Was the Late-glacial advance at ~14.0 ka B.P. in Torres del Paine (Patagonia, 51S) the most extensive glacial pulse of Oxygen Isotope Stage 2?

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ADS bibcode
2010AGUFMGC21A0860G
year
2010
Listed Authors
Garcia, J.
Hall, B. L.
Kaplan, M. R.
Schaefer, J. M.
Vega, R. M.
Schwartz, R.
Finkel, R. C.
Listed Institutions
Department of Earth Sciences/Climate Change Institute, University of Maine, Orono, ME, USA
Department of Earth Sciences/Climate Change Institute, University of Maine, Orono, ME, USA
Geochemistry, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
Geochemistry, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
Instituto de Geociencias, Universidad Austral de Chile, Valdivia, Chile
Geochemistry, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
Cams, Lawrence Livermore National Laboratory, Livermore, CA, USA

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