KMS Institute of Vertebrate Paleontology and Paleoanthropology
Tetrapod turnover during the Permo-Triassic transition explained by temperature change | |
Liu, Jun1,2,3; Abdala, Fernando4,5; Angielczyk, Kenneth D.5,6; Sidor, Christian A.7,8 | |
2022 | |
发表期刊 | EARTH-SCIENCE REVIEWS |
ISSN | 0012-8252 |
卷号 | 224期号:0页码:10 |
摘要 | Global temperatures significantly changed from the late Permian to the Early Triassic: the Earth transformed from a cool world to a hothouse climate. This transition undoubtedly had a strong impact on tetrapod physiology and distribution. During the global cooling, tetrapods generally increased their size; and the currently recognized late Permian tetrapod extinction, exemplified by the record preserved in the South African Karoo Basin, occurred in the late stage of cooling. Rapid warming in the Early Triassic is predicted to have resulted in extinctions and/ or local extirpation of low latitude tetrapods, but the very limited fossil record from this region makes testing this hypothesis difficult. Warming is predicted to have had less negative impacts on the tetrapod diversity of mid latitudes, and promoted the success of tetrapods in the high latitudes. Based on the known fossil record, a tetrapod gap could have existed in central Pangea between similar to & nbsp;30(?)degrees N and similar to & nbsp;40(?)degrees S, and lasting from the Induan to the early Spathian. However, the exact boundaries of this gap likely varied over time, and it could have encompassed a larger area during the hottest phases (Griesbachian and near the Smithian-Spathain boundary). |
关键词 | P/Tr Permo-Triassic extinction Tetrapoda Lystrosaurus Dicynodontia Climate change |
DOI | 10.1016/j.earscirev.2021.103886 |
关键词[WOS] | ZONE BEAUFORT GROUP ; MAMMAL-LIKE REPTILE ; KAROO BASIN ; SOUTH-AFRICA ; EARLIEST EVIDENCE ; MASS EXTINCTION ; BOUNDARY ; BIOSTRATIGRAPHY ; SUPERGROUP ; THERAPSIDA |
收录类别 | SCI |
语种 | 英语 |
资助项目 | Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000] ; International Partnership Program of Chinese Academy of Sciences[132311KYSB20190010] ; CONICET (Argentina) ; National Research Foundation (South Africa) |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000786657900002 |
出版者 | ELSEVIER |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.205/handle/311034/22049 |
专题 | 中科院古脊椎所(2000年以后) |
通讯作者 | Liu, Jun |
作者单位 | 1.Chinese Acad Sci, Key Lab Vertebrate Evolut & Human Origins, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 2.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 4.Conicet Fdn Miguel Lillo, Unidad Ejecutora Lillo, Miguel Lillo 251, San Miguel De Tucuman, Argentina 5.Univ Witwatersrand, Evolutionary Studies Inst, ZA-2050 Johannesburg, South Africa 6.Field Museum Nat Hist, Negaunee Integrat Res Ctr, Chicago, IL 60605 USA 7.Univ Washington, Burke Museum, Seattle, WA 98195 USA 8.Univ Washington, Dept Biol, Seattle, WA 98195 USA |
推荐引用方式 GB/T 7714 |
Liu, Jun,Abdala, Fernando,Angielczyk, Kenneth D.,et al. Tetrapod turnover during the Permo-Triassic transition explained by temperature change [J]. EARTH-SCIENCE REVIEWS,2022,224(0):10. |
APA |
Liu, Jun,Abdala, Fernando,Angielczyk, Kenneth D.,&Sidor, Christian A..(2022). Tetrapod turnover during the Permo-Triassic transition explained by temperature change .EARTH-SCIENCE REVIEWS,224(0),10. |
MLA |
Liu, Jun,et al." Tetrapod turnover during the Permo-Triassic transition explained by temperature change ".EARTH-SCIENCE REVIEWS 224.0(2022):10. |
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