Magnetite as a precursor for green rust through the hydrogenotrophic activity of the iron‐reducing bacteria Shewanella putrefaciens
Abstract
Magnetite (Fe(II) Fe(III) 2 O4 ) is often considered as a stable end product of the bioreduction of Fe(III) minerals (e.g., ferrihydrite, lepidocrocite, hematite) or of the biological oxidation of Fe(II) compounds (e.g., siderite), with green rust (GR) as a mixed Fe(II) -Fe(III) hydroxide intermediate. Until now, the biotic transformation of magnetite to GR has not been evidenced. In this study, we investigated the capability of an iron-reducing bacterium, Shewanella putrefaciens, to reduce magnetite at circumneutral pH in the presence of dihydrogen as sole inorganic electron donor. During incubation, GR and/or siderite (Fe(II) CO3 ) formation occurred as secondary iron minerals, resulting from the precipitation of Fe(II) species produced via the bacterial reduction of Fe(III) species present in magnetite. Taking into account the exact nature of the secondary iron minerals and the electron donor source is necessary to understand the exergonic character of the biotic transformation of magnetite to GR, which had been considered to date as thermodynamically unfavorable at circumneutral pH. This finding reinforces the hypothesis that GR would be the cornerstone of the microbial transformations of iron-bearing minerals in the anoxic biogeochemical cycle of iron and opens up new possibilities for the interpretation of the evolution of Earth's history and for the understanding of biocorrosion processes in the field of applied science.
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Green rust might be the product of a bacterially mediated reaction involving Fe(III)-reducing bacteria and magnetite.
“Etique et al. (2015) demonstrated that green rust might be the product of a bacterially mediated reaction involving Fe(III)-reducing bacteria and magnetite.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Etique et al., 2015
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Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history
Konhauser, K. O., Planavsky, N. J., Hardisty, D. S., Robbins, L. J., Warchola, T. J., Haugaard, R., Lalonde, S. V., Partin, C. A., Oonk, P. B. H., Tsikos, H., et al. (2017) · Earth-Science Reviews · doi:10.1016/j.earscirev.2017.06.012 · Cited by 537 · see citing works
- Authors
- Etique, M., Jorand, F. P. A., & Ruby, C.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- Corresponding author
- Etique, M.
- Venue
- Geobiology
- Publisher
- Wiley
- Published
- 2015-12-30
- Volume
- 14
- Issue
- 3
- Pages
- 237-254
- ISSN
- 1472-4669 (ISSN-L)
- 1472-4677
- OpenAlex
- W2326926306
- Cited by
- 37
- References
- 90
- Citations by year
- 2026: 1 · 2024: 3 · 2023: 2 · 2022: 8 · 2021: 4 · 2020: 6 · 2019: 2 · 2018: 5 · 2017: 3 · 2016: 2 · 2015: 1
- FWCI
- 2.64
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geobiology (publishedVersion)
- PubMed (publishedVersion)
- HAL (submittedVersion)
- Funders
- Agence Nationale pour la Gestion des Déchets Radioactifs
- Centre National de la Recherche Scientifique
- Topics
- Physical Sciences › Environmental Science › Environmental Engineering › Microbial Fuel Cells and Bioremediation
- 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
- magnetite, green rust, Shewanella putrefaciens, iron-reducing bacteria, siderite, secondary iron minerals, biomineralization, iron biogeochemical cycle, microbiologically influenced corrosion, circumneutral pH
- MeSH terms
- Ferric Compounds, Iron, Oxidation-Reduction, Shewanella putrefaciens, Ferrosoferric Oxide
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