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

被引:41
作者
Fogwill, CJ [1 ]
Kubik, PW
机构
[1] Univ Edinburgh, Sch Geosci, Inst Geog, Edinburgh EH8 9XP, Midlothian, Scotland
[2] ETH Honggerberg, Inst Particle Phys, Paul Scherrer Inst, CH-8093 Zurich, Switzerland
关键词
Antarctic Cold Reversal; South America; Patagonia; Late Glacial; geomorphology; cosmogenic;
D O I
10.1111/j.0435-3676.2005.00266.x
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Initial cosmogenic Be-10 results from a former ice limit in Torres del Paine indicate a short-lived 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.
引用
收藏
页码:403 / 408
页数:6
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