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Timing and style of Late Pleistocene glaciation in the Queer Shan, northern Hengduan Mountains in the eastern Tibetan Plateau

文献类型:期刊论文

作者Xu, Liubing1,2; Ou, Xianjiao1,2; Lai, Zhongping2; Zhou, Shangzhe1; Wang, Jie3; Fu, Yingchun1
刊名JOURNAL OF QUATERNARY SCIENCE
出版日期2010-09-01
卷号25期号:6页码:957-966
关键词Eastern Tibetan Plateau Glacial Advance South Asian Monsoon Marine Isotope Stages 2 And 3 Osl Dating Esr Dating
文献子类Article
英文摘要Glacial landforms and sediments provide evidence for the existence of two Late Pleistocene major glacial advances in the Queer Shan, northern Hengduan Mountains in the eastern Tibetan Plateau. In the current study, optically stimulated luminescence and electron spin resonance dating results reveal that the two glacial advances occurred during Marine Isotope Stage (MIS) 3 and the Last Glacial Maximum (LGM) in MIS 2, respectively. Geomorphic evidence shows that the glacial advance during MIS 3 was more extensive than that in MIS 2. This glacial advance is synchronous with other glaciated areas in the Himalaya and Tibet, but contrasts with global ice volumes that reached their maximum extent during the LGM. Glaciers in the Queer Shan are of the summer accumulation type and are mainly fed by precipitation from the south Asian monsoon. Palaeoclimate proxies show that during MIS 3 the south Asian monsoon strengthened and extended further north into the Tibetan Plateau to supply more precipitation as snow at high altitudes. This in turn led to positive glacier mass balances and caused glaciers to advance. However, during the LGM, despite cooler temperature than in MIS 3, the weakened south Asian monsoon and the associated reduced precipitation were not as favourable for glacier expansion as in MIS 3. Copyright (C) 2010 John Wiley & Sons, Ltd.
WOS关键词LATE QUATERNARY GLACIATION ; CHINESE LOESS ; INDIAN MONSOON ; GROWTH-CURVE ; THAR DESERT ; ICE CORE ; LUMINESCENCE CHRONOLOGY ; SOUTHERN MARGIN ; SUMMER MONSOON ; QUARTZ
WOS研究方向Geology ; Paleontology
语种英语
WOS记录号WOS:000281858800013
源URL[http://ir.isl.ac.cn/handle/363002/5943]  
专题青海盐湖研究所_青海盐湖研究所知识仓储
青海盐湖研究所_盐湖地质与环境实验室
作者单位1.S China Normal Univ, Dept Geog, Guangzhou 510631, Guangdong, Peoples R China
2.Chinese Acad Sci, Qinghai Inst Salt Lakes, Luminescence Dating Grp, Key Lab Salt Lake Resources & Chem, Xining, Peoples R China
3.Lanzhou Univ, Dept Geog, Lanzhou 730000, Peoples R China
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GB/T 7714
Xu, Liubing,Ou, Xianjiao,Lai, Zhongping,et al. Timing and style of Late Pleistocene glaciation in the Queer Shan, northern Hengduan Mountains in the eastern Tibetan Plateau[J]. JOURNAL OF QUATERNARY SCIENCE,2010,25(6):957-966.
APA Xu, Liubing,Ou, Xianjiao,Lai, Zhongping,Zhou, Shangzhe,Wang, Jie,&Fu, Yingchun.(2010).Timing and style of Late Pleistocene glaciation in the Queer Shan, northern Hengduan Mountains in the eastern Tibetan Plateau.JOURNAL OF QUATERNARY SCIENCE,25(6),957-966.
MLA Xu, Liubing,et al."Timing and style of Late Pleistocene glaciation in the Queer Shan, northern Hengduan Mountains in the eastern Tibetan Plateau".JOURNAL OF QUATERNARY SCIENCE 25.6(2010):957-966.

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来源:青海盐湖研究所

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