Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing

doi:10.1007/BF02878963

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

	Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing
	An, ZS; Wang, SM; Wu, XH; Chen, MY; Sun, DH; Liu, XM; Wang, FB; Li, L; Sun, YB; Zhou, WJ; Zhou, J; Liu, XD; Lu, HY; Zhang, YX; Dong, GG; Qiang, XK
	1999-06
发表期刊	SCIENCE IN CHINA SERIES D-EARTH SCIENCES
卷号	42 期号:3 页码:258-271
文章类型	Article
摘要	On the basis of a newly-constructed record of magnetic susceptibility (SUS) and the depositional rate change of eolian loess-red clay sequences in the last 7.2 Ma BP from the Loess Plateau, together with a comparison of a record of delta(18)O values from the equatorial East Pacific Ocean and eolian Quartz nux variations from the North Pacific Ocean, the evolutionary process of the Late Cenozoic Great Glaciation in the Northern Hemisphere can be divided into three stages: the arrival stage around 7.2-3.4 Ma BP, the initial stage at shout 3.4-2.6 Ma BP, and the Great Ice Age since 2.6 Ma BP. The evolution of the East Asian monsoon is characterized by paired winter and summer monsoons, and it is basically composed of the initial stage of weak winter and summer monsoons, the transitional stage of simultaneous increase in intensity of winter and summer monsoons, and the prevailing stage of strong winter and weak summer monsoons, or weak winter and strong summer monsoons. The Late Cenozoic global tectonic uplift, particularly the Qinghai-Xizang Plateau uplift and the associated CO2 concentration variation, controls the cooling processes of the onset of Great Glaciation and the long-term changes of East Asian monsoom climate in the Northern Hemisphere to a large extent. The accelerating uplift of the Qinghai-Xizang Plateau between 3.4 and 2.6 Ma BP provided an important driving force to global climiatic change.
关键词	Late Cenozoic eolian deposits of Loess Plateau Great Glaciation in the Northern Hemisphere East Asian monsoon evolution Qinghai-Xizang Plateau uplift
学科领域	Geology
DOI	10.1007/BF02878963
关键词[WOS]	SOUTHERN ASIA ; AMERICAN WEST ; EVOLUTION ; CLIMATE ; BASIN ; HIMALAYA ; HISTORY
收录类别	SCI ; SCIE
语种	英语
WOS研究方向	Geosciences, Multidisciplinary
WOS记录号	WOS:000081744900005
出版者	SCIENCE PRESS
引用统计	被引频次：72[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/361006/11911
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	An, ZS,Wang, SM,Wu, XH,et al. Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,1999,42(3):258-271.
APA	An, ZS.,Wang, SM.,Wu, XH.,Chen, MY.,Sun, DH.,...&Qiang, XK.(1999).Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,42(3),258-271.
MLA	An, ZS,et al."Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 42.3(1999):258-271.