Evaluation of Dissimilatory Microbial Iron Oxide Reduction as a Mechanism for the Generation of Banded Iron Formation Minerals

Details Evaluation of Dissimilatory Microbial Iron Oxide Reduction as a Mechanism for the Generation of Banded Iron Formation Minerals Evaluation of Dissimilatory Microbial Iron Oxide Reduction as a Mechanism for the Generation of Banded Iron Formation Minerals

Apr 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpico1538.5247p&link_type=abstract

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

Biology

Scientific paper

This research seeks to define the potential for dissimilatory microbial
Fe(III) oxide reduction to generate Fe(II)-bearing minerals, analogous
to those found in BIFs, in reaction systems that mimick conditions in
Archean ocean sediments.

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