Prehistoric human occupation and adaptation on the hinterland of the Tibetan Plateau in the Early Holocene

Author:

Jin Sunmei12ORCID,Hou Guangliang123,Chen Youcheng4,Qiao Hong5,Han Bin6,E Chongyi78,LanCuo Zhuoma9,Gao Jingyi78,WenDe Zhuoma78

Affiliation:

1. Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), College of Geographical Science, Qinghai Normal University, Xining, China

2. Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining, China

3. Academy of Plateau Science and Sustainability, People’s Government of Qinghai Province and Beijing Normal University, Xining, China

4. School of History, Capital Normal University, Beijing, China

5. Qinghai Provincial Institute of Cultural Relics and Archaeology, Xining, China

6. Department of Archaeology and Anthropology, School of Humanities, University of Chinese Academy of Sciences, Beijing, China

7. Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), College of Geographical Science, Qinghai University, Xining, China

8. Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai University, Xining, China

9. School of Finance and Economics, Qinghai University, Xining, China

Abstract

The occupation process and survival strategies of prehistoric humans on the Tibetan Plateau are important scientific questions for understanding human adaptation to extreme high-altitude environments. Here, we report a newly discovered microlithic site at Daiqu (DQ) in the Tongtian River basin of the central-eastern plateau. We collected 239 lithic artifacts from the DQ site for typological analysis. OSL and AMS14C dating samples were collected from the human active layer. Lipid residues from hearth sediments were analyzed, and we simulated and assessed environmental extremity and route accessibility for the site. Dating results suggest that the stable sedimentary layers began to form around 10.96 ± 0.56 ka BP at the DQ site. Human activity at DQ as early as 9271 ± 143 cal a BP, making it the earliest reported Holocene site with accurate stratigraphic dating on the plateau hinterland to date. Hearths and lithic artifacts indicate that the DQ site was a frequently used seasonal hunting camp, where quality lithic raw material was obtained and microliths processed. Prehistoric humans occupying the site relied on non-ruminant terrestrial animals as food resources. The DQ site is ideally situated to serve as a transit station for hunter-gatherers as they migrated between high and low elevations. Ameliorating Holocene climate promoted prehistoric human exploration of more environmentally extreme areas.

Funder

National Natural Science Foundation of China

Publisher

SAGE Publications

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous),Geography, Planning and Development

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