The Genome Sequence of Methanohalophilus Mahii SLPT
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Regeneration of Unconventional Natural Gas by Methanogens Co
www.nature.com/scientificreports OPEN Regeneration of unconventional natural gas by methanogens co‑existing with sulfate‑reducing prokaryotes in deep shale wells in China Yimeng Zhang1,2,3, Zhisheng Yu1*, Yiming Zhang4 & Hongxun Zhang1 Biogenic methane in shallow shale reservoirs has been proven to contribute to economic recovery of unconventional natural gas. However, whether the microbes inhabiting the deeper shale reservoirs at an average depth of 4.1 km and even co-occurring with sulfate-reducing prokaryote (SRP) have the potential to produce biomethane is still unclear. Stable isotopic technique with culture‑dependent and independent approaches were employed to investigate the microbial and functional diversity related to methanogenic pathways and explore the relationship between SRP and methanogens in the shales in the Sichuan Basin, China. Although stable isotopic ratios of the gas implied a thermogenic origin for methane, the decreased trend of stable carbon and hydrogen isotope value provided clues for increasing microbial activities along with sustained gas production in these wells. These deep shale-gas wells harbored high abundance of methanogens (17.2%) with ability of utilizing various substrates for methanogenesis, which co-existed with SRP (6.7%). All genes required for performing methylotrophic, hydrogenotrophic and acetoclastic methanogenesis were present. Methane production experiments of produced water, with and without additional available substrates for methanogens, further confrmed biomethane production via all three methanogenic pathways. Statistical analysis and incubation tests revealed the partnership between SRP and methanogens under in situ sulfate concentration (~ 9 mg/L). These results suggest that biomethane could be produced with more fexible stimulation strategies for unconventional natural gas recovery even at the higher depths and at the presence of SRP. -
Chemotaxonomic Characterization of the Thaumarchaeal Lipidome
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Aberdeen University Research Archive Chemotaxonomic characterization of the thaumarchaeal lipidome Running title: Comparative analysis of the thaumarchaeal lipidome Felix J. Elling1+, Martin Könneke1,2#, Graeme W. Nicol3, Michaela Stieglmeier4, Barbara Bayer5, Eva Spieck6, José R. de la Torre7, Kevin W. Becker1†, Michael Thomm8, James I. Prosser9, Gerhard J. Herndl5,10, Christa Schleper4, Kai-Uwe Hinrichs1 1 Organic Geochemistry Group, MARUM - Center for Marine Environmental Sciences & Department of Geosciences, University of Bremen, 28359 Bremen, Germany. 2 Marine Archaea Group, MARUM Center for Marine Environmental Sciences & Department of Geosciences, University of Bremen, 28359 Bremen, Germany. 3 Environmental Microbial Genomics, Laboratoire Ampère, École Centrale de Lyon, Université de Lyon, 69134 Ecully, France 4 Department of Ecogenomics and Systems Biology, Center of Ecology, University of Vienna, 1090 Vienna, Austria. 5 Department of Limnology and BioOceanography, Center of Ecology, University of Vienna, 1090 Vienna, Austria. 6 Biocenter Klein Flottbek, Department of Microbiology and Biotechnology, University of Hamburg, 22609 Hamburg, Germany. 7 Department of Biology, San Francisco State University, San Francisco, CA, USA. 8 Lehrstuhl für Mikrobiologie und Archaeenzentrum, Universität Regensburg, 93053 Regensburg, Germany. 9 Institute of Biological and Environmental Sciences, University of Aberdeen, Cruickshank Building, Aberdeen, AB24 3UU, United Kingdom. 10 Department of Marine Microbiology and Biogeochemistry, Royal Netherlands Institute for Sea Research, Utrecht University, 1790 AB Den Burg, Texel, The Netherlands #Corresponding author. Tel.: + 49 421 218 65747. Fax: +49 421 218 65715. E-mail: [email protected] +present address: Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA. -
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 -
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. -
Isolation and Characterization of Methanohalophilus Portucalensis Sp
INTERNATIONALJOURNAL OF SYSTEMATICBACTERIOLOGY, July 1993, p. 430-437 Vol. 43, No. 3 0020-7713/93/030430-08$02.00/0 Copyright 0 1993, International Union of Microbiological Societies Isolation and Characterization of Methanohalophilus portucalensis sp. nov. and DNA Reassociation Study of the Genus Methanohalophilus DAVID R. BOONE,ly2* INDRA M. MATHRLWI,~?YITAT LIU,l JOSE A. G. F. MENAIA,1-4 ROBERT A. AND JANE E. BOONE' Departments of Environmental Science and Engineering' and Chemical and Biological Sciences, Oregon Graduate Institute of Science & Technology, 19600 N. W. von Neumann Drive, Beaverton, Oregon 97006- 1999; School of Public Health, University of California, Los Angeles, California 900243; and Laboratbrio Nacional de Engenharia e Tecnologia Industrial, Estrada das Palmeiras, 2745 Queluz, Portugal4 Six strains of coccoid, halophilic methanogens were isolated from various salinaria and natural hypersaline environments. These isolates (strains FDF-lT [T = type strain], FDF-2, SF-2, Ret-1, SD-1, and Cas-1) grew on media containing methanol and mono-, di-, and trimethylamines as catabolic substrates, but not on media containing dimethyl sulfide, methane thiol, H,, formate, or acetate; when cells were provided with H, in addition to methanol or trimethylamine, they grew on the medium containing a methyl substrate but did not catabolize H,. All of the strains were capable of growth in mineral medium to which trimethylamine was added as a catabolic substrate, although some strains were greatly stimulated by biotin or p-aminobenzoate. DNA reassociation and denaturing electrophoresis of whole-cell proteins indicated that strains FDF-lT, FDF-2, SF-2, and Ret-1, together with previously described strains SF-1, 2-7302, 2-7401, 2-7404, and 2-7405, belong to a new taxon named Methunohalophilzuportucalensis sp. -
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. -
Miniaturized Biosignature Analysis Reveals Implications for the Formation of Cold Seep Carbonates at Hydrate Ridge (Off Oregon, USA) T
Miniaturized biosignature analysis reveals implications for the formation of cold seep carbonates at Hydrate Ridge (off Oregon, USA) T. Leefmann, J. Bauermeister, A. Kronz, V. Liebetrau, J. Reitner, V. Thiel To cite this version: T. Leefmann, J. Bauermeister, A. Kronz, V. Liebetrau, J. Reitner, et al.. Miniaturized biosignature analysis reveals implications for the formation of cold seep carbonates at Hydrate Ridge (off Oregon, USA). Biogeosciences Discussions, European Geosciences Union, 2007, 4 (6), pp.4443-4458. hal- 00297947 HAL Id: hal-00297947 https://hal.archives-ouvertes.fr/hal-00297947 Submitted on 28 Nov 2007 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Biogeosciences Discuss., 4, 4443–4458, 2007 Biogeosciences www.biogeosciences-discuss.net/4/4443/2007/ Discussions BGD © Author(s) 2007. This work is licensed 4, 4443–4458, 2007 under a Creative Commons License. Biogeosciences Discussions is the access reviewed discussion forum of Biogeosciences Biosignature analysis of cold seep carbonates T. Leefmann et al. Miniaturized biosignature analysis reveals Title Page implications for the formation of cold Abstract Introduction seep carbonates at Hydrate Ridge Conclusions References (off Oregon, USA) Tables Figures T. Leefmann1, J. Bauermeister1, A. Kronz1, V. -
Differences in Lateral Gene Transfer in Hypersaline Versus Thermal Environments Matthew E Rhodes1*, John R Spear2, Aharon Oren3 and Christopher H House1
Rhodes et al. BMC Evolutionary Biology 2011, 11:199 http://www.biomedcentral.com/1471-2148/11/199 RESEARCH ARTICLE Open Access Differences in lateral gene transfer in hypersaline versus thermal environments Matthew E Rhodes1*, John R Spear2, Aharon Oren3 and Christopher H House1 Abstract Background: The role of lateral gene transfer (LGT) in the evolution of microorganisms is only beginning to be understood. While most LGT events occur between closely related individuals, inter-phylum and inter-domain LGT events are not uncommon. These distant transfer events offer potentially greater fitness advantages and it is for this reason that these “long distance” LGT events may have significantly impacted the evolution of microbes. One mechanism driving distant LGT events is microbial transformation. Theoretically, transformative events can occur between any two species provided that the DNA of one enters the habitat of the other. Two categories of microorganisms that are well-known for LGT are the thermophiles and halophiles. Results: We identified potential inter-class LGT events into both a thermophilic class of Archaea (Thermoprotei) and a halophilic class of Archaea (Halobacteria). We then categorized these LGT genes as originating in thermophiles and halophiles respectively. While more than 68% of transfer events into Thermoprotei taxa originated in other thermophiles, less than 11% of transfer events into Halobacteria taxa originated in other halophiles. Conclusions: Our results suggest that there is a fundamental difference between LGT in thermophiles and halophiles. We theorize that the difference lies in the different natures of the environments. While DNA degrades rapidly in thermal environments due to temperature-driven denaturization, hypersaline environments are adept at preserving DNA. -
Halophilic Methylotrophic Methanogens May Contribute to the High Ammonium Concentrations Found in Shale Oil and Shale Gas Reservoirs
ORIGINAL RESEARCH published: 07 March 2019 doi: 10.3389/fenrg.2019.00023 Halophilic Methylotrophic Methanogens May Contribute to the High Ammonium Concentrations Found in Shale Oil and Shale Gas Reservoirs Biwen Annie An 1,2*, Yin Shen 2, Johanna Voordouw 2 and Gerrit Voordouw 2 1 Division 4.1 Biodeterioration and Reference Organisms, Federal Institute for Materials Research and Testing, Berlin, Germany, 2 Petroleum Microbiology Research Group, Department of Biological Sciences, University of Calgary, Calgary, AB, Canada Flow-back and produced waters from shale gas and shale oil fields contain high ammonium, which can be formed by methanogenic degradation of methylamines Edited by: into methane and ammonium. Methylamines are added to fracturing fluid to prevent Claire Dumas, clay swelling or can originate from metabolism of the osmolyte triglycinebetaine (GB). Institut National de la Recherche We analyzed field samples from a shale gas reservoir in the Duvernay formation Agronomique (INRA), France Reviewed by: and from a shale oil reservoir in the Bakken formation in Canada to determine the Qaisar Mahmood, origin of high ammonium. Fresh waters used to make fracturing fluid, early flow-back COMSATS University Islamabad, waters, and late flow back waters from the shale gas reservoir had increasing salinity Pakistan Mohanakrishna Gunda, of 0.01, 0.58, and 2.66 Meq of NaCl, respectively. Microbial community analyses Qatar University, Qatar reflected this fresh water to saline transition with halophilic taxa including Halomonas, Jorge Gonzalez-Estrella, Halanaerobium, and Methanohalophilus being increasingly present. Early and late University of New Mexico, United States flow-back waters had high ammonium concentrations of 32 and 15 mM, respectively. -
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. -
A Systematic Approach Re-Analyzing the Effects of Temperature
www.nature.com/scientificreports OPEN A systematic approach re-analyzing the efects of temperature disturbance on the microbial Received: 12 September 2018 Accepted: 12 April 2019 community of mesophilic anaerobic Published: xx xx xxxx digestion Grace Tzun-Wen Shaw , Chieh-Yin Weng, Cheng-Yu Chen , Francis Cheng-Hsuan Weng & Daryi Wang Microbial communities are key drivers of ecosystem processes, but their behavior in disturbed environments is difcult to measure. How microbial community composition and function respond disturbances is a common challenge in biomedical, environmental, agricultural, and bioenergy research. A novel way to solve this problem is to use a systems-level perspective and describe microbial communities as networks. Based on a mesophilic anaerobic digestion system of swine manure as a tool, we propose a simple framework to investigate changes in microbial communities via compositions, metabolic pathways, genomic properties and interspecies relationships in response to a long-term temperature disturbance. After temperature disturbance, microbial communities tend towards a competitive interaction network with higher GC content and larger genome size. Based on microbial interaction networks, communities responded to the disturbance by showing a transition from acetotrophic (Methanotrichaceae and Methanosarcinaceae) to methylotrophic methanogens (Methanomassiliicoccaceae and Methanobacteriaceae) and a fuctuation in rare biosphere taxa. To conclude, this study may be important for exploring the dynamic relationships between disturbance and microbial communities as a whole, as well as for providing researchers with a better understanding of how changes in microbial communities relate to ecological processes. Environmental disturbances are important factors in shaping the structure of plant, animal or microbial pop- ulations. In the past few decades, remarkable progress has been made towards understanding how disturbance afects microbial composition, biodiversity loss and ecological processes1–5.