Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ...
Data obtained during cruises 7, 11, 13, and 14 of R/V Akademik Sergei Vavilov (1990, 1997, and 1998) contributed a lot to reconstruction of paleogeographic environments that existed in the Barents Sea during the last glaciation maximum. This was possible owing to extensive acoustic profiling with Pa...
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Online Access: | https://dx.doi.org/10.1594/pangaea.763669 https://doi.pangaea.de/10.1594/PANGAEA.763669 |
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ftdatacite:10.1594/pangaea.763669 2024-09-15T17:57:47+00:00 Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ... Pavlidis, Yury A Bogdanov, Yury A Levchenko, Oleg V Murdmaa, Ivar O Tarasov, Gennadiy A 2005 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.763669 https://doi.pangaea.de/10.1594/PANGAEA.763669 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Sample, optional label/labor no Sample type Age, dated Age, dated standard deviation Drilling/drill rig Age, 14C benzol synthesis Calculated Archive of Ocean Data ARCOD dataset Supplementary Dataset Dataset 2005 ftdatacite https://doi.org/10.1594/pangaea.763669 2024-08-01T11:00:37Z Data obtained during cruises 7, 11, 13, and 14 of R/V Akademik Sergei Vavilov (1990, 1997, and 1998) contributed a lot to reconstruction of paleogeographic environments that existed in the Barents Sea during the last glaciation maximum. This was possible owing to extensive acoustic profiling with Parasound equipment and use of a new approach to study of the upper part of the sedimentary cover. It is established that during the last glaciation maximum the Barents Sea was substantially smaller. It was almost completely surrounded by ice caps that descended to the shelf from glaciation centers on the land. The sea was connected with the World Ocean only by a narrow strait corresponding to the Bear Trough. Sea areas free of bottom glaciers were covered with floating ice: either by old pack ice or by plates of widespread shelf glaciers. Particular glaciomarine sediments accumulated under the floating ice. Destruction of the shelf glaciers during deglaciation resulted in formation of anomalously thick bottom ... : Supplement to: Pavlidis, Yury A; Bogdanov, Yury A; Levchenko, Oleg V; Murdmaa, Ivar O; Tarasov, Gennadiy A (2005): New data on the natural environment in the Barents Sea at the end of the Valdai glaciation. Translated from Okeanologiya, 2005, 45(1), 92-106, Oceanology, 45(1), 85-98 ... Dataset Barents Sea Pechora Pechora Sea DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock Sample, optional label/labor no Sample type Age, dated Age, dated standard deviation Drilling/drill rig Age, 14C benzol synthesis Calculated Archive of Ocean Data ARCOD |
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DEPTH, sediment/rock Sample, optional label/labor no Sample type Age, dated Age, dated standard deviation Drilling/drill rig Age, 14C benzol synthesis Calculated Archive of Ocean Data ARCOD Pavlidis, Yury A Bogdanov, Yury A Levchenko, Oleg V Murdmaa, Ivar O Tarasov, Gennadiy A Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ... |
topic_facet |
DEPTH, sediment/rock Sample, optional label/labor no Sample type Age, dated Age, dated standard deviation Drilling/drill rig Age, 14C benzol synthesis Calculated Archive of Ocean Data ARCOD |
description |
Data obtained during cruises 7, 11, 13, and 14 of R/V Akademik Sergei Vavilov (1990, 1997, and 1998) contributed a lot to reconstruction of paleogeographic environments that existed in the Barents Sea during the last glaciation maximum. This was possible owing to extensive acoustic profiling with Parasound equipment and use of a new approach to study of the upper part of the sedimentary cover. It is established that during the last glaciation maximum the Barents Sea was substantially smaller. It was almost completely surrounded by ice caps that descended to the shelf from glaciation centers on the land. The sea was connected with the World Ocean only by a narrow strait corresponding to the Bear Trough. Sea areas free of bottom glaciers were covered with floating ice: either by old pack ice or by plates of widespread shelf glaciers. Particular glaciomarine sediments accumulated under the floating ice. Destruction of the shelf glaciers during deglaciation resulted in formation of anomalously thick bottom ... : Supplement to: Pavlidis, Yury A; Bogdanov, Yury A; Levchenko, Oleg V; Murdmaa, Ivar O; Tarasov, Gennadiy A (2005): New data on the natural environment in the Barents Sea at the end of the Valdai glaciation. Translated from Okeanologiya, 2005, 45(1), 92-106, Oceanology, 45(1), 85-98 ... |
format |
Dataset |
author |
Pavlidis, Yury A Bogdanov, Yury A Levchenko, Oleg V Murdmaa, Ivar O Tarasov, Gennadiy A |
author_facet |
Pavlidis, Yury A Bogdanov, Yury A Levchenko, Oleg V Murdmaa, Ivar O Tarasov, Gennadiy A |
author_sort |
Pavlidis, Yury A |
title |
Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ... |
title_short |
Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ... |
title_full |
Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ... |
title_fullStr |
Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ... |
title_full_unstemmed |
Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea ... |
title_sort |
radiocarbon dates of plant detritus from sedimentary deposits of drill hole bav-480, pechora sea ... |
publisher |
PANGAEA |
publishDate |
2005 |
url |
https://dx.doi.org/10.1594/pangaea.763669 https://doi.pangaea.de/10.1594/PANGAEA.763669 |
genre |
Barents Sea Pechora Pechora Sea |
genre_facet |
Barents Sea Pechora Pechora Sea |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.763669 |
_version_ |
1810433969273962496 |