Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited

The Kapp Ekholm site, in central Spitsbergen, shows alternating units of glaciomarine sandy silt and diamicton representing three glacial cycles and is key in reconstructing the Late Pleistocene glacial history of Svalbard. Part of the site is reinvestigated here by focusing on re-dating two units (...

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Main Authors: Eccleshall, Sarah, Hormes, Anne, Hovland, Alexander, Preusser, Frank
Format: Article in Journal/Newspaper
Language:unknown
Published: Research Online 2016
Subjects:
re
Online Access:https://ro.uow.edu.au/smhpapers/4139
id ftunivwollongong:oai:ro.uow.edu.au:smhpapers-5163
record_format openpolar
spelling ftunivwollongong:oai:ro.uow.edu.au:smhpapers-5163 2023-05-15T18:29:32+02:00 Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited Eccleshall, Sarah Hormes, Anne Hovland, Alexander Preusser, Frank 2016-01-01T08:00:00Z https://ro.uow.edu.au/smhpapers/4139 unknown Research Online https://ro.uow.edu.au/smhpapers/4139 Faculty of Science, Medicine and Health - Papers: part A chronology pleistocene ekholm kapp constraining visited svalbard re glaciations Medicine and Health Sciences Social and Behavioral Sciences article 2016 ftunivwollongong 2020-02-25T11:31:45Z The Kapp Ekholm site, in central Spitsbergen, shows alternating units of glaciomarine sandy silt and diamicton representing three glacial cycles and is key in reconstructing the Late Pleistocene glacial history of Svalbard. Part of the site is reinvestigated here by focusing on re-dating two units (B and F) interpreted as interglacial/interstadial glaciomarine deposits, in order to constrain the controversial chronology. A combination of Optical Stimulated Luminescence (OSL) on quartz, infrared stimulated luminescence with a 50 °C readout temperature (IRSL50) and post infrared-infrared stimulated luminescence (pIR), both on feldspar, was applied. While Formation B was beyond the dateable range of OSL, IRSL50 and pIR ages lead to the conclusion that this unit represents the Last Interglacial, Marine Isotope Stage (MIS) 5e, and the underlying diamicton the MIS 6 glacial. Formation F yielded ages implying that the formation represents the MIS 5a interstadial and the underlying diamicton is interpreted to represent the MIS 5b stadial. This agrees with conclusions drawn concerning the Pleistocene glaciations elsewhere on Svalbard. Article in Journal/Newspaper Svalbard Spitsbergen University of Wollongong, Australia: Research Online Kapp Ekholm ENVELOPE(16.533,16.533,78.573,78.573) Svalbard
institution Open Polar
collection University of Wollongong, Australia: Research Online
op_collection_id ftunivwollongong
language unknown
topic chronology
pleistocene
ekholm
kapp
constraining
visited
svalbard
re
glaciations
Medicine and Health Sciences
Social and Behavioral Sciences
spellingShingle chronology
pleistocene
ekholm
kapp
constraining
visited
svalbard
re
glaciations
Medicine and Health Sciences
Social and Behavioral Sciences
Eccleshall, Sarah
Hormes, Anne
Hovland, Alexander
Preusser, Frank
Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited
topic_facet chronology
pleistocene
ekholm
kapp
constraining
visited
svalbard
re
glaciations
Medicine and Health Sciences
Social and Behavioral Sciences
description The Kapp Ekholm site, in central Spitsbergen, shows alternating units of glaciomarine sandy silt and diamicton representing three glacial cycles and is key in reconstructing the Late Pleistocene glacial history of Svalbard. Part of the site is reinvestigated here by focusing on re-dating two units (B and F) interpreted as interglacial/interstadial glaciomarine deposits, in order to constrain the controversial chronology. A combination of Optical Stimulated Luminescence (OSL) on quartz, infrared stimulated luminescence with a 50 °C readout temperature (IRSL50) and post infrared-infrared stimulated luminescence (pIR), both on feldspar, was applied. While Formation B was beyond the dateable range of OSL, IRSL50 and pIR ages lead to the conclusion that this unit represents the Last Interglacial, Marine Isotope Stage (MIS) 5e, and the underlying diamicton the MIS 6 glacial. Formation F yielded ages implying that the formation represents the MIS 5a interstadial and the underlying diamicton is interpreted to represent the MIS 5b stadial. This agrees with conclusions drawn concerning the Pleistocene glaciations elsewhere on Svalbard.
format Article in Journal/Newspaper
author Eccleshall, Sarah
Hormes, Anne
Hovland, Alexander
Preusser, Frank
author_facet Eccleshall, Sarah
Hormes, Anne
Hovland, Alexander
Preusser, Frank
author_sort Eccleshall, Sarah
title Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited
title_short Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited
title_full Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited
title_fullStr Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited
title_full_unstemmed Constraining the chronology of Pleistocene glaciations on Svalbard: Kapp Ekholm re-visited
title_sort constraining the chronology of pleistocene glaciations on svalbard: kapp ekholm re-visited
publisher Research Online
publishDate 2016
url https://ro.uow.edu.au/smhpapers/4139
long_lat ENVELOPE(16.533,16.533,78.573,78.573)
geographic Kapp Ekholm
Svalbard
geographic_facet Kapp Ekholm
Svalbard
genre Svalbard
Spitsbergen
genre_facet Svalbard
Spitsbergen
op_source Faculty of Science, Medicine and Health - Papers: part A
op_relation https://ro.uow.edu.au/smhpapers/4139
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