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Iron Reduction

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Encyclopedia of Astrobiology

Acronyms

DIR:

Dissimilatory iron reduction

DIRM:

Dissimilatory iron reducing microorganisms

Definition

Dissimilatory iron reduction (DIR) is a form of anaerobic (without oxygen) microbial respiration whereby energy is generated by coupling the oxidation (removal of electrons) of organic matter (chemoorganotrophy) or H2 (chemolithotrophy) to the reduction (addition of electrons) of ferric iron [Fe(III)]. DIR can by generalized by the following equations, where “CH2O” represents a single unit of organic carbon, and Fe(OH)3 represents an iron oxide mineral phase:

Chemoorganotrophic Fe(III) reduction:

$$ {\mathrm{CH}}_2\mathrm{O}+4\mathrm{Fe}{\left(\mathrm{OH}\right)}_3+7{\mathrm{H}}^{+}\to 4{\mathrm{Fe}}^{2+}+{\mathrm{H}\mathrm{CO}}_3^{-}+10{\mathrm{H}}_2\mathrm{O} $$
(1)

Chemolithotrophic Fe(III) reduction:

$$ {\mathrm{H}}_2+2\mathrm{Fe}{\left(\mathrm{OH}\right)}_3+4{\mathrm{H}}^{+}\to 2{\mathrm{Fe}}^{2+}+6{\mathrm{H}}_2\mathrm{O} $$
(2)

Overview

Microbial Fe(III) reduction plays an...

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Correspondence to Eric E. Roden .

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Fortney, N.W., Napieralski, S.A., Roden, E.E. (2020). Iron Reduction. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5402-1

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_5402-1

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