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      Tracking Electron Uptake from a Cathode into Shewanella Cells: Implications for Energy Acquisition from Solid-Substrate Electron Donors

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          ABSTRACT

          While typically investigated as a microorganism capable of extracellular electron transfer to minerals or anodes, Shewanella oneidensis MR-1 can also facilitate electron flow from a cathode to terminal electron acceptors, such as fumarate or oxygen, thereby providing a model system for a process that has significant environmental and technological implications. This work demonstrates that cathodic electrons enter the electron transport chain of S. oneidensis when oxygen is used as the terminal electron acceptor. The effect of electron transport chain inhibitors suggested that a proton gradient is generated during cathode oxidation, consistent with the higher cellular ATP levels measured in cathode-respiring cells than in controls. Cathode oxidation also correlated with an increase in the cellular redox (NADH/FMNH 2) pool determined with a bioluminescence assay, a proton uncoupler, and a mutant of proton-pumping NADH oxidase complex I. This work suggested that the generation of NADH/FMNH 2 under cathodic conditions was linked to reverse electron flow mediated by complex I. A decrease in cathodic electron uptake was observed in various mutant strains, including those lacking the extracellular electron transfer components necessary for anodic-current generation. While no cell growth was observed under these conditions, here we show that cathode oxidation is linked to cellular energy acquisition, resulting in a quantifiable reduction in the cellular decay rate. This work highlights a potential mechanism for cell survival and/or persistence on cathodes, which might extend to environments where growth and division are severely limited.

          IMPORTANCE

          The majority of our knowledge of the physiology of extracellular electron transfer derives from studies of electrons moving to the exterior of the cell. The physiological mechanisms and/or consequences of the reverse processes are largely uncharacterized. This report demonstrates that when coupled to oxygen reduction, electrode oxidation can result in cellular energy acquisition. This respiratory process has potentially important implications for how microorganisms persist in energy-limited environments, such as reduced sediments under changing redox conditions. From an applied perspective, this work has important implications for microbially catalyzed processes on electrodes, particularly with regard to understanding models of cellular conversion of electrons from cathodes to microbially synthesized products.

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          Most cited references57

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          Electricity Production by Geobacter sulfurreducens Attached to Electrodes

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            Feast and famine--microbial life in the deep-sea bed.

            The seabed is a diverse environment that ranges from the desert-like deep seafloor to the rich oases that are present at seeps, vents, and food falls such as whales, wood or kelp. As well as the sedimentation of organic material from above, geological processes transport chemical energy--hydrogen, methane, hydrogen sulphide and iron--to the seafloor from the subsurface below, which provides a significant proportion of the deep-sea energy. At the sites on the seafloor where chemical energy is delivered, rich and diverse microbial communities thrive. However, most subsurface microorganisms live in conditions of extreme energy limitation, with mean generation times of up to thousands of years. Even in the most remote subsurface habitats, temperature rather than energy seems to set the ultimate limit for life, and in the deep biosphere, where energy is most depleted, life might even be based on the cleavage of water by natural radioisotopes. Here, we review microbial biodiversity and function in these intriguing environments.
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              Subseafloor sedimentary life in the South Pacific Gyre.

              The low-productivity South Pacific Gyre (SPG) is Earth's largest oceanic province. Its sediment accumulates extraordinarily slowly (0.1-1 m per million years). This sediment contains a living community that is characterized by very low biomass and very low metabolic activity. At every depth in cored SPG sediment, mean cell abundances are 3 to 4 orders of magnitude lower than at the same depths in all previously explored subseafloor communities. The net rate of respiration by the subseafloor sedimentary community at each SPG site is 1 to 3 orders of magnitude lower than the rates at previously explored sites. Because of the low respiration rates and the thinness of the sediment, interstitial waters are oxic throughout the sediment column in most of this region. Consequently, the sedimentary community of the SPG is predominantly aerobic, unlike previously explored subseafloor communities. Generation of H(2) by radiolysis of water is a significant electron-donor source for this community. The per-cell respiration rates of this community are about 2 orders of magnitude higher (in oxidation/reduction equivalents) than in previously explored anaerobic subseafloor communities. Respiration rates and cell concentrations in subseafloor sediment throughout almost half of the world ocean may approach those in SPG sediment.
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                Author and article information

                Contributors
                Role: Editor
                Journal
                mBio
                MBio
                mbio
                mbio
                mBio
                mBio
                American Society for Microbiology (1752 N St., N.W., Washington, DC )
                2150-7511
                27 February 2018
                Jan-Feb 2018
                : 9
                : 1
                : e02203-17
                Affiliations
                [a ]Department of Earth Sciences, University of Southern California, Los Angeles, California, USA
                [b ]Department of Microbiology, University of Minnesota, St. Paul, Minnesota, USA
                [c ]BioTechnology Institute, University of Minnesota, St. Paul, Minnesota, USA
                [d ]Department of Physics and Astronomy, University of Southern California, Los Angeles, California, USA
                [e ]Global Research Center for Environment and Energy Based on Nanomaterials Science, National Institute for Materials Science (NIMS), Tsukuba, Ibaraki, Japan
                [f ]Department of Biological Sciences, University of Southern California, Los Angeles, California, USA
                [g ]Department of Chemistry, University of Southern California, Los Angeles, California, USA
                University of California, Irvine
                Author notes
                Address correspondence to Annette R. Rowe, annettrr@ 123456usc.edu .

                This work is C-DEBI contribution 417 and NAI-LU contribution 125.

                This article is a direct contribution from a Fellow of the American Academy of Microbiology. Solicited external reviewers: Caroline Ajo-Franklin, Lawrence Berkeley National Laboratory; Buz Barstow, Princeton University.

                Article
                mBio02203-17
                10.1128/mBio.02203-17
                5829830
                29487241
                96e32b82-9e07-49e2-bc27-1caf5c14bca0
                Copyright © 2018 Rowe et al.

                This is an open-access article distributed under the terms of the Creative Commons Attribution 4.0 International license.

                History
                : 18 December 2017
                : 21 December 2017
                Page count
                supplementary-material: 10, Figures: 7, Tables: 1, Equations: 0, References: 69, Pages: 19, Words: 12804
                Funding
                Funded by: NSF;
                Award ID: OCE award 0939564
                Award Recipient :
                Funded by: JSPS;
                Award ID: NNA13AA92A
                Award Recipient : Award Recipient :
                Funded by: DOE;
                Award ID: DE-FG02-13ER16415
                Award Recipient : Award Recipient :
                Funded by: ONR;
                Award ID: N000141310552
                Award Recipient : Award Recipient :
                Funded by: AOR;
                Award ID: GA9550-06-01-0292
                Award Recipient :
                Funded by: NASA;
                Award ID: NNA13AA92A
                Award Recipient : Award Recipient : Award Recipient :
                Categories
                Research Article
                Custom metadata
                January/February 2018

                Life sciences
                electron uptake,energy acquisition,reverse electron transport,shewanella,systems biology

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