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Hoffmann, R. A wiki for the life sciences where authorship matters. Nature Genetics (2008)
 
 
 

Role of humic-bound iron as an electron transfer agent in dissimilatory Fe(III) reduction.

The dissimilatory Fe(III) reducer Geobacter metallireducens reduced Fe(III) bound in humic substances, but the concentrations of Fe(III) in a wide range of highly purified humic substances were too low to account for a significant portion of the electron-accepting capacities of the humic substances. Furthermore, once reduced, the iron in humic substances could not transfer electrons to Fe(III) oxide. These results suggest that other electron-accepting moieties in humic substances, such as quinones, are the important electron-accepting and shuttling agents under Fe(III)-reducing conditions.[1]

References

  1. Role of humic-bound iron as an electron transfer agent in dissimilatory Fe(III) reduction. Lovley, D.R., Blunt-Harris, E.L. Appl. Environ. Microbiol. (1999) [Pubmed]
 
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