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The mid-Holocene decline of the East Asian summer monsoon indicated by a lake-to-wetland transition in the Sanjiang Plain, Northeast China
Z. Q. Zhang, K. B. Liu, T. A. Bianchette and G. P. Wang
2018
发表期刊Holocene
卷号28期号:2页码:246-253
其他摘要A comprehensive and integrative view of East Asian monsoon evolution during the Holocene is still under debate, and additional high-resolution proxy records from climatically sensitive locations are requisite to solve this complex issue. In this paper, we present three well-dated mud/peat cores from a paleo-pingo depression in the Sanjiang Plain, a climatically sensitive region to monsoon variation, to reveal the paleoenvironmental history of the wetland and discuss the regional impacts from monsoon evolution. A paleolake developed in the study area before 5.5 ka BP, and a peatland initiated thereafter consequent upon the gradual shrinking of the paleolake. This transition lasted until 4.5 ka BP, when the paleolake changed entirely to a wetland. Considering the prevalent monsoon climate in the Sanjiang Plain, we suggest that the lake-to-wetland transition from 5.5 to 4.5 ka BP indicates a rapid decline of the East Asian summer monsoon in addition to autogenic basin infilling processes. Such a remarkable monsoon weakening event has been documented across northern China, and we associate this with ocean-atmosphere interactions throughout low-latitude regions.
文献类型期刊论文
条目标识符http://ir.iga.ac.cn/handle/131322/9209
专题湿地生态系统管理学科组
推荐引用方式
GB/T 7714
Z. Q. Zhang, K. B. Liu, T. A. Bianchette and G. P. Wang. The mid-Holocene decline of the East Asian summer monsoon indicated by a lake-to-wetland transition in the Sanjiang Plain, Northeast China[J]. Holocene,2018,28(2):246-253.
APA Z. Q. Zhang, K. B. Liu, T. A. Bianchette and G. P. Wang.(2018).The mid-Holocene decline of the East Asian summer monsoon indicated by a lake-to-wetland transition in the Sanjiang Plain, Northeast China.Holocene,28(2),246-253.
MLA Z. Q. Zhang, K. B. Liu, T. A. Bianchette and G. P. Wang."The mid-Holocene decline of the East Asian summer monsoon indicated by a lake-to-wetland transition in the Sanjiang Plain, Northeast China".Holocene 28.2(2018):246-253.
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