Climate background of the evolution from Paleolithic to Neolithic   cultural transition during the last deglaciation in the middle reaches   of the Yellow River

doi:10.1360/02tb9014

CORC > 北京大学 > 城市与环境学院

	Climate background of the evolution from Paleolithic to Neolithic cultural transition during the last deglaciation in the middle reaches of the Yellow River
	Xia, ZK ; Chen, G ; Zheng, GW ; Chen, FY ; Han, JQ
刊名	科学通报英文版
	2002
关键词	Jixian County in Shanxi Province Shizitan site sporopollen analysis last deglaciation Paleolithic-Neolithic cultural transition
DOI	10.1360/02tb9014
英文摘要	Shizitan in Jixian County, Shanxi Province, is a site of transitional period from Paleolithic to Neolithic. The dating and the sporopollen analysis show that the middle reaches of the Yellow River where the site is located had been maintaining a steppe environment during 35.1-9.4 kaBP, in which, 35.1-17 kaBP belonged to the last glacial. With cold and dry climate, this period featured a desert steppe environment. In the late of this period, the area had a cold and half-humid steppe environment. The 17.0-11.9 kaBP belonged to the early- and mid-period of the last deglaciation. Mild and half-arid steppe alternates with mild and half-arid steppe, with a small amount of deciduous broadleaf species. During the period of 11.9-10.5 kaBP, cold and dry glacial climate appeared once more, featuring a desert steppe environment. During 10.5-9.4 kaBP, it is mild and half-arid, and later transited toward warm and half-humid. The early phase of this period featured a steppe environment and the later transited into a steppe environment with fairly more deciduous broadleaf species. Microlith, a mark of a transitional period from Paleolithic to Neolithic, was distributed mainly in 17.0-11.9 kaBP. The relatively warm, half-arid and fluctuating steppe environment in the early and medium period of the last deglaciation made a contribution to the appearance and development of Microlithic culture.; http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000173988800014&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 ; Multidisciplinary Sciences; SCI(E); 13; ARTICLE; 1; 71-75; 47
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/160889]
专题	城市与环境学院
推荐引用方式 GB/T 7714	Xia, ZK,Chen, G,Zheng, GW,et al. Climate background of the evolution from Paleolithic to Neolithic cultural transition during the last deglaciation in the middle reaches of the Yellow River[J]. 科学通报英文版,2002.
APA	Xia, ZK,Chen, G,Zheng, GW,Chen, FY,&Han, JQ.(2002).Climate background of the evolution from Paleolithic to Neolithic cultural transition during the last deglaciation in the middle reaches of the Yellow River.科学通报英文版.
MLA	Xia, ZK,et al."Climate background of the evolution from Paleolithic to Neolithic cultural transition during the last deglaciation in the middle reaches of the Yellow River".科学通报英文版 (2002).