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Please use this identifier to cite or link to this item: http://dspace.bsu.edu.ru/handle/123456789/29674
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dc.contributor.authorChendev, Yu. G.-
dc.contributor.authorLupo, E. R.-
dc.contributor.authorLebedeva, M. G.-
dc.contributor.authorBorbukova, D. A.-
dc.date.accessioned2020-04-28T12:27:59Z-
dc.date.available2020-04-28T12:27:59Z-
dc.date.issued2015-
dc.identifier.citationRegional specificity of the climatic evolution of soils in the southern part of Eastern Europe in the second half of the Holocene / Yu. G. Chendev, A. R. Lupo, M. G. Lebedeva [et al.] // Eurasian Soil Science. - 2015. - Vol. 48, № 12. - P. 1279–1291. - Doi: 10.1134/S1064229315120042. - Refer.: P. 1289-1291.ru
dc.identifier.urihttp://dspace.bsu.edu.ru/handle/123456789/29674-
dc.description.abstractThe analysis of characteristic features of chernozems and chestnut soils of different ages that have been formed in the south of the East European Plain in the past 5000 years attests to the spatial and temporal heterogeneity of the rate and direction of pedogenetic processes, i.e., to the metachronous development of the soil coverru
dc.language.isoenru
dc.subjectagricultureru
dc.subjectpedologyru
dc.subjectsoilsru
dc.subjectchernozemsru
dc.subjectpaleosolsru
dc.subjectclimateru
dc.subjectevolution of soilsru
dc.subjectholoceneru
dc.subjectEastern Europeru
dc.subjectEast European Plainru
dc.titleRegional specificity of the climatic evolution of soils in the southern part of Eastern Europe in the second half of the Holoceneru
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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