Iron, Carbon, and Oxygen Isotope Compositions of Banded Iron Formation Carbonates Demonstrate a Major Role for Microbial Dissimilatory Iron Reduction in 2.5 b.y. old Marine Environments

Details Iron, Carbon, and Oxygen Isotope Compositions of Banded Iron Formation Carbonates Demonstrate a Major Role for Microbial Dissimilatory Iron Reduction in 2.5 b.y. old Marine Environments Iron, Carbon, and Oxygen Isotope Compositions of Banded Iron Formation Carbonates Demonstrate a Major Role for Microbial Dissimilatory Iron Reduction in 2.5 b.y. old Marine Environments

Apr 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpico1538.5265j&link_type=abstract

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

Biology

Scientific paper

Fe, C, and O isotope data on carbonates of 2.5 Ga banded iron formations
demonstrate formation via microbial dissimilatory iron reduction rather
than precipitation from seawater, establishing the importance of this
metabolism on the early Earth.

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