The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms
The Pechora Sea is optimally located for studying the coalescence of a glacial and periglacial continental shelf zone in the high Arctic. Here, we present data acquired during cruises of the RV Akademik Nikolaj Strakhov in 2018–2021, revealing the distribution of submarine glacial landforms in the c...
Published in: | Geosciences |
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Main Authors: | , , , , , , , , , , , |
Format: | Text |
Language: | English |
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Multidisciplinary Digital Publishing Institute
2023
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Online Access: | https://doi.org/10.3390/geosciences13020053 |
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author | Sergey Nikiforov Roman Ananiev Martin Jakobsson Evgeny Moroz Sergey Sokolov Nikolay Sorokhtin Nikolay Dmitrevsky Elena Sukhikh Igor Chickiryov Yulia Zarayskaya Anatoly Razumovskiy Igor Semiletov |
author_facet | Sergey Nikiforov Roman Ananiev Martin Jakobsson Evgeny Moroz Sergey Sokolov Nikolay Sorokhtin Nikolay Dmitrevsky Elena Sukhikh Igor Chickiryov Yulia Zarayskaya Anatoly Razumovskiy Igor Semiletov |
author_sort | Sergey Nikiforov |
collection | MDPI Open Access Publishing |
container_issue | 2 |
container_start_page | 53 |
container_title | Geosciences |
container_volume | 13 |
description | The Pechora Sea is optimally located for studying the coalescence of a glacial and periglacial continental shelf zone in the high Arctic. Here, we present data acquired during cruises of the RV Akademik Nikolaj Strakhov in 2018–2021, revealing the distribution of submarine glacial landforms in the central part of the Pechora shelf area. Based on moraines and the distribution of glacial lineations, the extent of the ice sheet during the Last Glacial Maximum (LGM) is proposed. The crests of the moraine ridges and the slopes of their sides express a variation in morphology, and the ridges combine into irregular complexes. The moraines are primarily composed of coarse cobble-sized material with an addition of coarse sand and other sedimentary fractions. The mapped glacial landforms clearly indicate that an ice sheet extended over the area, while the Pechora basin, at the same time, was comprised of lowland characterized by a cryogenic subaerial landscape. Based on the result from this study, the extent and ice-flow pattern of the Barents-Kara Ice Sheet during the LGM were determined. |
format | Text |
genre | Arctic Ice Sheet Pechora Pechora Sea |
genre_facet | Arctic Ice Sheet Pechora Pechora Sea |
geographic | Arctic |
geographic_facet | Arctic |
id | ftmdpi:oai:mdpi.com:/2076-3263/13/2/53/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/geosciences13020053 |
op_relation | https://dx.doi.org/10.3390/geosciences13020053 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Geosciences; Volume 13; Issue 2; Pages: 53 |
publishDate | 2023 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2076-3263/13/2/53/ 2025-01-16T20:21:35+00:00 The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms Sergey Nikiforov Roman Ananiev Martin Jakobsson Evgeny Moroz Sergey Sokolov Nikolay Sorokhtin Nikolay Dmitrevsky Elena Sukhikh Igor Chickiryov Yulia Zarayskaya Anatoly Razumovskiy Igor Semiletov agris 2023-02-09 application/pdf https://doi.org/10.3390/geosciences13020053 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/geosciences13020053 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 13; Issue 2; Pages: 53 glacial landforms moraines ice sheet arctic shelf glacial lineations Text 2023 ftmdpi https://doi.org/10.3390/geosciences13020053 2023-08-01T08:43:48Z The Pechora Sea is optimally located for studying the coalescence of a glacial and periglacial continental shelf zone in the high Arctic. Here, we present data acquired during cruises of the RV Akademik Nikolaj Strakhov in 2018–2021, revealing the distribution of submarine glacial landforms in the central part of the Pechora shelf area. Based on moraines and the distribution of glacial lineations, the extent of the ice sheet during the Last Glacial Maximum (LGM) is proposed. The crests of the moraine ridges and the slopes of their sides express a variation in morphology, and the ridges combine into irregular complexes. The moraines are primarily composed of coarse cobble-sized material with an addition of coarse sand and other sedimentary fractions. The mapped glacial landforms clearly indicate that an ice sheet extended over the area, while the Pechora basin, at the same time, was comprised of lowland characterized by a cryogenic subaerial landscape. Based on the result from this study, the extent and ice-flow pattern of the Barents-Kara Ice Sheet during the LGM were determined. Text Arctic Ice Sheet Pechora Pechora Sea MDPI Open Access Publishing Arctic Geosciences 13 2 53 |
spellingShingle | glacial landforms moraines ice sheet arctic shelf glacial lineations Sergey Nikiforov Roman Ananiev Martin Jakobsson Evgeny Moroz Sergey Sokolov Nikolay Sorokhtin Nikolay Dmitrevsky Elena Sukhikh Igor Chickiryov Yulia Zarayskaya Anatoly Razumovskiy Igor Semiletov The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms |
title | The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms |
title_full | The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms |
title_fullStr | The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms |
title_full_unstemmed | The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms |
title_short | The Extent of Glaciation in the Pechora Sea, Eurasian Arctic, Based on Submarine Glacial Landforms |
title_sort | extent of glaciation in the pechora sea, eurasian arctic, based on submarine glacial landforms |
topic | glacial landforms moraines ice sheet arctic shelf glacial lineations |
topic_facet | glacial landforms moraines ice sheet arctic shelf glacial lineations |
url | https://doi.org/10.3390/geosciences13020053 |