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The Vertical Distribution of Sediment Archaeal Community in the (Black Bloom) Disturbing Zhushan Bay of Lake Taihu
Hindawi Publishing Corporation Archaea Volume 2016, Article ID 8232135, 8 pages http://dx.doi.org/10.1155/2016/8232135 Research Article The Vertical Distribution of Sediment Archaeal Community in the (Black Bloom) Disturbing Zhushan Bay of Lake Taihu Xianfang Fan1,2 and Peng Xing1 1 State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, China 2State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China Correspondence should be addressed to Peng Xing; [email protected] Received 20 August 2015; Revised 27 November 2015; Accepted 20 December 2015 Academic Editor: William B. Whitman Copyright © 2016 X. Fan and P. Xing. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Using the Illumina sequencing technology, we investigated the vertical distribution of archaeal community in the sediment of Zhushan Bay of Lake Taihu, where the black bloom frequently occurred in summer. Overall, the Miscellaneous Crenarchaeotal Group (MCG), Deep Sea Hydrothermal Vent Group 6 (DHVEG-6), and Methanobacterium dominated the archaeal community. However, we observed significant difference in composition of archaeal community among different depths of the sediment. DHVEG-6 dominated in the surface layer (0–3 cm) sediment. Methanobacterium was the dominating archaeal taxa in the L2 (3– 6 cm) and L3 (6–10) sediment. MCG was most abundant in the L4 (10–15 cm) and L5 (15–20 cm) sediment. Besides, DHVEG-6 was significantly affected by the concentration of total phosphorus ).(TP And loss on ignition (LOI) was an important environmental factor for Methanobacterium. -
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. -
THE MASS of L-PYRROLYSINE in METHYLAMINE METHYLTRANSFERASES and the ROLE of ITS IMINE BOND in CATALYSIS DISSERTATION Presented I
THE MASS OF L-PYRROLYSINE IN METHYLAMINE METHYLTRANSFERASES AND THE ROLE OF ITS IMINE BOND IN CATALYSIS DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in the Graduate School of The Ohio State University by Jitesh Anthony Aloysius Soares, M.S. The Ohio State University 2008 Dissertation Committee: Dr. Joseph A. Krzycki, Advisor Approved by Dr. Charles J. Daniels Dr. Mark Morrison ______________________ Dr. F. Robert Tabita Advisor Graduate Program in Microbiology ABSTRACT Methanosarcina barkeri is an archaeon capable of producing methane from methylamines. Methylamine methyltransferases initiate methanogenesis from methylamines by transferring methyl groups to a cognate corrinoid protein. Each gene encoding a methylamine methyltransferase has been shown to contain a single in-frame amber codon. Further studies have shown that in the monomethylamine methyltransferase, mtmB , the amber codon encodes a novel amino acid, L-pyrrolysine. X-ray crystal structures of MtmB have shown that the structure of this amino acid is a lysine residue with the epsilon-nitrogen in amide linkage to a (4R, 5R)-4-substituted pyrrolyine-5-carboxylate ring. However, these structures did not allow an assignment of the pyrroline ring C4 substituent as a methyl or amine group. In this thesis (Chapter 2) mass spectrometry of chymotryptic digests of methylamine methyltransferases is employed to show that pyrrolysine in present in all three types of methylamine methyltransferase at the position corresponding to the amber codon in their respective genes. The mass of this amber-encoded residue was observed to coincide with the predicted mass of pyrrolysine with a methyl- group at the C4 position. -
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. -
Characteristics and Metabolic Patterns of Soil Methanogenic Archaea Communities in the High Latitude Natural Wetlands of China
Characteristics and Metabolic Patterns of Soil Methanogenic Archaea Communities in the High Latitude Natural Wetlands of China Di Wu Northeast Forestry University Caihong Zhao Northeast Forestry University Hui Bai Forestry Science Research Institute of Heilongjiang Province Fujuan Feng Northeast Forestry University Xin Sui Heilongjiang University Guangyu Sun ( [email protected] ) Northeast Forestry University Research article Keywords: Wetlands, Methanogens, Community diversity, Indicator species, Methanogenic metabolic patterns Posted Date: August 12th, 2020 DOI: https://doi.org/10.21203/rs.3.rs-54821/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Page 1/18 Abstract Background: Soil methanogenic microorganisms are one of the primary methane-producing microbes in wetlands. However, we still poorly understand the community characteristic and metabolic patterns of these microorganisms according to vegetation type and seasonal changes. Therefore, to better elucidate the effects of the vegetation type and seasonal factors on the methanogenic community structure and metabolic patterns, we detected the characteristics of the soil methanogenic mcrA gene from three types of natural wetlands in different seasons in the Xiaoxing'an Mountain region, China. Result: The results indicated that the distribution of Methanobacteriaceae (hydrogenotrophic methanogens) was higher in winter, while Methanosarcinaceae and Methanosaetaceae accounted for a higher proportion in summer. Hydrogenotrophic methanogenesis was the dominant trophic pattern in each wetland. The results of principal coordinate analysis and cluster analysis showed that the vegetation type considerably inuenced the methanogenic community composition. The methanogenic community structure in the Betula platyphylla – Larix gmelinii wetland was relatively different from the structure of the other two wetland types. -
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). -
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. -
Translation of the Amber Codon in Methylamine Methyltransferase Genes of a Methanogenic Archaeon
TRANSLATION OF THE AMBER CODON IN METHYLAMINE METHYLTRANSFERASE GENES OF A METHANOGENIC ARCHAEON DISSERTATION Presented in Partial Fulfillment of the Requirements for The Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Gayathri Srinivasan, M. S. * * * * * The Ohio State University 2003 Dissertation Committee: Dr. Joseph A. Krzycki, Advisor Approved by Dr. Charles J. Daniels Dr. Tina M. Henkin ________________________ (Advisor) Dr. John N. Reeve Department of Microbiology ABSTRACT Members of the Methanosarcinaceae family can in addition to hydrogen/carbon dioxide utilize several methylated compounds and convert them to methane. Methanogenesis from methylamines involves methylamine specific methyltransferases that transfer the methyl group from the methylamines to a corrinoid protein. The methylamine specific methyltransferase genes contain a single in-frame amber codon that is not read as a translational stop. The residue encoded by the amber codon, has been found to be a novel amino acid, pyrrolysine in MtmB. Multiple copies of monomethylamine methyltransferase genes (mtmB) containing a single amber codon within their open reading frames, along with the genes encoding their cognate corrinoid proteins (mtmC), exist within the genomes of the members of the Methanosarcinaceae family. The two copies of mtmCB genes from M. barkeri MS are differentially transcribed. Editing of the mtmB2 transcript was not detected suggesting a mechanism of amber codon readthrough occurring in the organism. Similar to selenocysteine incorporation at UGA codons, the Methanosarcinaceae also appear to have a unique mechanism for amber codon readthrough. An amber decoding tRNA gene, pylT, along with its cognate lysyl tRNA synthetase, pylS, are found near the MMA methyltransferase gene cluster. -
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).