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...

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Published in:Geosciences
Main Authors: Sergey Nikiforov, Roman Ananiev, Martin Jakobsson, Evgeny Moroz, Sergey Sokolov, Nikolay Sorokhtin, Nikolay Dmitrevsky, Elena Sukhikh, Igor Chickiryov, Yulia Zarayskaya, Anatoly Razumovskiy, Igor Semiletov
Format: Text
Language:English
Published: 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.
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Ice Sheet
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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