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Please use this identifier to cite or link to this item: http://dspace.bsu.edu.ru/handle/123456789/31598
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dc.contributor.authorChendev, Y.-
dc.contributor.authorAleksandrovskiy, A.-
dc.contributor.authorKhokhlova, O.-
dc.contributor.authorSkripkin, V.-
dc.date.accessioned2020-06-07T20:56:19Z-
dc.date.available2020-06-07T20:56:19Z-
dc.date.issued2018-
dc.identifier.citation14C dating to study the development of soils in the forest-steppe of the central russian upland as a result of bioclimatic changes and long-term cultivation / Y. Chendev, A. Aleksandrovskiy, O. Khokhlova [et al.] // Radiocarbon. - 2018. - Vol.60, N4. - P. 1185-1198.ru
dc.identifier.urihttp://dspace.bsu.edu.ru/handle/123456789/31598-
dc.description.abstractTemporal changes in soils of forest landscapes of the forest-steppe zone - Haplic Luvisols and Greyzemic Phaeozems - under the impact of Holocene climate changes (natural factor) and long-term cultivation (anthropogenic factor) were studied on level interfluves of the Central Russian Upland. To study soil evolution under the impact of climate changes, soil chronosequences of archaeological sites - paleosols buried under ramparts of ancient settlements and background surface soils of adjacent areas - were analyzedru
dc.language.isoenru
dc.subjectsoil scienceru
dc.subjectChernozemsru
dc.subjectclimate changeru
dc.subjectforest-steppe zoneru
dc.subjectHoloceneru
dc.subjectLuvisolsru
dc.subjectPhaeozemsru
dc.subjectsoil evolutionru
dc.title14C dating to study the development of soils in the forest-steppe of the central russian upland as a result of bioclimatic changes and long-term cultivationru
dc.typeArticleru
Appears in Collections:Статьи из периодических изданий и сборников (на иностранных языках) = Articles from periodicals and collections (in foreign languages)

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