Arid
DOI10.1002/jqs.1180
Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3
Wen, Xiaohao1; Li, Baosheng1,3; Zheng, Yanming1; Zhang, David Dian2; Ye, Jianping1
通讯作者Li, Baosheng
来源期刊JOURNAL OF QUATERNARY SCIENCE
ISSN0267-8179
EISSN1099-1417
出版年2009
卷号24期号:1页码:61-74
英文摘要

Fluctuations in climatic proxies of the Milanggouwan section in the Salawusu River valley of the Ordos Plateau (inner Mongolia, China) during Marine Isotope stage 3 (MIS 3) coincide well with sedimentary cycles for palaeo-mobile dune sands alternating with fluvial-lacustrine facies and palaeosols. We compared the palaeo-mobile dune sands with modern mobile dune sands (products of a cold and dry climate dominated by the East Asian winter monsoon), whereas the fluvial-lacustrine facies and palaeosols, were controlled by a wet-warm climate similar to that of the East Asian summer monsoon. The MIS 3 climate of the Salawusu River valley appears to have experienced at least nine wet-warn) and ten cold-dry fluctuations, divided into five stages: MIS 3e (58 900-49 500 yr BP), MIS 3d (49 500-40 700 yr BP), MIS 3c (40 700-36 900 yr BP), MIS 3b (36 900-27 000 yr BP) and MIS 3a (27 000-22 300 yr BK The 19 cold-warm climatic fluctuations corresponded roughly to the GRIP and Guliyan records, and with fluctuations in the North Atlantic climate. Notable peaks in the spectral analysis Occurred at 19 500 yr, 1020 yr, 640 yr and 500 yr. Our results show that the millennial-centennial climate was closely related to the relative strengths of East Asian monsoons, which are controlled by the North Atlantic thermohaline circulation, and which is also closely linked to the Sun’s precession period. Copyright (C) 2008 John Wiley & Sons, Ltd.


英文关键词Salawusu River valley climate variability Marine Isotope Stage 3 (MIS 3) East Asian monsoon Chenchuan Formation
类型Article
语种英语
国家Peoples R China
收录类别SCI-E
WOS记录号WOS:000262615700006
WOS关键词LAST INTERGLACIAL PERIOD ; MU US DESERT ; 150 KA BP ; NORTH-ATLANTIC ; EUROPE ; ICE ; RECORD ; GLACIATION ; SECTION ; OCEAN
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
来源机构中国科学院地球环境研究所
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/161748
作者单位1.S China Normal Univ, Sch Geog Sci, Guangzhou 510631, Guangdong, Peoples R China;
2.Univ Hong Kong, Dept Geog, Hong Kong, Hong Kong, Peoples R China;
3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China
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GB/T 7714
Wen, Xiaohao,Li, Baosheng,Zheng, Yanming,et al. Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3[J]. 中国科学院地球环境研究所,2009,24(1):61-74.
APA Wen, Xiaohao,Li, Baosheng,Zheng, Yanming,Zhang, David Dian,&Ye, Jianping.(2009).Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3.JOURNAL OF QUATERNARY SCIENCE,24(1),61-74.
MLA Wen, Xiaohao,et al."Climate variability in the Salawusu River valley of the Ordos Plateau (Inner Mongolia, China) during Marine Isotope Stage 3".JOURNAL OF QUATERNARY SCIENCE 24.1(2009):61-74.
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