Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic

Ice-rafted tephra deposits, of Marine Isotope Stage 6 (MIS 6) age, from Site U 1304 on the Gardar Drift, North Atlantic were examined for their shard size distribution and major element composition. The heterogeneous composition, large shard sizes and association with ice-rafted debris (IRD) indicat...

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Main Authors: Kuhs, Marion, Austin, William E. N., Abbott, Peter M., Hodell, David A.
Format: Book Part
Language:unknown
Published: The Geological Society 2014
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/3169/
http://sp.lyellcollection.org/content/early/2014/02/05/SP398.8
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spelling ftucambridgeesc:oai:eprints.esc.cam.ac.uk:3169 2023-05-15T16:40:39+02:00 Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic Kuhs, Marion Austin, William E. N. Abbott, Peter M. Hodell, David A. 2014-02 http://eprints.esc.cam.ac.uk/3169/ http://sp.lyellcollection.org/content/early/2014/02/05/SP398.8 unknown The Geological Society Kuhs, Marion and Austin, William E. N. and Abbott, Peter M. and Hodell, David A. (2014) Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic. In: Marine Tephrochronology. Special publication, 398 (398). The Geological Society, pp. 141-155. 01 - Climate Change and Earth-Ocean Atmosphere Systems Book Section PeerReviewed 2014 ftucambridgeesc 2020-08-27T18:09:33Z Ice-rafted tephra deposits, of Marine Isotope Stage 6 (MIS 6) age, from Site U 1304 on the Gardar Drift, North Atlantic were examined for their shard size distribution and major element composition. The heterogeneous composition, large shard sizes and association with ice-rafted debris (IRD) indicate that these late MIS 6 deposits were transported by iceberg-rafting from Iceland to Site U 1304. Comparison of individual shard geochemistry with the geochemistry of Holocene volcanic systems from Iceland allows the identification of different potential volcanic source regions. This detailed geochemical analysis, when combined with Icelandic Ice Sheet (IIS) flow models for the Last Glacial Maximum (LGM), suggests that the IIS had calving margins to both the north and south during the late MIS 6 and that icebergs could have been transported to the Site U 1304 by following surface ocean circulation patterns similar to those that prevailed during the LGM. We demonstrate that the descriptive concept of Icelandic glass in the characterization of tephra components within North Atlantic IRD can be significantly improved through quantitative characterization and that such data hold the potential to help constrain surface ocean circulation models, while also potentially yielding new information about the IIS during earlier glacial periods. Supplementary material: Statistical tests, major element concentrations of analysed shards, primary and secondary standards are available at http://www.geolsoc.org.uk/SUP18716 Book Part Ice Sheet Iceland North Atlantic University of Cambridge, Department of Earth Sciences: ESC Publications
institution Open Polar
collection University of Cambridge, Department of Earth Sciences: ESC Publications
op_collection_id ftucambridgeesc
language unknown
topic 01 - Climate Change and Earth-Ocean Atmosphere Systems
spellingShingle 01 - Climate Change and Earth-Ocean Atmosphere Systems
Kuhs, Marion
Austin, William E. N.
Abbott, Peter M.
Hodell, David A.
Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic
topic_facet 01 - Climate Change and Earth-Ocean Atmosphere Systems
description Ice-rafted tephra deposits, of Marine Isotope Stage 6 (MIS 6) age, from Site U 1304 on the Gardar Drift, North Atlantic were examined for their shard size distribution and major element composition. The heterogeneous composition, large shard sizes and association with ice-rafted debris (IRD) indicate that these late MIS 6 deposits were transported by iceberg-rafting from Iceland to Site U 1304. Comparison of individual shard geochemistry with the geochemistry of Holocene volcanic systems from Iceland allows the identification of different potential volcanic source regions. This detailed geochemical analysis, when combined with Icelandic Ice Sheet (IIS) flow models for the Last Glacial Maximum (LGM), suggests that the IIS had calving margins to both the north and south during the late MIS 6 and that icebergs could have been transported to the Site U 1304 by following surface ocean circulation patterns similar to those that prevailed during the LGM. We demonstrate that the descriptive concept of Icelandic glass in the characterization of tephra components within North Atlantic IRD can be significantly improved through quantitative characterization and that such data hold the potential to help constrain surface ocean circulation models, while also potentially yielding new information about the IIS during earlier glacial periods. Supplementary material: Statistical tests, major element concentrations of analysed shards, primary and secondary standards are available at http://www.geolsoc.org.uk/SUP18716
format Book Part
author Kuhs, Marion
Austin, William E. N.
Abbott, Peter M.
Hodell, David A.
author_facet Kuhs, Marion
Austin, William E. N.
Abbott, Peter M.
Hodell, David A.
author_sort Kuhs, Marion
title Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic
title_short Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic
title_full Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic
title_fullStr Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic
title_full_unstemmed Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic
title_sort iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial north atlantic
publisher The Geological Society
publishDate 2014
url http://eprints.esc.cam.ac.uk/3169/
http://sp.lyellcollection.org/content/early/2014/02/05/SP398.8
genre Ice Sheet
Iceland
North Atlantic
genre_facet Ice Sheet
Iceland
North Atlantic
op_relation Kuhs, Marion and Austin, William E. N. and Abbott, Peter M. and Hodell, David A. (2014) Iceberg-rafted tephra as a potential tool for the reconstruction of ice-sheet processes and ocean surface circulation in the glacial North Atlantic. In: Marine Tephrochronology. Special publication, 398 (398). The Geological Society, pp. 141-155.
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