中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A perspective on the archaeology of the Pleistocene-Holocene transition in North China and the Qinghai-Tibetan Plateau

文献类型:期刊论文

作者Huang, WW(黄慰文) ; Hou, YM(侯亚梅)
刊名QUATERNARY INTERNATIONAL
出版日期1998
卷号50期号:0页码:117—127
ISSN号1040-6182
通讯作者Huang, WW (reprint author), Acad Sinica, Inst Vertebrate Paleontol & Paleoanthropol, POB 643, Beijing 100044, Peoples R China.
中文摘要According to geological research, North China was in a dry-cold stage from 25,000 to 10,000 BP, which can be correlated temporally with Oxygen isotope stage 2 of the deep-sea record. Since ca. 10,000 BP, North China and the Qinghai-Tibetan Plateau entered the Holocene warm stage. Though there have been some shifts from cool to warm and from dry to humid in this stage, and several cold events can be recognized in many places, the general tendency has been toward warming. Along with the environmental amelioration at the end of the Pleistocene, human occupation in these regions emerged in more vigorous condition than ever before. The scale of migration and diffusion reached a maximum in the Optimum of the middle Holocene. Archaeologically, the most obvious sign of the Pleistocene-Holocene transition was the development of microliths. (C) 1998 INQUA/Elsevier Science Ltd. All rights reserved.
公开日期2013-11-27
源URL[http://119.78.100.205/handle/311034/4000]  
专题古脊椎动物与古人类研究所_古人类及旧石器研究室
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Huang, WW,Hou, YM. A perspective on the archaeology of the Pleistocene-Holocene transition in North China and the Qinghai-Tibetan Plateau[J]. QUATERNARY INTERNATIONAL,1998,50(0):117—127.
APA Huang, WW,&Hou, YM.(1998).A perspective on the archaeology of the Pleistocene-Holocene transition in North China and the Qinghai-Tibetan Plateau.QUATERNARY INTERNATIONAL,50(0),117—127.
MLA Huang, WW,et al."A perspective on the archaeology of the Pleistocene-Holocene transition in North China and the Qinghai-Tibetan Plateau".QUATERNARY INTERNATIONAL 50.0(1998):117—127.

入库方式: OAI收割

来源:古脊椎动物与古人类研究所

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