Pliocene Paleoenvironment and Antarctic Ice Sheet Behavior: Evidence From Wright Valley

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Pliocene Paleoenvironment and Antarctic Ice Sheet Behavior: Evidence from Wright Valley

Investigations in Wright Valley, adjacent to the Transantarctic Mountains in East Antarctica, shed light on the question of whether high-latitude Pliocene climate was warm enough to cause widespread deglaciation of the East Antarctic craton with a concurrent Magellanic moorland-like environment. If Pliocene-age diatoms, presently in glaciogenic deposits high in the Transantarctic Mountains, had...

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The Late Pliocene epoch is a potential analogue for future climate in a warming world. Here we reconstruct Plio-Pleistocene East Antarctic Ice Sheet (EAIS) variability using cosmogenic nuclide exposure ages and model simulations to better understand ice sheet behaviour under such warm conditions. New and previously published exposure ages indicate interior-thickening during the Pliocene. An ice...

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Pliocene paleoclimate and East antarctic ice-sheet history from surficial ash deposits.

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ژورنال

عنوان ژورنال: The Journal of Geology

سال: 1997

ISSN: 0022-1376,1537-5269

DOI: 10.1086/515922