Candidatus Galacturonibacter Soehngenii
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Acetogen Communities in the Gut of Herbivores and Their Potential Role in Syngas Fermentation
fermentation Article Acetogen Communities in the Gut of Herbivores and Their Potential Role in Syngas Fermentation Chunlei Yang Institute of Dairy Science, MoE Key Laboratory of Molecular Animal Nutrition, College of Animal Sciences, Zhejiang University, Hangzhou 310058, China; [email protected] Received: 2 May 2018; Accepted: 4 June 2018; Published: 7 June 2018 Abstract: To better understand the effects of host selection on gut acetogens and their potential role in syngas fermentation, the composition and hydrogenotrophic features of acetogen populations in cow and sheep rumens, rabbit ceca, and horse feces were studied. The acetogens detected in horses and rabbits were more phylogenetically diverse than those in cows and sheep, suggesting that the host species plays an important role in shaping gut acetogen populations. Acetogen enrichments from these animals presented good capacities to use hydrogen, with acetate as the major end product. Minor propionate, butyrate, and isovalerate were also produced. During 48 h of incubation, acetogen enrichments from horse consumed 4.75 moles of H2 to every 1 mole of acetate—significantly lower than rabbits, cows, and sheep (5.17, 5.53, and 5.23 moles, respectively) (p < 0.05)—and produced significantly more butyrate (p < 0.05). Enrichments from cows and sheep produced significantly higher amounts of propionate when compared to rabbits or horses (p < 0.05); enrichments from sheep produced the highest amounts of isovalerate (p < 0.05). These short chain fatty acids are important precursors for the synthesis of biofuel products, suggesting that gut contents of herbivores may be promising sources for harvesting functional acetogens for biofuel production. -
Rewiring Hydrogenase-Dependent Redox Circuits in Cyanobacteria
Rewiring hydrogenase-dependent redox circuits in cyanobacteria Daniel C. Ducata,b, Gairik Sachdevac, and Pamela A. Silvera,b,1 aDepartment of Systems Biology, Harvard Medical School, Boston, MA 02115; bWyss Institute for Biologically Inspired Engineering, Harvard University, Boston, MA 02115; and cSchool of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138 Edited by David Baker, University of Washington, Seattle, WA, and approved January 26, 2011 (received for review October 26, 2010) þ þ − ↔ Hydrogenases catalyze the reversible reaction 2H 2e H2 The hydrogen production capacity of a variety of cyanobacter- with an equilibrium constant that is dependent on the reducing ial and algal species has been surveyed (8–10), and the highest potential of electrons carried by their redox partner. To examine rates of hydrogen evolution are typically observed in algae the possibility of increasing the photobiological production of and some nitrogen-fixing cyanobacteria. Algal species frequently hydrogen within cyanobacterial cultures, we expressed the [FeFe] possess [FeFe]-hydrogenases that accept low-potential electrons hydrogenase, HydA, from Clostridium acetobutylicum in the non- from ferredoxins that are, in turn, linked to the light reactions of nitrogen-fixing cyanobacterium Synechococcus elongatus sp. 7942. photosynthesis (11). Nitrogen-fixing microorganisms, including We demonstrate that the heterologously expressed hydrogenase is many cyanobacteria (12), produce hydrogen gas as a byproduct functional in vitro and in -
The Carbon-Isotope Record of the Sub-Seafloor Biosphere
geosciences Review The Carbon-Isotope Record of the Sub-Seafloor Biosphere Patrick Meister 1,* and Carolina Reyes 2 1 Department of Geodynamics and Sedimentology, University of Vienna, Althanstr. 14, 1090 Vienna, Austria 2 Department of Environmental Geosciences, University of Vienna, Althanstr. 14, 1090 Vienna, Austria; [email protected] * Correspondence: [email protected] Received: 13 November 2019; Accepted: 29 November 2019; Published: 5 December 2019 Abstract: Sub-seafloor microbial environments exhibit large carbon-isotope fractionation effects as a result of microbial enzymatic reactions. Isotopically light, dissolved inorganic carbon (DIC) derived from organic carbon is commonly released into the interstitial water due to microbial dissimilatory processes prevailing in the sub-surface biosphere. Much stronger carbon-isotope fractionation occurs, however, during methanogenesis, whereby methane is depleted in 13C and, by mass balance, DIC is enriched in 13C, such that isotopic distributions are predominantly influenced by microbial metabolisms involving methane. Methane metabolisms are essentially mediated through a single enzymatic pathway in both Archaea and Bacteria, the Wood–Ljungdahl (WL) pathway, but it remains unclear where in the pathway carbon-isotope fractionation occurs. While it is generally assumed that fractionation arises from kinetic effects of enzymatic reactions, it has recently been suggested that partial carbon-isotope equilibration occurs within the pathway of anaerobic methane oxidation. Equilibrium fractionation might also occur during methanogenesis, as the isotopic difference between DIC and methane is commonly on the order of 75%, which is near the thermodynamic equilibrium. The isotopic signature in DIC and methane highly varies in marine porewaters, reflecting the distribution of different microbial metabolisms contributing to DIC. -
The Genetic Basis of Energy Conservation in the Sulfate-Reducing Bacterium Desulfovibrio Alaskensis G20
Lawrence Berkeley National Laboratory Recent Work Title The genetic basis of energy conservation in the sulfate-reducing bacterium Desulfovibrio alaskensis G20. Permalink https://escholarship.org/uc/item/7b44z00f Journal Frontiers in microbiology, 5(OCT) ISSN 1664-302X Authors Price, Morgan N Ray, Jayashree Wetmore, Kelly M et al. Publication Date 2014 DOI 10.3389/fmicb.2014.00577 Peer reviewed eScholarship.org Powered by the California Digital Library University of California ORIGINAL RESEARCH ARTICLE published: 31 October 2014 doi: 10.3389/fmicb.2014.00577 The genetic basis of energy conservation in the sulfate-reducing bacterium Desulfovibrio alaskensis G20 Morgan N. Price 1*, Jayashree Ray 1, Kelly M. Wetmore 1, Jennifer V. Kuehl 1, Stefan Bauer 2, Adam M. Deutschbauer 1 and Adam P.Arkin 1,2,3* 1 Physical Biosciences Division, Lawrence Berkeley Lab, Berkeley, CA, USA 2 Energy Biosciences Institute, University of California, Berkeley, CA, USA 3 Department of Bioengineering, University of California, Berkeley, CA, USA Edited by: Sulfate-reducing bacteria play major roles in the global carbon and sulfur cycles, but Thomas E. Hanson, University of it remains unclear how reducing sulfate yields energy. To determine the genetic basis Delaware, USA of energy conservation, we measured the fitness of thousands of pooled mutants of Reviewed by: Desulfovibrio alaskensis G20 during growth in 12 different combinations of electron donors Caroline M. Plugge, Wageningen University, Netherlands and acceptors. We show that ion pumping by the ferredoxin:NADH oxidoreductase Rnf is Ulrike Kappler, University of required whenever substrate-level phosphorylation is not possible. The uncharacterized Queensland, Australia complex Hdr/flox-1 (Dde_1207:13) is sometimes important alongside Rnf and may *Correspondence: perform an electron bifurcation to generate more reduced ferredoxin from NADH Morgan N. -
Acetogenesis in the Energy-Starved Deep Biosphere – a Paradox?
HYPOTHESIS AND THEORY ARTICLE published: 13 January 2012 doi: 10.3389/fmicb.2011.00284 Acetogenesis in the energy-starved deep biosphere – a paradox? Mark Alexander Lever* Department of Bioscience, Center for Geomicrobiology, Aarhus University, Aarhus, Denmark Edited by: Under anoxic conditions in sediments, acetogens are often thought to be outcompeted Andreas Teske, University of North by microorganisms performing energetically more favorable metabolic pathways, such as Carolina at Chapel Hill, USA sulfate reduction or methanogenesis. Recent evidence from deep subseafloor sediments Reviewed by: Matthew Schrenk, East Carolina suggesting acetogenesis in the presence of sulfate reduction and methanogenesis has University, USA called this notion into question, however. Here I argue that acetogens can successfully Aharon Oren, The Hebrew University coexist with sulfate reducers and methanogens for multiple reasons. These include (1) of Jerusalem, Israel substantial energy yields from most acetogenesis reactions across the wide range of *Correspondence: conditions encountered in the subseafloor, (2) wide substrate spectra that enable niche Mark Alexander Lever , Department of Bioscience, Center for differentiation by use of different substrates and/or pooling of energy from a broad range Geomicrobiology, Aarhus University, of energy substrates, (3) reduced energetic cost of biosynthesis among acetogens due Ny Munkegade 114, bng 1535-1540, to use of the reductive acetyl CoA pathway for both energy production and biosynthesis DK-8000 Århus C, Denmark. coupled with the ability to use many organic precursors to produce the key intermediate e-mail: [email protected] acetyl CoA. This leads to the general conclusion that, beside Gibbs free energy yields, variables such as metabolic strategy and energetic cost of biosynthesis need to be taken into account to understand microbial survival in the energy-depleted deep biosphere. -
Biosolids Technology Fact Sheet, Multi-Stage Anaerobic Digestion
Biosolids Technology Fact Sheet Multi-Stage Anaerobic Digestion DESCRIPTION the organisms that perform the methane forma- tion step (the methanogenic bacteria). The Anaerobic digestion is a naturally occurring bio- acidogenic bacteria are also less sensitive than logical process in which large numbers of the methanogenic bacteria to changes in organic anaerobic bacteria convert organic matter into strength and composition in the incoming feed methane and carbon dioxide (a mixture called stream. Therefore, although many wastewater biogas) in the absence of air. It is a widely used treatment plants have traditionally performed biological process for treating wastewater solids. anaerobic digestion processes in a single tank (in This process stabilizes the organic matter in a process called single-stage anaerobic digestion) wastewater solids, reduces pathogens and odors, at a constant temperature, some facilities have and reduces the total solids/sludge quantity by separated the process into multiple stages, by converting part of the volatile solids (VS) frac- physically separating the stages or by controlling tion to biogas. Anaerobic digestion results in a the process to separate the stages in time, or product that contains stabilized solids, as well as both. This approach allows the facilities to opti- some available forms of nutrients such as am- mize the various stages of the anaerobic monia-nitrogen. digestion process to meet their needs. The process of anaerobic digestion can be divided The standard multi-stage anaerobic digestion into three separate steps, each of which is per- system is a two-stage acid/gas (AG)-phased formed by a different group of microorganisms: system, in which the acid-forming steps (hy- • Hydrolysis, during which the proteins, cellu- drolysis and volatile acid fermentation) are lose, lipids, and other complex organics are physically separated from the gas-forming step broken down into smaller molecules and be- (methane formation) by being conducted in sepa- come soluble by utilizing water to split the rate digestion tanks. -
Microbial Bioenergy: Hydrogen Production Microbial Bioenergy: Hydrogen Production
Advances in Photosynthesis and Respiration 38 Including Bioenergy and Related Processes Davide Zannoni Roberto De Philippis Editors Microbial BioEnergy: Hydrogen Production Microbial BioEnergy: Hydrogen Production Different Ways for BioHydrogen Production The four possible ways for producing H2 , by exploiting microbial activities, are shown here. Biophotolysis : H2 production by microalgae (through H 2 -ase) or Cyanobacteria (through H2 -ase or N 2 -ase) by using low potential reductants derived from either water or stored sugars via the photosynthetic machinery. Photofermentation : H2 production by anoxygenic photosynthetic bacteria (through N2 -ase) by using reductants obtained from the oxidation of organic compounds as well as solar energy used through photosynthesis. Dark fermentation : H2 production by mesophilic or thermophilic chemoheterotrophic bacteria (through H2 -ase) by using reductants and energy obtained from the oxidation of organic compounds. Microbial Electrolysis Cell (MEC): H2 production by means of cathodic proton reduction with applied potential exploiting the low redox potential produced by exoelectrogenic bacteria at the anode. This fi gure is adapted from Fig. 1.3 in Chap. 1 of this book. Advances in Photosynthesis and Respiration Including Bioenergy and Related Processes VOLUME 38 Series Editors: GOVINDJEE * ( University of Illinois at Urbana- Champaign , IL , U.S.A ) THOMAS D. SHARKEY ( Michigan State University , East Lansing , MI , U.S.A ) * Founding Series Editor Advisory Editors: Elizabeth AINSWORTH, United States Department of Agriculture , Urbana , IL , U.S.A. Basanti BISWAL, Sambalpur University , Jyoti Vihar , Odisha , India Robert E. BLANKENSHIP, Washington University , St Louis , MO , U.S.A. Ralph BOCK, Max Planck Institute of Molecular Plant Physiology , Postdam - Golm , Germany Julian J. -
Methanogens: Pushing the Boundaries of Biology
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Biochemistry -- Faculty Publications Biochemistry, Department of 12-14-2018 Methanogens: pushing the boundaries of biology Nicole R. Buan Follow this and additional works at: https://digitalcommons.unl.edu/biochemfacpub Part of the Biochemistry Commons, Biotechnology Commons, and the Other Biochemistry, Biophysics, and Structural Biology Commons This Article is brought to you for free and open access by the Biochemistry, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Biochemistry -- Faculty Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Emerging Topics in Life Sciences (2018) 2 629–646 https://doi.org/10.1042/ETLS20180031 Review Article Methanogens: pushing the boundaries of biology Nicole R. Buan Department of Biochemistry, University of Nebraska-Lincoln, 1901 Vine St., Lincoln, NE 68588-0664, U.S.A. Correspondence: Nicole R. Buan ([email protected]) Downloaded from https://portlandpress.com/emergtoplifesci/article-pdf/2/4/629/484198/etls-2018-0031c.pdf by University of Nebraska Libraries user on 11 February 2020 Methanogens are anaerobic archaea that grow by producing methane gas. These microbes and their exotic metabolism have inspired decades of microbial physiology research that continues to push the boundary of what we know about how microbes conserve energy to grow. The study of methanogens has helped to elucidate the thermodynamic and bioener- getics basis of life, contributed our understanding of evolution and biodiversity, and has garnered an appreciation for the societal utility of studying trophic interactions between environmental microbes, as methanogens are important in microbial conversion of biogenic carbon into methane, a high-energy fuel. -
Acetogenesis and the Wood–Ljungdahl Pathway of CO2 Fixation
Biochimica et Biophysica Acta 1784 (2008) 1873–1898 Contents lists available at ScienceDirect Biochimica et Biophysica Acta journal homepage: www.elsevier.com/locate/bbapap Review Acetogenesis and the Wood–Ljungdahl pathway of CO2 fixation Stephen W. Ragsdale ⁎, Elizabeth Pierce Department of Biological Chemistry, MSRB III, 5301, 1150 W. Medical Center Drive, University of Michigan, Ann Arbor, MI 48109-0606, USA article info abstract Article history: Conceptually, the simplest way to synthesize an organic molecule is to construct it one carbon at a time. The Received 2 July 2008 Wood–Ljungdahl pathway of CO2 fixation involves this type of stepwise process. The biochemical events that Received in revised form 12 August 2008 underlie the condensation of two one-carbon units to form the two-carbon compound, acetate, have Accepted 13 August 2008 intrigued chemists, biochemists, and microbiologists for many decades. We begin this review with a Available online 27 August 2008 description of the biology of acetogenesis. Then, we provide a short history of the important discoveries that fi Keywords: have led to the identi cation of the key components and steps of this usual mechanism of CO and CO2 fi fl Acetogenesis xation. In this historical perspective, we have included re ections that hopefully will sketch the landscape Nickel of the controversies, hypotheses, and opinions that led to the key experiments and discoveries. We then Iron–sulfur describe the properties of the genes and enzymes involved in the pathway and conclude with a section Cobalamin describing some major questions that remain unanswered. Methanogenesis © 2008 Elsevier B.V. All rights reserved. -
Aquatic Microbial Ecology 79:177
Vol. 79: 177–195, 2017 AQUATIC MICROBIAL ECOLOGY Published online June 12 https://doi.org/10.3354/ame01826 Aquat Microb Ecol Contribution to AME Special 6 ‘SAME 14: progress and perspectives in aquatic microbial ecology’ OPENPEN ACCESSCCESS REVIEW Microbial community assembly in marine sediments Caitlin Petro**, Piotr Starnawski**, Andreas Schramm*, Kasper U. Kjeldsen Section for Microbiology and Center for Geomicrobiology, Department of Bioscience, Aarhus University, 8000 Aarhus C, Denmark ABSTRACT: Marine sediments are densely populated by diverse communities of archaea and bacteria, with intact cells detected kilometers below the seafloor. Analyses of microbial diversity in these unique environments have identified several dominant taxa that comprise a significant portion of the community in geographically and environmentally disparate locations. While the distributions of these populations are well documented, there is significantly less information describing the means by which such specialized communities assemble within the sediment col- umn. Here, we review known patterns of subsurface microbial community composition and per- form a meta-analysis of publicly available 16S rRNA gene datasets collected from 9 locations at depths from 1 cm to >2 km below the surface. All data are discussed in relation to the 4 major pro- cesses of microbial community assembly: diversification, dispersal, selection, and drift. Microbial diversity in the subsurface decreases with depth on a global scale. The transition from the seafloor to the deep subsurface biosphere is marked by a filtering of populations from the surface that leaves only a subset of taxa to populate the deeper sediment zones, indicating that selection is a main mechanism of community assembly. The physiological underpinnings for the success of these persisting taxa are largely unknown, as the majority of them lack cultured representatives. -
Acetogenesis from H2 Plus CO2 and Nitrogen Fixation by an Endosymbiotic Spirochete of a Termite-Gut Cellulolytic Protist
Acetogenesis from H2 plus CO2 and nitrogen fixation by an endosymbiotic spirochete of a termite-gut cellulolytic protist Moriya Ohkumaa,b,1, Satoko Nodaa,c, Satoshi Hattorid, Toshiya Iidaa, Masahiro Yukib, David Starnsa,e, Jun-ichi Inouea, Alistair C. Darbye, and Yuichi Hongoha,f aJapan Collection of Microorganisms/Microbe Division, RIKEN BioResource Center, and bBiomass Research Platform Team, RIKEN Biomass Engineering Program Cooperation Division, RIKEN Center for Sustainable Resource Science, Ibaraki 305-0074, Japan; cInterdisciplinary Graduate School of Medicine and Engineering, University of Yamanashi, Yamanashi 400-8511, Japan; dDepartment of Food, Life, and Environmental Sciences, Yamagata University, Yamagata 997-8555, Japan; eInstitute of Integrative Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom; and fDepartment of Biological Sciences, Tokyo Institute of Technology, Tokyo 152-8550, Japan Edited by Patrick J. Keeling, University of British Columbia, Vancouver, Canada, and accepted by the Editorial Board April 16, 2015 (received for review December 15, 2014) Symbiotic associations of cellulolytic eukaryotic protists and di- cellulose digestion. The protists phagocytose ingested wood verse bacteria are common in the gut microbial communities of particles and almost completely decompose and ferment the termites. Besides cellulose degradation by the gut protists, re- cellulose to produce acetate, H2, and CO2 (6, 8). The host ter- ductive acetogenesis from H2 plus CO2 and nitrogen fixation by mite uses the produced acetate as a major carbon and energy ’ gut bacteria play crucial roles in the host termites nutrition by source. The produced H2 is a key metabolic intermediate that contributing to the energy demand of termites and supplying nitro- fuels many bacteria in the gut (9). -
Opportunistic Interactions on Fe0 Between Methanogens and Acetogens 2 from a Climate Lake
bioRxiv preprint doi: https://doi.org/10.1101/556704; this version posted December 6, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Opportunistic interactions on Fe0 between methanogens and acetogens 2 from a climate lake 3 Paola Andrea Palacios 1 and Amelia-Elena Rotaru1* 4 1Nordcee, Department of Biology, University of Southern Denmark, Odense, Denmark 5 * Correspondence: 6 Amelia-Elena Rotaru 7 [email protected] 8 Keywords: microbial influenced corrosion, acetogens, methanogens, interspecies interactions, 9 iron corrosion, Clostridium, Methanosarcinales, Methanothermobacter. 10 Abstract 11 Microbial-induced corrosion has been extensively studied in pure cultures. However, Fe0 corrosion 12 by complex environmental communities, and especially the interplay between microbial 13 physiological groups, is still poorly understood. In this study, we combined experimental physiology 14 and metagenomics to explore Fe0-dependent microbial interactions between physiological groups 15 enriched from anoxic climate lake sediments. Then, we investigated how each physiological group 16 interacts with Fe0. We offer evidence for a new interspecies interaction during Fe0 corrosion. We 17 showed that acetogens enhanced methanogenesis but were negatively impacted by methanogens 18 (opportunistic microbial interaction). Methanogens were positively impacted by acetogens. In the 19 metagenome of the corrosive community, the acetogens were mostly represented by Clostridium and 20 Eubacterium, the methanogens by 21 Methanosarcinales, Methanothermobacter and Methanobrevibacter. Within the corrosive 22 community, acetogens and methanogens produced acetate and methane concurrently, however at 0 23 rates that cannot be explained by abiotic H2-buildup at the Fe surface.