Late Quaternary ice sheet history and dynamics in central and southern Scandinavia
Recent work suggests an emerging new paradigm for the Scandinavian ice sheet (SIS); one of a dynamically fluctuating ice sheet. This doctoral research project explicitly examines the history and dynamics of the SIS at four sites within Sweden and Norway, and provides results covering different time...
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Institutionen för naturgeografi och kvartärgeologi (INK)
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ftstockholmuniv:oai:DiVA.org:su-38611 2023-05-15T16:40:01+02:00 Late Quaternary ice sheet history and dynamics in central and southern Scandinavia Johnsen, Timothy 2010 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-38611 eng eng Institutionen för naturgeografi och kvartärgeologi (INK) Stockholm : Department of Physical Geography and Quaternary Geology, Stockholm University Dissertations from the Department of Physical Geography and Quaternary Geology, 1653-7211 22 http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-38611 urn:isbn:978-91-7447-068-0 info:eu-repo/semantics/openAccess Scandinavian ice sheet ice sheet dynamics luminescence dating cosmogenic exposure dating geochronology moraine interstadial deglaciation nunatak Geology Geologi Doctoral thesis, comprehensive summary info:eu-repo/semantics/doctoralThesis text 2010 ftstockholmuniv 2023-02-23T21:42:28Z Recent work suggests an emerging new paradigm for the Scandinavian ice sheet (SIS); one of a dynamically fluctuating ice sheet. This doctoral research project explicitly examines the history and dynamics of the SIS at four sites within Sweden and Norway, and provides results covering different time periods of glacial history. Two relatively new dating techniques are used to constrain the ice sheet history: the optically stimulated luminescence (OSL) dating technique and the terrestrial cosmogenic nuclide (TCN) exposure dating technique. OSL dating of interstadial sediments in central Sweden and central Norway indicate ice-free conditions during times when it was previously inferred the sites were occupied by the SIS. Specifically, the SIS was absent or restricted to the mountains for at least part of Marine Isotope Stage 3 around 52 to 36 kyr ago. Inland portions of Norway were ice-free during part of the Last Glacial Maximum around 25 to 20 kyr ago. Consistent TCN exposure ages of boulders from the Vimmerby moraine in southern Sweden, and their compatibility with previous estimates for the timing of deglaciation based on radiocarbon dating and varve chronology, indicate that the southern margin of the SIS was at the Vimmerby moraine ~14 kyr ago. In central Sweden, consistent TCN ages for boulders on the summit of Mt. Åreskutan and for the earlier deglaciated highest elevation moraine related to the SIS in Sweden agree with previous estimates for the timing of deglaciation around 10 ka ago. These results indicate rapid decay of the SIS during deglaciation. Unusually old radiocarbon ages of tree remains previously studied from Mt. Åreskutan are rejected on the basis of incompatibility with consistent TCN ages for deglaciation, and incompatibility with established paleoecological and paleoglaciological reconstructions. Altogether this research conducted in different areas, covering different time periods, and using comparative geochronological methods demonstrates that the SIS was highly dynamic and sensitive to ... Doctoral or Postdoctoral Thesis Ice Sheet Stockholm University: Publications (DiVA) Norway |
institution |
Open Polar |
collection |
Stockholm University: Publications (DiVA) |
op_collection_id |
ftstockholmuniv |
language |
English |
topic |
Scandinavian ice sheet ice sheet dynamics luminescence dating cosmogenic exposure dating geochronology moraine interstadial deglaciation nunatak Geology Geologi |
spellingShingle |
Scandinavian ice sheet ice sheet dynamics luminescence dating cosmogenic exposure dating geochronology moraine interstadial deglaciation nunatak Geology Geologi Johnsen, Timothy Late Quaternary ice sheet history and dynamics in central and southern Scandinavia |
topic_facet |
Scandinavian ice sheet ice sheet dynamics luminescence dating cosmogenic exposure dating geochronology moraine interstadial deglaciation nunatak Geology Geologi |
description |
Recent work suggests an emerging new paradigm for the Scandinavian ice sheet (SIS); one of a dynamically fluctuating ice sheet. This doctoral research project explicitly examines the history and dynamics of the SIS at four sites within Sweden and Norway, and provides results covering different time periods of glacial history. Two relatively new dating techniques are used to constrain the ice sheet history: the optically stimulated luminescence (OSL) dating technique and the terrestrial cosmogenic nuclide (TCN) exposure dating technique. OSL dating of interstadial sediments in central Sweden and central Norway indicate ice-free conditions during times when it was previously inferred the sites were occupied by the SIS. Specifically, the SIS was absent or restricted to the mountains for at least part of Marine Isotope Stage 3 around 52 to 36 kyr ago. Inland portions of Norway were ice-free during part of the Last Glacial Maximum around 25 to 20 kyr ago. Consistent TCN exposure ages of boulders from the Vimmerby moraine in southern Sweden, and their compatibility with previous estimates for the timing of deglaciation based on radiocarbon dating and varve chronology, indicate that the southern margin of the SIS was at the Vimmerby moraine ~14 kyr ago. In central Sweden, consistent TCN ages for boulders on the summit of Mt. Åreskutan and for the earlier deglaciated highest elevation moraine related to the SIS in Sweden agree with previous estimates for the timing of deglaciation around 10 ka ago. These results indicate rapid decay of the SIS during deglaciation. Unusually old radiocarbon ages of tree remains previously studied from Mt. Åreskutan are rejected on the basis of incompatibility with consistent TCN ages for deglaciation, and incompatibility with established paleoecological and paleoglaciological reconstructions. Altogether this research conducted in different areas, covering different time periods, and using comparative geochronological methods demonstrates that the SIS was highly dynamic and sensitive to ... |
format |
Doctoral or Postdoctoral Thesis |
author |
Johnsen, Timothy |
author_facet |
Johnsen, Timothy |
author_sort |
Johnsen, Timothy |
title |
Late Quaternary ice sheet history and dynamics in central and southern Scandinavia |
title_short |
Late Quaternary ice sheet history and dynamics in central and southern Scandinavia |
title_full |
Late Quaternary ice sheet history and dynamics in central and southern Scandinavia |
title_fullStr |
Late Quaternary ice sheet history and dynamics in central and southern Scandinavia |
title_full_unstemmed |
Late Quaternary ice sheet history and dynamics in central and southern Scandinavia |
title_sort |
late quaternary ice sheet history and dynamics in central and southern scandinavia |
publisher |
Institutionen för naturgeografi och kvartärgeologi (INK) |
publishDate |
2010 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-38611 |
geographic |
Norway |
geographic_facet |
Norway |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
Dissertations from the Department of Physical Geography and Quaternary Geology, 1653-7211 22 http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-38611 urn:isbn:978-91-7447-068-0 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766030379065540608 |