@article {3045,
	title = {H Is a Major Intermediate in  Corrosion of Iron.},
	journal = {mBio},
	volume = {14},
	year = {2023},
	month = {2023 Apr 25},
	pages = {e0007623},
	abstract = {<p>Desulfovibrio vulgaris has been a primary pure culture sulfate reducer for developing microbial corrosion concepts. Multiple mechanisms for how it accepts electrons from Fe have been proposed. We investigated Fe oxidation with a mutant of  in which hydrogenase genes were deleted. The hydrogenase mutant grew as well as the parental strain with lactate as the electron donor, but unlike the parental strain, it was not able to grow on H. The parental strain reduced sulfate with Fe as the sole electron donor, but the hydrogenase mutant did not. H accumulated over time in Fe cultures of the hydrogenase mutant and sterile controls but not in parental strain cultures. Sulfide stimulated H production in uninoculated controls apparently by both reacting with Fe to generate H and facilitating electron transfer from Fe to H. Parental strain supernatants did not accelerate H production from Fe, ruling out a role for extracellular hydrogenases. Previously proposed electron transfer between Fe and  via soluble electron shuttles was not evident. The hydrogenase mutant did not reduce sulfate in the presence of Fe and either riboflavin or anthraquinone-2,6-disulfonate, and these potential electron shuttles did not stimulate parental strain sulfate reduction with Fe as the electron donor. The results demonstrate that  primarily accepts electrons from Fe via H as an intermediary electron carrier. These findings clarify the interpretation of previous  corrosion studies and suggest that H-mediated electron transfer is an important mechanism for iron corrosion under sulfate-reducing conditions.  Microbial corrosion of iron in the presence of sulfate-reducing microorganisms is economically significant. There is substantial debate over how microbes accelerate iron corrosion. Tools for genetic manipulation have only been developed for a few Fe(III)-reducing and methanogenic microorganisms known to corrode iron and in each case those microbes were found to accept electrons from Fe via direct electron transfer. However, iron corrosion is often most intense in the presence of sulfate-reducing microbes. The finding that Desulfovibrio vulgaris relies on H to shuttle electrons between Fe and cells revives the concept, developed in some of the earliest studies on microbial corrosion, that sulfate reducers consumption of H is a major microbial corrosion mechanism. The results further emphasize that direct Fe-to-microbe electron transfer has yet to be rigorously demonstrated in sulfate-reducing microbes.</p>},
	keywords = {Corrosion, Desulfovibrio, Desulfovibrio vulgaris, Hydrogenase, Iron, Lactic Acid, Oxidation-Reduction, Sulfates},
	issn = {2150-7511},
	doi = {10.1128/mbio.00076-23},
	author = {Woodard, Trevor L and Ueki, Toshiyuki and Lovley, Derek R}
}
@article {507,
	title = {Heat-shock sigma factor RpoH from Geobacter sulfurreducens.},
	journal = {Microbiology},
	volume = {153},
	year = {2007},
	month = {2007 Mar},
	pages = {838-46},
	abstract = {Recent studies with Myxococcus xanthus have suggested that homologues of the Escherichia coli heat-shock sigma factor, RpoH, may not be involved in the heat-shock response in this delta-proteobacterium. The genome of another delta-proteobacterium, Geobacter sulfurreducens, which is considered to be a representative of the Fe(III)-reducing Geobacteraceae that predominate in a diversity of subsurface environments, contains an rpoH homologue. Characterization of the G. sulfurreducens rpoH homologue revealed that it was induced by a temperature shift from 30 degrees C to 42 degrees C and that an rpoH-deficient mutant was unable to grow at 42 degrees C. The predicted heat-shock genes, hrcA, grpE, dnaK, groES and htpG, were heat-shock inducible in an rpoH-dependent manner, and comparison of promoter regions of these genes identified the consensus sequences for the -10 and -35 promoter elements. In addition, DNA elements identical to the CIRCE consensus sequence were found in promoters of rpoH, hrcA and groES, suggesting that these genes are regulated by a homologue of the repressor HrcA, which is known to bind the CIRCE element. These results suggest that the G. sulfurreducens RpoH homologue is the heat-shock sigma factor and that heat-shock response in G. sulfurreducens is regulated positively by RpoH as well as negatively by the HrcA/CIRCE system.},
	keywords = {Adaptation, Physiological, Base Sequence, Binding Sites, Consensus Sequence, DNA, Bacterial, Gene Expression Regulation, Bacterial, Genome, Bacterial, Geobacter, Heat-Shock Proteins, Hot Temperature, Molecular Sequence Data, Promoter Regions, Genetic, RNA, Bacterial, RNA, Messenger, Sigma Factor, Transcription, Genetic},
	issn = {1350-0872},
	doi = {10.1099/mic.0.2006/000638-0},
	author = {Ueki, Toshiyuki and Lovley, Derek R}
}
