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  4. 岩石圈演化国家重点实验室
Global cooling and enhanced Eocene Asian mid-latitude interior aridity

文献类型：期刊论文

作者Li, J. X.1,2; Yue, L. P.2,3; Roberts, A. P.4; Hirt, A. M.5; Pan, F.1,2; Guo, Lin1; Xu, Y.1; Xi, R. G.1; Guo, Lei1; Qiang, X. K.3
刊名NATURE COMMUNICATIONS
出版日期2018-08-02
卷号9
ISSN号2041-1723
DOI10.1038/s41467-018-05415-x
文献子类Article
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 tele-connected 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.
WOS关键词CHINESE LOESS PLATEAU ; TIBETAN PLATEAU ; RED CLAY ; QAIDAM BASIN ; YELLOW-RIVER ; AEOLIAN DUST ; TARIM BASIN ; GRAIN-SIZE ; ALTUN SHAN ; NW CHINA
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000440617500002
出版者NATURE PUBLISHING GROUP
资助机构National Natural Science Foundation of China (NNSFC)(41002052) ; National Natural Science Foundation of China (NNSFC)(41002052) ; National Key Research and Development Program of China(2016YFA0601903) ; National Key Research and Development Program of China(2016YFA0601903) ; NNSFC(41430962 ; NNSFC(41430962 ; China Geological Survey ; China Geological Survey ; Land Resources Survey Project(1212011121185) ; Land Resources Survey Project(1212011121185) ; Nonprofit Special Project of Land Resources(201311126) ; Nonprofit Special Project of Land Resources(201311126) ; Australian Research Council(DP110105419) ; Australian Research Council(DP110105419) ; 41072136 ; 41072136 ; 41202133 ; 41202133 ; 90814005) ; 90814005) ; National Natural Science Foundation of China (NNSFC)(41002052) ; National Natural Science Foundation of China (NNSFC)(41002052) ; National Key Research and Development Program of China(2016YFA0601903) ; National Key Research and Development Program of China(2016YFA0601903) ; NNSFC(41430962 ; NNSFC(41430962 ; China Geological Survey ; China Geological Survey ; Land Resources Survey Project(1212011121185) ; Land Resources Survey Project(1212011121185) ; Nonprofit Special Project of Land Resources(201311126) ; Nonprofit Special Project of Land Resources(201311126) ; Australian Research Council(DP110105419) ; Australian Research Council(DP110105419) ; 41072136 ; 41072136 ; 41202133 ; 41202133 ; 90814005) ; 90814005) ; National Natural Science Foundation of China (NNSFC)(41002052) ; National Natural Science Foundation of China (NNSFC)(41002052) ; National Key Research and Development Program of China(2016YFA0601903) ; National Key Research and Development Program of China(2016YFA0601903) ; NNSFC(41430962 ; NNSFC(41430962 ; China Geological Survey ; China Geological Survey ; Land Resources Survey Project(1212011121185) ; Land Resources Survey Project(1212011121185) ; Nonprofit Special Project of Land Resources(201311126) ; Nonprofit Special Project of Land Resources(201311126) ; Australian Research Council(DP110105419) ; Australian Research Council(DP110105419) ; 41072136 ; 41072136 ; 41202133 ; 41202133 ; 90814005) ; 90814005) ; National Natural Science Foundation of China (NNSFC)(41002052) ; National Natural Science Foundation of China (NNSFC)(41002052) ; National Key Research and Development Program of China(2016YFA0601903) ; National Key Research and Development Program of China(2016YFA0601903) ; NNSFC(41430962 ; NNSFC(41430962 ; China Geological Survey ; China Geological Survey ; Land Resources Survey Project(1212011121185) ; Land Resources Survey Project(1212011121185) ; Nonprofit Special Project of Land Resources(201311126) ; Nonprofit Special Project of Land Resources(201311126) ; Australian Research Council(DP110105419) ; Australian Research Council(DP110105419) ; 41072136 ; 41072136 ; 41202133 ; 41202133 ; 90814005) ; 90814005)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88136]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Liu, Q. S.
作者单位1.Xian Ctr Geol Survey, Res Ctr Orogen Geol, Xian 710054, Shaanxi, Peoples R China
2.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710127, Shaanxi, Peoples R China
3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China
4.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 2601, Australia
5.Eidgenoss Tech Hsch Zurich, Inst Geophys, CH-8092 Zurich, Switzerland
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
7.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266237, Peoples R China
8.Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Peoples R China
9.Chinese Acad Geol Sci, Inst Geomech, Lab Paleomagnetism, Beijing 100081, Peoples R China
10.Southern Univ Sci & Technol, Dept Ocean Sci & Engn, Shenzhen 518055, Peoples R China
推荐引用方式
GB/T 7714		 Li, J. X.,Yue, L. P.,Roberts, A. P.,et al. Global cooling and enhanced Eocene Asian mid-latitude interior aridity[J]. NATURE COMMUNICATIONS,2018,9.
APA Li, J. X..,Yue, L. P..,Roberts, A. P..,Hirt, A. M..,Pan, F..,...&Liu, Q. S..(2018).Global cooling and enhanced Eocene Asian mid-latitude interior aridity.NATURE COMMUNICATIONS,9.
MLA Li, J. X.,et al."Global cooling and enhanced Eocene Asian mid-latitude interior aridity".NATURE COMMUNICATIONS 9(2018).

入库方式： OAI收割

来源：地质与地球物理研究所

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