Global cooling and enhanced Eocene Asianmid-latitude interior aridity
Li,J.X1,2; Yue, L.P2,3; Roberts, A.P4; Hirt, A.M5; Pan, F1,2; Guo, L(Guo, Lin)1; Xu, Y1; Xi, R.G1; Guo, L(Guo, Lei)1; Qiang, X.K3; Gai,C.C6,7; Jiang, Z.X4,7; Sun, Z.M9; Liu, Q.S10
2018-08
发表期刊NATURE COMMUNICATIONS
卷号9期号:1页码:3026
文章类型期刊论文
摘要Tibetan Plateau uplift has been suggested as the main driving force for mid-latitude Asian inland aridity (AIA) and for deposition of thick aeolian sequences in northern China since the Miocene. However, the relationship between earlier AIA and Tibetan Plateau mountain building is uncertain because of a lack of corresponding thick aeolian sequences with accurate age constraints. We here present results for a continuous aeolian sequence that spans the interval from >51 to 39 Ma from the eastern Xorkol Basin, Altun Shan, northeastern Tibetan Plateau. The basal age of the studied sequence postdates initial uplift of the Tibetan Plateau by several million years. Our results indicate that the local palaeoclimate was teleconnected strongly to the overall global cooling pattern, so that local enhanced aridification recorded by the studied aeolian sequence is dominantly a response to global climatic forcing rather than plateau uplift.
DOI10.1038/s41467-018-05415-x
收录类别SCI
所属项目编号41002052 ; 2016YFA0601903 ; 41430962 ; 41072136 ; 41202133 ; 90814005 ; 1212011121185 ; 201311126 ; DP110105419
语种英语
项目资助者NationalNatural Science Foundation of China ; NationalNatural Science Foundation of China ; National KeyResearch and Development Program of China ; National KeyResearch and Development Program of China ; “Geological Elite Program” of theChina Geological Survey, Land Resources Survey Project ; “Geological Elite Program” of theChina Geological Survey, Land Resources Survey Project ; Nonprofit Special Project of Land Resources ; Nonprofit Special Project of Land Resources ; AustralianResearch Council ; AustralianResearch Council
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文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/5278
专题黄土与第四纪地质国家重点实验室(2010~)
通讯作者Liu, Q.S
作者单位1.Research Center for Orogenic Geology, Xi’an Center of Geological Survey, China Geological Survey, Xi’an 710054, China
2.State Key Laboratory forContinental Dynamics, Department of Geology, Northwest University, Xi’an 710127, China
3.State Key Laboratory of Loess and Quaternary Geology, Instituteof Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China
4.Research School of Earth Sciences, Australian National University, Canberra 2601ACT, Australia
5.Institute of Geophysics, Eidgenössische Technische Hochschule Zürich, CH-8092 Zürich, Switzerland
6.State Key Laboratory ofLithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
7.Laboratory for Marine Geology, QingdaoNational Laboratory for Marine Science and Technology, Qingdao 266237, China
8.College of Marine Geosciences, Ocean University of China, Qingdao266100, China
9.Laboratory of Paleomagnetism, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
10.Departmentof Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
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GB/T 7714
Li,J.X,Yue, L.P,Roberts, A.P,et al. Global cooling and enhanced Eocene Asianmid-latitude interior aridity[J]. NATURE COMMUNICATIONS,2018,9(1):3026.
APA Li,J.X.,Yue, L.P.,Roberts, A.P.,Hirt, A.M.,Pan, F.,...&Liu, Q.S.(2018).Global cooling and enhanced Eocene Asianmid-latitude interior aridity.NATURE COMMUNICATIONS,9(1),3026.
MLA Li,J.X,et al."Global cooling and enhanced Eocene Asianmid-latitude interior aridity".NATURE COMMUNICATIONS 9.1(2018):3026.
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