История развития водосбора оз. Юуса в позднеледниковье и голоцене
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, is...
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ftbelarusianstun:oai:elib.bsu.by:123456789/91327 2023-05-15T17:57:32+02:00 История развития водосбора оз. Юуса в позднеледниковье и голоцене Новик, А. А. 2013 http://elib.bsu.by/handle/123456789/91327 Минск : БГУ ru rus Вестник БГУ. Серия 2, Химия. Биология. География. - 2013. - №1. - С. 88-93 2308-9164 http://elib.bsu.by/handle/123456789/91327 ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::География Article 2013 ftbelarusianstun 2020-07-09T16:22:29Z 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 Article in Journal/Newspaper permafrost Belarusian State University: Electronic Library BSU |
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Open Polar |
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Belarusian State University: Electronic Library BSU |
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ftbelarusianstun |
language |
Russian |
topic |
ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::География |
spellingShingle |
ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::География Новик, А. А. История развития водосбора оз. Юуса в позднеледниковье и голоцене |
topic_facet |
ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::География |
description |
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 |
format |
Article in Journal/Newspaper |
author |
Новик, А. А. |
author_facet |
Новик, А. А. |
author_sort |
Новик, А. А. |
title |
История развития водосбора оз. Юуса в позднеледниковье и голоцене |
title_short |
История развития водосбора оз. Юуса в позднеледниковье и голоцене |
title_full |
История развития водосбора оз. Юуса в позднеледниковье и голоцене |
title_fullStr |
История развития водосбора оз. Юуса в позднеледниковье и голоцене |
title_full_unstemmed |
История развития водосбора оз. Юуса в позднеледниковье и голоцене |
title_sort |
история развития водосбора оз. юуса в позднеледниковье и голоцене |
publishDate |
2013 |
url |
http://elib.bsu.by/handle/123456789/91327 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
Вестник БГУ. Серия 2, Химия. Биология. География. - 2013. - №1. - С. 88-93 2308-9164 http://elib.bsu.by/handle/123456789/91327 |
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1766165998784741376 |