Experimental constraints on Fe isotope fractionation during magnetite and Fe carbonate formation coupled to dissimilatory hydrous ferric oxide reduction
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Fe(III)-Si gels are resistant to phase transformations when exposed to dissolved Fe(II).
“when exposed to dissolved Fe(II), Fe(III)-Si gels are resistant to phase transformations that may occur in dissolved Fe(II)-ferrihydrite experiments (e.g., Johnson et al., 2005)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Johnson et al., 2005
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- Authors
- Johnson, C. M., Roden, E. E., Welch, S. A., & Beard, B. L.
- Affiliations
- University of Wisconsin–Madison (US)
- University of Alabama (US)
- Corresponding author
- Johnson, Clark M.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2005-02
- Volume
- 69
- Issue
- 4
- Pages
- 963-993
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2128185490
- Cited by
- 237
- References
- 103
- Citations by year
- 2026: 5 · 2025: 7 · 2024: 11 · 2023: 7 · 2022: 7 · 2021: 12 · 2020: 13 · 2019: 10 · 2018: 6 · 2017: 15 · 2016: 10 · 2015: 12 · 2014: 12 · 2013: 11 · 2012: 10
- FWCI
- 13.52
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- ANU Open Research (Australian National University) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Geomagnetism and Paleomagnetism Studies
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- iron isotope fractionation, magnetite, siderite, dissimilatory iron reduction, Shewanella putrefaciens, Shewanella algae, Geobacter sulfurreducens, kinetic isotope fractionation, equilibrium fractionation, banded iron formations, microbial iron reduction
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