and Holocene
Abstract. 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 hist...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.624.2202 2023-05-15T17:57:35+02:00 and Holocene Aliaksei Novika Jaan-mati Punninga Valentina Zernitskayac The Pennsylvania State University CiteSeerX Archives 2009 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.624.2202 http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2010/issue_1/earth-2010-1-63-79.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.624.2202 http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2010/issue_1/earth-2010-1-63-79.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2010/issue_1/earth-2010-1-63-79.pdf Key words lake level fluctuation lake sediments lithology Late Glacial Holocene Belarus text 2009 ftciteseerx 2016-01-08T15:08:41Z Abstract. 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. Text permafrost Unknown |
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ftciteseerx |
language |
English |
topic |
Key words lake level fluctuation lake sediments lithology Late Glacial Holocene Belarus |
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Key words lake level fluctuation lake sediments lithology Late Glacial Holocene Belarus Aliaksei Novika Jaan-mati Punninga Valentina Zernitskayac and Holocene |
topic_facet |
Key words lake level fluctuation lake sediments lithology Late Glacial Holocene Belarus |
description |
Abstract. 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 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Aliaksei Novika Jaan-mati Punninga Valentina Zernitskayac |
author_facet |
Aliaksei Novika Jaan-mati Punninga Valentina Zernitskayac |
author_sort |
Aliaksei Novika |
title |
and Holocene |
title_short |
and Holocene |
title_full |
and Holocene |
title_fullStr |
and Holocene |
title_full_unstemmed |
and Holocene |
title_sort |
and holocene |
publishDate |
2009 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.624.2202 http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2010/issue_1/earth-2010-1-63-79.pdf |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2010/issue_1/earth-2010-1-63-79.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.624.2202 http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2010/issue_1/earth-2010-1-63-79.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766166046832590848 |