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 language | English |
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Pages (from-to) | 403-408 |
Number of pages | 6 |
Journal | Geografiska Annaler, Series A: Physical Geography |
Volume | 87 |
Issue number | 2 |
DOIs | |
Publication status | Published - 2005 |
Externally published | Yes |
ASJC Scopus subject areas
- Geography, Planning and Development
- Geology
Keywords
- Antarctic Cold Reversal
- Cosmogenic
- Geomorphology
- Late Glacial
- Patagonia
- South America