The Climate Change during Early Holocene Recordedby Trace Elements of Shenmu Section, Mu Us Desert

doi:10.1134/S0016702917140038

CORC > 地球环境研究所 > 中国科学院地球环境研究所 > 黄土与第四纪地质国家重点实验室（2010~）

	The Climate Change during Early Holocene Recordedby Trace Elements of Shenmu Section, Mu Us Desert
	Li,Baosheng ; Liu,HB(Liu,Haibo)2; Li,BS(Li,Baosheng)1,2; Zheng,CH(Zheng,Chunhong)2; Si,YJ(Si,Yuejun)6; Wen,XH(Wen,Xiaohao)2; Niu,DF(Niu,Dongfeng)3; Du,SH(Du,Shuhuan)4; Shu,PX(Shu,Peixian)5
刊名	Geochemistry International
	2017-10
卷号	55 期号:12 页码:1171–1179
关键词	Shenmu Section Early Holocene Trace Elements Paleo Climate Changes
DOI	10.1134/S0016702917140038
文献子类	期刊论文
英文摘要	Through nine trace elements of the Shenmu section, Mu Us Desert is analyzed for the climate changes during Early Holocene. Except Sr, a migration process of P, Mn, Cr, Rb, Nb, Cu, Zn, and V is found in the dune sands, indicating the accumulation processes of the Asian winter monsoon-driven wind erosion and transport and deposition under the cold climatic phase. And accumulation of these elements in different layers of paleo sol dune sands is related to regional geomorphology and element properties. 8.5 winter-summer monsoon cycles in the early Holocene are observed. The duration time and climate of the stronger winter monsoon phases can be compared with the cold climate in the North Atlantic and other parts of China. The result of Red fit 3.8 power spectra shows 310a, 210a, 90a, and 70a centennial cycles for the element, which are consistent with the solar oscillation cycles. These suggest that the external solar activities of the Earth may have great influences on driving the winter and summer monsoon cycles during early Holocene.
项目编号	2013CB955903 ; 41471159
语种	英语
资助机构	National BasicResearch Program of China ; National BasicResearch Program of China
内容类型	期刊论文
源URL	[http://ir.ieecas.cn/handle/361006/5620]
专题	地球环境研究所_黄土与第四纪地质国家重点实验室（2010~）
通讯作者	Li,Baosheng
作者单位	1.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences,Xi’an, 710061 China 2.School of Geography, South China Normal University, Guangzhou, 510631 China 3.Lingnan Normal University, Zhanjiang, 524048 China 4.Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanlolgy, Chinese Academy of Sciences,Guangzhou, 510630 China 5.Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, 710061 China 6.School of Geography and Planning, Guangxi Teachers Education University, Nanning, Guangxi, 530001 China
推荐引用方式 GB/T 7714	Li,Baosheng,Liu,HB,Li,BS,et al. The Climate Change during Early Holocene Recordedby Trace Elements of Shenmu Section, Mu Us Desert[J]. Geochemistry International,2017,55(12):1171–1179.
APA	Li,Baosheng.,Liu,HB.,Li,BS.,Zheng,CH.,Si,YJ.,...&Shu,PX.(2017).The Climate Change during Early Holocene Recordedby Trace Elements of Shenmu Section, Mu Us Desert.Geochemistry International,55(12),1171–1179.
MLA	Li,Baosheng,et al."The Climate Change during Early Holocene Recordedby Trace Elements of Shenmu Section, Mu Us Desert".Geochemistry International 55.12(2017):1171–1179.