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Dissimilatory Fe(III) and Mn(IV) reduction.

D. Lovley, D. Holmes, K. Nevin

1991.6.1Advances in Microbial Physiology

DOI: 10.1016/s0065-2911(04)49005-5

tlooto Summary

The physiological characteristics of Geobacter species appear to explain why they have consistently been found to be the predominant Fe(III)- and Mn(IV)-reducing microorganisms in a variety of sedimentary environments.

Abstract

Abstract is not available.

Citation format

LOVLEY, D.; HOLMES, D.; NEVIN, K. Dissimilatory fe(iii) and mn(iv) reduction. Advances in Microbial Physiology, 1991, 49: 219–86.