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University of Wisconsin-Madison, Department of Geology and Geophysics, 1215 West Dayton Street, Madison WI 53706, USA; NASA Astrobiology Institute, USA
University of Wisconsin, Department of Geoscience, 1215 West Dayton Street, Madison, WI 53706, USA; NASA Astrobiology Institute, USA
Fe, C, and O isotope compositions of banded iron formation carbonates demonstrate a major role for dissimilatory iron reduction in ~2.5 Ga marine environments
Iron isotope fractionation between aqueous ferrous iron and goethite
The role of volatile exsolution and sub-solidus fluid/rock interactions in producing high 56Fe/54Fe ratios in siliceous igneous rocks
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