Sources and Contributions of Oxygen During Microbial Pyrite Oxidation: The Triple Oxygen Isotopes of Sulfate as a Biosignature

Details Sources and Contributions of Oxygen During Microbial Pyrite Oxidation: The Triple Oxygen Isotopes of Sulfate as a Biosignature Sources and Contributions of Oxygen During Microbial Pyrite Oxidation: The Triple Oxygen Isotopes of Sulfate as a Biosignature

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2245z&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2245

Physics

Scientific paper

Microbial pyrite oxidation experiments in spiked water and the triple
oxygen isotopes of resulting sulfate suggest that Δ17OSO4
signatures can trace microbial vs. inorganic sulfate formation, and,
therefore, have the potential as biosignature.

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