Environmental change since mid-Pleistocene recorded in Shangshan   achaeological site of Zhejiang

doi:10.1007/s11442-008-0247-6

CORC > 北京大学 > 城市与环境学院

	Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang
	Mao Longjiang ; Mo Duowen ; Jiang Leping ; Jia Yaofeng ; Liu Xiaoyan ; Li Minglin ; Zhou Kunshu ; Shi Chenxi
刊名	journal of geographical sciences
	2008
关键词	environmental change reticulate red clay TL/OSL dating mid-Pleistocene Shangshan culture Zhejiang PLATEAU CHINA
DOI	10.1007/s11442-008-0247-6
英文摘要	At about 173 ka BP of the late period of mid-Pleistocene, the second terrace of the river had been formed as a result of uplift happening in Shangshan area because of the climate, sea level change and tectonic action. Between 173-75 ka BP, aeolian deposited on the terrace, a layer of reticulate red clayey soil about 80-100 cm thick deposited and developed under the warmer and higher temperature. In the last glacial period, the drop of the temperature and the decrease of the precipitation induced the dust-storms increased, A layer of Xiashu loess about 1.0-1.5 m thick accumulated on Shangshan terrace in the last glacial, which has the reticulate red clayey soil buried. At the beginning of the Holocene (11500 a BP-), temperature went higher gradually and precipitation got more, the pre-persons moved on the Shangshan terrace (11,400-8600 a BP), which is one of the most important archaeological sites, and can connect the paleolithic culture with Neolithic culture. It could be assumed from the results that the lower reaches of the Yangtze River are the home of rice cultivation, too. The lower place to the west of the Shangshan site experienced the two cycles process of the fluvial facies and the lacustrine facies, indicating that the water source of the pre-historical Shangshan is the river water or lake water. Two AIVIS (14)C age proved the water source disappeared more than 1000 years ago.; http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000254970800011&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 ; Geography, Physical; SCI(E); 中国科技核心期刊(ISTIC); 中国科学引文数据库(CSCD); 5; 2; 247-256; 18
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/161166]
专题	城市与环境学院
推荐引用方式 GB/T 7714	Mao Longjiang,Mo Duowen,Jiang Leping,et al. Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang[J]. journal of geographical sciences,2008.
APA	Mao Longjiang.,Mo Duowen.,Jiang Leping.,Jia Yaofeng.,Liu Xiaoyan.,...&Shi Chenxi.(2008).Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang.journal of geographical sciences.
MLA	Mao Longjiang,et al."Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang".journal of geographical sciences (2008).