@article {3047, title = {Genetic Manipulation of Desulfovibrio ferrophilus and Evaluation of Fe(III) Oxide Reduction Mechanisms.}, journal = {Microbiol Spectr}, volume = {10}, year = {2022}, month = {2022 Dec 21}, pages = {e0392222}, abstract = {

The sulfate-reducing microbe Desulfovibrio ferrophilus is of interest due to its relatively rare ability to also grow with Fe(III) oxide as an electron acceptor and its rapid corrosion of metallic iron. Previous studies have suggested multiple agents for extracellular electron exchange including a soluble electron shuttle, electrically conductive pili, and outer surface multiheme -type cytochromes. However, the previous lack of a strategy for genetic manipulation of limited mechanistic investigations. We developed an electroporation-mediated transformation method that enabled replacement of genes of interest with an antibiotic resistance gene via double-crossover homologous recombination. Genes were identified that are essential for flagellum-based motility and the expression of the two types of pili. Disrupting flagellum-based motility or expression of either of the two pili did not inhibit Fe(III) oxide reduction, nor did deleting genes for multiheme -type cytochromes predicted to be associated with the outer membrane. Although redundancies in cytochrome or pilus function might explain some of these phenotypes, overall, the results are consistent with primarily reducing Fe(III) oxide via an electron shuttle. The finding that is genetically tractable not only will aid in elucidating further details of its mechanisms for Fe(III) oxide reduction but also provides a new experimental approach for developing a better understanding of some of its other unique features, such as the ability to corrode metallic iron at high rates and accept electrons from negatively poised electrodes. is an important pure culture model for Fe(III) oxide reduction and the corrosion of iron-containing metals in anaerobic marine environments. This study demonstrates that is genetically tractable, an important advance for elucidating the mechanisms by which it interacts with extracellular electron acceptors and donors. The results demonstrate that there is not one specific outer surface multiheme -type cytochrome that is essential for Fe(III) oxide reduction. This finding, coupled with the lack of apparent porin-cytochrome conduits encoded in the genome and the finding that deleting genes for pilus and flagellum expression did not inhibit Fe(III) oxide reduction, suggests that has adopted strategies for extracellular electron exchange that are different from those of intensively studied electroactive microbes like and species. Thus, the ability to genetically manipulate is likely to lead to new mechanistic concepts in electromicrobiology.

}, keywords = {Cytochromes, Electron Transport, Ferric Compounds, Iron, Oxidation-Reduction, Oxides}, issn = {2165-0497}, doi = {10.1128/spectrum.03922-22}, author = {Ueki, Toshiyuki and Woodard, Trevor L and Lovley, Derek R} } @article {3128, title = {Magnetite compensates for the lack of a pilin-associated c-type cytochrome in extracellular electron exchange.}, journal = {Environ Microbiol}, volume = {17}, year = {2015}, month = {2015 Mar}, pages = {648-55}, abstract = {

Nanoscale magnetite can facilitate microbial extracellular electron transfer that plays an important role in biogeochemical cycles, bioremediation and several bioenergy strategies, but the mechanisms for the stimulation of extracellular electron transfer are poorly understood. Further investigation revealed that magnetite attached to the electrically conductive pili of Geobacter species in a manner reminiscent of the association of the multi-heme c-type cytochrome OmcS with the pili of Geobacter sulfurreducens. Magnetite conferred extracellular electron capabilities on an OmcS-deficient strain unable to participate in interspecies electron transfer or Fe(III) oxide reduction. In the presence of magnetite wild-type cells repressed expression of the OmcS gene, suggesting that cells might need to produce less OmcS when magnetite was available. The finding that magnetite can compensate for the lack of the electron transfer functions of a multi-heme c-type cytochrome has implications not only for the function of modern microbes, but also for the early evolution of microbial electron transport mechanisms.

}, keywords = {Cytochrome c Group, Electron Transport, Electrons, Ferrosoferric Oxide, Fimbriae Proteins, Fimbriae, Bacterial, Gene Expression Regulation, Bacterial, Geobacter, Heme, Oxides}, issn = {1462-2920}, doi = {10.1111/1462-2920.12485}, author = {Liu, Fanghua and Rotaru, Amelia-Elena and Shrestha, Pravin M and Malvankar, Nikhil S and Nevin, Kelly P and Lovley, Derek R} } @article {3114, title = {Seeing is believing: novel imaging techniques help clarify microbial nanowire structure and function.}, journal = {Environ Microbiol}, volume = {17}, year = {2015}, month = {2015 Jul}, pages = {2209-15}, abstract = {

Novel imaging approaches have recently helped to clarify the properties of {\textquoteright}microbial nanowires{\textquoteright}. Geobacter sulfurreducens pili are actual wires. They possess metallic-like conductivity, which can be attributed to overlapping pi-pi orbitals of key aromatic amino acids. Electrostatic force microscopy recently confirmed charge propagation along the pili, in a manner similar to carbon nanotubes. The pili are essential for long-range electron transport to insoluble electron acceptors and interspecies electron transfer. Previous claims that Shewanella oneidensis also produce conductive pili have recently been recanted, based on novel live-imaging studies. The putative pili are, in fact, long extensions of the cytochrome-rich outer membrane and periplasm that, when dried, collapse to form filaments with dimensions similar to pili. It has yet to be demonstrated whether the cytochrome-to-cytochrome electron hopping documented in the dried membrane extensions takes place in intact hydrated membrane extensions or whether the membrane extensions enhance electron transport to insoluble electron acceptors such as Fe(III) oxides or electrodes. These findings demonstrate that G. sulfurreducens conductive pili and the outer membrane extensions of S. oneidensis are fundamentally different in composition, mechanism of electron transport and physiological role. New methods for evaluating filament conductivity will facilitate screening the microbial world for nanowires and elucidating their function.

}, keywords = {Cytochromes, Electric Conductivity, Electron Transport, Electrons, Ferric Compounds, Fimbriae, Bacterial, Geobacter, Microscopy, Atomic Force, Nanowires, Oxides, Periplasm, Shewanella}, issn = {1462-2920}, doi = {10.1111/1462-2920.12708}, author = {Lovley, Derek R and Malvankar, Nikhil S} } @article {517, title = {A putative multicopper protein secreted by an atypical type II secretion system involved in the reduction of insoluble electron acceptors in Geobacter sulfurreducens.}, journal = {Microbiology}, volume = {152}, year = {2006}, month = {2006 Aug}, pages = {2257-64}, abstract = {Extracellular electron transfer onto Fe(III) oxides in Geobacter sulfurreducens is considered to require proteins that must be exported to the outer surface of the cell. In order to investigate this, the putative gene for OxpG, the pseudopilin involved in a type II general secretion pathway of Gram-negative bacteria, was deleted. The mutant was unable to grow with insoluble Fe(III) oxide as the electron acceptor. Growth on soluble Fe(III) was not affected. An analysis of proteins that accumulated in the periplasm of the oxpG mutant, but not in the wild-type, led to the identification of a secreted protein, OmpB. OmpB is predicted to be a multicopper protein, with highest homology to the manganese oxidase, MofA, from Leptothrix discophora. OmpB contains a potential Fe(III)-binding site and a fibronectin type III domain, suggesting a possible role for this protein in accessing Fe(III) oxides. OmpB was localized to the membrane fraction of G. sulfurreducens and in the supernatant of growing cultures, consistent with the type II secretion system exporting OmpB. A mutant in which ompB was deleted had the same phenotype as the oxpG mutant, suggesting that the failure to export OmpB was responsible for the inability of the oxpG-deficient mutant to reduce Fe(III) oxide. This is the first report that proposes a role for a multicopper oxidase-like protein in an anaerobic organism. These results further emphasize the importance of outer-membrane proteins in Fe(III) oxide reduction and suggest that outer-membrane proteins other than c-type cytochromes are required for Fe(III) oxide reduction in Geobacter species.}, keywords = {Bacterial Outer Membrane Proteins, Electron Transport, Ferric Compounds, Fimbriae Proteins, Geobacter, Manganese Compounds, Mutation, Oxidation-Reduction, Oxides}, issn = {1350-0872}, doi = {10.1099/mic.0.28864-0}, author = {Mehta, Teena and Childers, Susan E and Glaven, Richard and Lovley, Derek R and Mester, T{\"u}nde} } @article {534, title = {A novel Geobacteraceae-specific outer membrane protein J (OmpJ) is essential for electron transport to Fe(III) and Mn(IV) oxides in Geobacter sulfurreducens.}, journal = {BMC Microbiol}, volume = {5}, year = {2005}, month = {2005}, pages = {41}, abstract = {BACKGROUND: Metal reduction is thought to take place at or near the bacterial outer membrane and, thus, outer membrane proteins in the model dissimilatory metal-reducing organism Geobacter sulfurreducens are of interest to understand the mechanisms of Fe(III) reduction in the Geobacter species that are the predominant Fe(III) reducers in many environments. Previous studies have implicated periplasmic and outer membrane cytochromes in electron transfer to metals. Here we show that the most abundant outer membrane protein of G. sulfurreducens, OmpJ, is not a cytochrome yet it is required for metal respiration. RESULTS: When outer membrane proteins of G. sulfurreducens were separated via SDS-PAGE, one protein, designated OmpJ (outer membrane protein J), was particularly abundant. The encoding gene, which was identified from mass spectrometry analysis of peptide fragments, is present in other Geobacteraceae, but not in organisms outside this family. The predicted localization and structure of the OmpJ protein suggested that it was a porin. Deletion of the ompJ gene in G. sulfurreducens produced a strain that grew as well as the wild-type strain with fumarate as the electron acceptor but could not grow with metals, such as soluble or insoluble Fe(III) and insoluble Mn(IV) oxide, as the electron acceptor. The heme c content in the mutant strain was ca. 50\% of the wild-type and there was a widespread loss of multiple cytochromes from soluble and membrane fractions. Transmission electron microscopy analyses of mutant cells revealed an unusually enlarged periplasm, which is likely to trigger extracytoplasmic stress response mechanisms leading to the degradation of periplasmic and/or outer membrane proteins, such as cytochromes, required for metal reduction. Thus, the loss of the capacity for extracellular electron transport in the mutant could be due to the missing c-type cytochromes, or some more direct, but as yet unknown, role of OmpJ in metal reduction. CONCLUSION: OmpJ is a putative porin found in the outer membrane of the model metal reducer G. sulfurreducens that is required for respiration of extracellular electron acceptors such as soluble and insoluble metals. The effect of OmpJ in extracellular electron transfer is indirect, as OmpJ is required to keep the integrity of the periplasmic space necessary for proper folding and functioning of periplasmic and outer membrane electron transport components. The exclusive presence of ompJ in members of the Geobacteraceae family as well as its role in metal reduction suggest that the ompJ sequence may be useful in tracking the growth or activity of Geobacteraceae in sedimentary environments.}, keywords = {Amino Acid Sequence, Bacterial Outer Membrane Proteins, Base Sequence, Biological Transport, Deltaproteobacteria, DNA Primers, Ferric Compounds, Gene Deletion, Genome, Bacterial, Geobacter, Manganese Compounds, Molecular Sequence Data, Oxides, Peptide Fragments, Phylogeny, Protein Structure, Secondary, Spectrometry, Mass, Matrix-Assisted Laser Desorption-Ionization}, issn = {1471-2180}, doi = {10.1186/1471-2180-5-41}, author = {Afkar, Eman and Reguera, Gemma and Schiffer, Marianne and Lovley, Derek R} } @article {545, title = {Dissimilatory Fe(III) and Mn(IV) reduction.}, journal = {Adv Microb Physiol}, volume = {49}, year = {2004}, month = {2004}, pages = {219-86}, abstract = {Dissimilatory Fe(III) and Mn(IV) reduction has an important influence on the geochemistry of modern environments, and Fe(III)-reducing microorganisms, most notably those in the Geobacteraceae family, can play an important role in the bioremediation of subsurface environments contaminated with organic or metal contaminants. Microorganisms with the capacity to conserve energy from Fe(III) and Mn(IV) reduction are phylogenetically dispersed throughout the Bacteria and Archaea. The ability to oxidize hydrogen with the reduction of Fe(III) is a highly conserved characteristic of hyperthermophilic microorganisms and one Fe(III)-reducing Archaea grows at the highest temperature yet recorded for any organism. Fe(III)- and Mn(IV)-reducing microorganisms have the ability to oxidize a wide variety of organic compounds, often completely to carbon dioxide. Typical alternative electron acceptors for Fe(III) reducers include oxygen, nitrate, U(VI) and electrodes. Unlike other commonly considered electron acceptors, Fe(III) and Mn(IV) oxides, the most prevalent form of Fe(III) and Mn(IV) in most environments, are insoluble. Thus, Fe(III)- and Mn(IV)-reducing microorganisms face the dilemma of how to transfer electrons derived from central metabolism onto an insoluble, extracellular electron acceptor. Although microbiological and geochemical evidence suggests that Fe(III) reduction may have been the first form of microbial respiration, the capacity for Fe(III) reduction appears to have evolved several times as phylogenetically distinct Fe(III) reducers have different mechanisms for Fe(III) reduction. Geobacter species, which are representative of the family of Fe(III) reducers that predominate in a wide diversity of sedimentary environments, require direct contact with Fe(III) oxides in order to reduce them. In contrast, Shewanella and Geothrix species produce chelators that solubilize Fe(III) and release electron-shuttling compounds that transfer electrons from the cell surface to the surface of Fe(III) oxides not in direct contact with the cells. Electron transfer from the inner membrane to the outer membrane in Geobacter and Shewanella species appears to involve an electron transport chain of inner-membrane, periplasmic, and outer-membrane c-type cytochromes, but the cytochromes involved in these processes in the two organisms are different. In addition, Geobacter species specifically express flagella and pili during growth on Fe(III) and Mn(IV) oxides and are chemotactic to Fe(II) and Mn(II), which may lead Geobacter species to the oxides under anoxic conditions. 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. In comparison with other respiratory processes, the study of Fe(III) and Mn(IV) reduction is in its infancy, but genome-enabled approaches are rapidly advancing our understanding of this environmentally significant physiology.}, keywords = {Archaea, Biodegradation, Environmental, Ferric Compounds, Geobacter, Manganese, Manganese Compounds, Oxidation-Reduction, Oxides, Shewanella, Soil Microbiology, Soil Pollutants}, issn = {0065-2911}, doi = {10.1016/S0065-2911(04)49005-5}, author = {Lovley, Derek R and Holmes, Dawn E and Nevin, Kelly P} } @article {586, title = {Geobacter metallireducens accesses insoluble Fe(III) oxide by chemotaxis.}, journal = {Nature}, volume = {416}, year = {2002}, month = {2002 Apr 18}, pages = {767-9}, abstract = {Microorganisms that use insoluble Fe(III) oxide as an electron acceptor can have an important function in the carbon and nutrient cycles of aquatic sediments and in the bioremediation of organic and metal contaminants in groundwater. Although Fe(III) oxides are often abundant, Fe(III)-reducing microbes are faced with the problem of how to access effectively an electron acceptor that can not diffuse to the cell. Fe(III)-reducing microorganisms in the genus Shewanella have resolved this problem by releasing soluble quinones that can carry electrons from the cell surface to Fe(III) oxide that is at a distance from the cell. Here we report that another Fe(III)-reducer, Geobacter metallireducens, has an alternative strategy for accessing Fe(III) oxides. Geobacter metallireducens specifically expresses flagella and pili only when grown on insoluble Fe(III) or Mn(IV) oxide, and is chemotactic towards Fe(II) and Mn(II) under these conditions. These results suggest that G. metallireducens senses when soluble electron acceptors are depleted and then synthesizes the appropriate appendages to permit it to search for, and establish contact with, insoluble Fe(III) or Mn(IV) oxide. This approach to the use of an insoluble electron acceptor may explain why Geobacter species predominate over other Fe(III) oxide-reducing microorganisms in a wide variety of sedimentary environments.}, keywords = {Bacterial Proteins, Chemotaxis, Deltaproteobacteria, DNA-Binding Proteins, Ferric Compounds, Ferrous Compounds, Fimbriae Proteins, Fimbriae, Bacterial, Flagella, Manganese Compounds, Movement, Oxidation-Reduction, Oxides, Solubility}, issn = {0028-0836}, doi = {10.1038/416767a}, author = {Childers, Susan E and Ciufo, Stacy and Lovley, Derek R} }