Evolution of the Indian summer monsoon during the interval 32.7-11.4 cal. ka BP: Evidence from the Baoxiu peat, Yunnan, southwest China
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文摘

Multi-proxy mineralogical and geochemical records to investigate the climatic evolution of the ISM during the interval 32.7–11.4 ka BP.

δ13CTOC values in the Baoxiu peat core are thought to record surface air temperature.

Decipher the phase relationship between the ISM and EASM during the last glacial period.

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