Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley
The hyper-arid, cryotic, wind-dominated conditions in the high-elevation McMurdo Dry Valleys of Antarctica are among Earth’s most extreme environments and represent the closest terrestrial analog to the surface of Mars. These unique conditions result in complex surface processes that occur in the ov...
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ftvuwellington:oai:researcharchive.vuw.ac.nz:10063/6228 2023-08-15T12:37:56+02:00 Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley Trinh-Le, Cassandra Anh Dickinson, Warren Norton, Kevin 2017 http://researcharchive.vuw.ac.nz/handle/10063/6228 en_NZ eng Victoria University of Wellington http://researcharchive.vuw.ac.nz/handle/10063/6228 Permafrost Optically stimulated luminescence Meteoric beryllium-10 Soil geochemistry Sedimentation McMurdo Dry Valleys Mars analog Text Master's 2017 ftvuwellington 2023-07-25T17:26:55Z The hyper-arid, cryotic, wind-dominated conditions in the high-elevation McMurdo Dry Valleys of Antarctica are among Earth’s most extreme environments and represent the closest terrestrial analog to the surface of Mars. These unique conditions result in complex surface processes that occur in the overall absence of liquid water. However, since water is typically believed to be required for these processes to occur, the mechanisms responsible for how these processes can persist in this environment are poorly understood. Previous studies that focused on individual processes of sedimentation in the Dry Valleys leave questions regarding the role of water in dry cryotic sedimentation as well as the rates at which these processes occur. This thesis addresses these questions by combining Optically Stimulated Luminescence (OSL) dating, meteoric Beryllium-10 (10Be) measurements, soil geochemistry analysis, and petrographic microscopy analysis on ice-cemented permafrost cores taken from University Valley, one of the high-elevation Dry Valleys, where the availability and effects of liquid water are minimal. These analyses were used to explore four main sedimentation processes that occur in the Dry Valleys: chemical weathering, fine particle translocation, eolian transport, and physical weathering. Analyzed together, findings from these analyses comprehensively describe the complex processes involved in dry cryotic sedimentation and determine the roles of different phases of water in this environment. Sediments in University Valley have accumulated at a rate of approximately 2.1 mm/ka for the last 200 ka, as dated by OSL, from erosion of the valley walls and deposition of windblown dust. Sediment accumulation is influenced by topography of the valley floor, depth of the ice table, aspect of the valley walls, wind direction, and mechanical breakdown of rocks due to solar heating. While persistent winds constantly remobilize fine particles and dust in the upper few cm of the dry ground, sediment grains that are sand-sized or ... Master Thesis Antarc* Antarctica Ice McMurdo Dry Valleys permafrost Victoria University of Wellington: ResearchArchive McMurdo Dry Valleys University Valley ENVELOPE(160.667,160.667,-77.867,-77.867) |
institution |
Open Polar |
collection |
Victoria University of Wellington: ResearchArchive |
op_collection_id |
ftvuwellington |
language |
English |
topic |
Permafrost Optically stimulated luminescence Meteoric beryllium-10 Soil geochemistry Sedimentation McMurdo Dry Valleys Mars analog |
spellingShingle |
Permafrost Optically stimulated luminescence Meteoric beryllium-10 Soil geochemistry Sedimentation McMurdo Dry Valleys Mars analog Trinh-Le, Cassandra Anh Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley |
topic_facet |
Permafrost Optically stimulated luminescence Meteoric beryllium-10 Soil geochemistry Sedimentation McMurdo Dry Valleys Mars analog |
description |
The hyper-arid, cryotic, wind-dominated conditions in the high-elevation McMurdo Dry Valleys of Antarctica are among Earth’s most extreme environments and represent the closest terrestrial analog to the surface of Mars. These unique conditions result in complex surface processes that occur in the overall absence of liquid water. However, since water is typically believed to be required for these processes to occur, the mechanisms responsible for how these processes can persist in this environment are poorly understood. Previous studies that focused on individual processes of sedimentation in the Dry Valleys leave questions regarding the role of water in dry cryotic sedimentation as well as the rates at which these processes occur. This thesis addresses these questions by combining Optically Stimulated Luminescence (OSL) dating, meteoric Beryllium-10 (10Be) measurements, soil geochemistry analysis, and petrographic microscopy analysis on ice-cemented permafrost cores taken from University Valley, one of the high-elevation Dry Valleys, where the availability and effects of liquid water are minimal. These analyses were used to explore four main sedimentation processes that occur in the Dry Valleys: chemical weathering, fine particle translocation, eolian transport, and physical weathering. Analyzed together, findings from these analyses comprehensively describe the complex processes involved in dry cryotic sedimentation and determine the roles of different phases of water in this environment. Sediments in University Valley have accumulated at a rate of approximately 2.1 mm/ka for the last 200 ka, as dated by OSL, from erosion of the valley walls and deposition of windblown dust. Sediment accumulation is influenced by topography of the valley floor, depth of the ice table, aspect of the valley walls, wind direction, and mechanical breakdown of rocks due to solar heating. While persistent winds constantly remobilize fine particles and dust in the upper few cm of the dry ground, sediment grains that are sand-sized or ... |
author2 |
Dickinson, Warren Norton, Kevin |
format |
Master Thesis |
author |
Trinh-Le, Cassandra Anh |
author_facet |
Trinh-Le, Cassandra Anh |
author_sort |
Trinh-Le, Cassandra Anh |
title |
Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley |
title_short |
Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley |
title_full |
Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley |
title_fullStr |
Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley |
title_full_unstemmed |
Dry sedimentation processes in the high-elevation McMurdo Dry Valleys, Antarctica: A case study in University Valley |
title_sort |
dry sedimentation processes in the high-elevation mcmurdo dry valleys, antarctica: a case study in university valley |
publisher |
Victoria University of Wellington |
publishDate |
2017 |
url |
http://researcharchive.vuw.ac.nz/handle/10063/6228 |
long_lat |
ENVELOPE(160.667,160.667,-77.867,-77.867) |
geographic |
McMurdo Dry Valleys University Valley |
geographic_facet |
McMurdo Dry Valleys University Valley |
genre |
Antarc* Antarctica Ice McMurdo Dry Valleys permafrost |
genre_facet |
Antarc* Antarctica Ice McMurdo Dry Valleys permafrost |
op_relation |
http://researcharchive.vuw.ac.nz/handle/10063/6228 |
_version_ |
1774297105309892608 |