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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Main Author: Ramsey, Meridith Ann
Format: Thesis
Language:unknown
Published: North Dakota State University 2015
Subjects:
Online Access:https://hdl.handle.net/10365/27578
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spelling 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
institution Open Polar
collection North Dakota State University (NDSU) Digital Repository
op_collection_id 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
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