作者: Margit Schwikowski , Sabina Brütsch , Gino Casassa , Andrés Rivera
DOI: 10.3189/172756406781812014
关键词: Geology 、 Ice field 、 Altitude 、 Ice core 、 Geomorphology 、 Southern Hemisphere 、 Glacier 、 Paleoclimatology 、 Meltwater 、 Firn
摘要: The Patagonia icefields constitute a unique location in the Southern Hemisphere for obtaining non-polar paleo-records from ice cores south of 458 S. Nevertheless, no ice-core record with meaningful paleoclimate information has yet been obtained Patagonia. This deficiency is due to extremely harsh field conditions, and fact that main plateaus both Hielo Patagonico Norte (HPN; northern icefield) Sur (HPS; southern are strongly affected by meltwater percolation. In order explore suitability high-elevation glacier sites at HPS as archives, three shallow firn were retrieved covering altitude range 1543-2300 m a.s.l. glaciochemical records two lower confirm presence superimposed ice, clear sign formation core 2300 m, signature appears be preserved, indicating significant melting occurred. Although there might problems associated wind erosion extreme melt events, good potential well-preserved within glaciers located higher than m.