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Fe, C, and O isotope compositions of banded iron formation carbonates demonstrate a major role for dissimilatory iron reduction in ~2.5Ga marine environments

Marine GeologyBiogeochemistryEngineeringChemical OceanographyIsotope GeochemistryMarine ChemistryGeochemistry~2.5Ga Marine EnvironmentsEarth ScienceBanded Iron FormationDissimilatory Iron Reduction