Acronyms
Definition
Iron oxidation is a chemolithotrophic microbial metabolism whereby metabolic energy is generated via the removal of electrons (oxidation) from inorganic ferrous iron [Fe(II)]-containing compounds, resulting in the formation of ferric iron [Fe(III)]-containing compounds.
Overview
Prokaryotic organisms are capable of generating metabolic energy from the oxidation of Fe(II) to Fe(III), often coupled to autotrophic growth (chemolithoautotrophy) (Konhauser et al. 2011). A wide range of environments are present on Earth where microorganisms are known to participate in Fe(II) oxidation (Fig. 1). Due to the rapid rate of abiotic oxidation of soluble Fe(II) by oxygen at neutral pH (Singer and Stumm 1970), several strategies exist for iron-oxidizing bacteria (FeOB) to compete with abiotic oxidation including oxidation of soluble Fe(II) at neutral pH under low-oxygen conditions, oxidation of insoluble Fe(II) mineral phases at neutral pH,...
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References and Further Reading
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Napieralski, S.A., Fortney, N.W., Roden, E.E. (2020). Iron Oxidation. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5401-1
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DOI: https://doi.org/10.1007/978-3-642-27833-4_5401-1
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