Fe isotope fractionation during Fe(II) oxidation by the marine photoferrotroph Rhodovulum iodosum in the presence of Si – Implications for Precambrian iron formation deposition
Fe isotope fractionation during Fe(II) oxidation by the marine photoferrotroph Rhodovulum iodosum in the presence of Si – Implications for Precambrian iron formation deposition
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Keywords
Banded iron formations, Precambrian ocean, Phototrophic iron oxidation, Bacteria, Iron isotopes, Silica
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