Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China

doi:10.1016/j.quascirev.2013.04.022

	Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China
	Tan, Liangcheng 1; Yi, Liang 2; Cai, Yanjun 1; Shen, Chuan-Chou 3; Cheng, Hai 4,5; An, Zhisheng 1
刊名	QUATERNARY SCIENCE REVIEWS
	2013-07-15
卷号	72 页码:137-145
关键词	Stalagmite Annual layer Growth rate Temperature Modern process Central China
ISSN号	0277-3791
DOI	10.1016/j.quascirev.2013.04.022
文献子类	Article
英文摘要	We used the annual growth rate of a stalagmite (XL21) collected from Xianglong Cave, central China, to quantitatively reconstruct regional terrestrial temperature changes over the last 95 years (1912-2006 AD). Based on a significant positive correlation between the growth rate and the observed temperature, a transfer function was designed, and the temperature from the previous September to May (P-9-5) was reconstructed, with an explained variance of 43.5%. Our results show an increasing trend in temperature during the last century, and especially over the last 30 years. The temperature variability from central China recorded here bears a striking similarity to that in the Northern Hemisphere, and also to global trends. However, the cooling between the 1980s and the early 1990s seen in the stalagmite record, which interrupted the warming trend that began in the 1960s, is not observed in the mean conditions found in China, the Northern Hemisphere, neither globally. This methodology for reconstructing historical temperature from stalagmite growth rates overcomes the limitation of the short meteorological observation period and supports the potential of stalagmite lamina climatology. (C) 2013 Elsevier Ltd. All rights reserved.
WOS关键词	ASIAN WINTER MONSOON ; MALAN ICE CORE ; TIBETAN PLATEAU ; TREE-RINGS ; LAST MILLENNIUM ; HOLOCENE CLIMATE ; UNITED-STATES ; YANGTZE-RIVER ; LOWER REACHES ; PROXY RECORD
WOS研究方向	Physical Geography ; Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000321685700010
资助机构	CAS Strategic Priority Research Program(XDA05080502) ; CAS Strategic Priority Research Program(XDA05080502) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; National Science Foundation of China(41001061) ; National Science Foundation of China(41001061) ; National Basic Research Program of China(2013CB955902 ; National Basic Research Program of China(2013CB955902 ; 2010CB833405) ; 2010CB833405) ; CAS Strategic Priority Research Program(XDA05080502) ; CAS Strategic Priority Research Program(XDA05080502) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; National Science Foundation of China(41001061) ; National Science Foundation of China(41001061) ; National Basic Research Program of China(2013CB955902 ; National Basic Research Program of China(2013CB955902 ; 2010CB833405) ; 2010CB833405) ; CAS Strategic Priority Research Program(XDA05080502) ; CAS Strategic Priority Research Program(XDA05080502) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; National Science Foundation of China(41001061) ; National Science Foundation of China(41001061) ; National Basic Research Program of China(2013CB955902 ; National Basic Research Program of China(2013CB955902 ; 2010CB833405) ; 2010CB833405) ; CAS Strategic Priority Research Program(XDA05080502) ; CAS Strategic Priority Research Program(XDA05080502) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; Key Program of the Chinese Academy of Sciences(KZZD-EW-04-01) ; National Science Foundation of China(41001061) ; National Science Foundation of China(41001061) ; National Basic Research Program of China(2013CB955902 ; National Basic Research Program of China(2013CB955902 ; 2010CB833405) ; 2010CB833405)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/88030]
专题	中国科学院地质与地球物理研究所
通讯作者	Tan, Liangcheng
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 3.Natl Taiwan Univ, Dept Geosci, High Precis Mass Spectrometry & Environm Change L, Taipei 106, Taiwan 4.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China 5.Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA
推荐引用方式 GB/T 7714	Tan, Liangcheng,Yi, Liang,Cai, Yanjun,et al. Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China[J]. QUATERNARY SCIENCE REVIEWS,2013,72:137-145.
APA	Tan, Liangcheng,Yi, Liang,Cai, Yanjun,Shen, Chuan-Chou,Cheng, Hai,&An, Zhisheng.(2013).Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China.QUATERNARY SCIENCE REVIEWS,72,137-145.
MLA	Tan, Liangcheng,et al."Quantitative temperature reconstruction based on growth rate of annually-layered stalagmite: a case study from central China".QUATERNARY SCIENCE REVIEWS 72(2013):137-145.