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Ellenbogen JB, Borton MA, McGivern BB, Cronin DR, Hoyt DW, Freire-Zapata V, McCalley CK, Varner RK, Crill PM, Wehr RA, Chanton JP, Woodcroft BJ, Tfaily MM, Tyson GW, Rich VI, Wrighton KC. Methylotrophy in the Mire: direct and indirect routes for methane production in thawing permafrost. mSystems 2024; 9:e0069823. [PMID: 38063415 PMCID: PMC10805028 DOI: 10.1128/msystems.00698-23] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/06/2023] [Accepted: 10/24/2023] [Indexed: 01/24/2024] Open
Abstract
While wetlands are major sources of biogenic methane (CH4), our understanding of resident microbial metabolism is incomplete, which compromises the prediction of CH4 emissions under ongoing climate change. Here, we employed genome-resolved multi-omics to expand our understanding of methanogenesis in the thawing permafrost peatland of Stordalen Mire in Arctic Sweden. In quadrupling the genomic representation of the site's methanogens and examining their encoded metabolism, we revealed that nearly 20% of the metagenome-assembled genomes (MAGs) encoded the potential for methylotrophic methanogenesis. Further, 27% of the transcriptionally active methanogens expressed methylotrophic genes; for Methanosarcinales and Methanobacteriales MAGs, these data indicated the use of methylated oxygen compounds (e.g., methanol), while for Methanomassiliicoccales, they primarily implicated methyl sulfides and methylamines. In addition to methanogenic methylotrophy, >1,700 bacterial MAGs across 19 phyla encoded anaerobic methylotrophic potential, with expression across 12 phyla. Metabolomic analyses revealed the presence of diverse methylated compounds in the Mire, including some known methylotrophic substrates. Active methylotrophy was observed across all stages of a permafrost thaw gradient in Stordalen, with the most frozen non-methanogenic palsa found to host bacterial methylotrophy and the partially thawed bog and fully thawed fen seen to house both methanogenic and bacterial methylotrophic activities. Methanogenesis across increasing permafrost thaw is thus revised from the sole dominance of hydrogenotrophic production and the appearance of acetoclastic at full thaw to consider the co-occurrence of methylotrophy throughout. Collectively, these findings indicate that methanogenic and bacterial methylotrophy may be an important and previously underappreciated component of carbon cycling and emissions in these rapidly changing wetland habitats.IMPORTANCEWetlands are the biggest natural source of atmospheric methane (CH4) emissions, yet we have an incomplete understanding of the suite of microbial metabolism that results in CH4 formation. Specifically, methanogenesis from methylated compounds is excluded from all ecosystem models used to predict wetland contributions to the global CH4 budget. Though recent studies have shown methylotrophic methanogenesis to be active across wetlands, the broad climatic importance of the metabolism remains critically understudied. Further, some methylotrophic bacteria are known to produce methanogenic by-products like acetate, increasing the complexity of the microbial methylotrophic metabolic network. Prior studies of Stordalen Mire have suggested that methylotrophic methanogenesis is irrelevant in situ and have not emphasized the bacterial capacity for metabolism, both of which we countered in this study. The importance of our findings lies in the significant advancement toward unraveling the broader impact of methylotrophs in wetland methanogenesis and, consequently, their contribution to the terrestrial global carbon cycle.
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Affiliation(s)
- Jared B. Ellenbogen
- Department of Soil and Crop Science, Colorado State University, Fort Collins, Colorado, USA
| | - Mikayla A. Borton
- Department of Soil and Crop Science, Colorado State University, Fort Collins, Colorado, USA
| | - Bridget B. McGivern
- Department of Soil and Crop Science, Colorado State University, Fort Collins, Colorado, USA
| | - Dylan R. Cronin
- Department of Microbiology, The Ohio State University, Columbus, Ohio, USA
| | - David W. Hoyt
- Environmental Molecular Sciences Laboratory, Earth and Biological Sciences Division, Pacific Northwest National Laboratory, Richland, Washington, USA
| | | | - Carmody K. McCalley
- Gosnell School of Life Sciences, Rochester Institute of Technology, Rochester, New York, USA
| | - Ruth K. Varner
- Department of Earth Sciences and Institute for the Study of Earth, Oceans and Space, University of New Hampshire, Durham, New Hampshire, USA
| | - Patrick M. Crill
- Department of Geological Sciences, Bolin Center for Climate Research, Stockholm University, Stockholm, Sweden
| | - Richard A. Wehr
- Department of Ecology and Evolutionary Biology, University of Arizona, Tucson, Arizona, USA
| | - Jeffrey P. Chanton
- Earth Ocean and Atmospheric Sciences, Florida State University, Tallahassee, Florida, USA
| | - Ben J. Woodcroft
- Centre for Microbiome Research, School of Biomedical Sciences, Queensland University of Technology (QUT), Translational Research Institute, Woolloongabba, Queensland, Australia
| | - Malak M. Tfaily
- Department of Environmental Science, University of Arizona, Tucson, Arizona, USA
| | - Gene W. Tyson
- Centre for Microbiome Research, School of Biomedical Sciences, Queensland University of Technology (QUT), Translational Research Institute, Woolloongabba, Queensland, Australia
| | - Virginia I. Rich
- Department of Microbiology, The Ohio State University, Columbus, Ohio, USA
| | - Kelly C. Wrighton
- Department of Soil and Crop Science, Colorado State University, Fort Collins, Colorado, USA
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Ruiz-Perez D, Gimon I, Sazal M, Mathee K, Narasimhan G. Unfolding and De-confounding: Biologically meaningful causal inference from longitudinal multi-omic networks using METALICA. BIORXIV : THE PREPRINT SERVER FOR BIOLOGY 2023:2023.12.12.571384. [PMID: 38168315 PMCID: PMC10760167 DOI: 10.1101/2023.12.12.571384] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/05/2024]
Abstract
A key challenge in the analysis of microbiome data is the integration of multi-omic datasets and the discovery of interactions between microbial taxa, their expressed genes, and the metabolites they consume and/or produce. In an effort to improve the state-of-the-art in inferring biologically meaningful multi-omic interactions, we sought to address some of the most fundamental issues in causal inference from longitudinal multi-omics microbiome data sets. We developed METALICA, a suite of tools and techniques that can infer interactions between microbiome entities. METALICA introduces novel unrolling and de-confounding techniques used to uncover multi-omic entities that are believed to act as confounders for some of the relationships that may be inferred using standard causal inferencing tools. The results lend support to predictions about biological models and processes by which microbial taxa interact with each other in a microbiome. The unrolling process helps to identify putative intermediaries (genes and/or metabolites) to explain the interactions between microbes; the de-confounding process identifies putative common causes that may lead to spurious relationships to be inferred. METALICA was applied to the networks inferred by existing causal discovery and network inference algorithms applied to a multi-omics data set resulting from a longitudinal study of IBD microbiomes. The most significant unrollings and de-confoundings were manually validated using the existing literature and databases.
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Affiliation(s)
- Daniel Ruiz-Perez
- Bioinformatics Research Group (BioRG), Florida International University, Miami, FL 33199, USA
| | - Isabella Gimon
- Bioinformatics Research Group (BioRG), Florida International University, Miami, FL 33199, USA
| | - Musfiqur Sazal
- Bioinformatics Research Group (BioRG), Florida International University, Miami, FL 33199, USA
| | - Kalai Mathee
- Florida International University, Miami, FL 33199, USA
- Biomolecular Sciences Institute, Florida International University, Miami, FL 33199, USA
| | - Giri Narasimhan
- Bioinformatics Research Group (BioRG), Florida International University, Miami, FL 33199, USA
- Biomolecular Sciences Institute, Florida International University, Miami, FL 33199, USA
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3
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Abdel Azim A, Vizzarro A, Bellini R, Bassani I, Baudino L, Pirri CF, Verga F, Lamberti A, Menin B. Perspective on the use of methanogens in lithium recovery from brines. Front Microbiol 2023; 14:1233221. [PMID: 37601371 PMCID: PMC10434214 DOI: 10.3389/fmicb.2023.1233221] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/01/2023] [Accepted: 07/19/2023] [Indexed: 08/22/2023] Open
Abstract
Methanogenic archaea stand out as multipurpose biocatalysts for different applications in wide-ranging industrial sectors due to their crucial role in the methane (CH4) cycle and ubiquity in natural environments. The increasing demand for raw materials required by the manufacturing sector (i.e., metals-, concrete-, chemicals-, plastic- and lubricants-based industries) represents a milestone for the global economy and one of the main sources of CO2 emissions. Recovery of critical raw materials (CRMs) from byproducts generated along their supply chain, rather than massive mining operations for mineral extraction and metal smelting, represents a sustainable choice. Demand for lithium (Li), included among CRMs in 2023, grew by 17.1% in the last decades, mostly due to its application in rechargeable lithium-ion batteries. In addition to mineral deposits, the natural resources of Li comprise water, ranging from low Li concentrations (seawater and freshwater) to higher ones (salt lakes and artificial brines). Brines from water desalination can be high in Li content which can be recovered. However, biological brine treatment is not a popular methodology. The methanogenic community has already demonstrated its ability to recover several CRMs which are not essential to their metabolism. Here, we attempt to interconnect the well-established biomethanation process with Li recovery from brines, by analyzing the methanogenic species which may be suitable to grow in brine-like environments and the corresponding mechanism of recovery. Moreover, key factors which should be considered to establish the techno-economic feasibility of this process are here discussed.
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Affiliation(s)
- Annalisa Abdel Azim
- Centre for Sustainable Future Technologies, Fondazione Istituto Italiano di Tecnologia, Turin, Italy
| | - Arianna Vizzarro
- Centre for Sustainable Future Technologies, Fondazione Istituto Italiano di Tecnologia, Turin, Italy
- Department of Environment, Land and Infrastructure Engineering, Politecnico di Torino, Turin, Italy
| | - Ruggero Bellini
- Centre for Sustainable Future Technologies, Fondazione Istituto Italiano di Tecnologia, Turin, Italy
| | - Ilaria Bassani
- Centre for Sustainable Future Technologies, Fondazione Istituto Italiano di Tecnologia, Turin, Italy
| | - Luisa Baudino
- Department of Applied Science and Technology, Politecnico di Torino, Turin, Italy
| | - Candido Fabrizio Pirri
- Centre for Sustainable Future Technologies, Fondazione Istituto Italiano di Tecnologia, Turin, Italy
- Department of Applied Science and Technology, Politecnico di Torino, Turin, Italy
| | - Francesca Verga
- Department of Environment, Land and Infrastructure Engineering, Politecnico di Torino, Turin, Italy
| | - Andrea Lamberti
- Centre for Sustainable Future Technologies, Fondazione Istituto Italiano di Tecnologia, Turin, Italy
- Department of Applied Science and Technology, Politecnico di Torino, Turin, Italy
| | - Barbara Menin
- Centre for Sustainable Future Technologies, Fondazione Istituto Italiano di Tecnologia, Turin, Italy
- Istituto di Biologia e Biotecnologia Agraria, Consiglio Nazionale Delle Ricerche, Milan, Italy
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Webster G, Cragg BA, Rinna J, Watkins AJ, Sass H, Weightman AJ, Parkes RJ. Methanogen activity and microbial diversity in Gulf of Cádiz mud volcano sediments. Front Microbiol 2023; 14:1157337. [PMID: 37293223 PMCID: PMC10244519 DOI: 10.3389/fmicb.2023.1157337] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/02/2023] [Accepted: 05/09/2023] [Indexed: 06/10/2023] Open
Abstract
The Gulf of Cádiz is a tectonically active continental margin with over sixty mud volcanoes (MV) documented, some associated with active methane (CH4) seepage. However, the role of prokaryotes in influencing this CH4 release is largely unknown. In two expeditions (MSM1-3 and JC10) seven Gulf of Cádiz MVs (Porto, Bonjardim, Carlos Ribeiro, Captain Arutyunov, Darwin, Meknes, and Mercator) were analyzed for microbial diversity, geochemistry, and methanogenic activity, plus substrate amended slurries also measured potential methanogenesis and anaerobic oxidation of methane (AOM). Prokaryotic populations and activities were variable in these MV sediments reflecting the geochemical heterogeneity within and between them. There were also marked differences between many MV and their reference sites. Overall direct cell numbers below the SMTZ (0.2-0.5 mbsf) were much lower than the general global depth distribution and equivalent to cell numbers from below 100 mbsf. Methanogenesis from methyl compounds, especially methylamine, were much higher than the usually dominant substrates H2/CO2 or acetate. Also, CH4 production occurred in 50% of methylated substrate slurries and only methylotrophic CH4 production occurred at all seven MV sites. These slurries were dominated by Methanococcoides methanogens (resulting in pure cultures), and prokaryotes found in other MV sediments. AOM occurred in some slurries, particularly, those from Captain Arutyunov, Mercator and Carlos Ribeiro MVs. Archaeal diversity at MV sites showed the presence of both methanogens and ANME (Methanosarcinales, Methanococcoides, and ANME-1) related sequences, and bacterial diversity was higher than archaeal diversity, dominated by members of the Atribacterota, Chloroflexota, Pseudomonadota, Planctomycetota, Bacillota, and Ca. "Aminicenantes." Further work is essential to determine the full contribution of Gulf of Cádiz mud volcanoes to the global methane and carbon cycles.
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Affiliation(s)
- Gordon Webster
- Microbiomes, Microbes and Informatics Group, School of Biosciences, Cardiff University, Cardiff, Wales, United Kingdom
- School of Earth and Environmental Sciences, Cardiff University, Cardiff, Wales, United Kingdom
| | - Barry A. Cragg
- School of Earth and Environmental Sciences, Cardiff University, Cardiff, Wales, United Kingdom
| | - Joachim Rinna
- School of Earth and Environmental Sciences, Cardiff University, Cardiff, Wales, United Kingdom
- Aker BP ASA, Lysaker, Norway
| | - Andrew J. Watkins
- School of Earth and Environmental Sciences, Cardiff University, Cardiff, Wales, United Kingdom
- The Wales Research and Diagnostic Positron Emission Tomography Imaging Centre (PETIC), School of Medicine, Cardiff University, University Hospital of Wales, Cardiff, Wales, United Kingdom
| | - Henrik Sass
- School of Earth and Environmental Sciences, Cardiff University, Cardiff, Wales, United Kingdom
| | - Andrew J. Weightman
- Microbiomes, Microbes and Informatics Group, School of Biosciences, Cardiff University, Cardiff, Wales, United Kingdom
| | - R. John Parkes
- School of Earth and Environmental Sciences, Cardiff University, Cardiff, Wales, United Kingdom
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5
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Boltyanskaya YV, Kevbrin VV, Grouzdev DS, Detkova EN, Koziaeva VV, Novikov AA, Zhilina TN. Halonatronomonas betaini gen. nov., sp. nov., a haloalkaliphilic isolate from soda lake capable of betaine degradation and proposal of Halarsenatibacteraceae fam. nov. and Halothermotrichaceae fam. nov. within the order Halanaerobiales. Syst Appl Microbiol 2023; 46:126407. [PMID: 36906934 DOI: 10.1016/j.syapm.2023.126407] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/20/2022] [Revised: 02/11/2023] [Accepted: 02/22/2023] [Indexed: 02/27/2023]
Abstract
A search for the organisms responsible for anaerobic betaine degradation in soda lakes resulted in isolation of a novel bacterial strain, designated Z-7014T. The cells were Gram-stain-negative, non-endospore-forming rods. Growth occurred at 8-52 °C (optimum 40-45 °C), pH 7.1-10.1 (optimum pH 8.1-8.8) and 1.0-3.5 M Na+ (optimum 1.8 M), i.e. it can be regarded as a haloalkaliphile. The strain utilized a limited range of substrates, mostly peptonaceous but not amino acids, and was able to degrade betaine. Growth on betaine occurred only in the presence of peptonaceous substances which could not be replaced by vitamins. The G + C content of the genomic DNA of strain Z-7014T was 36.1 mol%. The major cellular fatty acids (>5% of the total) were C16:0 DMA, C18: 0 DMA, C16:1ω8, C16:0, C18:1 DMA, C16:1 DMA, C18:1ω9, and C18:0. Phylogenetic analysis of the 16S rRNA gene sequence revealed that strain Z-7014T formed a distinct evolutionary lineage in the order Halanaerobiales with the highest similarity to Halarsenitibacter silvermanii SLAS-1T (83.6%), Halothermothrix orenii H168T (85.6%), and Halocella cellulosilytica DSM 7362T (85.6%). AAI and POCP values between strain Z-7014T and type strains of the order Halanaerobiales were 51.7-57.8%, and 33.8-58.3%, respectively. Based on polyphasic results including phylogenomic data, the novel strain could be distinguished from other genera, which suggests that strain Z-7014T represents a novel species of a new genus, for which the name Halonatronomonas betaini gen. nov., sp. nov. is proposed. The type strain is Z-7014T (=KCTC 25237T = VKM B-3506T). On the basis of phylogenomic data, it is also proposed to evolve two novel families Halarsenitibacteraceae fam. nov. and Halothermotrichaceae fam. nov. within the current order Halanaerobiales.
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Affiliation(s)
- Yulia V Boltyanskaya
- Winogradsky Institute of Microbiology, Research Center of Biotechnology of the Russian Academy of Sciences, 33, bld. 2, Leninsky Ave., Moscow 119071, Russia
| | - Vadim V Kevbrin
- Winogradsky Institute of Microbiology, Research Center of Biotechnology of the Russian Academy of Sciences, 33, bld. 2, Leninsky Ave., Moscow 119071, Russia.
| | | | - Ekaterina N Detkova
- Winogradsky Institute of Microbiology, Research Center of Biotechnology of the Russian Academy of Sciences, 33, bld. 2, Leninsky Ave., Moscow 119071, Russia
| | - Veronika V Koziaeva
- Institute of Bioengineering, Research Center of Biotechnology of the Russian Academy of Sciences, 33, bld. 2, Leninsky Ave., Moscow 119071, Russia
| | | | - Tatjana N Zhilina
- Winogradsky Institute of Microbiology, Research Center of Biotechnology of the Russian Academy of Sciences, 33, bld. 2, Leninsky Ave., Moscow 119071, Russia
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6
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Pardo Z, Mateos I, Saro C, Campos R, Argüello H, Lachica M, Ranilla MJ, Fernández-Fígares I. The Effect of Supplementation with Betaine and Zinc on In Vitro Large Intestinal Fermentation in Iberian Pigs under Heat Stress. Animals (Basel) 2023; 13:ani13061102. [PMID: 36978642 PMCID: PMC10044697 DOI: 10.3390/ani13061102] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/19/2023] [Revised: 03/03/2023] [Accepted: 03/15/2023] [Indexed: 03/22/2023] Open
Abstract
We investigated the effects of betaine and zinc on the in vitro fermentation of pigs under heat stress (HS). Twenty-four Iberian pigs (43.4 ± 1.2 kg) under HS (30 °C) were assigned to treatments for 4 weeks: control (unsupplemented), betaine (5 g/kg), and zinc (0.120 g/kg) supplemented diet. Rectal content was used as the inoculum in 24-hincubations with pure substrates (starch, pectin, inulin, cellulose). Total gas, short-chain fatty acid (SCFA), and methane production and ammonia concentration were measured. The abundance of total bacteria and several bacterial groups was assessed. Betaine increased the acetate production with pectin and inulin, butyrate production with starch and inulin, and ammonia concentration, and decreased propionate production with pectin and inulin. The abundance of Bifidobacterium and two groups of Clostridium decreased with betaine supplementation. Zinc decreased the production of SCFA and gas with starch and inulin, associated with diminished bacterial activity. Propionate production decreased with starch, pectin, and inulin while butyrate production increased with inulin, and isoacid production increased with cellulose and inulin in pigs supplemented with zinc. The ammonia concentration increased for all substrates. The Clostridium cluster XIV abundance decreased in pigs fed zinc supplemented diets. The results reported were dependent on the substrate fermented, but the augmented butyrate production with both betaine and zinc could be of benefit for the host.
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Affiliation(s)
- Zaira Pardo
- Departamento de Nutrición y Producción Animal Sostenible, Estación Experimental del Zaidín, Consejo Superior de Investigaciones Científicas, (CSIC) Profesor Albareda 1, 18008 Granada, Spain
| | - Iván Mateos
- Departamento de Producción Animal, Universidad de León, Campus de Vegazana s/n, 24071 León, Spain
- Instituto de Ganadería de Montaña, CSIC-Universidad de León, Finca Marzanas s/n, Grulleros, 24346 León, Spain
| | - Cristina Saro
- Departamento de Producción Animal, Universidad de León, Campus de Vegazana s/n, 24071 León, Spain
- Instituto de Ganadería de Montaña, CSIC-Universidad de León, Finca Marzanas s/n, Grulleros, 24346 León, Spain
| | - Rómulo Campos
- Departamento de Producción Animal, Universidad de León, Campus de Vegazana s/n, 24071 León, Spain
- Departamento de Ciencia Animal, Universidad Nacional de Colombia, Carrera 32 # 12-00, Palmira 76531, Colombia
| | - Héctor Argüello
- Departamento de Sanidad Animal, Universidad de León, Campus de Vegazana s/n, 24071 León, Spain
| | - Manuel Lachica
- Departamento de Nutrición y Producción Animal Sostenible, Estación Experimental del Zaidín, Consejo Superior de Investigaciones Científicas, (CSIC) Profesor Albareda 1, 18008 Granada, Spain
| | - María José Ranilla
- Departamento de Producción Animal, Universidad de León, Campus de Vegazana s/n, 24071 León, Spain
- Instituto de Ganadería de Montaña, CSIC-Universidad de León, Finca Marzanas s/n, Grulleros, 24346 León, Spain
| | - Ignacio Fernández-Fígares
- Departamento de Nutrición y Producción Animal Sostenible, Estación Experimental del Zaidín, Consejo Superior de Investigaciones Científicas, (CSIC) Profesor Albareda 1, 18008 Granada, Spain
- Correspondence: or
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7
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Holland SI, Vázquez-Campos X, Ertan H, Edwards RJ, Manefield MJ, Lee M. Metaproteomics reveals methyltransferases implicated in dichloromethane and glycine betaine fermentation by ' Candidatus Formimonas warabiya' strain DCMF. Front Microbiol 2022; 13:1035247. [PMID: 36569084 PMCID: PMC9768040 DOI: 10.3389/fmicb.2022.1035247] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/02/2022] [Accepted: 11/15/2022] [Indexed: 12/12/2022] Open
Abstract
Dichloromethane (DCM; CH2Cl2) is a widespread pollutant with anthropogenic and natural sources. Anaerobic DCM-dechlorinating bacteria use the Wood-Ljungdahl pathway, yet dechlorination reaction mechanisms remain unclear and the enzyme(s) responsible for carbon-chlorine bond cleavage have not been definitively identified. Of the three bacterial taxa known to carry out anaerobic dechlorination of DCM, 'Candidatus Formimonas warabiya' strain DCMF is the only organism that can also ferment non-chlorinated substrates, including quaternary amines (i.e., choline and glycine betaine) and methanol. Strain DCMF is present within enrichment culture DFE, which was derived from an organochlorine-contaminated aquifer. We utilized the metabolic versatility of strain DCMF to carry out comparative metaproteomics of cultures grown with DCM or glycine betaine. This revealed differential abundance of numerous proteins, including a methyltransferase gene cluster (the mec cassette) that was significantly more abundant during DCM degradation, as well as highly conserved amongst anaerobic DCM-degrading bacteria. This lends strong support to its involvement in DCM dechlorination. A putative glycine betaine methyltransferase was also discovered, adding to the limited knowledge about the fate of this widespread osmolyte in anoxic subsurface environments. Furthermore, the metagenome of enrichment culture DFE was assembled, resulting in five high quality and two low quality draft metagenome-assembled genomes. Metaproteogenomic analysis did not reveal any genes or proteins for utilization of DCM or glycine betaine in the cohabiting bacteria, supporting the previously held idea that they persist via necromass utilization.
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Affiliation(s)
- Sophie I. Holland
- Water Research Centre, School of Civil and Environmental Engineering, University of New South Wales, Sydney, NSW, Australia
| | - Xabier Vázquez-Campos
- School of Biotechnology and Biomolecular Sciences, University of New South Wales, Sydney, NSW, Australia
| | - Haluk Ertan
- School of Chemical Engineering, University of New South Wales, Sydney, NSW, Australia,Department of Molecular Biology and Genetics, Istanbul University, Istanbul, Turkey
| | - Richard J. Edwards
- School of Biotechnology and Biomolecular Sciences, University of New South Wales, Sydney, NSW, Australia
| | - Michael J. Manefield
- Water Research Centre, School of Civil and Environmental Engineering, University of New South Wales, Sydney, NSW, Australia,School of Chemical Engineering, University of New South Wales, Sydney, NSW, Australia
| | - Matthew Lee
- Water Research Centre, School of Civil and Environmental Engineering, University of New South Wales, Sydney, NSW, Australia,*Correspondence: Matthew Lee,
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8
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Sorokin DY, Merkel AY, Abbas B. Ecology of Methanonatronarchaeia. Environ Microbiol 2022; 24:5217-5229. [PMID: 35726892 PMCID: PMC9796771 DOI: 10.1111/1462-2920.16108] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/28/2022] [Accepted: 06/19/2022] [Indexed: 01/07/2023]
Abstract
Methanonatronarchaeia represents a deep-branching phylogenetic lineage of extremely halo(alkali)philic and moderately thermophilic methyl-reducing methanogens belonging to the phylum Halobacteriota. It includes two genera, the alkaliphilic Methanonatronarchaeum and the neutrophilic Ca. Methanohalarchaeum. The former is represented by multiple closely related pure culture isolates from hypersaline soda lakes, while the knowledge about the latter is limited to a few mixed cultures with anaerobic haloarchaea. To get more insight into the distribution and ecophysiology of this enigmatic group of extremophilic methanogens, potential activity tests and enrichment cultivation with different substrates and at different conditions were performed with anaerobic sediment slurries from various hypersaline lakes in Russia. Methanonatronarchaeum proliferated exclusively in hypersaline soda lake samples mostly at elevated temperature, while at mesophilic conditions it coexisted with the extremely salt-tolerant methylotroph Methanosalsum natronophilum. Methanonatronarchaeum was also able to serve as a methylotrophic or hydrogenotrophic partner in several thermophilic enrichment cultures with fermentative bacteria. Ca. Methanohalarchaeum did not proliferate at mesophilic conditions and at thermophilic conditions it competed with extremely halophilic and moderately thermophilic methylotroph Methanohalobium, which it outcompeted at a combination of elevated temperature and methyl-reducing conditions. Overall, the results demonstrated that Methanonatronarchaeia are specialized extremophiles specifically proliferating in conditions of elevated temperature coupled with extreme salinity and simultaneous availability of a wide range of C1 -methylated compounds and H2 /formate.
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Affiliation(s)
- Dimitry Y. Sorokin
- Winogradsky Institute of Microbiology, Research Centre of BiotechnologyRussian Academy of SciencesMoscowRussia,Department of BiotechnologyDelft University of BiotechnologyDelftThe Netherlands
| | - Alexander Y. Merkel
- Winogradsky Institute of Microbiology, Research Centre of BiotechnologyRussian Academy of SciencesMoscowRussia
| | - Ben Abbas
- Department of BiotechnologyDelft University of BiotechnologyDelftThe Netherlands
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9
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Differences in the methanogen community between the nearshore and offshore sediments of the South Yellow Sea. J Microbiol 2022; 60:814-822. [DOI: 10.1007/s12275-022-2022-2] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/18/2022] [Revised: 05/10/2022] [Accepted: 05/11/2022] [Indexed: 10/17/2022]
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10
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Liang L, Sun Y, Dong Y, Ahmad T, Chen Y, Wang J, Wang F. Methanococcoides orientis sp. nov., a methylotrophic methanogen isolated from sediment of the East China Sea. Int J Syst Evol Microbiol 2022; 72. [DOI: 10.1099/ijsem.0.005384] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/18/2022] Open
Abstract
A novel methylotrophic methanogen Methanococcoides orientis sp. nov. was isolated from East China Sea sediment. Type strain LMO-1T of Methanococcoides orientis sp. nov. was irregular 1–2 µm cocci without flagella. Strain LMO-1T could utilize a variety of methylated compounds including methanol, methylamine, dimethylamine and trimethylamine for growth and methanogenesis, while H2/CO2 or acetate could not be used for growth or methanogenesis. Optimum growth temperature was 30–35 °C, optimum pH range for growth was 7.0–7.5, while the optimum salinity spectrum for growth was 1.0%–5.0% NaCl. Based on 16S rRNA gene similarity, strain LMO-1T belongs to
Methanococcoides
, with the highest sequence similarity to
Methanococcoides methylutens
DSM 2657T (99.8 %),
Methanococcoides vulcani
SLH33T(99.4 %), followed by
Methanococcoides alaskense
AK-5T(98.1 %),
Methanococcoides burtonii
DSM 6242T (98.0 %). Digital DNA–DNA hybridization also showed highest similarity with
Methanococcoides methylutens
DSM 2657T, with the value of 58.4 %. The average nucleotide identity between strain LMO-1T and
Methanococcoides methylutens
DSM 2657T was 94.06 %. In summary, LMO-1T represents a novel species of the genus Methaococcoides, for which the name Methanococcoides orientis sp. nov. is proposed. The type strain is LMO-1T (=MCCC 4K00106T=JCM 39195T).
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Affiliation(s)
- Lewen Liang
- State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai, 200240, PR China
| | - Yu Sun
- School of Oceanography, Shanghai Jiao Tong University, Shanghai, 200240, PR China
| | - Yijing Dong
- School of Physics and Astronomy, Shanghai Jiao Tong University, Shanghai, 200240, PR China
| | - Tariq Ahmad
- State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai, 200240, PR China
| | - Yifan Chen
- State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai, 200240, PR China
| | - Jing Wang
- School of Oceanography, Shanghai Jiao Tong University, Shanghai, 200240, PR China
| | - Fengping Wang
- School of Oceanography, Shanghai Jiao Tong University, Shanghai, 200240, PR China
- State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai, 200240, PR China
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11
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Chen Y, Wu N, Liu C, Mi T, Li J, He X, Li S, Sun Z, Zhen Y. Methanogenesis pathways of methanogens and their responses to substrates and temperature in sediments from the South Yellow Sea. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 815:152645. [PMID: 34998777 DOI: 10.1016/j.scitotenv.2021.152645] [Citation(s) in RCA: 7] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/29/2021] [Revised: 12/19/2021] [Accepted: 12/19/2021] [Indexed: 06/14/2023]
Abstract
Although coastal sediments are major contributors to the production of atmospheric methane, the effects of environmental conditions on methanogenesis and the community of methanogenic archaea are not well understood. Here, we investigated the methanogenesis pathways in nearshore and offshore sediments from the South Yellow Sea (SYS). Moreover, the effects of the supply of methanogenic substrates (H2/CO2, acetate, trimethylamine (TMA), and methanol) and temperature on methanogenesis and the community of methanogenic archaea were further determined. Methylotrophic, hydrogenotrophic and acetotrophic methanogenesis were found to be responsible for biogenic methane production in nearshore sediments. In the offshore sediments, methylotrophic methanogenesis was the predominant methanogenic pathway. The changes in methanogenic community structure under different substrate amendments were characterized. Lower diversities were detected in substrate-amended samples with methanogenic activity. Hydrogenotrophic Methanogenium, multitrophic Methanosarcina, methylotrophic Methanococcoide, Methanococcoide or methylotrophic Methanolobus were dominant in H2/CO2-, acetate-, TMA- and methanol-amended sediment slurries, respectively. PCoA showed that the methanogen community in H2/CO2 and acetate amendments exhibited greater differences than those in other treatments. Lower temperature (10 °C) limits hydrogenotrophic and acetoclastic methanogenesis, but methylotrophic methanogenesis is much less affected. The response of methanogen diversity to the incubation temperature varied among the different substrate-amended slurries. The multitrophic methanogen Methanosarcina became increasingly abundant in H2/CO2- and acetate-amended sediment slurries when the temperature increased from 10 to 30 °C.
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Affiliation(s)
- Ye Chen
- Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266237, China; Key Laboratory of Marine Environment and Ecology, Ocean University of China, Ministry of Education, Qingdao 266100, China; Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266071, China
| | - Nengyou Wu
- Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266237, China; College of Environmental Science and Engineering, Ocean University of China, Qingdao 266100, China; Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266071, China
| | - Changling Liu
- Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266237, China; Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266071, China
| | - Tiezhu Mi
- Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China; Key Laboratory of Marine Environment and Ecology, Ocean University of China, Ministry of Education, Qingdao 266100, China; College of Environmental Science and Engineering, Ocean University of China, Qingdao 266100, China
| | - Jing Li
- Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266237, China; Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266071, China
| | - Xingliang He
- Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266237, China; Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266071, China
| | - Siqi Li
- Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China; Key Laboratory of Marine Environment and Ecology, Ocean University of China, Ministry of Education, Qingdao 266100, China
| | - Zhilei Sun
- Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266237, China; Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266071, China
| | - Yu Zhen
- Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China; Key Laboratory of Marine Environment and Ecology, Ocean University of China, Ministry of Education, Qingdao 266100, China; College of Environmental Science and Engineering, Ocean University of China, Qingdao 266100, China.
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12
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Diverse methylotrophic methanogenic archaea cause high methane emissions from seagrass meadows. Proc Natl Acad Sci U S A 2022; 119:2106628119. [PMID: 35165204 PMCID: PMC8892325 DOI: 10.1073/pnas.2106628119] [Citation(s) in RCA: 14] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Accepted: 12/23/2021] [Indexed: 11/18/2022] Open
Abstract
Marine coastlines colonized by seagrasses are a net source of methane to the atmosphere. However, methane emissions from these environments are still poorly constrained, and the underlying processes and responsible microorganisms remain largely unknown. Here, we investigated methane turnover in seagrass meadows of Posidonia oceanica in the Mediterranean Sea. The underlying sediments exhibited median net fluxes of methane into the water column of ca. 106 µmol CH4 ⋅ m-2 ⋅ d-1 Our data show that this methane production was sustained by methylated compounds produced by the plant, rather than by fermentation of buried organic carbon. Interestingly, methane production was maintained long after the living plant died off, likely due to the persistence of methylated compounds, such as choline, betaines, and dimethylsulfoniopropionate, in detached plant leaves and rhizomes. We recovered multiple mcrA gene sequences, encoding for methyl-coenzyme M reductase (Mcr), the key methanogenic enzyme, from the seagrass sediments. Most retrieved mcrA gene sequences were affiliated with a clade of divergent Mcr and belonged to the uncultured Candidatus Helarchaeota of the Asgard superphylum, suggesting a possible involvement of these divergent Mcr in methane metabolism. Taken together, our findings identify the mechanisms controlling methane emissions from these important blue carbon ecosystems.
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13
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Medina-Chávez NO, Travisano M. Archaeal Communities: The Microbial Phylogenomic Frontier. Front Genet 2022; 12:693193. [PMID: 35154237 PMCID: PMC8826477 DOI: 10.3389/fgene.2021.693193] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/10/2021] [Accepted: 11/22/2021] [Indexed: 11/17/2022] Open
Abstract
Archaea are a unique system for investigating the diversity of life. There are the most diverse group of organisms with the longest evolutionary history of life on Earth. Phylogenomic investigations reveal the complex evolutionary history of Archaea, overturning longstanding views of the history of life. They exist in the harshest environments and benign conditions, providing a system to investigate the basis for living in extreme environments. They are frequently members of microbial communities, albeit generally rare. Archaea were central in the evolution of Eukaryotes and can be used as a proxy for studying life on other planets. Future advances will depend not only upon phylogenomic studies but also on a better understanding of isolation and cultivation techniques.
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Affiliation(s)
- Nahui Olin Medina-Chávez
- Ecology, Evolution and Behavior, University of Minnesota, St. Paul, MN, United States.,BioTechnology Institute, University of Minnesota, St. Paul, MN, United States
| | - Michael Travisano
- Ecology, Evolution and Behavior, University of Minnesota, St. Paul, MN, United States.,BioTechnology Institute, University of Minnesota, St. Paul, MN, United States.,Minnesota Center for the Philosophy of Science, University of Minnesota, Minneapolis, MN, United States
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14
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Bacteria and Archaea Synergistically Convert Glycine Betaine to Biogenic Methane in the Formosa Cold Seep of the South China Sea. mSystems 2021; 6:e0070321. [PMID: 34491083 PMCID: PMC8547467 DOI: 10.1128/msystems.00703-21] [Citation(s) in RCA: 9] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/20/2022] Open
Abstract
Cold seeps are globally widespread seafloor ecosystems that feature abundant methane production and flourishing chemotrophic benthic communities. Chemical evidence indicates that cold seep methane is largely biogenic; however, the primary methane-producing organisms and associated pathways involved in methanogenesis remain elusive. This work detected methane production when glycine betaine (GBT) or trimethylamine (TMA) was added to the sediment microcosms of the Formosa cold seep, South China Sea. The methane production was suppressed by antibiotic inhibition of bacteria, while GBT was accumulated. This suggests that the widely used osmoprotectant GBT could be converted to cold seep biogenic methane via the synergistic activity of bacteria and methanogenic archaea because archaea are not sensitive to antibiotics and no bacteria are known to produce ample methane (mM). 16S rRNA gene diversity analyses revealed that the predominant bacterial and archaeal genera in the GBT-amended methanogenic microcosms included Oceanirhabdus and Methanococcoides. Moreover, metagenomic analyses detected the presence of grdH and mtgB genes that are involved in GBT reduction and demethylation, respectively. Two novel species were obtained, including bacterium Oceanirhabdus seepicola, which reduces GBT to TMA, and a methanogenic archaeon, Methanococcoides seepicolus, which produces methane from TMA and GBT. The two strains reconstituted coculture efficiently converted GBT to methane at 18°C; however, at 4°C addition of dimethylglycine (DMG), the GBT demethylation product, was necessary. Therefore, this work demonstrated that GBT is the precursor not only of the biogenic methane but also of the cryoprotectant DMG to the microorganisms at the Formosa cold seep. IMPORTANCE Numerous cold seeps have been found in global continental margins where methane is enriched in pore waters that are forced upward from sediments. Therefore, high concerns have been focused on the methane-producing organisms and the metabolic pathways in these environments because methane is a potent greenhouse gas. In this study, GBT was identified as the main precursor for methane in the Formosa cold seep of the South China Sea. Further, synergism of bacteria and methanogenic archaea was identified in GBT conversion to methane via the GBT reduction pathway, while methanogen-mediated GBT demethylation to methane was also observed. In addition, GBT-demethylated product dimethyl glycine acted as a cryoprotectant that promoted the cold seep microorganisms at cold temperatures. GBT is an osmoprotectant that is widely used by marine organisms, and therefore, the GBT-derived methanogenic pathway reported here could be widely distributed among global cold seep environments.
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15
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Sorokin DY. Microbial Utilization of Glycine Betain in Hypersaline Soda Lakes. Microbiology (Reading) 2021. [DOI: 10.1134/s0026261721050143] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/23/2022] Open
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16
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Fischer PQ, Sánchez‐Andrea I, Stams AJM, Villanueva L, Sousa DZ. Anaerobic microbial methanol conversion in marine sediments. Environ Microbiol 2021; 23:1348-1362. [PMID: 33587796 PMCID: PMC8048578 DOI: 10.1111/1462-2920.15434] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/03/2020] [Revised: 02/09/2021] [Accepted: 02/10/2021] [Indexed: 01/15/2023]
Abstract
Methanol is an ubiquitous compound that plays a role in microbial processes as a carbon and energy source, intermediate in metabolic processes or as end product in fermentation. In anoxic environments, methanol can act as the sole carbon and energy source for several guilds of microorganisms: sulfate-reducing microorganisms, nitrate-reducing microorganisms, acetogens and methanogens. In marine sediments, these guilds compete for methanol as their common substrate, employing different biochemical pathways. In this review, we will give an overview of current knowledge of the various ways in which methanol reaches marine sediments, the ecology of microorganisms capable of utilizing methanol and their metabolism. Furthermore, through a metagenomic analysis, we shed light on the unknown diversity of methanol utilizers in marine sediments which is yet to be explored.
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Affiliation(s)
- Peter Q. Fischer
- Laboratory of MicrobiologyWageningen University & Research, Stippeneng 4Wageningen6708 WEThe Netherlands
- Department of Marine Microbiology and BiogeochemistryRoyal Netherlands Institute for Sea Research, P.O. Box 59Den BurgTexel7197 ABThe Netherlands
| | - Irene Sánchez‐Andrea
- Laboratory of MicrobiologyWageningen University & Research, Stippeneng 4Wageningen6708 WEThe Netherlands
| | - Alfons J. M. Stams
- Laboratory of MicrobiologyWageningen University & Research, Stippeneng 4Wageningen6708 WEThe Netherlands
- Centre of Biological EngineeringUniversity of Minho, Campus de GualtarBraga4710‐057Portugal
| | - Laura Villanueva
- Department of Marine Microbiology and BiogeochemistryRoyal Netherlands Institute for Sea Research, P.O. Box 59Den BurgTexel7197 ABThe Netherlands
- Faculty of GeosciencesUtrecht University, Princetonlaan 8aUtrecht3584 CBThe Netherlands
| | - Diana Z. Sousa
- Laboratory of MicrobiologyWageningen University & Research, Stippeneng 4Wageningen6708 WEThe Netherlands
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17
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Role of N, N-Dimethylglycine and Its Catabolism to Sarcosine in Chromohalobacter salexigens DSM 3043. Appl Environ Microbiol 2020; 86:AEM.01186-20. [PMID: 32631860 DOI: 10.1128/aem.01186-20] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/19/2020] [Accepted: 06/28/2020] [Indexed: 11/20/2022] Open
Abstract
Chromohalobacter salexigens DSM 3043 can grow on N,N-dimethylglycine (DMG) as the sole C, N, and energy source and utilize sarcosine as the sole N source under aerobic conditions. However, little is known about the genes and enzymes involved in the conversion of DMG to sarcosine in this strain. In the present study, gene disruption and complementation assays indicated that the csal_0990, csal_0991, csal_0992, and csal_0993 genes are responsible for DMG degradation to sarcosine. The csal_0990 gene heterologously expressed in Escherichia coli was proven to encode an unusual DMG dehydrogenase (DMGDH). The enzyme, existing as a monomer of 79 kDa with a noncovalently bound flavin adenine dinucleotide, utilized both DMG and sarcosine as substrates and exhibited dual coenzyme specificity, preferring NAD+ to NADP+ The optimum pH and temperature of enzyme activity were determined to be 7.0 and 60°C, respectively. Kinetic parameters of the enzyme toward its substrates were determined accordingly. Under high-salinity conditions, the presence of DMG inhibited growth of the wild type and induced the production and accumulation of trehalose and glucosylglycerate intracellularly. Moreover, exogenous addition of DMG significantly improved the growth rates of the four DMG- mutants (Δcsal_0990, Δcsal_0991, Δcsal_0992, and Δcsal_0993) incubated at 37°C in S-M63 synthetic medium with sarcosine as the sole N source. 13C nuclear magnetic resonance (13C-NMR) experiments revealed that not only ectoine, glutamate, and N-acetyl-2,4-diaminobutyrate but also glycine betaine (GB), DMG, sarcosine, trehalose, and glucosylglycerate are accumulated intracellularly in the four mutants.IMPORTANCE Although N,N-dimethylglycine (DMG) dehydrogenase (DMGDH) activity was detected in cell extracts of microorganisms, the genes encoding microbial DMGDHs have not been determined until now. In addition, to our knowledge, the physiological role of DMG in moderate halophiles has never been investigated. In this study, we identified the genes involved in DMG degradation to sarcosine, characterized an unusual DMGDH, and investigated the role of DMG in Chromohalobacter salexigens DSM 3043 and its mutants. Our results suggested that the conversion of DMG to sarcosine is accompanied by intramolecular delivery of electrons in DMGDH and intermolecular electron transfer between DMGDH and other electron acceptors. Moreover, an unidentified methyltransferase catalyzing the production of glycine betaine (GB) from DMG but sharing no homology with the reported sarcosine DMG methyltransferases was predicted to be present in the cells. The results of this study expand our understanding of the physiological role of DMG and its catabolism to sarcosine in C. salexigens.
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18
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Kurth JM, Op den Camp HJM, Welte CU. Several ways one goal-methanogenesis from unconventional substrates. Appl Microbiol Biotechnol 2020; 104:6839-6854. [PMID: 32542472 PMCID: PMC7374477 DOI: 10.1007/s00253-020-10724-7] [Citation(s) in RCA: 49] [Impact Index Per Article: 12.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/08/2020] [Revised: 05/27/2020] [Accepted: 06/04/2020] [Indexed: 12/15/2022]
Abstract
Abstract Methane is the second most important greenhouse gas on earth. It is produced by methanogenic archaea, which play an important role in the global carbon cycle. Three main methanogenesis pathways are known: in the hydrogenotrophic pathway H2 and carbon dioxide are used for methane production, whereas in the methylotrophic pathway small methylated carbon compounds like methanol and methylated amines are used. In the aceticlastic pathway, acetate is disproportionated to methane and carbon dioxide. However, next to these conventional substrates, further methanogenic substrates and pathways have been discovered. Several phylogenetically distinct methanogenic lineages (Methanosphaera, Methanimicrococcus, Methanomassiliicoccus, Methanonatronarchaeum) have evolved hydrogen-dependent methylotrophic methanogenesis without the ability to perform either hydrogenotrophic or methylotrophic methanogenesis. Genome analysis of the deep branching Methanonatronarchaeum revealed an interesting membrane-bound hydrogenase complex affiliated with the hardly described class 4 g of multisubunit hydrogenases possibly providing reducing equivalents for anabolism. Furthermore, methylated sulfur compounds such as methanethiol, dimethyl sulfide, and methylmercaptopropionate were described to be converted into adapted methylotrophic methanogenesis pathways of Methanosarcinales strains. Moreover, recently it has been shown that the methanogen Methermicoccus shengliensis can use methoxylated aromatic compounds in methanogenesis. Also, tertiary amines like choline (N,N,N-trimethylethanolamine) or betaine (N,N,N-trimethylglycine) have been described as substrates for methane production in Methanococcoides and Methanolobus strains. This review article will provide in-depth information on genome-guided metabolic reconstructions, physiology, and biochemistry of these unusual methanogenesis pathways. Key points • Newly discovered methanogenic substrates and pathways are reviewed for the first time. • The review provides an in-depth analysis of unusual methanogenesis pathways. • The hydrogenase complex of the deep branching Methanonatronarchaeum is analyzed.
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Affiliation(s)
- Julia M Kurth
- Department of Microbiology, Institute for Water and Wetland Research, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, The Netherlands
| | - Huub J M Op den Camp
- Department of Microbiology, Institute for Water and Wetland Research, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, The Netherlands.
| | - Cornelia U Welte
- Department of Microbiology, Institute for Water and Wetland Research, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, The Netherlands. .,Soehngen Institute of Anaerobic Microbiology, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, The Netherlands.
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19
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Tarnovetskii IY, Merkel AY, Pimenov NV. Analysis of Cultured Methanogenic Archaea from the Tarkhankut Peninsula Coastal Methane Seeps. Microbiology (Reading) 2020. [DOI: 10.1134/s0026261719060183] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/26/2022] Open
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20
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Wang P, Wang Y, Guo X, Huang S, Zhu G. Biochemical and phylogenetic characterization of a monomeric isocitrate dehydrogenase from a marine methanogenic archaeon Methanococcoides methylutens. Extremophiles 2020; 24:319-328. [PMID: 31970482 DOI: 10.1007/s00792-020-01156-2] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/07/2019] [Accepted: 01/06/2020] [Indexed: 12/13/2022]
Abstract
Monomeric isocitrate dehydrogenase (IDH) stands for a separated subgroup among IDH protein family. Up to now, all reported monomeric IDHs are from prokaryotes. Here, a monomeric IDH from a marine methanogenic archaeon Methanococcoides methylutens (MmIDH) was reported for the first time. BLAST search demonstrated that only a few marine archaea encode the monomeric IDH and all these organisms are methylotrophic. MmIDH shows the highest homology (~ 70%) to the monomeric IDHs from some marine bacteria, suggesting a lateral gene transfer event between marine bacteria and archaea. The monomeric state of MmIDH was determined by size exclusion chromatography. MmIDH is divalent cation-dependent and Mn2+ is the most favored. Kinetic analysis showed that MmIDH is highly specific to NADP+ and cannot utilize the NAD+. The optimal temperature for MmIDH activity is 50 °C and the optimal pH is 8.2. Heat inactivation assay revealed that MmIDH is a mesophilic enzyme. It sustained 50% activity after incubation at 39 °C for 20 min. Moreover, the putative coenzyme binding residues (His590, Arg601, and Arg650) of MmIDH were explored by mutagenesis. The triple mutant H590L/R601D/R650S displayed a 5.93-fold preference for NAD+ over NADP+, indicating that the coenzyme specificity of MmIDH was significantly switched from NADP+ to NAD+ by three key mutations.
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Affiliation(s)
- Peng Wang
- The Research Center of Life Omics and Health and Anhui Provincial Key Laboratory of the Conservation and Exploitation of Biological Resources, Anhui Normal University, Wuhu, 241000, Anhui, China
| | - Yuan Wang
- The Research Center of Life Omics and Health and Anhui Provincial Key Laboratory of the Conservation and Exploitation of Biological Resources, Anhui Normal University, Wuhu, 241000, Anhui, China
| | - Xiuxiu Guo
- The Research Center of Life Omics and Health and Anhui Provincial Key Laboratory of the Conservation and Exploitation of Biological Resources, Anhui Normal University, Wuhu, 241000, Anhui, China
| | - Shiping Huang
- The Research Center of Life Omics and Health and Anhui Provincial Key Laboratory of the Conservation and Exploitation of Biological Resources, Anhui Normal University, Wuhu, 241000, Anhui, China
| | - Guoping Zhu
- The Research Center of Life Omics and Health and Anhui Provincial Key Laboratory of the Conservation and Exploitation of Biological Resources, Anhui Normal University, Wuhu, 241000, Anhui, China.
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21
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Creighbaum AJ, Ticak T, Shinde S, Wang X, Ferguson DJ. Examination of the Glycine Betaine-Dependent Methylotrophic Methanogenesis Pathway: Insights Into Anaerobic Quaternary Amine Methylotrophy. Front Microbiol 2019; 10:2572. [PMID: 31787957 PMCID: PMC6855144 DOI: 10.3389/fmicb.2019.02572] [Citation(s) in RCA: 10] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/09/2019] [Accepted: 10/23/2019] [Indexed: 01/23/2023] Open
Abstract
Recent studies indicate that environmentally abundant quaternary amines (QAs) are a primary source for methanogenesis, yet the catabolic enzymes are unknown. We hypothesized that the methanogenic archaeon Methanolobus vulcani B1d metabolizes glycine betaine (GB) through a corrinoid-dependent GB:coenzyme M (CoM) methyl transfer pathway. The draft genome sequence of M. vulcani B1d revealed a gene encoding a predicted non-pyrrolysine MttB homolog (MV8460) with high sequence similarity to the GB methyltransferase encoded by Desulfitobacterium hafniense Y51. MV8460 catalyzes GB-dependent methylation of free cob(I)alamin indicating it is an authentic MtgB enzyme. Proteomic analysis revealed that MV8460 and a corrinoid binding protein (MV8465) were highly abundant when M. vulcani B1d was grown on GB relative to growth on trimethylamine. The abundance of a corrinoid reductive activation enzyme (MV10335) and a methylcorrinoid:CoM methyltransferase (MV10360) were significantly higher in GB-grown B1d lysates compared to other homologs. The GB:CoM pathway was fully reconstituted in vitro using recombinant MV8460, MV8465, MV10335, and MV10360. Demonstration of the complete GB:CoM pathway expands the knowledge of direct QA-dependent methylotrophy and establishes a model to identify additional ecologically relevant anaerobic quaternary amine pathways.
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Affiliation(s)
- Adam J Creighbaum
- Department of Microbiology, Miami University, Oxford, OH, United States
| | - Tomislav Ticak
- Department of Biological Sciences, University of Idaho, Moscow, ID, United States
| | - Shrameeta Shinde
- Department of Microbiology, Miami University, Oxford, OH, United States
| | - Xin Wang
- Department of Microbiology, Miami University, Oxford, OH, United States
| | - Donald J Ferguson
- Department of Microbiology, Miami University, Oxford, OH, United States.,Department of Biological Sciences, Miami University Regionals, Hamilton, OH, United States
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22
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Jones HJ, Kröber E, Stephenson J, Mausz MA, Jameson E, Millard A, Purdy KJ, Chen Y. A new family of uncultivated bacteria involved in methanogenesis from the ubiquitous osmolyte glycine betaine in coastal saltmarsh sediments. MICROBIOME 2019; 7:120. [PMID: 31464644 PMCID: PMC6716910 DOI: 10.1186/s40168-019-0732-4] [Citation(s) in RCA: 18] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/08/2019] [Accepted: 08/13/2019] [Indexed: 05/10/2023]
Abstract
BACKGROUND Coastal environments are dynamic and rapidly changing. Living organisms in coastal environments are known to synthesise large quantities of organic osmolytes, which they use to cope with osmotic stresses. The organic osmolyte glycine betaine (GBT) is ubiquitously found in marine biota from prokaryotic Bacteria and Archaea to coastal plants, marine protozoa, and mammals. In intertidal coastal sediment, GBT represents an important precursor of natural methane emissions and as much as 90% of total methane production in these ecosystems can be originated from methanogenesis from GBT and its intermediate trimethylamine through microbial metabolism. RESULTS We set out to uncover the microorganisms responsible for methanogenesis from GBT using stable isotope labelling and metagenomics. This led to the recovery of a near-complete genome (2.3 Mbp) of a novel clostridial bacterium involved in anaerobic GBT degradation. Phylogenetic analyses of 16S rRNA gene, functional marker genes, and comparative genomics analyses all support the establishment of a novel family Candidatus 'Betainaceae' fam. nov. in Clostridiales and its role in GBT metabolism. CONCLUSIONS Our comparative genomes and metagenomics analyses suggest that this bacterium is widely distributed in coastal salt marshes, marine sediments, and deep subsurface sediments, suggesting a key role of anaerobic GBT metabolism by this clostridial bacterium in these ecosystems.
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Affiliation(s)
- Helen J Jones
- School of Life Sciences, University of Warwick, Coventry, CV4 7AL, UK
| | - Eileen Kröber
- Microbial Biogeochemistry, RA Landscape Functioning, ZALF Leibniz Centre for Agricultural Landscape Research, 15374, Müncheberg, Germany.
| | - Jason Stephenson
- School of Life Sciences, University of Warwick, Coventry, CV4 7AL, UK
| | - Michaela A Mausz
- School of Life Sciences, University of Warwick, Coventry, CV4 7AL, UK
| | - Eleanor Jameson
- School of Life Sciences, University of Warwick, Coventry, CV4 7AL, UK
| | - Andrew Millard
- Department of Infection, Immunity and Inflammation, University of Leicester, Leicester, LE1 7RH, UK
| | - Kevin J Purdy
- School of Life Sciences, University of Warwick, Coventry, CV4 7AL, UK
| | - Yin Chen
- School of Life Sciences, University of Warwick, Coventry, CV4 7AL, UK.
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23
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Genome Sequences of Two Choline-Utilizing Methanogenic Archaea, Methanococcoides spp., Isolated from Marine Sediments. Microbiol Resour Announc 2019; 8:8/18/e00342-19. [PMID: 31048384 PMCID: PMC6498239 DOI: 10.1128/mra.00342-19] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/20/2022] Open
Abstract
The genomes of two Methanococcoides spp. that were isolated from marine sediments and are capable of carrying out methanogenesis from choline and other methylotrophic substrates were sequenced. The average nucleotide identity and in silico DNA-DNA hybridization analyses demonstrate that they represent species different from those previously described.
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24
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Lechtenfeld M, Heine J, Sameith J, Kremp F, Müller V. Glycine betaine metabolism in the acetogenic bacteriumAcetobacterium woodii. Environ Microbiol 2018; 20:4512-4525. [DOI: 10.1111/1462-2920.14389] [Citation(s) in RCA: 20] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/23/2018] [Revised: 08/10/2018] [Accepted: 08/17/2018] [Indexed: 12/01/2022]
Affiliation(s)
- Mats Lechtenfeld
- Department of Molecular Microbiology & BioenergeticsInstitute of Molecular Biosciences, Johann Wolfgang Goethe University Max‐von‐Laue Str. 9, D‐60438 Frankfurt Germany
| | - Julia Heine
- Department of Molecular Microbiology & BioenergeticsInstitute of Molecular Biosciences, Johann Wolfgang Goethe University Max‐von‐Laue Str. 9, D‐60438 Frankfurt Germany
| | - Janin Sameith
- Department of Molecular Microbiology & BioenergeticsInstitute of Molecular Biosciences, Johann Wolfgang Goethe University Max‐von‐Laue Str. 9, D‐60438 Frankfurt Germany
| | - Florian Kremp
- Department of Molecular Microbiology & BioenergeticsInstitute of Molecular Biosciences, Johann Wolfgang Goethe University Max‐von‐Laue Str. 9, D‐60438 Frankfurt Germany
| | - Volker Müller
- Department of Molecular Microbiology & BioenergeticsInstitute of Molecular Biosciences, Johann Wolfgang Goethe University Max‐von‐Laue Str. 9, D‐60438 Frankfurt Germany
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25
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Zabranska J, Pokorna D. Bioconversion of carbon dioxide to methane using hydrogen and hydrogenotrophic methanogens. Biotechnol Adv 2017; 36:707-720. [PMID: 29248685 DOI: 10.1016/j.biotechadv.2017.12.003] [Citation(s) in RCA: 88] [Impact Index Per Article: 12.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/28/2017] [Revised: 11/14/2017] [Accepted: 12/12/2017] [Indexed: 11/18/2022]
Abstract
Biogas produced from organic wastes contains energetically usable methane and unavoidable amount of carbon dioxide. The exploitation of whole biogas energy is locally limited and utilization of the natural gas transport system requires CO2 removal or its conversion to methane. The biological conversion of CO2 and hydrogen to methane is well known reaction without the demand of high pressure and temperature and is carried out by hydrogenotrophic methanogens. Reducing equivalents to the biotransformation of carbon dioxide from biogas or other resources to biomethane can be supplied by external hydrogen. Discontinuous electricity production from wind and solar energy combined with fluctuating utilization cause serious storage problems that can be solved by power-to-gas strategy representing the production of storable hydrogen via the electrolysis of water. The possibility of subsequent repowering of the energy of hydrogen to the easily utilizable and transportable form is a biological conversion with CO2 to biomethane. Biomethanization of CO2 can take place directly in anaerobic digesters fed with organic substrates or in separate bioreactors. The major bottleneck in the process is gas-liquid mass transfer of H2 and the method of the effective input of hydrogen into the system. There are many studies with different bioreactors arrangements and a way of enrichment of hydrogenotrophic methanogens, but the system still has to be optimized for a higher efficiency. The aim of the paper is to gather and critically assess the state of a research and experience from laboratory, pilot and operational applications of carbon dioxide bioconversion and highlight further perspective fields of research.
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Affiliation(s)
- Jana Zabranska
- University of Chemistry and Technology Prague, Department of Water Technology and Environmental Engineering, Technicka 5, CZ 166 28 Prague, Czech Republic.
| | - Dana Pokorna
- University of Chemistry and Technology Prague, Department of Water Technology and Environmental Engineering, Technicka 5, CZ 166 28 Prague, Czech Republic
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26
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Wong HL, Visscher PT, White RA, Smith DL, Patterson MM, Burns BP. Dynamics of archaea at fine spatial scales in Shark Bay mat microbiomes. Sci Rep 2017; 7:46160. [PMID: 28397816 PMCID: PMC5387419 DOI: 10.1038/srep46160] [Citation(s) in RCA: 45] [Impact Index Per Article: 6.4] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/18/2016] [Accepted: 03/09/2017] [Indexed: 01/07/2023] Open
Abstract
The role of archaea in microbial mats is poorly understood. Delineating the spatial distribution of archaea with mat depth will enable resolution of putative niches in these systems. In the present study, high throughput amplicon sequencing was undertaken in conjunction with analysis of key biogeochemical properties of two mats (smooth and pustular) from Shark Bay, Australia. One-way analysis of similarity tests indicated the archaeal community structures of smooth and pustular mats were significantly different (global R = 1, p = 0.1%). Smooth mats possessed higher archaeal diversity, dominated by Parvarchaeota. The methanogenic community in smooth mats was dominated by hydrogenotrophic Methanomicrobiales, as well as methylotrophic Methanosarcinales, Methanococcales, Methanobacteriales and Methanomassiliicoccaceae. Pustular mats were enriched with Halobacteria and Parvarchaeota. Key metabolisms (bacterial and archaeal) were measured, and the rates of oxygen production/consumption and sulfate reduction were up to four times higher in smooth than in pustular mats. Methane production peaked in the oxic layers and was up to seven-fold higher in smooth than pustular mats. The finding of an abundance of anaerobic methanogens enriched at the surface where oxygen levels were highest, coupled with peak methane production in the oxic zone, suggests putative surface anoxic niches in these microbial mats.
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Affiliation(s)
- Hon Lun Wong
- School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney, Australia.,Australian Centre for Astrobiology, University of New South Wales Sydney, Australia
| | - Pieter T Visscher
- Department of Marine Sciences, University of Connecticut, USA.,Australian Centre for Astrobiology, University of New South Wales Sydney, Australia
| | - Richard Allen White
- Earth and Biological Sciences Directorate, Pacific Northwest National Laboratory, Richland, Washington 99352, USA
| | - Daniela-Lee Smith
- School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney, Australia
| | | | - Brendan P Burns
- School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney, Australia.,Australian Centre for Astrobiology, University of New South Wales Sydney, Australia
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27
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Vyrides I, Stuckey DC. Compatible solute addition to biological systems treating waste/wastewater to counteract osmotic and other environmental stresses: a review. Crit Rev Biotechnol 2017; 37:865-879. [DOI: 10.1080/07388551.2016.1266460] [Citation(s) in RCA: 43] [Impact Index Per Article: 6.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/22/2022]
Affiliation(s)
- Ioannis Vyrides
- Department of Environmental Science and Technology, Cyprus University of Technology, Lemesos, Cyprus
| | - David C. Stuckey
- Department of Chemical Engineering, Imperial College London, London, UK
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28
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Glombitza C, Adhikari RR, Riedinger N, Gilhooly WP, Hinrichs KU, Inagaki F. Microbial Sulfate Reduction Potential in Coal-Bearing Sediments Down to ~2.5 km below the Seafloor off Shimokita Peninsula, Japan. Front Microbiol 2016; 7:1576. [PMID: 27761134 PMCID: PMC5051215 DOI: 10.3389/fmicb.2016.01576] [Citation(s) in RCA: 29] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/15/2016] [Accepted: 09/21/2016] [Indexed: 11/13/2022] Open
Abstract
Sulfate reduction is the predominant anaerobic microbial process of organic matter mineralization in marine sediments, with recent studies revealing that sulfate reduction not only occurs in sulfate-rich sediments, but even extends to deeper, methanogenic sediments at very low background concentrations of sulfate. Using samples retrieved off the Shimokita Peninsula, Japan, during the Integrated Ocean Drilling Program (IODP) Expedition 337, we measured potential sulfate reduction rates by slurry incubations with 35S-labeled sulfate in deep methanogenic sediments between 1276.75 and 2456.75 meters below the seafloor. Potential sulfate reduction rates were generally extremely low (mostly below 0.1 pmol cm-3 d-1) but showed elevated values (up to 1.8 pmol cm-3 d-1) in a coal-bearing interval (Unit III). A measured increase in hydrogenase activity in the coal-bearing horizons coincided with this local increase in potential sulfate reduction rates. This paired enzymatic response suggests that hydrogen is a potentially important electron donor for sulfate reduction in the deep coalbed biosphere. By contrast, no stimulation of sulfate reduction rates was observed in treatments where methane was added as an electron donor. In the deep coalbeds, small amounts of sulfate might be provided by a cryptic sulfur cycle. The isotopically very heavy pyrites (δ34S = +43‰) found in this horizon is consistent with its formation via microbial sulfate reduction that has been continuously utilizing a small, increasingly 34S-enriched sulfate reservoir over geologic time scales. Although our results do not represent in-situ activity, and the sulfate reducers might only have persisted in a dormant, spore-like state, our findings show that organisms capable of sulfate reduction have survived in deep methanogenic sediments over more than 20 Ma. This highlights the ability of sulfate-reducers to persist over geological timespans even in sulfate-depleted environments. Our study moreover represents the deepest evidence of a potential for sulfate reduction in marine sediments to date.
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Affiliation(s)
- Clemens Glombitza
- Department of Biosciences, Center for Geomicrobiology, Aarhus University Aarhus, Denmark
| | - Rishi R Adhikari
- MARUM Center for Marine Environmental Sciences, University of Bremen Bremen, Germany
| | - Natascha Riedinger
- Boone Pickens School of Geology, Oklahoma State University Stillwater, OK, USA
| | - William P Gilhooly
- Department of Earth Sciences, Indiana University-Purdue University Indianapolis Indianapolis, IN, USA
| | - Kai-Uwe Hinrichs
- MARUM Center for Marine Environmental Sciences, University of Bremen Bremen, Germany
| | - Fumio Inagaki
- Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and TechnologyKochi, Japan; Research and Development Center for Ocean Drilling Science, Japan Agency for Marine-Earth Science and TechnologyYokohama, Japan; Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and TechnologyYokosuka, Japan
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29
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Nigro LM, Hyde AS, MacGregor BJ, Teske A. Phylogeography, Salinity Adaptations and Metabolic Potential of the Candidate Division KB1 Bacteria Based on a Partial Single Cell Genome. Front Microbiol 2016; 7:1266. [PMID: 27597842 PMCID: PMC4993014 DOI: 10.3389/fmicb.2016.01266] [Citation(s) in RCA: 18] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/06/2016] [Accepted: 08/02/2016] [Indexed: 01/15/2023] Open
Abstract
Deep-sea hypersaline anoxic basins and other hypersaline environments contain abundant and diverse microbial life that has adapted to these extreme conditions. The bacterial Candidate Division KB1 represents one of several uncultured groups that have been consistently observed in hypersaline microbial diversity studies. Here we report the phylogeography of KB1, its phylogenetic relationships to Candidate Division OP1 Bacteria, and its potential metabolic and osmotic stress adaptations based on a partial single cell amplified genome of KB1 from Orca Basin, the largest hypersaline seafloor brine basin in the Gulf of Mexico. Our results are consistent with the hypothesis – previously developed based on 14C incorporation experiments with mixed-species enrichments from Mediterranean seafloor brines – that KB1 has adapted its proteins to elevated intracellular salinity, but at the same time KB1 apparently imports glycine betaine; this compatible solute is potentially not limited to osmoregulation but could also serve as a carbon and energy source.
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Affiliation(s)
- Lisa M Nigro
- Department of Marine Sciences, University of North Carolina at Chapel Hill Chapel Hill, NC, USA
| | - Andrew S Hyde
- Department of Marine Sciences, University of North Carolina at Chapel Hill Chapel Hill, NC, USA
| | - Barbara J MacGregor
- Department of Marine Sciences, University of North Carolina at Chapel Hill Chapel Hill, NC, USA
| | - Andreas Teske
- Department of Marine Sciences, University of North Carolina at Chapel Hill Chapel Hill, NC, USA
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30
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Quantification of glycine betaine, choline and trimethylamine N-oxide in seawater particulates: Minimisation of seawater associated ion suppression. Anal Chim Acta 2016; 938:114-22. [PMID: 27619093 DOI: 10.1016/j.aca.2016.07.016] [Citation(s) in RCA: 19] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/03/2016] [Revised: 07/11/2016] [Accepted: 07/17/2016] [Indexed: 11/22/2022]
Abstract
A liquid chromatography/mass spectrometry (LC/MS, electrospray ionisation) method has been developed for the quantification of nitrogenous osmolytes (N-osmolytes) in the particulate fraction of natural water samples. Full method validation demonstrates the validity of the method for measuring glycine betaine (GBT), choline and trimethylamine N-oxide (TMAO) in particulates from seawater. Limits of detection were calculated as 3.5, 1.2 and 5.9 pg injected onto column (equivalent to 1.5, 0.6 and 3.9 nmol per litre) for GBT, choline and TMAO respectively. Precision of the method was typically 3% for both GBT and choline and 6% for TMAO. Collection of the particulate fraction of natural samples was achieved via in-line filtration. Resulting chromatography and method sensitivity was assessed and compared for the use of both glass fibre and polycarbonate filters during sample collection. Ion suppression was shown to be a significant cause of reduced instrument response to N-osmolytes and was associated with the presence of seawater in the sample matrix.
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31
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Zou H, Chen N, Shi M, Xian M, Song Y, Liu J. The metabolism and biotechnological application of betaine in microorganism. Appl Microbiol Biotechnol 2016; 100:3865-76. [PMID: 27005411 DOI: 10.1007/s00253-016-7462-3] [Citation(s) in RCA: 55] [Impact Index Per Article: 6.9] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/20/2016] [Revised: 03/08/2016] [Accepted: 03/09/2016] [Indexed: 11/29/2022]
Abstract
Glycine betaine (betaine) is widely distributed in nature and can be found in many microorganisms, including bacteria, archaea, and fungi. Due to its particular functions, many microorganisms utilize betaine as a functional chemical and have evolved different metabolic pathways for the biosynthesis and catabolism of betaine. As in animals and plants, the principle role of betaine is to protect microbial cells against drought, osmotic stress, and temperature stress. In addition, the role of betaine in methyl group metabolism has been observed in a variety of microorganisms. Recent studies have shown that betaine supplementation can improve the performance of microbial strains used for the fermentation of lactate, ethanol, lysine, pyruvate, and vitamin B12, during which betaine can act as stress protectant or methyl donor for the biosynthesis of structurally complex compounds. In this review, we summarize the transport, synthesis, catabolism, and functions of betaine in microorganisms and discuss potential engineering strategies that employ betaine as a methyl donor for the biosynthesis of complex secondary metabolites such as a variety of vitamins, coenzymes, and antibiotics. In conclusion, the biocompatibility, C/N ratio, abundance, and comprehensive metabolic information of betaine collectively indicate that this molecule has great potential for broad applications in microbial biotechnology.
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Affiliation(s)
- Huibin Zou
- College of Chemical Engineering, Qingdao University of Science and Technology, Qingdao, 266042, China. .,CAS Key Laboratory of Bio-based Materials, Qingdao Institute of Bioenergy and Bioprocess Technology, Chinese Academy of Sciences, Qingdao, China.
| | - Ningning Chen
- College of Chemical Engineering, Qingdao University of Science and Technology, Qingdao, 266042, China
| | - Mengxun Shi
- College of Chemical Engineering, Qingdao University of Science and Technology, Qingdao, 266042, China
| | - Mo Xian
- CAS Key Laboratory of Bio-based Materials, Qingdao Institute of Bioenergy and Bioprocess Technology, Chinese Academy of Sciences, Qingdao, China
| | - Yimin Song
- College of Chemical Engineering, Qingdao University of Science and Technology, Qingdao, 266042, China
| | - Junhong Liu
- College of Chemical Engineering, Qingdao University of Science and Technology, Qingdao, 266042, China
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32
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Betaine chemistry, roles, and potential use in liver disease. Biochim Biophys Acta Gen Subj 2016; 1860:1098-106. [PMID: 26850693 DOI: 10.1016/j.bbagen.2016.02.001] [Citation(s) in RCA: 126] [Impact Index Per Article: 15.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/15/2015] [Revised: 01/26/2016] [Accepted: 02/01/2016] [Indexed: 12/17/2022]
Abstract
BACKGROUND Betaine is the trimethyl derivative of glycine and is normally present in human plasma due to dietary intake and endogenous synthesis in liver and kidney. Betaine is utilized in the kidney primarily as an osmoprotectant, whereas in the liver its primary role is in metabolism as a methyl group donor. In both organs, a specific betaine transporter mediates cellular uptake of betaine from plasma. The abundance of both betaine and the betaine transporter in liver greatly exceeds that of other organs. SCOPE OF REVIEW The remarkable contributions of betaine to normal human and animal health are summarized together with a discussion of the mechanisms and potential beneficial effects of dietary betaine supplements on liver disease. MAJOR CONCLUSIONS A significant amount of data from animal models of liver disease indicates that administration of betaine can halt and even reverse progression of the disruption of liver function. Betaine is well-tolerated, inexpensive, effective over a wide range of doses, and is already used in livestock feeding practices. GENERAL SIGNIFICANCE The accumulated data indicate that carefully controlled additional investigations in humans are merited. The focus should be on the long-term use of betaine in large patient populations with liver diseases characterized by development of fatty liver, especially non-alcoholic fatty liver disease and alcoholic liver disease.
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33
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Söllinger A, Schwab C, Weinmaier T, Loy A, Tveit AT, Schleper C, Urich T. Phylogenetic and genomic analysis of Methanomassiliicoccales in wetlands and animal intestinal tracts reveals clade-specific habitat preferences. FEMS Microbiol Ecol 2016; 92:fiv149. [PMID: 26613748 DOI: 10.1093/femsec/fiv149] [Citation(s) in RCA: 66] [Impact Index Per Article: 8.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Accepted: 11/24/2015] [Indexed: 01/30/2023] Open
Abstract
Methanogenic Thermoplasmata of the novel order Methanomassiliicoccales were recently discovered in human and animal gastro-intestinal tracts (GITs). However, their distribution in other methanogenic environments has not been addressed systematically. Here, we surveyed Methanomassiliicoccales presence in wetland soils, a globally important source of methane emissions to the atmosphere, and in the GITs of different animals by PCR targeting their 16S rRNA and methyl:coenzyme M reductase (α-subunit) genes. We detected Methanomassiliicoccales in all 16 peat soils investigated, indicating their wide distribution in these habitats. Additionally, we detected their genes in various animal faeces. Methanomassiliicoccales were subdivided in two broad phylogenetic clades designated 'environmental' and 'GIT' clades based on differential, although non-exclusive, habitat preferences of their members. A well-supported cluster within the environmental clade comprised more than 80% of all wetland 16S rRNA gene sequences. Metagenome assembly from bovine rumen fluid enrichments resulted in two almost complete genomes of both Methanomassiliicoccales clades. Comparative genomics revealed that members of the environmental clade contain larger genomes and a higher number of genes encoding anti-oxidative enzymes than animal GIT clade representatives. This study highlights the wide distribution of Methanomassiliicoccales in wetlands, which suggests that they contribute to methane emissions from these climate-relevant ecosystems.
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Affiliation(s)
- Andrea Söllinger
- Department of Ecogenomics and Systems Biology, University of Vienna, 1090 Vienna, Austria
| | - Clarissa Schwab
- Institute of Food, Nutrition and Health, ETH Zürich, 8092 Zurich, Switzerland
| | - Thomas Weinmaier
- Department of Microbiology and Ecosystem Science, University of Vienna, 1090 Vienna, Austria
| | - Alexander Loy
- Department of Microbiology and Ecosystem Science, University of Vienna, 1090 Vienna, Austria
| | - Alexander T Tveit
- Department of Arctic and Marine Biology, UiT The Arctic University of Norway, 9037 Tromsø, Norway
| | - Christa Schleper
- Department of Ecogenomics and Systems Biology, University of Vienna, 1090 Vienna, Austria
| | - Tim Urich
- Department of Ecogenomics and Systems Biology, University of Vienna, 1090 Vienna, Austria Institute for Microbiology, Ernst-Moritz-Arndt University Greifswald, 17489 Greifswald, Germany
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34
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Evidence of Active Methanogen Communities in Shallow Sediments of the Sonora Margin Cold Seeps. Appl Environ Microbiol 2015. [DOI: 10.1128/aem.00147-15 rlike (select (case when (5853=5853) then 0x31302e313132382f61656d2e30303134372d3135 else 0x28 end))-- yhjw] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/11/2023] Open
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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35
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Evidence of Active Methanogen Communities in Shallow Sediments of the Sonora Margin Cold Seeps. Appl Environ Microbiol 2015. [DOI: 10.1128/aem.00147-15 and (select (case when (4843=4843) then null else ctxsys.drithsx.sn(1,4843) end) from dual) is null] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/11/2023] Open
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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36
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Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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37
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Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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38
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Evidence of Active Methanogen Communities in Shallow Sediments of the Sonora Margin Cold Seeps. Appl Environ Microbiol 2015. [DOI: 10.1128/aem.00147-15 and (select (case when (4809=6114) then null else ctxsys.drithsx.sn(1,4809) end) from dual) is null-- zlmh] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/11/2023] Open
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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39
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Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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40
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Evidence of Active Methanogen Communities in Shallow Sediments of the Sonora Margin Cold Seeps. Appl Environ Microbiol 2015. [DOI: 10.1128/aem.00147-15 and extractvalue(5836,concat(0x5c,0x7162707671,(select (elt(5836=5836,1))),0x717a6b7171))-- jijh] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/11/2023] Open
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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41
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Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|
42
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Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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43
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Evidence of Active Methanogen Communities in Shallow Sediments of the Sonora Margin Cold Seeps. Appl Environ Microbiol 2015. [DOI: 10.1128/aem.00147-15 order by 1-- wjpz] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/11/2023] Open
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|
44
|
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|
45
|
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|
46
|
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|
47
|
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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48
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Evidence of Active Methanogen Communities in Shallow Sediments of the Sonora Margin Cold Seeps. Appl Environ Microbiol 2015. [DOI: 10.1128/aem.00147-15 or extractvalue(9645,concat(0x5c,0x7162707671,(select (elt(9645=9645,1))),0x717a6b7171))-- tzdx] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/11/2023] Open
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|
49
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Evidence of Active Methanogen Communities in Shallow Sediments of the Sonora Margin Cold Seeps. Appl Environ Microbiol 2015. [DOI: 10.1128/aem.00147-15 order by 1#] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/11/2023] Open
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|
50
|
Abstract
ABSTRACT
In the Sonora Margin cold seep ecosystems (Gulf of California), sediments underlying microbial mats harbor high biogenic methane concentrations, fueling various microbial communities, such as abundant lineages of anaerobic methanotrophs (ANME). However, the biodiversity, distribution, and metabolism of the microorganisms producing this methane remain poorly understood. In this study, measurements of methanogenesis using radiolabeled dimethylamine, bicarbonate, and acetate showed that biogenic methane production in these sediments was mainly dominated by methylotrophic methanogenesis, while the proportion of autotrophic methanogenesis increased with depth. Congruently, methane production and methanogenic
Archaea
were detected in culture enrichments amended with trimethylamine and bicarbonate. Analyses of denaturing gradient gel electrophoresis (DGGE) fingerprinting and reverse-transcribed PCR-amplified 16S rRNA sequences retrieved from these enrichments revealed the presence of active methylotrophic
Methanococcoides
burtonii
relatives and several new autotrophic
Methanogenium
lineages, confirming the cooccurrence of
Methanosarcinales
and
Methanomicrobiales
methanogens with abundant ANME populations in the sediments of the Sonora Margin cold seeps.
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|