Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary
Quaternary glacial stratigraphy and relative sea-level changes reveal at least four expansions of the Kara Sea ice sheet over the Severnaya Zemlya Archipelago at 79 degrees N in the Russian Arctic, as indicated from tills interbedded with marine sediments, exposed in stratigraphic superposition, and...
Published in: | Quaternary Science Reviews |
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Online Access: | https://lup.lub.lu.se/record/590638 https://doi.org/10.1016/j.quascirev.2006.02.016 |
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ftulundlup:oai:lup.lub.lu.se:a2eab09c-e676-48c2-a92d-1c36b0113240 2023-05-15T14:49:18+02:00 Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary Möller, Per Lubinski, D. Ingólfsson, Ó. Forman, S.L Siedenkrantz, M-S. Bolshiyanov, D. Yu. Lokrantz, H. Antonov, O. Pavlov, ´M. Ljung, Karl Zeeberg, J.J. Andreev, A. 2006 https://lup.lub.lu.se/record/590638 https://doi.org/10.1016/j.quascirev.2006.02.016 eng eng Elsevier https://lup.lub.lu.se/record/590638 http://dx.doi.org/10.1016/j.quascirev.2006.02.016 wos:000243286300017 scopus:33746596692 Quaternary Science Reviews; 25(21-22), pp 2894-2936 (2006) ISSN: 0277-3791 Geology contributiontojournal/article info:eu-repo/semantics/article text 2006 ftulundlup https://doi.org/10.1016/j.quascirev.2006.02.016 2023-02-01T23:28:24Z Quaternary glacial stratigraphy and relative sea-level changes reveal at least four expansions of the Kara Sea ice sheet over the Severnaya Zemlya Archipelago at 79 degrees N in the Russian Arctic, as indicated from tills interbedded with marine sediments, exposed in stratigraphic superposition, and from raised-beach sequences that occur at altitudes up to 140 m a.s.l. Chronologic control is provided by AMS C-14, electron-spin resonance, green-stimulated luminescence, and aspartic-acid geochronology. Major glaciations followed by deglaciation and marine inundation occurred during MIS 10-9, MIS 8-7, MIS 6-5e and MIS 5d-3. The MIS 6-5e event, associated with the high marine limit, implies ice-sheet thickness of > 2000m only 200km from the deep Arctic Ocean, consistent with published evidence of ice grounding at similar to 1000m water depth in the central Arctic Ocean. Till fabrics and glacial tectonics record repeated expansions of local ice caps exclusively, suggesting wet-based ice cap advance followed by cold-based regional ice-sheet expansion. Local ice caps over highland sites along the perimeter of the shallow Kara Sea, including the Byrranga Mountains, appear to have repeatedly fostered initiation of a large Kara Sea ice sheet, with exception of the Last Glacial Maximum (MIS 2), when Kara Sea ice did not impact Severnaya Zemlya and barely graced northernmost Taymyr Peninsula. Article in Journal/Newspaper Arctic Arctic Ocean Ice cap Ice Sheet Kara Sea Sea ice Severnaya Zemlya Taymyr Taymyr Peninsula Lund University Publications (LUP) Arctic Arctic Ocean Kara Sea Raised Beach ENVELOPE(163.783,163.783,-74.983,-74.983) Severnaya Zemlya ENVELOPE(98.000,98.000,79.500,79.500) Taymyr ENVELOPE(89.987,89.987,68.219,68.219) Quaternary Science Reviews 25 21-22 2894 2936 |
institution |
Open Polar |
collection |
Lund University Publications (LUP) |
op_collection_id |
ftulundlup |
language |
English |
topic |
Geology |
spellingShingle |
Geology Möller, Per Lubinski, D. Ingólfsson, Ó. Forman, S.L Siedenkrantz, M-S. Bolshiyanov, D. Yu. Lokrantz, H. Antonov, O. Pavlov, ´M. Ljung, Karl Zeeberg, J.J. Andreev, A. Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary |
topic_facet |
Geology |
description |
Quaternary glacial stratigraphy and relative sea-level changes reveal at least four expansions of the Kara Sea ice sheet over the Severnaya Zemlya Archipelago at 79 degrees N in the Russian Arctic, as indicated from tills interbedded with marine sediments, exposed in stratigraphic superposition, and from raised-beach sequences that occur at altitudes up to 140 m a.s.l. Chronologic control is provided by AMS C-14, electron-spin resonance, green-stimulated luminescence, and aspartic-acid geochronology. Major glaciations followed by deglaciation and marine inundation occurred during MIS 10-9, MIS 8-7, MIS 6-5e and MIS 5d-3. The MIS 6-5e event, associated with the high marine limit, implies ice-sheet thickness of > 2000m only 200km from the deep Arctic Ocean, consistent with published evidence of ice grounding at similar to 1000m water depth in the central Arctic Ocean. Till fabrics and glacial tectonics record repeated expansions of local ice caps exclusively, suggesting wet-based ice cap advance followed by cold-based regional ice-sheet expansion. Local ice caps over highland sites along the perimeter of the shallow Kara Sea, including the Byrranga Mountains, appear to have repeatedly fostered initiation of a large Kara Sea ice sheet, with exception of the Last Glacial Maximum (MIS 2), when Kara Sea ice did not impact Severnaya Zemlya and barely graced northernmost Taymyr Peninsula. |
format |
Article in Journal/Newspaper |
author |
Möller, Per Lubinski, D. Ingólfsson, Ó. Forman, S.L Siedenkrantz, M-S. Bolshiyanov, D. Yu. Lokrantz, H. Antonov, O. Pavlov, ´M. Ljung, Karl Zeeberg, J.J. Andreev, A. |
author_facet |
Möller, Per Lubinski, D. Ingólfsson, Ó. Forman, S.L Siedenkrantz, M-S. Bolshiyanov, D. Yu. Lokrantz, H. Antonov, O. Pavlov, ´M. Ljung, Karl Zeeberg, J.J. Andreev, A. |
author_sort |
Möller, Per |
title |
Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary |
title_short |
Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary |
title_full |
Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary |
title_fullStr |
Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary |
title_full_unstemmed |
Severnaya Zemlya, Arctic Russia: a nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary |
title_sort |
severnaya zemlya, arctic russia: a nucleation area for kara sea ice sheets during the middle to late quaternary |
publisher |
Elsevier |
publishDate |
2006 |
url |
https://lup.lub.lu.se/record/590638 https://doi.org/10.1016/j.quascirev.2006.02.016 |
long_lat |
ENVELOPE(163.783,163.783,-74.983,-74.983) ENVELOPE(98.000,98.000,79.500,79.500) ENVELOPE(89.987,89.987,68.219,68.219) |
geographic |
Arctic Arctic Ocean Kara Sea Raised Beach Severnaya Zemlya Taymyr |
geographic_facet |
Arctic Arctic Ocean Kara Sea Raised Beach Severnaya Zemlya Taymyr |
genre |
Arctic Arctic Ocean Ice cap Ice Sheet Kara Sea Sea ice Severnaya Zemlya Taymyr Taymyr Peninsula |
genre_facet |
Arctic Arctic Ocean Ice cap Ice Sheet Kara Sea Sea ice Severnaya Zemlya Taymyr Taymyr Peninsula |
op_source |
Quaternary Science Reviews; 25(21-22), pp 2894-2936 (2006) ISSN: 0277-3791 |
op_relation |
https://lup.lub.lu.se/record/590638 http://dx.doi.org/10.1016/j.quascirev.2006.02.016 wos:000243286300017 scopus:33746596692 |
op_doi |
https://doi.org/10.1016/j.quascirev.2006.02.016 |
container_title |
Quaternary Science Reviews |
container_volume |
25 |
container_issue |
21-22 |
container_start_page |
2894 |
op_container_end_page |
2936 |
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1766320360716763136 |