4.4 Article

Determination of the source for prehistoric obsidian artifacts from the lower reaches of Kolyma River, Northeastern Siberia, Russia, and its wider implications

Journal

QUATERNARY INTERNATIONAL
Volume 476, Issue -, Pages 95-101

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quaint.2018.02.017

Keywords

Archaeology; Obsidian sourcing; Kolyma river; Neolithic; Lake Krasnoe; Chukotka; Northeastern Siberia

Funding

  1. U.S. Civil Research and Development Foundation [RG1-2538-VL-03, RUG1-7097-NO-13]
  2. Tomsk State University Competitiveness Improvement Program
  3. U.S. National Science Foundation [NSF-1621158]

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Geochemical analysis of 102 obsidian artifacts from the lower reaches of the Kolyma River was performed to understand the provenance of the raw material; previously, there were no such studies in this region. Sites under investigation belong to the Arctic Neolithic, generally dated to ca. 6000-1500 BP. Based on the data for potential obsidian sources in Northeastern Siberia and neighboring territories, available to us, it was found that all obsidian artifacts originated from the Lake Krasnoe source in Chukotka, with a straight-line distance of ca. 800-1100 km from archaeological sites of the Kolyma River. This is a remarkable example of long-distance exchange/transport of obsidian in Northeastern Siberia during the Stone Age. The Lake Krasnoe locale was the primary obsidian source for prehistoric populations in this vast region, including Chukotka, the Kolyma River basin, and Okhotsk Sea coast; this obsidian was also identified at some Alaskan sites near the Bering Strait. (C) 2018 Elsevier Ltd and INQUA. All rights reserved.

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