Optically stimulated luminescence dating of Paleolithic sites reveals population shifts in North China during the last glacial period

doi:10.1016/j.gloplacha.2023.104339

IVPP-IR

	Optically stimulated luminescence dating of Paleolithic sites reveals population shifts in North China during the last glacial period
	Ge, Junyi 1,2; Sun, Xiao 3; Li, Yan 3; Wang, Chunxue 4; Sheng, Lishuang 5; Hu, Ke 3; Hua, Jiequn 1,2; Zhang, Xiaoling 1; Huan, Faxiang 1,2; Yang, Shixia 1; Olsen, John W.6,8; Gao, Xing1,2 ; Deng, Chenglong 2,7
	2024-02-01
发表期刊	GLOBAL AND PLANETARY CHANGE
ISSN	0921-8181
卷号	233 页码:13
通讯作者	Ge, Junyi(gejunyi@ivpp.ac.cn) ; Wang, Chunxue(chunxuewang@163.com) ; Olsen, John W.(olsenj@arizona.edu)
摘要	The Greater Khingan and Yanshan mountain ranges in northern China not only constitute a significant physical obstacle to the northward movement of monsoon circulation, but also represent a natural barrier for human migration and cultural interactions between in-migrating Paleolithic populations and those indigenous to East Asia during the Late Pleistocene. We dated two Paleolithic sites, Yangzhuangxishan and Taiziling, located in the southern piedmont of the Yanshan Mountains with artifacts typified by simple core and flake technology associated with foraging populations, to -39-29 ka and - 52-47 ka respectively, using the optically stimulated luminescence dating method. Our results indicate that northern China as far south as the Yanshan Mountains was occupied mainly by autochthonous East Asian Paleolithic populations using a core and flake lithic technology, although during this period Initial Upper Paleolithic (IUP) modern humans and Mousterian populations dispersed into East Asia. By synthesizing and integrating the ages of Northeast Asian Paleolithic sequences during the last glacial period (ca. 70-10 ka), we analyzed spatio-temporal variations in Late Pleistocene human populations during relatively cold stadial events (MIS 4 & 2) and warmer interstadials (e.g., MIS 3), revealing an "ebb and flow" pattern for migrations of Western IUP/Mousterian populations and indigenous core and flake technology populations in East Asia corresponding to the advance and retreat of the East Asian monsoon regime. The subsequent extremely cold climate phase engendered a major population shift during the Last Glacial Maximum (ca. 26.5-19 ka) which drove the reduction of both these Paleolithic populations, but afterward facilitated the emergence and rapid dispersal of microlithic technologies in East Asia. The peoples associated with microlithic technologies achieved their maximum geographical extent after the Bolling-Allerod Late Glacial interstadial event (ca. 14.7-12.9 ka) and then gradually decreased, perhaps due to the development of agriculture after -13 ka with concomitant increasing settlement stability.
关键词	Late Pleistocene hunter-gathers IUP population changes Core and flake technology Microlithic technology East Asian monsoon
DOI	10.1016/j.gloplacha.2023.104339
关键词[WOS]	MICROBLADE TECHNOLOGY ; DENISOVA CAVE ; K-FELDSPAR ; QUARTZ ; SINGLE ; IRSL ; SEDIMENTS ; HISTORY ; RATES ; ASIA
收录类别	SCI
语种	英语
资助项目	National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41977380] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA2004010102] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000] ; Second Tibetan Plateau Scientific Expedition and Research[2019QZKK0601] ; National Social Science Foundation of China[21@WTK001] ; Chinese Academy of Sciences President's International Fellowship Initiative Award (PIFI)[2018VCA0016] ; Je Tsongkhapa Endowment for Central and Inner Asian Archaeology at the University of Arizona
项目资助者	National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Second Tibetan Plateau Scientific Expedition and Research ; National Social Science Foundation of China ; Chinese Academy of Sciences President's International Fellowship Initiative Award (PIFI) ; Je Tsongkhapa Endowment for Central and Inner Asian Archaeology at the University of Arizona
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:001154755700001
出版者	ELSEVIER
引用统计
文献类型	期刊论文
条目标识符	http://119.78.100.205/handle/311034/23162
专题	中国科学院古脊椎动物与古人类研究所
通讯作者	Ge, Junyi; Wang, Chunxue; Olsen, John W.
作者单位	1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing, Peoples R China 2.Univ Chinese Acad Sci, Beijing, Peoples R China 3.China Univ Geosci Beijing, Sch Ocean Sci, Beijing, Peoples R China 4.Jilin Univ, Changchun, Peoples R China 5.Tianjin Cultural Heritage Protect Ctr, Tianjin, Peoples R China 6.Univ Arizona, Sch Anthropol, Tucson, AZ 85721 USA 7.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 8.Russian Acad Sci, Inst Archaeol & Ethnog, Siberian Branch, Novosibirsk, Russia
推荐引用方式 GB/T 7714	Ge, Junyi,Sun, Xiao,Li, Yan,et al. Optically stimulated luminescence dating of Paleolithic sites reveals population shifts in North China during the last glacial period[J]. GLOBAL AND PLANETARY CHANGE,2024,233:13.
APA	Ge, Junyi.,Sun, Xiao.,Li, Yan.,Wang, Chunxue.,Sheng, Lishuang.,...&Deng, Chenglong.(2024).Optically stimulated luminescence dating of Paleolithic sites reveals population shifts in North China during the last glacial period.GLOBAL AND PLANETARY CHANGE,233,13.
MLA	Ge, Junyi,et al."Optically stimulated luminescence dating of Paleolithic sites reveals population shifts in North China during the last glacial period".GLOBAL AND PLANETARY CHANGE 233(2024):13.