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sediments of the Zhuravka and Abrosimovo horizons (upper Oligocene, lower Miocene), the Pseudokomewuia Beds are included into local stratigraphic scheme. According to results of comparative analysis, similar and distinctive features of Oligocene-Miocene dinocyst assemblages from West Siberia, China and North America are elucidated. Based on palynological data, the local stratigraphic scheme of higher resolution is suggested for subdivision of Oligocene and Miocene deposits in southern part of West Siberia (Baraba and Kulunda lithofacies regions). 2009020079 阿根廷圣胡安省 La Herradura 溪晚古生代沉积 (Tupe 组 ) 孢粉 = Palynology of late Palaeozoic sediments (Tupe Formation) at La Herradura Creek, San Juan province, Argentina. ( 英文 ). Verge M. Alcheringa, 2008, 32(4): 339 - 352 Palynomorph assemblages recovered from the Tupe Formation at La Herradura Creek, San Juan province, Argentina, are analysed. The middle section of the sequence includes a marine fossiliferous interval belonging to the Tivertonia jachalensis-Streptorhynchus inaequiornatus (T-S) Faunal Biozone, recently ascribed an Early Permian age. The section below the marine fossiliferous unit yielded palynofloras typical of previously described 'Tupense' assemblages. The palynoflora recovered from beds above the marine horizon is diverse, relatively well preserved and includes species never recorded from the Tupe Formation. This latter palynoassemblage includes species diagnostic of Early Permian palynofloras such as Converrucosisporites confluens (Archangelsky & Gamerro) Playford & Dino, Pseudoreticulatispora pseudoreticulata (Balme & Hennelly) Bharadwaj & Srivastava, Horriditriletes ramosus (Balme & Hennelly) Bharadwaj & Salujha, Anapiculatisporites tereteangulatus (Balme & Hennelly) Playford & Dino, Laevigatosporites colliensis (Balme & Hennelly) Venkatachala & Kar, Marsupipollenites triradiatus Balme & Hennelly, Protohaploxypinus sewardii (Virkki) Hart and Pakhapites fusus (Bose & Kar) Men ndez. Correlations with assemblages from western Argentina and other Gondwanan regions suggest an Early Permian age (not older than Asselian-Sakmarian) for the upper part of the sequence, supporting the age attributed to the T-S Biozone 2009020080 阿根廷圣克鲁斯省下白垩统阿普特阶 Punta del Barco 组孢粉研究 — 系统描述 II: 具极部突起、网脊、三突具周壁三缝孢 , 及其古生态意义 = Palynological study of the Punta del Barco Formation, lower cretaceous (Aptian) of Santa Cruz Province, Argentina. Systematic descriptions II: Apiculate, murornate, tricrassate and perinate trilete spores. Paleoecological implications. ( 其他 ). Llorens M. Ameghiniana, 2008, 45(2): 273-288 Eighteen species of disperse trilete apiculate, murornate, tricrassate and perinate spores from the Punta del Barco Formation, in the Meseta Baquero area, Lower Cretaceous of Santa Cruz Province, are described. They belong to the genera Gleicheniidites, Clavifera, Ornamentifera, Ceratosporites, Concavissimisporites, Staplinisporites, Retitriletes and Lygodiidites. Besides, a new genus for a perisporate spore -Capsispora- is proposed, an indeterminate apiculate form and two new species of the genus Gleicheniidites, are described. Finally, some paleoecological implications are given from the study of this spores association, which are related to stress conditions by the strong volcanic activity during the sedimentary deposition of this unit. 2009020081 澳大利亚东南部白垩纪最晚期沉积山龙眼型花粉 = Pollen of proteaceous-type from latest Cretaceous sediments, southeastern Australia. ( 英文 ). Dettmann M E; Jarzen D M. Alcheringa, 1996, 20(2): 103 - 160 Abundant and diverse proteaceous-like triaperturate pollen from Campanian- Maastrichtian sediments in the Otway Basin, southeastern Australia are systematically documented and compared with pollen of extant Proteaceae. Segregation of fossil and extant pollen types has been effected on apertural characters of which six states have been identified. Apertures are colpoid, poroid or porate. Pores of Propylipollis Martin & Harris, 1974 conform with those of subfamilies Grevillioideae and Carnarvonioideae. Colpoids of Beaupreaidites Cookson emend. Martin, 1973, poroids of Lewalanipollis gen. nov., and pores of Cranwellipollis Martin & Harris, 1974 are represented in subfamilies Proteoideae and Persoonioideae. Pores of Proteacidites Cookson ex Couper, 1953 occur in 26
subfamilies Proteoideae and Sphalmioideae. In the Otway Basin fossil record, triporate apertures appear earlier than tricolpoids, triporoids and biporates; and diversity levels of proteaceous pollen are higher than reported from elsewhere implying the region may have been a diversification centre during Campanian and Maastrichtian times. Represented among the fossil pollen are types that conform with pollen of extant Proteaceae: Adenanthos, Beauprea, Beaupreopsis, and Stirlingia (subfamily Proteoideae); Persoonia (subfamily Persoonioideae); Carnarvonia (subfamily Carnarvonioideae); and Bleasdalia, Grevillea, Knightia, Macadamia and Telopea (subfamily Grevillioideae). The Late Cretaceous pollen record thereby implies the presence of sclerophyll and rainforest taxa in a vegetation which was composed of diverse podocarps (Dacrydium, Dacrycarpus, Lagarostrobos, Podocarpus, Microcachrys), araucarians, and a range of angiosperms (Nothofagus, Gunnera, Ilex, Ascarina, Callitriche, Trimeniaceae, Winteraceae, Ranunculaceae and possibly Epacridaceae). Thirty-one pollen species are described and referred to five genera, of which Lewalanipollis is new. New species include Lewalanipollis senectus, L. trycheros, Propylipollis areolatus, P. crotonoides, Proteacidites cooksoniae and Proteacidites variverrucatus. 2009020082 阿根廷里奥布兰科密西西比亚 Cortaderas 组系统孢粉研究 , 第二部分 = Systematic palynological study of the Cortaderas Formation, (Mississippian) Rio blanco Basin, Argentina. Part two. ( 英文 ). Loinaze V P. Ameghiniana, 2008, 45(2): 421-441 Well preserved Mississippian palynological assemblages have been obtained from the Cortaderas Formation in the Rio Blanco Basin, northwestern Argentina. In this second contribution, twenty-eight from a total of seventy-eight spore species are described. A new species of trilete spores is proposed: Densosporites scalabrinii sp. nov. Worldwide geographic and stratigraphic records of taxa are analysed. The Cortaderas Formation is dated as late Visean in age based on the presence of species of potential stratigraphic relevance, such as Reticulatisporites magnidictyus Playford and Helby, Verrucosisporites quasigobbettii Playford and Helby and Rugospora australiensis (Playford and Helby) Jones and Truswell and the absence of pollen grains. The samples collected in the uppermost level of this unit, contain some of spores typical of the Upper Carboniferous of Argentina and Brazil, although pollen grains are still absent. 2009020083 阿根廷西北部 Las Conchas Creek 地区晚白垩世萨尔塔群盆地 Las Curtiembres 组的孢粉 = Palynology of the Las Curtiembres Formation (Late Cretaceous, Salta Group Basin), Las Conchas Creek area, northwestern Argentina. ( 英文 ). Narvaez P L; Sabino I F. Ameghiniana, 2008, 45(2): 473-482 This study provides the first palynologic record of the Las Curtiembres Formation (Late Cretaceous, Salta Group Basin) in northwestern Argentina. Two palynologically productive samples were obtained from the Morales Member in the area of the Las Conchas creek, Salta Province. Nineteen morphospecies are recorded for the Formation. The samples show poor preservation of the specimens and low diversity. The palynomorph association is characterized by the prevalence of species that belong to the Ephedraceae (6 species with 57% of total abundance), possibly suggesting semiarid conditions and a warm-dry paleoclimate at the time of deposition. Low humidity could also be inferred from the low abundance and diversity of pteridophyte species and the presence of Cheirolepidiaceae (Classopollis sp.) and Proteaceae (Peninsulapollis gilhi (Cookson) Dettmann and Jarzen). The pollen grain Peninsulapollis gilhi is a chronostratigraphic indicator of an age not older than Campanian-Maastrichtian, which would be coincident with the previous dating (77 +/- 5 Ma) of the Las Conchas Basalt effusions. 2009020084 阿根廷巴塔哥尼亚利马河东南侧晚三叠世 Paso Flores 组孢粉记录 = Palynological record of the Paso Flores Formation (Late Triassic) on the southeastern side of the Limay River, Patagonia, Argentina. ( 英文 ). Zavattieri A; Meg N. Ameghiniana, 2008, 45(2): 483- 502 Well-preserved spore-pollen assemblages from the type locality of the Paso Flores Formation, in the Estancia Paso Flores area, on the southeastern side of the Limay River, northern Patagonia, Argentina, are presented in this contribution. In this area, the Paso 27
Page 2 and 3: 第 5 卷第 2 期古生物学
Page 4 and 5: calcite in 38% sulphuric acid. The
Page 6 and 7: 2009020010 细胞过度生长
Page 8 and 9: edistribution of continents, orogen
Page 10 and 11: Turner E C; Burdige D J. Geology, 2
Page 12 and 13: 遗迹化石 2009020028 美国
Page 14 and 15: trackways from Fumanya (south-east
Page 16 and 17: 华盛顿奥林匹克半岛
Page 18 and 19: sequenced and analysed the genome o
Page 20 and 21: estuarine sediments: Chezzetcook In
Page 22 and 23: preserved in the gypsum crystals of
Page 24 and 25: 文 ). Lian O B; Mathewes R W; Hico
Page 26 and 27: Lower Cretaceous of Santa Cruz prov
Page 30 and 31: Flores Formation is exposed along t
Page 32 and 33: egion in Late Permian times was pro
Page 34 and 35: Chlorogloeaopsis contexta, Obruchev
Page 36 and 37: deposition of organic-rich, low-oxy
Page 38 and 39: 东攀剖面二叠纪末期
Page 40 and 41: econcile with Ediacaran trace and b
Page 42 and 43: 2009020121 中国西北兰州
Page 44 and 45: Paleontologica Argentina, 2008, 45(
Page 46 and 47: 始新世至中始新世早
Page 48 and 49: assemblage is highly dominated by m
Page 50 and 51: Creek Limestone of the Molong High.
Page 52 and 53: 木属的 3 个同名 Cyclostig
Page 54 and 55: Ceratopteris are from the Eocene of
Page 56 and 57: covering of the spore mass. Ultrast
Page 58 and 59: Southern Floristic Province. It imp
Page 60 and 61: An anatomically preserved mature st
Page 62 and 63: and predation between the two ocean
Page 64 and 65: endemic or Andean forms and others
Page 66 and 67: islands" (Taylor and Wilson, 2003)
Page 68 and 69: analysis, SHE Community Structure I
Page 70 and 71: 2009020208 安第斯火地岛
Page 72 and 73: Miolepidocyclina, Nephrolepidina, E
Page 74 and 75: alaskensis n. gen. and sp., Virgula
Page 76 and 77: y the fissispongiid Fissispongia ja
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to a revival of Kiderlen's (1937) h
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gentle and slow extinction speed an
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Two new bryozoan species are descri
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onset of Lopingian recovery/radiati
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ut also found in the paterinates. I
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is reinstated as the reference for
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three species are widespread in the
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Caenogastropoda displayed considera
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Western Canada Province of the Old
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originally referred to Cypraea cont
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the Late Triassic mass extinction b
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of septal folding is still, however
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subspecies originally referred to a
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persisting in the Dry Valleys until
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Great Estuarine Group (Jurassic) of
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have been extended as a result of t
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Otekaike Limestone an inner shelf e
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arthropods (Notostraca and Insecta:
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with a lichenocrinid holdfast, and
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Gotland, in Homerian (upper Wenlock
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terms of growth and development. Gr
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characterises the genus Ditrupa and
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Middle-Late Devonian. A new onychod
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hachirhinchus. Here, we describe ne
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segmented pectoral fin. The small u
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两栖类离片椎类中褶
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南非卡洛下三叠统 Kat
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Formation (Lower - Middle Campanian
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traits evolved in Theropoda. Our re
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2009020428 联合王国威尔
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vestigial or absent 'A' horn-cores,
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anterior dorsal vertebrae and proba
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2009020449 谢佩岛下始新
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Ka BP. Canids in this assemblage in
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collaboration avec le regrett é Pr
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Eucyon remains from the Pliocene Ar
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Megatheriidae) from the Arroyo Chas
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The trilophodont gomphothere group
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oldest representative of Eobaatar i
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ugose, almost spongy aspect; suture
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Neues Jahrbuch fur Geologie u. Pala
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ca 500 kyr toward the precessional
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subdivided in detail in Russia shou
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sediments were deposited in an intr
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Group 1 gneiss-migmatitic rocks (ca
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and implies that these two continen
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1.6 Ma, that is to say, the isotopi
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millipede remains. A review of the
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Kimmeridgian-early Tithonian, Titho
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2009020548 藏东南特提斯
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events and their induced harsh envi
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esearchers, here we suggest that th
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adjacent paleosols that differ in t
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generally consistent northeast tren
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Palaeoclimatology Palaeoecology, 20
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stratigraphic context. Nevertheless
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esponsible for fossil orientation:
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sulfide assemblages in them, of Cen
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south of the island. The occurrence
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ecords in the Jiuquan Basin, northw
Page 198 and 199:
Myr younger than hitherto considere
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