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Please use this identifier to cite or link to this item: http://apo.ansto.gov.au/dspace/handle/10238/3834

Title: In-situ cosmogenic exposure dating in the Meirs and Garwood valleys, Denton Hills, Antarctica
Authors: Joy, K
Carson, N
Fink, D
Storey, B
Keywords: Valleys
Age estimation
Geomorphology
Hydrology
Beryllium 10
Aluminium 26
Issue Date: 23-Mar-2011
Publisher: 12th International Conference on Accelerator Mass Spectrometry (AMS-12)
Citation: Joy, K., Carson, N., Fink, D., Storey, B. (2011). In-situ cosmogenic exposure dating in the Meirs and Garwood valleys, Denton Hills, Antarctica, 12th International Conference on Accelerator Mass Spectrometry (AMS 12), 20th - 25th March 2011. Museum of New Zealand: Te Papa Tongarewa, Wellington, New Zealand.
Abstract: It has been hypothesised that during interglacials, thinning of the Ross Ice Shelf allowed a more open water environment with increased local precipitation. This resulted in adjacent glaciers within the Transantarctic Mountains to advance during moist warmer periods, apparently out of phase with colder arid dry periods. The geomorphology of the Denton Hills in the Royal Society Range, West Antarctica, is a result of Miocene fluvial incision reworked by subsequent warm and cold-based glacial advances throughout the Quaternary. Outlet glacials, which drain ice into the Shelf, should thus show maximum extent during interstadials. To understand the chronology of late Quaternary glaciations, 15 granitic boulders from terminal moraines in the Garwood and Miers Valleys were sampled for 10Be and 26Al cosmogenic dating. Obtaining reliable exposure ages of erratics within moraines that represent timing of deposition (i.e. glacial advances) is problematic in polar regions, where glacial activity is principally controlled by ice sheet dynamics. Recycling of previously exposed debris, uncertainty in provenance of glacially transported boulders and a lack of a post-depositional hydrologic process to remove previously exposed material from a valley system, leads to ambiguities in multiple exposure ages from a single coeval glacial landform. More importantly, cold-based ice advance can leave a landform unmodified resulting in young erratics deposited on bedrock that shows weathering and/or inconsistent age-altitude relationships. Primarily, inheritance becomes a difficulty in qualifying exposure ages from polar regions. Preliminary results based on average ages indicate that glaciers in the Denton Hills advanced to their maximum position between 30-35 ka, earlier than the Antarctic LGM (18-22 ka), then retreated leaving little evidence of late interglacial or Holocene advances. However, accounting for inheritance and taking the youngest 10Be ages, advance occurs at 20-22ka during the LGM. Hence support for the out-of-phase hypothesis depends largely on the exposure age model adopted. Copyright (c) 2011 AMS12.
URI: http://www.gns.cri.nz/ams12/AMS-12_Abstracts_Book_Final.pdf
http://apo.ansto.gov.au/dspace/handle/10238/3834
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