Pleistocene climate change, natural environments and palaeolithic occupation of the Altai area, west-central Siberia

Citation data:

Quaternary International, ISSN: 1040-6182, Vol: 80, Issue: 2001, Page: 131-167

Publication Year:
2001
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Repository URL:
http://publikace.k.utb.cz/handle/10563/1000019; http://hdl.handle.net/10563/1000019
DOI:
10.1016/s1040-6182(01)00023-4
Author(s):
Chlachula, Jiří
Publisher(s):
Elsevier BV; Elsevier, Pergamon Press
Tags:
Earth and Planetary Sciences; klimatické změny; zalednění; ekosystémy; Pleistocén; Altaj; Climate change; glaciations; ecosystems; Pleistocene; Altai
article description
Diversity of the relief and the Pleistocene environments of the mountain areas of SW Siberia played a major role in the history of the palaeolithic peopling of this territory. The geographical and contextual distribution of the cultural records reflects a climatic instability in the Altai area. Palaeoenvironmental proxy data indicate that the natural conditions during the earlier stages were generally more favourable for early human occupation than during the later stages. The cyclic nature of the glacial and interglacial periods led to periodic landscape transformations and generation of specific ecosystems adjusted to particular topographic settings and responding to climatic variations.