@article {3111, title = {Structural basis for metallic-like conductivity in microbial nanowires.}, journal = {mBio}, volume = {6}, year = {2015}, month = {2015 Mar 03}, pages = {e00084}, abstract = {

UNLABELLED: Direct measurement of multiple physical properties of Geobacter sulfurreducens pili have demonstrated that they possess metallic-like conductivity, but several studies have suggested that metallic-like conductivity is unlikely based on the structures of the G.~sulfurreducens pilus predicted from homology models. In order to further evaluate this discrepancy, pili were examined with synchrotron X-ray microdiffraction and rocking-curve X-ray diffraction. Both techniques revealed a periodic 3.2-{\r A} spacing in conductive, wild-type G.~sulfurreducens pili that was missing in the nonconductive pili of strain Aro5, which lack key aromatic acids required for conductivity. The intensity of the 3.2-{\r A} peak increased 100-fold when the pH was shifted from 10.5 to 2, corresponding with a previously reported 100-fold increase in pilus conductivity with this pH change. These results suggest a clear structure-function correlation for metallic-like conductivity that can be attributed to overlapping π-orbitals of aromatic amino acids. A homology model of the G.~sulfurreducens pilus was constructed with a Pseudomonas aeruginosa pilus model as a template as an alternative to previous models, which were based on a Neisseria gonorrhoeae pilus structure. This alternative model predicted that aromatic amino acids in G.~sulfurreducens pili are packed within 3 to 4~{\r A}, consistent with the experimental results. Thus, the predictions of homology modeling are highly sensitive to assumptions inherent in the model construction. The experimental results reported here further support the concept that the pili of G.~sulfurreducens represent a novel class of electronically functional proteins in which aromatic amino acids promote long-distance electron transport.

IMPORTANCE: The mechanism for long-range electron transport along the conductive pili of Geobacter sulfurreducens is of interest because these "microbial nanowires" are important in biogeochemical cycling as well as applications in bioenergy and bioelectronics. Although proteins are typically insulators, G.~sulfurreducens pilus proteins possess metallic-like conductivity. The studies reported here provide important structural insights into the mechanism of the metallic-like conductivity of G.~sulfurreducens pili. This information is expected to be useful in the design of novel bioelectronic materials.

}, keywords = {Amino Acids, Aromatic, Chemical Phenomena, Electrophysiological Phenomena, Fimbriae, Bacterial, Geobacter, Hydrogen-Ion Concentration, Models, Molecular, Nanowires, X-Ray Diffraction}, issn = {2150-7511}, doi = {10.1128/mBio.00084-15}, author = {Malvankar, Nikhil S and Vargas, Madeline and Nevin, Kelly and Tremblay, Pier-Luc and Evans-Lutterodt, Kenneth and Nykypanchuk, Dmytro and Martz, Eric and Tuominen, Mark T and Lovley, Derek R} } @article {486, title = {Characterization of extracellular minerals produced during dissimilatory Fe(III) and U(VI) reduction at 100 degrees C by Pyrobaculum islandicum.}, journal = {Geobiology}, volume = {6}, year = {2008}, month = {2008 Mar}, pages = {147-54}, abstract = {In order to gain insight into the significance of biotic metal reduction and mineral formation in hyperthermophilic environments, metal mineralization as a result of the dissimilatory reduction of poorly crystalline Fe(III) oxide, and U(VI) reduction at 100 degrees C by Pyrobaculum islandicum was investigated. When P. islandicum was grown in a medium with poorly crystalline Fe(III) oxide as an electron acceptor and hydrogen as an electron donor, the Fe(III) oxide was reduced to an extracellular, ultrafine-grained magnetite with characteristics similar to that found in some hot environments and that was previously thought to be of abiotic origin. Furthermore, cell suspensions of P. islandicum rapidly reduced the soluble and oxidized form of uranium, U(VI), to extracellular precipitates of the highly insoluble U(IV) mineral, uraninite (UO(2)). The reduction of U(VI) was dependent on the presence of hydrogen as the electron donor. These findings suggest that microbes may play a key role in metal deposition in hyperthermophilic environments and provide a plausible explanation for such phenomena as magnetite accumulation and formation of uranium deposits at ca. 100 degrees C.}, keywords = {Ferric Compounds, Ferumoxytol, Hot Temperature, Hydrogen, Minerals, Oxidation-Reduction, Pyrobaculum, Uranium, X-Ray Diffraction}, issn = {1472-4669}, doi = {10.1111/j.1472-4669.2007.00142.x}, author = {Kashefi, K and Moskowitz, B M and Lovley, D R} } @article {655, title = {Reduction of uranium by Desulfovibrio desulfuricans.}, journal = {Appl Environ Microbiol}, volume = {58}, year = {1992}, month = {1992 Mar}, pages = {850-6}, abstract = {The possibility that sulfate-reducing microorganisms contribute to U(VI) reduction in sedimentary environments was investigated. U(VI) was reduced to U(IV) when washed cells of sulfate-grown Desulfovibrio desulfuricans were suspended in a bicarbonate buffer with lactate or H2 as the electron donor. There was no U(VI) reduction in the absence of an electron donor or when the cells were killed by heat prior to the incubation. The rates of U(VI) reduction were comparable to those in respiratory Fe(III)-reducing microorganisms. Azide or prior exposure of the cells to air did not affect the ability of D. desulfuricans to reduce U(VI). Attempts to grow D. desulfuricans with U(VI) as the electron acceptor were unsuccessful. U(VI) reduction resulted in the extracellular precipitation of the U(IV) mineral uraninite. The presence of sulfate had no effect on the rate of U(VI) reduction. Sulfate and U(VI) were reduced simultaneously. Enzymatic reduction of U(VI) by D. desulfuricans was much faster than nonenzymatic reduction of U(VI) by sulfide, even when cells of D. desulfuricans were added to provide a potential catalytic surface for the nonenzymatic reaction. The results indicate that enzymatic U(VI) reduction by sulfate-reducing microorganisms may be responsible for the accumulation of U(IV) in sulfidogenic environments. Furthermore, since the reduction of U(VI) to U(IV) precipitates uranium from solution, D. desulfuricans might be a useful organism for recovering uranium from contaminated waters and waste streams.}, keywords = {Biodegradation, Environmental, Desulfovibrio, Kinetics, Oxidation-Reduction, Sulfates, Uranium, X-Ray Diffraction}, issn = {0099-2240}, author = {Lovley, D R and Phillips, E J} }