Methanosarcina Barkeri
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A Late Methanogen Origin for Molybdenum-Dependent Nitrogenase E
Geobiology (2011), 9, 221–232 DOI: 10.1111/j.1472-4669.2011.00278.x A late methanogen origin for molybdenum-dependent nitrogenase E. S. BOYD,1 A. D. ANBAR,2 S. MILLER,3 T. L. HAMILTON,1 M. LAVIN4 ANDJ.W.PETERS1 1Department of Chemistry and Biochemistry and the Astrobiology Biogeocatalysis Research Center, Montana State University, Bozeman, MT, USA 2School of Earth and Space Exploration and Department of Chemistry and Biochemistry, Arizona State University, Tempe, AZ, USA 3Department of Biological Sciences, University of Montana, Missoula, MT, USA 4Department of Plant Sciences, Montana State University, Bozeman, MT, USA ABSTRACT Mounting evidence indicates the presence of a near complete biological nitrogen cycle in redox-stratified oceans during the late Archean to early Proterozoic (c. 2.5–2.0 Ga). It has been suggested that the iron (Fe)- or vana- dium (V)-dependent nitrogenase rather than molybdenum (Mo)-dependent form was responsible for dinitrogen fixation during this time because oceans were depleted in Mo and rich in Fe. We evaluated this hypothesis by examining the phylogenetic relationships of proteins that are required for the biosynthesis of the active site cofactor of Mo-nitrogenase in relation to structural proteins required for Fe-, V- and Mo-nitrogenase. The results are highly suggestive that among extant nitrogen-fixing organisms for which genomic information exists, Mo-nitrogenase is unlikely to have been associated with the Last Universal Common Ancestor. Rather, the origin of Mo-nitrogenase can be traced to an ancestor of the anaerobic and hydrogenotrophic methanogens with acquisition in the bacterial domain via lateral gene transfer involving an anaerobic member of the Firmicutes.A comparison of substitution rates estimated for proteins required for the biosynthesis of the nitrogenase active site cofactor and for a set of paralogous proteins required for the biosynthesis of bacteriochlorophyll suggests that Nif emerged from a nitrogenase-like ancestor approximately 1.5–2.2 Ga. -
Direct Charging of Trnacua with Pyrrolysine in Vitro and in Vivo
letters to nature .............................................................. gene product (see Supplementary Fig. S1). The tRNA pool extracted from Methanosarcina acetivorans or tRNACUA transcribed in vitro Direct charging of tRNACUA with was used in charging experiments. Charged and uncharged tRNA species were separated by electrophoresis in a denaturing acid-urea pyrrolysine in vitro and in vivo 10,11 polyacrylamide gel and tRNACUA was specifically detected by northern blotting with an oligonucleotide probe. The oligonucleo- Sherry K. Blight1*, Ross C. Larue1*, Anirban Mahapatra1*, tide complementary to tRNA could hybridize to a tRNA in the David G. Longstaff1, Edward Chang1, Gang Zhao2†, Patrick T. Kang4, CUA Kari B. Green-Church5, Michael K. Chan2,3,4 & Joseph A. Krzycki1,4 pool of tRNAs isolated from wild-type M. acetivorans but not to the tRNA pool from a pylT deletion mutant of M. acetivorans (A.M., 1Department of Microbiology, 484 West 12th Avenue, 2Department of Chemistry, A. Patel, J. Soares, R.L. and J.A.K., unpublished observations). 3 100 West 18th Avenue, Department of Biochemistry, 484 West 12th Avenue, Both tRNACUA and aminoacyl-tRNACUA were detectable in the The Ohio State University, Columbus, Ohio 43210, USA isolated cellular tRNA pool (Fig. 1). Alkaline hydrolysis deacylated 4Ohio State University Biochemistry Program, 484 West 12th Avenue, The Ohio the cellular charged species, but subsequent incubation with pyrro- State University, Columbus, Ohio 43210, USA lysine, ATP and PylS-His6 resulted in maximal conversion of 50% of 5CCIC/Mass Spectrometry and Proteomics Facility, The Ohio State University, deacylated tRNACUA to a species that migrated with the same 116 W 19th Ave, Columbus, Ohio 43210, USA electrophoretic mobility as the aminoacyl-tRNACUA present in the * These authors contributed equally to this work. -
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. -
Hydrogenases of Methanogens
ANRV413-BI79-18 ARI 27 April 2010 21:0 Hydrogenases from Methanogenic Archaea, Nickel, a Novel Cofactor, and H2 Storage Rudolf K. Thauer, Anne-Kristin Kaster, Meike Goenrich, Michael Schick, Takeshi Hiromoto, and Seigo Shima Max Planck Institute for Terrestrial Microbiology, D-35043 Marburg, Germany; email: [email protected] Annu. Rev. Biochem. 2010. 79:507–36 Key Words First published online as a Review in Advance on H2 activation, energy-converting hydrogenase, complex I of the March 17, 2010 respiratory chain, chemiosmotic coupling, electron bifurcation, The Annual Review of Biochemistry is online at reversed electron transfer biochem.annualreviews.org This article’s doi: Abstract 10.1146/annurev.biochem.030508.152103 Most methanogenic archaea reduce CO2 with H2 to CH4. For the Copyright c 2010 by Annual Reviews. activation of H2, they use different [NiFe]-hydrogenases, namely All rights reserved energy-converting [NiFe]-hydrogenases, heterodisulfide reductase- 0066-4154/10/0707-0507$20.00 associated [NiFe]-hydrogenase or methanophenazine-reducing by University of Texas - Austin on 06/10/13. For personal use only. [NiFe]-hydrogenase, and F420-reducing [NiFe]-hydrogenase. The energy-converting [NiFe]-hydrogenases are phylogenetically related Annu. Rev. Biochem. 2010.79:507-536. Downloaded from www.annualreviews.org to complex I of the respiratory chain. Under conditions of nickel limitation, some methanogens synthesize a nickel-independent [Fe]- hydrogenase (instead of F420-reducing [NiFe]-hydrogenase) and by that reduce their nickel requirement. The [Fe]-hydrogenase harbors a unique iron-guanylylpyridinol cofactor (FeGP cofactor), in which a low-spin iron is ligated by two CO, one C(O)CH2-, one S-CH2-, and a sp2-hybridized pyridinol nitrogen. -
Methanogenic Burst in the End-Permian Carbon Cycle
Methanogenic burst in the end-Permian carbon cycle Daniel H. Rothmana,b,1, Gregory P. Fournierc, Katherine L. Frenchb, Eric J. Almc, Edward A. Boyleb, Changqun Caod, and Roger E. Summonsb aLorenz Center, bDepartment of Earth, Atmospheric, and Planetary Sciences, and cDepartment of Biological Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139; and dState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China Edited by John M. Hayes, Woods Hole Oceanographic Institution, Woods Hole, MA, and approved February 4, 2014 (received for review September 27, 2013) The end-Permian extinction is associated with a mysterious disrup- and its perturbation to the carbon cycle but also to amplify the tion to Earth’s carbon cycle. Here we identify causal mechanisms via development of marine anoxia. Taken as a whole, these results three observations. First, we show that geochemical signals indicate reconcile an array of apparently disparate observations about the superexponential growth of the marine inorganic carbon reservoir, end-Permian event. coincident with the extinction and consistent with the expansion of a new microbial metabolic pathway. Second, we show that the effi- Growth of the Marine Carbon Reservoir cient acetoclastic pathway in Methanosarcina emerged at a time sta- Fig. 1A displays the carbon-isotopic record in Meishan, China tistically indistinguishable from the extinction. Finally, we show that (5). Immediately preceding the extinction event, the isotopic com- nickel concentrations in South China sediments increased sharply at position δ1 of carbonate carbon declines by about 7‰ during the extinction, probably as a consequence of massive Siberian volca- a period of about 100 thousand years (Kyr), first slowly, and sub- nism, enabling a methanogenic expansion by removal of nickel lim- sequently rapidly. -
Supplementary Information
Retroconversion of estrogens into androgens by bacteria via a cobalamin-mediated methylation Po-Hsiang Wang, Yi-Lung Chen, Sean Ting-Shyang Wei, Kan Wu, Tzong-Huei Lee, Tien-Yu Wu, and Yin-Ru Chiang Supplementary Information Table of Contents Dataset Dataset S1. Genome annotation of strain DHT3 and transcriptomic analysis (RNA-Seq) of bacterial cells grown anaerobically with testosterone or estradiol. SI Tables Table S1. Oligonucleotides used in this study. Table S2. Selection of housekeeping genes of strain DHT3 used for constructing the linear regression line in the global gene expression profiles (RNA-Seq). Table S3. Selection of the cobalamin-dependent methyltransferases used for the un-rooted maximum likelihood tree construction. Table S4. UPLC–APCI–HRMS data of the intermediates involved in anaerobic estrone catabolism by strain DHT3. Table S5. 1H- (600 MHz) and 13C-NMR (150 MHz) spectral data of the HPLC-purified metabolite (AND2) and the authentic standard 5-androstan-3,17-diol Table S6. Selection of the bacteria used for comparative analysis of the gene organization for HIP degradation. SI Figures Fig. S1 Scanning electron micrographs of strain DHT3 cells. Fig. S2 Cobalamin as an essential vitamin during the anaerobic growth of strain DHT3 on estradiol. Fig. S3 Arrangement and expression analysis of the emt genes in strain DHT3. Fig. S4 The anaerobic growth of the wild type (A) and the emtA-disrupted mutant (B) of strain DHT3 with testosterone and estradiol. Fig. S5 APCI–HRMS spectrum of the HIP produced by estrone-fed strain DHT3. 1 Fig. S6 UPLC–APCI–HRMS spectra of two TLC-purified androgen metabolites, 17β-hydroxyandrostan-3-one (A) and 3β,17β-dihydroxyandrostane (B). -
Characterization of Methanosarcina Barkeri MST and 227, Methanosarcina Mazei S-6T, and Methanosarcina Vacuolata Z-76IT GLORIA M
INTERNATIONALJOURNAL OF SYSTEMATICBACTERIOLOGY, Apr. 1991, p. 267-274 Vol. 41, No. 2 0020-7713/91/020267-08$02.OO/O Copyright 0 1991, International Union of Microbiological Societies Characterization of Methanosarcina barkeri MST and 227, Methanosarcina mazei S-6T, and Methanosarcina vacuolata Z-76IT GLORIA M. MAESTROJUAN' AND DAVID R. BOONE172* Departments of Environmental Science and Engineering' and Chemical and Biological Science,2 Oregon Graduate Institute, 19600 N.W. von Neumann Drive, Beaverton, Oregon 97006-1999 Members of the genus Methanosarcina are recognized as major aceticlastic methanogens, and several species which thrive in low-salt, pH-neutral culture medium at mesophilic temperatures have been described. However, the environmental conditions which support the fastest growth of these species (Methanosarcina barkeri MST [T = type strain] and 227, Methanosarcina mazei S-6T, and Methanosarcina vacuolata Z-761T) have not been reported previously. Although the members of the genus Methanosarcina are widely assumed to grow best at pH values near neutrality, we found that some strains prefer acidic pH values. M. vacuolata and the two strains of M. barkeri which we tested were acidophilic when they were grown on H, plus methanol, growing most rapidly at pH 5 and growing at pH values as low as 4.3. M. mazei grew best at pH values near neutrality. We found that all of the strains tested grew most rapidly at 37 to 42°C on all of the growth substrates which we tested. None of the strains was strongly halophilic, although the growth of some strains was slightly stimulated by small amounts of added NaCI. -
A Genomic Timescale of Prokaryote Evolution: Insights Into the Origin of Methanogenesis, Phototrophy, and the Colonization of Land
BMC Evolutionary Biology BioMed Central Research article Open Access A genomic timescale of prokaryote evolution: insights into the origin of methanogenesis, phototrophy, and the colonization of land Fabia U Battistuzzi1, Andreia Feijao2 and S Blair Hedges*1 Address: 1NASA Astrobiology Institute and Department of Biology, 208 Mueller Laboratory, The Pennsylvania State University, University Park, PA 16802, USA and 2European Molecular Biology Laboratory, Meyerhofstrasse 1, 69117 Heidelberg, Germany Email: Fabia U Battistuzzi - [email protected]; Andreia Feijao - [email protected]; S Blair Hedges* - [email protected] * Corresponding author Published: 09 November 2004 Received: 07 August 2004 Accepted: 09 November 2004 BMC Evolutionary Biology 2004, 4:44 doi:10.1186/1471-2148-4-44 This article is available from: http://www.biomedcentral.com/1471-2148/4/44 © 2004 Battistuzzi et al; licensee BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Abstract Background: The timescale of prokaryote evolution has been difficult to reconstruct because of a limited fossil record and complexities associated with molecular clocks and deep divergences. However, the relatively large number of genome sequences currently available has provided a better opportunity to control for potential biases such as horizontal gene transfer and rate differences among lineages. We assembled a data set of sequences from 32 proteins (~7600 amino acids) common to 72 species and estimated phylogenetic relationships and divergence times with a local clock method. Results: Our phylogenetic results support most of the currently recognized higher-level groupings of prokaryotes. -
The Role of Stress Proteins in Haloarchaea and Their Adaptive Response to Environmental Shifts
biomolecules Review The Role of Stress Proteins in Haloarchaea and Their Adaptive Response to Environmental Shifts Laura Matarredona ,Mónica Camacho, Basilio Zafrilla , María-José Bonete and Julia Esclapez * Agrochemistry and Biochemistry Department, Biochemistry and Molecular Biology Area, Faculty of Science, University of Alicante, Ap 99, 03080 Alicante, Spain; [email protected] (L.M.); [email protected] (M.C.); [email protected] (B.Z.); [email protected] (M.-J.B.) * Correspondence: [email protected]; Tel.: +34-965-903-880 Received: 31 July 2020; Accepted: 24 September 2020; Published: 29 September 2020 Abstract: Over the years, in order to survive in their natural environment, microbial communities have acquired adaptations to nonoptimal growth conditions. These shifts are usually related to stress conditions such as low/high solar radiation, extreme temperatures, oxidative stress, pH variations, changes in salinity, or a high concentration of heavy metals. In addition, climate change is resulting in these stress conditions becoming more significant due to the frequency and intensity of extreme weather events. The most relevant damaging effect of these stressors is protein denaturation. To cope with this effect, organisms have developed different mechanisms, wherein the stress genes play an important role in deciding which of them survive. Each organism has different responses that involve the activation of many genes and molecules as well as downregulation of other genes and pathways. Focused on salinity stress, the archaeal domain encompasses the most significant extremophiles living in high-salinity environments. To have the capacity to withstand this high salinity without losing protein structure and function, the microorganisms have distinct adaptations. -
The Archaeal Concept and the World It Lives In: a Retrospective
Carl R. Woese (center) with His Majesty Carl XVI Gustaf of Sweden and Queen Silvia on the occassion of his receiving the 2003 Crafoord Prize, given by the Royal Swedish Academy of Sciences. Photo credit: Royal Swedish Academy of Sciences. Photosynthesis Research 80: 361–372, 2004. 363 © 2004 Kluwer Academic Publishers. Printed in the Netherlands. Personal perspective The archaeal concept and the world it lives in: a retrospective Carl R. Woese Department of Microbiology, University of Illinois at Urbana-Champaign, B103 Chemical and Life Sciences Laboratory, 601 South Goodwin Ave, Urbana, IL 61801-3709, USA (e-mail: [email protected]; fax: +1-217-244-6697) Received 9 July 2003; accepted in revised form 30 August 2003 Key words: archaea, evolution, genomics, molecular phylogeny, phylogenetic reconstruction, ribosomal RNA Abstract The present retrospective concerns the discovery and development of the archaea, the so-called ‘third form of life’ that no one anticipated and many did not, and still do not want. In its birth pangs, which the archaea had a plenty, the concept encountered biology unmasked; for it ran up against some of the key struts in the 20th century biological edifice. Consequently, the history of the development of the archaeal concept provides an excellent window on certain of the weaknesses in the 20th century biology paradigm, weaknesses that have now led that paradigm to a conceptual dead end. On the other hand, the archaeal concept has also provided us one of the pillars on which a new holistic paradigm for biology can be built. So, it would seem of value to retrace some of the twists and turns in the history of the development of the archaeal concept. -
Characterization of Methanosarcina Mazei JL01 Isolated from Holocene
Proceedings Characterization of Methanosarcina mazei JL01 Isolated from Holocene Arctic Permafrost and Study of the Archaeon Cooperation with Bacterium Sphaerochaeta associata GLS2T † Viktoriia Oshurkova 1,*, Olga Troshina 1, Vladimir Trubitsyn 1, Yana Ryzhmanova 1, Olga Bochkareva 2 and Viktoria Shcherbakova 1 1 Skryabin Institute of Biochemistry and Physiology of Microorganisms, Federal Research Center Pushchino Center for Biological Research of the Russian Academy of Sciences, prospect Nauki 5, Pushchino, 142290 Moscow, Russia; [email protected] (O.T.); [email protected] (V.T.); [email protected] (Y.R.); [email protected] (V.S.) 2 Institute of Science and Technology (IST Austria), Am Campus 1, 3400 Klosterneuburg, Austria; [email protected] * Correspondence: [email protected] † Presented at the 1st International Electronic Conference on Microbiology, 2–30 November 2020; Available online: https://ecm2020.sciforum.net/. Published: 18 December 2020 Abstract: A mesophilic methanogenic culture, designated JL01, was isolated from Holocene permafrost in the Russian Arctic. After long-term extensive cultivation at 15 °C, it turned out to be a tied binary culture of archaeal (JL01) and bacterial (Sphaerochaeta associata GLS2) strains. Strain JL01 was a strict anaerobe and grew on methanol, acetate, and methylamines as energy and carbon sources. Cells were irregular coccoid, non-motile, non-spore-forming, and Gram-stain-positive. Optimum conditions for growth were 24–28 °C, pH 6.8–7.3, and 0.075–0.1 M NaCl. Phylogenetic tree reconstructions based on 16S rRNA and concatenated alignment of broadly conserved protein- coding genes revealed 16S rRNA’s close relation to Methanosarcina mazei S-6T (similarity 99.5%). -
Reducing the Genetic Code Induces Massive Rearrangement of the Proteome
Reducing the genetic code induces massive rearrangement of the proteome Patrick O’Donoghuea,b, Laure Pratc, Martin Kucklickd, Johannes G. Schäferc, Katharina Riedele, Jesse Rinehartf,g, Dieter Söllc,h,1, and Ilka U. Heinemanna,1 Departments of aBiochemistry and bChemistry, The University of Western Ontario, London, ON N6A 5C1, Canada; Departments of cMolecular Biophysics and Biochemistry, fCellular and Molecular Physiology, and hChemistry, and gSystems Biology Institute, Yale University, New Haven, CT 06520; dDepartment of Microbiology, Technical University of Braunschweig, Braunschweig 38106, Germany; and eDivision of Microbial Physiology and Molecular Biology, University of Greifswald, Greifswald 17487, Germany Contributed by Dieter Söll, October 22, 2014 (sent for review September 29, 2014; reviewed by John A. Leigh) Expanding the genetic code is an important aim of synthetic Opening codons by reducing the genetic code is highly biology, but some organisms developed naturally expanded ge- promising, but it is unknown how removing 1 amino acid from netic codes long ago over the course of evolution. Less than 1% of the genetic code might impact the proteome or cellular viability. all sequenced genomes encode an operon that reassigns the stop Many genetic code variations are found in nature (15), including codon UAG to pyrrolysine (Pyl), a genetic code variant that results stop or sense codon reassignments, codon recoding, and natural from the biosynthesis of Pyl-tRNAPyl. To understand the selective code expansion (16). Pyrrolysine (Pyl) is a rare example of nat- advantage of genetically encoding more than 20 amino acids, we ural genetic code expansion. Evidence for genetically encoded constructed a markerless tRNAPyl deletion strain of Methanosarcina Pyl is found in <1% of all sequenced genomes (17).