The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology

We here report the results of luminescence and cosmogenic exposure dating of the Idre marginal moraine, located in the southern Scandinavian Mountains. This particular moraine is targeted because it is morphologically distinct and marks the margin of a former ice sheet. The till in the moraine conta...

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Published in:Quaternary Science Advances
Main Authors: Kleman, Johan, Hättestrand, Martina, Borgström, Ingmar, Preusser, Frank, Fabel, Derek
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2020
Subjects:
Online Access:http://eprints.gla.ac.uk/217046/
http://eprints.gla.ac.uk/217046/1/217046.pdf
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spelling ftuglasgow:oai:eprints.gla.ac.uk:217046 2023-05-15T16:40:06+02:00 The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology Kleman, Johan Hättestrand, Martina Borgström, Ingmar Preusser, Frank Fabel, Derek 2020-10 text http://eprints.gla.ac.uk/217046/ http://eprints.gla.ac.uk/217046/1/217046.pdf en eng Elsevier http://eprints.gla.ac.uk/217046/1/217046.pdf Kleman, J., Hättestrand, M., Borgström, I., Preusser, F. and Fabel, D. <http://eprints.gla.ac.uk/view/author/5585.html> (2020) The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology. Quaternary Science Advances <http://eprints.gla.ac.uk/view/journal_volume/Quaternary_Science_Advances.html>, 2, 100010. (doi:10.1016/j.qsa.2020.100010 <http://dx.doi.org/10.1016/j.qsa.2020.100010>) cc_by_nc_nd_4 CC-BY-NC-ND Articles PeerReviewed 2020 ftuglasgow https://doi.org/10.1016/j.qsa.2020.100010 2020-08-27T22:09:55Z We here report the results of luminescence and cosmogenic exposure dating of the Idre marginal moraine, located in the southern Scandinavian Mountains. This particular moraine is targeted because it is morphologically distinct and marks the margin of a former ice sheet. The till in the moraine contains erratics that provide strong evidence of flow from an ice sheet centred over Norway. The area immediately outside the moraine margin is an older residual soil. Luminescence ages of three samples taken from a sand lense within the moraine indicate that it formed at around 55 ka, during the early warm part of Marine Isotope Stage (MIS) 3. Median exposure ages (10Be) of ten samples from boulders embedded in the surface till indicate that about 30 ka of ice-free time have elapsed since formation of the moraine. The difference between the age of the ridge and the duration of exposure provides a measure of the time of ice-cover in the ice sheet core area. Previous research indicates that final deglaciation of the site occurred at approximately 10 ka ago, which in combination with our results implies that the area around the Idre marginal moraine was ice free for ca. 20 ka, i.e. from around 55 ka to around 35 ka. Thereafter, the area was glaciated and the marginal moraine was covered by the Late Weichselian ice sheet for around 25 ka without experiencing any significant erosion or morphological destruction. While earlier studies have already pointed towards MIS 3 ice free conditions in northern and central Sweden, this study contributes a measurement-based duration estimate for the MIS 3 interstadial. Article in Journal/Newspaper Ice Sheet University of Glasgow: Enlighten - Publications Norway Quaternary Science Advances 2 100010
institution Open Polar
collection University of Glasgow: Enlighten - Publications
op_collection_id ftuglasgow
language English
description We here report the results of luminescence and cosmogenic exposure dating of the Idre marginal moraine, located in the southern Scandinavian Mountains. This particular moraine is targeted because it is morphologically distinct and marks the margin of a former ice sheet. The till in the moraine contains erratics that provide strong evidence of flow from an ice sheet centred over Norway. The area immediately outside the moraine margin is an older residual soil. Luminescence ages of three samples taken from a sand lense within the moraine indicate that it formed at around 55 ka, during the early warm part of Marine Isotope Stage (MIS) 3. Median exposure ages (10Be) of ten samples from boulders embedded in the surface till indicate that about 30 ka of ice-free time have elapsed since formation of the moraine. The difference between the age of the ridge and the duration of exposure provides a measure of the time of ice-cover in the ice sheet core area. Previous research indicates that final deglaciation of the site occurred at approximately 10 ka ago, which in combination with our results implies that the area around the Idre marginal moraine was ice free for ca. 20 ka, i.e. from around 55 ka to around 35 ka. Thereafter, the area was glaciated and the marginal moraine was covered by the Late Weichselian ice sheet for around 25 ka without experiencing any significant erosion or morphological destruction. While earlier studies have already pointed towards MIS 3 ice free conditions in northern and central Sweden, this study contributes a measurement-based duration estimate for the MIS 3 interstadial.
format Article in Journal/Newspaper
author Kleman, Johan
Hättestrand, Martina
Borgström, Ingmar
Preusser, Frank
Fabel, Derek
spellingShingle Kleman, Johan
Hättestrand, Martina
Borgström, Ingmar
Preusser, Frank
Fabel, Derek
The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology
author_facet Kleman, Johan
Hättestrand, Martina
Borgström, Ingmar
Preusser, Frank
Fabel, Derek
author_sort Kleman, Johan
title The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology
title_short The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology
title_full The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology
title_fullStr The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology
title_full_unstemmed The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology
title_sort idre marginal moraine – an anchorpoint for middle and late weichselian ice sheet chronology
publisher Elsevier
publishDate 2020
url http://eprints.gla.ac.uk/217046/
http://eprints.gla.ac.uk/217046/1/217046.pdf
geographic Norway
geographic_facet Norway
genre Ice Sheet
genre_facet Ice Sheet
op_relation http://eprints.gla.ac.uk/217046/1/217046.pdf
Kleman, J., Hättestrand, M., Borgström, I., Preusser, F. and Fabel, D. <http://eprints.gla.ac.uk/view/author/5585.html> (2020) The Idre marginal moraine – an anchorpoint for Middle and Late Weichselian ice sheet chronology. Quaternary Science Advances <http://eprints.gla.ac.uk/view/journal_volume/Quaternary_Science_Advances.html>, 2, 100010. (doi:10.1016/j.qsa.2020.100010 <http://dx.doi.org/10.1016/j.qsa.2020.100010>)
op_rights cc_by_nc_nd_4
op_rightsnorm CC-BY-NC-ND
op_doi https://doi.org/10.1016/j.qsa.2020.100010
container_title Quaternary Science Advances
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