Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts

doi:10.1016/j.jseaes.2019.103912

CORC > 自然资源部第一海洋研究所 > 自然资源部第一海洋研究所 > 业务部门 > 海洋地质与地球物理研究室

	Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts
	Chen, Jinxia 1,3; Nan, Qingyun 2,3; Li, Tiegang 1,3; Sun, Rongtao 4; Sun, Hanjie 2,3; Lu, Jian 2,3
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2019-09
卷号	181
关键词	Grain size Organic carbon Isotope East Asian winter monsoon Ancient Chinese dynasties Yellow Sea
ISSN号	1367-9120
DOI	10.1016/j.jseaes.2019.103912
英文摘要	Changes in paleoenvironments from 3500 to 1300 cal. yr BP have been documented by a high-resolution grain-size and organic carbon isotope record in core Z8 from the Shandong mud wedge in the southern Yellow Sea (YS). The sensitive grain-size component, sorting coefficients and delta C-13(org) values were used to identify the paleohydrologic variations and the intensity of the East Asian winter monsoon (EAWM). The coarse fraction of sediment, together with organic isotope and sea surface temperature (SST) data, shows a weak EAWM during 3500-2300 cal. yr BP, a gradual increase in the EAWM from 2300 to 1700 cal. yr BP and an enhanced EAWM since 1700 cal. yr BP. Superimposed on this general trend, several prominent short-lived strong EAWM episodes peaked at approximately 3300, 3100, 2900, 2750, 2620, 2220, 1900, 1700 and 1400 cal. yr BP. The paleoenvironmental record matches ancient Chinese historical climate records as well as socioeconomic changes, with lower economic levels occurring during stronger EAWM episodes. The results show that prosperous stages of ancient Chinese dynasties mainly occurred in weak EAWM periods, while collapses and/or changes in ancient Chinese dynasties generally occurred during cold periods with a strong EAWM. We suggest that the persistent short-lived strengthening of the EAWM could have exerted a remarkable influence on ancient agricultural societies through decreases in both winter temperature and monsoonal precipitation.
资助项目	Shandong Provincial Natural Science Foundation, China[ZR2016DM12]
WOS研究方向	Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000482496600010
内容类型	期刊论文
源URL	[http://ir.fio.com.cn:8080/handle/2SI8HI0U/30100]
专题	业务部门_海洋地质与地球物理研究室
通讯作者	Nan, Qingyun
作者单位	1.SOA, Key Lab Marine Sediment Logy & Environm Geol, Inst Oceanog 1, Qingdao 266061, Shandong, Peoples R China 2.Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Shandong, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Shandong, Peoples R China 4.Shandong Univ Technol, Sch Resources & Environm Engn, Zibo, Peoples R China
推荐引用方式 GB/T 7714	Chen, Jinxia,Nan, Qingyun,Li, Tiegang,et al. Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts[J]. JOURNAL OF ASIAN EARTH SCIENCES,2019,181.
APA	Chen, Jinxia,Nan, Qingyun,Li, Tiegang,Sun, Rongtao,Sun, Hanjie,&Lu, Jian.(2019).Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts.JOURNAL OF ASIAN EARTH SCIENCES,181.
MLA	Chen, Jinxia,et al."Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts".JOURNAL OF ASIAN EARTH SCIENCES 181(2019).