Extracellular Electron Uptake in Methanosarcinales Is Independent of Multiheme
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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. -
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. -
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. -
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. -
Open Dissertation 4-7-09.Pdf
The Pennsylvania State University The Graduate School Department of Civil and Environmental Engineering IMPROVED ANAEROBIC DIGESTER STABILITY TO ORGANIC LOADING RATE SHOCKS WITH THE USE OF AN ENVIRONMENTALLY DERIVED INOCULUM A Dissertation in Environmental Engineering and Biogeochemistry by Lisa Marie Steinberg © 2009 Lisa Marie Steinberg Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy May 2009 The dissertation of Lisa Marie Steinberg was reviewed and approved* by the following: John Regan Associate Professor of Environmental Engineering Dissertation Advisor Chair of Committee Christopher House Associate Professor of Geosciences Bruce Logan Kappe Professor of Environmental Engineering Jenn Macalady Assistant Professor of Geosciences Peggy Johnson Department Head and Professor of Civil Engineering *Signatures are on file in the Graduate School ABSTRACT Anaerobic digestion broadly describes technology that utilizes microorganisms to break down organic matter under anaerobic conditions through the coordinated efforts of several trophic groups of microorganisms. The last step is catalyzed by methanogens which produce primarily methane, carbon dioxide, and water as products of metabolism. Anaerobic digestion occurs naturally in a variety of water-saturated sediments, but is also used to treat waste in constructed reactors. There are a number of advantages to treating waste with anaerobic digestion, but perhaps the greatest is that waste treatment can be coupled to energy generation by the production of a methane-rich biogas. Despite the advantages, anaerobic digestion is severely under-utilized in waste treatment mainly due to the belief that anaerobic digesters are less stable than aerobic treatment processes. Anaerobic digesters are typically operated under warm temperatures and circumneutral pH, with operation outside of these conditions leading to instability and potential reactor failure. -
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.