@article {415,
	title = {Geobacter: the microbe electric{\textquoteright}s physiology, ecology, and practical applications.},
	journal = {Adv Microb Physiol},
	volume = {59},
	year = {2011},
	month = {2011},
	pages = {1-100},
	abstract = {Geobacter species specialize in making electrical contacts with extracellular electron acceptors and other organisms. This permits Geobacter species to fill important niches in a diversity of anaerobic environments. Geobacter species appear to be the primary agents for coupling the oxidation of organic compounds to the reduction of insoluble Fe(III) and Mn(IV) oxides in many soils and sediments, a process of global biogeochemical significance. Some Geobacter species can anaerobically oxidize aromatic hydrocarbons and play an important role in aromatic hydrocarbon removal from contaminated aquifers. The ability of Geobacter species to reductively precipitate uranium and related contaminants has led to the development of bioremediation strategies for contaminated environments. Geobacter species produce higher current densities than any other known organism in microbial fuel cells and are common colonizers of electrodes harvesting electricity from organic wastes and aquatic sediments. Direct interspecies electron exchange between Geobacter species and syntrophic partners appears to be an important process in anaerobic wastewater digesters. Functional and comparative genomic studies have begun to reveal important aspects of Geobacter physiology and regulation, but much remains unexplored. Quantifying key gene transcripts and proteins of subsurface Geobacter communities has proven to be a powerful approach to diagnose the in situ physiological status of Geobacter species during groundwater bioremediation. The growth and activity of Geobacter species in the subsurface and their biogeochemical impact under different environmental conditions can be predicted with a systems biology approach in which genome-scale metabolic models are coupled with appropriate physical/chemical models. The proficiency of Geobacter species in transferring electrons to insoluble minerals, electrodes, and possibly other microorganisms can be attributed to their unique "microbial nanowires," pili that conduct electrons along their length with metallic-like conductivity. Surprisingly, the abundant c-type cytochromes of Geobacter species do not contribute to this long-range electron transport, but cytochromes are important for making the terminal electrical connections with Fe(III) oxides and electrodes and also function as capacitors, storing charge to permit continued respiration when extracellular electron acceptors are temporarily unavailable. The high conductivity of Geobacter pili and biofilms and the ability of biofilms to function as supercapacitors are novel properties that might contribute to the field of bioelectronics. The study of Geobacter species has revealed a remarkable number of microbial physiological properties that had not previously been described in any microorganism. Further investigation of these environmentally relevant and physiologically unique organisms is warranted.},
	keywords = {Biotechnology, Ecology, Environmental Remediation, Ferric Compounds, Geobacter},
	issn = {0065-2911},
	doi = {10.1016/B978-0-12-387661-4.00004-5},
	author = {Lovley, Derek R and Ueki, Toshiyuki and Zhang, Tian and Malvankar, Nikhil S and Shrestha, Pravin M and Flanagan, Kelly A and Aklujkar, Muktak and Butler, Jessica E and Giloteaux, Ludovic and Rotaru, Amelia-Elena and Holmes, Dawn E and Franks, Ashley E and Orellana, Roberto and Risso, Carla and Nevin, Kelly P}
}
@article {505,
	title = {Importance of c-Type cytochromes for U(VI) reduction by Geobacter sulfurreducens.},
	journal = {BMC Microbiol},
	volume = {7},
	year = {2007},
	month = {2007},
	pages = {16},
	abstract = {BACKGROUND: In order to study the mechanism of U(VI) reduction, the effect of deleting c-type cytochrome genes on the capacity of Geobacter sulfurreducens to reduce U(VI) with acetate serving as the electron donor was investigated.

RESULTS: The ability of several c-type cytochrome deficient mutants to reduce U(VI) was lower than that of the wild type strain. Elimination of two confirmed outer membrane cytochromes and two putative outer membrane cytochromes significantly decreased (ca. 50-60\%) the ability of G. sulfurreducens to reduce U(VI). Involvement in U(VI) reduction did not appear to be a general property of outer membrane cytochromes, as elimination of two other confirmed outer membrane cytochromes, OmcB and OmcC, had very little impact on U(VI) reduction. Among the periplasmic cytochromes, only MacA, proposed to transfer electrons from the inner membrane to the periplasm, appeared to play a significant role in U(VI) reduction. A subpopulation of both wild type and U(VI) reduction-impaired cells, 24-30\%, accumulated amorphous uranium in the periplasm. Comparison of uranium-accumulating cells demonstrated a similar amount of periplasmic uranium accumulation in U(VI) reduction-impaired and wild type G. sulfurreducens. Assessment of the ability of the various suspensions to reduce Fe(III) revealed no correlation between the impact of cytochrome deletion on U(VI) reduction and reduction of Fe(III) hydroxide and chelated Fe(III).

CONCLUSION: This study indicates that c-type cytochromes are involved in U(VI) reduction by Geobacter sulfurreducens. The data provide new evidence for extracellular uranium reduction by G. sulfurreducens but do not rule out the possibility of periplasmic uranium reduction. Occurrence of U(VI) reduction at the cell surface is supported by the significant impact of elimination of outer membrane cytochromes on U(VI) reduction and the lack of correlation between periplasmic uranium accumulation and the capacity for uranium reduction. Periplasmic uranium accumulation may reflect the ability of uranium to penetrate the outer membrane rather than the occurrence of enzymatic U(VI) reduction. Elimination of cytochromes rarely had a similar impact on both Fe(III) and U(VI) reduction, suggesting that there are differences in the routes of electron transfer to U(VI) and Fe(III). Further studies are required to clarify the pathways leading to U(VI) reduction in G. sulfurreducens.},
	keywords = {Biodegradation, Environmental, Cytochrome c Group, Ferric Compounds, Geobacter, Microscopy, Electron, Transmission, Mutation, Oxidation-Reduction, Periplasm, Uranium},
	issn = {1471-2180},
	doi = {10.1186/1471-2180-7-16},
	author = {Shelobolina, Evgenya S and Coppi, Maddalena V and Korenevsky, Anton A and DiDonato, Laurie N and Sullivan, Sara A and Konishi, Hiromi and Xu, Huifang and Leang, Ching and Butler, Jessica E and Kim, Byoung-Chan and Lovley, Derek R}
}
@article {551,
	title = {MacA, a diheme c-type cytochrome involved in Fe(III) reduction by Geobacter sulfurreducens.},
	journal = {J Bacteriol},
	volume = {186},
	year = {2004},
	month = {2004 Jun},
	pages = {4042-5},
	abstract = {A 36-kDa diheme c-type cytochrome abundant in Fe(III)-respiring Geobacter sulfurreducens, designated MacA, was more highly expressed during growth with Fe(III) as the electron acceptor than with fumarate. Although MacA has homology to proteins with in vitro peroxidase activity, deletion of macA had no impact on response to oxidative stress. However, the capacity for Fe(III) reduction was greatly diminished, indicating that MacA, which is predicted to be localized in the periplasm, is a key intermediate in electron transfer to Fe(III).},
	keywords = {Amino Acid Sequence, Bacterial Proteins, Cytochrome c Group, Deltaproteobacteria, Electron Transport, Ferric Compounds, Gene Deletion, Molecular Sequence Data, Oxidation-Reduction},
	issn = {0021-9193},
	doi = {10.1128/JB.186.12.4042-4045.2004},
	author = {Butler, Jessica E and Kaufmann, Franz and Coppi, Maddalena V and N{\'u}{\~n}ez, Cinthia and Lovley, Derek R}
}
