Extracellular Electron Uptake in Methanosarcinales Is Independent of Multiheme C-Type Cytochromes Mon Oo Yee & Amelia-Elena Rotaru*
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Methanospirillum Hungatei GP1 As an S Layer MAX FIRTEL,1 GORDON SOUTHAM,1 GEORGE HARAUZ,2 and TERRY J
JOURNAL OF BACTERIOLOGY, Dec. 1993, p. 7550-7560 Vol. 175, No. 23 0021-9193/93/237550-11$02.00/0 Copyright © 1993, American Society for Microbiology Characterization of the Cell Wall of the Sheathed Methanogen Methanospirillum hungatei GP1 as an S Layer MAX FIRTEL,1 GORDON SOUTHAM,1 GEORGE HARAUZ,2 AND TERRY J. BEVERIDGE'* Department ofMicrobiology' and Department ofMolecular Biology and Genetics, 2 College of Biological Sciences, University of Guelph, Guelph, Ontario, Canada N1G 2W1 Received 16 June 1993/Accepted 27 September 1993 The cell wall of MethanospiriUum hungatei GP1 is a labile structure that has been difficult to isolate and Downloaded from characterize because the cells which it encases are contained within a sheath. Cell-sized fragments, 560 nm wide by several micrometers long, of cell wall were extracted by a novel method involving the gradual drying of the filaments in 2% (wtlvol) sodium dodecyl sulfate and 10%0 (wt/vol) sucrose in 50 mM N-2-hydroxyeth- ylpiperazine-N'-2-ethanesulfonic acid (HEPES) buffer containing 10 mM EDTA. The surface was a hexagonal array (a = b = 15.1 nm) possessing a helical superstructure with a ca. 2.50 pitch angle. In shadowed relief, the smooth outer face was punctuated with deep pits, whereas the inner face was relatively featureless. Computer-based two-dimensional reconstructed views of the negatively stained layer demonstrated 4.0- and 2.0-nm-wide electron-dense regions on opposite sides of the layer likely corresponding to the openings of funnel-shaped channels. The face featuring the larger openings best corresponds to the outer face of the layer. -
Methanothermus Fervidus Type Strain (V24S)
UC Davis UC Davis Previously Published Works Title Complete genome sequence of Methanothermus fervidus type strain (V24S). Permalink https://escholarship.org/uc/item/9367m39j Journal Standards in genomic sciences, 3(3) ISSN 1944-3277 Authors Anderson, Iain Djao, Olivier Duplex Ngatchou Misra, Monica et al. Publication Date 2010-11-20 DOI 10.4056/sigs.1283367 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Standards in Genomic Sciences (2010) 3:315-324 DOI:10.4056/sigs.1283367 Complete genome sequence of Methanothermus fervidus type strain (V24ST) Iain Anderson1, Olivier Duplex Ngatchou Djao2, Monica Misra1,3, Olga Chertkov1,3, Matt Nolan1, Susan Lucas1, Alla Lapidus1, Tijana Glavina Del Rio1, Hope Tice1, Jan-Fang Cheng1, Roxanne Tapia1,3, Cliff Han1,3, Lynne Goodwin1,3, Sam Pitluck1, Konstantinos Liolios1, Natalia Ivanova1, Konstantinos Mavromatis1, Natalia Mikhailova1, Amrita Pati1, Evelyne Brambilla4, Amy Chen5, Krishna Palaniappan5, Miriam Land1,6, Loren Hauser1,6, Yun-Juan Chang1,6, Cynthia D. Jeffries1,6, Johannes Sikorski4, Stefan Spring4, Manfred Rohde2, Konrad Eichinger7, Harald Huber7, Reinhard Wirth7, Markus Göker4, John C. Detter1, Tanja Woyke1, James Bristow1, Jonathan A. Eisen1,8, Victor Markowitz5, Philip Hugenholtz1, Hans-Peter Klenk4, and Nikos C. Kyrpides1* 1 DOE Joint Genome Institute, Walnut Creek, California, USA 2 HZI – Helmholtz Centre for Infection Research, Braunschweig, Germany 3 Los Alamos National Laboratory, Bioscience Division, Los Alamos, New Mexico, USA 4 DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany 5 Biological Data Management and Technology Center, Lawrence Berkeley National Laboratory, Berkeley, California, USA 6 Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA 7 University of Regensburg, Archaeenzentrum, Regensburg, Germany 8 University of California Davis Genome Center, Davis, California, USA *Corresponding author: Nikos C. -
Genome-Resolved Meta-Analysis of the Microbiome in Oil Reservoirs Worldwide
microorganisms Article Genome-Resolved Meta-Analysis of the Microbiome in Oil Reservoirs Worldwide Kelly J. Hidalgo 1,2,* , Isabel N. Sierra-Garcia 3 , German Zafra 4 and Valéria M. de Oliveira 1 1 Microbial Resources Division, Research Center for Chemistry, Biology and Agriculture (CPQBA), University of Campinas–UNICAMP, Av. Alexandre Cazellato 999, 13148-218 Paulínia, Brazil; [email protected] 2 Graduate Program in Genetics and Molecular Biology, Institute of Biology, University of Campinas (UNICAMP), Rua Monteiro Lobato 255, Cidade Universitária, 13083-862 Campinas, Brazil 3 Biology Department & CESAM, University of Aveiro, Aveiro, Portugal, Campus de Santiago, Avenida João Jacinto de Magalhães, 3810-193 Aveiro, Portugal; [email protected] 4 Grupo de Investigación en Bioquímica y Microbiología (GIBIM), Escuela de Microbiología, Universidad Industrial de Santander, Cra 27 calle 9, 680002 Bucaramanga, Colombia; [email protected] * Correspondence: [email protected]; Tel.: +55-19981721510 Abstract: Microorganisms inhabiting subsurface petroleum reservoirs are key players in biochemical transformations. The interactions of microbial communities in these environments are highly complex and still poorly understood. This work aimed to assess publicly available metagenomes from oil reservoirs and implement a robust pipeline of genome-resolved metagenomics to decipher metabolic and taxonomic profiles of petroleum reservoirs worldwide. Analysis of 301.2 Gb of metagenomic information derived from heavily flooded petroleum reservoirs in China and Alaska to non-flooded petroleum reservoirs in Brazil enabled us to reconstruct 148 metagenome-assembled genomes (MAGs) of high and medium quality. At the phylum level, 74% of MAGs belonged to bacteria and 26% to archaea. The profiles of these MAGs were related to the physicochemical parameters and recovery management applied. -
The Genome Characteristics and Predicted Function of Methyl-Group Oxidation Pathway in the Obligate Aceticlastic Methanogens, Methanosaeta Spp
The Genome Characteristics and Predicted Function of Methyl-Group Oxidation Pathway in the Obligate Aceticlastic Methanogens, Methanosaeta spp. Jinxing Zhu1,2, Huajun Zheng3, Guomin Ai1, Guishan Zhang1, Di Liu4, Xiaoli Liu1, Xiuzhu Dong1* 1 State Key Laboratory of Microbial Resources, Institute of Microbiology, Chinese Academy of Sciences, Beijing, People’s Republic of China, 2 Graduate School, Chinese Academy of Sciences, Beijing, People’s Republic of China, 3 Shanghai-MOST Key Laboratory of Health and Disease Genomics, Chinese National Human Genome Center at Shanghai, Shanghai, People’s Republic of China, 4 Information center, Institute of Microbiology, Chinese Academy of Sciences, Beijing, People’s Republic of China Abstract In this work, we report the complete genome sequence of an obligate aceticlastic methanogen, Methanosaeta harundinacea 6Ac. Genome comparison indicated that the three cultured Methanosaeta spp., M. thermophila, M. concilii and M. harundinacea 6Ac, each carry an entire suite of genes encoding the proteins involved in the methyl-group oxidation pathway, a pathway whose function is not well documented in the obligately aceticlastic methanogens. Phylogenetic analysis showed that the methyl-group oxidation-involving proteins, Fwd, Mtd, Mch, and Mer from Methanosaeta strains cluster with the methylotrophic methanogens, and were not closely related to those from the hydrogenotrophic methanogens. Quantitative PCR detected the expression of all genes for this pathway, albeit ten times lower than the genes for aceticlastic methanogenesis in strain 6Ac. Western blots also revealed the expression of fwd and mch, genes involved in methyl-group oxidation. Moreover, 13C-labeling experiments suggested that the Methanosaeta strains might use the pathway as a methyl oxidation shunt during the aceticlastic metabolism. -
Phylogenetics of Archaeal Lipids Amy Kelly 9/27/2006 Outline
Phylogenetics of Archaeal Lipids Amy Kelly 9/27/2006 Outline • Phlogenetics of Archaea • Phlogenetics of archaeal lipids • Papers Phyla • Two? main phyla – Euryarchaeota • Methanogens • Extreme halophiles • Extreme thermophiles • Sulfate-reducing – Crenarchaeota • Extreme thermophiles – Korarchaeota? • Hyperthermophiles • indicated only by environmental DNA sequences – Nanoarchaeum? • N. equitans a fast evolving euryarchaeal lineage, not novel, early diverging archaeal phylum – Ancient archael group? • In deepest brances of Crenarchaea? Euryarchaea? Archaeal Lipids • Methanogens – Di- and tetra-ethers of glycerol and isoprenoid alcohols – Core mostly archaeol or caldarchaeol – Core sometimes sn-2- or Images removed due to sn-3-hydroxyarchaeol or copyright considerations. macrocyclic archaeol –PMI • Halophiles – Similar to methanogens – Exclusively synthesize bacterioruberin • Marine Crenarchaea Depositional Archaeal Lipids Biological Origin Environment Crocetane methanotrophs? methane seeps? methanogens, PMI (2,6,10,15,19-pentamethylicosane) methanotrophs hypersaline, anoxic Squalane hypersaline? C31-C40 head-to-head isoprenoids Smit & Mushegian • “Lost” enzymes of MVA pathway must exist – Phosphomevalonate kinase (PMK) – Diphosphomevalonate decarboxylase – Isopentenyl diphosphate isomerase (IPPI) Kaneda et al. 2001 Rohdich et al. 2001 Boucher et al. • Isoprenoid biosynthesis of archaea evolved through a combination of processes – Co-option of ancestral enzymes – Modification of enzymatic specificity – Orthologous and non-orthologous gene -
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. -
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 -
Methanosaeta Pelagica" Sp
Aceticlastic and NaCl-Requiring Methanogen "Methanosaeta pelagica" sp. nov., Isolated from Marine Tidal Flat Title Sediment Author(s) Mori, Koji; Iino, Takao; Suzuki, Ken-Ichiro; Yamaguchi, Kaoru; Kamagata, Yoichi Applied and Environmental Microbiology, 78(9), 3416-3423 Citation https://doi.org/10.1128/AEM.07484-11 Issue Date 2012-05 Doc URL http://hdl.handle.net/2115/50384 Rights © 2012 by the American Society for Microbiology Type article (author version) File Information AEM78-9_3416-3423.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP Mori et al. Title 2 Aceticlastic and NaCl-requiring methanogen “Methanosaeta pelagica” sp. nov., isolated from marine tidal flat sediment. 4 Authors 6 Koji Mori,1 Takao Iino,2 Ken-ichiro Suzuki,1 Kaoru Yamaguchi1 & Yoichi Kamagata3 1NITE Biological Resource Center (NBRC), National Institute of Technology and Evaluation (NITE), 8 2-5-8 Kazusakamatari, Kisarazu, Chiba 292-0818, Japan 2Japan Collection of Microorganisms, RIKEN BioResource Center, 2-1 Hirosawa, Wako, Saitama 10 351-0198, Japan 3Bioproduction Research Institute, National Institute of Advanced Industrial Science and Technology 12 (AIST), Central 6, 1-1-1 Higashi, Tsukuba, Ibaraki 400-8511, Japan 14 Corresponding author Koji Mori 16 NITE Biological Resource Center (NBRC), National Institute of Technology and Evaluation (NITE), 2-5-8 Kazusakamatari, Kisarazu, Chiba 292-0818, Japan 18 Tel, +81-438-20-5763; Fax, +81-438-52-2329; E-mail, [email protected] 20 Running title Marine aceticlastic methanogen, Methanosaeta pelagica 22 1 Mori et al. 2 ABSTRACT Acetate is a key compound for anaerobic organic matter degradation, and so far, two genera, 4 Methanosaeta and Methanosarcina, are only contributors for acetate degradation among methanogens. -
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. -
Archaeology of Eukaryotic DNA Replication
Downloaded from http://cshperspectives.cshlp.org/ on September 25, 2021 - Published by Cold Spring Harbor Laboratory Press Archaeology of Eukaryotic DNA Replication Kira S. Makarova and Eugene V. Koonin National Center for Biotechnology Information, National Library of Medicine, National Institutes of Health, Bethesda, Maryland 20894 Correspondence: [email protected] Recent advances in the characterization of the archaeal DNA replication system together with comparative genomic analysis have led to the identification of several previously un- characterized archaeal proteins involved in replication and currently reveal a nearly com- plete correspondence between the components of the archaeal and eukaryotic replication machineries. It can be inferred that the archaeal ancestor of eukaryotes and even the last common ancestor of all extant archaea possessed replication machineries that were compa- rable in complexity to the eukaryotic replication system. The eukaryotic replication system encompasses multiple paralogs of ancestral components such that heteromeric complexes in eukaryotes replace archaeal homomeric complexes, apparently along with subfunctionali- zation of the eukaryotic complex subunits. In the archaea, parallel, lineage-specific dupli- cations of many genes encoding replication machinery components are detectable as well; most of these archaeal paralogs remain to be functionally characterized. The archaeal rep- lication system shows remarkable plasticity whereby even some essential components such as DNA polymerase and single-stranded DNA-binding protein are displaced by unrelated proteins with analogous activities in some lineages. ouble-stranded DNA is the molecule that Okazaki fragments (Kornberg and Baker 2005; Dcarries genetic information in all cellular Barry and Bell 2006; Hamdan and Richardson life-forms; thus, replication of this genetic ma- 2009; Hamdan and van Oijen 2010). -
Insights Into Archaeal Evolution and Symbiosis from the Genomes of a Nanoarchaeon and Its Inferred Crenarchaeal Host from Obsidian Pool, Yellowstone National Park
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Microbiology Publications and Other Works Microbiology 4-22-2013 Insights into archaeal evolution and symbiosis from the genomes of a nanoarchaeon and its inferred crenarchaeal host from Obsidian Pool, Yellowstone National Park Mircea Podar University of Tennessee - Knoxville, [email protected] Kira S. Makarova National Institutes of Health David E. Graham University of Tennessee - Knoxville, [email protected] Yuri I. Wolf National Institutes of Health Eugene V. Koonin National Institutes of Health See next page for additional authors Follow this and additional works at: https://trace.tennessee.edu/utk_micrpubs Part of the Microbiology Commons Recommended Citation Biology Direct 2013, 8:9 doi:10.1186/1745-6150-8-9 This Article is brought to you for free and open access by the Microbiology at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Microbiology Publications and Other Works by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. Authors Mircea Podar, Kira S. Makarova, David E. Graham, Yuri I. Wolf, Eugene V. Koonin, and Anna-Louise Reysenbach This article is available at TRACE: Tennessee Research and Creative Exchange: https://trace.tennessee.edu/ utk_micrpubs/44 Podar et al. Biology Direct 2013, 8:9 http://www.biology-direct.com/content/8/1/9 RESEARCH Open Access Insights into archaeal evolution and symbiosis from the genomes of a nanoarchaeon and its inferred crenarchaeal host from Obsidian Pool, Yellowstone National Park Mircea Podar1,2*, Kira S Makarova3, David E Graham1,2, Yuri I Wolf3, Eugene V Koonin3 and Anna-Louise Reysenbach4 Abstract Background: A single cultured marine organism, Nanoarchaeum equitans, represents the Nanoarchaeota branch of symbiotic Archaea, with a highly reduced genome and unusual features such as multiple split genes. -
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.