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

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dc.title Pleistocene climate change, natural environments and palaeolithic occupation of the Altai area, west-central Siberia en
dc.contributor.author Chlachula, Jiří
dc.relation.ispartof Quaternary International
dc.identifier.issn 1040-6182 OCLC, Ulrich, Sherpa/RoMEO, JCR
dc.date.issued 2001
utb.relation.volume 80-81
utb.relation.issue 2001
dc.citation.spage 131
dc.citation.epage 167
dc.type article
dc.language.iso en
dc.publisher Elsevier, Pergamon Press en
dc.identifier.doi 10.1016/S1040-6182(01)00023-4
dc.relation.uri https://www.sciencedirect.com/science/article/pii/S1040618201000234
dc.subject klimatické změny cs
dc.subject zalednění cs
dc.subject ekosystémy cs
dc.subject Pleistocén cs
dc.subject Altaj cs
dc.subject Climate change en
dc.subject glaciations en
dc.subject ecosystems en
dc.subject Pleistocene en
dc.subject Altai en
dc.description.abstract 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. 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. en
utb.faculty Faculty of Technology
dc.identifier.uri http://hdl.handle.net/10563/1000019
utb.identifier.rivid RIV/70883521:28110/01:63500205
utb.identifier.obdid 11051745
utb.identifier.scopus 2-s2.0-0034815368
utb.identifier.wok 000171362400010
utb.source j-riv
utb.contributor.internalauthor Chlachula, Jiří
utb.fulltext.affiliation Jiri Chlachula Laboratory for Palaeocology, University Zlin, 762 72 Zlin, Czech Republic
utb.fulltext.dates -
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utb.fulltext.sponsorship Quaternary geology and geoarchaeology investigations (1997–2000) of the author in the broader Altai area were supported by the National Geographic Society, the Royal Society (London) and the NSERC of Canada.
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