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

Chlachula, Jiří

Název:

Autor:

Chlachula, Jiří

Typ dokumentu:

Recenzovaný odborný článek (English)

Zdrojový dok.:

Quaternary International. 2001, vol. 80-81, p. 101-130

ISSN:

1040-6182 (Sherpa/RoMEO, JCR)

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DOI:

https://doi.org/10.1016/S1040-6182(01)00022-2

Abstrakt:

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.

Plný text:

https://www.sciencedirect.com/science/article/pii/S1040618201000222

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Citace článku v časopise:
CHLACHULA, Jiří. Pleistocene climate change, natural environments and palaeolithic occupation of the upper Yenisei area, south-central Siberia. Quaternary International [online]. 2001, vol. 80-81, s. 101-130. [cit. 2024-12-12]. ISSN 1040-6182. Dostupné z: https://www.sciencedirect.com/science/article/pii/S1040618201000222.

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