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Please use this identifier to cite or link to this item: http://elib.bsu.by/handle/123456789/91327
Title: История развития водосбора оз. Юуса в позднеледниковье и голоцене
Authors: Новик, А. А.
Issue Date: 2013
Citation: Вестник БГУ. Серия 2, Химия. Биология. География. - 2013. - №1. - С. 88-93
Abstract: Sediment cores from lake Uusa from Estonia were eхamined to establish correlations between changes in lake conditions and catchment evolution since the postglacial period. Coring and sampling of the selected sites according to common methodology with the following application of the lithological, isotope (δ18O, δ13C), pollen, radiocarbon (14C), investigations. Common patterns in lake sedimentation and fluctuations, mainly due to the general tendency of climate warming at the beginning of the postglacial epoch and disappearance of permafrost, which led to the increase in infiltrating processes. Lake sedimentation began in territory of the modern catchment area, instead of in a lake hollow as glaciokarst most intensively proceeded on raised sites
URI: http://elib.bsu.by/handle/123456789/91327
ISSN: 2308-9164
Appears in Collections:Кафедра общего землеведения и гидрометеорологии (статьи)
2013, №1 (февраль)

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