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第 5 卷第 2 期古生物学文摘 ( 网络版 ) 目录 2009 年 6 月古生物学综论 ………………………(1) 遗迹化石 …………………(9) 分子古生物学 ……………(14) 古生态学 …………………(15) 微体古生物学综论 ………………………(19) 孢粉 ………………………(21) 疑源类 ……………………(30) 牙形石 ……………………(32) 小壳化石 …………………(37) 古植物学综论 ………………………(38) 藻类 ………………………(43) 地衣植物与苔藓植物 ……(48) 蕨类植物 ( 广义 )………(49) 早期种子植物 ……………(52) 裸子植物 …………………(54) 被子植物 …………………(56) 古无脊椎动物学综论 ………………………(58) 原生动物 …………………(62) 古杯、多孔及腔肠动物 …(70) 苔藓动物 …………………(78) 腕足动物 …………………(80) 软体动物 …………………(87) 节肢动物 …………………(98) 棘皮动物 …………………(110) 笔石动物 …………………(112) 分类位置不明 ……………(114) 古脊椎动物学综论 ………………………(116) 鱼类 ………………………(118) 两栖类 ……………………(123) 爬行类 ……………………(125) 鸟类 ………………………(137) 哺乳类 ……………………(139) 古人类学古人类学 …………………(155) 历史地质学、地层学综论 ………………………(155) 古地理学、古气候学 ……(156) 前古生界 …………………(157) 古生界 ……………………(165) 中生界 ……………………(168) 新生界 ……………………(177)
第 5 卷第 2 期古生物学文摘 ( 网络版 ) 2009 年 6 月古生物学综论 2009020001 新加里东岛 : 一个很老的进化的源泉 = New Caledonia: a very old Darwinian island. ( 英文 ). Grandcolas P; Murienne J; Robillard T. Philosophical Transactions of the Royal Society B: Biological Sciences, 2008, 363(1508): 3309-3317 New Caledonia has generally been considered a continental island, the biota of which largely dates back to Gondwanan times owing to its geological origin and the presence of phylogenetic relicts. This view is contradicted by geological evidence indicating long Palaeocene and Eocene submersions and by recent biogeographic and phylogenetic studies, with molecular or geophysical dating placing the biota no older than the Oligocene. Phylogenetic relicts do not provide conclusive information in this respect, as their presence cannot be explained by simple hypotheses but requires assumption of many ad hoc extinction events. The implication of this new scenario is that all the New Caledonian biota colonized the island since 37Ma Local richness can be explained by local radiation and adaptation after colonization but also by many dispersal events, often repeated within the same groups of organisms. Local microendemism is another remarkable feature of the biota. It seems to be related to recent speciation mediated by climate, orography, soil type and perhaps unbalanced biotic interactions created by colonization disharmonies. New Caledonia must be considered as a very old Darwinian island, a concept that offers many more fascinating opportunities of study. 2009020002 “ 分支分类 23” 中的争论问题 : 达尔文的系统演化关系理论 = Problematic issues of cladistics 23: Darwin's concept of phylogenetic relationship. ( 英文 ). Reif W-E. Neues Jahrbuch fur Geologie u. Palaontologie / Abhandlungen, 2007, 244(2): 227-245 Darwin discovered that, in the light of the therory of descent with modification, the interrelationships of the taxonomic groups in the Natural System become understandable as real, phylogenetic relationships (PhR) , and that all taxonomic group and the hierarchical structure of the organic diversity are real, rather than arbitrary. To make the notion of PhR understandable, he postulated a very close relationship between PhR and blood relationship among persons. As he failed to discriminate sharply between general PhR, relative PhR and absolute Phr he did not realize that systematics works only with relative PhR and that his postulate that "classifications will eventually become genealogies" could, at least in the literal sense, lnever come true. 2009020003 达尔文的两难选择 : 第一个种与显生宙多样性的假单源性原则 = The Darwinian delemma of the first species and the principle of pseudo-monophyly of Phanerozoic diversity. ( 英文 ). Reif W-E. Neues Jahrbuch fur Geologie u. Palaontologie / Abhandlungen, 2007, 244(3): 371-379 In his publications, Darwin avoided the discussion of the evolutionary origin of the mechanisms of life. his principle to its own unique bauplan and is hence derived from one single ancestor. This leads to the inevitable conclusion that the diversity of the Phanerozoic dates back to a single progenitor species. Hence, Darwin stated that life on Earth started with about 10 first plant and animal species, which is in accordance with the ecological laws. Most of the descendants of most of the first species died out, whereas the remaining ones underwent convergent evolution which led to the unity of type ("pseudo-monophyly"), and divergent evolution which led to the enormous Phanerozoic diversity on the species and on the ecosystem level. 2009020004 一种利用硫酸从石灰岩中提取大化石的新方法 = A new method for the extraction of macrofossils from calcareous rocks using sulphuric acid. ( 英文 ). Vodr á ž ka R. Palaeontology, 2009, 52(1): 187-192 A new method for the extraction of calcified and/or partly pyritized macrofossils has been developed. This method is based upon the differential speeds for the dissolving of microcrystalline and macrocrystalline 1
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 28 and 29: sediments of the Zhuravka and Abros
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.
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木属的 3 个同名 Cyclostig
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Ceratopteris are from the Eocene of
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covering of the spore mass. Ultrast
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Southern Floristic Province. It imp
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An anatomically preserved mature st
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and predation between the two ocean
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endemic or Andean forms and others
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islands" (Taylor and Wilson, 2003)
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analysis, SHE Community Structure I
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2009020208 安第斯火地岛
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Miolepidocyclina, Nephrolepidina, E
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alaskensis n. gen. and sp., Virgula
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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
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Myr younger than hitherto considere
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