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Secretion of flavins by Shewanella species and their role in extracellular electron transfer

Authors
Journal
Applied and Environmental Microbiology
0099-2240
Publisher
American Society for Microbiology
Publication Date
Keywords
  • Soluble Fumarate Reductase
  • Dissimilatory Fe(Iii)
  • Putrefaciens Mr-1
  • Mn(Iv) Reduction
  • Oneidensis Mr-1
  • Outer-Membrane
  • Sp. Nov
  • Strain
  • Oxide
  • Microorganisms
Disciplines
  • Biology

Abstract

Fe (III)-respiring bacteria such as Shewanella species play an important role in the global cycle of iron, manganese, and trace metals and are useful for many biotechnological applications, including microbial fuel cells and the bioremediation of waters and sediments contaminated with organics, metals, and radionuclides. Several alternative electron transfer pathways have been postulated for the reduction of insoluble extracellular subsurface minerals, such as Fe(III) oxides, by Shewanella species. One such potential mechanism involves the secretion of an electron shuttle. Here we identify for the first time flavin mononucleotide (FMN) and riboflavin as the extracellular electron shuttles produced by a range of Shewanella species. FMN secretion was strongly correlated with growth and exceeded riboflavin secretion, which was not exclusively growth associated but was maximal in the stationary phase of batch cultures. Flavin adenine dinucleotide was the predominant intracellular flavin but was not released by live cells. The flavin yields were similar under both aerobic and anaerobic conditions, with total flavin concentrations of 2.9 and 2.1 mu mol per gram of cellular protein, respectively, after 24 h and were similar under dissimilatory Fe (III)-reducing conditions and when fumarate was supplied as the sole electron acceptor. The flavins were shown to act as electron shuttles and to promote anoxic growth coupled to the accelerated reduction of poorly crystalline Fe(III) oxides. The implications of flavin secretion by Shewanella cells living at redox boundaries, where these mineral phases can be significant electron acceptors for growth, are discussed.

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