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Review: Implications of vertebrate fossils for paleo-elevations of the Tibetan Plateau
Deng, Tao1,2,3,4; Wang, Xiaoming1,5; Wu, Feixiang1,2; Wang, Yang6,7; Li, Qiang1,2,3; Wang, Shiqi1,2,3; Hou, Sukuan1,2
2019-03-01
发表期刊GLOBAL AND PLANETARY CHANGE
ISSN0921-8181
卷号174期号:0页码:58-69
摘要The uplift of the Tibetan Plateau is an important geological event, but there is considerable controversy about its growth history. Different geological observations contribute to this controversial issue, while data from geochemistry, tectonics, and paleontology further fuel the debate. Vertebrate fossils have provided significant evidence for documenting the uplift of the Tibetan Plateau in the geologic past. The earliest fossil evidence recently collected from the Oligocene Dingqing Formation in central Tibet includes the climbing perch and cyprinine fish fossils whose modern close relatives are distributed in the tropical zone of Asia and Africa. These discoveries not only are significant for the phylogeny and zoogeography of fishes, but also imply that the hinterland of the Tibetan Plateau was a warm and humid lowland at similar to 26 Ma. The co-existing plant assemblage, which includes palms and golden rain trees among others, indicates that the warm and humid airs from the Indian Ocean could flow deeply into central Tibet, consistent with the inference from the fish fossils. Since that time, the geographical features and natural environments within the Tibetan Plateau have greatly changed. The Tibetan Plateau was consistently uplifted in the Early Miocene and reached an elevation of similar to 3000 m, which was demonstrated by fish, mammal, and plant fossils. The endemic schizothoracines (snow carps) originated from the Miocene when the Tibetan Plateau turned into a barrier for mammalian migrations between north and south sides. A series of fish and mammal fossils provided unequivocal evidence that the Tibetan Plateau uplifted close to its modern elevation in the Pliocene and developed a cryospheric environment. As a result, the plateau region became the origination center for the cold-adapted Quaternary Ice Age fauna.
关键词Tibetan Plateau Paleo-elevation Vertebrate fossil Fish Mammal Plant
DOI10.1016/j.gloplacha.2019.01.005
关键词[WOS]KUNLUN PASS BASIN ; LUNPOLA BASIN ; SOUTHERN TIBET ; ASIAN MONSOON ; EARLY MIOCENE ; STABLE-ISOTOPES ; NORTHERN TIBET ; PALEOALTIMETRY ; UPLIFT ; PALEOELEVATION
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China[41430102] ; Chinese Academy of Science[XDA20070203] ; Chinese Academy of Science[XDB26000000] ; Chinese Academy of Science[QYZDY-SSW-DQCO22] ; Chinese Academy of Science[GJHZ1885]
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000461411900006
出版者ELSEVIER SCIENCE BV
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/9464
专题中国科学院古脊椎动物与古人类研究所
通讯作者Deng, Tao
作者单位1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China
2.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.Univ Chinese Acad Sci, Sch Earth Sci, Beijing 100039, Peoples R China
5.Nat Hist Museum Los Angeles Cty, Los Angeles, CA 90007 USA
6.Florida State Univ, Dept Earth Ocean & Atmospher Sci, Tallahassee, FL 32306 USA
7.Jinan Univ, Inst Groundwater & Earth Sci, Guangzhou 510632, Guangdong, Peoples R China
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Deng, Tao,Wang, Xiaoming,Wu, Feixiang,et al. Review: Implications of vertebrate fossils for paleo-elevations of the Tibetan Plateau[J]. GLOBAL AND PLANETARY CHANGE,2019,174(0):58-69.
APA Deng, Tao.,Wang, Xiaoming.,Wu, Feixiang.,Wang, Yang.,Li, Qiang.,...&Hou, Sukuan.(2019).Review: Implications of vertebrate fossils for paleo-elevations of the Tibetan Plateau.GLOBAL AND PLANETARY CHANGE,174(0),58-69.
MLA Deng, Tao,et al."Review: Implications of vertebrate fossils for paleo-elevations of the Tibetan Plateau".GLOBAL AND PLANETARY CHANGE 174.0(2019):58-69.
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