Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie

The paper presents the results of pollen and geological analyses from the fossil lake sediments at Kaliłów near Biała Podlaska. In pollen diagram 8 local pollen zones are distinguished, starting with the shrub tundra through the Pinus-Betula woodland and typical Mazovian Interglacial succession and...

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Main Authors: Binka, Krzysztof, Nitychoruk, Jerzy
Format: Article in Journal/Newspaper
Language:English
Published: Polish Geological Institute-National Research Institute 2013
Subjects:
Tundra
Online Access:https://gq.pgi.gov.pl/article/view/8246
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spelling ftjgq:oai:geojournals.pgi.gov.pl:article/8246 2024-09-15T18:39:42+00:00 Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie Binka, Krzysztof Nitychoruk, Jerzy 2013-02-19 application/pdf https://gq.pgi.gov.pl/article/view/8246 eng eng Polish Geological Institute-National Research Institute https://gq.pgi.gov.pl/article/view/8246/pdf_338 10.7306/gq.v40i2.8246.g6792 https://gq.pgi.gov.pl/article/view/8246 Geological Quarterly; Vol. 40 No. 2 (1996); 269-282 Geological Quarterly; Tom 40 Nr 2 (1996); 269-282 1641-7291 10.7306/gq.v40i2 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2013 ftjgq https://doi.org/10.7306/gq.v40i2 2024-07-30T03:29:08Z The paper presents the results of pollen and geological analyses from the fossil lake sediments at Kaliłów near Biała Podlaska. In pollen diagram 8 local pollen zones are distinguished, starting with the shrub tundra through the Pinus-Betula woodland and typical Mazovian Interglacial succession and finishing with plant communities with abundant heliophythes. Palaeolake district is believed to be associated with linear tectonic structures of pre-Quaternary substratum because of narrow and long, up to several tens of kilometers, palaeolake depressions filled with sediments or impressive thickness, locally more than 30 m. Article in Journal/Newspaper Tundra Geological Quarterly
institution Open Polar
collection Geological Quarterly
op_collection_id ftjgq
language English
description The paper presents the results of pollen and geological analyses from the fossil lake sediments at Kaliłów near Biała Podlaska. In pollen diagram 8 local pollen zones are distinguished, starting with the shrub tundra through the Pinus-Betula woodland and typical Mazovian Interglacial succession and finishing with plant communities with abundant heliophythes. Palaeolake district is believed to be associated with linear tectonic structures of pre-Quaternary substratum because of narrow and long, up to several tens of kilometers, palaeolake depressions filled with sediments or impressive thickness, locally more than 30 m.
format Article in Journal/Newspaper
author Binka, Krzysztof
Nitychoruk, Jerzy
spellingShingle Binka, Krzysztof
Nitychoruk, Jerzy
Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie
author_facet Binka, Krzysztof
Nitychoruk, Jerzy
author_sort Binka, Krzysztof
title Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie
title_short Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie
title_full Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie
title_fullStr Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie
title_full_unstemmed Geological and palaeobotanical setting of interglacial sediments at the Kaliłów site in southern Podlasie
title_sort geological and palaeobotanical setting of interglacial sediments at the kaliłów site in southern podlasie
publisher Polish Geological Institute-National Research Institute
publishDate 2013
url https://gq.pgi.gov.pl/article/view/8246
genre Tundra
genre_facet Tundra
op_source Geological Quarterly; Vol. 40 No. 2 (1996); 269-282
Geological Quarterly; Tom 40 Nr 2 (1996); 269-282
1641-7291
10.7306/gq.v40i2
op_relation https://gq.pgi.gov.pl/article/view/8246/pdf_338
10.7306/gq.v40i2.8246.g6792
https://gq.pgi.gov.pl/article/view/8246
op_doi https://doi.org/10.7306/gq.v40i2
_version_ 1810484059831271424

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