Nitrogen Fixation in Methanogens: the Archaeal Perspective
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Methane Production on Rock and Soil Substrates by Methanogens: Implications for Life on Mars
Bioastronomy 2007: Molecules, Microbes, and Extraterrestrial Life ASP Conference Series, Vol. 420, 2009 K. J. Meech, J. V. Keane, M. J. Mumma, J. L. Siefert, and D. J. Werthimer, eds. Methane Production on Rock and Soil Substrates by Methanogens: Implications for Life on Mars H. A. Kozup and T. A. Kral 1West Virginia University, WV 26505 2Arkansas Center for Space and Planetary Sciences, University of Arkansas, Fayetteville 72701 Abstract. In order to understand the methanogens as models for possible life on Mars, and some of the factors likely to be important in determining their abundance and distribution, we have measured their ability to produce methane on a few types of inorganic rock and soil substrates. Since organic ma- terials have not been detected in measurable quantities at the surface of Mars, there is no reason to believe that they would exist in the subsurface. Samples of three methanogens (Methanosarcina barkeri, Methanobacterium formicicum, and Methanothermobacter wolfeii) were placed on four substrates (sand, gravel, basalt, and a Mars soil simulant, JSC Mars-1) and methane production mea- sured. Glass beads were used as a control substrate. As in earlier experiments with JSC Mars-1 soil simulant, a crushed volcanic tephra, methane was pro- duced by all three methanogens when placed on the substrates, sand and gravel. None produced methane on basalt in these experiments, a mineral common in Martian soil. While these substrates do not represent the full range of materials likely to be present on the surface of Mars, the present results suggest that while some surface materials on Mars may not support this type of organism, others might. -
Histone Variants in Archaea and the Evolution of Combinatorial Chromatin Complexity
Histone variants in archaea and the evolution of combinatorial chromatin complexity Kathryn M. Stevensa,b, Jacob B. Swadlinga,b, Antoine Hochera,b, Corinna Bangc,d, Simonetta Gribaldoe, Ruth A. Schmitzc, and Tobias Warneckea,b,1 aMolecular Systems Group, Quantitative Biology Section, Medical Research Council London Institute of Medical Sciences, London W12 0NN, United Kingdom; bInstitute of Clinical Sciences, Faculty of Medicine, Imperial College London, London W12 0NN, United Kingdom; cInstitute for General Microbiology, University of Kiel, 24118 Kiel, Germany; dInstitute of Clinical Molecular Biology, University of Kiel, 24105 Kiel, Germany; and eDepartment of Microbiology, Unit “Evolutionary Biology of the Microbial Cell,” Institut Pasteur, 75015 Paris, France Edited by W. Ford Doolittle, Dalhousie University, Halifax, NS, Canada, and approved October 28, 2020 (received for review April 14, 2020) Nucleosomes in eukaryotes act as platforms for the dynamic inte- additional histone dimers can be taggedontothistetramertoyield gration of epigenetic information. Posttranslational modifications oligomers of increasing length that wrap correspondingly more DNA are reversibly added or removed and core histones exchanged for (3, 6–9). Almost all archaeal histones lack tails and PTMs have yet to paralogous variants, in concert with changing demands on tran- be reported. Many archaea do, however, encode multiple histone scription and genome accessibility. Histones are also common in paralogs (8, 10) that can flexibly homo- and heterodimerize in -
Methanobacterium Paludis Sp. Nov. and a Novel Strain of Methanobacterium Lacus Isolated from Northern Peatlands
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by The University of North Carolina at Greensboro Archived version from NCDOCKS Institutional Repository http://libres.uncg.edu/ir/asu/ Methanobacterium Paludis Sp. Nov. And A Novel Strain Of Methanobacterium Lacus Isolated From Northern Peatlands By: Suzanna L. Brauer, Hinsby Cadillo-Quiroz, Noah Goodson, Joseph B. Yavitt & Stephen H. Zinder Abstract Two mesophilic, hydrogenotrophic methanogens, designated strains SWAN1T and AL-21, were isolated from two contrasting peatlands: a near circumneutral temperate minerotrophic fen in New York State, USA, and an acidic boreal poor fen site in Alaska, USA, respectively. Cells of the two strains were rod-shaped, non- motile, stained Gram-negative and resisted lysis with 0.1 % SDS. Cell size was 0.6 1.5–2.8 mm for strain SWAN1T and 0.45–0.85 1.5–35 mm for strain AL-21. The strains used H2/CO2 but not formate or other substrates for methanogenesis, grew optimally around 32–37 6C, and their growth spanned through a slightly low to neutral pH range (4.7–7.1). Strain AL-21 grew optimally closer to neutrality at pH 6.2, whereas strain SWAN1T showed a lower optimal pH at 5.4–5.7. The two strains were sensitive to NaCl with a maximal tolerance at 160 mM for strain SWAN1T and 50 mM for strain AL-21. Na2S was toxic at very low concentrations (0.01–0.8 mM), resulting in growth inhibition above these values. The DNA G+C content of the genomes was 35.7 mol% for strain SWAN1T and 35.8 mol% for strain AL-21. -
METHANOGENS AS MODELS for LIFE on MARS. R. L. Mickol1, W. H. Waddell2, and T
Eighth International Conference on Mars (2014) 1005.pdf METHANOGENS AS MODELS FOR LIFE ON MARS. R. L. Mickol1, W. H. Waddell2, and T. A. Kral1,3, 1Arkansas Center for Space and Planetary Sciences, 202 Old Museum Building, University of Arkansas, Fayetteville, Arkansas, 72701, USA, [[email protected]], 2Dept. of Health, Human Performance, and Recreation, HPER 308, University of Arkansas, Fayetteville, Arkansas, 72701, USA, 3Dept. of Biological Sciences, SCEN 632, University of Arkansas, Fayetteville, Arkansas, 72701, USA. Introduction: The discovery of methane in the Sciences, University of Arkansas, Fayetteville, Arkan- martian atmosphere [1-4] has fueled the study of meth- sas. All four methanogen species were tested in these anogens as ideal candidates for life on Mars. Methano- experiments. Methanogens were grown in their respec- gens are chemoautotrophs from the domain Archaea. tive anaerobic growth media and placed into the cham- These microorganisms utilize hydrogen as an energy ber with a palladium catalyst box to remove residual source and carbon dioxide as a carbon source to pro- oxygen. The chamber was evacuated to a pre- duce methane. Methanogens can be considered ideal determined pressure and filled with 80:20 H2:CO2 gas. candidates for life on Mars because they are anaerobic, This procedure was repeated three times to ensure re- they do not require organic nutrients and are non- moval of the atmosphere. The chamber was then main- photosynthetic, indicating they could exist in sub- tained at the desired pressure (133-143 mbar, 67-72 surface environments. mbar, 33-38 mbar, 6-10 mbar, 7-20 mbar) for the dura- Our lab has studied methanogens as models for life tion of the experiments. -
Tackling the Methanopyrus Kandleri Paradox Céline Brochier*, Patrick Forterre† and Simonetta Gribaldo†
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by PubMed Central Open Access Research2004BrochieretVolume al. 5, Issue 3, Article R17 Archaeal phylogeny based on proteins of the transcription and comment translation machineries: tackling the Methanopyrus kandleri paradox Céline Brochier*, Patrick Forterre† and Simonetta Gribaldo† Addresses: *Equipe Phylogénomique, Université Aix-Marseille I, Centre Saint-Charles, 13331 Marseille Cedex 3, France. †Institut de Génétique et Microbiologie, CNRS UMR 8621, Université Paris-Sud, 91405 Orsay, France. reviews Correspondence: Céline Brochier. E-mail: [email protected] Published: 26 February 2004 Received: 14 November 2003 Revised: 5 January 2004 Genome Biology 2004, 5:R17 Accepted: 21 January 2004 The electronic version of this article is the complete one and can be found online at http://genomebiology.com/2004/5/3/R17 reports © 2004 Brochier et al.; licensee BioMed Central Ltd. This is an Open Access article: verbatim copying and redistribution of this article are permitted in all media for any purpose, provided this notice is preserved along with the article's original URL. ArchaealPhylogeneticsequencedusingrespectively). two phylogeny concatenated genomes, analysis based it of is datasetsthe now on Archaea proteinspossible consisting has ofto been thetest of transcription alternative mainly14 proteins established approach involv and translationed byes in 16S bytranscription rRNAusing machineries: largesequence andsequence 53comparison.tackling ribosomal datasets. the Methanopyrus Withproteins We theanalyzed accumulation(3,275 archaealkandleri and 6,377 of phyparadox comp positions,logenyletely Abstract deposited research Background: Phylogenetic analysis of the Archaea has been mainly established by 16S rRNA sequence comparison. With the accumulation of completely sequenced genomes, it is now possible to test alternative approaches by using large sequence datasets. -
WARREN LYNWOOD GARDNER Expression Vectors for the Methane-Producing Archaeon Methanococcus Maripaludis (Under the Direction of WILLIAM B
WARREN LYNWOOD GARDNER Expression vectors for the methane-producing archaeon Methanococcus maripaludis (Under the Direction of WILLIAM B. WHITMAN) Methanogens are strict anaerobes that use one and two carbon compounds for methanogenesis. They contain many unusual cofactors and enzymes, and many of their proteins are oxygen-sensitive and are present at low concentrations within the cells. An expression system that overexpresses homologous and heterologous proteins would facilitate research on the unique oxygen-sensitive enzymes in these organisms. However, traditional expression systems may lack the cofactors and maturation enzymes necessary for the expression of the active holoenzymes. Therefore, a major goal of this work was to develop expression vectors. To develop a shuttle vector, a series of integrative vectors were first constructed. The integrative vectors were based on the pUC-derivative pMEB.2. pMEB.2 provided the puromycin resistance marker for methanococci, an Escherichia coli origin of replication, and an ampicillin resistance marker for E. coli. A multiple cloning site and the Methanococcus voltae histone promoter (PhmvA) were added to form the integrative, expression vector pWLG14. To demonstrate the utility of PhmvA, pWLG14 was used to overexpress the genomic copy of the Methanococcus maripaludis acetohydroxyacid synthase. To form an expression shuttle vector suitable for heterologous genes, pWLG14 and the cryptic plasmid pURB500 from M. maripaludis strain were ligated together to form pWLG30. pWLG30 was the first expression shuttle vector for the methanogens. To demonstrate the utility of pWLG30, the E. coli b-galactosidase gene was cloned into pWLG30 to yield pWLG30+lacZ. Upon transformation into M. maripaludis, the recombinant strain expressed b-galactosidase to the level of 1% of the cellular protein. -
Extremophiles
Extremophiles These microbes thrive under conditions that would kill other creatures. The molecules that enable extremophiles to prosper are becoming useful to industry by Michael T. Madigan and Barry L. Marrs DEEP-SEA VENT HEAT-LOVING MICROBES (THERMOPHILES AND HYPERTHERMOPHILES) SEA ICE COLD-LOVING MICROBES (PSYCHROPHILES) Methanopyrus kandleri Polaromonas vacuolata thereby increasing efficiency and reduc- magine diving into a refreshingly ing costs. They can also form the basis of cool swimming pool. Now, think entirely new enzyme-based processes. I instead of plowing into water that tially serve in an array of applications. Perhaps 20 research groups in the U.S., is boiling or near freezing. Or consider Of particular interest are the enzymes Japan, Germany and elsewhere are now jumping into vinegar, household am- (biological catalysts) that help extremo- actively searching for extremophiles and monia or concentrated brine. The leap philes to function in brutal circumstanc- their enzymes. Although only a few ex- would be disastrous for a person. Yet es. Like synthetic catalysts, enzymes, tremozymes have made their way into many microorganisms make their home which are proteins, speed up chemical use thus far, others are sure to follow. As in such forbidding environments. These reactions without being altered them- is true of standard enzymes, transform- microbes are called extremophiles be- selves. Last year the biomedical field and ing a newly isolated extremozyme into cause they thrive under conditions that, other industries worldwide spent more a viable product for industry can take from the human vantage, are clearly ex- than $2.5 billion on enzymes for appli- several years. -
Microbial Processes in Oil Fields: Culprits, Problems, and Opportunities
Provided for non-commercial research and educational use only. Not for reproduction, distribution or commercial use. This chapter was originally published in the book Advances in Applied Microbiology, Vol 66, published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for non-commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who know you, and providing a copy to your institution’s administrator. All other uses, reproduction and distribution, including without limitation commercial reprints, selling or licensing copies or access, or posting on open internet sites, your personal or institution’s website or repository, are prohibited. For exceptions, permission may be sought for such use through Elsevier's permissions site at: http://www.elsevier.com/locate/permissionusematerial From: Noha Youssef, Mostafa S. Elshahed, and Michael J. McInerney, Microbial Processes in Oil Fields: Culprits, Problems, and Opportunities. In Allen I. Laskin, Sima Sariaslani, and Geoffrey M. Gadd, editors: Advances in Applied Microbiology, Vol 66, Burlington: Academic Press, 2009, pp. 141-251. ISBN: 978-0-12-374788-4 © Copyright 2009 Elsevier Inc. Academic Press. Author's personal copy CHAPTER 6 Microbial Processes in Oil Fields: Culprits, Problems, and Opportunities Noha Youssef, Mostafa S. Elshahed, and Michael J. McInerney1 Contents I. Introduction 142 II. Factors Governing Oil Recovery 144 III. Microbial Ecology of Oil Reservoirs 147 A. Origins of microorganisms recovered from oil reservoirs 147 B. Microorganisms isolated from oil reservoirs 148 C. Culture-independent analysis of microbial communities in oil reservoirs 155 IV. -
Extremophiles — Link Between Earth and Astrobiology
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Directory of Open Access Journals Zbornik Matice srpske za prirodne nauke / Proc. Nat. Sci, Matica Srpska Novi Sad, ¥ 114, 5—16, 2008 UDC 133.52:57 Dejan B. Stojanoviã1 , Oliver O. Fojkar2 , Aleksandra V. Drobac-Åik1 , Kristina O. Åajko3 , Tamara I. Duliã1 ,ZoricaB.Sviråev1 1 Faculty of Sciences, Department of Biology and Ecology, Trg Dositeja Obradoviãa 2, 21000 Novi Sad, Serbia 2 Institute for nature conservation of Serbia, Radniåka 20A, 21000 Novi Sad, Serbia 3 Faculty of Sciences, Department of Physics, Trg Dositeja Obradoviãa 4, 21000 Novi Sad, Serbia EXTREMOPHILES — LINK BETWEEN EARTH AND ASTROBIOLOGY ABSTRACT: Astrobiology studies the origin, evolution, distribution and future of life in the universe. The most promising worlds in Solar system, beyond Earth, which may har- bor life are Mars and Jovian moon Europa. Extremophiles are organisms that thrive on the edge of temperature, hypersalinity, pH extremes, pressure, dryness and so on. In this paper, some extremophile cyanobacteria have been discussed as possible life forms in a scale of astrobiology. Samples were taken from solenetz and solonchak types of soil from the Voj- vodina region. The main idea in this paper lies in the fact that high percentage of salt found in solonchak and solonetz gives the possibility of comparison these types of soil with “soil" on Mars, which is also rich in salt. KEYWORDS: Astrobiology, extremophiles, cyanobacteria, halophiles 1. INTRODUCTION 1.1. About astrobiology Astrobiology studies the origin, evolution, distribution and future of life in the universe. -
Life in Extreme Environments
insight review articles Life in extreme environments Lynn J. Rothschild & Rocco L. Mancinelli NASA Ames Research Center, Moffett Field, California 94035-1000, USA (e-mail: [email protected]; [email protected]) Each recent report of liquid water existing elsewhere in the Solar System has reverberated through the international press and excited the imagination of humankind. Why? Because in the past few decades we have come to realize that where there is liquid water on Earth, virtually no matter what the physical conditions, there is life. What we previously thought of as insurmountable physical and chemical barriers to life, we now see as yet another niche harbouring ‘extremophiles’. This realization, coupled with new data on the survival of microbes in the space environment and modelling of the potential for transfer of life between celestial bodies, suggests that life could be more common than previously thought. Here we examine critically what it means to be an extremophile, and the implications of this for evolution, biotechnology and especially the search for life in the Universe. ormal is passé; extreme is chic. While thriving in biological extremes (for example, nutritional Aristotle cautioned “everything in extremes, and extremes of population density, parasites, moderation”, the Romans, known for their prey, and so on). excesses, coined the word ‘extremus’, the ‘Extremophile’ conjures up images of prokaryotes, yet the superlative of exter (‘being on the outside’). taxonomic range spans all three domains. Although all NBy the fifteenth century ‘extreme’ had arrived, via Middle hyperthermophiles are members of the Archaea and French, to English. At the dawning of the twenty-first Bacteria, eukaryotes are common among the psychrophiles, century we know that the Solar System, and even Earth, acidophiles, alkaliphiles, piezophiles, xerophiles and contain environmental extremes unimaginable to the halophiles (which respectively thrive at low temperatures, low ‘ancients’ of the nineteenth century. -
Large Carbon Isotope Variability During Methanogenesis Under Alkaline Conditions Hannah M
Large carbon isotope variability during methanogenesis under alkaline conditions Hannah M. Millera Nabil Chaudhrya Mark E. Conradb Markus Billb Sebastian H. Kopfa Alexis S. Templetona Abstract 13 High carbon isotope values (δ CCH4 > −40‰) have widely been used as evidence that methane in alkaline rock-hosted fluids was formed abiotically, particularly in serpentinizing systems. However, isotope fractionation during microbial methanogenesis is relatively understudied at high pH. We isolated a hydrogenotrophic Methanobacterium sp. from hyperalkaline subsurface fluids in the Samail ophiolite to assess how carbon and hydrogen isotope values of CH4 varied depending upon pH and carbonate mineral source (NaHCO3 or CaCO3). The hydrogen isotope fractionation αH20/CH4 (1.46–1.66) did not vary across pH. In contrast, the expressed carbon isotope fractionation, αCO2/CH4, ranged from 1.028 to 1.089. Carbon isotope fractionation increased with pH, reaching a maximum 13C depletion of −85‰. However, the 13C depletion significantly diminished at pH ≥ 9 for 13 CaCO3-amended experiments, generating δ CCH4 as high as −28‰. To 13 evaluate the large variability in δ CCH4, we developed a steady-state model to assess how the rates of carbonate dissolution, cellular uptake of CO2 and irreversible CH4 production can affect the net isotope fractionation during 13 methanogenesis. Methanobacterium sp. can produce highly depleted δ CCH4 in simulated alkaline serpentinizing fluids when dissolved inorganic carbon levels are high and methanogenesis rates are slow. However, small carbon isotope fractionation occurs when rates of carbonate dissolution are slower 13 than cellular uptake, leading to relatively high δ CCH4 values (>∼−35‰) that are traditionally interpreted to be purely “abiotic”. -
Protein Complexing in a Methanogen Suggests Electron Bifurcation and Electron Delivery from Formate to Heterodisulfide Reductase
Protein complexing in a methanogen suggests electron bifurcation and electron delivery from formate to heterodisulfide reductase Kyle C. Costaa,b, Phoebe M. Wonga, Tiansong Wanga,c, Thomas J. Liea, Jeremy A. Dodswortha,b,1, Ingrid Swansona, June A. Burna, Murray Hackettc, and John A. Leigha,b,2 aDepartment of Microbiology, bNational Science Foundation Integrative Graduate Education Research Traineeship Program in Astrobiology, and cDepartment of Chemical Engineering, University of Washington, Seattle, WA 98195 Edited by William Metcalf, University of Illinois, Urbana, IL, and accepted by the Editorial Board May 6, 2010 (received for review March 19, 2010) In methanogenic Archaea, the final step of methanogenesis gen- Most methanogens can use H2 as the electron donor, and many fi erates methane and a heterodisul de of coenzyme M and co- can also use formate. Reduced coenzyme F420 (F420H2)isarequired fi enzyme B (CoM-S-S-CoB). Reduction of this heterodisul de by intermediate, and can be generated from H2 by F420-reducing hy- fi heterodisul de reductase to regenerate HS-CoM and HS-CoB is an drogenase (Fru) or by a cycle involving the enzymes H2-dependent Nat Rev Micro- exergonic process. Thauer et al. [Thauer, et al. 2008 methylene-H4MPT dehydrogenase and F420-dependent methylene- biol – 6:579 591] recently suggested that in hydrogenotrophic metha- H4MPT dehydrogenase (2). When formate is the electron donor, fi nogens the energy of heterodisul de reduction powers the most it is oxidized to CO2 by a formate dehydrogenase (Fdh) that endergonic reaction in the pathway, catalyzed by the formylmetha- yields F420H2. nofuran dehydrogenase, via flavin-based electron bifurcation.