Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów"
The late glacial at the turn of the San Glaciation and the Ferdynandw Interglacial, studied in the sections Ławki and Ławki I in the open mine "Bełchatw", indicates wavy-like climatic changes. Four waves with milder climate and three waves of returning coolings were distinguished on the ba...
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ftjgq:oai:geojournals.pgi.gov.pl:article/8382 2023-05-15T18:40:19+02:00 Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów" Baraniecka, Maria Danuta Konecka-Betley, Krystyna Sowiński, Leszek 2013-03-05 application/pdf https://gq.pgi.gov.pl/article/view/8382 https://doi.org/10.7306/gq.v36i2.8382 eng eng Polish Geological Institute-National Research Institute https://gq.pgi.gov.pl/article/view/8382/pdf_470 Geological Quarterly; Vol 36, No 2 (1992); 233-244 1641-7291 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2013 ftjgq https://doi.org/10.7306/gq.v36i2.8382 2019-08-13T19:05:53Z The late glacial at the turn of the San Glaciation and the Ferdynandw Interglacial, studied in the sections Ławki and Ławki I in the open mine "Bełchatw", indicates wavy-like climatic changes. Four waves with milder climate and three waves of returning coolings were distinguished on the basis of changing lithology, traces of chemical and weathering processes, initial and well developed soils, plant remains and pollen analysis. Presence of remains of water plants corresponds with initial deposition phase of lake sediments. There are also loesses deposited in water. Several types of tundra vegetation were distinguished. Upper part of till of the San Glaciation was dated at about 596 ka and sediments of the described late glacial period at 563 ka. Article in Journal/Newspaper Tundra Geological Quarterly |
institution |
Open Polar |
collection |
Geological Quarterly |
op_collection_id |
ftjgq |
language |
English |
description |
The late glacial at the turn of the San Glaciation and the Ferdynandw Interglacial, studied in the sections Ławki and Ławki I in the open mine "Bełchatw", indicates wavy-like climatic changes. Four waves with milder climate and three waves of returning coolings were distinguished on the basis of changing lithology, traces of chemical and weathering processes, initial and well developed soils, plant remains and pollen analysis. Presence of remains of water plants corresponds with initial deposition phase of lake sediments. There are also loesses deposited in water. Several types of tundra vegetation were distinguished. Upper part of till of the San Glaciation was dated at about 596 ka and sediments of the described late glacial period at 563 ka. |
format |
Article in Journal/Newspaper |
author |
Baraniecka, Maria Danuta Konecka-Betley, Krystyna Sowiński, Leszek |
spellingShingle |
Baraniecka, Maria Danuta Konecka-Betley, Krystyna Sowiński, Leszek Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów" |
author_facet |
Baraniecka, Maria Danuta Konecka-Betley, Krystyna Sowiński, Leszek |
author_sort |
Baraniecka, Maria Danuta |
title |
Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów" |
title_short |
Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów" |
title_full |
Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów" |
title_fullStr |
Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów" |
title_full_unstemmed |
Late glacial at the turn of the San Glaciation and the Ferdynandów Interglacial in the open mine "Bełchatów" |
title_sort |
late glacial at the turn of the san glaciation and the ferdynandów interglacial in the open mine "bełchatów" |
publisher |
Polish Geological Institute-National Research Institute |
publishDate |
2013 |
url |
https://gq.pgi.gov.pl/article/view/8382 https://doi.org/10.7306/gq.v36i2.8382 |
genre |
Tundra |
genre_facet |
Tundra |
op_source |
Geological Quarterly; Vol 36, No 2 (1992); 233-244 1641-7291 |
op_relation |
https://gq.pgi.gov.pl/article/view/8382/pdf_470 |
op_doi |
https://doi.org/10.7306/gq.v36i2.8382 |
_version_ |
1766229622451601408 |