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Marine Oxygen Isotope Stage(MIS)-6 Glacial Advances on the Tibetan Plateau More Extensive than during MIS-2 due to More Abundant Precipitation

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Acta Geologica Sinica(English Edition) 2022年第5期96卷 1484-1494页

作者： Marie-Luce CHEVALIER WANG Shiguang Anne REPLUMAZ LI Haibing Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources Institute of GeologyCAGSBeijing 100037China Jiangsu Donghai Crustal Activity in Deep Holes of the Continental Scientific Drilling National Observation and Research Station LianyungangJiangsu 222300China Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou) Guangzhou 511458China National Institute of Natural Hazards MEMCBeijing 100037China ISTerre UniversitéGrenoble AlpesCNRSGrenoble 38610France

Numerous studies dated glacial deposits within the Himalayan-Tibetan orogen.While most focus on young deposits,i.e.,younger than the Last Glacial Maximum(LGM or Marine oxygen Isotope Stage(MIS)-2,~20 ka),older moraines such as those from MIS-6(~130–191 ka)are much harder to date and interpret due to the less well-preserved nature of their surfaces and boulders,as well as their scattered and continuous age distribution due to long-lived erosion since deposition.Here,we dated with~(10)Be,two imbricated moraines near yadong in southern Tibet,as MIS-2 and 6,showing that the most extensive,smooth surfaces were abandoned during MIS-6.Compiling published data from 54 MIS-6 moraines on the Tibetan Plateau reveals that they exist in most regions,dry or humid.They are particularly well-preserved(sharp crests)in eastern and northern Tibet,while in southern and central Tibet,their crests are rounded to sub-rounded.Because both MIS-2 and 6 were equally cold,and because MIS-6 moraines are much more extensive than those from the LGM,we conclude that MIS-6 glacial advances were controlled by more abundant precipitation than during MIS-2.This would be consistent with the peak in Asian monsoon during MIS-6,revealed by sediments from the South China Sea.

关键词： yadong rift southern Tibet cosmogenic isotopes Quaternary paleo-precipitation moraine morphology Indian monsoon

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