Glacier fluctuations in the southern Peruvian Andes during the late-glacial period, constrained with cosmogenic 3He

The occurrence of pronounced climate reversals during the last glacial termination has long been recognised in palaeoclimate records from both hemispheres and from high to low latitudes. Accurate constraint of both the timing and magnitude of events, such as the Younger Dryas and Antarctic Cold Reve...

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Veröffentlicht in:	Journal of quaternary science 2011-01, Vol.26 (1), p.37-43
Hauptverfasser:	Bromley, Gordon R.M., Hall, Brenda L., Schaefer, Joerg M., Winckler, Gisela, Todd, Claire E., Rademaker, Kurt M.
Format:	Artikel
Sprache:	eng
Schlagworte:	Age Aridity Chronology Climate cosmogenic helium-3 Fluctuation Glaciers Hemispheres last termination late-glacial reversal Tropics
Online-Zugang:	Volltext
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