Major turnover of biotas across the Oligocene/Miocene boundary on the Tibetan Plateau

doi:10.1016/j.palaeo.2021.110241

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	Major turnover of biotas across the Oligocene/Miocene boundary on the Tibetan Plateau
	Deng, Tao 2,3,4; Wu, Feixiang 3,4; Wang, Shiqi 2,3,4; Su, Tao 1,2; Zhou, Zhekun 1
刊名	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
	2021-04-01
卷号	567 页码:12
关键词	Cenozoic Plant Animal Terrestrial ecosystem Tectonic uplift Climate change
ISSN号	0031-0182
DOI	10.1016/j.palaeo.2021.110241
通讯作者	Deng, Tao(dengtao@ivpp.ac.cn)
英文摘要	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.
资助项目	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] ; Second Comprehensive Scientific Expedition on the Tibetan Plateau[2019QZKK0705] ; Frontier Science Key Research Project[QYZDY-SSW-DQC022] ; National Natural Science Foundation of China[41430102] ; International Partnership Program[GJHZ1885]
WOS研究方向	Physical Geography ; Geology ; Paleontology
语种	英语
出版者	ELSEVIER
WOS记录号	WOS:000636761000012
资助机构	Strategic Priority Research Program of the Chinese Academy of Sciences ; Second Comprehensive Scientific Expedition on the Tibetan Plateau ; Frontier Science Key Research Project ; National Natural Science Foundation of China ; International Partnership Program
内容类型	期刊论文
源URL	[http://119.78.100.205/handle/311034/18472]
专题	古脊椎动物与古人类研究所_图书馆1
通讯作者	Deng, Tao
作者单位	1.Chinese Acad Sci, Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Mengla 666303, Yunnan, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 3.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China 4.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China
推荐引用方式 GB/T 7714	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,2021,567:12.
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,567,12.
MLA	Deng, Tao,et al."Major turnover of biotas across the Oligocene/Miocene boundary on the Tibetan Plateau".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 567(2021):12.