The evolution of coupling of Asian winter monsoon and high latitude climate of Northern Hemisphere - Grain evidence from 8.1 Ma loess-red clay sequence on the Chinese central Loess Plateau

doi:10.1007/BF02911986

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室（1985-2004）

	The evolution of coupling of Asian winter monsoon and high latitude climate of Northern Hemisphere - Grain evidence from 8.1 Ma loess-red clay sequence on the Chinese central Loess Plateau
	Lu, LQ; Fang, XM; Mason, JA; Li, JJ; An, ZS
	2001-10
发表期刊	SCIENCE IN CHINA SERIES D-EARTH SCIENCES
卷号	44 页码:185-191
文章类型	Article
摘要	The evolution and driving mechanism of the Asian winter monsoon system are of great importance to understanding the present-day climate. Through high-resolution particle size analysis of the oldest loess-red clay sequence known so far (with a basal age of about 8 Ma) and comparison of the results with oxygen isotope curves from North Atlantic marine sediments, 4 stages of the evolution of the Asian winter monsoon were clearly demonstrated. During the first stage, between about 8.1 and 4.3 Ma, there was no relation between Asian winter monsoon and Northern Hemisphere ice volume and high latitude climate inferred from marine sediments. A weak relation developed during the second stage, about 4.3 to 3.5 Ma. During the third stage (3.5 to 2.6 Ma) an Asian winter monsoon system similar to the present formed, initiating a stronger relation between the winter monsoon and Northern Hemisphere ice volume and high latitude climate. In the final stage (2.6 to 0 Ma) the present Asian winter monsoon system was fortified and stabilized and changes in the winter monsoon system were almost in phase with Northern Hemisphere ice volume and climate. The staggered uplift of Tibetan Plateau at similar to8, 3.6, 2.6 Ma and later might be the driving force for the evolution of the Asian winter monsoon.
关键词	loess-red clay Loess Plateau winter monsoon Tibetan Plateau
学科领域	Geology
DOI	10.1007/BF02911986
关键词[WOS]	TIBETAN UPLIFT ; SOUTHERN ASIA ; AMERICAN WEST ; TIMESCALE ; DEPOSITS ; SIZE
收录类别	SCI ; SCIE
语种	英语
WOS研究方向	Geosciences, Multidisciplinary
WOS记录号	WOS:000175181800022
出版者	SCIENCE CHINA PRESS
引用统计	被引频次：34[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/11972
专题	黄土与第四纪地质国家重点实验室（1985-2004）
推荐引用方式 GB/T 7714	Lu, LQ,Fang, XM,Mason, JA,et al. The evolution of coupling of Asian winter monsoon and high latitude climate of Northern Hemisphere - Grain evidence from 8.1 Ma loess-red clay sequence on the Chinese central Loess Plateau[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2001,44:185-191.
APA	Lu, LQ,Fang, XM,Mason, JA,Li, JJ,&An, ZS.(2001).The evolution of coupling of Asian winter monsoon and high latitude climate of Northern Hemisphere - Grain evidence from 8.1 Ma loess-red clay sequence on the Chinese central Loess Plateau.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,44,185-191.
MLA	Lu, LQ,et al."The evolution of coupling of Asian winter monsoon and high latitude climate of Northern Hemisphere - Grain evidence from 8.1 Ma loess-red clay sequence on the Chinese central Loess Plateau".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 44(2001):185-191.