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The scope of movement of modern humans during the Late Pleistocene in Northeast Asia
CHOI Cheolmin, GAO Xing, XIA Wenting, ZHONG Wei
Acta Anthropologica Sinica    2021, 40 (01): 12-27.   DOI: 10.16359/j.cnki.cn11-1963/q.2019.0055
Abstract   (626 HTML91 PDF(pc) (835KB)(413)  

Due to the development of technology and the increase in the number of specialized researchers, a considerable amount of Late Pleistocene sites have been found in Northeast Asia. Issues concerning modern human fossils, Pleistocene environment, lithic manufacturing techniques and human adaptation have been debated based on these archaeological sites. In particular, the provenance analysis of special raw materials as obsidian enables the researches on the movement and the scope of activities of modern humans during the late Pleistocene who had to continuously be on the move for survival. Most researchers have estimated the mobility of hunter-gatherers based on ethnographic researches. The direct and indirect scope of migration of the modern humans can be assumed through the range of Tanged Points and obsidian artifacts of Mt. Baekdu(Changbai). Unlike other lithic manufacturing techniques, the obsidian artifacts were not passed on to several generations but usually used and discarded by a single generation. Benefited from obsidian’s unique chemical composition, it could been seen as the most reliable evidence to indicate the scope of migration.
Lithic manufacturing techniques such as Levallois, Crest, and Yubetsu were widely disseminated over a long time, which is not appropriate to use these lithic techniques to estimate the scope of movement of modern humans. However, the Tanged Point, which had been popularly utilized in a short chronological period and enjoyed a limited distribution in the Northeast Asian region. Based on the distribution of obsidian artifacts from Mt. Baekdu (Changbai) and the Tanged Points, the scope of activity of the modern humans during the Late Pleistocene (MIS 2) is estimated as 193,000~520,000 km2.


遗址 Sites 地层 Layer 年代(BP) Age 测年方法 Dating method 样品号 Sample No. 样品类型
Sample type
参考文献
Reference
好坪洞(Hopyeong-dong) 3a 16190±50 AMS GX-29424 sediment [50]
好坪洞(Hopyeong-dong) 3a 16600±720 AMS GX-29423 sediment [50]
好坪洞(Hopyeong-dong) 3a 16900±500 AMS SNU02-324 charcoal [50]
好坪洞(Hopyeong-dong) 3a 17400±400 AMS SNU02-326 charcoal [50]
好坪洞(Hopyeong-dong) 3a 23900±400 AMS SNU03-841 charcoal [50]
好坪洞(Hopyeong-dong) 3a 24100±200 AMS SNU03-839 charcoal [50]
长兴里(Jangheung-ri) 2 24200±600 AMS SNU00-380 charcoal [51]
下花溪里III(Hahwagye-ri III) 2 13390±60 AMS SNU02-214 charcoal [52]
石壮里(Seokjang-ri) 20830±1,880 AMS AERIK-8 charcoal [53]
中里(Neulgeo-ri) 2 21240±150 AMS SNU13-373 charcoal [54]
新北(Sinbuk) 18500±300 AMS SNU03-912 charcoal [41]
新北(Sinbuk) 25500±100 AMS SNU03-914 charcoal [41]
Tab.3 Dates for excavated sites with obsidian artifacts in the Korean peninsula.
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