Abstract
The described stone artifacts are recovered from the 70 m-high terrace (4600 m a.s.l.) at the southeastern shore of the Siling Co on the northern Tibetan Plateau. The terrace was formed during the Interstadial period before the LGM, ca. 40–30 ka B.P. based on paleoenvironmental research. The Paleoliths from the Siling Co provide evidence for early human occupation of the northern Tibetan Plateau. They show technological and typological affinities with the European Middle Paleolithic suggesting that the early human occupation here might relate to migratory waves during the Late Pleistocene that dispersed humans across the Old World.
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References
Moore L G, Niermeyer S, Zammudio S. Human adaptation to high altitude: Regional and life-cycle perspectives. Yearbook of Physical Anthropology, 1998, 41: 25–64
Beall C. Adaptations altitude: A current assessment. Annu Rev Anthropol, 2001, 30: 423–456
Moore L G, Curran-Everett L, Dromaet T S, et al. Are Tibetans better adapted? Int J Sports Med, 1992, 13(suppl 1): 86–88
Niermeyer S, Yang P, Zhuang J, et al. Arterial oxygen saturation in Tibetan and Han infants born in Lhasa, Tibet. New Engl J Med, 1995, 333: 1248–1252
Debenath A, Dibble H L. Handbook of Paleolithic Typology. Vol 1: Lower and Middle Paleolithic of Europe. Library of Cataloging-in-Publication Data, University Museum of Pennsylvania, Philadelphia, 1994. 1–202
Huang W W. The prehistoric human occupation of the Qinghai-Xizang plateau. Göttinger Geogr Abhand, 1994, 95: 201–219
Frenzel B, Huang W, Liu S. Stone artifacts from south-central Tibet, China. “Quartär”, 2001, 51/52: 33–53
Shi Y F, Jia Y L, Yu G, et al. Features, impacts and causes of the high temperatures and large precipitation event in the Tibetan Plateau and its adjacent area during 40–30 ka B.P. J Lake Sci (in Chinese), 2002, 14(1): 1–11
Zheng M P, Yuan H R, Zhao X T, et al. The Quaternary Pan-lake(Overflow) Period and paleoclimate on the Qinghai-Tibetan Plateau. Acta Geol Sin (in Chinese), 2006, 80(2): 169–180
Li B Y. The last greatest lakes on the Xizang (Tibetan) Plateau. Acta Geogr Sin (in Chinese), 2000, 55(2): 174–182
Nomura R, Kashiwaya K, Tanaka S, et al. The geomorphic features on the coast of Siling-Co and lake level fluctuations in the Qing-Zang (Tibetan) Plateau. Geomorph Union, 1992, 13(2): 125–140
Lu P, Qu Y H, Li Q W, et al. Selincuo and Bangecuo extensional lake basins in the northern part of Tibet and present chasmic activities. Jilin Geol (in Chinese), 2003, 22(2): 15–19
Gasse F, Arnold M, Fontes J C, et al. A 13000-year climate record from western Tibet. Nature, 1991, 353: 742–745
Gu Z Y, Liu J Q, Yuan B Y, et al. Lacustrine authigenic deposition expressive of environment and the sediment record from Siling Co, Xizang(Tibet). China Quat Sci (in Chinese), 1994, 2: 162–174
Shi Y F, Yu G. Warm-humid climate and transgressions during 40–30 ka B.P. and their potential mechanisms. Quat Sci (in Chinese), 2003, 23(1): 1–11
Du N Q, Kong Z C. Palynoflora of the Qarhan Saline Lake and its significance in geography and botany—the sporo-poilen assemblages from CK2022 drilling core at the Bieletan. Acta Botanic Sin (in Chinese), 1983, 25(3): 275–282
Huang W W, Chen K Z, Yuan B Y. Paleolithic artifacts from Xiao Qaidam, Qinghai Province. In: Sino-Australian Quaternary Cooperative Research Team, Chinese Academy of Sciences, eds. Papers of Sino-Australian Quaternary Conference (in Chinese). Beijing: Science Press, 1987. 168–175
Zhang D D, Li S H. Optical dating of Tibetan human hand-and footprings: An implication for the palaeoenvironment of the last glaciation of the Tibetan Plateau. Geophys Res Lett, 2002, 29(5): 1072
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Supported by the RGC project “Ice age Tibetans and their living environment” HKSRA Government
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Yuan, B., Huang, W. & Zhang, D. New evidence for human occupation of the northern Tibetan Plateau, China during the Late Pleistocene. CHINESE SCI BULL 52, 2675–2679 (2007). https://doi.org/10.1007/s11434-007-0357-z
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DOI: https://doi.org/10.1007/s11434-007-0357-z