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Timing and structure of the Younger Dryas event in northern China

文献类型：期刊论文

作者Ma, Zhi-Bang1,2; Cheng, Hai3,4,5; Tan, Ming1; Edwards, R. Lawrence4; Li, Hong-Chun6; You, Chen-Feng7; Duan, Wu-Hui1; Wang, Xu1; Kelly, Megan J.4
刊名QUATERNARY SCIENCE REVIEWS
出版日期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
DOI10.1016/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
WOS记录号WOS:000304568400007
出版者PERGAMON-ELSEVIER SCIENCE LTD
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)
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.

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来源：地质与地球物理研究所

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