Timing and structure of the Younger Dryas event in northern China

doi:10.1016/j.quascirev.2012.03.006

	Timing and structure of the Younger Dryas event in northern China
	Ma, Zhi-Bang 1,2; Cheng, Hai 3,4,5; Tan, Ming 1; Edwards, R. Lawrence 4; Li, Hong-Chun 6; You, Chen-Feng 7; Duan, Wu-Hui 1; Wang, Xu 1; Kelly, Megan J.4
刊名	QUATERNARY SCIENCE REVIEWS
	2012-05-18
卷号	41 页码:83-93
关键词	Asymmetrical Younger Dryas structure Abrupt climate change Asian monsoon Kulishu Cave Northern China
ISSN号	0277-3791
DOI	10.1016/j.quascirev.2012.03.006
文献子类	Article
英文摘要	A high-resolution and absolute-dated stalagmite record from Kulishu Cave, Beijing characterizes Asian Monsoon (AM) history in northern China between ca 14 and 10.5 ka BP (thousand yrs before present, present = 1950), including the entire Younger Dryas (YD) event. Using Th-230 dates and counting of annual-layers, the shift into the YD began at 12,850 +/- 40 yr BP and took similar to 340 yrs and the shift out of the YD began at 11,560 +/- 40 yr BP and took <38 yrs (best estimate similar to 20 yrs), broadly similar to previously reported AM records from central and southeastern China. The more gradual nature of the start of the YD event as observed in the AM records appears to contrast with the more abrupt beginning observed in the Greenland ice records. The total amplitude of the AM YD event is also smaller than the amplitude of the AM Heinrich Stadial 1 event. In addition, the general rising trend of the AM during the Bolling-Allerod period contrasts with the general cooling trend in Greenland temperature during that time. The influence of rising insolation on the AM may explain this observation. (C) 2012 Elsevier Ltd. All rights reserved.
WOS关键词	INTERTROPICAL CONVERGENCE ZONE ; EAST-ASIAN MONSOON ; HIGH-RESOLUTION ; LAST DEGLACIATION ; SPELEOTHEM RECORD ; LATE PLEISTOCENE ; CLIMATE CHANGES ; DONGGE CAVE ; HULU CAVE ; PRECIPITATION
WOS研究方向	Physical Geography ; Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000304568400007
资助机构	National Basic Research Program of China (973 program)(2010CB950201) ; National Basic Research Program of China (973 program)(2010CB950201) ; National Natural Science Foundation of China(40872207) ; National Natural Science Foundation of China(40872207) ; Xi'an Jiaotong University(93K40208000004) ; Xi'an Jiaotong University(93K40208000004) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; U.S. NSF(0502535 ; U.S. NSF(0502535 ; 0908792 ; 0908792 ; 1103403) ; 1103403) ; National Basic Research Program of China (973 program)(2010CB950201) ; National Basic Research Program of China (973 program)(2010CB950201) ; National Natural Science Foundation of China(40872207) ; National Natural Science Foundation of China(40872207) ; Xi'an Jiaotong University(93K40208000004) ; Xi'an Jiaotong University(93K40208000004) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; U.S. NSF(0502535 ; U.S. NSF(0502535 ; 0908792 ; 0908792 ; 1103403) ; 1103403) ; National Basic Research Program of China (973 program)(2010CB950201) ; National Basic Research Program of China (973 program)(2010CB950201) ; National Natural Science Foundation of China(40872207) ; National Natural Science Foundation of China(40872207) ; Xi'an Jiaotong University(93K40208000004) ; Xi'an Jiaotong University(93K40208000004) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; U.S. NSF(0502535 ; U.S. NSF(0502535 ; 0908792 ; 0908792 ; 1103403) ; 1103403) ; National Basic Research Program of China (973 program)(2010CB950201) ; National Basic Research Program of China (973 program)(2010CB950201) ; National Natural Science Foundation of China(40872207) ; National Natural Science Foundation of China(40872207) ; Xi'an Jiaotong University(93K40208000004) ; Xi'an Jiaotong University(93K40208000004) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; State Key Laboratory of Loess and Quaternary Geology, CAS(SKLLQG1001) ; U.S. NSF(0502535 ; U.S. NSF(0502535 ; 0908792 ; 0908792 ; 1103403) ; 1103403)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/84510]
专题	中国科学院地质与地球物理研究所
通讯作者	Ma, Zhi-Bang
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 2.Minist Land & Resources, Key Lab Saline Lake Resources & Environm, Beijing 100037, Peoples R China 3.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China 4.Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA 5.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China 6.Natl Taiwan Univ, Dept Geosci, Taipei 617, Taiwan 7.Natl Cheng Kung Univ, Dept Earth Sci, Tainan 701, Taiwan
推荐引用方式 GB/T 7714	Ma, Zhi-Bang,Cheng, Hai,Tan, Ming,et al. Timing and structure of the Younger Dryas event in northern China[J]. QUATERNARY SCIENCE REVIEWS,2012,41:83-93.
APA	Ma, Zhi-Bang.,Cheng, Hai.,Tan, Ming.,Edwards, R. Lawrence.,Li, Hong-Chun.,...&Kelly, Megan J..(2012).Timing and structure of the Younger Dryas event in northern China.QUATERNARY SCIENCE REVIEWS,41,83-93.
MLA	Ma, Zhi-Bang,et al."Timing and structure of the Younger Dryas event in northern China".QUATERNARY SCIENCE REVIEWS 41(2012):83-93.