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...

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Published in:Quaternary Science Reviews
Main Authors: 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.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2006
Subjects:
Online Access:https://lup.lub.lu.se/record/590638
https://doi.org/10.1016/j.quascirev.2006.02.016
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spelling 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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