Geochronology and landscape-climatic environments of the Early Zyryanian Interstadial in West Siberia

The geochronology and landscape-climatic environments of the Early Zyryanian Interstadial in West Siberia were investigated. A relatively precise radioisotope age was determined for the Early Wrmian Interstadial in the continental section, which is correlated with climatic events dened in oceanic se...

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Published inDoklady earth sciences Vol. 421; no. 1; pp. 796 - 799
Main Authors Laukhin, S. A., Maksimov, F. E., Arslanov, Kh. A., Kuznetsov, V. Yu, Chernov, S. B., Shilova, G. N., Velichkevich, F. Yu
Format Journal Article
LanguageEnglish
Published Dordrecht SP MAIK Nauka/Interperiodica 01.07.2008
Springer Nature B.V
Subjects
Climate change
Earth and Environmental Science
Earth Sciences
Geography
Geological time
Landscape ecology
Oceanography
Paleobotany
Sediments
DOKLADY Earth Science
Arboreal Pollen
Peat Accumulation
Isochron
Green Moss
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Summary:The geochronology and landscape-climatic environments of the Early Zyryanian Interstadial in West Siberia were investigated. A relatively precise radioisotope age was determined for the Early Wrmian Interstadial in the continental section, which is correlated with climatic events dened in oceanic sediments and coeval sediments in the Russian Plain and West Europe.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X08050188