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VI. Microbial Reduction of Other Metals

VI. Microbial Reduction of Other Metals

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cury from contaminated environments (Goldstein et al., 1988; Barkay et al., 199 1 ;

Ogunseitan and Olson, 1991).


Microorganisms can enzymatically catalyze the reduction of a large number of

metals. For abundant metals such as Fe(II1) and Mn(IV), microorganisms have

evolved specific metabolic systems which permit them to conserve energy to

support growth by coupling the oxidation of organic matter to metal reduction.

Microbial Fe(II1) reduction accounts for most of the Fe(II1) reduction in many

anoxic soils and aquatic sediments. Nonenzymatic processes such as the reduction of Fe(II1) by organic compounds and sulfide are generally of minor significance. Mn(1V) reduction is more susceptible to reduction by nonenzymatic

processes, but enzymatic Mn(1V) reduction does predominate in some environments. Fe(II1) and Mn(IV) reduction are major processes for decomposition of

naturally occurring organic matter in some soils and sediments and can play an

important role in the degradation of organic contaminants. The microbial reduction of insoluble Fe(II1) and Mn(1V) oxides increases the solubility of these metals, releases nutrients and metals that were adsorbed on the oxides, leads to the

formation of new Fe(I1)- and Mn(I1)-containing minerals, and alters a variety of

soil properties. These changes can be both beneficial and detrimental to plant


Many Fe(II1)- and Mn(1V)-reducing microorganisms can also reduce highly

soluble U(V1) to insoluble U(1V). Microbial U(V1) reduction provides a likely

explanation for the reductive precipitation of uranium in anoxic soils and sediments. Furthermore, U(V1)-reducing microorganisms might be useful agents for

the bioremediation of uranium-contaminated environments.

In a similar manner, the microbial reduction of soluble selenate to insoluble Se'

removes selenium from water and this metabolism can be employed to immobilize

selenium in environments with high selenium concentrations. Microorganisms

can reduce highly soluble and toxic Cr(V1) to Cr(III), which is less soluble and

less toxic. However, the environmental significance of this metabolism and its

utility as a bioremediation technique have yet to be clearly demonstrated. Some

microorganisms can enzymatically reduce other metals such as mercury, vanadium, molybdenum, copper, gold, silver, and technetium. This metabolism may

affect the fate and mobility of these metals.

Although recent studies have demonstrated the importance of microbial metal

reduction and have identified organisms which may serve as models for this metabolism, very little is known about the biochemistry of this process. There is little

information on the organisms that are responsible for enzymatic metal reduction



in natural environments. It is not clear whether the metal-reducing microorganisms that are available in pure culture are representative of the important metal

reducers in soils and sediments. Further studies on the biochemistry and microbial

ecology of metal reduction would enhance our understanding of the factors controlling the rate and extent of this important process.


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