。 

2007010192 

新疆乌什下寒武统肖尔布拉克组软舌螺化 

石 = Hyoliths from the Lower Cambrian Xiaoerbulakr 

Formation of Wushi, Xinjiang. ( 中 

文 ). 钱逸 ; 李国祥 ; 朱茂炎 ; 尹恭正 . 微体古生 

物学报 , 2003, 20(4): 342-349 1 图版 . 

首次描述了采自新疆乌什县乌什磷矿 

肖尔布拉克组中部 Kepingaspis- 

Tianshanocephalus 带中的 2 个软舌螺新种 

Conotheca xinjiangensis sp. nov. , 

Nitrocornus wushiensis sp. nov. 和下部 

Ushbaspis 带中的 1 个软舌螺未定种 

Adyshevithecasp.。这些软舌螺化石材料 

为研究新疆乌什地区下寒武统中部地层与 

邻区相当层位的对比提供了新的证据 , 认 

为肖尔布拉克组中部 2 个三叶虫化石带和 

其中的软舌螺化石相当于我国扬子地台下 

寒武统沧浪铺阶中部 , 即乌龙箐亚阶和红 

井哨亚阶之间 , 可与俄罗斯西伯亚利和哈 

萨克斯坦下寒武统波特姆阶 (Botomian) 

中的三叶虫带 Ushbaspis 和软舌螺带 

Erraticornus-Nitorcornus 带对比。 

2007010193 

南沙群岛永暑礁泻湖南永 3 井晚全新世微 

型双壳类 = Late Holocene microbivalves of 

Core Nanyong-3 in Yongshu Reef Lagoon of 

the Nansha Islands, South China Sea. ( 中文 ). 

蔡华伟 ; 蓝琇 ; 冯伟民 . 微体古生物学报 , 2003, 

20(4): 389-406 5 图版 . 

59

南沙群岛永暑礁泻湖南永 3 井取岩屑 

样 88 个 , 均有丰富的微型双壳类。本文描 

述了该井 1680 年以来的微型双壳类 24 属 

26 种 , 包括 1 新种 Philobrya(Neocardia) 

xishaensis Lan,Cai et Feng sp. nov.。13 个 

种为南沙群岛海区首次记录。该井微型双 

壳类以 Condylocuna flemingyi Maxwell 最为 

丰富 ,Borniopsis ariakensis Habe,Cadella 

semitorta ( Reeve ) , Wallucina 

(Wallucina)xishaensis Lan 为常见种。该 

动物群以热带、亚热带分子为主 , 亦见有 

热带 - 温带的分子 , 显示了典型的热带岛礁 

双壳类动物群特征。同时也发现一些澳大 

利亚和新西兰的分子 , 表明西太洋经向暖 

流对于双壳类的跨纬度分布起着重要的作 

用。本区双壳类以生活于潮间带和潮下带 

的生表栖息型为主 , 悬食型和食沉积物型 

几乎各占一半。 

2007010194 

贵州凯里生物群中软舌螺的初步研究 = 

Preliminary research on hyolithids from the 

Kaili Biota, Guizhou. ( 中文 ). 陈笑媛 ; 赵元龙 ; 

王萍丽 . 微体古生物学报 , 2003, 20(3): 296- 

302 1 图版 . 

本文描述了采自贵州台江县革东镇八 

郎中寒武世凯里生物群中的软舌螺化石 , 计 

有 1 种 ,3 相似种和 1 个未定种。即 : Ambrolinevitus 

cf. ventricosus, Glossolites sp., 

Haplophrentis cf. carinatus, Linevitus 

opimus, Hyolithes cf. cariniferus。凯里生物 

群中软舌螺特点是 :1) 壳体通常较大 , 呈宽 

锥形 ;2 ) 背、腹壳区分明显 , 常具中槽或中 

脊 ;3) 特别是以软舌螺目中的软舌螺科和线 

带螺科的软舌螺保存数量最多。完全与欧 

洲、北美相当层位中出现的软舌螺组合面 

貌相似 ; 并与澄江动物群中的软舌螺在演化 

特征上是可衔接的。凯里生物群中的软舌 

螺除具有世界性属种外 , 还具地区特有的属 

种。这对研究软舌螺的地理分布、演化进 

程以及与凯里生物群组合关系有重要意 

义。 

2007010195 

哈萨克斯坦一个新的奥陶纪喙壳类软体动 

物 = A new Ordovician rostroconch mollusc 

from Kazakhstan. ( 英文 ). Popov L E; Cope J 

C W; Nikitin I F. Alcheringa, 2003, 27(3/4): 

173-179 

The rostroconch mollusc Eopteria aiteneria 

sp. nov. is described from the Late Ordovician 

Angrensor Formation of northeastern 

Central Kazakhstan it is the first and 

only known representative of this group from 

the Ordovician of central Asia. By the beginning 

of the Late Ordovician Eopteria and the 

family Eopteriidae were on the verge of extinction 

and the new Kazakhstan species 

represents the youngest preserved record of 

the family in the Ordovician. It is likely that 

the group found a refuge in the diverse, but 

rather conservative, faunal assemblage of the 

Hiberno-Salairian type associated with Late 

Ordovician carbonate algal build-ups and mud 

mounds which spread widely during the late 

Caradoc to mid Ashgill across Kazakhstanian 

volcanic island arcs and microplates. 

2007010196 

西澳大利亚坎宁盆地晚泥盆世腹足类 = 

Late Devonian gastropods from the Canning 

Basin, Western Australia. ( 英文 ). Cook A G; 

Blodgett R B; Becker R T. Alcheringa, 2003, 

27(3/4): 181-207 

Frasnian and Famennian gastropods from 

the Canning Basin, Western Australia, constitute 

one of the most diverse Late Devonian 

gastropod faunas known, with 28 taxa, including 

four new genera and 14 new species. This 

is the first formal description of Famennian 

gastropods from Australia. New genera described 

are the pleurotomarioids Tasselliana 

australis gen. et sp. nov., Playfordia australis 

gen. et sp. nov. and Westralospira dickinsi gen. 

et sp. nov., and the platyceratid Cancelloplatyceras 

abowsheri gen. et sp. nov. New 

species described are Retispira christinae, 

Euconospira nodosa, Mourlonia teichertensis, 

Baylea teicherti, Euryzone hullensis, Hesperiella 

canningensis, Brokenriveria virginensis, 

Gyronema minutiforma, Roemeriella 

alticonus and Palaeozygopleura canningensis. 

The plexus of nodose and lirate Devonian gyronernatines 

continues through the Late Devonian, 

exemplified by Brokenriveria and 

Pseudoplagiothyra. The range of Brokenriveria 

is here extended from Givetian to Famennian. 

Conspicuously and oddly ornamented 

Murchisonia also extended into the Late Devonian 

following the Early-Middle Devonian 

radiation of such forms. The absence of large 

numbers of Platyceras (sensu stricto) continues 

to be a feature of eastern Australian faunas 

during the Devonian, but strong links to the 

Old World Realm Faunas are evident. 

2007010197 

澳大利亚维多利亚 Otway 盆地古新世 - 始新 

世界线 Trochocyathus-Trematotrochus 带 

60

的宏体古生物学 = Macropalaeontology of 

the Trochocyathus-Trematotrochus band (Paleocene/Eocene 

boundary), Dilwyn Formation, 

Otway Basin, Victoria. ( 英文 ). Stilwell J D. 

Alcheringa, 2003, 27(3/4): 245-275 

Our limited knowledge of latest Paleocene 

and earliest Eocene Australian macrofaunas 

is much reduced with the report here of 

37 species of invertebrates and vertebrates 

from coastal outcrops of the Dilwyn Formation 

in the Otway National Park, Victoria. The 

Trochocyathus-Trematotrochus band in the 

lowermost part of the Dilwyn Formation has 

yielded the highest taxonomic diversity in the 

formation, with 29 species of shallow marine 

bivalves, gastropods and scaphopods, along 

with less common brachiopods, echinoderms 

and cnidarians, and sparse vertebrate remains 

(shark teeth, otoliths). At least seven (possibly 

ten) molluscan species are common to the underlying 

Pebble Point Formation. Four new 

species are the gastropods Drepanocheilus 

(Tulochilus) retisurus sp. nov., Cerithiella 

leptopyrga sp. nov., Volutomitra (Waimatea) 

dilwyni sp. nov. and Mauidrillia otwayensis sp. 

nov. Eight probably new taxa are: Euspira sp. 

nov., Nassaria sp. nov., Odostomia sp. 

nov., Circulus sp. nov., Proximitra sp. nov. 

cf. R trirugulata Darragh, 1997, Microvoluta 

sp. nov., Dentalium sp. nov. and Trematotrochus 

sp. nov. All macroinvertebrate species 

are, on present knowledge, endemic to Victoria, 

with the exception of Parvamussium sp. 

which is known from Western Australia. 

2007010198 

南极阿尔布期菊石 Aioloceras 属 = The Albian 

ammonite Aioloceras Whitehouse in 

Antarctica. ( 英文 ). Medina F A; Riccardi A C; 

Ghiglione M. Alcheringa, 2003, 27(1/2): 85- 

91 

The first record of the Albian ammonite 

Aioloceras is documented from the Kotick 

Point Formation, James Ross Island, northern 

Antarctic Peninsula. The material is identified 

with the type species, Aioloceras argentinum 

(Bonarelli, 1921), previously only known 

from southern Patagonia. It is associated with 

Desmoceras sp., Anagaudryceras sp., Parasilesites 

sp., Rossalites sp. and Phyllopachyceras 

sp. On the basis of this assemblage, the 

presence of the Aioloceras argentinum Assemblage 

Zone from Patagonia, which is considered 

coeval to the upper lower Albian 

Mammillatum Superzone, is extended to Antarctica. 

2007010199 

美国阿巴拉契亚盆地北部宾西法尼亚纪非 

海相双壳类序列、古生态、演化和物种形 

成 = Succession, palaeoecology, evolution, 

and speciation of Pennsylvanian non-marine 

bivalves, Northern Appalachian Basin, USA. 

( 英文 ). Eagar R M C; Belt E S. Geological 

Journal, 2003, 38(2): 109-143 

Seventeen horizons of non-marine bivalves 

are described within the Appalachian 

succession from the base of the Pottsville 

Group of Westphalian A-B age to the Uniontown 

coal of Stephanian C age at the top of 

the Carboniferous System. A new highly variable 

fauna of Anthraconaia from the roof 

shales of the Upper Freeport coal near Kempton, 

west Maryland, dates from late Westphalian 

D or very early Cantabrian time, on 

the evidence of non-marine shells and 

megafloras. Below this horizon, the Appalachian 

sequence reveals zones of Anthraconauta 

phillipsii and Anthraconauta tenuis in 

the same order as in Britain, whereas faunas of 

Anthraconaia of these zones are less common 

and differ from those of Britain. In all horizons 

above the Upper Freeport coal all nonmarine 

bivalve faunas consist of stages in the 

sequences of two natural species, the groups 

of Anthraconaia prolifera and Anthraconaia 

puella-saravana. The first shows evidence of 

having lived in well-oxygenated, probably 

shallow, fresh water conditions of relatively 

wide extent. The second group lived preferentially 

in a plant-rich environment of relatively 

stagnant fresh water. Both groups are found in 

horizons associated with coal seams and may 

be seen together in the same habitats, but diagrams 

of variation (pictographs) suggest that 

there was no interbreeding between the two 

groups in either the Northern Appalachians or 

in southern Germany where the species split 

was first recognized. In the northern Spanish 

coalfields of Guardo-Valderrueda and Central 

Asturia, facies evidence suggests how an initial 

split may have taken place in the same 

morphological directions and into the same 

palaeoenvironments as the later split into two 

species. 

Appalachian deposition was generally 

slow and intermittent with frequent palaeosols. 

There is also evidence of erosion and of small 

palaeontological breaks in the sequence, especially 

near the eastern edge of the Northern 

Appalachian Basin in western Maryland. The 

amount of accumulated sediment was less 

than one-tenth of that of western Europe when 

basin centre deposition is compared. We 

61

found no evidence of a major palaeontological 

break representing Westphalian D strata overlain 

by Stephanian C strata. We figure nonmarine 

bivalve faunas of Stephanian B age in 

association with the Pittsburgh and the Little 

Pittsburgh coals. Two new species of nonmarine 

bivalves are described: Anthraconaia 

anthraconautiformis sp. nov. and Anthraconaia 

extrema sp. nov. Copyright (C) 2003 

John Wiley Sons, Ltd. 

2007010200 

长江源各拉丹冬地区上三叠统巴贡组沉积 

特征及菊石生物群 = Sedimentary characters 

and ammonoid fauna from the Upper Trassic 

Bagong Formation in the Geladandong area of 

the source land of the Yangtze River. ( 中文 ). 

牛志军 ; 徐光洪 ; 马丽艳 . 地层学杂志 , 2003, 

27(2): 129-133,137 1 图版 . 

上三叠统巴贡组分布于长江源各拉丹 

冬地区南北两侧 , 南部靠近羌塘盆地中央隆 

起带 , 沉积环境为三角洲至浅海相 , 陆源物 

资供应丰富 , 以砂岩沉积为主 , 地层厚度 

大。北部雀莫错一带沉积环境为陆棚相 , 陆 

源物资供应相对较少 , 以泥质岩、灰岩沉积 

为主 , 生物丰富 , 沉积古地理格局显示出南 

浅北深的特点。在雀莫错一带采集了大量 

的菊石化石 , 建立 N odotibetites cf. nodosus- 

Paratibetites cf. wheeleri 组合 , 生物组合所反 

映的地质时代为诺利早 — 中期 , 与藏南珠穆 

朗玛峰地区、藏北唐古拉山地区及青海玉 

树地区同期地层中的菊石生物群可以很好 

对比。 

2007010201 

乌拉圭海相全新世软体动物组合 : 组分、 

地质年代和古环境意义 = Molluscan assemblages 

from the marine Holocene of Uruguay: 

composition, geochronology, and paleoenvironmental 

signals. ( 英文 ). Martinez S; Rojas 

A; Ubilla M; Verde M; Perea D; Pineiro G. 

Ameghiniana, 2006, 43(2): 385-397 

Dates of marine Holocene molluscs from 

Uruguay (Villa Soriano Formation) range 

from 6849 to 1858 cal. years BP. There are no 

significative gaps among the different ages 

obtained, with the exception of the interval 

2276-2830 calculated years BP. Two kinds of 

concentrations are distinguished: autochthonous, 

for which a low energy depositional environment 

is inferred, and parautochthonous, 

deposited in foreshore and nearshore highenergy 

environments. Results of different 

types of multivariate analyses on presenceabsence 

and abundance data show that only 

three localities are clearly differentiated from 

the others. The discrimination of two of them 

(Arazati, Las Cafias) is explained by the presence 

of only one or two species, but the third 

(Punta Rasa) is the only one where characteristic 

species of rocky or hard substrates are 

undoubtedly represented. Analyses of salinity 

and temperature ranges of the various mollusc 

assemblages suggest a displacement of the Rio 

de la Plata estuary about 300 km westwards 

along the Uruguayan coast from its present 

position, and the presence of warmer waters 

than those found today at the same latitude. 

With the exception of the currently northwards 

displaced Anomalocardia brasiliana 

(Gmelin), Marshallora nigrocincta (C.B. Adams), 

Nioche subrostrata (Lamarck), Bulla 

striata Brugulere and Miralda sp., all species 

are present today at the Uruguayan coast. 

2007010202 

阿根廷丘布特巴塔哥尼亚石炭纪和二叠纪 

双壳类。第四部分 :Aviculopectinidae, 

Deltopectinidae 和 Schizodidae = Carboniferous 

and Permian bivalves from Patagonia 

(Chubut, Argentina). Part IV: Families Aviculopectinidae, 

Deltopectinidae and Schizodidae. 

( 其他 ). Pagani M A. Ameghiniana, 2006, 

43(2): 461-476 

A thorough systematic analysis is performed 

on the bivalve fauna of the Upper Paleozoic 

of the Tepuel-Genoa Basin (Chubut 

Province Argentina), as a contribution to the 

knowledge of early Permian faunas of Argentina. 

This fourth part comprises the families 

Aviculopectinidae, Deltopectinidae and 

Schizodidae, of which abundant well preserved 

specimens allowed the recognition of 

three new species, Limipecten herrerai nov. 

sp., Streblopteria lagunensis n. sp. and Streblopteria 

minuta n. sp. Two new records of 

Aviculopecten sp. and Aviculopecten sp. are 

included too. On the basis of new material 

from the Tepuel-Genoa Basin, the diagnoses 

of Orbicidopecten parma Gonzalez and 

Schizodus paucus Gonzalez are emended. In 

addition, the descriptions of these and other 

previously known species are supplemented 

by new information and their geographical 

ranges are expanded. Detailed comparisons of 

all species with taxa from other regions are 

also provided. A new record of Schizodus sp. 

is discussed too. 

62

2007010203 

阿根廷圣胡安省 La Delfina 河 Tivertonia 


生物带述评 = A review of the Tivertonia 


biozone in La Delfina Creek, San Juan Province, 

Argentina. ( 英文 ). Cisterna G A; Sterren 

A F; Archbold N W. Ameghiniana, 2006, 

43(2): 487-491 

2007010204 

阿根廷西北部早奥陶世特马豆克阶双壳类 

畸铰亚纲新科 Ucumariidae = Ucumariidae 

new family (Bivalvia, Anomalodesmata) and 

other bivalves from the Early Ordovician 

(Tremadocian) of northwestern Argentina. ( 英 

文 ). Sanchez T M; Vaccari N E. 

Ameghiniana, 2003, 40(3): 415-424 

A new Tremadocian bivalve fauna is described 

from the Floresta Formation at Sierra 

de Mojotoro, Jujuy Province. The new genus 

Ucumaris is described and is the basis for a 

new family of Anomalodesmata, the 

Ucumariidae, extending the record of the 

anomalodesmatans back to the Tremadocian. 

Intilwarella simplicidentata nov. gen. et sp. 

included in a new family of Actinodontoida, 

the Intihuarellidae nov. and an undetermined 

Redoniidae, are also described. Additionally, 

several specimens of Goniophorina (Cosmogoniophorina) 

cf. tenuicostata Harrington 

are described and illustrated. These taxa indicate 

a significant diversification of bivalves in 

Gondwanan shelves at the beginning of the 

early Ordovician. 

2007010205 

阿根廷西部晚奥陶世双壳类 Heteroconchia 

( 类圆蛤科和 Glyptarcidae 科 ) = Late 

Ordovician Bivalvia Heteroconchia (Cycloconchidae 

and Glyptarcidae) from western 

Argentina. ( 英文 ). Sanchez T M; Marengo L; 

Astini R A. Ameghiniana, 2003, 40(3): 433- 

440 

On the basis of existing and new collections 

from northwestern Argentina (Sierra de 

Zapla and Sierra de Mojotoro) as well as from 

the Precordillera (San Juan Province), two 

new genera of the Superorder Heteroconchia 

Hertwig are erected. Specimens from the 

Santa Gertrudis Formation (Late Llanvirn- 

Early Caradoc, Quebrada del Gallinato, Sierra 

de Mojotoro) assigned to Cycloconcha cf. C. 

oblonga Foerste were revised, and on the basis 

of new collections from the Capillas Formation 

(Sierra de Zapla) a new taxon of Glyptarcidae 

Cope, Zaplaella capillaensis gen. and sp. 

nov., is erected. Poladonta sanjuanina gen. 

and sp. nov. is proposed for unnamed, previously 

studied specimens of Cycloconchidae 

Ulrich from Early Caradoc pebbles contained 

in the basal diamictite of the Don Braulio 

Formation (Precordillera basin). 

2007010206 

阿根廷圣胡安省 Calingasta-Uspallata 盆地 

巴日尔山脉石炭纪双壳类 = Carboniferous 

bivalves from the Sierra de Barreal, Calingasta-Uspallata 

basin, San Juan province. ( 其他 ). 

Sterren A F. Ameghiniana, 2003, 40(3): 469- 

481 

Taxonomic analysis of bivalves was carried 

out in different sections of the Sierra de 

Barreal, San Juan province. As a result five 

species of bivalves are reconized. The new 

species Streblochondria sanjuanensis sp. nov. 

and also Nuculanella camachoi (Gonzalez), 

Aviculopecten barrealensis Reed, Streblochondria 

stappenbecki (Reed), Streblochondria 

sp. and Streblopteria sp. are described 

and figured. Bivalves are analized from a 

morphofunctional viewpoint mainly based on 

shell characters. One infaunal shallow burrower 

and five epifaunal bivalves are distinguished. 

Relationships between morphology 

and hypothetical life strategies are proposed. 

A Late Carboniferous age is suggested for the 

studied bivalves in view of their occurrence 

along with brachiopods belonging to the 

Levispustula Biozone in the Hoyada Verde 

Formation and Balakhonia-Geniculifera Biozone 

in the Esquina Gris and Mono Verde 

Formations. 

2007010207 

中古生代一归于 euomphaloidean 腹足类的 

新亚科 : Odontomariinae 亚科 = Odontomariinae, 

a new Middle Paleozoic subfamily of 

slit-bearing euomphaloidean gastropods 

(Euomphalomorpha, Gastropoda). ( 英文 ). 

Fryda J; Heidelberger D; Blodgett R B. Neues 

Jahrbuch fur Geologie u. Palaontologie / 

Monatschefte, 2006, (4): 225-248 

A new subfamily, the Odontomariinae 

subfam. nov., is established herein for a distinctive 

group of uncoiled, slit-bearing Middle 

Devonian euomphalid gastropods. The genera 

Odontomaria and Tubiconcha n. gen. belonging 

to this new subfamily are enlarged based 

on studies on new material of the following 

species: Odontomaria semiplicata, Odontomaria 

gracilis, Odontomaria jankei, Odontomaria 

cheeneetnukensis, Odontomaria cin- 

63

diprellerae and Tubiconcha leunissi. Members 

of the Odontomariinae were mainly sedentary 

organisms in high-energy, moderately shallow 

water. 

2007010208 

最早的双柱型双壳类 : 中国南部中三叠世的 

Protostrea = Protostrea from the Middle Triassic 

of southern China, the earliest dimyoid 

bivalve. ( 英文 ). Chen Jinhua; Stiller F; 

Kormatsu T. Neues Jahrbuch fur Geologie u. 

Palaontologie / Monatschefte, 2006, (3): 148- 

164 

The oyster-like, dimyarian, cementing 

bivalve genus Protostrea and its type species 

Protostrea sinensis from the upper anisian of 

the Qingyan Formatio, Guizhou Province, 

south-western China, are re-described and 

emended. The genus most probably is the earliest 

representative of the family Dimyidae. 

But Protostrea is a peculiar dimyid because in 

adult growth stages its shell is fairly large and 

thick, the resilifer is rectangular, broad, shallow 

and sometimes multiple, and the crura 

usually are weak. These features resemble 

some thick-shelled Prospondylidae. The features 

of pre-adult growth stages of P. sinensis 

idicate possible affinities to the order Pectinoida. 

2007010209 

阿根廷卡塔马卡和图库曼省圣玛利亚峡谷 

中新世圣何塞组和 Chiquimil 组新的软体 

动物 = New molluscs from the Miocene San 

Jose and Chiquimil formations, Santa Maria 

Valley, Catamarca and Tucuman provinces, 

Argentina.. ( 其他 ). Morton L S; Herbst R. 

Ameghiniana, 2003, 40(2): 205-216 

Eight species of molluscs are described 

from the San Jose and Chiquimil Formations 

(Upper Middle to Upper Miocene), of which 

four gastropods are new: Biomphalaria sanjosensis 

Morton n. sp. Littoridina bossii Morton 

n. sp., L. gavriloffi Morton n. sp., Potamolithus 

bertelsae Morton n. sp.; Bulimulus sp. 

and Lymnaea viatrix (d'Orbigny) are also present. 

Two bivalves are also new: Neocorbicula 

herbsti Morton n. sp. and N. anzoteguiae Morton 

n. sp. They represent additions to the previously 

described assemblage from these units. 

This is a fresh- to brackish water fauna and a 

marine paleoenvironment is definitively excluded. 

2007010210 

匈牙利 Aszofo 地区中三叠世安尼期鹦鹉螺 

= Middle Triassic (Anisian) nautilid cephalopods 

from Aszofo (Balaton Highland, Hungary). 

( 英文 ). Voros A. Fragmenta Palaeontologica 

Hungarica, 2001, (19): 1-14 

A nautilid fauna of medium abundance 

(38 specimens) was collected from the Aszofo 

section, well known for its rich ammonoid 

(Balatonites ) fauna, its biostratigraphic importance. 

The nautilid fauna is diverse: ten 

species were determined. Systematic description 

of the ten species is given; from among 

them Encoiloceras balatonicum sp. n., Encoiloceras 

lojosi sp. n. are new. 

2007010211 

匈牙利 Gerecse 山脉托尔期 (Toarcian) 腹足 

类 = Toarcian gastropods from the Gerecse 

Mts (Hungary). ( 英文 ). Galacz A; Szabo J. 

Fragmenta Palaeontologica Hungarica, 2001, 

(19): 15-24 

A relatively rich gastropod fauna has 

been found in the Toarcian of the Gerecse Mts, 

in a facies that is usually extremely poor in 

benthic fossils just like other localies of the 

Mediterranean Faunal Province. Nine species 

are separable in spite of the poor state of preservation. 

Most of them are deep water dwellers 

but two species seem "exotic" in the inferable 

palaeoenvironment. 

2007010212 

匈牙利 Sumeg 地区坎潘期头足类 = Campanian 

(Late Cretaceous)cephalopods from 

Sumeg (Transdanubian Central Range, Hungary). 

( 英文 ). Fozy I. Fragmenta Palaeontologica 

Hungarica, 2001, (19): 25-37 

Campanian ammonite assemblage, incluging 

Hypophylloceras sp., Pachydiscus cf. 

levyi , Pachydiscus cf. precolligatus and Menabites 

(Delawarella ) suemegensis sp. n., and 

a single specimen of Angulithes cf. westphalicus 

of the same age, are described and 

figured for the first time from Hungary. 

2007010213 

匈牙利 Borzsony 山脉 Szokolya-2 钻孔中中 

新世多板类 = Middle Miocene (Badenian) 

Polyplacophora (Mollusca) remains from 

borehole Szokolya - 2 (Borzsony Mts, Hungary, 

Central Paratethys). ( 英文 ). Dulai A. 


(19): 39-49 

Five determinable specimens refer to a 

very diverse fauna: Lepidochitona lepida, A- 

64

canthochitona faluniensis, Cryptoplax 

weinlandi, Cryptoplax margitae n. sp. With 

the exception of the new species, the other 

three ones belong to the most frequent Miocene 

Polyplacophora remains of the Central 

Paratethys (they are also common in the 

Korytnica Basin, Vienna Basin and Transylvanian 

Basin). The accompanying fauna contains 

diverse mollusc and bryozoa remains. 

2007010214 

印度西部卡奇侏罗系腹足类一新属 : Bhujnerita 

= Bhujnerita (Neritidae), a new gastropod 

genus from the Kachchh Jurassic 

(western India). ( 英文 ). Jaitly A K; Szabo J. 


(20): 49-52 

Bhujnerita n. gen. is the first new gastropod 

genus that has been established during the 

exploration of the Jurassic faunas from 

Kachchh. Beside this, Bhujnerita n. gen. is 

one of the few genera that seem to be endemic 

within the Ethiopian Faunal Province. In the 

family Neritidae, Bhujnerita n. gen. belong to 

the group of those non-limpet shaped forms 

which have an inner lip plate that partially 

closes the aperture. The type species is also 

new: B. bhattii n. sp. 

2007010215 

罗马尼亚 Alsorakos 地区 Vadasz(1915) 所 

列举的动物小区系中 euomphalomorph 腹 

足类一新属 = A new euiophalomorph gastropod 

genus in the faunula, listed by Vadasz 

(1915) from Alsorakos (Persani Mts, Romania; 

Early Jurassic). ( 英文 ). Szabo J. Fragmenta 

Palaeontologica Hungarica, 2002, (20): 

61-67 

Five species are distiguishable from the 

available, most probably Early Jurassic material, 

consisting of a few poorly preserved inner 

casts and a specimen with shell. The latter one 

preserved also the original shell microstructure 

that was different from that fo the comparable 

genera just like some of the megascopic 

character. These gave a basis for establishment 

of Valamidiscus persanyensis n. gen & n. 

sp. Short descriptions of the steinkerns are 

also given in the systematic part of the paper. 

Because Valamidiscus n. gen. cannot be fitted 

into the existing families without objection, its 

accommodation has been tentatively chosen. 

2007010216 

长江源美杜塘一带发现古近纪双壳类化石 

= Discovery of Paleogene bivalve fossils in 

the Meidutang area at the source of the Yangtze 

River. ( 中文 ). 王建雄 ; 牛志军 ; 汤朝阳 ; 白 

云山 ; 段其发 . 地质通报 , 2003, 22(3): 216- 

217 

长江源各拉丹冬地区位于唐古拉山北 

部 . 大地构造位置属东特提斯构造域北部 , 居 

拉竹龙 - 金沙江板块结合带与班公湖 - 怒江板 

块结合带之间的羌塘地块 , 北与可可西里盆 

地相接 . 在各拉丹冬西部赤布张错周缘分布 

有大面积的时代有争议的暗红色砂、砾岩 

地层 . 笔者在开展 1:25 万赤布张错幅野外地 

质调查过程中 , 在测制美杜塘剖面时采获数 

量较多的双壳类化石 , 对解决长江源区这套 

红层的地质时代具有重要意义 . 实测地层剖 

面位于各拉丹冬以西美杜塘一带 ( 图 1), 剖面 

起点坐标为东经 90°31′24″, 北纬 33°31′23″, 

总长为 3 850m. 

2007010217 

贵州关岭三叠系竹杆坡组、小凹组头足类 

化石 — 兼论关岭生物群的时代 = Triassic 

cephalopods from the Zhuganpo and Xiaowa 

Formations in Guanling,Guizhou,with a discussion 

on the age of the Guanling biota. ( 中 

文 ). 徐光洪 ; 牛志军 ; 陈辉明 . 地质通报 , 2003, 

22(4): 248-253 4 图版 . 

贵州关岭地区中、上三叠统竹杆坡组 

和小凹组产较丰富的头足类化石 , 计有 11 科 

19 属 37 种 , 其中 Enoploceras, Alloceratites,Sibyllites 

等属以及 Trachyceras aon 种系 

国内首次报道。自下而上可识别出 

(1)Xenoprotrachyceras primum 带 ; 

(2)Protrachyceras deprati 带 ; 

(3)Protrachyceras costulatum 带 ; 

(4)Trachyceras multituberculatum 带 ; 

(5)Sirenites cf. senticosus 带等 5 个菊石 

带。讨论了每个菊石带的特征 , 并与国外同 

期菊石带进行了对比 , 指出 (1) 带与欧洲拉丁 

期早期 R. reitzi 带相当 ,(2) 和 (3) 带分别与拉丁 

期晚期 E. curionii 带和 P. archelaus 带相当 ,(4) 

和 (5) 带分别与欧洲早卡尼期早期 T. aon 带和 

北美的早卡尼期晚期 Sirenites nanseni 带对 

比。关岭生物群产出层位与 Trachyceras 

multituberculatum 菊石带层位一致 , 时代应为 

早卡尼期早期。 

2007010218 

述评中国奥陶纪双壳类兼论双壳类早期演 

化 = An introduction to Ordovician bivalves 

of southern China, with a discussion of the 

early evolution of the Bivalvia. ( 英文 ). Fang 

65

Zongjie. Geological Journal, 2006, 41(3/4): 

303-328 

This paper introduces the Ordovician bivalves 

of southern China to non-Chinese colleagues, 

and then incorporates them into the 

global Ordovician bivalve database compiled 

by Cope (2004). This will provide a firmer 

basis for the discussion of the initial adaptive 

radiation of the Bivalvia. A new scenario for 

the early evolution of the class Bivalvia is advanced 

herein based on the integration of a 

wide variety of evidence concerning bivalves, 

including morphological features, ontogenetic 

trajectory, benthic environment and lithologic 

setting, so as to explain reasonably why the 

initial explosive radiation of bivalves in the 

Early Ordovician followed a long-term macroevolutionary 

lag since their first appearance 

during the Cambrian explosion. The early evolution 

of the Bivalvia can be divided into three 

phases: (a) the origination and macroevolutionary 

lag phase in the Early and Middle 

Cambrian; (b) the crisis phase in the Late 

Cambrian; and (c) the Ordovician radiation 

phase, which can be subdivided into two radiation 

pulses or intervals (the Arenig and the 

Caradoc radiation intervals). It is the Cambrian 

substrate revolution that caused a transformation 

of shallow subtidal seafloors from 

more coherent Neoproterozoic-style matgrounds 

to soupier Phanerozoic-style mixgrounds, 

thus compelling Cambrian 'archetype' 

bivalves to sink into the infaunal realm 

and to adapt themselves to the development of 

the mixed layer in siliciclastic soft substrate 

environments. As a result, Cambrian 'archetype' 

bivalves entered a tight bottleneck and 

became extinct while the latest common ancestor 

of 'modern-type' bivalves originated 

from a certain founder population somewhere 

in the Gondwanan shelf seas. The rapidly 

evolving founder population may be the place 

of origin of evolutionary novelties and it became 

the starting point of the evolution of 

'modern-type' bivalves. The macroevolutionary 

lag of the Bivalvia ended in the earliest 

Ordovician as a result of the successful invasion 

of the infaunal adaptive zone. The bivalve 

die of 'modern-type' was cast during the 

Ordovician, when all principal clades and all 

four principal life-habit groups underwent 

initial development. A series of morphological 

innovations, especially the evolution of the 

muscular hydraulic foot with burrowing adaptations, 

byssus, and feeding gill, are responsible 

for the initial adaptive radiation. It is these 

morphological innovations that provide evolutionary 

access to the new adaptive zone for 

bivalves. 

2007010219 

副特提斯中部 ( 匈牙利 Bakony 山脉 Band 

和 Devecser 地区 )Badenian 阶多板类 = Badenian 

(Middle Miocene) Polyplacophora 

from the Central Paratethys (Band and Devecser, 

Bakony Mountains, Hungary). ( 英文 ). 

Dulai A. Fragmenta Palaeontologica Hungarica, 

2005, (23): 29-50 

The isolated valves of Polyplacophora 

species are rare elements of the Hungarian 

Miocene fossil assemblages. This paper provides 

description of a rich and well-preserved 

chiton fauna from Band and Devecser collected 

by two amateur collectors. Eight species 

of six genera were identified in this Early 

Badenian fauna. The widespread Central 

Paratethyan species, C. weinlandi is represented 

by particularly rich and variable material, 

tendering the study of ontogenetic 

changes. The taxonomic composition of this 

chiton material corresponds well to the other 

Polyplacophora faunas known from the Central 

Paratethys (e. g. Poland, Austria, Ronania). 

2007010220 

西班牙志留纪兰多维列世特列奇期双壳类 

= Telychian (Llandovery, Silurian) Bivalves 

from Spain. ( 英文 ). Kříž J. Palaeontology, 

2005, 48(3): 455-477 

Twenty species of bivalves (14 new) and 

14 genera (six new) are described from two 

localities in the Silurian, upper Telychian, Oktavites 

spiralis Biozone of Spain: Cardavia 

cathleenae gen. et sp. nov., C. hafi sp. nov., 

C. stefani sp. nov.; Copenychia franta gen. et 

sp. nov., C. pristina sp. nov.; Stolidotus marco 

sp. nov.; Telycardia malinka gen. et sp. nov.; 

Silurinka vetula gen. et sp. nov.; Bolsopteria 

lentilka gen. et sp. nov.; Nennapteria ibericola 

gen. et sp. nov., N. ollicula sp. nov.; Actinopteria 

dakryodes sp. nov., A. isabelae sp. nov. 

and Dceruska hispanica sp. nov. They comprise 

two closely related communities, the 

Copenychia-Cardavia-Actinopteria Community 

and the Dceruska-Copenychia-Stolidotus 

Community, which belong to the Snoopyia 

Community Group. The occurrence of Dceruska 

Barrande, 1881, Dualina Barrande, 

1881, Patrocardia Barrande, 1881, Silurinka, 

gen. nov., Slava Barrande, 1881 and Stolidotus 

Hede, 1915 in the Telychian of the Central 

Iberian Domain, Spain, supports palaeogeographical 

relationships with other Lower 

Silurian regions of north Gondwanan and 

66

Perunican Europe: the Carnic Alps (Austria), 

the Montagne Noire (France), Sardinia (Italy) 

and the Prague Basin (Bohemia), and also to 

Avalonia: the Welsh Borderland (Great Britain) 

and Baltica–Skåne (Sweden). These genera 

together with the new genera Cardavia, 

Copenychia (the earliest known representatives 

of the Silurian family Cardiolidae), Telycardia 

(the oldest known representative of the 

family Praecardiidae) and Silurinka belong to 

a Bohemian type of bivalve. Bolsopteria lentilka 

is closely related to Bolsopteria elliptica 

(Hind, 1910) from the Aeronian (middle 

Llandovery) of Scotland. 

2007010221 

Baltoscandia 下 — 中奥陶统下部具多对肌痕 

的鹦鹉螺 = Nautiloids with multiple paired 

muscle scars from Lower–Middle Ordovician 

of Baltoscandia. ( 英文 ). Kroeger B; Mutvei H. 


The number, outline and arrangement of 

muscle scars on the internal mould of the body 

chamber of five species of Early and Middle 

Ordovician nautiloids from Baltoscandia are 

described. The ellesmeroceratids Oelandoceras 

haelluddenense Foerste and Pictetoceras 

oliviae King have 9–10 pairs of muscle 

scars. The oncoceratid Phtanoncoceras ellipticum 

(Lossen), and Botellusoceras torpense 

gen. et sp. nov., order and family indeterminate, 

have eight and nine pairs of muscle scars, 

respectively. The tarphycerid Estonioceras 

imperfectum (Quenstedt) has four pairs of 

muscle scars. 

2007010222 

三叠纪双壳类磷酸盐化的软组织 = Phosphatized 

soft-tissue in Triassic Bivalves. ( 英 

文 ). Klug C; Hagdorn H; Montenari M. Palaeontology, 

2005, 48(4): 833-852 

Exceptionally preserved specimens of the 

genera Myophoria, Neoschizodus and 

Trigonodus (Bivalvia, Palaeoheterodonta, 

Trigonioida) from carbonate sediments of the 

Muschelkalk (Anisian, Ladinian) contain 

phosphatized soft-tissues. This is the oldest 

record of soft-tissue preservation in bivalves 

and the first from the German Muschelkalk. 

The phosphatized remains are here interpreted 

as relics of the originally chitinous gill supports, 

the gill axis, the labial palps (), the adductor 

muscles, the pedal retractor muscles, 

the mantle margin including the radial mantle 

musculature, and the 'siphons'. According to 

microprobe analysis, the mineral replacing the 

soft-tissue is mainly apatite and, more rarely, 

francolite. Additionally, quartz filled voids 

within the gill supports, and in one sample it 

occurs in minute crystals in the phosphatized 

remains of the adductor muscle of Neoschizodus. 

Myophoria, Neoschizodus and 

Trigonodus were soft-bottom dwellers and 

five of the specimens were discovered in life 

position. This is indicated by geopetal structures 

in three specimens. 

2007010223 

印度 Kutch 地区 Callovian Chari 组 

Eucycloceratin 类菊石 = Eucycloceratin 

Ammonites from the Callovian Chari Formation, 

Kutch, India. ( 英文 ). Jana S K; Bardhan 

S; Halder K. Palaeontology, 2005, 48(4): 883- 

924 

The subfamily Eucycloceratinae Spath, 

1928, belonging to the family Sphaeroceratidae, 

is an important Indo-Madagascan faunal 

element and is reported here from the Callovian 

of Kutch, India. Previously the subfamily 

was considered to consist of 14 morphospecies 

placed in four morphogenera. The 

present study is based on re-examination of 

the type material and more than 350 new 

specimens, collected with secure stratigraphical 

control, from sections in mainland Kutch. 

It reveals that the subfamily includes only two 

highly variable monospecific genera: Eucycloceras 

Spath, 1924 and Idiocycloceras 

Spath, 1928. Dimorphism in Eucycloceratinae, 

which was not previously recognized, is 

firmly established. Cladograms have been 

constructed, based on numerous morphological 

characters, which show relationships 

among different subfamilies of the Sphaeroceratidae 

and genera of the Macrocephalitinae 

and Eucycloceratinae. The palaeobiogeography 

and evolution of the Eucycloceratinae are 

discussed in the light of the new data. 

2007010224 

古生代软体动物中的掘足化 = Scaphopodization 

in Palaeozoic Molluscs. ( 英文 ). Peel J 

S. Palaeontology, 2006, 49(6): 1357-1364 

The relationship of a variety of problematic 

Early Palaeozoic fossils to the true scaphopods 

(Late Palaeozoic–Recent) is clarified 

by the recognition that a trend towards the 

development of a tubular shell is a recurrent 

theme within Palaeozoic benthic molluscs. 

This trend is here termed scaphopodization 

and can be recognized already in the Cambrian 

in helcionelloids such as Yochelcionella 

and Eotebenna. The problematic Early Palaeozoic 

tubular fossils Janospira, Jinonicella 

67

and Rhytiodentalium are interpreted as 

pseudo-scaphopod derivatives of the apparently 

exogastric ribeirioid rostroconchs. The 

direction of coiling of the protoconch indicates 

that they are not closely related to the 

true scaphopods, which were derived from 

endogastric concocardioidean rostroconchs in 

the Devonian or Carboniferous. Scaphopods 

show a comparable underlying morphological 

blueprint to these conocardioideans, but they 

represent a distinct stream-lining to the infaunal 

habitat. 

2007010225 

牙买加 Maastrichtian 期新的具管 

Antillocaprinid 类厚壳蛤双壳动物 = New 

tube-bearing Antillocaprinid Rudist Bivalves 

from the Maastrichtian of Jamaica. ( 英文 ). 

Mitchell S F; Gunter G C. Palaeontology, 

2006, 49(1): 35-57 

Two genera of tube-bearing antillocaprinid 

rudist bivalves from the Maastrichtian of 

Jamaica are recognised: Titanosarcolites 

Trechmann and Parasarcolites gen. nov. Titanosarcolites 

is recumbent, broadly equivalve 

and coils parallel to the myocardinal line, with 

tubes on the anteriodorsal, anterior, and anterioventral 

regions of the inner layer; there are 

two teeth and two teeth-like myophores in the 

left valve. Sockets for teeth have conical tabulae, 

those for myophores are filled with normal 

shell structure. A ligamental cavity is 

lacking. Parasarcolites is recumbent, with 

equal, subequal or moderately inequal valves, 

and the plane of coiling is at an angle of 34– 

63 degrees to the mediocardinal line. It has 

tubes in the dorsal and anterior-dorsal regions, 

and a myocardinal structure with blade like 

myophores, with the posterior tooth and 

socket strongly flattened. The position of the 

ligament is indicated by a comma-shaped cavity 

situated dorsalwards of the posterior tooth. 

Additional toothlets are present in the left 

valve. All sockets are filled with canal-bearing 

shell-structure. Five new species of Parasarcolites 

are described from the Upper Maastrichtian 

of Jamaica: Parasarcolites atkinsoni, 

P. baileyi, P. greeni, P. monotubularis and P. 

quadratus. 

2007010226 

中国西南青岩中三叠统安尼阶新的 

Mysidiellidae 科双壳动物 = New Mysidiellidae 

(Bivalvia) from the Anisian (Middle Triassic) 

of Qingyan, South-west China. ( 英文 ). 

Stiller F; Chen Jinhua. Palaeontology, 2006, 

49(1): 213-227 

Three new genera including four new 

species of the bivalve family Mysidiellidae are 

described from late middle to early late Anisian 

(Middle Triassic) deposits of Qingyan, 

Guizhou Province, south-west China. The new 

taxa Leidapoconcha gigantea gen. et sp. nov., 

Waijiaoella elegans gen. et sp. nov., Waijiaoella 

speciosa gen. et sp. nov. and Qingyaniola 

mirabilis gen. et sp. nov. significantly 

increase the known taxonomic diversity within 

the Mysidiellidae. These findings suggest a 

somewhat endemic evolutionary development 

within this small bivalve family during the 

Middle Triassic in south-west China. 

2007010227 

早三叠统异齿目双壳类软体动物的最初记 

录 : 古生态学重要性及对 Lazarus 难题的 

意义 = First record of a Heterodont Bivalve 

(Mollusca) from the early Triassic: palaeoecological 

significance and implications 

for the 'Lazarus problem'. ( 英文 ). Hautmann 

M; Nützel A. Palaeontology, 2005, 48(6): 

1131-1138 

The heterodont bivalve Sinbadiella pygmaea 

gen. et sp. nov. is described from the 

Sinbad Limestone Member (Olenekian, 

Smithian) of the Lower Triassic Moenkopi 

Formation of Utah (USA). The new taxon is 

tentatively assigned to the Lucinidae on the 

grounds of its external morphology, larval 

shell morphology and hinge characters. It is 

the only definite representative of the Superorder 

Heterodonta in the Olenekian, removing 

this major clade of bivalves from the 

long list of Early Triassic Lazarus taxa. Although 

at least locally very abundant, the new 

taxon has been overlooked by earlier workers, 

probably due to its minute size. Dwarfism is a 

widespread phenomenon in Early Triassic 

faunas, which has been attributed to ongoing 

reduction of primary production. If 

S. pygmaea was a lucinid, a chemosymbiotic 

feeding mode can be inferred, which might 

explain why it was able to thrive in conditions 

that suppressed filter feeding heterodonts. 

2007010228 

软舌螺类形态学及其功能意义 = The morphology 

of Hyolithids and its functional implications. 

( 英文 ). Martí Mus M; Bergström J. 


The exceptionally preserved hyolithids 

Gompholites striatulus, Maxilites robustus, 

Maxilites snajdri and Maxilites sp. are described 

with particular emphasis on helen and 

muscle scar morphology. These two aspects of 

68

hyolithid morphology have remained controversial. 

In life position, each helen curved 

ventrally. When the operculum closed the aperture 

of the conch, each helen was locked at 

the commissure slit with its dorsal edge tilted 

forward. Inside the conch, it was held in the 

dorsal apertural plane and clear of the inner 

surface of the operculum. Previously unidentified 

muscle scars are described from both the 

operculum and the conch. Dorsal scars on the 

conch aperture held muscles directed to the 

operculum. Comparative study of the muscle 

insertion pattern indicates that hyolithids did 

not have serially arranged muscles and that all 

hyolithids may have had a common skeletomuscular 

system. The arrangement of the 

muscle scars with respect to the helens suggests 

that the latter were capable of relatively 

complex movements and could have been 

used to propel the organism over the substrate. 

The general morphology and orientation of the 

helens suggests that in addition they functioned 

to stabilize the organism on the seafloor. 

2007010229 

大不列颠哥伦比亚 Taseko 湖早侏罗世早新 

涅缪尔期晚期菊石 = Late early Sinemurian 

(Early Jurassic) Ammonites from the Taseko 

lakes map area, British Columbia. ( 英文 ). 

Macchioni F; Smith P L; Tipper H W. Palaeontology, 

2006, 49(3): 557-583 

Abundant and well-preserved Early Jurassic 

ammonite assemblages occur in the Taseko 

Lakes map area on the Cadwallader Terrane 

in the southern Coast Mountains of British 

Columbia. The ammonite assemblage described 

herein includes nine genera and 14 

species, most of them already known from 

classical localities of northern and southern 

Europe. The presence in particular of 

Caenisites brooki (Sowerby) and C. turneri 

(Sowerby) permits high-resolution correlation 

with the Turneri Zone of the north-west European 

Sinemurian zonation. The specimens 

were collected at four localities but most come 

from an olistolith where the ammonite assemblage 

is dominated by Coroniceras (Paracoroniceras) 

mutabile Macchioni, Smith and 

Tipper, associated with Lytotropites fucinii 

(Bonarelli) and Hypasteroceras montii (De 

Stefani). The latter two species, whose exact 

age is here established for the first time, have 

a Mediterranean distribution. 

2007010230 

英格兰多塞特下侏罗统的 

Phragmoteuthida( 头足纲 , 鞘形亚纲 ) = 

Phragmoteuthida(Cephalopoda: Coleoidea) 

from the lower Jurassic of Dorset, England. 

( 英文 ). Donovan D T. Palaeontology, 2006, 

49(3): 673-684 

Phragmoteuthida from the Lower Jurassic 

(Upper Sinemurian) of Dorset, England, 

are fully described for the first time. Two species 

are recognized and described: Phragmoteuthis 

montefiorei (J. Buckman) and 

P. huxleyi sp. nov. Phragmocones have an 

apical angle of between 20 and 30 degrees, 

and relatively few chambers compared with 

belemnoids. The conotheca is multi-layered. 

The siphuncle is thick-walled. The proostracum 

is long and three-lobed as in the Triassic 

species. Arms are short and bear pairs of 

slightly curved hooks. Shell and siphuncle 

structure do not indicate a close relationship 

with other coleoids. 

2007010231 

加拿大大不列颠哥伦比亚早侏罗世菊石 

Badouxia = The early Jurassic Ammonite 

Badouxia from British Columbia, Canada. ( 英 

文 ). Longridge L M; Smith P L; Tipper H W. 


Most species of the Lower Jurassic ammonite 

genus Badouxia are restricted to the 

eastern Pacific where they are of fundamental 

importance to the Hettangian/Sinemurian 

ammonite zonation of North America. The 

fauna from the type area for the genus has 

been restudied and four species and two transitional 

forms are now recognized. Badouxia 

forticostata and Badouxia castlensis are new. 

Badouxia occidentalis (Frebold) and Badouxia 

oregonensis Taylor are placed in synonymy 

with Badouxia canadensis (Frebold). These 

major taxonomic changes and subsequent 

modification to the range of B. canadensis 

require revisions to the current zonation for 

the Western Cordillera of North America. The 

Oregonensis Zone is re-named the Mineralense 

Zone. The Canadensis Zone is abandoned 

and its previously defined Rursicostatum 

and Columbiae subzones are elevated 

to the level of full zones. Large samples indicate 

that most species of Badouxia display a 

remarkable range of continuously variable 

morphology. In addition, the genus shows 

some of the best-documented evidence of sexual 

dimorphism in Early Jurassic ammonites. 

Badouxia spans the Hettangian/Sinemurian 

boundary and based on the range of different 

69

species, five stratigraphic intervals are recognized. 

Intervals 1–3 correlate with the northwest 

European Angulata Zone. The majority 

of interval 4 and the whole of interval 5 correlate 

with the north-west European Bucklandi 

Zone. The age of the base of interval 4 is uncertain. 

2007010232 

日本东北北上山地 (Kitakami Massif) 南 

部上八濑 - 饭森地区 (Kamiyasse-Imo district) 

的中二叠世菊石化石 = Middle Permian 

ammonoids from the Kamiyasse-Imo 

district in the Southern Kitakami Massif, 

Northeast Japan. ( 英文 ). Ehiro Msayuki; 

Misaki Adihiro. Paleontological Research, 

2005, 9(1): 1-14 

Middle Permian ammonoid faunas are 

recognized from the Hosoo and Kamiyasse 

Formations in the Kamiyasse-Imo district, 

north of Kesennuma, Southern Kitakami Massif, 

Northeast Japan. The faunas comprise the 

following genera: Parastacheoceras, Demarezites, 

Demarezites, Waagenoceras, Timorites, 

Tauroceras, Cardiella, Adrianites, 

Agathiceras, Agathiceras, Paraceltites and 

Cibolites. Parastacheoceras bidentatus gen. 

and sp. nov. is newly proposed. The genera 

Demarezites, Tauroceras, Cardiella and Adrianites 

are described for first time from Japan. 

Based on these ammonoids, the middle part of 

the Hosoo Formation, upper part of the Hosoo 

Formation to the lower middle part of the 

Kamiyasse Formation, and upper middle part 

of the Kamiyasse Formation are correlatable 

with the Middle Permian Roadian, Wordian 

and Capitanian, respectively. The discovery of 

genera Demarezites and Cardiella strongly 

supports the previous hypothesis that the 

South Kitakami Paleoland was located in the 

equatorial province during the Middle Permian. 

2007010233 

日本西南部三宝山加积复合体 (Sambosan 

accretionary complex) 中的晚三叠世双壳 

类及它们的生物地理意义 = Late Triassic 

bivalves from Sambosan accretionary complex, 

southwest Japan, and their biogeographic 

implications. ( 英文 ). Onoue Tetsuji; Tanaka 

Hitoshi. Paleontological Research, 2005, 9(1): 

15-25 

This paper records eight species of Late 

Triassic Tethyan bivalves from the oceanic 

limestone and associated basaltic volcaniclastic 

rocks which belong to the Sambosan accretionary 

complex in southwest Japan. The bivalve-bearing 

succession consists of basaltic 

volcaniclastic rocks (ca. 60m thick) conformably 

succeeded by dark gray bedded 

limestone (ca. 10m thick), which is, in turn, 

overlain by massive limestone (ca. 50m thick). 

The succession is dated as Carnian to Norian 

by means of conodonts and bivalves. Upper 

Triassic bivalves, including Gruenewaldia 

decussata, G. woehrmanni and Costatoria 

gold-fussi, are recorded from the examined 

succession. Their occurrence implies a 

Tethyan affinity for the examined Sambosan 

oceanic rocks. No bivalve species characteristic 

of a high latitudinal zone occurs in this 

succession. 

2007010234 

塞浦路斯中新统 Pakhna 组八腕目船蛸属 = 

A Paper Nautilus (Octopoda, Argonauta) from 

the Miocene Pakhna Formation of Cyprus. ( 英 

文 ). Martill D M; Barker M J. Palaeontology, 

2006, 49(5): 1035-1041 

The fossil organic trace of an argonaut 

shell from the Pakhna Formation (Serravillian, 

Middle Miocene) of southern Cyprus is described. 

The new find represents one of only a 

very few argonaut egg cases reported from the 

fossil record of the Tethyan region and is the 

first to be reported from the eastern Mediterranean. 

It is assigned to a new species of Argonauta 

as A. absyrtus sp. nov. 

2007010235 

早提塘阶菊石属 Semiformiceras 前进进化 

的分支系统学研究 = Anagenetic evolution of 

the early Tithonian Ammonite genus Semiformiceras 

tested with cladistic analysis. ( 英 

文 ). Cecca F; Rouget I. Palaeontology, 2006, 

49(5): 1069-1080 

The Early Tithonian ammonite genus 

Semiformiceras represents a lineage that lasted 

almost 3 myr. Previously, a gradual, anagenetic 

evolutionary pattern has been proposed 

on the basis of both biostratigraphic 

data and the interpretation of morphological 

changes in successive species, subspecies or 

morphotypes. The existence of two almost 

homeomorphic species, S. birkenmajeri and 

S. gemmellaroi, at two separate stratigraphic 

intervals in the early Tithonian contrasts with 

the transformation of characters suggested by 

the stratigraphic distribution of others. New 

descriptions of 18 specimens of the poorly 

known species Semiformiceras gemmellaroi 

(Zittel) allow a more accurate analysis of its 

70

characters. Cladistic analysis of a taxoncharacter 

matrix is based on nine Semiformiceras 

phena (species, chronosubspecies and 

morphotypes) and two outgroup taxa (Taramelliceras 

and Streblites), using 14 morphological 

characters. The phyletic relationships 

inferred from these do not fit the anagenetic 

pattern and question the adequacy of the fossil 

record in reconstructing phyletic lineages. 

2007010236 

现代光真笠螺 (Patellogastropoda, Gastropoda, 

Mollusca) 的壳体结构 = The shell 

structure of the Recent Patellogastropoda 

(Mollusca : Gastropoda). ( 英文 ). Fuchigami 

Takeshi; Sasaki Takenori. Paleontological 

Research, 2005, 9(2): 143-168 

The shell microstructure of 44 species 

belonging to 19 genera and 5 families of Patellogastropoda 

was observed by scanning 

electron microscopy on the basis of material 

mainly from the Northwest Pacific. As a result, 

17 microstructures of prismatic, crossed, and 

lamellar structures were recognized. The 

comparison among species revealed 20 shell 

structure groups which are defined by microstructures 

and shell layer arrangement. The 

relations between taxa and shell structural 

composition indicate that the Recent patellogastropods 

generally have distinctive and 

stable shell structures at the genus level. This 

high level of consistency provides a firm basis 

for the application of shell structural characters 

to identify fossil patellogastropods. However, 

the evolutionary process of microstructures 

and homology across different shell layers 

are mostly ambiguous in the absence of 

robust phylogeny and undoubted positional 

criteria for comparison. More studies from 

phylogenetic, ontogenetic and mineralogical 

viewpoints should be undertaken to discuss 

the process of shell structure diversification in 

patellogastropods. 

2007010237 

岩石生钻孔双壳类外侧不对称性的功能和 

进化 = The function and evolution of lateral 

asymmetry in boring endolithic bivalves. ( 英 

文 ). Enrico S. Paleontological Research, 2005, 

9(2): 169-187 

A substantial lateral asymmetry of the 

shell is observed in the bivalve genera Claudiconcha 

(Petricolidae), Jouannetia (Pholadidae), 

Clavagella and Bryopa (Clavagellidae) that 

bore in rock or mineralised biogenic substrates. 

Two general adaptive patterns emerge from 

this study. (1) Lateral asymmetry is associated 

with cementation of one valve to the substrate, 

or is otherwise functional in preventing one 

valve from moving within the borehole, and (2) 

it is associated with determinate shell growth 

and appears only in the adult stage. The only 

important exception to the latter pattern is 

Bryopa, which secondarily lost the determinate 

growth pattern originally present in clavagellids. 

These features have evolved independently 

in each family, and differ in several 

constructional and functional respects among 

families. 

2007010238 

钻孔双壳类 Zirfaea subconstricta 

(Pholadidae) 在发育早期的功能性壳体形态 

= Functional shell morphology in early developmental 

stages of a boring bivalve Zirfaea 

subconstricta (Pholadidae). ( 英文 ). Ito Yasuhiro. 

Paleontological Research, 2005, 9(2): 

189-202 

Early shell development at the larval and 

early postlarval stages of a boring bivalve Zirfaea 

subconstricta is described using scanning 

electron microscopy, with discussion of its 

functional significance for achieving boring 

behavior. In Z. subconstricta, the boring function 

performed by the shell morphology drastically 

develops in a short time after the beginning 

of metamorphosis. This species shares 

common characteristics with other pholads 

regarding the early ontogenetic appearance of 

the boring morphology. These characteristics 

provide much information of primary shell 

morphology as basal condition of boring function, 

which is usually modified during the 

later growth. 

2007010239 

日本白垩纪叠瓦蛤类的分异度变化 = Diversity 

changes in Cretaceous inoceramid bivalves 

of Japan. ( 英文 ). Takahashi Akinori. 

Paleontological Research, 2005, 9(3): 217- 

232 

Temporal species-diversity changes in 

Japanese Cretaceous inoceramid bivalves 

were analyzed from an extensive literature 

survey and statistical analysis, with the following 

results : (1) Species diversity increased 

gradually from the Upper Albian to Lower 

Campanian, and then dropped suddenly across 

the Lower/Upper Campanian (LCa/UCa) 

boundary; (2) There is no statistical correlation 

between ammonoid and inoceramid diversity 

changes in Japan, which must reflect 

the different ecologies of both groups; (3) 

71

Relatively high extinction ratios occurred at 

boundaries near Oceanic Anoxic Events 

(OAEs). The extinction events at the Albian/Cenomanian, 

Cenomanian/Turonian, and 

Turonian/Coniacian boundaries were potentially 

caused by OAE1d, 2 and the onset of 

OAE3, respectively. The drastic diversity decrease 

at the LCa/UCa boundary probably 

resulted from an abrupt and large-scale relative 

sea-level fall in the Yezo forearc basin; 

and (4) The pattern of diversity changes is 

similar to that of long-term (2nd-order) 

eustatic sea-level changes. The following hypotheses 

are presented as the cause of these 

phenomena : changes in shelf area, the primary 

inoceramid habitat, controlled their diversity, 

or changes in the Cretaceous outcrop 

area (rock volume) associated with sea-level 

changes controlled their diversity. It is possible 

that a combination of both factors controlled 

diversity patterns. 

2007010240 

日本中新世海扇蛤类 Nanaochlamys 

notoensis 的生活模式和分类关系 = The 

mode of life and taxonomic relationship of a 

Japanese Miocene pectinid bivalve 

Nanaochlamys notoensis. ( 英文 ). Hayashida 

N; Tanabe K. Paleontological Research, 2006, 

10(1): 1-10 

The mode of life of the Japanese Miocene 

bizarre pectinid Nanaochlamys notoensis 

(Yokoyama, 1929) is postulated on the basis 

of functional morphologic and biometric examinations 

of a large sample from the Middle 

Miocene Moniwa Formation in northern Japan. 

This species exhibits a remarkable ontogenetic 

change of shell morphology; i.e., the weight of 

valves becomes negatively allometric to the 

cube of shell size, indicating relative thinning 

of the shell with growth. Following this allometric 

change, the mnboftat angle increases, 

the auricles become symmetrical, and the 

ctenolium disappears. Comparison of shell 

morphology with Recent pectinids strongly 

suggests that the present species changed its 

life style from byssally attached to free-living 

during ontogeny. This pectinid probably could 

swim in the later growth stage, but its swimming 

ability appears to have been poor in 

view of the high convexity of the left valve. 

Secondary flaring of the shell and splitting of 

the first-order plicae are apomorphic features 

in N. notoensis, suggesting that this species is 

not a direct ancestor of the extant North Pacific 

pectinid Swiftopecten swiftii, with seemingly 

similar overall shell morphology. 

2007010241 

日本北海道一种白垩纪 desmoceratine 菊石 

Tragodesmoceroides subcostatus Matsumoto, 

1942 的壳体个体发育 = ontogenetic 

shell development of a Cretaceous desmoceratine 

ammonoid “Tragodesmoceroides 

subcostatus” Matsumoto, 1942 from Hokkaido, 

Japan. ( 英文 ). Nishimura T; Maeda H; Shigeta 

Y. Paleontological Research, 2006, 10(1): 

11-28 

Ontogenetic shell development of the Turonian 

desmoceratine ammonoid Tragodesmoceroides 

subcostatus is examined based on 

more than 200 specimens collected by detailed 

biostratigraphic survey in the Tappu and Saku 

areas, Hokkaido, Japan. After the anunonitella 

stage, the mode of ribbing on the shell surface 

becomes coarser with growth. The shell surface 

ornament changes from stage 1 (almost 

smooth) to stage 3 (coarse ribbing) via stage 2 

(weak ribbing). Stage 1 is subdivided into an 

earlier substage la with desmoceratid-type 

constrictions and a subsequent substage lb 

without constrictions. Appearance order of 

these four ornament stages and substages 

seems to be ontogenetically fixed in the present 

species. Other characters, such as 

anunonitella and early shell shape and whorl 

geometry are also stable. 

On the other hand, the shifting-timing 

from stages 1 to 2 and from stages 2 to 3 

changes chronologically, Le., it becomes ontogenetically 

earlier in upward sequence. In 

the Lower and Middle Turonian, the adult or 

subadult shells still remain stage 1 or 2. In 

contrast the strongly ribbed holotype and paratypes 

showing stage 3 are regarded as the Upper 

Turonian peramorphic endmembers of the 

single biospecies T. subcostatus. Taking these 

features into consideration, T. subcostatus 

should be taxonomically revised. 

2007010242 

普适性的菊石流体静力学模型 , 及该模型 

在 Intornites 上和 Amaltheus 种内变异上 

的应用 = Generalized ammonoid hydrostatics 

modelling, with application to Intornites and 

intraspecific variation in Amaltheus. ( 英文 ). 

Hammer O; Bucher H. Paleontological Research, 

2006, 10(1): 91-96 

A numerical procedure for calculating the 

buoyancy, apertural orientation and rotational 

stability of ammonoids can accommodate 

noncircular apertures and allometries. The 

hydrostatic properties of the Triassic oxyconic 

ammonite Intornites nevadanus were esti- 

72

mated from measured coiling parameters, 

body chamber length and digitized whorl section. 

The calculations indicate close to neutral 

buoyancy. The orientation of the aperture is 

33 degrees from the horizontal, and the stability 

index relatively high at 0.054. Unlike for 

many other ammonites, these values are comparable 

to those of Nautilus, suggesting a 

similar nektobenthic lifestyle. An apertural 

interior shell callus does not contribute to stability 

in this genus, and its function remains 

unknown. In Amaltheus margaritatus, hydrostatic 

properties and body chamber length 

vary significantly as a result of intraspecific 

variation in shell shape. Covariation between 

septal spacing and whorl shape can be given a 

functional explanation in terms of hydrostatic 

properties. Buckman's second law of covariation 

between ribbing and sutural complexity 

can possibly be thought of in terms of heterochrony. 

2007010243 

日本上至更新世沉积物中的 Trophonopsis 

Bucquoy, Dautzenberg and Dollfus, 1882 

(Gastropoda, Muricidae) = Trophonopsis 

Bucquoy, Dautzenberg and Dollfus, 1882 

(Gastropoda, Muricidae) from the Plio- 

Pleistocene deposits in Japan. ( 英文 ). Amano 

K. Paleontological Research, 2006, 10(2): 

163-176 

The Plio-Pleistocene Trophonopsis in 

northern Japan consists of seven species: T. 

kamchat-kana (Dall), T. uyemurai (Yokoyama), 

T. sasae Sawada, T. vermeiji Amano, sp. nov., 

T. aff. densicostata Golikov in Golikov and 

Scarlato, T. aff. undocostata Golikov and Sirenko 

and T. sp.. Trophon toyamai Hatai and 

Nisiyama and T. kagaensis Hatai and Nisiyama 

are synonymous with Trophonopsis uyemurai. 

By the end of the early Pleistocene, T. uyemurai, 

T. sasae and T. vermeiji became extinct and T. 

aff. undocostata and T. sp. might have become 

extinct, owing to decrease of salinity in shallow 

water during the low stands of the glacial 

Pleistocene. 

2007010244 

个体发育的异时性 : 能作为研究变异和系 

统发育关系的工具吗例 : 非洲上白垩统 

菊石尼日尔菊石属 . = Ontogenetic heterochronies: 

a tool to study both variability and 

phyletic relationships Example: Nigericeras, 

Ammonitina of the African Upper Cretaceous. 

( 法文 ). Courville P; Cronier C. Comptes Rendus 

Palevol, 2003, 2(6-7): 535-546 

The Nigericeras gadeni ontogenesis (Saharian 

Upper Cretaceous) is characterized by 

three ornamental stages: multi-tuberculate 

inner-whorls, ombilical bi-tuberculate medium-whorls, 

then finally smooth adult stage. 

Ontogenetic Heterochonies account for their 

adult variability, which extends between both 

paedomorphic (thick/ornamented) morphotype, 

and peramorphic (thin/smooth) morphotype. 

That species may take root in the older Pseudocalycoceras. 

A peramorphocline characterizes 

the evolution of these ammonites and 

their younger relatives, leading to different 

Nigerian and Nigerien, highly compressed 

taxa. Such morphologies seem to be related to 

shallow-water palaeo-environments. The general 

transgressive context leads to the progressive 

scarcity of their supposed ecological 

niches 

2007010245 

螺旋状索的个体发育变化作为 muricid 壳 

饰模式的关键创新 : 腹足类 Muricopsis- 

Murexsul 谱系的示例 = Ontogenetic 

changes of the spiral cords as keys innovation 

of the muricid sculptural patterns: the example 

of the Muricopsis-Murexsul lineages (Gastropoda 

: Muricidae : Muricopsinae). ( 法文 ). 

Merle D; Houart R. Comptes Rendus 

Palevol, 2003, 2(6-7): 547-561 

The primary cords of 68 species belonging 

to the Muricopsis/Murexsul lineages (Priabonian 

to Recent) are analysed. The study of 

their development allows distinguishing three 

derived sculptural patterns in Muricopsis and 

three in the Murexsul group. They appear late 

in the evolutionary history of the studied lineages, 

mainly in tropical waters. They are produced 

by heterochronies affecting precise 

cords by paedomorphosis, whereas others 

poorly evolved or may be hypermorphic. 

These results suggest that the phase of sculptural 

increase yielding the primitive pattern is 

followed by a selective phase, preserving or 

increasing the relief of the probable most 

functional cords. 

2007010246 

法国西南部夏郎德塞诺曼阶和土仑阶下部 

双壳类 Rhynchostreon suborbiculatum 的 

变异和异时性 = Variability and heterochronies 

of Rhynchostreon suborbiculatum (Lamarck, 

1801) (Bivalvia : Ostreoidea : Gryphaeidae 

: Exogyrinae) from the Cenomanian 

and the Lower Turonian of Charentes (SW 

France).. ( 法文 ). Videt B; Neraudeau D. 

73

Comptes Rendus Palevol, 2003, 2(6-7): 563- 

576 

Polymorphism of R. suborbiculatum 

could be summed up as the double occurrence 

of individuals partially costulated and individuals 

completely smooth within the same 

population and a great inter-population variability 

of general size. After having put aside 

all altered assemblages, causes of these polymorphisms 

are analyzed from a palaeoenvironmental 

point of view and in terms of heterochronies 

of development. Environment 

seems to play a minor role in the control of 

these parameters. Among the several combinations 

between these two kinds of polymorphism, 

it is possible to observe a general trend 

to hypermorphosis during the Cenomanian- 

Turonian transgression. 

节肢动物 

2007010247 

甲虫物理特征如何影响其化石保存 = How 

physical characteristics of beetles affect their 

fossil preservation. ( 英文 ). Smith D M; Cook 

A; Nufio C R. Palaios, 2006, 21(3): 305–310 

Although insect size and robustness often 

have been hypothesized to be factors that lead 

to taphonomic bias in the insect fossil record, 

no studies have examined how these factors 

directly affect an insect's preservation potential. 

In this study, laboratory experiments were 

performed on modern Coleoptera (beetles) to 

examine the importance of insect morphology 

on preservation potential. A rotary tumbling 

barrel was used to determine how insect size 

and robustness would influence sinking and 

disarticulation rates. Although size and robustness 

were not correlated directly, beetles 

that were larger and more robust were more 

resistant to disarticulation than smaller, lessrobust 

beetles. Waterlogged specimens gained 

increased flexibility in their exoskeletons, and 

were difficult to puncture. Sinking and disarticulation 

rates were correlated, although it 

took fewer days for beetles to sink than it took 

to begin disarticulating. A white-colored film 

was apparent on all specimens within a few 

days of their introduction to the tumbling barrel; 

however, major disarticulation did not 

occur until the specimens sank to the bottom. 

An examination of the fossil-beetle literature 

also suggests the importance of hardness in 

preservation potential. Although often considered 

fragile, given the right physical characteristics 

and environmental conditions, insects 

can be resistant to disarticulation and decay. 

2007010248 

印度北部下泥盆统 Muth 组冈瓦纳海岸节 

肢动物遗迹生物群 : 古环境和造迹动物的 

行为 = A Gondwanan coastal arthropod 

ichnofauna from the Muth Formation (Lower 

Devonian, northern India): Paleoenvironment 

and tracemaker behavior. ( 英文 ). Draganits E; 

Braddy S J; Briggs D E G. Palaios, 2001, 

16(2): 126–147 

The recent discovery of abundant trace fossils 

in the Lower Devonian Muth Formation (Pin 

Valley, Spiti, northern India) contributes to 

our understanding of the diversity and distribution 

of Early Devonian arthropod activities 

in a marginal marine environment. The ichnoassemblage 

consists of abundant Palmichnium 

antarcticum and Diplichnites gouldi with rarer 

Diplopodichnus biformis, Taenidium barretti, 

Didymaulichnus cf. lyelli, Didymaulyponomos 

cf. rowei, Selenichnites isp., and vertical 

burrows of unclear affinity. The abundance of 

trackways enables the documentation of sizeand 

gait-variations among producers of single 

trackway ichnotaxa. The paleoenvironment of 

the Muth Formation is interpreted as a barrier 

island system. Four different facies associations 

are recognized; arthropod trackways 

occur only in beach to coastal dune environments 

(facies association 2). Most of the Palmichnium 

and Diplichnites trackways are 

interpreted as subaerial. The abundance and 

frequently sub-parallel orientation of the Palmichnium 

antarcticum trackways, predominantly 

perpendicular to the paleocoastline, 

suggest that stylonurid eurypterids, which are 

interpreted as their producer, were migrating 

across the shoreline and climbing up slip 

faces of barrier island dunes. The similarity of 

this ichnofauna to others in marginal marine 

environments of similar age in Antarctica and 

Australia allows the identification of a recurrent 

Lower Devonian ichnocoenosis around 

the margins of eastern Gondwana. 

2007010249 

美国南加州中新世 Barstow 组湖相沉积中 

特殊保存的节肢动物群古生态 = Paleoecology 

of an exceptionally preserved arthropod 

fauna from lake deposits of the Miocene Barstow 

Formation, Southern California, U.S.A. 

( 英文 ). Park L E; Downing K F. 

Palaios, 2001, 16(2): 175–184 

A unique aquatic arthropod Konservat 

Lagerstätte occurs in lacustrine-derived carbonate 

concretions within the Miocene Barstow 

Formation of southern California. Faunal 

74

elements are primarily aquatic, salinitytolerant, 

autochthonous predaceous diving 

beetle larvae, fly larvae and pupae, mosquito 

and thrip larvae, and fairy shrimp. Threedimensional 

preservation of soft tissues is via 

replacement by silica-based minerals as well 

as calcite, celestite, apatite, and gypsum. 

The fauna occurs in three beds (each 1–3 

m thick) within an approximately 100 m sequence 

of predominantly microlaminated 

mudstone deposited in a saline-alkaline lacustrine 

environment. Faunal composition is consistent 

between sites and concretion beds, but 

faunal composition and diversity changed significantly 

during lake history, corresponding 

to differences in brine chemistry as well as 

preservational facies, resulting from the shift 

toward a more nearshore regime. The changes 

in lake chemistry and subsequent changes in 

fauna indicate lake shallowing as well as regional 

and global climate change towards 

greater aridity during the Miocene that also is 

coincident with regional uplift. 

2007010250 

论非洲叶肢介科的分类 = Review of the 

classification of the Family Afrograptidae 

(Crustacea: Conchostraca). ( 中文 ). 沈炎彬 . 古 

生物学报 , 2003, 42(4): 590-597 1 图版 . 

叶肢介化石生长线下缘锯齿状构造曾 

作为非洲叶肢介科 (Afrograpddae) 分类的主 

要特征 , 通过扫描图像 , 从比较解剖学研 

究人手 , 揭示了现生与化石叶肢介壳瓣的 

锯齿构造是由于分布于生长线的一排刚 

毛 , 基部关节脱落而形成的 ; 分析了生长 

线刚毛的形态是属于长针形的轴刚毛 , 主 

要司触角功能 ; 在 5 科 18 属现生叶肢介 

中 , 至少 3 科 7 属 32 种具有生长线刚毛 , 

22 属化石叶肢介有锯齿构造 ; 作者认为这 

一构造被视为非洲叶肢介科分类的主要依 

据是不合适的 , 壳瓣的放射褶或粗瘤构造 

在高级分类上更重要 , 进而对该科的含义 

进行了厘定 ; 从壳瓣具有多条放射褶这一 

构造特征来看 , 它与小叶肢介超科 

(Estheriellioidea) 的成员在发生关系上比较 

密切 , 小叶肢介超科可提升为亚目 

(Estheriellina), 包括小叶肢介超科和非洲叶 

肢介超科 , 是中生代初兴起的一个类群 , 

在白垩纪中期消失。 

2007010251 

介形类系统分类与起源演化的形态、分子 

和化石证据 = The origin and phylogenetic 

relationships of Ostracoda based on molecular, 

morphologic and fossil data. ( 中文 ). 张克云 ; 

郝家胜 ; 杨群 . 微体古生物学报 , 2003, 20(3): 

213-224 

介形类 (Ostracoda) 因其丰富的化石记 

录和广布的海陆现生代表类群 , 而被认为是 

进化生物学中研究生物多样性产生机制和 

演变历程的颇具潜力的重要模式生物。介 

形类在甲壳亚门中的谱系发生位置、起源 

及其内部各类群间的系统关系还存在诸多 

争议。基于其体制构造的形态学特征 , 介形 

类被归入甲壳亚门下的颚足纲 

(Maxillopoda) , 但来自 18S r DNA 序列数据 

分析却显示 Maxillopoda 不是单系群。基于 

化石记录和壳体形态特征 , 高肌虫 (Bradoriida) 

长期以来被认为是介形类的一个祖 

先类群 , 但保存有软躯体的早寒武世化石的 

研究表明 ,Bradoriida 不是介形类甚至可能 

也不属于甲壳类。不同的研究者所强调的 

壳体和肢体形态特征各异 , 导致介形类最大 

的现生类群速足目 (Podocopida) 的四个超科 

之间的关系也存在诸多推测。壳体和肢体 

特征在系统演化意义上的不兼容 , 需要分子 

生物学等证据的介入。分子、形态和化石 

证据的积累及各种信息整合是系统演化研 

究的必然趋势。 

2007010252 

甘肃潮水盆地潮参 1 井侏罗纪介形类化石 

= Jurassic ostracods from Hole Chaocan-1 in 

the Chaoshui Basin, Gansu,nw china. ( 中文 ). 

杨静 ; 王志萍 ; 王海宏 . 微体古生物学报 , 2003, 

20(3): 303-308 1 图版 . 

潮水盆地潮参 1 井发现 Darwinula- 

Timiriasevia 化石组合 , 化石丰富 , 保存完好 , 

组合特征显示其地质时代为中侏罗世晚 

期。 

2007010253 

新疆塔里木盆地北部晚奥陶世中期介形类 

= Ostracodes from the Ordovician of northern 

Tarim Basin,Xinjiang. ( 中文 ). 武涛 . 微体古 

生物学报 , 2003, 20(3): 318-324 2 图版 . 

本文记述的介形类化石采自塔里木盆 

地北部柯坪地区大湾沟剖面坎岭组 , 共计 8 

属 14 种 , 其中包括 2 新种和 3 未定种。 

Thrallella,Octonaria,Predarwinula 三属为本 

介形类组合最为重要且最具特色的分子。 

据此推测 , 坎岭组时代为晚奥陶世中期 

(Caradocian)。 

2007010254 

75

欧洲和亚洲新的古近纪蜜蜂化石 = New 

Palaeogene bees from Europe and Asia. ( 英 

文 ). Nel A; Petrulevicius J F. Alcheringa, 

2003, 27(3/4): 277-293 

New taxa of Apoidea (Apidae and Halictidae) 

described from the Oligocene of France 

and Turkey are Oligoapis beskonakensis gen. 

nov. and sp. nov.; Paraelectrobombus patriciae 

gen. nov. and sp. nov.; Xylocopa celineae 

sp. nov.; and Lasioglossum celinae sp. nov. 

The Palcocene Probombus hirsutus is transferred 

into the Megachilidae, and the Oligocene 

Anthophorites gaudryi (Anthophorini) is 

considered an Insecta incertae sedis. These 

discoveries support Engel's (2001c) hypothesis 

concerning the high diversity of bees during 

the Palaeogene in Western Europe. 

2007010255 

西班牙下白垩统昆虫纲鞘翅目伪天牛科一 

新种 = The Mesozoic Laurasian family 

Parandrexidae (Insecta : Coleoptera), new 

species from the Lower Cretaceous of Spain. 

( 英文 ). Soriano C; Kirejtshuk A G; Delclos X. 

Comptes Rendus Palevol, 2006, 5(6): 779-784 

Martyliopsis laticollis gen. n., sp. n. of 

the Laurasian Mesozoic beetle family Parandrexidae 

from the Barremian (Lower Cretaceous) 

of Spain, is described. The diagnosis of 

the family is revised and emended, and a new 

synonymy for the generic names Parandrexis 

Martynov, 1926 and Parandrexia Hong, 1983 

is proposed. Martynopsis laticollis gen. n., sp. 

n. enlarges the palaeogeogaphic distribution of 

the family from Asia to western Europe, and 

amplifies the fossil record of the family from 

the Middle-Upper Jurassic to the Lower Cretaceous. 

2007010256 

西班牙下白垩统昆虫纲鞘翅目伪天牛科一 

新种 = The Mesozoic Laurasian family 

Parandrexidae (Insecta : Coleoptera), new 

species from the Lower Cretaceous of Spain. 

( 英文 ). Soriano C; Kirejtshuk A G; Delclos X. 


Martyliopsis laticollis gen. n., sp. n. of 

the Laurasian Mesozoic beetle family Parandrexidae 

from the Barremian (Lower Cretaceous) 

of Spain, is described. The diagnosis of 

the family is revised and emended, and a new 

synonymy for the generic names Parandrexis 

Martynov, 1926 and Parandrexia Hong, 1983 

is proposed. Martynopsis laticollis gen. n., sp. 

n. enlarges the palaeogeogaphic distribution of 

the family from Asia to western Europe, and 

amplifies the fossil record of the family from 

the Middle-Upper Jurassic to the Lower Cretaceous. 

2007010257 

内蒙古宁城县道虎沟叶肢介化石群的时代 

= Age of the fossil conchostracans from Daohugou 

of Ningcheng,Inner Mongolia. ( 中文 ). 

沈炎彬 ; 陈丕基 ; 黄迪颖 . 地层学杂志 , 2003, 

27(4): 311-313 

内蒙古赤峰宁城县道虎沟含丰富的叶 

肢介壳瓣及许多珍罕的软体化石 , 计有 1 属 

4 种 : Euestheria ziliu-jingensis Chen, Euestheria 

haifanggouensis Chen ,Euestheria jingyuanensis 

Chen,Euestheria luanpingensis 

Shen etNiu。这些分子都是我国中侏罗世早 

期自流井真叶肢介 (Euestheria ziliujingensis) 

动物群的重要成员 , 以个体较小、壳瓣圆或 

椭圆形、生长带具小网状装饰、种类单 

调、密集群生为特点 , 主要出现于中侏罗世 

早中期 (Bajocian- MiddleBothonia)。特别是 

Euestheria luanpingensis Shen et Niu 及其软 

体化石在道虎沟的发现 , 证明其层位应与冀 

北滦平九龙山组相当。道虎沟叶肢介群与 

中侏罗世晚期的假线叶肢介 (Pseudograpta) 

动物群的面貌相差甚远 , 与比其层位更高的 

大北沟组的尼斯脱叶肢介 (Nestoria) 动物群 

及义县组的东方叶肢介 (Eosestheria) 动物群 

迥然不同 . 

2007010258 

阿根廷拉里奥哈省上中新统 Desencuentro 

组介形类和轮藻化石 = Ostracods (Crustacea, 

Ostracoda) and charophytes (Chlorophyta, 

Charales) from the Desencuentro Formation 

(Upper Miocene), La Rioja province, Argentina. 

( 其他 ). Cusminsky G; Garcia A; Herbst 

R. Ameghiniana, 2006, 43(2): 327-338 

The association has low diversity with 

six ostracod taxa: Encypris sp., Darwinula sp., 

Cyamocytheridea sp., Cyprideis salebrosa 

hartmanni Ramirez, Limnocythere aff. L. reticulata 

Sharpe, Limnocythere sp. and two 

charophytes: Chara zeylanica s. l. Klein ex 

Willdenow and Chara musacchioi Garcia sp. 

nov. The availability of twenty well preserved 

gyrogonites of Chara musacchioi sp. nov. allowed 

to observe the intra-populational morphological 

variability, to relate the new species 

with the extant Chara hornemannii 

Wallman, and to conclude that it is a new species. 

The assemblage indicates a calm aquatic 

environment with oligohaline to mesohaline 

water, with a possible input of fresher water, 

76

in a tropical to subtropical area, with mean 

temperature of about 15-20 degrees C. 

2007010259 

阿根廷西北部早奥陶世油栉虫型三叶虫 

Jujuyaspis keideli 个体发育 = Ontogeny of 

the Early Ordovician olenid trilobite Jujuyaspis 

keideli Kobayashi from northwestern 

Argentina. ( 英文 ). Tortello M F; Clarkson E 

N K. Ameghiniana, 2003, 40(3): 257-275 

The Early Ordovician olenid trilobite Jujuyaspis 

keideli Kobayashi is well-preserved 

in black shale facies of the Santa Rosita 

Fomation at Purmamarca, northwestern Argentina. 

Although protaspides are not represented 

in the collections, isolated tagmata and 

articulated specimens from the early meraspid 

stages onwards are available for ontogenetic 

study. Meraspid Group 1 is characterized by 

having an hexagonal cephalic outline, three 

distinct glabellar furrows, and seven marginal 

spines. In meraspid Group 2 the cephalon has 

become reniform in outline, the glabellar furrows 

are less developed, and the fixigenae 

exhibit a pair of ocular ridges. Meraspid 

Group 3 is characterized by an adult-like 

cephalon lacking both ocular ridges and paired 

marginal spines. At this stage the thorax has 

very long pleural spines which, contrasting 

greatly with those of the adult, are laterally 

splayed out. In meraspid Group 4 the cephalon 

bears a well-developed occipital spine or a 

conspicuous occipital node, the glabella possesses 

two pairs of lateral furrows, and the 

thorax exhibits axial nodes on the anterior 

segments and shorter, more posteriorly directed 

lateral spines. Early holaspides retain 

some of the later meraspid morphological features. 

The hypostome of the species is documented 

for the first time. Information on the 

intraspecific variability of J. keideli enables us 

to discuss its systematic affinities in a new 

context. A monospecific, age-sorted clustered 

assemblage assignable to holaspid Group 1 

could represent specimens that aggregated 

together for synchronized exuviation. Early 

meraspides of Jujuyaspis are assumed to be 

pelagic, a fact that must have facilitated the 

worldwide distribution of the genus, whereas 

holaspides may have had a nekto-benthic 

mode of life. 

2007010260 

阿根廷胡胡伊前科迪耶拉奥陶纪古足类、 

光足类和 eridostraca 介形类 = Ordovician 

palaeocope, leiocope and eridostraca ostracods 

from the Precordillera of San Juan, Argentina. 

( 其他 ). Salas M J. Ameghiniana, 2003, 40(3): 

345-360 

Ostracod faunas from the Early Llanvirnian 

to Early Caradocian rocks of the Precordillera 

Basin (Las Chacritas and Las 

Aguaditas Formations) are described. One 

new genus, Chattertonella gen. nov., and nine 

species are recognized, three of which are new 

(Chattertonella rugosa gen. et sp. nov., Saccelatia 

minuta sp. nov. and Conchoprimitia 

elongata sp. nov.). Two different associations 

are recognized, one Early Llanvirnian and 

another the Early Caradocian in age. They 

allow local correlation between the basal part 

of the Las Aguaditas Formation and the Las 

Chacritas Formation and between the middle 

part of the Las Aguaditas Formation and the 

Mogotes Azules section. Two of the nine genera 

described are endemic, Saccelatia also 

occurs in Laurentia and Ningulella and Ordovizona 

are also known in Laurentia and Baltica. 

2007010261 

朝鲜南部早白垩世 Mesoraphidiidae 科 

Raphidioptera 类骆驼虫化石 = Fossil 

snakeflies from the Early Cretaceous of southern 

Korea (Raphidioptera: Mesoraphidiidae). 

( 英文 ). Engel M S; Lim J-D; Baek K-S. Neues 


Monatschefte, 2006, (4): 249-256 

Two new mesoraphidiid snakeflies are 

described and figured from the Early Cretaceous 

of southern Korea. Mesoraphidia koreensis 

n. sp. and M. phantasma n. sp. are distinguished 

from other mesoraphidiids on the 

basis on wing venation. The age and distribution 

of Mesoraphidia species are briefly reviewed. 

These are the first fossil snakeflies 

recorded from the Korean Peninsula. 

2007010262 

阿根廷前科迪耶拉圣胡安组三叶虫 : 多股 

虫科 = Trilobites from the San Juan formation, 

Argentine Precordillera: Pliomeridae Raymond.. 

( 其他 ). Vaccari N E. 

Ameghiniana, 2003, 40(2): 239-248 

A revision of pliomerid trilobites from 

the San Juan Formation, Argentine Precordillera 

is carried out. It includes a new diagnosis 

for the genus Benedettia Toro and Monaldi, 

which is further included within the Subfamily 

Cybelopsinae Fortey Besides, Encrinurus 

niquivilensis Harrington and Leanza and 

Benedettia huaquensis Toro and Monaldi are 

regarded as synonyms. Two new species: B. 

77

margaritae (Early Arenig) and Pliomerina 

sanjuanina (Early Llanvirn) are recognized. 

The latter is clearly distinguished among the 

pangondwanic species of the trilobite Pliomerina 

Chugaeva by its unusual pygidium. 

2007010263 

古昆虫学的发展、存在问题与展望 = The 

development ,existing problems and prospect 

on the palaeoentomology. ( 中文 ). 洪友崇 . 地 

质通报 , 2003, 22(1): 71-86 2 图版 . 

对国际古昆虫学的发展作了回顾 , 大体 

上将其分为两个大的发展阶段 : 开始与积累 

阶段 , 发展和繁荣阶段。这两个阶段又可分 

为 8 个时期。在古昆虫学的发展史上曾有 

过 3 次历史性的重要总结 , 即 HandlirschA. 

(1906-1908) 的《 DieFossilInsektenunddie 

Phylogeniederrezenten Formen 》 , RohdendorfB.B.etal 

(1962) 的《Foundamentalsof Paleonentomology 

》 ,Carpenter F.A.(1992) 的 

《Hexapoda》, 以及各国区域性昆虫化石研 

究和以分类为核心的总结 , 等等。通过国际 

古昆虫工作者的共同努力 , 一部以分类为核 

心的古昆虫学专著基本完成。在国际古昆 

虫学及中国古昆虫学研究新成就的基础上 , 

提出了古昆虫学研究中还存在的一些问题 : 

如加强基础研究工作 , 包括化石采集、分 

类、描述 ; 古昆虫学研究与地质学、地质背 

景相结合 ; 化石昆虫群的演化序列及其发展 

史的建立 ; 昆虫的起源 ; 加强国际合作与交流 , 

崇尚科学精神 , 促进学科发展等。 

2007010264 

冀北滦平盆地大店子组中网雕饰叶肢介 

Clithrograpta 属的发现及其意义 = Discovery 

of conchostracan genus Clithrograpta and 

its significance in the Dadianzi Formation,Luanping 

basin,northern Hebei. ( 中文 ). 

牛绍武 ; 李佩贤 ; 田树刚 ; 庞其清 ; 柳永清 . 地质 

通报 , 2003, 22(2): 95-104 3 图版 . 

在深入研究滦平盆地大店子组叶肢介 

化石时 , 于该组上部首次发现了网雕饰叶肢 

介 Clithrograpta 属 , 产出层数多 , 个体数量大 , 

种的分异度高 , 为冀北滦平盆地大店子组的 

地层划分与对比 , 正确建立冀北 — 辽西陆相 

侏罗 — 白垩系的地层格架 , 提供了关键而有 

力的古生物证据。根据这一发现和大北沟 

组至西瓜园组叶肢介化石组合序列 , 本区大 

店子组上部 (3~4 段 ) 可与辽西建昌盆地 “ 义 

县组 ” 下部 ( 原大新房子组 ) 对比 ; 证明辽西地 

区缺失相当于本区的大店子组下部 (1~2 段 ) 

地层 , 西瓜园组大体相当于辽西的义县组。 

2007010265 

贵州关岭生物群海百合 Traumatocrinus 的 

再研究 = Restudy of the crinoids Traumatocrinus 

of the Guanling biota,Guizhou. ( 中 

文 ). 王传尚 ; 汪啸风 ; 陈孝红 ; 陈立德 . 地质通 

报 , 2003, 22(4): 248-253 2 图版 . 

在前人的研究基础上 , 通过对大量新发 

掘的贵州关岭地区晚三叠世海百合化石标 

本的再研究 , 肯定了 Traumatocrinus 的有效 

性。根据目前的材料 , 认为该属只有 1 个有 

效种 , 即 Traumatocrinus hsui; 而根据化石的 

埋藏学特征 , 认为幼年体 Traumatocrinus hsui 

营假浮游生活 , 成年体是否能够适应底栖生 

活环境尚需进一步证实。 

2007010266 

贵州关岭地区中 — 上三叠统海参骨片化石 

的首次发现 = Discovery of Middle-Upper 

Triassic holothurian sclerites from 

Yongning,Guanling,Guizhou. ( 中文 ). 陈辉明 ; 

陈立德 ; 汪啸风 ; 陈孝红 . 地质通报 , 2003, 

22(4): 266-270 1 图版 . 

报道了贵州关岭地区中 — 上三叠统竹 

杆坡组发现的海参骨片化石 5 属 6 种及 2 

个属种未定的形态类型。分析了海参化石 

属种的历史分布特征 , 上述化石指示竹杆坡 

组为晚三叠世沉积产物。这一发现进一步 

丰富了关岭生物群的内容 , 为探讨中国三叠 

纪海参骨片化石的分类及演化增加了新的 

资料。 

2007010267 

滇中妥甸组中首次发现昆虫化石 = Discovery 

of fossil insects in the Tuodian Formation,central 

Yunnan. ( 中文 ). 张志军 ; 卢立伍 ; 

靳悦高 ; 方晓思 ; 洪友崇 . 地质通报 , 2003, 

22(6): 452-455 1 图版 . 

首次在云南滇中地区晚侏罗世妥甸组 

滥泥阱剖面和级山坡一带发现昆虫化石 2 

新种 : Mesoblattula tuodianensis sp. nov. 和 

Neorthophlebia yunnanensis sp. nov., 未定种 

3 种。其中长翅目新直脉蝎蛉新直脉蝎蛉属 

(Neorthophlebia) 在国内为首次发现。 

2007010268 

拟柯尔定虫属的次异名 : 寒武纪三叶虫古 

舒马德虫属 = Eoshumardia (Trilobita, Cambrian), 

a junior synonym of Koldinioidia. ( 英 

文 ). Zhu Xuejian; Peng Shancheng. Alcheringa, 

2006, 30(2): 183-189 

78

Well-preserved internal and external 

moulds of a shumardiid species are described 

from the late Furongian (Late Cambrian) 

"Fengshan Formation" at Poben, Napo, 

southwestern Guangxi, which is close to the 

type locality of Shumardia orientalis, the type 

species of Eoshumardia. All features observed 

on the internal moulds indicate that the new 

material is definitely S. orientalis, whereas the 

morphology of the external moulds indicates 

that S. orientalis should be referred to Koldinioidia. 

The change of generic assignment of 

the type species means that Eoshumardia is a 

junior synonym of Koldinioidia. 

2007010269 

志留纪三叶虫 Dalmanites wandongensis 的 

系统分类、古环境和地层及其澳大利亚维 

多利亚 Kilmore 地区构造地质的意义 = 

Systematics, palaeoenvironments and stratigraphy 

of the Silurian trilobite Dalmanites 

wandongensis Gill, 1948 and its bearing on 

the structural geology of the Kilmore area, 

Victoria. ( 英文 ). Sandford A C. Alcheringa, 

2006, 30(2): 213-232 

One of the most prolific trilobites in the 

mid-Palaeozoic of central Victoria is the dalmanitid 

Dalmanites wandongensis Gill, 1948. 

Extensive museum collections permit a revised 

diagnosis and a redescription of the species, 

and an interpretation of its distribution. 

The affinities of D. wandongensis lie with 

South American species assigned to Dalmanites 

and the closely related Kasachstania 

rather than northern hemisphere taxa including 

the D. caudata group. It occurs between 

Heathcote and Yan Yean in central Victoria, 

in late Wenlock and early Ludlow (Silurian) 

strata of the Dargile Group, on the eastern 

margins of the Melbourne Zone; its greatest 

abundance is between Kilmore and Wandong, 

where it is documented from over fifty localities, 

occurring rarely with other trilobite taxa. 

At Heathcote, Upper Plenty, Yan Yean and 

Kilmore East D. wandongensis stratigraphically 

underlies a more diverse trilobite fauna 

dominated by the encrinurid Cromus simpliciculus. 

This trilobite faunal succession 

defines a significant macrofaunal biostratigraphic 

datum in the sequence, complementing 

brachiopod and graptolite zonations. This 

datum is coincident with a subtle but widespread 

change in lithology that defines the 

lithostratigraphic boundary between the Yan 

Yean Formation and the Melbourne Formation. 

In the structurally complex and poorly exposed 

sequences of the Kilmore East area the 

distribution of D. wandongensis is used as a 

primary tool in mapping the distribution of 

these units. Outcrop patterns reveal the presence 

of two large scale east-northeast-oriented 

faults traversing the area that support a model 

of deformation for the Melbourne Zone in 

which transverse shearing is significant. Taphofacies 

and biofacies distribution in the Yan 

Yean Formation indicate a deep-water shelf 

depositional environment, at depths below 

maximum storm-wave base in the Kilmore- 

Wandong area, deepening eastwards, with 

outer shelf environments between Yan Yean 

and Christmas Hills. 

2007010270 

化石节肢动物的器官保存 : 实验性研究 = 

The organic preservation of fossil arthropods: 

an experimental study. ( 英文 ). Gupta N S; 

Michels R; Briggs D E G; Evershed R P; Pancost 

R D. Proceedings of the Royal Society B: 

Biological Sciences, 2006, 273(1600): 2777 - 

2783 

Modern arthropod cuticles consist of chitin 

fibres in a protein matrix, but those of fossil 

arthropods with an organic exoskeleton, 

particularly older than Tertiary, contain a 

dominant aliphatic component. This apparent 

contradiction was examined by subjecting 

modern cockroach, scorpion and shrimp cuticle 

to artificial maturation 

(350°C/700bars/24h) following various 

chemical treatments, and analysing the products 

with pyrolysis–gas chromatography/mass 

spectrometry (Py–GC/MS). Analysis of artificially 

matured untreated cuticle yielded moieties 

related to phenols and alkylated substituents, 

pyridines, pyrroles and possibly indenes 

(derived from chitin). n-Alkyl amides, C 16 and 

C 18 fatty acids and alkane/alk-1-ene homologues 

ranging from C 9 to C 19 were also generated, 

the last indicating the presence of an n- 

alkyl component, similar in composition to 

that encountered in fossil arthropods. Similar 

pyrolysates were obtained from matured pure 

C 16 and C 18 fatty acids. Py–GC/MS of cuticles 

matured after lipid extraction and hydrolysis 

did not yield any aliphatic polymer. This provides 

direct experimental evidence that lipids 

incorporated from the cuticle were the source 

of aliphatic polymer. This process of in situ 

polymerization appears to account for most of 

the fossil record of terrestrial arthropods as 

well as marine arthropods that lacked a 

biomineralized exoskeleton. 

2007010271 

79

河北下白垩统新建中华脉属 ( 新名 ) 

( Hebeigramma nom. nov.) 替代晚出名 

Mesogramma Hong, 1984 ( 中华脉科 ) = 

Hebeigramma nom.nov.,a new name for 

Mesogramma Hong,1984 (Caloneurodea) 

from the Lower Cretaceous of Hebei Province,China. 

( 英文 ). 洪友崇 . 地质通报 , 2003, 

22(9): 686-687 

1984 年 , 笔者发表河北早白垩世华脉目 

(Caloneurodea) 的中华脉科、属 : Mesogrammatidae 

Hong, 1984 和 Mesogramma 

Hong,1984。属名与 1850 年 Stephens 采用过 

的鳞翅目 Mesogramma 属和 1865,1872,Loew 

采用过的双翅目 Mesograpta 属是异物同名 , 

必须废除笔者后来建立的科、属学名 , 重新 

命名 , 以维护《法规》中命名优先权的原 

则。故原 Mesogramma Hong,1984 属名重新 

命名为 Hebeigramma nom.nov., 原 

MesogrammatidaeHong, 1984 科名随属名的 

更改而重新命名为 Hebeigrammidae 

nom.nov., 在此申明。 

2007010272 

英国晚石炭世昆虫类古网翅目新发现的 

homoiopterids 化石 = New homoiopterids 

from the Late Carboniferous of England (Insecta 

: Palaeodictyoptera). ( 英文 ). Prokop J; 

Smith R; Jarzembowski E A; Nel A. Comptes 


A new palaeodictyopteran, Anglopterum 

magnificum gen. et sp. n., is described from 

concretions of Late Carboniferous (Langsettian) 

in the Lancashire County (UK). The new 

genus, based on the hind-wing venation, is 

attributed to Homoiopteridae and compared 

with other homoiopterid genera. A previously 

figured homoiopterid from Late Carboniferous 

(Upper Asturian) roof shales in Somerset (UK) 

is bearing venation pattern of anal area similar 

to Mazonopterum wolfforum Kukalova-Peck 

and Richardson, 1983. These are the first formally 

described species of Homoioptericlae 

from the British Isles. Furthermore, their similarity 

in venation pattern to Mazonopterum 

wolfforum Kukalova-Peck and Richardson, 

1983 from Mazon Creek (USA) provides evidence 

for a Euramerican connection during 

the Late Carboniferous. 

2007010273 

法国上石炭统 Montceau 特异埋葬中的甲 

壳类 Syncarid = Syncarid Crustaceans from 

the Montceau Lagerstätte (upper Carboniferous; 

France). ( 英文 ). Perrier V; Vannier J; 

Racheboeuf P R; Charbonnier S; Chabard D; 

Sotty D. Palaeontology, 2006, 49(3): 647-672 

Key aspects of the morphology, autecology, 

systematics and taphonomy of the crustacean 

syncarids from the Montceau Lagerstätte 

(Upper Carboniferous, Stephanian B; France) 

are presented. Palaeocaris secretanae is the 

most abundant faunal element of the Montceau 

biota and shows striking morphological 

similarities with Palaeocaris typus from the 

Mazon Creek Lagerstätte (Westphalian D; 

Illinois, USA). Palaeocaris secretanae was a 

shrimp-like animal with a short head (no head 

shield), large mandibles, 14 trunk segments 

(the first one being reduced) and a fan-like 

caudal termination. Both the body and the appendage 

design indicate abilities for crawling 

on the substratum (slender endopods) and for 

escape reaction (uropodal fan, pleonal flexibility), 

although swimming activities may have 

been reduced (trunk appendages with small 

flap-like exopods). Details of the appendages 

involved in feeding, e.g. mandibles and maxillipeds, 

indicate poor ability for predation but 

point to an omnivorous detritus feeding mode. 

Poorly developed respiratory organs (small 

cylindrical epipods) suggest a relatively low 

level of locomotory activity. The field of vision 

may have been large and panoramic 

(stalked eyes). Rows of pores on 12 trunk 

segments are interpreted as possible sensory 

organs used for current detection. Females 

were brooding eggs (clusters of eggs preserved 

along anteroventral trunk). Microprobe 

analysis indicates that siderite is the major 

component of the nodules. Four events played 

a key-role in the three-dimensional preservation 

of syncarids: (1) rapid burial, (2) minimal 

decomposition, (3) phosphatic mineralization 

shortly after the animal's death and (4) nodule 

formation around the carcass. Palaeocaris 

secretanae is morphologically close to Recent 

syncarids such Anaspides tasmaniae (freshwater 

streams, Australia) in its general body plan 

and detailed anatomy, e.g. mouth parts, indicating 

morphological stasis in syncarids over 

more than 200 million years. 

2007010274 

瑞典上寒武统 "Orsten" 产地 Phosphatocopina 

( 甲壳类 ) 的形态 , 个体发育和系统发 

育 = Morphology, ontogeny and phylogeny of 

the Phosphatocopina (Crustacea) from the 

Upper Cambrian "Orsten" of Sweden.. ( 英文 ). 

Maas A; Waloszek D; Muller K J. Fossils and 

Strata, 2003, (49): 1-238 

80

About 2500 specimens of different Phosphatocopina 

species from the Upper Cambrian 

"Orsten" of Sweden were investigated using 

scanning electron microscopy with reference 

to their morphology, ontogeny, systematics 

and phylogeny. Major morphological aspects 

of the shields and partly of the ventral morphology 

are described and documented. Ontogeny 

was described and documented in detail 

for the best preserved species, Hesslandona 

Unisulcata. Characters of all species 

were compared and a character matrix was 

drawn up, forming the basis for a computeraided 

phylogenetic analysis of the Phosphatocopina. 

2007010275 

日本东北部中新统新宿卡组 ( 新宿峠组 ) 

的一个豆蟹 (Decapoda:Brachyura: Pinnotheridae) 

新种 = A new pinnotherid crab 

(Decapoda: Brachyura: Pinnotheridae) from 

the Miocene Niijukutoge Formation, northeast 

Japan. ( 英文 ). Hisayoshi Kato. Paleontological 

Research, 2005, 9(1): 73-78 

A new fossil pinnotherid crab, Globihexapus 

kosekii sp. nov. is described from the 

early to middle Miocene Niijukutoge Formation 

in Shichikashuku-machi, Miyagi Prefecture, 

northeast Japan. Based on the presence of 

five pairs of pereiopods as revealed in an examination 

of the present material and reexamination 

of the types of Globihexapus 

Schweitzer and Feldmann, 2001, this genus is 

transferred from the family Hexapodidae 

Miers, 1886 to the subfamily Asthenognathinae 

Stimpson, 1858 of the family Pinnotheridae 

de Haan, 1833. 

2007010276 

日本西南部淡路岛岩屋组 (Iwaya Formation) 

的始新世介形虫 = Eocene ostracodes 

from the Iwaya Formation on Awajishima 

Island, southwestern Japan. ( 英文 ). Yamaguchi 

T; Matsubara T; Kamiya T. Paleontological 

Research, 2005, 9(4): 305-318 

The ostracode fauna from the middleupper 

Eocene Iwaya Formation on Awajishima 

Island, Hyogo Prefecture, southwestern 

Japan was studied to reveal a band of the 

Eocene ostracode faunal spec trum in the middle 

latitudes of the northwestern Pacific. 

Based on lithofacies and previously reported 

cal careous nannofossiis, molluscs, and benthic 

foraminifers, the ostracodes were found to 

have inhabited inner shelf environments. The 

ostracodes entirely differ from the Eoceneearliest 

Oligocene faunas in Kyushu, southwestern 

Japan and the East China Sea, both in 

generic and specific composition. The difference 

is con sidered to be due to paleoclimatic 

and paleogeographic differences between 

Awajishima Island and more southern latitudes 

at that time. 

2007010277 

晚泥盆世镜眼虫类三叶虫的发育变异 = 

Developmental variations in Neodevonian 

phacopide trilobites.. ( 法文 ). Cronier C; 

Courville P. Comptes Rendus Palevol, 2003, 

2(6-7): 577-585 

Heterochrony refers to changes in the 

timing and the rate of development of ancestral 

morphological features. This phenomenon 

has been observed in some neodevonian 

phacopide trilobites. Their evolution is 

marked by progressive displacement of the 

visual complex towards the external margins, 

accompanied by displacement of the facial 

suture. This evolutionary pathway is a result 

of paedomorphosis. These features seem to be 

adaptative, and may occur in all lineages, 

leading to convergences between several taxa. 

A paedomorphic phenomenon also concerns 

the change of moulting behaviour. This particular 

feature may not be related to environment 

but represents a feature inherited from 

the ancestral forms. 

2007010278 

经化石校准的分子演化研究表明 : 潜叶蛾 

的辐射晚于其主要寄主植物出现百万年后 

= Fossil-calibrated molecular phylogenies reveal 

that leaf-mining moths radiated millions 

of years after their host plants. ( 英文 ). Lopez- 

Vaamonde C; Wikstrom N; Labandeira C; 

Godfray H C J; Goodman S J; Cook J M. 


1314-1326 

Coevolution has been hypothesized as the 

main driving force for the remarkable diversity 

of insect–plant associations. Dating of 

insect and plant phylogenies allows us to test 

coevolutionary hypotheses and distinguish 

between the contemporaneous radiation of 

interacting lineages vs. insect 'host tracking' of 

previously diversified plants. Here, we used 

nuclear DNA to reconstruct a molecular phylogeny 

for 100 species of Phyllonorycter leafmining 

moths and 36 outgroup taxa. Ages for 

nodes in the moth phylogeny were estimated 

using a combination of a penalized likelihood 

method and a Bayesian approach, which takes 

into account phylogenetic uncertainty. To con- 

81

vert the relative ages of the moths into dates, 

we used an absolute calibration point from the 

fossil record. The age estimates of (a selection 

of) moth clades were then compared with fossil-based 

age estimates of their host plants. 

Our results show that the principal radiation of 

Phyllonorycter leaf-mining moths occurred 

well after the main radiation of their host 

plants and may represent the dominant associational 

mode in the fossil record. 

2007010279 

Sinea spinipes (Heteroptera: Reduviidae) 幼 

虫的描述 , 及其生活史和实验室培养 = 

Life History and Laboratory Rearing of Sinea 

spinipes(Heteroptera: Reduviidae) with Descriptions 

of Immature Stages. ( 英文 ). Shurtz 

R A; McPherson J E. Annals of the Entomological 

Society of America, 2005, 98(1): 18-36 

The life history of the harpactorine reduviid 

Sinea spinipes (Herrich-Schaeffer) was 

studied in southern Illinois from February 

2001 to November 2002, and the immature 

stages were described. The bug also was 

reared from egg to adult under controlled 

laboratory conditions. This univoltine species 

occurred on vegetation along roadsides within 

forests, in open fields beneath or near scattered 

trees, and along forest edges. It overwinters 

as adults, which emerged in mid-April 

and were found through early September. 

Nymphs were found from early June through 

late September. The bug was reared in the 

laboratory on larval beet armyworm, Spodoptera 

exigua (Hübner), at 26 ± 3.0°C under a 

photoperiod of 16:8 (L:D) h. The incubation 

period averaged 15.13 d; eyespots appeared in 

7 d. The five stadia averaged 8.15, 9.22, 9.21, 

11.43, and 19.59 d, respectively. The total 

developmental period averaged 72.73 d. Instars 

can be distinguished by differences in 

several anatomical features, including body 

length and width and progressive development 

of size, number, and pattern of spines. 

2007010280 

新热带区 Choreutid 属 Rhobonda Walker 

and Zodia Heppner ( 鳞翅目 : Choreutidae 

科 ) 幼虫和蛹的描述 = Larval and Pupal Descriptions 

of the Neotropical Choreutid Genera 

Rhobonda Walker and Zodia Heppner 

(Lepidoptera: Choreutidae). ( 英文 ). Rota J. 

Annals of the Entomological Society of America, 

2005, 98(1): 37-47 

Larvae and pupae of two Neotropical 

choreutids, Rhobonda gaurisana Walker and 

Zodia scintillana (Walker) (Lepidoptera: 

Choreutidae), are described. Photographs, 

drawings, and scanning electron micrographs 

are provided for both species, and observations 

on larval behavior and biology are reported. 

The larval head in both genera is reinterpreted 

as being semiprognathous. The D2 

setae on A9 arise from a common middorsal 

pinaculum in Rhobonda, Zodia, and other 

choreutid genera. Previously, this character 

was regarded as one of the defining characters 

for the Tortricidae. The implications of its 

presence in choreutids are discussed. The 

variability of the arrangement of pupal dorsal 

spines between the Millieriinae and the other 

two subfamilies Brenthiinae and Choreutinae 

is so great that the inclusion of the Millieriinae 

with the Choreutidae is questioned. 

2007010281 

Cervantistellus: 墨西哥 Acanthocephalini 

的一个新属 ( 半翅目 : Coreidae 科 : Coreinae) 

= Cervantistellus: A New Genus of 

Acanthocephalini from Mexico (Hemiptera: 

Coreidae: Coreinae). ( 英文 ). Brailovsky H; 

Barrera E. Annals of the Entomological Society 

of America, 2005, 98(1): 48-54 

Cervantistellus Brailovsky & Barrera, new 

genus, and two new species (C. guerrerensis 

and C. insolitus) from México are described in 

the tribe Acanthocephalini (Coreidae). The 

nymphs and adults are associated with bamboo. 

A key to the known species is included. 

2007010282 

Dohrniphora(Diptera: Phoridae) 的一些新 

种 = New Species of Dohrniphora Related to 

D. longirostrata (Diptera: Phoridae). ( 英文 ). 

Kung G A; Brown B V. Annals of the Entomological 

Society of America, 2005, 98(1): 

55-62 

Five new species of Neotropical Dohrniphora 

related to D. longirostrata are described: 

D. apharea, D. bicostula, D. 

conlanorum, D. oricilla, and D. perpendicularis. 

Most species differences are found in 

the area of the ventrobasal concavity of the 

posterior face of the male hind femur. The D. 

longirostrata-group is diagnosed, each species 

illustrated with scanning electron micrographs, 

and a key to males of all species is presented. 

2007010283 

Megamelus scutellaris ( 半翅目 : Delphacidae 

科 ) 的生活史及其未成熟阶段的描述 = 

82

Life History of Megamelus scutellaris with 

Description of Immature Stages (Hemiptera: 

Delphacidae). ( 英文 ). Sosa A J; Marino De 

Remes Lenicov A M; Mariani R; Cordo H A. 

Annals of the Entomological Society of America, 

2005, 98(1): 66-72 

The five immature stages of Megamelus 

scutellaris Berg (Hemiptera: Delphacidae) are 

described and illustrated. The main characters 

that distinguish the various stages are body 

size, number of tarsomeres and tibial spines, 

color, and number of teeth on the metatibial 

spur. New biological data based on laboratory 

rearing and field observations show that M. 

scutellaris can carry out its biological cycle 

successfully on water hyacinth, Eichhornia 

crassipes (Martius) Solms Laubach (Pontederiaceae). 

Mating occurs close to the water 

level and one to four eggs per scar are laid in 

apical portion of petiole and pseudolaminae. 

Ovipositional scars are recognized by three 

parallel marks. In addition, the efficient rearing 

in captivity, the high survivorship registered, 

and overwintering on only water hyacinth 

suggest M. scutellaris as a potential biocontrol 

agent of this invasive aquatic weed. 

2007010284 

Permocoleus, 北美二叠纪最老的一个甲虫新 

属 = Permocoleus, New Genus, the First Permian 

Beetle (Coleoptera) from North America. 

( 英文 ). Lubkin S H; EngelA M S. Annals of 

the Entomological Society of America, 2005, 

98(1): 73-76 

Permocoleus wellingtonensis, new genus and 

new species, is based on an elytron from the 

Permian Wellington Formation of Oklahoma 

and is the only Paleozoic record of the order 

Coleoptera from North America and the oldest 

record for the New World. Until now, Permian 

Coleoptera were known only from Europe, 

Australia, southern Africa, and South America 

but were conspicuously absent from North 

America, despite the Wellington Formation 

being among the most diverse deposits of 

Permian insects. Permocoleus provides evidence 

that early beetles were globally distributed. 

2007010285 

地中海果蝇 ( 双翅目 : Tephritidae) 在以色列 

中部地区的时空分布模式 = Spatiotemporal 

Distribution Patterns of Mediterranean Fruit 

Fly (Diptera: Tephritidae) in the Central Region 

of Israel. ( 英文 ). Israely N; Ziv Y; Oman 

S D. Annals of the Entomological Society of 

America, 2005, 98(1): 77-84 

The geographical distribution of Mediterranean 

fruit fly, Ceratitis capitata (Wiedemann), 

is limited to relatively warm regions 

and does not cross the 41° north latitude. A 

recent study has demonstrated that, in contrast 

to the earlier suggested hypothesis, that Mediterranean 

fruit fly can survive the winter in 

relatively cold areas, it does not overwinter in 

such areas but reinvades them annually from 

adjacent warmer sites. In the present work, we 

use a large-scale spatial approach to describe 

the spatiotemporal dynamics of Mediterranean 

fruit fly in a large heterogeneous landscape as 

well as discuss the consequences of such dynamics 

for basic research and control practices. 

During a 2-yr period (2000–2001), over the 

central part of Israel (6,875 km2), adult males 

were monitored and recorded weekly by using 

Steiner-like traps. Data obtained were incorporated 

into a geographic information system 

to produce weekly distribution maps of C. 

capitata within the study area. The patterns of 

change in population sizes through time were 

consistent in both years, suggesting that C. 

capitata overwinters along the coastal plain 

and the Jordan Valley. Reinvasion to the 

higher altitudes is followed by a population 

increase in the warmer, lower altitudes, during 

the spring and early summer. By midsummer, 

flies were found at all sites within the study 

area. However, flies started disappearing from 

the high-altitude areas during fall and were 

absent from these areas during winter. We 

suggest that understanding such spatiotemporal 

dynamics has far-reaching consequences 

for future basic research as well as control and 

eradication programs. 

2007010286 

介形类对摩洛哥 Essaouira-Agadir 盆地下 

白垩统巴雷姆期 - 凡兰吟期层序解释的贡献 

= Contribution of the ostracods to the sequential 

interpretation of the Lower Cretaceous 

(Berriasian-Valanginian) of the Essaouira- 

Agadir Basin (Morocco).. ( 法文 ). Rossi A; 

Rey J; Andreu B; Taj-Eddine K. Comptes 


Contribution of the ostracods to the sequential 

interpretation of the Lower Cretaceous 

(Berriasian-Valanginian) of the Essaouira-Agadir 

Basin (Morocco). The analysis 

of the ostracod fauna from the Berriasian- 

Valanginian of the Essaouira-Agadir Basin 

(Morocco) allows us to make a narrow relationship 

between the sequential evolution (es- 

83

tablished on sedimentary, biostratigraphical 

and geochemical data) and the evolution of 

statistical parameters of ostracods. So, the 

number of individuals and the number of species 

present comparable fluctuations and follow 

perfectly the sequential evolution; classes 

of dominant and fortuitous frequency are the 

most meaningful, the specific renewal rate 

shows extremes values at the limits of sequences 

and at the basis of transgressive systems 

tracts. 

2007010287 

南美洲南部 3 个地区火蚁 Decapitating 

Flies(Diptera: Phoridae: Pseudacteon) 的分 

布和丰度 = Distribution and Abundance of 

Fire Ant Decapitating Flies (Diptera: Phoridae: 

Pseudacteon) in Three Regions of Southern 

South America. ( 英文 ). Calcaterra L A; Porter 

S D; Briano J A. Annals of the Entomological 


The distribution and abundance of fire 

ant decapitating flies (Diptera: Phoridae: 

Pseudacteon Coquillett) were studied in three 

regions of southern South America, primarily 

from September 2002 to September 2004. A 

total of 2,421 flies belonging to 14 Pseudacteon 

species were found at 51% of the 662 fire 

ant mounds examined at 125 collecting sites. 

Flies occurred in a variety of habitats at altitudes 

from sea level to 2,280 m. Pseudacteon 

obtusus Borgmeier (large form) was found at 

the highest altitude and at the most western 

longitude. Flies were active between 16 and 

37°C, 20 and 90% RH, and 0 and 11.6 km/h 

wind speed. Pseudacteon curvatus Borgmeier 

showed the highest abundance and one of the 

broadest geographical distributions. Pseudacteon 

tricuspis Borgmeier, P. litoralis Borgmeier, 

the large form of P. obtusus, P. nudicornis 

Borgmeier, and P. nocens Borgmeier 

also were widely distributed. These species 

seem to be the most generalized within saevissima-group. 

Pseudacteon solenopsidis 

Schmitz was only collected attacking isolated 

workers. A new Pseudacteon species was discovered 

in northwestern Argentina. Seven fly 

species were reported for the first time on a 

new fire ant host in this region. Pseudacteon 

cultellatus Borgmeier was found for the first 

time on Solenopsis invicta Buren in Corrientes 

province in northeastern Argentina, where up 

to nine fly species have been found to cooccur. 

Males of P. tricuspis and P. obtusus were the 

only males normally attracted to disturbed fire 

ant colonies. 

2007010288 

摩擦容器内 (Coleoptera: Tenebrionidae) 热 

振蛋白质表达变化与发育阶段 , 曝光时间 

和温度的关系 = Changes in Expression of 

Heat Shock Proteins in Tribolium castaneum 

(Coleoptera: Tenebrionidae) in Relation to 

Developmental Stage, Exposure Time, and 

Temperature. ( 英文 ). Mahroof R; Zhu K Y; 

Subramanyam B. Annals of the Entomological 


The use of elevated temperatures or heat 

treatments for managing insect pests in foodprocessing 

facilities is becoming a popular 

alternative to methyl bromide fumigation. We 

found that young larvae (first instars) of red 

flour beetle, Tribolium castaneum (Herbst) 

(Coleoptera: Tenebrionidae), were relatively 

more tolerant to elevated temperatures than 

eggs, old larvae, pupae, and adults. Our objective 

was to determine whether heat shock proteins 

(HSPs) confer thermotolerance in T. castaneum 

life stages. Western blot analyses by 

using HSP 70 antibody showed constitutive 

expression of HSP 70 in all stages of T. castaneum. 

However, the expression of HSP 70 in 

young larvae increased by 33%, after the larvae 

were exposed to 40°C for 1 h. The expression 

of HSP 70 in other stages did not vary 

significantly, but for eggs the expression of 

HSP 70 showed significant reduction at 40°C. 

Young larvae possessed two distinct HSPs 

with molecular masses of 70 and 24 kDa, both 

recognized by a monoclonal anti-bovine brain 

HSP 70 antibody. Our study suggests that increased 

thermotolerance in young larvae could 

be due to increased expression of HSP 70 at 

higher temperatures. Time- and temperaturedependent 

expression of HSP 70 showed that 

the increased thermotolerance in young larvae 

might last as long as 8 h at 40°C or 30 min at 

46°C. 

2007010289 

Thermobia domestica (Insecta: Zygentoma) 

初期受精卵的孪生胚胎在自然和人工处理 

后的区别 = Primordial Germ Cell Differentiation 

in Natural and Manipulated Twin Embryos 

of Thermobia domestica (Insecta: Zygentoma). 

( 英文 ). Rost M M; Flakus A; Klag 

J. Annals of the Entomological Society of 

America, 2005, 98(1): 108-112 

In eggs of many insects there exists a 

characteristic structure called an oosom that is 

required for the formation and differentiation 

of primordial germ cells (PGCs). Thermobia 

domestica (Packard) belongs to the group of 

84

insects in which there are no visible signs of 

such germ cell determinants and PGCs are 

formed at the later stages of development. 

Spontaneous and experimental polyembryony 

helps to resolve the problem of germ cells determinants 

existence. The stratification of cytoplasmic 

inclusions in T. domestica eggs 

causes the displacement of germ cells determinants. 

As a result, all twin embryos and 

some single embryos (experimental polyembryony) 

have sterile gonads. 

2007010290 

携带 Sr2 标记物的 Ceratitis capitata (Diptera: 

Tephritidae) 的遗传学和交配竞争应 

变 = Genetics and Mating Competitiveness of 

Ceratitis capitata (Diptera: Tephritidae) 

Strains Carrying the Marker Sergeant, Sr2. ( 英 

文 ). Niyazi N; Caceres C; Delprat A; Wornoayporn 

V; Ramirez Santos E; Franz G; Robinson 

A S. Annals of the Entomological Society 

of America, 2005, 98(1): 119-125 

A dominant mutation, Sergeant (Sr 2 ), 

which affects expression of a third stripe on 

the abdomen of the Mediterranean fruit fly, 

Ceratitis capitata (Wiedemann), was recently 

isolated and the results of an extended genetic 

analysis are reported here. In addition, field 

cage data are presented on the mating competitiveness 

of strains carrying this mutation, 

including a genetic sexing strain (GSS). The 

incorporation of a phenotypic marker, such as 

Sr 2 , in a Mediterranean fruit fly GSS would 

complement, and could replace, the use of 

fluorescent dye for monitoring sterile insect 

technique programs and increase program efficiency 

by improving sterile and wild fly 

identification procedures. The mutation is 

homozygous lethal, and it is located on chromosome 

5 at position 78B and 60D on the 

salivary and trichogen polytene maps, respectively. 

The development of the Sr 2 GSS is described 

here, together with data on fitness and 

penetrance of the mutation. The field-cage 

results demonstrated 1) random mating between 

males and females of laboratory strains 

carrying or lacking Sr 2 , 2) comparable sexual 

compatibility of Sr 2 and non-Sr 2 GSS with two 

wild populations, and 3) comparable mating 

competitiveness of males from Sr 2 and non- 

Sr 2 GSS with wild males. From these results, 

no significant effects of the mutation on the 

sexual competitiveness of strains carrying Sr 2 

were detectable. The findings of this study 

point to a satisfactory overall genetic as well 

as mating behavior profile of Mediterranean 

fruit fly strains carrying the Sr 2 mutation and 

clearly warrant further evaluation of this mutation 

in Mediterranean fruit fly GSS. 

2007010291 

基于线粒体 DNA 序列的叶蝉亚属 

Errhomus (Erronus) (Hemiptera: Cicadellidae) 

的语系发生 = Phylogeny of Leafhopper 

Subgenus Errhomus (Erronus) (Hemiptera: 

Cicadellidae) Based on Mitochondrial DNA 

Sequences. ( 英文 ). Johnson D G; Carstens B 

C; Sheppard W S; Zack R S. Annals of the 

Entomological Society of America, 2005, 

98(1): 165-172 

The Nearctic leafhopper genus Errhomus 

Oman (Hemiptera: Cicadellidae) exhibits high 

host-plant selectivity and female brachyptery, 

which may limit gene flow. Two subgenera, 

Errhomus (Errhomus) and Errhomus (Erronus), 

are recognized based on morphological 

and behavioral differences. We used mitochondrial 

DNA sequencing to elucidate the 

phylogenetic relationships among members of 

the subgenus Errhomus (Erronus). Portions of 

the NADH dehydrogenase subunit 1 (ND1) 

and the leucine (CUN) transfer RNA (tRNA- 

Leu) genes were sequenced and were analyzed 

with parsimony and maximum likelihood. Our 

results generally verified the findings of Hamilton 

and Zack (1999); however, both optimality 

criteria revealed a paraphyletic Errhomus 

(Erronus). Errhomus (Erronus) calvus does 

not seem to be a member of the subgenus Errhomus 

(Erronus) but seems to be more 

closely aligned with the subgenus Errhomus 

(Errhomus). We tested two a priori null hypotheses: 

1) that the phylogeny estimated 

from the molecular data matched a previous 

phylogeny based on morphology and biogeography 

from Hamilton and Zack (1999) and 2) 

that diagnostic characters of the male genitalia 

(serrated aedeagal processes and triangular 

aedeagal shaft tip) were synapomorphies that 

defined major clades. We rejected these hypotheses 

with both Bayesian tests and parametric 

bootstraps. 

2007010292 

Anastrepha (Tephritidae) 属在核子基因时 

期的分子分类学 = Molecular Systematics of 

Nuclear Gene period in Genus Anastrepha 

(Tephritidae). ( 英文 ). Barr N B; Cui Liwang; 

McPheron B A. Annals of the Entomological 


The nuclear gene period is used to reconstruct 

the phylogeny of Anastrepha, a genus of 

tephritid fruit flies. Specifically, a region of 

period termed C3C5 that is located in the 

85

dCLK:CYC inhibition domain (CCID) is analyzed. 

This is the first study using this C- 

terminal region of the period gene for phylogenetics. 

Variation in the gene is informative 

for this genus, and period trees are compared 

with phylogenies based on mitochondrial 

and morphological data sets. In general, 

branches that are supported in the other data 

sets are recovered in the period tree; moreover, 

trees built using the period gene support 

branching patterns previously unresolved with 

16S rRNA gene data. Important relationships 

recovered in the period gene tree include a 

paraphyletic placement of Anastrepha with 

respect to Toxotrypana, support for the separation 

of Anastrepha species groups into two 

evolutionary sections (with the exception of 

the pseudoparallela species group), and evidence 

that several species groups are not monophyletic. 

2007010293 

Fidicina variegata, 哥斯达黎加发现蝉的一 

个新种 ( 半翅目 : Cicadomorpha: Cicadidae) 

= Fidicina variegata, a New Cicada Species 

from Costa Rica (Hemiptera: Cicadomorpha: 

Cicadidae). ( 英文 ). Sanborn A F. Annals of 

the Entomological Society of America, 2005, 

98(2): 187-190 

The Neotropical cicada Fidicina variegata 

Sanborn is described as a new species. This 

work validates a name previously assigned to 

this species and considered a nomen nudum. 

Comparisons are made to other members of 

the genus found in Costa Rica. A summary of 

the biology of the species is provided. 

2007010294 

Streblote panda ( 鳞翅目 : Lasiocampidae) 

的产卵能力与体型大小的关系及其它生殖 

问题 = Fecundity–Body Size Relationship and 

Other Reproductive Aspects of Streblote 

panda (Lepidoptera: Lasiocampidae). ( 英文 ). 

Calvo D; Molina J Ma. Annals of the Entomological 

Society of America, 2005, 98(2): 191- 

196 

The relationship between fecundity and 

body size in females of the moth Streblote 

panda Hübner was studied in laboratory by 

using both virgin and mated females. Strong 

relationships among fecundity and pupal 

weight, adult weight, and forewing length 

were found. The number of eggs in virgin and 

mated females was similar; mean egg load 

(number of eggs per female) was 278.4 ± 8.7 

(SE), suggesting that S. panda females eclose 

with all their eggs fully developed. Larger 

females were more fecund than smaller ones. 

Mated females laid eggs soon after emergence 

without any obvious preoviposition period, 

and no relationship between female body size 

and age-specific fecundity or female longevity 

were found. Male size did not show any effects 

on egg size or hatchability. Data suggest 

that determinants of larval development such 

as temperature and food plant may influence 

fecundity through their effects on pupal 

weight and adult body size. All studied reproductive 

traits are characteristic of the capital 

breeding strategy. 

2007010295 

通过热应力约束方法对 Rhagoletis mendax 

(Diptera: Tephritidae) 蛹的滞育的实现 = 

Heat Stress Inhibits the Completion of Pupal 

Diapause in Rhagoletis mendax (Diptera: 

Tephritidae). ( 英文 ). Luís A F Teixeira; Polavarapu 

S. Annals of the Entomological Society 

of America, 2005, 98(2): 197-204 

Blueberry maggot, Rhagoletis mendax 

Curran, pupae that are exposed to high temperature 

toward the end of diapause will not 

develop beyond a specific heat-sensitive stage. 

The temporal relationship between heat sensitivity 

and diapause was studied by exposing 

cohorts of pupae at different stages of diapause 

to 25:35°C (photoperiod of 12:12 [L:D] 

h) for 20 d and comparing the length of time 

to emergence. Results showed that the longest 

delay in emergence was induced in pupae that 

were exposed to high temperature

were investigated by topically applying exogenous 

20-hydroxyecdysone on these pupae. 

Application of the hormone caused 41% of the 

individuals to develop to the adult stage, suggesting 

that heat-induced damage to the endocrine 

system caused the failure to develop. 

Overall, this study indicates that in the blueberry 

maggot, during a 10-d sensitive stage 

immediately before the completion of diapause, 

heat-induced stress on the endocrine 

system can prolong diapause and delay adult 

emergence for a period of time similar to the 

duration of the exposure. 

2007010296 

Parasitoids (Hymenoptera) 增强性碳富集的 

稳定同位素的研究 = Enhanced Carbon Enrichment 

in Parasitoids (Hymenoptera): A 

Stable Isotope Study. ( 英文 ). Langellotto G A; 

Rosenheim J A; Williams M R. Annals of the 

Entomological Society of America, 2005, 

98(2): 205-213 

By considering the magnitude of isotope 

enrichment associated with trophic transfers in 

biologically important elements such as carbon 

( 13 C/ 12 C) and nitrogen ( 15 N/ 14 N), it is possible 

to infer trophic interactions in systems 

where direct observations are logistically difficult. 

Several recent reviews have estimated 

that consumers become enriched in the heavy 

nitrogen isotope on the order of 2.3 to 3.4‰ 

with each trophic transfer. Furthermore, these 

same reviews have estimated that consumers 

become enriched in the heavy carbon isotope 

between 0.4 and 0.5‰ per trophic transfer. 

Although these estimates have been used to 

infer trophic interactions in a variety of taxa, 

the applicability of these estimates for studies 

of arthropod community ecology is poorly 

understood. Specifically for insect parasitoid 

communities, estimates of nitrogen and carbon 

isotope enrichment from a comprehensive 

study have yet to be published. Here, we present 

the results of nitrogen and carbon stable 

isotope analyses for a suite of hymenopteran 

parasitoids that attack the gall-making midge, 

Rhopalomyia californica Felt (Diptera: Cecidomyiidae), 

on coyote bush, Baccharis pilularis 

(Compositae), in northern California. 

Mean carbon enrichment for all parasitoids 

developing on R. californica was considerably 

higher than expected, based on recent reviews. 

In fact, discrimination among trophic levels 

was possible, based on carbon enrichment 

values alone. Mean nitrogen isotope enrichment 

was slightly lower than values reported 

in recent reviews. However, the variation associated 

with our estimate of nitrogen enrichment 

falls well within the range of values reported 

in the reviews. Mechanisms behind the 

greater than expected enrichment in carbon 

are currently unknown and will require further 

investigation. 

2007010297 

美国北部 Pasiphila rectangulata (Lepidoptera:Geometridae) 

一种新的入主 , 季节性爆 

发模式 , 飞翔与新分布的记录 = Hosts, Pattern 

of Seasonal Emergence and Flight, and 

New Distributional Records of Palearctic 

Pasiphila rectangulata (Lepidoptera: Geometridae) 

in the Northeastern United States. ( 英 

文 ). Maier C T. Annals of the Entomological 


Hosts, pattern of seasonal emergence and 

flight, and distribution of the palearctic moth 

Pasiphila rectangulata (L.) (Lepidoptera: Geometridae) 

were examined in the upper northeastern 

United States. Larvae developed on 29 

hosts in three genera (Amelanchier, Malus, 

and Pyrus) in the Rosaceae. At Hamden, CT, 

larval density was significantly higher on ‘Delicious’ 

and ‘McIntosh’ apple, Malus domestica 

Borkhausen, than on ‘Bartlett’ pear, Pyrus 

communis L. Larvae were absent from ‘Napoleon’ 

sweet cherry, Prunus avium L.; ‘Shiro’ 

Japanese plum, Prunus salicina Lindley; and 

‘Stanley’ European plum, Prunus domestica 

L., which grew in the same orchard as the infested 

apples and pear. In the Hamden orchard, 

moths were captured in emergence traps beneath 

apple trees over 12–15 d between late 

May and mid-June in 1999–2001. In 2000 and 

2001, emergence was earlier for males than 

females, and in all years the sex ratio did not 

depart significantly from 1:1. Based on captures 

at a mercury vapor light-trap in 2000 and 

2001, the adult flight lasted 1 mo between late 

May and late June, with the mean date of capture 

being statistically equal for the sexes. In 

2001, more males than females were captured. 

The distributional range of P. rectangulata in 

the northeastern United States includes the 

New England states, extreme eastern New 

York, and northernmost New Jersey; specimens 

collected in Connecticut, New Jersey, 

New York, and Vermont represent new state 

records. The biology of univoltine P. rectangulata 

is similar in Europe and the northeastern 

United States, although the moth apparently 

has a broader range of larval hosts in 

Europe. 

87

棘皮动物 

2007010298 

最早星状棘皮动物的骨骼同源性、系统发 

生及其分类 = Skeletal homologies, phylogeny 

and classification of the earliest asterozoan 

echinoderms. ( 英文 ). Shackleton J D. 

Journal of Systematic Palaeontology, 2005, 

3(1): 29-114 

A thorough reappraisal of extant and fossil 

asterozoan plate systems is used to construct 

working hypotheses of primary plate 

homologies for Ordovician Asterozoa. Results 

indicate that inferomarginal ossicles of asteroids, 

somasteroids and the primitive ophiuroid 

Phragmactis are likely to be homologous with 

edrioasteroid marginals. The intermediate virgals 

and coverplates of somasteroids are identified 

as modified actinals and the sub-laterals 

of certain stenurids are axial, here termed podial 

plates, with laterals in these taxa homologous 

to true lateral plates and adambulacrals 

of ophiuroids and asteroids, respectively. The 

nature of the asterozoan mouth frame is reinvestigated 

as a result of new study of the 

mouth frames of key taxa, with a reappraisal 

of existing developmental and symmetry data. 

It is argued that primitive asterozoan mouth 

angle plates were entirely ambulacral and 

probably not spine-bearing, but that mouth 

spines evolved in asteroids and ophiuroids 

either on the existing first ambulacrals or by 

the superposition of first adambulacrals adoral 

to first ambulacrals. These new data are used 

to undertake a cladistic analysis of all known 

genera of Ordovician asterozoan echinoderms 

(38 taxa), based on a dataset of 150 morphological 

characters, rooted on the Middle Cambrian 

edrioasteroid taxa Stromatocystites and 

Cambraster. The resulting tree is fully resolved 

although some deeper branches show 

poor support. It reveals that Ordovician asteroids 

form a monophyletic group (defined by 

the presence of an unpaired auxillary inferomarginal, 

opposing ambulacrals and blocky 

abutting adambulacrals) and are a sister group 

to the remaining asterozoans, including the 

somasteroids. Somasteroids are monophyletic 

and, with the primitive taxon Phragmactis, are 

a sister group to the remaining ophiuroids. 

The class Ophiuroidea is diagnosed by the 

near-simultaneous appearance of apomorphies 

including an interradial disc with highly separated 

arms and aboral and oral interambulacral 

longitudinal musculature. 

A phylogenetic tree constructed for asterozoans 

based on current stratigraphic occurrence 

data indicates that at the time of their 

first appearance, asteroids and ophiuroid body 

plans were already established. This suggests 

a significant but unobserved pre-Ordovician 

history. Comparison of observed and phylogenetic 

diversity together with the appearance 

of relatively young taxa close to the base 

of the tree point to a poor asterozoan record, 

particularly in the Lower Ordovician. A revised 

classification for stem-group asterozoans 

is proposed based on well-supported 

clades with the new taxon Eopentaroida 

erected. Mapping of character states on the 

most parsimonious solution suggests that 

whilst asteroid morphological evolution was 

conservative in the Ordovician, ophiuroids 

underwent a profound morphological diversification. 

Functionally, these changes are 

linked to the adoption of carnivory by derived 

Ordovician ophiuroids. In contrast, asteroids 

probably remained dominantly deposit-feeders 

throughout the period. Character distribution 

on the cladogram refutes none of the hypotheses 

of primary plate homology, although it 

suggests that podial ossicles were developed 

in two clades independently and that the marginals 

of eopentaroids may not be homologous 

to those of other asterozoans and edrioasteroids. 

2007010299 

撒丁岛及阿尔及利亚上奥陶统 (Ashgill 期 ) 

棘皮动物化石 = Echinoderms of the Upper 

Ordovician (Ashgill) from Sardinia and Algeria. 

( 法文 ). Botquelen A; Menn J L; Loi A. 

Geobios, 2006, 39(1): 13-23 

Research on the influence of sea level 

variations on the benthic faunas have been 

carried out in the Upper Ordovician of Sardinia. 

Study of the depositional facies and sequence 

analysis of the upper part (Lower Ashgill) 

of the Portixeddu Formation led to the 

identification of the sedimentary environments. 

Cystoids and crinoids are associated to bryozoans 

and brachiopods in most levels. The 

numerical analysis of associations and 

megaguilds shows that crinoids and cystoids 

have a higher frequency in the proximal and 

median facies of the upper offshore. The columnal 

association characterized by Conspectocrinus 

celticus and the coronoid Mespilocystites 

tregarvanicus has been discovered in the 

upper part of the formation. This material and 

complementary samples from Upper Ordovician 

of Sardinia and Kabylia (Algeria) bring 

additional data on the systematic and show the 

wide distribution of this fauna outside of the 

Ibero-armorican domain. The distribution of 

88

this echinoderm association supports a palaeogeographical 

position of the Iberoarmorican 

domain and Sardinia within the 

north gondwanan margin during the Lower 

Palaeozoic. 

2007010300 

加拿大棘皮动物两个奇异的海座星的形态 

和系统分类再解释 = Morphological and systematic 

reinterpretation of two enigmatic 

edrioasteroids (Echinodermata) from Canada. 

( 英文 ). Sumrall C D; Gahn F J. Canadian 

Journal of Earth Sciences, 2006, 43(4): 497- 

507 

Reinterpretation of two enigmatic Canadian 

edrioasteroids, Thresherodiscus ramosus 

Foerste, 1914 from the Upper Ordovician 

Verulam Formation of Ontario and Lispidecodus 

plinthotus Kesling, 1967 from the 

Lower Mississippian Banff Formation of Alberta, 

shows that previous accounts of these 

taxa were largely erroneous. Unlike other isorophid 

edrioasteroids, Thresherodiscus has 

branching ambulacra, an unusual hydrogonopore, 

differentiated interambulacral 

plates bearing respiratory structures, and ambulacra 

that extend onto the peripheral rim. 

Except for the turreted thecal shape, Lispidecodus 

is a rather typical discocystinid edrioasteroid. 

Phylogenetic analysis weakly supports 

the placement of Thresherodiscus within 

Agelacrinitidae and strongly places Lispidecodus 

within Discocystinae. 

2007010301 

早三叠纪的蛇尾类 : 他们的古生态、埋葬 

学和分布 = Early Triassic ophiuroids: Their 

paleoecology, taphonomy, and distribution. 

( 英文 ). Twitchett R J; Feinberg J M; O'connor 

D D; Alvarez W; Mccollum L B. 

Palaios, 2005, 20(3): 213–223 

The Permian–Triassic transition was an 

important time for many marine groups, including 

echinoderms. However, the fossil record 

of ophiuroids through this interval is 

poorly understood. Recent discoveries in 

Lower Triassic rocks from northern Italy and 

western US suggest that ophiuroids were more 

common during this time than previously has 

been appreciated. Evidence from resting traces 

(Asteriacites lumbricalis) indicates that Early 

Triassic ophiuroids lived on fine-grained 

siliciclastic sediments in oxygenated, shallowmarine 

environments within storm wave base. 

No resting traces have been recorded from 

deeper and/or oxygen-restricted settings. 

However, following death and decay, ophiuroid 

skeletal elements sometimes were transported 

into offshore, low-oxygen environments. 

All known occurrences of Early Triassic 

ophiuroids fall within the paleotropics, but 

this is attributed to sampling bias. Articulated 

body fossils and their trace fossils are most 

common in latest Lower Triassic (Olenekian) 

rocks, but disarticulated ossicles occur 

throughout the Induan and Olenekian. At 

times and places, ophiuroids were the dominant 

marine benthos, carpeting the substrate in 

prodigious numbers. However, at other times, 

they also comprised minor components of diverse 

benthic assemblages, living alongside 

crinoids (Holocrinus), bryozoans, bivalves, 

gastropods, and brachiopods. Morphological 

comparison with extant ophiuroids suggests 

that all known Early Triassic taxa were small 

surface-dwellers. 

2007010302 

阿根廷丘布特 Tepuel-Genoa 盆地晚古生代 

棘皮动物海百合纲尖顶海百合科及石炭纪 - 

二叠纪界线 = The family Acrocrinidae 

(Echinodermata, Crinoidea) and the Carboniferous-Permian 

boundary in the Neopaleozoic 

sequences of Tepuel-Genoa basin (Chubut, 

Argentina). ( 其他 ). Hlebszevitsch J C. 

Ameghiniana, 2004, 41(3): 381-391 

Acrocrinida from the Carboniferous of 

West Central Patagonia are described for the 

first time in South America. One species is 

assigned to Denariocrinus Webster and Jell, 

previously known from the Neerkol Formation, 

Australia; and two are assigned to new genera: 

Sueroacrocrinus torresverdinei gen. et sp. nov. 

and Patagononcrocrinus giganteus gen. et sp. 

nov. These crinoids were found in Sierra de 

Tepuel (Pampa de Tepuel Formation) and sierra 

de Langui (n) over tilde eo (Las Salinas 

Formation, LS2 Member). They are comparable 

with acrocrinids from Australia. Faunal 

relationships with Australia are so striking, as 

similarly shown by bryozoans, that they allow 

assignment of the fossiliferous levels to the 

Late Carboniferous. 

2007010303 

helicoplacoid 棘皮动物的埋葬学和环境分 

布 = Taphonomy and environmental distribution 

of Helicoplacoid Echinoderms. ( 英文 ). 

Dornbos S Q; Bottjer D J. Palaios, 2001, 

16(3): 197–204 

Helicoplacoids are Early Cambrian echinoderms 

with triradiate ambulacra that are 

covered by helically-arranged columns of cal- 

89

cite plates. They are abundant only in shales 

of the Middle Member of the Lower Cambrian 

Poleta Formation (Atdabanian) at Westgard 

Pass in the White-Inyo Mountains of California. 

To identify and understand the unique 

taphonomic conditions that led to their preservation, 

146 helicoplacoid specimens were examined 

along with the rocks in which they are 

preserved. Considering their loosely articulated 

skeletal construction, together with their 

common occurrence at the base of cm-scale 

graded beds, helicoplacoids most likely were 

preserved during obrution events. A majority 

(69%) of helicoplacoid specimens are partially 

disarticulated, probably indicating that most 

helicoplacoids underwent some combination 

of pre-burial and post-burial decay. Because 

most (73%) helicoplacoid specimens are preserved 

on the same bedding plane as at least 

one other individual, and many (39%) are preserved 

on bedding planes containing at least 

10 individuals, it appears that helicoplacoids 

were gregarious and frequently were preserved 

in mass mortality obrution deposits. 

Low levels of bioturbation, possible microbial 

stabilization of the sediment, a shallow redox 

boundary, and a normally calm depositional 

environment capable of preserving obrution 

deposits are all factors that aided in the preservation 

of helicoplacoids. Additionally, the 

presence of helicoplacoids in several facies of 

the Middle Member of the Poleta Formation 

indicates that they lived in a wider range of 

paleoenvironments than those represented by 

the shales, where they are found most commonly. 

The exceptional preservation of helicoplacoids, 

therefore, is most likely narrowly 

restricted stratigraphically and geographically 

because the proper balance of energy regimes, 

together with the factors mentioned above, 

was achieved only rarely during the Early 

Cambrian, not because helicoplacoids were 

restricted to living in one paleoenvironment. 

2007010304 

性双型的海胆 : 鉴定 Pentechinus mirabilis 

的性别 = Sexually dimorphic sea urchins: 

identifying the sexes in Pentechinus mirabilis. 

( 英文 ). Jeffery C H; Emlet R B. Alcheringa, 

2003, 27(1/2): 117-123 

The sexes of most sea urchin species are 

externally indistinguishable from one another. 

Where gross sexual dimorphism does exist, it 

is invariably associated with nonplanktotrophy. 

In the most extreme examples, female morphology 

has become modified to create depressions 

on the test where offspring may be 

sheltered throughout development. Since a 

number of the features used for taxonomic 

classification are lost on fossilization, it can be 

difficult to recognize fossil individuals as the 

dimorphic males and females of the same species. 

In addition, diagnoses of dimorphic taxa 

commonly concentrate on the striking female 

traits, hindering identification of the simpler 

male form. Here, we present an approach 

based on morphology and Crystallographic 

determination of developmental mode that 

allows the recognition of the males of marsupiate 

echinoid taxa. Males of the brooding 

temnopleurid Pentechinus mirabilis from the 

Oligocene of Victoria, Australia are described 

for the first time. 

2007010305 

不列颠群岛兰多维列统海百合纲以及爱尔 

兰西部特列奇阶 Kilbride 组海百合一新种 

的描述 = Llandovery Crinoidea of the British 

Isles, including description of a new species 

from the Kilbride Formation (Telychian) of 

western Ireland. ( 英文 ). Donovan S K; Harper 

D A T. Geological Journal, 2003, 38(1): 85- 

97 

A new species of cladid() crinoid, Segmentocolumnus 

(cot.) clarksoni, based on distinctive, 

disarticulated stem material, is described 

from the Upper Llandovery Kilbride 

Formation. Hitherto, this unit has yielded two 

taxa based on single, nearly complete crinoids. 

In contrast, S. (cot.) clarksoni is known from 

numerous specimens, including common long 

pentagonal, pentameric, heteromorphic pluricolumnals 

with symplectial articulations, 

broad pentagonal lumina and narrow claustra. 

A related morphospecies is known from the 

Ashgill (Upper Ordovician) of Ireland. The 

fossil echinoderms of the Llandovery (Lower 

Silurian) are poorly known globally. Where 

present in this interval, echinoderms are more 

commonly preserved as disarticulated ossicles 

and rarely as complete specimens. Complete 

crinoids have now been identified from nine 

horizons in the Llandovery of the British Isles, 

making this one of the better known pelmatozoan 

faunas from this time interval. However, 

only two of these occurrences have yielded as 

many as five or more identifiable taxa. Seven 

of the nine occurrences are Upper Llandovery 

(Telychian). Genera are typical of the Silurian 

or (Upper Ordovician + Silurian); the only 

remnant Ashgill taxon that did not survive the 

Llandovery was the morphogenus Segmentocolumnus 

(cot.) Donovan, an 'extinction' that 

90

probably owes more to taxonomic method 

than any evolutionary pattern. 

2007010306 

法国旧石器时期燧石核中的海胆化石 = A 

fossil echinoid preserved on a palaeolithic 

flint core (Tercis open-air site, near Dax, Landes, 

France). ( 法文 ). Odin G S; Pelegnin J; 

Neraudeau D. Comptes Rendus Palevol, 2006, 

5(5): 743-748 

A flint core collected from the Les 

Vignes archaeological site (at Tercis, near Dax, 

Landes, SW France) comprises a silicified 

internal mould of a Cyclaster (Echinoid, 

Spatangoid). The nucleus is assumed to be 

Mousterian and is the single one known from 

Europe with a fossil echinoid shown off by the 

Knapper. Flint and fossil of the flint core and 

from the geological site are compared for 

documenting the provenance. We speculate 

about possible interpretations concerning the 

human Knapper's intention. 

2007010307 

德国艾费尔地区中泥盆世稀少的 Gasterocomidae 

科海百合 = Rare Gasterocomidae 

(Crinoidea) from the Middle Devonian of the 

Eifel (Rhenish Slate Massif, Germany). ( 英文 ). 

Bohaty J. Neues Jahrbuch fur Geologie u. 

Palaontologie / Abhandlungen, 2006, 239(3): 

399-443 

As a result, the Lecythocrinidae Kirk, 

1934 are rejected due to incorrect diagnosis. 

The genera Lecythocrinus and Tetrapleurocrinus 

are trnsferred to the Gasterocomida, but 

Cestocrinus, Corynecrinus and Othozecrinus 

are tentatively tranferred to the Euspirocrinidae. 

The holotype of Scoliocrinus eremita is 

duscussed as a possible aberrant cup of Tetrapleurocrinus 

eifelensis. Two new species and 

a new subspecies of the genus Nanocrinus are 

described: N. scutratus n. sp., N. subvexus 

subvexus n. sp. n. ssp., and N. subvexus granulatus 

n. sp. n. ssp. From the Ahbach- formation 

of the Hillesheim syncline, the large 

Gasterocoma luekeni n. sp. is described. 

2007010308 

胚胎学和古生物学的结合 : 海胆类前 - 后轴 

的起源 = Combining embryology and paleontology: 

origins of the anterior-posterior axis in 

echinoids. ( 英文 ). Saucede T; Mooi R; David 

B. Comptes Rendus Palevol, 2003, 2(6-7): 

399-412 

The tendency of the periproct to move 

outside the apical system occurred in eight 

independent sea urchins lineages, but only one 

succeeded. The origin of the anterior-posterior 

axis in irregular echinoids results from that 

successful attempt, and is primarily achieved 

by eccentricity of the periproct. The mechanism 

by which this occurs is best understood 

through synthesis of data from embryology, 

paleontology, and phylogenetics. In irregular 

echinoids, the complete escape of the periproct 

from the apical system (exocyclism) is 

a consequence of changes in the embryological 

sequence that governs periproctal eccentricity. 

The adaptative significance of this 

change is discussed. 

2007010309 

Gould 氏、mitrates 和畸形生物 = Stephen J. 

Gould, mitrates and monsters. ( 法文 ). Lefebvre 

B. Comptes Rendus Palevol, 2003, 2(6- 

7): 509-522 

The interest of analyses based on teratological 

specimens to understand the mechanisms 

and rules of ontogenetic development is 

a central theme in Gould's literature. This paper 

deals with monsters through two topics 

focusing on a group of atypical Palaeozoic 

echinoderms: mitrate stylophorans. The first 

topic deals with the phyletic position of stylophorans 

within deuterostomes. Three rival 

scenarios have been proposed, based on different 

interpretations of the stylophoran appendage. 

One of these scenarios implies that 

mitrates are > (calcichordate 

theory). An analogy with various 

hypotheses formulated for the disappearance 

of dinosaurs shows that the calcichordate 

model is not a scientific hypothesis, unlike the 

two other interpretations, which can be tested. 

The second topic is dedicated to the description 

of an abnormal specimen of the mitrate 

Mitrocystites mitra, from the Middle Ordovician 

of Bohemia. The abnormal plating of its 

lower surface suggests that the insertion of 

centrals within the posterior region of the 

marginal thecal frame is an iterative phenomenon 

in Mitrocystitida. 

2007010310 

下白垩统棘皮动物箭星海胆属的形态变动 

和异时性 = Morphological fluctuations and 

heterochronies of Toxaster (echinoid, Lower 

Cretaceous). ( 法文 ). Francois E; Marchand D; 

David B. Comptes Rendus Palevol, 2003, 2(6- 

7): 597-605 

Several steps of the diversification of the 

spatangoid Toxaster are described with an 

analysis of six species distributed over the 

91

north-west Tethyan margin, and ranging from 

the Lower Valanginian to the Barremian. 

Morphological variation was investigated with 

the analysis of two parameters (angles), which 

allowed recognition of three modules on the 

test. Comparison of ontogenetic trajectories of 

two reference species (T. granosus kiliani and 

T. retusus) suggests a peramorphic heterochronic 

pattern. However, no peramorphocline 

can be attested when comparisons are extended 

to adults of the six species. Evolution 

among these species is partially driven by allometric 

changes in one module, indicating an 

important influence of size. On the temporal 

and spatial scale of the study, the evolution of 

Toxaster appears globally quite conservative. 

笔石动物 

2007010311 

加拿大育空和西北大陆地区 Embayment 河 

及 Selwyn 盆地奥陶纪特马豆克阶笔石动物 

群生物地层和生态地层意义 = Biostratigraphical 

and ecostratigraphical significance 

of Tremadoc (Ordovician) graptolite faunas 

from the misty Creek Embayment and Selwyn 

Basin in Yukon and Northwest Territories. ( 英 

文 ). Jackson D E, Norford B S. Canadian 


348 

Graptolite zones of early and late Tremadoc 

ages are described from the Elmer 

Creek Formation in the Selwyn Basin and 

from the Duo Lake Formation in the Misty 

Creek Embayment. In ascending order, these 

are: Staurograptus dichotomus, Anisograptus 

matanensis, Adelograptus cf. A. tenellus and 

Aorograptus victoriae Biozones. The uppermost 

zone embraces the Adelograptus antiquus 

Biozone, Kiaerograptus pritchardi 

Biozone, and the Paradelograptus kinnegraptoides 

Biozone in the Richardson Trough. 

Twenty five species are recorded and fourteen 

species are described, including the first record 

of the Rhabdinopora fauna in the early 

Tremadoc of northwest Canada and Kiaerograptus 

magnus Williams and Stevens and 

Paratemnograptus isolatus Williams and Stevens 

in the late Tremadoc. When modifications 

to Cooper's (1999) ecostratigraphic 

model are made based on data from Yukon 

and Northwest Territories, the upper slope 

biotope and lower slope - ocean-floor biotope 

become so similar that there is little basis for 

recognising both biotopes. 

2007010312 

阿尔及利亚撒哈拉 Tinrhert 地区卡拉道克 

阶笔石的首次记录 = First record of Caradocian 

graptollites in the Tinrhert, Algerian Sahara. 

( 法文 ). Kichou-Braik F; Samar L; 

Fekirine B; Legrand P. Comptes Rendus 

Palevol, 2006, 5(5): 675-683 

Caradocian graptolites have been recovered 

for the first time from several bore-holes 

in the Timbert region of the Algerian Sahara. 

Stratigraphically, they belong to the Oued 

Ahara upper Member of the Edieleh Formation. 

The graptolites are assigned to the new 

sub-species Diplograptus foliaceus tinrherti 

that is briefly described. The occurrence of D. 

foliaceus (sensu lato), whose upper stratigraphic 

limit is Upper Soudleyan, indicates a 

probable Burrellian (Middle Caradocian) age 

for a more or less important part of the upper 

Oued Ahara Member. This is an additional 

age constraint for the beginning of the Late 

Ordovician glacial episode in the region, since 

the first glacial sediments (Gara Louki Formation) 

lie in erosional disconformity on the 

Oued Ahara Member. 

2007010313 

奥陶纪笔石的演化辐射 : 述评 = Ordovician 

graptolite evolutionary radiation: a review. ( 英 

文 ). Chen Xu; Zhang Yuandong; Fan 

Juanxuan. Geological Journal, 2006, 41(3/4): 

289-301 

Based on the global graptolite genera and 

higher rank taxa, we propose three radiation 

stages through the Ordovician. The isograptid 

type of development is present within anisograptids 

predominating in the Tremadocian. 

Thus, the evolutionary radiation of the Anisograptid 

fauna from Tremadocian is proposed 

as the beginning of the Ordovician graptolite 

radiation. The second graptolite radiation 

event is the radiation of the Dichograptid 

fauna, which began from the T. fruticosus 

Biozone. The third radiation event, the radiation 

of Diplograptid fauna began immediately 

after that of the dichograptids. This radiation 

includes the peak in total diversity of all the 

Ordovician graptoloids in the Nemagraptus 

gracilis Biozone. The radiation extended 

through the Sandbian and Katian and then was 

interrupted by a major extinction during the 

early Hirnantian. Thus, the Ordovician graptolite 

radiation events coincide with those of the 

three graptolite faunas proposed by Bulman. 

The distribution and expansion of the Ordovician 

graptolites in South China may exemplify 

the graptolite origination pattern, which be- 

92

gins from the slope belt and expanded into 

both the shelf and oceanic zones 

2007010314 

中国上扬子区赫南特期 ( 奥陶世最晚期 ) 

的笔石 = Hirnantian (Latest Ordovician) 

Graptolites from the Upper Yangtze Region, 

China. ( 英文 ). Chen Xu; Fan Junxuan; Melchin 

M J; Mitchell C E. Palaeontology, 2005, 

48(2): 235-280 

The Upper Yangtze region yields a 

Hirnantian (latest Ordovician) graptolite fauna 

that includes 41 species assigned to 13 genera. 

This fauna is particularly important for understanding 

the Late Ordovician mass extinction 

event because it is the most diverse known 

from this interval. In addition, it records the 

survival, well into the Hirnantian, of many 

taxa of the Dicranograptidae-Diplograptidae- 

Orthograptidae (DDO) fauna, which was previously 

regarded as having gone extinct at the 

beginning of the Hirnantian. Taxa exhibiting 

six different astogenetic patterns, including 

taxa with reclined stipes, scandent, biserial, 

full-periderm and 'archiretiolitid' rhabdosome 

forms occur in the lower Normalograptus extraordinarius-N. 

ojsuensis Biozone. In contrast, 

in the upper N. persculptus Biozone only 

four genera remain, all but one of which are 

Normalograptidae: scandent and biserial taxa 

with Pattern H astogeny. Normalograptids are 

the dominant form of the succeeding, lower 

Rhuddanian, faunas. The Yangtze faunas also 

document the early expansion of normalograptids 

coeval with the decline of the DDO fauna. 

Many previously identified species considered 

endemic to China have been synonymized; 24 

of the 41 species recorded here have been recognized 

elsewhere. No new taxa are described. 

分类位置不明 

2007010315 

塔里木盆地顺 1 井几丁石发现的意义 = 

Significance of discovery of Chitinozoans 

from Late Ordovician to Early Silurian in 

Shun-1 Well, Tarim Basin. ( 中文 ). 蔡习尧 ; 毛 

树华 ; 陈跃 ; 邹元荣 ; 陈强路 ; 尤东华 . 新疆石油 

地质 , 2005, 26(5): 536-539 

顺 1 井中下志留亚系发育齐全 , 自下而 

上分为兰德维利统柯坪格组、塔塔埃尔塔 

格组与文洛克统依木干他乌组 . 柯坪塔格组 

又可细分为三段 : 上、下为砂岩段 , 中间为 

泥岩段 , 颜色为灰色、灰绿色 . 塔塔埃尔塔格 

组两分 , 下段为紫红色泥岩 , 上段为红褐色、 

红色泥岩与粉砂岩不等厚互层 . 依木干他乌 

组岩性为棕色、棕褐色泥岩夹粉砂岩与细 

砂岩 : 上奥陶统却尔却克组仅钻揭 110m, 

岩性主要为灰、深灰色泥岩 . 各组之间岩 

性、电性特征均较明显 . 在柯坪塔格组下段 

与却尔却克组上部获丰富的几丁石 , 鉴定出 

了 3 属 5 种 ,1 个比较种与众多的未定种 , 详 

细地讨论了几丁石属种的时代分布与地理 

分布 , 根据化石群特征 , 可将其归入 

Conochitina electa 与 Conochitina sp. 2 化石 

带 . 依据几丁石带在全球范围空间的分布规 

律 , 确定了顺 1 井含化石的地层时代 , 并以岩 

石地层为基础、生物地层为依据 , 结合测井 

地层 , 对顺 1 井中下志留亚系进行了重新划 

分 , 首次为本区中下志留亚系兰德维利统的 

划分与对比提供了重要的化石依据 . 

2007010316 

上扬子区奥陶系 Nemagraptus gracilis 笔石 

带的几丁虫 = Chitinozoans from the Upper 

Ordovician of the graptolite Nemagraptus 

gracilis zone of the central Yangtze region. 

( 中文 ). 张淼 ; 陈孝红 . 微体古生物学报 , 2005, 

22(4): 383-391 1 图版 . 

作者系统描述了在重庆城口廖子口和 

宜昌分乡普溪河奥陶系庙坡组 Nemagraptus 

gracilis 笔石带中发现的几丁虫化石 , 共 7 

属 9 种。由于此前对该层位的几丁虫研究 

较少 , 因此本次所发现的几丁虫化石具有 

重要的生物地层意义。 

2007010317 

格陵兰、加拿大和西伯利亚早寒武世疑问 

化石 Triplicatella = The problematic fossil 

Triplicatella from the Early Cambrian of 

Greenland, Canada, and Siberia. ( 英文 ). 

Skovsted C B; Peel J S; Atkins C J. Canadian 


1273-1283 

The cap-shaped Early Cambrian fossil 

Triplicatella, previously known only from 

Australia, is reported from the upper Lower 

Cambrian of North and North-East Greenland, 

western Newfoundland, and Siberia. The occurrence 

of Triplicatella in Laurentia 

strengthens faunal ties between Laurentia and 

the Australian margin of Gondwana in late 

Early Cambrian times and supports hypotheses 

advocating the close proximity for the two 

palaeocontinents. Two new species, Triplicatella 

sinuosa n. sp., and T. peltata n. sp. are 

described, morphological details of which 

help elucidate the functional morphology and 

taxonomic affinity of the group. Three opercular 

types attributable to Triplicatella are left in 

93

open taxonomy. The postulated affinity of 

Triplicatella to hyoliths is confirmed, although 

the genus can not be placed within 

either of the two orders of hyoliths currently 

recognized. 

2007010318 

中国西南部早寒武世蠕形动物星虫类 = 

Early Cambrian sipunculan worms from 

southwest China. ( 英文 ). Huang Di-Ying; 

Chen Jun-Yuan; Vannier J; Salinas IS. Proceedings 

of the Royal Society B: Biological 

Sciences, 2004, 271(1549): 1671 - 1676 

We report the discovery of sipunculan 

worms from the Lower Cambrian Maotianshan 

Shale, near Kunming (southwest China). 

Their sipunculan identity is evidenced by the 

general morphology of the animals (sausageshaped 

body with a slender retractable introvert 

and a wider trunk) and by other features, 

both external (e.g. perioral crown of tentacles, 

and hooks, papillae and wrinkle rings on the 

body surface) and internal (U-shaped gut, and 

the anus opening near the introvert-trunk junction). 

The three fossil forms (Archaeogolfingia 

caudata gen. et sp. nov., Cambrosipunculus 

tentaculatus gen. et sp. nov. and Cambrosipunculus 

sp.) have striking similarities to 

modern sipunculans, especially the Golfingiidae 

to which their evolutionary relationships 

are discussed. This study suggests that most 

typical features of extant sipunculans have 

undergone only limited changes since the 

Early Cambrian, thus indicating a possible 

evolutionary stasis over the past 520 Myr. 

2007010319 

Anomalocaridids 动物与节肢动物和曳鳃动 

物的区别 = Distinguishing anomalocaridids 

from arthropods and priapulids. ( 英文 ). Hou 

Xianguang, Bergstrom J, Jie Y. Geological 

Journal, 2006, 41(3/4): 259-269 

The Chengjiang fossil lagerstatte has 

yielded four described species of dinocaridids. 

These have been interpreted either as arthropods 

or as arthropod progenitors, occasionally 

with the anomalocaridid Parapeytoia yunnanensis 

serving as a link. This view is rejected 

both because anomalocaridids have a 

number of derived characters absent from 

early arthropods, and also because a shared 

origin gives a more parsimonious picture. 

Sclerites thought to belong to the mouth of P. 

yunnanensis differ fundamentally from those 

of its holotype and from those of other dinocaridids. 

It appears that they belong to a new 

large priapulid, described here as Omnidens 

amplus gen. et sp. nov. 

古脊椎动物学 

综论 

2007010320 

白垩纪四足动物的化石记录 = The fossil 

record of Cretaceous tetrapods. ( 英文 ). Fara E; 

Benton M J. Palaios, 2000, 15(2): 161-165 

The fossil record of the Cretaceous is 

critical for understanding the evolution of 

modern tetrapods. Using a measure of relative 

completeness of the fossil record—the Simple 

Completeness Metric (SCM)—quality of the 

fossil record and diversity during the Cretaceous 

appear to be closely related, suggesting 

an artifactual component. The SCM calculations 

also show that knowledge of the fossil 

record has improved in the last ten years. Recent 

proposals that modern orders of birds and 

mammals originated early in the Cretaceous 

are rendered unlikely by four arguments: (1) 

the SCM calculations indicate that the fossil 

record of Cretaceous birds and mammals is 

relatively good; (2) it is unlikely that all modern 

orders, independently, would have remained 

cryptic throughout the Cretaceous; (3) 

control samples of exquisitely preserved tiny 

Cretaceous tetrapods lack any specimens of 

modern groups of birds and mammals; and (4) 

the suggestion that the undiscovered ancestors 

of modern groups are to be found in unsampled 

parts of the Earth is not supported by 

cladistic evidence. 

2007010321 

南美洲南部中三叠世四足类足印 = Middle 

Triassic tetrapod footprints of southern South 

America. ( 法文 ). Marsicano C A; Arcucci A 

B; Mancuso A; Caselli A T. 

Ameghiniana, 2004, 41(2): 171-184 

In South America, tetrapod footprints of 

Middle Triassic age were only described from 

the Cuyana (Cerro de las Cabras Formation) 

and Ischigualasto-Villa Union (Los Rastros 

Formation) basins in west-central Argentina. 

They are scarce and remain mostly undescribed. 

Their significance and the putative 

trackmakers are identified and discussed 

within a phylogenetic context in the present 

contribution. Several groups of tetrapods are 

suggested to be represented, as nonmammalian 

therapsids, crurotarsal archosaurs 

and putative dinosaurs. The presence of crurotarsal 

archosaurs and non-mammalian therapsids 

in Cerro de las Cabras Formation suggests 

94

a tetrapod fauna more diverse than that documented 

by the known body fossil record. The 

ichnites described from the Los Rastros Formation 

are, until now, the only evidence of 

amniotes in the Ischigualasto-Villa Union Basin 

during the deposition of these levels. They 

indicate the presence of putative dinosaurs, 

crurotarsal archosaurs and non-mammalian 

therapsids, which are already well represented 

in the rest of the sequence by skeletal remains. 

2007010322 

匈牙利北部下上新统 Osztramos 1 产地的 

无尾类和有鳞类 = Anurans and squamates 

from the Lower Pliocene (MN 14) Osztramos 

1 locality (Northern Hungary). ( 英文 ). Venczel 


2001, (19): 79-90 

The Lower Pliocene (MN 14) locality of 

Osztramos 1 (Hungary) yielded at least 7 anurans: 

Latonia gigantea, Bombina sp. (Discoglossidae), 

Pliobatrachus cf. langhae (Palaeobatrachidae), 

Eopelobates sp. (Pelobatidae), 

Bufo bufo, B. viridis (Bufonidae), Rana 

sp. (Ranidae); and 14 squamate taxa: Geckonidae 

indet., Lacerta sp. (Lacertidae), Anguis 

fragilis, Pseudopus pannonicus (Anguidae), 

Eryx sp. (Boidae), Coluber hungaricus, Coronella 

austriaca, Elaphe kormosi, E. praelongissima, 

Elaphe sp., Natrix longivertebrata, cf. 

Neonatrix sp. (Colubridae), Vipera cf. ammodytes 

and V. cf. berus (Viperidae). A number 

of taxa (Eopelobates sp., Geckonidae indet., 

Eryx sp., cf. Neonatrix sp., Vipera cf. ammodytes 

and V. cf. berus) are reported for the 

first time from the Hungarian Neogene. The 

composition of the fauna suggests mild and 

wet climate and a diversified paleoenvironment, 

with a water source in the area, which 

permitted the co-occurrence of a number of 

extinct and extant genera during the accumulation 

of the sediments 

2007010323 

云南元谋含古猿地层猪科一新属 = A new 

suid from the upper miocene hominoid locality 

in Yuanmou of Yunnan Province. ( 中文 ). 

刘建辉 ; 潘悦容 . 云南地质 , 2003, 22(2): 176- 

191 3 图版 . 

记述产自云南元谋小河、雷老含古猿 

地层的猪科 (Suidae) 化石一新属新种 — 元谋 

臼齿猪 (Molarochoerus yuanmouensis gen.et 

sp. nov.)。以向前向外扩展的颧弓、后置的 

眼眶、P 4 和 P 4 臼齿化、P 4 跟座与主尖等高、 

P 3 有大而前移的舌侧尖等特征区别于其它 

猪类化石。可能是猪亚科 (Suinae) Propotamochoerini 

族的较进步类型 , 与 

Propotamochoerus 有较近的亲缘关系。 

2007010324 

美国怀俄明州 Bighorn 山晚奥陶世的脊椎 

动物 = Late Ordovician vertebrates from the 

Bighorn Mountains of Wyoming, USA. ( 英 

文 ). Sansom I J; Smith M P. Palaeontology, 

2005, 48(1): 31-48 

Late Ordovician vertebrate faunas occur 

in clastic sedimentary units along the length of 

the Rocky Mountains from Colorado to Montana, 

and across the border into Canada. Most 

research has, however, been conducted on 

localities in the southern part of the outcrop 

belt, particularly the Harding Sandstone Formation 

of Colorado. Micropalaeontological 

sampling of the coeval South Piney Member 

(Winnipeg Formation) in the Bighorn Mountains 

of Wyoming has revealed an abundant 

vertebrate fauna. The vertebrate assemblage 

includes a low-abundance fauna of 13 conodont 

taxa that together indicate an undatus 

Chronozone age (mid-Mohawkian; mid- 

Caradoc; Late Ordovician). The pteraspidomorphs 

Astraspis desiderata Walcott and 

Eriptychius americanus Walcott are also present 

together with one new taxon, Eleochera 

glossa gen. et sp. nov., which is interpreted as 

a derived stem-gnathostome on the basis of its 

scale histology and morphology. The fauna 

bears a strong similarity to that of the Harding 

Sandstone but is of lower diversity. In particular, 

it lacks the fine-grained, deeper water 

component of the Harding Sandstone that contains, 

inter alia, thelodonts and stemchondrichthyans. 

2007010325 

法国西南部图鲁兹渐新世最晚期 (MP30) 

和中新世最早期 (MN1) 脊椎动物 = Latest 

Oligocene (MP30) and Earliest Miocene (MNl) 

vertebrates from the Toulouse subway (SW 

France).. ( 法文 ). Antoine P O; Duranthon F; 

Hervet S; Fleury G. Comptes Rendus 

Palevol, 2006, 5(7): 875-884 

Latest Oligocene (MP30) and Earliest 

Miocene (MN1) vertebrates from the Toulouse 

subway (SW France). The excavation 

for the line B of the Toulouse subway led in 

2002-2003 to the discovery of various vertebrates, 

including the rhinocerotids Diaceratherium 

lemanense, Mesaceratherium paulhiacense, 

and Protaceratherium cf. minutum, 

an unidentified schizotheriine chalicotheriid, 

the artioclactyl Cainotherium sp., the theri- 

95

dormyid rodent Issiodoromys bransatensis, 

the testudinid tortoise 'Ergilemys' bruneti, and 

the small alligatoroid Diplocynodon sp. These 

first in situ diversified faunas of Toulouse 

confirm the Latest Oligocene (MP30) to Earliest 

Miocene age (MN1) of the micaceous 

sands interbedded with marl banks of the Toulouse 

underground. The fauna indicates the 

occurrence of various environments, ranging 

from forests to open habitats, nearby steady 

rivers for the concerned period and area. 

2007010326 

关于马达加斯加 Antsingiavo 亚化石地点的 

初步报告 = Preliminary report on Antsingiavo 

subfossils sites (Madagascar).. ( 法文 ). 

Gommery D; Senegas F; Mein P; Tombomiadana 

S; Ramanivosoa B; Cauvin J; Cauvin C. 


Two new sites, Antsingiavo A & B, have 

been discovered in the Narinda peninsula, 

situated in the North-West of Madagascar, 

Province of Mahajanga. Breccias contain microfauna 

associated with subfossil lemurs of 

an average size (Archaeolemur) and small 

(Microcebus). Until now, the subfossil microfauna 

of Madagascar was practically unknown. 

The sample from Antsingiavo offers information 

on past environments in the Narinda peninsula. 

The new discoveries contribute to an 

understanding of the diversity Archaeolemur 

with different forms in the different areas of 

Madagascar. 

2007010327 

脊椎动物特征和寒武纪脊椎动物 = Vertebrate 

characters and the Cambrian vertebrates. 

( 其他 ). Janvier P. Comptes Rendus 

Palevol, 2003, 2(6-7): 523-531 

The question of the developmental characters 

which conventionally define the vertebrates, 

neural crests and epidermal placodes, 

and their indirect identification in the fossil 

material is briefly discussed. Comments are 

made upon some presumed Cambrian vertebrate 

or vertebrate-related taxa, with particular 

reference to the most likely Cambrian vertebrates, 

Haikouichthys and Myllokunmingia 

鱼类 

2007010328 

早白垩纪西冈瓦纳大陆的解体及鱼类的分 

布 = Continental break up and the distribution 

of fishes of Western Gondwana during the 

Early Cretaceous. ( 英文 ). Maisey J G. Cretaceous 

Research, 2000, 21(2-3): 281-314 

Many Early Cretaceous fishes were endemic 

to western Gondwana, making their 

fossils potentially useful tools in biogeographic 

reconstruction. These occur in a 

variety of tectonic settings; for example, in rift 

basins of the East Brazilian Rift System 

(EBRIS) and corresponding sites in western 

Africa, in non-rift basins within the EBRIS 

region, and in interior localities far removed 

from this area in both Africa and Brazil. Furthermore 

these occurrences span much of the 

Early Cretaceous and include syn-rift and 

post-rift (transitional and marine) deposits. 

Development of a permanent equatorial seaway 

in the late Aptian is identified as a crucial 

event in the biogeographical history of western 

Gondwana, but several earlier tectonic 

events are recognized that could have played 

an important role in pre-drift intercontinental 

speciation. Different patterns of distribution 

are noted among non-marine fishes, some taxa 

occurring within areas of rifting while others 

are more widespread. The earliest Cretaceous 

marine fishes in NE Brazil are late Aptian and 

early Albian endemic circum-Gondwanan taxa. 

Their arrival coincides with the formation of 

the equatorial seaway but they occur in strata 

that were deposited under conditions of anoxia 

and abnormally high salinity. A more widespread 

marine invasion (probably from Caribbean 

Tethys) occurred in the middle and late 

Albian as oxygen and salinity levels were 

normalized and surface water exchange began 

in the equatorial Atlantic. 

2007010329 

德国南部早侏罗世 Synechodus smithwoodwardi 

的解剖学和系统分类 = Anatomy 

and systematics of the Early Jurassic 

neoselachian shark Synechodus smithwoodwardi 

(Fraas, 1896) from southern Germany. 

( 英文 ). Klug S; Kriwet J. Neues Jahrbuch fur 

Geologie u. Palaontologie / 

Monatschefte, 2006, (4): 193-211 

Synechodus smithwoodwardi, a member of 

Early Jurassic synechodontiform sharks, is 

redescribed in detail from the unique adult 

male specimen from the Toarcian of 

Holzmaden. It consists of an articulated portion 

of the vertebral column, two dorsal fin 

spines, the parts of the pectoral and pelvic 

girdles, the clasper organs, and a shagreen of 

placoid scales. The densely calcified cyclospondylous 

vertebrae, the morphology of the 

fin spines, and presence of non-growing placoidscales 

support its assignment to neoselachian 

sharThe clasper organs are well- 

96

preserved and allow a detailed account of 

copulation organs in Early Jurassic neoselachians 

for the first time. 

2007010330 

贵州晚三叠世关岭生物群大型鱼龙化石一 

新属种 = A new species of large-sized and 

long-body ichthyosaur from the Late Triassic 

Guanling biota,Guizhou,China. ( 中文 ). 陈孝 

红 ; 程龙 . 地质通报 , 2003, 22(4): 228-235 1 图 

版 . 

根据采自贵州关岭上三叠统小凹组下 

段两个分别具有完整骨架和呈立体保存的 

头骨标本 , 命名和描述为一种大型的长体型 

的鱼龙 Panjiangsaurus epicharis gen.et sp. 

nov.。这类鱼龙以下颌后部缺齿 , 荐前椎数 

约 69 节 , 前肢边缘的凹口出现在桡骨、接桡 

骨和远端腕骨上为特征。Panjiangsaurus 外 

鼻孔的骨片组成与中、晚三叠世 

Shastasaurus 和 Cymbospondylus 的外鼻孔相 

似 , 肩带和腰带也具有晚三叠世卡尼期 

Shonisaurus 的肩带和腰带的特点 , 但其桡 

骨、接桡骨和远端腕骨均发育有凹槽的前 

肢 , 可以与晚三叠世诺利期 Macgonwani 以及 

早侏罗世 Stenopterygius 的前肢相比较 , 而具 

有侏罗纪鱼龙的特征。 

2007010331 

首次报道出现于贵州关岭地区中上三叠统 

的软骨鱼类 = Discovery of the Middle-Late 

Triassic elasmobranch ichthyoliths from the 

Guanling area,Guizhou,SW China. ( 英文 ). 陈 

立德 ;Gilles Cuny. 地质通报 , 2003, 22(4): 

236-247 3 图版 . 

应用 Johns 等 (1997) 的形态分类系统 , 对 

首次报道出现于贵州关岭地区中上三叠统 

的软骨鱼类的微体化石进行了初步研究 , 描 

述了其中的 1 个牙齿化石 ( 可能属于弓鲛鲨 

科的 ) 和 7 个鳞片类化石的形态属种 , 其中包 

括两个鳞片类化石的新属种 , 即 

Lobaticorona cf.floriditurris,Sacrisubcorona 

cf.circabasis,Glabrisubcorona 

cf.arduidevexa,Parvicorona dacrysuca 

n.gen.et.n.sp.s.f.,Annulicorona pyramidalis 

n.gen.et.n.sp.s.f.,new()parageneraA 和 

new()parageneraB。还初步探讨了软骨鱼 

类微体化石在三叠纪地层划分中的应用 , 以 

及中国西南部三叠纪软骨鱼类与北美相当 

地层中软骨鱼类的洲际对比。 

2007010332 

波兰中部 Wąwał 下白垩统凡兰吟阶新软骨 

鱼类鲨鱼及放射状牙齿 = Neoselachian 

Shark and Ray Teeth from the Valanginian, 

Lower Cretaceous, of Wąwał, Central Poland. 

( 英文 ). Rees J A N. Palaeontology, 2005, 

48(2): 209-221 

Valanginian strata at Wąwał in central 

Poland have yielded the oldest marine neoselachian 

assemblages from the Cretaceous of 

Europe. The faunas comprise seven taxa including 

Heterodontus polonicus sp. nov., an 

indeterminate orectolobiform, Protolamna sp., 

Palaeoscyllium sp., Synechodus nitidus, 

Squatina cranei and Belemnobatis sp. Heterodontus 

polonicus is recognized primarily by 

the high amount of reticulate ornamentation 

on the lower labial side of the anterior teeth. 

The faunas from Wąwał are numerically 

dominated by neoselachian genera such as 

Synechodus, Heterodontus and Belemnobatis 

that were already well established in the Jurassic. 

More modern taxa include the oldest recorded 

occurrence of the true Squatina-lineage, 

and the presence of Protolamna is one of the 

earliest undoubted lamniform occurrences so 

far reported. 

2007010333 

美国达科他州 Williston 盆地上麦斯里希特 

阶 Fox Hills 及 Hell Creek 组浅海相软骨鱼 

类 Ischyodus 一新种 = A new species of Ischyodus 

(Chondrichthyes: Holocephali: Callorhynchidae) 

from upper Maastrichtian shallow 

marine facies of the Fox Hills and Hell 

creek Formations, Williston Basin, North Dakota, 

USA. ( 英文 ). Hoganson J W; Erickson J 

M. Palaeontology, 2005, 48(4): 709-721 

A new species of chimaeroid, Ischyodus 

rayhaasi sp. nov., is described based primarily 

upon the number and configuration of tritors 

on palatine and mandibular tooth plates. This 

new species is named in honour of Mr Raymond 

Haas. Fossils of I. rayhaasi have been 

recovered from the Upper Maastrichtian Fox 

Hills Formation and the Breien Member and 

an unnamed member of the Hell Creek Formation 

at sites in south-central North Dakota and 

north-central South Dakota, USA. Ischyodus 

rayhaasi inhabited shallow marine waters in 

the central part of the Western Interior Seaway 

during the latest Cretaceous. Apparently it was 

also present in similar habitats at that time in 

the Volga region of Russia. Ischyodus rayhaasi 

is the youngest Cretaceous species of 

Ischyodus known to exist before the Cretaceous/Tertiary 

extinction, and the species ap- 

97

parently did not survive that event. It was replaced 

by Ischyodus dolloi, which is found in 

the Paleocene Cannonball Formation of the 

Williston Basin region of North Dakota and is 

widely distributed elsewhere. 

2007010334 

澳大利亚昆士兰下石炭统一新种 

Gyracanthides Hawkinsi 及对 Gyracanthid 

的修订 = Gyracanthides Hawkinsi sp. nov. 

(Acanthodii, Gyracanthidae) from the lower 

Carboniferous of Queensland, Australia, with 

a review of Gyracanthid taxa. ( 英文 ). Turner 

S; Burrow C J; Warren A. Palaeontology, 

2005, 48(5): 963-1006 

A new species of Gyracanthides from the 

mid-Viséan Ducabrook Formation of Middle 

Paddock site, near Springsure in the Drummond 

Basin, central Queensland, is based on 

isolated three-dimensionally preserved elements. 

The specimens comprise paired and 

unpaired spines and pectoral girdle elements, 

procoracoids and scapulocoracoids, and include 

growth series. The morphology, especially 

of the shoulder girdle bones and the 

form and tubercular ornamentation of the 

paired fin spines, is used to distinguish the 

new taxon. These characters also help differentiate 

the numerous described gyracanthid 

species. Aspects of palaeobiology including 

possible sexual dimorphism are explored. A 

hypothetical reconstruction of the fish is based 

on our interpretation of the articulation of isolated 

elements combined with examination of 

wear patterns on fin spines. Gyracanthides 

hawkinsi sp. nov. is compared with other Australian 

taxa as well as with gyracanthids from 

North America, Europe, Russia, Iran, Africa 

and Antarctica, some of which are tentatively 

reassigned here to the Gondwanan genus Gyracanthides. 

2007010335 

盾皮鱼 Cosmacanthus 的系统评述及苏格 

兰上泥盆统棘皮鱼化石的描述 = A systematic 

review of the Placoderm genus Cosmacanthus 

and a description of Acanthodian 

remains from the Upper Devonian of Scotland. 

( 英文 ). Newman M J. Palaeontology, 2005, 

48(5): 1111-1116 

A number of fin spines were described by 

Duff (1842) from the Upper Devonian locality 

of Scat Craig, Scotland. Only one of these 

specimens was described by Agassiz (1845) as 

a fin spine. This was the holotype of Cosmacanthus 

malcolmsoni Agassiz, 1845. Denison 

(1978) later removed C. malcolmsoni 

from the Acanthodii and placed it in the Placodermi, 

but without a full systematic description. 

In this paper, Denison's (1978) opinion as 

to the affinity of C. malcolmsoni is confirmed. 

A full systematic description of 

C. malcolmsoni is presented, including a complete 

synonymy list. New material has recently 

been collected from Scat Craig, which 

can be ascribed to the Acanthodii, but is not 

well preserved and so is kept in open nomenclature. 

With C. malcolmsoni being placed 

within the Placodermi, the acanthodian remains 

represent the only known record of this 

group from the Upper Devonian of Scotland. 

2007010336 

挪威斯匹次卑尔根群岛首次发现泥盆纪肺 

鱼 = First Devonian dipnoans (Vertebrata, 

Sarcopterygii) from Spitsbergen. ( 英文 ). 

Clement G; Dupret V; Goujet D; Pernegre V; 

Roy J C. Comptes Rendus Palevol, 2006, 5(7): 

893-900 

For the first time, dipnoan remains are 

described from the Devonian of Spitsbergen. 

According to the stratigraphy and the associated 

vertebrate fauna, they are considered as 

Late Emsian-Early Eifelian in age. Unfortunately 

remains are too sketchy and nondiagnostic 

to be referred or compared to a 

known Devonian dipnoan. This new material, 

determined as Dipnoi gen. et sp. indet., is nevertheless 

important in biostratigraphical and 

palaeobiogeographical points of view, since it 

is amongst the earliest dipnoan occurrences, 

and the first one in the Devonian of Spitsbergen. 

2007010337 

美国宾夕法尼亚州晚泥盆世 Catskill 期肺 

鱼 = Late Devonian (Famennian) Lungfishes 

from the Catskill Formation of Pennsylvania, 

USA. ( 英文 ). Friedman M; Daeschler E B. 


Occurrences of fossil lungfishes (Dipnoi: 

Sarcopterygii) in the Famennian Catskill Formation 

of Pennsylvania are reviewed. A 

nearly complete dermal skull roof is assigned 

to a new genus and species, Apatorhynchus 

opistheretmus. Other recently discovered 

lungfish specimens include an incomplete 

postcranium similar to that of the Frasnian 

genus Fleurantia, a small parasphenoid of 

uncertain affinities, and isolated toothplates. 

Previously described dipnoan remains from 

the Catskill Formation include a partial skull 

roof of Soederberghia groenlandica, tooth- 

98

plates assigned to several species of Dipterus, 

a putative rostral or symphysial region placed 

in the problematic form taxon Ganorhynchus, 

and sedimentary structures interpreted as burrows. 

The toothplates attributed to Dipterus 

are indeterminate and are placed in open nomenclature, 

while the specimen identified as 

Ganorhynchus is not convincingly dipnoan. 

The status of the burrows remains uncertain 

pending the discovery of lungfish remains 

within these or similar structures in Catskill 

deposits. The distinct ichthyofaunas within the 

Catskill Formation and their lungfish components 

are briefly reviewed. Lungfishes are 

found in the Holoptychius- and Bothriolepisdominated 

faunas common in the Catskill succession, 

as well as in the compositionally distinctive 

Red Hill assemblage. Many of the 

Devonian continental faunas that contain 

tetrapods also include long-snouted, denticlebearing 

lungfishes ('rhynchodipterids', fleurantiids, 

or both). The composition of Late Devonian 

ichthyofaunas may have predictive qualities 

that will allow researchers to identify localities 

likely to produce the remains of early 

tetrapods. 

2007010338 

石炭纪 Strepsodus 及 Archichthys 属 : 对 

150 年的混乱的澄清 = The Carboniferous 

fish genera Strepsodus and Archichthys (Sarcopterygii: 

Rhizodontida): clarifying 150 

years of confusion. ( 英文 ). Jeffery J E. Palaeontology, 

2006, 49(1): 113-132 

The Carboniferous genus Strepsodus 

contains several described species, but has 

been mired in taxonomic confusion for nearly 

150 years. The little-known genus Archichthys 

(with two described species) is usually treated 

as a junior synonym of Strepsodus. These 

problems have been caused by, among other 

things, the poor quality of most specimens, 

and a heavy reliance on tooth and scale morphology 

when erecting new species. Both 

genera are known from Upper and Lower 

Carboniferous river and lake deposits in the 

UK, particularly coal shales, cementstones and 

freshwater limestones. However, Strepsodus 

has also been discovered at a number of North 

American localities (e.g. Greer in Iowa, USA, 

and Horton Bluff in Nova Scotia, Canada) and 

more recently in Australia (Ducabrook, 

Queensland). Rhizodontid remains from two 

Upper Devonian sites (one in Colombia, one 

in Turkey) have been attributed to Strepsodus, 

due to a misunderstanding of the defining 

characteristics (autapomorphies) of the genus. 

This paper reviews what is known of Strepsodus 

and Archichthys, and advocates that 

each be treated as a monospecific genus until 

reliable morphological evidence of further 

speciation is found. A neotype specimen for 

Strepsodus sauroides is proposed, and a 

check-list of published rhizodontid species is 

appended. 

2007010339 

西班牙 Celtiberia 早泥盆世一腔鳞鱼类及 

对西班牙的腔鳞鱼类的修订 = A new early 

Devonian Thelodont from Celtiberia (Spain), 

with a revision of Spanish Thelodonts. ( 英文 ). 

Botella H; Valenzuela-Ríos J; Carls P. Palaeontology, 

2006, 49(1): 141-154 

A revision of thelodont scales from the 

Lower Devonian of the Iberian Chains enables 

their grouping into two taxa: Turinia pagei 

and T. nachoi sp. nov. These taxa are clearly 

distinguishable by morphological and histological 

features; they also have a different 

stratigraphic range (T. pagei is restricted to 

Lochkovian strata, whereas T. nachoi sp. nov. 

occurs within lower–middle Pragian rocks). 

The new species is represented by head, transitional 

(cephalopectoral) and trunk scales. 

2007010340 

英格兰南部怀特岛早白垩世 Wealden 群非 

海相 Wessex 组一新软骨鲨类 = A Neoselachian 

Shark from the Non-marine Wessex 

Formation (Wealden group: early Cretaceous, 

Barremian) of the Isle of Wight, Southern 

England. ( 英文 ). Sweetman S C; Underwood 

C J. Palaeontology, 2006, 49(2): 457-465 

Bulk screening of Early Cretaceous (Barremian) 

Wessex Formation strata exposed on 

the south-east coast of the Isle of Wight, 

southern England, has resulted in the recovery 

of neoselachian shark teeth referred to the 

scyliorhinid Palaeoscyllium. These are the 

first neoselachian remains from the British 

Wealden Group and represent the geologically 

oldest neoselachian yet recovered from a 

freshwater deposit. This is also the only 

known example of a non-marine occurrence of 

a member of the Scyliorhinidae. 

2007010341 

泰国下白垩统一新软骨鱼群 = A new Elasmobranch 

assemblage from the lower Cretaceous 

of Thailand. ( 英文 ). Cappetta H; Buffetaut 

E; Cuny G; Suteethorn V. Palaeontology, 

2006, 49(3): 547-555 

99

The discovery of a new elasmobranch assemblage 

from the Lower Cretaceous of Thailand 

allows expansion of the faunal list and 

refinement of our knowledge of the dental 

morphological features of some previously 

described taxa. The root morphology of 

Thaiodus is now known and a more complete 

description of the dentition of the genus Heteroptychodus, 

known formerly by a single 

tooth from Japan, is given. A new genus and 

species, Acrorhizodus khoratensis, characterized 

by teeth of very special morphology is 

described. Besides these taxa, some teeth of a 

genus probably close to Hybodus, but with 

more bulbous teeth, are present. Owing to the 

sedimentological characters of the deposits 

and the associated fauna (dinosaurs), it is 

probable that this elasmobranch fauna lived in 

a freshwater or brackish environment. The 

simultaneous occurrence of teeth of Heteroptychodus 

in Thailand and Japan favours the 

existence of a large continental area in southeast 

Asia during the Early Cretaceous. 

2007010342 

意大利 Monte Bolca 始新统 Scombrid 的修 

订 = A revision of Scombrid fishes (Scombroidei, 

Perciformes) from the middle Eocene 

of Monte Bolca, Italy. ( 英文 ). Monsch K A. 


A taxonomic revision of mackerel-like 

fishes (Scombridae, Scombroidei, Perciformes) 

from the Monte Bolca localities in Italy is presented 

as part of continuing research into phylogenetic 

relationships of fossil and Recent 

scombroids. Three new genera are proposed: 

Godsilia, Pseudauxides and Thunnoscomberoides. 

In addition, species generally known as 

Thynnus bolcensis, Thynnus lanceolatus, 

Scombrosarda propterygia, Scomberomorus 

speciosus and Scomberomorus tenuis are renamed 

Thunnoscomberoides bolcensis comb. 

nov., Godsilia lanceolata comb. nov., Auxides 

propterygius comb. nov. and Pseudauxides 

speciosus comb. nov., respectively. S. tenuis, a 

nomen nudum, is a junior synonym of 

P. speciosus. Provisional phylogenetic hypotheses 

of these Monte Bolca scombrids are 

as follows. Auxides and Pseudauxides are 

most likely primitive sister taxa of the mackerels 

Scomber and Rastrelliger with Pseudauxides 

as the most primitive. Godsilia may 

be placed between Scombrinae and 

Scomberomorinae. Thunnoscomberoides 

seems to fit between Scombrinae and 

Thunnini. 

2007010343 

鼠鲨 (Chondrichthyes: Elasmobranchii) 的 

演化史 , 及牙齿特征对鼠鲨系统分类作出 

的贡献 = Phylogeny of lamniform sharks 

(Chondrichthyes: Elasmobranchii) and the 

contribution of dental characters to lamniform 

systematics. ( 英文 ). Kenshu S. Paleontological 

Research, 2005, 9(1): 55-72 

Lamniform sharks (Chondrichthyes: Elasmobranchii) 

are common in the fossil record 

but are represented mainly by isolated teeth. A 

phylogenetic analysis of 15 extant lamniform 

species based on 42 morphological characters 

using Scyliorhinus (Carcharhiniformes) as an 

outgroup produces a consensus tree with the 

following generic relationships: [Mitsukurina+[Carcharias+Odontaspis+Pseudocarchari 

as+Megachasma+[Alopias+[Cetorhinus+[[Isur 

us+Carcharodon]+Lamna]]]]]. When an extinct 

form, Cretoxyrhina mantelli, is added to 

the analysis, the fossil taxon occurs within the 

Alopias clade. Comparisons among the cladogram 

based on 29 non-dental characters alone, 

that based on 19 dental characters, and that 

based on combined (48) characters, suggest 

that dental characters provide at least some 

phylogenetic signal. Mapping of quantitative 

dental data on the cladogram based on nondental 

characters suggests 1) a decrease in the 

number of tooth rows through lamniform phylogeny, 

2) possible relationships between the 

crown heights and food types or feeding habits, 

and 3) that narrower crowns are plesiomorphic 

in lamniforms. 

2007010344 

关于日本西南地区 Tanegashima 更新世鲱 

鱼 Clupanodon tanegashimaensis (Saheki, 

1929) 的修订 = Revision of the Pleistocene 

clupeid fish Clupanodon tanegashimaensis 

(Saheki, 1929) from Tanegashima, Southwest 

Japan. ( 英文 ). Yabumoto Y; Sakamoto Y; 

Otsuka H. Paleontological Research, 2005, 

9(4): 299-304 

Clupea tanegashimaensis was described 

by Saheki (1929) on the basis of a single 

specimen from Sumiyoshi, Katanoyama, Tanegashima 

Island, Japan. The holotype is reexamined 

and redescribed with additional 

specimens excavated from the type locality in 

1988 and 1989. This species is not a member 

of the genus Clupea. It belongs to the genus 

Clupanodon because of the presence of dorsal 

scutes and the elongated last dorsal fin ray. 

The fossil fish fauna from Tanegashima has 

the potential to be an important basis for un- 

100

derstanding the origin and evolution of a 

number of species in the Pacific coastal fish 

fauna. 

2007010345 

泰国晚侏罗世 - 早白垩世辐鳍鱼亚纲一个新 

的半椎鱼化石 = A new Semionotid (Actinopterygii, 

Neopterygii) from the Late Jurassic- 

Early Cretaceous of Thailand. ( 英文 ). Cavin L; 

Suteethorn V; Khansubha S; Buffetaut E; 

Tong H Y. Comptes Rendus Palevol, 2003, 

2(5): 291-297 

A new semionotid fish, Lepidotes 

buddhabutrensis n. sp., is described from the 

continental Late Jurassic-Early Cretaceous 

Phu Kradung Formation, Phu Nam Jun, Kalasin 

Province. L. buddhabutrensis is characterized 

notably by the pattern of its cheek 

bones, by its short preorbital region, and by its 

numerous and well-developed premaxillary 

teeth. L. buddhabutrensis is provisionally 

placed in the genus Lepidotes; it shares, however, 

derived characters with other 

semionotids, such as Araripelepidotes and 

Pliodetes. 

2007010346 

墨西哥东北部 Agua Nueva 组新的真骨鱼 

类化石 = New Teleostei from the Agua 

Nueva Formation (Turonian), Vallecillo (NE 

Mexico). ( 英文 ). Blanco A; Cavin L. Comptes 


A new genus and new species of an ichthyodectiform 

fish, a new species of the 

pachyrizodontid Goulmimichthys, as well as 

specimens of Araripichthys sp. are described 

from the Agua Nueva Formation (Turonian) 

of Vallecillo, State of Nuevo Leon, NE Mexico. 

The ichthyodectiform fish shows a combination 

of characters from different families, 

warranting the creation of a new genus and 

questioning the monophyly of these families. 

We report herein the first record of Goulmimichthys 

and Araripichthys in North America. 

两栖类 

2007010347 

匈牙利更新世飞蜥的首次记录 = First record 

of an agamid lizard from the Pleistocene of 

Hungary. ( 英文 ). Meszoely Ch A M; Gasparik 


2002, (20): 1-2 

In 1998 a small fragment of an agamid 

lizard mandible was discovered among the 

reptile bones from the locality of Tokod. It is 

the first agamid remain from the Pleistocene 

of Hungary. The presence of this taxon indicates 

a warm interglacial climate and raises 

the possibility that the age of the locality is 

Eemian, i. e. older than previouly thought. 

2007010348 

格陵兰岛东部晚泥盆世四足动物 

Ichthyostega 的分类学修订 = Taxonomic 

revision of the Late Devonian tetrapod Ichthyostega 

from East Greenland. ( 英文 ). Blom 

H. Palaeontology, 2005, 48(1): 111-134 

Two morphologically distinct assemblages 

of the Late Devonian tetrapod Ichthyostega 

from East Greenland are described 

on the basis of a large collection of skulls and 

postcranial elements. Skull specimens collected 

on Gauss Halvø show that the assemblage 

from the lower Aina Dal Formation has 

proportionally narrower skulls and finer skull 

roof sculpture than the assemblage from the 

higher Britta Dal Formation. The assemblages 

are compared with the stratigraphically unconstrained 

type material from the north side of 

Celsius Bjerg on Ymer Ø, allowing a taxonomic 

revision. From the original description 

of seven taxa, three species are recognized and 

related to the assemblages from Gauss Halvø. 

I. stensioei is comparable with the Aina Dal 

Formation assemblage while I. eigili and 

I. watsoni are valid for specimens found in the 

Britta Dal Formation. Ichthyostegopsis wimani 

is not a valid genus or species and may be regarded 

as a juvenile I. eigili. This example of 

species-level variability is the earliest known 

from the fossil record of early tetrapods. 

2007010349 

波兰上三叠统离椎类 Cyclotosaurus = The 

temnospondyl amphibian Cyclotosaurus from 

the Upper Triassic of Poland. ( 英文 ). Sulej T; 

Majer D. Palaeontology, 2005, 48(1): 157-170 

A gap in the Late Triassic fossil record of 

the capitosaur amphibian Cyclotosaurus is 

filled by new material from lacustrine deposits 

at Krasiejów, Poland, corresponding in age to 

the Lehrberg Beds (late Carnian) of Germany. 

The skull of the Polish cyclotosaur is intermediate 

in several respects between that of 

Cyclotosaurus robustus from the middle 

Carnian Schilfsandstein of Germany and the 

younger C. mordax from the early Norian 

Stubensandstein. It shows a decrease in the 

width of the skull and in the degree of concavity 

of the posterior margin of the skull roof. 

The differences are significant enough to warrant 

erection of a novel species, the name 

101

Cyclotosaurus intermedius sp. nov. being proposed. 

The pectoral girdle, identified for the 

first time in Cyclotosaurus, suggests the genus 

was more fully adapted to an aquatic mode of 

life than was Paracyclotosaurus. 

2007010350 

南非下三叠统一陆生离片椎类动物 : 

Lydekkerina Huxleyi 的颅后骨架 = A terrestrial 

Stereospondyl from the lower Triassic 

of South Africa: the Postcranial skeleton of 

Lydekkerina Huxleyi (Amphibia: Temnospondyli). 

( 英文 ). Pawley K; Warren A. Palaeontology, 

2005, 48(2): 281-298 

Description of the postcranial skeleton of 

the basal stereospondyl amphibian Lydekkerina 

huxleyi from new material shows it to 

be heavily ossified with large processes for 

muscle attachment and well-developed articulation 

surfaces. The structure of the postcranial 

skeleton implies a substantial capability 

for terrestrial locomotion, rather than a primarily 

aquatic existence as has been suggested 

for most other stereospondyls. The postcranial 

skeleton is most similar to that of Uranocentrodon 

and the Archegosauroidea, and is 

unlike that of the poorly ossified, more derived 

stereospondyls and Dvinosauria. The 

postcranial skeleton does not display any of 

the particular apomorphies of the fully ossified 

Permian terrestrial temnospondyls. 

Cladistic analysis using the postcranial data 

obtained in this study indicates that within the 

Stereospondyli Lydekkerina huxleyi is neither 

a member of the Rhinesuchidae nor the Mastodonsauroidea, 

rather the Lydekkerinidae are 

a separate taxon. 

2007010351 

坦桑尼亚中北部始新世火山口湖中一新的 

Pipine 蛙 = A new Pipine Frog from an Eocene 

Crater lake in North-central Tanzania. 

( 英文 ). Báez A M; Harrison T. Palaeontology, 

2005, 48(4): 723-737 

The fossiliferous site of Mahenge, Tanzania, 

interpreted as a small lake that formed 

in a kimberlite intrusion, has yielded a vertebrate 

assemblage that includes scarce frog 

remains. Radiometric dating of the pipe indicates 

that the volcanic activity took place at 

45·83 ± 0·17 Ma, whereas infilling of the crater 

was completed in 0·2–1·0 myr after emplacement. 

The frogs, described herein, are 

preserved as partially articulated skeletons that 

represent a new pipine taxon, Singidella latecostata 

gen. et sp. nov. A parsimony analysis 

of fossil and extant pipoid frogs indicates that 

Singidella is more closely related to African 

Hymenochirus and Pseudhymenochirus than 

to South American Pipa. It also provides weak 

support for the sister-group relationship of 

Singidella and the bizarre Late Cretaceous 

Pachycentrata taqueti (replacement name for 

Pachybatrachus taqueti) from Niger, although 

the incomplete preservation of Pachycentrata 

precludes thorough comparisons. This record 

indicates that prior to the rifting in the Miocene 

the distribution of pipines extended into 

eastern Africa where they do not occur today. 

爬行类 

2007010352 

北美下白垩统上龙类首次记录 = The first 

record of a pliosaurid (Plesiosauria, Pliosauridae) 

from the Lower Cretaceous of North 

America. ( 英文 ). Haggart J W; Nicholls E L; 

Bartlett R. Cretaceous Research, 2003, 24(2): 

129-133 

The fragmentary remains of a plesiosaur 

have been collected from the Haida Formation 

(Albian, Lower Cretaceous) at Cumshewa 

Inlet, Queen Charlotte Islands, British Columbia. 

The specimen is identified as a member of 

the family Pliosauridae, based on tooth structure. 

This is the first record of a pliosaurid 

from the west coast of North America, and the 

first pliosaurid from the Lower Cretaceous of 

North America. 

2007010353 

英格兰南部多塞特 Purbeck 灰岩组 ( 下白 

垩统 : 贝里亚斯阶 )‘granicones’ 的形态 

学、组织学及鉴定 = Morphology, histology 

and identification of the ‘granicones’ from the 

Purbeck Limestone Formation (Lower Cretaceous: 

Berriasian) of Dorset, southern England. 

( 英文 ). Barrett P M; Clarke J B; Brinkman 

D B; Chapman S D; Ensom P C. Cretaceous 

Research, 2002, 23(2): 279-295 

The identification of the ‘granicones’, 

small, conical and shield-like phosphatic 

structures with a pustulate surface ornamentation, 

from the Purbeck Limestone Formation 

of Dorset, has been problematic for over 130 

years. They have been interpreted as the osteoderms 

of theropod or ornithischian dinosaurs, 

lizards or crocodiles, though only circumstantial 

evidence was presented in support 

of these hypotheses. Here, we provide anatomical, 

histological and geological evidence 

that demonstrates the true affinities of the 

granicones: they are the limb osteoderms of 

turtles and may be referable to either Heloche- 

102

lydra (=Tretosternon) anglica or ‘Tretosternon’bakewelli 

. 

2007010354 

新疆昌吉下白垩统的 "ornithurine": 鸟还 

是翼龙 = The "ornithurine" from the Lower 

Cretaceous of Changji, Xinjiang (China): bird 

or pterosaur. ( 英文 ). Buffetaut E. Cretaceous 

Research, 1996, 17(4): 505-508 

A tibia with a fused fibula from the 

Lower Cretaceous of Changji (Xinjiang, 

China), originally interpreted as possibly belonging 

to an ornithurine bird, is redescribed 

and interpreted as belonging to a dsungaripterid 

pterosaur. 

2007010355 

初龙类的呼吸和鳄型类的腰带辅助呼吸 = 

Archosaurian respiration and the pelvic girdle 

aspiration breathing of crocodyliforms. ( 英文 ). 

Claessens L P A M. Proceedings of the 

Royal Society B: Biological Sciences, 2004, 

271(1547): 1461 - 1465 

Birds and crocodylians, the only living 

archosaurs, are generally believed to employ 

pelvic girdle movements as a component of 

their respiratory mechanism. This in turn provides 

a phylogenetic basis for inferring that 

extinct archosaurs, including dinosaurs, also 

used pelvic girdle breathing. I examined lung 

ventilation through cineradiography (highspeed 

X-ray filming) and observed that alligators 

indeed rotate the pubis to increase tidal 

volume, but did not observe pelvic girdle 

movement contributing to lung ventilation in 

guinea fowl, emus or tinamous, despite extensive 

soft-tissue motion. Re-examination of 

fossil archosaurs reveals that pubic rotation 

evolved in basal crocodyliforms and that pelvic 

girdle breathing is not a general archosaurian 

mechanism. The appearance of 

pelvic aspiration in crocodyliforms is a striking 

example of the ability of amniotes to increase 

gas exchange or circumvent constraints 

on respiration through the evolution of novel 

accessory breathing mechanisms. 

2007010356 

阿根廷里奥内格罗省晚白垩世 

Comahuesuchus brachybuccalis 新的颅骨 

化石 = New cranial remains of the bizarre 

notosuchid Comahuesuchus brachybuccalis 

(Archosauria, Crocodyliformes) from the Late 

Cretaceous of Rio Negro Province (Argentina). 

( 英文 ). Martinelli A G. Ameghiniana, 2003, 

40(4): 559-572 

New cranial remains of Comahuesuchus 

brachybuccalis Bonaparte from the Late Cretaceous 

Bajo La Carpa Formation of Rio Negro 

Province (Argentina) are described. Comahuesuchus 

brachybuccalis differs from all 

other crocodyliforms in having the association 

of the following derived features: extremely 

short, wide and circular snout; five anterior 

small teeth in the maxilla except the third hypertrophied 

caniniform; eleven teeth in the 

dentary with the anterior ones procumbent; all 

lower teeth small and circular in cross section 

except the tenth hypertrophied caniniform; 

dorsally opened paracanine fossa in the posterior 

maxillary region; contact among the ectopterygoid, 

pterygoid and palatine in the ventral 

region of the pterygoid wing; lachrymal 

with a long and thin process projecting laterally; 

and anterior portion of the dentary low 

and transversely broad, with an anteroposterior 

elongated symphysis extending at the 

level of the ninth tooth. The phylogenetic 

analysis nests C. brachybuccalis within the 

notosuchian clade, also represented by Malawisuchus 

mwakasyungutiensis and Chimaerasuchus 

paradoxus from the Early Cretaceous 

of Africa and China, and Notosuchus 

terrestris and Sphagesaurus huenei from the 

Late Cretaceous of South America. This group 

is diagnosed by having the external surface of 

the premaxilla and maxilla with two plane of 

exposure, one facing laterally (almost vertical) 

and the other dorsolaterally (almost horizontal); 

the dentary extending beneath the mandibular 

fenestra; a reduced number of maxillary 

teeth; and the articular facet for the quadrate 

condyle almost twice as long as wide 

lacking a posterior transversely ridge (uncertain 

in Comahuesuchus and Spliagesaurus). 

2007010357 

阿根廷恩特雷里奥斯白垩纪 Puerto Yerua 

组恐龙新证据 = New evidence of dinosaurs 

from the Puerto Yerua (Cretaceous) Formation 

(Entre Rios, Argentina). ( 其他 ). De Valais S; 

Apesteguia S; Sauthier D U. 

Ameghiniana, 2003, 40(4): 631-635 

2007010358 

白垩纪 Dinilysia patagonica 的生活习态 = 

Life habit of the Cretaceous snake Dinilysia 

patagonica Woodward.. ( 其他 ). Albino A M; 

Caldwell M W. Ameghiniana, 2003, 40(3): 

407-414 

Palaeoecological reconstructions of the 

Patagonian Cretaceous snake Dinilysia patagonica 

are discussed in relation to hypothe- 

103

sized life modes for an "ancestral snake", and 

in relation to the ecotypes of basal snakes. A 

comparison of orbit orientation (e.g., dorsally 

exposed eyes) and aspects of postcranial osteology 

in diverse ecological types of snakes 

does not clearly resolve life modes and habits. 

Dinilysia is interpreted here as a partially terrestrial 

snake whose morphology may have 

been adaptable to semi-aquatic (seasonal lagoons 

and streams) or semi-fossorial habits 

(dune fields and interdune basin deposits). 

Partially terrestrial snakes with large bodies 

that may have fed on small to medium-sized 

prey items would have appeared earlier in 

snake phylogeny than has been previously 

supposed. 

2007010359 

阿根廷巴塔哥尼亚中侏罗世蜥脚龙次亚目 

Patagosaurus 属齿骨 = A dentary of Patagosaurus 

(Sauropoda) from the Middle Jurassic 

of Patagonia. ( 英文 ). Rauhut O W M. 

Ameghiniana, 2003, 40(3): 425-432 

A sauropod dinosaur dentary from the 

Middle Jurassic (Callovian) of the Canadon 

Asfalto Formation of southern Argentina is 

described. The dentary can be referred to 

Patagosaurus fariasi Bonaparte. Differences 

between several specimens referred to 

Patagosaurus indicate that more than one 

taxon of sauropod is represented in this material. 

A critical discussion of several new and 

previously used sauropod dentary characters is 

presented. On the basis of dentary and dental 

characters taken from published phylogenetic 

analyses, an advanced, non-neosauropodan 

eusauropodan position for Patagosaurus is 

indicated. Sauropod dentaries exhibit numerous 

characters of potential phylogenetic value, 

but more detailed investigations and new finds 

are necessary to explore their distribution and 

phylogenetic utility 

2007010360 

关于归于恐龙类蜥脚龙次亚目雷龙的骨板 

的思考 = Considerations on the bony plates 

assigned to titanosaurs (Dinosauria, Sauropoda). 

( 英文 ). Salgado L. Ameghiniana, 2003, 

40(3): 441-456 

Several bony plates referred to titanosaurs 

are reviewed. Two groups of plates, exhumated 

from two different localities, 

LagoPellegrini-Cinco Saltos and Salitral Moreno, 

in the province of Rio Negro, are described. 

Several characters diferenciate the 

two groups, as the presence in one group of a 

shallow dorsal depression (Type I sense 

Huene), a dorsal awe, a ventral ridge, and a 

cingulum. Generally, most of the plates are 

symmetrical, although a few present a marked 

asymmetry. The former apparently were located 

in the midline of the body over the neural 

spines, and the others laterally on both 

sides of the animal body. Histologically, the 

plates are composed ventrally by cancellous 

bone and externally by Haversian bone, and 

the Sharpey's fibers are present, mainly, in the 

periphery on the dorsal surface of the plates. 

2007010361 

美国新墨西哥中东部 Moenkopi 组上部 

Anton Chico 段一新的巨大初龙类 = A new, 

large archosauriform from the Anton Chico 

Member of the upper Moenkopi Formation 

(Middle Triassic), east-central New Mexico, 

USA. ( 英文 ). Nesbitt S J; Lucas S G; Schoch 

R R. Neues Jahrbuch fur Geologie u. 


289-311 

We document teo incomplete skeletons 

of a new taxon of a large archosauriform from 

a lacustrine deposit in the upper Anton Chico 

Member of the Moenkopi Formation in eastcentral 

New Mexico. This new reptile is the 

largest known from the Moenkopi Formation 

and, though incomplete, it belongs to at least 

the archosauriform clade based on the presence 

of osteoderms and the structure of the 

pelvis. The Moenkopi reptile is another example 

of the previously little known diversity of 

reptiles from the early Middle Triassic of 

North America. 

2007010362 

阿根廷新的三叠纪食肉性恐龙 = A new Triassic 

carnivorous dinosaur from Argentina. 

( 英文 ). Arcucci A B; Coria R A. 

Ameghiniana, 2003, 40(2): 217-228 

A new Triassic theropod, Zupaysaurus 

rougieri is described from La Rioja Province 

and its phylogenetic relationships amongst 

Theropoda are discussed. Zupaysaurus shares 

with Tetanurae several features that include 

the presence of a tooth row that is anterior to 

the orbit, a pneumatized lacrimal, and a tibia 

with a posterolaterally concave and transversely 

expanded distal end. Features shared 

with some ceratosaurs, like the presence of a 

longitudinal alveolar ridge on the maxilla, a 

large antorbital fenestra, and a fused astragalus-calcaneum, 

are either homoplasies with 

some ceratosaurs or plesiomorphic features 

within Neotheropoda. Based on relative stratigraphical 

position, Zupaysaurus is regarded as 

104

Late Triassic in age, which makes it the oldest 

record of Tetanurae. Zupaysaurus provides 

data about the early evolution of theropods, 

strengthening the assumption about the origin 

of tetanurans in the Late Triassic, and indicating 

their simultaneous record with the oldest 

coelophysids (i.e. Coelophysis and Liliensternus). 

2007010363 

浙江永康发现 Faveoloolithidae 恐龙蛋化石 

= Faveoloolithidae dinosaur egg fossils found 

at Yongkang,Zhejiang. ( 中文 ). 俞云文 ; 陈景 ; 

金幸生 ; 颜铁增 ; 彭振宇 . 地质通报 , 2003, 

22(3): 218-219 

1995 年 , 在扩建永康至武义公路的施工 

中 , 于永康市区西侧西山头村边山坡上 

(N28°03′37″,E120°00′38") 发现恐龙骨骼和 

蛋化石 , 均产于永康群朝川组中 . 两者产出的 

位置距离约 50m. 

2007010364 

辽西热河群下白垩统非鸟虚骨龙类化石 = 

Non-avian dinosaur fossils from the Lower 

Cretaceous Jehol group of Western Liaoning, 

China. ( 英文 ). Xu Xing; Norell M A. Geological 

Journal, 2006, 41(3/4): 419-437 

Over the past 10 years, numerous dinosaur 

specimens covering several major dinosaurian 

clades have been recovered from the 

Lower Cretaceous Jehol Group of western 

Liaoning. Among ornithischians from the Jehol 

Group, ornithopod fossils shed new light 

on the evolution of this largest ornithischian 

group; ankylosaurian discoveries add morphological 

diversity relevant to the highly specialized 

ankylosaurian body-plan and ceratopsian 

occurrences offer a chance to study patterns of 

morphological change at the base of the Ceratopsia. 

The most significant discoveries are 

exceptionally well-preserved theropod specimens 

covering most major coelurosaurian 

groups. Most theropod taxa from the Jehol 

Biota are the earliest, most basal members of 

coelurosaurian sub-clades and provide substantial 

new information important for the reconstruction 

of coelurosaurian phylogeny and 

understanding the character evolution. The 

examination of character distributions along 

the coelurosaurian lineages reveals that the 

major structural modifications seen in birds 

were acquired sequentially and hierarchically 

early in coelurosaurian evolution. Most significantly, 

the Liaoning theropod discoveries 

advanced our understanding of two longdebated 

evolutionary issues: the origin and 

early evolution of feathers and the origin of 

avian flight. The known distribution of the 

feather-like integumentary structures and true 

feathers along the coelurosaurian lineages 

suggests that: (1) simple, filamentous integuments 

represent a primitive morph in feather 

evolution; (2) pennaceous feathers evolved 

early in maniraptoran evolution; and (3) feathers 

with aerodynamic features originated before 

the origin of birds. The presence of flight 

feathers on the metatarsus represents a new 

morph that is not known previously, but it has 

implications for understanding the origin of 

avian flight. The discovery of four-winged 

dinosaurs was suggested to provide strong 

evidence supporting the 'tree-down' hypothesis 

for the origin of avian flight, though in-depth 

analysis and more data are needed to confirm 

this. A brief analysis of the fossil preservation 

and faunal composition reveals several interesting 

characteristics: (1) Volcanic activity 

might have contributed to the exceptional 

preservation of dinosaurian skeletons and in 

particular their soft tissues; (2) Different from 

most other dinosaur faunas, the Jehol dinosaur 

fauna has a low ornithischian specific diversity 

relative to a high theropod specific diversity; 

and (3) the Liaoning theropods show a 

strong tendency toward secondary herbivory. 

The faunal composition suggests a complex 

biogeographic history for this fauna and provides 

negative evidence for the hypothesis that 

eastern Asia was isolated from the Middle 

Jurassic through late Early Cretaceous times. 

2007010365 

热河生物群的翼龙组合及其早白垩世翼龙 

辐射的意义 = Pterosaur assemblages of the 

Jehol Biota and their implication for the Early 

Cretaceous pterosaur radiation. ( 英文 ). Wang 

Xiaolin;, Zhou Zhonghe. Geological Journal, 

2006, 41(3/4): 405-418 

The Early Cretaceous Jehol Biota from 

northeast China is well known for many beautifully 

preserved feathered dinosaurs, early 

birds and angiosperms. A great number of 

pterosaurs have also been discovered from the 

same deposits in recent years, representing 

arguably the best pterosaur assemblage from 

the Lower Cretaceous. Two pterosaur assemblages 

are recognized from the Jehol Biota, 

and represent two major adaptive radiations in 

the Early Cretaceous. The first radiation was 

preserved mainly in the Yixian Formation, and 

shows a strong resemblance to the Upper Jurassic 

pterosaur radiation in the Solnhofen 

Limestone of Germany. The second radiation 

105

was preserved in the Jiufotang Formation, 

with many of its taxa much similar to those of 

the pterosaur assemblages from the Lower 

Cretaceous Santana Formation of Brazil. Recent 

biostratigraphic work and radiometric 

datings of the Yixian and Jiufotang formations 

have provided a reliable geochronologic 

framework for the Jehol pterosaur radiations. 

The two major radiations occurred at about 

125 Ma and 120 Ma, respectively. The radiations 

of the Jehol pterosaurs are characterized 

by a remarkable taxonomic diversity, great 

variation in body size, significant dietary differentiation, 

and occupancy of diverse niches. 

The appearance of several biological novelties 

was also critical in the success of the Jehol 

pterosaur radiations. The adaptive radiation of 

the Jehol pterosaurs was obviously coupled 

with the competition or co-evolution with 

many other groups of the Jehol Biota. Among 

the flying animals in the Jehol Biota, pterosaurs 

were the major competitors for niches 

and food with birds. Although the Jehol pterosaurs 

probably fed mainly on fishes, the coevolution 

between plants and pterosaurs in the 

Jehol Biota might also have played a significant 

role in the pterosaur radiations, as is the 

case for plants and insects, birds, mammals 

and dinosaurs. 

2007010366 

加拿大不列颠哥伦比亚东北部上白垩统 

Kaskapau 组中土仑期恐龙古环境 = Middle 

Turonian dinosaur paleoenvironments in the 

Upper Cretaceous Kaskapau Formation, 

northeast British Columbia. ( 英文 ). Rylaarsdam 

J R; Varban B L; Plint A G; Buckley L G; 

McCrea R T. Canadian Journal of Earth Sciences, 

2006, 43(6): 631-652 

The Kaskapau Formation is a mudstonedominated 

wedge up to 950 m thick that spans 

late Cenomanian to middle Turonian time. 

The formation has a prominent wedge geometry 

and was deposited in the foredeep of the 

Western Canada Foreland Basin. In outcrop in 

northeast British Columbia, nearshore sandstones 

are locally well developed and include 

rare wedges of nonmarine strata. On Quality 

Creek, near Tumbler Ridge, 11 m of nonmarine 

strata contain abundant dinosaur tracks 

and the first in situ dinosaur bone reported 

from British Columbia. This site, at a paleolatitude 

of about 67 degrees N, preserves a 

rare glimpse of Turonian terrestrial environments 

during global eustatic highstand. Three 

main dinosaur habitats are recognized: strandplain 

and beach-ridge; freshwater lake; and 

brackish lagoon. Back-beach sandstone has a 

relief of about 2.5 m, interpreted as beach 

ridges; sandy coals containing abundant dinosaur 

tracks represent inter-ridge slough deposits. 

Overlying lake deposits comprising laminated 

muds with freshwater molluscs grade up 

into rooted muddy siltstone and locally, dinoturbated 

sandstone. Lake deposits are capped 

by lagoonal mudstone with abundant brackishwater 

molluscs, locally including a dinosaurtrampled 

oyster bioherm. The upper parts of 

sandy lagoonal deltas are pervasively dinoturbated. 

Sandstone filling a tidal channel contains 

logs, oyster shells, and bones of dinosaurs, 

turtles, and crocodiles, as well as fish 

scales. The lagoonal succession is erosively 

overlain by offshore sandy mudstones. Various 

lines of evidence suggest that the mean 

annual temperature at this sea-level location 

was about 14 degrees C, with a cold-month 

mean no less than 5.5 degrees C. The highlatitude 

location implies a significant period of 

winter darkness, and correspondingly diminished 

plant productivity. 

2007010367 

阿根廷门多萨省上白垩统一个新的雷龙 = 

A new titanosaur (Dinosauria, Sauropoda) 

from the Upper Cretaceous of Mendoza Province, 

Argentina. ( 英文 ). Riga B J G. 

Ameghiniana, 2003, 40(2): 155-172 

Mendozasaurus neguyelap gen. et sp. nov. 

is a new titanosaur from the Upper Cretaceous 

of Neuquen Basin and the first known dinosaur 

species from Mendoza Province, Argentina. 

The remains were found in levels provisionally 

referred to the Rio Neuquen Formation 

(late Turonian-late Coniacian) of the 

Neuquen Group. They consist of 22 mostly 

articulated caudal vertebrae, a dorsal vertebra, 

numerous disarticulated appendicular bones 

and osteoderms. Autapomorphies of Mendozasaurus 

are: (1) subtriangular infrapostzygapophyseal 

fossae in anterior dorsal vertebrae; 

(2) postzygapostspinal laminae parallel to the 

plane of the postzygapophyseal facets in anterior 

dorsal vertebrae; (3) interzygapophyseal 

cavity dorsoventrally extended and limited by 

the spinopostzygapophyseal and spinoprezygapophyseal 

laminae in anterior caudal vertebrae; 

(4) middle caudal vertebrae slightly procoelous 

with reduced posterior condyles displaced 

dorsally; (5) laminar mid-posterior 

caudal neural spines with horizontal and 

straight dorsal border, and anterodorsal corner 

forming a right angle; (6) large subconicspherical 

osteoderms lacking cingulum. A 

106

cladistic analysis permits the inclusion of 

Mendozasaurus within Titanosauridae, according 

to the phylogenetic definition of this 

clade. Although this new species exhibits almost 

all the titanosaurid synapomorphies proposed 

by some authors, it lacks prominent 

posterior condyles in middle caudal centra. 

This and other plesiomorphic traits suggest 

that Mendozasaurus is a basal titanosaurid, 

more derived than Malawisaurus in the caudal 

procoely. 

2007010368 

阿根廷巴塔哥尼亚内乌肯盆地侏罗纪蜥脚 

类恐龙化石的首次发现 = First remains of 

sauropod dinosaurs in the Jurassic of the Neuquen 

Basin (Patagonia, Argentina). ( 其他 ). 

Garcia R; Salgado L; Coria R A. 

Ameghiniana, 2003, 40(1): 123-126 

2007010369 

匈牙利 Tokod 地区晚更新世蛇化石 = Fossil 

snakes from the Late Pleistocene of Tokod 

(Gerecse Mountains, Hungary). ( 英文 ). 

Meszoely C M; Venczel M; Gasparik M. 


(23): 1-4 

So far more than sixty species of vertebrates, 

ammong them at least eight genera of 

reptiles and amphibians have been recognized. 

Among the reptiles, four genera of snakes 

have been identified on basis of the morphology 

of the basiparasphenoid bone or vertebrae. 

All four of these snake genera: Coluber, 

Coronella, Natrix, and Vipera still occur in 

Hungary today. Due to the fragmentary nature 

of the fossil material, positive identification as 

to the species is not possible at this time and 

the four snake species are tentatively referred 

to the modern species found in Hungary: 

Coluber caspius, Coronella austriaca, Natrix 

natrix, and Vipera berus. 

2007010370 

意大利上三叠统海生双孔类 

Endennasaurus = The marine diapsid reptile 

Endennasaurus from the Upper Triassic of 

Italy. ( 英文 ). Muller J; Renesto S; Evans S E. 


The marine reptile Endennasaurus from 

the Upper Triassic Zorzino Limestone of 

northern Italy is redescribed and reassessed. 

New details of the skull and postcranial skeleton 

are revealed, confirming the attribution of 

this genus to the diapsid reptile clade Thalattosauriformes. 

Phylogenetic analysis suggests 

that Endennasaurus was related to the European 

genus Askeptosaurus and the Chinese 

Anshunsaurus. Despite a rather conservative 

postcranial morphology, Endennasaurus 

clearly occupied a highly specialized dietary 

niche as it combined a slender tapering premaxillary 

rostrum with a complete absence of 

either marginal or palatal teeth. 

2007010371 

巴塔哥尼亚中侏罗统一新的兽脚类的骨结 

构及其演化关系 = Osteology and relationships 

of a new theropod dinosaur from the 

Middle Jurassic of Patagonia. ( 英文 ). Rauhut 

O W M. Palaeontology, 2005, 48(1): 87-110 

A new taxon of theropod dinosaur is described 

as Condorraptor currumili gen. et sp. 

nov., from the Middle Jurassic (Callovian) 

Cañadón Asfalto Formation of Chubut Province, 

Argentinean Patagonia. The taxon is represented 

by a single fragmentary postcranial 

skeleton. Although incompletely known, Condorraptor 

is the second most complete theropod 

from the Middle Jurassic of Gondwana. 

The new taxon is characterized by the absence 

of a posterior incision between the fibular 

condyle and the medial side of the proximal 

articular end of the tibia, the pleurocoels in the 

anterior cervicals being situated posteroventral 

to the parapophyses, and the presence of a 

pronounced 'step' between the distal articular 

facet and shaft of Mt IV. Pneumatic features 

of the vertebral column show strong variation 

between the left and right side. Condorraptor 

gen. nov. can be referred to the Tetanurae and 

is a representative of a global radiation of 

basal tetanurans in the Early to Mid Jurassic. 

2007010372 

中亚吉尔吉斯斯坦 Fergana 洼地中侏罗统 

Balabansai Svita 的翼龙及恐龙遗体 = 

Pterosaur and dinosaur remains from the Middle 

Jurassic Balabansai Svita in the northern 

Fergana Depression, Kyrgyzstan (Central 

Asia). ( 英文 ). Averianov A O; Martin T; 

Bakirov A A. Palaeontology, 2005, 48(1): 

135-155 

Isolated pterosaur and dinosaur teeth and 

a sauropod metatarsal I and manual phalanx 

V-1 from the Middle Jurassic (Callovian) 

Balabansai Svita in the northern Fergana Valley, 

Kyrgyzstan, are described and attributed 

to the pterosaur taxon Rhamphorhynchinae 

indet., a theropod Tetanurae indet., a sauropod 

Neosauropoda indet., and a new pachycephalosaurid 

Ferganocephale adenticulatum gen. 

et sp. nov. The Balabansai theropod is possi- 

107

ly a stem-lineage representative of Dromaeosauridae. 

The new pachycephalosaurid is 

the oldest representative of the group and extends 

its known history by 10–20 myr. The 

Balabansai vertebrate assemblage is most 

similar to the Callovian assemblages from the 

Qigu and Upper Shaximiao formations in 

China, and intermediate in the evolutionary 

level of the taxa present between the Bathonian 

assemblages from Wucaiwan and the 

Lower Shaximiao formations (China) and the 

Late Jurassic Shar Teg fauna from Mongolia. 

2007010373 

印度中三叠统一新的初龙类 = A new rauisuchian 

archosaur from the Middle Triassic of 

India. ( 英文 ). Sen K. Palaeontology, 2005, 

48(1): 185-196 

Yarasuchus deccanensis gen. and sp. nov. 

is a new addition to the poorly known Middle 

Triassic terrestrial vertebrates. It is described 

on the basis of the fossil material of at least 

two incompletely preserved individuals and 

several isolated bones. It was a long-necked, 

gracile animal and might have had a facultatively 

bipedal gait. Apart from its characteristic 

elongate cervical vertebrae, other osteological 

features of Y. deccanensis resemble 

those of Prestosuchus, Saurosuchus, Ticinosuchus 

and 'Mandasuchus'. It is therefore referred 

to the Rauisuchian family Prestosuchidae 

despite the debated validity of this taxon. 

2007010374 

坦桑尼亚上二叠统 Geikia Locusticeps 的重 

新评价 = Reappraisal of Geikia Locusticeps 

(Therapsida: Dicynodontia) From the Upper 

Permian of Tanzania. ( 英文 ). Maisch M W; 

Gebauer E V I. Palaeontology, 2005, 48(2): 

309-324 

The holotype and only known specimen 

of Geikia locusticeps (von Huene, 1942) from 

the Kawinga Formation (Tatarian) of Kingori, 

south-west Tanzania, is redescribed. It is 

compared to the type specimen of the Tanzanian 

geikiid Pelanomodon tuberosus von 

Huene, 1942. It is demonstrated that 

G. locusticeps is a juvenile specimen of 

P. tuberosus. Ontogenetic changes in the skull 

of this taxon are recorded. They mainly concern 

the degree of skull ornamentation, 

whereas the major osteological and proportional 

features remain remarkably constant. 

Pelanomodon tuberosus is referred to Geikia 

locusticeps as a junior subjective synonym. 

G. locusticeps is compared to Geikia elginensis 

and South African representatives of Pelanomodon. 

G. locusticeps is demonstrated to 

represent a valid species, one that is so far 

endemic to the Ruhuhu Basin of south-west 

Tanzania. The relevance of the orientation of 

the postorbital bone to Permian pristerodontian 

systematics is discussed, and a phylogenetic 

analysis and new diagnosis for the family 

Geikiidae are presented. 

2007010375 

似鸵鸟龙的食物 = The diet of Ostrich Dinosaurs 

(Theropoda: Ornithomimosauria). ( 英 

文 ). Barrett P M. Palaeontology, 2005, 48(2): 

347-358 

The diets of ornithomimosaurian dinosaurs 

(Theropoda: Ornithomimosauria) have 

proved to be contentious owing to a dearth of 

unambiguous evidence in support of carnivory, 

omnivory or herbivory. Re-assessment of anatomical, 

taphonomical and palaeoecological 

evidence, and estimates of daily minimal energy 

budgets for two derived ornithomimosaurian 

genera, indicate that suspensionfeeding 

and carnivory were unlikely. The 

combined presence of a keratinized rhamphotheca 

and gastric mill is strongly indicative of 

a herbivorous habitus for these dinosaurs. 

Herbivorous and omnivorous forms are rare 

among the non-avian Theropoda, but are more 

common than previously suspected. Rejection 

of carnivorous habits for derived ornithomimosaurs 

redresses apparent discrepancies in 

the relative abundances of the herbivore and 

carnivore guilds of several Late Cretaceous 

faunas. 

2007010376 

南非下三叠统 Thrinaxodon Liorhinus 的生 

长模式 = Growth Patterns of Thrinaxodon 

Liorhinus, A Non-Mammalian Cynodont 

From the Lower Triassic of South Africa. ( 英 

文 ). Botha J; Chinsamy A. Palaeontology, 

2005, 48(2): 385-394 

The growth dynamics of the Early Triassic 

non-mammalian cynodont Thrinaxodon 

liorhinus were assessed through bone histology. 

Several limb bones of various sizes were 

examined, revealing a rapidly deposited, uninterrupted, 

fibro-lamellar bone tissue. A region 

of slowly deposited parallel-fibred bone occurs 

peripherally in most skeletal elements 

studied, becoming more extensively developed 

in the larger limb bones. On the basis of 

the bone histology, it is proposed that Thrinaxodon 

liorhinus grew rapidly during early 

ontogeny, and at a slower rate with increasing 

108

age, possibly once sexual maturity was 

reached. Variation in bone tissue patterns at 

different stages of ontogeny is noted and discussed. 

Given that growth rings are generally 

absent from the skeletal elements studied, and 

that the environment was seasonal, it appears 

that Thrinaxodon liorhinus growth was unaffected 

by environmental fluctuations. 

2007010377 

澳大利亚早三叠世一短吻的窝龙 : 已知最 

早的窝龙 = A short-snouted trematosauroid 

(Tetrapoda, Temnospondyli) from the Early 

Triassic of Australia: the oldest known trematosaurine. 

( 英文 ). Nield C M; Damiani R; 

Warren A. Alcheringa, 2006, 30(2): 263-271 

The trematosauroid temnospondyl Tirraturhinus 

smisseni gen. et sp. nov. from the 

Arcadia Formation of central Queensland, 

Australia, is described on the basis of its rostrum. 

This is the first trematosaurine (shortsnouted) 

trematosauroid from Australia, and is 

considered to be most closely related to Tertrema 

acuta from Spitzbergen. Tirraturhinus 

smisseni occurs alongside lonchorhynchine 

(long-snouted) trematosauroids in the Arcadia 

Formation; the co-occurrence of both trematosauroid 

morphotypes in that fauna is repeated 

in a number of non-marine Early Triassic faunas 

elsewhere in Pangaea. The Arcadia Formation 

is probably Griesbachian (earliest Triassic), 

so that T. smisseni is the oldest known 

trematosaurine. 

2007010378 

关于最早的恐龙的足迹 : 恐龙单系假说的 

意义 = On the tracks of the earliest dinosaurs: 

implications for the hypothesis of dinosaurian 

monophyly. ( 英文 ). Thulborn T. Alcheringa, 

2006, 30(2): 273-311 

From the record of dinosaurian skeletal 

remains it has been inferred that the origin and 

initial diversification of dinosaurs were rapid 

events, occupying an interval of about 5 million 

years in the Late Triassic. By contrast 

numerous reports of dinosauroid tracks imply 

that the emergence of dinosaurs was a more 

protracted affair extending through much of 

the Early and Middle Triassic. This study 

finds no convincing evidence of dinosaur 

tracks before the late Ladinian. Each of the 

three dinosaurian clades - Theropoda, Sauropodomorpha, 

Ornithischia - produced a unique 

track morphotype that appears to be an independent 

modification of the chirotherioid pattern 

attributed to stem-group archosaurs (thecodontian 

reptiles). The existence of three 

divergent track morphotypes is consistent with 

the concept of dinosaurian polyphyly but can 

be reconciled with the hypothesis of dinosaurian 

monophyly only by invoking many and 

rapid reversals in the locomotor anatomy of 

early dinosaurs. The origin of dinosaurs was 

not the correlate or consequence of any single 

event or process, be it global change, competitive 

replacement, or opportunism in the wake 

of mass extinction. Instead the origin of dinosaurs 

is envisaged as a series of three cladogenetic 

events over an interval of at least 10 million 

years and possibly as much as 25 million 

years. This scenario of dinosaurian polyphyly 

is as well-supported by fossil evidence as is 

the currently favoured view of dinosaurian 

monophyly. 

2007010379 

现生鳄类的起源 : 来自澳大利亚白垩纪的新 

证据 = The origin of modern crocodyliforms: 

new evidence from the Cretaceous of Australia. 

( 英文 ). Steven W. Salisbury S T; Molnar 

R E; Frey E; Willis P M A. Proceedings of the 

Royal Society B: Biological Sciences, 2006, 

273(1600): 2439 - 2448 

While the crocodyliform lineage extends 

back over 200 million years (Myr) to the Late 

Triassic, modern forms—members of Eusuchia—do 

not appear until the Cretaceous. 

Eusuchia includes the crown group Crocodylia, 

which comprises Crocodyloidea, Alligatoroidea 

and Gavialoidea. Fossils of noncrocodylian 

eusuchians are currently rare and, 

in most instances, fragmentary. Consequently, 

the transition from Neosuchia to Crocodylia 

has been one of the most poorly understood 

areas of crocodyliform evolution. Here we 

describe a new crocodyliform from the mid- 

Cretaceous (98–95Myr ago; Albian– 

Cenomanian) Winton Formation of Queensland, 

Australia, as the most primitive member 

of Eusuchia. The anatomical changes associated 

with the emergence of this taxon indicate 

a pivotal shift in the feeding and locomotor 

behaviour of crocodyliforms—a shift that may 

be linked to the subsequent rapid diversification 

of Eusuchia 20Myr later during the Late 

Cretaceous and Early Tertiary. While Laurasia 

(in particular North America) is the most 

likely ancestral area for Crocodylia, the biogeographic 

events associated with the origin 

of Eusuchia are more complex. Although the 

fossil evidence is limited, it now seems likely 

that at least part of the early history of Eusuchia 

transpired in Gondwana. 

109

2007010380 

威尔士南部下侏罗统楔齿类一新种 = A new 

species of the Sphenodontian Reptile 

Clevosaurus from the lower Jurassic of South 

Wales. ( 英文 ). Säilä L. Palaeontology, 2005, 

48(4): 817-831 

Small reptiles from the Early Jurassic 

Pant 4 fissure fill in Glamorgan, South Wales 

(St. Bride's Island, Pant Quarry), were formerly 

provisionally attributed to three species 

of sphenodontian lepidosaurs. A re-analysis, 

aided by new material, has found this herpetofauna 

to consist almost exclusively of a single 

new species, Clevosaurus convallis sp. nov., 

with only one specimen referable to Sphenodontia 

incertae sedis. Clevosaurus is known 

from the Upper Triassic and Lower Jurassic in 

various parts of the world, but C. convallis 

represents the first occurrence of the genus in 

the Jurassic of Britain. The material is fragmentary 

but includes numerous premaxillae, 

maxillae, dentaries and palatines, and the new 

species is distinguished by the unique combination 

of six large additional dentary teeth and 

a very short nasal process of the premaxilla, 

along with the diagnostic Clevosaurus features. 

2007010381 

中国中三叠统一基部 Mixosaurid 鱼龙 = A 

basal Mixosaurid Ichthyosaur from the middle 

Triassic of China. ( 英文 ). Jiang DaYong; Hao 

WeiChen; Maisch M W; Matzke A T; Sun 

YuanLin. Palaeontology, 2005, 48(4): 869- 

882 

New specimens of a mixosaurid ichthyosaur 

are described from the People's Republic 

of China. They consist of an almost complete 

skull, forefin and shoulder girdle of a single 

individual, and a second partial skull from the 

Anisian Guanling Formation of Guizhou Province 

that belongs to the same taxon. A phylogenetic 

analysis shows this species to be the 

sister-taxon of all other mixosaurids. It is distinguished 

from Mixosaurus, Contecotpalatus 

and Phalarodon by features of its dentition 

and cranial morphology. There is only one 

maxillary tooth row. The posterior maxillary 

teeth are blunt and rounded, and much wider 

than the premaxillary teeth, but they are not 

strongly elongated anteroposteriorly. The teeth 

are subthecodontously implanted. The postorbital 

skull segment is long. The jugalquadratojugal 

notch is deep and these two 

elements remain separated externally. The 

postorbital separates supratemporal and postfrontal. 

There are no postaxial ossifications of 

the forefin. Autapomorphies include a long 

ventral process of the postorbital lamina of the 

postorbital as well as characteristic morphologies 

of the coracoid and humerus. The material 

is therefore clearly distinguished from 

other known mixosaurids. It can be referred, 

on the basis of the features of the humerus and 

coracoid, to Mixosaurus maotaiensis Young, 

1965. As it is generically distinct from 

Mixosaurus, a new generic name, Barracudasaurus 

gen. nov. is proposed. The phylogenetic 

relevance of the external separation of 

jugal and quadratojugal in some Triassic ichthyosaurs 

is discussed and it is concluded that 

it does not demonstrate the initial presence of 

a lower temporal fenestra in ichthyosaurs. The 

new material suggests that mixosaurids could 

have also originated in the Eastern rather than 

the Western Tethys, as previously assumed. 

2007010382 

摩洛哥晚白垩世土仑期一个新的沧龙类化 

石 = A new mosasauroid (Squamata) from the 

Late Cretaceous (Turonian) of Morocco. ( 英 

文 ). Bardet N; Suberbiola X P; Jalil N E. 


Tethysaurus nopcsai gen. et sp. nov. is 

described on the basis of both cranial and 

postcranial material from the Late Cretaceous 

(Early Turonian) of the Goulmima region, 

southern Morocco. This new mosasauroid is 

mainly characterized by a parietal table ending 

posteriorly in two pointed pegs; jugal with a 

large ascending ramus; splenial with a large 

and notched dorsomedial process; surangular 

exposed medially ventral to the coronoid; 

large paracotylar and parazygosphenal foramina 

on vertebrae. A phylogenetic analysis 

shows that Tethysaurus is the sister-group of 

Mosasauridae. It fills the gap between the aigialosaurids 

(mainly Cenomanian) and the mosasaurids 

(known from the Middle-Late Turonian 

to the Latest Maastrichtian). (C) 2003 

Academie des sciences. Published by Elsevier 

SAS. All rights reserved. 

2007010383 

法国奥德 Saint-Papoul 地区下始新统两个 

新的龟鳖类化石 = Two new turtles from the 

Lower Eocene of Saint-Papoul (Aude, 

France).. ( 法文 ). Hervet S. Comptes Rendus 

Palevol, 2003, 2(8): 617-624 

Two new turtles from the Lower Eocene 

of Saint-Papoul (Aude, France). Among the 

fossil turtles from of the Lower Eocene of 

Saint-Papoul (Aude, France), two new taxa of 

freshwater Testudinoidea are described. The 

110

first is a new species of the genus Palaeoemys, 

known before in the Lutetian of Germany. The 

second taxon is a new genus, also described 

on material of Pepieux-Cesseras and Eygalayes. 

(C) 2003 Academie des sciences. 

Publie par Elsevier SAS. Tous droits reserves. 

2007010384 

日本下白垩统一长身蜥蜴 = A long-bodied 

Lizard from the Lower Cretaceous of Japan. 

( 英文 ). Evans S E; Manabe M; Noro M; Isaji 

S; Yamaguchi M. Palaeontology, 2006, 49(6): 

1143-1165 

Platynotan lizards underwent a dramatic 

Late Cretaceous radiation into marine habitats. 

Beginning with small-bodied forms, the lineage 

culminated with the mosasaurs, large 

predatory lizards with a world-wide distribution 

in the Santonian–Campanian. Moreover, 

the marine squamate radiations of the Cenomanian–Turonian 

are remarkable in having 

produced a range of long-bodied, reducedlimbed 

swimmers (dolichosaurs, adriosaurs, 

coniasaurs and limbed snakes) that seem to 

have thrived in the shallow coastal environments 

of the Western Tethys region. Until 

now, none of these long-bodied aquatic squamates 

has been recorded prior to the Cenomanian, 

none has been recovered from a nonmarine 

locality and none is known from Asia. 

Here we describe a small, gracile, long-bodied 

mosasauroid lizard from a swampy continental 

deposit in the Lower Cretaceous of Japan. 

2007010385 

Archegosaurus Decheni 颅后骨及离片椎类 

颅后骨的系统分析 = The Postcranium of 

Archegosaurus Decheni, and a Phylogenetic 

analysis of Temnospondyl Postcrania. ( 英文 ). 

Witzmann F; Schoch R R. Palaeontology, 

2006, 49(6): 1211-1235 

The gharial-like Archegosaurus decheni 

from the Permian/Carboniferous boundary of 

south-west Germany is one of the best known 

temnospondyls. Based largely on new material, 

we restudied the postcranial anatomy of this 

species, including ontogenetic aspects. 

A. decheni has 24 presacral vertebrae, and the 

length of the deep tail exceeds the length of 

the rest of the body. Neural spines are moderately 

high and slowly become differentiated 

during ontogeny. The intercentra start to ossify 

very late. Distal uncinate processes are 

developed on the anterior ribs in adult specimens. 

Only the ventral portion of the scapula 

is ossified. The slender ilium and the ischium 

are not co-ossified, and the pubis remained 

cartilaginous. Among stereospondylomorph 

temnospondyls, the very short and rudimentarily 

developed humerus exhibits a unique morphology. 

Carpals and tarsals start to ossify 

only in the largest specimens. The poorly ossified 

postcranium indicates that A. decheni was 

primarily an aquatic temnospondyl. We undertook 

a phylogenetic study of A. decheni and 

16 other temnospondyls, based exclusively on 

postcranial characters. We analysed 52 characters, 

obtaining a single most parsimonious 

tree that agrees in many aspects with craniumbased 

analyses: Trimerorhachis and Dvinosaurus 

form a basal clade (Dvinosauria), followed 

by monophyletic euskelians (dissorophoids 

plus eryopids) and finally the stereospondylomorphs, 

within which A. decheni is 

nested above Sclerocephalus. Among stereospondyls, 

trematosaurids and metoposaurids 

form a clade, whereas the chigutisaurid 

Siderops is nested with capitosauroids. The 

primitive condition of Temnospondyli is still 

not adequately understood, especially the degree 

of terrestriality of the earliest temnospondyls. 

2007010386 

非洲尼罗湾鳄 Crocodylus niloticus 种级辐 

散的分子证据 = Molecular evidence for species 

level divergence in African Nile Crocodiles 

Crocodylus niloticus (Laurenti, 1786). 

( 英文 ). Schmitz A; Mansfeld P; Hekkala E; 

Shine T; Nickel H; Amato G; Bohme W. 


Relationships of the newly discovered 

dwarf crocodiles from Mauritania were inferred 

from mitochondrial 12S sequences. 

Specimens from 13 different Crocodylus 

niloticus populations (from East Africa, West 

Africa and Madagascar) were compared. Additional 

representatives of the genus Crocodylus 

(one from Africa and one from Australia), 

the African genus Osteolaemus and the South 

American alligatorid Paleosuchus palpebrosus 

(as outgroup) were included in the analysis. 

Maximum-likelihood and Bayesian analyses 

yielded relationships that were strikingly different 

from currently prevailing phylogenetic 

hypotheses. Both analyses consistently revealed 

two groups, one consisting of the monophyletic 

West- and Central African populations 

and the other of a paraphyletic group 

containing the East African and Madagascan 

populations. High genetic divergence between 

those groups indicates separation on the species 

level. Furthermore 'C' cataphractus is 

clearly shown not to be a member of the genus 

111

Crocodylus. The resulting nomenclatural 

changes are discussed 

2007010387 

巴西南部西圣保罗上白垩统 Bauru 群一新 

泰坦龙 = A new Titanosaur from western São 

Paulo state, Upper Cretaceous Bauru group, 

South-east Brazil. ( 英文 ). Santucci R M; Bertini 

R J. Palaeontology, 2006, 49(1): 59-66 

Material from a new titanosaur from the 

Bauru Basin (Bauru Group), Brazil is described 

and compared with well-known titanosaurs. 

Adamantisaurus mezzalirai gen. et sp. 

nov. is based on six articulated anterior caudal 

vertebrae and two haemapophyses collected 

from the Adamantina Formation, which is 

considered to be Campanian–Maastrichtian 

in age. Adamantisaurus mezzalirai is characterized 

by the following combination of characteristics: 

anterior caudal vertebrae with 

straight or slightly backwardly-projecting neural 

spines with strongly expanded distal ends, 

stout prespinal lamina, very wide pre- and 

postzygapophyseal articular facets, and concave 

postzygapophyseal articular facets on 

anterior caudal vertebrae. Although our cladistic 

analysis has produced equivocal results, 

Adamantisaurus mezzalirai shares with DGM 

'Series B' (Peirópolis titanosaur) and 

Aeolosaurus the presence of postzygapophyses 

with concave articular facets, and shares 

with DGM 'Series B' the presence of laterally 

expanded neural spines and stout prespinal 

lamina. Additionally, A. mezzalirai shares 

with DGM 'Series' C (other titanosaur from 

Peirópolis) the presence of short neural spines. 

2007010388 

阿根廷中新统一新的 Snake Mackerel = A 

New Snake Mackerel from the Miocene of 

Algeria. ( 英文 ). Carnevale G. Palaeontology, 

2006, 49(2): 391-403 

A new genus and species of gempylid is 

described from the Late Miocene (Messinian) 

diatomite deposits of the Chelif Basin, northeast 

Algeria. Although its skeleton is incomplete, 

Chelifichthys goujeti gen. et sp. nov. 

possesses a unique combination of features 

that justifies its recognition as a new genus. 

Chelifichthys goujeti is characterized by remarkably 

elongate and serrated dorsal-fin 

spines, the absence of external pelvic-fin elements, 

and sculptured frontals and opercular 

bones. Chelifichthys appears to be closely related 

to the living genera Nealotus, Prometichthys, 

Rexea and Rexichthys. Chelifichthys goujeti 

represents the third record of the family 

Gempylidae in the Neogene of the Mediterranean. 

2007010389 

巴西 Rio Grande Do Sul 上三叠统 

Clevosaurus 一新种 = A new species of 

Clevosaurus (Lepidosauria: Rhynchocephalia) 

from the upper Triassic of Rio Grande Do Sul, 

Brazil. ( 英文 ). Bonaparte J F; Sues H. Palaeontology, 

2006, 49(4): 917-923 

Well-preserved cranial remains of a small 

sphenodontian lepidosaur from the Upper Triassic 

Caturrita Formation of Rio Grande do 

Sul, Brazil, are the first record of the genus 

Clevosaurus Swinton, 1939 from South America. 

They represent a new species, Clevosaurus 

brasiliensis, which is distinguished by a 

very short antorbital region of the skull (corresponding 

to about 20 per cent of skull length) 

and the presence of teeth in addition to two 

longitudinal rows on the pterygoid. 

C. brasiliensis most closely resembles 

C. bairdi from the Lower Jurassic of Nova 

Scotia (Canada) and C. mcgilli from the 

Lower Jurassic of Yunnan (China). The discovery 

of Clevosaurus in the Upper Triassic 

of southern Brazil provides a significant range 

extension of this widely distributed sphenodontian 

genus. Along with other recent finds, 

it also suggests that there may have been less 

biotic provincialism among terrestrial vertebrates 

during the Late Triassic than has previously 

been assumed. 

2007010390 

兽脚类 Ornitholestes Hermanni 的前肢功 

能 = Forelimb function in Ornitholestes Hermanni 

Osborn (Dinosauria, Theropoda). ( 英 

文 ). Senter P. Palaeontology, 2006, 49(5): 

1019-1027 

Ornitholestes hermanni is a Late Jurassic 

theropod dinosaur from North America. This 

kinematic study of Ornitholestes uses manual 

manipulations of forelimb casts to determine 

range of motion. The manual phalanges of the 

O. hermanni holotype, previously unidentified, 

are here identified as phalanges I-1, I-2 (ungual), 

II-2 and II-3 (ungual). At all represented 

manual joints, hyperextensibility is small or 

absent, whereas flexion is strong, as in most 

other theropods. The elbow can be strongly 

flexed beyond a right angle. When data on 

range of forelimb motion in Ornitholestes are 

added to such data from other theropods, high 

elbow flexion is present in maniraptoriform 

coelurosaurs but not in basal theropods. Fore- 

112

limb functions requiring strong elbow flexion 

(such as holding objects to the chest, or tucking 

the forearms in for their protection or to 

reduce wind resistance or heat loss) were 

therefore available to maniraptoriform coelurosaurs 

but not to basal theropods. 

2007010391 

瑞士阿尔卑斯 - 喀尔巴阡北上三叠统一新基 

部翼龙属 = A new basal pterosaur genus 

from the upper Triassic of the Northern Calcareous 

Alps of Switzerland. ( 英文 ). Fröbisch 

N B; Fröbisch J. Palaeontology, 2006, 49(5): 

1081-1090 

A lower jaw with multicusped teeth and a 

number of unique characteristics was discovered 

in an extensive exposure of the Upper 

Triassic Kössen Formation in the Northern 

Calcareous Alps. The ramus of the jaw is high 

and dominated by a row of large, oval foramina 

that lies parallel to the tooth row. In addition, 

the anterior portion of the dentary exhibits 

a large number of nutritive foramina and 

small pits, which might indicate an association 

with a soft tissue structure and/or the presence 

of a keratinous cover of that area during life. 

All elements of the jaw are thin-walled and 

hollow, possibly pneumatic. Two teeth are 

preserved within the dentary. One is tricuspid 

and the other bears four cuSPS. The teeth are 

noticeably small in comparison with the overall 

size of the ramus, being only one-third of 

the height of the ramus. The teeth show a 

strong similarity to those of the well-known 

basal pterosaur genus Eudimorphodon, whose 

jaw morphology, however, clearly differs 

from the specimen described in this study. The 

dentition and the pneumatic bone structure 

make an assignment to the Pterosauria plausible. 

Based on the great number of distinct 

morphological characters the specimen is described 

as Caviramus schesaplanensis gen. et 

sp. nov. 

2007010392 

日本中部下白垩统手取群 (Tetori Formation) 

桑岛组 (Kuwajima Formation) 的 

海龟蛋壳化石 = Chelonian eggshells from 

the lower Cretaceous Kuwajima Formation of 

the Tetori Group, Central Japan. ( 英文 ). Isaji 

S; Matsushita A; Hirayama R. Paleontological 

Research, 2006, 10(1): 29-36 

Chelonian eggshell fossils from the 

Lower Cretaceous Kuwajima Formation of the 

Tetori Group are described. The eggs were 

originally spherical or ellipsoidal in shape. 

The eggshells consist of a single layer of 

spherulitic shell units composed of needle-like 

crystallites originating from a nucleation center. 

This corresponds to modern rigid-shelled 

chelonian eggs. The eggshell fragments are 

commonly found buried together and are 

known from deposits of subaerial environments, 

such as vegetated swamps. In contrast, 

the vast majority of turtle remains are known 

primarily from nearby shallow lake deposits, 

indicating that they are aquatic; no terrestrial 

turtles are known from this formation. These 

taphonomic settings suggest that the eggs 

were laid on land by lacustrine turtles in a 

process still apparent today. 

2007010393 

摩洛哥晚白垩世土仑期一新的 polycotylid 

类 = A new polycotylid plesiosaur from the 

Late Cretaceous (Turonian) of Morocco. ( 英 

文 ). Bardet N; Suberbiola X P; Jalil N E. 


A new Polycotylidae (Plesiosauria) from 

the Late Cretaceous (Turonian) of southern 

Morocco is described. Thililua longicollis gen. 

et sp. nov. is based on a complete cranium and 

37 associated vertebrae. It differs from other 

polycotylids in several cranial and especially 

vertebral characters, such as the occurrence of 

30 cervical vertebrae, whose centra are nearly 

as long as high and bear laterally longitudinal 

ridges. Thililua is the first polycotylid hitherto 

found in Africa and under subtropical palaeolatitudes 

2007010394 

Sharovipteryx mirabilis 的飞行 : 世界上第 

一架三角翼滑翔机 = Flight of Sharovipteryx 

mirabilis: the world's first delta-winged glider. 

( 英文 ). Dyke G J; Nudds R L; Rayner J M V. 


1040-1043 

The 225 million-year-old reptile 

Sharovipteryx mirabilis was the world's first 

delta-winged glider; this remarkable animal 

had a flight surface composed entirely of a 

hind-limb membrane. We use standard deltawing 

aerodynamics to reconstruct the flight of 

S. mirabilis demonstrating that wing shape 

could have been controlled simply by protraction 

of the femora at the knees, and by variation 

in incidence of a small forelimb canard. 

Our method has allowed us to address the 

question of how identifying realistic glide performance 

can be used to set limits on aerodynamic 

design in this small animal. Our novel 

113

interpretation of the bizarre flight mode of S. 

mirabilis is the first based directly on interpretation 

of the fossil itself and the first grounded 

in aerodynamics 

2007010395 

兽孔目似哺乳类爬行动物的起源及早期辐 

射 : 一个古生物假说 = The origin and early 

radiation of the therapsid mammal-like reptiles: 

a palaeobiological hypothesis. ( 英文 ). 

Kemp T S. Journal of Evolutionary Biology, 

2006, 19(4): 1231-1247 

The replacement of the basal synapsid 

pelycosaurs by the more 'mammal-like' 

therapsids in the Permian was an important 

event in the history of tetrapods because it 

initiated the eventual transition to the mammals. 

It is also an example of taxon replacement 

in the fossil record that is unusually 

amenable to explanation, based on a combination 

of analysis of the biological significance 

of the inferred character changes, with the 

stratigraphic, palaeogeographic and palaeoecological 

circumstances of the time. An 

hypothesis is presented in which the origin of 

the therapsids resulted from a correlated progression 

of character evolution leading to 

higher levels of metabolic activity and homeostatic 

regulation of the body. It was a response 

to the availability of a seasonally arid, savanna-like 

biome. The subsequent explosive 

radiation of therapsids was associated with 

habitat expansion made possible by the Mid- 

Permian development of geographical continuity 

between that biome and the temperate 

biomes. The final extinction of the pelycosaurs 

was a case of incumbent replacement by 

the new therapsid lineages. 

2007010396 

翼龙的肢骨分异和翼部形状 = Limb disparity 

and wing shape in pterosaurs. ( 英文 ). Dyke 

G J; Nudds R L; Rayner J M V. Journal of 

Evolutionary Biology, 2006, 19(4): 1339-1342 

The limb proportions of the extinct flying 

pterosaurs were clearly distinct from their living 

counterparts, birds and bats. Within pterosaurs, 

however, we show that further differences 

in limb proportions exist between the 

two main groups: the clade of short-tailed 

Pterodactyloidea and the paraphyletic clades 

of long-tailed rhamphorhynchoids. The 

hindlimb to forelimb ratios of rhamphorhynchoid 

pterosaurs are similar to that seen in 

bats, whereas those of pterodactyloids are 

much higher. Such a clear difference in limb 

ratios indicates that the extent of the wing 

membrane in rhamphorhynchoids and pterodactyloids 

may also have differed; this is 

borne out by simple ternary analyses. Further, 

analyses also indicate that the limbs of Sordes 

pilosus, a well-preserved small taxon used as 

key evidence for inferring the extent and 

shape of the wing membrane in all pterosaurs, 

are not typical even of its closest relatives, 

other rhamphorhynchoids. Thus, a bat-like 

extensive hindlimb flight membrane, integrated 

with the feet and tail may be applicable 

only to a small subset of pterosaur diversity. 

The range of flight morphologies seen in these 

extinct reptiles may prove much broader than 

previously thought. 

2007010397 

比利时南部晚三叠世恐龙牙齿 = Late triassic 

dinosaur teeth from southern Belgium. ( 英 

文 ). Godefroit P; Knoll F. Comptes Rendus 

Palevol, 2003, 2(1): 3-11 

Isolated Dinosaur teeth have been discovered 

in the Upper Triassic locality of Habay-la-Vieille, 

in southern Belgium. Ornithischia 

are represented by three dental morphotypes; 

two of them closely resemble isolated 

teeth from the Middle or Upper Jurassic of 

Portugal and England. The presence of sauropods 

in the Upper Triassic of Europe is confirmed. 

Sauropods already had a wide geographical 

distribution during the Latest Triassic, 

as fossils have been discovered in South 

Africa, Thailand and western Europe. At Habay-la-Vieille, 

sauropods and prosauropods 

co-existed at the end of the Triassic. Two dental 

morphotypes may tentatively be referred to 

as theropod dinosaurs. The study of isolated 

teeth indicates that dinosaurs were already 

well diversified in the Latest Triassic of western 

Europe 

2007010398 

丹麦新的恐龙化石 = New dinosaurs from 

Denmark. ( 英文 ). Bonde N; Christiansen P. 


Only the Baltic island of Bornholm is 

likely ever to produce Danish dinosaurs, not 

the western mainland Denmark. The Mesozoic 

of Bornholm spans Late Triassic to Late Cretaceous, 

with some potentially dinosaur producing 

deposits from Early Jurassic to Early 

Cretaceous being continental, lagoon, littoral 

or marginal marine. So far the only dinosaurs 

have been found in 2000 and 2002 in the basal 

Jydegaard Fm., carrying a 'Purbeck-Wealden 

fauna' of the Earliest Cretaceous (Late Berriasian 

or Ryazanian) at Robbedale. Both are 

114

single tooth crowns; the first find, a 21-mm 

crown, is a dromaeosaurine, Dromaeosauroides 

bornholmensis Christiansen & Bonde 

2003, possibly the only true dromaeosaur from 

the Lower Cretaceous of Europe. Estimated 

length of the animal is over 3 m. The second 

find is a somewhat unusual sauropod, most 

likely titanosaurian, the crown being only ca 

15 mm high, with an unusual wear facet. Both 

teeth were derived from the lowermost 2-3 

metres of the formation. Future expectations 

from this deposit are small ornithopods - and 

possibly mammals 

2007010399 

法国的恐龙 = Dinosaurs of France. ( 法文 ). 

Allain R; Suberbiola X P. Comptes Rendus 

Palevol, 2003, 2(1): 27-44 

The French dinosaur record is one of the 

most extensive in Europe; it ranges stratigraphically 

from the Late Triassic to the Latest 

Cretaceous. All major clades of dinosaurs 

but marginocephalians are known. About 20 

species are based on significant material; the 

theropods are the best represented. Most of 

these taxa have been described or revised in 

recent years. Important specimens have been 

discovered in the Late Triassic of eastern 

France, the Middle Jurassic of Normandy, and 

the Late Cretaceous of Provence and Languedoc. 

The ichnological record is good for the 

Late Triassic-Early Jurassic, and the Late Cretaceous 

egg sites are among the richest in the 

world. 

2007010400 

意大利的恐龙 = Dinosaurs of Italy. ( 法文 ). 

Dal Sasso C. Comptes Rendus Palevol, 2003, 

2(1): 45-66 

In recent years, the idea that Italy was 

lacking dinosaurs has been denied by a striking 

series of finds. Several Triassic and Jurassic 

dinosaur tracksites were discovered in the 

mid-eastern Alps, in particular within the 

Dolomia Principale Fm. (Norian) and the Calcari 

Grigi Fm. (Hettangian to Pliensbachian), 

while thousands of Cretaceous (Santonian) 

prints came to light in Puglia (southern Italy). 

Three skeletal remains are known so far; they 

all belong to new, possibly endemic species 

that evolved during Sinemurian (Saltrio theropod), 

Albian (Scipionyx) and Santionian (Trieste 

hadrosaurs) times. Both footprints and 

bony remains come from coastal deposits and 

indicate a peculiar palaeobiogeographic condition. 

The model of Bahamas-like small islands 

is no longer consistent with the presence of 

large dinosaurs, which could only survive in 

definitely terrestrial ecosystems. As documented 

by the wide temporal range of the dinosaur-bearing 

Italian outcrops, the Mesozoic 

carbonate platforms of the Middle-Eastern 

Tethys might have emerged several times, and 

quite extensively. 

2007010401 

荷兰东南部、比利时东北部马斯特里赫特 

阶标准地点的恐龙 = Dinosaurs from the 

Maastrichtian-type area (southeastern Netherlands, 

northeastern Belgium). ( 英文 ). Jagt J W 

M; Mulder E W A; Schulp A S; Dortangs R 

W; Fraaije R H B. Comptes Rendus 

Palevol, 2003, 2(1): 67-76 

In comparison to pre-1980 records of 

nonavian dinosaur remains from the Maastrichtian 

type strata, material collected during 

the past 20 years is both fairly common and 

diverse, consisting mostly of isolated cranial 

and post-cranial remains of hadrosaurids. 

With the exception of the type specimen of 

Megalosaurus bredai Seeley, a fragmentary 

right femur, no theropod material is represented 

in collections screened by us. In the 

present contribution, specimens recognised in 

various collections subsequent to our last 

tabulation (1999) are illustrated and briefly 

discussed. Although we are fully aware that 

the material is too limited to draw meaningful 

conclusions from, the specimens are here tiedin 

with a preliminary sequence-stratigraphic 

interpretation of the type Maastrichtian, which 

is currently being refined by strontium-isotope 

studies of coleoid cephalopods. 

2007010402 

葡萄牙的恐龙 = Dinosaurs of Portugal. ( 英 

文 ). Antunes M T; Mateus O. Comptes Rendus 

Palevol, 2003, 2(1): 77-95 

A synthesis on the state of art on dinosaur 

knowledge in Portugal is presented The 

following genera have been recognized: Ceratosaurus, 

Torvosaurus, Lourinhanosaurus, 

Allosaurus, cf. Compsognathus, Stokesosaurus, 

cf. Richardoestesia, cf. Archaeopteryx, 

Euronychodon, cf. Paronychodon, Dinheirosaurus, 

Lourinhasaurus, Lusotitan, cf. Pleurocoelus, 

Lusitanosaurus, Dacentrurus, Dracopelta, 

Phyllodon, Hypsilophodon, Alocodon, 

Trimucrodon, Draconyx, Iguanodon, and 

Taveirosaurus. Most are from Late Jurassic 

localities at the Lourinh (a) over tilde area and 

Guimarota. A new genus, Lusotitan, is here 

raised to include the Late Jurassic 'Brachiosaurus' 

atalaiensis. Lower Cretaceous until 

115

Cenomanian material is scarce, except for dinosaur 

footprints. An interesting Late- 

Cretaceous, mostly small dinosaur association 

has been collected between Aveiro and 

Taveiro. 

2007010403 

罗马尼亚的恐龙 = Dinosaurs of Romania. 

( 英文 ). Grigorescu D. Comptes Rendus 

Palevol, 2003, 2(1): 97-101 

The dinosaurs of Romania are exclusively 

Cretaceous. Lowermost Cretaceous 

dinosaurs come from a bauxite mine in the 

Bihor county (northwest Romania) that has 

yielded thousands of disarticulated bones. Uppermost 

Cretaceous dinosaurs have been 

known from the Haleg Basin (south Transylvania) 

since the end of the 19th century, 

mostly as bone concentrations ('fossiliferous 

pockets'); more recently, nests with dinosaur 

eggs, including hatchlings, have been found in 

Haleg. Although separated by a ca 60 Myr gap, 

the two dinosaur faunas from Romania share 

some common features: predominance of ornithopods, 

absence of large theropods (substituted 

in the case of the Maastrichtian Hateg 

assemblage by several small theropods), and, 

in general, the small size of the individuals 

(dwarfism). These aspects seem to be explained 

by the isolated island habitat of both 

assemblages. 

2007010404 

瑞士的恐龙 = Dinosaurs of Switzerland. ( 英 

文 ). Meyer C A; Thuring B. Comptes Rendus 

Palevol, 2003, 2(1): 103-117 

Until 1960, the record of dinosaurs was 

rather poor in Switzerland. Between 1960 and 

1980, several new localities with plateosaurid 

remains as well as prosauropod and theropod 

tracks were found in Late Triassic sabkha and 

floodplain environments. The discovery of 

large surfaces with sauropod tracks in the Late 

Jurassic of the Jura Mountains in 1987 triggered 

a stream of new data. More than 20 new 

localities with tracks from both sauropod and 

theropod dinosaurs in different stratigraphic 

levels have been found since then. The latest 

discoveries include trackways of iguanodontids 

from the Early Cretaceous of the central 

Swiss Alps and a large Late Jurassic surface 

with trackways of small sauropods in the 

northernmost part of the Jura Mountains. The 

best skeletal record comes from the Late Triassic, 

with scattered data from the Late Jurassic. 

The track and trackway record appears to 

be best in the Late Jurassic 

鸟类 

2007010405 

辽西早白垩世九佛堂组一新的初鸟类 = A 

new avian taxon from Lower Cretaceous Jiufotang 

Formation of western Liaoning. ( 中文 ). 

高春玲刘金远 . 世界地质 , 2005, 24(4): 313- 

318 2 图版 . 

描述了产于辽宁朝阳盆地联合乡回家 

子南山早白垩世九佛堂组一新的初鸟类化 

石。因其头骨下颌近前部具有一嵴状突 ; 

前肢短于后肢 , 前后肢长度比率为 0,82; 

掌骨未愈合 ; 后足纤细 , 第一趾反转 , 与 

其他三趾对握 ; 尾椎少于 23 节等特征 , 区 

别于其他任何已知的初鸟类 , 故命名为一 

新属、新种一粗颌大连乌 (Dalianraptor 

cuhe gen.et sp. nov)。 

2007010406 

塞尔维亚 Valjevo 盆地早中新世湖相沉积 

中 grebe 的一新属种 = A new genus and 

new species of grebe (Podicipediformes, Aves) 

from the Early Miocene lake deposits of Valjevo 

Basin (Serbia). ( 英文 ). Dimitrijevich V; 

Gal E; Kessler E. Fragmenta Palaeontologica 

Hungarica, 2002, (20): 3-7 

Miodytes serbicus, a new genus and species 

of grebe is introduced. The fossil bird bones of 

an almost complete wing skeleton are found in 

anatomical connection in a thin layer slate. 

The representatives of Podicipedidae are rare 

in Central European deposits of any age, and 

indicate the vicinity of a seacoast environment, 

i. e. Paratethys Sea. Among rare bird remains 

in the Neogene of Serbia, the fing from Valjevo 

Basin is the very first to enable species 

identification. 

2007010407 

辽宁鸟和恐龙的羽毛和 ' 似羽毛 ’ 覆盖物构造 

= Feathers and 'feather-like' integumentary 

structures in Liaoning birds and dinosaurs. ( 英 

文 ). Zhang Fucheng; Zhou Zhonghe; Dyke G. 

Geological Journal, 2006, 41(3/4): 395-404 

We provide an overview of the known 

feather and other 'feather-like' integumentary 

structure types known to-date in the birds and 

dinosaurs from the Cretaceous rocks of Liaoning, 

NE China. These feather-types are classified 

and compared with similar structures seen 

in Mesozoic and extant birds. We consider 

that integumentary feathers and 'feather-like' 

structures fall within two major structural 

categories ('shafted' and 'non-shafted'). Comments 

are also made on the possible aerody- 

116

namic or insulating function of leg and tail 

feathers in Mesozoic birds and theropods. 

哺乳类 

2007010408 

鸟类是插上翅膀的恐龙吗 = Did dinosaurs 

take wing. ( 中文 ). 钱迈平 . 江苏地质 , 2004, 

28(2): 82-89 

近年 , 越来越多的化石证据表明 : 过去 

长期被认为只有鸟类才有的 , 并作为鸟类区 

别于其他脊椎动物的一些重要特征 , 如羽 

毛、叉骨、胸骨、尾综骨、前肢可折叠于 

体侧、眼眶与下颞孔相连的头骨及耻骨向 

侧后伸展的骨盆等 , 却也在 1 亿多年前的不 

少小型兽足类恐龙身上或多或少地存在。 

于是 , 越来越多的人们相信鸟类是从小型兽 

足类恐龙起源。但迄今发现的所有具鸟类 

特征的恐龙 , 在时间上却晚于或至多也只是 

接近目前公认的最早鸟类 - 晚侏罗世的始祖 

鸟 , 而原始鸟类双弓型头骨似乎在暗示 : 鸟 

类可能起源于比恐龙更古老的初龙类。这 

些都对鸟类起源于恐龙的假说提出了质 

疑。就目前的化石记录而言 , 鸟类和兽足类 

恐龙系统演化关系密切是毋庸质疑的。但 

由于至今未找到在时间上足以演化出鸟类 

的更古老近裔恐龙 , 因此还不能说恐龙就是 

鸟类的祖先。它们可能只是与原始鸟类平 

行独立发展的姊妹群 , 二者也许出自一个共 

同祖先。 

2007010409 

意大利南部 Pirro Nord 地区早更新世 Hystrix 

refossa = Hystrix refossa Gervais, 1852 

from Pirro Nord (early Pleistocene, southern 

Italy).. ( 英文 ). Rook L; Sardella R. Revista 

Espanola de paleontologia, 2005, 111(3): 

489-496 

We describe fossil remains attributable to 

genus Hystrix, collected from fissure filings in 

the area between Apricena and Poggio Imperiale 

(Apulia, Italy). The vertebrate assemblage 

that yielded these Hystrix remains is 

known in the literature as Pirro Nord, and is 

one of the richest Early Pleistocene mammal 

assemblages from Italy. The porcupine remains 

from Pirro Nord are attributed to the 

species Hystrix refossa. The problem of the 

taxonomy of Plio-Pleistocene hystricids in the 

framework of their morphological variability 

is discussed. 

2007010410 

对 Glyptodon munizi 的重新描述和解剖 = 

Glyptodon munizi Ameghino (Mammalia, 

Cingulata, Gyptodontidae): Redescription and 

anatomy. ( 其他 ). Soibelzon E; Zurita A E; 

Carlini A A. Ameghiniana, 2006, 43(2): 377- 

384 

New records of Glyptodon munizi 

Ameghino (a taxon up to now only known by 

partial remains of the dorsal carapace) are reported. 

In this sense, these new findings allow 

us to sustain the validity of this species and to 

give a more precise and comprehensive diagnosis 

and description. The main differences 

with the Lujanian species of the genus Glyptodon 

are: a) a bigger size; b) an elongated 

skull with a remarkably narrowing between 

the postorbital process of yugal and the supraoccipital 

crest, c) first molariform with a 

primitive shape, without a marked lobulation. 

In addition, a ventral plastron and a high number 

of facial osteodermes, are described for 

the first time. This taxon is limited to the Ensenadan 

Stage (Late Pliocene-Middle Pleistocene), 

while from a palaeozoogeographic 

point of view, all the reports are restricted to 

the Buenos Aires Province. 

2007010411 

阿根廷 Pampean 地区更新世马的摄食、生 

态和绝灭 = Ancient feeding, ecology and 

extinction of Pleistocene horses from the 

Pampean Region, Argentina. ( 其他 ). Sanchez 

B; Prado J L; Alberdi M T. 

Ameghiniana, 2006, 43(2): 427-436 

To reconstruct the diet and habitat preference 

of fossil horses, we measured the carbon 

and oxygen isotope composition of 35 

bone and tooth samples of Equus (Amerhippus) 

neogeus Lund, Hippidion principale (Lund), 

and Hippidion devillei (Gervais) from 10 different 

Pleistocene localities in the Pampean 

region (Argentina). To compare the three species 

by stratigraphic age, we divided the samples 

into three groups: lower Pleistocene, 

middle-late Pleistocene and latest Pleistocene. 

Samples of Hippidion devillei from the lower 

Pleistocene were more homogeneous, with 

delta C-13 values ranging between -11.73 to - 

9.79 parts per thousand. These data indicate a 

diet exclusively dominated by C-3 plants. In 

contrast, Hippidion principale and Equus 

(Amerhippus) neogeus from middle-late Pleistocene 

showed a wide range of feeding adaptations 

(with a range of delta C-13 values between 

-12.05 to -8.08 parts per thousand in 

Hippidion and delta C-13 values between - 

11.46 to -7.21 parts per thousand in Equus 

(Amerhippus)). These data seem to indicate a 

mixed C-3-C-4 diet, while data from the latest 

117

Pleistocene suggest a tendency toward an exclusively 

C-3 diet for both species. Furthermore, 

the results of delta O-18 indicate an 

increase of approximately 4 degrees C from 

the early to latest Pleistocene in this area. Several 

nutritional hypotheses explaining latest 

Pleistocene extinctions are based on the assumption 

that extinct taxa had specialized diets. 

The resource partitioning preference of 

these species from latest Pleistocene in the 

Pampean region supports these hypotheses. 

2007010412 

阿根廷巴塔哥尼亚早古新世 Salamanca 组 

单孔类的股骨 = Femur of a monotreme 

(Mammalia, Monotremata) from the Early 

Paleocene Salamanca Formation of Patagonia, 

Argentina. ( 英文 ). Forasiepi A M; Martinelli 

A G. Ameghiniana, 2003, 40(4): 625-630 

2007010413 

新大陆热带箭猪的生物地理 : 通过泛生物 

地理方法综合现代和化石资料 = Biogeography 

of neotropical porcupines (Rodentia, 

Hystricognathi): Integrating recent and fossil 

data through a panbiogeographic approach. 

( 其他 ). Candela A M; Morrone J J. 

Ameghiniana, 2003, 40(3): 361-378 

This paper analyzes the geographic and 

temporal distribution of the family Erethizontidae 

(Rodentia, Hystricognathi) and other 

fossil and living groups of neotropical mammals, 

with the aim of identifying distributional 

patterns. These patterns were recognized using 

the panbiogeographic method, on the basis of 

three requirements: (1) current representation 

of the groups in the Brazilian Subregion, (2) 

arboreal habits, and (3) recognized monophyly 

from the Deseadense. Two ancestral biotas 

were identified: one comprising the current 

Patagonia and areas of intertropical latitude 

mainly in western South America, the other, 

essentially intertropical, includes the fossil 

localities of the caves of Lagoa Santa and Bahia. 

Both biotas would have differentiated 

very early, at least from late Oligocene. The 

fossil locality of La Venta (middle Miocene) 

would correspond to a complex area or node. 

Current Patagonia would have acted as an area 

of marginal differentiation with regard to the 

radiations of the living taxa. The central region 

of Patagonia experienced marine transgressions 

and volcanic activity during the 

middle Tertiary and could represent a baseline. 

Both the phylogenetic relationships and the 

temporal and geographic distribution of late 

Miocene erethizontids indicate a geographic 

differentiation between the Northwest and the 

Northeast Argentina, at least from late Miocene. 

2007010414 

阿根廷巴塔哥尼亚早和中中新世一新的箭 

猪 = A new porcupine (Rodentia, Hystricognathi, 

Erethizontidae) from the Early and 

Middle miocene of Patagonia. ( 英文 ). Candela 

A M. Ameghiniana, 2003, 40(3): 483-494 

A new erethizontid, Branisamyopsis australis 

gen. et sp. nov., from Colhuehuapian 

sediments (early Miocene) of the Sarmiento 

Formation cropping out at Gran Barranca, 

Chubut Province, Argentina, is described. The 

new genus is also identified in the middle 

Miocene (Collon Cura Formation) at Canadon 

del Tordillo (Neuquen, Argentina). The comparative 

study of the mandibular and tooth 

morphology of erethizontids indicates that 

Branisamyopsis australis gen. et sp. nov. is 

closely related to Patagonian porcupines Eosteiromys 

Ameghino and Steiromys Ameghino. 

Branisamyopsis australis gen. et sp. nov. 

shows that extinct erethizontids reached their 

greatest taxonomic diversity during the Colhuehuapian. 

The cheek-tooth morphology of 

Patagonian Colhuehuapian erethizontids could 

correspond to different dietary adaptations. 

The temporal and geographic distribution and 

the phylogenetic affinities of Branisamyopsis, 

Eosteiromys and Steiromys suggest that Patagonia 

was a marginal area of differentiation 

for the family, unconnected with the radiation 

of living porcupines. 

2007010415 

希腊埃维亚州 Kerassia 地区晚中新世独角 

犀类 = Late Miocene horned rhinoceroses 

(Rhinocerotinae, Mammlia) from Kerassia 

(Euboea,Greece). ( 英文 ). Giaourtsakis I; 

Theodorou G; Roussiakis S; Athanassiou A; 

Iliopoulos G. Neues Jahrbuch fur Geologie u. 


367-398 

Among the most complete and prominent 

findings are a juvenile skull and an adult mandible 

that belong to two different horned rhinoceros 

species. The juvenile skull from the 

Kerassia - 3 is assigned to Ceratotherium 

neumayri, while the adult mandible from the 

plausibly isochronous site Kerassia- 4 belongs 

to Dihoplus pikermiensis. These new specimens 

are compared with the known Eastern 

Miditerrancean rhinocerotid record, which is 

briefly reviewed and updated. The potential 

118

interspecific interaction of both species is discussed. 

2007010416 

Pliomegatherium 属的评述 = A review of 

Pliomegatherium Kraglievich, 1930 

(Xenarthra: Phyllophaga: Megatheriidae). ( 英 

文 ). Brandoni D. Neues Jahrbuch fur 

Geologie u. Palaontologie / 

Monatschefte, 2006, (4): 212-224 

Eight species of Megatheriinae have been 

recognized from the "Conglomerado osifero" 

of the Ituzaingo Formation of Argentina, but 

the validity of some of these taxa is doubtful. 

The taxonomic status of one of them, Pliomegatherium, 

is assessed based on restudy of 

the material on which the species were originally 

based. The morphological differences 

observed in the type specimens of Pliomegatherium 

lelongi and Pl. paranensis do 

not justify their specific separation. Thus Pl. 

paranensis is considered as a synonym of Pl. 

lelongi. 

2007010417 

阿根廷东北部一中新世 Drytomomys 

typicus 的系统分类和生物地理意义 = Systematics 

and biogeographic significance of 

Drytomomys typicus (Scalabrini in Ameghino, 

1889) nov. comb., a Miocene Dinomyidae 

(Rodentia, Hystricognathi) from Northeast of 

Argentina. ( 英文 ). Candela A; Nasif N L. 

Neues Jahrbuch fur Geologie u. Palaontologie 

/ Monatschefte, 2006, (3): 165-181 

Extinct dinomyids are yet poorly know. 

Among them, Drytomomys has a particular 

interest from a biogeographical perspective, 

since it is one of the few extinct mammal genera 

recordedboth in the "Mesopotamian" and 

Laventan faunas.The comparative study of the 

holotype of "Olenopsis" typicus, coming from 

the "Conglomerado osifero", enables the allocation 

of this species to genus Drytomomys. 

The assignment of specimens recovered from 

La Venta fauna to D. aequatorialis is confirmed. 

The geographical distribution of Drytomomys 

suggests a biogeographical relationship 

of the Northeast of Argentina with the 

North of South America during the Miocene. 

2007010418 

巴西更新世马和南美马 : 古生态和生物地 

理意义 = Pleistocene Equus (Amerhippus) 

and Hippidion (Mammalia, Perissodactyla) 

from Brazil. Paleoecological and biogeographical 

considerations.. ( 其他 ). Alberdi 

M T; Cartelle C; Prado J L. 

Ameghiniana, 2003, 40(2): 173-196 

Fossil remains belonging to Equidae 

from Brazilian localities are described and 

taxonomically determined. We compared the 

postcranial (McIII, MtIII, AS, CAL, 1FIII) 

remains from Brazil with other remains from 

several localities of South America using multivariate 

analysis. The results indicate that 

Equus (Amerhippus) neogens Lund is represented 

in all localities of Brazil. In the same 

way, Hippidion principale (Lund) and H. 

devillei (Gervais) are present in Brazil, the 

first grouped the large remains, and the second 

the smaller ones. The three species are present 

in Toca dos Ossos. Equus (A.) neogeus is also 

present in Lage Grande. We assigned the material 

described by Souza Cunha as Equus (A.) 

vandonii to Equus (A.) neogeus. We present 

an up-to-date fossil distribution and approximate 

date of the main localities. We discuss 

the role of dispersal from the North and examine 

the palaeobiogeographical implications. 

2007010419 

奥地利 Szentmargita 地区 Heterodelphis 

leiodontus 全模标本的埋葬学和古生态 = 

Taphonomy and palaeoecology of the holotype 

of Heterodelphis leiodontus Papp, 1905 

(Cetacea, Mammalia) from Szentmargita (St. 

Margarethen, Austria). ( 英文 ). Kazar E; Lantos 

Z. Fragmenta Palaeontologica Hungarica, 

2001, (19): 51-60 

Preservation of an articulated skeleton is 

exceptional for the Leithakalk. After death the 

studied specimen underwent rapid burial 

caused by sudden sediment redeposition, 

probably due to stormy eater movements. The 

burial took place in a shallow, euphotic, nearshore 

marine environment. The sediment eas 

coarse, calcareous sand composed mainly of 

red algal grains. We suppose that fragments of 

coralline algae have originated from maerl 

while other microfaunal elements have been 

transported from a sea-grass meadow community. 

Reefs were not present in the close vicinity. 

2007010420 

匈牙利晚第三纪长鼻目化石 : 综述 = Neogene 

proboscidean remains from Hungary; an 

overview. ( 英文 ). Gasparik M. Fragmenta 

Palaeontologica Hungarica, 2001, (19): 61-77 

In the Proboscidean record there are four 

Deinotheriidae, five Gomphotheriidae and two 

Mammutidae species. The earliest two taxa 

(Prodeinotherium hungaricum and Gom- 

119

photherium angustidens) appeared here 

probably already in the Late Enggenburgian. 

From the Ottnangian three Proboscidean taxa 

were demonstrated: P. hungaricum, G. angustidens 

and Zygolophodon turicensis. In 

MN 9 three new Proboscidean taxa appeared. 

During the Pontian (MN 11-13) two huge 

Proboscideans occurred. The first remains of 

Anancus arvernensis and Mammut horsoni 

were derived from the MN 13. In the Early 

Pliocene D. proavum and S. grandincisirus 

probably were present in Hungary, but from 

the Late Pliocene only two mastodonts survived: 

A. anvernensis and M. borsoni. The last 

occurrences of these two species in Hungary 

are of Early Pleistocene age. 

2007010421 

匈牙利始新世海牛 = Eocene sea cows (Sirenia, 

Mammalia) from Hungary. ( 英文 ). Kordos 

L. Fragmenta Palaeontologica Hungarica, 

2002, (20): 43-48 

Four taxa can be distinguished in the Eocene 

of Hungary: Sirenavus hungaricus, Anisosiren 

pannonica, Sirenia indet. I and Sirenia 

indet. II. The present paper includes a list of 

all Eocene Sirenia finds from Hungary housed 

in State collections and in private hand. 

2007010422 

贵州关岭三叠纪海龙类化石一新种 = A new 

species of Triassic Thalattosauria from 

Guanling,Guizhou. ( 中文 ). 程龙 . 地质通 

报 , 2003, 22(4): 274-284 

描述了采自贵州省关岭巴毛林小凹组 

的海龙类 ( 新铺龙属 ) 化石 , 并确定其为一新 

种 —Xinpusaurus bamaolinensis sp. nov.。头 

骨和下颌骨受到背腹向挤压 , 且有少许错 

位。各骨块形状、接触关系等方面与孙氏 

新铺龙都极为相似 , 所以认为其与孙氏新铺 

龙同为新铺龙属。但又以其特长的吻部 ( 吻 

长是头长之半 )、外鼻孔由鼻骨和上颌骨围 

成、较短的齿骨 ( 占下颌长度的 47.2%) 和非 

常靠后的顶孔等为特点与 Xinpusaurus suni 

相区别。 

2007010423 

早白垩世热河生物群中的哺乳动物群 : 中 

生代哺乳动物的多样性和生物学意义 = The 

mammal fauna in the Early Cretaceous Jehol 

Biota: implications for diversity and biology 

of Mesozoic mammals. ( 英文 ). Meng Jin; Hu 

Yaoming; Li Chuankuai ; Wang Yuanqing. 

Geological Journal, 2006, 41(3/4): 439-463 

Eleven species belonging to five major 

groups of mammals (multituberculates, eutriconodontans, 

'symmetrodontans', metatherians 

and eutherians) have been described from the 

Jehol Biota, Liaoning, China. These fossils 

came from three horizons of the Yixian Formation: 

Lujiatun (lowest), Jianshangou and 

Dawahgzhangzi (highest) beds. Ages and correlations 

of these beds are still in debate, but 

are generally accepted as Early Cretaceous. 

Biostratigraphic distributions of some Jehol 

mammals corroborate the Early Cretaceous 

age of the biota. Many species are represented 

by skulls and articulated skeletons, although in 

most cases a species is known only from a 

single holotype that is squashed. These fossils 

furnish a wealth of morphological data for 

Mesozoic mammals, from which large character 

data sets have been amassed to generate 

competing higher-level phylogenetic hypotheses 

of mammals. The Early Cretaceous divergence 

of eutherians is first documented as 

skull and skeletal fossils. The Jehol mammals 

indicate a diverse mammal fauna in which 

species range from 25 g to 14 000 g in body 

masses, have insectivorous, omnivorous and 

carnivorous diets (as reflected by their dentitions 

and by stomach content), and acquire 

scansorial, possibly arboreal and terrestrial 

habits (as inferred from articulated skeletons). 

The well-preserved material helps to clarify 

some anatomical uncertainties in the study of 

early mammals, such as an ossified Meckel's 

cartilage as the occupant for the internal 

groove on the lower jaw of some Mesozoic 

species and a dental formula I3-C1-P3-M4/i2- 

c1-p2-3-m5 for gobiconodontids as suggested 

by dentitions of several Jehol eutriconodontans. 

Evidence from cranial specimens of Jehol 

eutriconodontans also disfavours the 

brain-expansion model for the detachment of 

middle car ossicles from the dentary during 

evolution of mammals. 

2007010424 

哺乳动物 Eutatus seguini 肢复原 : 古生物 

学意义 = Limb reconstruction of Eutatus seguini 

(Mammalia : Xenarthra : Dasypodidae). 

Paleobiological implications. ( 英文 ). Vizcaino 

S F; Milne N; Bargo M S. Ameghiniana, 2003, 

40(1): 89-101 

Eutatus seguini Gervais is one of the 

largest members of the family Dasypodidae. It 

was very common during the Late Pliocene- 

Early Holocene in Uruguay and centraleastern 

Argentina. Some specimens that include 

well preserved and complete endoskele- 

120

tal elements allowed to perform morphofunctional 

and biomechanical studies in order 

to infer locomotory adaptations. Comparative 

anatomical descriptions of Eutatus seguini 

Gervais with the recent armadillos Chaetophractus 

villosus (Desmarest), Dasypus hybridus 

(Desmarest), And the only living species 

of similar size Priodontes maximus (Kerr), 

were made. Its body mass was estimated 

through allometric equations. Different indices 

were calculated in order to analyse its limb 

proportions and their correlation with digging 

habits. The indices were compared with the 

values recorded for all living armadillo tribes, 

from mostly cursorial through subterranean. 

The general architecture and proportions of 

the limbs of E. seguini, and therefore its digging 

habits, are similar to those of the Euphractini 

and Dasypodini. Eutatus seguini 

shows unique features, for it reaches the size 

of the hiperspecialised digger and mirmecophagous 

Priodontes maximus, but with less 

fossorial specialisation and markedly herbivorous 

feeding habits. 

2007010425 

匈亚利北部 Felsotarkany 3/2 处晚 Astaracian 

期 (MN 3/2) 脊椎动物群中的 Collimys 

n. sp. = Collimys dobosi n. sp. (Cricetidae, 

Mammalia) from the Late Astaracian (MN 8) 

vertebrate fauna of Felsotarkany 3/2 (Northern 

Hungary). ( 英文 ). Hir J. Fragmenta Palaeontologica 

Hungarica, 2005, (23): 5-18 

Description of a new Middle Miocene 

hamster species is given on the basis of 400 

molars. This is the most abundant sample of 

the Collimys genus from the fauna of the Felsotarkany 

Middle Miocene terrestrial sediments. 

On the basis of the paleobotanical material 

and the new rodent fauna, a subtropical 

forest environment with different levels of 

foliage may be presumed. The rodents and the 

preliminary results of the study of the insectivors 

and molluscs indicate Late Astaracian 

age (MN 8) of the material. 

2007010426 

匈牙利 Rudabanya 地区的 Anomalomys 属 : 

臼齿的定名 , 时代范畴和系谱分类解释 = 

Anomalomys (Rodentia, Mammalia) from 

Rudabanya, Hungary (Miocene, MN9): terminology 

of molars, age categories and phylogenetic 

interpretations. ( 英文 ). Kordos L. Fragmenta 

Palaeontologica Hungarica, 2005, (23): 

19-28 

Anomalomys rudabanyensis belongs to the 

Anomalomys gaudryi-rudabanyensis-petteri 

lineage. The genus Anomalomys is possibly a 

descendant of a small species of Eumyarion. 

Early Miocene species of Anomalomys, notably 

A. aliveriensis and A. minor, are primitive 

representaves of the group. Anomalomys cf. 

rudabanyensis has been reported from outside 

the Carpathian Basin. The terminology of molar 

age categories of Anomalomys is defined in 

the present paper. 

2007010427 

沙特阿拉伯 As-sarrar 中新统下部 

Paraphiomys 的新种 = New species of 

Paraphiomys (Rodentia, Thryonomyidae) 

from the lower Miocene of As-sarrar, Saudi 

Arabia. ( 英文 ). Antonanzas R L; Sen S. Palaeontology, 

2005, 48(2): 223-233 

The family Thryonomyidae is represented 

in the Lower Miocene of Saudi Arabia 

by a single species, Paraphiomys knolli sp. 

nov. This new taxon differs from all other 

thryonomyids in being small, lower molars 

having a short metalophulid II and an isolated 

anterolabial cuspid, and upper molars being 

antero-posteriorly compressed and pentalophodont. 

A cladistic analysis involving all 

extinct and extant species of thryonomyids is 

provided. Paraphiomys knolli branches as the 

sister-species of Paraphiomys pigotti, type 

species of the genus. 

2007010428 

澳大利亚早中新统蝙蝠群 Hipposiderid 一 

新属 = A new Hipposiderid genus (Microchiroptera) 

from an early Miocene Bat community 

in Australia. ( 英文 ). Hand S J; Archer M. 


A new genus and species of hipposiderid 

bat is described from an early Miocene cave 

deposit (Bitesantennary Site) in the Riversleigh 

World Heritage fossil property, northern 

Australia. Eight hipposiderid genera are 

now recorded from Riversleigh's Miocene 

sediments: Hipposideros, Brachipposideros, 

Rhinonycteris, Riversleigha, Xenorhinos, 

Miophyllorhina, Archerops and Brevipalatus 

gen. nov. The new taxon appears to be most 

closely related to Australian endemic Rhinonycteris 

and Brachipposideros species, but 

its autapomorphically very short palate distinguishes 

it from other members of this relatively 

plesiomorphic group. It is one of eight 

hipposiderid species recovered from the Bitesantennary 

Site deposit, and one of 11 recorded 

from Riversleigh's early Miocene 

sediments. Compared with modern bat faunas, 

the early Miocene Riversleigh bat community 

121

differs strikingly in its high hipposiderid diversity 

but may differ less in its overall trophic 

structure. 

2007010429 

比利时安特卫普中新统长鼻海豚 

Eurhinodelphis 的系统亲缘 = Phylogenetic 

affinities of the long-snouted Dolphin Eurhinodelphis 

(Cetacea, Odontoceti) from the 

Miocene of Antwerp, Belgium. ( 英文 ). Lambert 

O. Palaeontology, 2005, 48(3): 653-679 

A new skull belonging to the species Eurhinodelphis 

cocheteuxi (Cetacea, Odontoceti, 

Eurhinodelphinidae), found in the upper 

Lower–Middle Miocene of Antwerp (Belgium, 

southern margin of the North Sea Basin) associated 

with its ear bones (periotic, tympanic 

bullae, malleus and incus), is the basis of a 

redescription and systematic revision of the 

species. This species is then used as an isolated 

taxon in a phylogenetic study of extinct 

and extant odontocetes. The main results of 

the cladistic analyses are: a sister-group relationship 

between E. cocheteuxi and the extant 

family Ziphiidae (beaked whales), and a more 

basal position of the superfamily Physeteroidea 

(sperm whales) in the tree. The possible 

paraphyly of the family Eurhinodelphinidae 

needs further investigation. The results are 

compared with the most recent morphological 

and molecular analyses. The species E. bossi, 

described in the Miocene of Maryland (east 

coast of the USA, Calvert Formation) is recognized 

in the Miocene of Belgium for the 

first time. 

2007010430 

澳大利亚北部 Miralinidae 以及该科最年轻 

分子的出现 = Miralinidae (Marsupialia : Phalangeroidea) 

from northern Australia, including 

the youngest occurrence of the family. ( 英 

文 ). Schwartz L R S. Alcheringa, 2006, 30(2): 

343-350 

Five isolated molars from two localities 

in the Northern Territory, the middle Miocene 

Bullock Creek and late Oligocene Kangaroo 

Well sites, are assigned to the new miralinid 

genus Barguru, which includes the three new 

species: Barguru kayir, Barguru maru and 

Barguru kula. The Miralinidae was previously 

thought to be restricted to the late Oligocene 

and early Miocene, but the occurrence at Bullock 

Creek extends the time range of this family 

into the middle Miocene. Analysis of metaloph 

development in the Miralinidae suggests 

that loph formation in this family followed a 

different trajectory to that of phalangerids. 

2007010431 

澳大利亚昆士兰西北部 Riversleigh 地区中 

新世中期关于 Propalorchestes novaculacephalus 

新材料的描述 = Description of 

new material for Propalorchestes novaculacephalus 

(Marsupialia : Palorchestidae) from 

the mid Miocene of Riversleigh, northwestern 

Queensland. ( 英文 ). Black K. Alcheringa, 

2006, 30(2): 351-361 

Additional material referable to Propalorchestes 

novaculacephalus from System B 

and System C deposits from the Riversleigh 

World Heritage Area, northwestern Queensland, 

is described. One of these specimens, a 

juvenile maxilla, represents the most complete 

and least worn dentition currently known for 

the species, and includes a dP(3) and P-3. It 

supports Murray's (1990) hypothesis that Propalorchestes 

molars are transitional between 

the fully bilophodont Palorchestes and the 

subselenodont/ semilophodont wynyardiid 

molar morphologies. The paracone and stylar 

cusp C and the metacone and stylar cusp D are 

clearly differentiated on the protoloph and 

metaloph, respectively of P. novaculacephalus. 

Other, new material tentatively assigned to P. 

novaculacephalus extends the temporal range 

for the species from early to middle Miocene. 

2007010432 

澳大利亚昆士兰西北部 Riversleigh 地区中 

新世中期关于 Propalorchestes novaculacephalus 

新材料的描述 = Description of 

new material for Propalorchestes novaculacephalus 

(Marsupialia : Palorchestidae) from 

the mid Miocene of Riversleigh, northwestern 

Queensland. ( 英文 ). Black K. Alcheringa, 

2006, 30(2): 351-361 

Additional material referable to Propalorchestes 

novaculacephalus from System B 

and System C deposits from the Riversleigh 

World Heritage Area, northwestern Queensland, 

is described. One of these specimens, a 

juvenile maxilla, represents the most complete 

and least worn dentition currently known for 

the species, and includes a dP(3) and P-3. It 

supports Murray's (1990) hypothesis that Propalorchestes 

molars are transitional between 

the fully bilophodont Palorchestes and the 

subselenodont/ semilophodont wynyardiid 

molar morphologies. The paracone and stylar 

cusp C and the metacone and stylar cusp D are 

clearly differentiated on the protoloph and 

122

metaloph, respectively of P. novaculacephalus. 

Other, new material tentatively assigned to P. 

novaculacephalus extends the temporal range 

for the species from early to middle Miocene. 

2007010433 

比利时上新统下部一新的 Balaenid 幼体头 

骨形态学及系统发育 = Skull morphology 

and phylogenetic relationships of a new Diminutive 

Balaenid from the lower Pliocene of 

Belgium. ( 英文 ). Bisconti M. Palaeontology, 

2005, 48(4): 793-816 

A new small balaenid is described and 

compared to all fossil and living balaenid taxa. 

The specimen represents a new genus and 

species and is named Balaenella brachyrhynus. 

It was discovered in the Lower Pliocene of 

Kallo (north-west Antwerp, Belgium) and 

adds new information on the diversity and 

evolution of Balaenidae. Based on both comparative 

morphology and phylogenetic analysis, 

Balaenella brachyrhynus is morphologically 

closer to the genus Balaena, including 

the living Greenland Bowhead whale 

(B. mysticetus), and two Pliocene species 

(B. montalionis and B. ricei) from central Italy 

and the eastern USA. Balaenella 

brachyrhynus has very short nasals, a short 

rostrum relative to the total skull length and a 

horizontal supraoccipital. A cladistic treatment 

of 81 morphological character states scored 

for 10 balaenids and nine non-balaenid cetaceans 

revealed that the other small balaenids 

generally included in the genus Balaenula 

(including Balaenula astensis, B. balaenopsis 

and a Pliocene Balaenula sp. from Japan) are 

closer to the living genus Eubalaena (the 

Right whale). As the new skull is so different 

from the nominal Balaenula species, and as it 

is more closely related to Balaena than to 

Eubalaena, it is concluded that a small body 

size was a common condition in different 

Balaenidae clades. 

2007010434 

浙江天台盆地蛋化石与恐龙的绝灭 = Cretaceous 

fossil eggs from the Tiantai basin of 

Zhejiang,with a discus sion on the extinction 

of dinosaurs. ( 中文 ). 方晓思 ; 卢立伍 ; 蒋严根 ; 

杨良锋 . 地质通报 , 2003, 22(7): 512- 2 图版 . 

综合报道了浙江天台盆地产出的蛋化 

石 , 其中包括新建立的龟鳖化石蛋科 ( 新 

科 )Testudoolithidae fam. nov. 和天台蛋属 ( 新 

属 )Tiantaioolithus gen.nov., 以及 5 个新 

种 :Dendroolithus shuangtangensis sp. nov., 

Elongatoolithus chichengshanensis sp. nov, 

Elongatoolithus laijiaensis sp. nov, Spheroolithus 

jincunensis sp. nov, Tiantaioolithus 

jiangi sp.nov。这批蛋化石以赤城山组出现 

的类型最为丰富 , 有长形蛋、树枝蛋、圆形 

蛋、龟鳖类化石蛋等 ; 赖家组蛋化石数量少 , 

仅见长形蛋和圆形蛋类 , 其时代均为晚白垩 

世。推测天台蛋化石消失的原因是由于气 

候变冷 , 受精卵不能正常孵化所致。孵化率 

降低 , 生殖链打断 , 可能是引起恐龙绝灭的原 

因之一。 

2007010435 

关于群岛土著脊椎动物的绝灭 : 西班牙 

Canary 群岛特纳里夫岛 Canariomys bravoi 

为例 = Extinction of endemic vertebrates 

on islands: The case of the giant rat Canariomys 

bravoi (Mammalia, Rodentia) on Tenerife 

(Canary Islands, Spain). ( 日文 ). Bocherens H; 

Michaux J; Talavera F G; Van der Plicht J. 


Fossil bone collagen C-14 dating and 

delta C-13 and delta N-15 isotopic measurements 

of the rodent Canariomys bravoi from 

Tenerife (Canary Islands.. Spain) were used to 

test two different hypotheses about the causes 

of extinctions of endemic vertebrates on islands. 

climate versus humans. For the Tenerife 

giant rat, we show that it survived the climatic 

change that occurred between the Middle and 

Late Holocene, but not the settlement of humans 

on the island. 

2007010436 

乌干达中新世中早期莫罗托 II 的新狭鼻类 

化石 = New Catarrhine fossils from Moroto II, 

Early Middle Miocene (ca 17.5 Ma) Uganda. 

( 英文 ). Pickford M; Senut B; Gommery D; 

Musiime E. Comptes Rendus Palevol, 2003, 

2(8): 649-662 

During the 1998-2003 field seasons of 

the Uganda Palaeontology Expedition, dental 

remains of three catarrhine species were recovered 

from Moroto 11, Uganda. Micromammals 

from the locality indicate a late 

Early Miocene to basal Middle Miocene (ca 

17.5-17 Ma) age, younger than Rusinga (17.8 

Ma), but similar in age to Buluk (17.2 Ma) 

and Kalodirr (17.2 Ma). This paper describes 

and interprets new catarrhines from the site, 

one of which is a victoriapithecid monkey, the 

second a new genus and species of smallbodied 

ape, and the third a large hominoid. A 

fourth species collected in the 1960's is attibuted 

to Afropithecus turkanensis. 

123

2007010437 

澳大利亚东南部维多利亚中生代至早第四 

纪哺乳动物群 = Mesozoic to early Quaternary 

Mammal faunas of Victoria, South-east 

Australia. ( 英文 ). Piper K J; Fitzgerald E M G; 

Rich T H. Palaeontology, 2006, 49(6): 1237- 

1262 

Twenty-two terrestrial and over 20 marine 

mammal faunas are currently recognized 

in the fossil record of Victoria, representing 

one of the most complete records of mammal 

evolution in Australia. Although the earliest 

recorded terrestrial mammals come from the 

Early Cretaceous, the majority of the faunas 

are concentrated in the Pliocene and Pleistocene, 

whereas the marine mammal record 

spans the Late Oligocene–Holocene. Despite 

the generally fragmentary nature of the fossil 

remains, many of the faunas are diverse and 

offer insights into the changes in palaeoecology 

and palaeoenvironmental conditions of 

the region over time. The terrestrial mammal 

faunas follow the global trend with the appearance 

of more arid-adapted species in the 

late Pliocene; however, a number of Pliocene– 

Pleistocene coastal sites indicate the continued 

presence of wet forest refugia, with several 

relict species occurring in the Early Pleistocene. 

Most of the faunas are well dated, providing 

a basis for the production of a biostratigraphic 

framework, essential for the 

more accurate dating of mammals in Australia. 

Two new diverse mammal sites, Childers 

Cove and Portland, are a welcome addition to 

the Pliocene records of both terrestrial and 

marine mammals. Marine mammal research is 

only in its early stages, but the Victorian record 

is fundamental in understanding the evolution 

of cetaceans in the southern oceans. The 

known diversity of species has increased substantially 

as a result of recent research. Some 

well-preserved specimens, including complete 

skulls, have implications for cetacean systematics, 

including basal mysticetes. However, 

much more work needs to be focused on the 

cataloguing, preparation, description and interpretation 

of the faunas to take full advantage 

of this excellent record. 

2007010438 

二齿兽颅后骨解剖结构的功能及演化特性 

= Functional and evolutionary aspects of the 

Postcranial anatomy of Dicynodonts (Synapsida, 

Therapsida). ( 英文 ). Ray S. Palaeontology, 

2006, 49(6): 1263-1286 

Restoration of the major skeletal muscles 

and functional morphological analysis of the 

postcranium were carried out on two Triassic 

dicynodont genera, Wadiasaurus and Lystrosaurus. 

A phylogenetic analysis of 12 selected 

Permian and Triassic dicynodont taxa was 

conducted and the postcranial character states 

were then mapped onto the most parsimonious 

tree. The analysis revealed changes in pectoral 

girdle and forelimb morphology, which included 

reduction of the coracoid plate, increasing 

robustness of the deltopectoral crest, 

change in humeral orientation from lateral to 

caudolateral, increasing prominence of the 

humeral head, and increasing robustness of the 

radius. Such changes can be associated with a 

functional tendency to reduce the lateral component 

of the propulsive force while still in an 

abducted mode. On the other hand, changes 

associated with the pelvic girdle included expansion 

of the preacetabular iliac process, reduction 

of the postacetabular iliac process, 

craniocaudal expansion of the iliac blade, 

change in the shape of the pubis from flat and 

plate-like to small and rod-like with a cranial 

process, and change in acetabular orientation 

from lateral to caudolateral. The femoral head, 

starting from a cranioproximal position, progressively 

became dorsally pronounced and 

offset from the body. Other features/changes 

associated with the femur included increasing 

robustness of the trochanter major, and increasing 

flattening of the femoral midshaft. 

Changes in the axial skeleton included increasing 

stiffening of the trunk to reduce lateral 

undulations, increasing dorsoventral flexion, 

and increasing sacral vertebral count, 

which can be correlated with the preacetabular 

iliac expansion. These findings suggest that 

the dicynodont postcranial skeleton evolved 

towards more upright hindlimb morphology 

with the body held well off the ground. 

2007010439 

非洲猎狗谱系中的渐进演化 - 系统分类意义 

= Gradual evolution in the African hunting 

dog lineage - Systematic implications. ( 英文 ). 

Martinez-Navarro B; Rook L. Comptes Rendus 

Palevol, 2003, 2(8): 695-702 

The hunting dog, Lycaon pictus, is one of 

the most representative species of the extant 

African fauna and one of the most efficient 

predators in the World. This species is actually 

a relict within Sub-Saharan Africa, but its 

lineage is well recorded in Eurasia during the 

Pliocene, and in Eurasia and Africa during the 

Early Pleistocene, while its record during the 

Middle Pleistocene is not well documented. 

Though postcranial skeletal remains dating 

124

from the Early Pleistocene show a tetradactyl 

forelimb, a characteristic feature of the extant 

lycaon, unique among canids, the upper and 

lower dentitions show gradual evolution from 

a primitive morphology in the Late Pliocene 

specimens to the highly specialized trenchant 

carnassials of the extant predatory species. We 

propose a new systematics for the lineage, 

grouping all the forms within the genus Lycaon 

2007010440 

灵长类动物成种作用的时间调配与节奏 = 

Timing and tempo of primate speciation. ( 英 

文 ). Curnoe D; Thorne A; Coate J A. Journal 

of Evolutionary Biology, 2006, 19(1): 59-65 

Published molecular clocks for primates 

are used to estimate typical divergence times 

for phylogroups (1.6 Ma), species (3.3 Ma), 

sister species (2.7 Ma), genera (8.9 Ma) and 

sister genera (8.6 Ma). Significant median 

differences exist between major groups (infraorders 

and superfamilies) for various divergence 

times. These data are employed to estimate 

typical maximum duration of speciation. 

Typical primate values (1.1 Ma) suggest this 

process to be faster than is characteristic of 

many vertebrates. However, after considering 

divergence times for hybridizing congeneric 

and confamilial primates, this value is likely 

only to estimate the commencement of prezygotic 

isolating mechanisms, rather than the 

completion of reproductive isolation. Thus, 

speciation typically takes around 1.0 Ma to 

more than 4.0 Ma to occur, depending on 

whether prezygotic or post-zygotic isolating 

mechanisms are emphasized. Typical primate 

genus age is around 5.3 Ma, but we note differences 

among major groups. In light of these 

estimates, the classification of humans and 

chimpanzees is reconsidered using a molecular 

yardstick approach. Three taxonomic 

frameworks may flow from molecular analyses, 

all of them having major implications for 

understanding the evolution of humans and 

chimpanzees. 

2007010441 

欧洲新生代啮齿动物演化中渐变论的示例 . 

= Cases of gradualism in rodent evolution during 

the Cainozoic in Europe.. ( 法文 ). Vianey- 

Liaud M; Michaux J. Comptes Rendus 

Palevol, 2003, 2(6-7): 455-472 

Since several decades, conflicting interpretations 

of the fossil record are well known 

when the latter is used to understand mechanisms 

and modes of biological evolution. 

Once recalled peculiarities of the paleontological 

material and approach, several cases 

studies conducted by teams of the laboratory 

of Montpellier are presented. It clearly appears 

that Theridomyidae, Gliridae and Murinae 

rodents illustrate gradual evolution at the geological 

time scale. At the same time scale, 

these groups do not give obvious examples of 

stasis. The understanding in terms of mechanisms 

of morphological evolution illustrated 

by fossils will remain a long running debate. 

And this despite consideration of the time 

scales involved in Earth History on the one 

hand, and in Biology and Ecology on the other 

hand, as well as of the gap between morphological 

change in individuals and genetic 

change within populations 

2007010442 

哺乳动物的辐射 : 关于它们系统发育和演 

化的最新进展 = The radiation of Mammals: 

recent advances concerning their phylogeny 

and evolutionary innovations. ( 法文 ). Hartenberger 

J L. Comptes Rendus Palevol, 2003, 

2(6-7): 473-482 

In the 3,5 billion years of the History of 

the Life, that of Mammals seems to us all the 

more brief that their future seems to have deceived 

in some million years, at the very beginning 

of the Cenozoic times. For their understanding, 

palaeontologists as well as 

molecularists try to build up the phylogenetic 

tree of the mammals. Here some of the reasons 

for the conflicts and controversies between 

both communities are analysed. Also 

the main evolutionary novelties as observed in 

Early Tertiary mammals are described. This 

catalogue shed light on this extraordinary 

event. 

2007010443 

泰国中中新世早期石炭兽 Brachyodus 属的 

发现 = Occurrence of the anthracotheriid 

Brachyodus (Artiodactyla, Mammalia) in the 

early Middle Miocene of Thailand. ( 日文 ). 

Ducrocq S; Chaimanee Y; Suteethorn V; Jaeger 

J J. Comptes Rendus Palevol, 2003, 2(4): 

261-268 

Remains of Brachyodus cf. onoideus 

from the Ban Na Sai Basin (Thailand) are described. 

They correspond to the first occurrence 

of that genus in South Asia, and might 

document the latest record of the genus in the 

Old World. Sihongotherium from the Middle 

Miocene of eastern China is likely a representative 

of Brachyodus that was misinterpreted. 

125

古人类学 

2007010444 

萨拉乌苏河流域化石智人的身高 = Estimation 

of the stature of Paleolithic Man from 

Salawusu Valley. ( 中文 ). 尚虹 . 人类学学 

报 , 2004, 23(3): 196-199 

采用股骨骨干下部横径等 , 根据中国汉 

族男女性长骨碎骨的身高推断回归方程推 

测有比较明确地层记载的萨拉乌苏河流域 

化石智人的身高。据此计算复原股骨长。 

采用一系列身高推测公式 , 得出该标本可能 

的身高范围并比较。该化石的身材比北京 

直立人高。与晚更新世智人相比 , 该流域化 

石智人的身材比山顶洞化石人类矮 , 比柳江 

化石人类高 . 

2007010445 

北地中海带现代人类的出现 = Emergence of 

modern man in the North-Mediterranean zone.. 

( 法文 ). Onoratini G. Comptes Rendus 

Palevol, 2006, 5(1/2): 193-202 

To a Mousterian rich of scrapers and denticulates, 

characterized by a cold stage of the 

isotopic level 4, succeeds without relationship, 

in Liguria and Provence, the Protoaurignacian 

with Dufour bladelets. This allochtonous facies 

appears during the Wurmian interpleniglacial 

period (isotopic level 3). This cultural 

facies, first complex of the North- 

Mediterranean Upper Palaeolithic, is the fact 

of Modem Men issued from the East. In Venetia, 

towards 40000 BP, these Modem Men 

supplant autochtonous Mousterian groups of 

the Western zone. At the same period, in a 

parallel direction, by the Danubian way, an 

other flow of settlement, more inner and earlier, 

has reached the Centre of Europe, and 

will be to the origin of the typical Aurignacian 

of the western Europe. In Liguria, we find 

again the Protoaurignacian at the Mochi shelter 

(37000 BP). This Mediterranean flow of 

Modem Men diffuses rapidly because, between 

35000 and 34000 BP, we find it in 

Provence, Languedoc and Ardeche. Later, in 

Liguria, the typical Aurignacian succeeds to 

the initial cultural facies at the last pleniglacial 

event (isotopic level 2). 

2007010446 

旧石器时代的艺术、季节和气候 = Palaeolithic 

art, seasons and climates.. ( 法文 ). Delluc 

B; Delluc G. Comptes Rendus 

Palevol, 2006, 5(1/2): 203-211 

During the glaciation of the Wurm, the 

rock and movable art of the hunters - gatherers 

of Cro-Magnon (approximately 35 000 to 

8000 years ago) is made of animals, human 

beings and geometrical signs. The everyday 

life is given rhythm by the seasons. They are 

rather often reflected in the morphology 

and/or the behaviour of the big herbivores 

represented. The presence of certain sorts indicates 

cold episodes: mammoths, woolly rhinoceros, 

ovibos, reindeers, megaceros. Others 

testify of reheating (as the interstadium of 

Lascaux): horses, bisons and especially aurochs, 

deer and hinds, ibexes. At the end the 

glaciation, the cold fauna is not any more represented. 

The great big animal art of the Cro- 

Magnons disappears, being replaced by an 

outdoor rock art, simplistic and often narrative. 

2007010447 

北地中海地区艺术的出现 = The appearance 

of art in the northern Mediterranean region. 

( 法文 ). Onoratini G. Comptes Rendus 

Palevol, 2006, 5(1/2): 223-227 

The appearance of art in the northern 

Mediterranean region happens in a progressive 

manner, as early as the arrival of modem man 

in Neanderthal territory. At a first stage 

around 45 ka BP, art is born with the preparation 

of objects used as body ornaments 

(pierced teeth and shells) and non-figurative 

decorated objects. At a secondary stage, 

around 35 ka BP, we witness the appearance 

of figurative art in the form of statuettes, in 

the High Danube region, and in the form of 

schematic paintings in Venetia. The final stage, 

around 32 ka BP, succeeds in the realisation of 

grand sanctuaries in caves where animals and 

symbols are represented in a complex and 

structured composition. The artistic evolution 

appears in relation with an attempt of explanation 

and symbolic domination of frightening 

natural forces and of laws that govern the 

world. 

2007010448 

脑膜中动脉的形态变异及其在人类进化上 

的意义 = Morphological variation of middle 

meningeal artery and its significance in human 

evolution. ( 中文 ). 吴秀杰 . 人类学学报 , 2003, 

22(1): 19-28 

对现代人、直立人、早期智人、晚期 

智人脑膜中动脉前支和后支压迹的形态的 

观察和对比发现 : 从直立人到现代人脑膜中 

动脉管径从粗到逐渐变细 , 分枝从简单到逐 

渐复杂 , 前支趋向于增大 , 后支趋向于缩小 , 呈 

126

现出一定的规律性 , 有地域性差异。作者认 

为脑膜中动脉的这种分布形式间接地反映 

了直立人向智人演化及现代人类形成过程 

中 , 大脑各部分比例的变化和功能的日益复 

杂对供血需求的影响。在研究颅骨与大脑 

之间的关系上及脑演化上 , 脑膜中动脉有一 

定的意义。 

2007010449 

应用古人骨的元素、同位素分析研究其食 

物结构 = Study on the diet of ancient people 

by analyzing bone elements and isotopes. ( 中 

文 ). 张雪莲 . 人类学学报 , 2003, 22(1): 75-84 

本文从原理和方法上对目前由人骨元 

素、同位素分析研究古人类食物结构的三 

个主要方面 , 即骨胶原碳十三、氮十五的分 

析 , 微量元素锶、钡分析以及同位素锶、铅 

的分析逐一做了介绍。在此基础上结合自 

己的工作将国内该研究领域中有关的研究 

现状和主要研究成果 , 特别是获得的新进展 

做了回顾和总结。 

2007010450 

3200 年前中国新疆哈密古人骨的 mtDNA 

多态性研究 = Study on mtDNA polymorphism 

of ancient human bone from Hami of 

Xinjiang,China 3 200 BPbp. ( 中文 ). 何惠琴 ; 

金建中 ; 许淳 ; 姜言睿 ; 朱琪泉 ; 谭婧泽 ; 黄微 ; 徐 

永庆 ; 金力 ; 任大明 . 人类学学报 , 2003, 22(4): 

329-338 

本文对新疆哈密五堡古墓地出土的 3 

200 年前的古人骨进行了 mtDNA D 环高度 

可变区的多态性分析 , 结合人类学头骨形态 

分析数据 , 探讨利用分子生物学技术进行人 

种鉴别研究。结果显示 , 在 3 200 年前 , 新疆 

哈密地区就有蒙古人种存在 , 并有可能发生 

亚、欧两种不同人类种群混居的现象。 

2007010451 

化石人类脑演化研究概况 = The study of 

fossil hominid brains. ( 中文 ). 吴秀杰 . 人类学 

学报 , 2003, 22(3): 249-255 

脑演化是人类演化的一个重要组成部 

分 , 其研究可以为人类起源、演化、人群关 

系及语言、智力等方面提供重要的信息。 

脑演化的主要证据是通过研究颅内模 

(endocast) 及颅骨的形态得到的。颅内模是 

从颅骨内表面得到的脑的外部形态。有时 

颅骨的内腔充满泥沙 , 并且为钙质所结固 , 可 

以自然形成颅内模。也可以人工制作颅内 

模。颅内模和颅骨的内表面能够提供人类 

脑髓及神经进化方面的直接证据。对化石 

人类脑演化的研究主要包括以下几个方面 

的内容 : 测量或估计脑量的大小及其和身体 

大小之间的关系 ; 研究脑量随时间的变化过 

程 ; 通过对早期人类颅内模表面沟回形态特 

征的研究 , 探索脑功能区在早期人类和猿类 

的区别及在演化上的变化 ; 左右大脑不对称 

性与一侧优势关系 , 探讨语言的起源和惯用 

手的脑功能基础等 ; 脑膜中动脉系统、静脉 

窦系统及与血液循环相关的排泄孔的变化 , 

探讨大脑各部分比例的变化和功能的日益 

复杂对供血需求的影响 ; 通过对人类脑演化 

的研究 , 探讨人类进化的原因。本文通过对 

以上几个方面及其中国化石脑演化研究的 

介绍 , 对化石人类脑演化的研究概况作综合 

论述和简单回顾 . 

2007010452 

广饶新石器时代人类头骨的小变异 = Minor 

skeletal variants of neolithic human skulls 

from Guangrao,Shandong. ( 中文 ). 尚虹 ; 韩康 

信 ; 李振光 . 人类学学报 , 2003, 22(3): 218- 

224 

通过对山东广饶新石器时代大汶口文 

化墓地 90 年代发掘的 61 具成年头骨进行 

小变异特征出现率的观察与统计并在此基 

础上进行聚类分析和主成分分析研究认为 , 

广饶人群的蒙古人种地区类型属于东亚类 

型。同时本文结果提示 , 在明确蒙古人种地 

区类型的主成分分析研究中 , 贡献率较大的 

三个小变异特征为下颌舌骨肌线桥、舌下 

神经管二分、眶上孔 , 这将为以后人们用小 

变异方法从事这方面的研究中如何选择观 

察项目方面提供了基础 . 

2007010453 

河北阳原姜家梁新石器时代遗址头骨非测 

量性状的观察与研究 = The observation and 

investigation of the skulls of Jiangjialiang 

neolithic age site in Yangyuan, Hebei with 

special reference to nonmetric cranial traits. 

( 中文 ). 李法军 ; 朱泓 . 人类学学报 , 2003, 

22(3): 206-217 

本文对河北阳原姜家梁新石器时代遗 

址头骨进行了非测量性状的观察。选择了 

在时间和空间上与之相关的 12 个人群作为 

研究对比组 , 求出各对比组之间的平均差异 

度 (MMD) 值 , 以 MMD 值为基础进行了聚类 

分析和主坐标分析。结果表明 , 姜家梁新石 

器时代居民在非测量性状上有着比较明显 

的特点 : 既与其它某些人群 ( 特别是与贝加尔 

人群、华北组 ) 有着某种联系 , 但现在还没有 

证据说明这种联系的密切程度以及是何种 

127

方式的联系 ; 同时 , 姜家梁组可能是因为还存 

在着某些独立的特征 ( 比如其较高的或者较 

低的非测量性状特征 ), 使之不能完全地归入 

到某种人群中去。我们期待从这一地区及 

其周邻地区发现更多的古人骨材料 , 以期从 

研究中得出更细致的结论 . 

2007010454 

南京汤山直立人颅容量的推算 = Cranial 

capacity estimation for Homo erectus from 

Tangshan,Nanjing. ( 中文 ). 张银运 ; 刘武 . 人 

类学学报 , 2003, 22(3): 201-205 

以耳上颅高推算现代人颅容量的公式 

可适用于汤山直立人 1 号头骨的颅容量的 

推算。汤山直立人 1 号头骨的颅容量推算 

值为 871ml, 与周口店直立人 3 号头骨的颅 

容量值相近 , 提示了汤山直立人的年代 “ 早于 

4 0 万年或更早 ” 的看法更可取些 . 

2007010455 

盘县大洞古人类遗址的地层和古气候 

研究 = Stratigraphic and paleoenvironmental 

studies at the Dadong cave,Panxian. ( 中文 ). 

王頠 ; 刘军 ; 侯亚梅 ;Lynne A; Shepartz; Sari 

Miller-Antonio; William Jack Rink; 斯信强 ; 

黄慰文 . 人类学学报 , 2003, 22(2): 131-138 

贵州盘县大洞的堆积物 , 自上而下可以 

分为 3 层。大洞主体堆积物为角砾堆积 , 来 

源于洞顶灰岩的崩塌 , 另外有人类遗物以及 

洞外片流作用带入的泥砂。人类化石、旧 

石器和哺乳动物化石主要分布在第 2 层角 

砾堆积中。堆积物在洞厅各部位均有相应 

分布 , 属同一沉积序列。已知的早期人类活 

动时间大约从 260ka.B.P. 开始 , 到 142ka .B.P. 

前后结束 , 对应于深海氧同位素的第 6、7 

阶段。角砾层下段 , 发育一套遭强烈溶蚀和 

风化的堆积物 , 地球化学分析结果显示其湿 

热的沉积环境 , 时间大约在 260—180kaB .P . 

期间 , 对应于深海氧同位素第 7 阶段 ; 大洞堆 

积物在气候变化周期上与黄土、青藏高原 

冰期序列可以对比 . 

2007010456 

青藏高原北部祁漫塔格地区发现古人类活 

动遗迹 = Discovery of ancient human relics 

in Qimantage, northern Qinghai-Tibet Plateau. 

( 中文 ). 拜永山 ; 王进寿 ; 常革红 ; 索生飞 ; 谈生 

祥 . 地质通报 , 2003, 22(5): 369-370 1 图版 . 

祁漫塔格位于柴达木盆地西南缘 , 东昆 

仑西段 , 平均海拔 4 000 m 左右 .2001 年作者 

在该区从事地质调查工作期间 , 首次发现 2 

处灰烬层、1 处牧羊遗址、2 处吐蕃文化遗 

迹、2 件石器 . 这些人类活动遗迹、遗物的 

发现 , 为探讨青藏高原远古人类活动及生态 

环境变迁 , 提供了十分难得的宝贵资料 . 现将 

相关成果分述 

2007010457 

远东上更新世晚期人类居住地 : 多变分析 

和变异的地理模式 = Late Upper Pleistocene 

human peopling of the Far East: multivariate 

analysis and geographic patterns of variation. 

( 英文 ). Demeter F; Manni F; Coppens Y. 


This research deals with the History of 

the human peopling of Far East Asia during 

the Late Upper Pleistocene. It brings some 

new answers to the question of modem human 

migrations in the Far East. This study is based 

on morphometric analysis of 45 fossil crania. 

The results of the multivariate analyses, combined 

with the recognition of geographic patterns 

of variation, separate the fossils into 

three morphological classes. These three clusters 

enable us to propose a likely scenario for 

the human peopling of the Far East from about 

67 000 years ago. 

2007010458 

肯尼亚西土尔卡那 Nachukui 组上新世 - 更 

新世考古地点 : 综合结果 1997-2001 = Plio- 

Pleistocene archaeological sites in the Nachukui 

Formation, West Turkana, Kenya: synthetic 

results 1997-2001.. ( 法文 ). Roche H; 

Brugal J P; Delagnes A; Feibel C; Harmand S; 

Kibunjia M; Prat S; Texier P J. Comptes Rendus 

Palevol, 2003, 2(8): Kenya; West Turkana; 

Plio-Pleistocene archaeology; Pre-Oldowan; 

Oldowan; Early Acheulean 

Stretched along the western side of the 

Turkana Basin, the Nachukui Formation preserves 

a large number of Plio-Pleistocene archaeological 

sites. Research carried out by the 

WTAP documents hominid behavioral evolution 

and technical diversity, through a time 

period ranging from 2.35 Myr to 0.7 Myr and 

within a relatively precise chronostratigraphic 

and paleoenvironmental frame. This work is 

based on comprehensive excavations conducted 

between 1997 and 2001 at the Late 

Pliocene and Early Pleistocene site complexes 

of the formation. 

2007010459 

肯尼亚西土尔卡那 Nachukui 组上新世 - 更 

新世主要考古点的动物群和古环境 = Faunas 

and paleoenvironments from main archaeological 

Plio-Pleistocene sites of the 

128

Nachukui Formation (West Turkana, Kenya).. 

( 法文 ). Brugal J P; Roche H; Kibunjia M. 


The Nachukui Formation is currently under 

archaeological investigation, especially 

within the Kalochoro (2.35 - 1.9 Myr) and 

Kaitio (1.9 - 1.65 Myr) Members. Six main 

archaeological sites have been excavated from 

this time period, which yield rich vertebrate 

faunas collected in situ or in close vicinity to 

the site. Paleontological studies help to precise 

the specific diversity for each site and increase 

our documentation for each Member with the 

discovery of new taxa. They allow to provide 

new informations about the biotope diversities 

exploited by Hominids and show a climatic 

tendency towards more humid environment 

between the Members. 

2007010460 

肯尼亚西土尔卡那段新的人科牙齿 = New 

hominid teeth from the Kaitio member (1.65- 

1.9 Myr) in West Turkana (Kenya).. ( 法文 ). 

Prat S; Brugal J P; Roche H; Texier P J. 


New hominid teeth have been recovered 

from the archaeological sites of Kokiselei I 

and Naiyena Engol 1. These two sites are located 

in the west side of the Turkana Basin 

and belong to the Kaitio member of the 

Nachukui Formation. They are dated between 

1.65-1.79 and 1.7-1.8 Myr respectively. The 

four teeth (left maxillary canine and first molar, 

right maxillary third molar and left mandibular 

third molar) discovered in Kokiselei I 

are attributed to Australopithecus boisei. The 

right mandibular first premolar found in Naiyena 

Engol I is referred to Homo sp. aff. ergaster. 

(C) 2003 Academie des sciences. 

Publie par Elsevier SAS. Tons droits reserves. 

2007010461 

肯尼亚 Aka Aiteputh 组 Diamantohyus nadirus 

的部分头盖骨 = a partial cranium of 

Diamantohyus nadirus from the Aka Aiteputh 

Formation (16-15 Ma), Kenya. ( 英文 ). 

Pickford M; Tsujikawa H. Paleontological 

Research, 2005, 9(4): 319-328 

Sanitheres are poorly understood suiforms 

of small body size. Recent advances in 

knowledge have been made, especially regarding 

their postcranial skeleton, but, apart from 

dento-gnathic remains, the cranium remains 

incompletely known. Field work in the Middle 

Miocene Aka Aiteputh Formation, near 

Baragoi, Kenya, has resulted in the recovery 

of a snout and a crushed neurocranium of 

Diamantohyus nadirus which throw a great 

deal of light on the systematic affinities of the 

sanitheres, but do not completely resolve 

their phylogenetic status. 

2007010462 

Kromdraai B 地区的早期人属 : 下部齿式 

的概率和形态分析 = Early Homo at Kromdraai 

B: probabilistic and morphological 

analysis of the lower dentition. ( 英文 ). Braga 

J; Thackeray J F. Comptes Rendus 

Palevol, 2003, 2(4): 269-279 

Kromdraai B, situated less than 2 km east 

of Sterkfontein, in the Gauteng province of 

South Africa, has yielded 27 specimens, attributed 

to a single Plio-Pleistocene hominid 

species, including the type specimen of 

Paranthropus (Australopithecus) robustus. By 

using resampling and morphological analysis, 

and after considering the most diagnostic features 

that have been used in the past for the 

lower dentition, we here suggest that one 

specimen from Kromdraai B, KB 5223, is 

clearly distinct from P. robustus and represents 

early Homo 

2007010463 

新种 Homo cepranensis 和非洲 - 欧洲中更新 

世人类的演化 = Homo cepranensis sp nov 

and the evolution of African-European Middle 

Pleistocene hominids. ( 英文 ). Mallegni F; 

Carnieri E; Bisconti M; Tartarelli G; Ricci S; 

Biddittu I; Segre A. Comptes Rendus 

Palevol, 2003, 2(2): 153-159 

The hominid calvarium from Ceprano 

(Italy) shows peculiar characters, especially in 

the frontal bone. This specimen differs from 

the other hominid species (H. ergaster, H. 

erectus, and H. heidelbergensis). The morphometric 

and the cladistic analyses show that 

the Italian fossil is a new hominid species. The 

typical characters of European H. heidelbergensis 

are absent in the frontal morphology of 

Ceprano, which is a representative of an African 

population that perhaps migrated at about 

1.0 Ma (represented by the specimen from 

Bouri and as demonstrated by the cladistic 

analysis) and that did not ultimately contribute 

to the human population of Europe during the 

Middle and Late Pleistocene. On the other 

hand, Ceprano shares features with Middle 

Pleistocene H. rhodesiensis, and this allows us 

to suppose that Ceprano is an early relative of 

this African form. 

历史地质学、地层学 

129

综论 

2007010464 

LOWESS 在锶同位素地层学中的应用 = 

Application of LOWESS fit to strontium isotope 

stratigraphy. ( 中文 ). 张萌 ; 黄思静 ; 谢国 

刚 ; 王麒翔 ; 侯杰 . 地球科学与环境学报 , 2004, 

26(2): 1-5 

锶同位素地层学是海相地层定年和全 

球对比的有效工具。为了建立全球范围的 w 

( 87 Sr)/w( 86 Sr) 比值年龄数据库 , 就必须对大量 

的 w ( 87 Sr)/w( 86 Sr) 比值年龄数据进行拟合 , 寻 

找最佳方法用于缩小最佳拟合曲线的区间 

范围是目前锶同位素地层学所面临的难题 

之一。在各种统计与拟合方法 

中 ,LOWESS( 局部加权回归散点修匀法 ) 为 

研究计算全球标准锶曲线最佳拟合模式提 

供了一种非参数拟合的精妙方法 , 拟合得出 

的最佳曲线能较好地作为海相地层的定年 

和进行全球对比的基础数据 , 并具有较高的 

置信区间。 

2007010465 

理论地层学与应用地层学 — 现代地层学概 

念 = Theoretical stratigraphy and apllied 

stratigraphy. ( 中文 ). 张守信 . . Pages:340. 高 

等教育出版社 .2006.7-04-018702-7. 

本书是国内第一本关于地层学理论及 

其应用的论著。全书系统介绍了现代地层 

学的发展历史、原理、各种地层单位和应 

用领域等各个方面 , 同时引入了当代最新 

古地磁地层学和应用地层学方面内容。对 

穿时普遍性原理、反效应原理、生物年代 

图解对比法及其数学性能等进行了补充 , 

突出了多重地层划分理论 , 修订了传统叠 

覆原理的使用范围 , 并且从现代区域地层 

学等方面阐明了地层学的应用和实践。在 

地层学的学科属性、地质时间的概念、界 

线层型等方面都根据国际地层学研究的最 

新成果进行了更新。 

2007010466 

地层学的几个基本问题及中国地层学可能 

的发展趋势 = Some fundamental problems of 

stratigraphy and the possible tendency of development 

of stratigraphy in China. ( 中文 ). 王 

鸿祯 . 地层学杂志 , 2006, 30(2): 97-102 

对地层学的几个基本问题 , 包括地层 

分类、国际地层表的建立、全球地层标准 

剖面及剖面点进行了讨论。在各种地层分 

类体系中 , 年代地层学和岩石地层学是分 

类中的主体 , 其他系统都居于补充或从属 

的地位。国际地层表是地质学的基本文件 

和地学研究的主要参照 . 其建立的基础应 

是地史上关键性地质事件的记录 , 其方法 

应是多学科的综合研究。前寒武纪与显生 

宙划分的建立标准应是一致的。国际地层 

委员会制订的 GSSP 做出了重大贡献 , 但 

所定点位不够稳定 , 点位以外无法对比 , 

在实践上和认知上都有不足。可考虑用多 

学科综合研究 , 寻觅接近等时的物理界面 

取代剖面点作为地层界面。在中国地层研 

究方面 , 以三次全国地层会议为准 , 分阶 

段概括论述了半世纪以来做出的主要成 

果。对今后中国地层研究的可能趋势提出 

了一些看法。主要是 : 应从系统论、整体 

观和复杂性观点的高度开展多学科的融 

合 , 共同解决地层的时空关系和划分对比 

等复杂问题 ; 应当扩大服务面和扩展研究 

面 , 着重开展以古环境和古气候为中心的 

地层研究 , 协助解决与经济建设中的资源 

与环境两大主题有关的地质课题 ; 制订 

2008 年后的中、长期规划 , 改进 GSSP 程 

序 , 持续完善《国际地层表》这一永恒任 

务 ; 开展高分辨率、高精度地层学研究 , 

建立融合及协调多种分支学科的综合地层 

学 } 扩大地层学对整个地球科学的服务 , 使 

中国地层学研究进入一个新的阶段。 

2007010467 

国际地层委员会与吕文会议 = ICS and the 

Leuven Conference. ( 中文 ). 陈旭 ; 戎嘉余 ; 彭 

善池 . 地层学杂志 , 2006, 30(2): 143-146 

国际地层委员会 (International Commission 

on Stratigrahy,ICS) 是国际地球科 

学联合会 (International Union of Geological 

Sciences,lUGS) 下属最大的一个科学机 

构 , 它的职能和组织可以下表来表达 ( 表 

1)。 

2005 年 9 月初 , 在比利时的吕文布 

(Leuven) 召开了国际地层委员会全会。除 3 

位法定官员 ( 主席、副主席、秘书长 ) 和分会 

的主席 ( 也即国际地层委员会的选举委员 ) 之 

外 , 还有少量有关组织的代表 , 如国际第 

四系联合会 (INQUA) 下属的地层和年代委 

员会主席、地层学新刊物主编、俄罗斯地 

层委员会代表和东道主列席了会议。在吕 

文会议上 , 先由各分会主席或副主席报告 

了分会两年来的工作和取得的成果 , 其后 

重点讨论了两件事 : 即第四系的问题和各 

分会全球界线层型剖面和点位 (GSSP) 确立 

的倒记时进度问题。 

经过热烈的讨论和争论 , 对第四系的 

定义进行了表决 , 结果大多数赞同一个 “ 折 

130

衷 ” 方法 , 即将第四系改为第四亚界 , 其底 

界与格拉斯阶 (Gelasian) 

的底界一致 , 其同位素年龄值为距今 

2.6Ma( 表 2)。 

2007010468 

首现和末现时间的地层差异 = Stratigraphic 

variation in the timing of first and last occurrences. 

( 英文 ). Holland S M; Patzkowsky M E. 

Palaios, 2002, 17(2): 134–146 

With the exception of the Neogene, it is 

difficult in much of the fossil record to measure 

range offset; that is, the difference in age 

between the first or last occurrence of a species 

in a local section and its time of origination 

or extinction within the sedimentary basin. 

A coupled simulation that incorporates a 

model of sedimentary basin fill, a randombranching 

model of evolution, and a model of 

the ecological characteristics of species is 

used here to explore stratigraphic and ecologic 

controls on range offset. Median values of 

range offset in much of the fossil record are 

predicted to range from several hundred k.y. 

to a few m.y., for a wide variety of stratigraphic 

architectures and species ecologies. 

Higher than average values of range offset are 

favored by unconformities of long duration, 

rapid facies changes of large magnitude, persistent 

monotonic trends in facies change, increased 

facies specificity of species, and decreased 

species abundance. These model predictions 

can be used as a guide for interpreting 

field data on first and last occurrences, such as 

evaluating zones of likely high or low biostratigraphic 

precision. Similarly, these results 

can be used to evaluate the support for paleobiological 

interpretations of local radiations, 

migrations, and extinction episodes. 

2007010469 

新的挑战新的使命 -- 附记国际地层委员会 

2002 年 6 月全会 = New challenge and new 

mission for the ics. ( 中文 ). 戎嘉余 . 地层学杂 

志 , 2003, 27(1): 1-10,18 

新世纪初国际地层委员会 (ICS) 面临着 

来自两方面的挑战 : 一是国际地质科学联合 

会 (IUGS) 向 ICS 提出硬性要求 :2008 年必须 

完成显生宙各个系、各个阶的全球层型剖 

面和点位 (GSSPs) 的选定工作 , 有关分会不能 

再无限期地拖下去了 ; 二是 ICS 的自身思考 : 

将来是就此停步还是继续履行其职责、但 

改变其方向和托管方式 ICS 必须面对现实 , 

改革思变 . 动力地层学显示高分辨率的全球 

变化的地质过程是激动人心和具有强烈社 

会责任的一个挑战 , 因为当今全球环境的恶 

化是人类所面临的一个极其紧迫的重大问 

题 . 地层学在这项研究中将扮演重要角色 . 根 

据详细的化石记录 , 可以进行精确的地层对 

比 , 洞察控制全球变化的动态驱动力 . 将这个 

给地层学定向的地质过程作为一个新的任 

务是最有意义的 .2002 年召开的 ICS 会议主 

要目的是让各分会主席对 ICS 未来的方向 

和组织结构取得一致意见 ; 加强内部交流与 

合作 , 企划将来的活动 ; 讨论如何应对来自 

IUGS 的挑战 . 文内简述各分会 ( 包括末元古 

系、寒武系、奥陶系、志留系、泥盆系、 

石炭系、二叠系、三叠系、侏罗系、白垩 

系、古近系、新近系、第四系等 13 个地层 

分会 ) 在会上交流的情况 , 并对 ICS 的未来发 

展方向、ICS 的组织和机构性质、ICS 的强 

项和弱势、GSSPs 的综合地层学、建立新 

的 " 地层信息服务 " 机构、创立 ICS 自己的 

刊物、地层资料数据库 ( 如 Chronos 系统 ) 和 

标准地质年表、ICS 新创国际地层奖、恢复 

第四纪分会的建议、ICS 组织的建议和 

2008 年后的可能性等问题进行概述 . 界线地 

层只是地层学的一个组成部分 ; 地层学领域 

除 GSSP 的工作外 , 还有许多内容值得去深 

入研究 . 国际地层委员会在进入新世纪后迎 

来的新的挑战和新的使命、委员会内部酝 

酿已久的转轨思路和改革方案 , 值得我们思 

考和借鉴 . 

2007010470 

全球已批准的和潜在的层型剖面和点位 

(GSSPs) = Overview of global boundary stratotype 

sections and points(GSSPS). ( 中文 ). J. 

Ogg 等 ; 戎嘉余 ; 李建国 ; 张海春 ; 朱学剑 . 地层 

学杂志 , 2003, 27(1): 11-18 

自 1978 年确立全球泥盆系底界层型和 

点位以来 , 国际地层委员会动员全球许多领 

域的地层学家为地质历史各个断代 ( 包括 

界、系、统、阶 ) 确立底界层型和点位 ( 俗 

称 “ 金钉子 ”)。这在国际地层学发展史上 , 是 

一个重要的里程碑。尽管在实施原理和方 

法上还有不同的意见、工作中也出现一些 

不尽如人意的地方 , 但其功绩 , 特别是在为 

寻求全球地质学基础的共同语言中所建立 

的功勋 , 将永载史册。然而 , 当前国际地层 

委员会已认识到这项工作并不是、也不能 

代表地层学的全部。从目前情况看 , 在显生 

宙 13 个系内约 100 个层型剖面和点位中 , 

已有 45 个被批准确立 ,18 个或条件已经成 

熟或接近完成 , 预计 2003 年将被提出并批 

准 ; 还有约 37 个的研究正在进行之中。新 

131

生代的大部分完成了 ; 中生代 ( 特别是白垩 

系和三叠系 ) 的还有一大半没有定 , 任务不 

轻 ; 古生代的以志留系和泥盆系的确立最 

早 , 但前者还存在一些问题 , 奥陶系的虽起 

步不晚 , 但由于种种原因 , 进展稍慢 , 正在加 

紧进行 , 石炭系和寒武系的也在努力之中。 

国际地层委员会已经决定这项工作必须在 

2008 年全部完成 , 以利于尽早转入下一个阶 

段更加深入的、全球地层学各领域的协同 

研究。 

2007010471 

层序充填动力学 —— 层序地层研究的新方 

向 = Sequence-filling dynamics——a new 

study direction on sequence stratigraphy. ( 中 

文 ). 侯明才 ; 陈洪德 ; 田景春 . 地层学杂 

志 , 2003, 27(4): 358-364 

层序地层学经过近半个世纪的发展 , 研 

究领域由当初的被动大陆边缘盆地扩展到 

了活动大陆边缘盆地、前陆盆地和陆相盆 

地 ; 从研究全盆地的层序地层到研究盆地中 

某一具体相带的层序地层 , 研究时代也从起 

初的中新生代拓宽到了古生代。定年技术 

的发展和同位素等手段的使用 , 使得对层序 

级别的划分越来越细 , 对层序发育控制因素 

的研究更加具体 , 冰川、气候、沉积物供应 

速率等因素对高级别 ( 三级或三级以上 ) 层 

序发育的控制较为明显 , 但对影响层序发育 

四大因素 ( 全球海平面变化、构造、气候、 

沉积物供应 ) 的动力机制一直未作根本性的 

探讨 ; 大陆地质是地球动力学的信息库 , 沉积 

盆地是大陆地质过程的信息反馈和载体 , 是 

壳、幔动力活动的记录和见证 , 层序作为盆 

地演化的充填块体 , 记载着盆地的成生、发 

展、演化的信息 , 层序的旋回性是地球运动 

节律的直接反映。因此 , 以此为研究对象的 

层序充填动力学是沉积盆地动力学乃至地 

球动力学研究的基础 , 是层序地层研究的新 

方向。 

2007010472 

日本广岛湾全新世相对海平面变化 : 基于 

介形虫材料的半定量重建 = Holocene relative 

sea-level change in Hiroshima Bay, Japan: 

a semi-quantitative reconstruction based on 

ostracodes. ( 英文 ). Yasuhara M; Seto K. Paleontological 

Research, 2006, 10(2): 99-116 

Holocene relative sea-level changes in Hiroshima 

Bay were reconstructed from fossil 

ostracodes from a core, using a semiquantitative 

method. In Hiroshima Bay, relative 

sea level rose rapidly (about 25 m) between 

ca. 9000 cal yr BP and ca. 5800 cal yr BP, 

after which it gradually fell (about 5 m) to its 

present level. The peak in relative sea level 

occurred at ca. 5800 cal yr BP. The sea-level 

curve for Hiroshima Bay is similar to curves 

for tectonically stable areas of Japan (e.g., 

Osaka Bay). 

古地理学、古气候学 

2007010473 

刚果 - 乌干达爱德华湖高分辨率的地球化 

学记录和晚全新世非洲赤道地区干旱的时 

限及成因 = A high-resolution geochemical 

record from Lake Edward, Uganda Congo and 

the timing and causes of tropical African 

drought during the late Holocene. ( 英文 ). 

Russell J M; Johnson T C. Quaternary Science 

Review, 2005, 24(12-13): 1375-1389 

High-resolution analyses of the elemental 

composition of calcite and biogenic silica (BSi) 

content in piston cores from Lake Edward, 

equatorial Africa, document complex interactions 

between climate variability and lacustrine 

geochemistry over the past 5400 years. 

Correlation of these records from Lake Edward 

to other climatically-forced geochemical 

and lake level records from Lakes Naivasha, 

Tanganyika, and Turkana allows us to develop 

a chronology of drought events in equatorial 

East Africa during the late Holocene. Major 

drought events of at least century-scale duration 

are recorded in lacustrine records at about 

850, 1500, 2000, and 4100 cal year BP. Of 

these, the most severe event occurred between 

about 2050 and 1850 cal year BP, during 

which time Lake Edward stood about 15 m 

below its present level. Numerous additional 

droughts of less intensity and/or duration are 

present in the Lake Edward record, some of 

which may be correlated to other lacustrine 

climate records from equatorial East Africa. 

These events are superimposed on a long-term 

trend of increasingly arid conditions from 

5400 to about 2000 cal year BP, followed by a 

shift toward wetter climates that may have 

resulted from an intensification of the winter 

Indian monsoon. Although the causes of decade- 

to century-scale climate variability in the 

East African tropics remain obscure, timeseries 

spectral analysis suggests no direct 

linkage between solar output and regional 

rainfall. Rather, significant periods of 725, 

125, 63–72, 31–25, and 19–16 years suggest a 

tight linkage between the Indian Ocean and 

African rainfall, and could result from coupled 

ocean-atmosphere variability inherent to the 

tropical monsoon system. 

132

2007010474 

湖泊沉积有机质的地球化学记录与古气候 

古环境重建 = Lacustrine sediments as a record 

of changes of regional climate and environment. 

( 中文 ). 卢粤晗 ; 孙永革 ; 翁焕新 . 地 

球化学 , 2004, 33(1): 20-28 

与深海沉积与冰芯记录相比 , 湖泊沉积 

主要反映区域气候变迁史 , 可以揭示百年、 

甚至十年尺度的古气候事件 , 是高分辨率古 

环境、古气候重建的理想场所 . 传统的地质 

地球化学方法主要侧重于宏观物理 / 化学特 

性描述和孢粉学的研究 , 近 10 年来 , 沉积有 

机质分子碳、氢同位素地球化学技术的渗 

入 , 使研究工作从传统的宏观、微观层次向 

分子级水平发展 , 对诸如古生产率估算、 

C 3 /C 4 植被演替史、古二氧化碳分压及古温 

度计算等深层次问题解决提供了强有力支 

持 . 本文评述了湖泊沉积有机质分子与碳、 

氢同位素地球化学记录及其在区域古环 

境、古气候研究中的应用前景 . 

2007010475 

Cauvery 盆地 ( 印度东南部 ) 晚白垩纪和 

早第三纪地层的粘土矿物 : 对 K/T 界线沉 

积物来源和古气候的意义 = Clay mineralogy 

of the Late Cretaceous and early Tertiary 

successions of the Cauvery Basin (southeastern 

India): implications for sediment source 

and palaeoclimates at the K/T boundary. ( 英 

文 ). Madhavaraju J; Ramasamy S; Ruffell A; 

Mohan S P. Cretaceous Research, 2002, 23(2): 

153-163 

Clay mineral analyses were carried out 

on late Maastrichtian–early Palaeocene (Cretaceous–Tertiary) 

sedimentary rocks in the 

Ariyalur area of the Cauvery Basin (southeastern 

India). These investigations were 

aimed at determining the sedimentary provenance 

and palaeoclimate of the area in the latest 

Cretaceous and earliest Tertiary. The late 

Cretaceous deposits show significant palaeogeographic 

variation in clay mineral contents 

across the study area. Mixed-layer illitesmectites 

dominate the clay mineral content of 

the uppermost Maastrichtian of all areas, with 

elevated smectite, illite, palygorskite, sepiolite, 

kaolinite and chlorite occurring at intervals 

through the succession. This combination and 

widespread variation in the clay mineral suite 

suggests a lithologically highly variable 

source terrain and lack of sediment mixing 

during transport. Mixed-layer clays occur with 

both kaolinite and palygorskite, interpreted in 

terms of a seasonal (warm and wet, warm and 

dry) source area. The uppermost Maastrichtian 

of the Niniyur section displays an upward increase 

in illite content, suggesting that the adjacent 

continental area became strongly influenced 

by physical weathering just prior to the 

K/T boundary. The return of mixed-layer 

clays, smectite, illite and kaolinite during the 

early Tertiary suggests that chemical weathering 

in a seasonal climate once again controlled 

the formation of clay minerals. These results 

imply that the volcanism associated with the 

Deccan Traps had no sudden effect on the 

Cretaceous or Tertiary sedimentation and clay 

mineralogy of this area. 

2007010476 

加拿大艾伯塔塞泊瑞斯山 Stampede 地点古 

土壤和沉积物的古环境解释 = Paleoenvironmental 

interpretation of the paleosols and 

sediments at the Stampede site (DjOn-26), 

Cypress Hills, Alberta. ( 英文 ). Klassen J. Canadian 


741-753 

A 3.65 m-thick sequence of paleosols and 

sediments exposed at the Stampede archaeological 

site provides an opportunity for studying 

climate change and its impact on ancient 

site utilization over a 7200-year period. Three 

radiocarbon dates establish temporal boundaries 

for the lower sequence of paleosols and 

sediments at 7200 and 6100 BP. This lower 

sequence is characterized by lack of cultural 

material in most paleosols, high accumulation 

rates, and evidence for fluvial deposition. The 

upper sequence dates from 6100 BP and is 

characterized by low accumulation rates, increased 

pedogenesis, and increased evidence 

for human occupation, particularily between 

4660 and 5230 BP. Phytoliths provide a strong 

signal for grassland vegetation beginning at 

6100 years BP coincident with the most intensive 

occupation of the site. Stable carbon isotopes 

and carbon/nitrogen (C/N) ratios support 

the presence of grass. The differences evident 

between the lower and upper sequences can be 

attributed to the change from warm dry conditions 

to cooler, moister conditions and agree 

to a first approximation with the information 

inferred from the nearby Elkwater Lake and 

Harris Lake records. However, the persistence 

of forest at the Stampede site for a 1400-year 

time interval, when the Harris Lake record 

indicates more arid conditions, suggests that 

springs and north-facing slopes made the Cypress 

Hills an "oasis" for both animals and 

people. 

133

2007010477 

Gaspe 阿巴拉契亚 Matapedia 盆地古地 

理 : 加拿大 Gaspe 带继承盆地的开始 = 

Paleogeography of the Matapedia basin in the 

Gaspe Appalachians: initiation of the Gaspe 

Belt successor basin. ( 英文 ). Malo M. Canadian 


553-570 

The Matapedia basin consists of the uppermost 

Ordovician - lowermost Silurian 

deep-water, fine-grained carbonatesiliciclastic 

rocks of the Honorat (Garin Formation) 

and Matapedia groups (Pabos and 

White Head formations), the lower rock assemblage 

of the Gaspe Belt in the Gaspe Appalachians. 

Paleogeographic maps of eight 

time slices from the Caradocian to the Llandoverian 

are presented to better understand the 

tectonosedimentary evolution of the 

Matapedia basin. Deposition evolved from 

siliciclastic (Garin Fm.) to argillaceous limestones 

(Pabos Fm.), to limestones (White 

Head Fm.). The overall change from terrigenous 

(Garin Fm.) to limestone facies (White 

Head Fm.) reflects a change in the source area. 

Paleocurrent directions and composition of 

sandstones indicate an orogenic source area to 

the south for the Garin Formation, which is 

believed to be the inliers of the Humber and 

Dunnage zones in the southern Gaspe and 

New Brunswick Appalachians. Lime muds 

deposited by turbidity currents coming from 

the north suggest the Anticosti active carbonate 

platform as the source area for the White 

Head Formation. The Matapedia basin was 

filled from south to north. First deposits, the 

Garin Formation, occurred south of the Taconian 

thrust sheets (Humber Zone) and also 

south of the Grenville basement. This region 

was the domain of the Ordovician Iapetus 

Ocean (Dunnage Zone). The northern limit of 

the basin migrated northward during deposition 

of the Matapedia Group in Ashgillian- 

Llandoverian times and reached its actual 

northern limit at the very end of the Llandoverian 

(C-6), when siliciclastic facies of the 

lower Chaleurs Group were deposited. 

2007010478 

准南山前断褶带紫泥泉子组层序地层及岩 

相古地理 = Sequence stratigraphy and lithofacies 

paleogeography in Ziniquanzi Formation 

in piedmont fault-fold belt, southern margin 

of Junggar Basin. ( 中文 ). 沈玉林 ; 郭英海 ; 

李壮福 ; 冉启贵 ; 贲旭东 . 新疆石油地质 , 2006, 

27(2): 169-172 

通过露头与钻井、测井资料的对比研 

究 , 依据紫泥泉子组存在两个区域稳定发 

育的大套泥岩 , 以及区域不整合、河道下 

切面或沉积体系转换面 , 将准噶尔盆地南 

缘山前断褶带古近系紫泥泉子组划分为 2 

个三级沉积层序 , 建立研究区层序地层格 

架。编制了以层序为单位的岩相古地理 

图 , 探讨了层序地层格架内的古近系紫泥 

泉子组沉积期间岩相古地理特征及沉积演 

化。其中 , 紫泥泉子组沉积早期 ( 层序 

一 ) 岩相古地理格局为冲积扇、辫状河 - 辫 

状河三角洲 - 湖泊共存 ; 紫泥泉子组沉积晚 

期 ( 层序二 ) 湖泊扩张 , 为以湖泊沉积为 

主的辫状河 - 辫状河三角洲 - 浅湖沉积组合。 

2007010479 

加拿大育空永冻区喀斯特内叠层石 : 对全 

新世高湿期古气候的指示 = Endostromatolites 

from permafrost karst, Yukon, Canada: 

paleoclimatic proxies for the Holocene hypsithermal. 

( 英文 ). Clark I; Lauriol B; Marschner 

M; Sabourin N; Chauret Y; Desrochers 

A. Canadian Journal of Earth Sciences, 2004, 

41(5): 387-399 

A remarkable biogenic calcite precipitate 

forms carpets of finely laminated similar to1 

mm diameter columns lining fissures within 

limestone bedrock in the permafrost regions of 

the northern Yukon. This material, "endostromatolite," 

for its laminated morphology and 

growth hidden within the carbonate rock, is 

ubiquitous within limestone terrains of the 

Arctic and grew during the early Holocene 

hypsithermal. Dissolution on the interior fissure 

faces is accompanied by biomineralization 

of the opposing faces; a previously unrecognized 

weathering process in permafrost regions. 

Occurrence is restricted to outcrops 

with a southern orientation in permafrost regions, 

in this case, from the Ogilvie Mountains, 

northern Yukon. Growth occurs in water-saturated 

talik during periods of permafrost 

degradation during insolation maxima. Their 

enriched delta(13)C values (-1.7e to 11.4e) are 

generated in a methanogenic environment during 

anaerobic degradation of soil-derived organic 

carbon. A paleotemperature signal extracted 

from the delta(18)O values demonstrates 

that growth occurred during a hypsithermal 

period with an average summer air 

temperature 7 +/- 2 degreesC higher than today. 

Corrected radiocarbon age measurements 

of the calcite and organic matter preserved 

within the endostromatolites indicate that 

biomineralization occurred during the late 

134

Pleistocene - early Holocene hypsithermal 

event. Profiles along the columns document 

late Pleistocene climate improvement, with 

maximum warmth coincident with the insolation 

maximum for 65degreesN, followed by 

cooling and end of growth in the mid to late 

Holocene. 

2007010480 

川西甘孜黄土磁性地层学研究及其古气候 

意义 = Magnetostratigraphy and its paleoclimatic 

significance of a loess-soil sequence 

from ganzi area, West Sichuan Plateau. ( 中文 ). 

乔彦松 ; 赵志中 ; 王燕 ; 王书兵 ; 傅建利 ; 李朝柱 ; 

蒋复初 . 第四纪研究 , 2006, 26(2): 250-256 

文章对川西甘孜地区甘孜寺剖面进行 

了系统的磁性地层学研究及石英颗粒表面 

形态特征分析。磁性地层学研究结果显 

示 ,B/M 界线出现在 S 8 的顶部 , 并且在剖面 

下部 12.7-14.0m 处出现了松山负向期的 

贾拉米洛正向极性亚带。本次测试以及结 

合以前的研究结果表明 , 甘孜地区典型的 

风尘堆积形成于约 1.15MaB.P. 以前。 

石英颗粒表面形态特征的分析结果说明风 

尘物质可能经历了风、流水、冰川等多种 

外动力作用 , 进一步证明该区的风尘物质 

主要来源于青藏高原及其周缘地区的冰水 

沉积。另外 , 研究结果指示青藏高原及其 

周缘地区的环境状况大约在 

1.15MaB.P. 发生了很大变化 , 主要表 

现为干旱化程度以及高原冬季风的明显增 

强 , 而这些变化又与青藏高原在该时期的 

快速隆升密切相关。磁性地层的研究结果 

将为在该区进一步开展古环境演化过程的 

对比分析及阶地地貌发育历史的研究奠定 

基础。 

2007010481 

泸定昔格达组时代认定与古环境 = Age and 

paleoenvironment of Xigeda Formation in 

Luding,Sichuan. ( 中文 ). 王书兵 ; 赵志中 ; 乔彦 

松 ; 蒋复初 . 第四纪研究 , 2006, 26(2): 257- 

264 

文章对泸定海子坪昔格达组重新进行 

了详细的古地磁测试 , 结果显示昔格达组 

发育时代为 4.2-2.6MaB.P., 地质时 

代属上新世中、晚期 , 与前人的研究结果 

一致。泸定海子坪剖面是目前所知的记录 

昔格达古湖沉积起始年代最早的剖面。泸 

定海子坪剖面记录了 5 个大的从粗 → 细的 

沉积旋回 ,15 个沉积阶段。沉积物中值粒 

径的 Φ 值直接指示了各旋回的沉积阶段 , 

Φ 值小 , 水动力较强 , 为动荡的沉积环 

境 ;Φ 值大 , 水动力较弱 , 为稳定的沉积 

环境。另外 , 沉积记录显示在约 

2.8MaB.P. 青藏高原的强烈隆升就已开 

始 , 昔格达古湖为过水湖 ; 至 

2.6MaB.P., 昔格达古湖完全消失 , 与 

黄土高原风尘沉积环境由红粘土堆积转变 

为黄土堆积的显著的改变相一致。海子坪 

剖面 TOC 高值段 , 沉积物的 Φ 值也较大 , 

沉积物为粘土、粉砂质粘土沉积 ;TOC 低 

值段 , 沉积物的书值也较小 , 沉积物为 

中、粗砂沉积 , 表明昔格达古湖沉积物有 

机质含量主要受岩性控制。 

2007010482 

长江中游砂山的粒度特征及古气候环境意 

义 = Grain size characteristics of aeolian sanddune 

at the middle reaches of the Yangtze 

River and Its Paleoclimatic and Environmental 

Significance. ( 中文 ). 胡思辉 ; 袁胜元 ; 霍炬 ; 李 

长安 . 地质科技情报 , 2006, 25(1): 35-40 

通过对江西梁家渡剖面的野外考察、 

系统采样和粒度测试 , 在与中原邙山黄土 

研究对比的基础上 , 分析和讨论了长江中 

游晚更新世风成砂堆积序列 ( 江西梁家渡 

剖面 ) 的粒度特征 ; 并结合热释光年龄测 

试数据 , 按照安芷生等的粒度年龄模式获 

得相应的年代时间标尺 , 根据粒度与古气 

候环境之闻的内在联系建立了长江中游地 

区晚更新世以来的气候环境演化序列 ; 发 

现长江中游末次冰期以来至少发生过 10 次 

暖湿一千冷的气候旋回 , 其中还记录了发 

生在约 22.0,29.5ka BP 的 2 次 Heinrich 

事件。 

2007010483 

西藏阿里地区札达盆地香孜剖面环境变化 

信息 — 来自粒度、磁化率及碳酸盐环境指 

标的证据 = Information of enviromental 

change at the Qangze section in the Zanda 

basin, Ngari area, Tibet, China: Evidence 

from enviromental proxies. ( 中文 ). 余佳 ; 韩建 

恩 ; 孟庆伟 ; 吕荣平 ; 孟宪刚 ; 朱大岗 ; 邵兆刚 . 

地质通报 , 2006, 25(6): 715-720 

通过对西藏札达盆地香孜剖面沉积物 

粒度、磁化率、碳酸盐等多项环境指标的 

分析 , 探讨了香孜组 2.68~1.36Ma 以来的 

气候环境演变。结果表明 2.68Ma 的古格运 

动以后 , 香孜组的气候逐步向干旱、寒冷 

转变 , 在约 1.81Ma 之后 , 札达第三纪古 

湖经象泉河向南外泄并被疏干。上述 3 项 

环境指标指示的环境特征和演变与介形 

135

虫、孢粉等资料 , 以及喜马拉雅山的隆升 

都有很好的对应关系。 

2007010484 

江汉平原江陵地区近 9kaB.P. 以来的气候演 

化 : 有机碳同位素记录 = Climatic change 

over the past 9 ka in the Jiangling area, Jianghan 

plain: Records of organic carbon isotopes. 

( 中文 ). 谢远云 ; 李长安 ; 王秋良 ; 殷鸿福 . 

中国地质 , 2006, 33(1): 98-103 

通过对江陵剖面沉积物的高密度采样 

和有机碳同位素分析 , 重建了江汉平原江 

陵地区近 9.0kaB.P. 以来的古气候古环境 

演化。江汉平原江陵地区 9.0- 

6.31kaB . P . 属相对温暖湿润的气候环 

境 , 晚期向干旱方向发展 ;6.31 ~ 

4.97kaB . P . 为冷干气候环境 , 在 

5.78kaB . P . 达到极盛 ; 4.97- 

2.50kaB.P. 为暖湿气候时期 , 其间 3.44- 

2.50kaB.P. 湖沼泥炭发育 ,3360a B.P.、 

3110aB . P . 、 2935aB . P . 和 

2710aB . P . 为明显的降温期 , 尤以 

2710aB . P . 的降温幅度最大 ;2.50ka 

B.P. 以来温度相对较低 , 为冷期。江陵 

地区近 9ka B.P、以来的气候变化与国内 

相邻区域的研究资料相一致 , 但又有区域 

的差异性。 

2007010485 

摩洛哥中部 Mouchenkour 组新的晚 

Asbian 期 / 早 Brigantian 期 ( 密西西比亚纪 

晚维宪期 ) 时限及古地理 = New Late Asbian/Early 

Brigantian (Late Visean, Mississippian) 

dates in the Mouchenkour Formation 

(central Morocco): palaeogeographical consequences. 

( 英文 ). Vachard D; Orberger B; 

Rividi N; Pille L; Berkhli M. Comptes Rendus 

Palevol, 2006, 5(6): 769-777 

New datings of calcareous sandstone 

lenses and olistolites exposed in the middle 

part of the siliciclastic Mouchenkour Formation 

indicate a Late Asbian/Early Brigantian 

age (Cfm7/Cfm8 Moroccan biozone). The 

calcareous microfossil assemblages are characterized 

by the problematic algae Ungdarella, 

Fasciella and Koninckopora and foraminifers 

Archaediscus (concavus stage), Pseudoendothyra 

and Eostaffella. An Asbian/Brigantian 

palaeogeography based on the depositional 

environments is reconstructed from northwest 

to southeast, from the Tizra to the Mouchenkour 

areas. The units, although in tectonic contacts, 

nearly preserve their initial location and 

relations. 

2007010486 

初论造山带古地理学 = An approach to orogen-paleogeography. 

( 中文 ). 吴根耀 . 地层学 

杂志 , 2003, 27(2): 81-98,115 

造山带古地理学属构造古地理学 , 是造 

山带地层学的姐妹学科 , 其核心是活动论构 

造观。简述了造山带古地理学的形成和内 

涵 , 重点讨论了地质记录已发生移位、歪曲 

和混杂的造山带地区 ( 或经造山作用改造的 

克拉通地区 ) 正确地进行构造 — 古地理重建 

的三个问题 : 一是不能用 “ 将今论古 ” 的方法 

恢复地史期间的隆起区和堆积区 , 地史期间 

的物源区并非一成不变 , 要充分认识物源供 

应的多样性和多重性 ; 二是沉积相带的展布 

受区域构造应力场及基底构造格局控制 , 要 

特别重视边缘相及其物源区的研究 ; 三是辨 

析原生沉积盆地与构造盆地 , 对盆地进行正 

确的构造复位是古地理重建的基础。 

2007010487 

最后冰期气候快速变化年代学 = Chronology 

of fast climatic changes during the last 

glacial period.. ( 法文 ). Bard E; Rostek F; 

Menot-Combes G. Comptes Rendus 

Palevol, 2006, 5(1-2): 13-19 

The history of the glacial climate is punctuated 

by events occurring at the scale of a 

human life. They are characterised by temperature 

changes of large amplitude, simultaneously 

in Greenland and the North Atlantic. 

These events affected not only the surface 

hydrology, but also the deep circulation of this 

oceanic basin. A by-product of the obvious 

correspondence between Dansgaard-Oeschger 

and Heinrich in the polar ice and marine 

sediments is to allow, by correlation, the construction 

of a calendar chronology for the marine 

records. This chronostratigraphic approach 

was validated by means of radiocarbon 

dating of deep-sea sediments raised on the 

Iberian Margin. Our study also contributes to 

the international effort of calibration of the 

radiocarbon time scale by providing significant 

results in the interval between 33000 and 

41000 years calendar BP. 

2007010488 

古气候和气候机制 = Paleoclimates and climatic 

mechanisms. ( 法文 ). Labeyrie J. 

Comptes Rendus Palevol, 2006, 5(1-2): 27-34 

Two mechanisms are described here, 

which generated the two main types of palaeoclimates 

- warm and cold - having affected 

the whole Earth from the post- 

Mesozoic cooling and the creation of the Gulf 

136

Stream (the latter having imposed alternations 

of warm periods and glaciations in the Northern 

Hemisphere since the Pliocene times. 

2007010489 

热带非洲在过去百万年的气候和水文变化 

= Climate and hydrological changes in tropical 

Africa during the past million years. ( 英 

文 ). Gasse F. Comptes Rendus Palevol, 2006, 

5(1-2): 35-43 

Tropical African climate has oscillated 

between markedly wetter and drier conditions 

on all timescales in response to global climate 

disturbances. A step-like increase in aridity 

over the past 3 Ma has been primarily paced 

by orbital cycles coupled with the onset and 

amplification of high-latitude glacial cycles. 

On the 10(4)-10(3)-ka timescales, observed 

changes imply interactions between insolation, 

sea-surface conditions and vegetation. Highfrequency 

variations could be linked to oscillations 

in major atmospheric circulation 

modes, in solar output, or to major volcanic 

events. 

2007010490 

第四纪气候和大气组分 : 新的冰核 = Quaternary 

climate and atmospheric composition: 

new ice cores.. ( 法文 ). Jouzel J; Lorius C; 

Raynaud D. Comptes Rendus Palevol, 2006, 

5(1-2): 45-55 

Over the last 20 years, studies of Antarctic 

and Greenland ice cores have provided a 

wealth of information directly relevant to the 

past and to the future evolution of our climate 

with, as more important, the discovery of a 

link between greenhouse gases and climate in 

the past and the characterization of rapid climate 

changes. These results are based on the 

analysis of deep ice cores such as the one 

drilled at the Vostok site, which allows us to 

describe the evolution of Antarctic climate 

and of atmospheric composition over 420 ka 

(thousands of years), and GRIP and GISP2 

(Greenland), which precisely depict the 

rhythm of rapid changes during the last 100 ka. 

Information available from ice cores has considerably 

increased in 2004 thanks to the 

EPICA Dome C ice core in Antarctica and to 

the North GRIP one, in Greenland. We present 

these two successful international programs 

and describe the first results they have provided, 

with the EPICA Dome C core covering 

eight climatic cycles (800 ka) and the North 

GRIP one allowing us to reach, for the first 

time from a northern-hemisphere ice core, the 

Eemian, the warmest past of the last interglacial 

around 120 ka ago. 

2007010491 

地中海地区更新世气候变化 = Climatic 

variations in the Mediterranean region during 

the Pleistocene.. ( 法文 ). Paterne M. Comptes 

Rendus Palevol, 2006, 5(1-2): 57-64 

One peculiar feature of the Mediterranean 

Sea is the existence of numerous layers 

of dark pelagic sediments, rich in organic carbon, 

known as sapropels. They occurred during 

warm climatic periods as well as during 

cold and transitional periods since 7 Ma, and 

similar deposits were recognised from tectonically 

uplifted marine cliffs since 25 Ma. They 

attest brief periods of bottom water anoxia, 

attributed to a decrease in the Mediterranean 

Sea surface density and consequently a reduction 

of the Mediterranean Sea overturning. 

Such a decrease may be related either to huge 

floods of the Nile related to the intensity of the 

African monsoon or to a change of the precipitation-evaporation 

budget over the Mediterranean 

region. As precisely dated by orbital 

tuning, these events permit the attainment of a 

global time-scale of the geological record for 

the Late Neogene. 

Author Keywords: Mediterranean Sea; 

sapropels; African monsoon; hydrological 

cycle 

2007010492 

长花粉序列对更新世气候变化的知识的贡 

献 = Contribution of long pollen sequences to 

the knowledge of climatic variations in Pleistocene 

countrysides. ( 法文 ). de Beaulieu J L; 

Andrieu-Ponel V; Cheddadi R; Guiter F; 

Ravazzi C; Reille M; Rossi S. Comptes Rendus 

Palevol, 2006, 5(1-2): 65-72 

The already well-known pollen sequence 

from Velay illustrates the great complexity of 

the climate oscillations during the last 450 000 

years (four climatic cycles). This sequence is 

compared with two records from northern Italy, 

Leffe (Lower Pleistocene till ca-1 Ma) 

and Pianico Sellere (starting at ca -800 ka). It 

confirms that the glacial/interglacial cycles 

dramatically changed between 1 Ma and 800 

ka. Lower Pleistocene cycles are shorter and 

warmer, with poorly marked glacial intervals; 

the climatic amplitude of Middle Pleistocene 

cycles is greater, from cold and dry glacial to 

interglacial optimums similar to the present. 

This change corresponds to the setting of the 

100 000-year cycles associated with a major 

137

extinction phase for forest trees unable to survive 

during glacial intervals. 

2007010493 

关于长花粉记录的考古孢粉学 = Archaeological 

palynology with regards to long pollen 

records.. ( 法文 ). Renault-Miskovsky J; Lebreton 

V. Comptes Rendus Palevol, 2006, 5(1- 

2): 73-83 

Pollen analyses from archaeological deposits 

or from framing prehistoric occupation 

layers are a contribution to the knowledge of 

the flora, environment and climate conditions 

synchronous of occupations of a territory by 

Hominids. Palynological results are compared 

with glacial and interglacial episodes from 

long pollen sequences. Palaeoenvironmental 

and palaeoclimatic data are interpreted and 

placed within the Quaternary and Prehistory 

chronological framework. The Ca' Belvedere 

di Monte Poggiolo and La Pineta open-air 

sites (Italy) and the Vallonnet cave (South- 

East of France) show evidences for an early 

colonization of the European Mediterranean 

basin during the Early Pleistocene. Pollen 

analyses undertaken in those prehistoric sites 

have provided new data on the Hominid and 

their surrounding landscapes. These data are 

faced with some Early Pleistocene climatic 

cycles recorded in long and continuous pollen 

sequences. 

2007010494 

晚更新世智利南部 "Cueva del Milodon" 放 

射性碳年代学和气候条件 = Radiocarbonic 

chronology and climatic conditions in the 

"Cueva del Milodon" (southern Chile) during 

the Late Pleistocene. ( 法文 ). Tonni E 

P;Carlini A A; Tane G J S,;Figini A J. 

Ameghiniana, 2003, 40(4): 609-615 

A synthesis of the radiocarbon ages on 

different remains of Mylodon sp. from "Cueva 

del Milodon" (Chile) is included and reanalysed; 

the climatic conditions in the area are 

discussed and hypothesis about the use of the 

alimentary resources for Mylodon sp. are formulated. 

We concludes that: 1) Mylodon sp. 

inhabited the cave among 13560 180 and 

10200 400 years radiocarbon BP; 2) during 

that lapse it is verified in the area an advance 

of the glaciers; 3) Mylodon sp. could have 

developed a hibernation strategy to overcome 

unfavorable conditions; 4) the presence of 

Mylodon sp. in caves, without evidences of 

human activity, support the hypothesis about 

the use of it by this xenarthra. 

2007010495 

坦桑尼亚中部 Manonga-Wembere 峡谷中 

新世 - 更新世发现的古土壤层的古气候意义 

= Paleoclimatical significance of the paleosol 

levels occurring in the Miocene-Pleistocene 

stratigraphy of the Manonga-Wembere Valley 

in Central Tanzania. ( 英文 ). Kafumu P D. 

Episodes, 2004, 27(2): 107-111 

Micromorphological characteristics of 

jour paleosol levels of the Manonga - Wembere 

deposits in Central Tanzania indicate periods 

of wetter climate in the Pliocene than at 

present. The stratigraphy of the studied section 

shows a series of lacustrine calcareous clay 

sediments alternating with gravel, sand and 

silt. The sediments are believed to have been 

deposited in the Manonga - Wembere paleolake 

environment. Paleosols intercalate these 

sediments and were formed when stable landscapes 

developed on former lake beds during 

regression periods. Micromorphological features 

of the paleosols indicate strong clay illuviation 

of red to yellow typic clay coating and 

some Fe-Mn hydoxide hypocoatings in voids 

and channels. The groundmass consists of 

either an accumulation of bioturbated yellow 

to red clay coating fragments or an argillic red 

to yellow groundmass of clay mass. Such an 

illuviation and its associated groundmass is 

comparable to intense clay illuviation fronts 

that are found in present-day calcareous sediments 

of warm and wet climates. The paleosol 

levels therefore represent wetter climatic conditions 

than today in the area during the 

Lower Pliocene. 

2007010496 

坦桑尼亚中部 Manonga-Wembere 峡谷中 

新世 - 更新世发现的古土壤层的古气候意义 

= Paleoclimatical significance of the paleosol 

levels occurring in the Miocene-Pleistocene 

stratigraphy of the Manonga-Wembere Valley 

in Central Tanzania. ( 英文 ). Kafumu P D. 

Episodes, 2004, 27(2): 107-111 

Micromorphological characteristics of 

jour paleosol levels of the Manonga - Wembere 

deposits in Central Tanzania indicate periods 

of wetter climate in the Pliocene than at 

present. The stratigraphy of the studied section 

shows a series of lacustrine calcareous clay 

sediments alternating with gravel, sand and 

silt. The sediments are believed to have been 

deposited in the Manonga - Wembere paleolake 

environment. Paleosols intercalate these 

sediments and were formed when stable landscapes 

developed on former lake beds during 

regression periods. Micromorphological fea- 

138

tures of the paleosols indicate strong clay illuviation 

of red to yellow typic clay coating and 

some Fe-Mn hydoxide hypocoatings in voids 

and channels. The groundmass consists of 

either an accumulation of bioturbated yellow 

to red clay coating fragments or an argillic red 

to yellow groundmass of clay mass. Such an 

illuviation and its associated groundmass is 

comparable to intense clay illuviation fronts 

that are found in present-day calcareous sediments 

of warm and wet climates. The paleosol 

levels therefore represent wetter climatic conditions 

than today in the area during the 

Lower Pliocene. 

古生界 

2007010497 

三塘湖盆地二叠纪构造层划分及其构造特 

点 = The division of Permian tectonic sequence 

and the feature of residual tectonic in 

Santanghu Basin. ( 中文 ). 李玮 ; 周鼎武 ; 柳益 

群 ; 梁积伟 . 西北大学学报 ( 自然科学 

版 ), 2005, 35(5): 617-620 

目的研究二叠纪构造层的划分及其构 

造特点。方法依据三塘湖盆地二叠纪地层 

与上覆地层的区域性不整合关系在地震剖 

面上的反映及其不同构造层的构造变形差 

异性 , 划分出二叠纪构造层 , 并对其构造 

格局和残留构造特点进行研究。结果二叠 

纪沉积盖层形成后 , 遭受晚海西期构造运 

动的影响 , 导致中央拗陷带残余二叠纪地 

层中宽缓褶皱和冲断构造组合的发育 ; 在 

遭受多期构造叠加改造后 , 残余的二叠纪 

构造层在盆地中表现为西南部残余厚度 

大 , 东北部残余厚度小的现今构造格局。 

结论二叠纪构造层具有残留盆地的特征 , 

主要含油层分布在条湖凹陷的西南缘和马 

郎凹陷。 

2007010498 

新疆伊宁盆地尼勒克地区二叠纪地层研究 

新进展 = New advances in the study of Permian 

stratigraphy at Nileke in the Yinin Basin, 

xinjiang. ( 中文 ). 宋志瑞 ; 肖晓林 ; 罗春林 ; 吴 

明仁 ; 凌联海 ; 程春华 . 新疆地质 , 2005, 25(4): 

334-338 

尼勒克地区二叠纪地层分布面积最 

广 , 地层出露齐全 , 接触关系清楚 , 包括 5 

个组的全部层型剖面在内 , 是在西天山研 

究二叠纪地层的经典地区 . 通过对 5 条层 

型剖面全部进行重测 , 系统采集样品 , 取 

得了成果 . 主要体现在火山喷发旋回研 

究、生物化石及岩相分析研究 , 并进行较 

详细的地层划分 , 为西天山二叠纪地层划 

分与对比提供了可靠依据 . 

2007010499 

通过 C27/C29 甾烷和有机碳同位素来判 

断早古生代和前寒武纪的烃源岩的生物来 

源 = Biological origin of Early Palaeozoic and 

Precambrian hydrocarbon source rocks based 

on c27/c29 sterane ratio and organic carbon 

isotope. ( 中文 ). 孟凡巍 ; 周传明 ; 燕夔 ; 袁训来 ; 

尹磊明 . 微体古生物学报 , 2006, 23(1): 51-56 

在早古生代与前寒武纪的石油与源岩 

中 , 经常出现令人困惑的 C 29 甾烷势 , 而在 

有机地球化学中 C 29 甾烷优势被认为是陆相 

有机质输入的标志。作者通过对比文献中 

各种海相藻类的热模拟产物分析 , 提出了 

早古生代与前寒武纪的石油与源岩中 C 29 。 

甾烷优势主要来源于浮游绿藻的观点 , 并 

通过 C 27 , 甾烷 /C 29 甾烷的比值提出了区分 

早古生代及前寒武纪石油源岩沉积环境的 

方法 , 对中国南方前寒武纪和早寒武世黑 

色岩系的有机地球化学分析也支持上述推 

断。此外 , 本文还提出了用有机碳同位素 

来进一步区分 C 29 。甾烷优势生物来源的方 

法。 

2007010500 

青海南部治多 — 杂多一带二叠系尕笛考组 

= On the Gadikao Formation in Zhidoi and 

Zadoi areas, southern Qinghai. ( 中文 ). 牛志军 ; 

段其发 ; 王建雄 ; 白云山 ; 曾波夫 ; 涂兵 ; 卜建军 . 

地层学杂志 , 2006, 30(2): 109-115 

青海南部二叠系尕笛考组厚度变化 

大 , 分布广 , 空间上呈链状展布。通过在 

该区地质调查对该组进行厘定 , 尕笛考组 

岩性组合为玄武岩、火山集块岩、火山角 

砾岩夹灰岩、砂岩和泥岩 , 与上覆九十道 

班组呈整合或假整合接触 , 为火山 - 沉积体 

系。尕笛考组产筵类 Misellina— 

Schwagerina 组合、非篷有孔虫、珊瑚。 

wentzellophyllum—szechuanophyllum 组合和 

腕足类等 , 表明地质时代为早二叠世罗甸 

期 , 与华南、西秦岭、藏东等地同期生物 

群可很好地对比 , 揭示出昌都地块在二叠 

纪时生物古地理区系属于特提斯大区华夏 

区。在构造古地理上为泛华夏大陆群或扬 

子板块的一个组成部分。 

2007010501 

吉林中部 “ 一拉溪组 ” 扬弃或续用浅析 = " 

Yilaxi Formation" of central Jilin. ( 中文 ). 殷 

139

长建 ; 陈跃军 ; 彭玉鲸 . 地层学杂志 , 2006, 

30(2): 136-140 

吉林省吉中地区二叠系岩石地层单位 

“ 一拉溪组 ” 为原长春地质学院吉林区测队 

在 1960 年创立。《吉林省岩石地层》 

(1997) 等明确为不采用之单位 ,《中国 

地层典二叠系》(2000) 等标明为采用地 

层单位。已有的实际材料证明 : 在 “ 一拉溪 

组 ” 建组剖面 —— 九台市波泥河子 “ 一拉溪 

组 ” 剖面的灰、黑色粉砂岩中发现 

Neocalamites 、 Eguisetites 、 Citenis 、 

Ginkgoites 及 Cladophlebis 为主的早侏罗世植 

物群 ; 原认为在范家屯组建组剖面 , 该组 

假整合于范家屯组之上 , 现叉在该剖面上 

部 (10 层以上 ) 发现 4 个产植物化石的层 

位 , 15 层除产植物 Pecopteris 

sp . ( P . cf . anthriscifolia ) 、 

Phyllothecacf.deliguescens、Paracalamites 

tenuicostata、Noeggerathhiopsis sp. 等外 , 

还见有淡水叶肢介 Cyclotoguzites sp., 确 

证 “ 一拉溪组 ” 系不整合于杨家沟组之上。 

因此 , 作为二叠系岩石地层单位的 “ 一拉溪 

组 ” 已不可能为了优先权而加以保留。但在 

统一研究该区中生代岩石地层序列时 , 一 

拉溪组和其他单位一样 , 可按优先权法则 

参与竞选。 

2007010502 

全球寒武系四统划分框架正式确立 = A new 

global framework with four series for Cambrian 

System. ( 中文 ). 彭善池 . 地层学杂 

志 , 2006, 30(2): 147-148 

国际地层委员会最近陆续发布了 2005 

和 2006 年版《国际地层表》(http : 

//www.stratigraphy.org/cheu.pdf), 这 

两张新表较以往各版最为突出的变动是将 

寒武系分为四个统和十个阶 , 不再采用国 

际地学界沿用了近一百七十年的上、中、 

下 3 统的传统划分方法。这一改写是全球 

地层学的重大事件 , 也是寒武纪年代地层 

研究继确立首个寒武系 “ 金钉子 ” 后所取得 

的又一突破性的进展 , 无疑具有重要的科 

学意义 ...... 

2007010503 

安徽巢湖地区泥盆纪 - 石炭纪界线地层的新 

认识 = New views on the Devonian- 

Carbonifereous boundary stratigraphy of the 

Chaohu region ,Anhui Province. ( 中文 ). 侯明 

金 ; 齐敦伦 . 地层学杂志 , 2006, 30(2): 156- 

170 

通过对研究区内的五通组几条代表性 

剖面的岩性、岩相及化石特征和地层区域 

展布等研究并进行区域对比 , 结合近年来 

的区调及科研成果 , 提出巢湖地区五通组 

观山段至擂鼓台段中部的下黏土层的时代 

属于晚泥盆世晚期斯图期 , 而擂鼓台段中 

部的上黏土层与上部为早石炭世早期杜内 

期。泥盆系一石炭系界线位于上、下黏土 

层之间石英砂岩中 ( 狮子口剖面 31 层的顶 

面 ); 擂鼓台段下部与中部之间有一沉积 

间断面 , 有铁质风化壳 , 局部见褐铁矿化 

砾岩层 , 这一间断面是泥盆纪末期大海退 

在本区的反映 ; 巢湖地区五通组并非陆相 

沉积 , 而是一套海相的滨岸相沉积 , 海水 

主要来自北东方向 , 与过去的陆相沉积和 

海侵来自南西方向的论点有所不同。 

2007010504 

扬子区下、中奥陶统大湾组及其同期地层 

= The Lower to Middle Ordovician Dawan 

Formation and its coeval rocks in the Yangtze 

region. ( 中文 ). 陈朋飞 ; 詹仁斌 . 地层学杂 

志 , 2006, 30(1): 11-20 

华南扬子区不同地点奥陶纪的岩相、 

生物相变化显著。下、中奥陶统大湾组及 

其同期地层的总体走向为南西一北东向 , 

横向上呈带状分布 , 从近岸到远岸呈渐变 

过渡。对四川长宁大官山组、贵州桐梓和 

沿河湄潭组以及湖北宜昌大湾组的比较研 

究发现 , 扬子区下、中奥陶统阿仑尼格期 

(Arenig) 的地层按照其离岸的远近 , 在 

地层厚度、沉积相以及腕足动物分异度上 

呈现出规律性的变化。华南早、中奥陶世 

腕足动物的辐射首先发生在处于正常浅海 

底域环境的桐梓和沿河一带。 

2007010505 

贵州台江八郎凯里组层序地层及海平面变 

化初探 = Discussion on the sequence stratigraphy 

and sea-level changes of the Kaili 

Formation at Balang, Taijiang, Guizhou. ( 中 

文 ). 王约 ; 喻羡艺 ; 彭进 ; 王平丽 . 地层学杂 

志 , 2006, 30(1): 34-40 2 图版 . 

贵州台江八郎凯里组以含钙质泥岩 — 

泥灰岩、含钙质泥岩 — 粉砂岩和含钙质泥 

岩 — 灰岩等 3 种韵律性沉积为主 , 沉积体 

系域类型主要包含有大陆边缘体系域、海 

侵体系域和早期高水位体系域。在凯里组 

沉积初期 , 台江地区的水体相对较浅、生 

物相对较少 ; 随着海平面的上升 , 生物在 

分异度和丰度上的大大增加 , 构成了台江 

生物群 ; 当海平面升至最高点时 , 台江沉 

140

积区处于一个相对深水的环境 , 以大量的 

浮游类和较强游泳能力的生物为特征 , 成 

为了凯里生物群的开始 ; 海平面逐渐下 

降 , 浮游生物逐渐减少 ; 至凯里组沉积晚 

期 , 海平面的下降使台江地区的水体再度 

变浅、生物化石相对稀少。在台江八郎剖 

面上 , 凝缩段之下早寒武世的三叶虫 

Bathynotus 消失 ,Oryctocephalus indicus 等 

三叶虫在凝缩段底界出现。凝缩段底界与 

下、中寒武统界线基本一致 , 表明了凝缩 

段是该区下、中寒武统地层划分、对比的 

关键。 

2007010506 

加拿大东部下古生代微动物群的生物地层 

意义 = Biostratigraphic significance of lower 

Paleozoic microfaunas from eastern Canada. 

( 英文 ). Asselin E; Achab A; Soufiane A. Canadian 


489-505 

Chitinozoan studies recently carried out 

in the Appalachian Forelands and St. Lawrence 

Platformo National Geoscience Mapping 

Program (NATMAP) project have confirmed 

the regional biostratigraphic value of a 

number of chitinozoan species and led to a 

better documentation of their stratigraphic and 

geographic distribution in eastern Canada. The 

typical Darriwilian microfaunas first described 

from the Table Head Group of western Newfoundland 

and containing Conochitina chydaea 

are now recognised in the Riviere Ouelle 

Formation at Les Mechins, Gaspe Peninsula. 

In the Upper Ordovician successions of the St. 

Lawrence Platform at Neuville and in the 

Charlevoix area, Quebec, Conochitina primitiva 

is indicative of the multidens-preamericanus 

graptolite zonal range, Hercochitina 

duplicitas of the americanus Zone, 

and Hercochitina spinetum and Acanthochitina 

cancellata characterize the ruedemanni 

- lower spiniferus zonal interval. The occurrence 

of Cyathochitina vaurealensis and Hercochitina 

crickmayi in turbidite deposits of the 

Grog Brook Group of northwestern New 

Brunswick confirms the minimal facies dependence 

of these two Richmondian index 

species. Eisenackitina dolioliformis, characteristic 

of the late Aeronian and Telychian successions 

of Arctic Canada, Gaspe Peninsula, 

and Anticosti Island, is now recognised in 

samples from the Upsalquitch Formation of 

northwestern New Brunswick and the Cabano 

Formation of the Rimouski area in Quebec. 

The palynological data from Devonian successions 

of the Matapedia Valley, the Rimouski 

area, and the Beauce - Eastern Townships region 

show that the succession of Lower Devonian 

chitinozoan assemblages of the Forillon 

Peninsula based on short-ranging species can 

be used in establishing regional correlations in 

the Gaspe Belt. 

2007010507 

加拿大魁北克南部加斯佩带新的地层框架 

及其对加拿大东部前 Acadian 期阿巴拉契 

地质演化的意义 = A new stratigraphic 

framework for the Gaspe Belt in southern 

Quebec: implications for the pre-Acadian Appalachians 

of eastern Canada. ( 英文 ). Lavoie 

D; Asselin E. Canadian Journal of Earth Sciences, 

2004, 41(5): 507-525 

The post-Taconian units in the Quebec 

and northern New Brunswick Appalachians 

constitute the Gaspe Belt and geological studies 

have mostly focussed on its eastern Quebec 

segment. Biostratigraphic data indicate 

that the succession in southern Quebec is no 

older than Late Silurian and extends into the 

Early Devonian. Two distinct stratigraphic 

assemblages are present. The first assemblage 

(Saint-Luc, Cranbourne, and Lac Aylmer formations, 

and Glenbrooke Group) unconformably 

overlies the Humber and Dunnage zones. 

The units show a basal alluvial conglomerate 

that passes progressively to deeper marine 

facies upsection, which have recorded a post- 

Late Silurian transgressive event. The second 

assemblage (Saint-Francis Group and Frontenac 

Formation) is faulted against either Dunnage 

units or autochthonous post-Taconian 

units. It locally unconformably overlies units 

of the Dunnage Zone; the succession shows 

progressively deeper marine conditions upsection 

and also has recorded a post-Late Silurian 

transgressive event. The biostratigraphic 

framework suggests that some of the units that 

were assumed to be vertically stacked are 

rather laterally equivalent. Independant evidence 

supports the hypothesis that the Gaspe 

Belt in southern Quebec formed after the collapse 

of the Taconian orogen in Late Silurian 

time. This event is ascribed to the Salinian 

Orogeny. The framework from southern Quebec 

is incorporated in a regional scenario. The 

Gaspe Belt experienced a Pridolian- 

Lochkovian sea-level rise. In Pragian time, 

shallower marine conditions were established 

in southern Quebec, whereas in the Gaspe 

Peninsula, the shallower conditions only occurred 

in early Emsian time. 

141

2007010508 

加拿大新不伦瑞克北部晚奥陶世至泥盆纪 

Gaspe 带地层和大地构造 - 沉积演化 : 

Restigouche 地区的证据 = Stratigraphy and 

tectono-sedimentary evolution of the Late Ordovician 

to Middle Devonian Gaspe Belt in 

northern New Brunswick: evidence from the 

Restigouche area. ( 英文 ). Wilson R A; Burden 

E T; Bertrand R; Asselin E; McCracken A 

D. Canadian Journal of Earth Sciences, 2004, 

41(5): 527-551 

The Gaspe Belt in the Restigouche area 

comprises three successions separated by a 

Late Silurian (Salinic) disconformity and an 

Early Devonian angular unconformity. The 

lower, Upper Ordovician to Lower Silurian 

sequence consists of siliciclastic turbidites of 

the Boland Brook and Whites Brook formations 

(Grog Brook Group), overlain by calcareous 

turbidites of the Pabos and White 

Head formations (Matapedia Group), and 

slope and shelf deposits of the Upsalquitch 

and Limestone Point formations (lower 

Chaleurs Group). Above the Salinic disconformity, 

the upper Chaleurs Group and the 

Dalhousie Group record a transgressiveregressive 

cycle. The former comprises Pridolian 

carbonate rocks of the West Point Formation 

and overlying Pridolian to Lochkovian 

sedimentary rocks of the Indian Point Formation. 

The Chaleurs Group is conformably 

overlain by Lochkovian to early Emsian 

subaerial volcanic rocks of the Dalhousie 

Group (Val d'Amour Formation), which is 

unconformably overlain by alluvial-lacustrine 

deposits of the late Emsian Campbellton Formation. 

Acadian orogenesis began during the 

Emsian and is characterized by open to closed 

folding, heterogenous cleavage development, 

and reverse and strike-slip faults. The Salinic 

orogeny is manifested in extensional block 

faulting, within-plate volcanism, and uplift 

and deep erosion of Early Silurian strata. 

Early Devonian high-level intrusion of the 

Matapedia Group, White Head clasts in Indian 

Point conglomerate, and thermal maturation 

data all indicate an extended period of Late 

Silurian - Early Devonian uplift in parts of the 

Restigouche area. Thermal maturities of West 

Point and Indian Point strata are within the oil 

and condensate windows and suggest potential 

for hydrocarbons in the study area. 

2007010509 

加拿大魁北克南部下泥盆统 Compton 组 : 

从三角洲前缘到原三角洲沉积 = The Lower 

Devonian Compton Formation in southern 

Quebec: from delta front to pro-delta sedimentation. 

( 英文 ). Lavoie D. Canadian Journal of 

Earth Sciences, 2004, 41(5): 571-585 

The Lower Devonian Compton Formation 

is the uppermost unit of the St. Francis 

Group in the Connecticut Valley - Gaspe synclinorium 

of southern Quebec. The Compton 

Formation is composed of three informal 

members. Five distinct sedimentary facies 

have been recognized in the lower two members 

of the Compton Formation. High-energy, 

shallow-marine, and channel sands dominate 

the Milan member. The overlying Lac Drolet 

member consists of below wave base mud and 

silt deposits with abundant turbidite sand. The 

Milan member is interpreted to represent deposits 

of a river-dominated delta-front environment, 

whereas the Lac Drolet member is 

suggestive of below storm-wave base prodelta 

deposits. The transition from the Milan 

member to the Lac Drolet member is correlated 

with the deepening event recognized in 

coeval succession in the Gaspe Peninsula and 

known as the T2 event. There, the coeval Indian 

Point Formation is interpreted to represent 

pro-delta sediments. The new paleogeographic 

map for the Lochkovian illustrates 

the development of deltaic lobes from northern 

Gaspe to southern Quebec. In Lochkovian, 

deltaic regimes were established in southern 

Quebec and northeastern Gaspe, whereas the 

intervening successions (western Gaspe Peninsula 

- New Brunswick) experienced significant 

synsedimentary tectonic collapse. 

2007010510 

加拿大纽芬兰西部 Anticosti 前陆盆地早泥 

盆世陆相沉积 :Red Island Road 组 = The 

Red Island Road Formation: Early Devonian 

terrestrial fill in the Anticosti Foreland Basin, 

western Newfoundland. ( 英文 ). Quinn L; 

Bashforth A R; Burden E T; Gillespie 

H;,Springer R K; Williams S H. Canadian 


602 

More than 100 m of nearly flat-lying, 

fluvially derived, thick-bedded and lensoid, 

clast-supported conglomerate and sandstone 

are found on Red Island, off the coast of the 

Port au Port Peninsula, western Newfoundland. 

Formally described herein and named Red 

Island Road Formation, the strata represent a 

unique lithologic formation not exposed or 

known anywhere else in the region. Characteristic 

features include abundant, rounded, 

highly weathered and varnished cobbles and 

boulders derived from an unknown mixed 

142

volcanic and very low to low-grade metamorphic 

terrane. Although the unit is largely unfossiliferous, 

a thin sandstone bed near the top 

of the type section contains primitive dichotomously 

branched plant remains and biostratigraphically 

significant palynomorphs. 

Among more than 25 species of spores, it is 

the diversity of Emphanisporites, Dictyotriletes, 

and Dibolisporites, and in particular 

Dibolisporites echinaceus, Dictyotriletes 

canadensis, Emphanisporites annulatus, E. 

erraticus, and E. schultzii that indicate the Red 

Island Road Formation was deposited during 

the early and early late Emsian Emphanisporites 

annulatus - Camarozonotriletes sextantii 

Assemblage Zone. Biostratigraphy places 

age constraints on Acadian tectonism, local 

thrusting, and foreland basin development in 

this part of the Anticosti Basin. The suite of 

clasts indicates a radical shift in provenance as 

compared with siliciclastic units lower in the 

foreland basin sequence. Clearly, the source 

for these clasts is not local. Terranes farther 

afield, such as the La Poile Group in southwestern 

Newfoundland, should be examined 

as possibilities for the provenance of these 

rocks. 

2007010511 

塔里木盆地麦盖提斜坡西段上石炭统研究 

新进展 = Novel progress of Upper Carboniferous 

study in west section of Mageti slope, 

Tarim Basin. ( 中文 ). 张现军 ; 王月华 ; 玛丽克 ; 

曾昌民 ; 冯晓军 ; 韩利军 ; 曲东峰 . 新疆石油地 

质 , 2006, 27(1): 56-58 

通过麦盖提斜坡西段上石炭统对比研 

究发现 , 该区石炭系内部存在两个重要的 

不整合面 : 一个不整合面位于二叠系南闸 

组与石炭系小海子组大套灰岩内 , 该不整 

合面在覆盖区不仅具有明显的岩电特征 , 

而且还具有重要的控油作用 ; 另一个不整 

合面在麦盖提斜坡西段石炭系卡拉沙依组 

顶部 , 是一个大的区域不整合面 , 推测该 

不整合面是受晚石炭世海退作用及构造运 

动共同影响的结果。 

2007010512 

右江盆地二叠纪生物礁时空分布和沉积构 

造演化新知 = Recent approach to space-time 

distribution and sedimentary structural evolution 

of Permian reef in Youjiang Basin. ( 中文 ). 

陆刚 ; 胡贵昂 ; 张能 ; 张耿 ; 潘艺文 ; 彭阳 . 地质 

论评 , 2006, 52(2): 190-197 1 图版 . 

笔者等在右江盆地开展的 1:5 万区域 

地质调查工作中 , 研究了二叠纪海绵礁、 

藻礁的分布、时代、岩石类型、发育特征 

及发展演化 , 取得了新的认识 , 认为沿大 

小台地边缘断续发育的礁滩相沉积 , 是一 

套具有成因联系、密切相关的广义礁灰岩 

组合 ; 礁灰岩主要形成于高水位期 ; 成礁 

时代始于早二叠世紫松期晚期 , 并一直延 

续至晚二叠世末 , 划分为三个造礁期。完 

整连续、环状的礁滩相带及台缘沉积岩墙 

群、假不整合构造的分布、发育特征 , 证 

明右江盆地从泥盆纪至三叠纪是连续发育 

的沉积海盆 ; 包含于三叠系中的晚古生代 

地层是孤立碳酸盐台地沉积 , 是原地系 

统 , 而非后期推覆构造形成的无根异地系 

统。 

2007010513 

西班牙西南部 Pendleian( 早谢尔普霍夫 

世 ) 海相碳酸岩 : 沉积岩、生物地层和沉 

积模式 = Pendleian (early Serpukhovian) marine 

carbonates from SW Spain: sedimentology, 

biostratigraphy and depositional model. 

( 英文 ). Cozar P; Rodriguez S. Geological 

Journal, 2004, 39(1): 25-47 

The San Antonio-La Juliana tectonosedimentary 

unit contains the only Namurian 

marine carbonates in the southwestern part of 

the Iberian Peninsula. The analysis of this unit 

is fundamental in understanding the sedimentary 

evolution and tectonic movements which 

operated during the Namurian in this area. 

Using foraminifera the succession has been 

assigned to two biozones (Zones 17 and 18), 

both occurring in the Pendleian (early Namurian). 

Seven stratigraphic sections have 

been analysed: San Antonio, Burjadillo, 

Lavadero de la Mina, Cornuda, Lozana, Caridad 

and Via Crucis. The stratigraphic succession 

of the San Antonio-La Juliana Unit consists 

of olistolites in the basal part, with common 

debris-flow deposits (mainly of carbonates, 

with minor siliciclastic rocks), and turbidites, 

all of them embedded in shales. These 

rocks, interpeted as slope deposits, pass up 

into shallow-water platform facies, with sediments 

characteristic of the inner platform and 

tidal flats. Above these rocks, terrigenous deltaic 

deposits occur. Thus, the stratigraphic 

sections show an overall shallowing-upward 

trend. The isolation of some outcrops, and the 

duplication and absence of some parts of the 

stratigraphic succession are explained by tectonic 

movements. Overall, tectonic factors 

seem to be the main control rather than glacio- 

143

eustatic or autocyclic processes, and sedimentation 

took place in a strike-slip regime. 

2007010514 

下古生界化石库印痕化石碳稳定同位素的 

组成 = Stable carbon-isotope compositions of 

compression fossils from Lower Paleozoic 

Konservat-Lagerstätten. ( 英文 ). Duca S T L; 

Pratt L M. Palaios, 2002, 17(3): 287–291 

Taxon-specific stable carbon-isotope ratios 

were determined for 7 graptolite (consumer) 

and 4 alga (primary producer) taxa 

preserved as thin organic compressions within 

North American Silurian Konservat- 

Lagerstätten. Values range from −26.6‰ for a 

graptolite from the Goat Island Formation, 

New York, to −32.3‰ for an alga from the 

Cape Phillips Formation, Arctic Canada. Cooccurring 

graptolite taxa display nearly identical 

δ 13 C compositions (within 0.2‰). Algal 

taxa co-occurring with graptolite taxa have 

δ 13 C compositions which are 1–2‰ more 

negative than those of associated graptolites. 

The observed isotopic offset between associated 

graptolites and macroalgae, both of which 

are common sources of organic matter in Paleozoic 

strata, holds implications for the interpretation 

of time-series δ 13 C org curves, and 

suggests that stable carbon-isotope composition 

could serve as a chemosystematic tool for 

discerning the affinities of organic macrofossil 

problematica. 

2007010515 

单一岩性地层的高分辨率对比 : 辛辛那提 

地区上奥陶统 Kope 组 = High-resolution 

correlation in apparently monotonous rocks: 

Upper Ordovician Kope Formation, Cincinnati 

Arch. ( 英文 ). Holland S M; Meyer D L;Miller 

A I. Palaios, 2000, 15(1): 73-80 

Short stratigraphic sections in apparently 

monotonous strata pose several challenges to 

high-resolution (

ing in pulsatory or intermittent uplifts and 

short periods of tectonic quiescence. Conglomerates 

(allochthonus faunas) and black 

shales (autochthonous faunas) are the most 

important rocks of these two tectonic moments. 

This subphase spans the N. gracilis to 

C. bicornis Zones. 

2007010517 

晚、中、早、遗迹寒武纪 : 寒武纪四分的 

世的易于交流的专门术语 = 

Late/Middle/Early/Ichnocambrian: a communication-friendly 

nomenclature for the epochs 

of a quadripartite Cambrian Period. ( 英文 ). 

Rowland S M; Hicks M. Episodes, 2006, 

29(2): 128-129 

The International Subcommission on 

Cambrian Stratigraphy has voted to abandon 

the traditional tripartite subdivision of the 

Cambrian Period in favor of a quadripartite 

structure. Each of the four newly defined epochs 

will be assigned a name based on the 

location of the GSSP that defines the base of 

its basal stage. We do not question the biostratigraphic 

appropriateness of subdividing 

the Cambrian Period into four epochs rather 

than three, however we argue that it is unnecessary 

and unwise to completely abandon the 

widely used, easily remembered, relativeposition-specific 

names Early, Middle, and 

Late Cambrian. We propose a simple epoch 

nomenclature, which retains the familiar 

names for the intervals of strata to which they 

have traditionally been applied, and adds just 

a single, new, easily-remembered name - Ichnocambrian 

- for the ichnofossil-defined, pretrilobite-bearing 

portion of the Cambrian. 

2007010518 

东秦岭古生代生物古地理 = Biopalaeogeography 

of the Paleozoic in East Qinling 

Mountains. ( 中文 ). 裴放 ; 王凌云 . 古地理学 

报 , 2006, 8(1): 1-16 

秦岭褶皱带位于华北板块和扬子板块 

结合部位 , 其在河南省内的部分多划为东 

秦岭。东秦岭以商南 - 镇平缝合带分为东秦 

岭北部和东秦岭南部。东秦岭古生代生物 

古地理演变可以划分为 6 个阶段。在寒武 

纪至中奥陶世早期 , 东秦岭北部二郎坪海 

槽的寒武纪放射虫和早奥陶世牙形石与东 

秦岭南部淅川陆棚北部的寒武纪三叶虫、 

早奥陶世牙形石和头足类属华南生物省 , 

而淅川陆棚南部的寒武纪三叶虫和早奥陶 

世牙形石属于华南生物省 , 兼有华北生物 

省分子。在中奥陶世晚期至奥陶纪末 , 二 

郎坪海槽的腹足类、头足类和珊瑚与淅川 

陆棚的牙形石、珊瑚、腕足类、头足类和 

三叶虫均属华北生物省。在早志留世 , 二 

郎坪海槽的珊瑚与淅川陆棚的笔石属华南 

生物省。在中志留世至早泥盆世 , 东秦岭 

未发现古生物化石 , 很可能为陆地 , 并与 

华北陆块联为一体。在中泥盆世至早石炭 

世 , 东秦岭北部柿树园海槽与东秦岭南部 

南湾海槽的孢子及淅川陆棚的晚泥盆世珊 

瑚、腕足类和古植物及早石炭世蜓属华南 

生物省。晚石炭世至二叠纪末 , 柿树园海 

槽的孢子见于华北生物省 , 东秦岭南部缺 

乏海相沉积。总之 , 在古生代 , 东秦岭经 

历了由华南生物省 → 华北生物省 → 华南生 

物省 → 华北陆 → 华南生物省 → 华北生物省 6 

个阶段 , 组成 3 个演变旋回。东秦岭北部 

和南部生物古地理具有明显的演变方向的 

统一性和演变时间的相似性。 

2007010519 

新甘交界北山地区早二叠世红柳河群的建 

立 = Establishment of the Early Permian 

Hongliuhe Group in the Beishan area on the 

border region of Xinjiang and Gansu,China. 

( 中文 ). 李金宝 ; 康旭 ; 王涛 ; 李伍平 ; 童英 . 地 

质通报 , 2006, 25(4): 465-468 

经 1:5 万区域地质调查研究 , 北山地 

区原红柳河组规模巨大 , 岩性、岩相差异 

明显 , 按岩石地层划分原则 , 应进一步分 

组。原红柳河组内部有 4 套岩性、岩相差 

异较大的岩石组合 , 以 3 次砾岩事件和 1 

次火山岩事件为标志 , 代表了 4 个不同的 

沉积阶段 , 与之对应出现了 4 个重要的沉 

积 ( 不整合 ) 界面。依据这 4 个界面对早 

二叠世红柳河组进行了重新划分 , 即下二 

叠统河西组 (P 1 h)、红柳村组 (P 1 hl)、 

芦苇井组 (P 1 l) 和红柳井组 (P 1 hj)。在 

河西组采集到大量的腕足、苔藓虫等海相 

动物化石 , 在芦苇井组第二岩性段舍炭粉 

砂岩中获孢粉化石组合 , 其时代属于二叠 

纪。本区新建的 4 个组实际上是由一个规 

模较大的老组再分组的结果。按岩石地层 

单位修定的要求 , 建议原红柳河组上升为 

群。 

2007010520 

南非陆相二叠系 - 三叠系界线研究进展 = 

Advance in study of terrestrial Permian- 

Triassic boundary in South Africa. ( 中文 ). 彭 

元桥 ; 高勇群 ; 杨逢清 ; 殷鸿福 ;G R Shi. 地质 

科技情报 , 2006, 25(1): 1-8 

145

从岩石地层研究着手 , 介绍了南非卡 

鲁盆地内综合地层研究的相关成果。在生 

物地层方面。脊椎动物和植物化石的研究 

在该区具有传统优势。孢粉化石的研究则 

是在最近几年才取得较大进展 , 在陆相界 

线地层研究中菌孢化石在 2- 叠系 - 三叠系界 

线处约 1m 厚的地层内的富集事件属首次报 

道。在地球化学地层方面 , 南非有机碳同 

位素在二叠系 - 三叠系界线附近的变化趋势 

与海相二叠系 - 三叠系界线地层存在相似的 

对应关系。可以作为海、陆相界线地层对 

比的辅助标志。在磁性地层方面 , 南非卡 

鲁盆地内的磁极性存在从反向到正向然后 

再反转 (R—N—R) 的变化 , 二叠系 - 三叠 

系界线则位于第一反向极性带的顶部。同 

时 , 结合目前全球陆相二叠系 - 三叠系界线 

的研究现状及特点 , 分析了陆相界线地层 

研究中存在的基本问题 , 指出华南地区可 

能为突破传统观念的研究地区 , 陆地事件 

地层研究意义重大。 

2007010521 

西天山阿沙勒河中上游二叠系的发现及环 

境分析 = Discovery of Permian strata along 

middle- upper reaches of Ashale River and its 

environment analysis,western Tianshan. ( 中 

文 ). 黄勇 ; 邓贵标 ; 跃连红 ; 吴滔 . 贵州地 

质 , 2006, 23(1): 20-24 

近年在西天山阿沙勒河中上游的博罗 

霍洛山地层小区新发现陆相二叠系 , 分布面 

积较大 , 其岩石组合及岩相特征与区域上的 

中下二叠统乌郎组相同 , 并采获二叠纪孢粉 

化石 , 这是该地区二叠纪地层古生物工作取 

得的新进展 , 具有重要的研究意义 . 

2007010522 

内蒙古东南部西乌珠穆沁旗地区石炭纪 - 二 

叠纪岩石地层和层序地层 = Carboniferous- 

Permian marine lithostratigraphy and sequence 

stratigraphy in Xi Ujimqin Qi, southeastern 

Inner Mongolia, China. ( 中文 ). 鲍庆 

中 ; 张长捷 ; 吴之理 ; 王宏 ; 李伟 ; 苏养正 ; 桑家和 ; 

刘永生 . 地质通报 , 2006, 25(5): 572-579 

通过 1:25 万区域地质调查 , 对西乌珠 

穆沁旗 - 林西地区石炭纪 - 二叠纪地层进行了 

岩石地层学研究与重新归并划分 , 并进行了 

生物地层、层序地层及不整合面地层的多 

重地层划分与对比 . 研究了测区各地层的基 

本层序、沉积环境和沉积相 , 将石炭纪 - 二叠 

纪地层划分为 3 个沉积层序 , 建立了岩石地 

层和年代地层格架 . 石炭纪 - 早二叠世本巴图 

组 (CPb)、格根敖包组 (CPg) 和阿木山 

组 (CPa) 三者为石炭纪 - 二叠纪西乌珠穆 

沁旗海槽同期异相地层的观点 , 能很好地解 

释这几套地层的相互关系 . 寿山沟组 

(P 1 ss) 地层呈超覆不整合覆于以前地层或 

地质体之上 ; 大石寨组 (P 2 ds) 为达到最大 

海泛面时海 ( 水 ) 下火山喷发的产物 ; 哲斯 

组 (P 2 z) 是海盆地萎缩期的沉积产物 . 

2007010523 

通过 C27/C29 甾烷和有机碳同位素判断早 

古生代及前寒武纪的烃源岩的生物来源 = 

Tht biological origin for Early Paleozoic and 

Precambrian hydrocarbon source rocks based 

on C27/C29 sterane ratio and organic carbon 

isotope. ( 中文 ). 孟凡巍 ; 周传明 ; 燕夔 ; 袁训来 ; 

尹磊明 . in: 杨勇 . 地学与资源研究新进展 . . 

Pages: 241(71-76). 中国石油大学出版社 . 

2006. 7-5636-2235-7. 

在早古生代与前寒武纪的石油与源岩 

中 , 经常出现令人困惑的 C 29 甾烷优势 , 而 

在有机地球化学分析中 C 29 甾烷优势被认为 

是陆相有机质输入的标志。本文通过对比 

文献中各种海洋藻类的热模拟产物分析 , 

提出了早古生代及前寒武纪的石油与源岩 

中 C 29 甾烷优势主要来源于浮游绿藻的观 

点 , 并通过 C 27 甾烷与 C 29 甾烷的比值提出了 

区分早古生代及前寒武纪石油源岩沉积环 

境的方法 , 对中国南方前寒武纪和早寒武 

世黑色岩系的有机地球化学分析也支持上 

述推断。此外 , 本文还提出了用有机碳同 

位素来进一步区分 C 29 甾烷优势生物来源的 

方法。 

2007010524 

青海南部治多 — 杂多地区二叠系阳新统上 

部层位的发现和尕日扎仁组、索加组的建 

立 = Discovery of the upper part of the Permian 

Yanghsinian Series and establishment of 

the Garizaren and Suojia formations in the 

Zhidoi-Zadoi area, southern Qinghai, China. 

( 中文 ). 牛志军 ; 段其发 ; 王建雄 ; 白云山 ; 涂兵 ; 

卜建军 . 地质通报 , 2006, 25(1-2): 176-182 

在青海南部治多 - 杂多一带 1:25 万地 

质填图中 , 发现二叠系阳新统上部层位的 

筵类动物群 , 新建尕日扎仁组和索加组。 

尕日扎仁组以泥质岩、细粒石英砂岩为 

主 , 夹粉砂岩、灰岩、玄武岩 , 属陆棚 

相 , 产少量非筵有孔虫、腕足类、双壳类 

化石 , 地质时代为阳新世孤峰期晚期 , 与 

下伏九十道班组整合接触。索加组分为 2 

个段 , 下段以透镜状滨岸相底砾岩为特 

征 , 上段以合燧石条带及结核的台地相灰 

146

岩为特征 , 产筵类、非筵有孔虫、腕足类 

等 , 地质时代为阳新世冷坞期 , 与下伏尕 

日扎仁组平行不整合接触。 

2007010525 

上扬子区下寒武统的层序地层格架及其形 

成的古地理背景 = Sequence-stratigraphic 

frameworks and their forming backgrounds of 

paleogeography for the Lower Cambrian of 

the Upper-Yangtze region. ( 中文 ). 梅冥相 ; 张 

丛 ; 张海 ; 孟晓庆 ; 陈永红 . 现代地质 , 2006, 

20(2): 195-208 

上扬子区特别是贵州及邻区的下寒武 

统发育完整 , 是一套从黑色页岩系到碳酸 

盐岩的地层序列 , 该序列构成一个复杂而 

有序的层序地层格架。在时问变化方面 , 

下寒武统组成一个二级层序 , 其中可以进 

一步划分为 5 个三级层序 , 形成一个有序 

的海侵一海退旋回序列 ; 在二级层序之 

中 , 三级层序形成一个有序的垂直叠加形 

式 , 自下而上三级层序由 “ 凝缩段 (CS)+ 

高水位体系域 (HST)” 序列演变为 “ 海侵 

体系域 (TST)+ 凝缩段 (CS)+ 高水位 

体系域 (HST)”, 层序界面类型由淹没不 

整合型层序界面演变为明显的暴露间断 

面 , 意味着二级层序的相序组构与三级层 

序存在相似性。在空间变化方面 , 从北西 

向南东随着古地理背景由浅变深 , 下寒武 

统厚度变薄 , 向东南变为一个难以进行三 

级层序划分的凝缩序列。该层序地层格架 

不但表明了三级层序的两大属性 ——“ 空间 

上相序的有序性和时间上环境变化的同步 

性 ”, 而且反映出地层记录中 “ 两种相变面 

和两种穿时性 ”。同时 , 所建立的层序地层 

格架表明了其复杂的古地理背景 ; 具有不 

同特点的三级层序代表了不同的古地理背 

景 , 意味着早寒武世复杂的古地理变迁。 

因此 , 系列层序地层格架栅状图反映出每 

一个三级层序的相序组构的时空变化 , 而 

系列古地理图又代表了各个三级层序形成 

时期的独具特色的古地理背景。 

2007010526 

广西柳桥深水相二叠系 / 三叠系界线剖面 

有机碳同位素地层学对比研究及事件响应 

= Stratigraphy of organic carbon iotope and 

associated events across the Permian/Triassic 

boundary in the Dongpan deep-water section 

in Liuqiao Area, Guangxi, South China. ( 中 

文 ). 张凡 ; 冯庆来 ; 蒙有言 ; 何卫红 ; 顾松竹 . 现 

代地质 , 2006, 20(1): 42-48 

研究了广西柳桥地区东攀剖面有机碳 

同位素的组成 , 并和浙江煤山剖面进行了 

对比。结果表明东攀剖面在 δ 13 C org 变化趋势 

上 , 既具有全球 PTB 剖面普遍存在的共 

性 , 又具有其独特性。在东攀剖面一个显 

著的 δ 13 C org 负漂移出现在事件界线 (EB) 

之上和二叠系 / 三叠系界线 (PTB ) 之 

下 , 这与煤山剖面具有相似性。显著的 

δ 13 C org 负漂移指示了 P/T 之交生物绝灭后 

海水表层水原始生产率的降低以及大气和 

海水中 CO 2 含量的增加 , 并得到放射虫绝灭 

事件、火山事件和海退事件的响应。煤山 

剖面 δ 13 C org 负漂移从第 27 层就开始向 13 C 富 

集的方向恢复 , 而东攀剖面 δ^13Corg 在下 

Induan 阶仍持续亏损 , 表明东攀剖面早三 

叠世的生物复苏明显滞后于煤山剖面的。 

2007010527 

吉林中部地区二叠纪岩相古地理及沉积构 

造背景 = Permian sedimentary facies, palaeogeography 

and tectonic background in central 

Jilin Province, China. ( 中文 ). 杨宝忠 ; 夏文臣 ; 

杨坤光 . 现代地质 , 2006, 20(1): 61-68 

以沉积体系研究为基础 , 综合应用沉 

积岩碎屑物质成分统计、岩石地球化学分 

析等方法 , 详细地研究了吉林中部地区二 

叠纪沉积特征。结合沉积构造背景分析 , 

重建吉林中部地区二叠纪岩相古地理及构 

造古地理。研究发现 : 早 - 中二叠世吉林中 

部地区具活动大陆边缘的复合边缘海盆特 

征 , 早二叠世发育了碳酸盐岩陆架、陆架 

边缘沉积体系及 ( 次 ) 深水盆地沉积体 

系 , 相序具有向上变浅的旋回特征 ; 中二 

叠世初期 , 地壳活动强烈 , 火山发育 , 其 

后沉积了盆缘冲积扇沉积体系、( 次 ) 深 

水盆地沉积体系以及向上变浅的碳酸盐缓 

坡沉积体系等 ; 晚二叠世东北中、小板块 

群与华北板块沿西拉木伦河 - 长春 - 延吉缝合 

带拼合 , 古地理发生重大变化 , 整个地区 

由海相环境转为陆相环境 , 仅局部地区有 

残留的海水 , 发育了湖缘冲积扇、次深湖 

沉积体系。 

2007010528 

内蒙古西部额济纳旗晚奥陶世生物地理和 

奥陶 - 志留系分界 = Late Ordovician biogeography 

and Ordovician-Silurian boundary in the 

Zhusilenhaierhan area, Ejin, western Inner 

Mongolia. ( 中文 ). 戎嘉余 ; 陈旭 ; 詹仁斌 ; 周志 

强 ; 郑昭昌 ; 王怿 . 古生物学报 , 2003, 42(2): 

149-167 1 图版 . 

147

通过最近对内蒙古额济纳旗东南珠斯 

楞海尔罕一带 ( 阿拉善地块 ) 奥陶 - 志留系界 

线地层和生物群的野外调查和室内研究 , 首 

次在上奥陶统上部巴丹吉林组中发现阿什 

极尔中期 (mid Ashgill) 腕足动物化石巨大全 

嘴贝 (Holorhynchus giganteus Kiaer), 这是该 

属在我国奥陶系中的首次记录 . 根据未成年 

个体的切片所发现的腹壳顶端发育中隔板 

构造 , 修订该属定义 , 并证明研究小个体对识 

别物种特征、探讨个体发育和系统演化有 

重要意义 . 分析了全嘴贝属的群落生态、生 

物地理和演化意义后 , 发现它在奥陶纪末大 

灭绝过程中 , 因居群规模和分布范围极大地 

缩减 , 至今未发现其化石记录 ; 但在志留纪初 

环境好转后继续存活 , 可暂视其为复活属 . 根 

据在拐子湖组近底部发现志留系最下部 

Akidograptus ascensus 带的重要分子 

Normalograptus lubricus Chen et Lin, 确定本 

区的奥陶 - 志留系分界 . 阿拉善地块因不发育 

Hirnantia 动物群 , 表明奥陶纪末期它与扬子 

区、西藏、滇西等富含该动物群的地区属 

于不同的生物地理区系 ; 在阿什极尔中期可 

能位于热带海域 , 与祁连山、中亚、乌拉尔 

等地有重要联系 . 文中描记 H. giganteus 种 , 评 

述正常笔石类 (normalograptid) 的系统分类 

位置并描记 N. lubricus 种 . 

2007010529 

皖南震旦纪 - 早寒武世沉积岩有机碳、氮元 

素记录 = Organic carbon and nitrogen records 

in the Sinian-Early Cambrian succession of 

Southern Anhui, China. ( 英文 ). 王金权 . 微体 

古生物学报 , 2003, 20(4): 419-424 

安徽南部晚震旦世蓝田组、皮园村组 

和早寒武世荷塘组主要由黑色页岩和硅质 

岩组成。分析结果表明 , 蓝田组和荷塘组 

的总有机碳 ( 可达 10%-18%) 和总有机氮 

( 可达 2.0‰-2.6‰) 的高含量 , 应归于富 

有机质埋藏所致 , 反映新元古代末次冰期 

后和早寒武世海洋浮游生物处于大发展时 

期。由于海洋植物的光合作用产生大量 

O 2 , 并消耗大量 CO 2 , 导致大气中 O 2 /CO 2 

比率明显增加 , 为震旦纪晚期多细胞真核 

生物的辐射、后生动物的出现和 ‘ 寒武纪生 

物大爆发 ’ 提供了条件。蓝田组黑色页岩中 

部的有机碳与有机氮含量大体呈现正比例 

增加 , 并且分别达到 17.74% 和 2.66‰ 的最 

高值 , 与该剖面发现的蓝田植物群相对 

应 ; 荷塘组黑色页岩的有机碳和有机氮垂 

直分布曲线之间呈现相互背离 , 即有机氮 

含量与时增加 , 而有机碳含量与时减少 , 

与扬子地台相应的地层层位产生的澄江动 

物群相对应 , 表明 TON 和 TOC 分布特征有 

可能与早期生物演化历程相关。 

2007010530 

为加拿大魁北克南部至纽芬兰西部寒武纪 - 

奥陶纪裂陷和被动边缘沉积序列的地层框 

架 = Stratigraphic framework for the Cambrian-Ordovician 

rift and passive margin successions 

from southern Quebec to western 

Newfoundland. ( 英文 ). Lavoie D; Burden E; 

Lebel D. Canadian Journal of Earth Sciences, 

2003, 40(2): 177-205 

The Taconian Humber Zone stretches 

from western Newfoundland to southern Quebec. 

The Early Cambrian slope succession in 

Newfoundland is found in the Curling Group, 

whereas in Quebec, various units were deposited 

during that first time slice. Biostratigraphic 

data allow correlation of the Curling 

Group with the Labrador Group in Newfoundland 

and with the newly time-constrained 

slope succession in Quebec. The end of the 

rift-drift transition is marked by a sea-level 

lowstand at the end of the Early Cambrian. 

The Middle Cambrian to latest Early Ordovician 

passive margin history recorded five cyclic 

sea-level fluctuations. Three of these cycles 

are recorded in the shallow-marine Middle 

to Late Cambrian platform (Port au Port 

Group) and slope sediments preserved in the 

Cow Head and Northern Head groups in Newfoundland. 

The biostratigraphic information 

assists correlation with Cambrian passive 

margin units in Quebec. Major sea-level lowstands 

are recognized along the continental 

margin in early-middle Late Cambrian (Steptoan) 

and in late Late Cambrian (Sunwaptan). 

Even if the Quebec succession can be tied 

with its Newfoundland correlative, some significant 

differences in the nature of Upper 

Cambrian slope conglomerates argue for a 

tectonic control on the depth of erosion of the 

Cambrian continental margin. The Lower Ordovician 

record of the passive margin consists 

of two depositional cycles (Tremadocian- 

Arenigian) separated by a sea-level lowstand. 

This last event is well expressed in platform 

succession and is also recognized in conglomerate 

units found in the slope succession. 

2007010531 

加拿大魁北克西南部蒙特利尔地区 

Beekmantown 群沉积和地层再评估 : 对了 

解加拿大东部下 - 中奥陶统劳伦古陆被动边 

缘的沉积演化的指示意义 = Reappraisal of 

148

the Beekmantown Group sedimentology and 

stratigraphy, Montreal area, southwestern 

Quebec: implications for understanding the 

depositional evolution of the Lower-Middle 

Ordovician Laurentian passive margin of eastern 

Canada. ( 英文 ). Hersi O S; Lavoie D; 

Nowlan G S. Canadian Journal of Earth Sciences, 

2003, 40(2): 149-176 

Detailed lithostratigraphic mapping of 

the Beekmantown Group of southwestern 

Quebec has refined the field application of the 

previously proposed tripartite division of the 

group (i.e., Theresa, Beauharnois, and Carillon 

formations). The group is a peritidaldominated 

succession that accumulated on the 

epicontinental Laurentian passive margin. 

Biostratigraphic data based on conodonts from 

this group indicate an Early to early Middle 

Ordovician age and are partially timecorrelative 

with the Wallace Creek to Naylor 

Ledge strata of the Philipsburg Group, southern 

Quebec. This conodont biostratigraphy 

sheds new light on the temporal evolution and 

depositional framework of the Beekmantown 

platform. The platform evolved as a distally 

steepened ramp during deposition of the 

Theresa Formation and the Ogdensburg Member 

of the Beauharnois Formation (early to 

middle Ibexian). Correlative strata of the Philipsburg 

Group include the Wallace Creek and 

Morgan Corner formations, which represent 

outer platform sediments. The coarse-grained 

sandstone of the Theresa Formation accumulated 

in the innermost platform, whereas 

coarse-grained carbonates of the Ogdensburg 

Member indicate open-marine, subtidal to intertidal 

carbonate sand shoals. By late Ibexian, 

the platform developed a pronounced margin 

where thrombolites flourished under highenergy 

conditions. These are represented by 

the thrombolite-rich Hasting Creek and Naylor 

Ledge formations of the Philipsburg Group. 

Consequently, a broad lagoon formed on the 

lee side of the platform margin, where lowenergy 

conditions prevailed and accumulation 

of burrow-mottled dolostones of the Huntingdon 

Member of the upper Beauharnois Formation 

took place. The lagoon became more restricted 

during the latest stages of the basin fill 

(Whiterockian), and high intertidal to supratidal 

sediments of the Carillon Formation 

were deposited. 

2007010532 

内蒙古苏里格庙地区晚古生代层序地层学 

研究 = Sequence stratigraphy of Late Palaeozoic 

deposits in Suligemiao area, Inner Mongolia. 

( 中文 ). 李文厚 ; 屈红军 ; 魏红红 ; 陈全红 ; 

刘锐娥 ; 赵虹 . 地层学杂志 , 2003, 27(1): 41- 

44 

通过岩心观察 , 结合测井曲线和地震反 

射资料分析 , 并根据层序地层和层序界面的 

识别标志 , 建立了苏里格庙地区的层序地层 

格架 , 并将上古生界划分为 3 个二级层序 

( 超层序组 ) 和 15 个三级层序 , 其中本溪组 

和太原组的层序具二元体系域结构 , 即由海 

进体系域和高位体系域组成 ; 山西组、石盒 

子组和石千峰组的层序具三元体系域结构 , 

包括低位体系域、湖进体系域和高位体系 

域。剖析了陆表海浅陷沉积、陆表海碳酸 

盐岩与碎屑岩混合沉积及近岸内陆河流 — 

三角洲 — 湖泊沉积超层序组 ( 或层序组 ) 中 

层序的发育特征 , 论述了层序的演化过程。 

2007010533 

雪峰古陆边缘上石炭统陆源碎屑和碳酸盐 

混合沉积 = The Upper Carboniferous mixed 

siliciclastic and carbonate sediments on the 

margin of the Xuefeng Ancient Land. ( 中文 ). 

张雄华 . 地层学杂志 , 2003, 27(1): 54-56,58 

湖南沅陵雪峰古陆边缘上石炭统主要 

包括下列岩相类型 : 冲积扇砂砾岩相、前滨 

海滩砂岩相、浅滩碳酸盐相及混积岩相、 

潮下碳酸盐岩相及滩后局限碳酸盐岩相。 

通过沉积相分析和古岩溶面的确定 , 在该区 

上石炭统中共划分出 13 个海侵海退旋回及 

5 个三级层序。对上石炭统中发育的混积岩 

也进行了讨论。 

2007010534 

滇西南耿马弄巴地区南皮河组层型剖面地 

层层序、时代的重新认识 = New knowledge 

about stratigraphic sequence and age of the 

Stratotype section of the Nanpihe Formation 

in the Longba area,Gengma, Southwest Yunnan. 

( 中文 ). 段向东 ; 张志斌 ; 冯庆来 ; 王伟 ; 李 

宗亮 ; 杨仕潘 ; 张凡 . 地层学杂志 , 2003, 27(1): 

59-64 1 图版 . 

对前人建立的上二叠统南皮河组的层 

型剖面 —— 弄巴剖面进行了详细研究 , 发现 

该地层属于一套被动大陆边缘浊积岩为主 

的沉积岩系 , 可概括为四种层序类型特征 : 

一为代表浊流沉积的鲍马序列 ; 二为由泥质 

岩与岩屑石英 ( 杂 ) 砂岩透镜体 ( 层 ) 构成的 

水道沉积序列 ; 三为由薄层状砂岩与泥岩呈 

韵律状互层构成的浊流远端低密度流序列 ; 

四为薄层状硅质岩与硅质泥岩呈韵律状组 

成的基本层序。该组中采获了低等蕨类植 

物、牙形石和笔石等化石 , 证实其时代属于 

149

早泥盆世 — 晚泥盆世。根据该地层的岩性 

组合、沉积环境等特征及区域对比 , 应归于 

泥盆系温泉组。 

2007010535 

重庆秀山寒武纪海相碳酸盐的锶同位素组 

成及其地层学意义 = Strontium isotope composition 

of the Cambrian Luojiaguo section in 

Xiushan, Chongqing and its stratigraphic significance. 

( 中文 ). 石和 ; 黄思静 ; 沈立成 ; 张萌 . 

地层学杂志 , 2003, 27(1): 71-76 

锶同位素地层学是化学地层学的组成 

部分 , 简要介绍重庆市秀山县溶溪乡罗家沟 

寒武系剖面海相碳酸盐的锶同位素分析结 

果 , 建立了该剖面的锶同位素演化曲线 , 并 

与 Gao 及 Denison 等的同期锶演化曲线作 

了对比 , 秀山寒武纪锶同位素演化曲线与其 

他两条同期曲线有较大相似性 , 据此提出了 

秀山寒武系剖面部分主要年代地层界线的 

参考意见 , 并简述了寒武纪全球海平面变化 

的概况。 

2007010536 

国际泥盆系亚阶研究的进展 = Progress in 

the study of global Devonian Substages. ( 中 

文 ). 王成源 . 地层学杂志 , 2003, 27(1): 77-79 

2007010537 

论上扬子区南部中奥陶统大沙坝组 = Remarks 

on the Ordovician Dashaba Formation 

of South China. ( 中文 ). 詹仁斌 ; 程金辉 . 地层 

学杂志 , 2003, 27(2): 109-115 

中奥陶统上部大沙坝组的命名地点在 

四川长宁双河附近 , 岩性以泥质粉砂岩、粉 

砂质泥岩为主 , 夹钙质结核和灰岩透镜体 , 分 

布在川东南的长宁 — 兴文 — 叙永 — 古蔺一 

带 , 其中笔石和壳相化石经常交互出现 , 均比 

较丰富 ; 笔石动物属于上层下垂对笔石动物 

群 ( Didymograptus artus Fauna), 据此 , 大沙 

坝组的地层时代可定为中奥陶世达瑞威尔 

期 ( 相当于兰维恩期 ); 腕足动物可称作 

Saucrorthis- Parisorthis 动物群。大沙坝组的 

岩性和其中所含的动物群均明显有别于在 

黔北和黔东北广泛分布的、大致同期的以 

钙质泥岩和钙质粉砂岩为主的十字铺组。 

四川北部平武县水柏乡的中元古代大沙坝 

组 , 由于命名在后 , 应予以废弃。 

2007010538 

大别造山带北缘石炭系胡油坊组砾石特征 

及其构造意义 = Gravel features and tectonic 

implication in the Carbonifereous Huyoufang 

Formation on the northern margin of Dabie 

Orogenic Belt. ( 中文 ). 李双应 ; 李任伟 ; 岳书 

仓 ; 王道轩 ; 刘因 ; 孟庆任 ; 金福全 . 地层学杂 

志 , 2003, 27(2): 116-121 1 图版 . 

大别造山带北缘晚石炭世胡油坊组内 

含有一套岩块砾岩层 , 砾石主要由绿片岩相 

的石英片岩、绢云母石英片岩、石英岩和 

千枚岩组成 , 其次有变余砂岩和碳酸盐岩 

等。Rb- Sr 同位素测定表明 , 绿片岩相砾石 

经历了晚元古代末期和晚古生代两期变质 

事件 , 全岩等时线年龄为 565±30Ma 和 

307Ma。变质岩砾石不是来源于佛子岭群 

或信阳群 , 而可能来自于扬子陆块的中、晚 

元古代地层。砾石以及古生物的证据还表 

明 , 大别山在古生代时存在一个主要由扬子 

陆块早古生代碳酸盐岩和中、晚元古代变 

质岩组成的构造剥露区 , 不存在一个大别山 

古岛弧。 

2007010539 

太原西山上二叠统陆相地层的磁组构学研 

究 = A magnetic fabric study of the Upper 

Permian terrestrial strata in Xishan of Taiyuan, 

Shanxi. ( 中文 ). 刘育燕 ; 朱宗敏 ; 林文姣 ; 邓胜 

徽 ; 刘本培 ; 桂仁菊 ; 郑宏瑞 . 地层学杂 

志 , 2003, 27(2): 134-137 

对太原西山剖面上石盒子组 1 段至孙 

家沟组的 111 块定向标本所进行的磁组构 

学研究表明 , 其磁化率各向异性参数的主体 

特征为 : 磁化率介于 200—350 ( 10 - 6 SI) 之 

间 ; 各向异性度 ≥1.0 3, 各向异性明显 ; 压扁率 

>1, 磁化率各向异性数值椭球呈弱压扁型 ; 

磁面理度 > 磁线理度 , 磁面理发育 ; 磁面理倾 

角 ∠ 24°, 倾向多变 , 但沿纵向具向南趋势 ; 

磁面理置信角 ∠ 25° 。上述磁化率各向异性 

参数的沉积地层学意义为 : 自上石盒子组 1 

段至孙家沟组 , 沉积相为水流方向自由迂回 

摆动的曲流河相 , 沉积环境为地势平坦的冲 

积平原 ; 孙家沟组成岩之末 , 地形略呈北高 

南低之势 , 当时最近的海岸线位于太原之 

南。 

2007010540 

甘 ( 肃 ) 新 ( 疆 ) 交界地区的石炭系和二叠系 — 

— 兼论金窝子金矿围岩地层的时代 = The 

Carboniferous and Permian of the Gansu- 

Xinjiang border area with remarks on the age 

of the surrounding strata of the Jinwozi Gold 

Ore. ( 中文 ). 廖卓庭 ; 刘陆军 . 地层学杂 

志 , 2003, 27(3): 163-172 

通过对甘新交界地区 3 条石炭系和二 

叠系代表剖面的观察 , 结合多年调查东疆地 

150

层的资料积累 , 认为 :1) 因绿条山组岩性组合 

及所含生物群与东疆的东古鲁巴斯套组相 

同 , 甘新交界地区绿条山组分布区是北塔山 

地层小区石炭系的南延部分 , 应从黑鹰山地 

层小区分出 , 甘新交界地区的中南部普遍缺 

失杜内期沉积 ;2 ) 阿齐山 — 康古尔 — 雅满苏 

火山岛弧带与博格达 — 哈尔里克火山岛弧 

带的构造造山历程不同 , 彼此的兴衰转换存 

在一定的时间差 ; 3) 甘肃北山石炭纪生物群 

与天山一级地层区的生物群相似 , 具有特提 

斯区系和西伯利亚 — 北美区系相互交会、 

混生的过渡性质 ; 4 ) 来自兴蒙海槽的早二叠 

世海侵 , 未波及北疆地区 , 而是经由北山、红 

柳河谷地 , 终止于库姆塔格沙垄以东的狭小 

区域 , 根据雅满苏西大沟阿瑟尔期蜓类化石 

的发现 , 推断至今从未发现早二叠世蜓类化 

石的北山 , 主要原因是调查程度较低 ; 5 ) 在 

金窝子金矿、210 金矿及 230 矿脉附近找到 

许多早二叠世生物化石 , 对仅根据一个同位 

素年龄数据 ( 36 1.1Ma) 建立的 “ 金窝子组 ” 

提出质疑 , 否定区内存在泥盆纪地层 , 认为金 

窝子金矿围岩地层的时代是早二叠世 , 不是 

晚泥盆世。 

2007010541 

新疆和田地区志留系 — 中泥盆统塔里其组 

的建立 = The Silurian—Middle devonian 

Taliqi Formation in Hetian, Xinjiang. ( 中文 ). 

贺振建 ; 边雪梅 ; 修申成 ; 蒋光秀 ; 贾凤华 . 地层 

学杂志 , 2003, 27(3): 242-246,263 

塔里其组系从新疆塔里木地层区铁克 

里克地层分区棋盘地层小区古元古界埃连 

卡特群中独立出来的一个新组 , 为一套灰绿 

色的浅变质岩系 , 厚度较大 , 横向分布稳定。 

与上覆地层上泥盆统奇自拉夫组或上石炭 

统卡拉乌依组、阿孜干组呈不整合或断层 

接触 ; 底界未见出露 , 但根据其为和田推覆体 

最下部的一套地层 , 与下伏的准原地系统应 

为断层接触。该组中新发现有孢粉化石 , 并 

结合岩性特征、Rb- Sr 等时线法测年等资 

料及野外观测 , 将其时代定为志留纪 — 中泥 

盆世 . 

2007010542 

上奥陶统底界全球辅助层型剖面在我国的 

确立 = Global auxiliary stratotype section of 

the Upper Ordovician in China. ( 中文 ). 陈旭 ; 

王志浩 . 地层学杂志 , 2003, 27(3): 264-265 1 

图版 . 

2007010543 

论海南岛地区志留系 = On the Silurian strata 

of the Hainan Island area,China. ( 中文 ). 曾庆 

銮 ; 李志宏 ; 谢才富 ; 傅太安 ; 张淼 . 地层学杂 

志 , 2003, 27(4): 267-275 

海南岛志留系以往被划分为上、中、 

下三个统。志留系之上是南好组 , 其层位以 

往被确定为下石炭统岩关阶 , 并认为它与其 

下的上志留统足赛岭组呈不整合接触。最 

近在南好组选层型剖面发现早志留世特里 

奇期晚期 (L ate Telychian) 的 Xinanospirifer 

腕足动物群和三叶虫 Latiproetus cf. atilimbatus 

(Grabau) , 重新论证了以往被确认为中 

志留统靠亲山组所产的腕足类、三叶虫和 

珊瑚化石其实都是特里奇期早至中期的分 

子。现在以无可争辩的事实证明了久归于 

下石炭统岩关阶南好组 , 以及其下的、以往 

被确定为上志留统足赛岭组、中志留统靠 

亲山组等所谓两个构造层的地层都应改归 

于下志留统 (L landovery Series)。北区下志 

留统仅有鲁丹期中期至爱隆期早期的黑色 

碳质页岩相和泥页岩相沉积 , 未发现任何大 

化石。南区下志留统发育较全 , 为细至中粗 

粒碎屑岩相夹碳酸盐岩相沉积 , 产丰富介壳 

相各门类化石 ; 当时该区所生存的动物群与 

扬子区早志留世的关系非常密切 , 并在早志 

留世末期与扬子区大部分地区一样上升为 

陆 , 表明海南岛地区在当时属于扬子地台区 

范畴。 

2007010544 

浙江江山寒武系碳酸盐岩碳氧同位素特征 

及其古环境意义探讨 = A probe into the carbon 

and oxygen isotopic characteristics of the 

Cambrian carbonate rocks in Jiangshan,Zhejiang 

and its paleo-environment significance. 

( 中文 ). 郭福生 ; 彭花明 ; 潘家永 ; 杜 

杨松 ; 刘林清 ; 罗能辉 ; 饶明辉 ; 王正其 . 地层学 

杂志 , 2003, 27(4): 289-297 

对浙江江山碓边下寒武统上部 — 下奥 

陶统下部碳酸盐岩进行了碳氧同位素测 

定。δ 13 C、δ 18 O 值变化范围和均值分别为 - 

1.9‰~3.7‰、-13.0‰~- 1.3‰ 和 0.86‰、- 

9.76‰。碳氧同位素地层曲线与 Veizer et 

al.(1986 ) 的同位素年代演化曲线形状相似 , 

在寒武纪 — 奥陶纪界线附近没有明显的 

δ 13 C、δ 18 O 漂移现象。δ 13 C 地层曲线具旋回 

性变化特征 , 大陈岭组、杨柳岗组各形成一 

个完整的演化旋回 , 与根据露头层序地层研 

究推测的海平面变化曲线吻合性较好 , 表现 

出 δ 13 C 值的高值区是海盆水体变深的反 

151

映。一个明显的碳同位素正漂移发生于晚 

寒武世早期 ( 华严寺组下部 ), 与 Matthew et 

al.(2000 ) 报道的在美国内华达州中东部、 

哈萨克斯坦 Malyi Karatau 地区、澳大利亚 

昆士兰州西北部和湘西桃源瓦儿岗等地发 

现的 δ 13 C 正漂移记录 (SPICE— The Steptoean 

Positive CarbonIsotope Excursion) 和 

Veizer et al.(1986 ) 碳同位素年代演化曲线 

中的正漂移波峰一致 , 为晚寒武世全球性碳 

同位素正漂移提供了一个佐证。 

2007010545 

华南上扬子区早 - 中奥陶世疑源类古环境意 

义 = Palaeoenvironmental significance of the 

early—middle Ordovician acritarchs from the 

Upper Yangtze platform,South China. ( 中文 ). 

李军 ;T Servais; 燕夔 . 地层学杂志 , 2003, 

27(4): 298-305 

对上扬子区 7 个剖面早 — 中奥陶世疑 

源类研究表明 , 这些疑源类组合在分异度及 

属种组成上呈现有规律的变化 , 这种变化是 

上扬子区古环境变化的反映。在上扬子区 

西部 , 近岸碎屑岩相沉积的滇东红石崖组所 

产疑源类组合分异度低 , 为个体较小、壳饰 

较简单的分子 ; 上扬子区中部 , 以黔北湄潭组 

为代表的浅海相碎屑岩和灰岩沉积中 , 疑源 

类分异度较高 , 并出现许多个体较大、壳饰 

较复杂的分子 ; 而在上扬子区东部鄂西宜昌 

大湾组陆棚相灰岩与泥岩中 , 疑源类分异度 

继续增高 , 其中个体大、具粗大、长而复杂 

突起的分子占优势。 

2007010546 

阿根廷胡胡伊卡加斯山 Lampazar 组寒武 

纪最晚期三叶虫 : 生物地层和古环境意义 

= Latest Cambrian trilobites from the Lampazar 

Formation (Cajas Range, Jujuy, Argentina). 

biostratigraphic and paleoenvironmental 

implications. ( 其他 ). Tortello M F; Esteban S 

B. Ameghiniana, 2003, 40(3): 323-344 

The Lampazar Formation is well exposed 

in the northern part of Cajas Range, at the 

Azul and Llama Creeks (Jujuy, Eastern Cordillera, 

Argentina). It is mainly composed of 

shales and subordinate sandstones representing 

an outer shelf setting with some transitions 

to shallower environments. Oxygen and energy 

levels were not uniform during deposition: 

fine grained sediments vary from laminated 

black and dark grey shales (Facies 1 and 

2) in the lower part of the formation to laminated 

greenish shales (Facies 3) with intercalations 

of siltstones and sandstones (Facies 4-7) 

in the middle and upper parts. The unit contains 

the trilobites Lotagnostus (Distagnostus) 

sp., Gymnagnostus bolivianus (Hoek in 

Steinmann and Hoek), Gymnagnostus perinflatus 

(Harrington and Leanza), Micragnostus 

vilonii Harrington and Leanza, Pseudorhaptagnostus 

(Machairagnostus) tmetus Harrington 

and Leanza, Pseudorhaptagnostus 

(Machairagnostus) corrugattus (Suarez- 

Soruco), Akoldinioidia sp., Parabolina 

(Neoparabolina) frequens argentina (Kayser), 

Angelina hyeronimi (Kayser), Parabolinella 

coelatifrons Harrington and Leanza, Beltella 

ulrichi (Kayser), Plicatolina scalpta Harrington 

and Leanza, and Asaphellus cf. aspinus 

Robison and Pantoja-Alor. Some agnostoids 

previously described from the Azul Creek are 

revised here. Trilobites are assignable to the 

lower part of the Parabolina frequens argentina 

Biozone (Pseudorhaptagnostus- 

Gymnagnostus subzone; latest Cambrian). 

Olenid-agnostoid assemblages are especially 

diverse in dark shales, corroborating the suggestion 

that these faunas were especially 

adapted to low-oxygen-water bottom conditions. 

The Lampazar Formation in Cajas 

Range is correlated with the lower part of the 

Volcancito Formation (Famatina Range). 

2007010547 

滇东南地区泥盆纪层序地层格架及海平面 

变化 = The stratigraphic framework of Devonian 

sequence and sea level changes in Southeast 

Yunnan. ( 中文 ). 章正军 ; 丁俊 ; 侯蜀光 ; 钟 

维敷 . 云南地质 , 2003, 22(2): 131-141 

根据精细岩相分析 , 在滇东南泥盆纪台 

地及台地边缘沉积区识别出 9 个三级层序 , 

而在深水盆地沉积区仅能识别出 3 个三级 

层序。结合海平面波动及构造作用分析 , 认 

为在台地或台地边缘沉积区 , 能划分出的层 

序在盆地中难以一一对应的原因是 : 掀斜拉 

伸作用导致下沉一侧的沉降速度总大于海 

平面的下降及沉积速率 , 而保持盆地深水沉 

积体系的沉积特点或海侵沉积特点 , 或是以 

饥饿性盆地性质出现 , 以致形成的沉积层序 

相对较少。三级及三级以上 ( 高频沉积层序 ) 

沉积层序的形成主要受区域构造作用影响 , 

因构造活动强度的差异而难以进行大区域 

对比 , 同一层序界面在不同地区表现出不同 

的性质。 

2007010548 

云南泸沽湖畔石炭系 - 二叠系生物地层再研 

究 = A further study on the Carboniferous- 

Permian biostratigraphy beside Lugu 

152

Lake,Yunnan. ( 中文 ). 董致中 . 云南地 

质 , 2003, 22(2): 200-205 

着重讨论泸沽湖畔相当于石炭系 ( 三分 ) 

上统马平阶地层的划分和对比。认为其大 

部属于我国二叠系 ( 三分 ) 的下二叠统紫松阶 

( 阿瑟尔阶 ~ 萨克马尔阶 ), 上部的硅质页岩 

已进入隆林阶 ( 亚丁斯克阶 )。根据岩性特征 

及古生物混生现象 , 推测除顶部外 , 大部为斜 

坡相沉积。其中的部分生物应是再沉积产 

物。 

2007010549 

四川江油石炭纪锶同位素曲线 —— 年代地 

层对比和海平面变化 = Sr isotope curve 

from the Carboniferous section in Jiangyou,Sichuan:Chronostratigraphic 

correlation 

and sea level changes. ( 中文 ). 石和 ; 黄思静 ; 

赵鹏肖 . 地质通报 , 2003, 22(2): 113-117 

据从采自四川江油马角坝石炭系剖面 

中的未蚀变海相岩石样品中获得的 22 个锶 

同位素测试数据 , 建立了剖面的石炭纪锶同 

位素演化曲线。马角坝剖面的锶同位素曲 

线与我们在贵州惠水、Denison 等在北美建 

立的同时代锶同位素曲线总体上是一致的 , 

表明了锶同位素曲线对海相地层进行年代 

地层划分对比的重要性。根据对比结果 , 讨 

论了马角坝石炭系剖面的年代地层划分和 

海平面变化。 

2007010550 

甘肃北山红石山地区发现早古生代奥陶纪 

地层 = Discovery of Early Paleozoic Ordovician 

strata in the Hongshishan area,Beishan 

Mountains,Gansu,China. ( 中文 ). 赵彦庆 ; 刘明 

强 ; 张万仁 ; 代文军 . 地质通报 , 2003, 22(3): 

215-215 

在甘肃北山红石山以北的中蒙边境一 

带 , 前人工作成果表明 1, 只出露晚古生代地 

层 , 即最老地层为泥盆系雀儿山群 . 该群为一 

套富产腕足类、珊瑚等化石的碎屑岩及中 - 

酸性火山岩夹碳酸盐岩沉积 . 其下部以中 - 酸 

性火山熔岩及火山碎屑岩为主 , 夹钙质砂岩 

及少许灰岩 ; 上部以砂岩、板岩为主 , 夹中酸 

性火山熔岩及砂质大理岩、泥灰岩 . 未见 

顶、底 . 在碧云泉西北 - 双沟山一带 , 几乎全 

变为酸 - 中基性火山熔岩及火山碎屑岩 . 

2007010551 

西藏中南部雄马 — 措麦以南地区早、中二 

叠世地层及其意义 = Early and Middle Permian 

strata in the area south of Xungma- 

Comai in south-central Tibet and their significance. 

( 中文 ). 袁健芽 ; 李晓勇 ; 徐银保 ; 邹爱 

建 ; 欧阳克贵 ; 肖业斌 . 地质通报 , 2003, 22(6): 

412-418 

在西藏中南部雄马 — 措麦以南地区前 

人所定的属于中 — 晚侏罗世达雄群中采获 

了古生物化石 , 地层时代重新厘定为早 — 中 

二叠世。早二叠世早期拉嘎组中赋含重力 

滑塌块体和冰川漂砾 , 早二叠世晚期昂杰组 

碎屑岩中夹大量火山岩 , 中二叠世下拉组含 

大量火山岩碎屑等 , 与冈底斯 - 腾冲地层区广 

泛出露的早 — 中二叠世地层比较 , 岩性组合 

特征、沉积类型、沉积相、生物富集程度 

和属种组分及所处地质背景等诸方面均存 

在显著差异。该套地层的确定 , 对研究西藏 

早、中二叠世地层沉积相 , 重塑古地理环境 , 

以及研究青藏高原和邻区特提斯构造发展 

阶段的地层演化、盆地构造背景等都有重 

要意义。 

2007010552 

西秦岭武山杨河 — 礼县固城地区石炭纪地 

层的发现及其意义 = Discovery of the Carboniferous 

in the Yanghe(Wushan)- 

Gucheng(Lixian)area and its geological significance. 

( 中文 ). 裴先治 ; 郭俊锋 ; 李勇 ; 丁仨 

平 ; 苏春乾 ; 胡波 . 地质通报 , 2003, 22(7): 494- 

499 

通过区域地质调查 , 在西秦岭天水地区 

武山杨河 — 礼县固城一带原划上泥盆统大 

草滩群和中泥盆统舒家坝群中解体出一套 

石炭纪沉积地层。根据所发现的牙形刺、 

珊瑚、非有孔虫化石 , 确定其地质时代为早 

石炭世。 

2007010553 

西藏北部申扎地区志留纪岩石地层和生物 

地层 = Silurian lithostratigraphy and biostratigraphy 

in the Xainza area,northern Tibet. 

( 中文 ). 张树岐 ; 曲永贵 ; 郑春子 . 地质通 

报 , 2003, 22(11-12): 964-969 

在开展西藏北部多巴区幅 1∶ 

25 万区 

域地质调查时 , 对分布于申扎地区的志留纪 

地层进行了详细的研究和划分 , 厘定了该区 

志留纪岩石地层单元 , 建立了生物地层层 

序。首次提出了该区志留系四分方案 , 并为 

确定奥陶系与志留系的界线位置提出了具 

体意见。为西藏乃至全国的志留系的研究 

与划分提供了重要依据。 

2007010554 

长兴阶 ( 上二叠统 ) 之底的全球界线层型 

剖面和点位 = The Global Boundary Strato- 

153

type Section and Point (GSSP) for the base of 

Changhsingian Stage (Upper Permian). ( 英文 ). 

Jin Yugan; Wang Yue; Henderson C; Wardlaw 

B R, Shen Shuzhong; Cao Changqun. Episodes, 

2006, 29(3): 175-182 

The Global Stratotype Section and Point 

(GSSP) for the base-Changhsingian Stage is 

defined at the First Appearance Datum (FAD) 

of the conodont Clarkina wangi within the 

lineage from C. longicuspidata to C. wangi at 

a point 88 cm above the base of the Changxing 

Limestone in the lower part of Bed 4 (base 

of 4a-2) at Meishan D section, Changxing 

County, Zhejiang Province, South China. This 

level is consistent with the first appearance of 

Changhsingian index fusulinid Palaeofusulina 

sinensis and tapashanitid ammonoids. The 

speciation event from Clarkina longicuspidata 

to C. wangi occurs just above the flooding 

surface of the second parasequence in the 

Changxing Limestone. In addition, the boundary 

interval is clearly recognizable by the depletion 

of isotopic carbon ratios and the normal 

polarity zone appearing above the Late 

Wuchiapingian reversed polarity zone. Section 

C, about 300 m to the west of Section D, exposes 

more of the upper Longtan Formation. It 

clearly shows the transitional nature of deposition 

across the Longtan/Changxing formational 

boundary, and thus is described as a 

supplementary reference section. 

2007010555 

赫南特阶 ( 奥陶系最上部 ) 之底的全球界 

线层型剖面和点位 = The Global boundary 

Stratotype Section and Point (GSSP) for the 

base of the Hirnantian Stage (the uppermost of 

the Ordovician System). ( 英文 ). Chen Xu; 

Rong Jiayu; Fan Juanxuan; Zhan Renbin; 

Mitchell C E; Harper D A T; Melchin M J; 

Peng P; Finney S C; Wang X F. Episodes, 

2006, 29(3): 183-196 

The Global boundary Stratotype Section 

and Point (GSSP) for the base of the 

Hirnantian Stage (the uppermost of the Ordovician 

System) is defined at a point 0.39m 

below the base of the Kuanyinchiao Bed in the 

Wangjiawan North section. The section is located 

near Wangjiawan village, 42 km north 

of Yichang city (western Hubei, China), at 30 

degrees 58'56"N and 111 degrees 25'10"E. 

The GSSP level coincides with the first appearance 

of the graptolite species Normalograptus 

extraordinarius (Sobolevskaya). Secondary 

markers include the onset of a positive 

carbon-isotope excursion, and a slightly earlier 

first appearance of Normalograptus 

ojsuensis (Koren and Mikhailova). The Wangjiawan 

North section possesses continuity of 

sedimentation and biozonation with completeness 

of exposures, abundant and wellpreserved 

graptolites and shelly fossils, i.e. the 

Hirnantia-Dalmanitina shelly fauna which is a 

key element for recognition of the Hirnantian 

Stage. The Wangjiawan North, South and 

Riverside sections possess favorable facies 

and widespread correlation potential, are free 

from structure complication, metamorphism 

and other alteration, anti have good accessibility. 

The Riverside section in particular possesses 

amenability to isotopic age determination. 

The beginning of the Hirnantian was followed 

by a global episode of a major extinction 

event, which happened in the Diceratograptus 

mirus Subzone. The proposal was 

voted by the International Subcommission on 

Ordovician Stratigraphy in October, 2004, 

approved by the International Commission on 

Stratigraphy in February, 2006, and ratified by 

the International Union of Geological Sciences 

in May, 2006. 

2007010556 

IGCP 项目 410(1977-2002) 的最终报告 – 

重大奥陶纪生物多样性事件 = Final report 

of IGCP Project 410 (1997-2002) - The great 

Ordovician biodiversification event. ( 英文 ). 

Webby B D; Droser M L; Paris F. Episodes, 

2004, 27(3): 203-208 

In 1997, IGCP Project No. 410 was established 

to appraise known records of Ordovician 

biotas, in order to evaluate one of the 

greatest-ever diversifications of life on Earth, 

between 489 and 443 million years ago. Data 

collection and analysis of biodiversity were 

coordinated through seven regional teams, and 

a global "clade" team. A web-based relational 

database was employed for input of results. 

Some 200 workers from 38 countries participated, 

resulting in approximately 1,000 publications. 

Global and/or regional diversity 

trends were determined for most fossil groups 

down to species level, and many other relevant 

aspects such as bio-events, biofacies, impacts 

of changing geographic and environmental 

regimes, and ocean and climatic states 

were studied. A new, highly resolved, wellcalibrated, 

and wholly integrated Ordovician 

timescale was established to allow precise 

local- to global-scale correlations of biodiversity 

data, and a standardized set of diversity 

measures developed to provide a consistent 

basis for communicating biodiversity results. 

The global Ordovician Radiation exhibited 

154

more-or-less uninterrupted biodiversity increase 

from the beginning of Ordovician time, 

but was punctuated by dramatic, more intensive, 

step-wise pulses of diversification 

through the Mid to Late Ordovician, prior to 

the glacially induced End Ordovician mass 

extinction. The events included a bewildering 

array of adaptive radiations of Cambrian-, 

Palaeozoic- and Modern-type evolutionary 

biotas in marine habitats, the first animals (arthropods) 

to walk on land, and the first plants 

(non-vascular bryophyte-like forms, based on 

cryptospore records) to colonize damp sites on 

land-all of these pivotal in shaping future evolutionary 

pathways 

中生界 

2007010557 

鄂尔多斯盆地西缘延安组层序地层划分 = 

Sequence Stratigraphic Division of Jurassic 

Yanan Formation in West Ordos Basin. ( 中文 ). 

王超勇 ; 郭英海 ; 姜波 ; 沈玉林 . 中国矿业大学 

学报 , 2004, 33(1): 15-18 

利用层序地层学基本原理 , 对小 ( 准 ) 层 

序进行了重新定义 , 它既可以是向上变浅的 

层序 , 也可以是向上变深的层序 ; 根据构造作 

用面、煤层或煤组具有的等时性 , 对鄂尔多 

斯地盆地西缘侏罗纪延安组进行了层序地 

层研究 , 划分为 21 个小层序 ,5 个小层序组 , 

组成了三个体系域 ; 初始充填体系域主要由 

辫状河沉积体系组成 , 超覆充填体系域由曲 

流河 - 三角洲 - 浅湖沉积体系组成 , 退覆充填 

体系域由曲流河 - 三角洲沉积体系组成 . 表明 

它是一个完整的三级层序 , 经历了盆地形 

成、发展、萎缩的过程 . 

2007010558 

牙买加中部上白垩统灰岩古喀斯特层面 = 

Palaeokarstic surfaces in the Upper Cretaceous 

limestones of central Jamaica. ( 英文 ). 

Miller D J; Mitchell S F. Cretaceous Research, 

2003, 24(2): 119-128 

Two prominent pitted surfaces in rhythmic, 

late Maastrichtian, rudist-bearing limestones 

in central Jamaica are described. The 

lower surface is pock-marked with small pits 

that form a nodular, mamillated surface. The 

pits are roughly circular to gently elliptical in 

plan view. They vary in diameter from 5– 

170 mm and in depth from 5–90 mm, and are 

orientated perpendicular to bedding. This surface 

is buried beneath a lignite-rich siltstone 

bed. The upper surface contains microkarren 

phenomena represented by small cylindrical 

potholes up to 40 mm in diameter and 30 mm 

deep. These surfaces are interpreted as palaeokarstic 

because the pits are: (1) perpendicular 

to bedding and not the present land 

surface; (2) infilled with very poorly sorted 

siltstone, and (3) overlain by lignitic shales 

indicating terrestrial influx. The presence of 

two palaeokarstic surfaces in late Maastrichtian 

limestones suggests short-period cycles 

in relative sea level, consistent with glacial-eustatic 

driving mechanisms. 

2007010559 

西 Basque 盆地塞诺曼期事件 :Leioa 剖面 

= Cenomanian events in the deep western 

Basque Basin: the Leioa section. ( 英文 ). Rodriguez-Lázaro 

J; Pascual A; Elorza J. Cretaceous 

Research, 1998, 19(6): 673-700 

Analysis of the microfaunas (foraminifera, 

ostracods) and the stable isotope values 

(δ 13 C, δ 18 O) of the Leioa section, as representative 

of the deep Basque Basin, has allowed 

us to propose a detailed palaeoenvironmental 

reconstruction of this region during the 

Cenomanian, as well as to register global 

chronostratigraphic reference levels to facilitate 

interregional correlations. During the 

Cenomanian, part of the basin, the Plentzia 

Trough, was occupied by intermediate water 

masses, as deduced by the relative percentages 

of planktonic (Rotalipora) and benthonic foraminifera. 

A noticeable change is observed at 

the middle-late Cenomanian transition: the 

replacement of the dominance of keeled (rotaliporids) 

by incipiently-keeled (dicarinellids, 

praeglobotruncanids) planktonic foraminifera, 

indicative of the new influence of the upper 

intermediate waters. The temporary effect of 

shallow waters is deduced in one interval of 

the latest early Cenomanian and two more of 

the middle Cenomanian, as indicated by the 

dominance of globular planktonic foraminifera 

(hedbergellids). These water masses were 

moderately to strongly hypoxic (

tinctions, showing benthonic perturbations 

from the time indicated by the base of the Rotalipora 

reicheli Zone onwards. From the beginning 

until the end of the middle Cenomanian, 

eleven of these perturbations are recorded 

as regional bioevents, using as bioevent-markers, 

intervals where microfauna 

was absent (including benthic-free intervals, 

B-FI; benthonic calcitic-free intervals, BC-FI; 

and ostracod-free intervals, O-FI). These 

changes led to the renewal of the microfaunas; 

benthonic foraminifera renewed their specific 

stocks during the early to early middle Cenomanian, 

with planktonic foraminifera and ostracods 

undergoing renewal at the end of the 

middle Cenomanian. Isotope values of δ 18 O 

and δ 13 C are consistent with the palaeoenvironmental 

changes detected by the microfaunas; 

their maximum and minimum shifts coincide 

with the bioevents. The double-peaked 

positive shift of δ 13 C for the mid-Cenomanian 

of northwest Europe (Jenkynset al., 1994; 

Paulet al., 1994a) has been recognized in this 

series of the Basque Basin. The palaeoenvironmental 

perturbations deduced in the 

Cenomanian of the Leioa section are attributed 

essentially to palaeoceanographic 

changes, where intermediate water masses 

profoundly influenced the planktonic and benthonic 

ecosystems. The influence of other local 

causes, such as volcanic activity at that 

time, or tectonics between the Iberian and 

European plates, are more difficult to prove. 

Several of the bioevents defined in the middle 

Cenomanian of this basin could probably be 

global in nature, and thus may be useful for 

establishing interregional correlations. 

2007010560 

阿尔必阶的底界 : 评论最近的建议 = The 

base of the Albian Stage; comments on recent 

proposals. ( 英文 ). Owen H G. Cretaceous 

Research, 2002, 23(1): 1-13 

Three recent proposals for defining the 

base of the Albian Stage (Casey 1999; Kennedy 

et al. 2000; Hancock, 2001) are discussed 

on the basis of the ammonite succession. 

Since Breistroffer (1947), the stage 

boundary in terms of ammonites has been 

placed at the first occurrence of Leymeriella 

(Proleymeriella) schrammeni, the earliest of a 

succession of three Leymeriella faunas. In 

terms of geographical occurrence, this specific 

boundary can only be recognised clearly in the 

classic north German succession in the Hannover-Braunschweig 

area in which no permanent 

section is available. Casey (1999) favoured 

the boundary to be placed earlier, at 

the first appearance of the geographically 

widespread genusHypacanthoplites , a partial 

return to a boundary accepted in the earlier 

half of the 20th Century. Unfortunately, this 

proposal is not supported by an uncondensed 

permanent section in which Acanthoplites 

(Nolaniceras) occurs below the boundary and 

Hypacanthoplites above. Kennedy et al. (2000) 

raised the boundary to a position within the 

succession of Leymeriella faunas established 

in north Germany. This proposal is supported 

by a relatively uncondensed, more permanent 

section in the Vocontian Basin, France, in 

which multidisciplinary studies have been 

made. However, in terms of ammonites, the 

boundary point chosen is of local value only, 

set within a series of Leymeriella species 

chrons which are essentially confined to the 

European Province and immediately adjacent 

Tethyan and Boreal areas. The occurrence of 

the geographically widespread nannofossil 

Praediscosphaera columnata close to their 

ammonite-based boundary, lends support to 

the proposal that the first occurrence of this 

species should mark the base of the Albian 

Stage. However, there is globally a dearth of 

correlation data provided by other taxa, which 

would confirm that the first occurrence of P. 

columnata is isochronous. It is concluded that 

all previous proposals for the emplacement of 

the Aptian/Albian boundary are unsatisfactory. 

The radical proposal of Hancock (2001) that 

the base of the Albian Stage be placed at the 

geographically widespread and interprovincial 

first occurrence of the ammonite Lyelliceras 

lyelli, formerly regarded as the base of the 

Middle Albian Substage, is supported. 

2007010561 

一个阿普弟阶 / 阿尔必阶界线的新位置的建 

议 = A proposal for a new position for the 

Aptian/Albian boundary. ( 英文 ). Hancock J. 


The Aptian/Albian boundary, as currently 

placed, presents problems which have not yet 

been solved and possibly never will be. No 

detailed definition of recent years can be applied 

on a world-wide scale, which will be 

needed for any definition acceptable to the 

Subcommission on Cretaceous Stratigraphy. 

The only satisfactory and workable solution is 

to choose a completely new position. It is suggested 

that this should be at the base of the 

Zone of Lyelliceras lyelli. This would change 

the start of the Albian from appproximately 

112 Ma to 109 Ma but it would be a standard 

156

which should be recognizable on all five continents. 

2007010562 

环太平洋地区西北部晚白垩纪古温度曲线 

= Palaeotemperature curve for the Late Cretaceous 

of the northwestern circum-Pacific. ( 英 

文 ). Zakharov Y D; Boriskina N G; Ignatyev 

A V; Tanabe K; Shigeta Y; Popov A M; Afanasyeva 

T B; Maeda H. Cretaceous Research, 

1999, 20(6): 685-697 

In the northwestern circum-Pacific, two 

main trends in Late Cretaceous temperatures 

can be recognized. (1) In general, a recurrent 

warming trend is thought to have begun in the 

Turonian–Campanian, reaching temperature 

maxima in the early Late Santonian and early 

Late Campanian, and temperature minima in 

the earliest Santonian and perhaps early Campanian. 

(2) During the Maastrichtian, temperatures 

dropped sharply, with only a slight 

warming in the early Late Maastrichtian. The 

existence of a thermal maximum at the Coniacian–Santonian 

transition has previously been 

expected, but is not confirmed by new isotopic 

results. 

2007010563 

危地马拉 Petén 盆地南部白垩纪地层和古 

环境 = Cretaceous stratigraphy and palaeoenvironments 

of the Southern Petén Basin, Guatemala. 

( 英文 ). Fourcade E; Piccioni L; Escribá 

J; Rosselo E. Cretaceous Research, 1999, 

20(6): 793-811 

The Cretaceous deposits of the Southern 

Petén Basin, an oil-producing province, are 

located to the south of the Yucatan Platform 

and to the east of the Chiapas Carbonate Platform 

of Mexico. The succession in the southern 

part of this basin has been studied both in 

wells and at outcrop by microfacies analysis. 

It is composed of 5000 m of shallow marine 

carbonates and evaporites with a few thin layers 

of pelagic limestones rich in organic carbon 

and planktic foraminifera deposited during 

peak transgressions or maximum flooding. 

The sedimentation of this thick succession 

was not continuous, and the section is punctuated 

by subaerial erosional bounding surfaces 

and a single hardground which marks the final 

drowning of the carbonate platform during the 

late Maastrichtian. New age determinations 

have been obtained on the basis of planktic 

and benthic foraminifera from the Aptian to 

Santonian Cobán Formation, D, C, B and A 

Members. Cobán C (Albian) and B (Cenomanian) 

Members are the present oil reservoirs. 

The rudist and alveolinid limestones of late 

Campanian and Maastrichtian age referred to 

the Campur Formation in the Southern Petén 

Basin are here reassigned to the Angostura 

Formation, as recognized in the Chiapas area. 

The Actela Formation is defined here to encompass 

the limestone breccia deposits that 

occur at the Cretaceous–Tertiary boundary 

and extend into the Parvularugoglobigerina 

eugubina Zone of early Danian age. The D, C, 

B and A Members of the Cobán Formation 

and the Angostura Formation represent second 

order transgressive and regressive trends in a 

passive margin area where the deposits indicate 

a succession of various environments, 

including fluviatile, salinas, shallow marine 

carbonate platform, outer shelf and intrashelf 

basin. High subsidence rates, sea-level 

changes and tectonic uplift controlled the 

sedimentation. 

2007010564 

俄罗斯东北部白垩系 Chauna 群火山灰新 

的 40Ar/39Ar 年龄及其对北太平洋地区地 

质历史和植物群演化的指示意义 = New 

40Ar/39Ar dates for Cretaceous Chauna 

Group tephra, north-eastern Russia, and their 

implications for the geologic history and floral 

evolution of the North Pacific region. ( 英文 ). 

Kelley S P; Spicer R A; Herman A B. Cretaceous 

Research, 1999, 20(1): 97-106 

Cretaceous nonmarine volcanogenicterrigenous 

sedimentary rocks that contain 

plant fossils are widespread in north-eastern 

Russia and phytostratigraphy has been a primary 

tool for regional mapping. The flora 

from the Chauna Group is, however, compositionally 

anomalous, making its proper age 

assignment uncertain. It has been considered 

to be late Albian in age, coeval with floral 

Zone II of the Chandler River sequence in 

northern Alaska, despite the presence of relatively 

advanced conifers and rare angiosperms 

typical of the Late Cretaceous. New radiometric 

data on extrusive volcanic rocks sharply 

constrain the age of the flora showing that it is 

younger than some biostratigraphers had suggested. 

Previous Rb-Sr dates from the Chauna 

Group ranged from 87 to 100 Ma. However, 

new 40 Ar/ 39 Ar (laser fusion and laser stepped 

heating) dates of plagioclase feldspar, biotite 

and amphibole all lie within 2σ errors of each 

other, close to 88 Ma, and all ages fall within 

the Coniacian stage of the Upper Cretaceous. 

Even with the younger age assignment the 

flora remains compositionally distinct and 

157

demonstrates the importance of accounting for 

elevation, edaphic conditions, and seral development 

when determining regional vegetation 

for stratigraphic and palaeoclimatic purposes. 

2007010565 

土耳其东南 Hekimhan 组 ( 坎潘阶 - 马斯特 

里赫特阶 )Çöreklik 段生物地层和同位素 

数据及其古环境意义 = Biostratigraphic and 

isotopic data on the Çöreklik Member of the 

Hekimhan Formation (Campanian- 

Maastrichtian) of SE Turkey and their palaeoenvironmental 

significance. ( 英文 ). 

Yildiz A; Özdemir Z. Cretaceous Research, 

1999, 20(1): 107-117 

The Çöreklik Member of the Hekimhan 

Formation crops out in the Hekimhan 

(Malatya) region of SE Turkey. It includes 

beds that are rich in planktic and benthic foraminifera, 

and in calcareous nannoplankton. 

Eighty-eight rock samples, considered to be 

representative of the stratigraphic section, 

were examined. Seventeen species of planktic 

foraminifera and the Globotruncana ventricosa,G 

lobotruncanita calcarata(Campanian), 

Globotruncanella havanensis, 

Globotruncana aegyptiaca, and 

Gansserina gansseri (Maastrichtian) planktic 

foraminiferal zones were recognised. Thirtytwo 

calcareous nannoplankton species and the 

Ceratolithoides aculeus(CC-20),Quadrum 

sissinghii(CC-21),Quadrum trifidum(CC-22) 

(Campanian),Tranolithus phacelosus(CC-23) 

(Late Campanian-Early Maastrichtian), 

Reinhardites levis(CC-24), Arkhangelskiella 

cymbiformis(CC-25), and Lithraphidites 

quadratus(Early-Late Maastrichtian) zones 

were identified. Analyses of the sediments, the 

distribution of planktic and benthic foraminifera 

and calcareous nannoplankton, the seasurface 

palaeotemperature values and palaeosalinity 

levels respectively calculated 

from δ 18 O‰ (PDB) andδ 13 C‰ (PDB) isotope 

values obtained from globotruncanid tests, and 

the abundance and diversity of temperaturesensitive 

calcareous nannoplankton groups 

allowed the following conclusions to be drawn. 

(1) Maximum phytoplankton abundances and 

highest sea level were reached during the 

Early Campanian; (2) both the numbers of 

phytoplankton and the sea level began to fall 

from the Late Campanian onwards, reaching 

their lowest levels during the Late Maastrichtian; 

and (3) sea-surface temperature values 

were stable through the Campanian-Early 

Maastrichtian but began to fall slowly and 

intermittently from the end of Early Maastrichtian, 

reaching minimum values during the 

Late Maastrichtian. 

2007010566 

法国东南部 Dauphinois 盆地早白垩纪沉积 

和构造发育 = Early Cretaceous sedimentary 

and tectonic development of the Dauphinois 

Basin (SE France). ( 英文 ). Wilpshaar M; 

Leereveld H; Visscher H. Cretaceous Research, 

1997, 18(3): 457-468 

A subsidence analysis is applied to two 

Valanginian-Albian composite columns of the 

Dauphinois Basin (SE France); one for the 

deeper part of the Dauphinois Basin (Vocontian 

Basin) and one for its marginal setting 

(Vercors Area). Within the Valanginian- 

Albian interval of both sequences, three 

phases of subsidence are recognized: (1) a 

Valanginian-Hauterivian phase characterized 

by relatively uniform tectonic subsidence patterns; 

(2) a Barremian-Gargasian phase characterized 

by profound shifts in subsidence; (3) 

a Clansayesian-Albian phase characterized by 

relatively small rates of tectonic subsidence or 

uplift. The Barremian-Gargasian phase can be 

further subdivided in three subphases viz. (1) 

uplift during the Early Barremian; (2) subsidence 

during the Late Barremian to early 

Bedoulian; (3) virtually no subsidence of the 

Vercors Area and subsidence of the Vocontian 

Basin during the late Bedoulian to Gargasian. 

This Barremian-Gargasian phase is related to 

compressional stress built up as a result of the 

changing tectonic regime of the Piemonte- 

Ligurian Ocean from extension to compression. 

As a consequence the Barremian- 

Gargasian tectonic phase forced the onset, 

progradation and eventual disappearance of 

extensive carbonate platforms at the margin of 

the Dauphinois Basin. It implies that these 

carbonate platforms document the very first 

sedimentary response to the changing tectonic 

regime. Vertical motions induced by such a 

changing tectonic regime in particular determine 

the regional sea-level curves established 

for these carbonate platforms and related basinal 

facies rather than global sea-level changes. 

2007010567 

南极 James Ross 盆地 Admiralty Sound 地 

区晚白垩纪地层 = Late Cretaceous stratigraphy 

of the Admiralty Sound region, James 

Ross Basin, Antarctica. ( 英文 ). Pirrie D; 

Crame J A; Lomas S A; Riding J B. Cretaceous 

Research, 1997, 18(1): 109-137 

Key exposures through the Late Cretaceous 

(Campanian-Maastrichtian) Marambio 

158

Group are located in the Admiralty Sound 

region, James Ross Island group, Antarctica. 

On southern James Ross Island, an extensive 

sequence of bioturbated silty mudstones, 

muddy sandstones, fine-grained sandstones, 

ash layers and rare conglomerates has been 

subdivided into two component members of 

the Santa Marta Formation: the Rabot Member 

and the overlying, newly defined, Hamilton 

Point Member. Both members are fossiliferous, 

and have yielded a variety of both 

macro- and microbiotas indicating relatively 

shallow (i.e., shelf depth) marine conditions. 

In particular the Rabot Member contains an 

assemblage of both heteromorph and regularly 

coiled ammonites, giant inoceramid bivalves, 

and other benthos. A combination of both 

ammonite and palynomorph evidence suggests 

that both the Rabot and Hamilton Point members 

are early to late Campanian in age. The 

Santa Marta Formation is believed to pass 

directly up into the newly defined Snow Hill 

Island Formation, which forms the majority of 

the exposure on Snow Hill Island and the 

south-westernmost tip of Seymour Island. 

This unit comprises poorly lithified grey 

sandy mudstones, lithified fine-grained sandstones, 

and dark mudstones. It contains numerous 

concretion horizons and is typified by 

the late Campanian-early MaastrichtianGunnarites 

antarcticusmolluscan assemblage. The 

Snow Hill Island Formation is in turn unconformably 

overlain by the López de Bertodano 

Formation, which, as redefined herein, is restricted 

to the northern tip of Snow Hill Island, 

Seymour Island, and one small exposure on 

Vega Island. An informal lithostratigraphical 

unit characterised by distinctive, pale grey 

weathering mudstones is identified at the base 

of the López de Bertodano Formation, and on 

the basis of palynological studies may be of 

mid- to late Maastrichtian age. The stratigraphical 

scheme presented here has enabled 

us to enhance regional correlation of the Late 

Cretaceous strata within the James Ross Basin. 

Based on these new correlations, we can prove 

that the Campanian-Maastrichtian sequence is 

between 2500 and 2900 m thick. This is one 

of the thickest onshore Late Cretaceous successions 

in the Southern Hemisphere, and has 

the potential to become a key reference section. 

In addition, given its high palaeolatitude 

location, it is a crucial locality to examine 

Late Cretaceous palaeoenvironmental change. 

2007010568 

加拿大艾伯特中、西部地下下侏罗统 

Fernie 组新的生物地层资料及其地层意义 

= New biostratigraphic data from the Lower 

Jurassic Fernie Formation in the subsurface of 

west-central Alberta and their stratigraphic 

implications. ( 英文 ). Asgar-Deen M; Hall R; 

Craig J; Riediger C. Canadian Journal of 

Earth Sciences, 2003, 40(1): 45-63 

Geophysical gamma-ray log responses 

and examination of cores from select wells of 

the lower Fernie Formation document important 

correlations of several new lithologic 

units recognized in the subsurface of westcentral 

Alberta. Ammonite faunas and coccolith 

floras recovered from these cores are illustrated 

and provide new ages for several of 

these units, requiring a revision of their correlation 

with surface stratigraphy of the westcentral 

Alberta foothills. The organic-rich, 

fine-grained west-central Alberta subsurface 

lower Fernie Formation sediments are Hettangian 

to late Toarcian in age and are, therefore, 

correlative with outcrops of unnamed basal 

Fernie strata of northeastern British Columbia, 

Nordegg Member cherty limestones of the 

Cadomin and Nordegg areas, and with the Red 

Deer Member and Poker Chip Shale at outcrop 

in west-central Alberta. 

2007010569 

冀中地区的侏罗系 = The Jurassic System of 

the Central Hebei. ( 中文 ). 陶明华 ; 彭维松 ; 崔 

俊峰 ; 吴建平 ; 张金岩 ; 万姗 . 地层学杂 

志 , 2003, 27(1): 33-40 

冀中地区侏罗系为一套杂色含煤碎屑 

岩层系 , 自下而上发育有 Osmundacidites- 

Cyathidites- Gleicheniidites-Protoconiferus、 

L eiotriletes- Cycadopites- Quadraeculina- 

Classopollis 及 Granulatisporites- Leiotriletes- 

Cyathidites- Cycadopites 等 3 个孢 

粉化石组合。冀中地区侏罗系岩性组成及 

化石组合特征与周边地区具有一定可对比 

性 , 但因其岩性具有明显的特殊性 , 故自下 

而上新建葛渔城组、杨村组和苏桥组。同 

时对冀中地区侏罗纪岩石地层系统的区域 

对比关系和地质时代进行了初步讨论。 

2007010570 

四川井研马门溪龙动物群地层学对比研究 

= Stratigraphy of the Mamenchisaurus fauna 

in Jingyan, Sichuan. ( 中文 ). 张玉光 ; 李建军 . 

地层学杂志 , 2003, 27(1): 50-53 

159

通过对四川井研的含马门溪龙动物群 

地层进行描述划分 , 并且将其中的化石与马 

门溪龙属中其他类型在形态特征、地层层 

位上逐一对比。综合分析得出了井研马门 

溪龙动物群出现于晚侏罗世早期、而且在 

形态组合上是较为原始的类群 , 形态学的鉴 

定和地层学结果相互吻合 , 同时也进一步清 

晰了马门溪龙属在晚侏罗世的演化脉络。 

2007010571 

古鄱阳湖盆地东北缘下、中侏罗统的发现 

= Discovery of the Lower-Middle Jurassic 

strata on the northeastern margin of the ancient 

Poyanghu Basin,Jiangxi. ( 中文 ). 蔡雄飞 ; 

章泽军 ; 顾延生 ; 秦松贤 . 地层学杂志 , 2003, 

27(1): 57-58 

2007010572 

内蒙古大青山地区中、上侏罗统大青山组 

的修订 = Revision of the Middle and Uppef 

Jurassic Daqingshan Formation in Daqingshan 

area, Inner Mongolia. ( 中文 ). 彭向东 ; 徐仲元 ; 

刘正宏 . 地层学杂志 , 2003, 27(1): 66-70 

内蒙古大青山地区侏罗纪地层发育齐 

全 , 下、中侏罗统五当沟组为一套含煤碎屑 

沉积 , 中侏罗统长汉沟组为灰绿色粉细砂岩 

夹灰岩及砂砾岩 , 中、上侏罗统大青山组为 

紫色碎屑岩系 , 构成了一个完整的盆地演化 

序列。由于区内中生代逆冲推覆构造极其 

发育 , 使得区内不同时代的地层均呈构造岩 

片相互叠置 , 给地层划分和对比带来许多困 

难 , 前人所划分的中、上侏罗统大青山组 , 

其中绝大部分并非大青山组 , 而是上二叠统 

脑包沟组和下白垩统李三沟组及固阳组。 

通过大量的野外调查工作 , 笔者对区内大青 

山组的地层层序、展布规律以及与下伏地 

层的接触关系性质等都重新给予厘定 , 提出 

大青山地区上侏罗统大青山组为一套干旱 

炎热气候条件下的河湖相沉积、生物贫乏 , 

分布严格受坝岩 — 席麻湾 — 金銮殿断裂控 

制 , 与下伏地层局部呈不整合 , 整体呈假整 

合接触 , 这些结论对区内地层划分、对比以 

及地质演化历史的研究具有重要意义。 

2007010573 

新疆吐哈盆地侏罗系旋回地层的初步研究 

= Preliminary study on the high-resolution 

cyclostratigraphy of the Jurassic system in 

Turpan-Hami Basin, Xinjiang. ( 中文 ). 姚益民 ; 

付国斌 ; 徐道一 ; 秦俭 ; 姚盛 . 地层学杂 

志 , 2003, 27(2): 122-128 

应用新疆吐哈盆地侏罗系 4 口井 7 个 

组的伽玛测井资料 , 进行高分辨率旋回地层 

的研究。结果表明 : 依据 412.9ka 的偏心率 

旋回 ,7 个组旋回堆积速率 ( AR) 的平均值为 

0.15 2 9m/ka, 它与北美东部上三叠统 4 个组 

合的 Mc L aughlin 旋回 AR 平均值 0.16 

39m/ka 相接近。本区与准噶尔盆地郝家沟 

八道湾组的野外剖面旋回地层对比 , 两者的 

优势旋回量度时间大体一致。吐哈盆地侏 

罗纪地层中在大约 3~10m 厚度、相当 

20~60ka 时间的范围内有小规模的气候变 

化 ; 而在 50~75m 厚度、约相当 100 和 

420ka 的时间中 , 又会出现较大的气候变 

化。 

2007010574 

漠河盆地中生代地层层序及时代 = Sequence 

and age of the Mesozoic strata in the 

Mohe Basin. ( 中文 ). 吴河勇 ; 杨建国 ; 黄清华 ; 

刘文龙 . 地层学杂志 , 2003, 27(3): 193-198 

依据近几年地层研究成果和野外地质 

调查获得的新资料 , 对漠河盆地中生代地层 

进行了厘定 , 将阿杭提河组划归绣峰组 , 木瑞 

组划归上库力组下部 , 上库力组和依列克得 

组之间的含煤地层划归上库力组上部。这 

样纵向上塔木兰沟组 — 上库力组 — 依列克 

得组为火山岩 — 碎屑岩夹火山岩、煤层 — 

火山岩旋回 , 与邻区具有很好的对比关系。 

依据新的同位素资料 , 将塔木兰沟组的时代 

厘定为早白垩世 ; 依据双壳类、腹足类、介 

形类、植物、孢粉等化石资料 , 对漠河盆地 

额木尔河群的时代进行了讨论 , 认为额木尔 

河群的时代为晚侏罗世。 

2007010575 

漠河盆地上侏罗统层序地层格架 = Upper 

Jurassic sequence-stratigraphic framework of 

the Mohe Basin. ( 中文 ). 辛仁臣 ; 吴河勇 ; 杨建 

国 . 地层学杂志 , 2003, 27(3): 199-204 

漠河盆地出露了较完整的上侏罗统 ,6 

条绣峰组、二十二站组、额木尔河组及开 

库康组露头剖面层序地层分析和不同剖面 

间层序对比结果表明 , 漠河盆地从绣峰组到 

开库康组在垂向上发育了 36 个三级层序 , 构 

成绣峰、二十二站、额木尔河和开库康 4 

个超层序。门都里东山绣峰组剖面和二十 

二站组剖面出露了较完整的绣峰和二十二 

站超层序 , 瓦拉干 — 二十二站绣峰组剖面出 

露的是绣峰超层序中上部和二十二站超层 

序底部地层 , 二十二站北山二十二站组剖面 

出露的是二十二站超层序中上部和额木尔 

160

河超层序下部地层 , 小丘古拉河额木尔河组 

剖面出露的是额木尔河超层序中上部和开 

库康超层序下部地层 , 开库康乡开库康组剖 

面出露的是开库康超层序的上部地层。 

2007010576 

苏鲁超高压变质带南部浅变质朋河石岩组 

地质特征及研究意义 = The epimetamorphic 

Pengheshi Formation complex in the south of 

the Jiangsu-Shandong uhpm belt and its geological 

significance. ( 中文 ). 宋明春 ; 宫述林 ; 

陈延贵 . 地层学杂志 , 2003, 27(3): 205-209 

通过对朋河石岩组分布区的地质填 

图、地质剖面观察及接触关系研究 , 将朋河 

石岩组分为二个段 , 并指出该岩组变质程度 

属低绿片岩相 , 上部变质压力较高 , 达中高压 

相系 ; 该岩组为浊流沉积产物 , 与下伏赋存榴 

辉岩的花岗质片麻岩呈构造叠覆接触关 

系。通过分析讨论认为 : 朋河石岩组形成的 

地质背景为晋宁期大陆碰撞之后的上叠盆 

地 , 在三叠纪前后构造滑覆于已抬升到地表 

的超高压变质岩之上 , 河石岩组底界为超高 

压变质带边界 . 

2007010577 

西藏北部班戈地层分区下白垩统郎山组、 

康曲组和余穷组地层层序研究 = Stratigraphic 

succession of the Lower Cretaceous 

Langshan,Kangqi and Yuqiong Formations in 

the Baingoin District, northern Tibet. ( 中文 ). 

曲永贵 ; 刘贵忠 ; 郑春子 ; 王永胜 ; 张树岐 . 地层 

学杂志 , 2003, 27(3): 220-226 

在西藏自治区北部区域地质调查过程 

中 , 在班戈地层分区的下白垩统郎山组之上 

发现一套厚约 1 800m 的滨海 — 浅海相碳酸 

盐岩、陆源细碎屑岩岩石组合 , 该套组合不 

属于郎山组定义之内 , 且出露良好、层序稳 

定、标志清楚、厚度巨大、化石丰富 , 并具 

有很强的可填图性。因此 , 我们将整合于郎 

山组之上 , 岩性以杂色微 — 薄层状钙质泥 

岩、钙质 ( 粉 ) 砂岩与泥质生物灰岩的韵律产 

出为特征 , 产圆笠虫、腹足类、双壳类等化 

石的地层命名为康曲组 ; 将整合于康曲组之 

上 , 下部以灰 — 深灰色中薄层状泥质生物灰 

岩、圆笠虫泥晶灰岩、钙质泥岩等韵律出 

现为特征 , 上部以灰色中 — 厚层状含硅质结 

核圆笠虫泥晶灰岩、圆笠虫泥晶灰岩夹灰 

绿色薄层状钙质砂岩为特征 , 富含圆笠虫、 

腕足类、腹足类、双壳类及海胆等化石的 

地层定名为余穷组。时代均置于早白垩世 

晚期 . 

2007010578 

辽宁义县 — 北票地区义县组地层层序 —— 

义县阶标准地层剖面建立和研究之一 = 

Stratigraphic sequence of the Yixian Formation 

of Yixian—Beipiao region,Liaoning—— 

a study and establishment of stratotype of the 

Yixian stage. ( 中文 ). 王五力 ; 张宏 ; 张立君 ; 郑 

少林 ; 杨芳林 ; 李之彤 ; 郑月娟 . 地层学杂 

志 , 2003, 27(3): 227-232 

义县地区广义的义县组可解体为王家 

屯组 ( 暂命名 ) 和义县组 ; 分属王家屯和义县 

火山旋回 , 前者为偏酸、偏碱性 , 后者主体为 

中基性、末期为中酸性火山岩系 , 并广泛发 

育潜火山岩相的玄武玢岩、安山玢岩和火 

山集块角砾熔岩筒。该区有七个主要沉积 

层 , 自下而上分别为王家屯组马神庙层、义 

县组老公沟层、业南沟层、砖城子层、大 

康堡层、朱家沟层和金刚山层 ; 产有较丰富 

的无脊椎动物、脊椎动物和植物化石。以 

砖城子层、大康堡层和金刚山层为界 , 义县 

火山旋回可划分为 4 个亚旋回 , 分别代表火 

山活动的初始期、主期、晚期和末期。北 

票四合屯地区的义县组相当义县地区义县 

组的第一和第二亚旋回 , 含鸟类化石的主沉 

积层 ( 尖山沟层和上园层 ) 可与砖城子层对 

比 . 

2007010579 

山东省白垩纪岩石地层序列与火山岩系地 

层划分 = Division of the Cretaceous 

lithostratigraphic and volcanic sequences of 

Shandong. ( 中文 ). 刘明渭 ; 张庆玉 ; 宋万千 . 地 

层学杂志 , 2003, 27(3): 247-253 

由于陆相地层 , 尤其火山岩系的复杂性 , 

研究者众多且多局限一隅 , 以往建立起的地 

层序列常只适用于某一地区 , 并且出现同物 

异名或异物同名现象。正确理解和运用 

《国际地层指南》、《中国地层指南 , 是准 

确划分中生代陆相火山岩盆地地层的理论 

依据。借鉴层序地层学的方法 , 对划分山东 

省白垩纪岩石地层层序与火山岩盆地地层 

序列有了新的认识 : 南、北莱阳群虽在岩性 

组合上有较大差异 , 但仍可归于同一岩石地 

层单位 ; 大盛群与青山群既不是严格的上下 

关系 , 也不是完全的同期相变 , 二者呈交叉对 

应关系 , 大盛群的底界稍高 ; 王氏群的林家庄 

组和辛格庄组应修订为寺前村组和孟疃组 , 

置于大盛群中。 

2007010580 

中国东南部侏罗纪 — 第三纪陆相地层沉积 

特征 = The sedimentary features of the Juras- 

161

sic-Tertiary terrestrial strata in Southeast 

China. ( 中文 ). 余心起 ; 舒良树 ; 邓平 ; 王彬 ; 祖 

辅平 . 地层学杂志 , 2003, 27(3): 254-263 

系统分析、总结了中国东南部地区中 

新生代地层的分布状况、沉积作用、构造 

特征 , 反映出地层分布总体上具 NE 走向、 

SE— NW 的分带现象 , 现今盆地的面貌有五 

种不同类型及相应的几何形态。分析认为 , 

中国东南部早、中侏罗世普遍为拉张裂陷 

沉积环境 , 在赣南、粤北、闽西一带发育双 

峰式火山岩 ; 稍后可能受到区域性挤压 , 如皖 

南、浙西、赣东北等地有南东向北西逆冲 

的压性构造 ; 早白垩世为火山喷发高峰期 , 研 

究区均不同程度发生了火山喷发 , 其中东南 

沿海发育大面积的火山岩 ; 早白垩世以后华 

南全区转为拉张 , 发育大量中、小型断陷盆 

地等伸展型盆地 ; 晚白垩世 — 第三纪地壳继 

续处于拉张松弛环境 , 形成以裂谷环境为主 

要特征的火山 — 沉积岩石组合。这些结果 

表明 , 早 — 中侏罗世受古特提斯构造域和太 

平洋构造域的共同影响 , 中侏罗世之后太平 

洋板块占主导 , 上述现象主要系太平洋板块 

在晚中生代不同阶段对中国东南部俯冲作 

用的方位、俯冲速率、俯冲角度有所变化 

所导致 . 

2007010581 

藏南康马地区三叠系研究新进展 = New 

advances in the study on the Triassic system 

of the Kangmar area,southern Tibet. ( 中文 ). 

徐兴永 ; 赵兴国 ; 李文庆 ; 贡布 ; 李尚林 . 地层学 

杂志 , 2003, 27(4): 328-331 

根据康马地区三叠系吕村组和涅如组 

新发现的化石及区域地质背景 , 把该区的地 

层时代分别厘定为中三叠世中晚期至晚三 

叠世早期和晚三叠世中晚期 , 并认为缺失早 

三叠世至中三叠世早期的沉积。研究表明 

康马地区三叠系与二叠系之间为微角度不 

整合接触 , 是 “ 藏南运动 ” 和 “ 印支伸展运动 ” 

共同影响形成的。晚二叠世末至中三叠世 

早期 , 康马地区露出海面 , 接受剥蚀并形成 

喀斯特化风化壳。中三叠世末至晚三叠世 , 

这一地区发生强烈伸展 — 裂陷 , 地壳迅速沉 

降 , 形成被动大陆边缘裂谷盆地 , 发育巨厚 

的半深海 — 深海复理石沉积 , 并伴随大量基 

性岩浆贯入。涅如组下部有两期基性岩侵 

入 , 早期基性岩床形成于印支晚期 , 晚期穿 

层侵入形成于燕山早期。 

2007010582 

鄂尔多斯东北缘东胜地区下白垩统划分的 

有关问题 = Relative problems concerning the 

Lower Cretaceous stratigraphic division of the 

Dongsheng area on the northeastern margin of 

the Ordos Basin. ( 中文 ). 程守田 ; 蒋磊 ; 李志德 ; 

刘星 ; 黄焱球 . 地层学杂志 , 2003, 27(4): 336- 

339 

鄂尔多斯东北缘东胜地区下白垩统的 

地层划分一直存在分歧。依据地层的沉积 

成因及保存特征 , 通过地层的相变关系及其 

对比分析 , 指出了东胜组和伊金霍洛组划分 

方案的不合理性 , 提出了该区下白垩统划分 

可采用三普的命名与划分方案 . 

2007010583 

鄂西香溪地区中二叠世地层新观察 = New 

observation on the Middle Permian strata in 

Xiangxi area,Western Hubei. ( 中文 ). 王小娟 ; 

廖卓庭 ; 严惠君 . 地层学杂志 , 2003, 27(4): 

352-357 1 图版 . 

鄂西香溪地区中二叠统发育良好。重 

新观察发现 : 新滩剖面的马鞍段并不缺失 ; 茅 

口组与吴家坪组之间的粘土岩应归属于吴 

家坪组 ; 隐石燕 (Cryptospirifer) 是与瘤状构 

造同源的再沉积埋葬。同时探讨了香溪及 

邻区中二叠世构造古地理演化轮廓及沉积 

格局 , 研究区栖霞期和茅口期的沉积相 “ 大同 

小异 ”。 

2007010584 

关于波兰南部 Krakow - Wielun 高地上侏 

罗统碳酸盐岩隆分布的构造控制 = Structural 

control on the distribution of Upper Jurassic 

carbonate buildups in the Krakow - 

Wielun Upland (south Poland). ( 英文 ). 

Matyszkiewicz J; Krajewski M; Zaba J. Neues 


Monatschefte, 2006, (3): 182-192 

Intensive growth of these structures was 

strongly controlled by structural properties of 

their bedrock. The Proterozoic and Palaeozoic 

bedrock of the Krakow - Wielun Upland is cut 

by an important fault zone which separates 

terrance-like crustal blocks. This zone is accompanied 

by manifestations of Palaeozoic 

magmatism, and particularly granitoid plutonism. 

The location of granitoid batholiths in the 

basement correlates very well with that jof the 

Upper Jurassic carbonate buildups. Some of 

the intrusions became probably erosionally 

exposed in the Early Mesozoic, forming topographic 

highs upon the Late Jurassic carbonate 

ramp. The areas underlain by those 

162

intrusions whose top parts were not eroded 

revealed less intense subsidence as compared 

to the neighbouring regions, thereby creating 

favourable structural highs upon the sea bottom. 

Such highs became colonised by benthic 

organisms, the intense development of which 

finally led to the growth of carbonate buildups. 

2007010585 

匈牙利 Balaton 高地中三叠世 Pelsonian 亚 

阶的地层新资料 = New data to the stratigraphy 

of the Pelsonian Substage at Koveskal 

(Middle Triassic, Balaton Highland, Hungary). 

( 英文 ). Voros A; Palfy J. Fragmenta Palaeontologica 

Hungarica, 2002, (20): 53-60 

New excavation and fossil collection at 

the classical Middle Triassic locality of 

Horog-hegy revealed that a nearly 40 m thick 

sequence of the Felsoors Limestone Formation 

represents the Pelsonian and Illyrian Substages. 

Within the Balatonicus Zone, the Balatonicus 

Subzone, the Zoldianus Subzone and a 

third, unnamed subzone are proved by detailed 

collections; the Trinodosus and Pseudohungaricum 

Subzones of the Trinodosus Zone haave 

been inferred from ammonoids found in loose 

blocks. Brachiopod limestone appears in two 

distinct horizons: in the Balatonicus Subzone 

and at the top of the Zoldianus Subzone. 

These two horizons were correlated with "recoaro" 

beds at other, well-dated sections of the 

Balaton Highland. 

2007010586 

浙江天台地区赖家组的划分与分布 = Redefinition 

and distribution of the Laijia Formation 

in the Tiantai basin, Zhejiang Province. 

( 中文 ). 方晓思 ; 程政武 ; 蒋严根 ; 杨良锋 . 地质 

通报 , 2003, 22(1): 21-27 1 图版 . 

赖家组建于 1978 年 , 根据岩性特征曾划 

分出 a、b 两段。该组产出恐龙骨骼和恐龙 

蛋等化石 ,20 多年来在国内外引起关注。 

1994 年赖家组一名被废弃 , 由两头塘组和赤 

城山组替代。本文用新修订的 “ 赖家组 ” 代 

表原赖家组 a 段地层 , 赤城山组代表原赖家 

组 b 段地层 , 并对天台盆地上白垩统分布做 

出修改。 

2007010587 

贵州关岭生物群的埋藏环境与古生态特点 

= Taphonomic environment and ecological 

characteristics of the Guanling biota. ( 中文 ). 

陈孝红 ; 陈立德 ; 王传尚 . 地质通报 , 2003, 

22(4): 278-284 

新建并逐层描述了含关岭生物群的上 

三叠统小凹组。根据小凹组下段岩石学、 

地球化学和生物群生态特征分析 , 指出关岭 

新铺乡一带在晚三叠世时为一个三面环 

陆、一面可能与特提斯大洋相通的局限海 

湾。关岭生物群中少量完好保存的植物化 

石的生态特点指示该区当时具有热带、亚 

热带的气候特点 , 雨水充沛。元素地球化学 

特征则显示海湾中的海水可能受间歇性大 

量淡水注入影响而出现间歇性淡化 , 并导致 

生物原来赖以生存的海洋环境出现间歇性 

缺氧 , 而发生生物集群死亡和埋藏。 

2007010588 

辽西上白垩统大兴庄组地层层序及时代 = 

Stratigraphic sequence and age of the Upper 

Cretaceous Daxingzhuang Formation in western 

Liaoning Province. ( 中文 ). 邴志波 ; 刘文 

海 ; 黄志安 ; 张福生 . 地质通报 , 2003, 22(5): 

351-355 

辽宁西部白垩系上统大兴庄组主要分 

布于锦州、义县地区 , 在朝阳波罗赤、阜新 

碱锅等地也有零星出露。除阜新等地区为 

中基性火山熔岩及火山碎屑岩外 , 均为中酸 

性、酸性火山熔岩、熔岩碎屑岩、火山碎 

屑岩、火山碎屑沉积岩及次火山岩。角度 

不整合覆于白垩系下统义县组、九佛堂 

组、沙海组之上 , 平行不整合覆于白垩系孙 

家湾组之上 ,K-Ar 同位素年龄值为 80.83Ma, 

属晚白垩世。该期火山活动以爆发 - 喷溢交 

替进行为特点 , 间有次火山岩侵入 , 活动强度 

微弱 , 分布局限。 

2007010589 

奥地利 Schafberg 地区早侏罗世动物群和 

相 = Early Jurassic fauna and facies of the 

Schafberg area (Salzkammergut, Austria). ( 英 

文 ). Voros A; Szabo J; Dulai A; Szente I; Ebli 

O; Lobitzer H. Fragmenta Palaeontologica 

Hungarica, 2003, (21): 51-82 

The studied area contains localities of 

classical palaeontological monographs, based 

on fossils of the Lower Liassic Hierlatz Formation 

and some other associated limestones. 

During the field work we attempted to locate 

the classical sites but most of the exposures 

are new. Characteristic megafossils are the 

brachiopods but bivalves and gastropods are 

also found. Beside notices on the microfaciesand 

microfossils, the identified species of the 

faunas are listed below, and, some palaeontological 

remarks are added to most of the 

163

listed species. The faunal lists are partly completed 

with museum materials. 

2007010590 

藏南特提斯晚侏罗世维美组的沉积环境 = 

Sedimentary environment of the Late Jurassic 

Weimei Formation in the southern Tibetan 

Tethys. ( 中文 ). 江新胜 ; 颜仰基 ; 潘桂棠 ; 廖忠 

礼 ; 朱弟成 . 地质通报 , 2003, 22(11-12): 900- 

911 

对维美组的沉积结构、构造、动物群 

生态特征、地层展布情况和放射虫硅质岩 

的产出环境等进行了分析 , 认为维美组与其 

南部的同期沉积门卡墩组顶部石英砂岩一 

样 , 同属典型的滨浅海沉积 , 晚侏罗世康马 - 

隆子和北喜马拉雅地层分区为统一的滨浅 

海 , 不存在次深海 — 深海环境。层序地层分 

析表明 , 当时曾发生了陆架海退和陆架暴露 

事件 , 造成了大面积石英砂岩的沉积和相关 

的层序不整合界面。侏罗纪的沉积环境演 

化与古地理变迁说明 , 藏南特提斯被动大陆 

边缘自形成以来并非一成不变 , 而是经历了 

多次活动、稳定 , 海侵、海退的过程。 

2007010591 

西藏北部永珠蛇绿岩带晚侏罗世 — 早白垩 

世日拉组、日拉组索尔碎屑岩及生物群特 

征 = The Late Jurassic-Early Cretaceous Rila 

Formation,Rila Formation Suor clastic rocks 

and characteristics of biotas in the Yun zhug 

ophiolite belt,northern Tibet. ( 中文 ). 曲永贵 ; 

张树岐 ; 郑春子 ; 王永胜 ; 吕鹏 ; 王洪双 ; 李学斌 ; 

李庆武 . 地质通报 , 2003, 22(11-12): 959-963 

在开展藏北多巴区幅 1∶ 

25 万区域地 

质调查时 , 在申扎地区永珠 — 雄梅 — 果芒错 

一带发现了一套沿永珠蛇绿岩带 () 分布 , 岩 

性特征及成因环境较为特殊的晚侏罗世 — 

早白垩世地层 , 建立了日拉组及日拉组索尔 

碎屑岩单位。 

2007010592 

西藏当惹雍错晚侏罗世 — 早白垩世扎列拿 

组、郎穷组和荣纳组的建立 = Establishment 

of the Late Jurassic-Early Cretaceous 

Zaliena Formation,Langqiong Formation and 

Rongna Formation in the Tangra Yumco 

area,Tibet. ( 中文 ). 肖志坚 ; 廖思平 ; 黄传冠 ; 谢 

国刚 ; 罗小川 ; 陈振华 . 地质通报 , 2003, 22(11- 

12): 970-976 

通过 1∶ 

25 万邦多区幅地质调查 , 发现 

晚侏罗世 — 早白垩世则弄群中存在 2 个喷 

发 - 沉积不整合界面 , 将则弄群自然分成 3 个 

部分 , 对应 3 个火山喷发 - 沉积旋回。新创建 

扎列拿组、郎穷组和荣纳组。描述了 3 个 

组的定义及层型、次层型的岩性、岩相、 

古生物、同位素年代特征及其分布情况。 

2007010593 

日本西南部中白垩统御所浦组的区域地层 

和双壳类化石群 = Stratigraphy and fossil 

bivalve assemblages of the mid-Cretaceous 

Goshoura Group, southwest Japan. ( 英文 ). 

Toshifumi K; Haruyoshi M. Paleontological 

Research, 2005, 9(2): 119-142 

The mid-Cretaceous Goshoura Group, 

non-marine to shallow marine fossiliferous 

clastic deposits, is typically exposed on 

Goshoura Island, Amakusa, western Kyushu, 

Japan. Based on precise sedimentological 

analyses, the group is subdivided into the following 

three formations, the Eboshi, Enokuchi 

and Karakizaki Formations in ascending order. 

These formations are herein redefined, and the 

Eboshi and Enokuchi Formations are newly 

subdivided into members, i.e., the Eboshi 

Formation is composed of the Tanoshiri, Hobashiraiwa 

and Arakuchizaki Members, and 

the Enokuchi Formation consists of Hokahira 

and Gannohana Members. Geological age of 

the group is determined by age-diagnostic 

ammonite species, e.g., the Late Albian Mortoniceras 

cf. rostratum from the Hokahira 

Member, and the Early Cenomanian Graysonites 

adkinsi from the overlying Gannohana 

Member. Fifty-eight bivalve species belonging 

to 42 genera are identified from the group. 

These bivalve fossils are grouped into 7 fossil 

assemblages whose occurrences are closely 

linked with depositional facies. Several species 

occur as in life position in situ. Diversified 

Pterotrigonia are abundant in marine bivalve 

assemblages. Brackish-water bivalves 

such as Tetoria shishijimensis, Pulsidis higoensis 

and Crassostrea kawauchidensis repeatedly 

occur from tidal flat deposits at variable 

stratigraphic levels. The faunal diversity 

of the brackish-water assemblage increases 

from the estuarine deposits of the Eboshi 

Formation to the tidal-flat deposits on the 

shoreface of the Karakizaki Formation. These 

results in the Goshoura Group provide a new 

paleoecological scheme of the mid-Cretaceous 

bivalve fauna in the Far East Realm. 

新生界 

2007010594 

美国夏威夷岛地区更新世雪线和冰川 = 

Pleistocene snowlines and glaciation of the 

Hawaiian Islands. ( 英文 ). Porter S C. Quater- 

164

nany International, 2005, 138-139(): 118 - 

128 

High volcanoes on two of the southeastern 

Hawaiian Islands experienced Pleistocene 

ice-cap glaciations. Drifts of three glaciations 

on the upper slopes of Mauna Kea (4206 m) 

are interstratified with lavas. During marine 

isotope stage (MIS) 2, an ice cap (70.5 km 2 ) 

formed when the snowline fell ca. 930 m to an 

altitude of ca. 3785 m. Drifts of MIS 4 and 6 

age, largely buried by hawaiite lavas, record a 

snowline about 100 m lower. Holocene lavas 

bury the upper slopes of Mauna Loa (4169 m), 

the summit of which likely intersected the 

snowline during the last glaciation. The reconstructed 

history of snowline variations and 

glaciation on Maui's Haleakala (3055 m) relies 

on evidence of the island's growth, isostatic 

subsidence, and tilting. The snowline may first 

have intersected Haleakala about 800,000 

years ago; ice caps waxed and waned during 

the next ca. 400,000 years (MIS 22-12) until 

subsidence and diminishing eruptive activity 

brought the summit below the snowline. Erosional 

morphology and thick diamictons indicative 

of subglacial eruptions are consistent 

with repeated summit glaciations. Whereas 

Haleakala's glacial history has ended, ice caps 

likely will regenerate on Mauna Kea ca. 

60,000 and 100,000 years in the future, after 

which the summit will subside below the glacial-age 

snowline.High volcanoes on two of 

the southeastern Hawaiian Islands experienced 

Pleistocene ice-cap glaciations. Drifts of three 

glaciations on the upper slopes of Mauna Kea 

(4206 m) are interstratified with lavas. During 

marine isotope stage (MIS) 2, an ice cap 

(70.5 km 2 ) formed when the snowline fell ca. 

930 m to an altitude of ca. 3785 m. Drifts of 

MIS 4 and 6 age, largely buried by hawaiite 

lavas, record a snowline about 100 m lower. 

Holocene lavas bury the upper slopes of 

Mauna Loa (4169 m), the summit of which 

likely intersected the snowline during the last 

glaciation. The reconstructed history of snowline 

variations and glaciation on Maui's 

Haleakala (3055 m) relies on evidence of the 

island's growth, isostatic subsidence, and tilting. 

The snowline may first have intersected 

Haleakala about 800,000 years ago; ice caps 

waxed and waned during the next ca. 400,000 

years (MIS 22-12) until subsidence and diminishing 

eruptive activity brought the summit 

below the snowline. Erosional morphology 

and thick diamictons indicative of subglacial 

eruptions are consistent with repeated summit 

glaciations. Whereas Haleakala's glacial history 

has ended, ice caps likely will regenerate 

on Mauna Kea ca. 60,000 and 100,000 years 

in the future, after which the summit will subside 

below the glacial-age snowline. 

2007010595 

匈牙利 Buda 山脉 Matyas-hegy 剖面晚始 

新世碳酸盐台地边缘的层序地层解释 = 

Sequence stratigraphic interpretation of a Late 

Eocene carbonate platform margin (Matyashegy 

section, Buda Mountains, Hungary). ( 英 

文 ). Ozsvart P. Fragmenta Palaeontologica 

Hungarica, 2004, 22(): 63-68 

The Matyas-hegy section was carbonate 

platform margin during late Eocene time. The 

sea-level fluctuation curve of this area was 

built using benthic foraminifera associations. 

The geometry of the curve is used to estimate 

the approximate position of candidates for the 

systems tracts boundaries. I have been identified 

the Matyas-hegy section contains the Priabonian 

2 (Pr2) and Priabonian 3 (Pr3) sequence 

boundaries. The Pr3 bondary can be 

appointed exactly, while lthe Pr2 boundary by 

reason of incomplete exposed an not be exactly 

marked off. 

2007010596 

东海 2 万年来碳酸盐溶解作用变化 : 翼足 

类的记录 = Carbonate dissolution changes in 

the East China Sea during the last 20 ka as 

recorded by pteropods. ( 中文 ). 赵泉鸿 ; 翦知 

湣 ; 陈荣华 ; 王永吉 . 海洋地质与第四纪地 

质 , 2005, 25(4): 61-65 

对东海 84 个表层沉积样品和 5 个重力 

柱状样中的翼足类和浮游有孔虫丰度、浮 

游有孔虫碎壳率和底栖有孔虫群中胶结质 

类的比例等进行了定量分析 , 确定了东海现 

代文石补偿深度 (ACD) 位于约 600 m 处 , 

碳酸盐溶跃面在约 1 400 m 处 . 末次冰期时 

随着碳酸盐溶解作用的显著减弱 ,ACD 大幅 

度下降至现代的 1 000 m 之下 . 

2007010597 

层序地层学在饶阳凹陷中的应用 — 以饶南 

地区为例 = The application of sequence 

stratigraphy in raoyang depression. ( 中文 ). 王 

林 ; 纪友亮 . 新疆地质 , 2005, 23(3): 272-277 

根据陆相地层层序在地震剖面、电测 

曲线上的识别标志以及岩石类型组合特点 

等特征 , 将饶阳凹陷饶南地区的下古近系 

划分出了 3 个二级层序、10 个三级层 

序 . 其中三级层序 Ⅷ、Ⅸ、Ⅹ 为河流层 

序 , 可划分为基准面上升体系域和基准面 

165

下降体系域 , 其它均划分为 3 个体系 

域 . 针对研究区目的层段所划层序发育的 

特点 , 在层序地层单元划分和对比的基础 

上 , 结合构造发育史和地层厚度的变化反 

映出古地形特征 , 建立了该区的层序地层 

学模式 , 并初步探讨了层序地层学模式与 

含油气性的关系 , 对各三级层序的含油性 

做出了初步预测 . 

2007010598 

濮城油田沙三中亚段高分辨率层序地层学 

= High resolution sequence stratigraphy of 

Es23 in Pucheng Oilfield,Dongpu depress. ( 中 

文 ). 尹艳树 ; 吴胜和 ; 尹太举 . 地层学杂 

志 , 2006, 30(1): 54-59 

以东濮凹陷濮城油田沙三中亚段水下 

扇沉积地层为例 , 进行了水下扇储层高分 

辨率层序地层学研究。通过岩心和测井资 

料的综合分析 , 在濮城油田沙三中亚段水 

下扇中识别出超短期、短期、中期及长期 4 

个级次基准面旋回及其地层响应特征 , 在 

研究区划分出 1 个长期旋回、5 个中期旋 

回、27 个短期旋回及多个超短期旋回。在 

此基础上建立了研究区高分辨率等时地层 

格架 , 对基准面旋回控制下砂体发育规律 

进行了预测。 

2007010599 

东海陆架盆地台北坳陷新地层单位 —— 月 

桂峰组 = Yueguifeng Foramtion,a new stratigraphic 

uint in the taipei depression of the 

continental shelf, the East China Sea. ( 中文 ). 

姜亮 ; 李保华 ; 钟石兰 ; 张一勇 ; 王建平 . 地层学 

杂志 , 2003, 27(3): 210-211,215 

在微体古生物和岩石地层学分析基础 

上 , 建立了东海陆架盆地台北坳陷新的地层 

单元 —— 月桂峰组。月桂峰组分布于东海 

陆架盆地台北坳陷西带 , 由灰黑色泥岩、砂 

岩组成 , 上覆灵峰组、下伏石门潭组。它属 

古近纪古新世沉积 , 并推测可能为古新世早 

期。该地层相当于苏北盆地阜宁组一段。 

月桂峰组中微体化石特征表明月桂峰组当 

时沉积环境可能为淡水湖泊 . 

2007010600 

伊朗中伊朗盆地库姆组地层的时代 = Age 

of the Qom Formation in the Central Iranian 

Basin,Iran. ( 中文 ). 祁玉平 ; 祝幼华 ; 章炳高 ; 杨 

恒仁 ; 何承全 ; 王世虎 ; 张海峰 ; 宋来亮 ; 贺振建 . 

地层学杂志 , 2003, 27(4): 306-310 

对伊朗中伊朗盆地卡尚地区库姆组的 

微体化石样品分析 , 不仅发现了新的有孔虫 

和介形虫化石组合 , 而且还首次发现了较丰 

富的钙质超微及少量的沟鞭藻化石。依据 

这些化石的组合面貌 , 认为库姆组含始新世 

地层无疑 , 修正了以往认为库姆组地层时代 

为中 — 晚渐新世至早中新世的观点。 

2007010601 

阿根廷拉里奥哈省西北部文支那地区新近 

纪 Toro Negro 组地层和哺乳动物化石 = 

Stratigraphy and fossil mammals from the 

Toro Negro Formation (Neogene), Vinchina 

Department, northwestern La Rioja Province, 

Argentina.. ( 其他 ). Brizuela R R; Tauber A. 

Ameghiniana, 2006, 43(2): 257-272 

The Toro Negro Formation is exposed in 

the western range of the Sierra de Los Colorados, 

in the North-West of La Rioja Province, 

Argentina. The sequence in La Troya creek 

(type section) is composed by a succession of 

epiclastic and piroclastic deposits, where 

thick-bedded sandstones and mudstones with 

interbedded conglomeradic lenses and tuff 

levels predominate. The facies analysis suggests 

a fluvial depositional environment of 

sand bed braided rivers for the lower Member 

and high efficiency alluvial fans for the upper 

Member. The species recorded are: Proeuphractus 

limpidus Ameghino, Chorobates villosissimus 

(Rovereto) Reig, Paleuphractus sp. 

Bordas, Doellotatus inornatus (Rovereto) Castellanos, 

Lomaphorops corallinus Rovereto, 

Neuryurus cf. giganteus, cf. Urotherium sp. 

(Mammalia, Cingulata), Xyophorus aff. bondesioi 

Scillato Yane, cf. Plesiontegatheriii tit, 

cf. Proscelidodon sp. (Mammalia, Tardigrada), 

Abrocoma sp., Protabrocoma sp., 

Propediolagus sp. (Mammalia, Rodentia), 

Eoatichenia sp. (Mammalia, Litopterna). This 

faunistic association suggests: 1) Lower Pliocene 

age; 2) climate conditions that changed 

from and to warm-temperate, or the development 

of and areas in a general context of more 

humid conditions; 3) open areas of herbaceous 

and shrub vegetation and arbo-real formation 

probably existed; 4) the record of the 

nothrotherin Xyophorus aff. bondesioi is related 

to the faunistic and climatic changes during 

the Middle Miocene; 5) the existence of a 

zoogeographic connection between the subandean 

and Pampean regions during the Pliocene. 

166

Untitled

Create successful ePaper yourself

Delete template?

Save as template?