Untitled

第 4 卷第 1 期 

古生物学文摘 ( 网络版 ) 

目录 

2008 年 3 月 

古生物学 

综论 ………………………(1) 

遗迹化石 …………………(10) 

分子古生物学 ……………(13) 

古生态学 …………………(15) 

微体古生物学 

综论 ………………………(22) 

孢粉 ………………………(22) 

疑源类 ……………………(30) 

牙形石 ……………………(30) 

小壳化石 …………………(32) 

古植物学 

综论 ………………………(32) 

藻类 ………………………(34) 

蕨类植物 ( 广义 )………(36) 

早期种子植物 ……………(37) 

裸子植物 …………………(37) 

被子植物 …………………(38) 

古无脊椎动物学 

综论 ………………………(40) 

原生动物 …………………(40) 

古杯、多孔及腔肠动物 …(47) 

苔藓动物 …………………(49) 

腕足动物 …………………(49) 

软体动物 …………………(50) 

节肢动物 …………………(55) 

棘皮动物 …………………(64) 

笔石动物 …………………(67) 

分类位置不明 ……………(68) 

古脊椎动物学 

综论 ………………………(69) 

鱼类 ………………………(70) 

两栖类 ……………………(75) 

爬行类 ……………………(76) 

鸟类 ………………………(87) 

哺乳类 ……………………(89) 

古人类学 

古人类学 …………………(102) 

历史地质学、地层学 

综论 ………………………(105) 

古地理学、古气候学 ……(106) 

前古生界 …………………(107) 

古生界 ……………………(110) 

中生界 ……………………(128) 

新生界 ……………………(142)

第 4 卷第 1 期 

古生物学文摘 ( 网络版 ) 

2008 年 3 月 

古生物学 

综论 

2008010001 

意大利 Livorno 地区中更新世晚期冷水型 

非海相软体动物和小型哺乳动物群 = Late 

Middle Pleistocene cool non-marine mollusc 

and small mammal faunas from Livorno (Italy). 

( 英文 ). Zanchetta G; Becattini R; Bonadonna 

F P; Bossio A; Ciampalini A. Rivista 

Italiana di Paleontologia e stratigrafia, 2006, 

112(1): 135-155 

Non marine molluscs, small mammals and 

pollen allow a reconstruction of the environment 

present during the deposition of the alluvial 

plain deposits. The environment was 

mainly an open space, though sparse woodlands 

should have been present. The nonmarine 

fauna shows features intermediate between 

typical interglacial and glacial assemblages 

described so far in Italy. Worth of note 

is the presence of Orcula dolium and Vallonia 

enniensis, which now inhabit northern Italy. 

2008010002 

从古生代灰岩中分离钙质微体化石的一项 

改进了的技术 = An improved technique for 

extracting calcareous microfossils from Palaeozoic 

limestones. ( 英文 ). Tarsilli A; Warne 

M T. Alcheringa, 1997, 21(1/2): 57-64 

Well preserved calcareous microfossils, 

such as ostracods, can be extracted from 

strongly lithified Palaeozoic limestones of the 

Lachlan Fold Belt using highly concentrated 

acetic acid (95%) with minimal dissociation. 

This technique differs from the more dilute 

acetic acid or formic acid methods which are 

commonly used during the extraction of phosphatic 

microfossils, such as conodonts, and 

which destroy many calcitic specimens. Correlations 

made between representative microfossil 

assemblages and host rock thin sections 

expand knowledge of palaeoenvironmental 

parameters attributed to microfacies. 

2008010003 

德国巴登 - 符腾堡的化石保护 = The protection 

of fossils in Baden-Wurttemberg (Federal 

Republic of Germany). ( 英文 ). Bloos G. Rivista 

Italiana di Paleontologia e stratigrafia, 

2004, 110(1): 399-406 

In Baden-Wurttemberg , fossils of special 

scientific and public interet have been protected 

as culturl monuments by the Monument 

Protection Law since 1972. Two areas of outstanding 

importance, Holzmaden and Nusplingen, 

are declared Protected Excavation 

Area. Other important permanent fossil sites 

are protected by the Nature Conservation Law, 

either as Nature Reserve or as Monument of 

Nature. 

2008010004 

西班牙东南部 Murcia 省侏罗纪古生物遗迹 

= Jurassic paleontological heritage of Murcia 

(Betic Cordillera, south-eastern Spain). ( 英文 ). 

Romero G; Sandoval J; Caracuel J; Mancheno 

M A. Rivista Italiana di Paleontologia e 

stratigrafia, 2004, 110(1): 417-426 

Jurassic rocks of the External and Internal 

Zones of the Betic Cordillera are widespread 

in the province of Murcia. Four areas are considered 

of special interest for stratigraphical 

and paleontological analysis: a) Sierra Quipar 

and b) sierras Jugar-Corque, c)Sierra Ricote 

and d)Sierra Espuna. 

2008010005 

论热河生物群 = On the Mesozoic Johol biota 

of China. ( 中文 ). 季强 . 地质论评 , 2002, 

48(3): 290-296 

本文对中生代热河生物群的研究历史作 

了简要回顾 , 着重阐述了热河生物群的定 

义、组成、地层分布和时代 , 并讨论了与 

热河生物群相关的我国北方陆相侏罗系 - 

白垩系界线问题。 

2008010006 

东秦岭古生代古生物区与古地理变迁 = 

Paleozoic paleobiogeographic provinces and 

Paleogeographic Changes in the eastern 

Qinling. ( 中文 ). 王建平 ; 裴放 . 地质论 

评 , 2002, 48(6): 603-611 

本文根据对东秦岭古生代各纪古生物区 

的分析 , 指出在北秦岭褶皱带 , 二郎坪海 

槽寒武纪放射虫和微浮植物属华南区 , 奥 

陶纪头足类、腹足类、珊瑚为华北区 , 早 

志留世珊瑚为华南区 ; 柿树园海槽中泥盆 

世至二叠纪孢子主要见于华南区 ; 干江河 

1

海槽泥盆纪珊瑚、海百合为华南区。在南 

秦岭褶皱带 , 淅川陆棚寒武纪三叶虫有华 

北区和华南区的分子 , 奥陶纪牙形石、头 

中类由华南区变为华北区 , 晚奥陶世腕足 

类、三叶虫、珊瑚为华北区 , 而早志留世 

笔石、晚泥盆世珊瑚、腕足类和蜓、古植 

物以及早石炭世珊瑚和蜓均为华南区 ; 南 

湾海槽泥盆纪孢子为华南区。在此基础上 

探讨了东秦岭古生代古地理变迁过程。 

2008010007 

个体生态学和生态域的充填 : 关键后生动 

物的辐射 = Autecology and The Filling of 

Ecospace: Key Metazoan Radiations. ( 英文 ). 

Bambach R K; Bush A M; Erwin D H. Palaeontology, 

2007, 50(1): 1-22 

All possible combinations of six tiering positions 

in relation to the substratum/water interface, 

six motility levels and six feeding 

strategies define a complete theoretical ecospace 

of 216 potential modes of life for marine 

animals. The number of modes of life 

actually utilized specifies realized ecospace. 

Owing to constraints of effectiveness and efficiency 

the modern marine fauna utilizes only 

about half the potential number of modes of 

life, two-thirds of which (62 of 92) are utilized 

by animals with readily preserved, mineralized 

hard parts. Realized ecospace has increased 

markedly since the early evolution of 

animal ecosystems. The Ediacaran fauna utilized 

at most 12 modes of life, with just two 

practised by skeletal organisms. A total of 30 

modes of life are recorded in the Early and 

Middle Cambrian, 19 of which were utilized 

by skeletal organisms. The other 11 are documented 

from soft-bodied animals preserved in 

the Chengjiang and Burgess Shale Konservat- 

Lagerstätten. The number of modes of life 

utilized by skeletal organisms increased by 

more than 50 per cent during the Ordovician 

radiation to a Late Ordovician total of 30. Between 

the Late Ordovician and the Recent the 

number of utilized modes of life has doubled 

again. The autecological and taxonomic diversity 

histories of the marine metazoa appear to 

be broadly parallel, and future studies of theoretical 

ecospace utilization should provide 

more detailed tests of pattern and process in 

the ecological history of the metazoa. 

2008010008 

生命如何变得如此多样依据化石记录和 

分子系统学得出的多样化的机制 = How did 

life become so diverse The dynamics of diversification 

according to the fossil record and 

molecular phylogenetics. ( 英文 ). Benton M J; 

Emerson B C. Palaeontology, 2007, 50(1): 23- 

40 

The long-term diversification of life probably 

cannot be modelled as a simple equilibrial 

process: the time scales are too long, the potential 

for exploring new ecospace is too large 

and it is unlikely that ecological controls can 

act at global scales. The sum of many clade 

expansions and reductions, each of which 

happens according to its own dynamic, probably 

approximates more a damped exponential 

curve when translated into a global-scale species 

diversification curve. Unfortunately, it is 

not possible to plot such a meaningful globalscale 

species diversification curve through 

time, but curves at higher taxonomic levels 

have been produced. These curves are subject 

to the vagaries of the fossil record, but it is 

unlikely that the sources of error entirely 

overwhelm the biological signal. Clades radiate 

when the external and internal conditions 

are right: a new territory or ecospace becomes 

available, and the lineage has acquired a number 

of characters that open up a new diet or 

mode of life. Modern high levels of diversity 

in certain speciose clades may depend on such 

ancient opportunities taken. Dramatic climatic 

changes through the Quaternary must have 

driven extinctions and originations, but many 

species responded simply by moving to more 

favourable locations. Ecological communities 

appear to be no more than merely chance associations 

of species, but there may be real 

interactions among species. Ironically, high 

species diversity may lead to more speciation, 

not, as had been assumed, less: more species 

create more opportunities and selective pressures 

for other species to respond to, rather 

than capping diversity at a fixed equilibrium 

level. Studies from the scale of modern ecosystems 

to global long-term patterns in the 

fossil record support a model for the exponential 

diversification of life, and one explanation 

for a pattern of exponential diversification is 

that as diversity increases, new forms become 

ever more refinements of existing forms. In a 

sense the world becomes increasingly divided 

into finer niche space. Organisms have a propensity 

to speciate freely, species richness 

within ecosystems appears to generate opportunities 

for more speciation, clades show all 

kinds of patterns from sluggish speciation 

rates and constant diversity through time to 

apparently explosive speciation, and there is 

no evidence that rapidly speciating clades 

have reached a limit, nor that they are driving 

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other clades to extinction. A corollary of this 

view is that current biodiversity must be 

higher than it has ever been. Limits to infinite 

growth are clearly local, regional, and global 

turnover and extinction events, when climate 

change and physical catastrophes knock out 

species and whole clades, and push the rising 

exponential curve down a notch or two. 

2008010009 

远古时期的宏演化和宏生态学 = Macroevolution 

and macroecology through deep time. 

( 英文 ). Butterfield N J. Palaeontology, 2007, 

50(1): 41-55 

The fossil record documents two mutually 

exclusive macroevolutionary modes separated 

by the transitional Ediacaran Period. Despite 

the early appearance of crown eukaryotes and 

an at least partially oxygenated atmosphere, 

the pre-Ediacaran biosphere was populated 

almost exclusively by microscopic organisms 

exhibiting low diversity, no biogeographical 

partitioning and profound morphological/evolutionary 

stasis. By contrast, the post- 

Ediacaran biosphere is characterized by large 

diverse organisms, bioprovinciality and conspicuously 

dynamic macroevolution. The difference 

can be understood in terms of the 

unique escalatory coevolution accompanying 

the early Ediacaran introduction of eumetazoans, 

followed by their early Cambrian (Tommotian) 

expansion into the pelagic realm. 

Eumetazoans reinvented the rules of macroecology 

through their invention of multitrophic 

food webs, large body size, life-history 

trade-offs, ecological succession, biogeography, 

major increases in standing biomass, eukaryote-dominated 

phytoplankton and the potential 

for mass extinction. Both the pre- 

Ediacaran and the post-Ediacaran biospheres 

were inherently stable, but the former derived 

from the simplicity of superabundant microbes 

exposed to essentially static, physical environments, 

whereas the latter is based on 

eumetazoan-induced diversity and dynamic, 

biological environments. The c. 100-myr 

Ediacaran transition (extending to the base of 

the Tommotian) can be defined on evolutionary 

criteria, and might usefully be incorporated 

into the Phanerozoic. 

2008010010 

差异 : 形态学模式和发育背景 = Disparity: 

morphological pattern and developmental context. 

( 英文 ). Erwin D H. Palaeontology, 2007, 

50(1): 57-73 

The distribution of organic forms is clumpy 

at any scale from populations to the highest 

taxonomic categories, and whether considered 

within clades or within ecosystems. The fossil 

record provides little support for expectations 

that the morphological gaps between species 

or groups of species have increased through 

time as it might if the gaps were created by 

extinction of a more homogeneous distribution 

of morphologies. As the quantitative assessments 

of morphology have replaced counts of 

higher taxa as a metric of morphological disparity, 

numerous studies have demonstrated 

the rapid construction of morphospace early in 

evolutionary radiations, and have emphasized 

the difference between taxonomic measures of 

morphological diversity and quantitative assessments 

of disparity. Other studies have 

evaluated changing patterns of disparity across 

mass extinctions, ecomorphological patterns 

and the patterns of convergence within ecological 

communities, while the development 

of theoretical morphology has greatly aided 

efforts to understand why some forms do not 

occur. A parallel, and until recently, largely 

separate research effort in evolutionary developmental 

biology has established that the developmental 

toolkit underlying the remarkable 

breadth of metazoan form is largely identical 

among Bilateria, and many components are 

shared among all metazoa. Underlying this 

concern with disparity is a question about 

temporal variation in the production of morphological 

innovations, a debate over the relative 

significance of the generation of new 

morphologies vs. differential probabilities of 

their successful introduction, and the relative 

importance of constraint, convergence and 

contingency in the evolution of form. 

2008010011 

宏演化不同于持续的微演化吗 = Is 

macroevolution more than successive rounds 

of microevolution. ( 英文 ). Grantham T. Palaeontology, 

2007, 50(1): 75-85 

Whether macrovolution is reducible to 

microevolution is one of the persistent debates 

in evolutionary biology. Although the concept 

of emergence is important to answering this 

question, it has not been extensively discussed 

within palaeobiology. A taxonomy of emergence 

concepts is presented to clarify the ways 

in which emergence relates to this debate. 

Weak emergence is a particularly helpful way 

to understand the hierarchical nature of biology: 

it captures the ways in which higher-level 

traits depend on lower-level processes, while 

3

ecognizing that emergent traits can nonetheless 

provide the basis for autonomous higherlevel 

theories. A brief review of the biological 

literature suggests that geographical range size 

is weakly emergent. While some concepts of 

emergence do not block the attempt to reduce 

macroevolution (i.e. the attempt to explain all 

macroevolutionary phenomena in terms of 

microevolutionary processes), weak emergence 

does. Thus, if geographical range is 

weakly emergent, it provides a basis for arguing 

that macroevolutionary phenomena cannot 

be fully explained by microevolutionary processes. 

2008010012 

宏演化的尺度与层次 = Scale and hierarchy 

in macroevolution. ( 英文 ). Jablonski D. Palaeontology, 

2007, 50(1): 87-109 

Scale and hierarchy must be incorporated 

into any conceptual framework for the study 

of macroevolution, i.e. evolution above the 

species level. Expansion of temporal and spatial 

scales reveals evolutionary patterns and 

processes that are virtually inaccessible to, and 

unpredictable from, short-term, localized observations. 

These larger-scale phenomena 

range from evolutionary stasis at the species 

level and the mosaic assembly of complex 

morphologies in ancestral forms to the nonrandom 

distribution in time and space of the 

origin of major evolutionary novelties, as exemplified 

by the Cambrian explosion and 

post-extinction recoveries of metazoans, and 

the preferential origin of major marine groups 

in onshore environments and tropical waters. 

Virtually all of these phenomena probably 

involve both ecological and developmental 

factors, but the integration of these components 

with macroevolutionary theory has only 

just begun. Differential survival and reproduction 

of units can occur at several levels within 

a biological hierarchy that includes DNA sequences, 

organisms, species and clades. Evolution 

by natural selection can occur at any 

level where there is heritable variation that 

affects birth and death of units by virtue of 

interaction with the environment. This dynamic 

can occur when selfish DNA sequences 

replicate disproportionately within genomes, 

when organisms enjoy fitness advantages 

within populations (classical Darwinian selection), 

when differential speciation or extinction 

occurs within clades owing to organismic 

properties (effect macroevolution), and when 

differential speciation or extinction occurs 

within clades owing to emergent, species-level 

properties (in the strict sense species selection). 

Operationally, emergent species-level 

properties such as geographical range can be 

recognized by testing whether their macroevolutionary 

effects are similar regardless of the 

different lower-level factors that produce them. 

Large-scale evolutionary trends can be driven 

by transformation of species, preferential production 

of species in a given direction, differential 

origination or extinction, or any combination 

of these; the potential for organismic 

traits to hitch-hike on other factors that promote 

speciation or damp extinction is high. 

Additional key attributes of macroevolutionary 

dynamics within biological hierarchies are 

that (1) hierarchical levels are linked by upward 

and downward causation, so that emergent 

properties at a focal level do not impart 

complete independence; (2) hierarchical effects 

are asymmetrical, so that dynamics at a 

given focal level need not propagate upwards, 

but will always cascade downwards; and (3) 

rates are generally, although not always, faster 

at lower hierarchical levels. Temporal and 

spatial patterns in the origin of major novelties 

and higher taxa are significantly discordant 

from those at the species and genus levels, 

suggesting complex hierarchical effects that 

remain poorly understood. Not only are many 

of the features promoting survivorship during 

background times ineffective during mass extinctions, 

but also they are replaced in at least 

some cases by higher-level, irreducible attributes 

such as clade-level geographical range. 

The incorporation of processes that operate 

across hierarchical levels and a range of temporal 

and spatial scales has expanded and enriched 

our understanding of evolution. 

2008010013 

种间生态差异的宏演化意义 = The macroevolutionary 

consequences of ecological differences 

among species. ( 英文 ). McPeek M A. 

Palaeontology, 2007, 50(1): 111-129 

In this paper, I examine the dynamics of 

species richness in a model system in which 

multiple species compete in a metacommunity 

(multiple patches linked by dispersal). Patches 

lie along an environmental gradient, and new 

species are introduced into the system by 

speciation of existing species. This model is 

used to explore how the ecological similarity 

of species influences the patterns in community 

structure that result and to determine 

whether patterns in fossil and systematics data 

may be signatures for different types of community 

structure. Making species more similar 

4

overall along the entire gradient or making 

new species that have more similar optimal 

positions along the gradient to their progenitor 

both increase the time required to drive species 

extinction. As a result, making species 

more similar ecologically to one another increases 

overall species richness because of an 

increased frequency of transient species in the 

system. Having more transient species in systems 

shifted the longevity distributions of species 

in the fossil record towards having a 

greater frequency of shorter duration species, 

and the age distribution of extant species that 

would be estimated from molecular phylogenies 

also had a higher frequency of younger 

aged species. Comparisons of these results 

with species longevity distributions extracted 

from two data sets and with species ages derived 

from species-level molecular phylogenies 

strongly suggest that transient species are 

an important component of real biological 

communities. 

2008010014 

Vetulicolians 的分类学及系统学关系 = The 

systematics and phylogenetic relationships of 

Vetulicolians. ( 英文 ). Aldridge R J; Hou 

Xian-Guang; Siveter David J; Siveter Derek J; 

Gabbott S. Palaeontology, 2007, 50(1): 131- 

168 

Vetulicolians have variously been considered 

to be unusual arthropods, stem-group 

deuterostomes or relatives of the tunicates. 

They are known from a number of Cambrian 

Lagerstätten, and are particularly diverse in 

the Chengjiang biota of Yunnan Province, 

China. We recognize two classes, Vetulicolida 

and Banffozoa, which together form a monophyletic 

group. Within the Chinese collections 

we also identify two new species and recognize 

one new genus: Vetulicola monile sp. nov. 

and Bullivetula variola gen. et sp. nov. The 

evidence from new and previously described 

specimens is used to undertake a phylogenetic 

analysis and to evaluate a range of hypotheses 

for the affinities of vetulicolians. Given the 

difficulties of interpreting features in enigmatic 

fossils and the apparently contradictory 

set of characters possessed by vetulicolians, it 

is not possible on current evidence to reach an 

unequivocal conclusion regarding the phylogenetic 

position of the group. One possibility 

is that they are a sister group of arthropods 

that lost limbs but gained gill structures analogous 

to those of deuterostomes, but several 

features remain unexplained by this model. If 

they are protostomes, a more generally parsimonious 

position is close to the kinorhynchs. 

An alternative is that they are deuterostomes, 

although a placement at the base of the clade 

is not supported by the evidence. If they are 

deuterostomes, it is more likely that they are 

close to the tunicates. 

2008010015 

墨西哥 Sonora 埃迪卡拉系和寒武系的标准 

化石 = Ediacaran and Cambrian index fossils 

from Sonora, Mexico. ( 英文 ). Sour-Tovar F; 

Hagadorn J W; Huitrón-Rubio T. Palaeontology, 

2007, 50(1): 169-175 

The Cambrian index fossil Treptichnus pedum 

is reported from the Puerto Blanco Formation 

near Pitiquito, Sonora, Mexico, and 

new occurrences of the Neoproterozoic index 

fossil Cloudina are reported from the underlying 

La Ciénega Formation. Considered together, 

these fossils constrain the location of 

the Ediacaran/Cambrian boundary in Mexico. 

The suite of fossils in this sequence is important 

because it provides an independent biostratigraphic 

datum for constraining the position 

of Laurentia during the onset of metazoan 

diversification, for testing proposed 

lithostratigraphic correlations among western 

North American Neoproterozoic–Cambrian 

successions, and for testing regional tectonic 

paradigms such as the Mojave-Sonora 

Megashear hypothesis. 

2008010016 

澳大利亚东北部 Clarke 河盆地早石炭世杜 

内中期 Ruxton 组新的高度矿化植物群和三 

叶虫 = New permineralized flora and trilobites 

from the mid Tournaisian (early Carboniferous) 

Ruxton Formation, Clarke river basin, 

north-east Australia. ( 英文 ). Galtier J; Feist R; 

Talent J A; Meyer-Berthaud B M. Palaeontology, 

2007, 50(1): 223-243 

An association of a new permineralized 

flora with preserved anatomy and decalcified 

trilobite remains is described from early 

crenulata Zone (mid Tournaisian; Early Carboniferous) 

calcareous siltstones in a predominantly 

shale and minor limestone sequence 

low in the Ruxton Formation of the 

eastern Clarke River Basin, north-east Queensland. 

Whereas the trilobites belong to Linguaphillipsia, 

a common and diversified taxon 

in eastern Australia, the plants (with the exception 

of Stauropteris that was earlier identified 

from the Burdekin Basin) were known 

previously only from the Mississipian (Lower 

Carboniferous) of Western Europe. The plants 

5

epresent a diverse assemblage comprising 

lycopsids, cladoxylaleans, a variety of fern 

rachises and seed plants, including stems 

(Tristichia-type), Lyginorachis petioles and a 

new cupule, Ruxtonia minuta gen. et sp. nov., 

containing Hydrasperma ovules. 

2008010017 

不断增加的回归者、生态反馈和早三叠世 

复苏 = Increasing returns, ecological feedback 

and the Early Triassic recovery. ( 英文 ). Erwin 

DH. palaeoworld, 2007, 16(1-3): 9-15 

Most models of biotic recovery following 

mass extinction generally invoke logistic 

growth, with increasing competition due to 

resource competition eventually causing a 

decline in the rate of increase in diversity. Yet 

one of the most interesting aspects of recoveries 

is the acquisition of new resources and the 

expansion of diversity. In other words, the 

carrying capacity of the ecosystem increases, a 

process not captured by logistic models. Insights 

from theories of economic growth, particularly 

of the sources of economic innovation, 

suggest an important role for the spillover 

effects of particular types of ecosystem 

engineering. The positive feedback effects of 

these spillovers allow the rapid expansion of 

biodiversity, as is seen during the late Early 

Triassic phase of biotic recovery. 

2008010018 

一位值得纪念的播种者 : 金玉玕教授对腕足 

动物古生物学和石炭纪 - 二叠纪地层学的贡 

献 = A true sower remembered: Prof. Yu-Gan 

Jin's contributions to brachiopod paleontology 

and Carboniferous and Permian stratigraphy. 

( 英文 ). Miao De-Sui; Shen Shu-Zhong; Wang 

Xiang-Dong. palaeoworld, 2007, 16(1-3): 4-8 

2008010019 

二叠纪末期浅海碳酸盐岩的削蚀作用及其 

对二叠纪 - 三叠纪界线事件的意义 = Erosional 

truncation of uppermost Permian shallow-marine 

carbonates and implications for 

Permian-Triassic boundary events. ( 英文 ). 

Payne J L; Lehrmann D J; Follett D; Seibel M;. 

Kump L R; Riccardi A. Geological Society of 

America Bulletin, 2007, 119(7-8): 771-784 

On shallow-marine carbonate buildups in 

south China, Turkey, and Japan, uppermost 

Permian skeletal limestones are truncated by 

an erosional surface that exhibits as much as 

10 cm of topography, including overhanging 

relief. Sedimentary facies, microfabrics, carbon 

isotopes, and cements together suggest 

that erosion occurred in a submarine setting. 

Moreover, biostratigraphic data from south 

China demonstrate that the surface postdates 

the uppermost Permian sequence boundary at 

the global stratotype section and truncates 

strata within the youngest known Permian 

conodont zone. The occurrences of similar 

truncation surfaces at the mass-extinction horizon 

on carbonate platforms across the global 

tropics, each overlain by microbial buildups, 

and their association with a large negative excursion 

in 13 C further suggest a causal link 

between erosion of shallow-marine carbonates 

and mass extinction. Previously proposed to 

account for marine extinctions, the hypothesis 

of rapid carbon release from sedimentary reservoirs 

or the deep ocean can also explain the 

petrographic observations. Rapid, unbuffered 

carbon release would cause submarine carbonate 

dissolution, accounting for erosion of 

uppermost Permian skeletal carbonates, and 

would be followed by a pulse of high carbonate 

saturation, explaining the precipitation of 

microbial limestones containing upwardgrowing 

carbonate crystal fans. Models for 

other carbon-release events suggest that at 

least 5 x 10 18 g of carbon, released in

cooler mesotrophic to warmer, more oligotrophic 

conditions, indicating a disturbed environment 

due to the warming of the ocean. 

Benthic foraminifer assemblages were also 

significantly affected by the MPBE; diversity 

of the assemblages and buliminids show net 

decline and the low food and opportunistic 

taxa increase in abundance. The reorganization 

of the planktic ecosystem possibly involved 

changes in the food flux (type and quantity) to 

the seafloor, thus triggering changes in the 

benthic communities. A 1 negative 13 C shift 

and a 30% carbonate content decrease are recorded 

in connection with the biotic event. 

This suggests that during the MPBE, as in the 

Paleocene-Eocene Thermal Maximum 

(PETM), an input of a large mass of isotopically 

depleted carbon into the ocean and atmosphere 

could have lowered the deep-sea pH, 

triggering a rapid shoaling of the lysocline and 

contributing to greenhouse warming. The 

MPBE was short lived: according to the 

counting of limestonemarl couplets, the stratigraphic 

expression of precession cycles 

throughout the Zumaia section, the MPBE 

lasted for 52–53 k.y., with the core of the 

event representing 10–11 k.y. The Zumaia 

section is the first land-based locality in which 

the MPBE is recognized and described in detail. 

Due to its expanded character and excellent 

paleontological record, this section may 

prove to be a global reference section for the 

study of this short-lived event. 

2008010021 

Eramosa 化石库 — 加拿大安大略省志留纪 

含有浅海壳相和生物搅动结构的特异保存 

的软躯体生物群 = Eramosa Lagerstätte— 

Exceptionally preserved soft-bodied biotas 

with shallow-marine shelly and bioturbating 

organisms (Silurian, Ontario, Canada). ( 英文 ). 

von Bitter P H; Purnell M A; Tetreault D K; 

Stott C A4. Geology, 2007, 35(10): 879-882 

The middle Silurian Eramosa Lagerstätte of 

Ontario, Canada, preserves taxonomically and 

taphonomically diverse biotas including articulated 

conodont skeletons and heterostracan 

fish, annelids and arthropods with soft body 

parts, and a diverse marine flora. Soft tissues 

are preserved as calcium phosphate and carbon 

films, the latter possibly stabilized by 

early diagenetic sulfurization. It is significant 

that the biotas also include a decalcified, 

autochthonous shelly marine fauna, and trace 

fossils. This association of exceptionally preserved 

and more typical fossils distinguishes 

the Eramosa from other Silurian shallowmarine 

Lagerstätten, such as the Waukesha 

Lagerstätte, and suggests that the Eramosa is 

not the product of exceptional preservation in 

an atypical environment, a bias claimed for 

many post-Cambrian Lagerstätten. The 

Eramosa Lagerstätte may provide a more reliable, 

balanced measure of what has been lost 

from the Silurian fossil record. 

2008010022 

加拿大曼尼托巴省特异保存的晚奥陶世生 

物群 = Exceptionally preserved Late Ordovician 

biotas from Manitoba, Canada. ( 英文 ). 

Young G A; Rudkin D M;. Dobrzanski E P; 

Robson S P; Nowlan G S. Geology, 2007, 

35(10): 883-886 

There are few body fossil biotas known 

from early Paleozoic accretionary shorelines, 

and very few examples of Ordovician softbodied 

assemblages. This study documents 

two recently discovered biotas from separate 

sedimentary basins in Manitoba, Canada, that 

provide unique information about tropical 

shoreline communities shortly before the Late 

Ordovician extinction event. Each site represents 

a distinct depositional environment, but 

they share biotic elements, including eurypterids, 

xiphosurids, and large problematic tubes. 

The William Lake biota, representing more 

restricted conditions, includes jellyfish that are 

among the best hydromedusan body fossils 

known. Rocks at the Airport Cove site, deposited 

under more open circulation, contain 

scolecodonts and noncalcified algae. These 

biotas have some parallels with the recently 

described Middle Ordovician Winneshiek 

Lagerstätte, but are also similar to some Late 

Silurian assemblages. Considered together, 

early Paleozoic marginal marine deposits are a 

rich but as yet poorly known source of paleobiodiversity 

data. 

2008010023 

Smithian-Spathian 界线事件 : 二叠纪末大 

灭绝之前全球气候变化的证据 = Smithian- 

Spathian boundary event: Evidence for global 

climatic change in the wake of the end- 

Permian biotic crisis. ( 英文 ). Galfetti T; Hochuli 

P A; Brayard A; Bucher H; Weissert H; 

Vigran J O5. Geology, 2007, 35(4): 291-294 

One of the most important carbon cycle 

perturbations following the end-Permian mass 

extinction event straddles the Smithian- 

Spathian boundary (SSB) (Olenekian, Early 

Triassic). This anomaly is characterized by a 

prominent positive carbon isotope excursion 

known from Tethyan marine rocks. Its global 

7

significance is established here by a new high 

paleolatitude record (Spitsbergen). Paleontological 

evidence, such as Boreal palynological 

data (Barents Sea, Norway) and global 

patterns of ammonoid distribution, indicates a 

synchronous major change in terrestrial and 

marine ecosystems near the SSB. The reestablishment 

of highly diverse plant ecosystems, 

including the rise of woody gymnosperms and 

decline of the formerly dominating lycopods, 

is interpreted as an effect of a major climate 

change. This hypothesis is supported by modeling 

of ammonoid paleobiogeography, the 

distribution patterns of which are interpreted 

as a proxy for sea surface temperatures (SST). 

The latest Smithian thus appears to have been 

a time of a warm and equable climate as expressed 

by an almost flat pole to equator SST 

gradient. In contrast, the steep Spathian SST 

gradient suggests latitudinally differentiated 

climatic conditions. We propose that this drastic 

climate change and the global carbon cycle 

perturbation were triggered by a massive end- 

Smithian CO 2 injection. The SSB event could 

therefore represent one of the causes for stepwise 

and delayed recovery of marine and terrestrial 

biotas in the wake of the end-Permian 

biotic crisis. 

2008010024 

南半球白垩纪 - 新近纪界线剖面中生产量降 

低及不协调复苏的动物群证据 = Faunal 

evidence for reduced productivity and uncoordinated 

recovery in Southern Hemisphere Cretaceous-Paleogene 

boundary sections. ( 英文 ). 

Aberhan M; Weidemeyer S; Kiessling W; 

Scasso R A; Medina F A. Geology, 2007, 

35(3): 227-230 

The mass extinction at the Cretaceous- 

Paleogene boundary is generally explained by 

a severe crisis in primary productivity, following 

a catastrophic bolide impact. Consistent 

with this scenario, Danian mollusk-dominated 

benthic shelf ecosystems of southern middle 

paleolatitudes (Neuquén Basin, Argentina) are 

characterized by (1) a stratigraphically limited 

low in macrofossil abundances; (2) an increase 

in starvation-resistant, nonplanktotrophic deposit 

feeders and chemosymbionts; (3) a reduction 

in the average body size of individuals; 

and (4) individuals with inactive lifestyles being 

more common than in the late Maastrichtian. 

Return to pre-extinction conditions 

of the various synecological attributes occurred 

over unequal time spans, indicating that 

recovery was uncoordinated with respect to 

ecological traits. Global comparison of ecological 

patterns suggests that reduced food 

supply (1) was a controlling factor in both 

hemispheres; (2) affected macrobenthic marine 

faunas at various distances from the 

Chicxulub impact site; and (3) was more effective 

in siliciclastic environments as compared 

to oligotrophic carbonate settings. 

2008010025 

为南半球白垩纪 - 新近纪界线剖面中生产量 

降低及不协调复苏的动物群证据 = Faunal 






35(3): 227-230 



























2008010026 

南半球白垩纪 - 新近纪界线剖面中生产量降 

低及不协调复苏的动物群证据 = Faunal 






35(3): 227-230 





8























2008010027 

澳大利亚东部下泥盆统礁灰岩形成中的微 

生物影响 = Microbial impacts on the genesis 

of Lower Devonian reefal limestones, eastern 

Australia. ( 英文 ). Adachi N; Ezaki Y. palaeoworld, 

2007, 16(4): 301-310 

Microbial contributions to reefal limestones 

are evident in eastern Australian Lower Devonian 

microbial frame/bindstones, red algalmicrobial-stromatoporoid 

bindstones, and microbial-stromatoporoid 

bindstones. Varied 

microbialite textures, such as stromatolites, 

thrombolites, and leiolites, originated as accumulations 

and partial aggregations of calcimicrobes, 

peloids, and micrites, which also 

derived from microbial activities. In microbial 

frame/bindstones, calcimicrobes (e.g., Rothpletzella 

and Wetheredella) and dense micrite 

layers covered and bound underlying substrates. 

Stabilized substrates promoted the 

subsequent construction of layered, domal, 

and columnar frameworks, which were produced 

by combined accumulations and intermixed 

associations of calcimicrobes and micritic 

microbialites. Microbes flourished in the 

microbial-stromatoporoid bindstones and red 

algal-microbial-stromatoporoid bindstones 

during repeated growth interruptions of the 

framework-building skeletal organisms. Microbes 

bored into and eroded the skeletal 

frameworks to subsequently leave micritic 

envelopes, on which microbial and skeletal 

encrustations took place in turn. The importance 

of microbial colonization on the skeletal 

frameworks was first as subsidiary encrusters 

that helped to preserve them from erosion, and 

second as modifiers of the spaces suitable for 

succeeding encrusters. Partial aggregations of 

Renalcis filled in the interstices of the skeletal 

and microbial frameworks, thereby enhancing 

their rigidity. 

The microbial impacts on the genesis of 

reefal limestones are: (1) origination of components 

(calcimicrobes, peloids, and micrites); 

(2) formation of characteristic microbial textures; 

(3) main and subsidiary reef construction 

and encrustation; and (4) destruction of 

these components, textures, and structures, but 

also the protection of resultant constructions 

in turn. The Lower Devonian reefal limestones 

treated herein, surprisingly, preserve excellent 

records of a variety of microbial impacts. 

Similar effects may also have been common, 

although variable in preservation, in other ancient 

reefal deposits. 

2008010028 

显生宇海洋生物多样性具双曲线趋势 = 

Phanerozoic marine biodiversity follows a 

hyperbolic trend. ( 英文 ). Markov A V; Korotayev 

A V. palaeoworld, 2007, 16(4): 311-318 

Changes in marine biodiversity through the 

Phanerozoic correlate much better with hyperbolic 

model (widely used in demography and 

macrosociology) than with exponential and 

logistic models (traditionally used in population 

biology and extensively applied to fossil 

biodiversity as well). The latter models imply 

that changes in diversity are guided by a firstorder 

positive feedback (more ancestors, more 

descendants) and/or a negative feedback arising 

from resource limitation. Hyperbolic 

model implies a second-order positive feedback. 

The hyperbolic pattern of the world 

population growth arises from a second-order 

positive feedback between the population size 

and the rate of technological growth. The hyperbolic 

character of biodiversity growth can 

be similarly accounted for by a feedback between 

the diversity and community structure 

complexity. The similarity between the curves 

of biodiversity and human population probably 

comes from the fact that both are derived 

from the interference of the hyperbolic trend 

with cyclical and stochastic dynamics. 

2008010029 

今日古生物学之我见 ( 英文 ) = My opinion 

for today’s paleontology. ( 英文 ). 杨敬之 . 微 

体古生物学报 , 2001, 18(2): 217-218 

9

当今的古生物学 , 不论大化石的研究还是 

微体化石的研究 , 都面临着方法的改进和技 

术的更新。从外部形态的描述和内部构造 

的探索 , 走向与外部环境的综合研究 ; 从古生 

物学的单一学科的研究 , 走向与其它相关的 

多学科的综合研究。相辅相成 , 共同提高 , 开 

拓进取 , 使古生物学的研究跃上新的台阶。 

遗迹化石 

2008010030 

英格兰南部 Wessex 亚盆地下白垩统 Vectis 

组恐龙足迹的古环境与埋葬学研究 = Palaeoenvironment 

and taphonomy of dinosaur 

tracks in the Vectis Formation (Lower Cretaceous) 

of the Wessex Sub-basin, southern 

England. ( 英文 ). Radley J D;Barker M 

J;Harding I C. Cretaceous Research, 1998, 

19(3-4): 471-487 

Reptilian ichnofossils are documented from 

three levels within the coastal lagoonal Vectis 

Formation (Wealden Group, Lower Cretaceous) 

of the Wessex Sub-basin, southern 

England (coastal exposures of the Isle of 

Wight). Footprints attributable toIguanodonoccur 

in arenaceous, strongly trampled, marginal 

lagoonal deposits at the base of the formation, 

indicating relatively intense ornithopod 

activity. These were rapidly buried by 

influxes of terrestrial and lagoonal sediment. 

Poorly-preserved footcasts within the upper 

part of the Barnes High Sandstone Member 

are tentatively interpreted as undertracks. In 

the stratigraphically higher Shepherd's Chine 

Member, footcasts of a small to medium-sized 

theropod and a small ornithopod originally 

constituted two or more trackways and are 

preserved beneath a distinctive, laterally persistent 

bioclastic limestone bed, characterised 

by hypichnialDiplocraterion. These suggest 

relatively low rates of dinosaurian activity on 

a low salinity, periodically wetted mudflat. 

Trackway preservation in this case is due to 

storm-induced shoreward water movements 

which generated influxes of distinctive bioclastic 

lithologies from marginal and offshore 

lagoonal settings. The rapidly-deposited footprint-fills 

occasionally contain fully articulated 

shallow burrowing bivalves. 

2008010031 

英格兰南部西撒克斯亚盆地下白垩统威尔 

顿群 Barnes High 砂岩中的双壳类遗迹 = 

Bivalve trace fossils (Lockeia) from the Barnes 

High Sandstone (Wealden Group, Lower 

Cretaceous) of the Wessex Sub-basin, southern 

England. ( 英文 ). Radley J D; Barker M J; 

Munt M C. Cretaceous Research, 1998, 19(3- 

4): 505-509 

Lockeiais described from the upper part of 

the Barnes High Sandstone Member (Vectis 

Formation, Wealden Group) of the Isle of 

Wight, southern England. It is associated with 

bivalve escape structures and attributed to unionid 

and corbiculid bivalves. Preservation of 

the trace fossil and the generating bivalves in 

probable life position was owing to episodically 

rapid deposition beneath prograding deltaic 

sand in a freshwater or oligohaline environment. 

2008010032 

得克萨斯州 Woodbine 组 ( 赛诺曼阶 ) 鸟 

和恐龙足迹化石 = Bird and dinosaur footprints 

in the Woodbine Formation (Cenomanian), 

Texas. ( 英文 ). Lee Y N. Cretaceous 

Research, 1997, 18(6): 849-864 

The ichnofauna of the Woodbine Formation 

(Cenomanian), Denton County, Texas includes 

bird and dinosaur tracks. A new bird 

trackway,Magnoavipes loweiichnogen. et ichnosp. 

nov., appears to represent the largest 

bird tracks known from the Mesozoic. A theropod 

trackway,Fuscinapedis woodbinensisichnogen. 

et ichnosp. nov., is characterized 

by long digits of uniform width and pointed 

small claws. Six hadrosaurid trackways,Caririchnium 

protohadrosaurichnosichnosp. 

nov., are the oldest hadrosaurid 

tracks associated with skeletal elements. They 

include one isolated small footprint, a medium 

sized quadrupedal, and five large bipedal 

hadrosaurid trackways. 

2008010033 

美国堪萨斯州上白垩统 Niobrara 白垩 

Smoky Hill 段化石化的反刍物 = Fossilized 

regurgitate from Smoky Hill Member of Niobrara 

Chalk (Upper Cretaceous) of Kansas, 

USA. ( 英文 ). Hattin D E. Cretaceous Research, 

1996, 17(4): 443-450 

Chalky strata of the Cretaceous of Kansas 

have yielded many fossilized specimens of 

digestive waste derived primarily from fish. 

The fine-grained matrix of these specimens is 

composed predominantly of fluorapatite that 

originated mainly as finely macerated vertebrate 

remains. This paper discusses both 

coiled and non-coiled fish coprolites of presumably 

piscine origin but focuses on an unusual 

coprolite-like mass that contains bony 

material, cirriped plates, and coccoliths. Lack 

10

of digestive etching of cirriped plates, nearly 

articulated arrangement of plates from the cirriped 

peduncle, abundance of coccoliths, and 

irregular shape suggest origin as a regurgitate, 

probably from the ray-like chondrichthy an 

Ptychodus. 

2008010034 

遗迹化石 Psilonichnus 的古环境意义 = The 

paleoenvironmental significance of Psilonichnus. 

( 英文 ). Nesbitt E A; Campbell K A. 

Palaios, 2006, 21(2): 187–196 

The ichnogenus Psilonichnus and its named 

ichnospecies are evaluated for their utility in 

paleoenvironmental reconstructions. A combined 

ichnological-sedimentological model for 

shoreface-estuarine-fluvial settings is presented 

herein to show distributions of the ichnospecies 

of Psilonichnus in an ichnofacies 

framework. High-resolution differentiation of 

coastal paleoenvironments may be achieved in 

strata containing Psilonichnus only if the trace 

fossils are identified to ichnospecies level, and 

if they are assessed as sedimentary structures 

within a depositional context. The simple Y-, 

J-, and I-shaped, vertical to inclined burrows 

referred to as Psilonichnus include three distinct 

ichnospecies–P. tubiformis, P. upsilon, 

and P. lutimuratus. Each can be attributed to 

either of two decapod crustacean progenitors, 

thalassinoid mud shrimp, or ocypodid ghost 

crabs. The ichnogenus occurs in association 

with the Psilonichnus, Glossifungites, and 

Skolithos ichnofacies in estuary/bay to backshore/dune 

sedimentary settings. Psilonichnus 

has proved to be an effective paleoenvironmental 

indicator, especially in studies of sequence 

stratigraphy. To date, however, inconsistencies 

in both ichnotaxonomic and ichnofacies 

assignments for Psilonichnus, and confusion 

regarding probable tracemakers, have 

diminished its usefulness to sedimentary geology. 

To avoid such problems, each new field 

occurrence of a potential Psilonichnus trace 

must be evaluated thoroughly within its biological, 

ecological, and physical context. 

2008010035 

青海曲麻莱 - 治多地区巴颜喀拉山群 ( 上三叠 

统 ) 遗迹化石 = Trace fossils of the Upper Triassic 

Bayanharshan Group in the Qumarleb- 

Zhidoi area, southern Qinghai. ( 中文 ). 赵小明 ; 

牛志军 ; 段其发 ; 汤朝阳 ; 姚华舟 ; 曾波夫 ; 涂兵 . 

古生物学报 , 2007, 46(1): 122-134 

首次对青海南部曲麻莱 - 治多地区巴颜喀 

拉山群上部 ( 上三叠统 ) 遗迹化石进行了系统 

采集 , 共采获遗迹化石 33 属 54 种。据遗迹 

化石的形态、习性、水深等环境成因特征 , 

可划分为两类组合 : 一类以 Cosmorhaphe, 

Helminthopsis, Helminthoida, Megagrapton, 

Paleodictyon 等为主 , 产生于浊流事件前 ; 另 

一类以 Chondrites, Neonereites, Palaeophycus, 

Phycosiphon, Planolites, Zoophycos 等为 

主 , 产生于浊流事件后 , 两者均为半深海 - 深 

海 Nereites 遗迹相的典型代表 , 反映晚三叠世 

研究区应为浊流沉积发育的复理石相沉 

积。 

2008010036 

西藏吉隆地区白垩纪复理石相遗迹化石及 

其地质意义 = Trace fossils of Cretaceous 

flysch facies in the Gyirong area,Tibet,and 

their geological significance. ( 中文 ). 孙立新 ; 

李金和 ; 张振利 . 地质通报 , 2002, 21(11): 

745-748 

系统描述了西藏南部吉隆地区白垩纪甲 

不拉组和宗卓组首次发现的复理石相遗迹 

化石 5 属、7 种。主要遗迹属有 Chondrites, 

Cosmorhophe helminthoida, Muensteria, Phycosiphon, 

Phymatoderma 。遗迹化石的形 

态、习性、水深分布等环境成因特征清楚 

地显示其为深海 Nereites 遗迹相的典型代表 , 

反映复理石相深水沉积环境特征。 

2008010037 

葡萄牙中西部沿 Caldas da Bainha 构造的 

上侏罗统露头 : 一个区域地质遗迹评述 = 

Upper Jurassic outcrops along the Caldas da 

Rainha diaper, West Central Portugal: A regional 

geoheritage overview. ( 英文 ). Dinis J; 

Bernardes C. Rivista Italiana di Paleontologia 

e stratigrafia, 2004, 110(1): 407-415 

The Mesozoic Portuguese geological heritage 

is very rich and varied, a legacy of the 

position in the western margin of Iberia and its 

relationship with its evolution of the North 

Atlantic, with an interesting tectonic history 

since the Late Triassic. Regarding the Upper 

Jurassic several connections can be established 

between the tectonics and the stratigraphic 

record in the area surrounding the 

Caldas da Rainha structure: the basement and 

salt pillow control on deposition; the beginning 

of a diapiric and magmatic cycle associated 

to the onset of sea-floor; the exhumation 

of both Jurassic deposits and the core their 

controlling diapers. The nature of the outcrops 

and richness in sedimentary environments, 

related with the different phases of rifting, is a 

remarkable case for extensional basin studies. 

11

2008010038 

日本全新世浅海沉积物中最年轻的遗迹化 

石 Rosselia socialis 的记录 = The youngest 

record of trace fossil Rosselia socialis: Occurrence 

in the Holocene shallow marine deposits 

of Japan. ( 英文 ). Naru M; Haga M. Paleontological 

Research, 2007, 11(1): 21-27 

The trace fossil Rosselia socialis Dahmer, 

1937 is a thickly mud-lined and spindleshaped 

tube oriented vertically or obliquely to 

the bedding plane. It is known to record detailed 

information on the paleoenvironment. 

Although it has been reported from Lower 

Cambrian to upper Pleistocene deposits, no 

Holocene specimens have previously been 

found. Well preserved specimens of R. sociales 

are herein reported form the Holocene 

shallow marine deposits at Shima, Tako Town, 

Chiba Prefecture, central Japan, co-occurring 

with some prehistoric earthenware vessels that 

were made from 9950 to 2950 yrs. B. P. This 

is the youngest record of R. socialis. 

2008010039 

早、中奥陶世之交陆架周期性缺氧 : 来自美 

国犹他州的遗迹沉积学证据 = Periodic anoxic 

shelf in the Early - Middle Ordovician 

transition: ichnosedimentologic evidence from 

west and central Utah of USA. ( 中文 ). 龚一 

鸣 ;Mary L Droser. 古地理学报 , 2002, 4(4): 

81-89 

美国犹他州中西部、北美早、中奥陶世 

之交重要地层剖面上的遗迹沉积学证据表 

明 , 在奥陶纪生物爆发的重要时期 - 早、 

中奥陶世之交和重要生态领域 - 陆架区 , 

存在持续 3.4 Ma 周期性的陆架缺氧事件。 

主要的遗迹沉积学证据包括 : 低的遗迹化 

石分异度 , 非常浅的生物扰动层厚度和潜 

穴深度 ( 小于 4 cm, 现代陆架区大于 20 

cm), 稀少的居住滤食迹 , 遗迹化石和遗 

迹组构的分布与风暴事件层密切相关 ; 细 

小的 Chondrites 阶层占据较浅或最浅的生态 

阶层 ( 中生代以来 , 细小的 Chondrites 阶层 

总是占据最深的生态阶层 ); 地层序列具 

轨道旋回地层结构 , 并且富含呈黄铁矿假 

象的褐铁矿结核。早古生代较低的大气氧 

水平 , 快速和高幅度的奥陶纪耗氧生物大 

幅射 , 早、中奥陶世之交陆架区快速和高 

幅度的海进和温暖的陆架环境可能是导致 

早、中奥陶世之交陆架环境周期性缺氧的 

主要原因。轨道旋回地层的研究表明 , 这 

次周期性缺氧事件始于 473.27 Ma, 结束于 

469.87 Ma, 持续时间约 3.4 Ma, 如果早、 

中奥陶世之交的同位素年龄值为 473.0 

Ma。早、中奥陶世之交陆架环境周期性缺 

氧事件的发现 , 给正确认识奥陶纪生物辐 

射、古生代演化生物群起源环境和显生宙 

生物集群绝来与缺氧关系增添了新资料。 

2008010040 

澳大利亚中部下寒武统 Plagiogmus arcuatus 

的古生物学意义 = Palaeobiological significance 

of Plagiogmus arcuatus from the 

lower Cambrian of central Australia. ( 英文 ). 

McIlroy D; Heys G R. Alcheringa, 1997, 

21(3/4): 161-178 

The Cambrian trace fossil Plagiogmus is the 

floor of a backfilled burrow which is common 

in the deltaic sediments of the Arumbera 

Sandstone in central Australia. The Plagiogmus 

forming organism/s was/were connected 

to the surface by a siphon that formed a longitudinal 

furrow. Collapse associated with the 

movement of the siphon through the sediment 

may have produced a variety of trace fossil 

morphologies similar to the ichnogenera Gordia, 

Cochlichnus and Taphrhelminthopsis. 

Other parts of the Plagiogmus burrow may be 

compared with Olivellites, Aulichnites, Laminites, 

Climactichnites and Psammichnites ispp. 

The distinctive transverse bars of the Plagiogmus 

structure are interpreted as being 

produced by a posterior sucker used by the 

animal during locomotion. It is interpreted that 

the burrow flu was composed solely of feeding 

wastes and not the spoils of tunnelling. 

The laminae within the backfill are not related 

to the transverse bars. Bilobed burrows overlying 

the Plagiogmus component are related to 

the presence of a siphon that we interpret to 

have been used in surface deposit feeding. The 

biological affinities of the Plagiogmusforming 

animal remain obscure, but it was 

probably vermiform and shared characters 

with the Mollusca, Annelida, Hirundinea 

and/or some echinuran worms. 

2008010041 

俄罗斯欧洲部分晚二叠世大型兽孔目脚印 

的首次发现 = First occurrence of footprints 

of large Therapsids from the Upper Permian 

of European Russia. ( 英文 ). Surkov M V; 

Benton M J; Twitchett R J; Tverdokhlebov V 

P; Newell A J. Palaeontology, 2007, 50(3): 

641-652 

Large footprints of terrestrial tetrapods have 

been found in the Cis-Urals region of European 

Russia. The footprint horizon is in Late 

Permian (Changhsingian) deposits of the 

12

Vyatkian Gorizont (uppermost Tatarian) approximately 

50 m below the local Permian/Triassic 

boundary. Seventeen randomly 

orientated footprints were excavated and are 

referred to the ichnospecies Brontopus giganteus. 

The footprints were emplaced in a reddish-brown 

mudstone that was deposited from 

suspension beneath shallow ponded water in a 

floodplain environment. They were subsequently 

cast by the base of the overlying finegrained 

sandstone, which was deposited from 

a sheet-flood event. The footprints were produced 

by a large therapsid, possibly a dinocephalian, 

but more probably a dicynodont, 

and represent the first ichnological record of 

the Therapsida from the Upper Permian of 

Russia. 

2008010042 

中国中 - 新生代陆相沉积中的遗迹群落 = 

The ichnocoenoses of Mesozoic-Cenozoic 

terrestrial deposits of China. ( 中文 ). 胡斌 ; 齐 

永安 ; 张国成 ; 姜在兴 . 沉积学报 , 2002, 20(4): 

574-581 2 图版 . 

中国中新生代陆相沉积地层中的遗迹化 

石已知七大生态类型近 40 种 , 按其形成的 

沉积环境可大致划分为三大遗迹群落 , 即 

1Scoyenia 遗迹群落 , 代表冲积平原或三角 

洲平原至滨湖环境 ;2Macaronichnus- 

Planolites 遗传群落 , 主要产生于浅湖环境 

及水下砂扇 ( 扇三角洲、冲积扇 ) 沉积环 

境 ;3Mermoides-Neonereites 遗迹群落 , 属 

典型半深 - 深湖环境的产物。 

2008010043 

太古代微生物遗迹化石的直接测龄 = Direct 

dating of Archean microbial ichnofossils. ( 英 

文 ). Banerjee N R; Simonetti A; Furnes H; 

Muehlenbachs K et al. Geology, 2007, 35(6): 

487-490 

Well-preserved Archean pillow lavas from 

the ca. 3.35 Ga Euro Basalt of the Pilbara Craton, 

Western Australia, contain micron-sized 

tubular structures mineralized by titanite (Ca- 

TiSiO 4 ) with residual organic carbon preserved 

along their margins. Direct U-Pb dating 

of titanite in the tubular structures demonstrates 

an Archean age. These tubular microstructures 

are identical to microbial ichnofossils 

in modern basalts, ophiolites, and greenstone 

belts, and are interpreted as a biogenic 

signature in these ancient rocks. Microbial 

colonization of basaltic glass thus appears to 

have been part of a deep subsurface biosphere 

established early in Earth's history. 

分子古生物学 

2008010044 

分子古生物学 = Molecular Palaeobiology. 

( 英文 ). Peterson K; Summons R; Donoghue P 

J. Palaeontology, 2007, 50(4): 775-809 

For more than a generation, molecular biology 

has been used to approach palaeontological 

problems, and yet only recently have attempts 

been made to integrate research utilizing 

the geological and genomic records in uncovering 

evolutionary history. We codify this 

approach as Molecular Palaeobiology for 

which we provide a synthetic framework for 

studying the interplay among genotype, phenotype 

and the environment, within the context 

of deep time. We provide examples of 

existing studies where molecular and morphological 

data have been integrated to provide 

novel insights within each of these variables, 

and an account of a case study where each 

variable has been tackled to understand better 

a single macroevolutionary event: the diversification 

of metazoan phyla. We show that the 

promise of this approach extends well beyond 

research into the evolutionary history of animals 

and, in particular, we single out plant 

evolution as the single greatest opportunity 

waiting to be exploited by molecular palaeobiology. 

Although most of our examples consider 

how novel molecular data and techniques 

have breathed new life into longstanding 

palaeontological controversies, we 

argue that this asymmetry in the balance of 

molecular and morphological evidence is an 

artefact of the relative ‘newness’ of molecular 

data. In particular, palaeontological data provide 

unique and crucial roles in unravelling 

evolutionary history given that extinct taxa 

reveal patterns of character evolution invisible 

to molecular biology. Finally, we argue that 

palaeobiologists, rather than molecular biologists, 

are best placed to exploit the opportunity 

afforded by molecular palaeobiology, though 

this will require incorporating the techniques 

and approaches of molecular biology into their 

skill-set. 

2008010045 

晚太古宙古菌和地表下热液生物圈存在的 

分子证据 = Molecular evidence of Late Archean 

archaea and the presence of a subsurface 

hydrothermal biosphere. ( 英文 ). Ventura 

G T; Kenig F; Reddy C M; Schieber J; 

Frysinger G S; Nelson R K; Dinel E; Gaines R 

B; Schaeffer P. proceedings of the National 

13

Academy of Sciences, 2007, 104(36): 14260- 

14265 5 图版 . 

Highly cracked and isomerized archaeal 

lipids and bacterial lipids, structurally changed 

by thermal stress, are present in solvent extracts 

of 2,707- to 2,685-million-year-old (Ma) 

metasedimentary rocks from Timmins, ON, 

Canada. These lipids appear in conventional 

gas chromatograms as unresolved complex 

mixtures and include cyclic and acyclic biphytanes, 

C 36 –C 39 derivatives of the biphytanes, 

and C 31 –C 35 extended hopanes. Biphytane and 

extended hopanes are also found in highpressure 

catalytic hydrogenation products released 

from solvent-extracted sediments, indicating 

that archaea and bacteria were present 

in Late Archean sedimentary environments. 

Postdepositional, hydrothermal gold mineralization 

and graphite precipitation occurred before 

metamorphism (2,665 Ma). Late Archean 

metamorphism significantly reduced the kerogen's 

adsorptive capacity and severely restricted 

sediment porosity, limiting the potential 

for post-Archean additions of organic matter 

to the samples. Argillites exposed to hydrothermal 

gold mineralization have disproportionately 

high concentrations of extractable 

archaeal and bacterial lipids relative to what is 

releasable from their respective high-pressure 

catalytic hydrogenation product and what is 

observed for argillites deposited away from 

these hydrothermal settings. The addition of 

these lipids to the sediments likely results 

from a Late Archean subsurface hydrothermal 

biosphere of archaea and bacteria. 

2008010046 

浙江长兴更新世红土中的分子化石及其古 

环境意义 = Molecular fossils as indicators for 

paleoenvironment from quaternary red earth in 

Changxing, Zhejiang. ( 中文 ). 王志远 ; 喻建华 ; 

顾延生 ; 吕春英 ; 易轶 ; 谢树成 . 海洋地质与第 

四纪地质 , 2002, 22(1): 97-102 

利用 GC/MS 从浙江长兴更新世红土中检 

测出种类繁多但含量甚微的分子化石 , 主 

要包括正构烷烃、长链三环萜、五环三 

萜、一元正脂肪酸、正脂肪醇、正烷基 -2- 

酮等系列。红土中的这些分子化石 , 特别 

是正构烷烃的特征表明本区的红土是在多 

水的环境下形成的 , 并且其上发育了以草 

本植物为主的高等植被。三环萜烷与三萜 

烷比值 (C 23 /C 30 ) 随地层的变化与红土网 

纹化程度密切相关 , 可能具有潜在的古气 

候指示意义。 

2008010047 

从叶绿素 trnL-F 和 rps4-trnS 序列推断中 

国和大洋洲 Polystichum 羊齿属的系统发 

育及生物地理意义 = Phylogeny and biogeography 

of Chinese and Australasian Polystichum 

ferns as inferred from chloroplast trnL- 

F and rps4-trnS sequence data. ( 英文 ). Li 

Chun-Xiang ; Lu Shu-Gang ; Yang Qun. palaeoworld, 

2007, 16(4): 294-300 

Polystichum, one of the largest genera of 

ferns, occurs worldwide with the greatest diversity 

in southwest China and adjacent regions. 

Although there have been studies of 

Chinese Polystichum on its traditional classification, 

geographic distributions, and even a 

few on its molecular systematics, its relationships 

to other species outside China remain 

little known. Here, we investigated the phylogeny 

and biogeography of the Polystichum 

species from China and Australasia. The evolutionary 

relationships among 42 Polystichum 

species found in China (29 taxa) and Australasia 

(13 taxa) were inferred from phylogenetic 

analyses of two chloroplast DNA sequence 

data sets: rps4-trnS and trnL-F intergenic 

spacers. The divergence time between Chinese 

and Australasian Polystichum was estimated. 

The results indicated that the Australasian 

species comprise a monophyletic group that is 

nested within the Chinese diversity, and that 

the New Zealand species are likewise a monophyletic 

group nested within the Australasian 

species. The divergence time estimates suggested 

that Chinese Polystichum migrated into 

Australasia from around 40 Ma ago, and from 

there to New Zealand from about 14 Ma. The 

diversification of the New Zealand Polystichum 

species began about 10 Ma. These results 

indicated that Polystichum probably 

originated in eastern Asia and migrated into 

Australasia: first into Australia and then into 

New Zealand. 

2008010048 

早期后生动物的种系年代学 : 分子与化石 

资料的联合证据 = Phylochronology of early 

metazoans: combined evidence from molecular 

and fossil data. ( 英文 ). Yang Qun;Ma 

Junye; Sun Xiaoyan; Cong Peiyun. Geological 

Journal, 2007, 42(3-4): 281 - 295 

Timing the evolutionary appearances of 

early Metazoa on Earth may rely on the combined 

information of fossil occurrences, molecular 

divergences and the geological background. 

Recent advances in the studies of 

Neoproterozoic and earliest Cambrian strata in 

14

South China and elsewhere, together with numerous 

works on molecular dating, provide an 

opportunity to draw a more precise timescale 

for the early metazoan evolution. This study 

presents a synthesis of available molecular 

and fossil dating results, placed in the palaeoenvironmental 

background, which leads to 

the recognition of the following time events 

for early metazoan cladogenesis: (1) Animal 

multicellularity occurred most probably during 

early to middle Neoproterozoic times (between 

1000 and 660 Ma) during the geological 

period of gradual increase in oxygen content; 

(2) Eumetazoans and sponges (or sponge-like 

organisms) parted from each other during the 

Neoproterozoic glaciation interval (ca. 750- 

580 Ma), but both experienced adaptive radiation 

after the glaciations as evidenced by the 

Doushantuo Biota (ca. 635-551 Ma); (3) A 

great metazoan radiation event (MRE) occurred 

during the late Ediacaran and earliest 

Cambrian periods (ca. 550-530 Ma), interpreted 

here as a metazoan radiation at higher 

taxonomic levels, as compared with the early 

Cambrian radiation representing one at lower 

taxonomic levels (lower than subphylum or 

class). In order to better constrain the phylochronology 

of early metazoans, we present 

evidence for the divergences of arthropod 

subgroups on the basis of molecular dating 

results and the fossil record. It is shown that 

the arthropod stem group diverged from its 

sister taxon at between 700 and 565 Ma and 

major arthropod subgroups originated coevally 

with MRE. The MRE is probably correlatable 

with the 13C negative anomaly in the 

late Ediacaran Period. 

Although the phylochronology of early 

Metazoa is gradually emerging, a great deal of 

research still will be needed in the following 

directions in order to reduce uncertainties in, 

and discrepancies among, dating results: (1) 

Evaluate different molecular dating techniques 

so as to establish a proper set of standard procedures 

for dating early metazoan events; (2) 

Set up a standard set of fossil calibration 

points suitable for dating early metazoan divergences; 

(3) Use both molecular and fossil 

constraints as far as possible; (4) Place the 

time sequence in the geological and palaeoecological 

background so that one can 

visualize a logical evolutionary scenario. We 

suggest that the fossil record plus the geological 

background should serve to construct a 

general timeframe for evolution, while molecular 

dating will supplement and probably 

increase the precision of the chronology. 

古生态学 

2008010049 

委内瑞拉西部上阿尔拜阶 - 下马斯特里赫特 

阶地层中记录的海洋及气候变化的地球化 

学特征 = Geochemical characterization of 

oceanographic and climatic changes recorded 

in upper Albian to lower Maastrichtian strata, 

western Venezuela. ( 英文 ). Erlich R N; 

Palmer-Koleman S E; Lorente M A. Cretaceous 

Research, 1999, 20(5): 547-581 

Organic and inorganic geochemical data 

(Rock-Eval, TOC, biomarker GC/MS, and 

mineral, major and trace element analyses) 

were used to characterize the palaeoceanographic 

and palaeoclimatic conditions that 

influenced the deposition of upper Albian to 

Maastrichtian rocks of western Venezuela. 

These data show that the late Albian to early 

Santonian was characterized by the accumulation 

and preservation of hydrogen-rich marine 

algal and foraminiferal organic matter, and 

was modulated, in part, by siliciclastic dilution 

(via eolian and fluvial/turbidite processes). 

The contemporaneous development of palaeobathymetric 

barriers surrounding the Maracaibo 

and Barinas/Apure Basins resulted in 

stagnation and poor circulation, and along 

with high evaporation rates, produced salinity 

stratification and entrapment of anoxic bottom 

waters. Bottom water oxygen levels increased 

from the late Santonian through the end of the 

Cretaceous as seasonal upwelling intensified, 

and stratified and entrapped anoxic bottom 

waters underwent frequent overturn and ventilation. 

These major changes in depositional 

patterns can now be identified and linked to 

regional or global oceanographic and climatic 

events. The depositional events that best demonstrate 

this link include: (1) late Albian to 

early Cenomanian drowning of the Maraca 

Formation carbonate platform (linked to the 

global mid-Cretaceous platform drowning 

event); (2) Cenomanian-Turonian drowning of 

the Guayacan Member (Capacho Formation) 

carbonate platform (southern Maracaibo Basin) 

and deposition of organic carbon-rich sediments 

(linked to the global Cenomanian- 

Turonian oceanic anoxic event); (3) depositions 

of Tres Esquinas Member (La Luna 

Formation) phosphates and glauconites in the 

Santonian to Campanian (linked to a regional 

increase in fluvially derived sediments); and 

(4) onset of delta progradation from Colombia 

into western Venezuela during the Campanian 

through Maastrichtian (linked to regional tectonic 

activity and cooling global climate). 

15

2008010050 

意大利中部 Umbria-Marche 盆地 Selli 层 

的有机物特征 = Organic matter characterisation 

of the Selli Level (Umbria-Marche Basin, 

central Italy). ( 英文 ). Baudin F; Fiet N; Coccioni 

R; Galeotti S. Cretaceous Research, 

1998, 19(6): 701-714 

The Selli Level is a marker-bed in the 

Umbria-Marche Apennines that represents the 

regional sedimentary expression of the Lower 

Aptain Oceanic Anoxic Event 1a. This one to 

three-metre-thick interval shows a remarkable 

uniformity on a regional scale, with a green to 

grey marly lower part overlain by black shales. 

Bulk geochemical studies and an examination 

of palynofacies were carried out on three sections 

in order to characterise the distribution 

and nature of the organic matter in the Selli 

Level which has been poorly known hitherto. 

The organic content is medium (0.5 to 2.9% 

TOC) in the basal part and higher (4.5% on 

average, and up to 18% TOC) in the black 

shales. Pyrolysis and palynological data indicate 

that the organic matter is mainly of marine 

origin. The geochemical characteristics of 

the Selli Level are compared to other, more or 

less organic-rich marker-beds in the Cretaceous 

succession of the Umbria-Marche Apennines. 

2008010051 

英格兰东南部下白垩统 Weald Clay 组植 

物、昆虫及其他有机壁微体化石的古环境 

意义 = Palaeonenvironmental implications of 

plant, insect and other organic-walled microfossils 

in the Weald Clay Formation (Lower 

Cretaceous) of southeast England. ( 英文 ). 

Batten D J. Cretaceous Research, 1998, 19(3- 

4): 279-315 

A remarkable variety of plant and other 

organic-walled microfossils that are between 

0.1 and 5.0 mm in maximum diameter have 

been recovered from two Weald Clay sections 

in Surrey, southeast England. The associations 

of these ‘mesofossils’ with each other, and 

with lithofacies, invertebrate macro- and microfossil 

occurrences and palynofacies require 

further investigation, but among a number of 

preliminary conclusions that have been drawn 

based on the data accumulated so far are the 

following. The amount of particulate organic 

matter of mesofossil size in a bed can usually 

be estimated from the general aspect of the 

lithology, but its composition is much harder 

to predict. As for older Wealden (Hastings 

Beds) occurrences, deposits in which megaspores 

are abundant often contain scattered 

small wood and cuticle fragments that are 

visible to the naked eye. Those displaying remains 

of insects of similar or larger size tend, 

not surprisingly, to yield the richest assemblages 

of mesofossil-sized fragments of this 

group. However, such zooclasts occur more 

widely than is apparent from the horizons that 

are obviously insect-bearing. This suggests 

that, more often than has generally been appreciated, 

minute black particles in standard 

palynological preparations of nonmarine 

sedimentary successions may include arthropod 

fragments. The common occurrence of 

charred remains ofWeichselia reticulataand 

other plants in association with disarticulated 

bits of insects may partly reflect both a type of 

vegetation that was prone to desiccation and 

some of the insects that lived within it, lightning-induced 

fire during droughts having been 

responsible for their death. A tendency towards 

an inverse relationship between this 

plant-insect association and large numbers of 

megaspores and/or seeds indicates that other 

habitats are also represented. Several of the 

megaspore genera are probably the products 

of aquatic or waterside plants. Delicate leafy 

shoots of uncertain affinity occur in several 

beds, but the general scarcity of larger pieces 

of wood and foliage suggests that the conifers 

and other gymnosperms may have been confined 

mainly to better drained parts of the 

Wealden lowland, and to the higher ground 

bordering it. Indicators of fresh to low salinity 

water were recovered from more than half of 

the samples examined. This is consistent with 

the general environment of sediment deposition 

inferred from the associated invertebrate 

faunas and dinoflagellate cyst assemblages. 

2008010052 

英格兰南部 Isle 下白垩统 Wealden 群介壳 

层的古环境分析 : 一次初步尝试 = Palaeoenvironmental 

analysis of shell beds in the 

Wealden Group (Lower Cretaceous) of the 

Isle of Wight, southern England: an initial 

account. ( 英文 ). Radley J D; Barker M J. Cretaceous 

Research, 1998, 19(3-4): 489-504 

Initial results of a palaeoenvironmental 

study of Wealden shell beds on the Isle of 

Wight, southern England are presented. Wellpreserved 

biofabrics reflect ‘background’ and 

‘event’ depositional processes in coastal alluvial 

plain and marginal marine lagoonal environments. 

‘Event’ deposits are largely attributable 

to overbank floods in alluvial facies and 

16

shoreward storms in lagoonal environments. 

These locally preserve concentrations of articulated 

bivalves, producing molluscan 

Lagerstätten. Additionally, lagoonal bioclastic 

tempetites preserve a variety of environmentally 

diagnostic sole structures. Bivalve trace 

fossils (Lockeia) occur in lagoonal sand facies. 

Irregular rainfall in the hinterland accounts for 

influxes of derived Jurassic fossils and probably, 

the generation of seasonal growth bands 

in unionid bivalves. Etched shells in the Wessex 

Formation and lower part of the Vectis 

Formation indicate acidic surface waters. Bivalve 

faunas attain greatest species diversity 

in stable freshwater and mesohalinebrachyhaline 

phases, whilst the environmentally 

tolerant corbiculids represent species 

diversity minima, equating to environments of 

unstable salinity. 

2008010053 

墨西哥东北部西特提斯侏罗 - 白垩纪之交的 

古海洋学变化 = Paleoceanographic changes 

at the Jurassic–Cretaceous boundary in the 

Western Tethys, northeastern Mexico. ( 英文 ). 

Adatte T; Stinnesbeck W; Remane J; Hubberten 

H. Cretaceous Research, 1996, 17(6): 

671-689 

Mexico is usually considered to have 

formed the western end of the Tethys during 

Late Jurassic and Early Cretaceous times. The 

circumstances of the opening of the Gulf of 

Mexico Basin towards the Tethys and the exact 

stratigraphic timing, however, are not clear. 

Four sections covering this time interval, located 

in northeastern Mexico, have been 

measured and sampled in detail, in order to 

clarify their stratigraphic position during the 

Late Jurassic to Early Cretaceous time interval 

and the paleogeographic and oceanographic 

changes that accompanied this opening. Our 

studies include microfacies, micro- and 

macropaleontology, whole rock and claymineral 

x-ray diffraction and stable isotopes 

analyses. Our data indicate that the Jurassic- 

Cretaceous boundary, as defined by the Lyon- 

Neuchâtel Colloquium of 1973, cannot be determined 

precisely in northeastern Mexico due 

to the near-absence of calpionellids and endemism 

of ammonite taxa. In the lower and 

upper Berriasian sediments, we detected 

Mediterranean ammonite taxa so far unknown 

from Mexico, corresponding to the appearance 

of typical calpionellid-rich facies. These faunas 

allow direct biostratigraphic correlation 

with European ammonite and calpionellid 

zones. 

We propose that a major oceanographic 

change occurred in the upper part of calpionellid 

Zone B of the Early Berriasian. At this 

time, sediments in northeastern Mexico present 

increasingly pelagic facies, a dramatic 

appearance of Tethyan microfossils (calpionellids) 

and ammonites, changes in stable 

isotopic values, whole rock and clay-mineral 

mineralogy. We suggest that these changes are 

due to a global sea-level rise that connected 

directly northeastern Mexico to the European 

Tethys and ended the endemic, semi-restricted 

and anoxic environment of the Late Jurassic 

La Casita and equivalent La Caja and La Pimienta 

Formations. 

2008010054 

加拿大西部白垩纪阿尔拜期 - 土伦期科罗拉 

多群的古环境变化 : 微体化石、沉积学及地 

球化学证据 = Paleoenvironmental changes in 

the Cretaceous (Albian to Turonian) Colorado 

Group of western Canada: microfossil, sedimentological 

and geochemical evidence. ( 英 

文 ). Schröder-Adams C J; Leckie D A; Bloch 

J; Craig J; McIntyre D J; Adams P J. Cretaceous 

Research, 1996, 17(3): 311-365 

Paleoenvironmental interpretations presented 

here for a portion of the Cretaceous 

Colorado Group marine shale succession in 

western Canada are based on the synthesis of 

biofacies, sedimentological and geochemical 

data. Vertical and lateral variations in foraminiferal, 

coccolith and dinoflagellate assemblages, 

in sediment fabric, structures and 

grain size, and in organic matter abundance 

and composition indicate shale deposition in a 

dynamic and variable basin setting. The upper 

Albian to middle Turonian Colorado Group 

shales were deposited during an overall 

eustatic sea-level rise punctuated by local, 

tectonically-induced, relative sea-level drops 

and variable circulation patterns. 

The upper Albian Westgate Formation 

was deposited during the initial stage of 

Mowry Sea transgression under a dominantly 

low-salinity, cool, Boreal watermass. Up to 

three coarsening-up cycles identified within 

this unit indicate local sea-level fluctuations or 

changes in sediment supply and/or distribution. 

The exclusively agglutinated foraminiferal 

assemblage is Boreal in affinity and reflects 

changes in substrate grain-size. Sedimentary 

structures and generally well-bioturbated 

sediment indicate deposition at or above 

storm-wave base beneath oxygenated bottomwaters. 

17

The basal lithology of the overlying 

lower Cenomanian Fish Scales Formation is a 

regionally extensive bioclastic conglomerate 

interpreted as either a wave-winnowed lag 

formed during a relative sea-level fall and 

subsequent rise, or a current-winnowed lag in 

deeper water. Deep-water bottom currents 

possibly were generated by mixing of the cool, 

low-salinity Boreal waters with warm, normal-salinity 

waters of Tethyan affinity as the 

Mowry Sea opened to the south forming the 

Western Interior Seaway (WIS). Organic matter 

is dominantly Type II, comprising a large 

component of marine algal material. The overlying 

barren, well-laminated sediments that 

comprise the bulk of the Fish Scales Formation 

were deposited under a stratified water 

column with anoxic bottom-waters and are 

characterized as a condensed section. 

The middle to upper Cenomanian Belle 

Fourche Formation conformably overlies the 

Fish Scales Formation. A regional sea-level 

drop occurred during Belle Fourche time as 

indicated by the progradation of Dunvegan 

deltaic sediments in northwestern Alberta. 

Widespread dysoxic conditions persisted 

throughout the middle to late Cenomanian in 

this region as shown by the limited agglutinated 

foraminiferal assemblage and sparse 

bioturbation. Increased detrital input is evident 

as an increase in silt content relative to the 

Fish Scales Formation and a re-introduction of 

significant amounts of Type III organic matter. 

The occurrence of numerous bioclastic conglomerates 

throughout the upper portion of the 

Belle Fourche Formation is possibly the result 

of relative sea-level drops affecting areas of 

different water depth with variable erosional 

intensity. 

Maximum transgression in latest Cenomanian 

to early Turonian time brought fully marine 

conditions and planktic Tethyan fauna 

into the Canadian portion of the WIS. This 

time period is represented by the Second 

White Specks Formation. Productivity in the 

upper water column was high and anoxic bottom 

waters preserved abundant Type II organic 

matter. 

Lateral facies variations and a diachronous 

introduction of Tethyan foraminifera and 

coccoliths to various parts of the basin indicate 

pathways of oceanic circulation. The influence 

of major Cordilleran detrital sources 

limited pelagic faunal development in the west. 

A significant unconformity in central Saskatchewan 

indicates local basin floor doming 

and subsequent erosion in late Turonian to 

Santonian time. 

2008010055 

巴黎盆地早白垩世铁质鲕粒 : 土壤起源对海 

洋起源及它们的古气候意义 = Early Cretaceous 

iron ooids in the Paris Basin: pedogenic 

versus marine origin and their palaeoclimatic 

significance. ( 英文 ). Taylor K G. Cretaceous 

Research, 1996, 17(1): 109-118 

Oolitic ironstones occur within the subsurface 

Lower Cretaceous sediments of the Pays 

de l’Ourcq region of the Paris Basin. Goethite 

ooids in these ironstones are of three types. 

Type 1 ooids are characterized by welldeveloped 

concentric lamination and the absence 

of a clear nucleus. Type 2 ooids are 

characterized by thin, concentrically laminated 

cortices and nuclei of iron oxide or quartz 

grains. These nuclei show structures (iron oxide 

veining in quartz grains, iron oxide platelets) 

similar to that formed within lateritic 

soils. Type 3 ooids are small, generally lack 

concentric lamination and commonly contain 

‘desiccation ’ features. The goethite in the 

ironstones has negligible Al-substitution, indicative 

of formation in the marine environment. 

It is proposed that the ooids formed 

through accretion on the sea-floor, or just below 

the sediment surface. However, the nuclei 

of type 2 ooids, and many of the detrital grains 

within the ironstones, were derived from lateritic 

soils upon nearby massifs. Therefore, 

evidence is present within the ironstones for a 

warm, sub-tropical climate during the Early 

Cretaceous, although the process of oolitic 

ironstone formation was most likely controlled 

by marine sedimentary processes rather than 

climate. 

2008010056 

贵州中寒武世凯里生物群中纳罗虫 ( 节肢动 

物门 ) 的埋葬学 = Taphonomy of Naraoiids 

(Arthropoda) from the Middle Cambrian Kaili 

Biota, Guizhou Province, South China. ( 英文 ). 

Lin J P. Palaios, 2006, 21(1): 15–25 Naraoiids 

in the Kaili biota (Taijiangian Stage, 

Wulingian Series, lower Middle Cambrian) 

are preserved in a variety of taphonomic states. 

Decomposition, entombment, and fossil 

diagenesis of Kaili naraoiid specimens (n = 69) 

are described. The decay rates of appendages, 

internal organs, and dorsal sclerites are different, 

and should be treated as separate taphonomic 

elements. A classification scheme 

to delineate the preservational states is proposed 

here to distinguish carcasses from molts 

18

in deposits with exceptional preservation. For 

example, at least 35% of Kaili naraoiids represent 

carcasses. Among them, 21% of individuals 

are interpreted as having been buried 

alive (Type A preservational state) and 79% 

showed some evidence of decay prior to burial 

(Type B preservational state). 65% of naraoiids 

can be either molts or decayed carcasses, 

and molts typically are articulated 

(Type C preservational state). Disarticulated 

(Type D preservational state) specimens are 

rare. 

Kaili naraoiids were buried in three orientations 

with respect to bedding: (1) parallel, (2) 

oblique, and (3) folded-over (specimens with 

noticeably shortened anterior shields). Due to 

the nature of the naraoiid bauplan, most 

specimens (77%) tend to be buried parallel to 

bedding. All naraoiid specimens with foldedover 

anterior shields (10%) represent carcasses. 

Identified taphonomic modifications 

caused by post-burial processes include extruded 

gut contents, three-dimensionally preserved 

internal organs, and sclerite fractures. 

Preservation of three-dimensional soft-parts 

accompanied by flattened hard-parts is interpreted 

here as the result of syndiagenetic anaerobic 

microbial decay. The relief and size of 

preserved midguts depend on: (1) availability 

of volatile tissues, (2) abundance and types of 

microbes, and (3) duration of anaerobic microbial 

decay prior to compactional dewatering. 

2008010057 

早寒武世食物链 : 来自中国西南部帽天山页 

岩生物群的新证据 = Early Cambrian food 

chain: New evidence from fossil aggregates in 

the Maotianshan Shale Biota, SW China. ( 英 

文 ). Vannier J; Chen J Y. Palaios, 2005, 20(1): 

3–26 | 

Three categories of fossil aggregates are 

recognized in the Lower Cambrian Maotianshan 

Shale biota from SW China: (1) elliptical 

aggregates with randomly distributed exoskeletal 

remains of typically small- to medium-size 

bivalved arthropods (e.g., ostracode-like 

bradoriids, phyllocarid-like waptiids), 

hyoliths, and trilobites are interpreted as 

coprolites, possibly produced by anomalocaridids 

(e.g., waptiid-rich coprolites) and/or 

unknown epibenthic predators; (2) elongate, 

ribbon-like aggregates composed of oriented 

small hyolith shells, interpreted as the feces of 

infaunal carnivorous worms such as priapulids; 

and (3) concentric aggregates, typically with a 

central nucleus (e.g., remains of medusoid 

eldoniids or bivalved arthropod carapaces) and 

peripheral exoskeletal fragments, possibly 

generated by bottom currents whirling around 

carcasses. These new coprolite data add to 

morphofunctional information obtained from 

fossil organisms and indicate that predation 

occurred at different levels of the water column 

with: (1) endobenthic predators (diverse 

priapulid fauna) feeding near the sedimentwater 

interface; (2) epibenthic predators/scavengers 

(almost exclusively arthropods); 

(3) predators living in the lower levels 

of the water column (e.g., anomalocaridids); 

and (4) mid-water predators exploiting upper 

levels in the water column (e.g., eldoniids, 

ctenophores, chaetognaths). Communities living 

at or close to the water-sediment interface 

(epibenthic sensu stricto, meiobenthic, and 

demersal animals) were exposed to a multidirectional 

predatorial pressure from infaunal, 

epifaunal, and mid-water predators. Although 

predation was diverse, nothing indicates that 

the food chain extended beyond the level of 

primary carnivores. Animals already had acquired 

complex behaviors such as hunting 

(e.g., anomalocaridids, priapulids) and predator 

avoidance in which sensory systems were 

involved. The example of the Maotianshan 

Shale indicates that the burst of anatomical 

innovations (new body plans) that characterizes 

the early Cambrian also was accompanied 

by the rapid development of new feeding 

strategies and by an unprecedented expansion 

of ecological interactions (prey-predator relationships). 

2008010058 

地质时期捕食强度与全球生物多样性的相 

关性 = Coupling of predation intensity and 

global diversity over geologic time. ( 英文 ). 

Holland S M. proceedings of the National 


14886 

The geologic history of earth's biodiversity, 

and the origins of this pattern, are central 

problems in paleobiology and evolutionary 

biology. The basic picture for marine organisms 

was outlined in 1860 (1) but was considerably 

refined in the 1980s and 1990s by the 

late Jack Sepkoski. His databases of marine 

animal families and genera produced an iconic 

pattern of an early Paleozoic rise in diversity, 

followed by a late Paleozoic plateau or slow 

decline, a low after the end-Permian extinction, 

and a final protracted rise through the Mesozoic 

and Cenozoic (2, 3). The explanation for 

19

this pattern has been an active area of research, 

with interpretations ranging from preservational 

artifacts to a host of biologically 

mediated processes (4–7). Predation has been 

regarded as potentially important, but the data 

to establish its significance have been limited 

in scope (8–11). The work of Huntley and 

Kowalewski (12) in this issue of PNAS demonstrates 

for the first time a strong correlation 

between predation intensity and marine 

biodiversity throughout the Phanerozoic Eon. 

Their results are particularly compelling because 

the data are independent of the globalscale 

taxonomic lists used to generate diversity 

curves, making a spurious correlation between 

the two unlikely. The authors' evidence 

strongly suggests that predation and biodiversity 

are highly correlated in the marine realm, 

although which is cause and which is effect 

remains . . . 

2008010059 

显生宙化石记录中捕食强度与多样性之间 

的强相关性 = Strong coupling of predation 

intensity and diversity in the Phanerozoic fossil 

record. ( 英文 ). Huntley J W; Kowalewski 

M. proceedings of the National Academy of 

Sciences, 2007, 104(38): 15006-15010 3 图版 . 

The importance of ecological interactions in 

driving the evolution of animals has been the 

focus of intense debate among paleontologists, 

evolutionary biologists, and macroecologists. 

To test whether the intensity of such interactions 

covaries with the secular evolutionary 

trend in global biodiversity, we compiled a 

species-level database of predation intensity, 

as measured by the frequency of common predation 

traces (drillings and repair scars ranging 

in age from Ediacaran to Holocene). The 

results indicate that the frequency of predation 

traces increased notably by the Ordovician, 

and not in the mid-Paleozoic as suggested by 

multiple previous studies. Importantly, these 

estimates of predation intensity and global 

diversity of marine metazoans correlate 

throughout the Phanerozoic fossil record regardless 

of corrections and methods applied. 

This concordance may represent (i) an ecological 

signal: long-term coupling of diversity 

and predation; (ii) a diversity-driven diffusion 

of predatory behaviors: an increased probability 

of more complex predatory strategies to 

appear at higher diversity levels; or (iii) a spurious 

concordance in signal capture: an artifact 

where rare species and less-frequent (e.g., 

trace-producing) predatory behaviors are both 

more detectable at times when sampling improves. 

The coupling of predation and diversity 

records suggests that macroevolutionary 

and macroecological patterns share common 

causative mechanisms that may reflect either 

historical processes or sampling artifacts. 

2008010060 

显生宙海洋古多样性曲线的形态 : 能从西 

欧沉积岩石记录中得到多少推测 = The 

shape of the Phanerozoic Marine Palaeodiversity 

Curve: How much can be Predicted from 

the sedimentary rock record of Western 

Europe. ( 英文 ). Smith A B; McGowan A J. 


Palaeodiversity curves are constructed from 

counts of fossils collected at outcrop and thus 

potentially biased by variation in the rock record, 

specifically by the amount of sedimentary 

rock representative of different time intervals 

that has been preserved at outcrop. To 

investigate how much of a problem this poses 

we have compiled a high-resolution record of 

marine rock outcrop area in Western Europe 

for the Phanerozoic and use this to generate a 

model that predicts the sampled diversity 

curve. We find that we can predict with high 

accuracy the variance of the marine genus 

diversity curve (itself dominated by European 

taxa) from rock outcrop data and a three-step 

model of diversity that tracks supercontinent 

fragmentation, coalescence and fragmentation. 

The size and position of two of the five major 

mass extinction spikes are largely predicted by 

rock outcrop data. We conclude that the longterm 

trends in taxonomic diversity and the 

end-Cretaceous extinction are not the result of 

rock area bias, but cannot rule out that rock 

outcrop area bias explains many of the shortterm 

rises and falls in sampled diversity that 

palaeontologists have previously sought to 

explain biologically. 

2008010061 

内陆安曼早二叠世 Pachycyrtella 层定量古 

生态 = Quantitative palaeoecology in the 

Pachycyrtella Bed, Early Permian of Interior 

Oman. ( 英文 ). Angiolini L. palaeoworld, 

2007, 16(1-3): 233-245 

The population dynamics and community 

structure of the Pachycyrtella Bed at the base 

of the Lower Permian Saiwan Formation (Interior 

Oman) are described. The populations 

of the brachiopod Pachycyrtella omanensis 

and the bivalve Dickinsartella pistacina are 

census populations, which show a stable structure, 

with individuals growing successfully to 

maturity due to fast initial growth rate. P. 

20

omanensis and D. pistacina are opportunist 

species that colonized a physically stressed 

environment, characterized by high mobility 

of the substrate, high energy and high nutrient 

influx at the end of the Gondwanan deglaciation. 

Both P. omanensis and D. pistacina have 

a large biovolume with respect to surface area 

and this may reflect an adaptation to cool climate 

conditions, whereas their thick shell substance 

could be the result of increasing biocalcification 

in the high O 2 /CO 2 Early Permian 

atmosphere. Community structure records the 

combined effect of rich food resources and an 

unstable environment, as low (individuals) to 

very low (biovolume) diversity values and 

short suspension feeding chains characterize 

the pioneer palaeocommunities of the Pachycyrtella 

Bed. The slight increase in diversity 

in the upper part of the bed is interpreted to 

have resulted from a change in the environmental 

stability, probably connected to decreasing 

hydrodynamic energy during a small 

scale sea-level rise. More favourable conditions 

at the top of the bed are also suggested 

by the relative abundance of the newly recognized 

small-sized strophalosiid species Strophalosia 

ericinia n. sp., which spent part of its 

life firmly attached to P. omanensis and bivalves. 

2008010062 

贵州台江中寒武世凯里生物群古生态研究 

= Paleoecology of the Kaili Biota from Middle 

Cambrian in Taijiang County, Guizhou Province, 

China. ( 中文 ). 杨瑞东 ; 赵元龙 ; 毛家仁 ; 

聂爱国 ; 陈笑媛 . 沉积学报 , 2002, 20(1): 129- 

134,155 

凯里生物群是世界三大布尔吉斯页岩型 

生物群之一。本文通过古生物个体埋藏保 

存情况、古生物个体生态学、沉积学和地 

球化学等的研究和分析 , 认为凯里生物群 

中大部分分子是从异地搬运到陆棚环境埋 

藏的。同时 , 提出了凯里生物群的埋藏机 

理模式和生态复原因。 

2008010063 

一种巨菌类记录的泥盆纪景观的多相性 = 

Devonian landscape heterogeneity recorded 

by a giant fungus. ( 英文 ). Boyce C K; Hotton 

C L; Fogel M L; Cody G D et al.. Geology, 

2007, 35(5): 399-402 

The enigmatic Paleozoic fossil Prototaxites 

Dawson 1859 consists of tree-like trunks as 

long as 8 m constructed of interwoven tubes 

宾夕法尼亚亚系泥沼森林内的生态梯度 = 

Ecological gradients within a Pennsylvanian 

mire forest. ( 英文 ). DiMichele W A; Falcon- 

Lang H J; Nelson W J; Elrick S D; Ames P R. 

Geology, 2007, 35(5): 415-418 

Pennsylvanian coals represent remains of 

the earliest peat-forming rain forests, but there 

is no current consensus on forest ecology. Localized 

studies of fossil forests suggest intermixture 

of taxa (heterogeneity), while, in contrast, 

coal ball and palynological analyses imply 

the existence of pronounced ecological 

gradients. Here, we report the discovery of a 

spectacular fossil forest preserved over 1000 

ha on top of the Pennsylvanian (Desmoinesian) 

Herrin (No. 6) Coal of Illinois, United 

States. The forest was abruptly drowned when 

fault movement dropped a segment of coastal 

mire below sea level. In the largest study of its 

kind to date, forest composition is statistically 

analyzed within a well-constrained paleogeographic 

context. Findings resolve apparent 

conflicts in models of Pennsylvanian mire 

ecology by confirming the existence of forest 

heterogeneity at the local scale, while additionally 

demonstrating the emergence of ecological 

gradients at landscape scale. 

微体古生物学 

综论 

2008010065 

西澳大利亚奥菲瑟盆地新元古代微体化石 

= Neoproterozoic microfossils from the Officer 

Basin, Western Australia. ( 英文 ). Cotter K 

L. Alcheringa, 1997, 21(3/4): 247-270 

Microfossil assemblages are described from 

the early Neoproterozoic Madley and Browne 

Formations, western Officer Basin. One chert 

and eleven siliciclastic samples yielded microfossils. 

Myxococcoides cantabrigiensis occurs 

as pustular mats in the chert sample and Eomicrocystis 

malgica, Pterospermopsimorpha 

granulata, Skiagia sp. cf. S. pusilla, and undetermined 

species of Obruchevella, Heliconema, 

and Trachystrichosphaera are present 

in acid macerated samples. Leiosphaeridia spp. 

and Siphonophycus spp. are also found in finegrained 

siliciclastic samples, with clusters of 

Synsphaeridium sp. in some samples. These 

findings enable a more substantial reconstruction 

of the palaeoenvironment of Supersequence 

1 in the western Centralian Superbasin. 

The acanthomorph acritarchs are considered to 

be planktonic eucaryotes washed into environments 

which ranged from coastal sabkha 

through to tidal flats, which may be the source 

of the prokaryotic, benthic, matforming 

cyanobacteria. 

2008010066 

晚新元古代瓮安生物群研究新进展 = New 

progress of studies on Late Neoproterozoic 

Weng'an Biota at Weng' an -Fuquan and Kaiyang 

areas, Guizhou, China. ( 中文 ). 吴祥和 . 

贵州地质 , 2002, 19(1): 1-5 

产于贵州瓮安、福泉、开阳地区晚新元 

古代陡山陀期磷块岩中的多细胞藻类 , 大 

型带刺疑源类 , 蓝菌丝状体和细菌化石 , 

球状微体化石、后生动物化石等构成的瓮 

安生物群是世界上目前发现保存最完美的 

一个古生物群之一。本文在简单介绍瓮安 

生物群研究现状的基础上 , 首次批露了笔 

者近些年来觅获和初步研究的单细胞原生 

动物、多细胞类海绵动物和类腕足类后生 

动物等一批新的动物化石资料 , 为地球早 

期动物起源 , 早期生物组织分化 , 适应辐 

射、生物多样化和早期海洋生物生态系统 

提供了珍贵的化石实证材料。此外 , 还论 

述了瓮安生物群发现的科学意义。 

孢粉 

2008010067 

以色列 Mount Hermo 东南边缘侏罗纪 - 白 

垩纪界线孢粉学研究 = A palynological investigation 

across the Jurassic-Cretaceous 

boundary on the south-east flanks of Mount 

Hermon, Israel. ( 英文 ). Conway B H. Cretaceous 

Research, 1996, 17(2): 197-214 

The disconformable contact across the Jurassic-Cretaceous 

boundary on the south-east 

flanks of Mount Hermon, Israel was studied 

palynologically. The youngest Jurassic sediments 

(Beer-Sheva and Haluza Formation J6- 

J7) are of late Oxfordian age. Miospores, 

probably of (late) Berriasian age, were discovered 

within sediments in a volcanic sequence, 

the E’Shatr sequence, above the contact, 

and are considered to be the oldest Cretaceous 

fossils in northern Israel. Overlying 

clastic sediments (basal Hatira Formation, 

‘Nubian Sandstone’ equivalent) previously 

thought to be devoid of fossils yielded miospores 

and dinoflagellate cysts deposited during 

a transgressive pulse of probable late Barremian 

age. The new combination of the spore 

speciesBiretisporites aegyptiacanov. comb. is 

proposed. 

2008010068 

22

保加利亚南部不同海拔梯度的晚冰期 / 全新 

世植被转变 = Elevational gradients during 

the Late-Glacial/Holocene vegetational transition 

in southern Bulgaria. ( 英文 ). Stefanova V; 

Lazarova M; Wright H E. Vegetation History 

and Archaeobotany, 2006, 15(4): 333-343 

The Late Glacial and early-Holocene vegetational 

history of a newly dated pollen and 

macrofossil diagram from Besbog, a cirque 

lake at 2250 m just above the forest limit in 

the Pirin Mountains of southwestern Bulgaria, 

is compared with a newly dated pollen diagram 

for the mire Shiroka Polyana at 1400 m 

in the conifer forest of the nearby Rhodope 

Mountains in order to investigate the chronology 

of major changes in the vegetation at different 

elevations. In the Lake Besbog record 

the non-arboreal pollen assemblage of the 

Late Glacial changed abruptly to that of 

Betula, Quercus and other deciduous types. 

The date for this change is about 11.6 ka cal 

B.P. The Quercus assemblage may be composed 

of pollen blown from intermediate elevations, 

to which deciduous forest had expanded 

because of higher summer temperatures 

related to high summer insolation. At 

Shiroka Polyana (1400 m) in the modern conifer 

belt, a similar change did not occur until 

about 8.8 ka cal B.P. The persistence of the dry 

steppe or steppe forest in the early Holocene 

at this lower site can also be attributed to high 

summer insolation. Thus as atmospheric temperature 

increased at the end of the Late Glacial, 

deciduous forests expanded first at intermediate 

elevations in the Pirin Mountains and 

only later in the Rhodope Mountains at lower 

elevations as summer insolation decreased. 

2008010069 

墨西哥东南部 5000 年来孢粉记录的热带森 

林和红树林历史及对海面上升的意义 = 

Tropical forest and mangrove history from 

southeastern Mexico: a 5000 yr pollen record 

and implications for sea level rise. ( 英文 ). 

Torrescano N; Islebe G A. Vegetation History 


A 250 cm long core from El Palmar, a 

swamp area located along the Rio Hondo river 

in the south of the Yucatan Peninsula, near the 

Belizean border, reveals the environmental 

history of the mangrove and tropical forest of 

the last 5000 years. The period between 5000 

and 4600 B.P. shows sandy deposits, which 

form the early infill and development of the 

swamp. A medium-statured tropical forest 

covered the area and members of the 

Moraceae and Fabacaeae dominated this early 

forest. The period between 4600 and 4000 B.P. 

presents a clear change to a mangrove system 

with Conocarpus erecta and Rhizophora mangle 

as dominant trees. This vegetational 

change is due to flooding of the Rio Hondo 

river, which deposits sediments of high salinity 

due to higher sea-level. The mediumstatured 

forest became established at some 

distance from the swamp area. After 4400 B.P. 

C. erecta appears as the dominant mangrove 

species and the R. mangle stands are less predominant 

in the area. The tropical forest was 

close to the swamp area and was mainly composed 

of members of the Moraceae, Arecaceae 

and Fabaceae as dominant taxa of this vegetational 

mosaic. 

2008010070 

英国铁器时代农作物生产和消费的再分析 

及其含义 = A re-analysis of agricultural production 

and consumption: implications for 

understanding the British Iron Age. ( 英文 ). 

Veen van der M; Jones G. Vegetation History 


Patterning in the carbonized seed assemblages 

from Iron Age sites in Britain has led to 

the development of several explanatory models. 

The most influential of these, by Martin 

Jones, proposed that grain-rich assemblages 

represent producer sites and weed-/chaff-rich 

assemblages consumer sites. The assumptions 

underlying this model and the method of constructing 

the diagrams are discussed and a new 

approach is put forward, stressing the need for 

appropriate levels of analysis and interpretation. 

It is concluded that a predominance of 

grain-rich samples is far more likely to be an 

indicator of the scale of production and consumption, 

than a means of distinguishing between 

the two. A review of the evidence from 

Iron Age Britain indicates that grain-rich site 

assemblages primarily occur in the south of 

the country, and frequently co-occur with pits, 

used for the storage of surplus grain. Moreover, 

such pits are concentrated in hillforts. It 

is proposed that the grain stored in such pits 

may have been used in large communal feasts 

and that the hillforts functioned as locations 

for feasting. 

2008010071 

旧房子中干燥植物遗存的考古分析价值 : 

农作物杂草组合的研究方法及解释 = The 

value of the archaeobotanical analysis of desiccated 

plant remains from old buildings: 

methodological aspects and interpretation of 

crop weed assemblages. ( 英文 ). Ernst M; 

23

Jacomet S. Vegetation History and Archaeobotany, 

2006, 15(1): 45-56 

Plant material like threshing remains has 

been used systematically as filling and insulation 

material in buildings for a long time. Such 

plant material can be found in several places, 

for example in floor cavities (internal floor 

deposits, Fehlböden) or in beam holes. For the 

first time in Switzerland, desiccated plant material 

like this has been investigated. In this 

article the analysis of the material from three 

different sites is presented, each dated to a 

different period, from the late medieval period 

to the time just before the industrial revolution. 

The samples consisted of chaff from Triticum 

spelta in bulk, and smaller amounts of other 

cereals such as T. monococcum, Avena sativa, 

Panicum miliaceum and Secale cereale, plus 

various weeds. The assemblages in the late 

medieval samples show evidence of threefield 

rotation: the high percentage of grassland 

species is interpreted as an indicator of the 

fallow land phase within the three-field system. 

A higher ratio of annual to perennial 

plants in the more modern samples indicates 

the development of more intensive tillage and 

cultivation. Methodological questions regarding 

sampling strategies of the floor cavity subsamples 

are investigated. The analyses suggest 

that the volume of these subsamples should be 

more than two litres. 

2008010072 

乌拉圭塞罗拉尔戈省 "El Baron" 溪二叠纪 

Melo 组孢粉和沉积 = Palynology and sedimentology 

of Melo Formation (Permian) in 

"El Baron" stream, Departamento Cerro Largo, 

Uruguay. ( 其他 ). Beri A; Pecoits E. 

Ameghiniana, 2001, 38(4): 419-428 

A palynological analysis of one surface 

sample of black shale from the "El Baron" 

stream, Cerro Largo, Uruguay, was performed. 

Twenty one species were found, corresponding 

to 16 genera. The assemblage is almost 

exclusively,composed of striated pollen grains. 

The most frequent genera are: Vittatina, Weylandites, 

Marsupipollenites, Lunatisporites 

and Lueckisporites. This assemblage was 

compared with others from the same basin 

using principal components analysis (PCA). 

The results of this analysis indicate that the El 

Baron palynological assemblage is very similar 

to that found in borehole 221 (Cerrillada) 

and is rather different from the rest of the palynoflorae 

described from the Melo Formation. 

From the biostratigraphical point of view, this 

palynoflora is comparable with the Lueckisporites 

virkkiae Biozone from the Parana basin 

in Brazil and with the Striatites Biozone 

from the Chaco-Parana basin in Argentina, 

which is interpreted as Late Permian in age. It 

is inferred that arid environmental conditions 

prevailed at the moment of the deposition of 

the studied sediments. 

2008010073 

新疆库车库尔哈剖面两个新生代孢粉组合 

的时代和环境意义 = Two Cenozoic palynological 

assemblages of the Kurha section,Kuqa,Xin 

jiang and their age and environmental 

significance. ( 中文 ). 金小赤 ; 王大 

宁 ; 柳永清 ; 张建平 . 地质通报 , 2002, 21(12): 

823-833 4 图版 . 

库车盆地的新生界发育比较完整 , 笔者在 

库车县城北东方向约 50km 的库尔哈村西的 

河谷中测制了剖面。于 66 层的 44 号样和 

90 层的 50 号样品中获得了两个孢粉组合。 

66 层和 90 层皆属于康村组 , 两个样品之间 

相差约 200m( 真厚度 )。在此之前 , 尚未见到 

有关康村组孢粉化石的报道。44 号样的孢 

粉组合中被子植物花粉占绝对优势 , 含量高 

达 94.5%, 裸子植物花粉和蕨类植物孢子均 

少量出现。孢粉面貌反映以草原和灌丛为 

主的植被类型。50 号样的孢粉组合中被子 

植物花粉占优势 (66.5%), 裸子植物花粉有较 

高含量 (32.0%), 蕨类植物孢子零星出现。孢 

粉面貌反映盆地周缘广泛分布有以松科为 

主的高山针叶林带。 

2008010074 

青藏高原晚新生代孢粉组合与古环境演化 

= Late Cenozoic environmental evolution of 

the Qinghai-Tibet Plateau as indicated by the 

evolution of sporopollen assemblages. ( 中文 ). 

吴珍汉 ; 吴中海 ; 叶培盛 ; 胡道功 ; 彭华 . 中国地 

质 , 2006, 33(5): 966-979 2 图版 . 

对取自沱沱河盆地、通天河盆地、那曲 

盆地、东温泉盆地、乌郁盆地的新近纪湖 

相沉积与取自巴斯错、错鄂、纳木错的晚 

第四纪湖相沉积 , 进行孢粉分析 ; 结合西宁 — 

民和盆地、伦坡拉盆地、南木林盆地、渭 

河盆地的孢粉资料 , 分析青藏及邻区新生代 

晚期古植被和古环境的演化过程。发现渐 

新世晚期 — 中新世早期青藏与周边邻区的 

古环境发生了显著分异 , 导致青藏地区热带 

亚热带植物濒临消亡 , 与全球温暖气候条件 

和青藏地区古纬度环境不符 , 是青藏高原隆 

升的重要标志。中新世早期 — 第四纪晚期 , 

青藏高原落叶阔叶林和针叶林呈现总体减 

24

少趋势和准周期性波动 , 与全球气候变化呈 

良好对应关系。第四纪晚期草本植物含量 

逐步增高 , 出现蒿 — 松 — 桦为主 , 针叶林、落 

叶阔叶林、灌木、草本植物混生的植被景 

观。 

2008010075 

浙江湘湖地区全新世孢粉记录及其古气候 

意义 = Holocene sporopollen records in the 

Xianghu area, Zhejiang and their palaeoclimatic 

significance. ( 中文 ). 顾明光 ; 陈忠大 ; 卢 

成忠 ; 汪庆华 ; 覃兆松 ; 张素君 . 中国地 

质 , 2006, 33(5): 1144-1148 

依据钱塘江南岸跨湖桥全新世地层剖面 

的孢粉分析 , 结合 14 C 测年以及沉积物岩性岩 

相特征 , 将浙江湘湖地区全新世早、中期 

(10~2.9 ka B.P.) 划分为 3 个古气候发展阶 

段。概述了孢粉组合、植被类型以及气候 

冷暖、干湿的交替、演化规律 , 并指出第 Ⅱ 

气候阶段 (7.7~5.0 ka B.P.) 相当于与全球变 

化相一致的全新世气候最适宜期 , 跨湖桥文 

化就是在这样的气候背景中孕育和发展 

的。本区全新世早期的气候变化与中国南 

方的深圳湾地区有很好的可比性。 

2008010076 

甘肃北山北部红石山地区泥盆纪雀儿山群 

及古孢子化石组合基本特征 = Features of 

the strata for Devonian Queershan Group in 

Hongshishan area of Beishan′s northern 

belt,Gansu. ( 中文 ). 张国英 . 西北地质 , 2006, 

39(1): 83-88 

在 1∶25 万红宝石幅 (K47C002001) 图幅 

中 , 雀儿山群分布于哈萨克斯坦板块南缘 , 红 

石山蛇绿混杂岩带以北地带的双沟山 — 雀 

儿山一带 , 为一套宏观色调为灰绿色中基 

性、中酸性火山岩及其火山碎屑岩夹碎屑 

岩和灰岩的岩石组合。碎屑岩及灰岩中含 

腕足、珊瑚、三叶虫、海百合茎等生物化 

石。其中 :Latonotoechia cf. latana(Barrande) 

原产于波希来亚地区布拉格期。 

Acrospirifer cobedanus varius Kaplun 见于哈 

萨克斯坦地区下泥盆统中上部和新疆的和 

布克赛尔组。Eoschuchertella guangxiensis 

Wang et Rong 原于广西郁江组上部六景 

段。该群形成于与岛弧有关的滨浅海环境 , 

在区域上可与新疆大南湖组、头苏泉组及 

和布克赛尔组对比。该群形成时代为早 — 

中泥盆世 , 年代地层为下 — 中泥盆统。 

2008010077 

兴梅地区早石炭世古孢子化石的组合特征 

= Characteristics of Early Carboniferous spore 

assemblage in the Xingmei area. ( 中文 ). 李文 

辉 . 广东地质 , 2002, 17(1): 44-50 

粤东北兴梅地区早石炭世大湖组和忠信 

组的古孢子化石组合以具有泥盆 - 石炭纪 

过渡类型为特征。根据其产出的地层位置 

和组成特征 , 定为 Dictyotriletes submarginatus 

- Triquitrites tricuspis 组合带。其中的 

孢子较原始 , 组成较复杂 , 以具有泥盆 - 

石炭世过渡类型为主 , 但含有较多的繁盛 

于早石炭世分子 , 故其时代定为早石炭世 

杜内期 - 维宪期早期。 

2008010078 

湛江田洋玛珥湖孢粉组合与古气候变化 = 

Pollen assemblages and paleoclimate changes 

from a core in Tianyang Maar Lake of Zhanjiang. 

( 中文 ). 陈俊仁 ; 姚伯初 ; 吴能友 . 广东地 

质 , 2002, 17(3): 21-32 

田洋玛珥湖位于我国雷州半岛热带亚热 

带地区 , 以其独特的封闭性与特殊的物化 

条件 , 成为研究全球古气候变化的重要场 

所。根据孢粉组合研究 , 按冷、暖 , 湿 

润、干燥的变化 , 把近 40 万 a 来的古气候 

划分为 13 个气候期。第 11 气候期 (35 万 

a B.P.) 最热 , 年平均气温 23℃ 以上 ; 第 7 

气候期 (20 万 a B.P.) 气候炎热 , 年平均气 

温 23℃ 左右 , 是玉木 / 里斯间冰期 ;7 万 

-1.2 万 a B.P. 气候变冷 , 称玉木冰期。第 

3 气候期 (4.8 万 -3 万 a B.P.) 相对温暖 , 

称玉木亚间冰期 , 表现为湿热多雨。第 2 

气候期 (3.0 万 -1.2 万 a B.P.) 最冷 , 年平 

均气温为 14℃, 称为玉木主冰期。第 1 气 

候期就是近 1.2 万 a 以来的温暖的全新世 , 

年平均气温 22℃ 左右。 

2008010079 

银川盆地晚第四纪孢粉记录的快速气候波 

动事件 = Late Quaternary sporopollen records 

of rapid climatic fluctuation events in 

the Yinchuan basin. ( 中文 ). 范淑贤 ; 郑宏瑞 ; 

刘平贵 ; 郭盛乔 . 中国地质 , 2002, 29(4): 431- 

434 

笔者根据 CK 1 孔孢粉研究结果 , 分析了银 

川盆地 15 万年以来的万年尺度和千年尺度 

的气候波动事件 , 并利用频谱分析方法得到 

银川盆地沉积物孢粉记录的气候变化周 

期。经研究认为 , 这种万年尺度周期变化的 

气候波动可与高纬度地区米兰科维奇的规 

道变化相对比 , 而千年尺度准周期可与 D/O 

相对应。它反映银川盆地存在着万年尺度 

和千年尺度的气候波动事件。 

25

2008010080 

江汉盆地始新世中、晚期气候变化周期性 

的孢粉学证据 = Palynological evidence of 

Middle-Late Eocene climatic cycles in Jianghan 

Basin. ( 中文 ). 童国榜 ; 贾秀梅 ; 郑绵平 ; 袁 

鹤然 ; 刘俊英 ; 王伟铭 . 地球学报 - 中国地质科 

学院院报 , 2002, 23(2): 159-164 

采用时间序列分析方法对江汉盆地明钾 1 

孔的孢粉数据进行了处理 , 发现在中、晚 

始新世时期孢粉植物群的波动存在各种周 

期成分。长周期有 1.2 Ma、2.0 Ma 及 5.0 

Ma, 中周期有 0.2 Ma、0.4 Ma、0.6 Ma、 

0.8 Ma, 其中 1.2 Ma 及 0.2 Ma、0.4 Ma、 

0.6 Ma 的周期成分在第四纪孢粉植物群的 

演化中也存在 , 且与 8.0 Ma B.P. 以来的构 

造气候旋回 , 亚旋回的准 1.2 Ma 及 0.4 Ma 

周期相一致。这表明地球运动轨道变化对 

气候的制约作用由来已久。该孔孢粉时间 

序列的趋势成分显示最少有 4 个水平 , 反 

映了孢粉植物群演化的 4 个阶段。曲线还 

揭示 36 Ma B.P. 前后的波动周期及振幅都 

有明显的变异 , 可能预示了一次大的环境 

变革。这一变化在很大程度上与喜马拉雅 

一期运动和地球南半球一次大的海洋和气 

候变冷事件相吻合。 

2008010081 

西藏拉萨地块设兴组孢粉化石新发现及其 

地层学意义 = New palynological materials 

from the Shexing Formation in the Lhasa 

block, Tibet, and their stratigraphic significance. 

( 中文 ). 纪占胜 ; 杨欣德 ; 臧文拴 ; 姚建 

新 ; 吴中海 ; 武桂春 . 地球学报 - 中国地质科学 

院院报 , 2002, 23(4): 323-328 1 图版 . 

拉萨地体的典中 - 那玛剖面设兴组上部 

新发现孢粉组合 , 其特征为 : 孢粉化石多 

为第三纪常见分子 , 未发现早白垩世和晚 

白垩世特征分子。因此样品产出的层位不 

可能属于白垩纪的沉积。孢粉组合以落 

叶 , 阔叶植物为主体 , 主要为桦科的桤木 

粉 ( Alnipollenites) , 桦粉 

( Betulaepollenites) , 枥粉 

( Carpinipites ), 山毛榉科的栎粉 

( Quercoidites) 胡桃科的胡桃粉 

( Juglanspollentites) , 榆科的榆粉 

( Ulmipollenites) , 椴科的椴粉 

(Tiliaepollenites) 等 , 热带 , 亚热带植物孢 

粉少量出现 ; 草本植物花粉再现很少 , 如 

晚第三纪常见的藜科 (Chenopodiaceae), 

菊科 (Compositae), 禾本科 (Gramineae) 

及蓼科 (Polygonaceae) 等 , 指示了样品所 

在层位沉积时的气候并不干旱 ; 早第三纪 

早期大量出现的三孔沟 , 网面三孔沟等花 

粉少量出现 ; 孢粉总的面貌反映了温凉 , 

温润的温带气候 , 指示了落叶 , 阔叶森林 

广泛分布。孢粉组合更接近于早第三纪中 

晚期的面貌 , 其时代可能属于始新世 - 渐 

新世。本次孢粉的面貌与伦坡拉盆地的牛 

堡组中段孢粉化石面貌有想相似 , 与牛堡 

组上段和牛堡组之上的丁青组 ( 渐新统 ) 

孢粉面貌相差甚远。因此推测 , 典中 - 那 

玛剖面设兴组产出孢粉的层位与牛堡组中 

段可能处于大致相同的时代或稍晚的时 

代。典中 - 那玛剖面的设兴组可能不仅仅包 

括晚白垩世晚期的地层 , 还包括下第三系的 

成分。 

2008010082 

三塘湖盆地晚二叠世芦草沟组孢粉组合 = 

Late Permian sporopollen assemblage from 

Lucaogou Formation in Santanghu basin. ( 中 

文 ). 尹凤娟 ; 刘洪福 ; 华洪 . 石油与天然气地 

质 , 2002, 23(4): 392-396 1 图版 . 

三塘湖盆地芦草沟组为一套以灰色泥岩 

为主的浅湖半深湖相沉积。泥岩中产丰富 

的孢粉化石 , 计有 26 属 28 种。经研究表明 , 

芦草沟组孢粉组合是以裸子植物花粉占绝 

对优势、蕨类植物孢子含量很低为特征。 

Cordaitina,Hamipollenites,Protohaploxypinus 

,Striato 

abieites ,Striatopodocarpites 和 Alisporites 等 

花粉在组合中占主导地位。根据孢粉组合 

特征及其对比 , 芦草沟组的地质时代属晚二 

叠世早期 ; 孢粉颜色反映当时的古地温应为 

60~110℃, 有机质演化属低成熟阶段。 

2008010083 

西藏札达盆地晚上新世古植被型分析 = 

Palaeovegetation type analysis of the Late 

Pliocene in Zanda Basin of Tibet. ( 中文 ). 李 

建国 ; 周勇 . 古地理学报 , 2002, 4(1): 52-58 

札达盆地晚上新世生长着以高山荒漠小 

灌木、草原、亚高山常绿针叶林和中低山 

常绿针叶林为主的植被。气候显示了从干 

旱寒冷至温暖湿润的垂向分异 , 总体偏于 

干、寒 , 属亚热带高山或亚高山类型。当 

时区内海拔已较高 , 南低北高的地势特征 

也已形成。古植被重建及现青藏高原的植 

被调查资料表明 , 当时盆地最低处的海拔 

可能不会超过 2 500 m, 其周围及北部可能 

存在海拔 4 000 m 的高地或更高的山峰。 

中、晚上新世迄今 , 该地区隆升的高度可 

26

能不会超过 1 000 m, 其幅度小于喜马拉雅 

山中部地区。 

2008010084 

阿根廷门多萨前科第勒拉泥盆纪 

Villavicencio 组孢粉新瓷料 = New palynological 

data from the Devonian Villavicencio 

Formation, Precordillera of Mendoza, Argentina. 

( 英文 ). Rubinstein C V; Steemans P. 

Ameghiniana, 2007, 44(1): 3-9 

New terrestrial and marine palynomorphs of 

the lower part of the Villavicencio Formation, 

San Isidro Creek, Precordillera of Mendoza, 

Argentina, are evaluated. The palynomorph 

assemblage is dominated by miospores, and 

also contains acritarchs and scarce chitinozoans. 

Different processing methods have been 

tested due to the poor preservation state of the 

palynomorphs. The new slides provided abundant 

and diverse palynomorphs and allowed 

the recognition of 13 miospore species and 

two acritarch species. This review suggests a 

late Pragian to early Emsian age, thus confirming 

and refining previous palynological 

dating. The miospore assemblage may be correlated 

with the upper part of the Ems Biozone 

in terms of the Devonian miospore zonation of 

the Brazilian Amazon Basin. Palaeogeographically; 

acritarchs show perigondwanan 

affinities. In the light of this refined 

age determination, the stratigraphic and phytogeographic 

inferences for the Precordillera 

land plants should be reconsidered. 

2008010085 

根据阿根廷火地岛南部 Beagle 海峡孢粉资 

料推断全新世海平面变化 = Holocene sealevel 

change inferred from palynological data 

in the Beagle Channel, southern Tierra del 

Fuego, Argentina. ( 其他 ). Borromei A M; 

Quattrocchio M. Ameghiniana, 2007, 44(1): 

161-171 

An early-middle Holocene section in Bahia 

Lapataia (54 degrees 50'S, 68 degrees 34' W), 

Beagle Channel, Tierra del Fuego, Argentina 

has been examined taking into account its 

sporomorphs and organic-walled microplankton. 

The palynological assemblage suggests 

nearshore environments. Two relatively higher 

sea levels were identified by the increased 

abundance of organic-walled dinoflagellate 

cysts (Brigantedinium spp., Selenopemphix 

sp., Operculodinium centrocarpum sensu Wall 

and Dale, Spiniferites spp.), the acritarch 

Halodinium sp. and zoomorph remains (test 

linings of foraminifera and copepod eggenvelopes). 

The littoral vegetation at the time 

of the marine incursion was mainly arboreal, 

as can be seen in the pollen records by significant 

increase in Nothofagus dombeyi type frequencies, 

while a forest-steppe vegetational 

pattern developed regionally. After comparison 

with another nearby fossil marine terrace, 

the palynological analysis has demonstrated 

that these terraces represent the same transgressive-regressive 

event. The relative altitudinal 

differences between these terraces in the 

area may be the result of seismotectonic activity 

during the Holocene. 

2008010086 

山东济宁煤田 ( 东区 ) 晚古生代孢粉组合 

= Study on Late Paleozoic sporopollen assemblages 

in east part of Jining Coalfifld, Shandong 

Province. ( 中文 ). 蒋汉朝 ; 王明镇 ; 张锡 

麒 ; 李增学 . 地质科学 , 2002, 37(1): 47-61 

鉴定了山东济宁煤田 ( 东区 ) 晚古生代 

孢粉组合中的孢粉化石 70 属 189 种。据孢 

粉化石在地层中的分布和垂向的变化规律 

自上而下建立了 5 个孢粉组合 :V. Cyclogranisporties 

pressus-Lycospora pellucida 组 

合 ,IV. Granulatiporites piroformis 组合 ,III. 

Sinulatisporites sinensis 组合 ,II. Thymospora 

pseudothiessenii-T. thiessenii 组合 , 

I. Densosporites annulatus 组合。通过与邻区 

及华北部分地区对比 , 确定本区孢粉组合 

的地质时代应为 : 晚石炭世晚期 ( 组合 

I), 早二叠世早期 ( 组合 II), 早二叠世 

中期 ( 组合 III), 早二叠世晚期 ( 组合 

IV) 和晚二叠世早期 ( 组合 V), 本区石 

炭系 - 二叠系界线应置于太原组第 11 层灰 

岩之底。 

2008010087 

家燕 (Hirundo rustica) 粪便的孢粉分析 = 

Pollen analysis of barn swallow faeces (Hirundo 

rustica). ( 英文 ). Bińka K. Acta Palaeobotanica, 

2005, 45(2): 187–194 

Pollen analysis of barn swallow faeces collected 

at ca. 12-day intervals since their arrival 

from Africa for late summer flights has been 

made. This study showed that through the 

alimentary canals of insect-consuming barn 

swallows, a high proportion of pollen of entomophilous 

plants from the close vicinity of 

the study area can be transmitted again into 

environment. Pollen of anemophilous plants, 

attached to the bodies of insects have also 

been passed to these areas. Also, grains of 

plants growing not only in the close vicinity 

but also occurring in more distant areas – sev- 

27

eral kilometres away of the study area are 

noted in the pollen spectra. This shows that 

pollen spectra from swallow faeces are representative 

for territories larger than it is suggested 

by their foraging distances. Pollen 

grains passing through the intestines of barn 

swallows and selected insects analysed both at 

light (LM) and transmission (TEM) microscopy, 

showed in some cases ultrastructural 

signs of initial destruction of the endexine 

structure or sporadically degraded exine. 

2008010088 

内蒙古东胜中侏罗世孢粉植物群与沉积环 

境 = Middle Jurassic palynoflora and its evvironmental 

significance of Dongsheng, Inner 

Mongolia. ( 中文 ). 江德昕 ; 王永栋 . 沉积学 

报 , 2002, 20(1): 47-54 2 图版 . 

基于内蒙古东胜地区中侏罗统延安组发 

现的孢子花粉 34 属 63 种的研究 , 建立了 

研究区中侏罗世早期孢粉植物群。根据孢 

粉植物的特征探讨了该区早中侏罗世古生 

态、古气候和沉积环境及其对煤炭、石油 

和天然气形成的关系。研究结果表明 , 暖 

湿 ( 或湿热 ) 气候条件下的湖泊沼泽沉积 

对煤和油气的形成有巨大潜力。 

2008010089 

塔里木盆地石油运移的孢粉学证据 = Palynological 

Evidence for Petroleum Migration in 

Tarim Basin. ( 中文 ). 江德昕 ; 王永栋 ; 魏江 . 沉 

积学报 , 2002, 20(3): 524-529 1 图版 . 

基于塔里木盆地塔北、库车、喀什和叶 

城四个含油气区 44 个原油样品和 3 个天然 

气样品中发现的化石孢子花粉 89 属 183 种 

的研究 , 在盆地地质背景下探讨了石油运 

移的机理。研究内容包括石油运移的通 

道、相态、方向、路线和期次。研究结果 

表明 , 在油气源岩成岩过程中由异常高压 

形成的微裂隙是石油初次运移的通道 ; 断 

层、不整合面 ; 节理和其他裂隙是石油二 

次运移的通道 ; 在运移过程中石油可保持 

其原有相态 , 液态与气态混合相是塔里木 

盆地石油运移过程中的主要相态 ; 石油运 

移的方向因油藏类型而异 , 或以垂直运移 

为主 , 或以侧向运移为主。 

2008010090 

新疆吐哈盆地侏罗纪古植被与古气候及古 

环境的探讨 = Jurassic palaeoclimate, palaeovegetation 

and palaeoenvironment in the 

Tuha Basin in Xinjiang. ( 中文 ). 张代生 ; 付国 

斌 ; 秦恩鹏 ; 侯全政 ; 李兴亮 . 现代地质 , 2002, 

16(2): 147-152 

通过对新疆吐哈盆地侏罗系孢粉植物 

群、特殊岩性、泥质岩中的元素和粘土矿 

物分布规律的研究 , 探讨了古植被、古气 

候及古环境的纵向演化特点 , 认为研究区 

内侏罗纪古气候特点早侏罗世至中侏罗世 

早期为温暖潮湿的亚热带 , 局部有干旱趋 

势 ; 中侏罗世中晚期为半潮湿、半的温 

带 — 亚热带气候 ; 从中侏罗世末期开始转 

为炎热干旱的亚热带气候。 

2008010091 

藏北多格错仁红层及孢粉组合特征 = Strata 

and spores association of Dogai Coring redbeds 

of North Tibetan Plateau. ( 中文 ). 吴珍汉 ; 

江万 ;Doug Nelson; Bill Kidd. 现代地 

质 , 2002, 16(3): 225-230 

青藏高原北部羌塘地块广泛出露第三纪 

陆相红层 , 确定这些红层及其变形的时代 

对认识青藏高原形成演化过程具有非常重 

要的意义。1998-1999 年 ,INDEPTH-III 项 

目地质课题组人员 2 次深入西藏可可西里 

地区进行科学考察 , 新发现藏北多格错仁 

红层 , 并在其中发现较多种属的孢粉化 

石。该孢粉组合反映以温带早生草原为主 

体的古植被面貌。通过对青藏高原北部及 

邻区主要新生代盆地孢粉组合与古环境演 

化的对比分析 , 结合多格错仁红层上覆弱 

变形玄武岩 2.5 - 3.2Ma 的 40 Ar— 39 Ar 高精度 

测年资料 , 推断多格错仁红层的形成时代 

为晚中新世 , 多格错仁红层挤压变形所致 

的约 50% 的地壳缩短量发生在中新世末一 

上新世纪。这些资料为建立青藏高原动力 

学模式提供了新的年代依据。 

2008010092 

青海北祁连区早三叠世中 — 晚期孢粉组合 

= Sporo pollen assemblages of middle to late 

stage of Early Triassic Epoch in North Qilian, 

Qinghai. ( 中文 ). 冀六祥 . 青海地质 , 2001, 

11(1): 61-72 4 图版 . 

青海北祁连区早三叠世中 - 晚期 , 孢粉 

丰富 , 保存完整 , 共发现孢子花粉 80 属 

129 种 , 疑源类 15 属 20 种。孢粉组合是以 

Aratrisporits-Klans-ipollenites- 

Micrhystridium 广泛出现为主要特征 , 地质 

时代为奥伦尼克阶 (Olenikian) 期。 

2008010093 

云南鹤庆盆地的孢粉记录及 1.0Ma 以来的 

构造抬升与气候变迁 = Pollen records and 

28

environmental evolution of Heqing basin in 

Yunnan Province since 1.0 Ma. ( 中文 ). 蒋雪 

中 ; 羊向东 ; 王苏民 . 海洋地质与第四纪地 

质 , 2002, 22(2): 99-104 

依据鹤庆盆地 168m 钻孔孢粉资料 , 对该 

区 1.0 MaBP 以来古值衩演替的阶段性特征 

进行了研究 , 探讨了该区植被和气候对高 

原隆升不同阶段的响应特点。明显的气候 

转型发生在 0.73 和 0.42~0.368 MaBP。 

0.165 MaBP 前后 , 山体抬升引起的树线变 

化植被响应不甚明显 , 可能与山体上升到 

一定高度和垂直带谱的稳定形成有关。13.2 

kaBP 时 , 构造的差异升降和气候变化导致 

湖盆被切穿。 

2008010094 

中国石炭系孢粉组合带序列 = Carboniferous 

miospore zonation in China. ( 中文 ). 朱怀 

诚 . 微体古生物学报 , 2001, 18(1): 48-54 

我国是世界上唯一的在石炭纪发育有欧 

美植物区、华夏植物区、安加拉植物区和 

冈瓦纳植物区植物群的国家 , 并以欧美 — 华 

夏植物群最为发育。本文总结了近 20 年来 

华北和西北 ( 新疆、甘肃、宁夏 ) 的石炭系孢 

粉研究成果 , 提出了适合我国大部分地区的 

石炭系孢粉组合带序列方案 ( 计 15 个孢子 

带 ), 描述了各带的特征 , 依据孢子带的对比 

和同层所产动物化石 , 讨论了它们的时代。 

2008010095 

江苏太湖平原北翼的第四纪孢粉与环境 = 

Quaternary pollen analysis and paleoenvironmental 

evolution in the northern part 

of Taihu Plain, Jiangsu. ( 中文 ). 周曙 ; 邹松梅 ; 

刘志平 ; 蒋梦林 ; 朱志远 ; 刘金陵 ; 钟石兰 ; 李星 

学 ; 穆西南 ; 韩辉友 ; 李升峰 . 微体古生物学 

报 , 2001, 18(1): 55-69 

本文根据太湖东北侧 4 个钻孔的孢粉分 

析 , 14 C 和古地磁测试 , 并结合钙质超微化 

石、介形类和有孔虫所确定的海侵地层 , 将 

太湖地区划为 10 个孢粉带 , 再参照长江下游 

相关资料 , 着重对 12.7— 1.5 万年以来的 4 

个孢粉带作了较深入的环境探讨 , 揭示出 Ⅵ 

带 (12.7—7.0 万年 ) 为常绿落叶阔叶混交林 , 

反映温暖湿润的亚热带气候 , 其主要温暖阶 

段冬温较今高 4— 5°C, 当时湿度相对偏 

大 , 当然其中也有凉湿与干凉时段。Ⅶ 带 

(7.0—3.0 万年 ) 为疏林草原 , 反映冷 ( 半 ) 干气 

候 , 其主要寒冷阶段年均温为 8°C 左右。但 

仍存在剧烈的气候波动。Ⅷ 带 (3.0—2.1 万 

年 ) 为温性常绿落叶阔叶混交林 , 反映温凉湿 

润的季风海洋性气候 , 其主要温凉阶段生长 

季月均温比现在低约 3°C。其中亦有更为 

干冷或暖湿时期。Ⅸ 带 (2.1— 1.5 万年 ) 为 

森林草原 — 草原或干草原植被 , 其极干冷阶 

段年均温约 8°C, 年降雨量 400mm 左右。 

2008010096 

新疆三塘湖盆地塘浅 3 井早侏罗世孢粉组 

合 = Early Jurassic sporopollen assemblage 

from Tangqian-3 well of the Santanghu basin, 

Xinjiang. ( 中文 ). 黄嫔 . 微体古生物学 

报 , 2001, 18(1): 76-88 4 图版 . 

本文对在新疆三塘湖盆地塘浅 3 井 701— 

834m 层段发现的孢粉植物群进行了系统的 

分析研究 , 共获孢粉 45 属 93 种 ( 包括 1 新 

种 ), 疑源类化石 5 属 5 种及一个未定类型 , 组 

成以 Osmundacidites- Piceites- Pinuspollenites-Quadraeculina 

为主的孢粉组合。根 

据孢粉组合特征 , 认为其时代应归为早侏罗 

世晚期。对组合中主要孢粉属种可能的母 

体植物的生长环境进行分析 , 推测新疆三塘 

湖地区在早侏罗世晚期为温带 — 亚热带气 

候。 

2008010097 

西藏西部札达盆地上新世孢粉植物群及古 

环境 = Pliocene palynoflora from the Zanda 

Basin, west Xizang (Tibet), and the palaeoenvironment. 

( 中文 ). 李建国 ; 周勇 . 微体古生物 

学报 , 2001, 18(1): 89-96 2 图版 . 

孢粉组合以松科两气囊花粉与被子植物 

藜科花粉为主 , 禾本科及麻黄花粉有一定的 

含量 , 含有少量亚热带常绿或落叶阔叶林分 

子 , 蕨类孢子少量。时代属上新世中晚期 , 亦 

不能完全排除更新世的可能。孢粉植物群 

显示比较清晰的植被垂直分带现象 , 反映了 

较高海拔下的草原、灌丛草原、亚高山针 

叶林、低山落叶阔叶林、低山常绿阔叶 — 

针叶林植被。当时气候偏干 , 可能与现在当 

地气候已较相似。盆地内地势可能为南低 

北高 , 其最低处的海拔可能在 2 000—2 500 

m 左右。上新世至今地势无疑又有 1 千多 

米的隆升。 

2008010098 

神农架大九湖 12.5kaBP 以来的孢粉与植被 

序列 = Palynofloras of the Dajiuhu basin in 

Shennongjia mountains during the last 12.5ka. 

( 中文 ). 刘会平 ; 唐晓春 ; 孙东怀 ; 王开发 . 微体 

古生物学报 , 2001, 18(1): 102-109 

在神农架海拔 1 700 m 的大九湖盆地 

12.5 ka BP 以来晚第四纪中 , 高密度地取得 3 

个钻孔的孢粉样品 , 建立起晚第四纪高分辨 

29

率孢粉组合序列 , 划分出 15 个综合孢粉带 , 

代表 15 个不同时代类型的古植物群落。根 

据植被演替及其所反映的气候变化过程 , 本 

文还讨论了第四纪植被与气候阶段的划分 

问题 , 认为高分辨率孢粉 — 植被序列的建立 

与研究可以反映多种时间尺度 , 特别是小尺 

度的环境变化与事件 , 从而更详细地揭示其 

演变轨迹与特点。 

2008010099 

新疆吐哈盆地北缘黄山街组孢粉组合 = 

Sporopollen assemblage of the Huangshanjie 

Formation from the northern margin of the 

Tuha Basin of Xinjiang, NW China. ( 中文 ). 

刘兆生 . 微体古生物学报 , 2001, 18(2): 163- 

172 2 图版 . 

新疆鄯善照壁山沟口和柯柯亚剖面黄山 

街组的孢粉化石 , 经研究 , 共有 52 属 77 种。 

命名为 Dictyophyllidites- Aratrisporites- 

Parataeniaesporites 组合 ( 简称 DAP 组合 )。 

根据组合主要分子的已知时代分布、含量 

高低变化 , 以及与有关已知时代孢粉组合进 

行对比 , 鉴定其地质时代为晚三叠世早中 

期。根据孢粉组合恢复古植被 , 反映当时的 

气候为温暖潮湿的温带类型。 

2008010100 

江西九江第四纪红土中的植物硅酸体及孢 

粉 = Phytolith and pollen records of Quaternary 

red earth in Jiujiang City, Jiangxi Province. 

( 中文 ). 黄翡 ; 熊尚发 . 微体古生物学 

报 , 2001, 18(2): 203-210 1 图版 . 

九江第四纪红土中植物硅酸体、孢粉记 

录表明 : 该地红土是湿热环境下的产物 ; 红土 

形成时期发育了亚热带常绿落叶阔叶类植 

被 ; 九江第四纪红土中植物硅酸体保存不如 

中国北方黄土。古土壤 A 层被侵蚀及铁、 

铝氧化物的高含量可能是造成红土中植物 

硅酸体保存不佳的主要原因 ; 亚热带植被中 

乔木类植物硅酸体抗溶解力弱 ; 红土中禾本 

科植物硅酸体保存与风化指标、全有机碳 

成正相关 ; 禾本科植物硅酸体总量自剖面底 

部 ( 网纹红土 )— 顶部 ( 褐黄土层 ) 逐渐增多 , 

可能暗示中更新世晚期以来存在较为普遍 

的气候恶化趋势 , 气候总体向变冷、变干方 

向发展 ; 红土剖面 5m 及 3.0m 左右古土壤 A 

层的出现及剖面风化指标与元素地球化学 

特征表明 : 该地红土经历了堆积与风化同时 

进行的加积型风化过程。 

2008010101 

河南贾湖遗址植硅石组合及其在环境考古 

学上的意义 = Phytolith assemblages of the 

Neolithic site at Jiahu, Henan Province and its 

significance in environmental archaeology. 

( 中文 ). 陈报章 . 微体古生物学报 , 2001, 

18(2): 211-216 

本文对取自河南贾湖新石器时代遗址的 9 

块考古样品进行了植硅石分析 , 结合孢粉分 

析资料 , 恢复了该遗址的古生态环境 , 进而较 

好地解释了栖息于淮河流域的贾湖先民较 

早开始稻耕农业的生态学原因。 

疑源类 

2008010102 

早寒武世疑源类的古生物地理学意义 = 

Early Cambrian palaeobiogeography of acritarch. 

( 中文 ). 尹凤娟 ; 薛祥煦 . 西北大学学报 

( 自然科学版 ), 2002, 32(2): 177-180 

根据早寒武世疑源类在全球的古地理分 

布 , 并参考古地磁和动物化石等方面的资料 , 

进行了早寒武世疑源类的古地理分区。结 

果表明 : 早寒武世在全球范围内可分为 2 个 

疑源类古地理大区 , 即波罗的海 - 北美 - 亚、 

澳大区和地中海大区 ; 我国西南地区早寒武 

世筇竹寺期 , 可根据疑源类分为两个生态区 , 

即扬子区和江南区。这一研究结果为今后 

各区生态结构分析 , 提供了重要基础资料。 

2008010103 

浙江江山奥陶系宁国组疑源类化石的发现 

及其地质意义 = The discovery and the geological 

significance of acritarchs the Ningguo 

Formation in Jiangshan area, Zhejiang Province. 

( 中文 ). 许玩宏 ; 尹磊明 ; 郭福生 ; 彭花明 . 

华东地质学院学报 , 2002, 25(1): 6-8 

报道了发现于浙江江山奥陶系宁国组的 

疑源类化石 , 计 16 属 , 以 Baltisphaeridium, 

Leiosphaeridia, Multiplicisphaeridium, 

Peteiosphaeridium, Rhopaliophora 最常见。 

结合其它地层古生物资料 , 简要讨论这些 

微体化石的地层及环境意义。 

牙形石 

2008010104 

泰国北部 Chiang Dao 燧石岩中上泥盆统 - 

下石炭统牙形石 = Upper Devonian-Lower 

Carboniferous conodonts from Chiang Dao 

cherts, northern Thailand. ( 英文 ). Randon C; 

Wonganan N; Caridroit M; Perret-Mirouse M- 

F; Degardin J-M. Rivista Italiana di Paleontologia 


In Northern Thailand, radiolarites are very 

common and their study provides an important 

30

tool to understand the regional geology and 

moreover to localise the suture zone(s). Some 

of these deep and distal oceanic series yield 

conodonts which provide to obtain precise age 

datings. The present work is focused on the 

Upper Devonian and Lower Carboniferous 

conodonts from the Chiang Dao area. The 

conodont faunas from these oceanic cherts 

display juvenile characters which are interpreted 

to be a result from a constraining environment. 

2008010105 

掌鳞刺属演化及晚泥盆世环境变迁 = Textural 

evolution of Palmatolepis and environmental 

change in Late Devonian. ( 中文 ). 王超 

勇 ; 夏文臣 . 广西地质 , 2006, 15(2): 21-30 

牙形石掌鳞刺属 Palmatolepis 齿台结构和 

形态随时间演替 , 由近正三角形向长三角 

形、长菱形演化 , 在 F/F 界线附近受地质事件 

的影响而中断 , 使 Palmatolepis 齿台结构呈二 

段式发展 , 在 Palmatolepis 的分子中 , 那些演 

化速度快 , 结构变化大的分子首先灭绝 , 而那 

些演化速度慢 , 结构变化小的分子延续时间 

长 , 分布范围也更加广泛 , 在地质事件中被保 

留下来并得以延续 , 这种演化规律可能是生 

物有选择性灭绝与复苏的原因之一。晚泥 

盆世 F/F 之交环境的变化可能是由于海退 , 海 

底毒气喷发 , 超量金属元素的污染造成的。 

2008010106 

江西乐平地区晚二叠世 — 早三叠世的牙形 

石动物群 = Conodont fauna of Late Permian 

to Early Triassic in Leping area,Jiangxi Province. 

( 中文 ). 武桂春 ; 姚建新 ; 纪占胜 . 北京大 

学学报 ( 自然科学版 ), 2002, 38(6): 790-795 1 

图版 . 

讨论了赣中乐平地区沿沟剖面上二叠统 

至下三叠统地层的牙形石动物群 , 列出了牙 

形石的各个形态属种在地层中的分布及其 

数量变化。根据特征牙形石分子的地层分 

布 , 将该段地层自下而上划分为 3 个牙形石 

带 , 分别是 :Clarkina changxingensis-Cl. deflecta-Cl. 

subcarinata 组合带 ;Hindeodus 

latidentatus 带和 Hindeodus parvus 带。鉴于 

在晚二叠世至早三叠世 , Hindeodus 属种的 

牙形石分子的 Pa 分子成为界定种之间的主 

要标志特征 , 本文描述了两个重要牙形石种 

即 Hindeodus latidentatus 和 Hindeodus parvus 

的 Pa 分子 , 并探讨了二者之间所具有的演化 

关系 ; 此外 , 还指出这些保存完美的 Pa 分子具 

有重要的研究价值。 

2008010107 

海南岛昌江地区石炭纪牙形刺化石 = Carboniferous 

conodonts from the Changjiang 

area, Hainan Island,South China. ( 中文 ). 张仁 

杰 ; 王志浩 ; 胡宁 . 微体古生物学报 , 2001, 

18(1): 35-42 2 图版 . 

海南岛昌江地区前人所称南好组第四段 

及第三段分别发现的牙形刺 Siphonodella 

isosticha-S. cooperi 组合及 Mesogondolella 

clarki 组合 , 表明该组包括了早石炭早期及晚 

石炭世早中期 , 而不是传统认为的属早石炭 

世并可能包括中 — 晚泥盆世。同时还证实 

原南好组第三段层位远远高于第四段 , 而不 

是位于其下。从而纠正了前人长期沿用的 

该地区石炭系层序的错误。并指出昌江地 

区石炭纪牙形刺属华南古生物地理区。 

2008010108 

广西来宾瓜达鲁普统 - 乐平统界线地层的牙 

形类化石 — 一个独立验证报告 ( 英文 ) = 

Conodonts around the Guadalupian-Lopingian 

boundary in Laibin area, South China: a report 

of independent test. ( 英文 ). 查尔斯 M; 亨得森 . 

微体古生物学报 , 2001, 18(2): 122-132 

王成源 (Wang,2000 ) 和金玉玕 (Jin,2000 ) 

提出了关于乐平统底界定义的不同论点。 

为了对此进行独立的验证 , 卡尔加里大学微 

体古生物实验室对采自华南广西来宾地区 

瓜达鲁普统 — 乐平统界线地层的牙形类化 

石大块样品进行了处理。结果如 

下 :1.Jinogondolella 和 Clarkina 在样品中没有 

共生 ; 2. 由 Jinogondolella granti 演化为 

Clarkina postbitteri 的变化发生在层 115—6 

i;3. C. postbitteri 的首次出现层位 (FAD) 在 

蓬莱滩剖面位于层 115—6 i 上部 ; 4. 这个变 

化标志着一个显著的生物信号和一个重要 

的点断演化事件。Jinogondolella granti 演化 

为 Clarkina postbitteri 的事件很可能是受瓜 

达鲁普统与乐平统之交的海平面降至最低 

水位所触发和控制。层 115—6 i 下部为较 

浅水相颗粒灰岩 , 代表瓜达鲁普统末期层序 

高位域之顶或上覆层序低位域之底部。作 

为 Clarkina 属的第一个代表 ,Clarkina postbitteri 

是界线地层中最易识别的种之一 , 而 

Clarkina postbitteri 带的识别较容易和稳定 

一致。Clarkina postbitteri 和 Clarkina 

dukouensis 可以通过基于锯齿型式 , 居群和 

个体发育的分类体系来加以稳定地区分。 

Clarkina postbitteri 和 Clarkina dukouensis 之 

间的过渡是渐变的 , 其间的合办分界点只 

能人为地确定。如果采用这样一个人为确 

31

定的点来定义全球界线层型 (GSSP), 将 

难以稳定一致地对其加以识别。来自层 

114.6-6k 的被 Wang (2000) 鉴定为 Clarkina 

dukouensis 的标本应当是 C. postbitteri, 或精 

确地说可能是 C. postbitteri 的一个新亚 

种。没有争议的 Clarkina dukouensis 在蓬莱 

滩剖面最早出现于层序 114 - 7E。从生物演 

化和层序地层的角度看 ,C. postbitteri 的首 

次出现的层位 (FAD) 是瓜达鲁普统和乐 

平统界线的最清楚的候选位置。 

小壳化石 

2008010109 

贵州瓮安陡山沱期矿化生物群的研究进展 

和意义 = Advances in the study of permineralized 

biota of Doushantuo stage in Weng\'an, 

Guizhou Province and their geological significance. 

( 中文 ). 尹崇玉 ; 高林志 ; 邢裕盛 . 地球 

学报 - 中国地质科学院院报 , 2002, 23(1): 47- 

54 2 图版 . 

贵州瓮安陡山沱期矿化 ( 磷酸盐化和硅 

化 ) 生物群的研究近年来倍受关注 , 它为 

研究包括后生动物在内的多细胞生物早期 

演化提供了十分难得的机遇。最近 , 由于 

其中部分磷酸盐化球状化石保存了与某些 

后生动物胚胎早期发育阶段类似的卵袭特 

征 , 被认为是后生动物的休眠卵和胚胎化 

石。但是 , 由于至今未发现可靠的囊胚期 

到原肠胚期和幼体孵化的化石语气 , 此类 

化石的动、植物之争一直没有停止。作者 

近期对该套含磷地层进行了系统的分析研 

究 , 除已报道的大量休眠卵和胚胎化石 

外 , 还发现保存原肠胚发育特征的磷酸盐 

化实体化石、蓝藻细胞集合体、可疑海绵 

动物化石及类似瓶形的不明化石等。研究 

表明 , 陡山沱期矿化生物群具有多样性特 

征 , 包含了多种门类的不同类型 , 是迄今 

为止全球保存最完好的末元古纪磷质化石 

库。 

2008010110 

陕南新元古代末期奇异骨骼化石新发现及 

其意义 = The new discovery of peculiar 

skeleton fossils from the uppermost Neoproterozoic 

strata in South Shaanxi and its significance. 

( 中文 ). 华洪 ; 张录易 ; 谢从瑞 . 地球 

学报 - 中国地质科学院院报 , 2002, 23(5): 

387-394 

陕西宁强新元古代末期灯影组高家山段 

上部发现与 Cloudina, Sinotubulites 等管状动 

物骨骼化石共生的大量微体奇异骨骼化 

石 , 其中的一些似与寒武纪早期的小壳化 

石有一定的亲缘 , 如形态奇特的铆钉状化 

石、腹足类化石等 , 证实寒武纪与前寒武 

纪生物界之间存在明显的边续性 ; 奇异骨 

骼与陡山沱期生物也存在一定的相似性 , 

如一些分枝的管状化石 , 这一化石在组合 

具有承前启后的作用。该组合包含了可能 

的矿化后生藻类 ( 具各种分枝类型 )、矿 

化的蓝绿藻类化石等。种种迹象表明 , 在 

新元古代末期整个生物界发生了一次强烈 

的生物矿化事件 , 这一发现弥补了国内外 

新元古代末期矿化后生植物资料的空缺 ; 

磷酸盐化球状化石的研究已成为国内外研 

究的热点 , 本文所展示的球状化石由于形 

态多样 , 数量众多 , 内部结构各异 , 对其 

进行深入研究 , 可望在后生动物起源和早 

期演化研究方面取得突破。 

古植物学 

综论 

2008010111 

西藏坚扎弄组的植物化石新资料和再认识 

= New materials and further understanding of 

fossil plants in the Jianzhalong Formation,Tibet. 

( 中文 ). 石和 ; 陶晓风 ; 刘登忠 ; 胡新 

伟 ; 马润则 ; 周家云 . 地质通报 , 2002, 21(7): 

428-430 

1∶25 万措勤幅区域地质调查中 , 在夏康 

坚雪山的坚扎弄组中新采集到 Glossopteris 

sp.,Pecopteris(Ptychocarpus)sp.,Yuania 

sp.,Dicranophyllum sp. 等植物化石 , 进一步 

完善了夏康坚植物群的组合面貌 , 证实了此 

植物群确属华夏 - 冈瓦纳混合植物群。 

2008010112 

陆生植物的起源和维管植物的早期演化 = 

The Origin of land plants and the early evolution 

of land vascular plants. ( 中文 ). 郝守刚 ; 

王德明 ; 王祺 . 北京大学学报 ( 自然科学 

版 ), 2002, 38(1): 286-293 

陆生植物的起源和演化是地球生命中的 

重大事件 , 它影响到地球上所有的其他生命 

和全球环境。在过去的 20 年中 , 从中奥陶世 

历经整个志留纪至早泥盆世的岩层中 , 化石 

植物 ( 微化石和大化石 ) 的新发现改变了人们 

对陆生植物起源的认识 , 并且为陆生植物和 

维管植物早期演化分异提供了基部类群分 

化的时间框架。据此人们识别出地史中的 3 

个陆生植物的时代 : 始胚植物时代、始维管 

植物时代和真维管植物时代。另一方面 , 分 

子系统的研究使人们深入认识了植物的系 

统发育和早期分支。通过比较形态学研究 

32

和基因序列的共同努力 , 建立了植物系统发 

育树。总结了最近的进展和新的认识 , 评价 

了基于分支分析的系统发育研究。 

2008010113 

埋藏古木树轮碳、氢、氧同位素研究与古 

气候重建 = Carbon,hydrogen oxygen isotope 

studies on imbedded old tree ring and paleoclimate 

reconstruction. ( 中文 ). 孙艳荣 ; 穆治 

国 ; 崔海亭 . 北京大学学报 ( 自然科学 

版 ), 2002, 38(2): 294-301 

树轮作为自然档案的一种 , 其同位素研究 

对探讨全球气候和环境变化具有重要的意 

义。文章系统地介绍了树轮碳、氢、氧同 

位素的分馏原理 , 研究方法以及纤维素的提 

取等。研究表明 , 树轮同位素作为环境变化 

的示踪剂 , 是古环境再造和了解现代环境气 

候变化的一个强有力工具。尤其是在过去 

全球变化 (PAGES) 研究中 , 埋藏古木纤维素 

中的碳、氢、氧同位素分析已成为环境演 

化研究的主要量化手段。另外 , 对于中国这 

样典型的季风气候国家 , 开展树轮稳定同位 

素随季节性变化的研究具有重要的意义。 

我国在树轮研究方面起步较晚 , 研究方法和 

研究内容上也比较简单 , 还存在不小差距 , 既 

要进一步积累基础资料 , 又要做区域对比 , 加 

强与相关学科的交叉研究。 

2008010114 

青藏高原多年冻土沉积物中埋藏植物 DNA 

特征的初步分析 = DNA extracted from the 

plant materials buried in perennial frozen 

sediments. ( 中文 ). 林清 ; 施苏华 ; 彭平安 ; 程国 

栋 . 冰川冻土 , 2002, 24(1): 28-31 

多年冻土沉积物长期处于负温及封闭条 

件下 , 使得其中埋藏植物材料得到较好的保 

存 , 成为获取古 DNA 分子的理想材料。采 

用常规的 CTAB 法提取多年冻土中埋藏植 

物材料的 DNA, 并用琼脂糖凝胶凝胶电泳 

检测。结果表明 , 从多年冻土埋藏植物材料 

中可以提出 DNA, 而且所提出的 DNA 不仅 

具有降解的小分子量 DNA 分子 , 而且还有 

大分子量 DNA。提取的埋藏植物材料的 

DNA 多呈棕褐色 , 指示了在埋藏过程可能 

发生一定的聚合。电泳结果表明 , 随埋藏时 

间的增加 ( 深度增加 ), 埋藏植物材料中 DNA 

含量呈下降趋势。由于埋藏植物材料在不 

同时代的多年冻土中均有发现 , 其 DNA 分 

子的提取为深入研究其特征所带遗传信息 , 

重现植物大分子物质在地质历史中的演化 

提供了可能。 

2008010115 

鄂西香溪组植物化石的新发现及时代问题 

= New palaeo-plants and their age from the 

Xiangxi Formation of western Hubei. ( 中文 ). 

李旭兵 ; 孟繁松 . 华南地质与矿产 , 2002, (4): 

35-40 1 图版 . 

描述了发现于鄂西香溪组的两种植物化 

石 Ctenozamites sarrani Zeiller 和 Eboracia 

lobifolia(Phillips)。香溪组下部 Todites prinjceps 

Czekanowskia 植物组合和上部 

Coniopteris murrayana Ptilophyllum 植物组 

合虽都以真蕨类 Coniopteris 和双扇蕨科植物 

为特色 , 但下组合银杏类很多 , 苏铁类却较少 , 

而上组合苏铁类则很发达 , 尤其是 Otozamites 

hsiangchiensis,O. mixomorphus,Ptilophyllum 

contiguum 等未在下组合中出现 , 银杏类亦相 

对较少 , 上、下植物组合的这种差异明显与 

当时的气候环境有关。同时 , 依据上组合含 

Ctenozamites sarrani 和 Thaumatopteris 等分 

子和它们尚未在中侏罗世发现 , 提出香溪组 

上部的时代为早侏罗世晚期。 

2008010116 

2005 年国际生物学大会 (IBC)“ 蔷薇科演 

化 ” 专题讨论会论文集引言 = Introduction to 

the 2005 IBC symposium papers on the evolution 

of Rosaceae. ( 英文 ). Wissemann V; 

Campbell C S. Plant Systematics and Evolution, 

2007, 266(1-2): 1-3 

2008010117 

云南上新世杜鹃属和松属化石木研究及其 

古气候意义 = Pliocene rhododendron and 

pinus fossil woods of Yunan Province and 

palaeoclimate. ( 中文 ). 扆铁梅 ; 李承森 ; 姜笑 

梅 ; 王宇飞 . 古地理学报 , 2002, 4(4): 99-108 2 

图版 . 

研究了云南西部龙陵县上新世的化石 

木 , 鉴定出两种木材类型。杜鹃花科杜鹃 

属的腋花杜鹃相似种 Rhododendron cf. racemosum 

Franchet, 其主要木材特征有散孔 

材 , 生长轮略明显 , 导管具多角形轮廓 , 

螺纹加厚出现在整个导管壁上 , 梯状穿孔 

板 , 射线异形 II 型。松科华山松 Pinus armandii 

Franchet 的主要特征有交叉场纹孔窗 

格状 , 具正常轴向和纵向树脂道 , 且泌脂 

细胞壁薄 , 射线管胞内壁平滑或具稀疏的 

微锯齿。两种类型的化石木在我国均属首 

次报道。根据化石木结构和现代相应树种 

和植被的生境范围 , 当时植物生长于亚热 

带温凉湿润的山地环境 , 其海拔大约在 1 

800 m 左右。 

33

藻类 

2008010118 

新西兰上白垩统新的沟鞭藻种 : 三个属之 

间的形态中间体 = A new dinoflagellate species 

from the Upper Cretaceous of New Zealand 

- a morphological intermediate between 

three genera. ( 英文 ). Roncaglia L. Alcheringa, 

2000, 24(1/2): 135-146 

The new dinoflagellate Isabelidinium marshallii 

sp. nov. was encountered in the lower 

to middle Campanian Satyrodinium haumuriense 

Interval Zone and in the middle to 

upper Campanian Isabelidinium korojonense 

Interval Zone, in southern Marlborough, South 

Island, New Zealand. The new taxon is attributed 

to Isabelidinium but it also closely resembles 

species of Alterbidinium and Satyrodinium. 

Despite its close morphological affiliation 

to three dinoflagellate genera, I. marshallii 

represents a discrete population of 

peridinioid cysts that has a stratigraphically 

useful range in New Zealand. 

2008010119 

云南禄丰地区首次发现晚侏罗世早期轮藻 

化石组合 = Discovery of an early Late Jurassic 

charophyte assemblage in Yunnan. ( 中文 ). 

刘俊英 ; 方晓思 ; 卢立伍 . 地质通报 , 2002, 

21(2): 92-94 

近年来云南禄丰地区在地层学方面有两 

项重要的进展 :1 川街盆地不仅具有 “ 禄丰蜥 

龙动物群 ”, 在其上部还相继发现了中侏罗世 

“ 川街龙动物群 ” 和相当晚侏罗世的恐龙化 

石 ;2 按照国际地层规范 , 厘定并新建了一套 

侏罗纪岩石地层单位。新近又在前人称之 

为 “ 上禄丰组 ” 下部 ( 川街组 ) 及 “ 酒红层 ”( 麻 

地山组 ) 中分别鉴定出中侏罗世轮藻组合 

Aclistochara maanshanensis-Aclistochara 

abshirira-Aclistochara karierica 和晚侏罗世 

早期轮藻组合 Aclistochara jaisalmerensis- 

Aclistochara karierica-Mesochara voluta。这 

一晚侏罗世早期轮藻化石组合在中国属首 

次发现。 

2008010120 

湘西震旦纪武陵山生物群的化石形态学特 

征和归属 = Morphology and systematics of 

fossils in the Sinian Wulingshan biota from 

western Hunan Province. ( 中文 ). 陈孝红 ; 汪 

啸风 . 地质通报 , 2002, 21(10): 638-645 2 图 

版 . 

湘西桃源理公港震旦系留茶坡组中部黑 

色页岩中的炭质压膜化石 , 为研究末前寒武 

纪晚期生物学提供了一个稀有的布吉斯页 

岩型分类学窗口。根据已知属种和新获材 

料的研究 , 确定了 17 个明显的形态类型 , 讨 

论了每种形态类型特征及其可能的生物学 

属性 , 指出除个别化石可能为两侧对称动物 

外 , 其余绝大多数化石可以解释为原核生物 

或多细胞藻类 , 系统发育上与绿藻、褐藻、 

蓝藻细菌等相关。具固着器、叶状体为球 

状或具同心纹构造的 Apsidium sphaericus 的 

发现 , 进一步证明典型埃迪卡拉动物群 ( 或白 

海生物群 ) 中简单的圆盘状化石可能为多细 

胞藻类 , 而不是水母。武陵山生物群中具同 

心纹结构的大型圆盘状化石的出现及其共 

生生物特点 , 指示该生物群是埃迪卡拉期生 

物分异发展阶段的产物 , 是末前寒武纪晚期 

一个以多细胞藻类发育为特色的新型生物 

群。 

2008010121 

密西西比纪 - 宾夕法尼亚纪藻类 : 

Calcifoliaceae 科 = The family Calcifoliaceae 

emend., Mississippian-Early Pennsylvanian 

algae. ( 英文 ). Vachard D; Cozar P. Rivista 

Italiana di Paleontologia e stratigrafia, 2006, 

112(1): 23-34 

The family Fasciellaceae was created as a 

group of red algae. It was emended as a tribe 

Fascielleae of Incertae sedis algae, and related 

to the tribe Calcifolieae Shuuysky emend. Vachard 

& Cozar. The tribes Fascielleae and 

Calcifoliear both constitute the family Calcifoliaceae 

emend. This family is actually a homogeneous 

group, and could be more or less 

closely related with some questionable Moravamminales 

and Aoujgaliales: claracrustaceae, 

Labyrinthoconaceae and Donezellaceae. 

All these microfossils were successively considered 

as green algae, red algae, "phylloid" 

algae, or fibres of calcispongia. 

2008010122 

意大利中部 Piobbico 地区 Scisti a Fucoidi 

组沟鞭藻曩孢地层 : 特提斯区域阿尔布阶的 

校准事件 = Dinoflagellate cyst stratigraphy 

of the Scisti a Fucoidi Formation (Early Cretaceous) 

from Piobbico, Central Italy: Calibrated 

events for the Albian of the Tethyan 

realm. ( 英文 ). Torricelli S. Rivista Italiana di 

Paleontologia e stratigrafia, 2006, 112(1): 95- 

111 

Distributions of 83 taxa, plotted against the 

independent stratigraphic framework established 

from planktonic foraminifers and 

nannofossils, are compared with ranges 

34

documented in the literature in order to identify 

and calibrate reference horizons for the 

Albian dinoflagellate cyst stratigraphy of the 

Tethyan Realm. The events have been selected 

and calibrated. 

2008010123 

泰国北部中新世轮藻植物 Nitellopsis 属 = 

Nitellopsis (Charophyta) from the Miocene of 

northern Thailand. ( 英文 ). SoulieMarsche I; 

Gemayel P; Chaimanee Y; Suteethorn V; Jaeger 

JJ; Ducrocq S. Alcheringa, 1997, 21(1/2): 

141-156 

Charophyte gyrogonites from two Miocene 

sites in northern Thailand are studied and 

compared for population variation. Morphometrical 

differences between the two 

populations, determined as Nitellopsis merianii 

and N. merianii globula, correspond to 

variation at the interpopulation level and do 

not justify the distinction of two separate species 

as made by previous authors. The first 

exhaustive synonymy for both taxa is listed. 

Morphological differences can be attributed to 

environmental differences as reflected by distinct 

lithologies of the samples concerned. The 

eurasian character of N. merianii is underlined 

through its biogeographical distribution in 

China The flora is in accordance with the 

early Middle Miocene age(16-14 My) previously 

published for vertebrate faunas from the 

same sites. 

2008010124 

河北阳原东目连第四纪叠层石古环境分析 

= Analysis of the palaeoenvironment of Quaternary 

stromatolites at Dongmulian, Yangyuan 

County of Hebei Province. ( 中文 ). 闵 

隆瑞 ; 迟振卿 ; 朱关祥 ; 姚培毅 ; 牛平山 . 地质学 

报 , 2002, 76(4): 446-453 

组成阳原县东目连湖积台地的第四纪 “ 泥 

河湾层 ” 地层中 , 发育多层藻迹层和一层 “ 菜 

花形 ”、“ 锥体状 ” 大叠层石 ( 个体高 20 cm), 

大叠层石层延伸 1 km, 构成古藻坪微地貌。 

经 OSL 和古地磁测试 , 大叠层石年龄推测为 

220 ka 左右。镜下叠层石片子中见蓝藻门的 

纤细席藻种 Phormidium 

tenue(Menegh)Genegh 和湖泊鞘丝藻种 

Lyngbya Limnetica Lemmermann 等。不同形 

态叠层石反映不同发育阶段 , 藻迹发育于高 

水位边缘部位 , 大叠层石发育于高水位与低 

水位之间边缘部位。亮层和暗层交替出现 

的纹层构造是组成叠层石的基本结构构造 , 

它们是由蓝藻丝体生长代谢活动所致。据 

同位素、磁化率、粒度、地球化学元素、X 

衍射、孢粉和生物化石等分析 , 认为气候暖 

干、盐度高及大量苔藓虫、介形虫、龙介 

科蠕虫等生物存在的环境有利于大叠层石 

形成。叠层石可能属半咸水湖、滨湖浅水 

环境 , 但据首次在第四纪泥河湾层中发现的 

苔藓虫和龙介科蠕虫管分析 , 其成因是否与 

海水有过联系尚待进一步研究。 

2008010125 

坦桑尼亚海岸上侏罗统甲藻孢囊两属 : 

Wanaea 和 Komewuia = Occurrence of 

dinoflagellate cyst genera Wanaea and Komewuia 

in Upper Jurassic strata, coastal Tanzania. 

( 英文 ). Msaky E S. Paleontological 

Research, 2007, 11(1): 41-58 

Species of the dinoflagellate cyst genera 

Komewuia and Wanaea are well represented 

in surface and subsurface, Upper Jurassic 

strata of coastal Tanzania. One new species of 

Wanaea, W. tendaguruensis, is described from 

the Trigonia smeei Bed of the Tendaguru 

Formation in the Mandawa Basin; it appears 

to be a useful index of the Kimmeridgian. 

Wanaea clathrata, W. spectabilis, and W. 

talea are rare to common constituents of the 

Oxfordian strata of the middle part of the Bagamoyo 

Formation in the Ruvu Basin. Komewuia 

glabra, characteristic of the Kimmeridgian-Tithonian 

in the southern hemisphere, 

is recorded from the offshore Kipatimu 

Formation and from the Trigonia 

smeei Bed. The Kipatimu Formation was previously 

dated as Early Cretaceous, but is now 

considered Late Jurassic due to its content of 

K. glabra. The informally designated Komewuia 

sp. A occurs sporadically in the Nerinea 

Bed (Oxfordian- Kimmeridgian) of the 

Tendaguru Formation. The species documented 

herein have short stratigraphic ranges 

in the Upper Jurassic of coastal Tanzania and 

are thus potentially useful for regional biozonation 

and correlation. 

2008010126 

全球早、中寒武世藻类生物地理分区初探 

= Study on global distribution of algae biogeographic 

biota in Early and Middle Cambrian. 

( 中文 ). 杨瑞东 ; 毛家仁 ; 张位华 ; 姜立君 . 

古地理学报 , 2002, 4(2): 12-18 

澄江生物群、凯里生物群、加拿大布尔 

吉斯生物群和西伯利亚藻群中均有丰富的 

藻类化石。根据前寒武纪宏观藻类的分布 

以及凯里生物群和布尔吉斯页岩生物群中 

藻类和后生动物的相似性 , 讨论了前寒武 

纪至中寒武世期间生物地理分区的控制因 

35

素。对几个生物群中的藻类化石和后生动 

物化石的对比研究发现 , 在相近的纬度范 

围内 , 动植物化石组合特征非常相似 ; 而 

纬度有明显差异时 , 藻类生物群及后生动 

物群也具有明显的差异。由于后生生物在 

前寒武纪至中寒武世期间具有低的演化程 

度和分异能力 , 因此生物地理分布的主要 

控制因素是古纬度。而 Schopf(1976) 的 

生物地理分区模式不适合这一时期的生物 

地理分区。结合前寒武纪至中寒武世后生 

生物化石的分布情况 , 建立了前寒武纪 - 

中寒武世时期的生物地理分区模式。这个 

模式较好地解释了分布在北美大陆和华南 

大陆上的寒武纪生物群相似的原因。 

2008010127 

我国咸化湖泊沉积中钙质超微化石特征及 

其地质意义 = Characteristics and geologic 

significance of calcareous nanofossils in 

sediments of terrestrial salinized lakes. ( 中文 ). 

孙镇城 ; 杨革联 ; 乔子真 ; 杨藩 ; 李东明 ; 景民昌 . 

古地理学报 , 2002, 4(2): 56-63 

对我国西北和东北 ( 内蒙古东部 )36 个 

地点的新生代 - 现代陆相咸化湖泊沉积中 

的 433 块标本进行了采样分析 , 在基保 15 

个地点 38 块标本中发现钙质超微化石 10 

个属 :Coccolithus , Reticulofenestra , 

Cyclicargolithus , Quadrum , Discoaster , 

Gephyrocapsa , Calcidiscus , 

Umbilicasphaera , Cotonocyclus , 

Watznaueria 等 , 多数为原地沉积 , 也有一 

部分属于再沉积来源。由此可见 , 不能笼 

统地把所有钙质超微化石的发现都当作海 

相或海侵的证据。陆相咸化湖泊沉积中钙 

质超微化石的特点是 : 丰度低、数量稀 

少 , 属种分异度低 , 常与陆相喜盐水生生 

物共生。第四系和现代陆相咸化湖泊沉积 

中发现的钙质超微化石属种往往是海相第 

四系或现代海洋中常见类型。在青海柴达 

木盆地七个泉构造七心 1 井中 - 上始新统 

下干柴沟组上段岩心中 , 发现 

Reticulofenestra bisecta。这是始新世 - 渐新 

世海相沉积中标志化石。看来 , 利用钙质 

超微化石进行海、陆相地层对比探索巳取 

得一定进展 , 但离 “ 统 ” 级的地层对比还有 

很大距离。 

2008010128 

南海北部陆坡 ODP 1144 站位第四纪硅藻 

及其古环境演变 = Quaternary diatoms from 

the South China Sea, Leg 184, Site 1144 and 

their palaeoenvironmental evolution. ( 中文 ). 

李家英 . 地质论评 , 2002, 48(5): 542-551 

中国南海北部陆坡 ODP 1144 站位硅藻植 

物群的研究 , 建立了西太平洋边缘海一个 

新的中更新世晚期以来的硅藻生物地层图 

式。根据硅藻化石中具有指示意义的硅藻 

化石中具有指示意义的硅藻种的分布和生 

态变化 ( 暖水种和冷水种 ), 划分了 8 个 

硅藻组合带 , 其硅藻组合带分别在不同的 

高低海面环境下形成的。根据 ODP 1144 站 

位氧同位素 (OIS) 测定结果 ,8 个硅藻组 

合带与 OIS 1~8 期相对应。1、3、5、7 硅 

藻组合带相当于 OIS 1、3、5、7 期 , 间冰 

期是以热带和亚热带硅藻占优势 , 其中冷 

期出现大量的沿岸硅藻为特征 , 反映高海 

平面温暖的气候条件 ;2、4、6、8 硅藻组 

合带相当于 OIS2、4、6、8 期 , 冰期是以 

亚热带、热带和出现较多冷水硅藻为特 

征 , 反映低海平面较冷气候条件。硅藻丰 

度值的变化与冰期和间冰期有关 , 可以证 

实间冰期时期高的海平面和较低的生物生 

产力以及冰期时低的海平面和高的生物生 

产力 , 而生物生产力的变化又与沉积时期 

沿岸流或上升流的强弱及水团活动有密切 

关系 , 进而揭示该区古海洋环境的演化与 

季风强弱之间的内在关系。 

蕨类植物 ( 广义 ) 

2008010129 

澳大利亚白垩纪首次发现 Tempskya 属蕨 

类植物 T.judithae ( 新种 ) = First record from 

Australia of the Cretaceous fern genus 

Tempskya and the description of a new species, 

T. judithae. ( 英文 ). Clifforda H T; Dettmann 

M E. Review of Palaeobotany and Palynology, 

2005, 134(1-2): 71-84 4 图版 . 

Silicified fragments of false-trunks of the 

fern, Tempskya judithae sp. nov., are described 

from lower Cretaceous (latest Albian) 

sediments near Winton, central-western 

Queensland. The species is characterised by a 

three-layered sclerenchymatous cortex and a 

two-layered pith of sclerenchyma cells. In 

possessing these characters, T. judithae is 

more similar to T. readii than to other species 

of Tempskya. However, the Australian species 

differs from T. readii in the abaxial shape of 

the petiole xylem trace (concave in T. judithae, 

convex in T. readii) and in symmetry attributes 

of the leaf-bases within the false-trunk 

(random in T. judithae and radially symmetrical 

in T. readii). T. judithae is the first record 

of Tempskya from Australia and the second 

36

from Gondwana; the known distribution range 

of the genus embraces a broad area in midhigh 

latitudinal regions of Laurasia and the 

Gondwana record now comprises Australia 

and Argentina. Ecological signals of plant 

fossil assemblages recorded from the Australian 

sediments are in accord with flood plain 

habitats and a temperate climatic regime 

2008010130 

长江流域中三叠世肋木植物的衰退及其适 

应性生存对策 = Declension and survival 

strategy of the Middle Triassic pleuromeia in 

the Yangtze valley. ( 中文 ). 孟繁松 ; 李旭兵 . 

华南地质与矿产 , 2002, (2): 60-65 1 图版 . 

肋木植物茎细 , 不分枝 , 茎上却顶生一枚十 

分庞大的孢子囊穗 , 给人以头重脚轻的印象 , 

因而被视为生命力不强的特化类群。这类 

植物为了更好地延续物种后代和防止衰退 , 

采取了增强生殖力、生殖器官远距离传播 

能力和叶形态多样化等一系列适应性生存 

对策。肋木在长江流域的分布层位由东向 

西逐渐升高 , 表明安尼早期它在该地区几乎 

是同时出现的 , 其扩展方向由西向东而入 , 而 

中、晚期分布区则由东向西逐渐缩小。 

早期种子植物 

2008010131 

对 “Corystospermales 目认识的新途径 ” 和 

南极化石记录的不同意见 = The "New Approach 

to Corystospermales" and the Antarctic 

Fossil Record: A critique. ( 英文 ). Axsmith B 

J ; Taylor E L; Taylor T N. 

Ameghiniana, 2007, 44(1): 223-23 

Much is now known about the Mesozoic 

pteridosperm order Corystospermales based 

on overseventy years of research. However, 

several concepts of corystosperm evolution 

have been proposed that avoid wellestablished 

phylogenetic methodology and 

arbitrarily discount evidence of the group 

from Antarctica. Here, we focus on the "New 

approach to Corystospermales" published by 

Artabe and Brea, which establishes a phylogeny 

for corystosperms based mainly on a restricted 

concept of anomalous wood anatomy 

in this group, and assumed relationships with 

cycads and medullosan pteridosperms. These 

authors also question evidence regarding attached 

corystospermalean organs from Antarctica. 

Based on a reconsideration of the Antarctic 

record, we reaffirm the evidence for a 

Dicroidium leaf in attachment to branches that 

also bear distinctive short shoots. Umkomasia 

cupulate organs occur on identical attached 

short shoots. We also emphasize that wood 

morphotaxa attributed to the corystosperms 

from Antarctica, including Jeffersonioxylon 

and Kykloxylon, indicate that anomalous secondary 

growth is not necessarily basic to the 

corystosperms. We conclude that a greater 

understanding of the corystosperms will require 

a consideration of all relevant evidence, 

and will not be advanced by single organ phylogenies 

based on fossils from one region. 

2008010132 

关于阿根廷圣路易斯 Beazley 地区三叠纪 

沉积中心的基岩 Cacheuta 组 Dicroidium 

odontopteroides var. moltenense 的出现 = 

On the presence of Dicroidium odontopteroides 

(Morris) Gothan var. moltenense Retallack 

in the Cacheuta Formation, subsoil of the 

Triassic depocentre of Beazley (San Luis, Argentina). 

( 其他 ). Stipanicic P N. 

Ameghiniana, 2007, 44(1): 251-253 

裸子植物 

2008010133 

澳大利亚维多利亚下白垩统 Koonwarra 化 

石层新的麻黄植物 = New ephedroid plant 

from the Lower Cretaceous Koonwarra Fossil 

Bed, Victoria, Australia. ( 英文 ). Krassilov V 

A; Dilcher D L; Douglas J G. Alcheringa, 

1998, 22(1/2): 123-133 

A revision of the Lower Cretaceous Koonwarra 

material first assigned to angiosperms 

and subsequently to sphenopsids shows morphological 

and anatomical characters typical 

of ephedroid (gnetophyte) affinities. Shoots 

are preserved as clayey-ferruginous films deposited 

beneath the cuticle reflecting with the 

interior relief of the epidermal cell pattern or 

subepidermal sclerenchymous strands (rugulate 

striations) and vascular tissue of the intermodes. 

The articulate shoots are similar to 

Ephedra foliata and some other extant species 

with 3-4 decussate, basally connate leaves at 

each node, sunken stomata in intercostal zones, 

alternating large and small vascular bundles, 

paired leaf traces, and the morphology of tracheary 

elements, but differ in the leaf number 

per node ranging from two to eight and in the 

considerably lower ratio leaves to internode 

vascular bundles. A new genus and species 

Leongathia elegans is described. The cooccurrence 

of gnetophytes and early angiosperms 

in the lower Aptian of Koonwarra is of 

certain evolutionary and palaeoecological significance. 

The Koonwarra material increases 

the known diversity of the Cretaceous 

37

gnetaleans by presenting a hitherto unrecorded 

Ephedra-like shoot morphology. 

2008010134 

新疆准噶尔盆地中侏罗世 Sphenobaiera( 楔 

拜拉 ) 一新种 = A new species of Sphenobaiera 

from Middle Jurassic of Junggar Basin,Xinjiang,China. 

( 中文 ). 孙革 ; 苗雨雁 ; 陈 

跃军 . 吉林大学学报 ( 地球科学版 ), 2006, 

36(5): 717-722 

报道了新疆准噶尔盆地西部玛纳斯及白 

杨河中侏罗世西山窑组 (J 2 x) 银杏类楔拜拉 

属的一个新种准噶尔楔拜拉 (Sphenobaiera 

junggarensis sp. nov.) 的首次发现。该新种 

以表皮构造为双面气孔式、上表皮气孔 

少、下表皮气孔密度大、孔缝基本定向、 

普通表皮细胞具不规则角质化隆丘及气孔 

器保卫细胞角质化放射纹之间发育有梳状 

“ 细耙 ” 等特征 , 区别于楔拜拉属已知种。还 

讨论了该新种的发现在研究楔拜拉属的分 

类及其古气候等方面的意义。 

被子植物 

2008010135 

波兰晚第三纪竹叶化石及花粉 = Leaves and 

pollen of bamboos from the Polish Neogene. 

( 英文 ). Worobiec E; Worobiec G. Review of 

Palaeobotany and Palynology, 2005, 133(1-2): 

39-50 3 图版 . 

Recently discovered fossil bamboo leaves 

and pollen are described from the Neogene of 

Poland. Morphological analysis of fossil 

leaves from the Late Miocene deposits of the 

Bełchatów Lignite Mine, Central Poland have 

allowed them to be determined as “Bambusa” 

lugdunensis Saporta. It is the first record of 

this species in the Cenozoic of Poland. The 

fossils have been compared with other records 

of bamboos from the Cenozoic of Europe. 

Pollen grains from the Middle Miocene (Badenian) 

deposits from the Legnica brown coal 

deposit (Lower Silesia) provide additional 

evidence of bamboos. These are assigned to 

Graminidites bambusoides Stuchlik, and are 

similar to those of recent Arundinaria. We 

infer that plant (plants) that produced the 

pollen of G. bambusoides could have grown in 

swamp forests and/or reed marshes. This report 

provides a general survey of the occurrence 

of bamboos in the European Neogene, 

from which the leaves and pollen documented 

here present important data on the distribution 

of this group of monocots in Poland and eastern 

Europe 

2008010136 

马达加斯加科尔盖伦群岛渐新世单子叶植 

物大化石 Paracordyline kerguelensis = 

Paracordyline kerguelensis, an Oligocene 

monocotyledon macrofossil from the 

Kerguelen Islands. ( 英文 ). Conran J G. Alcheringa, 

1997, 21(1/2): 129-140 

The monocotyledon macrofossil Desmiophyllum 

sp, or Seward & Conway is recognised 

as being close in its cuticular features 

and stomatal sculpturing to several New Zealand 

and Mascarene species of Cordyline. 

However because the fossil cannot be placed 

unequivocally in Cordyline it is assigned to a 

new form genus Paracordyline as P. kerguelensis 

with affinities to the extant aborescent 

woody monocot Cordyline (Lomandraceae). 

2008010137 

蔷薇科化石历史的简要回顾 —— 以美国华 

盛顿州东部及加拿大不列颠哥伦比亚奥柯 

那根 (Okanogan) 高地的始新统为重点 = 

A brief review of the fossil history of the family 

Rosaceae with a focus on the Eocene Okanogan 

Highlands of eastern Washington State, 

USA, and British Columbia, Canada. ( 英文 ). 

DeVore M L; Pigg K B. Plant Systematics and 

Evolution, 2007, 266(1-2): 45-57 

Many of the oldest definitive members of 

the Rosaceae are present in the Eocene upland 

floras of the Okanogan Highlands of northeastern 

Washington State and British Columbia, 

Canada. Over a dozen rosaceous taxa representing 

extant and extinct genera of all four 

traditionally recognized subfamilies are 

known from flowers, fruits, wood, pollen, and 

especially leaves. The complexity seen in Eocene 

Rosaceae suggests that hybridization and 

polyploidy may have played a pivotal role in 

the early evolution of the family. Increased 

species diversity and the first appearance of 

additional modern taxa occur during the Late 

Paleogene in North America and Europe. The 

Rosaceae become increasingly important 

components of fossil floras during the Neogene, 

with taxa adapted to many habitats. 

2008010138 

Pyrinae 亚族 ( 原蔷薇科苹果亚科 ) 系统演 

化 : 对具复杂演化史的类群的限制性分类 

方案 = Phylogeny of subtribe Pyrinae (formerly 

the Maloideae, Rosaceae): Limited 

resolution of a complex evolutionary history. 

( 英文 ). Campbell C S; Evans R C; Morgan D 

R; Dickinson T A; Arsenault M P. Plant Systematics 

and Evolution, 2007, 266(1-2): 119– 

145 

38

Generic relationships in the Pyrinae 

(equivalent to subfamily Maloideae) were assessed 

with six chloroplast regions and five 

nuclear regions. We also plotted 12 nonmolecular 

characters onto molecular phylogenies. 

Chloroplast DNA trees are incongruent 

with those from nuclear regions, as are most 

nuclear regions with one another. Some of this 

conflict may be the result of hybridization, 

which occurs between many genera of Pyrinae 

in the present and may have occurred in the 

past, and duplication of nuclear loci. Sequence 

divergence between genera of Pyrinae, which 

is significantly less than that between genera 

of another large clade in Rosaceae, the Rosoideae, 

is concentrated in terminal branches, 

with short internal branches. This pattern is 

consistent with an ancient, rapid radiation, 

which has also been hypothesized from the 

fossil record. Even with about 500,000 bp of 

sequence, our results resolve only several 

small groups of genera and leave much uncertainty 

about phylogenetic relationships within 

Pyrinae. 

2008010139 

间断分布于东亚和北美东部的檫木 ( 樟 

科 ) 的系统演化和生物地理 = Phylogeny 

and biogeography of Sassafras (Lauraceae) 

disjunct between eastern Asia and eastern 

North America. ( 英文 ). Nie Z L; Wen J; Sun 

H. Plant Systematics and Evolution, 2007, 

267(1-4): 191-203 

Sassafras (Lauraceae) consists of three species 

disjunct between eastern Asia (S. tzumu 

and S. randaiense) and eastern North America 

(S. albidum). Phylogenetic analysis based on 

sequences of nuclear ribosomal ITS and three 

chloroplast non-coding regions (rpl16, trnL-F, 

and psbA-trnH) showed that Sassafras is monophyletic 

and that the eastern North American 

S. albidum is sister to the clade of its two 

eastern Asian counterparts. Their intercontinental 

divergence was estimated to be 13.80 ± 

2.29−16.69 ± 2.52 million years ago (mya) 

using the penalized likelihood method with 

the ITS and three chloroplast markers. Biogeographic 

analyses combined with fossil evidence 

suggest that Sassafras has a relict distribution 

in the Northern Hemisphere without a 

Gondwanan link. The divergence time of the 

two eastern Asian species (the continental 

Chinese Sassafras tzumu and S. randaiense 

endemic to Taiwan) is estimated to be 0.61 ± 

0.75−2.23 ± 0.76 mya. Sassafras randaiense 

from Taiwan was most likely derived from an 

ancestor from continental China. 

2008010140 

槭属槭组的演化历史和分类系统 —— 有关 

低水平系统发生学的个案研究 = Evolutionary 

history and systematics of Acer section 

Acer – a case study of low-level phylogenetics. 

( 英文 ). Grimm G W; Denk T; Hemleben V. 

Plant Systematics and Evolution, 2007, 267(1- 

4): 215-253 

The phylogenetic and systematic position of 

all species of Acer section Acer from North 

America, East Asia, and western Eurasia are 

evaluated using various splits-based networks 

(distance networks, bipartition networks), ITS 

motif analysis, and morphology. Molecular 

analyses are based on 276 ITS clones obtained 

from 101 specimens collected mainly from 

natural stands. The large sample size ensures 

to cover sufficiently inter- and intraspecific 

ITS variability of this group. Formerly recognised 

species are generally supported by ITS 

data and morphology; the combination of molecular 

(ITS) and morphological criteria allows 

defining seven (supraspecific) taxonomic 

groups prior to a phylogenetic reconstruction. 

Phylogenetic signals captured in modern ITS 

sequences are partly incompatible but clearly 

suggest that Acer section Acer underwent 

three major radiations. Horizontal gene flow is 

indicated between ancestors of extant taxa that 

are isolated at present times. The level of ITS 

derivation can be estimated and corresponds 

to levels of morphological differentiation and 

(palaeo-) biogeographical patterns. Based on 

our results we question the potential of cladistic 

approaches to infer low-level evolution in 

an adequate manner and demonstrate that 

speciation in members of Acer section Acer is 

not generally linked to cladogenesis. The data 

and methodologies provided here allow to 

trace pathways of low-level evolution and to 

analyse such data sets with a less restricted 

(non-dichotomous) dynamic concept. 

古无脊椎动物学 

综论 

2008010141 

密西西比冰缘湾的缺氧热泉 = Hypoxia hotspots 

in the Mississippi Bight. ( 英文 ). Brunner 

C A; Beall J M. Journal of Foraminiferal 

Research, 2006, 36(2): 95-107 

Foraminiferal proxies of hypoxia indicate 

apparent low oxygen to hypoxic conditions in 

several hotspots in the Mississippi Bight. The 

foraminiferal hypoxia proxies, the Ammonia 

39

to Elphidium (A/E) index and the Pseudononion-Epistominella-Buliminella 

(PEB) index, 

were tabulated from three sets of core tops 

collected in 1951–1956. Additionally, the 

oxygenation history of a site near the Balize 

delta was evaluated over the past one hundred 

years based on A/E and PEB indices and size 

distributions of pyrite framboids in a gravity 

core dated by 210Pb geochronology. 

The results from the 1950’s core-top collections 

show apparent, recurrent low-oxygen to 

hypoxic bottom water on the inner shelf at 

hotspot locales seaward of the Mississippi- 

Alabama barrier islands and the eastern distributaries 

of the Balize delta. Specifically, 

the A/E index exceeds 90% on the inner shelf 

seaward of Horn and Dauphin islands, both of 

the Mississippi-Alabama barrier islands, and a 

center between Pass à Loutre and Main Pass 

of the Balize delta. In partial support of these 

results are reports of present-day low oxygen 

to hypoxic concentrations in bottom waters 

associated with seasonally high surface chlorophyll 

a and seasonal strengthening of a 

brackish-water cap at these locales. In contrast, 

the PEB index in core tops suggests good 

oxygenation at mid-shelf depths >30 m. The 

PEB index, size distributions of framboidal 

pyrite, and other indicators in a gravity core 

44 km northeast of Pass à Loutre indicate no 

clear change in conditions over the past century, 

constraining the seaward extent of the 

hotspot near the Balize delta. 

2008010142 

桂北泥盆纪末至早石炭世生物群及年代地 

层划分 = Classification of chronostratigraphic 

and the biota from the end of Devonian period 

to Early Carboniferous epoch of northern 

Guangxi. ( 中文 ). 李镇梁 ; 徐杰邦 ; 李英华 ; 刘 

融涛 ; 蔡宁 ; 廖开立 ; 石显雄 . 广西地质 , 2006, 

15(2): 13-20 

文章根据近年桂北地区 1∶5 万区域地质 

调查和专题研究成果 , 对泥盆纪末至早石炭 

世生物群作了较系统的总结 , 划分了若干可 

与区域乃至世界对比的生物 ( 组合 ) 带 : 有孔 

虫 12 个 , 珊瑚 11 个 , 腕足类 6 个 , 牙形刺 5 个 , 

菊石、介形类各 2 个 ; 并提出了年代地层划 

分的意见。 

原生动物 

2008010143 

陆架中部到斜坡中部地带现生的 63-150µm 

的小有孔虫 = Living small-sized (63-150µm) 

foraminifera from mid-shelf to mid-slope. ( 英 

文 ). Gérald Duchemin; Fontanier C. Journal 

of Foraminiferal Research, 2007, 37(1): 12- 

32 3 图版 . 

Live (rose Bengal stained) foraminiferal 

faunas of the 63–150 µm size fraction have 

been investigated in surficial sediment (0–1 

cm) from mid-shelf to mid-slope environments 

in the Bay of Biscay. Eleven stations 

were sampled in April 2002 and March 2004 

between 80 and 2000 m water depth (mwd). 

Earlier studies on the temporal variability of 

phytoplankton primary production suggest 

that our stations were sampled at the most eutrophic 

period of the year. In response to the 

decrease of exported organic matter flux to the 

seafloor along our bathymetric transect, foraminiferal 

standing stocks decrease from 

~1400–2000 specimens per 50 cm3 on the 

continental shelf (100–140 mwd) and upper 

slope (550 mwd) to about 400 specimens per 

50 cm3 at mid-slope stations (2000 mwd). At 

all stations, the faunas contain an important 

amount of small opportunistic species that are 

favored by seasonal phytodetritus input. On 

the continental shelf where phytoplankton 

bloom, events may be geographically restricted; 

the foraminiferal response is dependent 

on the distance to the surface-water primary-production 

cells. Textularia porrecta is 

very abundant at an 80-m-deep station that is 

close to the coast and characterized by a high 

sedimentation rate of fine-grained particles. 

Foraminiferal faunas are dominated by Nonionella 

iridea, Cassidulina carinata and Bolivina 

ex. gr. dilatata at the outer-shelf stations 

(110–140 mwd) that are under the direct influence 

of spring bloom phytodetritus input in 

the northern Bay of Biscay. A fauna dominated 

by Bolivina dilatata/spathulata and Bolivina 

subaenariensis is found in the southeastern 

Bay of Biscay at a 140-m-deep outershelf 

station located seaward of the Adour 

River estuary, where the sediment is probably 

enriched in terrestrial organic matter. Apparently, 

differences in foraminiferal composition 

between outer-shelf areas in the northern and 

southeastern Bay of Biscay are related to differences 

in organic matter quality. On the continental 

slope, a bathymetric zonation of taxa 

is observed from upper-slope sites (550–1000 

mwd) rich in Epistominella exigua and U- 

vigerina peregrina to mid-slope stations 

(1600–2000 mwd), where Nuttallides pusillus 

and Gavelinopsis translucens dominate the 

small-sized living fauna. This bathymetric 

foraminiferal zonation probably reflects a trophic 

gradient between upper-slope eutrophic 

40

stations and mid-slope, more oligotrophic sites. 

Our zonal description of small-sized living 

foraminifera (63–150 µm) is new for the Bay 

of Biscay and may provide the basis to reconstruct 

former export production regimes in 

marginal paleo-environments from temperate 

latitude areas. 

2008010144 

北冰洋西部生物时间带内的有孔虫群落的 

群落结构 = Community structure of foraminiferal 

communities within temporal biozones 

from the western Arctic Ocean. ( 英文 ). 

Hayek L-A C; Buzas M A. Journal of Foraminiferal 

Research, 2007, 37(1): 33-40 

Community structure is often an overlooked 

dimension of biodiversity. Knowledge of 

community structure, the statistical distribution 

of the relative species abundance vector, 

makes possible comparisons and contrasts 

across time, space and/or environmental conditions. 

Our results indicate that species of 

Arctic foraminifera in age-correlated cores 

from abyssal depths are each best described by 

log-series distributions. Using this structural 

information, we were able to determine that 

structural stability exists for at least 50 ka. The 

foraminiferal communities in this study show 

remarkable concordance, distributional similarity 

and support the neutral theory of biodiversity. 

2008010145 

浅层海水的热泉活动对底栖有孔虫的影响 

( 伊特鲁亚海风成弧 ) = The effect of shallow 

marine hydrothermal vent activity on benthic 

foraminifera (aeolian ARC, tyrrhenian 

SEA). ( 英文 ). Panieri G. Journal of Foraminiferal 

Research, 2006, 36(1): 3-14 3 图 

版 . 

An exceptional intensification of hydrothermal 

degassing activity occurred on November 

3, 2002, to the east of Panarea, the 

smallest island of the Aeolian Archipelago 

(Tyrrhenian Sea, Italy). This event represents 

a unique opportunity to study benthic foraminiferal 

assemblages under the ecological 

stress of hydrothermal emissions in shallow 

(10–15 m water depth) environments. Benthic 

foraminifera (>63 µm) were collected by a 

scuba diver from sediments and seagrass of a 

Posidonia oceanica meadow off the coast of 

Panarea. Assemblages were studied to assess 

mortality and monitor the composition of benthic 

communities following the sudden venting 

event, characterized by an intensification 

of the emission of gases with high temperatures 

(40–50°C), low pH (~5), and high concentrations 

of HCl, HF, SO2 and some H2S. 

Surface foraminiferal assemblages were monitored 

during surveys on November 13–14, 

2002, and May 22–24, 2003. In November 

2002 (10 days after the venting event) agglutinated 

forms dominated the assemblages in 

sediment samples, whereas hyaline forms 

dominated the assemblages collected from the 

leaves and roots of P. oceanica. Six months 

later, in May 2003, when environmental conditions 

had returned to normal, sediment samples 

were barren of foraminifera, whereas the 

assemblages associated with P. oceanica were 

composed of allogromiids, which can be considered 

opportunistic pioneer species able to 

colonize disturbed environments. 

2008010146 

化石群落与层序地层的耦合关系研究 — 以 

塔里木盆地西部中新生代有孔虫群落与层 

序地层关系研究为例 = Coupling relationships 

between fossil communities and sequence 

stratigraphy:A case study of the relationships 

between the Meso-Cenozoic foraminiferal 

community and sequence stratigraphy 

in the western part of the Tarim Basin. 

( 中文 ). 郭宪璞 ; 彭阳 ; 丁孝忠 . 地质通报 , 2002, 

21(7): 377-383 

本文研究的是大陆边缘海以底栖有孔虫 

为主的化石群落与层序地层的关系。海平 

面变化是控制化石群落演替和识别划分层 

序的主要因素。化石群落在一个完整海水 

进退旋回中呈机会种群落、平衡种群落、 

终极种群落演替变化 , 在化石丰度、多样 

度、均衡度、成壳类型等方面分异显著 , 与 

层序地层的三级层序的海进体系域、凝缩 

期沉积、高位体系域具有密切的耦合关 

系。化石群落的演替变化是对海洋环境变 

迁的能动反映。因此 , 化石群落的研究可以 

帮助识别和优化层序、沉积体系域和层序 

界面 , 从而为层序地层的准确识别划分提供 

新的思路。 

2008010147 

东昆仑布喀达坂峰地区发现二叠纪冷温动 

物群 = Discovery of a cold-water fauna in the 

Mount Buka Daban area,East Kunlun. ( 中文 ). 

王秉璋 ; 宋泰忠 ; 王瑾 ; 叶占福 ; 薛宁 . 地质通 

报 , 2002, 21(7): 411-414 

东昆仑西段布喀达坂峰地区发现了以单 

通道 (Monodiexodina) 为主的冷温动物群 , 产 

于东昆中缝合带与东昆南缝合带之间一套 

41

以浅海相碳酸盐岩为主的中下二叠统中 , 可 

与空喀山口加温达坂组及西藏吞龙共巴组 

对比。 

2008010148 

长江源各拉丹冬一带发现 Gallowayinella 

蜓类动物群 = Discovery of the Late Permian 

Gallowayinella fauna in the Gêladaindong 

area in the source region of the Yangtze River. 

( 中文 ). 牛志军 ; 曾波夫 ; 卜建军 ; 王建雄 . 地质 

通报 , 2002, 21(11): 756-758 

在 1∶25 万赤布张错幅区域地质调查中 , 

于原划下二叠统开心岭石灰岩组中发现晚 

二叠世长头期 Gallowayinella 蜓类动物群化 

石 , 表明该区二叠纪地层非属早二叠世 , 而似 

应与青海省南部晚二叠世鸟丽群对比。 

2008010149 

桂西北天峨地区下石炭统有孔虫带及地层 

划分 = Stratigraphic division and foraminifera 

zones of Lower Carboniferous in Tian'e western-northern 

Guangxi. ( 中文 ). 陆刚 ; 胡贵昂 ; 

张喜 ; 李玉坤 . 广西地质 , 2006, 15(3): 9-14 

桂西北天峨地区孤立碳酸盐台地 , 上泥盆 

统顶部至上石炭统下部有孔虫十分发育 , 可 

划分 15 个有孔虫生物组合带 , 它们是地层划 

分对比的重要依据。以有孔虫 Eoendothyra 

与 Quasiendothyra 的灭绝、Bisphaera 的大量 

出现划分泥盆系 / 石炭系 , 以 Eoparastaffella 

的出现作为维宪阶的底界 , 以 Globivalvulina 

或 Pseudostaffella 的出现作为上、下石炭统 

的划分标志 , 生物分带明显 , 与岩石地层分界 

吻合或基本一致 , 是较理想的地层分界。 

2008010150 

渤海沿岸黄土中有孔虫化石对古风场的指 

示意义 = The significance of foraminifera 

from loess along the coast of the Bohai Sea for 

palaeowind directions. ( 中文 ). 李杰 ; 旺罗 ; 赵 

华 ; 刘东生 . 地质学报 , 2002, 76(3): 409-412 

通过对渤海沿岸末次冰期黄土中有孔虫 

化石的研究 , 发现含有主要生活在南黄海和 

东海水体较深的浮游有孔虫化 

石 :Globigerina falconensis 、 Globorotalia 

pumilio 和 Neogloboquadrina dutertrei, 后者的 

含量高达 6.4%。进一步对比沉积在不同地 

貌单元上黄土中有孔虫的丰度和浮游有孔 

虫化石出现的频率 , 发现沉积在北坡 ( 阴坡 ) 

和南坡 ( 阳坡 ) 的有孔虫化石有显著的差异 , 

北坡的有孔虫丰度和出现频次明显高于南 

坡 , 分析认为渤海沿岸的黄土不但具有西北 

风和东北风从渤海和北黄海搬运来的成分 , 

还有东南风从南黄海和东海搬运带来的成 

分。 

2008010151 

泰国东北部黎府 (Loei Province ) Pak 

Chom 地区晚泥盆世至早石炭世放射虫动 

物群 = Late Devonian to Early Carboniferous 

radiolarian fauna from the Pak Chom area, 

Loei Province, northeastern Thailand. ( 英文 ). 

Saesaengseerung D; Sashida K; Sashida A. 

Paleontological Research, 2007, 11(2): 109- 

121 

A Late Devonian to Early Carboniferous 

radiolarian fauna is present in chert and siliceous 

shale of a chert-clastic section along the 

Khong River, Pak Chom area, at the Thai-Lao 

border of northeastern Thailand. The radiolarian 

fauna is composed of Stigmosphaerostylus 

variospina, Astroentactinia stellata, Astroentactinia 

multispinosus, Archocyrtium wonae, 

Archocyrtium riedeli, and other species and 

corresponds to the Famennian (Late Devonian) 

to Tournaisian (Early Carboniferous) radiolarian 

fauna reported from northwestern Europe, 

Australia, northern and southern Thailand, and 

southern China. Ten radiolarian species belonging 

to four genera including one unidentified 

genus are investigated. The radiolarianbearing 

sequence was probably deposited in a 

pelagic or hemipelagic environment within the 

Paleotethys Ocean during Late Devonian to 

Early Carboniferous time. Furthermore, this 

chert-clastic section of Pak Chom area is 

thought to be deposited on the Nakhon Thai 

Block and subducted beneath the Indochina 

Block. This suggests that the age of subduction 

and accretion of the Nakhon Thai Block 

is thought to have occurred at least after Early 

Carboniferous indicated by the occurrence of 

Late Devonian to Early Carboniferous radiolarians. 

2008010152 

西澳大利亚南 Carnarvon 盆地 Gascoyne 

台地 Giralia 砂屑石灰岩标准剖面的中始新 

世有孔虫 = Middle Eocene foraminifera from 

the type Giralia Calcarenite, Gascoyne platform, 

Southern Carnarvon Basin, Western 

Australia. ( 英文 ). Haig D W; Smith M; Apthorpe 

M C. Alcheringa, 1997, 21(3/4): 229- 

245 

Foraminifera from the type section of the 

Giralia Calcarenite indicate an upper zone P12 

correlation and a Middle Eocene age (probably 

within the interval 41.5-40.5 Ma, BKSA95 

time scale). The type Giralia Calcarenite is 

considered to represent one sequence (with 

42

maximum thickness of 40-50 m preserved on 

the Gascoyne Platform) and to reflect late 

transgressive and early highstand deposition 

about a maximum flooding event. Initial retrogradation 

of the shoreline produced a 

maximum water depth of about 50 m at the 

type locality (5-6 m above base of stratigraphic 

section). The formation may correlate 

with shallow marine deposits found elsewhere 

in the Southern Carnarvon Basin (e.g. Eocene 

limestones at Yaringa and Red Bluff, and the 

Merlinleigh Sandstone), and correlates with 

Middle Eocene transgressive units in the Perth, 

Eucla, Great Australian Eight and Otway Basins. 

2008010153 

澳大利亚西部近岸含 Fabiania 属的早新生 

代 ( 古新世 ) 有孔虫动物群 = An Early 

Cainozoic (Paleocene) foraminiferal fauna 

with Fabiania from offshore eastern Australia. 

( 英文 ). Quilty P G; Shafik S; Jenkins C J; 

Keene J B. Alcheringa, 1997, 21(3/4): 299- 

315 

Early Paleocene marine sediments are recorded 

from a single dredge sample taken 

from the continental slope (3533-3306 m) off 

the central coast of New South Wales. They 

probably belong to the Early Paleocene NP4 

calcareous nannoplankton zone (Pie or P1d/P2 

in standard foraminiferal zonal terms) and 

thus are the first Palaeogene marine rocks 

known from the region and the first record of 

marine biota of this age from the Australian 

margin other than Western Australia. The age 

is based on analysis of calcareous nannofossils. 

The sediment accumulated in very shallow, 

warm, fully marine conditions, apparently off 

a coast of periodically low runoff, and the 

fauna lacks any planktonic foraminiferal species. 

While it is dominated by several typically 

Paleocene benthic forms well known 

from southern and southwestern Australia, 

several otherwise typical Australian forms 

appear to be absent. Fabiania (the new species 

F. macgowrani) is recorded for the first time 

from Australia, apparently the earliest known 

occurrence of the genus. Paleocene rocks of 

this age are also known from the Perth Basin 

and Northwest Shelf of Western Australia and 

it seems these indicate the need for recognition 

of a new sedimentation cycle in the Cainozoic 

of Australia. 

2008010154 

福建深沪湾潮间带全新世有孔虫及其环境 

意义 = Holocene foraminifera and it's environmental 

significance in Shenhu Bay, Fujian. 

( 中文 ). 王绍鸿 ; 俞鸣同 ; 唐丽玉 ; 赵希涛 ; 王雪 

梅 ; 黄向华 . 台湾海峡 , 2002, 21(1): 6-11 

本文对深沪湾西部潮间带表层沉积物和 

两个钻孔岩芯共 30 个样品的有孔虫组成进 

行了定性和定量分析。结果表明 , 表层沉 

积物中有孔虫群分布规律明显 , 随着离岸 

向海越远 , 水深越大 , 有孔虫数量从 1 位 

数上升到 5 位数 , 种数为 9-69 种 , 多变度 

V31 ~ 44, 复合分异度 H(s)3.25 ~ 3.45。 

从钻孔岩芯中的全新世有孔虫群特征可看 

出 , 中全新世以来海面升降和海洋环境可 

分为 2 个阶段 :(1) 海水初到钻孔位置 , 

有孔虫数量和种数较少 , 分异度不高 , 海 

相性程度较低。(2) 后期 ( 埋深 1.8m 和 

2.0m 以浅 ), 海面有所升高 , 变为潮间带 

( 高潮位 → 中潮位 → 低潮位 ) 环境。 

2008010155 

滇西北中甸地区哈工组放射虫及其构造古 

地理意义 = Radiolarings from Hagong Formation 

in Zhongdian, NW Yunan, and its tectono-paleogeographic 

implications. ( 中文 ). 冯 

庆来 ; 张世涛 ; 葛孟春 ; 严城民 ; 余华 ; 段国玺 ; 包 

俊跃 . 地质科学 , 2002, 37(1): 70-78 1 图版 . 

位于甘孜 - 理塘构造带和金沙江构造带之 

间的德格 - 中甸微板块 , 可分为乡城晚三叠 

世岛弧带、义敦晚三叠世弧后盆地带和中 

咱地块等次级构造单位。滇西北中甸地区 

上三叠统哈工组包含大量沉积混杂岩块 , 

与乡城、得荣泥砾混杂岩相连 , 形成晚三 

叠世沉积混杂岩带。哈工组沉积序列和沉 

积混杂岩沉积特征研究表明 , 中甸地区沉 

积混杂岩带为义敦晚三叠世弧后盆地形成 

过程中 , 由盆地边缘垮塌沉积形成 , 混杂 

岩块物源为近源下伏地层。沉积混杂岩块 

主要为晚古生代灰岩 , 但也有含中泥盆 

世、早石炭世和中二叠世放射虫化石的层 

状硅质岩 , 说明德格 - 中甸微板块晚古生代 

不是统一的碳酸盐台地 , 而是碳酸盐台地 

与深水断陷盆地并存的构造古地理格局。 

另外 , 哈工组三段还发现侏罗纪放射虫化 

石 , 说明金沙江带以东地区侏罗纪仍存在 

海盆。 

2008010156 

新疆东昆仑木孜塔格蛇绿混杂岩发现早石 

炭世放射虫 = Discovery of Early Carboniferous 

radiolarias in Muztag ophiolitic melange, 

east Kunlun, Xinjiang. ( 中文 ). 兰朝利 ; 吴峻 ; 

43

李继亮 ; 俞良军 ; 李红生 ; 王义天 . 地质科 

学 , 2002, 37(1): 104-106 2 图版 . 

在新疆木孜塔格蛇绿混杂岩的燧石中发 

现了早石炭世杜内期的放射虫化石 , 首次 

为这套蛇绿混杂岩提供了时代依据。结合 

在邻区的祁漫塔格和可可西里发现的放射 

虫 , 认为青藏高原北缘在早石炭世期间曾 

沿多处裂解。它们之间可能有狭窄的通道 

相连 , 是否构成统一的大洋尚待进一步研 

究。 

2008010157 

意大利东北部威尼斯地区上渐新统大有孔 

虫 = Larger Foraminifera from the Upper Oligocene 

of the Venetian Area, North-East Italy. 

( 英文 ). Bassi D; Hottinger L; Nebelsick J H. 


A moderately diverse larger foraminiferal 

fauna from the north-east Italian ‘Arenarie e 

calcari di S. Urbano’ formation with important 

stratigraphic, palaeoecological and palaeobiogeographical 

implications is described with 

respect to its position in the Western Tethys 

area. The fauna is dominated by hyaline perforated 

and porcellaneous forms including Amphistegina, 

Archaias, Austrotrillina, 

Miogypsinoides, Neoplanorbulinella, Neorotalia, 

Nummulites, Operculina and Spiroclypeus. 

The presence of Miogypsinoides 

complanatus allows the age of the formation 

to be determined as late Chattian (Shallow 

Benthic Zone SBZ 23). The palaeoenvironmental 

setting is interpreted as a shallow ramp 

environment ranging from (1) well lit, highly 

translucent, shallowest part of the photic zone 

characterized by Archaias and Austrotrillina, 

the deeper part of the inner ramp with Nummulites, 

to (2) the shallow part of the middle 

ramp with Spiroclypeus and miogypsinids and 

Operculina, to (3) a deeper middle-ramp setting 

dominated by coralline rhodoliths along 

with lepidocylinids. The presence of Archaias 

hensoni Smout and Eames shows that members 

of much more diverse Middle Eastern 

associations of shallow-water larger porcellaneous 

foraminifera are also present in the 

north-western parts of the Western Tethys, 

and reveals a corresponding diversity gradient 

among larger foraminiferal faunas in the 

Western Tethys, which is related to a decrease 

in temperature. 

2008010158 

更新世深海底栖有孔虫绝灭的南大西洋记 

录 = Pleistocene Extinctions Of Deep-Sea 

Benthic Foraminifera: The South Atlantic Record. 

( 英文 ). Óneill T A; Hayward B W; Kawagata 

S; Sabaa A T; Grenfell H R. Palaeontology, 

2007, 50(5): 1073-1102 

Sixty-two species and 19 genera of elongate, 

cylindrical benthic foraminifera disappeared 

from the deep-sea in the south-east Atlantic 

(ODP Sites 1082 and 1083) and the Atlantic 

sector of the Southern Ocean (ODP Site 1088) 

during the Early and Middle Pleistocene as 

part of the global extinction of the families 

Pleurostomellidae, Stilostomellidae and portions 

of the Nodosariidae. During the mid- 

Pleistocene Climate Transition (1·2–0·6 Ma) 

in the Southern Ocean, these extinct taxa exhibited 

three pulses of glacial decline in abundance 

and diversity separated by partial interglacial 

recoveries. Beneath the highproductivity 

Benguela Current upwelling region 

(Sites 1082, 1083), glacial declines in the 

extinct taxa were suppressed by favourable 

high organic-carbon flux and consequent lowoxygen 

bottom conditions. Here two major 

pulses of diversity loss occurred at c. 1·3– 

1·2 Ma and 1·0–0·7 Ma. At all three locations, 

the most dramatic decline in abundance and 

diversity occurred c. 0·85–0·80 Ma (marine 

isotope stage 20), and the final disappearance 

of Extinction Group taxa was completed by 

0·67 Ma beneath the Benguela Current and 

0·60 Ma in the Southern Ocean. We speculate 

that this period of enhanced global extinctions 

was linked to a pulsed decline in glacial temperatures 

and/or increase in ventilation of 

deep and intermediate water masses, associated 

with polar ice cap growth since the late 

Pliocene. 

2008010159 

华南梅山剖面二叠纪 - 三叠纪集群绝灭中 

的有孔虫幸存分子 = Foraminiferal survivors 

from the Permian-Triassic mass extinction in 

the Meishan section, South China. ( 英文 ). 

Song Hai-Jun; Tong Jin-Nan; Zhang Ke-Xin; 

Wang Qin-Xian; Z.Q. Chen. palaeoworld, 

2007, 16(1-3): 105-119 

This paper documents abundant and diverse 

foraminifers from Permian-Triassic (P-Tr) 

boundary strata and reports for the first time 

foraminifers from the Lower Triassic Yinkeng 

and Helongshan formations in the Meishan 

section, the global stratotype for the P-Tr 

boundary. The important foraminifer elements 

are illustrated and described. Most of these 

foraminifers were the Permian holdovers, occurring 

above the main extinction event horizon 

(base of Bed 25) at Meishan, and thus 

44

were survivors from the P-Tr mass extinction. 

At Meishan foraminifers underwent a second 

drop in diversity coinciding with the base of 

Bed 28, exhibiting a comparable extinction 

pattern to brachiopod faunas. Both foraminifer 

and brachiopod extinction patterns partly support 

the view that one potential extinction horizon 

coincides with the boundary between 

Beds 27 and 28. 

2008010160 

放射虫研究在古海洋学中的进展 = Progress 

in the study on radiolarians in paleoceanography. 

( 中文 ). 常凤鸣 ; 庄丽华 ; 阎军 . 海洋与湖 

沼 , 2002, 33(6): 20-23 

放射虫是海洋微体古生物的一个重要类 

群 , 广泛分布于从赤道至两极的各种海 

域 , 同时垂直分布于从表层到上千米深的 

水层中 , 其分布格局和群落结构受水体温 

度、盐度、生物产量和营养盐含量等环境 

因素控制 , 又与水体的迁移交换密切相 

关。沉积物中的放射虫化石蕴含着丰富的 

古生态、古海洋环境等地质历史信息 , 其 

丰富的种类性、极高的分异度和对突发性 

海洋 - 气候事件的灵敏反应 , 对建立高分 

辨率地层层序、恢复古气候及重建高精度 

短时间序列的古环境具有重要意义。特别 

是其不易溶的硅质壳 , 在 CCD 以下的深海 

区具有其他钙质类微体化石不可替代的作 

用。自 Meyen1834 年首次研究放射虫以来 

已有 160 多年的历史 , 初期侧重于分类描 

述、生态分布的研究 ,DSDP 和 ODP 的相 

继开展 , 大大促进了其在古海洋学方面的 

进展。本文综述了放射虫在生态分类、生 

物地层、古海洋学参数测定和古海洋环境 

记录等方面的研究进展 , 揭示了放射虫在 

古海洋学研究中的发展趋势和广阔前景。 

2008010161 

冲绳海槽北部表层沉积物中放射虫的分布 

与环境 = Radiolarian distribution in surface 

sediments of the northern Okinawa Trough 

and its relationship to environmental factors. 

( 中文 ). 常凤鸣 ; 庄丽华 ; 李铁刚 ; 阎军 . 海洋地 

质与第四纪地质 , 2002, 22(2): 21-26 

对冲绳海槽北部 80 个表层沉积样品中放 

射虫进行了定量研究表明 , 其丰度和分异 

度西北部低 , 东南部高 , 由西北向东南递 

增 ; 从西北陆架到东南海槽放射虫分布可 

分为陆架低值区、海槽边缘中值区和中央 

高值区。放射虫的组成以泡沫虫目占绝对 

优势 , 总体面貌为热带大洋暖水动物群。 

沉积物中放射虫的分布与现代表层海水温 

度、盐度的分布和变化趋势一致 , 但与营 

养盐和初级生产力的分布呈负相关关系 ; 

同时 , 放射虫的分布又与研究区的海流和 

水团有密切关系 , 其中黑潮对其有控制性 

影响。沉积物类型极大地影响着放射虫的 

分布 , 放射虫的丰度和分异度明显地随粒 

度的增大和陆源物质含量的增加而减小。 

此外 , 放射虫的分布也显示了与沉积物中 

火山物质含量的密切相关性。 

2008010162 

南海巽他陆坡晚更新世以来的微体化石和 

古环境 = Microfossils and paleoenvironments 

of the Sunda slope of the South China Sea 

since the Late Pleistocene. ( 中文 ). 赵泉鸿 ;W 

Kuhnt;K Stattegger; 成鑫荣 . 海洋地质与第四 

纪地质 , 2002, 22(2): 63-68 

柱状样 18288-2 采自于南海南部巽他陆 

坡 (5°44'N、110°44‘E, 水深 788m, 柱长 

6.8m), 通过与邻近柱状样同位素的对 

比 , 其揭示了末次冰盛期以来的沉积。柱 

状样中指示水深较大的介形类和浮游有孔 

虫丰度自下而上呈现明显增加的趋势 , 而 

指示水深较浅的介形类丰度及介形虫 / 浮游 

有孔虫比值和底栖有孔虫在有孔虫全群中 

的丰度都呈下降趋势 , 反映了研究区末次 

冰盛期以来海面上升和海水加深的过程。 

这两类的变化在 YD 至全新世早期最为显 

著 , 与该时期海面快速上升造成成的环境 

急剧变化相对应。异地介形虫广见于末次 

冰期和全新世早期的沉积中 , 反映冰期低 

海面和冰后期海侵初期频繁发生源于陆架 

的顺坡搬运。依据末次冰期沉积中含较多 

的底栖有孔虫 Uvigerina 和 Bulimina、介形虫 

Polycope 和 Cytherella , 及底栖有孔虫 U. 

peregrina 较低的 δ 13 C, 推测冰期低海面时底 

层水状况为低氧和高营养 , 在冰盛期尤为 

发育。 

2008010163 

南黄海 EY02-2 孔底栖有孔虫群落特征与全 

新世沉积速率 = Foraminiferal faunas and 

Holocene sedimentation rates of core EY02-2 

in the South Yellow Sea. ( 中文 ). 庄丽华 ; 常凤 

鸣 ; 李铁刚 ; 阎军 . 海洋地质与第四纪地 

质 , 2002, 22(4): 7-14 

南黄海中部泥质区的 EY02-2 孔揭示了氧 

同位素 6 期以来的海侵海退序列。该孔浮 

游有孔虫匮乏。底栖有孔虫丰富。 

93.87%~100% 底栖有孔虫为玻璃质壳。对 

45

33 个变量 98 个样品的 Q 型因子分析得到 5 

个主因子 , 方差累积贡献为 96.51。主因子 

1 为 Ammonia beccarii vars。组合。代表滨 

岸环境 , 主因子 2 为 Protelphidium tuberculatum 

组合 , 代表黄海沿岸流冷水分布区或 

水体较凉的浅海沉积环境 ; 主因子 3 为 

Elphidium magellanicum 组合 , 代表近岸浅 

海环境 ; 主因子 4 为 Ammonia ketienziensis 

组合 , 代表水深大于 50 m 的浅海环境 ; 主 

因子 5 为 Buccella frigida 组合 , 代表较冷的 

沉积环境。南黄海中部涡旋泥开始形成的 

时代约为 9.7kaBP。大致在 4.6 kaBP 南黄海 

中部全新世海平面高度超过现今海平面。 

0~7.9kaBP 期间 , 沉积速率较低 , 为 0.133 

mm/a; 7.9~10.16kaBP 期间 , 沉积速率较高 , 

为 0.426 mm/a。 

2008010164 

南海南部晚中新世的放射虫及其环境探讨 

= Radiolarians of Late Miocene from Southern 

South China Sea and their environment 

implications. ( 中文 ). 陈木宏 ; 王汝建 ; 韩建修 ; 

陆钧 ; 杨丽红 . 热带海洋学报 , 2002, 21(2): 

66-74 

南海是东亚古季风产物的主要沉积盆 

地 , 保存着比陆地更加完整和连续的沉积 

记录。详细分析了 ODP 1143 号钻井晚中新 

世的放射虫化石群 , 主要根据标志种 

Diartus petterssoni, D. hughesi 和 Stichocorys 

delmontensis 等的分布特征 , 分别建立了南 

海南部晚中新世的 RN6,RN7 和 RN8 等 3 

个放射虫化石带 , 并讨论了其地层年龄。 

探讨了以地层中放射虫的丰度变化特征等 

在南海南部作为东亚古夏季风活动替代性 

指标的可能性 , 初步说明东亚古夏季风可 

能早于 8.7Ma B. P. 出现 , 约在 8.24Ma B.P. 

强化达到高峰 , 认为与印度季风的出现几 

乎同步或略早。 

2008010165 

塔里木盆地艾克提克群中放射虫化石及其 

意义 = New discovery of radiolarian fossils 

from Aiktik Group in Tarim Basin and its significance. 

( 中文 ). 李曰俊 ; 王招明 ; 买光荣 ; 吴 

浩若 ; 黄智斌 ; 谭泽金 . 新疆石油地质 , 2002, 

23(6): 496-500 

中国南天山西端的艾克提克群是卷入南 

天山造山带的一个重要的岩石地层单元 , 其 

与相邻地层单元均以断层接触。以往根据 

在其灰岩和砂质灰岩中发现的 

Pseudostaffella sp.,Profusulinella sp. 和 

Fusulinella sp. 将其归属于上石炭统。我们 

的放射虫化石发现于托什罕河上游的哈拉 

道克剖面 , 主要包括 Albaillella undulata 

Deflandre, Albaillella paradoxa Deflandre,Albaillella 

sp.aff. A. paradoxa Deflandre,Albaillella 

sp. cf. A. deflandrei Gourmelon, 

Albaillella sp., Albaillella excelsa 

Ishiga, Kito and Imoto(), Belowea variabilis(Ormiston 

et Lane), Callella cf. C. parvispinosa 

Won, Entactinia cf. E. tortispina 

Ormiston et Lane,Entactinia aff. E. tortispina 

Ormiston et Lane,Entactinia variospina Won, 

Entactinia sp. Eostylodictya rota (Won), 

Latentifistula impella (Ormistone et Lane) (), 

Latentifistula turgida Ormiston et Lane, Latentifistulidae 

gen. et. sp. indet. 和 Polyentactinia 

cf. aranea Gourmelon 。其中 , 

Albaillella excelsa Ishiga, Kito and Imoto () 

的时代为晚二叠世 ( 存疑 ), 其余可以划 

分出早石炭世早期和晚期两个放射虫化石 

组合 : 前者以 Albaillella undulata Deflandre, 

Albaillella paradoxa Deflandre 和 Albaillella 

sp. cf. A. deflandrei Gourmelon 为代表 , 后 

者以 Eostylodictya rota (W0n) 为代表。这是 

艾克提克群中首次发现放射虫化石 , 同时 

是在中国南天山首次发现晚二叠世放射虫 

化石 , 也是中国南天山最西部的放射虫化 

石点 , 具有重要的地质研究意义。 

2008010166 

南沙海区晚第四纪浮游有孔虫演化及其古 

海洋学意义 = Late Quaternary evolution of 

planktonic foraminifera in the southern South 

China Sea and their paleoceanographic significance. 

( 中文 ). 李保华 ; 赵泉鸿 ; 陈民本 ; 翦 

知湣 ; 汪品先 . 微体古生物学报 , 2001, 18(1): 

1-10 

通过对南沙海区 17957 和 17958 两柱状 

样中浮游有孔虫的研究 , 首次揭示了南海晚 

第四纪以来较长时间尺度上 (0 - 800ka BP) 

存在 δ 18 O 11 期 ( 约 400ka BP) 开始的粉红色 

Globigerinoides ruber 大量出现和 Globigerina 

rubescens 较高相对丰度 , δ 18 O 5e 期 ( 约 

120ka BP) 的粉红色 Globigerinoides ruber 绝 

灭 ,Globoquadrina conglomerata 大量出 

现 ,Globorotalia truncatulinoides 左旋型分子 

绝对优势开始 , 和 δ 18 O 4/5 期界线附近 ( 约 

80ka BP) 的 Globoquadrina conglomerata 绝灭 

等三次浮游有孔虫演化事件。南沙与南海 

北部及西北太平洋等海区的浮游有孔虫演 

化事件对比表明 : 南沙海区在 400ka BP 开始 

海水温跃层相对较深 ; 至 δ 18 O 5e 期 , 受西北太 

平洋中层水加强的影响、南沙海水温跃层 

变浅 ; 在 δ 18 O 5e 至 4/5 期界线这段时期内与 

西北太平洋水体交换比较自由。 

46

2008010167 

蜓类 Yabeina 与 Chusenella 生态环境的对 

比研究 = A comparative study on ecological 

environments of Yabeina and Chusenella, 

Permian fusulinaceans. ( 中文 ). 徐光伟 ; 杨湘 

宁 ; 施贵军 ; 刘家润 ; 孙历 . 微体古生物学 

报 , 2001, 18(1): 29-33 

对贵州盘县火铺剖面茅口组蜓类分布规 

律的研究显示 , 尽管蜓类 Yabeina 及 

Chusenella 生存时代相同 , 并可见于同一剖面 , 

但两者在具体产出层位上却具有互不共生 

的特点。利用多元统计分析方法对 Yabeina 

及 Chusenella 分布层位的沉积环境进行了对 

比研究。结果表明 ,Yabeina 生活在水动力条 

件较强的正常浅海、台地及水能量较高的 

近岸浅滩 ;Chusenella 则主要适应于低能环 

境 , 生活在水动力条件较弱的清澈浅海、局 

限浅水台地。 

2008010168 

土耳其西北部卡拉卡娅混杂岩中二叠世有 

孔虫 Chitralinidae 科新属种 = New Middle 

Permian foraminifers (Chitralinidae) from the 

Karakaya Complex, in northwestern Turkey. 

( 英文 ). Okuyucu C. Comptes Rendus 

Palevol, 2007, 6(5): 311-319 

One new foraminiferal genus, Rectoformata 

gen. nov., with two new species, has been described 

from a Permian limestone block in the 

Karakaya Complex in the South of the Balya 

district (Balikesir, northwestern Turkey). The 

type species of Rectoformata, Rectoformata 

tekini sp. nov., is characterized by a quadrangular 

transverse section having a calcareous 

microgranular wall with fine alveolar structures, 

whereas Rectoformata acari sp. nov. is 

recognized by a pentagonal transverse section 

having a calcareous microgranular wall with 

fine alveolar structures. The age of the described 

taxa is assigned as Midian 

( = Capitanian) based on the association with 

small foraminifers and fusulinids. These new 

taxa are included in the family Chitralinidae, 

which is emended herein. 

2008010169 

贵州紫云晒瓦群中放射虫 Neoalbaillella 动 

物群的发现 = Discovery of the Neoalbaillella 

radiolarian fauna in the Shaiwa Group of Ziyun 

District, Guizhou. ( 中文 ). 王玉净 ; 尚庆华 . 

微体古生物学报 , 2001, 18(2): 111-121 2 图 

版 . 

首次报道贵州紫云晚二叠世晒瓦群顶部 

硅质岩中 Neoalbaillella 动物群 , 计 12 种 ,5 未 

定种 , 归属于 12 属 9 科 4 超科 2 亚目 , 其中 1 

新属 (Spongosphaeradiscus gen.nov.),2 新种 

(Spongosphaeradiscus shaiwaensis sp. nov. 

和 Copicyntra shaiwaensis sp. nov.)。根据这 

个动物群建立 Neoalbaillella ornithoformis- 

Spongosphaeradiscus shaiwaensis 带 , 与东亚 

和美国西海岸长兴期的 Neoalbaillella ornithoformis 

带对比。 

古杯、多孔及腔肠动物 

2008010170 

黔东北志留纪兰多维列世的似发珊瑚属 

(Pilophyllia Ge et Yü,1974) 新资料 = New 

information on Silurian Rugosan genus Pilophyllia 

ge et yü, 1974 in northeastern Guizhou. 

( 中文 ). 唐兰 ; 何心一 ; 陈建强 . 古生物学 

报 , 2007, 46(1): 98-112 4 图版 . 

Pilophyllia Ge et Yü,1974 具有典型的包珊 

瑚型隔壁 , 是包珊瑚科的主要分子。该属广 

泛分布于上扬子区志留纪兰多维列世地 

层。首次对采自贵州石阡中兰多维列世 

(Llandovery) 爱隆期 (Aeronian) 香树园组和雷 

家屯组的大量 Pilophyllia Ge et Yü,1974 标本 

进行详细研究 , 经鉴定 , 共计有 9 种 , 其中包括 

6 新种 ,1 未定种 , 它们是 : Pilophyllia simplex 

Chen,1986, P. fenggangensis Ge et Yü,1974, 

P. vesiculosa Tang sp. nov., P. conica Tang sp. 

nov., P. ultimuma Tang sp. nov., P. stylaris 

Tangsp. nov., P. raritabulata Tang sp. nov., P. 

leijiatunensis Tang sp. nov., Pilophyllia sp.。 

此外 , 根据新的研究材料补充和修订 

Pilophyllia 部分属征 , 并将石阡地区香树园组 

和雷家屯组的 Pilophyllia 种群特征与川北、 

陕南宁强组 (Telychian 阶 ) 的进行比较。 

2008010171 

藏北申扎地区晚二叠世早期的皱纹珊瑚 = 

Early Late Permian rugosa in the Zainza 

area,northern Tibet. ( 中文 ). 程立人 ; 武世忠 ; 

张予杰 . 地质通报 , 2002, 21(1): 24-28 1 图版 . 

作者在进行申扎县幅 1∶25 万区域地质 

调查工作中 , 发现一套巨厚的白云岩和白云 

质灰岩组成的岩系 , 整合覆于早二叠世中晚 

期地层下拉组之上 , 并在此岩系底部采集到 

晚二叠世早期的皱纹珊瑚 Waagenophyllum 

indicum var. crassiseptatum Wu 和 Liangshanophyllum 

streptoseptatum Wang, 从而确 

定本区有晚二叠世地层的存在。 

2008010172 

47

藏北申扎地区上二叠统木纠错组的建立及 

皱纹珊瑚组合 = Establishment of the Upper 

Permian Mujiu Co Formation and rugose coral 

assemblage in the Xainza area,northern Tibet. 

( 中文 ). 程立人 ; 王天武 ; 李才 ; 武世忠 . 地质通 

报 , 2002, 21(3): 140-143 

在申扎县城东南木纠错南东岸附近发现 

一套巨厚的以白云岩、白云质灰岩为主组 

成的岩系 , 厚达 2348m。该岩系整合覆于下 

二叠统下拉组之上 , 并于其底部发现中国南 

方晚二叠世早期珊瑚动物群中的重要分子 

Waagenophyllum indicum crassiseptatum Wu 

和 Liangshanophyllum streptoseptatum Wang 

两种 , 与其共生的还有 Lobatophyllum zakangense 

Wu 和 Waagenophyllum megacolumetum 

Wu, 它们共同组成一个晚二叠世早期特 

有的皱纹珊瑚动物组合 , 命名为 

Waagenophyllum-Liangshanophyllum- 

Lobatophyllum 组合。将含有这一珊瑚化石 

组合的以白云岩、白云质灰岩为主的岩系 

另建立新组 ——— 木纠错组 , 该组在层位上 

相当于中国南方上二叠统的吴家坪组。 

2008010173 

北天山上石炭统奇尔古斯套组中发现早二 

叠世珊瑚化石 = Discovery of the Early Permian 

coral fossils in the Upper Carboniferous 

Qiergusitao Formation in the North Tianshan,Xinjiang. 

( 中文 ). 何世平 ; 胡云绪 ; 赵振 

明 ; 冯益民 . 地质通报 , 2002, 21(10): 648-652 

新近于北天山艾维尔沟北原划为上石炭 

统的奇尔古斯套组火山岩系所夹灰岩中 , 采 

到了结节脊板杯珊瑚 Cyathocarinia tuberculata 

Soshkina, 其时代属于早二叠世 , 表明该 

区奇尔古斯套组的一部分应属下二叠统。 

另外 , 于头屯河原划为上石炭统的奇尔古斯 

套组火山 - 碎屑岩系所含灰岩砾石中 , 采到伊 

万诺夫格鲁特珊瑚 Grootia ivanovi Dubrolyubova, 

时代属于晚石炭世 , 与达拉阶 ( 即莫 

斯科阶 ) 相当 , 故地层时代应晚于晚石炭世达 

拉期 , 根据区域对比推测该地层的一部分也 

应属于下二叠统。艾维尔沟一带早二叠世 

珊瑚化石的发现 , 表明北天山石炭纪强烈的 

拉张事件可以持续到早二叠世。 

2008010174 

白垩纪珊瑚属 Paronastreae 的形态 , 系统分 

类和分布 = Morphology, taxonomy and distribution 

of the Cretaceous coral genu Paronastraea 

(Barremian-Cenomanian; Scleractinia). 

( 英文 ). Loser H. Rivista Italiana di 

Paleontologia e stratigrafia, 2006, 112(1): 

113-121 

The Middle Cretaceous genus Paronastraea 

Beauvais, 1977 is being revised on the basis of 

dample material available from Italy, France, 

Germany, and Greece. Paronastraea, a 

plocoid and cerioid coral similar to Pachycoenia, 

is characterised by regular secondary septal 

apophyses arranged in pairs. Six species 

are distinguished by their respective numbers 

of septal cycles and systems, two of them in 

open nomenclature and one, Paronastraea 

occulta from the Early Aptian of Greece, is 

newly described. The genus occurred from the 

Barremian to the basal Cenomanian in the 

central and eastern Tethys. 

2008010175 

葡萄牙中新世 Mem Moniz 泥灰岩硅质海绵 

骨针及其环境意义 = Siliceous sponge spicules 

from the Miocene Mem Moniz marls 

(Portugal) and their environmental significance. 

( 英文 ). Pisera A; Cachao M; Marques 

da Silva C. Rivista Italiana di Paleontologia e 

stratigrafia, 2006, 112(2): 287-299 

The assemblage indicates that the sponge 

fauna was dominated by Astrophorida, and in 

particular by Geodiidae. The presence of Eurylus 

sp. and probably Geodia sp., Samus sp. 

and Alectona wallichii is also reported for the 

first time. The studied sponge assemblage is 

clearly neither characteristic of very shallow 

nor very deep marine environments. The 

dominance of astrophorids and the presence of 

lithistids and hexactinellids suggest a depth of 

at least several tens to one hundred metres, or 

even more. 

2008010176 

澳大利亚昆士兰北部 Burdekin 盆地中泥盆 

世层孔虫 - 刺毛虫类组合中的共生组合体 = 

Symbionts in a stromatoporoid-chaetetid association 

from the Middle Devonian Burdekin 

Basin, north Queensland. ( 英文 ). Zhen YY, 

West R R. Alcheringa, 1997, 21(3/4): 271-280 

A spectacular association between a 

chaetetid, a stromatoporoid (Salairella sp.), 

and straight, vertical tubes interpreted to have 

housed symbiotic worms is reported from the 

Givetian Burdekin Formation, Burdekin Basin, 

north Queensland. The final growth surface of 

Salairella sp. shows skeletal distortion characterised 

by long, rather continuous coenosteles 

and coenostroms with upturned edges, This 

distorted interface was probably the result of 

spatial competitive interaction between the 

encrusting chaetetid and the underlying stromatoporoid. 

Neither sediment infilling, erosion 

or surface breakage occurs on the final 

48

growth surface of the stromatoporoid skeleton. 

As such, the growth of the Salairella sp. 

specimen appears to have been supressed by 

the encrusting chaetetid. Worm tubes are continuous 

through the distorted interface without 

interruption. The skeletal association also 

suggests that the round, straight, vertical tubes 

had a symbiotic intergrowth relationship initially 

with the stromatoporoid and, subsequently, 

the chaetetid. 

苔藓动物 

2008010177 

利比亚西北部的黎波里塔尼亚地区上奥陶 

统 Jifarah (Djeffara) 组苔藓虫泥丘 = Bryozoan 

Mud-Mounds from the Upper Ordovician 

Jifarah (Djeffara) Formation of Tripolitania, 

north-west Libya. ( 英文 ). Buttler C J; 

Cherns L; Massa D. Palaeontology, 2007, 

50(2): 479-494 

A bryozoan fauna from carbonate mudmounds 

is described from subsurface well 

cores from the Upper Ordovician (Lower 

Ashgill) Jifarah (Djeffara) Formation of 

Tripolitania, north-west Libya. Among a diverse 

assemblage dominated by trepostomes, 

nine species of bryozoans are identified, including 

Jifarahpora libyensis gen. et sp. nov. 

Delicate and robust branching, encrusting and 

nodular bryozoan growth forms are all common. 

The bryozoan-rich limestones are mostly 

mudstones and wackestones, with bafflestone 

and floatstone textures, but the mounds apparently 

lack organic framework and microbial 

fabrics. Regional geophysical data indicate 

rapid thickness changes between wells, where 

mound complexes locally up to 100 m thick 

had limited topographic relief over the surrounding 

sea floor. The mounds formed in a 

high-latitude, cool-water carbonate belt that 

extended widely across the northern margin of 

Gondwana. Quaternary analogues from the 

Great Australian Bight suggest that these early 

Ashgill mounds may have developed in slope 

environments during an episode of glacial 

lowstand that preceded the late Ashgill, 

Hirnantian glacial event. 

2008010178 

苔藓虫古生态指示显生宙中期集群灭绝是 

长期环境应力的结果 = Bryozoan paleoecology 

indicates mid-Phanerozoic extinctions 

were the product of long-term environmental 

stress. ( 英文 ). Powers C M; Bottjer D J. Geology, 

2007, 35(11): 995-998 

We compiled the global onshore-offshore 

distribution of marine bryozoans within 396 

Permian–Early Jurassic bryozoan assemblages 

and show that bryozoan assemblage generic 

richness declined significantly in advance of 

the end-Permian and end-Triassic mass extinctions, 

starting as early as the Capitanian prior 

to the end-Permian and the Norian prior to the 

end-Triassic. We also show that offshore settings 

were affected first, prior to both extinctions, 

suggesting that environmental stress 

resulted from the gradual encroachment of 

some deep-water phenomenon onto the 

shelves. These patterns support long-term 

oceanographic, rather than extraterrestrial, 

extinction mechanisms, such as widespread 

euxinia triggered by massive volcanism and 

global warming. Tracking the onshoreoffshore 

environmental distribution of these 

marine invertebrates provides a unique approach 

to assessing prolonged environmentally 

induced stress through this 120 m.y. time interval. 

腕足动物 

2008010179 

大庆中央拗陷区早二叠世腕足动物群的发 

现及其地层意义 = Discovery of an Early 

Permian brachiopod fauna in the central depression 

of the Daqing prospect area and its 

stratigraphic significance. ( 中文 ). 廖卓庭 ; 万 

传彪 . 地质学报 , 2002, 76(1): 50-54 

位于大庆中央拗陷区腹部的杜 101 井 , 在 

1700 余米井下 , 首次发现保存完好的腕足类 

等多门类化石 , 经研究确认 : 腕足动物群属于 

天山 - 兴安沉积区早二叠世广泛分布的北山 

类群。从而肯定了大庆探区大面积中新生 

界之下存在正常沉积的海相下二叠统 , 说明 

松辽盆地北部盆地的基底为海西期浅层褶 

皱基底。这一发现不仅对松辽盆地二叠纪 

构造与生物古地理变迁机制等理论问题的 

深入研究有重要意义 , 也对大庆探区开展深 

部油气勘探 , 寻找新的油气接替层位提供了 

实际依据 , 应引起有关方面的重视。 

软体动物 

2008010180 

阿根廷 Neuquén 盆地下白垩统菊石 : 

Viluceras, 凡兰吟阶 Olcostephanus 的一个 

新亚属 = Lower Cretaceous ammonites from 

the Neuquén Basin, Argentina: Viluceras, a 

new Valanginian subgenus of Olcostephanus. 

( 英文 ). Aguirre-Urreta M B; Rawson P F. 

Cretaceous Research, 1999, 20(3): 343-357 

49

Viluceras is proposed as a new subgenus of 

Olcostephanus to accommodate a distinctive 

Argentinian Lower Cretaceous (Upper 

Valanginian) ammonite fauna originally assigned 

to the boreal genus Simbirskites and 

subsequently placed in Lemurostephanus . 

Based on extensive new collections from eight 

localities in the Neuquén Basin, three Viluceras 

species are described, including O. 

(Viluceras) duraznoensis sp. nov. With them 

occur rareO. (Olcostephanus) mingrammi 

(Leanza). The fauna characterises the Olcostephanus 

(Viluceras) permolestus Subzone, 

which may correlate approximately with the 

Himantoceras trinodosum Zone of the West 

Mediterranean Province. 

2008010181 

欧洲上坎帕阶和马斯特里赫特阶箭石生物 

地层综述 = A review of the Upper Campanian 

and Maastrichtian belemnite biostratigraphy 

of Europe. ( 英文 ). Christensen W K. 


The conventional belemnite zonation of 

northwest Europe includes three Upper Campanian 

Belemnitella zones, two Lower Maastrichtian 

Belemnella zones, in addition to the 

lower Upper Maastrichtian Belemnitella junior 

Zone and upper Upper Maastrichtian Belemnella 

casimirovensis Zone. These zones are 

critically assessed. Recent belemnite subdivisions 

of the Upper Campanian and Lower 

Maastrichtian are reviewed. The Upper Campanian 

of Norfolk has been subdivided into 

seven informal Belemnitella zones and subzones, 

and the Lower Maastrichtian of northwest 

Germany into six formal Belemnella 

zones. The timespan of the Early Maastrichtian 

zones is estimated and the duration 

varies from 0.12–0.60 Ma. It is shown that the 

base of the basal Maastrichtian Belemnella 

lanceolata Zone is slightly diachronous, and 

the base of theB. casimirovensis Zone is 

highly diachronous across Europe. 

2008010182 

西藏达雄群的化石新资料和再认识 = Some 

new fossil materials and new understanding of 

the Daxiong Group in Tibet. ( 中文 ). 石和 ; 陶 

晓风 ; 胡新伟 ; 马润则 ; 刘登忠 ; 周家云 . 地质通 

报 , 2002, 21(11): 784-786 

在达雄群中新发现的双壳 Ludbrookia 

daxungensis,L. daxungensis,Rasatrix cf. 

suzulii,Arctica subextensa 及腹足 Biplica 

obliqu 等化石 , 具早白垩世动物群组合面貌 , 

表明该群的沉积时代大致为早白垩世欧特 

里夫 — 阿尔布期 (Hauterivian-Albrian), 而不 

是前人划归的中 — 晚侏罗世 , 与区内的早白 

垩世则弄群上部相当。 

2008010183 

长江源各拉丹冬地区上三叠统结扎群双壳 

类组合与古环境 = Paleoecological environment 

and assemblage of fossil bivalves from 

the Upper Trassic Jieza Group in the headwaters 

of the Yangtze River. ( 中文 ). 汤朝阳 ; 王 

新昆 ; 姚华舟 ; 牛志军 ; 段其发 ; 赵小明 ; 王建雄 . 

新疆地质 , 2006, 24(3): 239-243 

在长江源各拉丹冬地区雀莫错一带上三 

叠统结扎群采获大量双壳类化石 , 根据产出 

层位 , 建立了 Quemocuomegalodon orientus- 

Neomegalodon boeckhi 、 Halobia superbescens-Halobia 

disperseinsecta、Amonotis togtonheensis-Cardium 

(Tulongocardium) xizangensis 

3 个组合 . 这一生物组合反映的地质时 

代为诺利期 , 依据双壳类化石的外部形态和 

内部构造特征及围岩岩石化学分析 , 说明垂 

向上双壳类生活的结扎群具浅 — 深 — 浅的 

古地理变化特征 , 为区域上地层对比及生物 

生存环境提供了基础资料 . 

2008010184 

日本新近系 Epilucina californica (Conrad) 

(Bivalvia: Lucinidae) 化石及 Epilucina 属 

的生物地理历史简论 = Occurrence of Epilucina 

californica (Conrad) (Bivalvia: Lucinidae) 

from the Neogene of Japan, with notes on the 

biogeographic history of Epilucina. ( 英文 ). 

Kurihara Y. Paleontological Research, 2007, 

11(1): 29-39 

The California lucine, Epilucina californica 

(Conrad, 1837), is reported from lower Middle 

Miocene to Upper Pliocene strata in Japan. 

This extends the oldest record of this species 

and represents the first detailed record of the 

species and genus in the western North Pacific 

region. Based on the Paleogene fossil record 

of Epilucina and the general migration pattern 

of Neogene North Pacific mollusks, it is inferred 

that E. californica originated in the 

eastern North Pacific during Late Oligocene 

or Early Miocene time and migrated westward 

to the western North Pacific during the early 

Middle Miocene. The western North Pacific 

populations of E. californica became extinct 

by the end of the Pliocene, whereas the eastern 

North Pacific populations survive in California. 

This species is, therefore, regarded as a 

northeastern Pacific restriction taxon. Two 

Japanese fossil species, Lucina (Myrtea) nip- 

50

ponica Nomura and Hatai, 1936 and Lucina 

japonica Ozaki, 1958 are junior synonyms of 

E. californica. 

2008010185 

越南北部 Song Da 盆地、An Chau 盆地下 

三叠统双壳类化石 = Lower Triassic bivalve 

fossils from the Song Da and An Chau Basins, 

North Vietnam. ( 英文 ). Komatsu T; Dang T H. 


144 

In North Vietnam, the Hua Tat, Pa Khom 

and Lang Son Formations yield abundant 

Lower Triassic bivalves. The occurrence of 

Eumorphotis sp. cf. E. multiformis, represents 

the first fossil reported from the Hua Tat Formation, 

while Claraia aurita, C. concentrica, 

and C. intermedia multistriata are found in the 

upper Lang Son Formation. The Pa Khom 

Formation contains C. intermedia multistriata, 

Claraia sp., and Lopha sp. The occurrence of 

C. intermedia multistriata indicates that the Pa 

Khom Formation and the upper Lang Son 

Formation are Olenekian in age. These 

Claraia spp. are found in wave-dominated 

nearshore deposits characterized by hummocky 

cross stratification and wave-ripple 

laminations, although Claraia in other areas is 

generally found in deep-sea mudstone. 

2008010186 

近 5000 年来冲绳岛一水下洞穴中的穴居双 

壳类动物群变化及环境变迁 = Changes in 

cavernicolous bivalve assemblages and environments 

within a submarine cave in the Okinawa 

Islands during the last 5,000 years. ( 英 

文 ). Kitamura A; Hiramoro M; Kase T; Yamamoto 

N; Amemiya M; Ohashi S-I. Paleontological 

Research, 2007, 11(2): 163-182 

Although many workers have investigated 

the ecological and evolutionary significance of 

cryptic organisms and short-term (seasonal to 

annuals) fluctuations in environments and 

fauna within submarine caves, no studies have 

examined millennia-scale variations in the 

organisms and environments. In this study, we 

analyzed the sedimentary characters and species 

composition of bivalves from surface and 

cored sediments within the Daidokutsu submarine 

limestone cave on the fore-reef slope 

of Ie Island, off the island of Okinawa, Japan. 

The sediments in the central and innermost 

area of the cave consist of carbonate mud. 

Their deposition indicates that a still-water 

environment prevailed over the past 5,000 

years. Analysis of the spatial and temporal 

distribution of the bivalves shows that species 

living in the innermost area of the cave became 

dominant over at least the past 5,000 yrs, 

while species living near the entrance of the 

cave declined in abundance. This indicates 

that the environmental conditions of the innermost 

cave area gradually spread to the entrance 

of the cave. We believe that this phenomenon 

is explained by spreading nutritional 

deficiency within Daikodutsu cave. 

2008010187 

侏罗纪箭石分布模式 : 南极和阿根廷新材 

料的意义 = Jurassic belemnite distribution 

patterns: implications of new data from Antarctica 

and Argentina. ( 英文 ). Doyle P, Kelly 

S R A, Pirrie D, Riccardi A C. Alcheringa, 

1997, 21(3/4): 219-228 

Belemnites are nektopelagic cephalopods 

which developed a widespread pattern of distribution 

in the Jurassic, and most authors 

have accepted that their centre of origin was 

Europe. Available data suggest that the belemnites 

developed a global distribution only 

in the Toarcian, some 15 Ma after their first 

appearence in the European Hettangian. Development 

of the Boreal and Tethyan belemnite 

realms took place in the Middle Jurassic 

and continued through to the Cretaceous. New 

data from Argentina and the Antarctic Peninsula 

reaffirms the development of the global 

distribution of belemnites in the Toarcian, and 

sheds new light on the biogeographical patterns 

for the Jurassic of the southern hemisphere. 

This has considerable implications for 

understanding the development of faunal 

realms in the Mesozoic. 

2008010188 

阿根廷巴塔哥尼亚中部 Gran Barranca 地 

区中始新世陆生 Charopidae 科微腹足类 = 

Middle Eocene land microgastropods 

(Charopidae) from Gran Barranca (Central 

Patagonia, Argentina).. ( 其他 ). Miquel S E; 

Bellosi E S. Ameghiniana, 2007, 44(1): 121- 

131 

New land microgastropods Charopidae 

were found in the Rosado carbonate paleosol 

(late Middle Eocene, Mustersan South American 

Land Mammal Age), of the Sarmiento 

Formation at the Gran Barranca locality (Chubut 

province, Argentina). The most ancient 

fossils of Rotadiscus and Lilloiconcha and the 

first Eocene record of Radiodiscus are described. 

Most of the fossil taxa are compared 

with extarit species (Rotadiscus amancaezensis 

(Hidalgo), Stephadiscus celinae (Hylton 

51

Scott), Radiodiscus riochicoensis Crawford 

and Lilloiconcha gordurasensis (Thiele)), and 

hence they would be their first fossil record. 

The high diversity of the assemblage (7 species) 

is unusual for a single bed, and it is comparable 

to the more diverse recent South 

American microgastropod faunas. The gastropod 

assemblage of the Rosado paleosol is 

similar to present-day northwestern Patagonia 

association, and indicates a humid and coldtemperate 

climate. Such conditions would 

have change during the late pedogenesis stage 

(Late Eocene) towards a dry climate. The 

abundance of the specimens and the preservation 

of their delicate sculptures reflect appropriate 

conditions for preservation related to 

soil carbonate cementation. 

2008010189 

头足类爱丽斯木角石目 ( 鹦鹉螺亚纲 , 头 

足纲 ) 的一些少为人知的特征 = Some 

lesser known features of the ancient Cephalopod 

Order Ellesmerocerida (Nautiloidea, 

Cephalopoda). ( 英文 ). Kröger B. Palaeontology, 

2007, 50(3): 565-572 

Three specimens of the small breviconic 

ellesmeroceratid Paradakeoceras minor 

Flower, 1964 from the Tremadocian of the 

New York area preserve the annular elevation 

and muscle scars in moulds of the body chamber. 

The annular elevation is positioned at the 

base of the body chamber and is wider on the 

convex side of the shell than on the concave 

side. Multiple paired muscle scars can be seen 

within this annular elevation. A wellpreserved 

body chamber of the breviconic 

ellesmeroceratid Levisoceras cf. edwardsi 

Ulrich, Foerste and Miller is described. Its 

body chamber shows a strong anterior– 

posterior asymmetry, which is common within 

the Ellesmeroceratida. The shape of the body 

chamber and of the soft body attachment 

structures has led to a reconstruction of an 

ellesmeroceratid soft body that is organized 

like a primitive conchiferan mollusc. Based on 

this reconstruction, a tryblidian cephalopod 

ancestor is supported. An evolutionary scenario 

is reconstructed from an ancestral nautiloid 

that is stretched along the anterior– 

posterior axis, and has serially arranged shell 

muscles and a small mantle cavity, towards a 

modern cephalopod with a dorsal–ventral 

body orientation, reduced number of shell 

muscles and a large mantle cavity. 

2008010190 

穿越二叠纪 / 三叠纪界线的菊石 : 分支分类 

学的视角 = Ammonoids across the Permian/Triassic 

boundary: a cladistic perspective. 

( 英文 ). McGowan A J; Smith A B. Palaeontology, 

2007, 50(3): 573-590 

The rapid diversification of ceratitid ammonoids 

during the earliest Mesozoic has 

been taken at face value as an example of explosive 

radiation following the Permian/Triassic 

mass extinction. However, the 

validity of this interpretation has never been 

tested within a phylogenetic framework. A 

total evidence cladistic analysis of Mid–Late 

Permian and Induan (earliest Triassic) ammonoids 

confirms the monophyly of the 

Ceratitida. Partitioned phylogenetic analysis 

of suture line characters vs. shell shape and 

ornament characters confirms the importance 

of suture-line characters for resolving the 

higher taxonomy of ammonoids. When the 

cladogram is compared with the observed fossil 

record, the resultant tree implies that the 

divergence of a number of early Triassic lineages 

actually occurred during the latest Permian. 

If these range extensions are taken into 

account the ammonoid per-genus extinction 

rate across the Permian/Triassic boundary 

drops from c. 85 per cent to c. 60 per cent. 

2008010191 

藏南喜马拉雅山菊石及二叠 / 三叠纪界线 = 

Ammonoids and the Triassic/Jurassic Boundary 

in the Himalayas of Southern Tibet. ( 英 

文 ). Yin Jiarun; Smith P L; Pálfy J; Enay R. 

Palaeontology, 2007, 50(3): 711–737 

The sections of Germig in the Nyalam area, 

southern Tibet, provide a continuous exposure 

of ammonoid-bearing, uppermost Triassic and 

basal Jurassic strata. Eighteen species (three of 

them new) are described and illustrated: Choristoceras 

marshi Hauer, C. aff. marshi, C. cf. 

nobile Mojsisovics, C. nyalamense sp. nov., 

Eopsiloceras germigense sp. nov., Pleuroacanthites 

aff. biformis (Sowerby), Rhacophyllites 

sp., Nevadaphyllites cf. psilomorphus 

(Neumayr), Neophyllites sp. indet., Neophyllites 

cf. biptychus (Lange), Psiloceras tibeticum 

sp. nov., P. calliphyllum (Neumayr), 

Euphyllites cf. struckmanni (Neumayr), Discamphiceras 

pleuronotum (Canavari), Alsatites 

spp., Kammerkarites frigga, and K. sp. 

The ammonoid fauna shows a strong affinity 

to that of the Northern Calcareous Alps, although 

diversity in the Calliphyllum Zone is 

markedly lower. The ammonoid succession 

across the Triassic/Jurassic boundary is subdivided 

into four zones: the Rhaetian Marshi, 

52

the basal Hettangian Tibeticum, the lower 

Hettangian Calliphyllum, and the middle Hettangian 

Pleuronotum zones. It is the only 

known succession across the Triassic/Jurassic 

boundary in the Tethyan Realm that is not 

condensed. The Marshi and Calliphyllum 

zones are correlated with the same zones in 

the Northern Calcareous Alps. The Tibeticum 

Zone, a new local zone, is transitional between 

the Marshi and the Calliphyllum zones in that 

it yields both choristoceratids and psiloceratids. 

Its base is taken to mark the base of the 

Jurassic System in the eastern Tethys. 

2008010192 

英格兰中侏罗世巴通期一牡蛎生长速率和 

形态的变化及其环境指示意义 = Variation 

in growth-rate and form of a Bathonian (Middle 

Jurassic) oyster in England, and its environmental 

implications. ( 英文 ). Johnson A; 

Liquorish M N; Sha Jingeng. Palaeontology, 

2007, 50(5): 1155-1173 

We review controls on extensional growth 

rate and shell thickness in the extant oyster 

Crassostrea. Data on these shell parameters 

for the ecologically similar Bathonian oyster 

Praeexogyra hebridica, sampled at carefully 

selected sites, are then used to test a hypothesis 

that small size in contemporaneous marine 

bivalves of north-west Europe was the product 

of reduced salinity. The hypothesis is refuted, 

at least to the extent that some additional factor 

must be involved. The relatively low extensional 

growth rate and shell thickness at the 

highest-salinity site, together with the elongate 

(‘etiolated’) shape there and the low extensional 

growth rate at all sites in comparison 

with Crassostrea, suggests that this factor is 

reduced primary productivity. Other faunal, 

sedimentological and diagenetic evidence is 

consistent with low productivity. We point to 

other possible instances of reduced productivity 

during the Middle Jurassic and discuss the 

possible role of this factor in encouraging the 

widespread colonization of brackish-water 

environments by bivalves in the Bathonian 

Stage. 

2008010193 

软舌螺侧面刺状突起 helens 的骨骼显微结 

构 = Skeletal microstructure of helens, lateral 

spines of hyolithids. ( 英文 ). Mus M M; 

Bergström J. Palaeontology, 2007, 50(5): 

1231-1243 

In hyolithids the skeleton consists of four 

elements: a conch, an operculum and a pair of 

long, logarithmically curved ‘spines’ called 

helens. These last elements are rarely preserved, 

and have therefore remained poorly 

known and enigmatic. We have studied threedimensionally 

preserved helens of the species 

‘Hyolithes’ lanceolatus, from the Permian of 

New South Wales, Australia, and ‘Hyolithes’ 

groenwalli, from the Cambrian of Bornholm, 

Denmark. Helens were massive calcareous 

elements. Their original microstructure, herein 

reported for the first time, consisted of concentric 

lamellae surrounding a narrow elongated 

core, which may have been rich in organic 

matter. This concentric pattern resulted 

from the successive accretion of shell material 

at the proximal, internal portion of helens. 

This growth model is in accordance with helen 

morphology and with the presence of a characteristic 

surface sculpture of overlapping lamellae. 

2008010194 

福建深沪湾晚更新世古牡蛎滩的发育与留 

存古环境 = The distribution and age feature 

of Late Pleistocene palaeo-oyster shell beach 

and the palaeo-environment of the oyster 

shells remained in Shenhuwan bay, Fujian 

Province. ( 中文 ). 徐起浩 . 海洋科学 , 2002, 

26(4): 58-62 

福建深沪湾晚更新世古牡蛎以牡蛎原 

生、分布原积大 , 年龄主要在 25 800±2 

490aB.P~15 460±420 aB.P 之间为其主要特 

征 , 在牡蛎生长期间 , 深沪湾地壳抬升速 

率与水动型海平面上升速率相当 , 深沪湾 

海水深度稳度 , 海岸环境稳定 , 古牡蛎繁 

盛生长 , 其后深沪湾地壳抬升成陆 , 古牡 

蛎滩脱离海水成为牡蛎滩台地 , 距今 7 

000a 和距今 2 000a 的两次强古地震 , 使古 

牡蛎滩速下沉到潮下带和潮间带海底 , 这 

是深沪湾晚更新世古牡蛎滩能留存到今天 

的重要原因。 

2008010195 

印度库奇中侏罗世巴通期新的菊石组合 = 

New Bathonian (Middle Jurassic) ammonite 

assemblages from Kutch, India. ( 英文 ). Roy P; 

Bardhan S; Mitra A; Jana S K. Journal of 

Asian Earth Sciences, 2007, 30(5-6): 629-651 

The Bathonian ammonite assemblages have 

been previously poorly recorded in Kutch. The 

present study has unearthed a rich array of 

ammonite taxa ranging from the Middle to 

Upper Bathonian. While Oxycerites Rollier 

(1909) is a new record from Kutch, the oldest 

occurrence of Choffatia Siemiradzki (1898) 

has been found from the Middle Bathonian 

53

horizon. Oxycerites cf. orbis (Giebel) is a 

zonal index of the Late Bathonian in other 

areas and thus facilitates interprovincial correlation. 

Besides, palaeobiogeographic and 

stratigraphic distribution of many species have 

been modified based on new information. For 

example, macrocephalitin species, i.e., Kamptokephalites 

cf. etheridgei Spath (1928), Macrocephalites 

bifurcatus transient intermedius 

Spath (1928), M. cf. mantataranus Boehm 

(1912) were previously known from West Pacific, 

Indonesia have been now found in Kutch. 

Gracilisphinctes Buckman (1920) has been 

previously known to occur during the Middle 

Bathonian time, the present work extends its 

stratigraphic distribution up to the definite 

Upper Bathonian horizon. Procerites hians 

(Waagen) an endemic species in Kutch previously 

known from the Upper Bathonian beds, 

its stratigraphic range has been extended down 

to the Middle Bathonian. Detail taxonomy of 

the newly obtained taxa has been done and in 

many cases sexual dimorphism has been recognized. 

2008010196 

印度西部库奇提塘期腹足类 Obornella 属 

一新种 = Record of a new species of Obornella 

Cox 1959 (Gastropoda) from the Tithonian 

of Kutch, western India. ( 英文 ). Das S S. 

Journal of Asian Earth Sciences, 2007, 30(2): 

207-212 

Obornella Cox 1959, is an extremely depressed 

genus of the family Pleurotomariidae. 

It first appeared during Toarcian in France and 

continued up to the Tithonian. Obornella is a 

Tethyan genus restricted only to western 

Europe except previous reports of migration 

of a species to Kutch during the Late Bathonian. 

The present find describes a new species 

of Obornella, i.e., Obornella lakhaparensis 

from immediately below the Jurassic– 

Cretaceous boundary in Kutch. The present 

species is quite distinct from other Obornella 

species and has many novelties. A detailed 

systematic description is provided. 

2008010197 

青藏高原东部 Changtai-Gacun 地区晚三叠 

世双壳类 Pergamidiidae 科一新属 = A new 

genus of Pergamidiidae (Bivalvia) from the 

Late Triassic of the Changtai-Gacun area, 

eastern Qinghai-Xizang Plateau, China. ( 英 

文 ). Lin Li; Zhu Lidong; Pang Yancun; Sha 

Jingeng. Journal of Asian Earth Sciences, 

2007, 30(1): 108-112 

The new epi-byssate bivalve Parapergamidia 

changtaiensis gen. et sp. nov. of the 

family Pergamidiidae occurs in the Upper Triassic 

( Late Carnian–Early Norian) Tumugou 

Formation of the Changtai-Gacun area, eastern 

Qinghai-Xizang Plateau, China. During 

the Late Triassic, this area was an intra-arc rift 

of the Yidun Island Arc along the eastern 

margin of the Tethyan seaway. The new taxon 

has a big byssal gape, prominent byssal retractor 

muscle scars, and anteriorly oblique and 

posteriorly to posteroventrally elongated 

shape. The thin shell is distinctly longer than 

high. 

2008010198 

奥地利阿尔卑斯晚三叠世内壳亚纲头足类 

Phragmoteuthis 属与壳体共同保存的外套 

膜、墨囊、墨汁、碗钩和软体碎屑 = The 

mantle, ink sac, ink, arm hooks and soft body 

debris associated with the shells in Late Triassic 

coleoid cephalopod Phragmoteuthis from 

the Austrian Alps. ( 英文 ). Doguzhaeva L A; 

Summesberger H; Mutvei H; Brandstaetter F. 

palaeoworld, 2007, 16(4): 272-284 

Fragmentarily preserved shells – mainly 

pro-ostraca, in several cases also phragmocones 

– occurring together with arm hooks 

and the ink sac of the Carnian (Late Triassic) 

coleoid cephalopod Phragmoteuthis bisinuata 

(Bronn) from Lunz (Austria) are examined 

with the scanning electron microscope and 

energy-dispersive spectrometer. The proostracum 

bears black, shiny, pitch-like sheets. 

The black sheets, the ink sac content and the 

arm hooks have a granular ultrastructure of 

0.1–1 μm grain size. The arm hooks and black 

sheets are micro-laminated; each lamina consists 

of fibres. The ink consists of an agglomerate 

of grains. On the ventral (internal) side 

of the pro-ostracum, the black sheets occasionally 

bear agglomerates of homogeneous, 

ink-like material along with heterogeneous 

structures. The pro-ostracum has crystalshaped 

units with lamello-columnar ultrastructure 

of the inner layer and plate ultrastructure 

of the outer layer. This resembles the Late 

Triassic Lunzoteuthis [Doguzhaeva, L.A., 

Mutvei, H., Summesberger, H., 2005a. A Late 

Triassic coleoid from the Austrian Alps: the 

pro-ostracum viewpoint. In: Kostak, M., 

Marek, J. (Eds.), Proceedings of the 2nd International 

Symposium on Coleoid Cephalopods 

Through Time. Short Papers/Abstracts Vol. 

Prague, 26–29 September, 2005, pp. 55–59] 

and Early Jurassic Belemnotheutis [Doguzhaeva, 

L.A., Donovan, D.T., Mutvei, H., 

54

2005b. The rostrum, conotheca and proostracum 

in the Jurassic coleoid Belemnotheutis 

Pearce from Wiltshire, England. In: 

Kostak, M., Marek, J. (Eds.), Proceedings of 

the 2nd International Symposium on Coleoid 

Cephalopods Through Time. Short Papers/Abstracts 

Vol. Prague, 26–29 September, 

2005, pp. 45–49]. The black sheets, the material 

on their inner surface, the ink and the arm 

hooks consist of carbon, occasionally with 

minor amounts of sulfur. The shell is of calcium 

carbonate. Based on their organic composition, 

position in the shell and lamellofibrillar 

ultrastructure, the black sheets are 

considered to be remains of the mantle, sometimes 

with ink sac and soft body debris. The 

carbon composition and granular ultrastructure 

of arm hooks, ink, and soft tissue remains 

indicate that the non-mineralized structures 

are pseudomorphosed by carbon (carbonization), 

possibly due to C-accumulating bacteria. 

2008010199 

阿拉斯菊石群的新材料 = New information 

on Araxoceratidae Ruzhencev. ( 中文 ). 马俊文 . 

煤田地质与勘探 , 2002, 30(1): 7-13 1 图版 . 

描述的菊石产自江西宜春、安福两地 , 

计有 1 新科、5 新属、8 新种和一个未定 

种。根据花桥菊石科 ( 新科 ) 和宜春菊石 

属 ( 新属 ), 阐述了菊石的演化 , 并对国 

际地层对比作了探讨。 

2008010200 

江西乐平煤系外胄菊石科的新发现 = New 

discovery on Episageceratidae Ruzhencev in 

Leping coal bearing strate, Jiangxi. ( 中文 ). 马 

俊文 . 煤田地质与勘探 , 2002, 30(3): 9-12 1 

图版 . 

描述的菊石标本采自江西安福乐平系 , 

计有 2 新属、2 新种和 1 个未定种。根据这 

些资料对晚二叠世早期华南海域的生态环 

境作了初步探讨。 

2008010201 

南海永暑礁泻湖 1 680 年来微型腹足类丰 

度变化的环境意义 = Environmental implication 

of microgastropod abundance variation in 

the Yongshujiao reef lagoon, South China Sea 

during the last 1 680 years. ( 中文 ). 冯伟民 . 微 

体古生物学报 , 2001, 18(1): 43-47 1 图版 . 

永暑礁南永 3 井记录了近 1 680 年来礁泻 

湖腹足类遗壳的沉积变化 , 其中腹足类丰度 

变化尤为显著 , 存在三个高丰度区和相间的 

三个低丰度区。全样单一的粉砂沉积 , 表明 

丰度的变化与底质类型无关 , 而高分异度显 

示了一部分腹足类遗壳为水动力搬运的结 

果。腹足类丰度与沉积速率的对比表明 , 高 

沉积速率和低沉积速率以及波动的沉积环 

境均不利于腹足类的发展 , 而适中的沉积速 

率和稳定的沉积环境将是腹足类发展的有 

利因素。发现环境的变化大约以 400 - 600 

年为周期。1 459- 1 680 年间为环境动荡期 , 

腹足类为低丰度 ;1 081- 1 459 年间为环境稳 

定期 , 腹足类丰度高 ;559- 1 081 年间为沉积 

速率急剧变化期 , 腹足类为低丰度 ;1- 559 年 

间沉积速率非常稳定 , 腹足类十分发育。 

节肢动物 

2008010202 

深海介形虫组合对晚白垩纪古海洋变化的 

回应 : 南部海洋 ODP 点位 689 = Response of 

deep-sea ostracod assemblages to Late Cretaceous 

palaeoceanographical changes: ODP 

Site 689 in the Southern Ocean. ( 英文 ). Majoran 

S; Widmark J G V. Cretaceous Research, 

1998, 19(6): 843-872 

Twenty-six deep-sea ostracod species are 

described from the late Campanian to late 

Maastrichtian of ODP Site 689 in the Southern 

Ocean. Three are described as new: Cytherelloidea 

megaspirocostata, Agulhasina sudoceanica 

and Pennyella foveolata. Correspondence 

analysis identified three faunal sample 

groups. The first is mainly characterised by A. 

sudoceanica, Kirthe sp. and Cytherellasp. 

This is replaced, first temporarily (betweenc. 

71 and 69 Ma) by a group mainly characterised 

by Argilloecia spp. and C. megaspirocostata, 

possibly a consequence of a shortlived 

global palaeoceanographic event marked 

by increased ventilation and cooling of intermediate 

waters at site 689. It then reappears 

before finally being replaced by a third group 

largely characterised by Eucythere cf. circumcostata, 

P. foveolata and Dutoitella mimica 

Dingle. This final change is coeval with a 

marked increase in the faunal density of ostracods, 

probably owing to an increase in food 

supply. However, the oxygen isotopic records 

of benthonic foraminifera suggests that the 

replacement of the first ostracod group by the 

third is a result of the long term Maastrichtian 

cooling of intermediate waters at high latitudes. 

This replacement is also coeval with a 

gradual change in benthonic foraminiferal 

assemblages at site 689. It is suggested, therefore, 

that Pennyella and Dutoitella had a 

greater potential of adapting to successively 

colder palaeoceanographical conditions than 

55

Agulhasina. The former genera have a cosmopolitan 

deep-sea distribution today 

2008010203 

冀北滦平陆相侏罗 — 白垩系生物地层界线 

及候选层型研究进展 = Advances in the 

study of non-marine Jurassic-Cretaceous biostratigraphi 

cal boundary and candidate stratotype 

in Luanping basin,northern Hebei. ( 中文 ). 

柳永清 ; 庞其清 ; 李佩贤 ; 田树刚 ; 牛绍武 . 地质 

通报 , 2002, 21(3): 176-180 

滦平盆地张家沟侏罗 — 白垩系界线上下 

为连续沉积的滨浅湖 — 半深湖序列 , 介形类 

和叶肢介类化石丰富 , 是中国陆相 J\K 界线理 

想的层型候选剖面。通过晚侏罗世和早白 

垩世介形类、叶肢介生物组合及沉积学与 

成因地层学的综合研究 , 认为陆相侏罗 — 白 

垩系生物地层界线以介形类大个体滦平介 

Luanpingella 的消失、女星介 Cypridea 的出 

现 , 叶肢介 Nestoria 、 Pseudograpta 及 

Keratestheria 等的消失以及 Eosestheria 的始 

现 , 扇三角洲平原或前缘亚相或等同亚、微 

相带的结束为标志。陆相界线层型研究和 

定义异于海相盆地 , 陆相环境生物化石的自 

然缺欠可以通过地层格架建立及沉积亚微 

相序列高精度地划分、对比予以弥补 , 并应 

纳入陆相界线层型的定义中。 

2008010204 

冀北滦平盆地大北沟组叶肢介化石研究新 

进展 = New progress in the study of conchostracon 

fossils from the Dabeigou Formation 

in the Luanping basin,northern Hebei 

Province of China. ( 中文 ). 牛绍武 ; 李佩贤 ; 田 

树刚 ; 柳永清 . 地质通报 , 2002, 21(4): 329- 

338 

系统研究了采自滦平盆地火斗山乡张家 

沟剖面大北沟组 (J 3 d) 的叶肢介化石 4 属 22 

种 ( 包括 11 个新种 )。其中 ,Nestoria 属占绝对 

优势 , 并贯穿整个大北沟组 , 故大北沟组可称 

为 Nestoria 群。在该剖面大北沟组首次发现 

了 Jibeilimnadia 属和 Keratestheria 属 , 分别产 

于该组下部和上部 , 可将 Nestoria 群进一步划 

分为下部 Nestoria-Jibeilimnadi 组合 ( 带 ) 和上 

部 Nestoria-Keratestheria 组合 ( 带 )。另外 , 在 

张家沟剖面大北沟组上部首次发现了中侏 

罗统土城子组中的重要分子 cf. Pseudograpta 

属 , 进一步证明了大北沟组的叶肢介动物 

群与土城子组的叶肢介关系密切 , 具有重要 

的时代意义。 

2008010205 

冀北滦平张家沟大北沟组 — 大店子组介形 

类的发现及生物地层界线研究 = Discovery 

of ostracods in the Dabeigou and Dadianzi 

Formations at Zhangjiagou,Luanping 

County,northern Hebei Province of China and 

new progress in the biostratigraphic boundary 

study. ( 中文 ). 庞其清 ; 李佩贤 ; 田树刚 ; 柳永清 . 

地质通报 , 2002, 21(4): 329-338 2 图版 . 

冀北滦平张家沟大北沟组 — 大店子组的 

剖面连续、沉积序列完整、介形类化石十 

分丰富 , 可分为 :Ⅰ.Luanpin-gella- 

Eoparacypris - Pseudoparacypridopsis, Ⅱ. 

Yanshanina – Cypridea - Rhinocypris 和 Ⅲ. 

Cypridea-Yanshanina-Timiriasevia 3 个组合 

带。Ⅰ 组合带分布在大北沟组 , 显示了晚侏 

罗世晚期的特征 ,Ⅱ、Ⅲ 组合带分布于大店 

子组 ,Cypridea 开始大量出现 , 明显地具有早 

白垩世早期的特征 , 故侏罗 — 白垩系的界线 

应置于第 Ⅰ 组合带与第 Ⅱ 组合带之间 , 即大 

北沟组与大店子组之间。两组间的砾岩和 

砂砾岩在张家沟剖面已相变为砂泥岩互层 , 

其间未找到生物化石的岩层厚度 , 由大店子 

东沟剖面的 56m 至张家沟剖面已减少至仅 

为 9.11m, 张家沟剖面优于井上 — 大店子东 

沟剖面 , 可作为中国北方陆相侏罗 — 白垩系 

的界线层型剖面进行深入研究。 

2008010206 

二叠纪末期集群灭绝后的古生态变化 : 中国 

南部广西省西北部早三叠世介形类 = Palaeoecological 

changes after the end-Permian 

mass extinction: Early Triassic ostracods from 

northwestern Guangxi Province, South China. 

( 英文 ). Crasquin-Soleau S; Galfetti T; Bucher 

H; Brayard A. Rivista Italiana di Paleontologia 


Thirty-seven species belonging to fourteen 

genera are recognized. Seven species are new. 

The Griesbachian assemblage from the basal 

microbial lemestone is well diversified and 

does not suggest any abnormal palaeoenvironmental 

conditions in terms of salinity, temperature 

or oxygen content. Particularly, the 

ostracods are typical of well oxygenated water 

and do not reflect any anoxia. Dienerian and 

Smithian ostracods are evidenced for the first 

time and the assemblages suggest less favourable 

palaeoenviromental condition. Diversity 

and abundance of ostracod assemblages recovered 

from the Spathian on. 

2008010207 

辽西热河生物群箭蜓科昆虫新类群 = New 

taxa of Gomphidae (Insecta:Odonata) in Jehol 

Biota from western Liaoning,China. ( 中文 ). 

56

常建平 ; 孙忠实 . 世界地质 , 2006, 25(2): 105- 

112 1 图版 . 

描述了箭蜓科 (Gomphidae) 一新属种 — 宽 

翅辽宁澜箭蜓 (Liaoninglanthus latus gen. et 

sp. nov.) 及新属一未定种 (Liaoninglanthus 

sp.), 还对义县光箭蜓 (Liogomphus yixianensis 

Ren et Gao,1996) 进行了补充描述。化石全 

部采自辽西北票黄半吉沟义县组下部 ( 晚侏 

罗世晚期 — 早白垩世 )。 

2008010208 

松辽盆地三肇地区扶余油层和杨大城子油 

层介形类古生态及沉积环境探讨 = Paleoecology 

and sedimentary environment of 

ostracods in the Fuyu and Yangdachengzi oil 

horizons in the Sanzhao area, Songliao basin. 

( 中文 ). 刘振文 ; 张智礼 ; 王佰长 ; 张铭 . 中国地 

质 , 2006, 33(5): 1159-1166 

笔者较系统地对松辽盆地三肇地区扶余 

油层和杨大城子油层 ( 以下简称扶、杨油层 ) 

介形类的组合特征、分布范围以及古生态 

进行了研究。研究表明 , 扶、杨油层沉积时 

期的介形类自初期少量出现 , 之后发展并繁 

盛 , 末期全部绝灭。这种变化不仅表现为介 

形类动物群的属和种数有较大幅度的增加 , 

而且其壳饰类型、分布范围与壳体保存状 

况也发生了规律性变化 , 但总体上仍为壳饰 

简单、属种类型较多、大小个体混生并生 

活于浅水湖泊环境的介形类群体。对介形 

类的埋葬环境与分布范围的分析表明 , 仅含 

有少量介形类化石碎片的杨五组、杨四组 

的沉积环境为冲积平原环境 , 而含有较丰富 

介形类化石的杨三组 — 扶上组的沉积环境 

则以浅湖环境为主 , 并自杨三组沉积时期在 

该区中部出现大范围的浅水湖泊后 , 随着时 

间的推移 , 湖泊分布范围与水深在缓慢的扩 

大或增加 , 至扶下组沉积时期该湖泊向西已 

扩大至大庆长垣以西 , 从而与齐家 — 古龙地 

区的湖泊连为一体 , 组成统一的松辽古湖 

泊。湖泊水体浅、气候干燥、氧化作用强 , 

可能是造成该时期湖相砂、泥沉积物呈现 

红色的主要原因。 

2008010209 

海生、咸水生介形虫的闭壳肌运动学特征 

及多样化的壳纹饰构成模式 = Kinematics of 

adductor muscle and pattern formation of 

various shell ornamentations in marine and 

brackish water ostracods. ( 英文 ). Tanaka G. 


133 

A new theoretical morphological model is 

introduced to describe various shell ornament 

patterns of cytheroidean ostracods. A wavesource 

model proposed here was designed 

with reference to the kinematics of adductor 

muscles. This model depicts the ornament patterns 

as composite waves that are defined in 

terms of amplitude and frequency of wave 

elements. Computer models successfully mimicked 

most of the ornament patterns seen in 

the Cytheroidea. The theoretical morphospace 

places the multiple-bracket ornamentation as 

an intermediate pattern among concentric, 

radial, and smooth patterns. The result suggests 

that any observed pattern can be readily 

derived from a multiple-bracket one by a 

slight change of developmental parameters. 

2008010210 

日本 Xestoleberis 属新种 (Cytheroidea, 

Ostracoda, Crustacea) 的分类和地理分布 

= Taxonomy and geographical distribution of 

recent Xestoleberis species (Cytheroidea, Ostracoda, 

Crustacea) from Japan. ( 英文 ). Sato T; 

Kamiya T. Paleontological Research, 2007, 

11(2): 183-227 

Thirteen living species of the genus 

Xestoleberis were found from 122 samples 

collected from the coast of Japan. Samples 

were mainly collected from algae, Corallina 

pilulifera and Sargassum thunbergii, in the 

intertidal zone and the uppermost infralittoral 

zone. Seven species are new and are described 

herein; Xestoleberis ikeyai sp. nov., Xestoleberis 

kuroshio sp. nov., Xestoleberis magnoculus 

sp. nov., Xestoleberis notoensis sp. nov., 

Xestoleberis planuventer sp. nov., Xestoleberis 

ryukyuensis sp. nov. and Xestoleberis sesokoensis 

sp. nov. Xestoleberis sagamiensis 

Kajiyama, 1913 is redescribed. The thirteen 

Xestoleberis species studied in this paper are 

subdivided into three groups based on the 

morphology of their carapace pore-systems. 

This grouping is consistent with their estimated 

phylogeny. The grouping is supported 

by general carapace shape, morphology of 

muscle scars, male copulatory organ and “Differentiation 

of Distributional pattern of Poresystems 

(DDP)” analysis, and is considered to 

reflect phylogeny. The geographical distribution 

of Xestoleberis around Japan is shown for 

the first time, and the distinctive distribution 

of species and groups, which correspond to 

marine climates, is clearly recognized. 

2008010211 

山东东营凹陷古近纪介形类优势分异度研 

究 = Study on the dominance diversity of Os- 

57

tracoda of the Paleogene in Dongying Sag of 

Shandong. ( 中文 ). 郑德顺 ; 李守军 . 古地理学 

报 , 2002, 4(2): 64-70 

优势分异度不仅能表明化石群内属种的 

多寡 , 而且能反映各种个数分配是否均 

匀。它对划分生物群落和恢复沉积环境具 

有重要意义。文中讨论了优势分异度的概 

念 , 并选用了信息函数熵 H(s) 作为分异 

度的计算方法 , 分析统计了山东济阳坳陷 

东营凹陷沙三段至沙一段沉积时期的介形 

类分析化验资料 , 并计算了东营凹陷现有 

资料井各时期的分异度值 , 做出了分异度 

等值线图。根据分异度的值及区域内的优 

势种 , 共划分出了各时期的 11 个生物群 

落 , 即 Limnocythere armata ( 具刺湖花 

介 )、Phacocypris huiminensis( 惠民小豆 

介 ),Pseudocandona boxingensis( 博兴假 

玻璃介 ),Camarocypris elliptica( 椭圆拱 

形介 ),Huabeinia unispinata( 单刺华北 

介 ),Camarocypris ovata ( 卵形拱星 

介 ),Huabeinia chinensis ( 中国华北 

介 ),Camarocypris ovata ( 卵形拱星 

介 ),Huabeinia chinensis ( 中国华北 

介 ),Cyprois mina ( 小型拟星介 ), 

Huabeinia obscura( 隐瘤华北介 )。个体古 

生态资料和优势分异度值对生物相划分和 

环境划分起着重要的作用 , 结合生物群落 

划分出了东营凹陷各时期的沉积环境。 

2008010212 

藏南洛扎地区晚侏罗世乃乡组的建立及日 

当组中 Cyclesthriopsis 的发现 = The establishment 

of the Late Jurassic Naixiang Formation 

and the discovery of Cyclesthriopsis in 

the Ridang Formation, Luozha, South Tibet. 

( 中文 ). 夏军 ; 钟华明 ; 童劲松 ; 李运怀 ; 徐生发 ; 

鲁如魁 ; 邱军强 . 安徽地质 , 2001, 11(1): 27- 

29 

在藏南的洛扎 — 江孜一带新发现了一套 

晚侏罗世碎屑岩地层 , 与西侧的维美组及 

东北部的卡东组、桑秀组为同期异相 , 岩 

性差异较大 , 延伸稳定 , 命名为乃乡组。 

在中侏罗世日当组中新发现似圆叶肢介化 

石。 

2008010213 

澳大利亚北部铝土质昆虫蛹壳 = Bauxitic 

insect pupal cases from northern Australia. ( 英 

文 ). Tilley D B; Barrows T T; Zimmerman E 

C. Alcheringa, 1997, 21(1/2): 157-160 

Within the Weipa bauxite deposit of northern 

Queensland, Australia, are rare ovoid 

structures averaging 49 x 30 mm in size and of 

a similar composition to the surrounding 

bauxite. Comprised of a thin shell with an 

opening near one end, these structures encase 

ordinary bauxitic pisoliths and are referred to 

as ovate compound pisoliths. A small proportion 

of them are completely hollow and have 

no apparent opening into their chamber. Similar 

calcareous structures are found along the 

west coast of Eyre Peninsula, South Australia 

These calcareous structures are interpreted to 

have been constructed by the larval stage of 

the weevil Leptopius duponti, for protection 

during pupation. The calcareous structures 

have a similar size and shape to bauxitic pisoliths, 

suggesting that ovate compound pisoliths 

may have been constructed by a similar 

organism, possibly belonging to the genus 

Leptopius. 

2008010214 

阿根廷圣胡安和门多萨前科第勒拉组寒武 

纪三叶虫生物相 . = Cambrian trilobite biofacies 

in the Alojamiento Formation, Precordillera 

of San Juan and Mendoza, Argentina.. ( 其 

他 ). Bordonaro O L; Banchig, A L. 

Ameghiniana, 2007, 44(1): 91-107 

Several Middle - Cambrian trilobite biofacies 

are defined from limestones of the Alojamiento 

Formation in the San Juan and Mendoza, 

Precordillera, Argentina. This study is 

based on the concept of dual biostratigraphy 

that defines biofacies as an informal biotic 

stratigraphic unit of environmental significance 

characterized by associations of higher 

taxa. The Alokistocaridae Biofacies is composed 

of 10 % polymeroids of the Alokistocaridae 

family representing high energy shoal 

- water grainstones - packstones from the cordon 

de Santa Clara (San Juan). The Peronopsis 

Biofacies is composed of similar to 25 % 

of the agnostoid Peronopsis occurring in outer 

platform shallow subtidal packstones - wackestones 

exposed in the quebrada of Aguilera in 

the cordon del Alojamiento (Mendoza). The 

Ptychagnostus Biofacies is defined by similar 

to 30 % of the agnostoid Ptychagnostus found 

in outer - platform deep subtidal mudstones - 

calcipelites cropping out in the Leon Creek, 

cordon del Alojamiento (Mendoza). Both biofacies 

and lithofacies show an East-West 

bathymetric increase from shallow inner - 

platform to deep outer - platform settings. The 

Ehmaniella, Oryctocephalus and Ptychagnostus 

gibbus Zones recognised within each biofacies 

indicate an Early Marjumian age. 

58

2008010215 

北京京西盆地旱白垩世同翅目化石一新属 

( 同翅目 : 蜡蝉总科 ) = New Early Cretaceous 

lalacid from Jingxi Basin of Beijing, 

China (Homoptera: Fulgoroidea). ( 英文 ). 张 

志军 . 动物分类学报 , 2002, 27(1): 20-23 

记述了北京京西盆地早白垩世卢尚坟组 

同翅目一新属新种翅痣白垩蜡蝉 Cretoxixius 

stigmatosus gen. et sp. nov., 化石采自卢尚 

坟组昆虫的典型产地卢尚坟村 , 时代属早 

白垩世巴列姆期 (Barremian Stage), 归卢 

尚坟昆虫群 ; 在分类上属蜡蝉总科拉蜡蝉 

科。模式标本保存于北京林业大学。 

2008010216 

我国侏罗纪脉翅目化石一新属一新种 ( 脉 

翅目 : 蚁蛉总科 ) = A new genus and new 

species of lacewings in the Jurassic of China 

(Neuroptera: Myrmeleontoidea). ( 英文 ). 任东 ; 

尹继才 . 动物分类学报 , 2002, 27(2): 269-273 

描述脉翅目化石一新属一新种 , 精细华 

蛉 Siniphes delicatus gen. et sp. nov., 标本采 

自辽宁省北票市晚侏罗世义县组地层中。 

讨论了华蛉属的科级分类问题。新属可归 

于蚁蛉总科 , 但科级位置不能确定。模式 

标本保存在首都师范大学生物系。 

2008010217 

内蒙古自治区中侏罗世表翼蛉化石一新种 

( 脉翅目 : 翼蛉科 ) = A new Middle Jurassic 

species of Epiosmylus from inner Mongolia, 

China (Neuroptera: Osmylidae). ( 中文 ). 

任东 ; 尹继才 . 动物分类学报 , 2002, 27(2): 

274-277 

描述表翼蛉属化石 1 新种 , 潘氏表翼蛉 

Episomylus panfilovi sp. nov., 讨论了表翼蛉 

属的科级分类问题。标本采自内蒙古自治 

区宁城县山头乡中侏罗世地层中。 

2008010218 

陕西铜川中三叠世中蝎蛉科新化石属种 

( 昆虫纲 : 长翅目 ) = Middle Triassic new 

fossils of Mesopanorpodidae (Insecta: Mecoptera) 

from Tongchuan, Shaanxi province, 

China. ( 英文 ). 洪友崇 ; 郭新荣 ; 王文利 . 动物 

分类学报 , 2002, 27(2): 278-283 

新的中蝎蛉科化石标本采自陕西铜川中 

三叠世铜川组下段上部灰绿色泥页岩中 , 划 

分为 2 属 2 种 , 其中有 1 新属 2 新种 : Erdosia 

pectinata gen. et sp. nov., Mesopanorpodes 

shaanxiensis sp. nov.。这些种类系陕西昆虫 

群 ( 属陕西生物群的一个化石门类 ) 铜川昆 

虫组合的新成员。铜川组的时代相当于欧 

洲拉丁尼期 (LadinianStage)。 

2008010219 

内蒙古宁城中侏罗世九龙山组昆虫群落生 

态的初步研究 = Palaeoecology of insect 

community from Middle Jurassic Jiulongshan 

Formation in Ningcheng County, Inner Mongolia, 

China. ( 中文 ). 谭京晶 ; 任东 . 动物分类 

学报 , 2002, 27(3): 428-434 

对内蒙古自治区宁城县山头乡中侏罗世 

九龙山组中昆虫群落进行了分析 , 共鉴别 

出 3 个昆虫群落 : 水生昆虫群落 Mesobaetis 

sibirica-Yanliaocorixa chinensis、土壤昆虫 

群落 Anthoscytina longa-Palaeontinodes haifanggouensis 

和森林草地昆虫群落 

Rhipidoblattina 

hebeiensis- 

Sinoprophalangopsis reticulata。根据定性和 

定量相结合的方法对各个昆虫群落的物种 

丰度、优势度和分异度等进行了分析。结 

果显示化石产地当时为近岸、浅水的湖泊 

环境 , 气候温暖、潮湿。 

2008010220 

沼泽野蜓雄性化石的首次发现及其脉序变 

异 = First discovery of male Rudiaeschna limnobia 

Ren, 1996 and its venational variability. 

( 中文 ). 李学凤 ; 任东 . 动物分类学报 , 2002, 

27(3): 486-490 

首次描述并图示了沼泽野蜓 Rudiaeschna 

limnobia Ren, 1996 雄性化石 , 讨论了其翅 

脉的变异特征 , 化石采自辽宁省北票市上 

侏罗统义县组地层中。 

2008010221 

古生代动物群取样偏差的影响极其对宏演 

化研究意义 = The effects of sampling bias on 

Palaeozoic faunas and implications for macroevolutionary 

studies. ( 英文 ). Tarver J E; 

Braddy S J; Benton M J. Palaeontology, 2007, 

50(1): 177-184 

Trilobites, a dominant component of marine 

faunas during the Cambrian and Ordovician 

and which survived until the end of the Permian 

(542–251 Ma) have been used in many 

macroevolutionary analyses. Here, we use a 

discovery curve to document the sampling 

history of trilobites, which we consider a 

proxy for Palaeozoic faunas in general. At 

higher taxonomic ranks, orders, suborders and 

superfamilies, the fossil record has been completely 

sampled, while the family rank also 

shows a high level of sampling completeness, 

having reached an asymptote in 1970. Impor- 

59

tantly, this levelling-off occurred even though 

worker effort continued to increase. However, 

at genus level the sampling record is incomplete, 

indicating that families should not be 

used as a proxy for genera. There is little 

variation among the different subsets of generic 

data, with the sampling history of different 

stratigraphic periods and among different 

orders being very similar. However, there is 

noticeable variation among geographical regions, 

caused by variations in worker effort, 

and this could cause problems when comparing 

speciation and diversity patterns across 

faunal provinces. The role of synonyms on 

sampling history has had little effect. 

2008010222 

巴西早白垩世 Crato 组蝎子的高阶分类学 

= Higher systematics of Scorpions from the 

Crato formation, lower Cretaceous of Brazil. 

( 英文 ). Menon F. Palaeontology, 2007, 50(1): 

185–195 

Several new specimens of Protoischnurus 

axelrodorum Carvalho and Lourenço and 

Araripescorpius ligabuei Campos from the 

Crato Formation, Brazil, are described. The 

preservation and recognition of new morphological 

features allows a re-diagnosis of both 

species and a modification of their familial 

placement. Protoischnurus axelrodorum is the 

oldest species belonging to the scorpionoid 

family Hemiscorpiidae Pocock (= Ischnuridae 

Simon; = Liochelidae Fet and Bechly) and the 

first Cretaceous record. It was originally 

placed in the extinct family Protoischnuridae 

Carvalho and Lourenço, which is here synonymized 

with Hemiscorpiidae. Araripescorpius 

ligabuei, now assigned to Chactidae Pocock, 

is the first chactoid recorded for the Cretaceous 

of Brazil. These findings confirm that 

the lineages of two modern families date back 

at least to the Early Cretaceous and, considering 

their current distribution, were probably 

present before the break-up of the supercontinent 

Gondwana. Palaeoecological inferences 

indicate the presence of tropical habitats in the 

vicinity of the Crato lake/lagoon. 

2008010223 

华南板块 Arenig–Llanvirn 期 Asaphoid 三 

叶虫 = Asaphoid Trilobites from the Arenig– 

Llanvirn of the South China plate. ( 英文 ). 

Turvey S T. Palaeontology, 2007, 50(2): 347- 

399 

Twenty-nine Arenig and Llanvirn trilobite 

species, representing 20 genera in the Asaphidae, 

Cyclopygidae, Dikelokephalinidae, 

Nileidae, Raphiophoridae, Remopleurididae, 

Taihungshaniidae and Trinucleidae, are 

treated in a taxonomic review of the South 

Chinese Asaphida. This review is based on 

large collections of trilobite material made 

from five formations at nine localities in western 

Hubei, northern Hunan and southern 

Shaanxi, representing a wide range of benthic 

marine environments across the Yangtze Platform 

and Jiangnan Transitional Belt regions of 

the South China Plate. Most South Chinese 

representatives of the Asaphidae are reassigned 

to the Nobiliasaphinae on the basis of 

cranidial and hypostomal characters, and 

taxonomic revisions are given for Liomegalaspides 

and Opsimasaphus pseudodawanicus. 

Taihungshania shui and T. tachengssuensis 

are revised and redescribed, and the establishment 

of lectotypes for these species and T. 

brevica clarifies the status of the type material 

of Taihungshania. Nileus walcotti is revised 

and restricted biogeographically to the South 

China Plate; material from Xinjiang previously 

assigned to this species is reassigned to 

N. sericeus sp. nov. The new raphiophorid 

species Raphioampyx sinankylosus is described. 

Aocaspis, Incaia and Raphioampyx 

are recorded for the first time from South 

China, and the latter two genera are also recorded 

for the first time from the Arenig. 

2008010224 

奥陶纪介形类一种新的性双形 = A new 

kind of sexual dimorphism in Ordovician Ostracodes. 

( 英文 ). Schallreuter R; Hinz- 

Schallreuter I. Palaeontology, 2007, 50(2): 

495-501 

In Ordovician ostracodes (genus Incisua) a 

new kind of sexual dimorphism is described, 

which is the first example among this group 

with males being the heteromorphs. The 

valves of males are larger and less frequent 

than the females, and are characterized by 

having a furrow in the ventral part. The furrow 

may have functioned as a device to enable the 

two sexes to cling together during mating. 

2008010225 

西班牙早白垩世 Coptoclavid 甲虫 ( 鞘翅 

目 : 肉食亚目 ): 一种新的甲虫取食策略 

= Coptoclavid Beetles (Coleoptera: Adephaga) 

from the lower Cretaceous of Spain: a new 

feeding strategy in Beetles. ( 英文 ). Soriano C; 

Ponomarenko A G; Delclòs X. Palaeontology, 

2007, 50(2): 525–536 

Currently the beetle family Coptoclavidae 

consists of four subfamilies known from the 

60

Upper Triassic–Lower Cretaceous (Aptian). 

We describe two new subfamilies, three new 

genera and five new species from the Las 

Hoyas (Cuenca Province) and El Montsec 

(Lleida Province) localities of Barremian 

(Early Cretaceous) age from Spain: the first 

new subfamily, Hispanoclavinae, is from Las 

Hoyas and comprises one new genus, Hispanoclavina, 

and two new species, 

H. diazromerali and H. gratshevi; the second, 

Coptoclaviscinae, is represented at El Montsec 

by one new species of Coptoclavella 

(C. inexpecta). In addition, at Las Hoyas the 

subfamilies Necronectinae and Coptoclavinae 

are each represented by one new genus and 

species: Ovonectes pilosum and Hoyaclava 

buscalionae, respectively. All beetles previously 

assigned to the family Coptoclavidae 

have been interpreted as active hunters. However, 

we consider Hispanoclavina and Hoyaclava 

to be filter-feeding, with forelegs 

adapted for filtering plankton (probably zooplankton 

because other members of the family 

are carnivorous) on and beneath the water surface. 

This represents a new feeding strategy in 

beetles (extant and extinct). The five new species 

extend the known geographical distribution 

of the Coptoclavidae into the western part 

of European Barremian deposits. The Las 

Hoyas locality now has the highest known 

diversity of coptoclavid species. 

2008010226 

中国一新志留纪板足鲎 ( 节肢动物门 : 螯 

肢动物亚门 ) = A New Silurian Eurypterid 

(Arthropoda: Chelicerata) From China. ( 英文 ). 

Tetlie O E; Selden P A; Ren Dong. Palaeontology, 

2007, 50(3): 619–625 

The oldest eurypterid from China is described 

as Hughmilleria wangi sp. nov., from 

the Xiaoxiyu Formation (Silurian: latest 

Llandovery) of Hunan Province. H. wangi is 

relatively similar to two species from North 

America, but differs in the development of 

epimera on the postabdomen, a slightly wider 

carapace, a styliform telson and the dimensions 

of the penultimate podomere of the paddle. 

The Llandovery age of the specimen substantially 

reduces the ghost range of the genus 

Hughmilleria. The exact phylogenetic relationship 

between the different species in 

Hughmilleria, the most basal genus in the 

pterygotoid clade, cannot be resolved because 

the plesiomorphic states within this clade are 

poorly known. The shapes of the telson and 

swimming paddle of the Chinese species suggest 

that it is more primitive than its North 

American relatives, which is in accord with its 

greater age. 

2008010227 

加拿大英属哥伦比亚省中寒武世布尔吉斯 

页岩中 Leanchoilia 属 ( 节肢动物门 , 蛛形 

亚门 ) 的重新评价 = Reassessment of the 

genus Leanchoilia (Arthropoda, Arachnomorpha) 

from The Middle Cambrian Burgess 

Shale, British Columbia, Canada. ( 英文 ). García-Bellido 

D; Collins D. Palaeontology, 2007, 

50(3): 693-709 

The collection, since 1975, of over 1500 

specimens of Leanchoilia Walcott by the 

Royal Ontario Museum has prompted reassessment 

of the genus and its species from the 

Middle Cambrian Burgess Shale. Among new 

characters in Leanchoilia superlata, the type 

species, are the presence of two pairs of eyes, 

a dorsal double carina bracketing the axis of 

the body segments, segmentation of the gill 

branch of the appendages, and serration along 

the body edges from the posterior third of the 

cephalic shield to the last body segment. 

Leanchoilia persephone Simonetta, previously 

synonymized with L. superlata, is also well 

represented in the Burgess Shale, and is reestablished 

as a valid species, owing to conspicuous 

differences from the type species. 

These are the absence of the diagnostic upcurving 

snout of the cephalic shield, the absence 

of carina, the shorter ‘great appendages’, 

the smooth edges of the body, and its overall 

shape in dorsal aspect. Leanchoilia superlata 

and L. persephone may be sexual dimorphs of 

each other. The ROM collections extend considerably 

the geographical distribution and 

stratigraphic range of Leanchoilia in western 

Canada. 

2008010228 

加拿大新不伦瑞克省早泥盆世 Atholville 

Campbellton 组 Pterygotus Anglicus Agassiz 

( 螯肢动物亚门 : 板足鲎亚纲 ) = 

Pterygotus Anglicus Agassiz (Chelicerata: 

Eurypterida) From Atholville, Lower Devonian 

Campbellton Formation, New Brunswick, 

Canada. ( 英文 ). Miller R F. Palaeontology, 

2007, 50(4): 981–999 

Specimens of the large eurypterid Pterygotus 

from the Early Devonian Campbellton 

Formation outcropping at Atholville, New 

Brunswick, are identified as Pterygotus anglicus 

Agassiz. The locality, in the Atholville 

beds near the western end of the Campbellton 

Formation exposure, is best known for its ver- 

61

tebrate fauna of ostracoderms, arthrodires, 

acanthodians and chondrichthyans, first described 

in 1881. Although a significant series 

of pterygotid fossils was acquired by the Natural 

History Museum, London, in 1892, it received 

little attention. A few small specimens 

from the Geological Survey of Canada collections 

were named Pterygotus atlanticus by 

Clarke and Ruedemann, considered here to be 

an invalid taxon. They suggested that 

P. atlanticus might turn out to be a small 

specimen of P. anglicus. The new material 

described here, including one relatively complete 

individual, confirms their suspicions and 

provides evidence of Pterygotus anglicus in 

the Lower Devonian of North America. 

2008010229 

美国蒙大拿州 Bear Gulch 灰岩中一石炭纪 

Synziphosurine( 剑尾目 ) = A Carboniferous 

Synziphosurine (Xiphosura) From The 

Bear Gulch Limestone, Montana, USA. ( 英 

文 ). Moore R A; McKenzie S C; Lieberman B 

S. Palaeontology, 2007, 50(4): 1013-1019 

A new synziphosurine, Anderella parva gen. 

et sp. nov., extends the known range of this 

group from the Silurian to the Carboniferous 

and is the youngest known so far from the 

fossil record. Previously the youngest synziphosurine, 

Kasibelinurus, was from the Devonian 

of North America. Anderella parva has 

a semi-oval carapace with pointed genal regions, 

nine freely articulating opisthosomal 

segments and a long styliform tail spine. It is 

the third xiphosuran genus to be described 

from the Bear Gulch Limestone and its discovery 

highlights this deposit as containing an 

unusually diverse xiphosuran biota. It is also 

the only known locality where synziphosurines 

occur alongside the more derived xiphosurids. 

Xiphosurans reached their greatest diversity 

in the Carboniferous when the xiphosurids 

began to occupy brackish and freshwater 

habitats and became dominant over the 

synziphosurines. The discovery of the only 

known Carboniferous synziphosurine in marine 

sediments may indicate their inability to 

exploit these same environments. 

2008010230 

三叶虫聚合眼中富集镁元素的透镜体间结 

构 = Magnesium-Rich Intralensar Structures 

in Schizochroal Trilobite Eyes. ( 英文 ). Lee M 

R; Torney C; Owen A W. Palaeontology, 

2007, 50(5): 1031-1037 

The interpretation of the lenses of 

schizochroal trilobite eyes as aplanatic doublets 

by Clarkson and Levi-Setti over 30 years 

ago has been widely accepted. However, the 

means of achieving a difference in refractive 

index across the interface between the two 

parts of each lens to overcome spherical aberration 

has remained a matter of speculation 

and lately it has been argued that the doublet 

structure itself is no more than a diagenetic 

artefact. Recent advances in technologies for 

imaging, chemical analysis and crystallographic 

characterization of minerals at high 

spatial resolutions have enabled a reexamination 

of the structure of calcite lenses 

at an unprecedented level of detail. The lenses 

in the eyes of the specimen of Dalmanites sp. 

used in the original formulation of the 

aplanatic doublet hypothesis are shown to 

have undergone diagenetic alteration, but its 

products reflect original differences in mineral 

chemistry between the upper lens unit and 

lower intralensar bowl. The turbidity of the 

bowl and of the core within the upper part of 

the lens are the result of their greater microporosity 

and abundance of microdolomite inclusions, 

both of which were products of 

diagenetic replacement of original magnesian 

calcite in these areas. Such a difference in 

magnesium concentration in the original calcite 

has long been postulated as one of the 

ways by which the interface between these 

lens units could have produced an aberrationfree 

image and the present study provides the 

first direct evidence of such a chemical contrast, 

thus confirming the doublet hypothesis. 

2008010231 

西藏西南部 Gyanyima 剖面乐平阶和二叠 

纪 - 三叠纪界线的介形类 = Ostracods from 

the Lopingian and Permian–Triassic boundary 

beds at the Gyanyima section in southwestern 

Tibet, China. ( 英文 ). Crasquin-SoleauS; Shen 

Shu-Zhong; Li Wen-Zhong ; Cao Chang-Qun. 

palaeoworld, 2007, 16(1-3): 222-232 

Ostracods are reported for the first time in 

the Late Permian Lopingian to earliest Triassic 

carbonate sequence in the Ngari region, 

southwestern Tibet, China. Fifty-three species 

are recognized, of which 19 are illustrated. 

One new species (Carinaknightina tibetensis n. 

sp.) is described and one species is renamed 

(Bairdia wangi n. nom.). The ostracod fauna 

as a whole is very similar to those in the Palaeo-Tethys 

and characteristic of warm water 

platform deposits. The Early Triassic ostracod 

assemblages in the section show no substantial 

62

difference from the Lopingian assemblages. 

The palaeoenvironments of the Late Permian 

and earliest Triassic appear to be open marine 

with normal salinity and oxygen concentration; 

there are no indications of anoxic conditions 

in the Early Triassic in the studied area. 

2008010232 

中国中生代昆虫化石研究新进展 = Progress 

in the study of Mesozoic fossil insects during 

the last decade in China. ( 中文 ). 任东 . 昆虫学 

报 , 2002, 45(2): 234-240 

回顾了 1990 年以来中国中生代昆虫化石 

研究的新进展 , 简述了我国学者在古昆虫 

分类学、昆虫内部形态学、昆虫系统学、 

古生态学、昆虫生物地层学、昆虫区系的 

历史演变、生物古地理学、昆虫与植物的 

关系等 8 个方面取得的突出贡献 , 并给出 

了我国发现的世界最低层位昆虫科级类群 

表。 

2008010233 

寒武纪最上部三叶虫 Missisquoia, 属的幼年 

期兼论这个属队科以上单元的分类意义 = 

Protaspides of uppermost Cambrian trilobite 

Missisquoia, with implications for suprafamilial 

level classification of the genus. ( 英文 ). 

Lee Dong-Chan; Chatterton B D E. Canadian 

Journal of Earth Sciences, 2007, 44(4): 493- 

506 

The protaspides of Missisquoia depressa 

(Missisquoiidae, Trilobita), from the uppermost 

Cambrian part of the Rabbitkettle Formation, 

Mackenzie Mountains, northwestern 

Canada, are described. Three metaprotaspid 

stages are recognized, using size as well as 

features of the anterior border of the 

cranidium and the shape of the glabella. The 

morphology of the protaspides is not typical of 

the Order Corynexochida, suggesting that 

Missisquoia is not a member of the order to 

which the genus has been previously assigned. 

This further indicates that its affinity to the 

stratigraphically younger styginids and illaenids 

is questionable. 

Une description des protaspides de Missisquoia 

depressa (Missisquoiidae, Trilobita), 

du Cambrien supérieur de la Formation de 

Rabbitkettle, des monts Mackenzie (Nord- 

Ouest canadien), est présentée. Les dimensions 

ainsi que les caractéristiques de la bordure 

antérieure du cranidium et la forme de la 

glabelle permettent de distinguer trois stades 

de métaprotaspides. La morphologie des protaspides 

n'est pas typique de l'ordre des 

Corynexochida, ce qui laisse croire que Missisquoia 

n'appartient pas à l'ordre auquel ce 

genre avait antérieurement été affecté. Cela 

jette en retour un doute sur son affinité avec 

les styginides et les illaenides stratigraphiquement 

plus jeunes 

2008010234 

辽西义县组细蜂总科 ( 昆虫纲 , 膜翅目 ) 昆虫 

化石 ( 英文 ) = Proctotrupoid wasps (insecta, 

hymenoptera) from the Yixian Formation of 

western Liaoning Province. ( 英文 ). 张海春 ; 张 

俊峰 . 微体古生物学报 , 2001, 18(1): 11-28 3 

图版 . 

描述了产自辽宁北票上园地区黄半吉沟 

上侏罗统义县组下部细蜂总科 (Proctotrupoidea) 

昆虫化石 10 属 12 种 , 其中 8 新属 12 

新种。这些化石分属于 3 科 , 其中 Gurvanotrupes 

stolidus sp. nov., Gurvanotrupes 

exiguus sp. nov., Liaoserphus perrarus gen. et 

sp. nov., Alloserphus saxosus gen. et sp. nov., 

Scalprogaster fossilis gen. et sp. nov., Steleoserphus 

beipiaoensis gen. et sp. nov., Saucrotrupes 

decorosus gen. et sp. nov. 和 Ocnoserphus 

sculptus gen. et sp. nov. 归入细蜂科 

(Serphidae=Proctotrupidae) ;Protocyrtus 

validus sp. nov. 和 Spherogaster coronata gen. 

et sp. nov. 归入柄腹细蜂科 (Heloridae) 

;Liaoropronia leonina gen. et sp. Nov. 和 

Liaoropronia regia gen. et sp. Nov. 归入窄腹 

细蜂科 (Roproniidae)。对我国中生代细蜂总 

科化石的研究状况作了回顾。 

2008010235 

Junonia(Nymphalidae: Nymphalinae) 蝴蝶 

的非洲外起源及调和分布分异度 = Out-of- 

Africa origin and dispersal-mediated diversification 

of the butterfly genus Junonia (Nymphalidae: 

Nymphalinae). ( 英文 ). Kodandaramaiah 

U; Wahlberg N. Journal of Evolutionary 

Biology, 2007, 20(6): 2181–2191 

The relative importance of dispersal and 

vicariance in the diversification of taxa has 

been much debated. Within butterflies, a few 

studies published so far have demonstrated 

vicariant patterns at the global level. We 

studied the historical biogeography of the 

genus Junonia (Nymphalidae: Nymphalinae) 

at the intercontinental level based on a 

molecular phylogeny. The genus is distributed 

over all major biogeographical regions of the 

world except the Palaearctic. We found 

dispersal to be the dominant process in the 

diversification of the genus. The genus 

originated and started diversifying in Africa 

63

about 20 Ma and soon after dispersed into 

Asia possibly through the Arabian Peninsula. 

From Asia, there were dispersals into Africa 

and Australasia, all around 5 Ma. The origin 

of the New World species is ambiguous; the 

ancestral may have dispersed from Asia via 

the Beringian Strait or from Africa over the 

Atlantic, about 3 Ma. We found no evidence 

for vicariance at the intercontinental scale. We 

argue that dispersal is as important as 

vicariance, if not more, in the global 

diversification of butterflies. 

2008010236 

山东东营盆地早第三纪介形虫壳体微量元 

素的特征及意义 = Characteristics of trace 

elements in Paleogene ostracod shells from 

the Dongying Basin and their significance. ( 中 

文 ). 刘传联 ; 赵泉鸿 . 微体古生物学报 , 2001, 

18(2): 156-162 

通过对山东东营盆地早第三纪生油层中 

介形虫化石壳体进行微量元素分析 , 得出在 

沙河街组一段中、下亚段沉积时期 , 湖水较 

浅、盐度高 , 气候干燥 , 古湖泊营养水平低 ; 

上亚段沉积时期 , 湖水变深、变淡 , 气候凉湿 , 

湖水营养化程度增高。这些结论与沉积 

学、古生物学和稳定同位素研究的结果是 

一致的 , 表明介形虫壳体微量元素化学分析 

对于早第三纪生油层沉积环境的再造能发 

挥重要的作用。 

2008010237 

阿拉斯加北端海岸带的现代介形类与环境 

= Recent Ostracoda and environment in 

coastal zone, the northwest Arctic Alaska. ( 中 

文 ). 李元芳 ; 张青松 ; 王国 . 微体古生物学 

报 , 2001, 18(2): 173-179 1 图版 . 

本文主要对北极阿拉斯加巴罗地区海岸 

带中的现代介形类动物群特征及其生态环 

境进行了探讨 , 其中在盐度为 0.157— 

4.41g/l 的河口和近河口段的河流沉积中发 

现 Elofsonia susitnensis Forester et Brouwers 

和 Cytheromorpha knikensis Forester et 

Brouwers 的活体。据报道 , 这两种介形类活 

体过去见于 59°— 61°N、盐度为 1.112— 

32.5 g/l 的阿拉斯加湾及其沿岸带 , 在白令 

海、波弗特海未见及。作者在纬度更北、 

盐度更低的水域发现它们 , 这对北极介形类 

动物群研究以及控制介形类分布的环境参 

数的研究都提供了新认识。同时根据介形 

类分布特征 , 划分出 4 个介形类生态组合。 

2008010238 

南美 Charipinae: 回顾及两新种的描述 ( 膜 

翅目 : 瘿蜂总科 : 环腹蜂科 ) = South 

American Charipinae: Review and Description 

of Two New Species (Hymenoptera: 

Cynipoidea: Figitidae). ( 英文 ). Pujade-Villar J; 

Diaz N; Evenhuis H H; Ros-Farre P. Annals of 

the Entomological Society of America, 2002, 

95(5): 541-546 

The Charipinae have been little studied in 

the Neotropical region. There are only three 

species in South America and some identifications 

are erroneous. In this work, all the species 

of Charipinae from South America were 

studied and two new species are described: 

Apocharips angelicae Pujade-Villar and 

Evenhuis sp. n. and Alloxysta desantisi Pujade-Villar 

and Díaz sp. n. New synonyms 

also are given. Several unusual morphological 

features of Apocharips angelicae are discussed 

and illustrated. Finally, we argue that 

the genera Bothriocynips and Emargo are 

synonymous. 

棘皮动物 

2008010239 

北非上白垩统海胆纲 Enallopneustes 的修 

订 = Revision of the echinoid Enallopneustes 

from the Upper Cretaceous of North Africa. 

( 英文 ). Jeffery C H. Cretaceous Research, 

1997, 18(2): 237-248 

A re-examination of the type material of the 

atelostomate echinoid Enallopneustes Pomel 

reveals that the type species E. jullieni (Peron 

& Gauthier) represents small specimens of 

Hemipneustes Agassiz. A new genus, Medjesia, 

is erected for E. meslei Gauthier, the only 

other species previously ascribed to Enallopneustes-a 

form with a Hemipneustes-like 

plastron, a marginal fasciole and an ethmophract 

apical system. Full descriptions of both 

these species are presented and details of plastron 

structure are given for the first time. 

2008010240 

德国下泥盆统埃姆斯阶下部 Hunsrück 

Slate 棘皮类海蛇尾纲动物 Brittlestar 一新 

种 = A new species of Brittlestar (Ophiuroidea, 

Echinodermata) from the Hunsrück Slate 

(lower Emsian, lower Devonian) of Germany. 

( 英文 ). Glass A; Poschmann M. Palaeontology, 

2006, 49(5): 969-981 

Lapworthura lehmanni, a new species of 

ophiuroid, is described from four specimens 

from the Lower Devonian Hunsrück Slate of 

Germany. It is the only known ophiuroid in 

the Hunsrück Slate with paired but unfused 

64

ambulacrals, and it exhibits unique rows of 

spine-bearing dorsal arm ossicles. The genus 

Lapworthura Gregory was previously known 

only from the Ordovician of Scotland and the 

Silurian of England and Australia. 

2008010241 

澳大利亚 mitrate 类 Victoriacystis 属的重 

新描述兼评其功能形态 = Redescription of 

the Australian mitrate Victoriacystis with 

comments on its functional morphology. ( 英 

文 ). Ruta M. Alcheringa, 1997, 21(1/2): 81- 

101 

Re-examination of the type material, and 

study of new specimens of the Upper Silurian 

mitrate Victoriacystis wilkinsi Gill & Caster 

from the Heathcote area of Victoria, Australia, 

reveal additional details of its anatomy. Mitrates 

from the Lower Silurian of Hawthorn 

and the Lower Devonian of Kinglake West 

(Victoria Australia) are assigned to V. wilkinsi. 

New morphological features of Victoriacystis 

are: a sculptured median upper lip plate; five 

transverse rows of ventral plates; a complex 

ornament on the internal surface of the anteriormost 

ventral plates; a flexible articulation 

between dorsal and ventral fore-tail plates; 

and the presence of knobs on the ventral hindtail 

plates. Victoriacystis was probably a semiinfaunal 

animal which moved rearward within 

the sediment pulled by its tail. Yawing was 

reduced by the deep lateral head walls. The 

fore-tail could be flexed laterally to a large 

extent, whereas the hind-tail could proably 

also act as a lever. Spines might have helped 

the animal to rest on sediment, to increase 

stability in water currents, and/or to bring food 

particles in suspension. 

2008010242 

不列颠群岛兰多维列世 ( 早志留世 ) 新的 

海百合类动物 ( 棘皮动物 ) = New Crinoids 

(Echinodermata) from the Llandovery (Lower 

Silurian) of the British Isles. ( 英文 ). Fearnhead 

F E; Donovan S K. Palaeontology, 2007, 

50(4): 905-915 

British Llandovery crinoids remain poorly 

known. Three species are documented herein 

that were originally described, but not published, 

by W. H. C. Ramsbottom. Clematocrinus 

ramsbottomi Fearnhead sp. nov. (Tortworth 

Inlier, Gloucestershire; Telychian) has a 

heteromorphic column, N434243414342434, 

radices directed away from the crown, and ten 

long, uniserial arms with a pustular aboral 

sculpture and long, slender pinnules. Clematocrinus 

spp. are widely distributed in the Silurian 

of England. Ptychocrinus mullochillensis 

Fearnhead and Donovan sp. nov. (Girvan 

district, Strathclyde; Rhuddanian) is the second 

report of this Upper Ordovician–Lower 

Silurian genus from outside North America. 

Although incompletely known, this species is 

distinguished by its hidden infrabasals, 20 

arms and sunken interbrachial plates with a 

strongly stellate sculpture. Petalocrinus bifidus 

(Bather MS) Donovan and Fearnhead sp. 

nov. (Woolhope Inlier, Herefordshire; Telychian) 

is locally common enough to give its 

name to a mappable lithostratigraphic unit, the 

Petalocrinus Limestone. Unlike other Petalocrinus 

species known from the Silurian of 

China, northern Europe and North America, 

the fused arms of P. bifidus are divided in two 

by a proximal adoral ridge and an associated 

distal notch. Unlike extant crinoids, Petalocrinus 

probably lived as a rheophobe; the fused 

arms may have acted to deter predators. 

2008010243 

苏格兰 St Andrews 密西西比亚纪维宪期 

Asbian 分支海百合一新属后肠软组织的保 

存 = Soft-tissue preservation of the hind gut in 

a new genus of cladid crinoid from the Mississippian 

(Visean, Asbian) at St Andrews, Scotland. 

( 英文 ). Kammer T W; Ausich W I. Palaeontology, 

2007, 50(4): 951-959 

Soft-tissue preservation of the hind gut, or 

anal sac, in the tegmen of Tubulusocrinus (gen. 

nov.) doliolus (Wright) from the Mississippian 

(Visean, Asbian) Pittenweem Formation at St 

Andrews, Scotland, is the first of its kind 

known in crinoids; it sheds important new 

light on the nature of the cladid tegmen. Many 

cladid crinoids had a calcite-plated anal sac 

that may have functioned like a chimney to 

prevent fouling of the ambulacra. The tubular, 

uncalcified anal sac of Tubulusocrinus may 

have functioned like a hose by pointing down 

current between the arms to avoid fouling of 

the ambulacra. Its smaller size may also have 

required less energy to produce than a heavyplated 

sac. The hind gut is apparently preserved 

by haematite replacement, which was 

probably altered from original authigenic pyrite 

that formed soon after catastrophic burial. 

2008010244 

英格兰和威尔士密西西比亚纪杜内期 

Ivorian 分支海百合和可曲海百合 = New 

cladid and flexible crinoids from the Missis- 

65

sippian (Tournaisian, Ivorian) Of England and 

Wales. ( 英文 ). Kammer T W; Ausich W I. 


The modern study of fossil crinoids began 

with J. S. Miller who, in 1821, described 

specimens from southern England, nearby 

Wales and other regions, and named several 

common Early Carboniferous genera. Later, in 

1950–60, James Wright monographed all 

known Early Carboniferous crinoids from the 

British Isles. In spite of such previous scrutiny, 

we recognize here two new genera among 

species already described: Glamorganocrinus 

gen. nov. (type species: Ophiurocrinus gowerensis 

Wright, 1960) from South Wales and 

Mendipocrinus gen. nov. (type species: Poteriocrinus 

latifrons Austin and Austin, 1847) 

from southern England. These new genera 

increase the number of advanced cladid genera 

in the Ivorian Substage of the Tournaisian 

in western Europe to 18, and the total number 

of crinoid genera to 36. A review of species 

assigned to Mespilocrinus has led to the recognition 

of M. granulifer De Koninck and 

LeHon, 1854 as a nomen dubium. A new species 

of Mespilocrinus, M. wrighti sp. nov., is 

described from the Ivorian of South Wales; 

this is the most highly derived species of the 

genus, as based on a phylogenetic analysis 

including ten species and 13 characters, with 

Pycnosaccus as the outgroup. A single, wellordered 

tree resulted from this analysis. Interpretation 

of this tree suggests that the centre of 

evolution for Mespilocrinus was North America, 

where three species appeared during the 

Kinderhookian (early Tournaisian), rapidly 

achieving morphological disparity within the 

genus. This radiation event was part of the 

overall explosive radiation of crinoids following 

the Late Devonian mass extinction event 

when crinoid diversity was at a global minimum 

during the Frasnian. Recovery began 

during the Famennian, followed by an explosive 

radiation in the Tournaisian. 

2008010245 

英格兰 Wenlock 世海星的分异度 = Starfish 

diversity in the Wenlock Of England. ( 英文 ). 

Herringshaw L G; Thomas A T; Smith M P. 


Although their record extends back to the 

Early Ordovician, the occurrence of fossil 

starfish (Echinodermata: Asteroidea) is dependent 

almost exclusively upon horizons of 

exceptional preservation. Thus, asteroids 

found in Silurian obrution deposits of the English 

Midlands and Welsh Borderlands are particularly 

significant to an understanding of the 

early diversity of the group. Six species are 

described here: Hudsonaster carectum sp. 

nov. (Hudsonasteridae), from the lower part of 

the Lower Elton Formation; and, from the 

Much Wenlock Limestone Formation, the 

hudsonasterids Doliaster brachyactis gen. et 

sp. nov. and Siluraster ketleyi (Spencer, 

1916), the lepidasterids Lepidaster grayi 

Forbes, 1850 and Lepidactis wenlocki Spencer, 

1918, and the palasterinid Palasterina orchilocalia 

sp. nov. Though few in number, 

they show a diverse range of body morphologies 

when compared with Ordovician taxa: 

L. wenlocki had long, slender rays when fully 

grown whereas D. brachyactis is the first asteroid 

with the short-rayed body form of extant 

cushion stars. Most distinctive of all is 

L. grayi, the earliest multiradiate taxon known, 

all complete specimens of which have 13 rays. 

This morphological variety is interpreted as 

indicating that by the Early Silurian starfish 

were exploiting a wide range of feeding habits 

and ecological niches. 

2008010246 

贵州上三叠统瓦窑组海百合化石群的一新 

种 = A new crinoid species from the Wayao 

Formation of Late Triassic in Guizhou Province. 

( 中文 ). 王柏艳 ; 白志强 ; 郝维成 ; 孙元林 ; 

江大勇 . 现代地质 , 2002, 16(3): 231-236 2 图 

版 . 

在贵州省关岭地区三叠统瓦窑组地层中 

发现了保存完好的海百合石群。化石保存 

在瓦窑组近底部的深灰色 - 灰黑色泥质灰岩 

层面上 , 与海百合共生的有菊石双壳类和 

牙形石等海洋生物。海百合石化数量丰 

富 , 保存完好 , 经鉴定分属于创孔海百合 

属 (Traumatocrinus Wohrmann , 1889 

emend. Mu , 1949 ) 的许氏创孔海百合 

(Traumatocrinus hsui Mu,1949), 关岭 

创孔海百合 (Traumatocrinus guanlingensis 

Yu , 2000 ) 和新铺创孔海百合 

(Traumatocrinus xinpuensis sp. nov.)。其 

中 , 新铺创孔海百合 (Traumatocrinus xinpuensis 

sp. nov.) 为一新种 , 该种成年人体 

较大 , 茎板厚度分 5 级 , 各级茎板排列顺 

序为 (1 为一级茎板 ;2 为二级茎板 , 以此 

类推 ):1、5、4、5、3、5、4、5、2、 

5、4、5、3、5、4、5、2、5、4、5、3、 

5、4、5、2、5、4、5、1, 一级茎板数与 

二级茎板数之比为 1/3。第一个粗羽枝分出 

在三级腕的第 3 块腕板上。据其骨骼排列 

66

的精度程度 , 推测该种海百合适合于水动 

力较弱的海洋环境。 

2008010247 

分枝海百合中不完全和全部辐射关节面 = 

Inplenary and explenary radial facets in cladid 

crinoids. ( 英文 ). Webster G D. palaeoworld, 

2007, 16(4): 325-328 

Three types of radial facets have been recognized 

in the cladid crinoids. These are: Angustary—the 

facet occupies less than 70% of 

the width of the distal end of the radial. Peneplenary—the 

facet occupies between 70% and 

99% of the width of the distal end of the radial. 

Plenary—the facet occupies the full width of 

the radial facet.Both the angustary and peneplenary 

radial facets have interradial notches 

between adjacent radial facets along the sutures 

on the distal ends of the radials. The radial 

facets are here referred to as inplenary if 

an interradial notch (here referred to as exinterradial 

notch) is between the distal ends of 

the transverse ridges and the aboral parts of 

the muscle fields are abutting at the suture. If 

the interradial notch is between the muscle 

fields and the distal ends of the transverse 

ridges are abutting, then the radial facet is referred 

to as explenary and the notch as ininterradial. 

The origin of these conditions is uncertain. 

However, they may be an evolutionary 

transition between the peneplenary and plenary 

conditions or they may be a secondary 

response to evolutionary changes in the cup 

structure. The explenary radial facets may 

have resulted in minimal contact of the primibrachials 

when opening, closing, or manipulating 

the arms. It is here proposed that the 

interradial notch be restricted to the condition 

wherein the nonarticular surface extends along 

the suture entirely across the distal end of the 

radial completely separating adjacent radial 

facets. Recognition of the inplenary and explenary 

radial facets should be useful in consistency 

of description, evolutionary studies, 

paleoecologic implications, and classification 

of the cladid crinoids. 

笔石动物 

2008010248 

东昆仑西段祁漫塔格群早志留世笔石化石 

的发现 = Discovery of Early Silurian graptolite 

fossils in the Qimantag Group in the western 

sector of the East Kunlun. ( 中文 ). 黎敦朋 ; 

樊晶 ; 肖爱芳 ; 周小康 ; 李新林 ; 杜少喜 . 地质通 

报 , 2002, 21(3): 136-139 

首次在东昆仑西段祁漫塔格山白干湖地 

区原划奥陶系祁漫塔格群浊积岩下部层位 

中发现 Monoclimacis griestoniensis(Nicol), 

Monograptus priodon (Bronn), Monograptus 

sp., Streptograptus cf. beck (Barrande), 

Torngnigraptus cf. arcuatus(Barrade) 早志留 

世笔石化石组合 , 表明祁漫塔格群除有奥陶 

纪地层外 , 还包含有早志留世地层。 

2008010249 

关于阿根廷门多萨前科迪勒拉晚奥陶世 

Empozada 组 “Rusconi 采集 ” 的笔石的新系 

统分类的认识 = New systematic insights 

about the graptolites of the "Rusconi collection" 

from the Late Ordovician Empozada 

Formation, Precordillera of Mendoza, Argentina. 

( 其他 ). Toro B A; Brussa E D. 

Ameghiniana, 2007, 44(1): 231-240 

The holotypes, paratypes and the best preserved 

material of twenty graptolite taxa proposed 

by Rusconi, and deposited in the "Juan 

Corneho Moyano" Natural and Anthropological 

Sciences Museum of Mendoza were reviewed. 

The fossils, which were collected 

from sedimentary deposits of the Empozada 

Formation that crop out in the San Isidro area, 

located in the Precordillera close to Mendoza 

city, were compared with the specimens collected 

by the authors in the same unit. This 

paper deals with the reasons Why the following 

taxa are invalid: Desmograptus australis 

(Rusconi), Tetragraptus bueyensis (Ruscord), 

Dichograptus quebradensis (Rusconi), Pterograptus 

longissimus (Rusconi), Cryptograptus 

crassispinus (Rusconi), Mendograptus inversus 

(Rusconi), Monograptus bayensis (Rusconi), 

Glyptograptus cuyanensis (Rusconi), 

Glyptograptus cuyunchensis (Rusconi) and 

Janograptus simplicidentatus (Rusconi); in 

addition, reasons for the doubtful classification 

of the following taxa are discussed: Janograptus 

alfaensis (Rusconi), Janograptus 

australis (Rusconi) and Janograptus bueyensis 

(Rusconi). Moreover, the descriptions of 

reassigned taxa such as: Thamnograptus sp., 

Climacograptus tubuliferus Lapworth, 

Orthoretiolites aff. hami Whittington, Hallograptus 

sp. and Plegmatograptus sp. are 

given. Corynoides sp. and Dicellograptus cf. 

minor Toghill are reported and described for 

the first time for the Empozada Formation. 

Finally, new information about the recognized 

graptolite assemblages and their biostratigraphic 

implications is also discussed. 

分类位置不明 

67

2008010250 

中国南方寒武系澄江化石库中古蠕虫类化 

石种 Tylotites petiolaris 的新观察 = New 

observations on the palaeoscolecid worm Tylotites 

petiolaris from the Cambrian Chengjiang 

Lagerstätte, south China. ( 英文 ). Han J; 

Yao Y; Zhang Z; Liu J; Shu D. Paleontological 

Research, 2007, 11(1): 59-69 

The Lower Cambrian Chengjiang Lagerstätte 

provides a remarkable window to enable 

investigation of the early diversification of 

introvert worms. Tylotites petiolaris Luo and 

Hu, 1999 is a very rare animal of the fauna 

originally regarded as a kind of lobopodian 

based on an incomplete specimen, but its affinities 

to recent phyla are still controversial. 

New materials of the taxon collected in recent 

years confirm that it is most closely related to 

the palaeoscolecidians with which it shares 

features such as a proboscis consisting of a 

slightly swollen introvert bearing many scalids, 

a collar (buccal cone) and a spinose pharynx. 

Both possess a smooth neck as a median zone 

between the introvert and the trunk, a pair of 

terminal hooks and a trunk bearing transverse 

ridges intercalated with furrows. Therefore, a 

new order Cricocosmida of the class Palaeoscoecida 

is erected herein based on these 

shared characters. The trunk spines of T. 

petiolaris are somewhat dorso-venrally differentiated 

indicating and epifaunal life on the 

sea floor. Numerous fine transverse wrinkles 

possibly beneath the uppermost cuticle of the 

ventral trunk of the animal are tentatively interpreted 

as the circular muscles, a feature 

crucial to understanding the problematic systematic 

position of the palaeoscolecidians. 

2008010251 

早寒武世叶足动物躯板的发育和分化 = 

Development and diversification of trunk 

plates of the Lower Cambrian Lobopodians. 

( 英文 ). Zhang Xiguang; Aldridge R J. Palaeontology, 

2007, 50(2): 401-415 

Isolated lobopodian plates are reported from 

Early Cambrian strata at five localities in 

southern China. A wide variety of morphologies 

is represented, reflecting a considerable 

diversification within the phylum at this time. 

The new taxon Microdictyon jinshaense is 

erected and new observations are recorded on 

established taxa, based on examination of 

more than 600 well-preserved plates; irregular 

patterns of node distribution and the presence 

of large spines are documented on some taxa 

for the first time. Rare specimens in which 

two plates are conjoined, with a larger plate 

underlying a smaller one, are interpreted as 

showing a new sclerite emerging underneath 

its predecessor, which has not yet been 

moulted. These specimens confirm the process 

of ecdysis in the lobopodians and contribute to 

a fuller understanding of the ontogeny of these 

organisms. A functional hypothesis that suggests 

that the plates were complex visual 

structures is refuted; it is possible that they 

were sites of muscle attachment, but a protective 

role is regarded as more plausible. 

2008010252 

新元古代矿化骨骼的进展 - 来自高家山动物 

群新的化石证据 = The advent of mineralized 

skeletons in Neoproterozoic Metazoa - new 

fossil evidence from the Gaojiashan Fauna. 

( 英文 ). Hua Hong; Zhe Chen; Yuan Xunlai. 

Geological Journal, 2007, 42(3-4): 263-279 

The terminal Neoproterozoic (Ediacaran) 

Dengying Formation in southern Shaanxi, 

China, hosts two types of conical fossils: one 

is the so-called Conotubus, found in siliciclastic 

rocks in the lower and middle part of the 

Gaojiashan Member; the other is the renowned 

Cloudina in carbonate rocks of the 

upper Gaojiashan Member and succeeding 

Beiwan Member. Conotublis are conical and 

gently curved tubular fossils, with a variable 

rate of expansion. They are built of multiple 

thin, steep, eccentrically nested funnels set 

one within the next. A detailed comparison of 

the two conical fossils suggests that the organic 

tubes of Conotubus may be the precursor 

of the mineralized Cloudina tubes; this 

inference is consistent with their similarities in 

both wall structure and life style. Our research 

thus suggests that the organic skeleton preceded 

the rise of the mineralized skeleton in 

Cloudina-like fossils. Sophisticated hypotheses 

have been advocated, some linking the 

skeletal genesis to increasing levels of Ca2+ in 

the seas. others to the enlargement of body 

sizes of animals. Yet our findings have supported 

the 'arms race' hypothesis: skeletons 

evolved primarily through selective predation 

pressure. 

古脊椎动物学 

综论 

2008010253 

现代与与中新世河马的食谱 : 来自碳同位素 

与牙齿珐琅质磨损的证据 = Diets of modern 

and late Miocene hippopotamids: Evidence 

from carbon isotope composition and microwear 

of tooth enamel. ( 英文 ). Boisserie J R; 

68

Zazzo A; Merceron G; Blondel C; Vignaud P; 

Likius A; Mackaye H T; Brunet M. Palaeogeography 

Palaeoclimatology Palaeoecology, 

2005, 221(1-2): 153-174 4 图版 . 

Carbon isotope composition and microwear 

analyses of tooth enamel were used to 

reconstruct the diet of late Miocene hippopotamids 

unearthed in the Toros-Ménalla area, 

Chad, contemporary to the oldest known 

hominids. A large sample of wild modern 

Hippopotamus amphibius from various locations 

in Africa was also analysed for comparison. 

Isotopic analyses showed that the modern 

hippo, reputedly a strict grazer, has a more 

varied diet than usually thought, including a 

significant amount of C 3 plants in closed to 

moderately open environments. Enamel 

formed before weaning was on average 3‰ 

depleted in 13 C compared to post-weaning 

enamel, a pattern that could be partially explained 

by milk consumption. The observed 

micro-wear pattern of the modern hippo differs 

from that of other modern ungulates. We 

explain the very abundant fine scratches and 

small pits found on these hippo teeth by the 

preference for fresh short grasses with low 

silicon content. The diet of the late Miocene 

hippopotamid was probably close to that of 

the modern Hip. amphibius, but included a 

larger amount of C 3 plants. This contradicts 

previous palaeoecological findings based on 

relative hypsodonty degree and indicates that 

the modern feeding behaviour of large hippos 

was already developed at the end of the Miocene, 

when C 4 grass exploitation by large ungulates 

became much more frequent in Africa. 

Finally, it also indicates that C 4 grasses were a 

significant component in late Miocene environments 

of Central Africa. 

2008010254 

纽约州 sewell 地区脊椎动物化石 REE 标 

志 : 对 K-T 界线位置的指示意义 = REE 

signatures in vertebrate fossils from sewell, NJ: 

implications for location of the K-T boundary. 

( 英文 ). Staron R M; Grandstaff B S; Gallagher 

W B; Grandstaff D E. Palaios, 2001, 

16(3): 255–265 

Rare Earth Element (REE) signatures have 

been used to test whether mosasaur bones in a 

basal Hornerstown Formation bonebed (the 

Main Fossiliferous Layer, or MFL) in New 

Jersey were reworked from the underlying 

Maastrichtian beds or deposited synchronously 

with the bones of other taxa in the 

Hornerstown Formation. The interpreted age 

of the bonebed (Maastrichtian vs. Danian) and 

the position of the K-T boundary in New Jersey 

are affected by the possible reworking. 

Statistical techniques, such as ANOVA and 

Discriminant Analysis, show that signatures of 

REE in MFL bones are different from those of 

bones in either the underlying Navesink Formation 

or the upper part of the Hornerstown 

Formation, suggesting a unique depositional 

setting for this bonebed. REE signatures of the 

MFL mosasaur bones conform with signatures 

in bones from other taxa within the MFL, suggesting 

that their deposition was contemporaneous 

with that of the other taxa. Thus, the 

MFL bonebed appears to be Cretaceous in age 

and the K-T boundary must be in or above the 

MFL, within the Hornerstown Formation. 

2008010255 

图库曼国家大学 Miguel Lillo 研究所古脊 

椎动物藏品中的非哺乳犬齿兽类目录及其 

评述 = Catalogue of non-mammalian cynodonts 

in the Vertebrate Paleontology Collection 

of the Institute Miguel Lillo, Universidad 

Nacional de Tucuman, with comments on species. 

( 英文 ). Abdala F. Ameghiniana, 2000, 

37(4): 463-476 

An annotated list of non-mammalian cynodont 

materials in the Vertebrate Paleontology 

Collection of the Institute Miguel Lillo (PVL), 

Universidad Nacional de Tucuman, is presented. 

This is the most important collection 

of South American Triassic tetrapods. The list 

is arranged at the familial level, with information 

on global geographic distribution and systematics. 

In addition, information about taxonomic 

status and synonymy is provided for 

each species represented in the collection. 

2008010256 

新疆水龙兽新材料兼论陆相二叠 - 三叠系界 

线 = The Lystrosaurus fossils from Xinjiang 

and their bearing on the terrestrial Permian- 

Triassic boundary. ( 中文 ). 刘俊 ; 李锦玲 ; 程政 

武 . 古脊椎动物学报 , 2002, 40(4): 267-275 

记述了新疆锅底坑组的两件水龙兽标本 , 

其中产自吉木萨尔县的一件层位最低 , 被鉴 

定为杨氏水龙兽相似种 (Lystrosaurus cf. L. 

youngi)。在支序分析的基础上对比了中国 

与南非的水龙兽 , 认为两地的水龙兽大多数 

分别构成单系类群。总结了中国新疆水龙 

兽在锅底坑组和韭菜园组下部出现的层位 , 

并讨论了以水龙兽来确定陆相二叠 - 三叠系 

界线。 

2008010257 

69

火山活动与辽西四合屯脊椎动物集群死亡 

关系的初步研究 = A study on the relationship 

between volcanic activities and mass 

mortalities of the Jehol vertebrate fauna from 

Sihetun, western Liaoning, China. ( 中文 ). 郭 

正府 ; 汪筱林 . 岩石学报 , 2002, 18(1): 117- 

125 

近年来在辽西北票四合屯发现了大量的 

早期鸟类及 “ 长毛 ” 的小型兽脚类恐龙化石 

层 , 完美的化石形态表明本区发生过多次 

非正常生物集群死亡事件。化石层与火山 

凝灰岩层 ( 或火山灰 ) 密切共生在一起。 

本文选择了其中四个化石数量巨大的脊椎 

动物化石层 , 对其中凝灰岩 ( 或火山灰 ) 

中的火山玻璃及斑晶矿物内原生岩浆包裹 

体的挥发发成分进行了电子探针测定。研 

究结果表明 , 与世界相同成分的其它火山 

相比 , 本区火山出气体的含量较高 ; 火山 

喷出的各种气体 (HCl、HF、H 2 S、SO 2 、 

SO 3 和 H 2 O 蒸汽 ) 的组成比例不同 , 对应着 

化石层内脊椎动物化石组合也存在差异。 

作者认为 , 火山喷出的气体及火山灰 

( 尘 ) 的综合气候效应是造成本区生物集 

群死亡的重要原因。 

鱼类 

2008010258 

墨西哥伊达尔戈州 tula de allende 地区附近 

上新世湖泊沉积物中的 Ictiobus 一新种 = A 

new fossil species of ictiobus(teleostei:catostomidae) 

from pliocene 

lacustrine sediments near tula de allende, Hidalgo, 

Mexico. ( 英文 ). Alvarado-Ortega Jesus; 

Carranza-Castañeda O; Alvarez-Reyes G. 

Journal of Paleontology, 2006, 80(5): 993- 

1008 6 图版 . 

A new fossil Ictiobus species is described, 

based on an abundant collection of wellpreserved 

isolated bones found in lacustrine 

deposits of Pliocene (Blancan) age near Tula 

de Allende, state of Hidalgo, central Mexico. 

This fossil Ictiobus species shows the diagnostic 

character of the genus. In the palatine bone 

the ethmoid process is longer than the premaxillary 

process. Suspensorial pleural ribs with 

trapezoidal shape and a dentary bone with 

extremely short and wide gnathic ramus are 

the characters that support the creation of this 

new Ictiobus species. The fossil record of Ictiobus, 

the first known in Mexico, extends the 

paleogeographical distribution known of this 

genus, which had been previously restricted to 

the USA. 

2008010259 

澳洲肺鱼 steichthyes 的感觉线和吻颅骨 = 

Sensory lines and rostral skull bones in lungfish 

of the family Neoceratodontidae (Osteichthyes 

: Dipnoi). ( 英文 ). Kemp A. Alcheringa, 

1999, 23(3/4): 289-307 

Skull bones in early lungfish contain permanent 

insignia of the sensory lines of the 

head, but osteological evidence of sensory 

lines in derived lungfish is reduced to foramina 

for nerves to neuromasts, superficial 

grooves, or elevated ridges on some bones. 

This is particularly evident in anterior bones, 

making definition of these bones difficult, and 

creating problems for phylogenetic analyses. 

Despite a close association of the sensory lines 

with the bones of the developing skull in the 

Australian lungfish, Neoceratodus forsteri, 

few traces of the lines remain in the bones of 

the adult animal. Among derived dipnoans, 

Mioceratodus, a genus of neoceratodont fossil 

lungfish from Tertiary deposits in central and 

northern Australia, is unusual because traces 

of the supraorbital sensory line are retained in 

the anterior skull roofing bones of large 

specimens. Equivalent traces are absent from 

the rostral bones of N. forsteri, and from small 

specimens of Mioceratodus. 

2008010260 

宁夏中卫纳缪尔期古鳕类化石一新属 = A 

new Namurian Palaeoniscoid fishfrom 

Zhongwei, Ningxia. ( 中文 ). 卢立伍 . 古脊椎 

动物学报 , 2002, 40(1): 1-8 

记述了产于宁夏中卫县石炭纪纳缪尔期 

地层的古鳕类化石一新属新种 — 潘氏黄河 

鳕 (huanghelepis pani gen.et sp.nov.)。新属 

种的个体中等大小 , 体形狭长 , 头长约为体长 

的 1/6 左右。颌悬挂很倾斜 , 具有长而窄的 

梯形鳃盖骨、相对较大的下鳃盖骨。全身 

覆鳞 , 体侧各有一列高度远大于宽度的长方 

形侧线鳞。这是在中国石炭纪地层中古鳕 

类化石的首次描述。 

2008010261 

滇东泥盆系几个含鱼层的时代和对比 = The 

age and correlation of some Devonian fishbearing 

beds of East Yunnan, China. ( 中文 ). 

刘玉海 . 古脊椎动物学报 , 2002, 40(1): 52-69 

从鱼化石的角度对滇东泥盆系下述含鱼 

地层进行了分析 , 并认为 :1) 曲靖地区下泥盆 

统徐家冲组与坡松冲组或四川的平驿铺 

组、广西的那高岭组层位相当 , 时代为布拉 

70

格期 ; 其层位低于含 duyunolepids- 

Kueichowlepis 鱼类组合的贵州乌当组或舒 

家坪组 , 后者时代为埃姆斯期。2) 滇东中泥 

盆统含两个不同时期的含鱼层 , 其中含 

Yinosteus-Wudinolepis 鱼类组合的武定地区 

旧城组属中泥盆统早期 , 该鱼类组合现仅知 

分布于武定地区。而中泥盆统晚期含鱼地 

层 , 在曲靖地区由下而上包括穿洞组、上双 

河组和海口组三个岩石组 ; 其中穿洞组 + 上 

双河组与武定的鱼子甸组对比 , 而海口组与 

曲靖组为同时异相 ; 武定茶花箐组与曲靖组 

对比。3) 文中时上述地层中的某些鱼化石 

的层位或鉴定作了评述或厘定。 

2008010262 

狗鱼 (Esox,Teleostei) 化石在中国的首次发 

现 = First discovery of fossil pike 

(Esox,pisces, Teleostei) from China. ( 中文 ). 

张弥曼 ; 周家健 . 古脊椎动物学报 , 2002, 

40(2): 81-96 

记述了山东龙口黄县洼里煤矿早始新世 

黄县组二段油页岩中的鱼化石。该鱼身体 

狭长 , 背鳍位置靠后 ; 额骨侧面有长形的、狗 

鱼所特有的副筛骨 ; 额骨甚长 ; 顶骨相对来说 

甚短 ; 口裂较长 ; 齿骨、前上颌骨及颚部许多 

骨片均生有扁而尖的牙齿 , 但上颌骨口缘光 

滑 ; 外翼骨甚粗壮 ; 鳃盖骨略呈长方形 ; 前鳃 

盖骨较直 , 中部略收缩 , 上、下枝夹角大 ( 约 

为 130°); 匙骨纵枝短而水平枝长大。困 

此属于狗鱼科中惟一的狗鱼属是毫无疑问 

的。根据其头长与体长之比、额骨及顶骨 

的形状和比例以及背鳍条数目与狗鱼属其 

他种的不同 , 我们将它订为一个新种 —— 龙 

口狗鱼。黄县的化石是狗鱼渐新世以前在 

北美以外地区的首次发现 , 也是狗鱼化石在 

亚洲的首次发现。黄县位于北纬 37°7′, 

远较现生狗鱼在亚洲分布的地区 (43° 和 4 

6° 以北 ) 靠南。而始新世全球气候偏暖 , 巨 

南北温差较小 , 始新世狗鱼或较现生种类更 

适应较温暖的气候。早始新世狗鱼在中国 

的发现为当时跨太平洋鱼类区系的存在提 

供了进一步的证据。 

2008010263 

云南文山早泥盆世盔甲鱼类的新发现 = 

New discovery of galeaspids from Early Devonian 

of Wenshan, southeastern Yunnan, 

China. ( 中文 ). 赵文金 ; 朱敏 ; 贾连涛 . 古脊椎 

动物学报 , 2002, 40(2): 97-113 

描述了采自云南东南部文山地区下泥盆 

统坡松冲组下部的无颌类化石 , 建立了盔甲 

鱼类的一新属、新种 ── 纸厂文山鱼 (W 

enshanaspis zhichangensis gen. et sp. Nov.), 

同时修订了两个盔甲鱼类的旧属、旧种 ── 

长吻三歧鱼 (Sanqiaspis rostrata) 及长角大窗 

鱼 (Macrothyraspis longicornis)。迄今为止 , 

长吻三歧鱼仅在四川江油雁门坝的平驿铺 

组中部发现并记述过 , 长角大窗鱼也仅有一 

件采自云南广南坡松冲组中的正型标本 , 而 

纸厂文山鱼为滇东南文山地区首次记述的 

多鳃鱼类新属种 , 它与滇东北昭通地区下泥 

盆统坡松冲组中的让氏昭通鱼 

(Zhaotongaspis janvieri) 最为相似。此次这 

三个盔甲鱼类属种在滇东南文山地区的发 

现 , 为该区下泥盆统的横向对比提供了重要 

的古鱼类学方面的证据。 

2008010264 

黑龙江密山 — 宝清早泥盆世盾皮鱼类化石 

= The discovery of Eearly Ddevonian placoderms 

from Baoqing and Mishan counties 

of Heilongjiang Province. ( 中文 ). 王俊卿 ; 王 

士涛 . 古脊椎动物学报 , 2002, 40(2): 161-163 

1993 年 , 原地矿部沈阳地质矿产研究所 

苏养正先生将其在黑龙江省东北部密山及 

宝清下黑台组中采到的 5 件泥盆纪鱼化石 

送交王士涛鉴定。经过修理和观察后认 

为 , 这些骨片属于盾皮鱼类 

(Placoderms)。这是迄今为止在东北地槽 

区内首次发现的泥盆纪鱼类化石 , 具有重 

要的生物地层学及古动物地理学意义。 

2008010265 

新疆柯坪志留纪兰多维列世无颌类化石 = 

Agnathans from Llandovery (Silurian) of Kalpin,Xinjiang,China. 

( 中文 ). 王俊卿 ; 王念忠 ; 

张国瑞 ; 王士涛 ; 朱敏 . 古脊椎动物学报 , 2002, 

40(4): 245-256 

描述了新疆柯坪县铁力克瓦铁村附近志 

留纪兰多维列世塔塔埃尔塔格组无颌类盔 

甲鱼亚纲的 3 个新属、新种。无颌类化石 

面貌表明 , 塔塔埃尔塔格组大致与长江中下 

游的溶溪组相当 , 其时代为兰多维列世的特 

列奇期 (Telychian)。塔塔埃尔塔格组时代 

的更正 , 使得塔里木盆地和扬子区中古生代 

地层可直接进行对比。同时 , 两地鱼群性质 

和沉积环境的相似性证明 , 在志留纪时它们 

可能彼此相距很近。 

2008010266 

辽西狼鳍鱼 (Lycoptera) 属一新种 = A new 

species of Lycoptera from Liaoning,China. 

( 中文 ). 张江永 . 古脊椎动物学报 , 2002, 

40(4): 257-266 

71

记述了辽宁阜新县大五家子镇三吉窝铺 

的鱼化石。该鱼具有颞孔 , 前上颌骨小 , 上颌 

骨大 , 辅上颌骨 1 块 , 口缘有一行锥形齿 , 背鳍 

小于臀鳍 ,1 6 根分叉尾鳍条 , 尾下骨 7 块 , 尾 

上骨 1 块 , 尾神经骨 3~4 块。这些特征基本 

上是狼鳍鱼的定义特征 , 因此 , 应该属于狼鳍 

鱼属。阜新标本的第三眶下骨呈半圆形 , 不 

同于狼鳍鱼属各已知种。阜新标本的下颌 

长而低 , 在狼鳍鱼属中 , 只有三棵榆树狼鳍鱼 

和德永氏狼鳍鱼的下颌与之相似。但阜新 

的标本在具有 10 根胸鳍主要鳍条、1 6 根 

尾鳍分叉鳍条以及 1 块尾上骨方面不同于 

三棵榆树狼鳍鱼。与德永氏狼鳍鱼相比 , 阜 

新标本的第三眶下骨小、半圆形、后端不 

伸达前鳃盖骨的前缘 , 辅上颌骨较大 , 身体较 

宽。根据上述阜新标本的特征 , 建立狼鳍鱼 

属一新种 — 阜新狼鳍鱼。 

2008010267 

澳大利亚新南威尔士格伦费尔附近法门期 

Hunter 粉砂岩盾皮鱼纲新的胴甲鱼 = New 

antiarchs (Placodermi) from the Hunter Siltstone 

(Famennian) near Grenfell, NSW. ( 英 

文 ). Johanson Z. Alcheringa, 1997, 21(3/4): 

191-217 

The Hunter Siltstone near Grenfell, New 

South Wales, contains a rich Upper Devonian 

fish fauna including the sinolepid Grenfellaspis 

and the new antiarchs Bothriolepis 

grenfellensis sp. nov. and Remigolepis redcliffensis 

sp. nov. Bothriolepis grenfellensis sp. 

nov. is the first bothriolepid species described 

from N.S.W., and R. redcliffensis sp. nov. is 

the first species of Remigolepis described 

from Australia. Traditionally, the Hunter Siltstone 

was considered to be uppermost Famennian 

or earliest Carboniferous in age based on 

the presence of Grenfellaspis, and the related 

taxon Sinolepis, which is known from the Wutung 

and Sanmentan formations of southeastern 

China. However, available data indicates 

the Hunter Siltstone may be early Famennian 

in age. Ongoing work suggests that all 

Famennian Bothriolepis from N.S.W., including 

B. grenfellensis, possess a trifid preorbital 

recess, but differ in other aspects of headshield 

morphology. In North China, the 

Famennian Zhongning Formation contains six 

species of Remigolepis and a species of Sinolepis. 

However, R. redcliffensis does not 

show any similarity to these species beyond 

those of Remigolepis as a whole. 

2008010268 

宁夏纳缪尔期含鱼地层新知 = A contribution 

to the knowledge of the Namurian in 

Ningxia. ( 中文 ). 卢立伍 ; 方晓思 ; 姬书安 ; 庞其 

清 . 地球学报 - 中国地质科学院院报 , 2002, 

23(2): 165-168 

宁夏石炭纪纳缪尔期地层为海陆交互 

相 , 富含植物、海生无脊椎动物化石。在 

这套地层的上部首次发现了保存完整的鱼 

化石 , 为该套地层划分为对比及沉积环境 

的恢复提供了新的证据。这一鱼群化石在 

中国石炭纪亦是首次发现。初步研究表 

明 , 该鱼群包括古鳕类 (palaeoniscoids) 

和软骨鱼类中的近似于 Listracanthus 化石。 

根据埋藏特征推断 , 这些鱼类的沉积环境 

为近岸滨海 , 但可能非原地沉积。建议在 

宁夏采用土坡组作为岩石地层单位来代表 

本区原 “ 靖远组 ” 和 “ 红土尘组 ” 的地层 , 而 

仅将靖远阶作为年代地层单位。 

2008010269 

内蒙古呼鲁斯太石炭纪脊椎动物化石 = 

Vertebrate remains from the Upper Carboniferous 

of Hulustai, Inner Mongolia. ( 中文 ). 卢 

立伍 ; 靳悦高 ; 方晓思 . 地质科技情报 , 2002, 

21(2): 45-47 

首次记叙了发现于内蒙古阿拉善左旗呼 

鲁斯太地区上石炭统土坡组上部和羊虎沟 

组下部的鱼类鳞片 , 其种类与在宁夏中卫 

纳缪尔期地层中发现的鱼类相似 , 均属古 

鳕类 (Palaeoniscoids); 同时记述了一枚 

产于土坡组上部的脊椎动物牙齿化石。 

2008010270 

苏格兰早石炭世 Cladodus 的颅骨和颌骨 = 

The Braincase and Jaws of Cladodus from the 

lower Carboniferous of Scotland. ( 英文 ). 

Ginter M; Maisey J G. Palaeontology, 2007, 

50(2): 305-322 

The jaws and an allegedly associated orbitotemporal 

region of a shark braincase are 

described from the Lower Carboniferous (Upper 

Viséan, Brigantian Stage, Clackmannan 

Group, Lower Limestone Formation) of Lugton, 

Ayrshire, Scotland. The braincase specimen 

is important because it is associated with 

a tooth of Cladodus elegans Newberry and 

Worthen, 1870, a form considered to be close 

to the type species Cladodus mirabilis Agassiz, 

1843. An occipital fragment, a basicranium 

and a fragment of palatoquadrate from the 

same locality are also described. All the material 

probably represents the same species, and 

it is even possible that some of the material 

came from a single individual. The braincase 

72

esembles those of Cladodoides and Tamiobatis, 

especially in the proportions of its otic 

region, the presence of an extensive dorsum 

sellae, and the arrangement of canals for major 

nerves and blood vessels. The internal 

structure of the occipital region is remarkably 

like that found in Tamiobatis braincases in 

having a prominent subnotochordal septum 

and paired subnotochordal and paroccipital 

chambers. Cladodus is no longer regarded as a 

nomen dubium, since only a few species 

founded on isolated teeth are now retained in 

the re-diagnosed genus, and one of these 

(C. elegans) is now associated with skeletal 

remains. The best systematic placement for 

Cladodus sensu stricto is among the Ctenacanthiformes 

or even the Ctenacanthidae. 

Cladodus may be a synonym of Ctenacanthus, 

but this cannot be confirmed with the available 

material. 

2008010271 

Spitsbergen 早泥盆世 Gigantaspis = The 

genus Gigantaspis heintz, 1962 (Vertebrata, 

Heterostraci) from the lower Devonian of 

Spitsbergen. ( 英文 ). Pernegre V; Goujet D. 


Material collected in 1969 by the CNRS- 

MNHN expedition to Spitsbergen includes a 

new species of Gigantaspis, G. minima, which 

is the smallest known species of this genus. 

The revision of Gigantaspis leads to the inclusion 

of Zascinaspis laticephala Blieck and 

Goujet in this genus. The phylogenetic analysis 

presented herein suggests that Gigantaspis 

is close to Zascinaspis, as suggested by Blieck. 

Moreover, it is also close to generalized representatives 

of the Protaspididae. Their shared 

character states allow the definition of a possible 

ancestral morphotype for the Protaspididae. 

2008010272 

得克萨斯早白垩世阿尔布期 Pawpaw 页岩 

中的 Anacoracid 类 = Anacoracid Sharks 

From The Albian (Lower Cretaceous) Pawpaw 

Shale of Texas. ( 英文 ). Siverson M; 

Lindgren J; Kelley L S. Palaeontology, 2007, 

50(4): 939-950 

Recent collecting from the Pawpaw Shale 

in north-east Texas has yielded several hundred 

teeth of anacoracid sharks. The material 

allows for a much-needed revision of the Late 

Albian anacoracids from North America. The 

previously recognized Squalicorax sp., also 

referred to as S. volgensis in more recent publications, 

is a mix of two different species: 

S. priscoserratus sp. nov. and S. pawpawensis 

sp. nov. In addition to these two new species, 

a single tooth is assigned to S. aff. 

S. baharijensis. Our data indicate that anacoracids 

were a considerably more diverse 

group in the North American Cretaceous than 

previously thought. We attribute much of the 

underestimation of diversity to vague species 

concepts, poor preparation techniques and the 

associated lack of attention to certain dental 

features, in particular neck morphology, root 

surface porosity and the root's vascularization. 

2008010273 

对存疑 Auchenaspis 的综述及其在 

Thyestidian 演化上的作用 = A Review Of 

The Problematic Osteostracan Genus 

Auchenaspis And Its Role In Thyestidian Evolution. 

( 英文 ). Sansom R. Palaeontology, 

2007, 50(4): 1001-1011 

The poorly understood osteostracan genus 

Auchenaspis, from the Upper Silurian of England, 

belongs to the thyestidians (Thyestiida), 

a controversial and important group that is key 

to the understanding of the evolution of the 

Osteostraci and paired pectoral fins. The two 

under-studied species of this genus are comprehensively 

reviewed using anatomical and 

novel statistical approaches. No reliable anatomical 

characters can be used to distinguish 

between the two species, yet discriminant 

analysis finds significant separation with respect 

to size. Potential causes of this conflict 

are discussed. The findings enable 

Auchenaspis to be considered in terms of 

wider thyestidian evolution and contradict 

previous interpretations of the genus as representing 

a paraphyletic taxon, whose morphology 

is intermediate between the general osteostracan 

condition and the highly derived tremataspids. 

2008010274 

西班牙北部比利牛斯山脉南部晚坎潘期及 

早马斯特里赫特期 ( 晚白垩世 ) 的 

Neoselachians = Neoselachians From The 

Upper Campanian And Lower Maastrichtian 

(Upper Cretaceous) Of The Southern Pyrenees, 

Northern Spain. ( 英文 ). Kriwet J; Soler-Gijón 

R; López-Martínez N. Palaeontology, 2007, 

50(5): 1051-1071 

Bulk sampling of upper Campanian to 

lower–middle Maastrichtian coastal and lagoonal 

deposits in five sections of the Tremp 

Formation in the south-central Pyrenees 

yielded numerous neoselachian teeth. The 

fauna comprises nine taxa of which three spe- 

73

cies and one genus are new: Hemiscyllium sp., 

Lamniformes indet., Paratrygonorrhina amblysoda 

gen. et sp. nov., Coupatezia trempina 

sp. nov., Coupatezia sp., Coupatezia sp., 

Rhombodus ibericus sp. nov. and Igdabatis 

indicus. The neoselachian fauna is dominated 

by small nectobenthic rays. This composition 

resembles assemblages known from the marine 

Upper Cretaceous, but differs from 

nearby localities of the Basque-Cantabrian 

region and continental selachian associations 

of the French Pyrenees. The results indicate 

that Rhombodus might not be a reliable biostratigraphic 

marker for the Maastrichtian. 

The faunal composition suggests a shallow 

trans-Tethyan connection between Eurasia and 

India at the end of the Cretaceous Period. 

2008010275 

加拿大阿尔伯塔赛诺曼阶中部 Dunvegan 

组泥质海相前三角洲环境中一新的 

paraclupeid 鱼 = A new paraclupeid fish 

(Clupeomorpha, Ellimmichthyiformes) from a 

muddy marine pro-delta environment: middle 

Cenomanian Dunvegan Formation, Alberta, 

Canada. ( 英文 ). Hay M J; Cumbaa S L; 

Murray A M; Plint A G. Canadian Journal of 

Earth Sciences, 2007, 44(6): 775-790 

A black marine mudstone in allomember A 

of the middle Cenomanian Dunvegan Formation, 

Alberta, yielded a well-preserved, deepbodied 

fish skeleton attributable to a new genus 

and species, Tycheroichthys dunveganensis, 

in the Paraclupeidae (Clupeomorpha, 

Ellimmichthyiformes). This new taxon appears 

most closely related to members of the 

subfamily Paraclupeinae, which includes 

largely freshwater and estuarine or marginal 

marine species known from South and Central 

America and China. The Dunvegan Formation 

represents a large delta complex deposited in 

the Western Interior Seaway at about 65°N, 

where mean sea water temperature may have 

been about 10 °C. The specimen was found 

about 60 km from the contemporaneous shoreline, 

and, in life, apparently inhabited a shallow, 

muddy pro-delta environment characterized 

by high turbidity and variable salinity. 

The fish may have died when it was engulfed 

by brackish floodwater that also introduced 

suspended mud that rapidly buried the body, 

preventing physical disarticulation of the 

skeleton. River outflow probably produced a 

salinity- and density-stratified water column 

that limited oxygen transfer to the sea floor, 

leading to dysaerobic bottom water and an 

absence of scavengers. High terrestrial phytodetrital 

content of the sediment also favoured 

anaerobic conditions that limited bacterial 

decay. 

2008010276 

阿尔及利亚切里夫盆地中新世狭长的翻车 

鱼 Ranzania 属的记录 = Record of the slender 

mola, genus Ranzania (Teleostei, 

Tetraodontiformes), in the Miocene of the 

Chelif Basin, Algeria. ( 英文 ). Carnevale G; 

Santini F. Comptes Rendus Palevol, 2007, 

6(5): 321-326 

A fossil slender mola (Tetraodontiformes, 

Molidae) is described from the Miocene 

(Messinian) of the Chelif Basin, Algeria. The 

material consists of a single individual largely 

incomplete, solely represented by part of the 

anal-fin pterygiophores complement. The 

specimen is referred to the genus Ranzania 

because of the elongate slender morphology 

and thick and well-ossified consistence of the 

bones, which are also characterized by a dense 

and moderately spongy texture. However, it 

has been left unnamed, awaiting more complete 

and better-preserved material. This is the 

first occurrence of the genus Ranzania, and 

more generally of the family Molidae, in the 

Messinian of the Mediterranean. It provides 

new data about the structure and diversity of 

Miocene pelagic fish communities of the Chelif 

Basin. 

两栖类 

2008010277 

德国早二叠世 Archegosaurus decheni 的头 

骨形态 = Skull morphology of Archegosaurus 

decheni Goldfuss (Amphibia, Temnospondyli) 

from the Early Permian of Germany. ( 英文 ). 

Gubin Y M. Alcheringa, 1997, 21(1/2): 103- 

121 

The Early Permian amphibian Archegosaurus 

decheni Goldfuss, originally reported from 

Germany, is described, based on a collection 

of thirteen skulls housed in the Museum of 

Victoria, Melbourne, Australia New and previously 

poorly known features described include: 

the presence of an intermaxillary foramen, 

pterygoid-vomer contact, well developed 

adductor flange of the pterygoid, very long 

choanae, absence of interchoanal and parachoanal 

tooth rows, and development of 

paired anterior palatal fossae. A scheme of 

cladistic relations between archegosauroid 

genera and other temnospondyl families is 

proposed. 

74

2008010278 

乌拉圭二叠 - 三叠纪 Buena Vista 组一新离 

椎类 = A New Temnospondyl From The 

Permo-Triassic Buena Vista Formation of 

Uruguay. ( 英文 ). Piñeiro G; Marsicano C; 

Lorenzo N. Palaeontology, 2007, 50(3): 627- 

640 

A partial skull recovered from conglomerates 

of the Permo-Triassic Buena Vista Formation 

in Uruguay belongs to a new species, 

Uruyiella liminea gen. et sp. nov. This species 

is characterized by a broadly triangular skull 

with laterally projecting posterior corners, 

rhytidosteid-like dermal sculpturing, and orbits 

positioned close to the skull margin. 

Uruyiella liminea is distinguished from other 

temnospondyls by a combination of primitive 

and derived character states, such as the anterior 

extent of the palatine ramus of the pterygoid, 

which excludes the ectopterygoid and 

most of the palatine from the lateral border of 

the interpterygoid vacuity, and the absence of 

both tabular horns and otic notches. A phylogenetic 

analysis places Uruyiella and the 

enigmatic Early Triassic Laidleria in a clade 

to which we attach the family name Laidleriidae. 

The Plagiosauridae and the Laidleriidae 

form a clade at the base of Dvinosauria, which 

is the sister group of a clade that includes 

Stereospondyli and Archegosauroidea. This 

result is unexpected because Laidleria and 

Plagiosauridae are nested deeply within 

Stereospondyli in most phylogenies. The sister-group 

relationship of Uruyiella and Laidleria 

suggests that a ghost lineage for the latter 

genus extends down into the earliest Triassic 

and perhaps even into the Late Permian, 

which in turn would suggest survivorship of 

the Laidleriidae through the Permo-Triassic 

extinction event. 

2008010279 

德国中三叠世 Mastodonsaurus jiganteus 模 

式标本和命名法则的修订 = Revision Of 

The Type Material And Nomenclature Of 

Mastodonsaurus Giganteus (Jaeger) (Temnospondyli) 

From The Middle Triassic Of Germany. 

( 英文 ). Moser M; Schoch R. Palaeontology, 

2007, 50(5): 1245-1266 

The type material of Mastodonsaurus is 

revised and its complicated taxonomic history 

resolved. The genus was erected by Jaeger in 

1828 without a species name, which was 

added subsequently by Holl (1829) who 

named the type species Mastodonsaurus jaegeri. 

The large tooth on which Jaeger based 

his Mastodonsaurus is chosen herein as lectotype 

of the type species. A smaller second 

individual, represented by a piece of an occiput, 

was also named by Jaeger in 1828 as 

Salamandroides giganteus and, owing to the 

find of a complete skull, was recognized in 

1833 by the same author as belonging to the 

same species as the Mastodonsaurus. Therefore, 

Mastodonsaurus giganteus (Jaeger, 1828) 

is a senior subjective synonym of the type 

species M. jaegeri Holl, 1829. The precedence 

of the two generic names was chosen in 1834 

by the first reviser, von Alberti, in favour of 

Salamandroides, but all later authors, including 

von Alberti himself, followed Jaeger, who 

decided in 1837 to retain the name Mastodonsaurus. 

The established usage of Mastodonsaurus 

is preserved formally herein (nomen 

protectum). The names Batrachosaurus Fitzinger, 

1837, and Labyrinthodon Owen, 1841 

are unjustified replacement names of Mastodonsaurus. 

The names M. jaegeri von Meyer, 

1832, S. jaegeri von Alberti, 1834 and 

M. salamandroides Jaeger, 1837 are junior 

homonyms and synonyms of M. jaegeri Holl, 

1829, and M. giganteus (Jaeger, 1828), respectively. 

A recent attempt to replace the 

universally used Capitosauroidea Watson, 

1919 by the unused and newly elevated Mastodonsauroidea 

Lydekker, 1885 is rejected. 

Two older synonyms of Mastodonsauridae 

Lydekker, 1885 (nomen protectum) are rejected 

as unavailable (Labyrinthodontidae von 

Meyer,1842) and nomen oblitum (Batrachosauridae 

Fitzinger, 1843), respectively. 

The holotype of Mastodonsaurus giganteus is 

reinstated and valid on the basis of three diagnostic 

features present: the tripartite posterior 

rim of the parasphenoid, a laterally pushed 

suture between the parasphenoid and basipterygoid, 

and a wide slit-like eustachian tube 

opening. Mastodonsaurus is known from 

specimens representing a continuous growth 

series, now also encompassing the lectotype of 

Mastodonsaurus jaegeri, which until rather 

recently stood isolated from other specimens 

as the largest find by far. 

爬行类 

2008010280 

日本中部 Toyama 地区东部下白垩统 

Tetori 群群居恐龙足迹的首次发现 = First 

trackway evidence of gregarious dinosaurs 

from the Lower Cretaceous Tetori Group of 

eastern Toyama prefecture, central Japan. ( 英 

文 ). Matsukawa M; Hamuro T; Mizukami T; 

Fujii S. Cretaceous Research, 1997, 18(4): 

603-619 

75

Early Cretaceous slender-toed bipedal dinosaur 

tracks are reported from the eastern part 

of the Tetori area, central Japan. They are 

small, bipedal and tridactyl impressions assigned 

toToyamasauripus masuiaeichnogen. 

and ichnosp. nov. based on biometric analysis. 

Thirty-three individuals ofToyamasauripus 

masuiaeshow the highest density of footprints 

of any dinosaur track-sites in Japan. This is 

also the first trackway evidence of gregarious 

dinosaurs reported from Japan.Toyamasauripus 

masuiaeappears to represent 

a small bipedal dinosaur track-maker that 

was relatively abundant. As no bones are 

known from the track-bearing beds, the footprints 

add much to our knowledge of dinosaur 

faunas at this time. 

2008010281 

美国爱荷华州密西西比统上部一新的基干 

四足类 : Sigournea multidentata = Sigournea 

multidentata, a new stem tetrapod from 

the upper Mississippian of Iowa, USA. ( 英文 ). 

Bolt J; Lombard R E. Journal of Paleontology, 

2006, 80(4): 717-725 2 图版 . 

Sigournea multidentata n. gen. and sp., an 

early tetrapod, is described from the Late Mississippian 

Delta locality of southern Iowa, 

USA. The holotype and only known specimen, 

a right mandible, is unique in the structure of 

the symphysial region, and in addition has a 

unique combination of characters that are 

shared with other tetrapods. The free ventral 

border of the single exomeckelian fenestra is 

formed by infradentary bones. Its visible portion 

shows several arch bases, separated by 

notched or straight intervals. This morphology 

is interpreted as indicating that the arch bases 

and intervals between them reflected a series 

of Meckelian fenestrae that were partly exoand 

partly endoskeletal, due to the fact that the 

exoskeletal arch bases continued dorsally in 

Meckelian cartilage. We suggest that this may 

exemplify a stage in the evolution of 

exomeckelian fenestrae, in at least some lineages 

of early tetrapods. The relations of Sigournea 

are indeterminate. That it is a 

tetrapod is indicated by the presence of pit and 

ridge ornamentation, an open lateral line sulcus, 

a dorsally directed glenoid, a single elongate 

exomeckelian fenestra, absence of intercoronoid 

fossae, absence of coronoid fangs, a 

single row of marginal teeth on the dentary, 

and an absence of dentition on the prearticular. 

It is at present impossible to determine its relationship 

with other early tetrapods, and we 

conclude that Sigournea is best considered as 

an early tetrapod incertae sedis. 

2008010282 

西非 iullemmeden 盆地古新世 Dyrosaurid 

组合的分类学修订 = Taxonomic revision of 

the Dyrosaurid assemblage (Crocodyliformes:Mesoeucrocodylia) 

from the Paleocene of 

the iullemmeden basin, west Africa. ( 英文 ). 

Jouve S. Journal of Paleontology, 2007, 81(1): 

163-175 1 图版 . 

The dyrosaurids of the Iullemmeden Basin 

(West Africa) are mainly represented by two 

genera, Hyposaurus and Rhabdognathus. Hyposaurus 

has been recognized in the Paleocene 

of Mali and Nigeria with two species, H. 

nopcsai and H. wilsoni. Diagnostic characters 

given by previous authors for these species do 

not enable their distinction from each other, 

nor from North American species. It is therefore 

reasonable to consider H. nopcsai and H. 

wilsoni as nomina dubia. In 1930, Swinton 

erected the new genus and species Rhabdognathus 

rarus on the basis of mandibular remains, 

and Buffetaut referred a skull to this 

species in 1980. A new skull was described in 

2002 by Brochu et al., and referred to Rhabdognathus 

sp. Unfortunately, it is impossible 

to refer either skull to the type species, the 

mandibular remains having no diagnostic 

characters at the specific level. Thus, R. rarus 

is a nomen dubium, and two new names are 

erected for the two skulls: R. keiniensis n. sp. 

and R. aslerensis n. sp., all the mandibular 

remains being referred to Rhabdognathus sp. 

The species Rhabdognathus compressus is 

reassigned to the genus Congosaurus, since its 

mandible is higher than that of Hyposaurus, 

shorter than that of Rhabdognathus, and the 

lateromedially compressed teeth demonstrate 

that C. compressus and C. bequaerti are 

closely related. 

2008010283 

横齿蜥蜴类的新类群及 "Teiids" 演化历史 

的新资料 = New taxa of transversely-toothed 

lizards (Squamata: Scincomorpha) and new 

information on the evolutionary history of 

"Teiids". ( 英文 ). Nydam R L; Eaton J G. 

Journal of Paleontology, 2007, 81(3): 538- 

549 3 图版 . 

New material of polyglyphanodontine lizards 

from the Late Cretaceous has been found 

in various localities in western North America. 

Several transversely oriented teeth representing 

a new species of Dicothodon were recov- 

76

ered from the Turonian of southern Utah. 

These specimens necessitate reassignment of 

Polyglyphanodon bajaensis to Dicothodon 

(Polyglyphanodon) bajaensis. From the Campanian 

of Utah, additional teeth and jaw fragments 

referable to Manangysaurus saueri 

have been recovered and this species is reassigned 

here to Peneteius (Manangysaurus) 

saueri. Also, an isolated tooth referable to 

Peneteius has been recovered from the Campanian 

of southern Texas. The results of a 

phylogenetic analysis support a monophyletic 

grouping of the transversely-toothed taxa with 

Bicuspidon as the sister taxon of Polyglyphanodontini 

new taxon, which is comprised 

of Polyglyphanodon, Dicothodon, and 

Peneteius. The phylogenetic analysis also 

places "teiid" lizards from the Cretaceous of 

Asia and North America in a monophyletic 

group, Borioteiioidea new taxon, which is the 

sister taxon to the Teiioidea (Teiidae + Gymnophthalmidae). 

This new hypothesis of the 

interrelationships of these taxa requires the 

reevaluation of several characteristics that 

were previously considered diagnostic for a 

more inclusive Teiidae. Another implication 

of our results is that Teiidae (sensu stricto) has 

no demonstrable pre-Tertiary occurrence. It 

appears that Teiioidea and Borioteiioidea diverged 

from a common ancestor by the Early 

Cretaceous. The Teiioidea entered South 

America and are currently represented by the 

Teiidae and Gymnophthalmidae, whereas 

Borioteiioidea radiated throughout North 

America with subsequent dispersal to Asia 

and Europe. 

2008010284 

基于一新发现的完整骨骼对 Saniwa ensidens 

的解剖学研究 = The anatomy of the 

fossil Varanid lizard Saniwa ensidens leidy, 

1870, based on a newly discovered complete 

skeleton. ( 英文 ). Rieppel O; Grande L. Journal 

of Paleontology, 2007, 81(4): 643-665 6 

图版 . 

The skeleton of a newly discovered, exceptionally 

preserved specimen of Saniwa ensidens 

is described in detail. The fossil consists 

of a complete articulated skeleton exposed 

in dorsal view. It adds important additional 

information to our knowledge of the 

anatomy of this fossil varanoid taxon, including 

a detailed description of the dermatocranium 

in dorsal view, complete vertebral 

counts, and a detailed account of the appendicular 

skeleton. Cartilage preservation allows 

the identification of treacheal rings, sternum, 

inscriptional ribs, epicoracoid and suprascapula. 

Patches of skin are preserved on 

dermal skull bones, and scattered scales surround 

the entire skeleton. Incomplete ossification 

of carpal and tarsal elements, as well as of 

epiphyses, indicate that the specimen is not 

fully mature. 

2008010285 

Eosaniwa koehni 的形态学新资料及对系统 

分析的修订 = New morphological data for 

Eosaniwa koehni haubold, 1977 and a revised 

phylogenetic analysis. ( 英文 ). Rieppel O; 

Conrad J L. Journal of Paleontology, 2007, 

81(4): 760-769 5 图版 . 

Eosaniwa koehni is an enigmatic platynotan 

that differs from related varanoids in the possession 

of a very long snout resulting in extremely 

elongate nasals and vomers; a robust 

and broad jugal; the presence of denticles on 

palatines, pterygoids, and vomers; the presence 

of a subdental shelf on the dentary; and a 

strongly twisted retroarticular process on the 

mandible. Phylogenetic analysis suggests that 

Eosaniwa is a derived varanoid platynotan, 

nested within a clade also including mosasauroids, 

Coniasaurus, and Paravaranus. 

2008010286 

阿根廷巴塔哥尼亚上白垩统蜥脚动物前颌 

骨中牙齿的替换 = Tooth replacement in a 

sauropod premaxilla from the Upper Cretaceous 

of Patagonia, Argentina. ( 英文 ). Coria 

R A; Chiappe L M. Ameghiniana, 2001, 38(4): 

463-466 

Anatomy and tooth replacement mechanism 

observed in a sauropod dinosaur left premaxilla 

from the Late Cretaceous of Patagonia are 

described. The specimen is assigned to 

Neosauropoda, and with doubts to Titanosauridae, 

due the presence of a stepped anterior 

margin, and long and cylindrical teeth 

with no denticles. The specimen presents a 

dental settlement pattern performed by intraalveolar 

packages of four dental elements, one 

functional and three germinals, which compose 

a comb-like arrangement only recorded 

in diplodocid and titanosaurid sauropods. 

2008010287 

阿根廷门多萨省中 - 晚三叠世发现膜质盾 

片 : 是否作为恩吐龙的证据 = Dermal 

scutes from the Potrerillos Formation (Middle- 

Late Triassic) of Mendoza Province: evidence 

for aetosaurs. ( 英文 ). Desojo J B. 

Ameghiniana, 2001, 38(3): 349-352 

77

The rare archosaurian records from the Triassic 

Cuyo Basin include that of actosaurs in 

the Potrerillos Formation. This putative record 

was based on a pair of poorly preserved, isolated 

dermal scutes that were tentatively referred 

to a new species of Typothorax Cope. 

Examination of this material led to the conclusion 

that it is not referable to this North 

American genus; moreover, its attribution to 

Aetosauria is doubtful. 

2008010288 

贵州关岭晚三叠世一大型鱼龙类头骨 = 

Cymbospondylus from the Upper Triassic of 

Guizhou, China. ( 中文 ). 李淳 ; 尤海鲁 . 古脊 

椎动物学报 , 2002, 40(1): 9-16 

记述了产自贵州关岭上三叠统杯椎鱼龙 

属一新种 —— 亚洲杯椎鱼龙 

(Cymbospondylus asiaticus sp. nov)。标本为 

两件几乎完整的头骨 , 产于法朗组瓦窑段的 

泥质灰岩中 , 这是目前已知惟一的晚三叠世 

Cymbospondylus 属的标本 , 也是该属时代最 

晚的一个种。亚洲杯椎鱼龙头部最明显的 

特征是下颌牙齿仅分布于齿骨的前半部 

分。此外 , 新种的吻部极长 , 超过头骨全长之 

半 , 上颌骨非常发达 , 并且具有已知鱼龙类中 

最小的眼眶。亚洲杯椎鱼龙是这一大型鱼 

龙类在北美和欧洲以外地区的首次记录。 

2008010289 

第四纪响蜥 (Tinosaurus) 化石的首次发现 = 

The first appearance of Tinosaurus fossil in 

the Quaternary. ( 中文 ). 李永项 ; 薛祥煦 . 古脊 

椎动物学报 , 2002, 40(1): 34-41 

在陕西洛南张坪洞穴的第四系中采得一 

些响蜥类 (Tinosaurus) 化石 , 有保存相当完好 

的上下齿骨和齿列 , 这是响蜥在第四纪的首 

次报道 , 使该属化石的地史分布从早第三纪 

延伸到第四纪。新材料下颌骨较粗壮 , 但个 

体很小 , 有齿间沟 , 同时兼具亚洲种及北美种 

的某些特征 , 因此建立一新种 Tinosaurus luonanensis 

sp.nov.。 

2008010290 

贵州兴义中三叠统法郎组竹杆坡段 

Lariosaurus 一新种 = A new species of 

Lariosaurus(sauroterygia: Nothosauridae)from 

Triassic of Guizhou, southwest China. ( 中文 ). 

李锦玲 ; 刘俊 ; 奥利维尔 · 瑞柏尔 . 古脊椎动物 

学报 , 2002, 40(2): 114-126 

记述了贵州兴义法郎组竹杆坡段鸥龙的 

一新种 ── 兴义鸥龙 (Lariosaurus xingyiensis 

sp. nov.)。兴义鸥龙以其上颞孔是眼眶长度 

的两倍 , 顶骨平台细长而不收缩 , 肱骨缺失外 

髁沟和旋后肌突 , 及肱骨短于股骨而有别于 

鸥龙的其他种。兴义鸥龙与意大利拉丁晚 

期的 Lariosaurus valceresii 最为相似。依据 

脊椎动物的对比 , 法郎组竹杆坡段的时代应 

为中三叠世晚期。 

2008010291 

内蒙古上白垩统二连组发现一新镰刀龙类 

( 英文 ) = A new therizinosauroid (dinosauria,theropoda) 

from the Upper Cretaceous 

Iren Dabasu Formation of Nei Mongol. ( 英文 ). 

徐星 ; 张晓虹 ; 保罗 · 塞雷诺 ; 赵喜进 ; 匡学文 ; 韩 

军 ; 谭琳 . 古脊椎动物学报 , 2002, 40(3): 228- 

240 

镰刀龙类化石主要分布于亚洲白垩纪地 

层 (Russell and Dong,1993;Xu et 

al.,1999a;Kirkland and Wolfe,2001)。最近发 

现于内蒙古上白垩统二连组的杨氏内蒙古 

龙 (Neimongosaurus yangi) 代表这一类群中 

较为原始的属种 ( 张晓虹等 ,2001)。通过研 

究产自同一化石地点的镰刀龙类新材料 , 我 

们鉴定出一个不同于杨氏内蒙古龙的新属 

种 , 美掌二连龙 (Erliansaurus bellamanus gen. 

et sp. nov.)。 

依据以下特征将 Erliansaurus bellamanus 

归入镰刀龙超科 : 肩胛骨干远端狭窄、肱骨 

近端角状、肱骨有后转子、肱骨的尺骨髁 

和桡骨髁位于肱骨干前部、肠骨髋臼后支 

远端加厚、距骨髁小和腓骨近端后缘窄。 

Erliansaurus bellomanus 的以下自近裔特征 

区别于其他镰刀龙类 : 前部尾椎具加大的滋 

养孔、肱骨后转子嵴状、肱骨后转子内侧 

有一卵形凹陷、肠骨外侧面坐骨柄上方有 

一多皱的肿状突起、腓骨近端后缘明显高 

于前缘以及腓骨前转子大、位置靠远端。 

本文对镰刀龙类的系统关系进行了初步的 

分析 , 结论如下 : 北票龙 (Beipiaosaurus) 代表 

除 Eshanosaurus 外最原始的属种 , 它没有以 

下一些其他镰刀龙类的进步性状 : 掌爪近端 

深、胫骨短于股骨、非常短的蹠骨以及第 

一蹠骨关连跗骨。 Erliansaurus 、 

Alxasaurus 、 Neimongosaurus 和 

Nothronychus 比 Beipiaosaurus 和 

Eshanosaurus 进步 , 但比镰刀龙科原始 , 它们 

没有镰刀龙科的一些进步特征 : 肠骨的髋臼 

前支深而后卷、肠骨背缘平直和极其狭窄 

的足爪。Erliansaurus 的肱骨也有一些原始 

特征 , 比如较平的尺骨髁和桡骨髁之间的槽 

较宽。相比而言 ,Erliansaurus 比 

Alxasaurus 、 Neimongosaurus 以及 

78

Nothronychus 要进步一些 , 它具有以下一些 

进步特征 : 背椎和尾椎侧凹缺失、肱骨有后 

转子、肠骨髋臼后支短。但是其他一些特 

征的分析则支持 Erliansaurus 的系统位置可 

能和 Neimongosaurus 较为接近的假说 , 二者 

共享一些独特的性状 , 比如肱骨干中部有一 

卵形凹陷、肠骨髋臼上嵴侧向发育以及腓 

骨嵴长。Erliansaurus 同时和其他一些镰刀 

龙类的属种也共享一些进步特 

征 :Erliansaurus 腓骨的前转子侧向延伸 , 这 

一特征类似于 Beipiaosaurus 和 

Nothronychus;Erliansaurus 和 Nothronychus 

以及 Segnosaurus 也共享一些进步的相似性 , 

比如腓骨前转子的位置在腓骨干中部。 

有关 Erliansaurus 准确系统位置的确定有 

待于一个定量的分支系统学分析。但初步 

的结论表明它的系统位置处于原始的镰刀 

龙类和进步的镰刀龙科的成员之间。 

Erliansaurus 的发现为镰刀龙类的分异提供 

了重要信息。 

2008010292 

湖北三叠纪海生爬行动物的层位及时代 = 

The horizon and age of the marine reptiles 

from Hubei Province, China. ( 中文 ). 李锦玲 ; 

刘俊 ; 李淳 ; 黄照先 . 古脊椎动物学报 , 2002, 

40(3): 241-244 

通过对化石点的实地调查证实 , 湖北南 

漳、远安发现的海生爬行类除孙氏南漳龙 

( 大冶组顶部或嘉陵江组底部 ) 外都产自嘉陵 

江组 , 它们的时代同为早三叠世奥伦尼克 

期。由孙氏南漳龙、南漳湖北鳄、湖北汉 

江蜥和远安贵州龙形成的这一海生爬行动 

物组合 , 是上扬子地区层位最低的 , 生存时代 

早于其他海生爬行动物组合。与产自欧洲 

的肿肋龙类有密切亲缘关系的贵州龙和汉 

江蜥 , 是该科最早的代表 , 也是鳍龙类最早的 

代表之一 , 为探讨鳍龙类和肿肋龙类的起源 

及传播提供了新的证据。 

2008010293 

辽宁北票地区一新的甲龙化 = A new armored 

dinosaur (Ankylosauria) from Beipiao 

basin,Liaoning Province,northeastern China. 

( 中文 ). 董枝明 . 古脊椎动物学报 , 2002, 

40(4): 276-285 

记述了辽宁省北票地区的甲龙化石一新 

属新种 : 步氏克氏龙 (Crichtonsaurus bohlini 

gen. et sp. nov.)。其主要特征是 : 中等大小的 

甲龙 , 下颌骨较低 , 外侧无骨甲覆盖 ; 牙齿小 , 

齿冠上有垂直向的棱嵴和边缘小齿 , 齿环发 

育不全 , 有愈合的颈甲板 , 膜质骨甲形态多样 , 

尾后部的椎体相连结成棒状 , 两侧有排列对 

称的甲板。步氏克氏龙的发现对探讨北票 

地区晚中生代地层的划分和时代归属 , 以及 

对甲龙类的系统演化和地理分布均具有重 

要的意义。 

2008010294 

Vallesaurus genensis Wild, 1991, 意大利北 

部晚三叠世 drepanosaurid 类之一种 = 

Vallesaurus genensis Wild, 1991, A Drepanosaurid 

(Reptilia, Diapsida) from the Late Triassic 

of northern Italy. ( 英文 ). Renesto S; 

Binelli G. Rivista Italiana di Paleontologia e 

stratigrafia, 2006, 112(1): 77-94 

Vallesaurus cenensis, a small drepanosaurid 

reptile from the Norian beds of the Calcare di 

Zorzino is described. The holotype and only 

known specimen represents the first drepanosaurid 

in which the skull is preserved articulated 

with the postcranial skeleton. The study 

of Vallesaurus anatomy confirms previous 

data about arboreal adaptation in all known 

drepanosaurids and permits more firm hypotheses 

about the phylogenetic relationships 

of the Drepanosauridae to be proposed. 

2008010295 

意大利晚三叠世一种与蛇颈龙有亲缘性的 

鳍龙类 = A new sauropterygian reptile with 

plesiosaurian affinity from the Late Triassic of 

Italy. ( 英文 ). Dalla Vecchia F M. Rivista Italiana 

di Paleontologia e stratigrafia, 2006, 

112(2): 207-225 

Bobosaurus forojuliensis, gen. et s. nov., is 

a large sauropterygian from the Alpine Late 

Triassic. The holotype is a moderately disarticulated 

skeleton consisting of the tip of the 

rostrum, part of the neck (including the atlasaxis 

complex), the trunk, most of the tail, parts 

of the limbs, and the pelvic girdle. The new 

taxon is characterized by a mosaic of "nothosaurian" 

and "plesiosaurian" features. It 

exhibits characters that were previously considered 

autapomorphies of different sauropterygian 

taxa. 

2008010296 

广元恐龙化石埋藏地沙溪庙组地球化学特 

征及对物源区和古风化作用的指示 = Geochemistry 

of the Shaximiao Formation in a 

dinosaur fossil site,Guangyuan, Sichuan, and 

its implications for the source area and paleoweathering. 

( 中文 ). 阚泽忠 ; 梁斌 ; 王全伟 ; 朱 

兵 . 中国地质 , 2006, 33(5): 1023-1029 

广元恐龙化石埋藏地是四川盆地中侏罗 

世重要的恐龙化石点 , 恐龙化石埋藏于中侏 

79

罗统沙溪庙组之中。笔者对该恐龙化石埋 

藏地沙溪庙组泥质岩的常量元素、微量元 

素和稀土元素特征进行了研究 , 并根据泥质 

岩的地球化学特征讨论了物源区性质、构 

造背景以及物源区的风化特征。主量元素 

和稀土元素表明其物源区以长英质岩石为 

主 , 构造背景为被动大陆边缘 : 指示化学风化 

程度的 CIA 指数及成分成熟度的 ICV 指数 , 

表明物源区经历了中等的化学风化作用 , 反 

映了中侏罗世恐龙生活在半干旱的古气候 

环境之中。 

2008010297 

澳大利亚新南威尔士格斯福德三叠纪 

Narrabeen 群 Parotosuchus wadei 的再解 

释兼评其的生长阶段 = Re-interpretation of 

Parotosuchus wadei Cosgriff, a capitosaurid 

from the Triassic Narrabeen Group at Gosford, 

New South Wales, with comments on its 

growth stage. ( 英文 ). Damiani R J; Warren A. 

Alcheringa, 1997, 21(3/4): 281-289 

The holotype and paratype of the capitosaurid 

Parotosuchus wadei (Cosgriff, 1972) 

from the Terrigal Formation (Narrabeen 

Group) near Sydney are re-examined. It is 

demonstrated that the holotype skull is an immature 

individual of the genus Parotosuchus, 

and that it exhibits no characters that are derived 

beyond the generic level. The paratype 

specimen consists of an impression of the 

skull, mandibles and dermal pectoral girdle 

but is largely indeterminate to family. P. 

wadei is therefore a nomen dubium. 

2008010298 

新西兰中新世鳄类化石 = A Miocene crocodilian 

from New Zealand. ( 英文 ). Molnar R E; 

Pole M. Alcheringa, 1997, 21(1/2): 65-70 

An incomplete indeterminate crocodilian 

angular from the Miocene Bannockburn Formation, 

Central Otago, South Island, New 

Zealand is described. The fossil (probably a 

new taxon) represents the first undoubted occurrence 

of a crocodilian in New Zealand. 

Local palaeoclimatic indicators suggest the 

crocodilian lived in a temperate climate. 

2008010299 

甘肃巴家嘴丽牛 (Leptobos) 的化石时代及环 

境 = On the skull of Leptobos from the Eraly 

Pleistocene Bajiazui fauna in Qingyang 

County,Gansu Province. ( 中文 ). 王健 ; 薛祥煦 . 

西北大学学报 ( 自然科学版 ), 2006, 36(3): 

449-452 

目的记述甘肃庆阳巴家嘴黄土层中发现 

的一件丽牛化石标本。方法运用经典的古 

生物方法 , 结合化石解剖、形态比较方法研 

究。结果该化石的主要特征是额面平 , 稍高 

出眼眶 ; 眼眶向侧方凸出 ; 角基起始于眼眶稍 

后 , 角直而细 , 亚柱状 , 两角心顺角基延长线大 

体成 105° 夹角 ; 这些主要特征与 Leptobos 

amplifrontalis 极为相似 , 定为 Leptobos cf. 

amplifrontalis。结论根据丽牛在欧洲和中 

国的发现及在巴家嘴动物群中的其他化石 

特征 , 巴家嘴丽牛的地质时代为第四纪早更 

新世早期 , 环境气候以湿冷为主。 

2008010300 

陕西洛南中晚更新世根田鼠化石 = The 

Middle-Late Pleistocene fossils of Microtus 

oeconomus from Luonan County,Shaanxi 

Province,China. ( 中文 ). 李永项 ; 薛祥煦 . 西北 

大学学报 ( 自然科学版 ), 2006, 36(4): 784- 

788 

目的研究陕西洛南张坪洞穴群中发现的 

根田鼠化石 Micccrotus oeconomus。方法运 

用经典古生物学方法 , 包括化石解剖、系统 

描述、形态对比、统计归纳。结果 M3 舌 

侧 3 褶沟 4 褶角 ;m1 有 4 个封闭的三角 , 第 5 

个与前帽贯通 , 后环位于齿列纵轴上 ;m3 唇 

侧 3 褶角 ;M3 和 m1 的长度、宽度从第 6 层 

洞到第 1 层洞逐渐变大 , 第 6 齿峡 (Is6) 的宽 

度变小。结论化石的主要特征可与周口店 

第 1 地点的 M. epiratticeps 相对比 , 主要测量 

值在现生种的变异范围之内 , 确定为中更新 

世以来不同时段的根田鼠化石 , 其颊齿趋于 

增大 , 第 6 齿峡趋于变窄。 

2008010301 

辽宁北票龙骨组织中类似血细胞结构的研 

究 = Small spheres preserved in a therizinosauroid 

dinosaur's blood vessels from Northeast 

China. ( 中文 ). 姚锦仙 ; 张昀 ; 唐治路 . 北 

京大学学报 ( 自然科学版 ), 2002, 38(2): 221- 

225 

在我国辽宁北票下白垩统义县组下部地 

层中出土的北票龙 (Beipiaosaurus inexpectus) 

化石由部分椎骨和肢骨碎片构成 , 其中保存 

有血管和类似血细胞的结构。在肢骨周围 

有褐色细丝状的皮肤衍生物的印痕。细丝 

状皮肤衍生物无分枝 , 大约 0.1 mm 宽 ,50~ 

60 mm 长。在光学显微镜下观察到其肱骨 

的纵切面上有褐色血管结构 , 一些管腔中有 

褐色小圆球 , 它们沿着管腔分布。这些小圆 

球的形状和大小显示它们有可能是恐龙血 

细胞的遗迹。另外 , 图像分析法结果显示北 

80

票龙骨组织有较高的血管密度 , 表示它具有 

较高的新陈代谢率。从骨组织特征及作为 

体表隔热层的细丝状皮肤衍生物的存在来 

看 , 北票龙可能为恒温动物。 

2008010302 

有鳞类爬行动物支系的演化分异 = Evolutionary 

diversification of clades of squamate 

reptiles. ( 英文 ). Ricklefs R E; Losos J B; 

Townsend T M. Journal of Evolutionary Biology, 

2007, 20(5): 1751–1762 

We analysed the diversification of squamate 

reptiles (7488 species) based on a new molecular 

phylogeny, and compared the results to 

similar estimates for passerine birds (5712 

species). The number of species in each of 36 

squamate lineages showed no evidence of 

phylogenetic conservatism. Compared with a 

random speciation–extinction process with 

parameters estimated from the size distribution 

of clades, the alethinophidian snakes 

(2600 species) were larger than expected and 

13 clades, each having fewer than 20 species, 

were smaller than expected, indicating rate 

heterogeneity. From a lineage-through-time 

plot, we estimated that a provisional rate of 

lineage extinction (0.66 per Myr) was 94% of 

the rate of lineage splitting (0.70 per Myr). 

Diversification in squamate lineages was independent 

of their stem age, but strongly related 

to the area of the region within which 

they occur. Tropical vs. temperate latitude 

exerted a marginally significant influence on 

species richness. In comparison with passerine 

birds, squamates share several clade features, 

including: (1) independence of species richness 

and age; (2) lack of phylogenetic signal 

with respect to clade size; (3) general absence 

of exceptionally large clades; (4) overrepresentation 

of small clades; (5) influence of 

region size on clade size; and (6) similar rates 

of speciation and extinction. The evidence for 

both groups suggests that clade size has 

achieved long-term equilibrium, suggesting 

negative feedback of species richness on the 

rate of diversification. 

2008010303 

日本千叶县中更新统水生龟类新种 Ocadia 

nipponica (Testudines: Testudinoidea: 

Geoemydidae) = Ocadia nipponica, a new 

species of aquatic turtle (Testudines: Testudinoidea: 

Geoemydidae) from the Middle Pleistocene 

of Chiba Prefecture, central Japan. ( 英 

文 ). Hirayama R; Kaneko N; Okazaki H. Paleontological 

Research, 2007, 11(1): 1-19 

A new species of the genus Ocadia (Testudines; 

Testudinoidea; Geoemydidae), O. nipponica, 

is described on the basis of a nearly 

complete skeleton from the Middle Pleistocene 

Kiyokawa Formatin of the Shimosa 

Group at Sodegaura City, Chiba Prefecture, 

central Japan. O. nipponica is distinguished 

from O. sinensis (Gray) by its more extensive 

secondary palate, smoother shell surface, narrower 

second and third vertebral scutes, and 

larger size (carapace up to 33 cm long). Considering 

that the living species O. sinensis is 

distributed in the coastal area of eastern to 

southeastern Asia in subtropical to tropical 

climates, the new fossil species may have 

been thrived in warmer paleoclimatic conditions 

for the Japanese Islands in the Pleistocene 

age than hitherto have been estimated on 

the basis of floral evidences. 

2008010304 

阿根廷拉里奥哈省上白垩统恐龙蛋化石的 

首次发现 = First finding of dinosaur eggs 

(Upper Cretaceous) in the La Rioja province, 

Argentina.. ( 其他 ). Tauber A A. 

Ameghiniana, 2007, 44(1): 11-28 

Numerous sites containing dinosaur eggshells 

have been found in the Los Llanos 

Formation in the Sanagasta Valle, La Rioja 

Province, Argentina. The eggs were classified 

as Sphaerovum erbeni Mones, corresponding 

to dinosaurs with a basic type of Dinosauroidspherulite 

organization and a filisferulitic 

morphotype, belonging to the Faveoloolithidae 

Oofamily, similar to others reported previously 

in Uruguay and in the Rio Negro and 

La Pampa provinces, Argentina. The fossils 

were found in situ, although fragmented 

mainly due to the process of paedogenesis. 

The studied eggshells indicate a Campanian- 

Maastrichtian age, being the first fossils of the 

age in the Sierra de Velasco region. 

2008010305 

阿根廷巴塔哥尼亚北部上白垩统 titanosaur 

颅骨化石 : 描述及对其内耳的认识 = A 

titanosaur (Dinosauria, Sauropoda) braincase 

from the Upper Cretaceous of north Patagonia: 

description and contribution to the knowledge 

of the dinosaur inner ear.. ( 其他 ). Paulina- 

Carabajal A; Salgado L. Ameghiniana, 2007, 

44(1): 109-120 

The braincase of a sauropod dinosaur from 

the Upper Cretaceous of Rio Negro, Argentina, 

is described. The material is assigned to the 

clade Titanosauria and some characters that 

resemble the condition present in the genus 

Antarctosaurus such as the presence of short 

81

and wide frontals and parietals, supraoccipital 

knob lacking a medial groove, reduced and 

dorsally exposed supratemporal fenestrae, 

frontals fused on the midline, and a single interfrontal 

medial knob are discussed. These 

characters are not diagnostic and they can be 

found in other titanosaurs such as Rapetosaurus, 

Nemegtosaurus, Saltasaurus and Bonatitan. 

The braincase, although incomplete, is 

well preserved, allowing the examination of 

certain delicate internal structures like the inner 

ear, which has been exposed through bone 

fractures. The titanosaurian inner ear is described 

here for the first time: it is morphologically 

similar to that of other sauropods 

such as Diplodocus and Brachiosaurus, 

mainly in the spatial disposition of the semicircular 

canals, although showing a proportionally 

more robust lagena. The angle between 

the planes on which the anterior and 

posterior semicircular canals lie is greater than 

909 degrees as in other herbivorous dinosaurs, 

and different from the theropod Allosaurus, 

where that angle is smaller. 

2008010306 

阿根廷门多萨 Potrerillos 地区三叠纪四足 

类的时代和地层位置 = Age and stratigraphic 

position of the tetrapods from the cerro Bayo 

at Potrerillos locality (Triassic), Mendoza, 

Argentina.. ( 其他 ). Zavattieri A M ; Arcucci 

A B. Ameghiniana, 2007, 44(1): 133-142 

The age of the Rio Mendoza Formation at 

Potrerillos, Cuyana Basin, was previously assigned 

to the Lower Triassic on the basis of its 

tetrapod content. However, many authors considered 

this as controversial and at present the 

unit is assigned to the Middle Triassic because 

it rests unconformably upon the Choiyoi 

Group, whose uppermost levels are locally 

established for the early Middle Triassic. The 

tetrapod remains formerly recovered in this 

sequence came from a few meters below thick 

tuffaceous beds (pink, grey, green) from violet 

and reddish mudstones which are attributed 

herein as proceeding from the middle to upper 

part of the Cerro de Las Cabras Formation. 

New material of kannemeyeriid dicynodonts 

and indeterminate eucynodonts from the 

northern side of Cerro Bayo of Potrerillos 

come from the same stratigraphic levels of the 

Cerro de Las Cabras Formation, instead of the 

Rio Mendoza Formation, as previously 

thought. Taking into account the microfloristic 

assemblage yielded by the Cerro de Las 

Cabras Formation, the age of the oldest amniotes 

recorded from the Cuyana Basin cannot 

be older than the late Middle Triassic. 

2008010307 

宁城中生代道虎沟生物群中两类具原始羽 

毛翼龙的发现及其地层学和生物学意义 = 

Discovery of two kinds of protofeathered 

pterosaurs in the Mesozoic Daohugou biota in 

the Ningcheng region and its stratigraphic and 

biologic significanes. ( 中文 ). 季强 ; 袁崇喜 . 地 

质论评 , 2002, 48(2): 221-224 

本文事实是地介绍了道虎沟生物群的组 

成及相关地层的岩性 , 并根据长尾型嘴口 

龙类 (Rhamphorhynchoidea) 翼龙与短尾型翼 

手龙类 (Pterodactyloidea) 翼龙同期共生的特 

点 , 确信道虎沟生物群的地质时代为晚侏 

罗世。此外 , 本文还研究了道虎沟生物群 

中翼龙身上发育的皮肤衍生物 , 初步认为 

它们是原始羽毛 (protofeathers), 至少是与 

羽毛同源的 (feather-homologous), 这对于了 

解羽毛 ( 广义 ) 的演化历史和早期的形态 

结构将具有十分重要的意义。 

2008010308 

南美晚三叠世初龙类 Neoaetosauroides engaeus 

头盖骨形态学 :Aetosaurian 多样性 

的证据 = Cranial morphology of the late Triassic 

South American Archosaur Neoaetosauroides 

engaeus: evidence for Aetosaurian 

diversity. ( 英文 ). Desojo J B; Báez A M. Palaeontology, 

2007, 50(1): 267–276 

The cranial anatomy of Neoaetosauroides 

engaeus Bonaparte, 1969 from the upper part 

of the Los Colorados Formation, western Argentina, 

is addressed herein. This description 

is based on material collected recently, which 

permits a complete restoration of the skull; 

previously, a partial lower jaw and premaxillary 

and maxillary fragments were the only 

cranial remains known. Unlike other aetosaurs 

for which the premaxillary dentition is known, 

in N. engaeus the upper tooth row extends 

anteriorly to reach near the expanded tip of the 

snout; this condition is not compatible with 

the presence of a keratinous beak previously 

suggested for other aetosaurs. The conical 

shape of the teeth of N. engaeus differs from 

the slightly compressed teeth of Desmatosuchus, 

Stagonolepis and Typothorax, and the 

distinctly recurved teeth of Aetosaurus and 

Aetosauroides. This diversity of dental morphology 

suggests a variety of food-item preferences 

among aetosaurs. 

2008010309 

82

摩洛哥 Argana 盆地晚三叠世一新 

Rauisuchian = A new Rauisuchian (Archosauria, 

Suchia) from the upper Triassic of 

the Argana basin, Morocco. ( 英文 ). Jaltl N; 

Peyer K. Palaeontology, 2007, 50(2): 417-430 

In the 1970s the Upper Triassic strata of the 

Argana Basin yielded archosaurian remains 

that were tentatively attributed to the rauisuchian 

Ticinosuchus. Restudy of this material 

together with new remains reveal new anatomical 

data and show that it in fact belongs to 

a new taxon, Arganasuchus dutuiti gen. et sp. 

nov. The systematics of the Rauisuchia are 

still unresolved; nevertheless, a monophyletic 

suprageneric group can be defined within the 

probable non-monophyletic rauisuchians. Arganasuchus 

dutuiti differs from all adequately 

known rauisuchians in three autapomorphies: 

acetabular rim on pubis runs anteroventrally 

parallel to pubic shift rather than being terminal 

and perpendicular to it; large contribution 

of pubis to acetabular depression; palatal 

process of maxillary low and confluent with 

interdental crest, rather than separated from it 

by a large area. The maxilla of Arganasuchus 

resembles those of Batrachotomus and Fasolasuchus 

in having a Y-shaped rather than a 

U-shaped form. As in rauisuchids, Arganasuchus 

dutuiti has short cervical vertebrae 

and a dorsal border of the proximal extremity 

of the pubis that is convex in lateral view. It 

shares one derived character state with Batrachotomus 

and Postosuchus (a tear-shaped and 

anteriorly orientated rugosity on the lateral 

side of the pubis, lying on a deep, longitudinal 

depression) and one more derived character 

state with Batrachotomus (narrow anteacetabular 

part of the pubis; hence, the anterior 

border of the proximal extremity of the 

pubis is almost contiguous with the actabular 

rim). 

2008010310 

德国西南部早侏罗世 Posidonia 页岩中蛇颈 

龙的分类学和系统学位置 = The taxonomic 

and phylogenetic position of the Plesiosauroidea 

from the lower Jurassic Posidonia shale 

of south-west Germany. ( 英文 ). Großmann F. 


The two plesiosauroid species from the 

Posidonia shale of Holzmaden, ‘Plesiosaurus’guilelmiimperatoris 

and ‘Plesiosaurus’brachypterygius, 

do not belong to Plesiosaurus 

but form new monotypic genera. The 

new genus Hydrorion is erected for 

‘P.’brachypterygius, and the genus Seeleyosaurus 

is re-established for ‘P.’ guilelmiimperatoris. 

The recently described species Plesiopterys 

wildii is regarded as a junior synonym 

of S. guilelmiimperatoris. A short phylogenetic 

analysis shows that 

S. guilelmiimperatoris and Muraenosaurus are 

basal elasmosaurs. H. brachypterygius, Occitanosaurus 

tournemirensis from France and 

Microcleidus homalospondylus from England 

form a monophyletic clade, which is the sister 

taxon to the Cretaceous elasmosaurs. A palaeobiogeographical 

comparison of plesiosaur 

localities in the Lower Jurassic shows distinct 

palaeobiogeographical zones for the Toarcian, 

with different plesiosaur taxa in England, 

Germany and France 

2008010311 

南非早三叠世 Platycraniellus elegans( 兽 

孔目 , 犬齿兽亚目 ) 的重新描述以及 

Eutheriodonts 的系统关系 = Redescription 

of Platycraniellus elegans (Therapsida, Cynodontia) 

from the Lower Triassic of South Africa, 

and the Cladistic Relationships of 

Eutheriodonts. ( 英文 ). Abdala F. Palaeontology, 

2007, 50(3): 591–618 

Platycraniellus elegans is an enigmatic Triassic 

cynodont from South Africa that has 

only been briefly described previously. New 

preparation of the holotype and additional unpublished 

material allows a detailed redescription 

and comparison with different cynodonts. 

Platycraniellus elegans is recognized as a 

valid species of basal cynodont. The distinct 

suborbital angulation of the zygomatic process, 

previously considered as a diagnostic character 

in chiniquodontid cynodonts, and more 

recently observed in some galesaurids, is also 

present in P. elegans. A larger, second specimen 

was initially referred to P. elegans, but 

most recently considered to belong to Galesaurus 

planiceps. Close comparison of this 

specimen with the holotype of P. elegans and 

with galesaurid specimens allows a tentative 

allocation to G. planiceps. A cladistic analysis 

of 32 taxa (two gorgonopsians, seven therocephalians 

and 23 cynodonts) and 96 craniodental 

characters places P. elegans as sister 

taxon of Eucynodontia. Results from the 

analysis favour a dichotomy between (1) Cynognathia, 

including the sectorial-toothed 

cynodonts Ecteninion, Cynognathus and the 

gomphodont cynodonts, and (2) Probainognathia, 

including most sectorial-toothed eucynodonts 

(e.g. Lumkuia, Probainognathus, 

Chiniquodon), tritheledontids, tritylodontids 

and mammaliaforms. The Late Triassic secto- 

83

ial-toothed Ecteninion is the most basal 

member of Cynognathia, whereas the Middle 

Triassic Lumkuia is the basal representative of 

Probainognathia. Tritylodontids (Oligokyphus 

and Kayentatherium) are placed among Probainognathia, 

forming a monophyletic group 

with the tritheledontid Pachygenelus, whereas 

Brasilitherium is the sister taxon of Mammaliaformes. 

The cladistic analysis also indicates 

paraphyly for Therocephalia, with the 

whaitsiid Theriognathus identified as sister 

taxon of Cynodontia. 

2008010312 

非洲东部坦桑尼亚晚侏罗世 Tendaguru 层 

第二例冈瓦纳 Diplodocid 恐龙 = A second 

Gondwanan Diplodocid Dinosaur from the 

upper Jurassic Tendaguru Beds of Tanzania, 

East Africa. ( 英文 ). Remes K. Palaeontology, 

2007, 50(3): 653-667 

A new genus and species of diplodocid 

sauropod (Sauropoda, Diplodocoidea), Australodocus 

bohetii, is described. The type material 

from the Upper Jurassic (Tithonian) 

Tendaguru Beds of Tanzania, East Africa, 

consists of two successive mid-cervical vertebrae. 

These vertebrae do not show the extreme 

elongation of the cervical vertebrae that is 

diagnostic for Tornieria, and, apart from proportional 

differences, exhibit four autapomorphic 

characters not seen in other diplodocids: 

(1) pleurocoel weakly developed; (2) ridge 

posterolateral to the anterior condyle strongly 

posteroventrally orientated; (3) triangular 

pneumatic cavity ventral to the prezygapophysis, 

enclosed by the lateral ramus of the centroprezygapophyseal 

lamina and an anteriorly 

extended prezygodiapophyseal lamina; and (4) 

prominent prezygapophyseal process pointed, 

laterally keeled and surpassing the prezygapophysis 

anteriorly. Australodocus bohetii is 

the second diplodocid known from Tendaguru, 

and thereby the second diplodocid known 

from Gondwana. This impedes the customary 

reference of isolated East African diplodocid 

material to Tornieria, which can now only be 

assigned to Diplodocidae indet. The find supports 

previously proposed vicariance models 

of diplodocid palaeobiogeography. 

2008010313 

不列颠和北欧始新世 Tomistominer 的系统 

学和分类学 = Systematics and Taxonomy of 

Eocene Tomistomine Crocodylians from Britain 

and Northern Europe. ( 英文 ). Brochu C A. 


The holotype of Dollosuchus dixoni (Owen) 

from the Early–Middle Eocene Bracklesham 

Beds of England is a set of mandibular fragments 

that cannot be distinguished from corresponding 

parts of other longirostrine crocodylians. 

An isolated humerus from the Bracklesham 

Beds is consistent with a gavialoid, but 

it cannot be referred to the holotype of 

D. dixoni. The name Dollosuchoides 

densmorei is established for the wellpreserved 

skull and skeleton of a tomistomine 

from the Middle Eocene of Belgium that had 

been referred to D. dixoni. It can be clearly 

distinguished from the basal tomistomine 

‘Crocodilus’ spenceri Buckland from the 

Lower Eocene of England, which cannot be 

referred to Dollosuchoides and is provisionally 

referred to Kentisuchus Mook. Although 

basal within Tomistominae, Dollosuchoides is 

more closely related to Tomistoma than to 

Kentisuchus. 

2008010314 

中国早白垩世角龙基部类群 Psittacosaurus 

的社会行为和集群死亡 = Social Behaviour 

And Mass Mortality In The Basal Ceratopsian 

Dinosaur Psittacosaurus (Early Cretaceous, 

People's Republic Of China). ( 英文 ). Zhao Qi; 

Barrett P M; Eberth D A. Palaeontology, 2007, 

50(5): 1023-1029 

An exceptionally preserved herd of the 

ceratopsian dinosaur Psittacosaurus was recovered 

from the Lujiatun Beds of the Lower 

Cretaceous Yixian Formation, Liaoning Province, 

north-east China. This specimen provides 

the earliest direct evidence of postnestling 

gregarious behaviour in this important 

dinosaur clade. The sediment in which the 

skeletons occur represents a lahar (volcanic 

mudflow), indicating that the six individuals 

present were entombed simultaneously during 

a catastrophic mass mortality event. Reconstruction 

of the herd age profile shows it was 

composed of offspring from at least two 

clutches, revealing that group fidelity in these 

dinosaurs extended beyond time spent together 

in the nest. This demonstrates that sociality 

appeared much earlier in ceratopsian 

evolution than is generally acknowledged and 

that such behaviour preceded the evolution of 

the elaborate horns and frills seen in derived 

ceratopsids. 

2008010315 

区别晚二叠世 Oudenodon bainii 和 Tropidostoma 

microtrema 的综合方法 = An Integrative 

Approach To Distinguishing The Late 

84

Permian Dicynodont Species Oudenodon 

Bainii And Tropidostoma Microtrema 

(Therapsida: Anomodontia). ( 英文 ). Botha J; 

Angielczyk K D. Palaeontology, 2007, 50(5): 

1175-1209 

The dicynodonts Oudenodon bainii and 

Tropidostoma microtrema are remarkably 

similar in most aspects of their morphology. 

The most obvious distinguishing feature is the 

presence of tusks and/or postcanine teeth in T. 

microtrema and their absence in O. bainii. 

However, some specimens of T. microtrema 

lack tusks or postcanine teeth. This variability 

raises the possibility that O. bainii and 

T. microtrema are not distinct species, but 

rather endpoints on a morphological continuum. 

Resolution of this uncertainty is necessary 

because both species play important roles 

in Upper Permian terrestrial biostratigraphy. 

Here we address this issue using several types 

of data. Our results show that the bone histology 

of T. microtrema is comparable with that 

of O. bainii, emphasizing their similarity. 

However, a geometric morphometric analysis 

of snout shape and a traditional morphometric 

analysis of skull dimensions can reliably differentiate 

tuskless specimens from those with 

tusks and/or postcanine teeth. We examine 

several scenarios (e.g. anagenesis, sexual dimorphism) 

that could explain the observed 

distinction, but multiple lines of evidence, 

including stratigraphic range data, suggest that 

the two morphotypes are regarded best as distinct 

species. Because O. bainii specimens 

have been collected at Tropidostoma Assemblage 

Zone localities in the Karoo Basin of 

South Africa, the first appearance of O. bainii 

can no longer be used to define the base of the 

Cistecephalus Assemblage Zone and Oudenodon-based 

correlations with other basins 

should be made with caution. 

2008010316 

关于 Nothosaurus 属的牙齿置换及齿系新 

资料 = New information on the dentition and 

tooth replacement of Nothosaurus (Reptilia: 

Sauropterygia). ( 英文 ). Shang Qing-Hua. palaeoworld, 

2007, 16(1-3): 254-263 

Dental morphology and tooth replacement 

of Nothosaurus are described and discussed in 

detail based on two well-preserved specimens 

of N. rostellatus and a skull of Nothosaurus sp. 

from the Middle Triassic Guanling Formation 

in Guizhou, South China. This study indicates 

that tooth replacement is sequentially alternative 

and asynchronous in the premaxilla, but 

with a wave-like pattern and synchronous in 

the maxilla in Nothosaurus. The replacement 

process is from front to back in the premaxilla, 

and three stages of tooth replace succession 

can be recognized. The incongruent tooth replacement 

rhythms in the premaxilla and maxilla 

may be related to different tooth functions. 

2008010317 

贵州三叠纪海生爬行动物研究进展 = Study 

advances on Triassic marine reptiles in 

Guizhou. ( 中文 ). 王立亭 . 贵州地质 , 2002, 

19(1): 6-9 

贵州三叠纪海生爬行动物主要产于中三 

叠统安尼阶关岭组第一段、第二段及上三 

叠统卡尼阶下部竹杆坡组、瓦窑组等 4 个 

层位。基本上涵盖了世界三叠纪海生爬行 

动物的主要类型 , 有真鳍龙类、鱼龙类、 

海龙类及楯齿龙类。初步研究表明贵州三 

叠纪海生爬行动物特征是 :(1) 其组成虽 

是地方性属种 , 就大的类群 , 总的特征以 

及特殊类群的相对性而言 , 更接近西特提 

斯海域的同期爬行动物群 ;(2) 这些海生 

爬行动物 , 特别是瓦窑组中的一些属种 

( 如周氏黔鱼龙 ) 兼具有三叠纪和侏罗纪 

同类群的一些特征。(3) 其生态分为两种 

类型 : 关岭组第一、二段的海生爬行动物 

类群 , 个体少 , 主要生活在近岸浅水域 ; 

竹杆坡组和瓦窑组的海生爬行动物类群 

多、个体多。主要生活在浅海深水域。 

2008010318 

孙氏新铺龙头骨再研究 = The restudy on the 

skull and mandible of Xinpusaurus suni. ( 中 

文 ). 罗永明 ; 喻羑艺 . 贵州地质 , 2002, 19(2): 

71-76 

本文在进一步修理正模标本的基础上 , 

结合另一完整、近立体的头骨新材料对孙 

氏新铺龙 (Xinpusaurus suni ) 作深入研 

究 , 较详细地描述了孙氏新铺龙头骨主要 

骨骼要素的特征及其相互关系 , 进一步完 

善了孙氏新铺龙的骨骼特征 , 并明确其分 

类位置。 

2008010319 

关岭生物群的生活环境 = Life environment 

of the Guanling biota. ( 中文 ). 王尚彦 ; 王宁 . 

贵州地质 , 2002, 19(4): 240-241 

产于贵州省关岭县新铺乡附近晚三叠世 

早期地层瓦窑组下部的关岭生物群科学意 

义重大、观赏性极好、生活环境独特。岩 

相古地理分析其生活环境为海湾。沉积和 

古生态特征显示生活环境水体平静。 

85

2008010320 

记贵州顶效中三叠世一新的海生爬行动物 

= On a new marine reptile from Middle Triassic 

Yangliujing Formation of Guizhou, China. 

( 中文 ). 刘冠邦 ; 尹恭正 ; 王雪华 ; 王尚彦 ; 黄理 

中 . 高校地质学报 , 2002, 8(2): 220-226 1 图 

版 . 

在贵州兴义顶效绿荫村西大约 150m 绿荫 

水泥厂南面采石场出露的中三叠统杨柳井 

组 ( 拉丁阶 ) 灰黑色中薄层灰岩中发现一 

新的海生爬行动物 —— 绿荫顶效龙 

Dingxiaosaurus luyinensis gen. et sp. nov.。 

它的肢骨形态和结构颇为独特 , 股骨、 

胫、腓骨以及跗骨的形状和结构相似于原 

始的鱼龙 , 而趾骨形状和数目有些相似于 

最早的蛇颈龙 , 但又与所有已知的鱼龙和 

蛇颈龙类的属种均明显不同 , 它是早期海 

生爬行动物进化的一个比较原始而孤立的 

新种类。它的发现对早期海生爬行动物进 

化多样性的认识具有十分重要的科学意 

义。 

2008010321 

辽宁下白垩统义县组恐龙类蜥脚亚目原始 

巨龙牙齿 = Basal titanosauriform (Dinosauria, 

Sauropoda) teeth from the Lower Cretaceous 

Yixian Formation of Liaoning Province, 

China. ( 英文 ). Barrett PM;Wang Xiao-Lin. 

palaeoworld, 2007, 16(4): 265-271 

The Yixian Formation of Liaoning Province, 

People's Republic of China has yielded a diverse 

fauna of non-avian dinosaurs, but is 

dominated by small-bodied taxa. Here, we 

describe a series of isolated teeth from the 

Lujiatun Beds of the formation that are referable 

to a basal titanosauriform sauropod. 

Some of the teeth possess a distinctive circular 

boss on the lingual surface, which suggests 

that they are referable to cf. Euhelopus sp. 

This identification provides some additional 

support for biostratigraphical correlations between 

the Jehol Group and the Mengyin Formation 

of Shandong Province that suggest an 

Early Cretaceous age for the latter unit. Moreover, 

the titanosauriform affinities of the teeth 

provide further evidence for the dominance of 

this sauropod clade in eastern Asia during the 

Cretaceous. 

2008010322 

根据中国下白垩统新化石的 CT 扫描观察 

恐龙类角龙亚目鹦鹉嘴龙的内颅骨的形态 

= Endocranial morphology of psittacosaurs 

(Dinosauria: Ceratopsia) based on CT scans of 

new fossils from the Lower Cretaceous, China. 

( 英文 ). Zhou Chang-Fu; Gao Ke-Qin; Fox R 

C; Du Xiang-Ke. palaeoworld, 2007, 16(4): 

285-293 

Psittacosaurs, small basal ceratopsians with 

a parrot-like beak, are among the most abundant 

dinosaurs, but occur only in the Early 

Cretaceous of East Asia. Although the general 

morphology of psittacosaurs is fairly well understood, 

the endocranial anatomy of the 

group has never been described. New discoveries 

of well-preserved skulls from the celebrated 

Liaoning beds in northeastern China 

provide the material for conducting research 

on psittacosaur endocranial morphology. Using 

computed tomography scans of threedimensionally 

preserved skulls, this study reveals 

basic endocranial anatomy of psittacosaurs 

and provides the first palaeoneurological 

evidence of psittacosaurs in relation to their 

behaviour. Although commonly believed to 

have had a small brain and small eyes, psittacosaurs 

had relatively high brain/body size 

ratios that are comparable to those in the large 

theropod Tyrannosaurus, and probably had a 

keen sense of smell and acute vision, as evidenced 

by their enlarged olfactory lobes and 

bulbous optic lobes. The configuration of the 

semicircular canals agrees with limb proportions 

to suggest that psittacosaurs were agile 

animals, perhaps better able to escape predation 

by carnivorous dinosaurs on that account. 

The behavioural adaptations implied by this 

study may have been crucial for the successful 

radiation of psittacosaurs during the Early 

Cretaceous of East Asia. 

2008010323 

加拿大曼尼托巴下坎潘阶 Pierre 页岩沧龙 

一新种 = A new species of mosasaur (Squamata: 

Mosasauridae) from the Pierre Shale 

(lower Campanian) of Manitoba. ( 英文 ). 

Cuthbertson R S; Mallon J C; Campione N E; 

Holmes R B. Canadian Journal of Earth Sciences, 

2007, 44(5): 593-606 

Plioplatecarpus nichollsae, sp. nov., from 

the lower Campanian (Pembina Member, Pierre 

Shale Formation) is diagnosed by the following: 

a thickened ventral rim of the external 

naris, a short supratemporal fenestra, a frontal 

shield with well-developed posterolateral lappets 

that overlap the parietal dorsally, proximal 

rib shafts with an approximately circular 

(but not inflated) cross section, a scapula 

shaped as in other Plioplatecarpus species but 

approximately the same size (not larger) than 

the coracoid, and a moderately large parietal 

86

foramen that reaches the frontoparietal suture 

but does not invade the frontal. The last two 

characters require that the diagnosis of the 

genus Plioplatecarpus be emended. With 

other Plioplatecarpus species, P. nichollsae 

shares a robust humerus with a distal expansion 

at least as great as the total length of the 

bone, a rectangular preorbital frontal shield, a 

"peg and socket" postorbitofrontal-jugal articulation, 

a transversely directed ectopterygoid 

process of the pterygoid, a large, robust 

quadrate with a distinct eminence on the posterior 

surface of its shaft, an unossified gap in 

the ventral wall of the basioccipital, and at 

least 11 pygal vertebrae. P. nichollsae also 

shares primitive features with Platecarpus, as 

well as features apparently intermediate between 

Platecarpus and Plioplatecarpus. Revision 

of the genus Platecarpus, currently hypothesized 

to be both paraphyletic and polyphyletic, 

as well as a better understanding of 

the early Campanian mosasaur fauna from the 

Morden area, are necessary before the phylogenetic 

significance of some of these characters, 

and therefore the relationships of Plioplatecarpus 

nichollsae, can be fully resolved. 

鸟类 

2008010324 

堪萨斯西部 Niobrara Chalk 的澘水型黄昏 

鸟和鱼鸟骨骼微结构 = Bone microstructure 

of the diving Hesperornis and the voltant Ichthyornis 

from the Niobrara Chalk of western 

Kansas. ( 英文 ). Chinsamy A; Martin L D; 

Dobson P. Cretaceous Research, 1998, 19(2): 

225-233 

We report on the bone microstructure of the 

Cretaceous birds Hesperornis regalisand Ichthyornis 

victor. Thin sections of representative 

elements of both these ornithurine birds show 

a rapid, sustained bone deposition without any 

pauses or interruptions in bone formation. 

This growth pattern contrasts sharply with the 

cyclical pattern of bone deposition previously 

reported for the Cretaceous non-ornithurine 

birds Patagopteryx and representatives of the 

enantiornithines. These findings suggest 

physiological advancement in Cretaceous ornithurine 

birds. The bone microstructure of the 

diving Hesperornisshows similarities to the 

bone structure of modern penguins, and to that 

of a loon from the Cretaceous of Antarctica. 

2008010325 

始鼠化石在甘肃省党河地区上渐新统的发 

现 = Discovery of Late Oligocene Eomyodon(rodentia,mammalia) 

from the Danghe 

area, Gansu, China. ( 中文 ). 王伴月 . 古脊椎 

动物学报 , 2002, 40(2): 139-145 

始鼠科 (Eomyidae) 是一类已绝灭的小型的 

鼠类 , 在古化纪和新近纪时文布全北区 , 

以北美 ( 中始新世 - 晚中新世 ) 和欧洲 

( 早渐新世 - 晚上新世 ) 发现的化石较丰 

富。过去在亚洲发现的始鼠化石极少。亚 

洲的第一个始鼠化石是 1982 年才发现的 

( 郑绍华等 ,1982)。20 世纪 90 年代以 

来 , 在亚洲陆续发现了一些始鼠化石 , 表 

明从中始新世到上新世时在亚洲已有始鼠 

生存过 (Wang and Emry, 1990; Qiu, 1994, 

1996; Tomida and Setoguchi, 1994; Emry et 

al., 1997; 王伴月 ,1999)。但发现化石的 

地点不多 , 而且化石的数量和种类都很有 

限。在甘肃省党河地区采集到的始鼠化 

石 , 是该科化石在这一地区的首次发现 , 

也是亚洲晚渐新世始鼠化石的第二个地 

点。化石虽不多 , 但为研究亚洲始鼠的性 

质与欧洲和北美大陆的有关种类的关系提 

供了有意义的信息。 

2008010326 

辽西含鸟化石层同位素年龄讨论 —— 来自 

磁性地层的证据 = A discussion of the isotopic 

age of the bird fossil-bearing bed in 

western Liaoning——Evidence from a magnetostratigraphic 

analysis of Cretaceous. ( 中 

文 ). 孙知明 ; 杨振宇 ; 赵越 ; 杨天水 ; 裴军令 ; 许 

坤 . 地质通报 , 2002, 21(1): 41-44 

通过对辽西及邻区白垩纪不同剖面的磁 

性地层资料的综合分析 , 对比国际中生代地 

磁极性年表 , 指出义县组含鸟化石层的地质 

时代至少应老于 M13 正极性时 (129.6Ma) 所 

对应的地质年代 , 介于 131.71~142.27Ma 之 

间。综合研究表明 ,Swisher 等通过沉凝灰岩 

中透长石 Ar-Ar 法测定的义县组含鸟化石 

层的同位素年龄 (124.6±0.2)Ma 值得商榷。 

2008010327 

中国首次发现真正会飞的 “ 恐龙 ”— 中华神 

州鸟 ( 新属新种 ) = Discovery of an avialae 

bird--Shenzhouraptor sinensis gen.et 

sp.nov.—from China. ( 中文 ). 季强 ; 姬书安 ; 尤 

海鲁 ; 张建平 ; 袁崇喜 ; 季鑫鑫 ; 李景路 ; 李印先 . 

地质通报 , 2002, 21(7): 377-383 2 图版 . 

记述了辽宁义县早白垩世九佛堂组的一 

件初鸟类 (Avialae) 化石 , 其嘴里无牙 , 前肢明 

显长于后肢 , 尾巴由 20 多节尾椎组成 , 叉骨 

呈 U 字形 , 飞行羽毛超过了身体的长度。各 

种特征表明 , 新发现的初鸟类真正具有了飞 

行能力 , 代表了恐龙向鸟类演化过程中的又 

87

一中间环节。正式将其命名为中华神州鸟 

(Shenzhouraptor sinensis gen. et sp. nov.)。 

2008010328 

澳大利亚早白垩世 enantiornithine 类新材 

料 = New material of enantiornithine birds 

from the Early Cretaceous of Australia. ( 英文 ). 

Kurochkin E N; Molnar R E. Alcheringa, 

1997, 21(3/4): 291-297 

Remains of tiny enantiornithines from the 

Early Cretaceous (Albian) of Queensland, 

Australia, include a proximal tibiotarsus and a 

cervical vertebra consistent in size with Nanantius 

eos (Molnar 1986). The new tibiotarsus 

differs in detail from the type and so probably 

does not pertain to the same species. The vertebra 

is platycoelous with a tendency toward 

opisthocoely. It shows that Enantiomithes had 

distinctive process of vertebral development, 

different from that in true birds which produces 

heterocoelous vertebrae. The excellent 

preservation of the vertebra permits the accurate 

orientation of fragmentary vertebrae in 

some Enantiomithes known from other continents. 

It also corroborates both the existence 

of Enantiomithines in the Early Cretaceous of 

Australia and the small size of the genus Nanantius. 

2008010329 

巴西晚古新世布谷鸟一新早期类群 : 

Eutreptodactylus itaboraiensis = Eutreptodactylus 

itaboraiensis gen et sp nov, an early 

cuckoo (Aves: Cuculidae) from the Late Paleocene 

of Brazil. ( 英文 ). Baird R F; Vickers 

Rich P. Alcheringa, 1997, 21(1/2): 123-127 

Eutreptodactylus itaboraiensis from Late 

Paleocene karst deposits of eastern Brazil is 

the oldest and most primitive member of the 

Cuculidae known to date. It is one of the oldest 

fossils that can be placed in a modem family 

of birds. The zygodactyl condition, characterising 

the cuculids, is present in Eutreptodactylus, 

but the relative rotation of the 

trochlea metatarsi TV is slight in comparison 

with that in extant cuculids, suggesting that 

this bird may not have been an obligate zygodactyl 

form. Since zygodactyly had developed 

within the Cuculiformes by the Late Paleocene, 

it follows that the other family in this 

order, the Musophagidae, must have diverged 

by the early part of the Cainozoic. 

2008010330 

中华神州鸟的发现及其科学意义 = Discovery 

of Shenzhouraptor sinensis Ji et 

al.,2002,and its scient ific value. ( 中文 ). 季强 . 

中国地质 , 2002, 29(3): 335- 

本文简要回顾了国际鸟类起源研究的历 

史 , 论述了中华神州鸟的发现在鸟类起源和 

早期演化研究中的科学意义 , 有力支持了鸟 

类的 “ 兽脚类恐龙起源假说 ” 和 “ 陆地奔跑飞 

行起源假说 ”。 

2008010331 

新西兰中更新世秧鸡化石 = A mid- 

Pleistocene rail from New Zealand. ( 英文 ). 

Worthy T H. Alcheringa, 1997, 21(1/2): 71-78 

Fossil bones of a new genus and species of 

rail (Aves: Rallidae) are described from one 

million year old shoreline deposits near Marton, 

North Island, New Zealand. Associated 

bones indicate the presence of a specifically 

indeterminate rail, an indeterminate avian species, 

and a moa (Aves: Dinomithiformes). 

These are the first described fossil terrestrial 

carinates from deposits older than 100,000 

years in New Zealand. 

2008010332 

鸟类的昨天、今天和明天 : 起源与演化 = 

Yesterday, today and tomorrow of Aves: 

Genesis and evolution. ( 中文 ). 季强 . 江苏地 

质 , 2002, 26(4): 193-199 

鸟类是现生生物中最具特色的动物之 

一 , 以其发育了许多独特的形态特征区别 

于其他的现生生物 , 如羽毛、角质喙、中 

空的骨骼、叉骨、具龙骨突的胸骨、尾综 

骨、对握状的脚趾等等。长期来人们一直 

想知道鸟类究竟由哪一类生物演化发展而 

来。但苦于化石材料的贫乏 , 鸟类的起源 

问题一直是个令人头疼的迷团 , 困扰我们 

长达 140 多年。通过回顾自 19 世纪中期以 

来世界上各种鸟类起源假说 , 指出随着中 

国辽西中华龙鸟、原始祖鸟、尾羽鸟等珍 

稀化石的发现 , 国际鸟类起源问题已基本 

上得到解决。越来越多的人相信 : 鸟类是 

由恐龙变来的 , 现代的鸟类就是恐龙的后 

代 , 是长羽毛的 “ 恐龙 ”。 

2008010333 

阿根廷恩特雷里奥斯省晚更新世鸟类 

Geronogyps reliquus = Geronogyps reliquus 

Campbell (Ciconfiformes : Vulturidae) in the 

late Pleistocene from the province of Entre 

Rios and its paleoenvironmental significance. 

( 其他 ). Noriega J I; Tonni E P. 

Ameghiniana, 2007, 44(1): 245-250 

2008010334 

88

辽宁北票首次发现初鸟类化石 - 东方吉祥 

鸟 = A new avialian bird-Jixiangornis orientalis 

gen. et sp. nov.-from the Lower Cretceous 

of western Liaoning, NE China. ( 中文 ). 

季强 ; 姬书安 ; 张鸿斌 ; 尤海鲁 ; 张建平 ; 王丽霞 ; 

袁崇喜 ; 季鑫鑫 . 南京大学学报 ( 自然科学 

版 ), 2002, 38(6): 723-736 

本文记述了辽宁北票义县组一件新的初 

鸟类 (Avialae) 化石 , 这是继中华神州鸟 

(Shenzhouraptor sinensis Ji et al.2002) 之 

后初鸟类化石的又一发现。它以上颌无齿 

而具角质喙、胸骨发达且具龙骨突、前肢 

显著长于后肢等特征与始祖鸟 

(Archaeopteryx) 不同 , 以后肢第 Ⅰ 趾爪 

已反转而与其它 3 趾对握等特征与神州鸟 

相区别 , 该化石被命名为东方吉祥鸟 ( 新 

属、新种 )(Jixiangornis orientalis gen.et 

sp. nov.)。中国辽西新近发现的中华神州 

鸟和东方吉祥鸟 ( 新属、新种 ) 目前是世 

界上最古老最原始真正具有角质喙和飞行 

能力的原始鸟类。 

哺乳类 

2008010335 

关于缅甸中新统 Tetraconodon 的修订及对 

该属一新种的描述 = A revision of Tetraconodon 

(Mammalia, Artiodactyla, Suidae) 

from the Miocene of Myanmar and description 

of a new species. ( 英文 ). Thaung H; 

Tsubamoto T; Takai M; Natori M; Egi N; 

Maung M; Chit S. Paleontological Research, 

2005, 9(3): 243-253 

We describe five new dento-gnathic specimens 

of Tetraconodon, a genus of Miocene 

tetraconodontine suid (Mammalia, Artiodactyla), 

discovered in Myanmar (=Burma). In 

Myanmar, we recognized three distinct species 

of Tetraconodon (T. minor, T. intermedius 

and T. malensis sp. nov.) and one specifically 

undetermined specimen, which is here 

named Tetraconodon sp. cf. T. intermedius. 

The new species, T. malensis, has characteristics 

of Tetraconodon, such as extremely 

enlarged P_4 and simple and relatively small 

M_3. It is distinct from the other Tetraconodon 

species in being much smaller, suggesting 

that it is the most primitive known Tetraconodon 

species. The dental size and characteristics 

of T. malensis suggest that Tetraconodon 

was derived during the late middle Miocene 

from the early middle Miocene Conohyus sindiensis, 

which was discovered in the Siwalik 

Group of Indo-Pakistan and Nepal and has 

also been found in the middle Miocene deposits 

of Thailand, or a close relative. The discovery 

of the most primitive form in Myanmar 

suggests that Tetraconodon may have originated 

in Myanmar. 

2008010336 

根据阿根廷更新世新材料对 Theriodictis 

platensis 的生态形态分析 = Ecomorphological 

analysis of the hypercarnivore canid 

Theriodictis platensis Mercerat based on new 

material from the Pleistocene of Argentina. 

( 其他 ). Prevosti F J; Palmqvist P. 

Ameghiniana, 2001, 38(4): 375-384 

Theriodictis was part of a South American 

clade of canids showing hypercarnivorous 

characters such as large carnassial teeth lacking 

the metaconid and the hypoconid, wide 

palate, and small postcarnassial molars. This 

genus comprises two species: T. platensis 

Mercerat, from the pampean region of Argentina, 

and T. tarijensis (Ameghino) from Tarija, 

Bolivia. Both are restricted to the Ensenadan 

Age, early to earliest late Pleistocene (Biozone 

of Tolypeutes pampeus, 1.8 to 0.5 Ma). The 

discovery of an almost complete skeleton of T. 

platensis (MLP 96-IX-1-1) permits an ecomorphological 

analysis. This approach uses 

principal component and discriminant function 

analyses, as well as multiple regression 

analysis for estimating ecomorphological adaptations 

and body mass in extinct canids. The 

body mass estimated for T. platensis was similar 

to37 kg. The craniodental morphology of 

this species was similar to that shown by extant 

hypercarnivorous canids whose diet includes 

>70% of herbivores and other carnivores. 

The potential ungulate prey of T, platensis 

included camelids (Lama sp.), cervids 

[Epieurycerus truncus Ameghino, Antifer ensenadensis 

(Ameghino)], equids [Equus 

(Amerhippus) sp., Hippidion devillei (Gervais)], 

and tayassuids (Catagonus metropolitanus 

Ameghino), as well as giant rodents 

(Neochoerus sp.), mesotherids (Mesotherium 

cristatum Serres), and giant dasypodids [Eutatus 

seguini (Gervais), Propraopus grandis 

Ameghino, Pampatherium sp.]. 

2008010337 

阿根廷布宜诺斯艾利斯省 Tandilia 晚更新 

世和全新世山 Galea 属 = Late Pleistocene 

and Holocene Galea (Rodentia, Caviidae) 

from the eastern Sierras de Tandilia, Buenos 

Aires Province, Argentina. ( 其他 ). Quintana C 

A. Ameghiniana, 2001, 38(4): 399-407 

A new record (Galea tixiensis n. sp.) and 

the anatomy of Galea from the archaeological 

89

sites Cueva Tixi and Cueva El Abra, Buenos 

Aires province are described herein. The bearing 

levels were radiometrically dated (C-14). 

Individuals of this species may reach a larger 

size than other known species of the genus, 

reaching a similar size to that of Cavia aperea 

Erxleben. This new species is characterized by 

a greater development of the interpremaxilar 

foramen, the rhomboid incisive foramen, wide 

palate, and robust zigomatic arch. This species 

became extinct during historical times. 

2008010338 

阿根廷土库曼塔菲峡谷晚更新世 

sigmodontines: 分类、埋葬学和古环境重 

建 = Late Pleistocene sigmodontines (Mammalia 

: Rodentia)from the Tafi valley (Tucuman, 

Argentina): Taxonomy, taphonomy 

and paleoenvironmental reconstruction. ( 其 

他 ). Ortiz P E; Pardinas U F J. 

Ameghiniana, 2001, 38(1): 3-26 

An exceptionally rich rodent assemblage of 

Lujanian age (latest Pleistocene) at La Angostura 

(26 degrees 55' 30" S, 65 degrees 41' 50" 

W, Tafi valley, Tucuman province; 1900 m 

above sea level) provides the first evidence of 

sigmodontine rodents in the fossil record of 

northwestern Argentina. Identified taxa are: 

Abrothrix illuteus Thomas, Akodon sp., 

Necromys cf. N. lactens (Thomas), 

Oxymycterus cf. O, paramensis Thomas, Oligoryzomys 

cf. O. flavescens (Waterhouse), 

Oligoryzomys cf. O. "longicaudatus" (Bennett), 

Andinomys edax Thomas, Calomys cf. C. 

laucha C. musculinus, Neotomys ebriosus 

Thomas, Phyllotis sp., Reithrodon auritus 

(Fischer), and dagger Tafimys powelli Ortiz et 

al. These include the first fossils of the genera 

Neotomys Thomas and Andinomys Thomas in 

Argentina. Taphonomic analysis indicates that 

the assemblage is a fossil owl pellet accumulation. 

Consequently, it can be assumed to be a 

biased representation of the small mammal 

fauna of a relatively small area over a relatively 

brief time span. This association has no 

modern analogue because today these species 

live at different altitudinal vegetation belts. 

The fauna indicates a community from the 

high-altitude grassland ecotone, with elements 

of the Yungas, Puna and High Andeans. Temperatures 

may have been lower than today. 

Although the species composition is similar to 

the modem sigmodontine community in the 

area, quantitative variations in proportional 

representation can be attributed to Holocene 

climatic conditions and, probably, to the impact 

of human populations in historical times. 

2008010339 

Glyptodon clavipes 的后肢中 osteoderms 的 

出现 = On the presence of osteoderms in the 

hindlimbs of Glyptodon clavipes Owen, 1839 

(Mammalia : cingulata).. ( 其他 ). Rinderknecht 

A. Ameghiniana, 2000, 37(3): 369-373 

Hind limb osteoderms of an individual assigned 

to Glyptodon clavipes Owen, from the 

Pleistocene of Uruguay are described. A great 

number of these bones were observed in the 

foot, as well as in the calf and thigh. These 

elements had been cited for gliptodonts, but 

their form and distribution had never been 

studied. 

2008010340 

澳大利亚西北部 Riversleigh 地区渐新世 - 中 

新世一个新的 petauroid = A new petauroid 

possum from the Oligo-Miocene of Riversleigh, 

northwestern Queensland. ( 英文 ). 

Brammall J R. Alcheringa, 1999, 23(1/2): 31- 

50 

Djaludjangi yadjana sp, nov, represents a 

previously unknown genus of petauroid possum 

from Riversleigh in northwestern Queensland. 

Of known phalangeridans Djaludjangi 

most closely resembles the Petauridae, but 

lacks synapomorphies previously used to define 

that family. Although considered likely a 

plesiomorphic petaurid, D. yadjana is referred 

here to Petauroidea: incertae sedis, pending 

comprehensive revision of phalangeriform 

dental character state distributions, Small possum 

diversity at Riversleigh indicates a complex 

and finely partitioned environment such 

as that found in present-day tropical forests; 

the discovery at Riversleigh of Australia's first 

Tertiary dactylopsiline species also argues for 

a rainforest palaeohabitat. 

2008010341 

安徽芜湖金盆洞旧石器遗址的偶蹄类 = 

Artiodactylia from the Jinpendong Site in 

Wuhu, Anhui Province. ( 中文 ). 董为 ; 金昌柱 ; 

郑龙亭 ; 孙承凯 ; 吕锦燕 ; 徐钦琦 . 人类学学 

报 , 2006, 25(2): 161-175 

经对 2002 年与 2004 年出土于安徽芜湖 

金盆洞遗址的偶蹄类所做的深入研究 , 金盆 

洞遗址的偶蹄类有 6 个种 : 李氏野猪 (Sus 

lydekkeri)、梅花鹿 (Cervus (Sika) nippon)、 

葛氏斑鹿 (Cervus (Sika) grayi)、马鹿 (Cervus 

elaphus)、麂未定种 (Muntiacus sp.) 及古中华 

野牛相似种 (Bison cf. palaeosinensis)。其中 

以鹿科为主 , 以梅花鹿和马鹿为优势种群 , 具 

90

有北方区动物群的特色。它们所指示的时 

代比和县龙潭洞动物群晚 , 与巢县银山巢县 

人动物群相当 , 为中更新世晚期 , 在古气候上 

处于 Riss 冰期。它们所处的生态环境以低矮 

森林为主、间有少量灌木密林及草地 , 当时 

的气候与现今的内蒙和甘肃相似。鹿属 3 

个种的同时出现反映金盆洞遗址是史前人 

类汇集处理猎物的场所。 

2008010342 

万寿岩旧石器时代遗址埋藏学研究 = A 

taphonomic study of the Wanshouyan Paleolithic 

site. ( 中文 ). 陈子文 ; 李建军 ; 范雪春 . 人 

类学学报 , 2006, 25(3): 220-226 

本文对福建三明万寿岩遗址文化层形 

成、遗物与动物骨骼埋藏、风化、破坏等 

现象进行观察 , 认为灵峰洞旧石器早期文 

化遗物和化石 , 由于暴露于洞内表面时间 

较长而经受强烈风化、侵蚀与钙质胶结 ; 

船帆洞旧石器晚期遗址因洞口坍塌和外部 

水流侵漫进洞而被废弃 , 在潮湿环境下 , 

遗物和化石遭受腐蚀、铁锰质浸染严重。3 

个文化层的遗物及伴生哺乳动物化石均属 

原地埋藏类型 ; 而船帆洞内 3 号支洞化石 

的集聚是高层洞穴作为排泄通道时由流水 

携带堆积而成的异地埋藏。 

2008010343 

芜湖金盆洞旧石器遗址的食肉类 = Study on 

carnivora fossil remains from the Jinpendong 

cave, Wuhu, Anhui. ( 中文 ). 刘金毅 ; 郑龙亭 ; 

徐钦琦 ; 孙承凯 ; 吕锦燕 ; 谢小成 . 人类学学 

报 , 2006, 25(3): 227-241 

安徽芜湖金盆洞为新近发现的一处旧石 

器遗址 ,2002--2004 年间两度发掘 , 除了 

人工制品外 , 另发掘出众多的哺乳动物化 

石。本文系统研究了其中的食肉类 , 经鉴 

定共计 9 属 11 种 , 即 Nyctereutes 

cf.N.sinensis、Canis variabilis、Arctonyx 

collaris rostratus、 Meles sp.、Mustela 

sibirica 、 Mustelidae gen . et sp . indet 、 

Ursus thibetanus kokeni 、 Ursus arctos 、 

Pachycrocuta brevirostris sinensis、Panthera 

tigris 和 Panthera sp.。食肉类化石数量不 

多 , 但种类颇丰 , 对于探讨和分析遗址的 

地质年代具有重要意义。短吻硕鬣狗中国 

亚种的存在排除了晚更新世的可能 , 对比 

表明它与安徽和县龙潭洞动物群最为接 

近 , 可能稍晚于后者 , 应为中更新世中晚 

期。金盆洞主要由北方类型的动物构成 , 

变异狼是长江以南地区的首次发现 , 黄鼬 

在南方同样十分少见 , 这表明金盆洞当时 

的气候较现今偏冷。与龙潭洞动物群相 

比 , 喜湿润的动物稀少 , 显然金盆洞的气 

候偏干些。 

2008010344 

内蒙古阿左旗乌兰塔塔尔早渐新世鬣齿兽 

化石 = Creodont (mammalia) remains from 

the Early Oligoceneof Ulantatal, Nei Mongol. 

( 中文 ). 黄学诗 ; 朱宝成 . 古脊椎动物学 

报 , 2002, 40(1): 17-22 

记述了在内蒙古阿左旗乌兰塔塔尔早渐 

新世乌兰塔塔尔组中发现的鬣齿兽一新 

种 — 内蒙古鬣齿兽 (Hyaenodon neimongoliensis 

sp.nov.)。新种在大小和特征上 

与 Hyaenodon pervagus 相近或相似 , 但它的 pl 

为单齿根 , 前面的下前臼齿之间有齿隙 , 下颊 

齿无舌侧齿带。 

2008010345 

甘肃临夏盆地晚中新世豪猪一新种 = A 

porcupine from Late Miocene of Linxia Basin, 

Gansu, China. ( 中文 ). 王伴月 ; 邱占祥 . 古脊 

椎动物学报 , 2002, 40(1): 23-33 

在甘肃临夏盆地发现豪猪化石一新种 , 甘 

肃豪猪 (Hystrix gansuensis)。其主要特征是 : 

个体大 ; 鼻骨较宽大 , 后缘圆凸 , 达 M3 的后上 

方 ; 门齿与 P4 间齿缺长 , 腭面较宽 , 两齿列彼 

此近于平行 ; 后鼻孔前缘弧形 ; 颊齿为中度单 

面高冠 ;P4 的前边脊短 , 褶 I 向颊侧开口 , 具低 

小的前附尖 ; 上臼齿褶 I 不向颊侧开口 ;M3 较 

少退化。根据共生的哺乳动物群判断 , 其时 

代为晚中新世。 

2008010346 

广西田东雾云洞更新世脊椎动物群 = Pleistocene 

vertebrate fauna from Wuyun Cave of 

Tiandong County, Guangxi. ( 中文 ). 陈耿娇 ; 

王頠 ; 莫进尤 ; 黄志涛 ; 田锋 ; 黄慰文 . 古脊椎动 

物学报 , 2002, 40(1): 42-51 1 图版 . 

发现于广西田东雾云洞之脊椎动物化石 

有 9 目 24 科 44 属种 , 根据动物群的组成分 

析并结合地貌特征判断 , 其时代为中更新世 

或晚更新世早期。根据动物习性分析 , 其生 

存的环境为热带 - 亚热带温暖湿润的环境。 

2008010347 

甘肃灵台雷家河新第三纪晚期的大哺乳动 

物组合及其时代 = The Late Neogene macromammalian 

assemblagesfrom Lingtai, 

Gansu Province, China. ( 中文 ). 陈冠芳 . 古脊 

椎动物学报 , 2002, 40(1): 70-79 

91

PP 

讨论的大哺乳动物化石出自甘肃灵台雷 

家河村东南小石沟 [72074(1)、72074(4)] 和 

文王沟 (93002) 等地的新第三纪晚期地层。 

它们包括 15 种 , 分属 8 属、9 科、4 目 , 可能 

代表两个不同时代的组合。第一组合所在 

的地层层位是 72074(4) 剖面的 L5~L3 层和 

72074(1) 剖面的第 3 层 , 主要由 Hipparion 

pater、Acerorhinus sp.、Nyctereutes.、 

Hyaeninae gen . et sp . indet . 和 Gazella 

niheensis 等类型组成 , 其性质与山西榆社高 

庄组南庄沟段和醋柳沟段产出的大哺乳动 

物的接近 , 时代可能为中上新世。第二组合 

所在的地层层位是 72074(1) 剖面的第 2 层 , 

以 Anancus sinensis 和 Cervidae gen . et 

sp.indet. 为代表 , 其性质与榆社麻则沟组 

动物群的相近 , 时代为晚上新世。 

2008010348 

安徽潜山晚古新世鼩鼱目 ( 哺乳纲 ) 一新属 = 

A new genus of soricomorpha (mammalia) 

fromthe Late Paleocene of Qianshan Basin, 

Anhui Province. ( 中文 ). 黄学诗 ; 郑家坚 . 古脊 

椎动物学报 , 2002, 40(2): 127-132 

记述了在安徽省潜山盆地晚古新世地层 

中发现的晌髓类的一个新属新种 ── 李氏皖 

掠兽 (Wanolestes lii gen. et sp. nov.)。新属以 

4 

臼齿化程度低 , 下颊齿跟座脊状 , 仅具两个 

下臼齿为其特点。 

2008010349 

山西垣曲盆地中始新世的原翼齿兽 ( 鬣齿兽 

科 , 肉齿目 , 哺乳纲 ) 化石 = Propterodon 

(Hyaenodontidae, Creodonta, mammalia) 

from the Middle Eocene of Yuanqu Basin, 

Shanxi Province. ( 中文 ). 刘丽萍 ; 黄学诗 . 古 

脊椎动物学报 , 2002, 40(2): 133-138 

记述了在山西省垣曲县王茅乡郭家村火 

石坡地点发现的原翼齿兽属一新种 ── 童氏 

原翼齿兽 (Dropterodon tongi sp. nov.)。新 

种比伊尔丁原翼齿兽 (P. irdinensis) 个体小、 

下颌联合部靠前、下前臼齿之间有齿隙、 

m3 跟座小。新材料为垣曲盆地可能存在中 

始新世伊尔丁曼哈期地层提供了证据。 

2008010350 

山西天镇后裂爪兽属 ( 哺乳动物纲 , 蹄兔目 ) 

化石初步报道 = Preliminary report on Postschizotherium 

(mammalia:Hyarcoidea) material 

from Tianzhen, Shanxi, China. ( 中文 ). 邱 

占祥 ; 卫奇 ; 裴树文 ; 陈哲英 . 古脊椎动物学 

报 , 2002, 40(2): 146-160 

山西天镇的蹄兔化石被定为 

Postschizotherium intermedium。这是该属目 

前所知最好的一批材料 , 使我们对该属头骨 

、下颌和牙齿的特征有了更多、更确切的 

了解。该属头骨吻部拉长变宽 , 门齿间有长的 

齿隙 ; 头骨和下颌骨具多个凹陷 ; 上臼齿单面 

高冠 , 白垩质发育。这些特征足以把它和所有 

其他相近的属区别开来。后裂爪兽属似有明 

显的雌、雄性差异 , 主要表现在个体大小和 

门齿的形态及粗壮程度上。天镇产后裂爪兽 

化石地层的地质时代 , 根据蹄兔化石的进化 

水平和整个动物群性质判断 , 比泥河湾典型 

层位要早 , 可能应在 1.8Ma~2.6Ma 之间。 

2008010351 

中国晚中新世陆相哺乳动物群序列 : 陕西蓝 

田的新证据 ( 英文 ) = Land mammal faunal 

sequence of the Late Miocene of China:new 

evidence from Lantian,Shaanxi Province. ( 英 

文 ). 张兆群 ;A W Gentry;A Kaakinen; 刘丽 

萍 ;J P Lunkka; 邱铸鼎 ;S Sen;R Scott;L Werdelin; 

郑绍华 ; 傅铭楷 . 古脊椎动物学报 , 2002, 

40(3): 165-176 

自 20 世纪 60 年代 , 陕西蓝田地区就以连 

续的晚新生代地层及丰富的哺乳动物化石 

而成为研究中国晚新生代哺乳动物与地层 

划分对比的经典地区之一。李传夔等 (1984) 

根据灞河组发现的哺乳动物化石建立了灞 

河期 , 并与欧洲的 Vallesian 期对比。邱占祥 

等 ( 1990,1995) 认为化石证据不充分 , 而将其 

与保德期合并。近年来 , 黄土高原三趾马红 

粘土大量的年代学资料表明 , 红粘土沉积最 

早可能开始于约 8Ma 前。因此 , 狭义的保德 

期可能只代表了晚中新世晚期 , 晚中新世哺 

乳动物分期的再划分问题又重新被提出。 

自 1997 年以来 , 我们课题组在蓝田地区共发 

现 52 个化石地点 , 其中的 26 个含有哺乳动 

物化石 , 大哺乳动物化石标本共计 1666 件。 

经过详细野外地层测量 , 绘制了综合地层剖 

面 , 并将主要含哺乳动物化石的地点对比标 

定到综合地层剖面上。经过对各门类化石 

的初步研究 , 以及对已有化石材料的初步修 

订 , 到目前为止 , 陕西蓝田灞河组共计发现哺 

乳动物化石 45 种 , 蓝田组 20 种。 

2008010352 

云南禄丰古猿地点的松鼠类化石 = Sciurids 

from the Late Miocene Lufeng hominoid locality, 

Yunnan. ( 英文 ). 邱铸鼎 . 古脊椎动物 

学报 , 2002, 40(3): 177-193 

92

记述了云南禄丰晚中新世石灰坝古猿地 

点发现的松鼠科化石。禄丰石灰坝动物群 

的松鼠动物共有 7 属 7 种 : 地松鼠 

Sciurotamias wangi sp. nov., 树松鼠 Tamiops 

sp .、Callosciurus sp .、Dremomys primitivus 

sp. nov. 和飞松鼠 Miopetaurista asiatica 

sp. nov .、Hylopetodon dianense gen. et sp. 

nov.、Pteromyinae gen. et sp. indet.。该动物 

群松鼠类动物的组成以树松鼠和飞松鼠为 

主 , 反映了较为湿润的热带 — 亚热带森林环 

境。在动物地理上 , 其成员几乎局限于东南 

亚分布 , 具有浓厚的现代东洋界色彩。 

2008010353 

狶科化石一新种在内蒙古上始新统的发现 

= A new species of Entelodontidae (artiodactyla, 

mammalia) from Late Eocene of Nei 

Mongol, China. ( 中文 ). 王伴月 ; 邱占祥 . 古脊 

椎动物学报 , 2002, 40(3): 194-202 

记述了在我国内蒙古沙拉木仑地区晚始 

新世乌兰戈楚组中发现的狶科化石 — 内蒙 

古短面狶 ( 新种 ) (Brachyhyops neimongolensis 

sp. nov.)。新种的主要特征是 : 下颌骨深 , 

前臼齿部分更缩短 , 下缘明显斜向前上方 , 颊 

齿主尖高锐 , 脊形 , 上臼齿梯形 , 已形成原脊 , 

原尖位置靠后 ,M3 具次尖 , 后齿带弱。研究 

表明 Eoentelodon 和 Brachyhyops 在下颌骨具 

骨质突起的刍形 , 前部缩短 , 下颌骨联合达 

p3,p3 与 p4 彼此紧靠 , 下臼齿的下前尖与下 

后尖明显分开 , 以及上颊齿的形态上都很接 

近。Eoentelodon 为 Brachyhyops 的后出同物 

异名。 

2008010354 

新疆布尔津地区晚始新世哺乳动物化石的 

发现及其意义 ( 英文 ) = The discovery of Late 

Eocene mammal fossils from Burqin of Xinjiang. 

( 英文 ). 叶捷 ; 孟津 ; 吴文裕 ; 伍少远 . 古脊 

椎动物学报 , 2002, 40(3): 203-210 

1995 年以来作者等人在新疆准噶尔盆地 

北缘乌伦古河地区开展了第三纪哺乳动物 

地层研究工作。在调查研究该区乌伦古河组 

地层同时 ( 叶捷等 ,2001a ,b), 为搞清乌伦古河 

组的区域分布 , 我们在 1999 年和 2001 年先 

后两次前往布尔津地区考察了那里的 “ 乌伦 

古河组 ”。在布尔津县城西北 14km 处额尔齐 

斯河北岸的一片新生代露头 , 长期被视为乌 

伦古河组 , 因而时代也被定为始新世至渐新 

世 , 但一直没有确凿的化石依据。 1 999 年我 

们首次在该套地层中采集到哺乳动物化石 

( 99027 地点 ),2001 年再次在同一地点、同 

一层位采集到化石并实测了地层剖面。布尔 

津的该乌伦古河组地层可大致分为两段 , 下 

段为富含铁质的砂岩与泥岩互层 , 上段为浅 

灰绿色砂岩与杂色泥岩互层 , 整套地层的风 

化表面呈黄棕色。在乌伦古河组建组的乌伦 

古河流域 , 乌伦古河组则由一套浅灰绿色砂 

岩与棕灰色含砂泥岩构成 , 整套地层风化表 

面呈灰白色 ( 叶捷等 ,2001a)。两个地区的乌 

伦古河组的岩性显然是不同的。野外追索证 

明 , 这两个地区的两套不同岩性的地层是两 

个不同沉积盆地的堆积物 , 这两个盆地在乌 

伦古湖附近 (87°12') 被一由古生代地层构成 

的山岭隔开。作为地质体 , 这两套地层间没有 

联系 , 不应当归为同一岩石地层单位。因此 , 

布尔津地区的乌伦古河组名称应该更改。 

在地形图上 , 布尔津地区似乎位于现代广义 

的斋桑盆地中 , 因而必须与斋桑盆地中的相 

应地层做详细对比才能对布尔津地区的该 

套地层冠名。 

2008010355 

犀貘 ( 哺乳纲 , 奇蹄目 , 貘超科 ) 化石在垣曲盆 

地的发现 = Notes on Hyrachyus (mammalia, 

Perissodactyla,Tapiroidea) from the Middle 

Eocene of Yuanqu Basin,Shanxi Province. ( 中 

文 ). 黄学诗 ; 王景文 . 古脊椎动物学报 , 2002, 

40(3): 211-218 

记述了在山西省垣曲盆地发现的犀貘一 

新种 —— 童氏犀貘 (Hyrachyus tongi sp. 

nov.)。它的发现揭示了在垣曲盆地有中中 

始新世地层存在的可能性。还对以往在中 

国境内发现的犀貘化石做了简要评述。 

2008010356 

山东五图早始新世更猴科 

(Plesiadapidae,Mammalia) 化石 = The new 

discovery of the plesiadapiformes from the 

Early Eocene of Wutu Basin, Shandong Province. 

( 中文 ). 傅静芳 ; 王景文 ; 童永生 . 古脊椎 

动物学报 , 2002, 40(3): 219-227 

记述了山东五图盆地早始新世五图组的 

一种更猴类 (plesiadapid) 化石 : 杨氏亚洲更猴 

(Asioplesiadapis youngi gen. et sp. nov.)。在 

它增大的下门齿上具有更猴科特有的下缘 

尖和下缘脊 , 但其下颊齿性状相当原始 ,p4 跟 

座呈盆状 ,m3 下次小尖呈锥状更类似白垩纪 

晚期出现的更猴形动物 Purgatorius 。 

Asioplesiadapis 的下臼齿形态可以说明亚洲 

更猴类虽然有北美和欧洲更猴的某些典型 

特征 , 但并不在同一进化支系。因此 , 另立一 

新亚科 —— 亚洲更猴亚科 (Asioplesiadapinae 

subf. nov.)。 

93

2008010357 

垣曲盆地新发现的始爪兽类化石 = New 

eomoropid (mammalia,perissodactyla) remains 

from the Middle Eocene of Yuanqu 

Basin. ( 中文 ). 黄学诗 . 古脊椎动物学 

报 , 2002, 40(4): 286-290 

记述了在垣曲盆地始新世地层两个层位 

中发现的始爪兽科化石 3 个种 , 其中包括 1 

个新种 — 周氏路南兽 (Lunania zhoui sp. 

nov.)。新种与属型种杨氏路南兽不同在于 

个体小、齿冠低、下前尖和下前脊及下斜 

脊更退化。 

2008010358 

铲齿象一新种在甘肃省党河地区下中新统 

的发现 = A new species of Platybelodon 

(gomphotheriidae,proboscidea,mammalia)from 

Early Miocene 

of the Danghe area,Gansu,China. ( 中文 ). 

王伴月 ; 邱占祥 . 古脊椎动物学报 , 2002, 

40(4): 291-299 

记述了甘肃省党河地区的铲齿象化石一 

新种 — 党河铲齿象 (Platybelodon dangheensis)。 

其主要特征是 : 下颌联合和下门齿构成 

宽短的铲形 ; 下门齿薄 , 由单层稀少的齿柱组 

成 ; 具较大的 p3 ,p4 前窄后宽 , 前齿带和跟座 

较小 ,m1 构造简单 , 齿冠较低 , 第一齿脊无前 

斜脊 , 前齿带和后跟座较小。它是欧亚大陆 

目前所知时代最早 ( 早中新世 )、构造最原 

始的一种铲齿象。 

2008010359 

宁夏同心中中新世三种植食性哺乳动物牙 

齿碳同位素分析 = The stable carbon isotopes 

in the tooth enamel of three species of the 

Middle Miocene fossil herbivorous mammals 

from Tongxin,Ningxia,China. ( 中文 ). 魏明瑞 ; 

郭建崴 . 古脊椎动物学报 , 2002, 40(4): 300- 

304 

宁夏同心中中新世 Platybelodon danovi 

cheni, Amebelodon tobieni 和 Stephanocemas 

thomsoni 化石牙齿的 δ 13 C 值为 - 8.7‰ ~ - 

10.3‰ , 说明这些动物可能以 δ 13 C 值为 - 

20.7‰~- 25.3‰ 的 C 3 植物作为主要食物来 

源。根据齿冠高低与取食嫩叶或硬草的关 

系 , 这三种动物的低冠齿所指示的食性支持 

了牙齿釉质的碳稳定同位素所指示的食 

性。 

2008010360 

临夏盆地晚中新世维氏大唇犀 ( 奇蹄目 , 犀科 ) 

肢骨化石 ( 英文 ) = Limb bones of chilotherium 

wimani (perissodactyla,rhinocerotidae) 

from the late miocene of the linxia basin in 

gansu,china. ( 英文 ). 邓涛 ;. 古脊椎动物学 

报 , 2002, 40(4): 305-316 

大唇犀 (Chilotherium 属 ) 是中国晚中新 

世三趾马动物群中占统治地位的类型 , 在 

亚洲的其他地区和南欧也有广泛的分布。 

然而 , 有关大唇犀头后骼的记述相当少。 

在山西保德和陕西府谷已经发现了丰富的 

大唇犀化石 , 但到目前为止仅有安氏大唇 

犀 (Ch. anderssoni) 的少量头后骨骼被记 

述。维氏大唇犀 (Ch. wimani) 最早发现于 

陕西府谷 , 被记述的材料仅包括头骨标 

本。最近我们在甘肃临夏盆地发现了大量 

晚中新世的 Ch. wimani 化石 , 其中不仅有众 

多的头骨 , 头后骨骼也相当丰富。本文研 

究的标本采自临夏盆地内众多的晚中新世 

三趾马动物群化石地点 , 包括和政县的大 

深沟 , 南阳山 , 大山庄 , 禾托和高家山 , 

广河县的后山 , 兰家山 , 山庄 , 寺沟 , 次 

滩 , 沙地沟 , 阳洼铺子和桥家 , 以及东乡 

县的双拱北等。在保德的三趾马动物群 

中 , 大唇犀以 Ch. anderssoni 和哈氏大唇犀 

(Ch. habereri) 为代表 , 而在临夏和府谷却 

是以 Ch. wimani 为代表。临夏盆地的三趾马 

动物群中共 3 种无角犀类 , 即 Ch. wimani, 

Acerorhinus corutus 和 A. hezhengensis. 根据 

头骨材料的统计。Ch. wimani 在犀类中占有 

绝对优势 ,A. hezhengensis 和 A. cornutus 的 

个体数量很少。与此对应 , 动物群中的无 

角犀为肢骨明显可以分为 3 组 , 其中具中 

等尺寸的一组占有绝对优势。结合形态特 

征 , 占绝大多数的这组肢骨被总总判定应 

属于 Ch. wimani。数量很少的小型和大型的 

两组肢骨可能分别属于 A. corutus 和 A. hezhengensis. 

本文详细记述了 Ch. wimani 的肢 

骨化石 , 它的前 , 后脚都为三趾 , 第三庶骨 

缺乏侧面对骰骨的关节面 , 肢骨相当短 

粗 , 其尺寸与保德发现的 Ch. anderssoni 接 

近 , 但粗装程度略小于后者。Ch. wimani 距 

骨对跟骨的第二和第三关节面愈合或仅有 

很小的间隔 ,Ch. wimani 的头骨性状显示它 

是目前 Chilotherium 属中已知最原始的一个 

种 , 而它的肢骨粗壮程度和距骨关节面特 

征也表明它比其他的大唇犀种更原始。Ch. 

wimani 的肢骨尺寸也与产自保德和新安的 

Acerorhinus palaeosinensis 接近 , 且后者的 

距骨对跟骨的关节面也愈合的 , 但后者肢 

骨的粗壮程度小于 Ch. wimani。Ch. wimani 

94

的肢骨更远比产自通古尔的 Acerorhinus 

zernowi 短粗。尽管 Ch. wimani 的前肢长于 

产自西班牙的 Alicornops simorrense, 但在欧 

洲发现的大多数 A. simorrense 的肢骨都比 Ch. 

wimani 细长。所有 Aceratherium incisivum 的 

肢骨也都比 Ch. wimani 细长 , 而 

Hoploaceratherium tetradactylum 的肢骨更是 

远远长于 Ch. wimani, 相应地也更为纤细。 

在可以对比的肢骨中 ,Plesiaceratherium 

gracile 的掌 , 庶骨比 Ch. wimani 细长得多 , 

同时前者距骨对跟骨的关节面也分得相当 

开。所以 , 在无角犀亚科中 , 大多数属种 

的肢骨都比大唇犀细长 , 这与它们的系统 

发育地位是吻合的。 

2008010361 

Hesperotherium( 黄昏兽 )— 后期爪兽一新 

属 = Hesperotherium -a new genus of the last 

chalicotheres. ( 中文 ). 邱占祥 . 古脊椎动物学 

报 , 2002, 40(4): 317 

记述了山西天镇早更新世爪兽一新属 — 

Hesperotherium。新属为低冠中等大小的爪 

兽 , 主要鉴别特征是 : 吻部极度缩短 , 门齿、 

犬齿和第一前臼齿消失 , 前臼齿高度退缩 , 上 

臼齿宽大于长 , 原尖孤立 , 下臼齿后齿带发 

育。这是爪兽科最后的代表。中国过去在 

晚上新世至早更新世地层中发现的 

Nestoritherium, 很可能都应该归入这个新 

属。这个属的化石目前仅发现于中国。 

2008010362 

辽西首次发现保存毛发和软体的中生代哺 

乳动物化石 = Discovery of a Mesozoic fossil 

mammal with hair and soft tissue in western 

Liaoning,China. ( 中文 ). 季强 . 地质通 

报 , 2002, 21(1): 29-34 2 图版 . 

中国辽西地区素以产出丰富多彩的中生 

代热河生物群闻名于世。特别是近几年来 , 

该区大量长羽毛的恐龙、原始鸟类、原始 

哺乳类和被子植物化石的发现更加引起了 

国际科学界的极大关注。1997 年秋 , 作者在 

辽宁北票四合屯地区发现了一块完整的保 

存有毛发和软体印痕的对齿兽类哺乳动物 

化石。身体保存有毛发和软体印痕的中生 

代哺乳动物化石在世界上也是罕见的。这 

对于研究对齿兽形态结构、生活习性、系 

统关系等方面均具有重要意义。 

2008010363 

甘肃临夏盆地发现已知最早的披毛犀化石 

= The earliest known wooly rhino discovered 

in the Linxia basin,Gansu Province,China. ( 中 

文 ). 邓涛 . 地质通报 , 2002, 21(10): 604-608 

披毛犀 (Coelodonta 属 ) 是已绝灭的最著名 

的冰期动物之一。然而 , 披毛犀的早期记录 

只有少量材料来自几个约 1.7MaBP 的中国 

地点。本项研究从甘肃临夏盆地最早的黄 

土沉积中发现一个带下颌骨的完整披毛犀 

头骨和一个具乳齿列的幼年头骨 , 古地磁年 

龄测定约为 2.5MaBP, 是世界上目前发现的 

最早的披毛犀遗存 , 将披毛犀的历史向前推 

进了 0.8Ma。这一发现对了解披毛犀的早 

期进化具有重要意义 , 因为其进步的特征显 

示 Coelodonta 属至少在上新世就已经从真犀 

族中分离出来。这些 Coelodonta 属的化石发 

现于代表干冷气候条件的黄土中 , 应是大冰 

期出现和青藏高原隆升所引起的结果。披 

毛犀起源于华北地区 , 在更新世时期广泛地 

扩散到欧亚大陆北部。 

2008010364 

蒙古上新世犬类一新种 Eucyon marinae, 兼 

评与该属相关的分子 = Eucyon marinae 

sp.nov. (Mammalia, Carnivora), A new canid 

species from the Pliocene of Mongolia, with a 

review of forms referable to the genus. ( 英文 ). 

Spassov N; Rook L. Rivista Italiana di Paleontologia 

e stratigrafia, 2006, 112(1): 123- 

133 

The species is characterised by very specific 

large but narrow premolars and slender 

mandible. The paper also provide a discussion 

on the ecology of the species as well as a review 

of Late Miocene and early Pliocene fossil 

canids from North America, Eurasia and 

Africa referable to the genus Eucyon. Problems 

related to the taxonomy of Eucyon and 

other Canis-Like forms are discussed. 

2008010365 

意大利北部 Zandobbio 附近伊姆阶碎石中 

一块完整的像狮子的猫的颅骨 = Systematic 

position of a complete lion-lime cat skull from 

the Eemian ossiferous rubble near Zandobbio 

(Bergamo, North Italy). ( 英文 ). Bona F. Rivista 


2006, 112(1): 157-166 

The skull shows the typical lion morphology 

and its relatively small dimensions suggest 

that it belonged to a female individual.Carnassial 

tooth analysis underlines advanced 

lion characters already recognized in 

Italy during the Eemian. According to skull 

and teeth characters it is possible to ascribe 

95

the specimen to the group of Upper Pleistocene 

lion-like cats Panthera leo spelaea. 

2008010366 

江苏镇江莲花洞动物化石铀系年代 = U- 

series dating of fossil teeth from Lianhua cave 

in Zhenjiang,Jiangsu Province. ( 中文 ). 潘亚 

娟 ; 沈冠军 ; 房迎三 . 人类学学报 , 2002, 21(2): 

155-157 

莲花洞位于镇江市南约 6km 的白龙岗山 

北坡 ( 原在丹徒县境内 ), 地理座标 119 

°24'E,32 °10'N。白龙山为宁镇山脉东支 , 

走向近东西 , 顶峰海拔 118m。溶洞发育于 

三迭纪青龙组灰岩 , 洞口标高约 35m。 

1981 年 , 南京博物院等单位对该地点进行 

发掘 , 获哺乳动物化石 16 种 , 其中人牙化 

石 1 枚。洞内堆积自下而上被分为 4 层 , 

其中第 2 层为棕红色亚粘土 , 含石灰岩碎 

块、铁锰质结核和大量动物化石。发掘者 

根据动物化石中有 3 个绝灭种 , 将该地点 

定在 “ 晚更新世或晚更新世早期 ”, 人牙化 

石被认为属于智人。韩德芬等认为莲花洞 

在我国晚更新世地点地层古生物年代系列 

中 , 不晚于周口店山顶洞 , 但也不早于建 

德乌龟洞和柳江人洞 ,“ 人类化石被认为可 

能属于晚期智人 ”。吴汝康等亦认为该人牙 

化石 “ 形态与现代人无异 ”。 

2008010367 

云南元谋古猿动物群化石埋藏学 = Taphonomy 

of the hominoid fauna in the Yuanmou 

Basin, Yunnan. ( 中文 ). 张云翔 ; 郑良 ; 吉学平 ; 

张家华 . 地质学报 , 2002, 76(1): 45-49 

云南元谋小河 — 雷老一带含古猿新近系 

( 上第三系 ) 是一套紫红色含砾细砂 — 粉砂岩 , 

夹有多层黄色砂砾石层。化石埋藏学研究 

及含化石层岩性特征、组合及沉积构造表 

明 , 该层以山前洪积堆积为主 , 并有发育的扇 

上河道沉积。通过 30 余个发掘地点化石野 

外埋藏资料及数千件化石标本的分析鉴定 , 

化石埋藏类型有两种 , 埋藏 Ⅰ 型的化石数量 

稀少、保存完整 , 赋存在扇体细粒沉积物中 ; 

埋藏 Ⅱ 型化石保存丰富但相当残破 , 赋存在 

粗粒沉积的扇上河道各个部位。化石埋藏 

类型与古气候、古生态有着密切的关系 , 化 

石埋藏特征表明该区自然环境分带已形 

成。元谋古猿动物群的生存时代是一个从 

森林向草原 - 灌丛环境过渡的动荡时期。 

2008010368 

更新世欧洲和近东地区动物群双向交流的 

分子生物学证据 : 以双色鼩鼱 (Crocidura 

leucodon, Soricidae) 为例 = Molecular evidence 

of Pleistocene bidirectional faunal exchange 

between Europe and the Near East: the 

case of the bicoloured shrew (Crocidura leucodon, 

Soricidae). ( 英文 ). Dubey S; Cosson J 

F; Vohralik V; Krystufek B; Diker E; Vogel P. 

Journal of Evolutionary Biology, 2007, 20(5): 

1799–1808 

We sequenced 1077 bp of the mitochondrial 

cytochrome b gene and 511 bp of the nuclear 

Apolipoprotein B gene in bicoloured shrew 

(Crocidura leucodon, Soricidae) populations 

ranging from France to Georgia. The aims of 

the study were to identify the main genetic 

clades within this species and the influence of 

Pleistocene climatic variations on the respective 

clades. The mitochondrial analyses revealed 

a European clade distributed from 

France eastwards to north-western Turkey and 

a Near East clade distributed from Georgia to 

Romania; the two clades separated during the 

Middle Pleistocene. We clearly identified a 

population expansion after a bottleneck for the 

European clade based on mitochondrial and 

nuclear sequencing data; this expansion was 

not observed for the eastern clade. We hypothesize 

that the western population was confined 

to a small Italo-Balkanic refugium, 

whereas the eastern population subsisted in 

several refugia along the southern coast of the 

Black Sea. 

2008010369 

乌干达 Napak 地区早中新世古食肉动物 

( Creodonta, Carvivora 和 Incertae 

sedis) 化石新材料 = New canivoran material 

(Creodonta, Carnivora and Incertae sedis) 

from the Early Miocene of Napak, Uganda. 

( 英文 ). Morales J; Pickford M; Soria D. Paleontological 

Research, 2007, 11(1): 71-84 

Eight species of creodonts and carnivores 

have previously been reported from the Early 

Miocene deposits at Napak, Uganda. This paper 

takes into account unpublished material 

from old collections made by W.W. Bishop 

during the 1950s and 1960s, as well as new 

samples made by the Uganda Palaeontology 

Expedition between 1985 and 2005. Four carnivoran 

species are reported from the site for 

the site for the first time, of which one is a 

new genus and species, and one species is removed 

from previous lists, making for a grand 

total of 12 species for Napak comprising 6 

creodonts, 4 fissipeds and two incertae sedis. 

2008010370 

96

肯尼亚科普萨拉曼 (Kipsaraman) 及东非 

其他地点的中中新世猪科、河马科化石 = 

Suidae and Hippopotamidae from the Middle 

Miocene of Kipsaraman, Kenya and other 

sites in East Africa. ( 英文 ). Pickford M. Paleontological 

Research, 2007, 11(1): 85-105 

African Middle Miocene suiform faunas 

are rather poorly known. Some taxa are well 

represented at one or two sites, but in general 

the material is rather scrappy. As a result, 

there has been confusion about which taxa are 

present at which localities, and differences of 

opinion exist about which specimens belong 

to which taxa. The discovery of a rich and 

diverse suoid fauna at Kipsaraman, a Middle 

Miocene site in Kenya, helps to throw light on 

several lineages including kubanochoeres and 

kenyapotamines. The fauna also contains remains 

of namachoerines and listriodonts. 

2008010371 

Parahyaenodon argentinus 的分类修订及 

其对南美中新世 - 上新世大型食肉类认识的 

意义 = Taxonomic revision of Parahyaenodon 

argentinus Ameghino and its implicances for 

the knowledge of the Mio-Pliocene large carnivorous 

mammals of South America.. ( 其他 ). 

Forasiepi A M; Martinelli A G; Goin F J. 

Ameghiniana, 2007, 44(1): 143-159 

Parahyaenodon argentinus, from the Late 

Miocene-Early Pliocene of Monte Hermoso 

(Buenos Aires Province, Argentina), was recognized 

by Ameghino in 1904, who regarded 

it as Hyaenodontidae (Eutheria, Creodonta). 

Based on its dental features, later authors assigned 

P. argentinus to Borhyaeninae 

(Metatheria, Sparassodonta, Borhyaenidae). 

Thus, this taxon would have represented the 

last known borhyaenid. A new analysis of the 

type and only known specimen led us to reassign 

P. argentinus to Procyonidae (Eutheria, 

Carnivora). In this context, the biochron of 

Borhyaeninae extends up just to Late Miocene 

(Huayquerian Age), being cf. Borhyaena and 

possibly Eutemnodus the last known representatives 

of this subfamily. Based on these results 

and in the first records of carnivorous 

placental immigrants in South America, it is 

evident that there was no "competitive displacement" 

between metatherian and eutherian 

carnivores: there is a gap of no less than four 

Ma between the extinction of the last 

Borhyaeninae and the arrival of their alleged 

ecological counterparts, the Carnivora. 

2008010372 

湖北房县桥上乡蛤蟆洞哺乳动物化石的发 

现及意义 = Discovery of mammal fossils in 

Hama cave, Fang County, Hubei Province and 

its significance. ( 中文 ). 龙昱 ; 周修高 . 地质科 

技情报 , 2002, 21(2): 49-50 

通过对挖掘的牙化石的初步鉴定 , 湖北 

省房县桥上乡蛤蟆洞洞穴堆积层中哺乳动 

物化石共有 4 个目 ( 啮齿目、食肉目、奇 

蹄目和偶蹄目 )、8 个种属 ( 豪猪、虎、 

熊、中国犀、巨貘、鹿、水牛和羊 ), 为 

中一晚更新世温暖、湿润、森林 - 草地化石 

动物群 ; 该化石动物群的发现和地理位置 

为神农架地区更新世哺乳动物群分布和演 

化的深入研究提供了新地点 , 并为该地区 

新构造抬升特点的研究提供可参考的证 

据 , 同时也为当地旅游经济的进一步发展 

提供了新的支点。 

2008010373 

新近纪初南美洲后兽类第一部分 : 前言 , 

Didelphimorphia 和 Sparassodonta. = South 

American Metatherians from the begining of 

the Neogene (Early Miocene, Colhuehuapan 

Land-mammal age). Part 1: Introduction, 

Didelphimorphia and Sparassodonta.. ( 其他 ). 

Goin F; Abello A;Bellosi E; Kay R; Madden 

R; Carlini A. Ameghiniana, 2007, 44(1): 29- 

71 

This work is the first, of a series of three, 

taxonomic reviews of the Early Miocene 

(Colhuehuapian Land-mammal Age) South 

American metatherians. Colhuehuapian levels 

from the Gran Barranca south of the Colhue 

Huapi lake (Sarmiento Department, Chubut 

Province, Argentina) are the richest ones in 

specimens of this age. Colhuehuapian landscapes 

from Central Patagonia developed in a 

coastal plain located in a peninsular area, 

which originally suffered an intense erosion 

and subsequentely was agradded with fluvial 

and loessic (eolian) sediments. Palinomorphs 

and phytoliths suggest a period characterized 

by significant environmental changes, from 

xeric (middle Early Miocene) to humid-warm 

conditions (late Early Miocene). In uplands or 

areas far from the sea, temperate-humid closed 

forests prevailed, but in lowlands or litoral 

areas herbaceous (grass) plants and shrubs 

dominated, with subordinated or patchy arboreal 

vegetation. Paleoclimate would have been 

warm-temperate to warm and probably subhumid, 

more rainy in highlands. The most 

important results of this analysis are: (1) the 

oldest record of Didelphoidea didelphimorphians, 

including, probably, the oldest known 

97

caluromyid; (2) the recognition of a great diversity 

of carnivores belonging to the Order 

Sparassodonta, including the oldest record of a 

Thylacosmilidae; (3) the recognition of a new 

species of the incertae sedis mammal Necrolestes. 

Among the taxa reviewed here we 

describe the new species Necrolestes mirabilis. 

2008010374 

玻利维亚南部中新世中期 Laventan Quebrada 

Honda 动物群及对其中南美有蹄动 

物的描述 = The middle Miocene (Laventan) 

Quebrada Honda fauna, southern Bolivia and 

a description of its notoungulates. ( 英文 ). 

Croft D A. Palaeontology, 2007, 50(1): 277- 

303 

The Laventan Quebrada Honda Fauna of 

southern Bolivia is one of the best sampled 

middle Miocene South American faunas. The 

present study describes the toxodontid, interatheriid 

and mesotheriid notoungulates 

from Quebrada Honda and summarizes the 

present state of knowledge of the fauna. 

Toxodontid specimens from Quebrada Honda 

include two isolated molars, one upper and 

one lower. The upper molar compares favourably 

with Paratrigodon and may represent 

a new species, but too little material is 

known to make an adequate diagnosis. The 

lower molar may pertain to the same taxon, or 

to a distinct species that is even more poorly 

represented. A new species of the interatheriid 

Miocochilius is described, M. federicoi, on the 

basis of a partial skull. It differs from M. anomopodus 

in its significantly smaller size (at 

least 20 per cent smaller based on linear upper 

molar dimensions); relatively wider P4 with 

deeper lingual sulcus; more prominent middle 

lobes on upper molars; and M3 with deeper 

lingual sulcus and more prominent metastyle 

(distal lobe). The generic allocation of this 

new species is considered tentative, pending a 

better understanding of the phylogenetic relationships 

among currently recognized species 

of Miocochilius and Protypotherium. 

Mesotheriids are represented at Quebrada 

Honda by a pair of poorly preserved mandibles 

that are referred to Plesiotypotherium 

minor, a species previously recorded from 

slightly older deposits near Cerdas, Bolivia. A 

newly revised faunal list for Quebrada Honda 

is compiled that includes 30 species of nonvolant 

mammals, 27 of which have been identified 

to at least genus level. This revised faunal 

list is used to compare Quebrada Honda to 

other well-sampled middle–late Miocene faunas 

(including La Venta, Columbia; Collón- 

Curá, Argentina; and Arroyo Chasicó, Argentina) 

using the Simpson Index of faunal similarity. 

In order to compensate for inadequately 

identified specimens (i.e. those not identified 

to genus level), minimum and maximum values 

of faunal similarly were estimated using 

two different sets of assumptions. The analysis 

indicates that the middle-latitude Quebrada 

Honda Fauna is more similar to the slightly 

older high-latitude fauna of Collón-Curá than 

to the contemporaneous low-latitude fauna of 

La Venta, suggesting that isolating mechanisms 

between the low and middle latitudes 

were in place during the early and/or middle 

Miocene. The relative paucity of taxa shared 

between Quebrada Honda and La Venta, despite 

their contemporaneity, suggests that the 

system of South American Land Mammal 

‘Ages’ (SALMAs) may not be useful for biocorrelation 

between low-latitude faunas and 

those from elsewhere in South America. 

2008010375 

Merycopotamus 的解剖学修订及其对亚洲 

晚中新世哺乳动物扩散的重要性 = Anatomical 

revision of the genus Merycopotamus 

(Artiodactyla; Anthracotheriidae): its significance 

for late Miocene Mammal dispersal in 

Asia. ( 英文 ). Lihoreau F; Barry J; Blondel C; 

Chaimanee Y; Jaeger J; Brunet M. Palaeontology, 

2007, 50(2): 503-524 

New fossil remains of the anthracothere 

genus Merycopotamus Falconer and Cautley, 

are described. Most of them were discovered 

by the Harvard University and Geological 

Survey of Pakistan joint research project (Y- 

GSP) in the well-dated Middle and Late Miocene 

deposits of the Potwar Plateau in northern 

Pakistan. This new material led us to revise 

the systematics of the genus with the 

validation of three species, M. nanus Falconer 

(M. pusillus Lydekker), M. dissimilis Falconer 

and Cautley, and M. medioximus Lihoreau 

et al., and allowed us to determine precisely 

their chronological distributions in a continuous 

Neogene sequence. Other specimens reported 

from the late Miocene deposits of the 

Khorat Plateau in north-east Thailand by the 

Department of Mineral Resources are the first 

remains of Merycopotamus to have been discovered 

in that region and are attributed to 

M. medioximus. These discoveries indicate a 

wider geographical distribution of the genus in 

the early Late Miocene. Anatomical investigations 

highlight the evolution of Merycopotamus 

through the Miocene towards more amphibious 

habits. Palaeobiogeographical and 

98

palaeoecological information for Merycopotamus 

stress the role of the Himalayan orogenesis 

as a dispersal barrier and the impact of 

a major global regression event on the evolution 

of Indian Subcontinent faunas from the 

Middle Miocene to the Late Pliocene. 

2008010376 

英格兰始新世早期一新的 Omomyid 及其 

古生物地理意义 = A New Microchoerine 

Omomyid (Primates, Mammalia) From The 

English Early Eocene And Its Palaeobiogeographical 

Implications. ( 英文 ). Hooker J J. 


A new genus and species of omomyid primate, 

Melaneremia bryanti, is described from 

the Early Eocene Blackheath Beds of Abbey 

Wood, London, UK. It shares unique derived 

characters with the European subfamily Microchoerinae 

and is its most primitive member. 

It is nevertheless more derived than the primitive 

omomyid Teilhardina belgica from the 

beginning of the European Eocene. Cladistic 

analysis shows that the Microchoerinae are 

sister group to a clade comprising subfamilies 

Omomyinae and Anaptomorphinae, but excluding 

Teilhardina belgica and T. asiatica, 

which are stem omomyids. The Mammalian 

Dispersal Event (MDE), which marks the beginning 

of the Eocene (55·8 Ma), saw the dispersal 

of primates, perissodactyls and artiodactyls 

into the Northern Hemisphere. At this 

time similar species of Teilhardina lived in 

Europe, Asia and North America. The Abbey 

Wood microchoerine lived about 1 million 

years later. It co-occurs with non-primate species 

identical or very similar to those that 

lived in North America. The latter were 

ground-dwellers, whereas the microchoerine 

and others that show distinct differences from 

North American relatives were tree-dwellers. 

Land-bridges connected North America and 

Europe via Greenland at the beginning of the 

Eocene, but 2 million years later these had 

been severed by submarine rifting. North 

American species at Abbey Wood indicate 

that a land connection still remained at 

c. 55 Ma. However, the forest belt that must 

have been continuous during the MDE to allow 

tree-dwellers to disperse between the continents 

is likely by this time to have been disrupted, 

perhaps by volcanic eruption. 

2008010377 

澳大利亚昆士兰岛西北部里弗斯利中新世 

晚期沉积物中的袋熊 Warendja 一新种 = A 

New Species of the Wombat Warendja from 

Late Miocene Deposits at Riversleigh, North- 

West Queensland, Australia. ( 英文 ). Brewer P; 

Archer M; Hand S; Godthelp H. Palaeontology, 

2007, 50(4): 811-828 

A new species of the plesiomorphic wombat 

Warendja is described. Warendja encorensis 

sp. nov., the second species to be attributed 

to this genus, is known from a single fossil 

locality (Encore Site) at Riversleigh, northwest 

Queensland. Specimens of W. encorensis 

are limited to isolated teeth, two mandibular 

fragments and a maxillary fragment. Two molars 

preserve the unworn crown morphology. 

Encore Site has been estimated to be late Miocene 

in age, making these the only known 

specimens of Warendja to be clearly older 

than Pleistocene. Warendja encorensis is also 

the first described species of wombat from 

Miocene deposits to which hypselodont teeth 

have been attributed. It differs from 

W. wakefieldi in its larger size, distribution of 

enamel, and in details of the incisor and premolar 

morphology. 

2008010378 

意大利北部更新世 Balaenopterid 鲸一新基 

部类群 = A New Basal Balaenopterid Whale 

From The Pliocene Of Northern Italy. ( 英文 ). 

Bisconti M. Palaeontology, 2007, 50(5): 

1103-1122 

A new basal balaenopterid genus and species, 

Archaebalaenoptera castriarquati, is 

described and compared with all the living and 

fossil members of the family Balaenopteridae 

and related fossil rorqual-like taxa. It was 

found in the Lower Pliocene of northern Italy, 

and is characterized by a supraoccipital with a 

transversely compressed anterior process, the 

zygomatic process of the squamosal diverging 

from the longitudinal axis of the skull, very 

long nasal bones, and subtle exposition of the 

parietal on the dorsal wall of the skull. It is 

primitive in having a maxilla with a long ascending 

process that is posteriorly unexpanded 

and round, and a dentary that is straight and 

not bowed outward, unlike that of living 

Balaenopteridae. In particular, the discovery 

of this new genus suggests that, among the 

early members of Balaenopteridae, the acquisition 

of the typical sutural pattern shown by 

maxilla, frontal, parietal and supraoccipital 

preceded the acquisition of the feeding-related 

traits that are characteristic of the family. The 

primitive morphology of the feeding-related 

structures of A. castriarquati (i.e. the straight 

dentary and the flat glenoid fossa of the 

squamosal) suggests that this whale was un- 

99

able to undertake the intermittent ram feeding 

typical of Balaenopteridae as efficiently as 

living members of the family. 

2008010379 

玻利维亚 Tiupampa 早古新世 

Pucadelphydae 的耳区及其世系演化意义 = 

The Auditory Region Of Early Paleocene Pucadelphydae 

(Mammalia, Metatheria) From 

Tiupampa, Bolivia, With Phylogenetic Implications. 

( 英文 ). Ladevèze S; De Muizon C. 


New petrosal bones, assigned to Pucadelphys 

and Andinodelphys, from the Lower Paleocene 

of Tiupampa, Bolivia, are described. 

These remains provide new information on the 

anatomy of the ear region of these taxa. The 

re-examination of characters from the petrosal 

and basicranium shed light on the phylogenetic 

relationships of the three Tiupampan 

genera known from complete cranial remains 

(i.e. Mayulestes, Pucadelphys and Andinodelphys). 

The combination of dental, general cranial 

and basicranial characters led to two alternative 

hypotheses. The first is that 

borhyaenoids (including Mayulestes) are 

nested within Notometatheria. Pucadelphyds 

(i.e. Pucadelphys and Andinodelphys) are the 

sister group of a clade comprising MHNC 

8369 (one isolated petrosal from Tiupampa) 

and Marsupialia. The second favours the paraphyly 

of ‘borhyaenoids’ (i.e. the exclusion of 

Mayulestes from borhyaenoids) and the polyphyly 

of ‘Notometatheria’. In this case, Mayulestes 

and borhyaenids represent the stem 

group of a clade including Asiatic, American 

and Australian metatherians. This analysis of 

combined datasets (dental, general cranial and 

basicranial) highlighted contradictory information 

in the dental and cranial characters, 

serving to emphasize that in a large anatomical 

complex like an entire skull mosaic evolution 

of the characters is likely. 

2008010380 

玻利维亚渐新世一新的普通 

Paucituberculatan 有袋动物及似鼩鼱负鼠 

的起源 = A New Generalized Paucituberculatan 

Marsupial From The Oligocene Of Bolivia 

And The Origin Of ‘Shrew-Like’ Opossums. 

( 英文 ). Goin F J; Sánchez-Villagra M R; 

Abello A; Kay R F. Palaeontology, 2007, 

50(5): 1267-1276 

Insights into the origin of ‘shrew-like’ 

oposssums of South America are gained 

thanks to a new fossil from the Oligocene 

Salla Beds in Bolivia. The specimen described 

here consists of a partial rostrum, palate and 

postcanine teeth, and shows several generalized 

features (cranial and dental) in the context 

of the Paucituberculata. On this basis we 

recognize Evolestes hadrommatos gen. et sp. 

nov. In order to evaluate the affinities of the 

new taxon, we performed a phylogenetic 

analysis including representatives of the 

Caenolestidae, Pichipilus and allies (not regarded 

here as caenolestids), Palaeothentidae, 

and Abderitidae, with three outgroups. 

Evolestes is the basalmost ‘caenolestoid’, and 

provides clues to the morphological changes 

involved in the origin of caenolestids. 

2008010381 

甘肃省东乡族自治县龙担黄土底部新发现 

的哺乳动物群初步报道 = Notes on the 

mammal fauna from the bottom of loess deposits 

at Longdan, Dongxiang County, Gansu 

Province. ( 中文 ). 邱占祥 ; 王伴月 ; 邓涛 ; 倪喜 

军 ; 王晓鸣 . 第四纪研究 , 2002, 22(1): 33-38 

龙担哺乳动物群发现于甘肃省东乡族自 

治县的早更新世黄土底部。此前我国早更 

新世的哺乳动物化石大多发现于河 - 湖相 

地层中 , 在黄土中极少发现 , 而且主要在 

六盘山以东。在龙担哺乳动物群中还发现 

了灵长类化石 , 这在我国西北地区尚属首 

次。龙担哺乳动物群产于黄土底部约 30m 

的地层中 , 最低的层位距 “ 底板 ”( 积石组 

砾岩 ) 仅约 3m。化石相当丰富 , 其中有不 

少新的种类。目前巳发现的化石共 21 种 , 

大体可以分为 3 类 :1) 与泥河湾哺乳动物 

群相同或很接近的 ;2) 与泥河湾哺乳动物 

群相比 , 在进化水平上稍低 , 因而可能代 

表较早地质时代的 ;3) 在泥河湾哺乳动物 

群中没有发现过的。龙担哺乳动物群的地 

质时代可能比泥河湾者稍早 , 可能约 

2MaB.P.。其组成倾向于表明 , 当时该地区 

周围还有相当面积的森林覆盖。 

2008010382 

试论野生水牛、四不像鹿和中国鼍在黄河 

中下游的绝迹 = Discussion on the vanishing 

of the wild buffalo, david deer and Chinese 

alligator in the middle-lower reaches of Yellow 

River. ( 中文 ). 周跃云 ; 何业恒 . 第四纪研 

究 , 2002, 22(2): 182-187 

本文利用考古、文献以及实地调查等资 

料 , 论述了全新世中期及其以前 , 野生水 

牛、四不像鹿和中国鼍都以黄河中下游地 

区为起源和栖息地。这些动物的大量存 

100

在 , 反映出当时气候温和多雨、河湖密布 

的景象 ; 到了全新世晚期特别是西汉以 

来 , 随着它们的绝迹 , 表明生态环境的日 

益恶化 , 到现在这里已是水贵如油、风沙 

肆虐。探讨这些变化特别是干旱的由来 , 

对于保持黄河中下游地区的生态平衡是十 

分有益的。 

2008010383 

准噶尔南缘 - 吐鲁番盆地晚二叠世 - 中三叠世 

早期二齿兽类的发育及生态环境探讨 = 

Dicynodon and ecological environment of 

Late Permian to early stage of Middle Triassic 

at Junggar southern margin-Turpan. ( 中文 ). 

屈迅 ; 吴绍祖 ; 李永安 ; 李强 . 新疆地质 , 2002, 

20(3): 187-191 

准噶尔南缘 - 吐鲁番盆地晚二叠世 - 中三叠 

世早期地层中、共有 5 个岩组发现有二齿 

兽类化石。这些二齿兽类生活在河流 - 浅水 

湖泊的古地理环境中 , 伴随古气候条件为 

热带 - 亚热带气候。该时期的 “ 红层 ” 可以作 

为热带 - 亚热带气候的标志之一。 

2008010384 

加拿大北极地区上新世一奇异新属 

Boreameryx 及北极化石哺乳动物的特有现 

象 = Boreameryx, an unusual new artiodactyl 

(Mammalia) from the Pliocene of Arctic Canada 

and endemism in Arctic fossil mammals. 

( 英文 ). Dawson M R; Harington C R. Canadian 

Journal of Earth Sciences, 2007, 44(5): 

585-592 

Boreameryx braskerudi, gen. et sp. nov., 

from Early Pliocene (about 5-4 Ma) deposits 

of Ellesmere Island, Nunavut, is represented 

by the posterior portion of a dentary with three 

molars, a partial calcaneum, unciform, and 

fragments of long bones and ribs. The incompletely 

known structure of Boreameryx must 

leave open the questions of its relationships 

within the pecoran ruminants. Even its possible 

affinities with early cervoids and the North 

American blastomerycines are speculative. 

We favour the tentative association of Boreameryx 

within the Cervoidea. Rather than 

evolving hypsodonty to deal with abrasive 

northern foods, Boreameryx apparently retained 

plesiomorphic dental structures—even 

augmenting those structures in a unique morphological 

development. We hypothesize, 

based on recorded relationships and ranges 

(both geological and geographical) of several 

Beaver Pond site mammals, including Boreameryx, 

that they indicate a significant interval 

of endemic development in a high 

northern biotic province prior to 5 Ma. 

2008010385 

法国奥弗涅上上新统哺乳动物兔形目 

Oryctolagus lacosti 的修订 = Revision of 

Oryctolagus lacosti (Lagomorpha, Mammalia) 

from the Upper Pliocene of Perrier (Auvergne, 

France). ( 法文 ). De Marfà R; Mein P. 

Comptes Rendus Palevol, 2007, 6(5): 327-334 

Fossil leporids from the Upper Pliocene 

of the locality of Perrier-Étouaires (Auvergne, 

France) are here revisited. They were initially 

attributed to Lepus lacosti by Pomel (1853), 

and later to the genus Oryctolagus. This material 

had been neither accurately described nor 

figured until now. Thus, a lectotype and two 

paralectotypes have been chosen among the 

material of the original collection. The diagnostic 

character of Oryctolagus lacosti is its 

big size, similar to that of modern hares 

(Lepus), together with other morphological 

characters that fit in the variability range of 

European rabbits (Oryctolagus cuniculus). 

Fossils of leporids similar to those of Perrier 

have also been found in several Plio- 

Pleistocene localities from western Europe. 

2008010386 

青藏高原东北部晚中新世哺乳动物偶蹄类 

目麂亚科的新材料 = New material of Muntiacinae 

(Artiodactyla, Mammalia) from the 

Late Miocene of the northeastern Qinghai- 

Tibetan Plateau, China. ( 英文 ). Dong Wei. 

Comptes Rendus Palevol, 2007, 6(5): 335-343 

Recent expeditions in the northeastern 

Qinghai-Tibetan Plateau have produced additional 

mammalian fossils from the Lower 

Baodean (equivalent to Vallesian, Late Miocene), 

and, significantly, a new large and the 

earliest muntjac, Muntiacus noringenensis sp. 

nov. It is phylogenetically closer to the Late 

Pliocene M. fenghoensis and extant M. vuqangensis 

than the other fossil and extant muntjacs 

are. The existence of this muntjac and 

other folivores in the Late Miocene Qaidam 

Basin suggests a forested period in the basin 

and the evolution from a forested and humid 

environment to a desert one today. Such a 

dramatic evolution in environments is an evidence 

of the effect of the uplift of the Qinghai- 

Tibetan Plateau and of its influence on continental 

climates. 

古人类学 

古人类学 

101

2008010387 

阿特拉斯克马格里布东部新石器时代牧羊 

人的生存行为 = Subsistence and symbolic 

behaviour of Neolithic shepherds from the 

eastern Atlasic Maghreb.. ( 法文 ). Roubet C. 

Comptes Rendus Palevol, 2006, 5(1/2): 441- 

451 

Subsistence and symbolic behaviour of 

Neolithic shepherds from the eastern Atlasic 

Maghreb. Neolithization through karstic territories 

from eastern Maghreb was in tandem 

with an initial form of pastoralism between 

7500-5000 cal BP (ca 78556859 cal BP and 

5471-4414 cal BP). Development and scattering 

of social organization was linked with development 

of the 'status of the shepherd'. The 

cultural context in which expanded this way of 

life was an Atlasic Neolithic with a Capsian 

tradition. Evolved Mechtoids and Proto- 

Mediterranean represented mixed shepherd 

communities. During their winter settlements 

in hilly terrain and lowland saline areas, shepherds 

started to exchange goods with peddling 

nomadic people. Polished stone axes and 

adzes and marine shell ornaments, coveted by 

the shepherds, were exchanged against flock 

meat/animal goods. The impact of foreign 

artefacts visibly documents a new behaviour 

and acculturation. To cite this article: C. 

Roubet, C. R. Palevol 5 (2006). (c) 2005 Academie 

des sciences. Publie par Elsevier SAS. 

Tons droits reserves. 

2008010388 

周口店田园洞古人类化石点地层学研究及 

与山顶洞的对比 = Mammalian biostratigraphy 

of Tianyuan Cave,compared with that of 

Upper Cave at Zhoukoudian(Choukoutien). 

( 中文 ). 同号文 ; 尚虹 ; 张双权 ; 刘金毅 ; 陈福友 ; 

吴小红 ; 李青 . 人类学学报 , 2006, 25(1): 68- 

81 

田园洞主体堆积厚度约 2.5m, 其动物群可 

分为上、下两个组合 : 上部组合物种多样性 

丰富 , 化石被啮齿类严重啮咬 ; 下部组合化石 

种类单调 , 以鹿类和绵羊类为主 , 但化石丰富 , 

极少有啮齿类咬痕。人类化石发现于下部 

组合 ; 东洋界动物主要出现在上部组合 , 例如 

猕猴、猪獾、果子狸和鬣羚等。而马鹿和 

绵羊只出现于下部组合。沟齿鼯鼠和豪猪 

在下部组合开始出现 , 但主要发现于上部组 

合。梅花鹿是田园洞的优势种 , 在各个阶段 

都出现。通过统计比较 , 发现山顶洞 3 个地 

层单元 ( 上室、下室和下窨 ) 中所含化石属种 

基本一致 , 代表同一个动物群。尽管田园洞 

动物群中尚未发现可靠绝灭种类 , 但却有 10 

种地区绝灭种 , 它与现生动物群有一定差异 ; 

而在堆积物特征及化石组合方面 , 与周口店 

山顶洞的更为接近。在田园洞和山顶洞出 

现的沟齿鼯鼠、猪獾、果子狸及鬣羚等是 

各自在华北地区的最早记录 , 可能代表了更 

新世末期自南而北的动物迁徙事件。 

2008010389 

关于萨拉乌苏遗址地层及人类化石年代的 

问题 = An issue on the date of fossil Human 

remains from Salawusu, Inner Mongolia. ( 中 

文 ). 尚虹 ; 卫奇 ; 吴小红 . 人类学学报 , 2006, 

25(1): 82-86 

本文回顾了与人类化石相关的萨拉乌苏 

河晚更新世地层及文化层的年代学研究 , 经 

过 14 C 测年和相关证据认为 , 采集的萨拉乌苏 

PA.62 号股骨不属于萨拉乌苏遗址的原生地 

层。 

2008010390 

南京 2 号人类头骨化石的复位和形态 = 

Restoration of the Nanjing 2 fossil hominid 

calvarium:morphology and taxonomic implications. 

( 中文 ). 张银运 ; 刘武 . 人类学学 

报 , 2006, 25(4): 267-275 

南京 2 号人类头骨化石仅保留部分的额 

骨、顶骨、枕骨和颞骨 , 为一不完整的颅盖 

骨。其顶骨和枕骨有数条断裂缝 , 各断块之 

间有程度不一的错动 , 致使该颅盖骨显得外 

形异常。本项研究是对该颅盖骨的错动部 

分进行复位 , 结果表明 , 南京 2 号头骨有较大 

的顶骨、较小的上枕鳞相对宽度、可能较 

大的颅容量。这些形态提示该头骨与直立 

人有所不同而与早期智人相近。该头骨所 

具有的角圆枕、颞鳞顶缘形状、枕骨圆枕 

发育程度、枕骨的枕平面与项平面过渡情 

况、枕内隆突点与枕外隆突点的距离、头 

骨骨壁厚度、脑膜中动脉分支情况、头骨 

枕面观之轮廓线样式等形态细节 , 还很难作 

为可靠的依据把南京 2 号头骨鉴定为直立 

人。南京 2 号头骨很大可能是属于智人亚 

种 (Homo sapiens sapiens) 中的一员。 

2008010391 

东昆仑北缘都兰县巴隆一带人类活动遗迹 

的发现及其环境背景 = Discovery of remains 

of human activity and its ancient environmental 

setting at Barun,Dulan County,Qinghai 

Province,on the northern margin of the East 

Kunlun Mountains. ( 中文 ). 向树元 ; 王国灿 ; 林 

102

启祥 ; 贾春兴 ; 王青海 . 地质通报 , 2002, 21(11): 

764-767 

青海都兰县巴隆乡朝火鹿陶勒盖含有人 

类活动遗迹黄土剖面的孢粉和环境磁学分 

析结果表明 , 该地区自中全新世以来气候经 

历了 3 个阶段 :4080aBP 以前气候温干偏 

湿 ;4080~3500aBP 气候温干与温干偏湿交 

替 ;3500aBP 以来气候以温干为主 , 气候逐渐 

恶化。其中 2890~1810aBP 相对降温和变 

干 , 是本地区环境最为恶劣时期。反映人类 

活动遗迹的木炭层 14C 年龄为 

(3970±90)aBP, 相当于黄河上游发现的齐家 

文化时期 , 比在昆仑山垭口发现的人类活动 

遗迹早 400 多年。 

2008010392 

非洲和中国直立人某些颅骨特征的比较 — 

— 中国与非洲人类头骨特征对比之一 = The 

comparisons of some cranial morphological 

features between the African and Chinese 

Homo erectus. ( 中文 ). 刘武 ;Emma Mbua; 吴 

秀杰 . 人类学学报 , 2002, 21(4): 255-267 

针对学术界有关非洲与亚洲直立人关系 

的争论 , 本文对一些用来支持非洲早期直立 

人从直立人中分离出来而归入匠人的主要 

形态学证据进行了检验。用于研究的标本 

包括迄今在东非发现的年代最早的直立人 

KNM-ER 3733、KNM-ER 3883 和 KNM- 

WT 15 000 头骨化石。这些化石是被提倡非 

洲与亚洲的直立人分属两个种的学者归入 

匠人的主要标本。对这些非洲早期直立人 

与中国直立人 18 项头骨特征对比显示 : 一些 

被认为是局限于亚洲直立人的独有特征在 

上述非洲直立人头骨都有出现。存在于非 

洲直立人与中国直立人之间颅骨特征上的 

差别主要体现在特征的表现程度与方式的 

不同。作者认为根据本文对比的颅骨特征 , 

非洲直立人与中国直立人在颅骨形态上非 

常相似 , 他们之间的形态差异反映了直立人 

具有较宽的形态变异范围。认为亚洲直立 

人具有特化的衍生性状的观点在本文不能 

得到支持。 

2008010393 

浙江桐庐人类头骨的铀系年代 = U-series 

dating of the hominid skull from Tonglu,Zhejiang. 

( 中文 ). 石丽 ; 金幸生 ; 程海 ; 沈冠 

军 . 人类学学报 , 2002, 21(4): 323-324 

本文报道浙江桐庐人头骨新生碳酸盐岩 

外模的 alpha 能谱和质谱法铀系年代。结果 

表明其年代很可能介于 0.5— 1 万年间。 

2008010394 

印尼爪哇动物群与周口店地区及华南动物 

群对比 = Java fauna: compared with that of 

Zhoukoudian area and South China. ( 中文 ). 

同号文 . 人类学学报 , 2002, 21(4): 325-336 

2002 年 4 月 , 笔者有幸参加了由联合国 

教科文组织驻雅加达办事处和印度尼西亚 

政府组织的 “ 北京猿人与爪哇猿人遗址研讨 

会 ”, 借此机会参观了有关遗址和博物馆 , 

并和印尼同行进行了有益交流。北京猿人 

和爪哇猿人遗址是亚洲地区最重要的直立 

人化石地点 , 也属世界上最重要的古人类 

化石地点之列 , 又要先后被联合国教科文 

组织列入世界文化遗产名录。但由于众所 

周知的原因 , 两国的学术交流在过去几十 

年不够畅通 , 国内同行对爪哇猿人遗址的 

了解很有限 , 笔者最近在研究我国第四纪 

貘类化石与现生马来貘的关系时就遇到很 

多疑难问题。笔者充分利用了这次富贵的 

机会 , 注意收集了有关爪哇猿人遗址伴生 

动物群的资料 , 并结合自己现场观察的感 

受写成此文 , 以便有助于国内同行对爪哇 

动物群及研究近况有个初步了解。 

2008010395 

古 DNA, 猪的驯化和新石器时代文化向欧 

洲的扩散 = Ancient DNA, pig domestication, 

and the spread of the Neolithic into Europe. 

( 英文 ). Larson G; Albarella U; Dobney K; 

Rowley-Conwy P; Schibler J; Tresset A; Vigne 

J-D, Edwards C J; Schlumbaum A; Dinu 

A; Balaçsescu A; Dolman G; Tagliacozzo A; 

Manaseryan N; Miracle P; Wijngaarden- 

Bakker L V; Masseti M; Bradley D G; Cooper 

A. proceedings of the National Academy of 

Sciences, 2007, 104(39): 15276-15281 1 图版 . 

The Neolithic Revolution began 11,000 

years ago in the Near East and preceded a 

westward migration into Europe of distinctive 

cultural groups and their agricultural economies, 

including domesticated animals and 

plants. Despite decades of research, no consensus 

has emerged about the extent of admixture 

between the indigenous and exotic populations 

or the degree to which the appearance 

of specific components of the "Neolithic cultural 

package" in Europe reflects truly independent 

development. Here, through the use of 

mitochondrial DNA from 323 modern and 221 

ancient pig specimens sampled across western 

103

Eurasia, we demonstrate that domestic pigs of 

Near Eastern ancestry were definitely introduced 

into Europe during the Neolithic (potentially 

along two separate routes), reaching 

the Paris Basin by at least the early 4th millennium 

B.C. Local European wild boar were 

also domesticated by this time, possibly as a 

direct consequence of the introduction of Near 

Eastern domestic pigs. Once domesticated, 

European pigs rapidly replaced the introduced 

domestic pigs of Near Eastern origin throughout 

Europe. Domestic pigs formed a key component 

of the Neolithic Revolution, and this 

detailed genetic record of their origins reveals 

a complex set of interactions and processes 

during the spread of early farmers into Europe. 

2008010396 

中国直立人变异的初步研究 = Preliminary 

study on the variations of Homo erectus in 

China. ( 中文 ). 吴新智 ; 尚虹 . 第四纪研 

究 , 2002, 22(1): 20-28 

巳发现的化石表现中国直立人的分布北 

至 39°41'N , 南至 25°45'N , 东达 

118°09'E, 西抵 101°55'E。中更新世可供比 

较的重要化石有周口店、和县及汤山的头 

骨 , 周口店、陈家窝及和县的下颌骨 ; 早 

更新世有公王岭和郧县曲远河口的头骨 , 

元谋和郧县梅铺的门牙。比较的结果显示 

各地的化石之间有同也有异 , 目前还没有 

足够的证据表明各地点化石之间的变异足 

以表现那时中国的人类可以像现代和新石 

器时代那样划分为南、北两大人群。中国 

的直立人有许多形态特征与中国的化石智 

人一致 , 个别标本还有个别特征与中国大 

多数标本不同 , 却在西方有较多的出现 , 

这些现象支持中国古人类 “ 连续进化附带杂 

交 ” 的假说。 

2008010397 

一个未公布的旧石器时代雕塑 : 法国塞纳 - 

滨海省 Gouy 地区女性浮雕 = An unpublished 

Palaeolithic sculpture: the bas-relief 

female outline of Gouy (Seine-Maritime, 

France). ( 法文 ). Martin Y. Comptes Rendus 

Palevol, 2007, 6(5): 345-358 

The subject of this note (a little depiction 

of a female body in left profile) belongs to the 

Palaeolithic cave of Gouy (Seine-Maritime). 

Executed in bas-relief (on limestone), it comprises 

pre-defined volumes comparable with 

the graphic conventions of figures of the Lalinde/Gönnersdorf 

type. Despite these convergences, 

the example from Gouy has no known 

equivalent at present, since this is the first 

time that the technique of bas-relief is encountered 

among these systematic silhouettes. The 

subject depicted is closely associated with a 

vertical cleft (that of a vulva), which forms the 

whole of its left edge. As analysis has progressed, 

various intentional traces have also 

been encountered and described, which are 

more or less comprehensible and slight; they 

only permit a few hypotheses. By revealing 

the presence of different vestiges (preserving 

shapes) that are truly carved in the cave's rock 

wall, the bas-relief highlights the use of sculpture 

in Gouy – this is a crucial fact – which 

only just escaped being totally unknown, because 

of the destruction of the front part of the 

cave. Together with the revelation of the variety 

of techniques used in Gouy, data have 

gradually been gathered together, which argue 

in favour of a frequentation of the cave over a 

long period. For the moment, there is no evidence 

enabling one to choose between the two 

probabilities of the bas-relief being either a 

‘portable object’ or a ‘wall fragment’. 

2008010398 

中旧石器时代中期百公里以上的原料采 

集 : 关于对尼安德特人社会了解的意义 = 

Raw material circulations over hundred kilometres 

during the Middle Palaeolithic; implications 

concerning our knowledge of Neanderthalian 

societies. ( 法文 ). Slimak L; Giraud 

Y. Comptes Rendus Palevol, 2007, 6(5): 359- 

368 Result list | previous < 7 of 8 > next 

In the Middle Palaeolithic of western 

Europe, raw material circulations seemed limited 

to a hundred of kilometres. This paper 

focuses on the circulation of flints on more 

than 250 km (minimal distances) in the Mousterian 

site of Champ Grand, France. Real distances 

are longer than 400 km. Modalities of 

circulation are exposed. The analyses of these 

products demonstrate an important anticipation 

concerning the mobile raw materials’ 

management. These data demonstrate that this 

Mousterian site is a point in a complex and 

ramified settlement of the landscape. Diachronic 

relations with behavioural aspects of 

Upper Palaeolithic societies are exposed. 

历史地质学、地层学 

综论 

2008010399 

从第 31 届国际地质大会看地层学研究进展 

= Development of stratigraphical research in 

the 31st international geologial congress. ( 中 

104

文 ). 王训练 ; 史晓颖 . 地质科技情报 , 2002, 

21(3): 35-42 

介绍了第 31 届国际地质大会有关地层学 

学术讨论的主要内容 , 包括地质年代表、 

生物地层学、事件地层学、层序地层学、 

磁性地层学、同位素地层学、综合地层 

学、沉积相与沉积古地理、生物古地理、 

构造古地理 10 个方面。这些研究可以明显 

反映出目前国际地层学研究的现状和发展 

趋势。地层学研究不断深入 , 特别是一些 

经典地区和关键层段的研究依然在不断深 

入 , 这些经典地区和关键层段在研究理论 

和研究方法上的突破带动了整个地层学研 

究的发展 ; 地层学研究领域不断扩大 , 服 

务范围也不断扩大 , 地层学与其它学科相 

互渗透 , 为地层学这门古老的学科注入了 

新的生命力 ; 地层学各分支学科相互结 

合 , 向多学科综合研究的综合地层学方向 

发展。 

2008010400 

露头层序地层学研究方法综述 = Summarization 

of outcrop-based sequence stratigraphy 

research methods. ( 中文 ). 王华 ; 肖军 ; 崔宝琛 ; 

陈亮 ; 严德天 . 地质科技情报 , 2002, 21(4): 

15-22 

从露头层序地层学的研究现状和大量的 

实际工作入手 , 论述了露头层序地层学研 

究的基本内容 , 所使用的研究手段、方法 

和流程 ; 描述与分析了露头层序地层学研 

究中的地层单元界面 , 如层面、准层序和 

准层序组界面、Ⅰ 型和 Ⅱ 型层序界面的地 

表特征及其识别标志 ; 针对野外层序地层 

学研究中的图件编制问题 , 提出 “ 点、线、 

面、体、时 ” 系列图件的编绘流程与方法。 

2008010401 

从层序地层学到高分辨率层序地层学 = 

From sequence stratigraphy to high resolution 

sequence stratigraphy. ( 中文 ). 孟万斌 . 成都 

理工大学学报 , 2002, 29(4): 380-385 

简要回顾了层序地层学的发展历史 , 将 

层序地层学划分为初期阶段、地震地层学 

和现代层序地层学三个阶段。总结了层序 

地层学的主要成就和存在的问题。扼要介 

绍了高分辨率层序地层学的理论基础和关 

键定义 , 并展望了其发展前景。 

2008010402 

高精度层序地层分析 : 建立沉积相和储层 

规模的等时地层格架 = High resolution sequence 

stratigraphy analysis: construction of 

chronostratigraphic sequence framework on 

facies and reserovir scale. ( 中文 ). 林畅松 ; 刘 

景彦 ; 刘丽军 ; 张韬 ; 李喜臣 . 现代地质 , 2002, 

16(3): 276-281 

高精度层序地层分析以三级层序内高精 

度的层序地层单元的划分和对比为主要目 

的 , 它可为沉积体系的沉积构成和油气 

储、盖组合等研究提供精细的地层对比框 

架。从滨浅海至陆相湖盆的充填分析均表 

明 , 三级层序内可依据高频的海 ( 湖 ) 泛 

面或沉积基准面的变化划分出若干高精度 

的层序地层单元 , 包括四、五级层序以及 

低位、水进、高位及下降等 4 个体系域。 

四级层序的识别和对比是建立高精度层序 

地层格架的关键。在煤、油气盆地中 , 甲 

级层序是对储集体和聚煤作用进行分析的 

基本地层单元。 

古地理学、古气候学 

2008010403 

根据土耳其安纳托利亚中部科尼亚盆地沉 

积记录的晚更新世气候变化的再造 = Reconstruction 

of climatic changes during the 

Late Pleistocene, based on sediment records 

from the Konya Basin (Central Anatolia, Turkey). 

( 英文 ). Kuzucuoglu C, Bertaux J, Black 

S, Denefle M, Fontugne M, Karabiyikoglu M, 

Kashima K, Limondin-Lozouet N, Mouralis D, 

Orth P. Geological Journal, 1999, 34(1/2): 

175-198 

Climatic changes during the last climatic 

cycle have been studied using three sediment 

cores from the Konya plain, a now dry, closed 

and semi-arid lacustrine basin at 1000 m altitude 

in central Anatolia, Turkey. The reconstruction 

of regional climatic characteristics 

and evolution is based on mineral, diatom, 

pollen and molluscan content of sediments. 

Correlations are made between cores using C- 

14 and U-Th ages, stratigraphy and drought 

levels shown by changes in mineral contents. 

Environmental responses to local and regional 

climatic changes are traced by trends in authigenic 

carbonates, evaporites, detrital mineral 

content and by diatom-inferred salinity levels. 

Our data have shown that, during the period 

covering the end of the previous Glacial 

(Termination II) and the last Interglacial (between 

c. 150 and 117 ka), pear and freshwater 

shallow lakes expanded. From 117 to 66 ka, 

the plain was occupied by lakes, the salinity 

and existence of which varied in time and 

space. Specific events are marked by mineralogic 

and stratigraphic signals at (i) c. 101 ka 

and (ii) 66 ka. From 66 ka to 30 ka, desicca- 

105

tion of the lake is marked by a hiatus. At c. 27 

ka, milder climatic conditions led to the extension 

of Freshwater marshes and lakes in the 

central depressions while palaeosols developed 

on the emerged parts-of the plain. From 

25 to 20.5 ka C-14 cal., the sediments of a 

freshwater to brackish lake are present in one 

core only. From 20.5 ka C-14 cal. onwards, 

strong evaporitic conditions occurred, the lake 

edges being transformed into playas. Upper 

parts of the sequences registered other lacustrine 

short phases. both before the Younger 

Dryas and during the Holocene. 

2008010404 

阿根廷 Cabo Virgenes 最近一千年气候变 

化 = Climrate variability during the last 1000 

years in Cabo Virgenes, Argentina.. ( 其他 ). 

Mancini M V. Ameghiniana, 2007, 44(1): 

173-182 

This paper presents the pollen analysis from 

two sequences located in the southeast of 

Patagonia, Argentina, to reconstruct paleoenvironmental 

conditions during the last millennium. 

A mire ("mallin") located at 52 degrees 

19' 45"S, 68 degrees 23' 01"W, as well as a 

road cut outcrop presenting a soil within Late 

Holocene eolian and colluvial deposits at 52 

degrees 19' 47"S, 68 degrees 22' 22"W, were 

sampled. Before ca. 1000 yr BP, shrubland in 

the mire sides and a grass-shrub steppe allow 

to infer drier climatic conditions than at present. 

The increase in Poaceae and Juncaginaceae 

and later Cyperaceae preponderance in 

the mire sequence, as well as a grass steppe 

similar to the present-day steppe at regional 

scales according to soil pollen records, suggest 

moisture increase after ca. 700 yr BP. Pollen 

record data from the upper section of the soil 

profile, buried by recent eolian deposits, present 

the highest Rumex values and could 

probably be related to the impact produced by 

the introduction of sheep at the end of 19th 

Century. 

2008010405 

跨越隔水层海水的地下渗透 : 为周缘盐盆地 

提供水和盐的源泉 = Subsurface seepage of 

seawater across a barrier: A source of water 

and salt to peripheral salt basins. ( 英文 ). Nunn 

J A; Harris N B. Geological Society of America 

Bulletin, 2007, 119(9-10): 1201-1217 

Many of the great Phanerozoic salt basins 

share a common paleogeography, in which a 

deep lake or sea is separated from the ocean 

by a narrow barrier. Examples include the Aptian 

evaporites of the South Atlantic rift basins 

and the Messinian salt deposits of the Mediterranean 

Sea and the North Caspian depression. 

Marine transgressions over the barrier have 

been proposed as the origin for saline conditions 

in these basins. We test an alternate hypothesis, 

that subsurface seepage of seawater 

through the barrier was a significant source of 

water, influencing both water level and water 

composition. Our model permits flux of water 

and salt into and out of the basin via (1) seepage 

through the barrier; (2) evaporation from 

the water surface; (3) rainfall and/or rivers; 

and (4) incorporation into basin sediments. 

Our investigation focuses on three settings, a 

modern analog in the Gregory Rift of northern 

Kenya, the Messinian Mediterranean basin, 

and the Early Cretaceous Aptian salt basins of 

the South Atlantic. We test our model through 

a numerical simulation, applying reasonable 

values for the dimensions of the barrier, differences 

in water level, and hydraulic conductivities 

to calculate flow rates through the barrier. 

Modeling results indicate that flux of 

seawater through a barrier to a peripheral basin 

ranges from the dominant component of 

lake water to insignificant, depending on the 

climate, size of the peripheral basin, and hydraulic 

conductivity of the barrier. The flux of 

salt is significant over the full range of modeled 

hydraulic conductivities, producing brines 

in the peripheral lake and/or sea within 0.5 

m.y. in most cases. This demonstrates that 

seepage through the barrier can account for 

lithologic and organic geochemical evidence 

for saline water conditions, and that marine 

transgressions across the barrier are not necessary 

to explain the apparent high salinities. 

2008010406 

鄂尔多斯东部 4 000 余年来的环境与人地 

关系的初步探讨 = Discussion on the environment 

changes and the effects of human 

impacts in the east Ordos Plateau since 4 

000aB.P.. ( 中文 ). 许清海 ; 孔昭宸 ; 陈旭东 ; 阳 

小兰 ; 梁文栋 ; 孙黎明 . 第四纪研究 , 2002, 

22(2): 105-112 

本文依据地处 39°28'08"N , 

110°09'92"E, 海拔 1 219m 的伊金霍洛旗杨 

家湾古土壤剖面取得的高时间分辨率孢粉 

分析和炭屑含量统计资料揭示 :4 500aB.P. 

之前 , 鄂尔多斯东部的毛乌素沙地地区曾 

出现明显的流沙扩展 , 此后 , 气候变得比 

较湿润 , 流动沙丘逐渐被固定下来 ;4 

200~3 500aB.P. 是本区的气候适宜期 , 这 

里曾有针阔叶混交林生长 ;3 500aB.P. 以 

后 , 气候变得干燥起来 , 森林从本区消 

106

失 ;2 700~2 400aB.P., 草原植被中藜科植 

物增加 , 气候进一步向干的方面发展 , 但 

降水量仍比现在高 ;2 400aB.P. 以后 , 在全 

新世晚期气候变干和人类活动的共同作用 

下 , 全新世中期本区发育的黑垆土遭到严 

重破坏 , 流动沙丘再次活跃起来。鄂尔多 

斯杨家湾古土壤剖面的炭屑浓度变化、考 

古遗址的发现较好地反映了人类活动强度 

的变化。 

前古生界 

2008010407 

柴达木盆地北缘 “ 达肯大坂群 ” 的再厘定 = 

Redefinition of the "Dakendaban Group" on 

the northern margin of the Qaidam Basin. ( 中 

文 ). 陆松年 ; 王惠初 ; 李怀坤 ; 袁桂邦 ; 辛后田 ; 

郑健康 . 地质通报 , 2002, 21(1): 19-23 

柴达木盆地北缘原划为古元古代的 “ 达肯 

大坂群 ” 出露相当广泛 , 不仅包含了变质程 

度不同的表壳岩 , 而且包括了时代迥然不同 

的变质深成侵入体。原 “ 达肯大坂群 ” 至少 

有四种类型的岩石组合 : 其中德令哈杂岩形 

成时代最老 , 为古元古代早期的产物 ; 厘定 

后所称的达肯大坂岩群为一套中至高级变 

质、并以副变质岩为主的表壳岩系统 , 推测 

其形成时代为古元古代晚期至中元古代 ; 第 

三套岩石组合为花岗片麻岩 , 主要形成于新 

元古代早期 , 不属于沉积地层范畴 , 其中大 

量出现榴辉岩包体 ; 榴辉岩除以规模较小的 

独立包体形式赋存于新元古代花岗片麻岩 

中外 , 还和大理岩、石英岩、含石榴石片岩 

共生在一起 , 在花岗片麻岩中形成规模较大 

的残块 , 这些榴辉岩及与其共生的表壳岩共 

同构成鱼卡河或沙柳河岩群。 

2008010408 

华北地台南缘新元古代地层的新认识 = 

New view of the Neoproterozoic strata on the 

southern margin of the North China platform. 

( 中文 ). 高林志 ; 尹崇玉 ; 王自强 . 地质通 

报 , 2002, 21(3): 130-135 

根据熊耳群顶部古风化壳的确立、汝阳 

群底部小沟背组下切河谷沉积特征、白草 

坪组大型具刺疑源类和洛峪口组宏观藻类 

的发现以及罗圈冰碛岩在地层柱中的对比 

位置 , 笔者对熊耳群之上至寒武系辛集组之 

下的地层进行了重新厘定 , 将其归入新元古 

界 (1000~570Ma), 代表华北地台在 Rodinia 

超大陆聚合 - 离散期的沉积记录 ( 青白口系和 

震旦系 )。 

2008010409 

宿松群、红安群、海州群的时代归属与讨 

论 = Age assignment of the Susong 

Group,Hong'an Group and Haizhou Group:A 

discussion. ( 中文 ). 汤加富 ; 侯明金 ; 高天山 ; 钱 

存超 . 地质通报 , 2002, 21(3): 166-171 

系统介绍了分布于大别山 — 苏鲁造山带 

南部的原红安群、原宿松群、原肥东群、 

原海州群的最新研究进展 , 在将其分别解体 

为变形变质侵入体及含磷变质火山沉积岩 

系的基础上 , 对有关地层时代及其中磷矿层 

位归属提出了新的论证。 

2008010410 

湖北大洪山地区原 “ 莲沱组 ” 时代质疑 = 

Doubt about the age of the original "Liantuo 

Formation"in the Dahongshan area,Hubei 

Province,central China. ( 中文 ). 李锦轶 . 地质 

通报 , 2002, 21(8-9): 579-583 

根据野外观察 , 出露在襄樊 - 广济断裂带 

南侧大洪山地区绿林 ( 厂河 ) 镇一带主要由紫 

红色砂砾岩组成的原 “ 震旦纪莲沱组 ”, 呈 

向南缓倾斜、倾角 40° 左右的单斜岩层产 

出 , 顶部与震旦纪陡山沱组之间以一条向 

南倾斜的逆断层为界 , 底部与下伏花山群 

之间为高角度不整合而不是微角度不整 

合 ; 下伏前震旦纪 () 花山群和构造上覆的 

震旦系 — 下三叠统共同卷入了与扬子地块 

盖层岩系构造变形类似的向南的叠瓦构造 

和向南的倒转褶皱。通过组成与构造变形 

方面的研究得出该套地层可能不是震旦系 

而是中生代红层一部分的结论。 

2008010411 

南秦岭大巴山地区的下震旦统及前震旦系 

= The lower Sinian and pre-Sinian of the Daba 

Mountain area in the South Qinling region. 

( 中文 ). 唐将 ; 林源 . 中国地质 , 2002, 29(2): 

143-146 

对南秦岭大巴山地区紧邻城口 — 房县深 

断裂北侧的一套碎屑岩及沉积火山碎屑岩 

的地层剖面特征进行了描述 , 探讨了地层划 

分及时代归属 , 依据岩性特征及地层接触关 

系 , 从上至下划分为下震旦统木座组、代安 

河组及前震旦系龙潭河组。 

2008010412 

华北晚前寒武纪 ( 中、新元古代 ) 岩石地层单 

位及多重划分对比 = Late Precambrian 

(Meso-to Neoproterozoic) lithostratigraphic 

units in North China and their multiple division 

and correlation. ( 中文 ). 武铁山 . 中国地 

质 , 2002, 29(2): 147-154 

107

晚前寒武纪地层是华北早前寒武纪褶皱 

变质基底之上的第一套沉积盖层。主要发 

育和分布于华北晚前寒武纪的一些裂谷 

系 — 裂陷槽中 , 但各地沉积开始时间早晚不 

一 , 后期遭受剥蚀程度不一。长期以来在地 

层划分、岩石地层命名、使用及年代属性 

上认识不统一 , 在一些地区认识分歧很大。 

笔者在岩石地层单位、地质特征认识的基 

础上 , 进行了全区 ( 群、组 ) 统一对比 , 明确了 

可作为华北晚前寒武纪沉积序列的代表性 

岩石地层单位及岩石组合特征 ; 并介绍晚前 

寒武纪叠层石组合、微古植物特征性分子 

和已发现的宏观藻类和后生动物 , 论述了层 

型所在地区年代地层划分及层型以外各地 

层分区岩石地层单位年代属性的确定依 

据。 

2008010413 

关于中国新元古界划分几个问题的讨论 = 

Discussion on the new subdivision of the 

Neoproterozoic in China. ( 中文 ). 陆松年 . 地 

质论评 , 2002, 48(3): 242-248 

2001 年 4 月正式出版的《中国地层指南 

及中国地层指南说明书》( 修订版 ) 中将 

新元古界从二分变为三分 , 自下而上分别 

为青白口系、南华系和震旦系。本文首先 

介绍了震旦系重新定义的背景和必要性。 

由于近些年国际末元古界分会酝酿在新元 

古代末期新建一个系 , 而多数学者的意见 

是该系的下界应置于冰碛层之上 , 即大致 

相当于我国陡山沱阶的底部。鉴于此 , 在 

1999 年 12 月初断代工作组会议期间 , 晚前 

寒武系工作组的与会专家一致认为 , 有必 

要对震旦系重新定义 , 并决定将原震旦系 

解体 , 原上统代表重新定义的震旦系 , 原 

下统独立新建一个系 , 命名为 “ 南华系 ”。 

由于震旦系的再分 , 新元古界也从二分变 

为的三分 , 重新界定的震旦系包括原上震 

旦统灯影组和陡山沱组 , 南华系包含了原 

下震旦统南沱组和莲沱组。笔者认为南华 

系标准剖面的候选剖面应具备下列基本条 

件 :1 上覆有震旦系下部陡山沱组及其相 

当层位的地层 , 该地层与南华系顶部地层 

之间沉积记录的缺失应是最少的 ;2 剖面 

中应包括寒冷性气候的冰川沉积记录 , 虽 

然在全国性南华系地层对比中 , 冰成岩层 

不是绝对的对比标志 , 但为有利于全球对 

比 , 我国南华系候选标准剖面应将冰成岩 

层包括其内 ;3 剖面中应出露莲沱组 ( 约 

750Ma) 或与其时代相近层位 ( 休宁组、 

志棠组等 ) 之下的一套地层 , 这套地层与 

莲沱组之间不应存在长期的沉积间断 , 且 

底部年龄不小于 800Ma , 也不大于 

850Ma;4 剖面中有良好的区域的、全国 

的 , 甚至洲际间的地层学对比标志 , 有较 

高的岩石地层学、年代地层学、生物地层 

学和其他方面的研究水平 ;5 剖面的连续 

性好、露头清晰、交通方便 , 且周围的自 

然环境较好。 

2008010414 

湖北宜昌峡东地区震旦系层型剖面化学地 

层特征及其国际对比 = Chemostratigraphic 

characteristic and correlation of the Sinian 

stratotype in the eastern Yangtze Gorges area, 

Yichang, Hubei Province. ( 中文 ). 王自强 ; 尹 

崇玉 ; 高林志 ; 柳永清 . 地质论评 , 2002, 48(3): 

408-415 

全球末元古系建系研究是当前国际地层 

学研究的重要课题之一。我国宜昌峡东地 

区震旦系沿江剖面研究历史悠久 , 已有相 

当深入的岩石地层、生物地层及层序地层 

研究 , 并被推荐为国际末元古系侯选层序 

剖面之一。为进一步提高其研究精度 , 本 

文系统地研究了震旦系沿江剖面碳酸盐岩 

同位素化学地层。研究结果表明 , 陡山沱 

组底部 “ 碳酸盐岩帽 ” 的 δ 13 C 为 -3.1‰~3.7‰ 

向上 , 向上为正偏移 , 至层序 III(DS3) 

最大值达 +6.7%‰。陡山沱组顶部 (DS6) 

再次出现负偏移 -2.5‰, 构成一个完整的变 

化周期。同时 , 87 Sr/ 86 Sr 表现出向上增大的 

变化 , 由陡山沱组底部 (DSI ) 的 

0.707743 逐渐增高至陡山沱组顶部 (DS6) 

的 0.707965; 灯影组蛤蟆井段 (DS7) 的 

δ 13 C 值变化在 -2.5‰~+5‰ 之间 (DS8), 

至石板滩段中部再次降至 +1.7‰ 

(DS10), 而后基本保持在 +1.7‰~3.6‰ 

之间平稳变动。白马沱段顶部 δ 13 C 再次降 

至 +0.5‰, 并有向负偏移的趋势。灯影组 

的 87 Sr/ 86 Sr 值依然出现由老至新递增的趋势 

(0.708244~0.708993) 与当前国际末元古 

系剖面的化学地层特征基本一致。 

2008010415 

前寒武纪生物起源时间的化石和分子钟研 

究 = Rossil records and molecular clock study 

of the time of origin of the Precambrian biologic 

lineages. ( 中文 ). 柯叶艳 ; 齐文同 . 地质 

论评 , 2002, 48(5): 457-462 

时间尺度的确定 , 对于估计生物有机体 

的分子和形态改变的速率 , 以及建立大进 

化和生物古地理学模式都是非常必要的。 

传统的化石记录和新兴的分子钟研究 , 是 

108

可以提供生物谱系起源和分支时间的两种 

手段。占整个地球生命历史七分之六的前 

寒武纪 , 是地球及地球上生命演化的重要 

时期。对前寒武纪相当繁荣的微生物的起 

源时间和后生动物各门类的分支演化时间 

的研究 , 一直存在着很大的争议。本文在 

总结化石记录和分子钟研究结果时发现 : 

由于分子钟研究得的早期微生物的起源时 

间明显晚于化石记录。而在后生物分支演 

化时间的估算上却早于化石资料。本文试 

图从两种方法自身的特点来讨论这种分支 

演化时间的重大差别。 

2008010416 

中国南方海相震旦系 — 中三叠统层序划分 

与对比 = Division and correlation of the sequences 

of marine Sinian system to Middle 

Triassic series in the south of China. ( 中文 ). 

陈洪德 ; 田景春 ; 刘文均 ; 许效松 ; 郑荣才 ; 牟传 

龙 ; 李余生 ; 覃建雄 . 成都理工大学学报 , 2002, 

29(4): 355-379 

在对中国南方不同地区海相震旦系 — 中 

三叠统基于干剖面和辅助剖面详细观测研 

究的基础上 , 对震旦系 — 中三叠统进行了 

系统的层序划分对比 , 共识别出 13 个超层 

序和 99 个三级层序 , 讨论了 13 个超层序 

的特征 , 建立了中国南方海相震旦系 — 中 

三叠统的层序格架。总体上看各超层在整 

个中国南方不同盆地、不同相带的剖面上 

可以完全对比 , 但同一个超层序内所包含 

的三级层序个数及完整性有所不同。对于 

三级沉积层序来说 , 半数以上可以得到化 

石带较为准确的年代控制并在同一个构造 

分区甚至整个中国南方进行对比 , 部分层 

序甚至还可以在三级层序的体系域层次进 

行对比。表明从整个中国南方来看二级相 

对海平面升降变化更具有一致性 , 而三级 

相对海平面的变化规律在不同盆地、不同 

相带有所差异。 

2008010417 

关于我国前寒武纪研究中几个重点问题的 

分析 = A review of major problems of Precambrian 

research. ( 中文 ). 陆松年 . 地质调查 

与研究 , 2002, 25(2): 66-72 

在综合分析国内外前寒武纪地质研究运 

动向的基础上 , 强调应加强研究的几个问 

题 , 其中包括在古大陆上进一步识别始太 

古代地壳和深化对古老地壳组成及特点的 

研究 ; 对我国元古界系统年代地层单位的 

南华系建系进行了分析 ; 对孔兹岩系 , 榴 

辉岩相变质和蛇绿岩等凝难地层和疑难地 

质事件时间维的确定应在进行微区测定的 

同时 , 深入对测年对象成因矿物学的研 

究 ; 在前寒武纪超大陆和超大陆事件的研 

究过程中 , 应加强综合地层学方法的研 

究 , 立足于实际 , 重点解决我国几个古大 

陆之间的相互关系及它们在超大陆中的位 

置 , 同时强调微大陆块体地史演化对研究 

造山带和古大陆复原工作的重要性 ; 最后 

讨论了重大地质事件所引发的资源与环境 

效应。 

2008010418 

柴北缘前震旦纪地层系统的新认识 = New 

idea on Pre-Sinian strata in the northern margin 

of Qaidam Massif. ( 中文 ). 辛后田 ; 郝国杰 ; 

王惠初 ; 陈能松 ; 韩英善 ; 祁生胜 . 地质调查与 

研究 , 2002, 25(2): 113-119 

柴北缘的变质基底具有复杂的岩石组 

成 , 除成因迥异的多期变质深成侵入体 

外 , 还包括变质程度不同的表壳岩。南带 

的沙柳河、鱼卡河等地出现露大理岩、石 

英岩、含石榴石片岩和条状斜长角闪岩等 

以副变质岩为主的表壳岩系 , 共同构成了 

中元古界沙柳河岩群 ; 而出露在北带全吉 

山、德令哈等地的中高级变质表壳岩系 , 

则为形成于古元古代并具有较强的钾质混 

合岩化的达肯大板岩群。柴北缘的榴辉岩 

分布在南带 , 除以规模较小的透镜体状赋 

存于新元古代花岗片麻岩中外 , 还和沙柳 

河岩群共生 , 但在北带的达肯大坂岩群中 

没有出现。全吉群的时代为南华纪至震旦 

纪。 

2008010419 

新元古代 “ 雪球 ” 冰川时期的气候旋回 = 

Climatic cycles during a Neoproterozoic 

"snowball" glacial epoch. ( 英文 ). Rieu R; Allen 

P A; Plötze M; Pettke T. Geology, 2007, 

35(4): 299-302 

The profound glaciations of the Neoproterozoic 

Cryogenian period (ca. 850–544 Ma) 

represent an extreme climatic mode when, it is 

claimed, Earth was fully or almost completely 

covered with ice for millions of years. We 

show that the geochemistry and mineralogy of 

fine-grained Neoproterozoic sedimentary 

rocks in Oman are best explained by climatic 

oscillations that drove variations in the intensity 

of chemical weathering on contemporary 

land surfaces. The cold climate modes of the 

Cryogenian were therefore cyclical, punctuated 

with well-defined warm-humid intergla- 

109

cial periods. The hydrological cycle and the 

routing of sediment were active throughout the 

glacial epoch, which requires substantial open 

ocean water. This reconstruction represents a 

significantly different target for numerical 

climate models at this critical time in the evolution 

of Earth's biosphere. 

2008010420 

南华纪地层及年代构造格架 = Nanhuaian 

strata and chrono-tectonic framework. ( 中文 ). 

冯国富 ; 孙海清 ; 陈俊 . 湖南地质 , 2002, 21(3): 

173-174 

根据湖南地层发育情况 , 依国际地层划 

分标准和中国地层指南要求 , 将湖南省境 

内原震旦纪早世划归新元古代南华纪 , 地 

层系统可分为 3 个相区。综合已有同柆素 

测年数据 , 初步建立起南华纪年代构造格 

架 , 确立南华纪底界年龄为 800 Ma 左右 , 

顶界年龄为 700 Ma 左右。 

古生界 

2008010421 

西藏措勤 — 申扎地层分区二叠系敌布错组 

的建立及其特征 = Permian Dibuco Formation 

in the Coqên-Xainza stratigraphic 

area,Tibet. ( 中文 ). 周幼云 ; 江元生 ; 王明光 . 地 

质通报 , 2002, 21(2): 79-82 

敌布错组为 1∶ 

25 万措勤区幅区域地质 

调查首次发现并建立的岩石地层单位。该 

组角度不整合于下二叠统下拉组之上 , 盛产 

冈瓦纳 — 华夏混合植物群化石 , 岩性组合呈 

现灰色复陆屑建造的特点 , 厚度大于 

830m。层型剖面位于西藏措勤县江让乡敌 

布错北缘 (E84°46',N30°51')。2001 年夏经专 

家实地考查确认 , 该剖面已完全具备建组条 

件。此套岩石组合的发现为进一步完善冈 

底斯构造带古生代地层系统提供了新的资 

料。 

2008010422 

辽东半岛南部寒武系与奥陶系的界线 = 

Cambrian-Ordovician boundary on the southern 

Liaodong Peninsula. ( 中文 ). 关培彦 ; 李超 

英 . 地质通报 , 2002, 21(2): 95-97 

在辽南瓦房店市长兴岛镇二龙山、长岭 

子等地的寒武纪 — 奥陶纪冶里组上部首次 

发现 Saukia,Calvinella 等属种的化石 , 确定了 

Saukia—Calvinella 组合带 , 为晚寒武世凤山 

阶最顶部的化石带。此外在该带之上采到 

了微体化石 Ulahconus beimadaoensis, 该化 

石属种为奥陶纪早期的标准分子。据此重 

新厘定了辽南地区寒武系与奥陶系的界 

线。 

2008010423 

滇西昌宁 — 孟连带的地层格架 = Stratigraphic 

framework of the Changning- 

Menglian belt in western Yunnan. ( 中文 ). 金 

小赤 ; 王义昭 ; 谢广连 . 地质通报 , 2002, 21(4): 

315-321 

显生宙地层在昌宁 — 孟连带呈南北向条 

带状分布 , 根据不同岩性的横向分布和纵向 

变化情况 , 可将带中的地层序列大致划分成 

4 种类型 :(1) 碎屑岩向上夹灰岩透镜体 , 并变 

成细粒碎屑岩和硅质岩交互出现 ;(2) 碎屑岩 

向上夹灰岩透镜体、少量硅质岩 , 顶部为二 

叠纪基性火山岩 ;(3) 碎屑岩 — 基性火山岩 / 火 

山碎屑岩 — 碳酸盐岩 — 碎屑岩 ;(4) 灰岩、白 

云质灰岩 — 灰黑色薄层灰岩、泥质灰岩、 

泥岩夹硅质泥岩。理清不同岩石地层单位 

间的关系是客观解释昌宁 — 孟连带发展演 

化的前提。 

2008010424 

西藏中南部尼雄 — 文部地区中 — 晚二叠世 

坚扎弄组的发现及其地质意义 = Discovery 

of the Mid-Late Permian Jianzalong Formation 

in the Nyixung-Ombu area in southcentral 

Tibet Autonomous region of China. 

( 中文 ). 李晓勇 ; 谢国刚 ; 徐银保 ; 徐祖丰 ; 欧阳 

克贵 . 地质通报 , 2002, 21(4): 339-344 

笔者在进行 1∶ 

25 万邦多区幅和措麦区 

幅区域地质调查期间 , 于措勤县尼雄和尼玛 

县文部等地发现一套陆相为主的海陆交互 

相地层。其岩性组合面貌非常特殊 , 富含植 

物化石 , 与坚扎弄组层型剖面可以对比。植 

物群面貌具有华夏和冈瓦纳植物群中非典 

型分子的双重性质 , 无论从植物化石本身、 

沉积特征 , 还是从海水进退规律及气候环境 

等方面综合分析 , 地层时代宜归晚二叠世 , 但 

不排除属中二叠世最晚期的可能性。 

2008010425 

西班牙北部中石炭统界线 : 全球层型剖面 

和点对比的难点 = The Mid-Carboniferous 

boundary in northern Spain: Difficulties for 

correlation of the global stratotype section and 

point. ( 英文 ). Sanz-Lopez J; Blanco-Ferrera S; 

Garcia-Lopez S; Sanchez de Posada L C. Rivista 


2006, 112(1): 3-22 

The stratigraphy of latest Arnsbergian to 

early Chokierian is described for the Barcaliente 

Formation in the Cantabrian Mountains. 

110

The conodont content has been studied at the 

Millaro section, where the appearance of Declinognathodus 

noduliferus Ellison & Graves, 

in the lower metres of the Barcaliente Formation 

is conformed, and the location of the Mississippian/Pennsylvanian 

boundary is discussed. 

The new subspecies D. noduliferus 

bernesgae is described and other records are 

also studied from the Pyrenean Azkarate section. 

2008010426 

西藏文部一姆错丙尼地区早二叠世拉嘎 

组 —— 兼述杂砾岩形成环境与成因 = Early 

Permian Raka Formation in the Ombu-Monco 

Bunnyiarea,Tibet--With a discussion of the 

formation environment and origin of 

petromictic conglomerate. ( 中文 ). 李晓勇 ; 谢 

国刚 ; 袁建芽 ; 肖业斌 ; 黄传冠 . 地质通 

报 , 2002, 21(11): 723-727 

通过 1∶ 

250000 邦多区幅和措麦区幅区 

域地质调查 , 对西藏文部 — 姆错丙尼地区的 

早二叠世拉嘎组进行了地层古生物及杂砾 

岩特征的研究 , 发现赋存于滑塌块体中的生 

物化石反映的地质时期为早二叠世 

Sakmarian—Artinskian 期 , 而滑塌块体的 “ 基 

质 ” 地层时代应稍晚于早二叠世 

Sakmarian—Artinskian 期 ; 沉积特征表明杂 

砾岩成因具冰海相和水下块体重力流的复 

合 ( 双重 ) 性质。 

2008010427 

中朝地台的志留系 — 纪念中、韩两国杰出 

的微体古生物学者安太庠和李河荣 = Discussion 

on Silurian in Sino-Korean Plateau:in 

commemoration of distinguished micropaleontologists 

AN T.X. of China and Lee H.Y. of 

Korea. ( 中文 ). 李东津 ; 殷长建 ; 路孝平 . 世界 

地质 , 2006, 25(4): 323-331 

中朝地台内部无争议的志留系只有朝鲜 

半岛平南盆地的谷山组和宝良里组。中朝 

地台北缘活动陆缘带志留系比较发育 , 有桃 

山组、西别河组 ( 至少其大部分 ) 等。李河荣 

等根据牙形刺将朝鲜半岛太白山盆地的桧 

洞里组划归志留系 , 但是从层序、岩石和安 

太庠修定的牙形刺化石来看 , 桧洞里组可能 

不是志留系 , 而是与中朝地台华北区峰峰组 

八陡段 ( 或包括部分耀县组 ) 可比的中奥陶世 

地层。微体古生物学家安太庠和李河荣分 

别为中国和韩国的牙形学及其生物地层学 

研究做出了重要贡献。他们的英年早逝 , 对 

东北亚地学研究是一个重大损失。 

2008010428 

西天山东段天格尔峰 — 艾维尔沟一带泥 

盆 — 二叠纪地层的厘定及地质意义 = Redefinition 

of the Devonian-Permian in the 

Tengger Mountain-Ewirgol area,eastern segment 

of the West Tianshan Mountains,and its 

geological significance. ( 中文 ). 苏春乾 ; 杨兴 

科 ; 崔建军 ; 刘继庆 . 中国地质 , 2006, 33(3): 

516-528 

天格尔峰 — 艾维尔沟一带处于东、西天 

山交界部位 , 长期以来 , 其地层单元划分、时 

代归属、分布范围和名称使用均不统一 , 给 

天山构造带的研究带来诸多的问题。通过 

东西 6 幅 1∶ 5万区域地质调查 , 在北天山原 

奇尔古斯套组 ( 天格尔组 ) 分布区域发现了两 

条不整合面和大量化石资料。结合岩石组 

合特征、同位素年龄数据、变质 - 变形作用 

和沉积背景的差异 , 进一步将原奇尔古斯套 

组 ( 天格尔组 ) 解体为上泥盆统天格尔组 ( 狭 

义 )、上石炭统奇尔古斯套组 ( 狭义 )、上石 

炭统后峡组和下二叠统阿尔巴萨依组 , 并填 

绘出了各地层单元的分布范围 , 厘定了测区 

的构造格局。为东西天山地层单元的对比 

和构造区划提供了重要依据。 

2008010429 

西藏北部永珠地区石炭系永珠组岩石地层 

和古生物特征 = Lithostratigraphic and paleontological 

characteristics of the Carboniferous 

Yunzhug Formation in the Yunzhug area, 

northern Tibet. ( 中文 ). 张树岐 ; 王永胜 ; 曲永 

贵 . 中国地质 , 2006, 33(5): 980-987 1 图版 . 

永珠地区位于申扎古生代盆地 , 区内发育 

连续的早奥陶世 — 中二叠世海相沉积序 

列。石炭系永珠组岩石组合特征为细粒石 

英砂岩、页岩、粉砂岩 , 夹多层生物碎屑灰 

岩 , 含丰富的生物化石 , 主要有腕足类、双壳 

类、牙形刺、珊瑚、苔藓虫、菊石、三叶 

虫。牙形刺 Gnathodus girtyi—Gnathodus 

texanus 为早石炭世晚期组合 ; 腕足类 

Productus—Rhipidomella tibetena 为早石炭 

世晚期组合 ,Choristites—Spirigerella 为晚石 

炭世早期下部组合 ,Trigonatreta cf. paucicostulata—Elivella 

baschkirica 为晚石炭世早 

期上部组合。Uncinunellina 是典型的冷水习 

性腕足类 ,Cyathaxonia 是典型的冷水习性珊 

瑚 , 表明了全球石炭纪冰期已影响到本区。 

确定了永珠组的时代为早石炭世晚期 — 晚 

石炭世早期 , 且早石炭世与晚石炭世分界线 

在第 11 层与第 12 层之间。 

2008010430 

111

四川九寨沟地区泥盆 — 三叠系多重地层划 

分对比及沉积环境 = Multiple stratigraphic 

classification and correlation of the Devonian- 

Triassic in the Jiuzhaigou area, Sichuan, and 

its sedimentary environment. ( 中文 ). 彭东 ; 谢 

云喜 ; 王明光 ; 吴树通 . 中国地质 , 2006, 33(5): 

1013-1022 

位于青藏高原东缘四川盆地接壤处的四 

川九寨沟地区发育了总厚 6 000m 以上的碳 

酸盐岩 , 通过 1:5 万区域地质调查和一系列 

专项调查 , 将该区内岩石地层划分为 9 个岩 

组。生物地层划分了 3 个珊瑚组合带 ,3 个 

腕足组合带 ,1 个腕足顶峰带 ,2 个双壳顶峰 

带以及有孔虫组合带和顶峰带各 1 个。生 

态地层研究划分了两个生态群落。根据地 

球化学元素特征划分了 11 个地球化学段。 

研究了地层的常量元素和碳同位素特征。 

对碳酸盐岩进行了微相分析。综合各项沉 

积标志进行了沉积环境判别 , 其中岷河组沉 

积环境最为特殊 , 属于碳酸盐岩和陆源碎屑 

的混合沉积体系。 

2008010431 

南华北上二叠统石千峰组物源与沉积环境 

分析 = Sedimentary environment patterns 

analysis on Shiqianfeng Formation of Upper 

Permian in southern part of North China. ( 中 

文 ). 白斌 ; 周立发 ; 刘彬辉 ; 谢其锋 . 西北大学 

学报 ( 自然科学版 ), 2006, 36(3): 461-466 

目的为恢复华北南部地区石千峰组原盆 

地沉积环境格局 , 为进一步研究华北南部地 

区二叠系沉积地质与盆地原型提供支持。 

方法根据岩石碎屑组分基本数据 , 运用地层 

厚度、砂岩百分含量、古水流、砂岩成分 

的系统分析方法。结果研究区地层自南西 

向北东呈现依次增厚的趋势 , 整体为北东方 

向倾斜的宽缓斜坡环境 ; 砂岩分布特征指示 

物源来自南部隆起区和沉积中心在研究区 

以北地区。结论华北南部地区石千峰组整 

体属于近山的海陆过渡相陆缘近海湖环境 

内的充填物 , 沉积物质主要来源于南部的秦 

岭古隆起 , 并向晚二叠世华北盆地南部提供 

了大量的陆源碎屑物质。 

2008010432 

西天山阿吾拉勒一带阿克沙克组的厘定 = 

Confirmation of the Akeshake Formation in 

the Awulale belt in the western Tianshan. ( 中 

文 ). 高永利 ; 李永军 ; 孔德义 ; 郭文杰 ; 栾新东 ; 

张家勇 . 新疆地质 , 2006, 24(3): 215-217 

在西天山阿吾拉勒一带前人确立的大哈 

拉军山组中 , 新发现一套富含早石炭世腕足 

和珊瑚等化石的浅海相碳酸盐岩 - 碎屑岩建 

造 , 其与上覆大陆裂谷双峰式火山岩建造 ( 伊 

什基里克组 ) 及下伏岛弧钙碱性火山岩建造 

( 大哈拉军山组 ) 间均为角度不整合接触 . 新 

发现地层在岩石组合、生物面貌、沉积环 

境、接触关系等方面均与阿克沙克组层型 

剖面可对比 , 故将其从大哈拉军山组解体出 

来 , 对比厘定为阿克沙克组 . 这一地层单位的 

合理确立 , 为区域地质填图建立了正确的岩 

石地层单位 , 并为本区的地层划分和区域对 

比提供了新的依据 . 

2008010433 

塔中地区寒武 — 奥陶系层序地层格架与沉 

积演化特征 = The research on sedimentation 

features in Cambrian-Ordovician sequence 

frame in the center of Tarim. ( 中文 ). 陈新军 ; 

蔡希源 ; 徐旭辉 ; 朱建辉 ; 唐大卿 . 新疆地 

质 , 2006, 24(3): 276-280 

通过层序地层学的划分与对比 , 将塔中地 

区寒武 — 奥陶系划分出 8 个超层序 . 其中寒 

武系包含 3 个超层序 , 奥陶系包含 5 个超层 

序 , 下奥陶统 2 个 , 中上奥陶统 3 个 . 塔中地区 

寒武 — 奥陶系沉积相具有典型的分层结构 , 

沉积相在纵向演化上 , 由下部的蒸发台地、 

局限台地相、开阔台地相 , 向上变为台地边 

缘相、浅水陆棚相、混积陆棚相及斜坡相 , 

代表了海水向上持续增深过程 . 

2008010434 

柴达木盆地石炭纪古生态与沉积环境 = 

Paleoecology and sedimentary environment of 

Carboniferous in Qaidam Basin. ( 中文 ). 杨平 ; 

胡勇 . 新疆石油地质 , 2006, 27(3): 280-284 

在建立了统一的地层格架和生物地层序 

列的基础上 , 结合古生态及沉积特征综合分 

析了柴达木盆地石炭纪沉积相。柴达木盆 

地东北缘下石炭统富含珊瑚、腕足等化 

石。珊瑚由小型单体向大型单体和复体演 

化 , 化石属种由少变多、丰度明显增加 , 反映 

了沉积环境趋于稳定和水体加深的过程。 

同时 , 石炭系剖面岩性出现由砂砾岩或砂、 

页岩 - 灰岩组成的两个沉积旋回 , 表明沉积环 

境由滨岸向碳酸盐台坪演变。上石炭统生 

物群以蜓类为主 , 腕足类、珊瑚次之 , 下部植 

物化石丰富。腕足个体变小和珊瑚化石减 

少 , 与浅水和变冷的气候有关。岩性为砂、 

页岩 - 灰岩互层 , 沉积环境以滨岸潮坪为主 , 

下部沼泽发育。西南缘下石炭统生物以珊 

瑚、腕足类为主 , 岩性和生物有与东北缘相 

似的旋回特征。上石炭统以竽蜓类为主 , 腕 

112

足次之 , 岩性以生物碎屑灰岩和鲕状灰岩为 

主。西南缘石炭纪沉积环境主要以浅海高 

能环境的台滩和能量较低的台坪交互发育 

为特征。分析表明 , 早石炭世两度海侵 , 晚石 

炭世持续海进 ; 西南缘多发育有利于储油的 

碳酸盐台滩相 , 东北缘多发育有利于形成生 

储盖配套体系的海陆交互相。 

2008010435 

塔里木盆地轮南奥陶系研究新进展 = Advances 

in Ordovician study of Lunnan area in 

Tarim Basin. ( 中文 ). 刘静江 ; 袁玉春 ; 龙维华 ; 

胡龙迪 . 新疆石油地质 , 2006, 27(6): 667-669 

受资料条件的限制 , 以往对轮南地区奥陶 

系内部的接触关系并不十分清楚。近期通 

过钻探和系统的地质研究发现了一些直接 

的地层不整合证据 , 证明轮南奥陶系内部存 

在多期地层不整合。桑塔木组、良里塔格 

组、吐木休克组之间都是不整合接触 , 而一 

间房组和吐木休克组之间则是整合接触。 

在连续的化石带里可能也会出现较长时间 

的地层不整合。 

2008010436 

湖南慈利晚二叠世长兴期珊瑚礁白云石化 

及其成岩环境 = Dolomitization and 

diagenetic environments of Late Permian 

Changxingian coral reefs in Cili, Hunan, 

South China. ( 中文 ). 杨万容 ; 杨长庚 ; 沈建伟 . 

地质学报 , 2002, 76(1): 114-123 

笔者对近期在湖南慈利发现的长兴期珊 

瑚礁的白云石化作用及成岩环境进行了研 

究。通过对礁灰岩白云石化的分布、岩石 

结构构造、微量元素和碳、氧稳定同位素 

成分的测试研究 , 对白云石化的环境进行了 

分析。主要有 :1 潮上蒸发形成的高盐度交 

代白云石化 ;2 深埋藏高盐度热水条件下白 

云石化 ;3 区域抬升埋藏变浅 , 大气水渗入淡 

化的热水条件下发生的白云石化。据各类 

白云石化在礁岩成岩序列中的位置 , 从早到 

晚分别命名为 Ⅰ、Ⅱ、 Ⅲ 3 个世代 , 并分析 

了埋藏白云石化的物源 , 建立了 Ⅱ、Ⅲ 两个 

世代埋藏白云石化的概略模式。最后通过 

实例说明了研究礁岩埋藏白云石化作用对 

油气、铅锌矿产勘探的实用意义。 

2008010437 

东昆仑早 — 中二叠世生物礁建造特征 = 

Reef-building mechanism in the Early-Middle 

Permian, the East Kunlun. ( 中文 ). 田树刚 ; 范 

嘉松 . 地质学报 , 2002, 76(2): 145-154 

本文从造礁群落演替、层序地层和海平 

面升降等方面 , 结合大地构造引起基底沉降 

的证据 , 论述了东昆仑早 — 中二叠世生物礁 

的建造特征。东昆仑生物礁中包含 6 种造 

礁群落 , 各群落生物组成和结构与环境因素 

密切相关 ,4 个生物礁发育阶段中群落演替 

关系显著。礁相地层中可识别 SB 1 层序界面 

1 个和 

SB 2 界面 4 个 , 可划分出 5 个三级层序。 

层序的沉积相序显示清晰 , 按曲线形态将海 

平面升降归为 4 个周期。据区域地层和相 

分布资料反映的古地理环境变迁 , 推论出石 

炭纪至早 — 中二叠世造礁期柴达木地块与 

羌塘地块间聚合离散的 4 个构造期。东昆 

仑生物礁的生长发育与造礁群落的演化阶 

段、海平面升降周期和大地构造期彼此吻 

合 , 证明生物礁建造与各控制因素间具密切 

制约关系。海西中 — 晚期柴达木地块与羌 

塘地块的开 — 合转换 , 为生物大规模造礁创 

造了长期稳定的环境。 

2008010438 

中国上石炭统上部及下二叠统海相地层中 

阶的划分 = Stages of upper Upper Carboniferos 

and Lower Permian marine strata in 

China. ( 中文 ). 夏国英 ; 丁蕴杰 . 中国地 

质 , 2002, 29(1): 20-29 

明确而详细地提出了中国上石炭统上部 

及下二叠统海相年代地层单位的具体框 

架。将上石炭统上部划分为逍遥阶、下杨 

家河阶 ; 下二叠统划分为上杨家河阶、范家 

河阶、垭口阶及隆林阶。明确了阶的定 

义、动物群特征、磁性地层特征及其与相 

关地层的关系。所划分的阶均能与世界标 

准年代地层进行详细而有依据的对比。 

2008010439 

西藏林周旁多地区晚古生代层序地层特征 

= Characteristics of C-P sequence stratigraphy 

in northern margin of Gondwana land-- 

Exemplified by Pangduo profile, Linzhou, 

Tibet. ( 中文 ). 杨欣德 ; 纪占胜 ; 臧文拴 . 地球 

学报 - 中国地质科学院院报 , 2002, 23(4): 

317-322 

通过详细的层序地层研究 , 重建了冈瓦 

纳大陆北缘石炭 - 二叠纪层序地层序列 , 在 

详细的岩相 , 准层序研究的基础上 , 划分出 

2 个二级层序和 11 个三级层序。研究区的 

含砾细碎屑岩系滨岩浅水冰筏 ( 或浮水 ) 

沉积物经密度流再搬运到深水区的产物。 

旁多群上部滨岸河流相沉积层序的发现 , 为 

113

石炭 - 二叠纪冰期研究提供了新的沉积岩 

石学资料。 

2008010440 

长江三峡地区乐平统与阳新统的分界 = 

Boundary between the Yangsingian and Lopingian 

series in the Yangtze Gorges area. ( 中 

文 ). 冯少南 ; 李旭兵 . 华南地质与矿产 , 2002, 

(2): 66-69 

长江三峡地区阳新世 — 乐平世沉积可以 

分为南型和北型。北型该期主要为浅海碳 

酸盐岩台地沉积 , 阳新世晚期的王坡组为粘 

土岩夹灰岩或硅质灰岩扁豆体 , 产 Yabenia 带 

及有孔虫 , 其上覆的吴家坪组产 Clarkina 

leveni, C. liangshanensis 等 , 阳新统与乐平统 

的分界置于 Yabenia 带的顶和含 C. leveni( 可 

能有 C. dukouensis 带 ) 的吴家坪组底。南型 

从阳新世晚期至乐平世主要为硅质岩、硅 

质灰岩 , 夹含煤碎屑岩 , 在吴家坪组的底部含 

牙形石 C. dukouensis 带和 C. leveni 带 , 该区阳 

新统与乐平统的分界置于 C. dukouens 带泥 

质灰岩 ( 腕足类富集层 ) 的底 , 下伏的煤系地 

层时代为阳新世晚期。 

2008010441 

川东二叠纪生物礁的再认识 = Restudies on 

Permian reefs in eastern Sichuan,China. ( 中 

文 ). 范嘉松 ; 吴亚生 . 石油与天然气地 

质 , 2002, 23(1): 12-18 

通过川东 8 口二叠纪长兴期钻井岩芯剖 

面的详细研究 , 铁山 5 井、天东 10 井代表典 

型的礁相剖面 ; 板东 4 井、双 15 井既有礁相 

沉积 , 且有棘屑滩沉积 ; 卧 117 井、黄龙 1 井 

以及云安 14 井基本上由碳酸盐台地沉积组 

成 ; 池 24 井出现两种类型的礁相 : 海绵骨架 

礁和海绵障积礁。川东礁相剖面中的白云 

岩以海水与淡水混合作用而成的白云石化 

为主导因素 , 但它们在深埋阶段以后 , 又遭受 

后期白云石化的叠加 , 因此表现出许多深埋 

白云石化的地化特征。白云岩的原始沉积 

既可能是礁骨架岩 , 也可能是棘屑滩 , 甚至是 

碳酸盐台地沉积。因此在寻找礁型白云岩 

储层时 , 还应注意滩相白云岩储层以及一般 

的碳酸盐台地白云岩储层。 

2008010442 

轮南 - 巴楚地区奥陶系生物礁储层特征 = 

Ordovicion reef in Lunan-Bachu area and 

their reservoir characteristics. ( 中文 ). 胡明毅 ; 

朱忠德 ; 贺萍 ; 张俊 ; 王青春 . 石油与天然气地 

质 , 2002, 23(2): 179-182 

塔里木盆地轮南巴楚地区奥陶系生物礁 

赋存于中奥陶统一间房组和上奥陶统桑塔 

木组 , 主要造礁生物为瓶筐石 , 其次为海绵 

类、苔藓虫类和有柄棘皮动物类。礁体规 

模较小 , 形态多样 , 礁体一般由礁基、礁核和 

礁盖三部分组成。含礁层系储层物性总体 

比较差 , 以低孔低渗或低孔中渗为特征 , 但是 

礁基、礁盖储层物性明显好于礁体本身。 

礁体储层类型为裂缝型或孔隙裂缝型储层 , 

储层性能主要受沉积相和成岩作用控制。 

2008010443 

华北地层大区寒武纪早期地层统一划分与 

对比问题 = On unified division and correlation 

of the Early Cambrian strata in the North 

China stratigraphic province. ( 中文 ). 刘德正 . 

安徽地质 , 2002, 12(1): 1-24 

基于华北地层大区数百条寒武纪早期地 

层剖面与安徽淮南地区基准层序 (2 组 2 亚 

组 15 段 1 个亚段 ) 和带序 (6 个三叶虫带 ) 的 

确切对比 , 编制了新的沉积分区图 ; 依据有无 

猴家山组和馒头组下亚组是否完整 , 划分出 

5 个沉积区 ; 讨论了各区与基准层序 — 带序 

的对比 ; 明确了各地方性岩石地层单位 ( 五山 

组、李官组、碱厂组、辛集组、朱砂洞 

组、苏峪口组、五道淌组、昌平组、府君 

山组、老庄户组、水洞组、黑沟组等 ) 的层 

位归属 ( 具体至段 ), 确认与寒武纪早期地层 

有关的 3 个沉积间断 ( 皖北上升、豫陕上升 

和燕辽上升 ), 归属于重新厘定的蓟县运动的 

3 个期次。 

2008010444 

苏里格庙地区上古生界层序地层学研究 = 

Sequence stratigraphy of Upper Paleozoic in 

Suligemiao region. ( 中文 ). 魏红红 ; 李文厚 ; 屈 

红军 ; 邵磊 . 西北大学学报 ( 自然科学 

版 ), 2002, 32(1): 55-59 

为查明苏里格庙地区天然气储集层的展 

布规律 , 根据地质、地震、测井及地球化学 

资料 , 将该区上古生界地层划分为 6 个层序 

15 个体系域 : 

DS 1 ,DS 2 ,DS 3 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 ;DS 4 ,DS 5 ,DS 6 层序具有三元体系域结构 , 

包括低位体系域、湖进体系域和高位体系 

域。层序发育特征反映了研究区从晚石炭 

世 — 早二叠世中期的陆表海环境逐渐向早 

二叠世晚期 — 晚二叠世的河流 — 三角洲 — 

湖泊环境的演化过程。其中 : DS 1 ,DS 2 ,DS 3 

层序中高位体系域的炭质泥岩、页岩及煤 

114

层是良好的烃源岩 ;DS 4 ,DS 5 层序中低位体 

系域的三角洲和河道砂体是物性良好的储 

层 ;DS 5 和 DS 6 层序中高位体系域及湖进体系 

域的泥岩是有利的盖层 , 它们在垂向上构成 

了有利的生储盖组合。 

2008010445 

华南二叠纪末缺氧海水中的有毒气体与生 

物集群绝灭 = Massive dissociation of gas 

hydrate during oceanic anoxia as a cause of 

mass extinction at the end of Permian. ( 中文 ). 

李玉成 ; 周忠泽 . 地质地球化学 , 2002, 30(1): 

57-63 

对华南 P/T 界线地层有机碳同位素和碳酸 

盐岩碳氧同位素和沉积特征进行研究表 

明 : 二叠纪末海洋中发生了大规模海水缺 

氧事件 , 持续时间约 6~10 万年 ; 海洋底 

层存在大量的 CO、CO 2 、H 2 S 和 CH 4 等水溶 

性有毒气体 , 在剧烈的火山爆发事件及相 

伴的温室效应影响下 , 这些气水化合物由 

海底及陆架沉积中快速分离释放 , 导致生 

物集群绝灭 , 最终造成灰岩的 δ 13 C 值发生 

强烈的负漂移。 

2008010446 

南天山造山带中段古生界构造地层研究新 

进展 = New progress in the tectonostratigraphic 

study of the Paleozoic in the central 

sector of the South Tianshan orogenic belt. 

( 中文 ). 张传恒 ; 周洪瑞 ; 刘本培 ; 李红生 ; 王训 

练 . 地质论评 , 2002, 48(1): 9-14 

南天山古生代地层的三度空间位置因造 

山作用改造而发生结构性重组。以测制综 

合地质构造剖面为纽带 , 将变形构造解 

析、沉积序列分析和微体古生物研究有机 

结合研究阿拉塔格组、查汗沙拉含矿岩系 

的地层序列与时代归属 , 取得两个主要进 

展。1 阿拉塔格组为一套连续喾的单向型 

旋回 , 下部以火山岩为主 , 向上碳酸盐岩 - 

硅质岩比例逐渐增大 , 碎屑岩颗粒向上逐 

渐变粗 , 它的地质时代至少可从早泥盆世 

延续至晚泥盆世 ;2 查汗沙拉地区出露异 

地志留纪生物碎屑灰岩和原地志留纪 - 石碳 

纪地层 , 赋矿地层位于浊积岩系上部 , 时 

代为中、晚泥盆世。以此研究为基础 , 探 

讨、提出了重建造山带地层序列的基本原 

则和主要途径。 

2008010447 

内蒙古大青山地区寒武系与奥陶系之间的 

一个重要的层序界面 = Am important sequence 

interface between the Cambrian and 

the Ordovician in Daqingshan, Inner Mongolia. 

( 中文 ). 彭向东 ; 程立人 ; 徐仲元 ; 刘正宏 . 

地质论评 , 2002, 48(1): 54-57 

大青山地区寒武纪 - 奥陶纪地层分布零 

星 , 是由中生代逆冲推覆构造就位于此的 

一系列近东西向延展的构造岩片组成。下 

寒武统色麻沟组直接覆盖在太古界变质岩 

之上 , 缺失中元古界什那干群 , 寒武系与 

奥陶系之间呈假整合接触 , 标志着区内寒 

武纪与奥陶纪之间发生过一次抬升构造运 

动 , 其形成机制与古亚洲洋内的稳定陆快 

向华北板块拼贴事件有关 , 是早奥陶世末 

期华北板块整体抬升的序幕。这个层序界 

面的识别 , 对于恢复华北板块北部边缘构 

造演化历史具有重要意义。 

2008010448 

二叠系乐平统底界全球层型剖面和点位问 

题 = Definition and position of conodonts for 

the base of the Lopingian Series. ( 中文 ). 梅仕 

龙 . 地质论评 , 2002, 48(3): 225-233 

乐平统被正式接纳为上二叠统的国际标 

准年代地层单位后 , 其底界的全球层型剖 

面和点位 (GSSP) 亟待确定。经金玉玕等 

多年研究 , 广西来宾县蓬莱滩剖面被公认 

为乐平统底界层型的最佳候选剖面 ; 该剖 

面牙形类化石 Clarkina postbitteri 带或 

Clarkina dukouensis 带之底均可作为乐平统 

底界的候选层位。C . postbitteri 由 

Jinogondolella granti (Mei and Wardlaw) 演 

化而来 , 其首次出现的点位 (FAD) 可在 

蓬莱滩剖面得到精确确定。1998 年 , 以 

C.postbitteri 带之底作为乐平统底界的方 

案被国内外牙形类化石专家一致接受 , 为 

国际二叠纪地层分会通过投票正式决定蓬 

莱滩剖面 C.postbitteri 带之底为全球层型 

剖面和点位铺平了道路。令人遗憾的是在 

此关键时期王成源声称 , 在原定界线之下 3 

米处发现 C . postbitteri , 并转而提出以 

C.dukouensis 带之底为界线的另一方案 , 

导致一次无谓的争端 , 延误了在中国建立 

乐平统底界的全球层型的进程。后经 

Henderson 重新研究有关样品证明 , 在原定 

界线之下 3m 处并未发现 C.postbitteri, 从 

而使牙形类化石专家达成新的共识。乐平 

统牙形类化石的演化以 Clarkina 属为主导 , 

属内各种的鉴别应以居群 (Population) 为 

基础。锯齿型式被证明是最能反映该属居 

群特征的较为稳定的鉴定标定。而齿台轮 

廓等其它形态性状在一个居群内变化较 

大 , 如作为 Clarkina 各种的主要鉴定特征 , 

115

常常将同一居群内的不同形态类型鉴定为 

不同的种 , 以致在一个样品内鉴别出 

Clarkina 的 10 个多个种 , 同时也会将不同 

居群的异质同形的个体归属同一种。结果 

使属内各种的演化关系模糊 , 延展时限人 

为地拉长 , 失去应有的地层价值。依据这 

种分类确定的种和地层界线 , 在为数很少 

的牙形类化石专家中都很难达成共识 , 更 

难为广大地质工作者应用。 

2008010449 

乐平统底界定义和点位的争论 = Arguments 

about the definition and the point of basal 

boundary of the Lopingian. ( 中文 ). 王成源 . 

地质论评 , 2002, 48(3): 234-241 

有关乐平统底界定义和点位的争论涉及 

到有关建立界线层型的一些基本原则。本 

文作者确信 , 乐平统的底界不可能建立在 

小间断上或层序界面上 ; 不能被证实的点 

断成种事件也不能用来建立界线成型 ; 定 

义种在连继演化谱系中首现的点位是确定 

的不是任意的 ; 必须考虑定义种的首现时 

期的居群特征 , 不能用定义种晚期的居群 

特征来确定 GSSP 的点位 ; 定义种的定义不 

能任意改动 , 要保持分类的稳定。不能过 

高估计或只认为齿脊征是区别晚二叠世舟 

刺分子的唯一标准。梅仕龙有关 C. postbitteri 

和 C. ukouensis 两个种区别特征的争辩是 

无用的 , 因为本文作者所使用的区别这两 

个种的标准正是梅仕龙等 (Mei et al, 

1994) 所提出的。现在没有必要为维护自 

己的界线定义或点位而修改有关种的定 

义。原来有关这两个种的定义和区别特征 

是科学。本文作者鉴定的 C. durouensis 

(Wang, 2000a, pl. 2, figs. 1~8) 是正确的 , 

符合原来的定义。乐平统底界定义应当是 

严格的科学的。金玉玕等 (Jin et al, 1994, 

1998) 从来没有提到更谈不上 “ 反复讨论 ” 

了 C. doukouensis 的 “ 首现 ” ( 梅仕龙 , 本 

期 )。虽然提到 C.postbitteri 的首现 , 但由 

于 C. postbitteri 的先驱种不清 , 这个定义是 

不科学的。乐平统底界的科学而严格的定 

义应是 : 在 Clarkikina postbitteri-C. 

dukouensis 连续的演化谱系中 C. Dukouensis 

的首次出现 (FAD)(Wang, 2000a), 其 

具体层位在蓬莱滩剖面的 6k 之底。梅文否 

定他们曾将 Clarkina postbitteri 的首现层位 

划在 6j 之底 , 但他们的文章清楚的写着 

Clarkina postbitteri 的首现层位在 6j (Mei & 

Wardlaw, 1999, p.97)。梅文称在他们的文章 

中 (1994 a ) 反复引用了 Glenister 等 

(1991) 的观点 , 事实上 , 没有引用。我 

国学者应尊重事实 , 尊重科学 , 共同努 

力 , 把乐平统的底界层型建立在中国的蓬 

莱滩。 

2008010450 

对比日本秋吉生物礁论湖南石炭纪生物成 

礁条件 = On factors of Carboniferous reef 

developing in Hunan: A comparing study with 

akiyoshi reef in Japan. ( 中文 ). 柳祖汉 . 地质 

科学 , 2002, 37(1): 38-46 

一个完好的石炭纪生物礁发育在日本秋 

吉地区的玄武岩熔岩和火山碎屑岩之上。 

其礁核相可划分为 6 个亚相。主要的造礁 

生物是钙藻类、刺毛虫、珊瑚和苔藓虫。 

这些造礁生物在湖南中部某些地区的石炭 

纪地层中也十分常见 , 其生物组成、形态 

和生态特征可以和秋吉礁礁核各亚相中的 

生物特征进行对比。湖南中部地区石炭纪 

浅海的海底地形存在高低差异 , 在地势较 

高的中高能地带具备生物礁发育的各种条 

件 , 已发现一些生物层 , 完全有可能发现 

生物礁。 

2008010451 

英格兰达德利志留系 Much Wenlock Limestone 

组碳酸盐沉积环境、层序地层学和骨 

骼的特异保存 = Carbonate depositional environments, 

sequence stratigraphy and exceptional 

skeletal preservation in the Much 

Wenlock Limestone Formation (Silurian) of 

Dudley, England. ( 英文 ). Ray D C; Thomas A 

T. Palaeontology, 2007, 50(1): 197-222 

The Much Wenlock Limestone Formation 

of the Dudley inliers, West Midlands, contains 

one of the world's richest and most exquisitely 

preserved Silurian marine biotas. However, 

for most museum specimens, little is known of 

their exact provenance and mode of preservation. 

Detailed comparisons between outcrops 

and museum collections allow the identification 

of five faunal-lithological associations 

and numerous horizons of exceptional skeletal 

preservation. The associations are interpreted 

as a series of transient carbonate mid-platform 

environments extending from below storm 

wave-base to above fair-weather wave-base. 

Erosive surfaces, condensed sections, flooding 

surfaces and the stacking patterns of genetically 

related bed-sets (parasequences) have 

allowed the formation to be interpreted as a 

single third-order sequence stratigraphic cycle 

of sea-level change. The articulated preservation 

of taxa such as pelmatozoan echinoderms 

116

and trilobites can be attributed to either rapid 

burial by obrution deposits close to fairweather 

wave-base or smothering by storm 

sequestered muds in slightly deeper-water 

settings. Such intervals of exceptional preservation 

are commonly associated with flooding 

surfaces, presumably reflecting reduced likelihood 

of reworking once rapid burial had taken 

place. 

2008010452 

布尔吉斯页岩中的化石成岩作用 = Fossil 

diagenesis in the Burgess shale. ( 英文 ). 

Butterfield N J; Balthasar U; Wilson L A. Palaeontology, 

2007, 50(3): 537-543 

Current models for the exceptional preservation 

of Burgess Shale fossils have focused 

on either the HF-extractable carbonaceous 

compressions or the mineral films identified 

by elemental mapping. BSEM, EDX and microprobe 

analysis of two-dimensionally preserved 

Marpolia, Wiwaxia and Burgessia 

identifies the presence of both carbonaceous 

and aluminosilicate films for most features, 

irrespective of original lability. In the light of 

the deep burial and greenschist facies metamorphism 

documented for the Burgess Shale, 

the aluminosilicate films are identified as 

products of late-stage volatilization and coincident 

mineralization of pre-existing compression 

fossils, whereas the three-dimensionally 

preserved gut-caecal system of Burgessia is 

interpreted as an aluminosilicate replacement 

of a pre-existing carbonate phase. The case for 

late diagenetic emplacement of aluminosilicate 

minerals is supported by the extensive 

aluminosilicification of trilobite shell and 

(originally) calcareous veinlets in the Burgess 

Shale, as well as documentation of other secondarily 

aluminosilicified compression fossils. 

By distinguishing late diagenetic alteration 

from the early diagenetic processes responsible 

for exceptional preservation, it is possible 

to reconcile the range of preservational modes 

currently expressed in the Burgess Shale. 

2008010453 

二叠纪卡皮敦阶 Kamura 冷却事件 : 古生 

代 - 中生代过渡的开始 = The Capitanian 

(Permian) Kamura cooling event: The beginning 

of the Paleozoic–Mesozoic transition. ( 英 

文 ). Isozaki Y; Kawahata H; Minoshima K. 

palaeoworld, 2007, 16(1-3): 16-30 

The Capitanian (late Guadalupian) high 

positive plateau interval of carbonate carbon 

isotope ratio (δ 13 C carb ) was recognized lately 

in a mid-Panthalassan paleo-atoll limestone in 

Japan as the Kamura event. This unique episode 

in the late-middle Permian indicates high 

productivity in the low-latitude superocean 

likely coupled with resultant global cooling. 

This event ended shortly before the Guadalupian–Lopingian 

(middle-late Permian) boundary 

(ca. 260 Ma); however, its onset time has 

not been ascertained previously. Through a 

further analysis of the Wordian (middle Guadalupian) 

to lower Capitanian interval in the 

same limestone at Kamura in Kyushu, we 

have found that the δ 13 C carb values started to 

rise over +4.5‰ and reached the maximum of 

+7.0‰ within the Yabeina (fusuline) Zone of 

the early-middle Capitanian. Thus the total 

duration of the Kamura event is estimated 

over 3–4 million years, given the whole Capitanian 

ranging for 5.4 million years. This 3– 

4 million years long unique cooling event occurred 

clearly after the Gondwana glaciation 

period (late Carboniferous to early Permian) 

in the middle of the long-term warming trend 

toward the Mesozoic. This cooling may have 

been a direct cause of the end-Guadalupian 

extinction of low-latitude, warm-water 

adapted fauna including the large fusulines 

(Verbeekinidae), gigantic bivalves (Alatoconchidae), 

and rugose corals (Waagenophyllidae). 

The Kamura event marks the first sharp 

excursion of δ 13 C carb values in the volatile 

fluctuation interval that lasted for nearly 

20 million years from the late-Middle Permian 

until the early-Middle Triassic. This interval 

with high volatility in δ 13 C carb values represents 

the transition of major climate mode 

from the late Paleozoic icehouse to the Mesozoic–Cenozoic 

greenhouse regime. The end- 

Paleozoic double-phased extinction occurred 

within this interval and the Capitanian Kamura 

event is regarded as the prelude to this 

transition. 

2008010454 

加拿大西部和平河盆地 Panthalassic 洋跨 

越二叠纪末集群绝灭的透光带闭塞环境的 

证据 = Evidence for photic zone euxinia 

through the end-Permian mass extinction in 

the Panthalassic Ocean (Peace River Basin, 

Western Canada). ( 英文 ). Hays L E; Beatty T; 

Henderson C M; Love G D; Summons R E. 

palaeoworld, 2007, 16(1-3): 39-50 

A combination of sequence stratigraphic 

and conodont biostratigraphic analyses of 

sediment cores from five petroleum exploration 

wells, together with reference to nearby 

outcrops, has allowed us to construct a composite 

geological section through the Per- 

117

mian–Triassic transition in the Peace River 

Basin of Western Canada. The cores contain 

significant contents of organic matter comprising 

kerogen and bitumen of low to moderate 

thermal maturity. Extraction and analysis of 

the bitumens has revealed patterns of biomarker 

hydrocarbons consistent with marine 

deposition and photic zone euxinia. In particular 

isorenieratane and aryl isoprenoids, derived 

from the carotenoid pigments of green 

sulfur bacteria (Chlorobiaceae), are abundant 

and pervasive throughout the section and indicate 

that hydrogen sulfide must have been 

present in the photic zone for significant periods 

of time. These findings mirror the geochemical 

results obtained for other Permian– 

Triassic boundary sections of the Tethys realm 

(e.g. Western Australia, East Greenland and 

South China) and suggest that euxinic conditions 

prevailed widely, though perhaps periodically, 

and that hydrogen sulfide toxicity 

could have been an important factor in the 

extinction of marine invertebrates. 

2008010455 

越南北部 Nhi Tao 剖面和 Lung Cam 剖面 

二叠纪 - 三叠纪界线剖面 : 碳同位素漂移 

和分子变化指示主要缺氧事件 = The Permian-Triassic 

boundary sections in northern 

Vietnam (Nhi Tao and Lung Cam sections): 

Carbon-isotope excursion and elemental variations 

indicate major anoxic event. ( 英文 ). Son 

T H; Koeberl C; Ngoc N L; Huyen D T. palaeoworld, 

2007, 16(1-3): 51-66 

Two Permian-Triassic boundary sections 

(Lung Cam and Nhi Tao) in shallow marine 

carbonates from northern Vietnam, near the 

border between Vietnam and China, were 

studied for major and trace elemental variations 

as well as carbon and oxygen isotopic 

compositions. At the Nhi Tao section, we observe 

a continuous transition from Late Permian 

limestones, siliceous limestones and microbial 

limestones (Dong Dang Formation) to 

Early Triassic limestones and dolomitic limestones 

(Hong Ngai Formation). At the Lung 

Cam section, a thin layer of shale (the uppermost 

part of the Dong Dang Formation-Late 

Permian) separates carbonate layers of the 

Dong Dang Formation (Late Permian) from 

those of the Hong Ngai Formation (Early Triassic). 

There is a clear negative shift of about 

2.5–3‰ in the δ 13 C values at both sections, 

beginning about 10 cm below the Permian- 

Triassic boundary as defined by paleontological 

and lithological data. The existence and 

extent of these excursions is compatible with 

introduction of 12 C-rich deep ocean water onto 

the shallow carbonate platform. In the Nhi 

Tao section, this negative shift in δ 13 C starts at 

about the same level as a change in magnetic 

susceptibility, indicating some input from terrestrial 

sources. The δ 13 C curves shows evidence 

for a rapid reduction in biomass, which 

may be related to the extinction event, and the 

long-term reduction in δ 13 C in the Early Triassic 

suggests long-term perturbation of the environment 

and slow recovery. The shift towards 

negative values indicates a reduction in 

carbon burial. The shape of the Ce/Ce* curve 

suggests that the redox conditions of depositional 

environments in both sections fluctuated, 

but that there was a decline in oxygenation 

with time, possibly into the anoxic range. Distinct 

negative anomalies coincide with the 

onset of the carbon isotope shifts, which might 

indicate additional influx of anoxic waters. 

The Th/U ratios in both sections are mainly 

less than 2, reinforcing this possibility. Upwelling 

of anoxic deep-ocean water onto the 

shallow carbonate platform at Nhi Tao and 

Lung Cam at the end of the Permian, with related 

disastrous consequences for the biosphere, 

is indicated by our data. 

2008010456 

南非南部 Karoo 盆地南部大陆区域中二叠 

纪 - 三叠纪界线地球化学和矿物学研究 = 

Geochemical and mineralogical investigation 

of the Permian–Triassic boundary in the continental 

realm of the southern Karoo Basin, 

South Africa. ( 英文 ). Coney L; Reimold W U; 

Hancox P J; Mader D. palaeoworld, 2007, 

16(1-3): 67-104 

Mineralogical and geochemical studies of 

the non-marine Permian–Triassic (P–Tr) 

boundary across two stratigraphically wellconstrained 

sections (Commando Drift Dam 

and Wapadsberg, Eastern Cape Province) in 

the southern Karoo Basin, South Africa, have 

been undertaken to provide further input on 

the cause of this mass extinction event, and so 

has a sedimentological and geochemical 

evaluation of a third P–Tr boundary section at 

Injusiti (Kwazulu-Natal) in the eastern Karoo 

Basin, South Africa. The Commando Drift 

Dam section has been constrained by previous 

palaeontological and palaeomagnetic work, 

with a palaeomagnetic reversal positioned 

5.3 m above the palaeontological P–Tr boundary. 

The Wapadsberg section has been constrained 

palaeontologically. All these P–Tr 

sections studied here mostly comprise mudstones, 

together with siltstones, sandstones, 

118

and in the southern Karoo Basin, carbonate 

nodular horizons. A change in colour of the 

mudstones from green-grey to red-brown 

takes place at the palaeontologically defined 

boundary. Variations in the major and trace 

element abundance profiles are usually limited 

to the carbonate nodular horizons, besides the 

overall effects of weathering. Bulk carbon 

isotopic studies of the Commando Drift Dam 

section revealed a negative δ 13 C bulk excursion 

(background values of −15 to −20‰, with 

total extent of excursion to −24.9‰) 2 cm 

below the palaeontological boundary, followed 

by a gradual recovery and then another 

decrease in values leading towards the palaeomagnetic 

boundary. Above this boundary 

recovery to less negative δ 13 C bulk values (ca. 

−18‰) occurs. The organic carbon record 

from the Commando Drift Dam (southern Karoo 

Basin) and Injusiti (eastern Karoo Basin) 

oscillates between −26.1 and −28.9‰, which 

is comparable to previous studies of different 

sections in the southern Karoo Basin. The 

magnitude of both the bulk and organic carbon 

isotopic variation can be interpreted to indicate 

a number of inputs (due to the fluctuating 

values) of organic carbon. The carbon isotope 

data for carbonates in the Injusiti section are 

different from the results on carbonates from 

other studies, but more work to expand this 

dataset is necessary. The palynological studies 

on the Commando Drift Dam section reveal 

the presence of a low diversity flora composed 

principally of bryophytes, lycophytes, and 

gymnosperms. These forms, including several 

Late Permian key-species, are traces of the 

surviving plants enduring after the major extinction-pulse. 

The presence of fungal palynomorphs 

and dearth of pollen/spores related 

to photosynthetic plants some metres above 

the palaeontological P–Tr boundary demonstrate 

similarities to the pattern of floral extinction 

at the Cretaceous–Palaeogene (K–Pg) 

boundary. The timing of vertebrate extinctions 

in the Karoo Basin has so far not been determined, 

but the 252.5 Ma age for a single zircon 

crystal from Commando Drift Dam dated 

here gives a maximum constraint on the age of 

the event bed, which is in agreement with the 

accepted age of the boundary. No evidence for 

impact-produced microdeformation features 

were found in quartz grains from either the 

Wapadsberg or Commando Drift Dam sections. 

Also, siderophile element data (including 

platinum group element (PGE) concentrations) 

do not support the possible presence of 

a meteoritic component at the boundary. Thus, 

a link between impact and P–Tr extinction is 

not indicated by the results of this study. 

2008010457 

华南广西来宾 - 合山二叠系生物地层和岩相 

= Biostratigraphy and lithofacies of the Permian 

System in the Laibin–Heshan area of 

Guangxi, South China. ( 英文 ). Shen 

Shuzhong; Wang Yue; Henderson C M; Cao 

Changqun; Wang Wei. palaeoworld, 2007, 

16(1-3): 120-138 

The Laibin–Heshan area is probably a 

unique area containing a suitable marine reference 

for the entire Permian system. Various 

fossils, sedimentary characteristics, lithofacies 

and palaeoenvironments including near shore, 

distal shelf, slope, and basin are developed. 

The Permian system in the Laibin–Heshan 

area is composed of the Maping, the Chihsia, 

the Maokou, the Heshan/Wuchiaping and the 

Talung formations in ascending order. The 

Maping Formation is characterized by restricted 

shoal or intertidal facies and ranges 

from the Late Carboniferous Kasimovian to 

Early Permian Artinskian. The Chihsia Formation 

(Artinskian–Kungurian) and the Maokou 

Formation (Roadian–Capitanian) represent 

a slope carbonate environment and a 

transgressive interval. By the end of the Guadalupian, 

the Permian sea was reduced to the 

confines of the Laibin area in South China and 

nearshore massive crinoid limestone was deposited, 

representing the most continuous marine 

deposits across the Guadalupian– 

Lopingian boundary. The Lopingian sequence 

in the Laibin–Heshan area reflects an independent 

transgression–regression system. During 

the Wuchiapingian basinal or slope phase, 

siliceous siltstone and chert and carbonates 

were deposited. During the Changhsingian, 

the Laibin–Heshan area subsided rapidly, accumulating 

about 600 m of limestone, tuffaceous 

sandstone, shale, siltstone before the 

basin was drained and terrestrial clastics with 

coal-seams developed. The end of the 

Changhsingian reflected the initial stage of the 

rapid transgression of the Triassic forthcoming 

supercycle. Limestone with latest Permian 

benthic faunas developed during the last stage 

of the Permian, which were immediately replaced 

by the nektic ammonoid and bivalvedominated 

faunas in the earliest Triassic. 

2008010458 

意大利南阿尔卑斯二叠纪地层和大地构造 

评述 = A stratigraphic and tectonic review of 

the Italian Southern Alpine Permian. ( 英文 ). 

119

Cassinis G; Perotti C R. palaeoworld, 2007, 

16(1-3): 140-172 

However, in the Carnic Alps, marine 

deposition began earlier, from Carboniferous 

times. In this context, two major and welldifferentiated 

tectono-stratigraphic units 

(TSUs) or cycles, separated by a marked regional 

unconformity and a gap of as-yet uncertain 

duration, are clearly evident. This paper 

aims at reviewing the current stratigraphic 

framework and correlating it to the most recent 

timescales. This research indicates that 

initial deposition of the Verrucano 

Lombardo/Val Gardena Sandstone red beds 

probably occurred in many places, such as in 

the Carnic Alps, during Middle Permian times. 

Consequently, this interpretation supports a 

reduction, at least locally, of the large timegap 

suggested between the two abovementioned 

cycles. Their respective evolution 

led to paleogeographic changes related to different 

structural and geodynamic settings. The 

Lower Permian stratigraphic sequence was 

mainly deposited in transtensional pull-apart 

and strike-slip intracontinental basins during 

the onset of regional uplift, with unroofing, 

collapse and stretching of the Variscan orogen, 

upwelling of the asthenosphere and intrusion 

of granitic melts into the crust. This episode 

could be interpreted as the final act of the 

“Hercynian (Variscan) Cycle”. It was followed 

by a tectonic event (the so-called “Mid- 

Permian Episode” in the literature) as a prelude 

to general plate reorganization and the 

opening of new oceans (such as Meliata- 

Maliak and Neotethys). In contrast, the Middle 

pro parte—Upper Permian stratigraphic 

sequence marks the development of more 

generalized extensional tectonics, compatible 

with a rifting regime. According to many authors, 

it is regarded as the beginning of the 

“Alpine Cycle”. 

2008010459 

俄罗斯远东地区南滨海中二叠世 ( 瓜德鲁 

普世 ) 生物地层及与中国东北部对比 = 

Middle Permian (Guadalupian) biostratigraphy 

in South Primorye, Russian Far East and 

correlation with Northeast China. ( 英文 ). Kotlyar 

G V; Shen Shu-Zhong ; Kossovaya O L; 

Zhuravlevc A V. palaeoworld, 2007, 16(1-3): 

173-189 

The Middle Permian (Guadalupian) strata in 

South Primorye, Russian Far East and Northeast 

China are well developed and characterized 

by the fusulinid Monodiexodina fauna, 

transitional brachiopod, coral and bryozoan 

faunas, but little has been done for the correlation 

between the areas in the two countries. 

This paper provides a review of the faunas in 

and around the Monodiexodina-bearing beds 

in all the key sections in the South Primorye 

area and a correlation with their equivalents in 

Northeast China. The Monodiexodina-bearing 

beds are of Wordian (Early Midian) age based 

on the associated conodont Jinogondolella cf. 

aserrata and the brachiopod Substriatifera 

vladivostokensis zones. These beds are commonly 

overlain by the Early Capitanian (Middle 

Midian) fusulinid Parafusulina stricta 

Zone, brachiopod Leptodus nobilis- 

Spiriferella Zone and coral Paracaninia 

columbina-Lophocarinophyllum chandalasicum 

Zone. The Monodiexodina-bearing beds 

are also found from the Hugete and Jisu 

Honguer formations in the Zhesi area, the Sijiashan 

Formation in the southern Daxinganling 

Range and the Daheshen Formation in 

Jilin Province in Northeast China. These 

Monodiexodina-bearing beds mostly occur in 

calcarenite and sandy limestone and are 

largely the same age in the northern temperate 

transitional zone. 

2008010460 

桂西晚古生代深水相地层 = Late Paleozoic 

strata of deep-water facies in western Guangxi. 

( 中文 ). 邝国敦 ; 吴浩若 . 地质科学 , 2002, 

37(2): 152-164 

详细描述了分别位于桂西的北、中、南 

部的几个晚古生代地层剖面 , 据此建立桂西 

晚古生代深水沉积的地层序列 , 其岩石地层 

单位自下而上可归入广西原有的平恩组、 

罗富组、榴江组、五指山组、鹿寨组、巴 

平组、南丹组、四大寨组和领薅组。和这 

些单位的命名剖面比较 , 桂西腹地的同期地 

层具有更典型的深水相沉积 , 并含大量玄武 

岩 , 构成从早泥盆世晚期到晚二叠世末的连 

续深水沉积。桂西晚古生代为广海远洋环 

境 , 其中孤立碳酸盐台地上泥盆 - 石炭系灰 

岩中出现的二叠纪 “ 化石脉 ”, 是古特提斯张 

裂作用的结果。 

2008010461 

北祁连造山带中 — 西段陆壳残块群的构 

造 — 地层特征 = Tectono-stratigraphic characteristics 

of continent crustal remnants in 

central-western sector of the North Qilian 

Orogen. ( 中文 ). 左国朝 ; 刘义科 ; 张崇 . 地质科 

学 , 2002, 37(3): 302-312 

北祁连造山带是一条多旋回的造山带 , 其 

最大特点是早古生代岩系中镶嵌有众多大 

120

小不一的由前震旦系变质岩系所组成的陆 

壳残块群 , 它们源于晋宁期末 , 统一的巨型华 

北古大陆早古生代初的裂解。寒武 - 奥陶纪 

西段演化为裂谷系 , 陆壳残块群组成裂谷系 

的正性隆起构造单元 ; 中段发育微洋盆沟弧 

盆体系 , 在南缘的陆壳残块群处于奥陶纪活 

动大陆边缘张裂带上 , 并构成被晚期弧后盆 

地及裂谷分开后的陆壳基底部位 , 少数陆壳 

残块为沟弧盆体系中的孤岛隆起。它们不 

是由中祁连推覆来的飞来峰或是外来移置 

的滑覆体 , 而是由统一的巨型华北古大陆西 

南缘古阿拉善地块于早古生代初裂解后向 

洋或裂谷演化过程中残留其中的大小不一 

的陆壳残块。北祁连早奥陶世海域与现在 

加拿大北部巴芬湾及伊丽莎白女王群岛的 

构造格局相似。 

2008010462 

海南岛泥盆 — 石炭系界线研究 = Study on 

Devonian-Carboniferous boundary in Hainan 

Island,South China. ( 中文 ). 胡宁 ; 张仁杰 ; 冯 

少南 . 地质科学 , 2002, 37(3): 313-319 

通过对新建立的海南岛上泥盆统昌江组 

及其下石炭统南好组多重地层的综合研究 , 

并以首次发现的南好组底部的河流相砾岩 

和砂砾岩为标志 , 指出海南岛在泥盆纪末期 

曾发生大规模海退事件 , 这恰好与泥盆纪 — 

石炭纪之交的全球海平面下降事件完全一 

致。不仅确认了昌江组与南好组为平行不 

整合接触关系 , 而且两者以 I 型层序界面相 

隔分别构成 2 个三级层序 , 因而认为海南岛 

泥盆 — 石炭纪年代地层界线已与层序界面 

重合为一个共同的分界面 — 平行不整合 

面。 

2008010463 

俄罗斯伏尔加 - 乌拉尔 Kazanian 与全球二 

叠纪年代表罗德阶的对比 = Correlation of 

the Kazanian of the Volga–Urals with the 

Roadian of the global Permian scale. ( 英文 ). 

Leonova T B. palaeoworld, 2007, 16(1-3): 

246-253 

Recent discovery of an ammonoid assemblage 

in the Kazanian of the Volga–Urals Region 

enabled the correlation of the Kazanian 

with the Roadian of the global Permian scale. 

The composition of the ammonoid assemblage 

is similar to other assemblages from Arctic 

Canada, Novaya Zemlya, and the Verkhoyansk 

Region. The taxonomic diversity of 

Roadian ammonoids in the Boreal region is 

discussed, and existing data on their stratigraphic 

and geographic distributions are analyzed. 

2008010464 

西藏中部拉萨地块古生代、中生代的超层 

序研究 = Recognition and correlation of supersequences 

in Lhasa Block,southern Tibet. 

( 中文 ). 李祥辉 ; 王成善 ; 吴瑞忠 . 沉积学 

报 , 2002, 20(2): 179-187 

识别划分了西藏南部拉萨地块 ( 措勤盆 

地 ) 古生代、中生代以海相为主的沉积地 

层相当于二级旋回的超层序 11 个 (CQ 1 ~ 

11), 其中早古生代 3 个 (CQ 1 ~3 ) 古生代 4 个 

(CQ 4 ~7) 中生代 4 个 (CQ 8 ~11); 描述了各个 

超层序的特征 ; 不仅在地块内进行了超层 

序对比 , 而且与印度北部边缘 ( 特提斯喜 

马拉雅 ) 显生宙的超层序进行了比较和讨 

论。研究表明 , 除早古生代外 , 藏南特提 

斯喜马拉雅和萨地块 ( 措勤盆地 ) 的超层 

序在数量、延时、结构方面极不相同 , 与 

所处地块构造背景和沉积盆地性质发生了 

变化有关。提出早古生代拉萨地块与印度 

次大陆同属冈瓦纳相区 ( 克拉通上的陆表 

海 ), 晚古生代早期以后它们已不属同一 

大陆 , 整个晚古生代拉萨地块可能为冈瓦 

纳与劳亚大陆之间过渡带的一部分 , 中生 

代则成为 Cimmeria 次大陆的南部块体 , 冈 

瓦纳大陆在西藏境内的北界应为雅鲁藏布 

江缝合带。 

2008010465 

四川盆地早古生代灰泥丘中的微生物及其 

造岩和成丘作用 = Microbial fossils and their 

biosedimentation & buildup in Paleozoic mud 

mounds, Sichuan Basin. ( 中文 ). 张廷山 ; 沈昭 

国 ; 兰光志 ; 王顺玉 ; 戴鸿鸣 . 沉积学报 , 2002, 

20(2): 243-248 1 图版 . 

作为生物礁的特殊类型 , 灰泥丘在古生 

代十分发育 , 许多学者都认为它们是通过 

微生物造岩作用而形成的 , 而且 , 也在现 

代湖泊中发现了由兰菌藻的生命活动所形 

成的灰泥沉积物及灰泥丘。但是国际上一 

直没有在古生代灰泥丘中发现过细菌等微 

生物的实体化石 , 微生物促使碳酸钙沉 

淀、聚集的能力和机理也不明确。四川盆 

地北缘寒武纪和志留纪灰泥丘发育 , 笔者 

通过扫描电镜及能谱分析 , 在国际上首次 

发现了 ( 川西北志留纪 ) 灰泥丘中菌藻类 

微生物的实体化石及其特征的造岩成丘现 

象 , 发现的菌藻类微生物实体化石有三种 

类型 :1. 表面光滑的卵形球体型 ;2. 表面 

粗糙的球体型 ;3. 网状结构型。而且 , 对 

121

寒武纪和志留纪灰泥丘凝块石作生物标志 

化合物分析也证明了其有机质生源为菌藻 

类微生物。这些凝块石灰泥丘中的菌藻类 

实体化石都显示了不同的沉积、造岩和成 

丘功能 , 因而证实了微生物在形成古生代 

灰泥丘中具重要作用。 

2008010466 

四川盆地东部晚二叠世 - 早三叠世飞仙关 

期礁、滩特征与海平面变化 = The characteristics 

of reef and bank and the fluctuation of 

sea-level in Feixianguan period of Late Permian-Early 

Triassic, East Sichuan Basin. ( 中 

文 ). 王兴志 ; 张帆 ; 马青 ; 杨满平 ; 王一刚 ; 文应 

初 ; 杨雨 ; 张静 . 沉积学报 , 2002, 20(2): 249- 

254 

据四川盆地东部上二叠统一下三叠统飞 

仙关组沉积特征和储层分布规律 , 认为区 

内长兴组生物礁和飞仙关组鲕粒滩特征和 

分布与海平面升降有关。长兴期生物礁发 

育于海平面快速上升阶段的缓坡坡折地带 

和缓坡内的局部 , 当生物礁的生长速度低 

于海平面的上升速度时 , 形成海侵追补型 

生物礁 , 当生物礁生长速度大于海平面上 

升速度时 , 则构成海侵并进型生物礁 ; 飞 

仙关鲕粒滩形成于海平面下降阶段的台地 

边缘和台内局部地区 , 单一台地边缘鲕粒 

滩分布广、厚度大 , 而台内鲕粒滩数量虽 

多 , 但单一厚度小 , 分布范围窄。总体来 

看 , 长兴生物礁发育层位逐渐向海侵方向 

升高 , 而飞仙关鲕粒滩随海退的进行 , 向 

台地增生方向迁移。区内上二叠统 - 下三叠 

统飞仙关组是一次较大规模海平面升降过 

程中的产物 , 海侵始于吴家坪初期 , 长兴 

期海平面快速上升 , 至飞仙关初期达到最 

高海平面 , 海平面开始下降 , 直至飞仙关 

末期。 

2008010467 

晚奥陶世五峰期扬子海盆海平面变化旋回 

与古水体深度 = The eustatic cycles and the 

depth of water mass of the latest Ordovician 

Wufengian in the Yangtse Basin. ( 中文 ). 何卫 

红 ; 汪啸风 ; 卜建军 . 沉积学报 , 2002, 20(3): 

367-373 2 图版 . 

通过晚奥陶世五峰期扬子海盆的古地理 

格局、岩性及生物发行的纵向变化、Ce 异 

常变化的旋回性和生物群对海水深度的指 

示作用的讨论 , 认为扬子海盆晚奥陶世五 

峰期经历了 5 个旋回的海平面变化 , 海水 

最浅为 50~80 m( 观音桥层 ), 海水最深 

约 500 m 左右。 

2008010468 

苏皖地区石炭系露头层序地层研究 = Study 

on outcrop sequence stratigraphy of the Carboniferous 

strata in Anhui and Jiangsu Province, 

China. ( 中文 ). 林春明 ; 张顺 ; 王淑君 ; 刘 

家润 ; 凌洪飞 . 沉积学报 , 2002, 20(4): 537- 

544 

应用露头层序地层学基本原理和方法 , 

在详细的岩石岩相学、沉积学。地球化学 

研究和精细的地层划分对比基础上 , 对苏 

皖地区石炭系地层进行了露头层序地层研 

究。阐述了沉积层序的各种界面的露头标 

志 , 探讨了三级层序和层序区域对比的基 

本特征。研究表明 , 苏皖地区石炭系可识 

别出 9 种主要岩相、20 种微相和 11 个三级 

沉积层序。I 型沉积层序边界识别标志有地 

表或海底侵蚀、地层上超 , 界面上下岩性 

岩相、古生物及氧碳同位素值的突变 , 界 

面的区域可对比性等 , 在研究区主要表现 

为古风化壳面、古岩溶面、侵蚀面和暴露 

面四种类型。陆表海盆海水较浅 , 沉积物 

常露出水面而遭受侵假冒 , 形成较多的 I 

型层序边界。三级层序发育 TST,LST 不 

发育或难以识别。 

2008010469 

皖南地区奥陶系层序地层学分析 = Analysis 

of the Ordovician sequence stratigraphy in 

southern Anhui. ( 中文 ). 吴跃东 ; 钟华明 . 现代 

地质 , 2002, 16(1): 45-52 

皖南东至地区奥陶系在地层分区上可以 

分为下扬子地层分区、过渡地层分区和江 

南地层分区 , 在沉积相上可分为台地、斜 

坡与盆地沉积。通过对位地台地、斜坡和 

盆地露头层序地层的研究 , 分别将奥陶纪 

地层自下而上划分为 3 个 I 类沉积层序和 2 

个 Ⅱ 类沉积层序 , 并详细分析了每个沉积 

层序各体系域的特征。区内的奥陶系总体 

为一向上变深的沉积层序 , 经历了镶边陆 

棚 - 淹没台地 - 浅海盆地 3 个演化阶段 , 

其盆地呈北西浅、南东深的沉积构造格 

局。 

2008010470 

藏南康马地区石炭系 - 二叠系研究新进展 = 

New advances in research of Permian- 

Carboniferous in the Kangmar region, southern 

Tibet. ( 中文 ). 陈俊兵 ; 徐兴永 ; 李文庆 ; 贡 

布 . 现代地质 , 2002, 16(3): 237-242 

122

根据西藏江孜幅和亚东幅 1:25 万区域 

地质调查工作的成果 , 阐述了西藏康马地 

区石炭系 - 二叠系统的划分方案 ; 并根据新 

采集的腕足采、单体珊瑚和菊石等化石组 

合 , 讨论了各组的地层时代 , 认为本区二 

叠纪沉积作用可延续到晚二叠世早期 ( 吴 

家坪期 ), 在原二叠系白定浦组之上建立 

了一个新组 - 江浦组 (P 3 j)。结合邻区的地 

层对比 , 分辨出 2 个伸展不整合 ;2 个 Ⅰ 类 

不整合和 3 个 Ⅱ 类不整合。最后初步分析 

了康马地区杂砾岩的成因 , 认为其与冰期 

一间冰期冻融环境下的滨岸附近古水道重 

力流有关。 

2008010471 

滇黔桂盆地及其邻区晚古生代层序地层格 

架及相对海平面变化 = Sequencestratigraphic 

framework and relative sealevel 

changes of Late Paleozoic in the Dianqiangui 

Basin and its adjacent areas. ( 中文 ). 梅冥相 ; 

马永生 ; 高金汉 ; 孟庆芬 ; 易定红 ; 李东海 . 现代 

地质 , 2002, 16(4): 365-373 

受同生断裂的控制 , 在晚古生代滇黔桂 

盆地及邻区形成特殊的 “ 台 - 盆 - 丘 - 槽 ” 的古 

地理格局 , 发育了复杂而有序的盆地充填 

序列。根据三级沉积层序的两大特性 , 在 

滇黔桂盆地及邻区的晚古生代地层中识别 

的 25 个三级沉积层序 ; 以地层记录中的两 

种相变面和两种穿时性界面为关键。建立 

了晚古生代的区域层序地层格架。研究表 

明 , 地层记录中的层序界面大致可以划分 

为 4 种类型。即构造不整合面 , 沉积不整 

合面 , 淹没不整合面以及它们的相关面 , 

而且它们还可以进一步归为暴露间断面以 

及加深间断面两种范畴的界面。 

2008010472 

南祁连那尔宗及邻区中二叠世一早、中三 

叠世层序地层特征 = Characteristics of sequence-stratigraphy 

of Middle Permian to 

Early-Middle Triassic Epoch in Naerzong and 

its adjacent area, South Qilian. ( 中文 ). 邓中林 ; 

王青海 ; 朱跃生 ; 安守文 ; 贾春兴 . 青海地 

质 , 2001, 11(1): 11-15 

在稳定的南祁连地区 , 对中二叠世 - 

早、中三叠世地层进行露头层序地层研 

究 , 建立了 2 个三级层序 (OS 1 、OS 2 ), 

分别由不同的副层序组合而成 , 每个层序 

又发育 TST、HST 以及 SS, 但缺乏 SMST。 

层序的发育与全球海平面的变化有密切关 

系 , 构造运动的持续作用 , 使南祁连地区 

海平面变化频繁 , 对该地区层序地层的组 

成具有直接影响。 

2008010473 

川东长兴组生物礁的高分辨率层序地层研 

究 = Research of the high-resolution sequence 

stratigraphy reef association in Changxing 

Formation of Permian, East Sichuan. ( 中文 ). 

谢继容 . 矿物岩石 , 2002, 22(1): 49-54 

高分辨率层序地层是近年来层序地层的 

新发展 , 它极大地提高了层序地层分析的分 

辨率和储层预测的准确性 , 对油气勘探具有 

重要意义。文章简要介绍了高分辨率层序 

地层在川东长兴组生物礁组合中的尝试研 

究 , 包括利用岩芯资料划分基准面短期旋回 ; 

利用岩芯标定 , 建立岩芯基准面的测井响应 

关系 ; 并建立了短期、中期、长期三级次的 

基准面旋回。在此基础上 , 运用基准面旋回 

的原理对川东开江地区长兴组生物礁组合 

进行了高分辨率层序地层对比分析 , 并建立 

了高分辨率等时地层格架。 

2008010474 

鄂尔多斯盆地上古生界高分辨率层序地层 

分析 = Analysis of high-resolution sequence 

stratigraphy for Upper Paleozoic in Ordos Basin. 

( 中文 ). 郑荣才 ; 文华国 ; 梁西文 . 矿物岩 

石 , 2002, 22(4): 66-74 

按基准面旋回原理 ,, 将鄂尔多斯盆地上 

古生界本溪组 (C 2 b)、太原组 (P 1 t)、山西 

组 (P 1 s) 和下石盒子组 (P 1 xs) 划分为 3 个超 

长期、8 个长期、19 个中期和 62 个短期旋 

回层序 ; 较为详细地介绍了各级别层序的结 

构类型、叠加样式和沉积演化序列 ; 建立以 

长期旋回层序为年代地层框架 , 中期旋回层 

序为等时地层对比单元的层序地层格架 ; 并 

讨论高分辨率层序地层与天然气藏的关 

系。 

2008010475 

安徽巢湖凤凰山剖面石炭系微相和层序地 

层特征 = Carboniferous microfacies and sequence 

stratigraphy of Fenghuangshan profile 

in Chaohu of Anhui Province, China. ( 中文 ). 

林春明 ; 黄志诚 ; 刘家润 ; 凌洪飞 ; 张顺 ; 赵彦彦 . 

岩石学报 , 2002, 18(3): 424-432 1 图版 . 

应用露头层序地层学基本原理和方法 , 

对巢湖凤凰山石炭系剖面进行重新研究。 

巢湖凤凰山石炭系总厚度为 79.02m, 在 

这个剖面中可以识别出 6 种主要岩相、18 

种微相和 11 个三级沉积层序 , 其中六个三 

级沉积层序属于 I 型沉积沉序 , 三个属于 

123

Ⅱ 型沉积层序 , 缺失第 9 和第 10 沉积层 

序。三级沉积层序在不同的古地理单元和 

不同的沉积环境中可以进行对比。根据各 

微相特征和成因 , 揭示了沉积间断面上存 

在的多期古岩溶现象。阐述了三级层序及 

其对应的三级海平面升降旋回的特征。 

2008010476 

三级层序界面野外露头的识别判断标志 - 以 

南盘江坳陷晚古生界地层为例 = Identificaton 

marks on the field outcrop of threegrade 

sequence interface. ( 中文 ). 张国常 . 贵 

州地质 , 2002, 19(2): 93-98 

在岩性及岩相观察基础上以不同类型的 

米级旋回层序作为分层和描述地层的基本 

工作单元 , 把米级旋回层序及有序叠加形 

式作为识别三级层序的基础 , 通过野外露 

头的详细观察、描述认为 : 在南盘江坳陷 

晚古生界地层中 SB 1 型层序界面是以区域平 

行不整合面、古风化壳、古土壤层、下伏 

地层的强烈白云石化以及沉积物转化面为 

识别标志 ;SB 2 型层序界面是以沉积物转化 

面、地层结构转化面及古土壤层为识别标 

志 :SB 3 型层序界面是以凝缩段直接覆盖在 

下伏地层之上为识别标志 ;SB 型层序界面 

是以上下地层的岩性组合、地层结构转化 

面及年代地层为识别标志。 

2008010477 

贵州丹寨 — 三都中上寒武统露头层序地层 

学研究 = Study on the sequence stratigraphy 

of the outcrop of the Cambrian in Danzhai- 

Sandu, Guizhou. ( 中文 ). 王贤 ; 张秀莲 . 贵州 

地质 , 2002, 19(4): 242-248 

作者对贵州丹寨一三都中上寒武统两个 

碳酸盐岩露头剖面进行了层序地层学研 

究 , 识别出 5 个 ( 三级 ) 层序。其中 , 寒 

武系顶界和都柳江组中部有 I 型层序边 

界 , 其余为 II 型层序边界。论述了该区构 

造演化史 , 指出由于构造升降运动 , 两露 

头剖面的沉积环境发生变化。受海洋物理 

化学条件的控制 , 碳酸盐岩生产率以及生 

物种群显著变化 , 在一定程度上影响了碳 

酸盐岩台地的堆积。诸多因素都对碳酸盐 

岩地层层序或沉积相在横向上和纵向上的 

展布和排列形式有重要的控制作用。在寒 

武纪时 , 区内有两个沉积模式 : 一为广阔 

的坡缓底平的广海陆棚模式 , 形成于早寒 

武纪 ; 二为台地 ( 斜坡 )- 广海 ( 盆地 ) 

沉积模式 , 形成于中晚寒武纪。 

2008010478 

晚古生代热带气候对冈瓦纳冰川减退的响 

应 = Late Paleozoic tropical climate response 

to Gondwanan deglaciation. ( 英文 ). Poulsen C 

J; Pollard D; Montañez I P; Rowley D. Geology, 

2007, 35(9): 771-774 

Coupled climate-biome model simulations 

of the late Paleozoic were developed to 

determine the response of Pangean tropical 

climate to Gondwanan deglaciation. The 

model simulations predict substantial changes 

over equatorial Pangea including continental 

drying, a reversal of equatorial winds, warming, 

heavier 18 O values of meteoric precipitation, 

and the expansion of deserts and the contraction 

of forests. The magnitude of these 

tropical responses is sensitive to the extent of 

Gondwana continental ice and the deglacial 

rise in atmospheric pCO 2 , boundary conditions 

that are not well known for the late Paleozoic. 

Nonetheless the model predictions are 

consistent with climatic and environmental 

trends determined from terrestrial proxy data, 

implying that the deglaciation of Gondwana 

was a transformational climate event in tropical 

Pangea. 

2008010479 

北美和东欧跨越全球莫斯科阶 - 卡西莫夫阶 - 

格舍尔阶界线间隔期的旋回层 [“ 数字化 ”] 对 

比和生物地层 = Cyclothem ["digital"] correlation 

and biostratigraphy across the global 

Moscovian-Kasimovian-Gzhelian stage 

boundary interval (Middle-Upper Pennsylvanian) 

in North America and eastern Europe. 

( 英文 ). Heckel P H; Alekseev A; SBarrick J E; 

Boardman D R; et al. Geology, 2007, 35(7): 

607-610 

The long-standing difficulty of correlating 

Pennsylvanian strata among provincial 

faunal regions is resolved by effecting "digital" 

correlation of major glacial-eustatic 

cyclothems that represent high-stands when 

certain species achieved more global distribution 

than usual. In the late Moscovian–early 

Gzhelian (late Desmoinesian–early Virgilian) 

succession in the midcontinent United States, 

several major cyclothems are correlated, by 

both conodont species in common and 

cyclothem scale, with cyclothems in Russia 

(Moscow Basin) and Ukraine (Donets Basin), 

and the remaining cyclothems fit into the 

framework by position and scale. In this way 

the suggested event marker for the global 

Kasimovian-Gzhelian stage boundary (first 

appearance of Idiognathodus simulator) is 

supported, while possible event markers for 

124

the Moscovian-Kasimovian boundary await 

further evaluation. 

2008010480 

黔桂地区二叠系层序地层格架及相对海平 

面变化研究 = Study on sequence stratigraphic 

framework and relative sea-level 

changes of the Permian in Guizhou and 

Guangxi areas, South China. ( 中文 ). 梅冥相 ; 

高金汉 ; 易定红 ; 孟庆芬 ; 李东海 . 高校地质学 

报 , 2002, 8(3): 318-333 

黔桂地区的二叠系以其明显的相分异而 

引人注目 , 在连陆台地上发育煤系地层 , 

而在连陆台地边缘及孤立台地上发育海绵 

生物礁 , 形成一个典型的 “ 台 - 盆 - 丘 - 槽 ” 的 

古地理格局 , 并且相分异最明显的时期正 

好是生物礁发育的时期。二叠系包括三个 

统即船山统、阳新统和乐平统 , 船山统与 

阳新统之交的黔桂运动主幕不整合面以及 

阳新统和乐平统之交的东吴运动主幕不整 

合面特征明显 , 同时还代表了沉积盆地性 

质发生较大变化的界面。在二叠系中 , 船 

山统与下伏石炭系顶部的地层构成 1 个三 

级沉积层序 (SQ19), 阳新统包含 4 个三 

级层序 (SQ20~SQ23), 乐平统包括 2 个 

三级层序 (SQ24,SQ25)。该地区的另一 

个特点是在二叠纪与三叠纪之交发生了较 

为典型的台地淹没事件 , 形成一个较为典 

型的淹没不整合面。因此 , 层序界面类型 

可以根据其所代表的地质涵义而划分为四 

大类型 : 构造不整合面、沉积不整合面、 

淹没不整合面以及它们的相关面。 

2008010481 

邵阳盆地二叠纪层序地层初步研究 = Primary 

study on strata of Permain in Shaoyang 

basin. ( 中文 ). 何欣 ; 孙海清 . 湖南地质 , 2002, 

21(1): 1-6 

邵阳盆地是湘中陆表海盆的一部分 , 二 

叠纪地层以育完整 , 微相类型齐全。基本 

层序类型总体上有局限碳酸盐台地变浅旋 

回型、较深水台盆相硅泥质沉积的韵律式 

非旋回型及三角洲相碎屑岩类中的向上变 

粗或变细型 3 个大类。纵向堆积结构 , 识 

别出了陆架边缘体系域、海侵体系域、凝 

缩段及高水位体系域 , 进而归并出 III 级层 

序 4 个 , 论述了层序格架及横向变化特 

征 ; 指出沉积锰矿与早期高水位体系域、 

煤矿与陆架边缘体系域相关联。 

2008010482 

湘南其昌岭基底起区泥盆纪地层格架探讨 

= Discussion on stratum frame of Devonian in 

upheaval zone of Qichang mountain basement, 

South Hunan. ( 中文 ). 陈贵玖 ; 郭爱民 ; 唐分配 ; 

龚述清 . 湖南地质 , 2002, 21(4): 261-264,274 

其昌岭基底隆起区泥盆纪地层方布 , 在 

不同的区域了不同的岩石组合 , 在分析研 

究了各岩石地层单位的基本特征和分布善 

的基础上 , 分东部、中部、西部三个区域 

时、空两个方面 , 对区内泥盆纪地层的基 

本格架作了探讨。 

2008010483 

试论准噶尔石炭纪 - 三叠纪重要气候事件 = 

Key climatic evenets during Carboniferous- 

Triassic in Junggar. ( 中文 ). 李强 ; 吴绍祖 ; 屈 

迅 ; 李永安 . 新疆地质 , 2002, 20(3): 192-195 

准噶尔石炭纪 — 三叠纪经历了 4 次重要 

的气候事件 , 即晚石炭世降温事件、中二 

叠世温室事件、晚二叠世 - 早三叠世干旱事 

件和中 - 晚三叠世潮湿事件。古气候的发展 

往往有周期性 , 每个大的周期又常常是许 

多水的波动 ( 小周期 ) 发展积聚的结果 , 

这种周期性变化与地球在太阳系中的位 

置、大气圈、海洋、极地冰川系统的变 

化、火山喷发以及块体位移有着紧密的联 

系。 

2008010484 

加拿大育空北部和北极阿拉斯加邻近地区 

泥盆纪和石炭纪古地理和造山运动 = Devonian-Carboniferous 

paleogeography and 

orogenesis, northern Yukon and adjacent Arctic 

Alaska. ( 英文 ). Lane L S. Canadian Journal 

of Earth Sciences, 2007, 44(5): 679-694 

Surface and Subsurface data from northern 

Yukon document a northward facies transition 

from shelf carbonates to basinal graptolitic 

shales and cherts from Late Cambrian to Early 

Devonian time. Parts of this north-facing continental 

margin were deformed during separate 

orogenic events of Early Devonian and Early 

Carboniferous ages. The first event, the Romanzof 

Orogeny, is identified in exposures 

across northwestern Yukon, in adjacent northeastern 

Alaska, and locally in the subsurface 

of the Alaska North Slope. It resulted in tight 

folds, north-directed thrust faults, and intrusion 

by Late Devonian posttectonic granitic 

plutons. Notwithstanding the thrust-fault orientations, 

southward diminution of deformation 

intensity combined with facies variations 

suggest that tectonic transport was generally 

southward. Evidence for an Early Carbonifer- 

125

ous event is preserved in the northern 

Richardson Mountains and locally in the subsurface 

of the Mackenzie Delta region. It consists 

of detached open folds and minor thrust 

faults. Geological and geophysical data front 

northern Yukon document the location and 

orientation of the Early Carboniferous deformation 

front, and define a regional tectonic 

transport direction toward the south or southeast. 

This event is a distal foreland element of 

the Ellesmerian Orogeny (sensu stricto) of the 

Canadian Arctic Islands and is distinct from 

the Romanzof event in age, intensity, and extent. 

Endicott and Lisburne group strata, deposited 

on a south west-facing subsiding shelf, 

overstep rocks deformed by the Romanzof 

event even as Ellesmerian deformation encroached 

from the north. 

2008010485 

齐姆根 — 桑株河地区石炭 — 二叠纪地层划 

分及对比 = Subdivision and correlation of the 

Carboniferous-Permian in Qimugen- 

Sangzhuhe area. ( 中文 ). 奚伯雄 ; 张健 ; 刘增仁 . 

新疆地质 , 2002, 20(S1): 58-66 

齐姆根 — 桑株河地区石炭 — 二叠系分布 

广泛 , 层位齐全 , 化石丰富 . 据实测剖面及系统 

采集的类及腕足、牙形石、孢粉等化石较 

准确地厘定了石炭 — 二叠系各地层单元界 

线和岩石组合特征 , 自下而上划分出卡拉巴 

西塔克组、克里塔克组、和什拉甫组、卡 

拉乌依组、阿孜干组、塔哈奇组和克孜里 

奇曼组、棋盘组、普司格组、达里约尔 

组、杜瓦组 , 其中下石炭统仅分布于莫莫克 

以西 . 早二叠世中晚期 — 晚二叠世早期新藏 

公路以东普司格组属河流 - 湖泊 - 冲积扇相沉 

积 , 莫莫克 — 齐姆根地区棋盘组 , 达里约尔组 

以浅海相与河流三角洲相交互沉积及湖泊 - 

河流相沉积为特征 , 晚二叠世晚期仅于新藏 

公路以东沉积冲积扇 - 扇三角洲相的杜瓦组 . 

2008010486 

济源西部石炭二叠系层序地层学特征 = 

Stratigraphic characteristics of Permo- 

Carboniferous sequances in western Jiyuan. 

( 中文 ). 王丽萍 ; 苏现波 . 煤田地质与勘 

探 , 2002, 30(1): 4-7 

根据野外露头观测 , 结合勘探阶段的资 

料 , 对河南省济源西部石炭二叠系层序地 

层学特征进行了系统研究 , 探讨了聚煤作 

用的控制因素 , 首次发现河南省境域内石 

炭纪的河流与三角洲沉积 , 并指出中条山 

可能是石炭二叠纪重要的物源区。该区层 

序地层学研究对河南省石炭二叠纪古地理 

再造具有重要意义。 

2008010487 

巴楚隆起与阿瓦提凹陷寒武系及奥陶系沉 

积古地理分析 = Sedimentology and palaeogeography 

of the Cambrian-Ordovician in 

Bachu uplift and Awati depression, the Tarim 

Basin. ( 中文 ). 何宏 ; 彭苏萍 ; 邵龙义 ; 高云峰 ; 

时宗波 . 煤田地质与勘探 , 2002, 30(6): 1-4 

根据野外露头、钻井资料分析 , 对塔里 

木盆地巴楚隆起东部和阿瓦提凹陷东南部 

寒武系和奥陶系进行了沉积与古地理分 

析。研究表明 , 该区寒武系和奥陶系总体 

上表现为从深 - 浅 - 深的沉积环境深化过程。 

早寒武世早期经历了短暂的深水盆地环境 

后 , 自早寒武世中晚期至中寒武世演变为 

局限台地 —— 蒸发盐台地环境 ; 晚寒武世 

至早奥陶世海平面开始逐渐上升 , 以开阔 

台地环境为主 , 至晚奥陶世中期演变为台 

地边缘斜坡环境。 

2008010488 

欧洲 Variscan 一些晚石炭世盆地的比较分 

析 = A comparative analysis of some Late 

Carboniferous basins of Variscan Europe. ( 英 

文 ). Oplustil S; Clear C J. Geological Magazine, 

2007, 144(3): 417-448 

Vegetation diversity and pattern changes, 

and their relation to tectono-sedimentary histories 

are compared between selected 

Euramerican Late Palaeozoic coalfields, to 

understand better the controls on the dynamics 

of the Pennsylvanian terrestrial ecosystems 

and to demonstrate the problems with comparing 

data from various basins. The analysis is 

based on data from the following basins of 

different geotectonic and palaeogeographical 

positions: the cratonic Pennines Basin, the 

foreland South Wales and Upper Silesia basins, 

and the fault-related Intra Sudetic and 

Central and Western Bohemia basins. The 

analysis indicates that complex factors are 

responsible for changes in plant diversity and 

vegetation patterns. These are related to climate, 

tectonics, preservation potential, sampling 

biases and the current state of revision of 

the flora in each basin. Plant diversity patterns 

in the basins differ because of local controls 

and/or the character and detail of the available 

data. Maximum diversity varies among the 

basins within the Langsettian and Duckmantian 

substages. Two apparent step-like 

drops in diversity were detected within coalbearing 

strata of most basins: at the Duck- 

126

mantian/Bolsovian boundary and at the 

Bolsovian/Asturian boundary. Further and 

more prominent falls are related to transitions 

from coal-bearing to non-coal-bearing (mostly 

red bed) strata or vice versa during Stephanian 

times. Interpretation of climatic signals recorded 

in the sedimentary successions indicates 

that Westphalian and middle Stephanian 

times were wet intervals, whereas early and 

late Stephanian times were drier. 

2008010489 

英国南部晚石炭世蜚蠊类昆虫的地层学潜 

力 = The stratigraphical potential of blattodean 

insects from the late Carboniferous of 

southern Britain. ( 英文 ). Jarzembowski E A; 

Schneider J W. Geological Magazine, 2007, 

144(3): 449-456 

The Blattodea (cockroaches sensu lato or 

roachoids) from the southern coalfields of the 

UK are reviewed or examined, especially species 

occurring in more than one coal basin 

including Mylacris abrupta (Bolton, 1930) 

comb. nov., and undescribed material from 

Writhlington (Somerset). It is proposed that a 

derived mylacrid Mylacris–Sooblatta assemblage 

is used to extend the latest Westphalian 

and earliest Stephanian insect zonation from 

the continent to southern Britain, thus augmenting 

the European Pennsylvanian scheme. 

中生界 

2008010490 

盎格鲁 - 巴黎盆地 Gault Clay( 阿尔拜阶 ) 磷 

块岩及其成因 = Phosphates and phosphogenesis 

in the Gault Clay (Albian) of the Anglo–Paris 

Basin. ( 英文 ). Knight R I. Cretaceous 

Research, 1999, 20(5): 507-521 

Textural and structural analyses of phosphatic 

nodules in Albian clays and glauconitic 

sandy clays from the Anglo–Paris Basin 

(‘Gault Clay’s.l.) indicate formation within a 

fluctuating, dynamic seafloor energy regime. 

They formed via phosphate precipitation 

around organic-rich clasts within anoxic, low 

pH sediments. Incremental growth is observed 

owing to reworking cycles of exhumation and 

reburial. Primary ultrastructure is preserved 

within the nodules, but provides only limited 

evidence as to the precipitation mechanism of 

phosphogenesis, although microbial and colloidal 

systems are most likely. 

2008010491 

澳大利亚 Eromanga 盆地东北部早白垩纪 

克拉通内盆海进过程的水深变化 = Bathymetric 

change during Early Cretaceous intracratonic 

marine transgression across the northeastern 

Eromanga Basin, Australia. ( 英文 ). 

Campbell R J; Haig D W. Cretaceous Research, 

1999, 20(4): 403-446 

Bathymetric change is investigated 

within the transgressive phase of an extensive 

Early Cretaceous (Aptian-Albian) marine 

flooding of the Australian continent. Lithofacies 

and biofacies associations, found in nine 

outcrop sections and four continuously cored 

bore sections in the northeastern Eromanga 

Basin, are used to reconstruct depositional 

environments and to determine palaeobathymetry. 

Shoreface (c . 0–2 m water depth), 

transitional (c .

德国北部下萨克森盆地巴列姆阶 - 阿普第阶 

界线有机地球化学和沉积历史 = Organic 

geochemistry and depositional history of the 

Barremian–Aptian boundary interval in the 

Lower Saxony Basin, northern Germany. ( 英 

文 ). Littke R; Jendrzejewski L; Lokay P; 

Wang S Q; Rullkötter J. Cretaceous Research, 

1998, 19(5): 581-614 

The Barremian–Aptian boundary interval 

in northern Germany is characterized by a 

major lithologic turnover from dark coloured, 

organic matter-rich towards light-coloured, 

organic matter-lean sedimentary rocks. To 

derive information on the respective environmental 

conditions and their development 

through time, organic matter from this interval 

was studied by petrographic and geochemical 

methods. The study was performed on five 

cored boreholes each recovering the Barremian–Aptian 

boundary interval, and also on 

two research wells in the same area covering 

the Late Albian for comparative purpose. 

The geochemical and petrographical data 

allow the differentiation to two organofacies. 

The lower succession is characterized by variable 

organic carbon contents which reach 

maximum values up to 7% C org in the paper 

shale units (‘Blättertone’) and in the early Aptian 

Fish Shale (‘Fischschiefer’; a possible 

product/equivalent of the Oceanic Anoxic 

Event 1a). Petrographically, the organic matter 

is mainly alginite and bituminite. It is moderately 

well preserved according to Hydrogen 

Index (HI) values between 150 and 450 mg 

HC/g C org for most of the samples. Thenalkane 

distribution reveals a contribution of 

both marine algae and terrestrial higher land 

plants. To explain these analytical results, a 

depositional model has been developed which 

is based on limited water exchange with the 

adjacent oceans having caused oxygen deficiency 

and deposition of numerous organic 

carbon-rich sediment layers. As revealed by 

HI values above 300 mg HC/g C org and by annalkane 

maximum atn-C 15 , the organic matter 

in the Fischschiefer is mostly of marine origin. 

Furthermore, the 28,30-dinor-hopane detected 

in only one sample probably indicates slight 

variation in redox conditions during 

Fischschiefer deposition. 

The major change of environmental conditions 

began before Fischschiefer deposition, 

i.e., in the earliest Aptian. A decrease in organic 

carbon content and HI values and a 

higher ratio of reworked vitrinite and inertinite 

over primary vitrinite indicate gradually 

changing conditions. The observed environmental 

change is related to the Aptian transgression 

leading to a clear domination of terrigenous 

organic matter in the sediment above 

the Fischschiefer (HedbergellaMarl and 

above). Completely different oceanic conditions 

existed in the Lower Saxony Basin from 

then on until the Late Cretaceous, when organic 

matter-poor sediments were deposited 

under oxygen-rich water. 

2008010493 

德国西北部盆地下阿普第阶主量和微量元 

素地球化学分析 = Major and minor element 

geochemistry of Lower Aptian sediments from 

the NW German Basin (core Hohenegglesen 

KB 40). ( 英文 ). Hild E; Brumsack H J. Cretaceous 

Research, 1998, 19(5): 615-633 

Two hundred and thirty-three samples 

from the Hoheneggelsen KB 40 drill core, 

located 30 km SE of Hannover, Germany, 

were analysed for 12 major elements, 14 minor 

elements, degree of pyritization, and S- 

isotopic composition. This early Aptian sequence 

consists of three lithological units: an 

upper marly section (Hedbergellamarl) that 

was deposited under strictly oxic conditions, 

an underlying fish shale horizon 

("Fischschiefer") which represents an anoxic 

stagnant phase of sedimentation, and a lower 

clay-rich section (dark coloured claystones) 

including scattered thin paper shale horizons 

("Blättertone") reflecting a suboxic to anoxic 

water column. Major and minor element profiles 

mirror the changing sedimentology of the 

individual units which can be explained by 

different palaeoceanographic and climatic 

conditions. A major shift in major element 

ratios, which is probably a result of a different 

source of the terrigenous detrital material or of 

variations in weathering intensity, took place 

before the onset of fish shale sedimentation. 

The high-resolution sampling and analysis 

(sampling intervals 1 to 5 cm) allows the detection 

of small-scale variations in element 

contents in individual sedimentary units and in 

transitional stages of suboxic to anoxic (dark 

claystone to paper shale) or anoxic to oxic 

(fish shale toHedbergellamarl) palaeoenvironments. 

2008010494 

南极南 Shetland 岛侏罗 - 白垩系 Byers 组 : 

修订的地层学和区域对比 = The Jurassic– 

Lower Cretaceous Byers Group, South Shetland 

Islands, Antarctica: revised stratigraphy 

and regional correlations. ( 英文 ). Hathway B; 

128

Lomas S A. Cretaceous Research, 1998, 19(1): 

43-67 

The Byers Group, exposed in the western 

South Shetland Islands, is a thick (at least 2.7 

km) succession recording Late Jurassic–Early 

Cretaceous sedimentation and volcanism on 

the Pacific flank of the Antarctic Peninsula 

magnetic arc. At least 1.3 km of marine clastic 

rocks are overlain by 1.4 km of non-marine 

strata. Penecontemporaneous, mainly intrusive, 

igneous rocks are present in much of the succession. 

At the base of the Byers Group, radiolarian-rich, 

hemipelagic mudstones of the 

Kimmeridgian–Tithonian Anchorage Formation 

are succeeded by terrigenous, slope-apron 

mudstones and sandstones of the Berriasian 

President Beaches Formation. These deepmarine 

strata are overlain by shallower-marine 

conglomerates and mudstones of the Berriasian–Valanginian 

Chester Cone Formation. 

The upper part of the marine succession also 

includes the volcanic breccias of the Start Hill 

Formation, interpreted as part of a debrisapron 

flanking a substantial volcanic edifice. 

Finally, following a Valanginian–Aptian erosional 

hiatus, non-marine volcaniclastic rocks 

of the Cerro Negro Formation were deposited 

in early Aptian times. Comparison with timeequivalent 

successions elsewhere in the Antarctic 

Peninsula region suggests that within 

the overall regressive trend, the Byers Group 

records regionally significant pulses or arc 

uplift in Tithonian–earliest Berriasian, latest 

Berriasian, and late Valanginian–Earliest Aptian 

times. 

2008010495 

美国 Lima Peaks 地区到蒙大拿和爱荷华西 

南部 Madison Range 地区的上白垩统地层 

对比 = Correlation of Upper Cretaceous strata 

from Lima Peaks area to Madison Range, 

southwestern Montana and southeastern Idaho, 

USA. ( 英文 ). Dyman T S; Tysdal R G; Perry 

W J; Obradovich J D; Haley J C; Nichols D J. 


An 40 Ar/ 39 Ar age of 85.81 Ma±0.22 my 

was obtained on sanidine from a volcanic procellanite 

bed near the top of the 2135+m-thick 

Upper Cretaceous Frontier Formation in the 

Lima Peaks area of southwestern Montana. 

This early Santonian age, combined with previously 

determined age data including a palynological 

age of Cenomanian for the lower 

Frontier at Lima Peaks, and a U-Pb isotopic 

date of about 95 Ma for the base of the Frontier 

Formation in the eastern Pioneer Mountains 

north of the Lima Peaks area, provides 

an age range for the nonmarine formation. In 

the Madison Range, farther east in southweastern 

Montana, this age range corresponds 

to marine strata of not only the Frontier Formation, 

but also the overlying Cody Shale and 

Telegraph Creek Formation, a sequence that 

totals less than 760 m thick. 

The Upper Cretaceous marine formations 

of the madison Range are closely zoned by 

molluscan faunas that are well constrained 

with radiometric dates. The 40 Ar/ 39 Ar age of 

85.81 Ma±0.22 my at Lima Peaks is bracketed 

by radiometric dates for theScaphites depressus—Protexanites 

bourgeoisianusbiozone and 

the overlying Clioscaphites saxitonianus— 

Inoceramus undulatopilcatusbiozone of the 

Western Interior. Fossils of both of these biozones 

are present in the Cody Shale and the 

Telegraph Creek Formation in the Madison 

Range. The Telegraph Creek contains two 

units of volcanic ash that are approximate time 

equivalents of the volcanic procellanite of the 

Lima Peaks area. Clasts in the conglomerate 

of the upper part of the Frontier in the Lima 

Peaks area were shed during the initial stages 

of uplift of the Blacktail-Snowcrest Highlands 

which rose to the north. The dated porcellanite 

lies above the conglomerates and indicates 

that the uplift was initiated by middle or late 

Coniacian, 87–88 Ma. 

2008010496 

塔里木盆地西南地区上白垩统生物丘 = 

Upper Cretaceous rudist bioherms in south 

western Tarim. ( 中文 ). 彭阳 ; 郭宪璞 ; 王易农 ; 

丁孝忠 . 地质通报 , 2002, 21(2): 83-87 1 图版 . 

塔里木盆地西南部昆仑山前缘地区上白 

垩统依格孜牙组中发育一套固着蛤生物丘 , 

横向上由西向东沿阿克彻依、乌依塔克、 

依格孜牙、吐依洛克、阿尔塔什至莫莫卡 

一线呈串珠状展布。丘基下部为潜在的生 

油岩 — 藻泥晶灰岩 , 上部为生物碎屑滩 , 主体 

丘核为簇状固着蛤灰岩 , 丘顶藻席可见清楚 

的上超。生物丘下伏地层及盖层均为膏泥 

岩 , 形成了一个顶底圈闭。 

2008010497 

辽北早白垩世泉头组沉积体系 = Study of 

the sedimentary system of the Early Cretaceous 

Quantou Formation in northern Liaoning. 

( 中文 ). 周勇 ; 胡晋伟 ; 李东涛 . 地质通 

报 , 2002, 21(3): 144-149 

通过辽北早白垩世泉头组地层研究 , 提出 

泉头组沉积层序划分方案 : 划分为 2 个层 

序 ,11 个旋回层序 ,20 个基本层序 ; 总结了层 

129

序划分的 4 种类型及其识别标志 ; 识别出 3 

种沉积体系 — 湖相三角洲分流河道沉积体 

系、浅湖相沉积体系、湖相三角洲前缘沉 

积体系。 

2008010498 

上黑龙江盆地中上侏罗统二十二站群的地 

层划分与时代 = Stratigraphic division and 

age of the Mid-Upper Jurassic Ershi'erzhan 

Group in the upper Heilongjiang River basin. 

( 中文 ). 孙广瑞 ; 刘旭光 ; 韩振哲 ; 刘世伟 ; 郭奎 

城 ; 张金莲 ; 朱春燕 ; 王德平 . 地质通报 , 2002, 

21(3): 150-155 

根据 1∶ 5万区域地质调查 , 大兴安岭北端 

上黑龙江盆地内的原中侏罗统二十二站组 

的时代被重新厘定为中、晚侏罗世 

Bajocian─Tithonian 期并改称为二十二站 

群。根据岩性特征和化石组合 , 将其进一步 

划分为两个组 : 下部称大西尔根气河组 , 其下 

部岩性以砂岩为主 , 上部以泥质粉砂岩 ─ 砂 

岩为主 , 含中侏罗世至晚侏罗世早期的双壳 

类动物群化石 , 可划分为 Sibireconcha─ Cuneopsis, 

Margaritifera─ Unio, Fergannoconcha 

3 个生物组合 ; 上部称马林组 , 主要由粉 

砂岩组成 , 夹有少量砾岩和粉砂质灰岩 , 含晚 

侏罗世中晚期的介形类动物群化石 , 可称为 

Eoparacypris─Rhinocypris─Yanshanina 组 

合。 

2008010499 

西藏班公湖 - 丁青蛇绿岩带东段侏罗纪盖层 

沉积的地层划分 = Stratigraphic division and 

geological significance of the Jurassic cover 

sediments in the eastern sector of the Bangong 

Lake-Dêngqên ophiolite belt in Tibet. ( 中文 ). 

王建平 ; 刘彦明 ; 李秋生 ; 岳国利 ; 裴放 . 地质通 

报 , 2002, 21(7): 405-410 

根据对西藏班公湖 — 丁青缝合带东段丁 

青蛇绿岩及其盖层沉积研究 , 确定丁青蛇绿 

岩时代为晚三叠世 , 盖层沉积地层时代为中 

晚侏罗世 , 进一步划分为德极国组、德吉弄 

组和机末组 , 并建立了 3 个生物地层组合。 

据此首次提出班公湖 — 丁青缝合带东段于 

三叠纪打开 , 晚三叠世发育成为较成熟洋盆 , 

并最终于早侏罗世末关闭。通过对班公 

湖 — 丁青缝合带东、西部地质特征的对比 , 

指出该缝合带关闭时间从东部的早侏罗世 

末到西部的晚侏罗世末 , 从而为特提斯洋演 

化进程提供了新证据。 

2008010500 

羌塘盆地北部马料山侏罗纪布曲组地层古 

生物及沉积环境 = Stratigraphy, paleontology, 

and sedimentary environment of the Jurassic 

Biqu Formation at Maliao Mountain,northern 

Qiangtang Basin. ( 中文 ). 赵兵 ; 伊海生 ; 林金 

辉 ; 时志强 ; 李保华 ; 黄继均 . 地质通报 , 2002, 

21(7): 415-420 

详细描述了羌塘盆地北部乌兰乌拉湖地 

区马料山侏罗系剖面 , 将剖面划分为雀莫错 

组、布曲组和夏里组 3 个岩石地层单位 , 其 

中布曲组出露齐全 , 化石丰富。根据沉积环 

境及相对海平面变化规律将布曲组划分为 2 

个沉积层序 , 并讨论了各体系域特征。依据 

马料山剖面布曲组的生物组合及分布特征 

建立了 1 个双壳类生物组合带即 

Chlamystipperi-Protocardia stricklandi 组合 

带 , 并细分为 3 个组合亚带 , 其时限为中侏罗 

世巴通期。 

2008010501 

四川木里海相侏罗纪地层的发现及地质意 

义 = Discovery of marine Jurassic strata at 

Muli,Sichuan,and its geological implications. 

( 中文 ). 王康明 ; 龙斌 ; 李雁龙 ; 朱科 ; 杨泽湘 ; 文 

登奎 . 地质通报 , 2002, 21(7): 421-427 

在川滇金沙江 - 哀牢山结合带以东 , 从未发 

现过海相侏罗纪地层。笔者最近在其以东 

数百公里的四川省木里县瓦厂地区的甘孜 - 

理塘结合带以东发现广泛分布的含层孔虫 

Claodocoropsis mirabilis, 珊瑚 Thecosmilia cf. 

Weberi Regny,Pratethmos cf. discus, 水螅 

Spongiomorpha cf. robusta 等生物群的海相 

侏罗纪地层。此套地层下部为陆源碎屑岩 , 

上部为富产层孔虫、珊瑚、水螅的正常广 

海台地相碳酸盐岩 , 底部以底砾岩与下伏晚 

三叠世曲嘎寺组平行不整合接触。其岩 

性、生物组合均可与西藏昌都地块侏罗纪 

地层对比。本区侏罗纪沉积盆地是在晚三 

叠世古特提斯洋闭合的基础上 , 随新特提斯 

洋开合而发展演化的 , 消亡于古近纪初期。 

2008010502 

内蒙古宁城道虎沟地区侏罗纪地层划分及 

时代探讨 = Stratigraphic division of the Jurassic 

in the Daohugou area, Ningcheng,Inner 

Mongolia. ( 中文 ). 任东 ; 高克勤 ; 郭子光 ; 姬书 

安 ; 谭京晶 ; 宋卓 . 地质通报 , 2002, 21(8-9): 

584-591 2 图版 . 

最近在内蒙古宁城道虎沟村新发现了一 

些翼龙、蝾螈等重要化石 , 有关道虎沟化石 

层的地层层序和时代归属产生了较大的争 

论。笔者根据野外调查结果和生物地层学 

130

资料 , 讨论了道虎沟化石层的地层层序和时 

代归属。详尽的区域地层踏勘和实测地层 

剖面充分显示 , 道虎沟化石层归属于中侏罗 

世九龙山组 , 而不是所谓的义县组 ; 道虎沟化 

石层与下伏太古宙马鞍山片麻岩而不是土 

城子组呈角度不整合接触。 

2008010503 

辽西凌源盆地含两个中生代生物群的地层 

层序和时代问题讨论 = Mesozoic biotabearing 

depositional successions in the Lingyuan 

basin,western Liaoning,and their 

ages:A discussion. ( 中文 ). 柳永清 ; 金小赤 . 地 

质通报 , 2002, 21(8-9): 592-595 

通过对凌源盆地含 2 个中生代生物群的 

地层序列及相关地层的野外调查研究 , 基本 

查明了产出地的地质背景及构造特征 , 阐述 

了凌源盆地含中生代生物群的地层层序及 

其与周边地区中生界的对比关系。西台子 

和帽子山一带含热河生物群的地层对应白 

垩系义县组 , 确定含道虎沟生物群沉积层序 

的地质年代还需进行更深入的工作。 

2008010504 

广东南雄盆地白垩系 — 古近系界线 = The 

Cretaceous-Paleogene boundary in the Nanxiong 

basin,Guangdong Province. ( 中文 ). 童永 

生 ; 李曼英 ; 李茜 . 地质通报 , 2002, 21(8-9): 

668-674 

在过去的 30 年中有数支考察队在广东南 

雄盆地进行了白垩纪和古近纪地层多学科 

的系统研究。本文综合了南雄盆地近年的 

岩石地层学、磁性地层学、地球化学、古 

生物学方面的研究成果和湖北新洲盆地时 

代相当于浓山组的地层中得到的同位素年 

龄 , 认为上湖组时代大体上与 Danian 期相当 , 

或相当于北美哺乳动物分期 Puercan 和 

Torrejonian 期 , 其底界接近于白垩系 — 古近 

系界线。 

2008010505 

北羌塘乌兰乌拉湖地区白垩纪岩石地层及 

沉积环境 = Cretaceous lithostratigraphy and 

sedimentary environment in the Ulan Ul Lake 

area,northern Qiangtang. ( 中文 ). 赵兵 ; 伊海生 ; 

林金辉 ; 时志强 ; 黄继均 ; 李保华 . 地质通 

报 , 2002, 21(11): 749-755 

详细描述了北羌塘乌兰乌拉湖地区白垩 

纪地层剖面 , 将区内白垩系划分为错居日组 

和桑恰山组。沉积相分析表明 , 乌兰乌拉湖 

地区错居日组主要为冲积扇至河流相沉积 , 

岩性及厚度变化较大 , 而桑恰山组为湖泊、 

湖三角洲至河流相沉积 . 初步认为错居日组 

为早白垩世地层 , 桑恰山组为早白垩世晚期 

至晚白垩世地层。 

2008010506 

贵州关岭上三叠统瓦窑组中碳酸盐岩结核 

形成的生物作用 = Biological processes for 

the formation of carbonate concretions in the 

Up per Triassic Wayao Formation of 

Guanling,Guizhou. ( 中文 ). 王尚彦 ; 王宁 ; 罗永 

明 ; 王红梅 ; 孙亚莉 . 地质通报 , 2002, 21(12): 

855-857 

贵州省关岭县新铺乡附近的晚三叠世早 

期地层瓦窑组底部产具重大科学意义的关 

岭生物群。关岭生物群产出地层中伴有大 

量大型碳酸盐岩结核。这些结核中部都有 

植物茎干 , 结核内的海百合、双壳、菊石、 

牙形刺等生物化石含量明显高于结核周围 

的岩石 , 且有许多生物化石直接附着在植物 

茎干上。这类结核的形成 , 除化学沉积作用 

外 , 还有生物作用的影响。海百合、双壳类 

和菊石类栖息在植物茎干上营假浮游生活 , 

随着栖息生物量和化学沉积物灰泥的增加 , 

逐渐沉积在海底形成结核。 

2008010507 

克罗地亚 Gorski Kotar 地区下三叠统浅海 

相序列 : 岩相和牙形石的时代测定 = The 

Lower Triassic shallow marine succession in 

Gorski Kotar region (External Dinarides, 

Croatia): Lithofacies and conodont dating. ( 英 

文 ). Aljinovic D; Kolar-Jurkovsek T; Jurkovsek 

B. Rivista Italiana di Paleontologia e 

stratigrafia, 2006, 112(1): 35-53 

The depositional environment is envisaged 

as shallow marine realm of a passive continental 

margin. Sedimentary complex differentiates 

in predominantly carbonate sedimentation 

that characterises the beginning of deposition 

with upward increasing trend of terrigeneous 

influx. Lithofacial units have been defined as 

oolitic bar facies, lagoonal facies, shorefaceoffshore 

facies, ooid-sandy shoal facies, restricted 

bay facies, shoreface-offshore facies, 

ooid-sandy shoal vacies, restricted bay facies 

and flat-pebble conglomerate facies. The following 

conodont taxa were collected: Ellisonia 

sp., Foliella gardenae, Hadrodontina sp., 

Hindeodus, Hindeodus sp., Pachycladina 

obliqua, Parachirognathus sp., Platyvillosus 

costatus and P. hamadai. 

2008010508 

131

辽西大平房 — 梅勒营子盆地九佛堂组珍稀 

化石层的划分与对比 = Division and correlation 

of unique fossil-bearing beds of Jiufotang 

Formation in Dapingfang-Meileyingzi Basin 

of western Liaoning. ( 中文 ). 段冶 ; 张立君 ; 李 

莉 ; 程绍利 . 世界地质 , 2006, 25(2): 113-119 

辽西是世界上研究鸟类起源、恐龙进 

化、鸟类、哺乳动物以及被子植物的早期 

演化等最重要地区之一。本文重点论述了 

辽西大平房 — 梅勒营子盆地九佛堂组含珍 

稀化石的地层划分与对比。珍稀化石层自 

下而上包括有 : 九佛堂组第二段的喇嘛沟 

层、第三段下部的黄花沟层及第三段上部 

的原家洼层。根据所含介形类化石组合特 

征 , 将联合乡小鱼沟和胜利乡南炉一带含鸟 

类、翼龙类的化石层与喇嘛沟层对比 , 胡家 

营子、八棱观和车杖子一带的含鸟类、翼 

龙类的化石层与原家洼层对比。 

2008010509 

黑龙江省东部鸡西群与龙爪沟群综合地层 

对比研究 = Integrated stratigraphic correlation 

of the Jixi Group and Longzhaogou 

Group in eastern Heilongjiang. ( 中文 ). 李仰 

春 ; 杨晓平 ; 周兴福 ; 王洪杰 . 中国地质 , 2006, 

33(6): 1312-1320 

利用最新古生物、磁性地层年代学资 

料对鸡西群、龙爪沟群进行了年代地层划 

分 , 确定了两群形成时间为早白垩世凡兰吟 

期 - 阿尔布中期。同时采用层序地层、盆地 

形成动力学、事件地层学、盆地湖 ( 海 ) 平面 

升降曲线与全球海平面升降曲线对比等方 

法 . 对两群进行了综合对比 . 证实两群为同一 

构造 - 沉降旋回背景下的等时异相关系。笔 

者认为龙爪沟群自下而上划分为 4 个组 , 即 

裴德组、七虎林河组、下云山组、朝阳组 , 

其在横向上分别对应鸡西群滴道组、城子 

河组、穆棱组、东山组。这一研究结果将对 

进一步讨论黑龙江东部中生代海陆变迁机 

制、地层、构造格架建立及煤矿预测等具 

有重要的指示意义。 

2008010510 

东北地区晚中生代地质群发事件及生物群 

响应 = Late Mesozoic geologic group events 

and biotic response in northeast China. ( 中文 ). 

黄清华 ; 吴河勇 ; 孔明华 ; 刘继莹 ; 邹宗义 . 石油 

学报 , 2006, 27(suppl.): 76-79 

中国东北地区内陆盆地下白垩统充填火 

山岩、火山碎屑岩和含媒碎屑岩沉积组合 , 

上白垩统充填以砂、泥碎屑岩为主的河流 

相、湖泊相沉积组合 . 盆地沉积演化史和生 

物发育史研究表明 , 地质群发事件阶段性特 

征明显 , 早白垩世的火山事件 , 中白垩世的超 

静磁带和极端温室气候及古湖泊缺氧事件 

与全球同期重大地质事件的发生具有较好 

的协同性 . 同时 , 盆地内湖生生物群演化表征 

为热河生物群、松花江生物群和明水生物 

群的顺序出现、突发演化和显著的种群绝 

灭现象 , 显示出生物与环境变化的一致性。 

2008010511 

西藏羌塘托纳木上侏罗统索瓦组地层学特 

征 = Stratigraphic features of Upper Jurassic 

Suowa Formation in Tuonamu region, Tibet. 

( 中文 ). 金玮 ; 王成善 ; 赵兵 ; 李亚林 . 西北地 

质 , 2006, 39(3): 97-105 1 图版 . 

羌塘盆地地处藏北高原 , 其南北界分别为 

班公错 - 怒江缝合带与拉竹龙 - 金沙江缝合带 , 

盆地面积约 180 000 km 2 。进一步可分为羌 

北坳陷、中央隆起带和羌南坳陷 3 个二级 

构造单元。双湖托纳木地区地处羌北坳陷 

与中央隆起带毗连地带 , 索瓦组分布于研究 

区北部大部分地区 , 根据地层层序及岩性组 

合特征 , 同时结合岩石、古生物、沉积旋 

回、接触关系等对地层进行了较系统的划 

分 , 将索瓦组划分为 4 个岩性段 ; 索瓦组一段 

到四段自下而上反映出一个完整的海侵 — 

海退序列 , 分别为碳酸盐台地 — 混积缓坡 — 

混积碳酸盐台地 — 混积外滨浅水陆棚沉积 

环境 ; 索瓦组三段礁灰岩和油页岩的发现对 

古环境的恢复以及油气的生储盖研究都具 

有重要意义 ; 根据区内索瓦组的古生物地层 

分布和组合特征 , 建立了珊瑚组合带和双壳 

类组合带 , 确定索瓦组为上侏罗统 , 大致与 

Oxfordian-Kimmeridgian 相当。 

2008010512 

新疆罗布泊地区侏罗纪地层的发现及其意 

义 = Discovery of Jurassic strata in Luobubo 

area,Xinjiang and its Geological Significance. 

( 中文 ). 杨瑞东 ; 罗新荣 ; 张传林 ; 王佰勋 ; 田敬 

全 ; 魏怀瑞 ; 王伟 . 西北地质 , 2006, 39(4): 10- 

15 1 图版 . 

在距罗布泊以西 20 km 的沙漠与戈壁交 

界处 (Y=157339013,X=4516330) 发现了完整 

的侏罗系 , 地层为早、中侏罗世苏康组砾 

岩、砂岩、粉砂岩、泥岩夹多层煤层 ( 线 ), 

在粉砂岩中保存有大量的硅化木化石 , 化石 

主要为石松柏纲 Coniferae 

sp.,Cupressinoxycon sp.。这为研究塔里 

木盆地侏罗纪植物群及古气候提供了重要 

的古生物化石资料。在塔里木盆地东北地 

区阿满坳陷东北向沙漠中发现的侏罗系 , 对 

132

确定侏罗系的分布范围具有一定的意义 , 而 

且也填补了罗布泊地区侏罗系的空白。同 

时 , 还发现侏罗系中多层煤层 , 这为塔里木盆 

地油气勘探研究提供了重要的材料。 

2008010513 

新疆北部二叠系特征及其与三叠系界线划 

分 = Characterristics of Permian and the 

boundary between Permian and Triassic system 

in the northern Xinjiang. ( 中文 ). 柳益群 ; 

周鼎武 ; 冯乔 ; 郝建荣 . 西北大学学报 ( 自然科 

学版 ), 2006, 36(4): 615-622 

目的对新疆准噶尔盆地南缘、吐哈盆地 

和三塘湖盆地的二叠系及其与三叠系界线 

的划分提供新的依据。方法在该区长期工 

作的基础上 , 参考前人地层划分成果及当地 

使用习惯 , 利用岩石地层、生物地层、火山 

岩同位素年龄、古地磁等方法进行综合分 

析 , 对三地区的二叠系进行了综合划分与对 

比。结果将新疆北部二叠系分别称下、 

中、上统 , 与中国南方及国际标准的 3 个统 

对应 ; 中二叠统对应于瓜德鲁普统 , 地质时代 

为早二叠世 (290~265 Ma), 中、上二叠统界 

线在中二叠统塔尔郎组上部 , 上二叠统与三 

叠系界线在上二叠统锅底坑组内 ; 中二叠统 

分布于准噶尔盆地中南部、吐哈盆地北部 

和三塘湖盆地南部。结论建议将大龙口、 

锅底坑、塔尔郎沟、照壁山剖面和跃进沟 

剖面分别作为北疆地区二叠系 — 三叠系标 

准剖面。 

2008010514 

安塞地区三叠系延长组层序地层分析 = 

Sequence analysis of the Triassic Yanchang 

Formation in the area of Ansai. ( 中文 ). 陈全 

红 ; 李文厚 ; 赵宏刚 ; 崔军平 ; 梁积伟 . 西北大学 

学报 ( 自然科学版 ), 2006, 36(5): 784-788 

目的详细划分安塞地区延长组层序 , 论述 

层序演化特征 , 并分析层序对油气藏的控制 

作用。方法在对露头剖面、钻井岩心及测 

井曲线综合分析的基础上 , 结合层序界面识 

别、准层序组样式、层序的划分和对比、 

沉积体系域识别及其组合样式 , 划分层序并 

进行分析。结果把延长组化分为 4 个三级 

层序 , 分别对应长 10— 长 9, 长 8— 长 7, 长 

6— 长 4+5 和长 3+2— 长 1 期沉积 ; 层序 1 至 

层序 4 分别经历了湖盆形成及扩张期、鼎 

盛期、回返期、萎缩消亡期 ; 区域规模的储 

层大都处在低位体系域中。结论层序控制 

着生储盖的组合、储层的展布及储层的储 

集性能。 

2008010515 

酒泉盆地晚白垩世 — 古新世构造特征 = A 

study on characteristics of the Late Cretaceous-Paleocene 

structures in Jiuquan Basin. 

( 中文 ). 程晓敢 ; 郑德文 ; 杨树锋 ; 肖安成 ; 陈汉 

林 . 石油与天然气地质 , 2006, 27(4): 522-527 

酒泉盆地普遍发育了始新统与下白垩统 

之间的不整合。通过对地震剖面和下白垩 

统中沟组残余厚度的分析 , 提出了酒泉盆地 

晚白垩世 — 古新世发生了强烈的构造变形 , 

构造线总体方向为北西向。晚白垩世 — 古 

新世的变形导致了早白垩世连通的酒泉盆 

地和民乐盆地、酒泉盆地的花海凹陷和石 

大凹陷开始分割。该期变形还对盆地的油 

气聚集和后期的沉积起到了控制作用。 

2008010516 

准噶尔盆地腹部侏罗系层序地层划分 = 

Characteristics of Jurassic sequence stratigraphy 

in the middle area of Junggar Basin. ( 中 

文 ). 邱春光 ; 邓宏文 ; 吴铁壮 ; 王胜建 . 新疆地 

质 , 2006, 24(2): 165-170 

根据工区内现有的钻井、测井和地震资 

料 , 应用以基准面为参照格架的高分辨层序 

地层学理论与研究方法 , 对准噶尔盆地腹部 

侏罗系进行了层序界面的识别 . 共识别出层 

序界面 7 个 , 对应划分出 1 个长期基准面旋 

回和 6 个中期基准面旋回 , 长期基准面旋回 

界面的性质为区域性角度不整合 , 中期基准 

面旋回界面性质包括局部不整合、沉积转 

换面和同沉积侵蚀面 . 沉积转换面的识别对 

中期基准面旋回界面的识别起重要作用 . 

2008010517 

西藏北部双湖地区海相侏罗纪磁性地层研 

究 = Magnetostratigraphic study of the marine 

Jurassic in the Shuanghu area, northern Tibet. 

( 中文 ). 朱同兴 ; 潘忠习 ; 庄忠海 ; 秦建华 ; 董文 

彤 ; 王小龙 ; 黄志英 ; 冯心涛 . 地质学报 , 2002, 

76(3): 308-316 

西藏北部双湖地区海相侏罗纪磁性地层 

采样剖面包括菊花山下侏罗统剖面和那底 

岗日中、上侏罗统剖面 , 采集样品共 1231 

件。磁性地层采样工作是在实测地层 ( 岩石 

地层和生物地层 ) 剖面后进行的。采样使用 

国产手提式气压钻机 , 钻取的岩心直径为 25 

mm, 长度为 20~50 mm, 用磁罗盘定向器定 

向取心。采样间距一般为 0.5~5 m, 但重要 

界面附近间距达到 5 cm。分析表明双湖地 

区海相侏罗系碳酸盐岩的天然剩磁普遍较 

高 , 一般达到 6.7×10 -3 ~3.8×10 -2 A/m。大多 

数样品在热退磁到 500~600℃ 区间时 , 剩磁 

133

衰减了 100%, 表明岩石中所含磁性载体力 

磁铁矿。系统研究表明双湖地区晚三叠世 

与早侏罗世之间缺失一个 NAUNESKI 反向 

极性带 , 界面的时间缺失量约为 2 Ma, 野外 

表现为不整合接触关系。中、下侏罗统之 

间为假整合接触关系 , 沉积间断时间约为 

320 ka。 

2008010518 

辽西朝阳地区含鸟化石层附近侏罗 — 白垩 

系磁性地层研究 = Magnetostratigraphy of 

the Jurassic-Cretaceous boundary near birdbearing 

beds in western Liaoning. ( 中文 ). 孙 

知明 ; 许坤 ; 马醒华 ; 梁鸿德 ; 杨天水 ; 杨振宇 ; 李 

荣辉 ; 李瑜 ; 赵越 . 地质学报 , 2002, 76(3): 317- 

324 

本文通过对辽西朝阳地区含鸟化石层附 

近侏罗 — 白垩系蓝旗组、土城子组、义县 

组地层共 1252 块古地磁样品的测试与分析 , 

建立了以上沉积地层的磁极性序列 , 发现蓝 

旗组、土城子组地层的磁极性序列具有频 

繁的正、反极性 , 而义县组则为单一正极性 , 

结合现有古生物和同位素年龄资料 , 对比国 

际中生代地磁极性年表 , 表明土城子组的磁 

极性序列相当于提塘期、基末里期、牛津 

期和卡洛期 , 其主体的地质时代应属晚侏罗 

世 (J 3 ), 土城子组底部的地质时代应属中侏罗 

世 (J 2 ); 并且根据义县组含鸟化石层以上层位 

的磁性地层研究结果 , 认为义县组合鸟化石 

的正极性带可与 M 16 正极性时相对应 , 义县 

组含鸟类化石层的时代应属早白垩世早期 , 

辽西白垩系 / 侏罗系界线很可能位于义县组 / 

土城子组之间。 

2008010519 

中国西藏南部喜马拉雅相的乐平统 = The 

Himalayan Lopingian Series (Late Permian) in 

southern Tibet, China. ( 中文 ). 沈树忠 ; 曹长群 ; 

王向东 ; 梅仕龙 ; 金玉玕 . 地质学报 , 2002, 

76(4): 454-461 

西藏南部二叠系色龙群、曲布日嘎组等 

“ 喜马拉雅相 ” 地层产有冈瓦纳区系的以 

Spiriferella rajah,Taeniothaerus densipustulatus,Neospirifer(Neospirifer)kubeiensis 

和 

Retimarginifera xizangensis 为典型代表的腕 

足动物群。其组成和演进层序与属于冈瓦 

纳大陆北缘的巴基斯坦盐岭的 Wargal 组上 

部和 Chhidru 组、克什米尔的 Zewan 组 , 印度 

斯区提 Kuling 页岩上部的 Gungri 组、尼泊尔 

西北部的 Senja 组和澳大利亚西部 Hardman 

组的很接近 ; 时代曾被归入瓜达鲁普世或乐 

平世早期等 , 分歧较大。近年来在盐岭等地 

发现这一冈瓦纳区系动物群明显高于乐平 

世下部牙形类 Clarkina dukouensis 带 , 并与菊 

石 Cyclolobus 和有孔虫 Colaniella 动物群共 

生。由此推定整个色龙群或曲布组和曲布 

日嘎组都应属于乐平统 , 它与上覆三叠系以 

牙形类化石 Hindeodus parvus 和菊石 

Otoceras 出现为界 , 代表冈瓦纳大陆北缘乐 

平世沉积的一个三级地层层序。层序以海 

进初期沉积的低水位体系域的曲布组石英 

砂岩为标志 , 其顶界则为比二叠系 - 三叠系界 

线略低的一个快速海进面。 

2008010520 

西藏羌塘阿木岗群硅质岩段时代归属 = The 

age of the Chert Member of the Amugang 

Group in Qiangtang,Tibet. ( 中文 ). 王国芝 ; 王 

成善 ; 吴山 . 中国地质 , 2002, 29(2): 139-142 

对阿木岗群硅质岩段与上覆和下伏地层 

的接触关系 , 灰岩砾石、灰岩夹层中所发现 

的生物化石及才玛尔错和绒马硅质岩中放 

射虫化石资料的对比研究表明 , 硅质岩段不 

属于基底地层 , 其时代相当于三叠纪 , 大致可 

与晚三叠世结扎群相对比。 

2008010521 

对江西晚白垩世赣州群茅店组的重新厘定 

= Revision of the Late Cretaceous Maodian 

Formation of the Ganzhou Group in Jiangxi 

Province. ( 中文 ). 衷存堤 ; 徐平 ; 肖晓林 ; 王迪 

文 ; 龙天 . 中国地质 , 2002, 29(2): 29/3=271- 

274 

根据 1∶ 5万区调最新成果资料 , 对《江西 

省岩石地层》中的赣州群茅店组进行了重 

新厘定 , 在原茅店组正层型剖面上 , 识别出了 

5 种不同性质的沉积界面 , 即沉积不整合界 

面、超覆不整合界面、平行不整合界面、 

相转变面、同相叠复面 , 从而将原茅店组划 

分为两个不同的组级岩石地层单位。按照 

岩石地层单位的命名原则 , 超覆不整合面之 

下的原茅店组中下部层位划归赣州群茅店 

组 , 其中发育的一套玄武岩 - 火山碎屑沉积岩 

组合单独划出 , 新建为陈坑火山岩段 ; 超覆不 

整合面之上的原茅店组上部层位的粗碎屑 

沉积岩 , 则划归晚白垩世灌溪群宏冈组。重 

新厘定的茅店组仅相当于原正层型茅店组 

的中、下部层位 , 且可细分为下段、陈坑火 

山岩段和上段。 

2008010522 

新疆塔里木盆地白垩纪 - 第三纪层序地层 

学研究 = A study of the Cretaceous-Tertiary 

sequence stratigraphy of Tarim Basin, Xinji- 

134

ang. ( 中文 ). 丁孝忠 ; 郭宪璞 ; 彭阳 ; 纪云龙 ; 李 

喜臣 ; 张韬 ; 刘丽军 ; 王易农 . 地球学报 - 中国地 

质科学院院报 , 2002, 23(3): 243-248 

通过对塔里木盆地西南坳陷区和东北坳 

陷区白垩纪 - 第三系典型剖面的层序地层 

学研究 , 结合地震和钻井资料的分析 , 划 

分出西南坳陷区 30 个三级层序 , 东北坳陷 

区 24 个三级层序 , 因其所处的构造位置和 

沉积环境不同 , 两坳陷区形成的三级层序 

并非一一对应 , 不能进行大区域的直接对 

比。而三级层序的有序叠置构成了二级超 

序及其体系域 , 基叠置方式包括进积组 

合、退积组织和加积组合。通过二级超层 

序的研究发现 , 两坳陷区白垩系 - 第三系 

( 中新统 ) 可划分为 4 个二组超层序 (SS1 

-SS4), 并可以等时对比 , 所反映的相对 

海平面变化周期也基本相同 , 并且与同受 

特提斯海水影响的西藏南部地区白垩 - 早 

第三纪沉积层序有海平面变化基本一致 , 

即西藏西南地区和塔里木盆地受特提斯构 

造和全球海平面变化的共同影响。从中新 

世开始 , 青藏高原快速隆升 , 塔里木盆地 

相对下降 , 造成了两地区层序类型及海平 

面变化速率的不同。 

2008010523 

西藏层序地层研究进展 = Advances in sequence 

stratigraphy of Tibet. ( 中文 ). 彭勇民 ; 

惠兰 ; 谭富文 ; 王全海 . 地球学报 - 中国地质科 

学院院报 , 2002, 23(3): 273-278 

迄今为止 , 西藏区内所开展的层序地层 

分析主要涉及到中生代的二级或三级层 

序。基于露头剖面的沉积相、古生物、磁 

性地层以及地质事件的综合研究 , 探讨了 

三叠纪、侏罗纪和白垩纪的层序地层模式 

及其形成机制。现今所取得的进展主要表 

现在 3 个方面 :1 初步建立了区内中生代 

层序地层年代格架 ;2 不同时代、不同类 

型盆地中的层序数量、结构与层序类型具 

有较大的差异 ;3 层序地层与磁性地层的 

结合研究 , 取得了重要的成果。未来区内 

的层序地层研究应在 3 个方面展开 ;1 高 

分辨率层序地层研究 , 树立株罗纪 - 第三 

纪海平面变化曲线 ;2 探索层序地层填图 

新方法 ;3 多岛弧造山模式和多机制的隆 

升模式等大陆动力学问题也是层序地层所 

遇到的新挑战。 

2008010524 

长江源地区中侏罗世巴通期层序地层 = A 

study on Bathonian sequence stratigraphy in 

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

盛贤才 ; 牛志军 . 华南地质与矿产 , 2002, (1): 

34-40 

长江源地区在侏罗纪巴通期发育一套稳 

定碳酸盐岩夹碎屑岩沉积 ( 布曲组 ), 其沉积 

环境经历了开阔海台地、台前缓坡、陆 

棚、近滨、陆棚、台前缓坡至开阔海台地 

等变化 , 于布曲组内部识别出三个 Ⅱ 型层序 

界面和四个不完整三级层序 , 在此基础上提 

出布曲组的顶底界面 ( 岩性界面 ) 可能不是一 

个等时面 , 而是穿时的 , 巴通期的相对海平面 

经历了下降、慢升快降、慢升慢降及慢降 

等变化。 

2008010525 

上泥盆统 “ 石梯组 ” 与侏罗系石梯组重名 = 

The Upper Devonian "Shiti Formation" should 

be renamed. ( 中文 ). 冯少南 ; 张淼 . 华南地质 

与矿产 , 2002, (1): 41-44 

王玉净等 1998 年撰写的 “ 广西钦州小董 - 

板城上古生代硅质岩相地层 ” , 新建了上泥 

盆统 “ 石梯组 ”, 该岩石地层单位与谢家荣、 

王植 1937 年在广西西湾创建的石梯系 ( 后 

更名石梯组 ) 重名。根据地层命名优先权 , 西 

湾侏罗系石梯组应予沿用 , 钦州板城上泥盆 

统 “ 石梯组 ” 应予废弃。钦州板城含有上泥 

盆统放射虫、牙形类的硅质岩与上覆含有 

下石炭统放射虫、牙形类的硅质岩不同 , 后 

者含有锰矿和赤铁矿 , 颜色较深 , 根据岩石地 

层学组的含义 , 将前者重新命名为桂南组。 

2008010526 

河南卢氏五里川盆地晚白垩世地层 = Late 

Cretaceous strata in Wulichuan basin,Henan 

Province. ( 中文 ). 朱广彬 ; 周世全 . 华南地质 

与矿产 , 2002, (4): 28-34 

位于东秦岭造山带核部的五里川盆地内 

的红层为一套具磨拉石建造特点的粗碎屑 

红色岩系。根据其中所含的恐龙蛋化石和 

同位素年龄资料以及少量孢粉、盆地发展 

演化史等综合分析 , 红层时代归属晚白垩世 

早期或中 - 早期较为合适。按照 “ 中国地层 

指南 ” 的规定 , 建议该红层使用朱阳关组一名 , 

停止使用马家村组、高沟组及三湾、桑 

坪、黄沙三组等名。 

2008010527 

贵州关岭中三叠统坡段组沉积特征及其形 

成环境 = Sedimentary characteristics and environments 

of the Poduan Formation of Middle 

Triassic in Guanling of Guizhou Province. 

135

( 中文 ). 范嘉松 ; 吴亚生 . 古地理学报 , 2002, 

4(1): 67-74 4 图版 . 

贵州中三叠世碳酸盐台地边缘的 “ 堤礁 ” 

向来受到人们的关注 , 并成为研究的热 

点。当前对台地边缘沉积的性质存在着不 

同的观点。某些人认为这些沉积是在浅水 

和扰动环境下形成的滩相沉积 ; 而另外一 

些研究者则仍坚持它们代表典型的礁相沉 

积 , 因为它含有丰富的造架生物 , 如六射 

珊瑚、苔藓虫、钙质海绵和龙介类等。在 

贵州中部关岭县扒子场出露了一套巨厚的 

和属于台地边缘的中三叠统。扒子场在关 

岭县城的东南 , 直距约 22 km。三叠系中 

下统沿着公路断面连续出露。中统包括安 

尼阶的坡段组及拉丁阶的垄头组和竹杆坡 

组。坡段组主要由砂砾屑 - 生屑颗粒岩组 

成 , 约占全剖面的 2/3。它们形成于水流激 

荡的滩相环境。其他岩石为骨屑 - 球粒粒泥 

岩和泥粒岩 , 约占全剖面的 1/3。根据该组 

的岩石结构、沉积构造和生物组分 , 坡段 

组代表由砂砾屑、生屑组成的粒屑滩 , 而 

非生物礁相沉积。仅在底部或下部出现少 

量的 Tubiphytes— 蓝细菌造礁骨架 , 组成局 

部的礁丘。 

2008010528 

塔里木盆地喀什凹陷侏罗纪古环境 = Paleoenvironments 

of the Jurassic of Kashi sag 

in Tarim Basin. ( 中文 ). 钟大康 ; 朱筱敏 ; 王贵 

文 ; 谢庆宾 . 古地理学报 , 2002, 4(4): 4=47-54 

通过对野外露头剖面的勘察采样和研 

究 , 从岩石的颜色、岩性、沉积构造、古 

生物化石以及地球化学等多项指标分析了 

喀什凹陷侏罗纪的古环境特征和演化。研 

究表明 : 早侏罗世莎里塔什组属干燥氧化 

环境下的冲积扇沉积 , 到康苏组时演化为 

潮湿气候条件下的河流沉积 ; 中侏罗世盆 

地南北出现差异 , 北部以淡水为主 , 而南 

部出现半咸水 - 咸水环境 , 古气候向半潮 

湿 - 半干燥演变 , 沉积相由三角洲前缘向 

深 - 半深湖再到滨浅湖沉积演化 ; 晚侏罗 

世盆地又演化为干燥 - 半干燥环境下的河 

流与冲积扇沉积。整个侏罗纪代表了一个 

水体由浅 - 深 - 浅、古气候由干燥 - 湿热 

- 干燥的演化过程。古水介质盐度基本上 

保持了陆相淡水湖体系 , 仅中侏罗世时期 

在南部表现为咸水环境。 

2008010529 

阿根廷内乌肯盆地下白垩统 Agrio 组 

Pilmatue 段生物相分析 = Biofacies analysis 

of the Pilmatue Member of the Agrio Formation, 

Lower Cretaceous, Neuqun Basin, Argentina.. 

( 其他 ). Lazo D G. 

Ameghiniana, 2007, 44(1): 73-89 

A biofacies analysis based on benthic macrofossils 

was carried out. The study unit is the 

Pilmatue Member of the Agrio Formation in 

three sections in the Neuquen Province. Six 

biofacies controlled by relative sea level 

changes, sedimentation rate, substrate consistency, 

oxygenation and salinity were recognised. 

The "Cucullaea-Mimachlamys- 

Steinmanella biofacies" is highly diverse and 

recorded in a shoreface environment characterized 

by a well-oxygenated soft sandy and 

patchy bioclastic substrate, reduced siliciclastic 

input, normal marine salinity, and warmtemperate 

waters. The "coral colonies biofacies" 

is associated with the former biofacies, 

but in a more shallow setting and probably 

temperatures above 16 degrees-18 degrees C. 

The "Cucullaea and Steinmanella biofacies" 

occurred in an open shelf environment characterized 

by low water energy, reduced siliciclastic 

input, firm muddy substrate, and normal 

marine conditions. The "Modiolus biofacies" 

also occurs on the shelf, but under low 

oxygenation. The "gregarious serpulids" and 

"gregarious oysters" biofacies correspond to 

an inner shelf setting characterized by an alternation 

of high and low water energy, low 

siliciclastic input, firm muddy substrate, welloxygenated 

bottom, and mixo-euhaline conditions. 

The "Cucullaea-Mimachlamys- 

Panopea" and "Cucullaea and Steinmanella" 

biofacies are related to changes of relative sea 

level in the scale of parasequences, while the 

"coral colonies", "Modiolus", "gregarious oysters", 

and "gregarious serpulids" respond to 

changes in the scale of sequences. 

2008010530 

西藏申扎县木纠错地区晚三叠世多布日组 

的发现及其地质意义 = The discovery of the 

Late Triassic Duoburi Formation in the Mujiucuo 

area,Shenzha County,Tibet and its geological 

significance. ( 中文 ). 张树岐 ; 曲永贵 ; 

郑春子 ; 王永胜 ; 冯德臣 . 吉林地质 , 2002, 

21(4): 9-14 

吉林地质调查院在开展西藏自治区 1∶25 

万多巴区幅区域地质调查时 , 在木纠错西的 

申扎县多布日一带发现一套陆相 — 海陆交 

互相 — 滨浅海相地层 , 并采集到了珊瑚化 

石、海参化石、植物化石、介形类化石、 

腹足化石、藻类化石和孢粉化石等。根据 

这些古生物化石确定该套地层为晚三叠世 

136

沉积。从而首次证明了冈底斯 — 腾冲区永 

珠蛇绿岩带以南存在晚三叠世地层。这一 

发现为我国三叠系的划分对比提供了重要 

的依据 , 并为古特提斯海的演化历史 , 古地理 

轮廓的确定以及青藏高原的形成演变历史 

提供了新的资料。 

2008010531 

松辽盆地徐家围子裂陷式盆地的层序发育 

特点 = Sequence characteristics of rifting basin 

of Xujiaweizi in Songliao Basin. ( 中文 ). 

赵国连 ; 何顺利 . 西北地质 , 2002, 35(1): 28- 

40 

关于层序地层学在陆相肖控条件下的适 

用性探讨一直在不断地进行着 , 尤其是陆 

相油气盆地占优势的中国 , 陆相层序地层 

学的研究已处于世界先进的行列。其中对 

松辽盆地层序地层的研究引人注目。层序 

地层学理论对于陆相盆地适用性问题的探 

讨 , 产生了众多层序地层学学派。笔者总 

结探讨了层序控制的基本因素因盆地类型 

的关系 , 在此基础上研究了断陷期层序地 

层发育特点。首次对晚侏罗世一早白垩世 

的松辽盆地徐家围子裂陷盆地阶段的地层 - 

火石岭组、沙河子组与营城组 , 进行了层 

序地层分析 , 对可容空间变化与充填情况 

进行了研究 , 划分了超层序 , 对其中的火 

岩地层、沉积岩地层分别进行了研究 , 并 

总结了火山作用与沉积作用的相互关系。 

从可容空间概念出发 , 把火山岩地层纳入 

层序框架 , 并对层序控制下的生储盖组合 

及油气勘探远景进行了评估。 

2008010532 

滇中鱼坝村组的建立及陆相侏罗系底界 = 

Establishment of the Yubacun Formation and 

the Lower Boundary of the continental Jurassic 

in central Yunnan. ( 中文 ). 庞其清 ; 方晓思 ; 

张子雄 ; 李永安 ; 李佩贤 ; 程政武 . 地质论 

评 , 2002, 48(1): 1-8 

滇中及相邻地区上三叠统舍资组含煤层 

下侏罗统冯家河组红层之间 , 连续沉积了 

一套杂色细碎屑岩过渡层。其分布稳定。 

该层所含化石及磁性地层特征表明其时代 

属早侏罗世。因此建立下侏罗统鱼坝村 

组 , 并确定该组底界为陆相侏罗系的底 

界。 

2008010533 

江西及广东北部中生代晚期地层层序和时 

代 - 兼论《江西省岩石地层》中存在的问题 

= Stratigraphical sequence and geochronology 

of the Late Mesozoic era in Jiangxi Province 

and northern Guangdong Province. ( 中文 ). 巫 

建华 ; 周维勋 ; 章邦桐 . 地质论评 , 2002, 48(1): 

44-53 

根据地层发育程度和沉积特征 , 以萍乡 - 

广丰溶断裂和三南 - 寻乌深断裂为界 , 江西 

及广东北部中生代晚期可划分为北、中、 

南三个地层区。根据不整合面和岩石组合 

特征 , 以群级岩石地层单位与火山旋回或 

沉积旋回相对应为原则 , 北区可划分出火 

把山群和圭峰群 , 中区可划分出武夷群、 

罗塘群或版石群和土峰群 , 南区可划分出 

余田群、版石群或罗塘群。根据岩性岩相 

特征 , 以组级岩石地层单位与复合岩相或 

沉积岩相相对应为原则 , 余田群可划分为 

迳组和菖蒲组 , 武夷群划分为双峰岭组、 

鹅湖岭组和石溪组 , 版石群划分为合水组 

和优胜组 , 罗塘群划分为白埠组、周田组 

和邓家组 , 火把山群划分为丘家组、天台 

山组、冷水坞组和周家店组 , 圭峰群划分 

为河口组、塘边组和莲荷组。根据同位素 

年龄数据和化石资料 , 余田群的地质时代 

属中侏罗世 ; 武夷群主体属晚侏罗世 , 顶 

部石溪组跨入早白垩世 ; 罗塘群或版石群 

属早白垩世晚期 - 晚白垩世早期 ; 火把山群 

属早白垩世 , 圭峰群属晚白垩世晚期。 

2008010534 

伊犁盆地南缘侏罗系高分辨率层序地层学 

研究 = Research for high resolution sequence 

stratigraphy of Jurassic on south margin in Ili 

basin. ( 中文 ). 田景春 ; 刘家铎 ; 孟万斌 ; 庹先国 ; 

袁智慧 . 成都理工大学学报 , 2002, 29(5): 

499-505 

以伊犁盆地南缘侏罗系为研究对象 , 运 

用高分辨率层序地层学理论详细分析了侏 

罗系短期基准面旋回、中期基准面旋回和 

长期基准面旋回的特征 , 在此基础上运用 

旋回等时对比原理 , 对不同钻井的基准面 

旋回进行了对比 , 建立了高分辨率层序对 

比格架。进而简述了储铀砂体在高分辨率 

层序地层格架中的分布特征。 

2008010535 

伊犁盆地南缘侏罗系地层学研究 = Study of 

Jurassic stratigraphy in the south margin of Ili 

Basin. ( 中文 ). 刘家铎 ; 孟万斌 . 成都理工大学 

学报 , 2002, 29(6): 650-655 

在伊犁盆地北缘和南缘下 - 中侏罗统沉 

积微相和岩石类型研究的基础上 , 对伊犁 

盆地北缘和南缘侏罗纪地层进行了详细对 

比 , 认为盆地南缘下一中侏罗统同样可以 

划分为八道湾组 , 三工河组和西山窑组 , 

137

并分别对应于水西沟群 I-Ⅷ 旋回 , 这一研 

究对于伊犁盆地基础地质研究和可地浸砂 

岩型铀矿床的勘探具有重要意义。 

2008010536 

库车坳陷侏罗经沉积环境和层序地层分析 

= Sequence stratigraphy and depositional environments 

of the Kuche depression. ( 中文 ). 

吴朝东 ; 林畅松 ; 申延平 ; 谢小建 ; 肖建新 ; 刘景 

彦 ; 史艳丽 . 沉积学报 , 2002, 20(3): 400-406 

通过对库车坳陷野外露头和钴井资料以 

及地震剖面的综合分析 , 对库车盆地侏罗 

纪沉积环境、层序划分进行了研究。库车 

盆地在侏罗纪时期为一非对称型坳陷型盆 

地 , 主要物源在盆地的北部。划分了 13 个 

三级层序 , 三个层序组 , 反映了三个大级 

别的旋回。最大湖侵期为阳霞组中上上 

部 , 与当时有一个明显的气候变热期相一 

致。沉积环境在侏罗纪早期为辫状河 - 辫 

状河三角洲环境、中期为曲流河 - 三角洲 

环境 , 后期为三角洲和浅湖环境 , 中期有 

短暂的侏罗世早期、晚期和最大湖侵和海 

泛的短暂时期 , 形成了厚层的烃源岩分 

布。库车坳陷侏罗系虽然砂体分布广泛 , 

厚度较大 , 然而由于陆相沉积环境的控 

制 , 非均质性较强。 

2008010537 

南盘江盆地早 — 中三叠世层序地层格架及 

相对海平面变化研究 = Sequence stratigraphy 

and relative sea-level changes from the 

early to the middle Triassic in the Nanpanjiang 

Basin. ( 中文 ). 梅冥相 ; 高金汉 ; 孟庆芬 ; 易 

定红 ; 李东海 . 现代地质 , 2002, 16(2): 137- 

146 

南盘江盆地的早 — 早三叠世地层中 , 沉 

积相形成复杂而有序的空间变化和时间变 

化。二叠纪与三叠纪之交的大规模台地淹 

没事件之后 , 三叠纪碳酸盐台地从缓坡型 

演化为镶嵌陆架型 ; 空间上 , 从连陆台地 

到浊积盆地相分异特别明显 , 而且在盆地 

中发育若干的孤立台地 , 特别是南宁和靖 

西一带 , 孤立台地上早叠世的鲕粒滩以及 

连陆台地边缘的礁滩相灰岩更是引人注 

目。尽管不同相带的三级沉积层序相序组 

构千差万变 , 并且它们的形成时限也不尽 

相同 , 但是由其所表征的相对海平面变化 

则具有大致的同步性 , 因此在早 — 中三叠 

世地层中可立南盘江盆地早 — 中三叠世的 

层序地层格架。 

2008010538 

安徽明光盆地第三系层序地层学分析 = 

Sequence stratigraphy of the Tertiary sediments 

in the Mingguang Basin of Anhui Province. 

( 中文 ). 吴跃东 ; 刘家云 ; 汪德华 . 现代地 

质 , 2002, 16(4): 374-381 

安徽明光盆地第三纪沉积物以陆相红色 

类磨拉石建造为主 , 晚期覆盖陆相火山岩 

建造 , 通过对陆相红色类磨拉石建造的分 

析表明其形成于冲积扇和扇前河湖环境 , 

在对明光盆地内各类陆相沉积建造的沉积 

环境 , 沉积相 , 陆相沉积体系域和地层层 

序界面的分析基础上 , 根据盆地的充填沉 

积序列划分出 5 个层序 ( 三级层序 ), 由 

于受到构造运动的影响 , 其层序发育皆不 

完整 , 在对其进行层序地层学分析的基础 

上 , 初步建立了明光盆地的地层格架。 

2008010539 

柴达木盆地西部红狮凹陷第三系下干柴沟 

组层序地层格架 = Sequence stratigraphic 

framework of the lower Ganchaigou Formation 

in Hongliuquan-Shizhigou area, western 

Qaidam Basin. ( 中文 ). 蒋宏忱 ; 于炳松 ; 王黎 

栋 ; 穆剑 ; 刘忠宝 . 现代地质 , 2002, 16(4): 382- 

388 

柴达木盆地西部红狮凹陷是青海油田公 

司的主要采油区 , 下第三系下干柴沟组是 

区内主要目的层段之一。以 Cross 的高分辨 

率层序地层学理论为指导。根据露头剖面 

和钻井资料 , 对区内下干柴沟组进行了详 

细的层序地层研究。共识别出 15 个三级层 

序 ,4 个超层序。在连井剖面的层序地层对 

比基础上 , 建立了该区的地层格架 , 并揭 

示出这 4 个超层序中上升半旋回陷下第三 

系有利储集岩的分布区 , 最大湖泛期密集 

段暗色泥岩是该区主力烃源岩的分布区。 

2008010540 

陆相盆地中的海侵层序特征 : 中欧盆地三 

叠系与松辽盆地白垩系对比研究 = The 

characters of transgressive sequence of terrigenous 

basin: correlation between the triassic 

in Centraleuropen basin and the cretaceous in 

Songliao basin of China. ( 中文 ). 王璞 

珺 ;Schneider Werner;Mattern Frank; 边伟华 . 

矿物岩石 , 2001, 22(2): 47-53 

中欧盆地三叠系是典型的海陆过渡相沉 

积 , 松辽盆地白垩系是含有海侵事件记录 

的陆相河湖盆地 . 两盆地的共同特点是 :1 

大陆克拉通上长期发育的大型坳陷盆地 ; 

2 靠近古大洋和 ( 或 ) 有向海通道 ;3 主要由 

互层状泥岩、粉砂岩、碳酸盐岩和膏盐层 

138

组成 ;4 无典型海相化石 , 可能发育有半 

咸水和 ( 或 ) 高盐度生物 ;5 海侵层中自生矿 

物的 δ 34 S, δ 13 C,δ 18 O 同位素比值及介质盐度 

指数 (Sr/Ba)、碱度指数 (Ca+Mg)/(Si+Al)、 

还原性指数 (Zn+Ni)/Ga、硫沉积通量指数 

( 归一化硫含量 ) 等显著高于相邻层位背 

景值。 

2008010541 

试论黔西北及邻区非海相三叠系 / 侏罗系 

界线 = Initial discussion on the boundary of 

the Triassic-Jurassic of the non-marine facies 

in Northwest Guizhou and its adjacent areas. 

( 中文 ). 王立亭 . 贵州地质 , 2002, 19(3): 175- 

178,162 

根据黔西北及邻区二桥组中双壳类的垂 

直分布 , 可将其分为两个组合 ; 下部 

Indosinion-Permophorus 组合及上部 

Qiyangia-Hunanella 组合。前一组合的时代 

为晚三叠世瑞替克期 , 后一组合的时代则 

为早侏罗世早中期。该区非海相三叠系 / 

侏罗系的界线应划在上述两个组合之间。 

故该区二桥组实为跨三叠系与侏罗系的岩 

石地层单位。 

2008010542 

南海及周边部分地区特提斯构造遗迹 : 问 

题与思考 = Reviews on Tethyan trace in 

South China Sea and some adjacent regions. 

( 中文 ). 颜佳新 ; 周蒂 . 热带海洋学报 , 2002, 

21(2): 43-49 

对全球二叠纪 — 三叠纪古气候特征的研 

究表明 , 东特提斯地区晚三叠世古气候标 

志具有带状分布的特征。北巴拉望地块卡 

拉棉群岛的晚三叠世沉积中发育反映较干 

燥古气候特征的鲕状灰岩 , 因此在古气候 

特征方面 , 北巴拉望地块晚三叠世地层不 

能与华南和印支地块同期地层对比 , 而应 

该与印度地块北缘喜马拉雅地区 ( 向西 ) 

和琉球群岛 ( 向东 ) 对比。根据该古气候 

分析 , 北巴拉望地块在晚三叠世时应该位 

于南部亚热带较干燥气候带内 , 其晚三叠 

世的古地理位置比钱支地块更靠南。对南 

海及南海周边部分地区特提斯构造遗迹的 

研究 , 将有助于深入了解南海北部陆缘区 

相关构造带的性质及正确恢复南海扩张之 

前该区的地质发展历史。南海北部陆缘区 

也是研究解决特提斯构造向东延伸问题以 

及特提斯构造 - 太平洋构造时空转化问题的 

关键地区。 

2008010543 

台西南盆地和北港隆起的中生界及其沉积 

环境 = Mesozoic strata and sedimentary environment 

is SW Taiwan basin of NE South 

China Sea and Peikang high of western Taiwan. 

( 中文 ). 周蒂 . 热带海洋学报 , 2002, 

21(2): 50-57 

我国南海海域广泛存在中生代沉积地 

层 , 在南海寻找中生界油气藏潜力极大。 

台西南盆地和北港隆起有数十口井钻遇中 

生界 , 经过详细生物地层学工作确定了下 

白垩统 ( 阿普特阶和下阿尔必阶 ) 和侏罗 

系 () 两套中生代地层 , 是迄今南海北 

部中生界地层研究最为深入的地区 , 可作 

为对比的样板。介绍了台西南盆地和台湾 

西部中生界的岩性、岩相和生物地层学特 

征 , 指出晚侏罗世 () 与早白垩世之间 

沉积环境发生了显著变化 , 台西南盆地由 

深海至半深海变为内陆 , 而北港隆起由内 

陆变为海陆交互和浅海环境。 

2008010544 

鉴别印度古吉拉特卡恰恰中生代 Kuar Bet 

层的时代 : 古植物和孢粉组合的重新研究 

= Resolving the age of the Mesozoic Kuar Bet 

Beds (Kachchh, Gujarat, India): A reinvestigation 

of palaeobotanical and palynological assemblages. 

( 英文 ). Jana B N; Hilton J. Journal 

of Asian Earth Sciences, 2007, 30(3-4): 

457-463 

Within the Mesozoic sedimentary sequences 

of India the age of the Kuar Bet Beds 

in Kachchh (Gujarat Province) has been hotly 

contested, with faunal evidence suggesting a 

Bathonian (Middle Jurassic) age, based on 

ammonite and foraminiferal occurrences, and 

palaeobotanical evidence suggesting an Early 

Cretaceous age, based on the presence of the 

index fossil Onychiopsis sp. cf. psilotoides 

(Stokes and Webb) Ward. Previously reported 

palynological evidence has documented numerous 

angiosperm pollen taxa, lending further 

support to an Early Cretaceous age. The 

present paper reinvestigates the palaeobotanical 

and palynological assemblages of the Kuar 

Bet Beds, and discounts previous identifications 

of Onychiopsis, considering these 

specimens to represent a new species of the 

genus Coniopteris, Coniopteris kuarbetensis 

sp. nov. The plant macrofossil assemblage 

also contains ovulate scales of Araucarites 

Presl and rooting organs. Palynological preparations 

revealed a diverse assemblage that includes 

Sphagnumsporites, Cyathidites, Dictyophyllidites, 

Todisporites, Concavissimis- 

139

porites, Klukisporites, Densoisporites, Callialasporites 

(two sp.), Alisporites spp., Podocarpidites, 

Araucariacites and Ginkgocycadophytus, 

all of which are long-ranging Mesozoic 

forms that occur in both Jurassic and Cretaceous 

sediments. Angiosperm pollen has not 

been observed, and the angiosperm grains reported 

by Mathur are here regarded as contaminants, 

introduced during the laboratory 

treatment of rock samples. Refuting the presence 

of Onychiopsis and of angiosperm pollen 

from the Kuar Bet Beds discounts an Early 

Cretaceous age, with the plant fossils and palynological 

assemblage being more consistent 

with a Middle Jurassic age, in general agreement 

with faunal data. However, the precise 

position within the Middle Jurassic remains 

uncertain with palaeobotanical and palynological 

results being most comparable with 

a late Middle Jurassic (Bathonian or Callovian) 

age while faunal evidence supports an early 

Middle Jurassic (Bajocian) age. 

2008010545 

土耳其西北部宗古尔达克巴雷姆阶 - 阿普特 

阶碳酸盐 - 硅质碎屑岩混合的内陆台的旋回 

地层和层序界线 = Cyclostratigraphy and 

sequence boundaries of inner platform mixed 

carbonate–siliciclastic successions (Barremian–Aptian) 

(Zonguldak, NW Turkey). ( 英 

文 ). Yılmaz I O; Altıner D. Journal of Asian 


Barremian–Aptian shallow marine mixed 

carbonate–siliciclastic successions of the 

Zonguldak area (NW Turkey) have been studied 

in detail along three measured stratigraphic 

sections. Field and laboratory analysis 

of microfacies and sedimentary structures 

have demonstrated that sections are composed 

of meter-scale shallowing-upward cycles. 

Cyclicity of shallow water mixed carbonate– 

siliciclastic successions are generally observed 

in the form of alternating sandstone/siltstone 

or sandy limestone and limestone. A prominent 

level of charophyte packstone within the 

successions of Zonguldak and Kozlu is interpreted 

as a sequence boundary. In the Çengellidere 

section, cyclicity is generally represented 

by an alternation of sandstone/conglomerate 

and bioclastic limestone. 

The first level of conglomerate within the section 

is interpreted as a sequence boundary. 

Smaller-scale cyclic arrangements are also 

recorded within meter-scale cycles. 4th-, 5thand 

6th-order cycles are superimposed and 

create a hierarchical stacking. However, 6thorder 

cycles present a relatively random distribution 

and termed as episodic. Thickness 

variation of cycles along the section and frequency 

of sand and/or silt rich cycle types are 

used to interpret systems tracts within the sequences. 

2008010546 

准噶尔盆地车排子地区侏罗系层序地层格 

架 = On Jurassic sequential framework of 

Chepaizi area in Junggar Basin. ( 中文 ). 李天 

明 ; 支东明 ; 靳军 . 新疆石油地质 , 2002, 23(4): 

286-289 

在前人对准噶尔盆地全盆地或局部层序 

地层大量研究成果的基础上 , 重点对盆地西 

北缘侏罗系地层格架特征开展了深入、细 

致的解剖和刻划 , 建立了层序地层格架 , 首次 

对车排子地区侏罗系层序及体系域界面特 

征进行了描述 , 并结合钻探井资料 , 划分了有 

利的沉积相带 , 对盆地侏罗系隐蔽型圈闭和 

油气藏的勘探提供了一种思路和方法。 

2008010547 

吐哈盆地西南部侏罗系时代划分 = Division 

of Jurassic strata in southwestern part of Turpan-Hami 

Basin. ( 中文 ). 杨殿忠 . 新疆石油地 

质 , 2002, 23(5): 385-389 

研究了采自吐哈盆地西南部早、中侏罗 

世的植物化石 , 在鉴定其种属的基础上 , 结合 

岩石地层学和层序地层学方法 , 描述了早、 

中侏罗世的植物组合特征 , 对其地层时代进 

行了新的厘定 , 提出了新的地层划分方案。 

新的划分方案不同于前人的划分结果 , 新方 

案一方面依据了新采集的植物化石资料 , 同 

时考虑到了野外实际工作的可操作性。此 

外 , 还提出了根据煤层发育程度、生物化石 

群、不整合面和岩性等特征 , 识别标志层的 

方法。 

2008010548 

准噶尔芦草沟组与黄山街组的古气候条件 

= Paleoclimatic conditions of Loucaogou and 

Huangshanjie Formations in Junggar. ( 中文 ). 

吴绍祖 ; 屈迅 ; 李强 . 新疆地质 , 2002, 20(3): 

183-186 

准噶尔中二叠统芦草沟组无论是从岩性 

还是所含古生物 , 均表明形成于持续炎热 

的气候条件之下 , 当时由于准噶尔古板块 

与塔里木古板块的拼合造山 , 造成准噶尔 

周缘火山强烈喷发和自欧洲东移的干旱炎 

热气流对准噶尔均有明显的影响。上三叠 

统黄山街组形成时干旱气候缓解 , 降水量 

增加 , 该组沉积物反映出温暖的亚热带气 

140

候特征。因此 , 从成油的古气候条件来 

说 , 芦草沟组要优于黄山街组。 

2008010549 

鄂尔多斯东北部太原组上部灰岩段高分辨 

层序地层分析 = High-resolution sequence 

analysis on Limestone Member, upper Taiyuan 

Formationb, northeastern Ordos. ( 中文 ). 

姜烨 ; 李宝芳 . 煤田地质与勘探 , 2002, 30(3): 

5-8 

根据对露头、测井和岩心资料的垂向分 

析和横向对比 , 结合古生物化石资料 , 在 

识别关键性界面的基础上 , 对鄂尔多斯东 

北部下二叠统太原组上部灰岩段建立了高 

分辨层序地层格架 , 划分出 5 个三级层 

序。研究层段为有陆源碎屑混入的碳酸盐 

缓坡沉积 , 形成于华北晚古生代最大海侵 

阶段。各层序分别由低位体系域的下切谷 

充填沉积的砂岩、砂砾岩 , 海侵体系的灰 

岩、泥灰岩、泥岩、煤和高位体系域的碎 

屑岩和煤组成。区内厚达数十米的桥头砂 

岩主要由几个层序低位域下切河谷充填沉 

积叠置而成。通过编制的各层序海侵域灰 

岩的厚度和分布图 , 证实层序 3、4 沉积期 

海侵范围最大。早二叠世早期海侵来自东 

南和西南两个方向。 

新生界 

2008010550 

船帆洞旧石器遗址洞穴形成过程与地层划 

分 = Formation and stratigraphy of the Chuanfan 

Cave. ( 中文 ). 李建军范雪春 . 人类学学 

报 , 2006, 25(2): 153-160 

本文根据最近发掘所获资料 , 对万寿岩山 

船帆洞旧石器时代晚期遗址洞穴的形成过 

程、洞内地层划分以及与洞外沉积物关系 

等问题进行初步探讨 . 提出 : 船帆洞洞穴的发 

育明显与区域性断裂及岩体的剪切节理有 

关 ; 洞内经历数次堆积和冲刷 ; 依岩性、地层 

关系和哺乳动物化石组合 , 洞内堆积物可分 

为 Ⅰ ( 中更新世晚期 )、 Ⅱ ( 晚更新世早期 )、 

Ⅲ ( 晚更新世晚期 ) 和 Ⅳ ( 全新世 )4 个地层单 

元。 

2008010551 

西藏纳木错第四纪湖相地层划分及纳木错 

群的建立 = Division of Quaternary lacustrine 

strata in the Nam Co area and establishment of 

the Nam Co Groupin Tibet. ( 中文 ). 朱大岗 ; 赵 

希涛 ; 孟宪刚 ; 吴中海 ; 邵兆刚 ; 马志邦 ; 冯向阳 ; 

吴珍汉 ; 王建平 ; 杨超斌 . 地质通报 , 2002, 

21(11): 708-716 

第四纪湖相地层剖面实测和水准仪测量 

表明 , 在西藏纳木错沿岸 , 发育有拔湖 48m 以 

下的 6 级湖岸阶地和拔湖 48m 以上最高至 

139.2m 的高位湖相沉积。纳木错湖相或湖 

滨相沉积的铀系等时线年龄测定结果表明 , 

高位湖相沉积形成于晚更新世早期 , 第六至 

第三级阶地则分别形成于晚更新世中期至 

晚期。 14 C 法测年表明 , 第二和第一级阶地的 

形成时间介于 13820~2350 年间 , 属全新 

世。根据沉积相、岩相组合等特征 , 并结合 

同位素测年、微体古生物鉴定等资料 , 将该 

套地层命名为纳木错群 , 由上更新统干玛弄 

组和全新统扎弄淌组组成。 

2008010552 

汤原断陷古近系层序地层及沉积体系分析 

= Characters of Paleogene sequence stratigraphy 

and its sedimentary system in Tangyuan 

fault depression. ( 中文 ). 柳蓉 ; 刘招君 ; 杨建国 ; 

王世辉 . 世界地质 , 2006, 25(4): 367-372 

根据层序地层学的基本原理 , 综合利用露 

头、钻井、测井和地震等资料 , 建立汤原断 

陷古近系层序地层格架 , 识别出 2 个超层 

序、11 个三级层序。运用体系域四分法在 

断陷两侧三级层序内同一体系域内识别出 

了相近的沉积体系。汤原断陷古近系主要 

发育扇三角洲 - 湖底扇、扇三角洲 - 半深湖、 

扇三角洲 - 湖底扇 - 半深湖、扇三角洲 - 滨浅 

湖 - 半深湖和扇三角洲 - 滨浅湖体系。 

2008010553 

西藏阿里札达盆地早更新世早期沉积及其 

古气候与古环境变化 = Early Pleistocene 

deposits and paleoclimatic and paleoenvironmental 

changes in the Zanda basin, Ngari area, 

Tibet. ( 中文 ). 朱大岗 ; 孟宪刚 ; 邵兆刚 ; 杨朝斌 ; 

韩建恩 ; 余佳 ; 孟庆伟 ; 吕荣平 . 中国地 

质 , 2006, 33(6): 1276-1284 

综合分析了西藏阿里札达盆地早更新 

世早期的多种与气候环境变化密切相关的 

地质记录 , 结果表明该区早更新世早期的沉 

积可划分为 3 种不同的沉积相和 4 个岩性 

段 ; 古气候与古环境变化可划分为 4 个阶 

段 :(1)2.68-2.45 Ma。为冲洪积相沉积。冻融 

褶皱开始出现 , 植被以乔木为主 , 主要为松、 

藜、蒿 , 属山地寒温气候 ;(2)2.45-2.11 Ma, 为 

冲洪积相 , 地层中冻融褶皱多呈扭曲状 , 草本 

植物迅速上升 , 显示出灌木草原气候特征 , 气 

候变得凉爽干燥 ;(3)2.11-1.49 Ma, 沉积相为 

冲洪积相 - 冰缘沉积相 , 以冰缘沉积相为主 , 

冻融褶皱层开始增多 , 出现了喜凉的介形类 

化石。草本植物数量和种类达到最大 , 灌木也 

141

相对增加 , 显示气候进一步趋于干 

旱 ;(4)1.49-1.36 Ma, 为冰湖沉积相。地层中普 

遍出现冻融褶皱 , 喜凉的介形类化石丰度很 

高 , 草本植物有小幅下降 , 但蕨类植物增加幅 

度较大 , 显示了干冷草原气候特征。气候干旱 

寒冷。 

2008010554 

关中盆地西部黄土台塬全新世气候事件研 

究 = Holocene climatic events on the loess 

tableland in the western Guanzhong Basin,China. 

( 中文 ). 黄春长 ; 庞奖励 ; 黄萍 ; 侯春 

红 ; 韩宇平 . 干旱区地理 , 2002, 25(1): 10-15 

通过对陕西歧山黄土剖面地层学和土壤 

学研究 , 磁化率、全铁、粒度、 

CaCO 3 和 TOC 测定分析 , 发现在全新世的全 

球性 “ 大暖期 ” 即将到来之前 , 黄土台塬面有 

洪水发生。在全新世大暖期当中 , 季风气候 

有明显的波动变化。尤其是在 6 000a BP 前 

后季风气候转折 , 形成了 6 000~5 000a BP 

显著的干旱阶段。这使得全新世大暖期分 

裂成为两个主要的温暖湿润阶段。各项气 

候代用指标显示 8 500~6 000a BP 是大暖期 

中最为温暖湿润的时期。在大约 310 0aBP 

季风格局发生变化 , 气候向着干旱化发展 , 全 

新世的成壤期为黄土堆积期所取代。这些 

事实对于我们客观地评价半湿润 — 半干旱 

地区的季风气候对于全球变化的响应规律 

具有重要的科学意义。 

2008010555 

甘青地区中晚全新世植被变化与人类活动 

= Study on the relationship between the vegetation 

change and the human activities in the 

Gansu-Qinghai region during the period from 

mid-to Late-Holocene. ( 中文 ). 安成邦 ; 陈发 

虎 ; 冯兆东 . 干旱区地理 , 2002, 25(2): 160- 

164 

史前时期人类对环境的影响是近几年来 

国际研究的热点。在甘青地区 , 全新世的孢 

粉资料比较多。但在中晚全新世 , 该区人类 

对环境的影响作用及其程度仍不清楚 , 许多 

孢粉分析资料中并没有充分考虑人类活动 

的影响。本文选取孢粉分辨率较高、代表 

性较好的青海湖、兰州、秦安大地湾三地 

的资料 , 着重研究了其中乔木成分的变化。 

分析发现 , 孢粉组合中乔木成分的变化与气 

候变化的趋势并不一致。通过对考古及历 

史资料的分析 , 笔者认为 , 该区的植被很早就 

受到人类活动的影响。自全新世中期 , 本区 

植被中的乔木成分波动下降。 5 000 - 3 

000a BP 期间 , 史前农业对植被的影响较 

大。 3 000 - 2 000a BP 期间 , 植被略有恢 

复。 2 000a BP 以后 , 人为影响加剧 , 植被中 

乔木成分迅速下降。研究者认为 , 依赖孢粉 

资料重建中晚全新世的气候变化历史应当 

慎重。 

2008010556 

柴达木盆地七个泉组和第四系 — 新近系的 

分界 = Qigequan Formation and Quaternary- 

Neogene boundary in Qaidam Basin. ( 中文 ). 

孙镇城 ; 乔子真 ; 景明昌 ; 张海泉 ; 孙乃达 ; 路艳 

丽 ; 王洪江 . 石油与天然气地质 , 2006, 27(3): 

422-431 

柴达木盆地东南部三湖坳陷 , 已发现 3 个 

上新统 - 第四系七个泉组气源岩的气田。把 

三湖坳陷七个泉组底界当成第四系与新近 

系的分界是一个误解。基于测井、地震地 

层和磁性生物地层的研究 , 三湖坳陷七个泉 

组底的年龄为 2.80 Ma, 位于涩北新深 1 井 1 

747 m。柴达木盆地第四系与新近系分界 , 

在许多论文中 , 有 3 种不同观点 :1 奥杜威 

末 ,1.67 Ma(1.80 Ma), 位于涩中 6 井 710 m, 

即测井标准层 K3 以上 19 m;2 松山与高斯 

分界 ,2.48 Ma(2.60 Ma), 位于涩深 1 井 1 460 

m, 即 K10 以下 37 m;3 马默思末 ,3.05 Ma, 位 

于达参 1 井 2 779 m。上述 3 个分界数据中 

无一与七个泉组底界对应。距今约 1.80 M 

a 的第四系与新近系分界定义已被国际地层 

委员会 1998 年投票通过 , 并于 1999 年经国 

际地科联批准。因此 , 依此定义来看 , 三湖坳 

陷大部分气源岩是晚新近纪 - 早第四纪的沉 

积 , 尤其是晚新近纪上新世。在柴达木盆地 

油气勘探开发研究中 , 作者建议最好使用地 

层单位名称七个泉组 , 而不用符号 Q 1+2 。连 

接地震反射 T 0 界面 ( 测井标准层 K 13 ) 和盆地 

边缘有局部不整合的七个泉组底界的对比 , 

对于研究构造运动、成气和成藏是很有用 

的。作为七个泉组底界 , 地震反射界面 T 0 

的对比 , 在柴达木盆地三湖坳陷中央具有 

实用性、等时性和可操作性等特点。 

2008010557 

北极 - 第三纪成分在喜马拉雅 - 横断山的发展 

及演化 = Evolution of Arctic-Tertiary flora in 

Himalayan-Hengduan Mountains. ( 中文 ). 孙 

航 . 云南植物研究 , 2002, 24(6): 671-688 

通过古植物学及古地史资料 , 论述了北极 

地区在第三纪早期气候变迁对喜马拉雅 - 横 

断山地区植物区系形成的影响 , 并通过一些 

142

喜马拉雅 - 横断山地区的特征类群 : 杜鹃属 , 

槭树属 , 柳属 , 桦木属和桤木属以及一些草本 

类群虎耳草科的落新妇族 , 金腰属和虎耳草 

属 , 忍冬科的莛子镳属的分布式样和起源分 

化的分析 , 说明了喜马拉雅 - 横断山区系中有 

相当一部分是这些北方起源的 , 北极 - 第三纪 

成分迁移是现代喜马拉雅 - 横断山植物区系 

成分的一个重要来源。并且讨论了喜马拉 

雅 - 横断山植物区系同北方植物区系可能的 

迁移路线 , 指出西南 - 秦岭 - 东北通道即西南 

沿四川盆地经秦岭和黄河至东北和西伯利 

亚和 “ 中亚高地通道 ” 即向西经帕米尔高原 

同北方交流 , 向东经西南 - 秦岭 - 东北通道迁 

移交流是喜马拉雅 - 横断山植物区系成分同 

北方交流的主要路线。由于第四纪冰期间 

冰期反复作用 , 各类成分在该地区保存、汇 

集、分化发展 , 使得该喜马拉雅 - 横断山地区 

成了北极 - 第三纪中心消失以后 , 在近代形成 

的温带和高山植物区系新的发展和分化中 

心。 

2008010558 

西藏岗巴古新世地层及构造作用的影响 = 

Palaeocene strata in Gamba, Tibet and influence 

of tectonism. ( 中文 ). 万晓樵 ; 梁定益 ; 李 

国彪 . 地质学报 , 2002, 76(2): 155-162 

西藏岗巴地区出露有完整的晚白垩世至 

古近纪地层 , 地层中化石丰富 , 根据化石研究 

准确地进行了地层时代的划分。本文认为 

该区白垩系 — 古近系界线位于宗山组和基 

堵拉组之间 , 以底栖大有孔虫 Orbitoides- 

Omphalocyclus 动物群的消亡和 Rotalia- 

Smoutina-Lockhartia 动物群的始现为标志。 

界线上下岩层为假整合接触 , 期间有一短暂 

的暴露面。古新世的砂砾岩直接覆于晚白 

垩世的陆棚碳酸盐岩沉积之上 , 沉积的重大 

转变代表一次构造运动。印度大陆北缘与 

冈底斯南缘直至白垩纪末均具有明显的浅 

海生物地理分区现象 , 期间被深海盆地所阻 

隔。古新世开始浅海相动物群在该地显示 

同一生物地理区系特征 , 说明两大陆间深水 

盆地的阻隔已消失 , 南北生物地理区同归于 

一残留海盆。沉积类型转变和地层古生物 

特征为印度 — 亚洲板块的起始碰撞时间研 

究提供了基础资料。据此推测大陆早期碰 

撞发生在白垩系 — 古近系的界线时期 ( 约 65 

Ma)。古新世中 — 晚期碳酸盐台地遭受不断 

的挤压与变形 , 进一步说明大陆的碰撞在古 

新世之初就已发生。沉积地层的破碎变形 

和滑塌堆积是持续碰撞与挤压的结果。 

2008010559 

塔里木盆地西部地区新近纪地层及古地理 

特征 = Neogene stratigraphy and palaeogeography 

in the western Tarim Basin. ( 中文 ). 

郝诒纯 ; 关绍曾 ; 叶留生 ; 黄有元 ; 周永昌 ; 关世 

桥 . 地质学报 , 2002, 76(3): 289-298 

渐新世末 , 印度板块与欧亚板块汇聚碰撞 

的 “ 远程效应 ” 结束了塔里木盆地与古地中 

海连通的历史 , 进入了陆盆发展阶段。在塔 

里木盆地西部地区接受了新近纪 ( 晚第三纪 ) 

以河流 — 湖泊相为主的巨厚陆相沉积。上 

第三系可划分为一群四组 , 由下而上为中新 

统乌恰群 (N 1 wq), 包括克孜洛依组 (N 1 k)、安 

居安组 (N 1 a) 和帕卡布拉克组 (N 1 p), 以及上新 

统阿图什组 (N 2 a)。岩性以碎屑岩为主夹蒸 

发岩 , 变化大 , 最大厚度达 6050m。文中特别 

对克孜洛依组的时代归属进行论述 , 根据其 

所含生物群的面貌 , 确定其时代为中新世早 

期。依据野外观察和沉积物特征的分析 , 在 

盆地中对比了乌恰群各组的地层 , 并对中新 

世各组沉积时期和上新世的沉积相特征进 

行了全面系统的阐述 , 绘制出中新世不同沉 

积时期的古地理图。 

2008010560 

塔里木盆地中新生代海侵和海相地层研究 

的新进展 = New progress in the study of marine 

transgressional events and marine strata 

of the Meso-Cenozoic in the Tarim Basin. ( 中 

文 ). 郭宪璞 ; 丁孝忠 ; 何希贤 ; 李汉敏 ; 苏新 ; 彭 

阳 . 地质学报 , 2002, 76(3): 299-307 

中新生代海侵是塔里木盆地地质发展史 

上的重要事件之一。通过对新近发现的古 

生物化石和海相地层资料研究 , 本文提出了 

早白垩世、晚白垩世、古近纪的海侵范围 

的新认识。同时 , 依据露头和钻井资料提出 

了中新世海水分布的新范围。这些新成果 

对厘定塔里木盆地中新生代地层时代、建 

立整个盆地中新生代地层格架和油气远景 

分析具有重要意义。 

2008010561 

杭嘉湖平原第四纪地层高精度对比方法研 

究 = High-resolution stratigraphic correlation 

method of the Quaternary in the Hangzhou- 

Jiaxing-Huzhou plain. ( 中文 ). 陈忠大 ; 覃兆松 ; 

梁河 ; 张素君 ; 廖福源 ; 彭振宇 . 中国地 

质 , 2002, 29(2): 275-280 

通过标准孔古气候旋回宏观识别标志的 

研究 , 并运用高分辨率层序地层理论 , 解决了 

杭嘉湖平原第四纪地层划分和 200 余个钻 

孔的等时对比问题 , 在此基础上制作了高精 

143

度对比的剖面图及准瞬时岩相古地理图 , 为 

研究杭嘉湖平原第四纪地层划分、古地貌 

变迁提供了更为精确的资料。运用 “ 基准面 

旋回 ” 作为层序地层的划分依据 , 以古土壤层 

及其可与之对比的暴露面和河流冲刷面为 

边界 , 将平原第四系划分为 9 个亚层序 , 并发 

现亚层序与气候旋回呈耦合关系。 

2008010562 

廊固凹陷古近系层序地层特征及油气储集 

规律探讨 = Paleogene sequence stratigraphy 

and oil-gas accumulation in the Langgu subd 

epression. ( 中文 ). 董国臣 ; 孙景民 ; 张守鹏 ; 梁 

冬梅 . 中国地质 , 2002, 29(4): 397-400 

笔者通过对钻孔岩心资料描述和对比 , 结 

合具有系统性、连续性和区域分布特点的 

地震资料 , 运用层序地层学和地震地层学基 

本原理对凹陷区内古近系进行了研究 , 划分 

了地层层序 , 揭示层序地层构造格架 , 探讨了 

区域沉积格架特征及其对油气成生、储集 

的控制作用。 

2008010563 

藏南岗巴 — 定日地区始新世化石碳酸盐岩 

微相与沉积环境 = Eocene fossil carbonate 

microfacies and sedimentary environment in 

Gangba-Tingri,southern Tibet. ( 中文 ). 李国彪 ; 

万晓樵 ; 其和日格 ; 梁定益 ; 刘文灿 . 中国地 

质 , 2002, 29(4): 401-406 

藏南岗巴 — 定日地区发育着西藏最晚期 

的海相沉积 , 对这套海相沉积的研究 , 可提供 

关于西藏特提斯演化晚期的良好信息。本 

文对岗巴 — 定日地区始新世遮普惹组的化 

石碳酸盐岩微相进行了较为详细的分析和 

研究 , 参考 Wilson(1975) 的标准微相 , 初步识 

别出 10 种微相和 5 种生物相类型。同时对 

遮普惹组中的砾状灰岩的成因机制作了有 

益的探讨 , 它完全是由沉积作用而成 ; 胶结物 

不是源于物质的重新分配 , 而是台地边缘斜 

坡的等深流沉积。以此为基础 , 对西藏特提 

斯晚期沉积环境的演变进行了较为详细的 

分析。笔者认为 : 岗巴 — 定日盆地在始新世 

Ypresian—Lutetian 早期接受海侵 ; 自 

Lutetian 晚期开始 , 区内总体处于一种海退 

环境 , 但由于受板块碰撞作用的影响 , 岗巴地 

区在 Lutetian 晚期 —Bartonian 晚期成为一 

深水坳陷盆地 ; 至 Priabonian 早期 , 海水完全 

退出本区。 

2008010564 

羌塘盆地查郎拉地区中新生代古气候演化 

初探 = A preliminary study of the Mesozoic- 

Cenozoic palaeoclimate evolution in Chalangla 

areas, Qiangtang Baisn, Northern Tibet. 

( 中文 ). 蔚远江 ; 杨晓萍 ; 雷宇 ; 张洪 ; 陆万雨 . 

地球学报 - 中国地质科学院院报 , 2002, 23(1): 

55-62 

通过野外遥感调研和收集整理大量剖面 

及路线地质资料 , 讨论了羌塘盆地查郎拉 

地区气候常量元素、变价元素及徽量元素 

物征 ; 气候沉积物及其分布特征 , 给合已 

有的气候指示性古生物化石及岩相古地理 

资料 , 首次系统地演绎了本区中新生代古 

气候特征及其变迁演化史。划分出 8 个气 

候旋回 , 指出晚三叠世为热带亚热带温热 

半潮湿 - 潮湿气候 , 组成第 I 气候旋回 ; 

中侏罗世呈热带亚热带半干旱 → 半潮湿气 

候的周期性变化 , 组成第 II、III 气候旋 

回 ; 晚侏世经历了热带炎热半干燥 → 温暖 

半潮湿和潮湿 → 炎热半干燥气候的演化 , 

组成第 IV、V 气候旋回 ; 白垩纪气候早期 

呈温暖半潮湿 , 晚期转为半干燥 - 干燥热 

带、亚热带气候 , 组成第 VI、VII 气候旋 

回 ; 第三纪为内陆亚热带的干燥、半干燥 

→ 高原温凉气候 ; 第四纪曾出现过 6 次冰 

期和 5 次间冰期 , 新生代总体经历了剧烈 

而频繁的冷暖波动 , 气候日益干燥和寒 

冷。最后简单分析了气候旋回与沉积旋 

回、构造运动和青藏高原隆升的叠加耦合 

关系 , 以及古气候变迁的主因。 

2008010565 

从化石群及壳体同位素看古近纪东营湖湖 

水化学 = Water chemistry of the Paleogene 

Dongying Lake: evidence from fossil assemblages 

and shell isotopes. ( 中文 ). 刘传联 ; 赵 

泉鸿 ; 汪品先 . 地球学报 - 中国地质科学院院 

报 , 2002, 23(3): 237-242 

从 “ 海源陆生化石 ”、壳体 O、C 和 S 同位 

素等几个新的角度和方法对山东东营凹陷 

古近纪古湖泊湖水化学性质进行讨论。通 

过与现生 “ 海源陆生生物 ” 的比较 , 得出原 

先认为是 “ 海相 ” 标志的有孔虫、钙质超微 

化石、沟鞭藻和疑源类、多毛类和钱等实 

际上是 “ 海源陆生化石 ”, 它们生活以在 

Cl - 和 Na + 为主的咸水湖泊环境。超微化石 S 

同位素分析表明 , 渐新世与始新世钙质超 

微化石的 87 Sr/ 86 Sr 比值都明显高于同时期海 

水的 87 Sr/ 86 Sr 比值 , 而与现代河、湖水的 

87 Sr/ 86 Sr 比值相近 , 进一步揭示它们生活的 

环境不是海 , 而是与海无关的湖。介形虫 

壳体 O、C 同位素分析则表明 , 古东营湖是 

一封闭型咸水湖泊 , 从另一角度也否定了 

144

与海连通的可能性。根据不同层段同位素 

特征讨论了湖水矿化度的相对变化。 

2008010566 

柴达木盆地归属问题 = Discussion on ownership 

of Qaidm Basin. ( 中文 ). 孙镇城 ; 乔子 

真 ; 杨革联 ; 张海泉 ; 景民昌 ; 杨藩 ; 孙乃达 . 古 

地理学报 , 2002, 4(1): 59-66 

柴达木盆地西部已找到 17 个第三系油源 

的油田 , 其主要烃源岩层位是陆相始新统 

下干柴沟组。有人提出下干柴沟组是海侵 

湖泊沉积 , 并被命名为下干柴沟海侵。最 

近又有人提出该组不是深湖相 , 应属于潟 

湖相 , 是塔里木盆地西南部始新世海湾潟 

湖相带被阿尔金断裂东错的残留潟湖部 

分 , 或塔里木盆地原型盆地在东部的错移 

部分 , 并提出重新认识柴达木盆地西部的 

油气勘探方向。文中展示了塔里木盆地西 

南部古新统 - 始新统的吐依洛克组、阿尔塔 

什组、齐姆根组、盖吉塔格组、卡拉塔尔 

组的沉积相和典型的海相生物化石群 , 它 

完全不同于柴达木盆地西部古新统 - 始新统 

的路乐河组和下干柴沟组沉积相和陆相湖 

泊生物化石群。作者不能支持柴达木盆地 

西部与塔里木盆地西南部在古近纪属于同 

一盆地或同一沉积单元的观点。把塔里木 

盆地西南部已知油气田的烃源岩划归古近 

系海相沉积 , 显然是误解 , 以此为根据指 

导柴达木盆地西部陆相沉积区的油气勘探 

似属不妥。科学的古地理观将有助于勘探 

工作的正确部署。 

2008010567 

明光一带渐新世明光组的发现 = Discovery 

of Oligocene Mingguang Formation around 

the city of Mingguang. ( 中文 ). 刘家云 ; 杜森 

官 ; 张志树 ; 鲁如魁 ; 吴海权 . 安徽地质 , 2001, 

11(3): 179-184 

明光城北地区出露不整合于定远组之上 

的碎屑岩 , 通过 ESR 年龄测定 , 认为属于渐 

新世的沉积。建立明光组填补了该区渐新 

世沉积的空白。 

2008010568 

安徽定远东部 — 明光地区古近 — 新近纪地 

层、沉积相特征及层序地层分析 = Paleogene-Neogene 

strata,features of sedimentary 

facies and analysis of sequence stratigraphy in 

the Dingyuan-Mingguang area,Anhui. ( 中文 ). 

吴跃东 ; 刘家云 . 安徽地质 , 2001, 11(3): 185- 

194 

安徽省定远东部 — 明光地区古近 — 新近 

系划分方案不一 , 通过地层剖面的测制和利 

用构造 — 岩性 — 岩相法进行 1∶ 

5 万地质填 

图 , 系统采集了 ESR 测年样 , 并结合区域对 

比 , 自下而上划分古近纪定远组、明光组 , 新 

近纪下草湾组和桂五组。该区古近 — 新近 

纪沉积物以陆相红色磨拉石和陆相火山岩 

建造为主 , 陆相红色类磨拉石的建造分析表 

明其形成于冲积扇和扇前河湖环境 , 碎屑物 

质来源于沉积区东边扬子地层区的浅变质 

岩和沉积区西北侧华北地层区变质岩和未 

变质岩石。其陆相火山喷发岩形成于大陆 

边缘活动性环境 , 是区内火山活动最盛的时 

期。其盆地类型为箕状断陷型、迁徒型和 

坳陷型。根据盆地充填沉积序列划分出 4 

个层序 (2 个二级和 2 个三级层序 ), 层序 Ⅰ 和 

层序 Ⅳ 不完整 , 层序 Ⅱ 和层序 Ⅲ 皆由冲积沉 

积体系域、湖扩张体系域和湖萎缩体系域 3 

个基本单位构成。层序界面主要有区域构 

造运动界面和盆地构造应力转换面 — 体系 

域转换界面两种类型。 

2008010569 

安徽凤阳石门山 — 清塘一带中新世石门山 

组的建立及其时代依据 = Establishment and 

age basis of Miocene Shimenshan Formation 

around the Shimenshan Qingtang area, Fengyang 

County, Anhui. ( 中文 ). 刘家云 ; 杜森官 . 

安徽地质 , 2002, 12(2): 92-96 

凤阳县石门山 — 清塘一带不整合于古近 

纪定远组之上 , 上为中更新世泊岗组角度不 

整合覆盖的一套松散的槽状交错层理发育 

的砂砾层 , 为典型的河流相沉积。上述砂砾 

层与下草湾组、定远组岩性及成岩程度上 

相差甚远 , 与南京地区 “ 六合组 ” 岩性相近 , 但 

时代不同 , 故新建 “ 石门山组 ”。 

2008010570 

厦门岛东南海岸贝壳层与风沙的研究 = 

Studies on shell bed and aeolian sands in 

Southeast coast of Xiamen Island. ( 中文 ). 杨 

顺良 ; 郑承忠 ; 翁宇斌 ; 郭允谋 . 台湾海 

峡 , 2002, 21(1): 12-17 

最近调查发现 , 厦门岛东南海岸剖面出 

露了三段长总计约 15m、厚度 0.4m 的古贝 

壳层。该层在高潮线之上 1 m 处 , 直接覆 

盖在古海滩之上 , 顶部被厚度达 4 ~5m 的 

三层风成沙所覆盖。本文根据贝壳种类鉴 

定及 14 C 年代测定和沉积物粒度分析进行研 

究 , 结果显示 , 厦门岛 1 510a 前的古海岸 

线比现在的海岸线高约 1 m、现代风成沙 

最早开始形成于隋唐时期 , 至今仍存在风 

145

沙隐患。为此 , 建议在开发利用中要因地 

制宜 , 防止风沙再度泛滥。 

2008010571 

生物壳体 Sr/Ca、Mg/Ca、87Sr/86Sr 比值 

在恢复古气候、古环境中的应用 - 以小渡口 

剖面为例 = The application of Sr/Ca 、 

Mg/Ca、87Sr/86Sr rations of biogenic shells 

in reconstruction of palaeoclimate and palaeoenvironment 

as examplified by Xiaodukou 

section. ( 中文 ). 贾玉鹤 ; 王世杰 . 地质地 

球化学 , 2002, 30(2): 54-58 

生物壳体的 Sr/Ca、Mg/Ca 比值能反映其 

沉积水体的 Sr/Ca、Mg/Ca 比值 , 在一定条 

件下反映水体的盐度、温度 , 并分别与宿 

生水体的盐度、温度呈正比关系。生物壳 

体的 87 Sr/ 86 Sr 比值是恢复盆地古水文条件的 

一种重要手段。本文以著名的泥河湾盆地 

小渡口剖面的第 28 层为实例 , 力图通过对 

有孔虫、介形虫、腹足类生物壳体 Sr/Ca、 

Mg/Ca 比值与 87 Sr/ 86 Sr 比值的对比研究 , 并 

结合前人所作的中更新世古地理特征研 

究 , 来恢复生物壳体沉积时泥河湾古湖水 

的温度、盐度 , 进而进行古气候、古环境 

的恢复。研究结果表明 : 在 0.97~0.94 Ma 

间 , 古泥河湾湖为一陆相湖泊 , 湖水的温 

度、盐度变化趋势相吻合 , 均呈低 - 高 - 低的 

演化特征 , 可能对应着盆地水体的扩展 - 退 

缩 - 扩展变化。其中 , 在 0.96~0.95 Ma 间 , 

古泥河湾湖具有较高的温度、盐度特征。 

2008010572 

澳大利亚南部 Murray 盆地渐新世 - 中新世 

地层修订 = Revised oligo-miocene stratigraphy 

of the Murray basin, southeast Australia. 

( 英文 ). Gallagher S J; Gourley T L. Australian 

Journal of Earth Sciences, 2007, 54(6): 

837-849 

This paper reconciles the outcrop and subsurface 

Oligo-Miocene marine stratigraphy of 

the Murray Basin to arrive at a basin-wide 

correlation. The initial open-marine transgressive 

marl and clay facies of the basin belong 

to the Ettrick Formation, a unit that is also 

laterally equivalent to the calcisiltite and calcarenite 

that are present on the surface and in 

the subsurface in the basin. Since this unit is 

lithologically indistinguishable from the previously 

identified Victorian Oligocene to 

Middle Miocene Winnambool Formation, we 

suggest that the latter unit be replaced as a 

stratigraphic unit in the basin. The majority of 

outcropping units in South Australia can be 

recognised lithostratigraphically in the subsurface 

of Victoria. The calcisiltite, calcarenite, 

marl and clay of the lower and upper Mannum, 

the Finniss, Glenforslan, Bryant Creek and 

Pata Formations can be distinguished in the 

Victorian Lower to Middle Miocene Duddo 

Limestone. Our work suggests that the 

lithostratigraphic unit the Duddo Limestone 

can also be replaced as a stratigraphic unit in 

the region. Direct correlation to the outcropping 

detailed stratigraphy in South Australia 

has been achieved across into Victoria for the 

first time. The correlations will allow a better 

understanding of the geometry of the Oligo- 

Miocene strata in the Murray Basin allowing 

improved hydrostratigraphy. It will also form 

the basis for ongoing polaeoenvironmental 

and palaeoceanographic studies in the area. 

2008010573 

最近 2.5 Ma 黄土高原环境变化研究进展 — 

来自洛川黄土地层的证据 = Luochuan loesspaleosol 

sequence and paleo-environmental 

implications: a brief review. ( 中文 ). 李玉梅 . 

地球科学进展 , 2002, 17(1): 

洛川黄土 — 古土壤序列记录了最近 2.5 

Ma 黄土高原自然环境的演化和变迁。国内 

外研究人员运用地层学、古生物学、土壤 

学、磁学、沉积学、岩石学、矿物学、地 

球化学等多学科的研究方法 , 统一地层划 

分 , 明确成因机制 , 建立时间标尺 , 分析 

气候指标 , 提取环境信息 , 逐步揭示了自 

早更新世以来该区气候由暖湿而冷干、频 

繁剧烈波动的历史以及古生物的演替过 

程 , 为全球变化研究提供了重要资料。 

2008010574 

12900 年前促成大型哺乳动物绝灭和新仙 

女木变冷事件的天外撞击事件证据 = Evidence 

for an extraterrestrial impact 12,900 

years ago that contributed to the megafaunal 

extinctions and the Younger Dryas cooling. 

( 英文 ). Firestone R B; West A; Kennett J P; 

Becker L; Bunch T E; Revay Z S; Schultz P H; 

Belgya T; Kennett D J; Erlandson J M; Dickenson 

O J; Goodyear A C; Harris R S; Howard 

G A; Kloosterman J B; Lechler P; 

Mayewski P A; Montgomery J; Poreda R; 

Darrah T; et al. proceedings of the National 


16021 4 图版 . 

A carbon-rich black layer, dating to 12.9 ka, 

has been previously identified at 50 Clovis-age 

sites across North America and appears contemporaneous 

with the abrupt onset of 

Younger Dryas (YD) cooling. The in situ 

146

ones of extinct Pleistocene megafauna, along 

with Clovis tool assemblages, occur below 

this black layer but not within or above it. 

Causes for the extinctions, YD cooling, and 

termination of Clovis culture have long been 

controversial. In this paper, we provide evidence 

for an extraterrestrial (ET) impact event 

at 12.9 ka, which we hypothesize caused 

abrupt environmental changes that contributed 

to YD cooling, major ecological reorganization, 

broad-scale extinctions, and rapid human 

behavioral shifts at the end of the Clovis Period. 

Clovis-age sites in North American are 

overlain by a thin, discrete layer with varying 

peak abundances of (i) magnetic grains with 

iridium, (ii) magnetic microspherules, (iii) 

charcoal, (iv) soot, (v) carbon spherules, (vi) 

glass-like carbon containing nanodiamonds, 

and (vii) fullerenes with ET helium, all of 

which are evidence for an ET impact and associated 

biomass burning at 12.9 ka. This 

layer also extends throughout at least 15 Carolina 

Bays, which are unique, elliptical depressions, 

oriented to the northwest across the Atlantic 

Coastal Plain. We propose that one or 

more large, low-density ET objects exploded 

over northern North America, partially destabilizing 

the Laurentide Ice Sheet and triggering 

YD cooling. The shock wave, thermal 

pulse, and event-related environmental effects 

(e.g., extensive biomass burning and food 

limitations) contributed to end-Pleistocene 

megafaunal extinctions and adaptive shifts 

among PaleoAmericans in North America. 

2008010575 

青海省西宁市大墩岭黄土剖面元素组分变 

化与第四纪古气候演化 = Variation of elements 

content along the dadunlin loess profile 

in Xining City,Qinghai,and paleoclimate evolution. 

( 中文 ). 王永明 ; 侯元才 . 青海地 

质 , 2002, 10(S1): 1-5,9 

根据黄土剖面中古土壤系列与砂质黄土 

中常量元素氧化物含量基本特征 , 主要地质 

特征、黄土堆积与古土壤形成古气候环 

境、演化过程与主要元素组分特征、关系 

进行了讨论 , 结合孢粉测年等资 

料 ,1.19MaB.P. 黄土形成以来的气候演变过 

程与元素组分变化关系。 

2008010576 

青藏高原东北缘 1.2MaB.P. 以来各阶段古 

气候演变 = Paleoclimate evolution in various 

stages since 1.2 Ma.B.P.in northeastern Qinghai-Xizang 

Plateau. ( 中文 ). 侯元才 ; 许伟林 ; 

俞建 ; 周亚芝 . 青海地质 , 2001, 10(S1): 10-16 

对青藏高原东北缘北祁连山、门源盆 

地、西宁盆地化隆、贵德 — 共和等地第四 

纪沉积物沉积特征、孢粉组合、 14 C 、 

TL( 热释光 ) 等测年资料 , 综合分析发现本区 

第四纪沉积物最早达 1.2Ma, 总结分析了 

1.2MaB.P. 以来古气候演变历程 , 可以确定存 

在四期主要寒冷事件。 

2008010577 

美国北达科他威利斯顿盆地古新世 - 始新世 

界线区域风化剖面的陆源证据 = Terrestrial 

records of a regional weathering profile at the 

Paleocene-Eocene boundary in the Williston 

Basin of North Dakota. ( 英文 ). Clechenko E 

R; Kelly D C; Harrington G J; Stiles C A. 

Geological Society of America Bulletin, 2007, 

119(3-4): 428-442 

The "orange zone" within the Bear Den 

Member of the Golden Valley Formation 

(Williston Basin, North Dakota) represents a 

terrestrial weathering profile formed by intense 

pedogenesis during an ancient (ca. 55 

Ma) global warming event referred to as the 

Paleocene-Eocene thermal maximum. Distinctive 

features of the orange zone include: (1) 

high abundances of kaolinite, (2) a strongly 

leached character with a bright orange ironenriched 

horizon, (3) poor organic carbon 

preservation, and (4) ferric pans/pisoliths at its 

basal contact, equivalent to modern lateritic 

materials. Though conclusive evidence, such 

as a distinctive Paleocene-Eocene thermal 

maximum flora and/or definitive carbon isotope 

excursion, is lacking, the stratigraphic 

succession of palynofloral datums preserved 

within the upper part of the Bear Den orange 

zone is similar to that associated with the later 

stages of other terrestrial Paleocene-Eocene 

thermal maximum records from the U.S. 

Western Interior. Bulk 13 C org ratios decrease 

through the orange zone as well, but the magnitude 

of this isotopic decrease is less than that 

of the carbon isotope excursion. Thus, the collective 

evidence indicates that the early initial 

stages of the Paleocene-Eocene thermal 

maximum are either preserved within the barren, 

condensed interval of the lower orange 

zone or are missing altogether from the Williston 

Basin stratigraphy, and that the orange 

zone likely developed during the later recovery 

stages of the Paleocene-Eocene thermal 

maximum. The Williston Basin records generally 

agree with the tenet that continental 

weathering intensified during the Paleocene- 

147

Eocene thermal maximum. Moreover, these 

records indicate that the paleohydrology of the 

basin varied markedly and that sequestration 

of terrestrial organic carbon was greatly reduced 

as this transient global warming event 

unfolded. 

2008010578 

从新西兰西南部卡斯卡德高原冰碛漂砾的 

宇宙成因核素时代推断自 100 ka 以来中纬 

度南半球冰川作用的轨道力 = Orbital forcing 

of mid-latitude Southern Hemisphere glaciation 

since 100 ka inferred from cosmogenic 

nuclide ages of moraine boulders from the 

Cascade Plateau, southwest New Zealand. ( 英 

文 ). Sutherland R; Kim K; Zondervan A; 

McSaveney M. Geological Society of America 

Bulletin, 2007, 119(3-4): 443-451 

Cosmogenic nuclide (Be-10) exposure 

dating of moraine boulders in the Cascade 

Valley, southwest New Zealand, reveals three 

phases of glaciation with similar maximum 

magnitude since 100 ka. In this area, 8–10 

lateral moraines were deposited during the 

Last Glacial Maximum (LGM) at 22–19 ka, 

and >15 lateral moraines and three end moraines 

were deposited during recession after 

the LGM. Also, three exposure ages of 29–33 

ka from pre-LGM deposits may indicate increased 

weathering and erosion at the onset of 

the LGM in New Zealand, as has been suggested 

by other studies. An exposure age of 

57.8 ± 2.7 ka from one of the highest moraines, 

combined with previous studies of cave speleothems, 

glacial features offset by the Alpine 

fault, the Vostok dust record, and sediment 

cores, supports the inference that a significant 

glacial phase culminated at 66–58 ka. A cluster 

of five exposure ages from older moraines 

reveals a glacial phase with at least three advance-retreat 

cycles at 79.0 ± 3.9 ka. Correlation 

between the ages of glacial periods and 

the timing of Southern Hemisphere summer 

insolation minima suggests that orbital forcing 

has played a first-order role in regulating glacial 

extent in New Zealand. 

2008010579 

探寻小冰期对中美洲东部热带低地的影响 

= Tracing the effects of the Little Ice Age in 

the tropical lowlands of eastern Mesoamerica. 

( 英文 ). Lozano-García M d S; Caballero M; 

Ortega B; Rodríguez A; Sosa S. proceedings 

of the National Academy of Sciences, 2007, 

104(41): 16200-16203 3 图版 . 

The causes of late-Holocene centennial to 

millennial scale climatic variability and the 

impact that such variability had on tropical 

ecosystems are still poorly understood. Here, 

we present a high-resolution, multiproxy record 

from lowland eastern Mesoamerica, studied 

to reconstruct climate and vegetation history 

during the last 2,000 years, in particular to 

evaluate the response of tropical vegetation to 

the cooling event of the Little Ice Age (LIA). 

Our data provide evidence that the densest 

tropical forest cover and the deepest lake of 

the last two millennia were coeval with the 

LIA, with two deep lake phases that follow the 

Spörer and Maunder minima in solar activity. 

The high tropical pollen accumulation rates 

limit LIA's winter cooling to a maximum of 

2°C. Tropical vegetation expansion during the 

LIA is best explained by a reduction in the 

extent of the dry season as a consequence of 

increased meridional flow leading to higher 

winter precipitation. These results highlight 

the importance of seasonal responses to climatic 

variability, a factor that could be of 

relevance when evaluating the impact of recent 

climate change. 

2008010580 

喀斯特区域地貌与原始森林关系的讨论 - 以 

贵州荔波茂兰、望谟、麻山为例 = Relationship 

between the Karst regional geomorphy 

and the virgin forest: A case study of 

Maolan at Libo and Mashan at Wangmo, 

Guizhou. ( 中文 ). 姚智 ; 张朴 ; 刘爱民 . 贵州地 

质 , 2002, 19(2): 99-102 

研究表明 , 喀斯特坡体上能否生长森 

林 , 与喀斯特区域地貌类型的关系极为密 

切 , 本文通过荔波茂与望谟麻山两地的对 

比认为 , 山盆期地貌保存良好的地区 , 有 

利于森林的生长与恢复 ; 而乌江期地貌叠 

加发育的地区 , 则不利于森林的生长。从 

而说明已石漠化的喀斯特坡体并非全是人 

为破坏所为 , 也非所有石漠化喀斯特地区 

一经封山便可恢复森林。 

2008010581 

2 万年来我国东部海陆环境变化的不同步 

现象 = Asynchrony of the marine and epicontinental 

climate records in the East Asia during 

the last 20 ka. ( 中文 ). 吕厚远 ; 刘振夏 ; 刘 

宝柱 ;Serge Berné;Yoshiki Saito; 李铁刚 ; 吴乃 

琴 . 海洋地质与第四纪地质 , 2002, 22(1): 17- 

23 

冲绳海槽 DG9603 孔高分辨率的硅藻、 

有孔虫、孢粉和植物硅酸体化石的记录 , 

148

提供了联系海洋与陆地气候变化的直接证 

据。结果显示 , 中国东部及邻海区最近 20 

kaBP 以来海洋环境的变化滞后陆地气候的 

变化约 1 000a, 初步认为这种滞后现象可 

能是北半球陆地气候快速变化的同步性和 

温盐环流从北大西洋缓慢传送到太平洋海 

域的时间差引起的。 

2008010582 

东海嵊山岛风尘黄土中的植物硅酸体与环 

境研究 = Phytolith and its paleoenvironmental 

significance in aeolian loess of Shengshan 

Island of the East China Sea. ( 中文 ). 郑祥民 ; 

赵健 ; 周立旻 ; 王伟铭 . 海洋地质与第四纪地 

质 , 2002, 22(1): 25-30 

东海岛屿风尘黄土地层的存在是下蜀黄 

土在东部的继续与延伸 , 红外释光测年 

(IRSL) 表明 , 东海嵊山岛黄土剖面形成 

年代约为 50~10 kaBP, 即形成于晚更新世 

末次冰期期间 ; 植物硅酸体分析了现该剖 

面样品中含有丰富的禾本科物硅酸体化 

石 , 且在剖面中变化较大 , 在对植物硅酸 

体进行分类的基础上 , 运用了判别分析、 

冷暖比值判别和古植物类型判别的方法 , 

对植物硅酸体所反映的古环境进行了分 

析 , 将岛屿风尘地层中的植物硅酸体划分 

为 7 个变化阶段 , 反映了岛屿黄土堆积期 

的 7 次气候变化过程 , 探讨了该地区末次 

冰期期间古环境、古气候变迁特征 , 发现 

该剖面沉积期间主要为干冷的草原环境且 

经过子一系列冷 - 暖气候变迁。 

2008010583 

P/E 界线全球事件在西藏定日地区的响应 = 

Sedimentary responses to the global event of 

transitional Paleocene-Eocene boundary in 

Tingri, southern Tibet. ( 中文 ). 李祥辉 ; 包向农 ; 

胡修棉 ; 王成善 ; 万晓樵 ; 范善发 . 海洋地质与 

第四纪地质 , 2002, 22(1): 69-74 

生物群、沉积物和有机地球化学变化显 

示 , 古新统 - 始新统 (P/E) 界线全球事件 

在西藏南部定日 ( 东特提斯残留海低纬度 

浅水 ) 地区存在明显响应 : 古新统宗浦组 

顶部有孔虫动物群的属、种绝灭率分别为 

87% 和 94%, 始新统遮普惹组底部有孔虫 

属、种新生率分别达 80% 和 69%; 岩层以 

( 生物滩相 ) 薄 - 中层向厚层 - 块状生物灰岩 

转化 , 泥质含量增加 ; 典型生物标志化合 

物参数变化明显 ,Pr/17 比值平均从 0.365 

增加到 0.86,Ph/18 由 0.56 变为 0.92,β/17 

由 12.843 剧增到 123.17,γ/17 由 2.46 突变 

为 29.5。结合西藏及邻区岩相分布、接触 

关系后认为 , 这种全球地质事件的响应在 

研究区可能是一种古海洋事件 , 可能由大 

洋环流 ( 古水团 ) 变化引起。 

2008010584 

雷州半岛珊瑚礁生物地貌带与全新世多期 

相对高海平面 = Biologicalgeomorphological 

zones in a coral reef area at 

Southwest Leizhou Peninsula unveil multiple 

sea level high-stands in the Holocene. ( 中文 ). 

余克服 ; 钟晋梁 ; 赵建新 ; 沈承德 ; 陈特固 ; 刘东 

生 . 海洋地质与第四纪地质 , 2002, 22(2): 27- 

33 

通过多次野外调查 , 将灯楼角珊瑚礁分 

为 8 个生物地貌带 : 礁前斜坡活珊瑚林 

带、外礁坪大块滨珊瑚礁岩带、中礁坪块 

状珊瑚混合带、中礁坪块状珊瑚 — 角孔珊 

瑚混合带、内礁坪角孔珊瑚带、沙坪台 — 

海滩、沙堤和洼地 , 它们是海平面和气候 

环境变化的产物。以珊瑚礁及其生物地貌 

带作为高海平面的标志 , 根据 13 个表层珊 

瑚礁样品的 TIMS 铀系年代和 1 个 14 C 年代 , 

指出全新世以来至少存在过 5 期相对高海 

平面 (7.2~6.7、约 5.8、5.0~4.2、2.8~ 

2.0、约 1.5 cal.kaBP), 每一期中还存在低 

海平面的波动。其中 6.7~7.2 kaBP 是整个 

全新世最高海平面时期 , 在这个时间段已 

经基本形成了现代珊瑚礁的地貌格局。这 

个时间段以后形成的珊瑚礁是在 6.7~7.2 

kaBP 形成的珊瑚礁礁坪的礁塘或礁坑等低 

洼地中形成的 , 迄今为止 , 没有再出现过 

高出 6.7~7.2 kaBP 时期的海平面。 

2008010585 

雷州半岛灯楼角珊瑚岸礁的特征 = Features 

of fringing reef at Dengloujiao, Leizhou Peninsula. 

( 中文 ). 赵焕庭 ; 王丽荣 ; 宋朝景 ; 余克 

服 ; 袁家义 . 海洋地质与第四纪地质 , 2002, 

22(2): 35-40 

雷州半岛西南海岸的珊瑚礁是中国大陆 

唯一的全新世中期之初海侵以来形成的岸 

礁。灯楼角岸段岸礁沿灯楼角岬角两侧共 

长 11.5 km, 宽 500~1 000m, 厚约 5 m。 

珊瑚化石的优势种是 Goniopora sp.。本海 

区的海水温度、盐度、透明度和环境质 

量 , 均适合造礁石珊瑚生长 , 采集到活珊 

瑚 8 科 16 属 25 种 , 其中优势种是 Acropora 

humilis , Porites lutea, Prities pukoensis 和 

Favia speciosa。岸礁可分为礁坪和礁前向 

海坡两个地貌单元。内礁坪上有薄层细砂 

堆积 “ 沙帽 ”, 主要由陆源碎屑沉积物 , 其 

次为生物碎屑组成。礁的 14 C 年龄主要为 7 

149

120~4 040 aBP。在全球变化引起表层海水 

温度增高和海平面上升的条件下 , 由于大 

陆架深层水的影响 , 琼州海峡的沿岸水受 

到调节 , 夏季不致过热 , 冬季不致过冷 , 

所以本区造礁石珊瑚仍能生长和繁殖 , 珊 

瑚礁仍存在和发展。 

2008010586 

南海北部 ODP1148 站中新世以来的碳酸盐 

含量变化及其古环境意义 = Carbonate content 

changes since the Miocene and paleoenvironmental 

implications, ODP Site 1148, 

northern South China Sea. ( 中文 ). 陈晓良 ; 赵 

泉鸿 ; 翦知湣 . 海洋地质与第四纪地质 , 2002, 

22(2): 69-74 

对南海北部 ODP 1148 站采自孔深 

465m 以上的 1 700 个沉积物样品 , 测定了 

CaCO 3 含量、CaCO 3 堆积速率、非钙质堆积 

速率、浮游有孔虫丰度、粗组分百分含量 

(>63 μm)、浮游有孔虫破壳率和底栖有 

孔虫在有孔虫全群中的百分含量。碳酸盐 

百分含量和碳酸盐堆积速率自 24Ma 以来的 

变化呈现逐步下降的趋势 , 但在 24.0~ 

15.8、14.2~11.6、10.6~4.8 和 3.4~0Ma 

四个时期具有高碳酸盐生产力 , 其中 

10.6~4.8Ma 的高生产力与印度洋和太平洋 

中新世晚期和上新世早期的 “ 生物勃发 ” 相 

对应。非钙质和碳酸盐两者堆积速率变化 

趋势在总体上相似 , 反映了陆源物质输入 

对碳酸盐生产力的影响。3.4Ma 后非钙质堆 

积速率的大幅度增长主要与青藏高原和台 

湾岛的隆起有关 , 它们也是上新世晚期和 

第四纪 CaCO 3 百分含量显著下降的主要原 

因。24Ma 以来南海北部碳酸盐的保存逐渐 

变弱 , 而碳酸盐溶解作用逐渐增强 , 在 

15.8~14.2、11.6~10.6 和 4.8~3.4Ma 存在 

3 个显著的碳酸盐溶解事件 , 其中 11.6~ 

10.6Ma 的溶解事件与赤道太平洋和加勒比 

海的中 — 晚中新世 “ 碳酸盐崩溃 ” 事件相 

当 , 说明该事件具更广泛的全球影响。 

2008010587 

最后间冰期时期大盆地和北大西洋同步的 

千年尺度的气候变化 = Synchronous millennial-scale 

climatic changes in the Great Basin 

and the North Atlantic during the last interglacial. 

( 英文 ). Denniston R F; Asmerom Y; 

Polyak V; Dorale J A; Carpenter S J; et al. 

Geology, 2007, 35(7): 619-622 

Stalagmites from Goshute Cave, located 

in the Great Basin of the western United States, 

preserve 20,000 yr of millennial-scale oxygen 

isotopic variability during marine isotope 

stages 5c and 5b, similar in timing and structure 

to Dansgaard-Oeschger (D-O) events 23– 

21 from the Greenland Ice Sheet Project 2 record. 

That D-O interstades 23–21 were of 

longer duration than many of the later D-O 

events, coupled with the asymmetric shape of 

the D-O oxygen isotope curve, and the direct 

U-Th dating of the Goshute Cave stalagmites, 

allows for an improved understanding of the 

synchroneity of climatic changes between the 

western continental United States and the 

North Atlantic. Eastern Pacific–atmosphere 

interactions are a likely mechanism for transmission 

of millennial-scale climate variability 

into the Great Basin. 

2008010588 

黄土中蜗牛壳 Mn~(2+) 的 EPR 研究及其古 

气候意义 = An EPR study on mollusk shells 

from loess-paleosol sequences in the Loss Plateau, 

central China. ( 中文 ). 盛雪芬 ; 陈骏 ; 季峻 

峰 ; 眭云霞 . 高校地质学报 , 2002, 8(1): 40-45 

对黄土高原陕西省洛川和甘肃省西峰 

剖面中黄土 - 古土壤层中的蜗牛壳进行了 

EPR 波谱分析 , 同时对洛川地区的现代蜗 

牛壳也进行了测定。结果显示 :(1) 不同 

种类的蜗牛壳具有相近的 EPR 信号强度 , 

表明不同种类的蜗牛对 Mn 2+ 的吸收没有差 

异性。(2) 黄土层中蜗牛壳的 EPR 信号强 

度远大于古土壤中的 , 即黄土中蜗牛壳所 

含的 Mn 2+ 远大于古土壤中的蜗牛壳的 Mn 2+ 

的含量 , 说明前者生活在比较还原的条件 

下 , 后者形成环境的氧化性较高。因此本 

文认为蜗牛壳中 Mn 2+ 的含量可反映其生长 

环境中 Mn 2+ 的含量和氧化还原条件 , 对古 

气候的重建具有重要意义。 

2008010589 

南沙岛礁区中西部海底岩石拖网和发现早 

第三纪半深海沉积的地质意义 = Phosphate 

and other rocks dredged from central and 

western Nansha block, southern South China 

Sea. ( 中文 ). 周蒂 ; 施小斌 ; 陈汉宗 ; 钟石兰 . 热 

带海洋学报 , 2002, 21(2): 32-42 

在南沙岛礁区中西部实施海底岩石拖 

网 , 有 3 个站获得海底岩石样品。其中在 

巽它陆架东北缘水深 200 多米的 NS99-17 

站见深灰色淤泥中有大量铁褐色含泥钙质 

结核 , 说明该区 ( 可能在末次冰期时 ) 处 

于滨海或海滩氧化环境形成结核 , 之后海 

平面上升了至少 150m。在南威岛西北方康 

泰滩的 NS99-57 站 1 360m 水深的海底获强 

溶蚀的白垩状多孔灰岩 , 含底栖有孔虫化 

150

石 , 指示康泰滩是从早 — 中中新世或更早 

开始生长的生物礁。在永署礁东北约 55km 

处的 NS99-52 站新命名了 “ 东生海山 ”, 其 

西北坡获含第四纪钙质超微化石的礁灰 

岩 , 以及由抱球虫类等生物碎屑和胶磷矿 

组成的钙质磷块岩和含磷生物屑灰岩滚 

石 , 指示半深海环境 , 其中的钙质超微化 

石大部分时代为中始新世 — 渐新世 , 以始 

新世可能较大 , 小部分属第四纪。这次海 

底岩石拖网为研究南沙岛礁区中部地质构 

造演变和油气资源评价提供了重要的 “ 硬证 

据 ”, 尤其是发现早第三纪半深海相钙质磷 

块岩离南海西南次海盆很近 , 不但证实了 

南沙海域广布下第三系海相沉积的推断 , 

而且为判断南海的张开时间提供了补充依 

据。 

2008010590 

整个始新世时期为稳定热带气候 = Stable 

warm tropical climate through the Eocene Epoch. 

( 英文 ). Pearson P N; van Dongen B E; 

Nicholas C J; Pancost R D; Schouten S; Singano 

J M; Wade B S. Geology, 2007, 35(3): 

211-214 

Earth's climate cooled from a period of 

extreme warmth in the early Eocene Epoch (ca. 

50 Ma) to the early Oligocene (ca. 33 Ma), 

when a large ice cap first appeared on Antarctica. 

Evidence from the planktonic foraminifer 

oxygen isotope record in deep-sea cores has 

suggested that tropical sea-surface temperatures 

declined by 5-10 degrees over this interval, 

eventually becoming much cooler than 

modern temperatures. Here we present paleotemperature 

estimates from foraminifer isotopes 

and the membrane lipids of marine 

Crenarcheota from new drill cores in Tanzania 

that indicate a warm and generally stable 

tropical climate over this period. We reinterpret 

the previously published isotope records 

in the light of comparative textural analysis of 

the deep-sea foraminifer shells, which shows 

that in contrast to the Tanzanian material, they 

have been diagenetically recrystallized. We 

suggest that increasingly severe alteration of 

the deep-sea plankton shells through the Eocene 

produced a diagenetic overprint on their 

oxygen isotope ratios that imparts the false 

appearance of a tropical sea-surface cooling 

trend. This implies that the long-term Eocene 

climatic cooling trend occurred mainly at the 

poles and had little effect at lower latitudes. 

2008010591 

末次盛冰期黄土高原蜗牛化石记录的气候 

快速变化及其影响机制 = Rapid climate 

variability recorded by mollusk species on the 

Loess Plateau during the last glacial maximum. 

( 中文 ). 吴乃琴 ; 刘秀平 ; 顾兆炎 ; 裴云鹏 . 第四 

纪研究 , 2002, 22(3): 283-291 

本文通过渭南黄土剖面末次盛冰期地层 

较高分辨率的蜗牛化石记录研究 , 发现这 

一时期特征蜗牛种类峰值的演替反映了古 

气候的演化过程和温、湿度的组合关系 , 

气候变化显示出百年 ~ 千年尺度波动的特 

征 , 温度的变化明显地要早于湿度 ( 降 

水 ) 的变化 1 000 ~ 2 000a, 表现为变冷 - 

冷湿 - 冷干 - 温干 - 温湿的气候过程 , 研 

究认为造成这一气候特点的原因是东亚 

冬、夏季风共同作用的结果。对喜温湿蜗 

牛种类的研究 , 揭示出东亚夏季风在这一 

时期至少能够持续地影响到黄土高原的东 

南部地区 , 这个时期冬季风强化的结果之 

一是影响了夏季风在这一地区滞留的时 

间 , 加大了季节性的差异。分析表明尽管 

夏季风在这一地区滞留的时间缩短 , 但维 

持了它固有的强度 , 提供了适量的水热条 

件供喜温湿蜗牛种类在这一寒冷阶段持续 

地生长和发育。 

2008010592 

云南鹤庆盆地近 1Ma 来的气候序列重建初 

探 = Reconstruction of climatic sequence of 

the past 1Ma in the Heqing basin, Yunnan 

Province. ( 中文 ). 童国榜 ; 刘志明 ; 王苏民 ; 羊 

向东 ; 王书兵 . 第四纪研究 , 2002, 22(4): 332- 

339 

云南鹤庆盆地近 1Ma 来的孢粉植物群很 

好的揭示了本区的环境演化过程。本文利 

用植物生态位知识 , 通过模糊数学方法对 

鹤庆 (QH) 孔孢粉序列所记录的古气候信 

息进行重塑 , 建立了近 1Ma 来的年均温、 

年降水量及年较差序列 , 并将本区气候演 

化分为 4 个气候旋回 ,32 个气候期。该序 

列可与黄土 - 古封序列及海洋 δ 18 O 阶段对 

比 , 但冷暖波动的幅度及降温时段持续的 

长短有其特色 , 表明本区气候既受全球气 

候变化的控制 , 又受青藏高原阶段隆升的 

制约 ; 近 1Ma 来气温的波动幅度呈递增趋 

势 ,0.30 MaB.P. 尤其显著 ; 冷、暖段间年 

均温的变化幅度由第一气候旋回的 7 ℃ 增 

大到第三气候旋回的 9 ℃( 按 4 次平滑值 

计算 ), 而样点的实际最大差值由 8 ℃ 增 

至 16 ℃; 最强烈的降温发生在第二气候旋 

151

回中的 0.45~0.14 Mab. p. 1Ma 来 , 西南季 

风区的气候组构与东南季风区不同。 

2008010593 

全新世中国热带北界变迁的探讨 = Shift of 

the north boundary of China's tropics during 

Holocene. ( 中文 ). 黄镇国 ; 张伟强 ; 江璐明 . 第 

四纪研究 , 2002, 22(4): 359-364 

本文根据孢粉、动物群、石笋、珊瑚 

礁、红树林等约 30 个全新世古环境分析实 

例 , 认为年均气温度化 2℃ 左右 , 就会引起 

热带界线的变动。热带北界的迁移过程可 

分 3 个阶段 : 全新世回暖期北返阶段 (11 

000~8 500 aB.P.), 热带北移 1.5 个纬 

度 ; 升温期北进阶段 (8 500 ~ 5 000 

aB.P.), 向北推进 3~5 个纬度 ; 降温期南 

归阶段 (5 000~3 000 aB.P.), 向南回归 

1~4 个纬度。热带北界的展布既有纬度地 

带性 , 也有经度地带性 , 这与东亚季风、 

寒潮、台风的影响以及地形格局有关。 

2008010594 

河北平原南部曲周地区早、中全新世冲积 

物的分析及古环境状况的推测 = Alluviums 

of the early and middle Holocene in the 

Quzhou area, the southern Hebei plain and 

palaeoenvironment inferences. ( 中文 ). 王红亚 ; 

石元春 ; 于澎涛 ; 汪美华 ; 郝晋民 ; 李亮 . 第四纪 

研究 , 2002, 22(4): 381-393 

在河北平原部的曲周县四町乡河部洼地 

一深为 250cm 的探坑中 , 取得 50~250cm 

深度范围的沉积物样品。对这此冲积物样 

品做了 AMS 14 C 测年、粒度分析、矿物磁性 

测量、碳酸盐中氧、碳稳定同位分析、全 

有机碳和碳 / 氮比值分析、孢粒分析。结果 

表明 , 全有机碳极低 , 孢粉甚少 ; 矿物磁 

性参数和稳定同位素今是随粒度的变化与 

黄土高原的黄土 - 古土壤序列中的情形十分 

相似。由此推测这些变化在一定程度上反 

映了成土作用对冲积物的影响和气候状况 

的变化 , 并对这一地区的早、中全新世古 

环境划分为 6 个变化阶段 : 在约 10 210~ 

10 000a B.P., 气候温暖湿润 ; 在 10 000~8 

500 a B.P., 气候凉干 ; 在 8 500~8 000a 

B.P., 气候又转为温暖湿润 ; 在 8 000~7 

200 a B.P. 气候再趋凉干 , 在 7200~ 约 6500 

a B.P., 气候再度变为温暖湿润 ; 在约 6 

500 a B.P. 以后 , 气候渐趋凉干。 

2008010595 

沿日本海东部始新世至渐新世序列的地层 

评述 : 对日本海早期开裂的意义 = Stratigraphic 

review of Eocene to Oligocene successions 

along the eastern Japan Sea: Implication 

for early opening of the Japan Sea. ( 英文 ). 

Kano K; Uto K; Ohguchi T. Journal of Asian 


Stratigraphic review of the on-land successions 

exposed on the back-arc side of Japan 

and Sakhalin, combined with supplemental 

radiometric dating, reveals the existence of 

Late Eocene or Oligocene marine sediments 

along the eastern coast of the Japan Sea. This 

finding implies that the origin of the Japan Sea 

dates back to the Oligocene or earlier time, 

much older than ever supposed. The host Eocene 

to Oligocene subaerial to shallow-water 

successions distribute immediate west of the 

volcanic front of that time and contain volcanic 

rocks, the chemistry of which is characteristic 

of continental rift or volcanic arc. They 

are associated with parallel dike swarms or 

normal faults, and could be infillings of an 

incipient back-arc rift. Collective evidence 

suggests that the rift was rapidly subsided and 

spread during the following Early to Middle 

Miocene time. However, a back-arc-wide unconformity 

was produced during a short period 

from the latest Oligocene to the earliest 

Miocene and was succeeded by extensive bimodal 

volcanism with rapid migration of the 

volcanic front to the fore-arc side. These 

short-term events could have been induced by 

upwelling or inflow of hot asthenosphere beneath 

the arc-rift system, followed by rapid 

subsidence and spreading of the Japan Sea. 

2008010596 

南襄盆地泌阳断陷高分辨率层序地层研究 

= Application of high-resolution sequence 

stratigraphy in Biyang fault depression of 

Nanxiang Basin. ( 中文 ). 胡受权 ; 郭文平 . 新 

疆石油地质 , 2002, 23(3): 201-204 

根据陆相层序在地震剖面及电测曲线上 

的识别标志 , 采用沉积旋回分析技术及 

Fischer 图解法 , 将泌阳断陷双河 - 赵凹地区下 

第三系核三上段划分为三个陆相层序 , 在研 

究区表现为冲积扇 - 扇三角洲 - 湖相沉积体系 

空间配置关系。在这三个陆相层序中发育 

低位加积型、退积型、高位加积型和进积 

型 4 类小层序组共 13 个 , 其中可识别的小层 

序达 40 余个 , 并进一步阐明了其沉积相 ( 微 

相 ) 构型特征。 

2008010597 

六盘山盆地中新生代沉积地层 = The sedimentary 

strata from Mesozoic to the Cenozoic 

152

in Liupanshan Basin. ( 中文 ). 付国斌 ; 李兴亮 . 

新疆石油学院学报 , 2002, 14(2): 24-27 

六盘山盆地中新生代沉积地层巨厚 , 纵 

向发育上三叠统、中株罗统、下白垩统、 

第三系及第四系 , 除中株罗统分布局限 

外 , 其它均分布广泛。本文通过大量的野 

外地质露头考察资料和室内综合研究 , 建 

立了六盘山盆地中新生界地层层序 , 归纳 

总结出盆地中新生界五个宏观划分对比标 

志层 , 指出盆地中新生界主要发育上三叠 

统和下白垩统两套烃源岩 , 生烃潜力巨 

大 , 并可形成相应的两套主要生储盖组 

合 , 为六盘山盆地地质综合研究及油气勘 

探工作的开展奠定基础。 

2008010598 

塔克拉玛干沙漠腹地第四纪地层划分与环 

境变迁 = Stratigraphic subdivision and climatic 

change of the Quaternary of the centre 

Taklimakan desert. ( 中文 ). 张鸿义 ; 门国发 . 

新疆地质 , 2002, 20(3): 256-261 

通过塔中地区 KT 1 孔和 KT 2 孔井下第四纪 

地质测试研究 , 首次揭示出 : 塔克拉玛干 

沙漠腹地在深度 653.80m 以上 , 沉积物可 

划分 42 层 , 基本属于第四系。第四系下限 

初步定在 761.17m 深处。第四纪以来的气 

候演化大体有过 3 次大的气候波动和 13 个 

较大气候波动旋回。沉积环境早更新世为 

河湖相泛滥平原 ; 中更新世以洼地湖泊相 

沉积为主 , 同时明显加入了风沙环境堆 

积 , 沙漠开始形成 ; 从中更新世晚期开 

始 , 经晚更新世到新世 , 沙漠大规模形 

成 , 并逐步发展成今日的大沙漠景观。 

格陵兰冰芯记录的南极气候特征 = Antarctic 

climate signature in the Greenland ice core 

record. ( 英文 ). Barker S; Knorr G. proceedings 

of the National Academy of Sciences, 

2007, 104(44): 17278-17282 4 图版 . 

A numerical algorithm is applied to the 

Greenland Ice Sheet Project 2 (GISP2) dust 

record from Greenland to remove the abrupt 

changes in dust flux associated with the Dansgaard–Oeschger 

(D–O) oscillations of the last 

glacial period. The procedure is based on the 

assumption that the rapid changes in dust are 

associated with large-scale changes in atmospheric 

transport and implies that D–O oscillations 

(in terms of their atmospheric imprint) 

are more symmetric in form than can be inferred 

from Greenland temperature records. 

After removal of the abrupt shifts the residual, 

dejumped dust record is found to match Antarctic 

climate variability with a temporal lag 

of several hundred years. It is argued that such 

variability may reflect changes in the source 

region of Greenland dust (thought to be the 

deserts of eastern Asia). Other records from 

this region and more globally also reveal Antarctic-style 

variability and suggest that this 

signal is globally pervasive. This provides the 

potential basis for suggesting a more important 

role for gradual changes in triggering more 

abrupt transitions in the climate system. 

2008010599 

塔里木西南乌恰群基干剖面及时代讨论 = 

Jigan section of Wuqia Group at the southwestern 

Tarim basin and its age discussion. 

( 中文 ). 周永昌 ; 刘百春 ; 袁定国 . 新疆地 

质 , 2002, 20(S1): 72-77 

塔里木盆地西南地区乌恰群可划分为 3 

个组 , 自下而上为克孜洛依组、安居安组、 

帕卡布拉克组 . 基干剖面包括 : 天山山前喀什 

区乌恰剖面 , 西昆仑山前英吉莎南区伊里亚 

斯沟剖面 , 昆仑弧弯叶城皮山区甫沙剖面 . 划 

分对比标志主要有 : 沉积物粒度旋回、标志 

层、岩性颜色组合、矿物和微量元素、古 

生物等 . 通过野外观测对比 , 结合古生物组合 

及接触关系等 , 重新厘定了克孜洛依组底界 

并论证乌恰群时代为新近纪中新世 . 

2008010600 

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