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:
Chemolithotrophic Fe(III) reduction:
Overview
Microbial Fe(III) reduction plays an...
References and Further Reading
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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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