No high Tibetan Plateau until the Neogene

doi:10.1126/sciadv.aav2189

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	No high Tibetan Plateau until the Neogene
	Su, T.1,2; Farnsworth, A.3; Spicer, R. A.1,4; Huang, J.1; Wus, F-X 5; Liu, J.1; Li, S-F 1; Xing, Y-W 1; Huang, Y-J 6; Deng, W-Y-D 1,2; Tang, H.1,2; Xu, C-L 1,2; Zhao, F.1,2; Srivastava, G.7; Valdes, P. J.3; Deng, T.5 ; Zhou, Z-K 1,6
	2019-03-01
发表期刊	SCIENCE ADVANCES
ISSN	2375-2548
卷号	5 期号:3 页码:8
摘要	The Late Paleogene surface height and paleoenvironment for the core area of the Qinghai-Tibetan Plateau (QTP) remain critically unresolved. Here, we report the discovery of the youngest well-preserved fossil palm leaves from Tibet. They were recovered from the Late Paleogene (Chattian), ca. 25.5 +/- 0.5 million years, paleolake sediments within the Lunpola Basin (32.033 degrees N, 89.767 degrees E), central QTP at a present elevation of 4655 m. The anatomy of palms renders them intrinsically susceptible to freezing, imposing upper bounds on their latitudinal and altitudinal distribution. Combined with model-determined paleoterrestrial lapse rates, this shows that a high plateau cannot have existed in the core of Tibet in the Paleogene. Instead, a deep paleovalley, whose floor was <2.3 km above mean sea level bounded by (>4 km) high mountain systems, formed a topographically highly varied landscape. This finding challenges prevailing views on tectonic processes, monsoon dynamics, and the evolution of Asian biodiversity.
DOI	10.1126/sciadv.aav2189
关键词[WOS]	LUNPOLA BASIN ; ASIAN MONSOON ; OLIGOCENE ; EOCENE ; PALEOELEVATION ; QIANGTANG ; NORTHERN ; HIMALAYA ; CLIMATE
收录类别	SCI
语种	英语
资助项目	Strategic Priority Research Program of CAS[XDA20070301] ; Strategic Priority Research Program of CAS[XDA20070203] ; National Natural Science Foundation of China (NSFC)[31470325] ; National Natural Science Foundation of China (NSFC)[31590823] ; National Natural Science Foundation of China (NSFC)[41430102] ; National Natural Science Foundation of China (NSFC)[41872006] ; NSFC-NERC (Natural Environment Research Council of the United Kingdom) joint research program[41661134049] ; NSFC-NERC (Natural Environment Research Council of the United Kingdom) joint research program[NE/P013805/1] ; XTBG International Fellowship for Visiting Scientists ; National Key R&D Program of China[2017YFC0505200] ; Key Research Program of Frontier Sciences, CAS[QYZDB-SSW-SMC016] ; Youth Innovation Promotion Association, CAS[2017439] ; Youth Innovation Promotion Association, CAS[2017103] ; CAS 135 program[2017XTBG-F01]
WOS研究方向	Science & Technology - Other Topics
WOS类目	Multidisciplinary Sciences
WOS记录号	WOS:000462564300055
出版者	AMER ASSOC ADVANCEMENT SCIENCE
引用统计	被引频次：190[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://119.78.100.205/handle/311034/9522
专题	中国科学院古脊椎动物与古人类研究所
通讯作者	Su, T.; Zhou, Z-K
作者单位	1.Chinese Acad Sci, Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Mengla 666303, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Univ Bristol, Sch Geog Sci, Bristol BS8 1SS, Avon, England 4.Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes MK7 6AA, Bucks, England 5.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China 6.Chinese Acad Sci, Kunming Inst Bot, Key Lab Plant Divers & Biogeog East Asia, Kunming 650204, Yunnan, Peoples R China 7.Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India
推荐引用方式 GB/T 7714	Su, T.,Farnsworth, A.,Spicer, R. A.,et al. No high Tibetan Plateau until the Neogene[J]. SCIENCE ADVANCES,2019,5(3):8.
APA	Su, T..,Farnsworth, A..,Spicer, R. A..,Huang, J..,Wus, F-X.,...&Zhou, Z-K.(2019).No high Tibetan Plateau until the Neogene.SCIENCE ADVANCES,5(3),8.
MLA	Su, T.,et al."No high Tibetan Plateau until the Neogene".SCIENCE ADVANCES 5.3(2019):8.

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