Windblown Pliocene diatoms and East Antarctic Ice Sheet retreat

A long-standing debate regarding the Pliocene history of the East Antarctic Ice Sheet was spurred by the discovery of marine diatoms in the Transantarctic Mountains. Here the authors show that the diatoms were emplaced by wind following a retreat of the ice sheet into coastal basins and subsequent i...

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Autores principales: Reed P. Scherer, Robert M. DeConto, David Pollard, Richard B. Alley
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2016
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Acceso en línea:https://doaj.org/article/946bb23d42314b39b681c33aa6fd692e
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