Marine Isotope Stage 3 paleotemperature inferred from reconstructing the Die Shan ice cap, northeastern Tibetan Plateau

Abstract Glacial extent mapping and dating indicate that the local last glacial maximum (LLGM) of the northeastern Tibetan Plateau occurred during mid-Marine Isotope Stage (MIS) 3. This is asynchronous with the global last glacial maximum (LGM) that occurred during MIS 2. The causes underlying this...

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Bibliographic Details
Published in:Quaternary Research
Main Authors: Cui, Hang, Wang, Jie, Yu, Beibei, Hu, Zhenbo, Yao, Pan, Harbor, Jonathan M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2018
Subjects:
Online Access:http://dx.doi.org/10.1017/qua.2017.115
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589417001156