OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica
High-elevation alluvial fans in the McMurdo Dry Valleys are a record of short-term, occasional melting events along the margins of the East Antarctic Ice Sheet. Sediment samples were dated from five fans using Optically Stimulated Luminescence (OSL) dating. OSL dates the time since quartz grains wer...
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North Dakota State University
2015
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ftnorthdakotasta:oai:library.ndsu.edu:10365/27578 2023-10-29T02:31:21+01:00 OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica Ramsey, Meridith Ann 2015 application/pdf https://hdl.handle.net/10365/27578 unknown North Dakota State University https://hdl.handle.net/10365/27578 NDSU Policy 190.6.2 Thesis 2015 ftnorthdakotasta 2023-10-05T17:40:25Z High-elevation alluvial fans in the McMurdo Dry Valleys are a record of short-term, occasional melting events along the margins of the East Antarctic Ice Sheet. Sediment samples were dated from five fans using Optically Stimulated Luminescence (OSL) dating. OSL dates the time since quartz grains were last exposed to sunlight; all sample preparation takes place in a dark room. Thirteen samples were dated for this thesis, the ages were stratigraphically consistent and ranged from 1.1 ka to 105.9 ka. Clusters of fan activity occurred between 1.1 and 3.1 ka and 8.1 and 11.1 ka. The melting events appear to be linked to insolation, with periods of fan activity occurring usually at times of increased mean annual insolation. The alluvial fans show promise as a possible archive for climate proxies in this region of Antarctica. Thesis Antarc* Antarctic Antarctica Ice Sheet McMurdo Dry Valleys North Dakota State University (NDSU) Digital Repository |
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Open Polar |
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North Dakota State University (NDSU) Digital Repository |
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ftnorthdakotasta |
language |
unknown |
description |
High-elevation alluvial fans in the McMurdo Dry Valleys are a record of short-term, occasional melting events along the margins of the East Antarctic Ice Sheet. Sediment samples were dated from five fans using Optically Stimulated Luminescence (OSL) dating. OSL dates the time since quartz grains were last exposed to sunlight; all sample preparation takes place in a dark room. Thirteen samples were dated for this thesis, the ages were stratigraphically consistent and ranged from 1.1 ka to 105.9 ka. Clusters of fan activity occurred between 1.1 and 3.1 ka and 8.1 and 11.1 ka. The melting events appear to be linked to insolation, with periods of fan activity occurring usually at times of increased mean annual insolation. The alluvial fans show promise as a possible archive for climate proxies in this region of Antarctica. |
format |
Thesis |
author |
Ramsey, Meridith Ann |
spellingShingle |
Ramsey, Meridith Ann OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica |
author_facet |
Ramsey, Meridith Ann |
author_sort |
Ramsey, Meridith Ann |
title |
OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica |
title_short |
OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica |
title_full |
OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica |
title_fullStr |
OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica |
title_full_unstemmed |
OSL Dating of High-Elevation Alluvial Sediments: McMurdo Dry Valleys, Antarctica |
title_sort |
osl dating of high-elevation alluvial sediments: mcmurdo dry valleys, antarctica |
publisher |
North Dakota State University |
publishDate |
2015 |
url |
https://hdl.handle.net/10365/27578 |
genre |
Antarc* Antarctic Antarctica Ice Sheet McMurdo Dry Valleys |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet McMurdo Dry Valleys |
op_relation |
https://hdl.handle.net/10365/27578 |
op_rights |
NDSU Policy 190.6.2 |
_version_ |
1781069505663860736 |