Mid‐MIS3 climate inferred from reconstructing the Dalijia Shan ice cap, north‐eastern Tibetan Plateau

• Published in: Journal of Quaternary Science
• Main Authors: WANG, JIE, CUI, HANG, HARBOR, JONATHAN M., ZHENG, LIMIN, YAO, PAN
• Other Authors: This study is financially supported by the National Natural Science Foundation of China
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2015
• Subjects: Ela; Ice cap
• Online Access: http://dx.doi.org/10.1002/jqs.2802; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.2802; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.2802

ABSTRACT The local last glacial maximum (LGM L ) on Dalijia Shan occurred during mid‐marine isotope stage 3 (MIS3), which is consistent with some Tibetan Plateau records, but asynchronous with the MIS2 global Last Glacial Maximum (LGM G ). Paleoclimatic reconstructions are key to advancing understan...