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Jonathan D. Toner, Ronald S. Sletten and Michael L. Prentice Soluble salt accumulations in Taylor Valley, Antarctica: Implications for paleolakes and Ross Sea Ice Sheet dynamics Journal of Geophysical Research: Earth Surface 118

Article first published online: 8 MAR 2013 | DOI: 10.1029/2012JF002467

Key Points

  • Soluble salt indicate the history of paleolakes and the Ross Sea Ice Sheet
  • The Ross Sea Ice Sheet dammed 300 m deep paleolakes in western Taylor Valley
  • Soluble salts are influenced by cation exchange and calcite/gypsum dissolution

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