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Can in-situ cosmogenic 14C be used to assess the influence of clast recycling on exposure dating of ice retreat in Antarctica?

Journal Article


Abstract


  • Cosmogenic nuclide exposure dating of glacial clasts is becoming a common and robust method for reconstructing the history of glaciers and ice sheets. In Antarctica, however, many samples exhibit cosmogenic nuclide ‘inheritance’ as a result of sediment recycling and exposure to cosmic radiation during previous ice free periods. In-situ cosmogenic 14C, in combination with longer lived nuclides such as 10Be, can be used to detect inheritance because the relatively short half-life of 14C means that in-situ14C acquired in exposure during previous interglacials decays away while the sample locality is covered by ice during the subsequent glacial. Measurements of in-situ14C in clasts from the last deglaciation of the Framnes Mountains in East Antarctica provide deglaciation ages that are concordant with existing 26Al and 10Be ages, suggesting that in this area, the younger population of erratics contain limited inheritance.

UOW Authors


  •   White, Duanne A. (external author)
  •   Fulop, Reka
  •   Bishop, Paul (external author)
  •   Mackintosh, Andrew (external author)
  •   Cook, Gordon T. (external author)

Publication Date


  • 2011

Citation


  • White, D., Fulop, R. Hajnalka., Bishop, P., Mackintosh, A. & Cook, G. (2011). Can in-situ cosmogenic 14C be used to assess the influence of clast recycling on exposure dating of ice retreat in Antarctica?. Quaternary Geochronology, 6 (3-4), 289-294.

Scopus Eid


  • 2-s2.0-79955724861

Ro Metadata Url


  • http://ro.uow.edu.au/smhpapers/4234

Has Global Citation Frequency


Number Of Pages


  • 5

Start Page


  • 289

End Page


  • 294

Volume


  • 6

Issue


  • 3-4

Place Of Publication


  • Netherlands

Abstract


  • Cosmogenic nuclide exposure dating of glacial clasts is becoming a common and robust method for reconstructing the history of glaciers and ice sheets. In Antarctica, however, many samples exhibit cosmogenic nuclide ‘inheritance’ as a result of sediment recycling and exposure to cosmic radiation during previous ice free periods. In-situ cosmogenic 14C, in combination with longer lived nuclides such as 10Be, can be used to detect inheritance because the relatively short half-life of 14C means that in-situ14C acquired in exposure during previous interglacials decays away while the sample locality is covered by ice during the subsequent glacial. Measurements of in-situ14C in clasts from the last deglaciation of the Framnes Mountains in East Antarctica provide deglaciation ages that are concordant with existing 26Al and 10Be ages, suggesting that in this area, the younger population of erratics contain limited inheritance.

UOW Authors


  •   White, Duanne A. (external author)
  •   Fulop, Reka
  •   Bishop, Paul (external author)
  •   Mackintosh, Andrew (external author)
  •   Cook, Gordon T. (external author)

Publication Date


  • 2011

Citation


  • White, D., Fulop, R. Hajnalka., Bishop, P., Mackintosh, A. & Cook, G. (2011). Can in-situ cosmogenic 14C be used to assess the influence of clast recycling on exposure dating of ice retreat in Antarctica?. Quaternary Geochronology, 6 (3-4), 289-294.

Scopus Eid


  • 2-s2.0-79955724861

Ro Metadata Url


  • http://ro.uow.edu.au/smhpapers/4234

Has Global Citation Frequency


Number Of Pages


  • 5

Start Page


  • 289

End Page


  • 294

Volume


  • 6

Issue


  • 3-4

Place Of Publication


  • Netherlands