Fe Isotope Variations in the Modern and Ancient Earth and Other Planetary Bodies

By B. Beard, Clark M. Johnson. 2004

259 citations recorded by the source corpus.

Subfields: Geochemistry and Petrology, Inorganic Chemistry, Paleontology

View Paper: https://www.semanticscholar.org/paper/45bee9220fd519c61788df4c563a7d3044dbc3c7

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In Geochemistry and Petrology

1. D. Bazylinski

In Inorganic Chemistry

1. D. Bazylinski

In Paleontology

1. D. Bazylinski

Citations in the corpus

• Magnetite as a prokaryotic biomarker: A review (2010, background): “…fractionations for the microbial magnetite–soluble Fe(II) system range from 4.2 to 0.0‰ [Mandernack et al., 1999; Polyakov and Mineev, 2000; Schauble et al., 2001; Johnson et al., 2003, 2004], which is nearly as broad as the entire range of terrestrial Fe isotope compositions observed in nature.”