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Clathrate formation and the fate of noble and biologically useful gases in Lake Vostok, Antarctica

  • Published:2003-07 Issue:13 Volume:30 Page:
  • ISSN:0094-8276
  • Container-title:Geophysical Research Letters
  • language:en
  • Short-container-title:Geophys. Res. Lett.

Author:

McKay C. P.1,Hand K. P.2,Doran P. T.3,Andersen D. T.4,Priscu J. C.5

Affiliation:

1. Space Science Division; NASA Ames; Moffett Field California USA

2. Department of Geological and Environmental Sciences; Stanford University; Stanford California USA

3. Department of Earth and Environmental Sciences; University of Illinois at Chicago; Chicago Illinois USA

4. Center for the Study of Life in the Universe; SETI Institute; Mountain View California USA

5. Department of Land Resources and Environmental Sciences; Montana State University; Bozeman Montana USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference31 articles.

1. Dissolved gases in perennially ice-covered Antarctic lakes of the McMurdo Dry Valleys;Andersen;Antarctic Science,1998

2. Non-stoicheiometric clathrate compounds of water;Barrer;Proc. Royal. Soc. London,1957

3. Origin and fate of Lake Vostok water frozen to the base of the East Antarctic ice sheet;Bell;Nature,2002

4. Empirical laws for dilute aqueous solutions of nonpolar gases;Benson;J. Chem. Phys.,1976

5. Helium isotopes and gases in Dye 3 ice cores;Craig;Eos Trans. AGU,1982

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