A glacial stage spanning the Antarctic Cold Reversal in Torres del Paine (51°S), Chile, based on preliminary cosmogenic exposure ages

C. J. Fogwill*, P. W. Kubik

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

Initial cosmogenic 10Be results from a former ice limit in Torres del Paine indicate a shortlived stillstand or readvance of Patagonian ice culminating at 12-15 kyr BP with a mean age of 13.2 ± 0.8 kyr BP. The glacier extended some 40 km beyond the present ice margin and was within 15 km of the presumed Last Glacial Maximum limits. The timing of the glacier stage spans the cooling event recorded in Antarctic ice cores, termed the Antarctic Cold Reversal (14.5-12.9 kyr BP). This result implies that glaciers at these latitudes were out of phase with those in the northern hemisphere; instead they mirrored the climate structure of Antarctica during the last glacial to interglacial transition.

Original languageEnglish
Pages (from-to)403-408
Number of pages6
JournalGeografiska Annaler, Series A: Physical Geography
Volume87
Issue number2
DOIs
Publication statusPublished - 2005
Externally publishedYes

ASJC Scopus subject areas

  • Geography, Planning and Development
  • Geology

Keywords

  • Antarctic Cold Reversal
  • Cosmogenic
  • Geomorphology
  • Late Glacial
  • Patagonia
  • South America

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