Spatial-temporal variations of Paleolithic human activities in Northeast China

IF 1.9 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
Niankang Chen , Bohan Ming , Yongxiang Chen , Haoyu Wang , Ying Zhao , Dongmei Jie , Guizai Gao , Honghao Niu
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Abstract

Northeast China played an irreplaceable role in population migrations and cultural exchanges in East Asia during the Paleolithic. This paper collected 182 archaeological sites to analyse the characteristics of spatial-temporal variations of Paleolithic human activities in Northeast China, and explored the driving mechanisms behind these variations in combination with the paleoenvironmental and archaeological studies. During the Lower Paleolithic, constrained by the relatively cold-dry climate and blocked by the Songnen paleo-lake basin, the population was sparse and distributed only near 40° N at the southern end of Northeast China. Upon entering the Middle Paleolithic, as humans developed greater tolerance to cold climates and adopted more sophisticated survival strategies with the application of small lithic tools, their numbers increased and geographical distribution expanded northward to 45° N at the central region of Northeast China. The Upper Paleolithic saw a considerable increase in population and expansion across almost all of Northeast China except for the eastern Inner Mongolia Plateau. We speculated that 50 ka and 30 ka BP were two key points, both of which may be associated with a significant increase in the frequency of migrations and communications among humans, and the widespread popularity of highly mobile microblade technology, respectively. In addition, the environmental analysis of archaeological sites revealed a continuous spread of Paleolithic humans to areas with higher elevations, steeper slopes, and lower temperatures. Meanwhile, they were becoming less reliant on water resources and were more widely conducting activities in open-air areas, showing that the environmental adaptability had been continuously improving over time. This study can provide a reference for the reconstruction of the migration history of early humans in East Asia, and is also of great significance for a comprehensive understanding of the evolutionary process of early human-environment interactions.

中国东北地区旧石器时代人类活动的时空变迁
中国东北地区在旧石器时代东亚人口迁移和文化交流中发挥了不可替代的作用。本文收集了182处考古遗址,分析了中国东北地区旧石器时代人类活动的时空变异特征,并结合古环境和考古学研究,探讨了这些变异背后的驱动机制。旧石器时代下期,受相对寒冷干燥气候的制约和松嫩古湖盆的阻隔,人口稀少,仅分布在东北地区南端北纬40°附近。进入旧石器时代中期后,随着人类对寒冷气候的耐受力增强,并应用小型石器采取了更复杂的生存策略,其数量有所增加,地理分布也向北扩展到中国东北中部地区的北纬 45°。上旧石器时代,除了内蒙古高原东部以外,几乎整个中国东北地区的人口都有了相当大的增长和扩张。我们推测,公元前 50 ka 和 30 ka 是两个关键点,这两个关键点可能分别与人类迁徙和交流频率的显著增加以及高移动性微刀技术的广泛普及有关。此外,对考古遗址的环境分析表明,旧石器时代的人类不断向海拔较高、山坡较陡、气温较低的地区扩散。同时,他们对水资源的依赖程度越来越低,在露天地区进行活动的范围也越来越广,这表明环境适应能力随着时间的推移在不断提高。这项研究可为重建东亚早期人类的迁徙史提供参考,对全面了解早期人类与环境互动的演化过程也具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Quaternary International
Quaternary International 地学-地球科学综合
CiteScore
5.60
自引率
4.50%
发文量
336
审稿时长
3 months
期刊介绍: Quaternary International is the official journal of the International Union for Quaternary Research. The objectives are to publish a high quality scientific journal under the auspices of the premier Quaternary association that reflects the interdisciplinary nature of INQUA and records recent advances in Quaternary science that appeal to a wide audience. This series will encompass all the full spectrum of the physical and natural sciences that are commonly employed in solving Quaternary problems. The policy is to publish peer refereed collected research papers from symposia, workshops and meetings sponsored by INQUA. In addition, other organizations may request publication of their collected works pertaining to the Quaternary.
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