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Major turnover of biotas across the Oligocene/Miocene boundary on the Tibetan Plateau
Deng, Tao1,2,3; Wu, Feixiang1,2; Wang, Shiqi1,2,3; Su, Tao3,4; Zhou, Zhekun4
2021-04-01
发表期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
卷号567期号:0页码:12
摘要In this paper, we review evidence for a major biotic turnover across the Oligocene/Miocene in the Tibetan Plateau region. Based on the recent study of six well-preserved fossil sites from the Cenozoic Lunpola and Nima basins in the central Tibetan Plateau, we report a regional changeover from tropical/subtropical ecosystems in the Late Oligocene ecosystem (26-24 Ma) to a cooler, alpine biota of the Early Miocene (23-18 Ma). The Late Oligocene fossil biota, comprising of fish (climbing perch), insects and plants (palms), shows that the hinterland of the Tibetan Plateau was a warm lowland influenced by tropical humidity from the Indian Ocean. In the Early Miocene, the regional biota became transformed, with the evolution and diversification of the endemic primitive snow carp. Early Miocene vegetation was dominated by temperate broad-leaved forest with abundant conifers and herbs under a cool climate, and mammals included the hornless rhinoceros, Plesiaceratherium, a warm temperate taxon. This dramatic ecosystem change is due to a cooling linked to the uplift of Tibetan region, from a Late Oligocene paleo-elevation of no greater than 2300 m a.s.l. in the sedimentary basin to a paleo-elevation of about 3000 m a.s.l. Another factor was the Cenozoic global climatic deterioration toward to an ice-house world.
关键词Cenozoic Plant Animal Terrestrial ecosystem Tectonic uplift Climate change
DOI10.1016/j.palaeo.2021.110241
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China[41430102] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA20070203] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA20070301] ; Frontier Science Key Research Project[QYZDY-SSW-DQC022] ; International Partnership Program[GJHZ1885] ; Second Comprehensive Scientific Expedition on the Tibetan Plateau[2019QZKK0705]
WOS研究方向Physical Geography ; Geology ; Paleontology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS记录号WOS:000636761000012
出版者ELSEVIER
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文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/18473
专题中科院古脊椎所(2000年以后)
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.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Mengla 666303, Yunnan, Peoples R China
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Deng, Tao,Wu, Feixiang,Wang, Shiqi,et al. Major turnover of biotas across the Oligocene/Miocene boundary on the Tibetan Plateau[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2021,567(0):12.
APA Deng, Tao,Wu, Feixiang,Wang, Shiqi,Su, Tao,&Zhou, Zhekun.(2021).Major turnover of biotas across the Oligocene/Miocene boundary on the Tibetan Plateau.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,567(0),12.
MLA Deng, Tao,et al."Major turnover of biotas across the Oligocene/Miocene boundary on the Tibetan Plateau".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 567.0(2021):12.
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