干旱区生态环境知识资源中心(Arid): Moisture variations in Lacustrine-eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene

Arid

DOI	10.1016/j.quascirev.2020.106210
	Moisture variations in Lacustrine-eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene
	Ming, Guodong 1,2,4,5; Zhou, Weijian 1,2,5; Wang, Hong 6; Cheng, Peng 1,2,3; Shu, Peixian 1,2,5; Xian, Feng 1,2,5; Fu, Yunchong 1,2,3
通讯作者	Zhou, Weijian
来源期刊	QUATERNARY SCIENCE REVIEWS
ISSN	0277-3791
出版年	2020
卷号	233
英文摘要	Paleoclimate records currently lack sufficient geographic detail to understand the spatiotemporal evolution of East Asian Summer Monsoon (EASM) rain belt since the late Pleistocene. In particular, there is no consensus on whether the EASM rain belt reached its modern northern limit by the early Holocene. Here, we present inferred moisture variations from a multi-parameter, absolute-dated lacustrine-eolian sequence from northern China that date back to the late Pleistocene (similar to 14 ka BP or thousand years ago). We observed a sharp transition towards wet conditions at the onset of the Holocene Epoch. Maximum wet climate occurred here during similar to 11.3-8.5 ka. The climate remained predominantly wet until similar to 4.2 ka, then it became progressively drier. We observed alternating organic-rich, fine-grained lake deposits and organic-depleted, coarse-grained eolian sand layers during similar to 14-7 ka. These layers correspond to sedimentation associated with the Allerod, Younger Dryas (YD), post YD warming, pre-Boreal oscillation (PBO), early Holocene and 8.2 ka event. We interpreted the orbital scale moisture variation at our study site to the changes in insolation, assigning these abrupt and short-lived changes during the late Pleistocene-Holocene transition to a persistent teleconnection between the North Atlantic and east Asian climate zones. (C) 2020 Elsevier Ltd. All rights reserved.
英文关键词	Paleo EASM variations Monsoon rainfall Climate instability Lacustrine-eolian sequence Desert-loess transition zone Northern China
类型	Article
语种	英语
国家	Peoples R China
收录类别	SCI-E
WOS记录号	WOS:000525787700002
WOS关键词	HOLOCENE CLIMATE-CHANGE ; LAST GLACIAL MAXIMUM ; SEDIMENTARY ORGANIC-MATTER ; NORTH-ATLANTIC OSCILLATION ; CHINESE LOESS PLATEAU ; INNER-MONGOLIA ; HIGH-RESOLUTION ; YOUNGER DRYAS ; PREBOREAL OSCILLATION ; LAKE XIARINUR
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向	Physical Geography ; Geology
来源机构	北京师范大学 ; 中国科学院地球环境研究所
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/315390
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China; 2.Xian Ams Ctr IEECAS, Shaanxi Key Lab Accelerator Mass Spectrometry Tec, Xian, Peoples R China; 3.Xi An Jiao Tong Univ, Xian 710049, Peoples R China; 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China; 5.CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China; 6.Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier, Beijing 100875, Peoples R China
推荐引用方式 GB/T 7714	Ming, Guodong,Zhou, Weijian,Wang, Hong,et al. Moisture variations in Lacustrine-eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene[J]. 北京师范大学, 中国科学院地球环境研究所,2020,233.
APA	Ming, Guodong.,Zhou, Weijian.,Wang, Hong.,Cheng, Peng.,Shu, Peixian.,...&Fu, Yunchong.(2020).Moisture variations in Lacustrine-eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene.QUATERNARY SCIENCE REVIEWS,233.
MLA	Ming, Guodong,et al."Moisture variations in Lacustrine-eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene".QUATERNARY SCIENCE REVIEWS 233(2020).