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Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr
Yang, YB (Yang, Yibo)1,2,3; Yang, RS (Yang, Rongsheng)1; Li, XY (Li, Xiangyu)4,5; Han, WX (Han, Wenxia)6; Zan, JB (Zan, Jinbo)1,2; Fang, XM (Fang, Xiaomin)1,2; Appel, E (Appel, Erwin)7; Galy, A (Galy, Albert)3; Wu, FL (Wu, Fuli)1,2; Yang, S (Yang, Song)8; Zhang, ZG (Zhang, Zhigao)9; Zhang, WL (Zhang, Weilin)1,2; Ye, CC (Ye, Chengcheng)1; Yang, YB
Source PublicationPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
2017
Volume476Issue:0Pages:181-191
DOI10.1016/j.palaeo.2017.04.007
AbstractExploring 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.
Subject Area地质学
WOS IDWOS:000402216100014
Language英语
Indexed BySCI
KeywordWestern Qaidam Basin South China Sea Drill Core Sg-1 Atmospheric Circulation Holocene Moisture North Pacific Gonghe Basin Monsoon Evolution Aeolian Activity Asian Interior
WOS Research AreaPhysical Geography; Geology; Paleontology
WOS SubjectGeography, Physical; Geosciences, Multidisciplinary; Paleontology
Cooperation Status国际
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8194
Collection图书馆
Corresponding AuthorYang, YB
Affiliation1.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.
Recommended Citation
GB/T 7714
Yang, YB ,Yang, RS ,Li, XY ,et al. Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2017,476(0):181-191.
APA Yang, YB .,Yang, RS .,Li, XY .,Han, WX .,Zan, JB .,...&Yang, YB.(2017).Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,476(0),181-191.
MLA Yang, YB ,et al."Glacial-interglacial climate change on the northeastern Tibetan Plateau over the last 600 kyr".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 476.0(2017):181-191.
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