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Pleistocene climate change, natural environments and palaeolithic occupation of the upper Yenisei area, south-central Siberia

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dc.title Pleistocene climate change, natural environments and palaeolithic occupation of the upper Yenisei area, south-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
dc.citation.spage 101
dc.citation.epage 130
dc.type article
dc.language.iso en
dc.publisher Elsevier, Pergamon Press en
dc.identifier.doi 10.1016/S1040-6182(01)00022-2
dc.relation.uri https://www.sciencedirect.com/science/article/pii/S1040618201000222
dc.subject klimatické změny cs
dc.subject spraše cs
dc.subject vegetační pásma cs
dc.subject paleolit cs
dc.subject Jenisej cs
dc.subject Climate change en
dc.subject loess en
dc.subject vegetation zones en
dc.subject paleolithic en
dc.subject Yenisei en
dc.description.abstract The upper Yenisei River area is of major importance for mapping the Pleistocene climate evolution over Siberia. An extensive loess cover with a suite of buried palaeosols from the Northern Minusinsk Basin has provided one of the most complete, high resolution Late Quaternary palaeoclimatic archives in north-central Asia. The loess-palaeosol records indicate establishment of periglacial steppe-tundra during cold stadial intervals, replaced by parkland steppe and boreal forest during warm interstadial intervals. en
utb.faculty Faculty of Technology
dc.identifier.uri http://hdl.handle.net/10563/1000021
utb.identifier.rivid RIV/70883521:28110/01:63500207
utb.identifier.obdid 11051744
utb.identifier.scopus 2-s2.0-0034816685
utb.identifier.wok 000171362400009
utb.source j-riv
utb.contributor.internalauthor Chlachula, Jiří
utb.fulltext.affiliation Jiri Chlachula Laboratory for Palaeoecology, University Zlin, 762 72 Zlin, Czech Republic
utb.fulltext.dates -
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utb.fulltext.sponsorship Quaternary investigations (1997–1998) in the Yenisei Basin (the Kurtak area) were supported by the National Geographic Society, the Royal Society (London) and the Siberian Branch of the Russian Academy of Sciences. Drs. N.I. Drozdov, V.P. Chekha and N.I. Ovodov (Institute of Archaeology and Ethnography, SB RAS, Krasnoyarsk) provided assistance during previous (1993–1994) field studies. Dr. E.V. Akimova (Archaeology Institute, Krasnoyarsk) kindly provided illustrations on the Listvenka site (Figs. 22–24). Edward Little (Geological Survey, Nunavut, NWT, Canada) helped with preparation of Figs. 1 and 17.
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