KMS Institute of Vertebrate Paleontology and Paleoanthropology
No high Tibetan Plateau until the Neogene | |
Su, T.1,2; Farnsworth, A.3; Spicer, R. A.1,4; Huang, J.1; Wus, F-X5; Liu, J.1; Li, S-F1; Xing, Y-W1; Huang, Y-J6; Deng, W-Y-D1,2; Tang, H.1,2; Xu, C-L1,2; Zhao, F.1,2; Srivastava, G.7; Valdes, P. J.3; Deng, T.5; Zhou, Z-K1,6 | |
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 | |
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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