KMS Nanjing Institute of Geology and Palaeonotology,CAS
Can the Lilliput Effect be detected in the brachiopod faunas of South China following the terminal Ordovician mass extinction? | |
Huang, Bing (黄冰)1; Harper, David A. T.2; Zhan, Renbin (詹仁斌)1; Rong, Jiayu (戎嘉余)1 | |
2010-01-15 | |
发表期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY |
ISSN | 0031-0182 |
卷号 | 285期号:3-4页码:277-286 |
摘要 | In the immediate aftermath of global extinctions, organisms were normally much smaller than those prior to these events. This 'Lilliput Effect' can be subdivided into two types: 1) a specific type, following the original definition of the effect which targets species-level taxa associated with inhospitable environments, and 2) a more general type, related to the reactions of higher-rank taxa above the species-level. The body sizes of brachiopods from South China through the Ordovician and Silurian transition (Late Katian, Hirnantian, and earliest Rhuddanian) are compared at generic, superfamilial, ordinal, and class levels. The results indicate that the body sizes of the taxa of lower rank (e.g. genus-level) are highly variable within these different intervals. The type of evidence for the Lilliput Effect through the end Ordovician mass extinction is thus quite different from that of the end Permian mass extinction probably reflecting differences in the intensity of these two major bioevents. However, the relationships between the contrasting trends in body-size change of some taxa. of higher rank (e.g. at the ordinal-level) and the relative dominance of these taxa in the latest Ordovician and earliest Silurian suggest that the brachiopods of the two major Ordovician groups, the strophomenoids and orthoids. adopted different survival strategies during and immediately after the crisis from those of the pentamerides and rhynchonellides, that were common in Silurian assemblages. (C) 2009 Elsevier B.V. All rights reserved. |
关键词 | Mass Extinction Survival Lilliput Effect Ordovician South China |
DOI | 10.1016/j.palaeo.2009.11.020 |
语种 | 英语 |
关键词[WOS] | End-permian Extinction ; Body-size ; Paleozoic Brachiopods ; Recovery ; Survival ; Crisis ; Transition ; Strategies ; Evolution ; Conodonts |
资助项目 | NSFC[J0630967] ; National Natural Science Foundation of China[40772002] ; Chinese Academy of Sciences[KZCX2-YW-Q05-01] ; Ministry of Science and Technology of China[2006CB806402] ; Ministry of Science and Technology of China[2006FY120300-5] ; State Key Laboratory of Palaeobiology and Stratigraphy[20081103] ; Geobiodiversity Database ; Danish Council for Independent Research ; Natural Sciences (FNU) |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS记录号 | WOS:000273930200012 |
项目资助者 | NSFC ; National Natural Science Foundation of China ; Chinese Academy of Sciences ; Ministry of Science and Technology of China ; State Key Laboratory of Palaeobiology and Stratigraphy ; Geobiodiversity Database ; Danish Council for Independent Research ; Natural Sciences (FNU) |
出版者 | ELSEVIER SCIENCE BV |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/381 |
专题 | 中国科学院南京地质古生物研究所 其他 |
通讯作者 | Huang, Bing (黄冰) |
作者单位 | 1.Chinese Acad Sci, State Key Lab Paleobiol & Stratig, Nanjing Inst Geol & Paleontol, Nanjing 210008, Peoples R China 2.Univ Copenhagen, Geol Museum, DK-1350 Copenhagen, Denmark |
推荐引用方式 GB/T 7714 | Huang, Bing ,Harper, David A. T.,Zhan, Renbin ,et al. Can the Lilliput Effect be detected in the brachiopod faunas of South China following the terminal Ordovician mass extinction?[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2010,285(3-4):277-286. |
APA | Huang, Bing ,Harper, David A. T.,Zhan, Renbin ,&Rong, Jiayu .(2010).Can the Lilliput Effect be detected in the brachiopod faunas of South China following the terminal Ordovician mass extinction?.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,285(3-4),277-286. |
MLA | Huang, Bing ,et al."Can the Lilliput Effect be detected in the brachiopod faunas of South China following the terminal Ordovician mass extinction?".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 285.3-4(2010):277-286. |
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