Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica

Citation:
Aciego, SM, Cuffey KM, Kavanaugh JL, Morse DL, Severinghaus JP.  2007.  Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica. Quaternary Research. 68:303-313.

Date Published:

Nov

Keywords:

accumulation, climate, core, delta O-18, delta O-18 of O-2, delta(18), Dome, glacier strain rates, greenland ice, horizontal ice core, margin, o-18 record, stratigraphy, taylor dome, taylor glacier, transition, west greenland

Abstract:

Ice exposed in ablation zones of ice sheets can be a valuable source of samples for paleoclimate studies and information about long-term ice dynamics. We report a 28-km long stable isotope sampling transect along a flowline on lower Taylor Glacier, Antarctica, and show that ice from the last glacial period is exposed here over tens of kilometers. Gas isotope analyses on a small number of samples confirm our age hypothesis. These chronostratigraphic data contain information about past ice dynamics and in particular should be sensitive to the longitudinal strain rate on the north flank of Taylor Dome, averaged over millennia. The imprint of climatic changes on ice dynamics may be discernible in these data. (c) 2007 University of Washington. All rights reserved.

Notes:

n/a

Website

DOI:

10.1016/j.yqres.2007.07.013