Global cooling and enhanced Eocene Asianmid-latitude interior aridity
文献类型：期刊论文
| 作者 | Guo, L(Guo, Lei)10; Li,J.X9,10; Roberts, A.P7; Liu, Q.S1; Sun, Z.M2; Jiang, Z.X4,7; Gai,C.C4,5; Qiang, X.K8; Pan, F9,10; Xi, R.G10 |
| 刊名 | NATURE COMMUNICATIONS
 |
| 出版日期 | 2018-08 |
| 卷号 | 9期号:1页码:3026 |
| DOI | 10.1038/s41467-018-05415-x |
| 文献子类 | 期刊论文 |
| 英文摘要 | 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. |
| 项目编号 | 41002052 ; 2016YFA0601903 ; 41430962 ; 41072136 ; 41202133 ; 90814005 ; 1212011121185 ; 201311126 ; DP110105419 |
| 语种 | 英语 |
| 资助机构 | 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 |
| 源URL | [http://ir.ieecas.cn/handle/361006/5278]  |
| 专题 | 地球环境研究所_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.Departmentof Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China 2.Laboratory of Paleomagnetism, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China 3.College of Marine Geosciences, Ocean University of China, Qingdao266100, China 4.Laboratory for Marine Geology, QingdaoNational Laboratory for Marine Science and Technology, Qingdao 266237, China 5.State Key Laboratory ofLithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 6.Institute of Geophysics, Eidgenössische Technische Hochschule Zürich, CH-8092 Zürich, Switzerland 7.Research School of Earth Sciences, Australian National University, Canberra 2601ACT, Australia 8.State Key Laboratory of Loess and Quaternary Geology, Instituteof Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China 9.State Key Laboratory forContinental Dynamics, Department of Geology, Northwest University, Xi’an 710127, China 10.Research Center for Orogenic Geology, Xi’an Center of Geological Survey, China Geological Survey, Xi’an 710054, China |
| 推荐引用方式 GB/T 7714 | Guo, L,Li,J.X,Roberts, A.P,et al. Global cooling and enhanced Eocene Asianmid-latitude interior aridity[J]. NATURE COMMUNICATIONS,2018,9(1):3026. |
| APA | Guo, L.,Li,J.X.,Roberts, A.P.,Liu, Q.S.,Sun, Z.M.,...&Guo, L.(2018).Global cooling and enhanced Eocene Asianmid-latitude interior aridity.NATURE COMMUNICATIONS,9(1),3026. |
| MLA | Guo, L,et al."Global cooling and enhanced Eocene Asianmid-latitude interior aridity".NATURE COMMUNICATIONS 9.1(2018):3026. |
入库方式： OAI收割
来源：地球环境研究所
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