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Quaternary glaciations in the Lopu Kangri area, central Gangdise Mountains, southern Tibetan Plateau
Zhang, Q (Zhang, Qian)1,2,3,4; Yi, CL (Yi, Chaolu)1,2; Dong, GC (Dong, Guocheng)5; Fu, P (Fu, Ping)6; Wang, NL (Wang, Ninglian)7; Capolongo, D (Capolongo, Domenico)4
Source PublicationQUATERNARY SCIENCE REVIEWS 
2018-12-01
Volume201Issue:0Pages:470-482
DOI10.1016/j.quascirev.2018.10.027
Abstract

The Gangdise Mountains are located in a transition zone between the Indian Summer Monsoon-dominated Himalaya Mountains and the Westerlies-dominated Qiangtang Plateau. The timing and extent of the paleoglaciations in the central Gangdise Mountains remain unclear. We investigated the glacial history of the southeastern slopes of Lopu Kangri using Be-10 exposure dating and summarized the dating results for the western and eastern sectors of the Gangdise Mountains. Glacial events were constrained to >= 243.88 +/- 25.88 ka, >= 43.09 +/- 4.18 ka, 24.19 +/- 2.29 ka, 19.78 +/- 1.9 ka, 10.62 +/- 1 ka, 2.75 +/- 0.37 ka, 1.8 +/- 0.18 ka, 0.32 +/- 0.04 ka and 0.22 +/- 0.04 ka, representing paleoglaciations which occurred during marine isotope stage (MIS) 8/7 or earlier, MIS 3 or earlier, early MIS 2, the global Last Glacial Maximum (LGM), the early Holocene, the Neoglacial and the Little Ice Age (LIA). Evidence of MIS 5 or earlier glaciations, and the glaciations during MIS 3, early and late MIS 2, the global LGM and the LIA, can be found in the western or eastern sectors of the Gangdise Mountains. The spatial trend in Delta ELA values in the Gangdise and surrounding mountain ranges would appear to have been controlled by particular precipitation distribution patterns. The glacial events identified in the Gangdise Mountains during MIS 2, the Neoglacial and the LIA appear consistent with previously-identified cold periods. Precipitation was most likely a contributory cause of the glaciations during the MIS 3, early Holocene, the Neoglacial and the LIA. (C) 2018 Elsevier Ltd. All rights reserved.

Subject Area地理学
WOS IDWOS:000452934700028
Language英语
Indexed BySCIE
KeywordBe-10 Surface Exposure Ice-age Pleistocene Glaciations Cosmogenic Be-10 Global Climate North-atlantic Western Tibet Fault System Half-life Tian-shan
WOS Research AreaPhysical Geography ; Geology
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary
Cooperation Status国际
ISSN0277-3791
Department环境变化与地表过程重点实验室
PublisherPERGAMON-ELSEVIER SCIENCE LTD
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8489
Collection图书馆
Corresponding AuthorYi, CL (Yi, Chaolu)
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;
2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China;
4.Univ Bari Aldo Moro, Dept Earth & Geoenvironm Sci, I-70125 Bari, Italy;
5.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China;
6.Univ Nottingham, Sch Geog Sci, Ningbo 315100, Zhejiang, Peoples R China;
7.Northwest Univ, Coll Urban & Environm Sci, Xian 710127, Shaanxi, Peoples R China.
Recommended Citation
GB/T 7714
Zhang, Q ,Yi, CL ,Dong, GC ,et al. Quaternary glaciations in the Lopu Kangri area, central Gangdise Mountains, southern Tibetan Plateau[J]. QUATERNARY SCIENCE REVIEWS ,2018,201(0):470-482.
APA Zhang, Q ,Yi, CL ,Dong, GC ,Fu, P ,Wang, NL ,&Capolongo, D .(2018).Quaternary glaciations in the Lopu Kangri area, central Gangdise Mountains, southern Tibetan Plateau.QUATERNARY SCIENCE REVIEWS ,201(0),470-482.
MLA Zhang, Q ,et al."Quaternary glaciations in the Lopu Kangri area, central Gangdise Mountains, southern Tibetan Plateau".QUATERNARY SCIENCE REVIEWS  201.0(2018):470-482.
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