陕西榆林和河南洛阳地区4 ka BP前后聚落演化差异及其古气候原因

doi:10.7605/gdlxb.2015.06.069

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Abstract

We analyzed the change of settlement density in Yulin area of Shaanxi Province and Luoyang area of Henan Province around 44 Ka BP. The culture of these two areas were both well developed during the period of Longshan (before 44 Ka BP) and the settlement densities of the two areas were on top of the list in China at that time. The further increase of the settlement density occured in Luoyang area during the period of the Xia and Shang Dynasties (after 44 Ka BP), but the density of population and settlement declined sharply in Yulin area after 44 Ka BP，which obviously reflected the decline of the culture. According to the geographical position differences，the mean annual precipitation in Luoyang area is 200mm higher than Yulin area. The landform of the loess hills is the main human activity place in Yulin area，where the limited water resource of river is not easy to be used. The development of dry farming mainly depends on the rainfall. The rainfall is abundant in Luoyang area and human beings can conveniently use river water resources in basin plain. So the fluctuations of the rainfall cannot influence the development of dry farming. The study of palaeoclimate showed that there was a significant climate event around 44 Ka BP. After this climate event，the mean annual precipitation declined approximately from 650mm to 500mm in Luoyang area. But it was still higher than the minimum precipitation that dryland farming needed. So the human culture could develop much further. The mean annual precipitation declined approximately from 450mm to 350mm in Yulin area，which made the climate change from sub-humid to semi-arid. The climate change made dryland farming cannot develop further. This study proves that the differences of the geographical setting and environmental characteristics between the two areas are the basic factors that affect their respective cultural evolution. The climate event around 44 Ka BP is the direct driving factor that leads to two different results．

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	Articles by authors
	Wang Jianjun
	Hu Ke
	Lu Peng
	Mo Duowen
	Jin Yuxiang
	Jiang Jiaqi
	Lü Jianqing

Key words： Yulin area Luoyang area settlement distribution environmental characteristics climate factor

Received: 15 June 2015 Published: 01 December 2015

ZTFLH:

K901.6

Corresponding Authors: Mo Duowen，born in 1955，is a professor of Peking University. He is mainly engaged in geomorphologic processes and sedimentation，environmental evolution and environmental archaeology. E-mail: dmo@urban.pku.edu.cn

About author: Wang Jianjun，born in 1988，is a master degree candidate of Peking University. His research direction is geomorphology，environmental evolution and environmental archaeology. E-mail: wangjjun_pku@163.com．

Cite this article:

Wang Jianjun,Hu Ke,Lu Peng et al. Difference and its palaeoclimate reason of settlement evolution between Yulin area of Shaanxi Province and Luoyang area of Henan Province around 44 Ka BP[J]. JOPC, 2015, 17(6): 841-850.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2015.06.069 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2015/V17/I6/841

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