Hydrothermal Alteration Chemistry of Archean Submarine Volcanic Rocks: Evidence for a Fully Oxygenated Atmosphere-Ocean System Since ~3.5 Ga

Details Hydrothermal Alteration Chemistry of Archean Submarine Volcanic Rocks: Evidence for a Fully Oxygenated Atmosphere-Ocean System Since ~3.5 Ga Hydrothermal Alteration Chemistry of Archean Submarine Volcanic Rocks: Evidence for a Fully Oxygenated Atmosphere-Ocean System Since ~3.5 Ga

Apr 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpico1538.5667o&link_type=abstract

Astrobiology Science Conference 2010: Evolution and Life: Surviving Catastrophes and Extremes on Earth and Beyond, held April 2

Biology

Scientific paper

Behaviors of redox sensitive elements (e.g., Fe, Mn, S, U, Cr, Ce) in
hydrothermally altered submarine volcanic rocks of Archean ages suggest
that the O2 and SO4 contents of ocean water and the atmospheric O2 level
have been essentially the same since at least ~3.5 Ga.

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