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Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr
Yang, Yibo1,2,3; Yang, Rongsheng1; Li, Xiangyu4,5; Han, Wenxia6; Zan, Jinbo1,2; Fang, Xiaomin1,2; Appel, Erwin7; Galy, Albert3; Wu, Fuli1,2; Yang, Song8; Zhang, Zhigao9; Zhang, Weilin1,2; Ye, Chengcheng1
2017-06-15
发表期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
卷号476页码:181-191
文章类型Article
摘要Exploring the interplay between the mid-latitude Westerlies and East Asian monsoon systems is crucial for revealing the mechanisms and processes behind the aridification of the central Asian interior. In this study, a high-resolution acid-dissolved Mn record of lacustrine sediments from a drilling core (SG-1) in the arid western Qaidam Basin on the northeastern Tibetan Plateau (TP) largely reveals the evolution of lake levels and climate change over the last 600 kyr. The climate in the western Qaidam Basin shows distinct glacial and interglacial changes in accordance with changes in the global climate, and in North Atlantic sea surface temperatures (SSTs), indicating the teleconnection between the basin's climate and the North Atlantic in the form of the Westerlies. However, the basin's climate also correlates closely with East Asian Winter Monsoon (EAWM) activity as recorded by the grain size variations in loess-paleosol sequences on the Chinese Loess Plateau (CLP) over a glacial-interglacial timescale. Even during glacial periods, some relatively warm/humid stages accompanied by high paleolake levels in the western Qaidam Basin are generally conformable with relatively weak EAWM, whereas these warm/humid stages show a weak relation with the East Asian Summer Monsoon (EASM) and North Atlantic SSTs. These results collectively provide evidence that climate change in the western Qaidam Basin is, and was, not only controlled by the Westerlies, but also strongly influenced by the Siberian High, at least during glacial periods. The exact driving mechanism, however, needs to be explored further in future studies. (C) 2017 Elsevier B.V. All rights reserved.
关键词Qaidam Basin Quaternary East Asian Winter Monsoon Siberian High Lake Levels
WOS标题词Science & Technology ; Physical Sciences ; Life Sciences & Biomedicine
关键词[WOS]WESTERN QAIDAM BASIN ; SOUTH CHINA SEA ; DRILL CORE SG-1 ; ATMOSPHERIC CIRCULATION ; HOLOCENE MOISTURE ; NORTH PACIFIC ; GONGHE BASIN ; MONSOON EVOLUTION ; AEOLIAN ACTIVITY ; ASIAN INTERIOR
收录类别SCI
语种英语
WOS研究方向Physical Geography ; Geology ; Paleontology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS记录号WOS:000402216100014
引用统计
文献类型期刊论文
条目标识符http://ir.isl.ac.cn/handle/363002/6220
专题青海盐湖研究所知识仓储
盐湖地质与环境实验室
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China
2.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
3.Univ Lorraine, CNRS, Ctr Recherches Petrog & Geochim, UMR7358, F-54500 Nancy, France
4.Chinese Acad Sci, Climate Change Res Ctr, Beifing 100029, Peoples R China
5.Chinese Acad Sci, Inst Atmospher Phys, Beijing 100029, Peoples R China
6.Chinese Acad Sci, Qinghai Inst Salt Lakes, Key Lab Salt Lake Resources & Chem, Xining 810008, Peoples R China
7.Univ Tubingen, Dept Geosci, Ctr Appl Geosci, Holderlinstr 12, D-72074 Tubingen, Germany
8.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China
9.Anyang Normal Univ, Sch Resource Environm & Tourism, Anyang 455002, Peoples R China
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Yang, Yibo,Yang, Rongsheng,Li, Xiangyu,et al. Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2017,476:181-191.
APA Yang, Yibo.,Yang, Rongsheng.,Li, Xiangyu.,Han, Wenxia.,Zan, Jinbo.,...&Ye, Chengcheng.(2017).Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,476,181-191.
MLA Yang, Yibo,et al."Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 476(2017):181-191.
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