A perspective on the archaeology of the Pleistocene-Holocene transition in North China and the Qinghai-Tibetan Plateau

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	A perspective on the archaeology of the Pleistocene-Holocene transition in North China and the Qinghai-Tibetan Plateau
	Huang, WW; Hou, YM; Huang, WW (reprint author), Acad Sinica, Inst Vertebrate Paleontol & Paleoanthropol, POB 643, Beijing 100044, Peoples R China.
	1998
发表期刊	QUATERNARY INTERNATIONAL
ISSN	1040-6182
卷号	50 期号:0 页码:117-127
文章类型	Article
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.; 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.
WOS标题词	Science & Technology ; Physical Sciences
收录类别	ISTP ; SCI
语种	英语
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:000074899300010
引用统计	被引频次：15[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://119.78.100.205/handle/311034/3999
专题	古人类及旧石器研究室
通讯作者	Huang, WW (reprint author), Acad Sinica, Inst Vertebrate Paleontol & Paleoanthropol, POB 643, Beijing 100044, Peoples R China.
作者单位	Acad Sinica, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
推荐引用方式 GB/T 7714	Huang, WW,Hou, YM,Huang, WW . 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,&Huang, WW .(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.