Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室(2005-2009)

	Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years
	An Z.S.; George J. Kukla; Stephen C; Xiao J.L.
	1991
Source Publication	Quaternary Research
Volume	36 Issue:1 Pages:29-36
Cooperation Status	国际
Abstract	The magnetic susceptibility of loess and paleosols in central China represents a proxy climate index closely related to past changes of precipitation and vegetation, and thus to summer monsoon intensity. Time series of magnetic susceptibility constructed for three loess-paleosol sequences in the southern part of the Chinese Loess Plateau document the history of summer monsoon variation during the last 130,000 yr. They correlate closely with the oxygen isotope record of stages 1 to 5 in deep-sea sediments. Soils were forming during intervals of strong summer monsoon, whereas loess units were deposited at times of reduced monsoon intensity. The Chinese loess-paleosol sequence can thus be viewed as a proxy record of Asian monsoon variability extending over the last 2.5 myr.
Subject Area	地质学 ; 地球化学
Indexed By	SCI
Language	英语
Document Type	期刊论文
Identifier	http://ir.ieecas.cn/handle/361006/2584
Collection	黄土与第四纪地质国家重点实验室(2005-2009)
Recommended Citation GB/T 7714	An Z.S.,George J. Kukla,Stephen C,et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years[J]. Quaternary Research,1991,36(1):29-36.
APA	An Z.S.,George J. Kukla,Stephen C,&Xiao J.L..(1991).Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years.Quaternary Research,36(1),29-36.
MLA	An Z.S.,et al."Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years".Quaternary Research 36.1(1991):29-36.

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