Holocene moisture and East Asian summer monsoon evolution in the northeastern Tibetan Plateau recorded by Lake Qinghai and its environs: A review of conflicting proxies

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• 作者：Fahu Chen^a ; ^b ; ^{fhchen@lzu.edu.cn} ; Duo Wu^a ; ^e ; ^{wud_2008@lzu.edu.cn} ; Jianhui Chen^a ; Aifeng Zhou^a ; Junqing Yu^c ; Ji Shen^d ; Sumin Wang^d ; Xiaozhong Huang^a
• 关键词：Northeastern Tibetan Plateau ; Lake Qinghai ; EASM evolution ; Middle Holocene EASM maximum
• 刊名：Quaternary Science Reviews
• 出版年：2016
• 出版时间：15 December 2016
• 年：2016
• 卷：154
• 期：Complete
• 页码：111-129
• 全文大小：3321 K
• 卷排序：154

文摘

Lake Qinghai and the adjacent lakes were generally low and aeolian sands were widely distributed in the northeastern Tibetan Plateau during the early Holocene. Ostracod δ18O records from Lake Qinghai cannot be used to reflect the strength of the East Asian summer monsoon or the intensity of monsoon precipitation. Moisture and precipitation at Lake Qinghai and its environs began to increase in the early Holocene, reached their maximum during the middle Holocene, and decreased during the late Holocene.