The development of Belarusian lakes during the Late Glacial and Holocene
Sediment cores from six lakes in northern, central, and southern Belarus were eхamined to establish correlations between changes in lake conditions and catchment evolution since the Older Dryas. Detailed studies were conducted in three areas with highly different landscape development history. Commo...
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ftbelarusianstun:oai:elib.bsu.by:123456789/97717 2023-05-15T17:57:36+02:00 The development of Belarusian lakes during the Late Glacial and Holocene Novik, Aliaksei Zernitskaya, Valentina Punning, Jaan-Mati 2014-06-06 http://elib.bsu.by/handle/123456789/97717 en eng http://elib.bsu.by/handle/123456789/97717 ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Геофизика Book 2014 ftbelarusianstun 2020-07-09T16:24:07Z Sediment cores from six lakes in northern, central, and southern Belarus were eхamined to establish correlations between changes in lake conditions and catchment evolution since the Older Dryas. Detailed studies were conducted in three areas with highly different landscape development history. Common patterns and synchronism in lake sedimentation and fluctuations are more diverse during the Late Glacial and early Holocene, 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. During the latter half of the Holocene lake level changes were asynchronous in different regions of Belarus. At that time most of the existing differences were caused by local factors. Book permafrost Belarusian State University: Electronic Library BSU |
institution |
Open Polar |
collection |
Belarusian State University: Electronic Library BSU |
op_collection_id |
ftbelarusianstun |
language |
English |
topic |
ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Геофизика |
spellingShingle |
ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Геофизика Novik, Aliaksei The development of Belarusian lakes during the Late Glacial and Holocene |
topic_facet |
ЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Геофизика |
description |
Sediment cores from six lakes in northern, central, and southern Belarus were eхamined to establish correlations between changes in lake conditions and catchment evolution since the Older Dryas. Detailed studies were conducted in three areas with highly different landscape development history. Common patterns and synchronism in lake sedimentation and fluctuations are more diverse during the Late Glacial and early Holocene, 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. During the latter half of the Holocene lake level changes were asynchronous in different regions of Belarus. At that time most of the existing differences were caused by local factors. |
author2 |
Zernitskaya, Valentina Punning, Jaan-Mati |
format |
Book |
author |
Novik, Aliaksei |
author_facet |
Novik, Aliaksei |
author_sort |
Novik, Aliaksei |
title |
The development of Belarusian lakes during the Late Glacial and Holocene |
title_short |
The development of Belarusian lakes during the Late Glacial and Holocene |
title_full |
The development of Belarusian lakes during the Late Glacial and Holocene |
title_fullStr |
The development of Belarusian lakes during the Late Glacial and Holocene |
title_full_unstemmed |
The development of Belarusian lakes during the Late Glacial and Holocene |
title_sort |
development of belarusian lakes during the late glacial and holocene |
publishDate |
2014 |
url |
http://elib.bsu.by/handle/123456789/97717 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
http://elib.bsu.by/handle/123456789/97717 |
_version_ |
1766166063121170432 |