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7 LIVING ON IRON

  • Andreas Kappler , Stefanie Becker and Allison M. L. Enright
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Abstract

Reduced and oxidized iron is present in virtually all of Earth’s environments. Iron is essential to all living organisms because it is a critical component of many biomolecules. It can also be used as an electron donor or terminal electron acceptor by microorganisms for metabolic redox reactions which generate energy and drive growth. In this chapter we introduce the environmental distribution and redox activity of iron and discuss how different types of Fe(II)-oxidizing (aerobic, microaerophilic, anoxygenic phototrophic, and anaerobic nitratereducing) and Fe(III)-reducing (ammonium-oxidizing, organic matter-oxidizing, methanotrophic, sulfur-oxidizing) microorganisms use the oxidation and reduction of Fe(II) and Fe(III), respectively, to generate energy and to produce biomass. In addition, we present some of the many biotechnological and environmental applications of iron-cycling microorganisms.

Abstract

Reduced and oxidized iron is present in virtually all of Earth’s environments. Iron is essential to all living organisms because it is a critical component of many biomolecules. It can also be used as an electron donor or terminal electron acceptor by microorganisms for metabolic redox reactions which generate energy and drive growth. In this chapter we introduce the environmental distribution and redox activity of iron and discuss how different types of Fe(II)-oxidizing (aerobic, microaerophilic, anoxygenic phototrophic, and anaerobic nitratereducing) and Fe(III)-reducing (ammonium-oxidizing, organic matter-oxidizing, methanotrophic, sulfur-oxidizing) microorganisms use the oxidation and reduction of Fe(II) and Fe(III), respectively, to generate energy and to produce biomass. In addition, we present some of the many biotechnological and environmental applications of iron-cycling microorganisms.

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