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Mara P, Geller-McGrath D, Edgcomb V, Beaudoin D, Morono Y, Teske A. Metagenomic profiles of archaea and bacteria within thermal and geochemical gradients of the Guaymas Basin deep subsurface. Nat Commun 2023; 14:7768. [PMID: 38012208 PMCID: PMC10681998 DOI: 10.1038/s41467-023-43296-x] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/31/2023] [Accepted: 11/02/2023] [Indexed: 11/29/2023] Open
Abstract
Previous studies of microbial communities in subseafloor sediments reported that microbial abundance and diversity decrease with sediment depth and age, and microbes dominating at depth tend to be a subset of the local seafloor community. However, the existence of geographically widespread, subsurface-adapted specialists is also possible. Here, we use metagenomic and metatranscriptomic analyses of the hydrothermally heated, sediment layers of Guaymas Basin (Gulf of California, Mexico) to examine the distribution and activity patterns of bacteria and archaea along thermal, geochemical and cell count gradients. We find that the composition and distribution of metagenome-assembled genomes (MAGs), dominated by numerous lineages of Chloroflexota and Thermoproteota, correlate with biogeochemical parameters as long as temperatures remain moderate, but downcore increasing temperatures beyond ca. 45 ºC override other factors. Consistently, MAG size and diversity decrease with increasing temperature, indicating a downcore winnowing of the subsurface biosphere. By contrast, specific archaeal MAGs within the Thermoproteota and Hadarchaeota increase in relative abundance and in recruitment of transcriptome reads towards deeper, hotter sediments, marking the transition towards a specialized deep, hot biosphere.
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Affiliation(s)
- Paraskevi Mara
- Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA
| | - David Geller-McGrath
- Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA
| | - Virginia Edgcomb
- Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA
| | - David Beaudoin
- Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA
| | - Yuki Morono
- Kochi Institute for Core Sample Research, Institute for Extra-cutting-edge Science and Technology Avantgarde Research (X-STAR), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Monobe, Nankoku, Kochi, Japan
| | - Andreas Teske
- Department of Earth, Marine and Environmental Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, 27599, USA.
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2
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Halevy I, Fike DA, Pasquier V, Bryant RN, Wenk CB, Turchyn AV, Johnston DT, Claypool GE. Sedimentary parameters control the sulfur isotope composition of marine pyrite. Science 2023; 382:946-951. [PMID: 37995229 DOI: 10.1126/science.adh1215] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/11/2023] [Accepted: 10/23/2023] [Indexed: 11/25/2023]
Abstract
Reconstructions of coupled carbon, oxygen, and sulfur cycles rely heavily on sedimentary pyrite sulfur isotope compositions (δ34Spyr). With a model of sediment diagenesis, paired with global datasets of sedimentary parameters, we show that the wide range of δ34Spyr (~100 per mil) in modern marine sediments arises from geographic patterns in the relative rates of diffusion, burial, and microbial reduction of sulfate. By contrast, the microbial sulfur isotope fractionation remains large and relatively uniform. Over Earth history, the effect of increasing seawater sulfate and oxygen concentrations on sulfate and sulfide transport and reaction may explain the corresponding increase observed in the δ34S offset between sulfate and pyrite. More subtle variations may be related to changes in depositional environments associated with sea level fluctuations and supercontinent cycles.
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Affiliation(s)
- I Halevy
- Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - D A Fike
- Earth and Planetary Sciences, Washington University in St. Louis, St. Louis, MO 63130-4899, USA
| | - V Pasquier
- Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - R N Bryant
- Earth and Planetary Sciences, Washington University in St. Louis, St. Louis, MO 63130-4899, USA
- Earth, Atmospheric and Planetary Sciences, Purdue University, W. Lafayette, IN 47907, USA
| | - C B Wenk
- Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - A V Turchyn
- Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
| | - D T Johnston
- Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA
| | - G E Claypool
- 8910 West Jewell Avenue, Unit 209, Lakewood, CO 80232, USA
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3
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Mara P, Zhou YL, Teske A, Morono Y, Beaudoin D, Edgcomb V. Microbial gene expression in Guaymas Basin subsurface sediments responds to hydrothermal stress and energy limitation. THE ISME JOURNAL 2023; 17:1907-1919. [PMID: 37658181 PMCID: PMC10579382 DOI: 10.1038/s41396-023-01492-z] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/08/2023] [Revised: 08/01/2023] [Accepted: 08/02/2023] [Indexed: 09/03/2023]
Abstract
Analyses of gene expression of subsurface bacteria and archaea provide insights into their physiological adaptations to in situ subsurface conditions. We examined patterns of expressed genes in hydrothermally heated subseafloor sediments with distinct geochemical and thermal regimes in Guaymas Basin, Gulf of California, Mexico. RNA recovery and cell counts declined with sediment depth, however, we obtained metatranscriptomes from eight sites at depths spanning between 0.8 and 101.9 m below seafloor. We describe the metabolic potential of sediment microorganisms, and discuss expressed genes involved in tRNA, mRNA, and rRNA modifications that enable physiological flexibility of bacteria and archaea in the hydrothermal subsurface. Microbial taxa in hydrothermally influenced settings like Guaymas Basin may particularly depend on these catalytic RNA functions since they modulate the activity of cells under elevated temperatures and steep geochemical gradients. Expressed genes for DNA repair, protein maintenance and circadian rhythm were also identified. The concerted interaction of many of these genes may be crucial for microorganisms to survive and to thrive in the Guaymas Basin subsurface biosphere.
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Affiliation(s)
- Paraskevi Mara
- Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA
| | - Ying-Li Zhou
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
| | - Andreas Teske
- Department of Earth, Marine and Environmental Sciences, University of North Carolina, Chapel Hill, NC, USA
| | - Yuki Morono
- Kochi Institute for Core Sample Research, Institute for Extra-cutting-edge Science and Technology Avant-garde Research (X-star), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Monobe, Nankoku, Kochi, Japan
| | - David Beaudoin
- Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA
| | - Virginia Edgcomb
- Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.
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4
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Degradation of biological macromolecules supports uncultured microbial populations in Guaymas Basin hydrothermal sediments. THE ISME JOURNAL 2021; 15:3480-3497. [PMID: 34112968 PMCID: PMC8630151 DOI: 10.1038/s41396-021-01026-5] [Citation(s) in RCA: 13] [Impact Index Per Article: 4.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 12/08/2020] [Revised: 05/26/2021] [Accepted: 05/27/2021] [Indexed: 02/05/2023]
Abstract
Hydrothermal sediments contain large numbers of uncultured heterotrophic microbial lineages. Here, we amended Guaymas Basin sediments with proteins, polysaccharides, nucleic acids or lipids under different redox conditions and cultivated heterotrophic thermophiles with the genomic potential for macromolecule degradation. We reconstructed 20 metagenome-assembled genomes (MAGs) of uncultured lineages affiliating with known archaeal and bacterial phyla, including endospore-forming Bacilli and candidate phylum Marinisomatota. One Marinisomatota MAG had 35 different glycoside hydrolases often in multiple copies, seven extracellular CAZymes, six polysaccharide lyases, and multiple sugar transporters. This population has the potential to degrade a broad spectrum of polysaccharides including chitin, cellulose, pectin, alginate, chondroitin, and carrageenan. We also describe thermophiles affiliating with the genera Thermosyntropha, Thermovirga, and Kosmotoga with the capability to make a living on nucleic acids, lipids, or multiple macromolecule classes, respectively. Several populations seemed to lack extracellular enzyme machinery and thus likely scavenged oligo- or monomers (e.g., MAGs affiliating with Archaeoglobus) or metabolic products like hydrogen (e.g., MAGs affiliating with Thermodesulfobacterium or Desulforudaceae). The growth of methanogens or the production of methane was not observed in any condition, indicating that the tested macromolecules are not degraded into substrates for methanogenesis in hydrothermal sediments. We provide new insights into the niches, and genomes of microorganisms that actively degrade abundant necromass macromolecules under oxic, sulfate-reducing, and fermentative thermophilic conditions. These findings improve our understanding of the carbon flow across trophic levels and indicate how primary produced biomass sustains complex and productive ecosystems.
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5
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Ramírez GA, Mara P, Sehein T, Wegener G, Chambers CR, Joye SB, Peterson RN, Philippe A, Burgaud G, Edgcomb VP, Teske AP. Environmental factors shaping bacterial, archaeal and fungal community structure in hydrothermal sediments of Guaymas Basin, Gulf of California. PLoS One 2021; 16:e0256321. [PMID: 34495995 PMCID: PMC8425543 DOI: 10.1371/journal.pone.0256321] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/10/2021] [Accepted: 08/03/2021] [Indexed: 01/04/2023] Open
Abstract
The flanking regions of Guaymas Basin, a young marginal rift basin located in the Gulf of California, are covered with thick sediment layers that are hydrothermally altered due to magmatic intrusions. To explore environmental controls on microbial community structure in this complex environment, we analyzed site- and depth-related patterns of microbial community composition (bacteria, archaea, and fungi) in hydrothermally influenced sediments with different thermal conditions, geochemical regimes, and extent of microbial mats. We compared communities in hot hydrothermal sediments (75-100°C at ~40 cm depth) covered by orange-pigmented Beggiatoaceae mats in the Cathedral Hill area, temperate sediments (25-30°C at ~40 cm depth) covered by yellow sulfur precipitates and filamentous sulfur oxidizers at the Aceto Balsamico location, hot sediments (>115°C at ~40 cm depth) with orange-pigmented mats surrounded by yellow and white mats at the Marker 14 location, and background, non-hydrothermal sediments (3.8°C at ~45 cm depth) overlain with ambient seawater. Whereas bacterial and archaeal communities are clearly structured by site-specific in-situ thermal gradients and geochemical conditions, fungal communities are generally structured by sediment depth. Unexpectedly, chytrid sequence biosignatures are ubiquitous in surficial sediments whereas deeper sediments contain diverse yeasts and filamentous fungi. In correlation analyses across different sites and sediment depths, fungal phylotypes correlate to each other to a much greater degree than Bacteria and Archaea do to each other or to fungi, further substantiating that site-specific in-situ thermal gradients and geochemical conditions that control bacteria and archaea do not extend to fungi.
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Affiliation(s)
- Gustavo A. Ramírez
- Department of Marine Sciences, University of North Carolina at Chapel Hill, NC, United States of America
- Department of Marine Biology, Leon H. Charney School of Marine Sciences, University of Haifa, Haifa, Israel
- College of Veterinary Medicine, Western University of Health Sciences, Pomona, CA, United States of America
- * E-mail:
| | - Paraskevi Mara
- Geology and Geophysics Dept., Woods Hole Oceanographic Institution, Woods Hole, MA, United States of America
| | - Taylor Sehein
- Geology and Geophysics Dept., Woods Hole Oceanographic Institution, Woods Hole, MA, United States of America
| | - Gunter Wegener
- MARUM, Center for Marine Environmental Sciences, University Bremen, Germany
- Max-Planck-Institute for Marine Microbiology, Bremen, Germany
| | - Christopher R. Chambers
- Department of Marine Sciences, University of North Carolina at Chapel Hill, NC, United States of America
| | - Samantha B. Joye
- Department of Marine Sciences, University of Georgia, Athens, GA, United States of America
| | - Richard N. Peterson
- School of Coastal and Marine Systems Science, Coastal Carolina University, Conway, SC, United States of America
| | - Aurélie Philippe
- Univ. Brest, Laboratoire Universitaire de Biodiversité et Ecologie Microbienne, Plouzané, France
| | - Gaëtan Burgaud
- Univ. Brest, Laboratoire Universitaire de Biodiversité et Ecologie Microbienne, Plouzané, France
| | - Virginia P. Edgcomb
- Geology and Geophysics Dept., Woods Hole Oceanographic Institution, Woods Hole, MA, United States of America
| | - Andreas P. Teske
- Department of Marine Sciences, University of North Carolina at Chapel Hill, NC, United States of America
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6
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Lai D, Hedlund BP, Xie W, Liu J, Phelps TJ, Zhang C, Wang P. Impact of Terrestrial Input on Deep-Sea Benthic Archaeal Community Structure in South China Sea Sediments. Front Microbiol 2020; 11:572017. [PMID: 33224115 PMCID: PMC7674655 DOI: 10.3389/fmicb.2020.572017] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/12/2020] [Accepted: 10/15/2020] [Indexed: 12/12/2022] Open
Abstract
Archaea are widespread in marine sediments and play important roles in the cycling of sedimentary organic carbon. However, factors controlling the distribution of archaea in marine sediments are not well understood. Here we investigated benthic archaeal communities over glacial-interglacial cycles in the northern South China Sea and evaluated their responses to sediment organic matter sources and inter-species interactions. Archaea in sediments deposited during the interglacial period Marine Isotope Stage (MIS) 1 (Holocene) were significantly different from those in sediments deposited in MIS 2 and MIS 3 of the Last Glacial Period when terrestrial input to the South China Sea was enhanced based on analysis of the long-chain n-alkane C31. The absolute archaeal 16S rRNA gene abundance in subsurface sediments was highest in MIS 2, coincident with high sedimentation rates and high concentrations of total organic carbon. Soil Crenarchaeotic Group (SCG; Nitrososphaerales) species, the most abundant ammonia-oxidizing archaea in soils, increased dramatically during MIS 2, likely reflecting transport of terrestrial archaea during glacial periods with high sedimentation rates. Co-occurrence network analyses indicated significant association of SCG archaea with benthic deep-sea microbes such as Bathyarchaeota and Thermoprofundales in MIS 2 and MIS 3, suggesting potential interactions among these archaeal groups. Meanwhile, Thermoprofundales abundance was positively correlated with total organic carbon (TOC), along with n-alkane C31 and sedimentation rate, indicating that Thermoprofundales may be particularly important in processing of organic carbon in deep-sea sediments. Collectively, these results demonstrate that the composition of heterotrophic benthic archaea in the South China Sea may be influenced by terrestrial organic input in tune with glacial-interglacial cycles, suggesting a plausible link between global climate change and microbial population dynamics in deep-sea marine sediments.
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Affiliation(s)
- Dengxun Lai
- State Key Laboratory of Marine Geology, Tongji University, Shanghai, China.,School of Life Sciences, University of Nevada, Las Vegas, NV, United States
| | - Brian P Hedlund
- School of Life Sciences, University of Nevada, Las Vegas, NV, United States.,Nevada Institute of Personalized Medicine, University of Nevada, Las Vegas, NV, United States
| | - Wei Xie
- School of Marine Sciences, Sun Yat-sen University, Zhuhai, China.,Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China
| | - Jingjing Liu
- State Key Laboratory of Marine Geology, Tongji University, Shanghai, China
| | - Tommy J Phelps
- Earth and Planetary Sciences, University of Tennessee, Knoxville, Knoxville, TN, United States
| | - Chuanlun Zhang
- Shenzhen Key Laboratory of Marine Archaea Geo-Omics, Southern University of Science and Technology, Shenzhen, China.,Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, China.,Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China.,Shanghai Sheshan National Geophysical Observatory, Shanghai, China
| | - Peng Wang
- State Key Laboratory of Marine Geology, Tongji University, Shanghai, China
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7
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Ramírez GA, McKay LJ, Fields MW, Buckley A, Mortera C, Hensen C, Ravelo AC, Teske AP. The Guaymas Basin Subseafloor Sedimentary Archaeome Reflects Complex Environmental Histories. iScience 2020; 23:101459. [PMID: 32861995 PMCID: PMC7476861 DOI: 10.1016/j.isci.2020.101459] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/05/2020] [Revised: 07/31/2020] [Accepted: 08/11/2020] [Indexed: 01/13/2023] Open
Abstract
We explore archaeal distributions in sedimentary subseafloor habitats of Guaymas Basin and the adjacent Sonora Margin, located in the Gulf of California, México. Sampling locations include (1) control sediments without hydrothermal or seep influence, (2) Sonora Margin sediments underlying oxygen minimum zone water, (3) compacted, highly reduced sediments from a pressure ridge with numerous seeps at the base of the Sonora Margin, and (4) sediments impacted by hydrothermal circulation at the off-axis Ringvent site. Generally, archaeal communities largely comprise Bathyarchaeal lineages, members of the Hadesarchaea, MBG-D, TMEG, and ANME-1 groups. Variations in archaeal community composition reflect locally specific environmental challenges. Background sediments are divided into surface and subsurface niches. Overall, the environmental setting and history of a particular site, not isolated biogeochemical properties out of context, control the subseafloor archaeal communities in Guaymas Basin and Sonora Margin sediments.
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Affiliation(s)
- Gustavo A. Ramírez
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, USA
- College of Veterinary Medicine, Western University of Health Sciences, Pomona, CA, USA
| | - Luke J. McKay
- Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, MT, USA
- Center for Biofilm Engineering, Montana State University, Bozeman, MT, USA
| | - Matthew W. Fields
- Center for Biofilm Engineering, Montana State University, Bozeman, MT, USA
- Department of Microbiology and Immunology, Montana State University, Bozeman, MT, USA
| | - Andrew Buckley
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, USA
| | - Carlos Mortera
- Instituto de Geofisica, Universidad Nacional Autónoma de México, Coyoacán, México
| | | | - Ana Christina Ravelo
- Ocean Sciences Department, University of California at Santa Cruz, Santa Cruz, CA, USA
| | - Andreas P. Teske
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, USA
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8
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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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9
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Vigneron A, Bishop A, Alsop EB, Hull K, Rhodes I, Hendricks R, Head IM, Tsesmetzis N. Microbial and Isotopic Evidence for Methane Cycling in Hydrocarbon-Containing Groundwater from the Pennsylvania Region. Front Microbiol 2017; 8:593. [PMID: 28424678 PMCID: PMC5380731 DOI: 10.3389/fmicb.2017.00593] [Citation(s) in RCA: 17] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/03/2016] [Accepted: 03/22/2017] [Indexed: 11/13/2022] Open
Abstract
The Pennsylvania region hosts numerous oil and gas reservoirs and the presence of hydrocarbons in groundwater has been locally observed. However, these methane-containing freshwater ecosystems remain poorly explored despite their potential importance in the carbon cycle. Methane isotope analysis and analysis of low molecular weight hydrocarbon gases from 18 water wells indicated that active methane cycling may be occurring in methane-containing groundwater from the Pennsylvania region. Consistent with this observation, multigenic qPCR and gene sequencing (16S rRNA genes, mcrA, and pmoA genes) indicated abundant populations of methanogens, ANME-2d (average of 1.54 × 104mcrA gene per milliliter of water) and bacteria associated with methane oxidation (NC10, aerobic methanotrophs, methylotrophs; average of 2.52 × 103pmoA gene per milliliter of water). Methane cycling therefore likely represents an important process in these hydrocarbon-containing aquifers. The microbial taxa and functional genes identified and geochemical data suggested that (i) methane present is at least in part due to methanogens identified in situ; (ii) Potential for aerobic and anaerobic methane oxidation is important in groundwater with the presence of lineages associated with both anaerobic an aerobic methanotrophy; (iii) the dominant methane oxidation process (aerobic or anaerobic) can vary according to prevailing conditions (oxic or anoxic) in the aquifers; (iv) the methane cycle is closely associated with the nitrogen cycle in groundwater methane seeps with methane and/or methanol oxidation coupled to denitrification or nitrate and nitrite reduction.
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Affiliation(s)
- Adrien Vigneron
- School of Civil Engineering and Geosciences, Newcastle UniversityNewcastle upon Tyne, UK.,Biodomain, Shell International Exploration and Production Inc.Houston, TX, USA
| | - Andrew Bishop
- Biodomain, Shell International Exploration and Production Inc.Houston, TX, USA
| | - Eric B Alsop
- Biodomain, Shell International Exploration and Production Inc.Houston, TX, USA.,DOE Joint Genome InstituteWalnut Creek, CA, USA
| | - Kellie Hull
- Biodomain, Shell International Exploration and Production Inc.Houston, TX, USA
| | | | | | - Ian M Head
- School of Civil Engineering and Geosciences, Newcastle UniversityNewcastle upon Tyne, UK
| | - Nicolas Tsesmetzis
- Biodomain, Shell International Exploration and Production Inc.Houston, TX, USA
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10
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Portail M, Olu K, Dubois SF, Escobar-Briones E, Gelinas Y, Menot L, Sarrazin J. Food-Web Complexity in Guaymas Basin Hydrothermal Vents and Cold Seeps. PLoS One 2016; 11:e0162263. [PMID: 27683216 PMCID: PMC5040445 DOI: 10.1371/journal.pone.0162263] [Citation(s) in RCA: 12] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/21/2015] [Accepted: 08/20/2016] [Indexed: 11/29/2022] Open
Abstract
In the Guaymas Basin, the presence of cold seeps and hydrothermal vents in close proximity, similar sedimentary settings and comparable depths offers a unique opportunity to assess and compare the functioning of these deep-sea chemosynthetic ecosystems. The food webs of five seep and four vent assemblages were studied using stable carbon and nitrogen isotope analyses. Although the two ecosystems shared similar potential basal sources, their food webs differed: seeps relied predominantly on methanotrophy and thiotrophy via the Calvin-Benson-Bassham (CBB) cycle and vents on petroleum-derived organic matter and thiotrophy via the CBB and reductive tricarboxylic acid (rTCA) cycles. In contrast to symbiotic species, the heterotrophic fauna exhibited high trophic flexibility among assemblages, suggesting weak trophic links to the metabolic diversity of chemosynthetic primary producers. At both ecosystems, food webs did not appear to be organised through predator-prey links but rather through weak trophic relationships among co-occurring species. Examples of trophic or spatial niche differentiation highlighted the importance of species-sorting processes within chemosynthetic ecosystems. Variability in food web structure, addressed through Bayesian metrics, revealed consistent trends across ecosystems. Food-web complexity significantly decreased with increasing methane concentrations, a common proxy for the intensity of seep and vent fluid fluxes. Although high fluid-fluxes have the potential to enhance primary productivity, they generate environmental constraints that may limit microbial diversity, colonisation of consumers and the structuring role of competitive interactions, leading to an overall reduction of food-web complexity and an increase in trophic redundancy. Heterogeneity provided by foundation species was identified as an additional structuring factor. According to their biological activities, foundation species may have the potential to partly release the competitive pressure within communities of low fluid-flux habitats. Finally, ecosystem functioning in vents and seeps was highly similar despite environmental differences (e.g. physico-chemistry, dominant basal sources) suggesting that ecological niches are not specifically linked to the nature of fluids. This comparison of seep and vent functioning in the Guaymas basin thus provides further supports to the hypothesis of continuity among deep-sea chemosynthetic ecosystems.
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Affiliation(s)
- Marie Portail
- Laboratoire Environnement Profond, REM/EEP, Institut Carnot Ifremer EDROME, Centre de Bretagne, Plouzané, France
- * E-mail:
| | - Karine Olu
- Laboratoire Environnement Profond, REM/EEP, Institut Carnot Ifremer EDROME, Centre de Bretagne, Plouzané, France
| | - Stanislas F. Dubois
- Laboratoire Ecologie Benthique, DYNECO, Ifremer, Centre de Bretagne, Plouzané, France
| | - Elva Escobar-Briones
- Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Mexico City D.F., Mexico
| | - Yves Gelinas
- GEOTOP and Chemistry and Biochemistry Department, Concordia University, Montréal, Québec, Canada
| | - Lénaick Menot
- Laboratoire Environnement Profond, REM/EEP, Institut Carnot Ifremer EDROME, Centre de Bretagne, Plouzané, France
| | - Jozée Sarrazin
- Laboratoire Environnement Profond, REM/EEP, Institut Carnot Ifremer EDROME, Centre de Bretagne, Plouzané, France
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11
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Matos MN, Lozada M, Anselmino LE, Musumeci MA, Henrissat B, Jansson JK, Mac Cormack WP, Carroll J, Sjöling S, Lundgren L, Dionisi HM. Metagenomics unveils the attributes of the alginolytic guilds of sediments from four distant cold coastal environments. Environ Microbiol 2016; 18:4471-4484. [PMID: 27348213 DOI: 10.1111/1462-2920.13433] [Citation(s) in RCA: 21] [Impact Index Per Article: 2.6] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/05/2016] [Accepted: 05/23/2016] [Indexed: 12/20/2022]
Abstract
Alginates are abundant polysaccharides in brown algae that constitute an important energy source for marine heterotrophic bacteria. Despite the key role of alginate degradation processes in the marine carbon cycle, little information is available on the bacterial populations involved in these processes. The aim of this work was to gain a better understanding of alginate utilization capabilities in cold coastal environments. Sediment metagenomes from four high-latitude regions of both Hemispheres were interrogated for alginate lyase gene homologue sequences and their genomic context. Sediments contained highly abundant and diverse bacterial assemblages with alginolytic potential, including members of Bacteroidetes and Proteobacteria, as well as several poorly characterized taxa. The microbial communities in Arctic and Antarctic sediments exhibited the most similar alginolytic profiles, whereas brackish sediments showed distinct structures with a higher proportion of novel genes. Examination of the gene neighbourhood of the alginate lyase homologues revealed distinct patterns depending on the potential lineage of the scaffolds, with evidence of evolutionary relationships among alginolytic gene clusters from Bacteroidetes and Proteobacteria. This information is relevant for understanding carbon fluxes in cold coastal environments and provides valuable information for the development of biotechnological applications from brown algae biomass.
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Affiliation(s)
- Marina N Matos
- Laboratorio de Microbiología Ambiental, Centro para el Estudio de Sistemas Marinos (CESIMAR, CONICET), Puerto Madryn, U9120ACD, Argentina
| | - Mariana Lozada
- Laboratorio de Microbiología Ambiental, Centro para el Estudio de Sistemas Marinos (CESIMAR, CONICET), Puerto Madryn, U9120ACD, Argentina
| | - Luciano E Anselmino
- Laboratorio de Microbiología Ambiental, Centro para el Estudio de Sistemas Marinos (CESIMAR, CONICET), Puerto Madryn, U9120ACD, Argentina
| | - Matías A Musumeci
- Laboratorio de Microbiología Ambiental, Centro para el Estudio de Sistemas Marinos (CESIMAR, CONICET), Puerto Madryn, U9120ACD, Argentina
| | - Bernard Henrissat
- Architecture et Fonction des Macromolécules Biologiques, CNRS, Aix-Marseille Université, Marseille, 13288, France.,INRA, USC 1408 AFMB, Marseille, F-13288, France.,Department of Biological Sciences, King Abdulaziz University, Jeddah, 21589, Saudi Arabia
| | - Janet K Jansson
- Earth and Biological Sciences Directorate, Pacific Northwest National Laboratory, Richland, WA, 99352, USA
| | - Walter P Mac Cormack
- Instituto Antártico Argentino, Ciudad Autónoma de Buenos Aires, C1064ABR, Argentina.,Instituto Nanobiotec, CONICET - Universidad de Buenos Aires, Ciudad Autónoma de Buenos Aires, C1113AAC, Argentina
| | - JoLynn Carroll
- Akvaplan-niva, Fram - High North Research Centre for Climate and the Environment, Tromsø, NO-9296, Norway.,CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, UiT The Arctic University of Norway, Tromsø, N-9037, Norway
| | - Sara Sjöling
- School of Natural Sciences and Environmental Studies, Södertörn University, Huddinge, 141 89, Sweden
| | | | - Hebe M Dionisi
- Laboratorio de Microbiología Ambiental, Centro para el Estudio de Sistemas Marinos (CESIMAR, CONICET), Puerto Madryn, U9120ACD, Argentina
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12
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Natarajan VP, Zhang X, Morono Y, Inagaki F, Wang F. A Modified SDS-Based DNA Extraction Method for High Quality Environmental DNA from Seafloor Environments. Front Microbiol 2016; 7:986. [PMID: 27446026 PMCID: PMC4917542 DOI: 10.3389/fmicb.2016.00986] [Citation(s) in RCA: 56] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/01/2016] [Accepted: 06/08/2016] [Indexed: 02/01/2023] Open
Abstract
Recovering high quality genomic DNA from environmental samples is a crucial primary step to understand the genetic, metabolic, and evolutionary characteristics of microbial communities through molecular ecological approaches. However, it is often challenging because of the difficulty of effective cell lysis without fragmenting the genomic DNA. This work aims to improve the previous SDS-based DNA extraction methods for high-biomass seafloor samples, such as pelagic sediments and metal sulfide chimney, to obtain high quality and high molecular weight of the genomic DNA applicable for the subsequent molecular ecological analyses. In this regard, we standardized a modified SDS-based DNA extraction method (M-SDS), and its performance was then compared to those extracted by a recently developed hot-alkaline DNA extraction method (HA) and a commercial DNA extraction kit. Consequently, the M-SDS method resulted in higher DNA yield and cell lysis efficiency, lower DNA shearing, and higher diversity scores than other two methods, providing a comprehensive DNA assemblage of the microbial community on the seafloor depositional environment.
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Affiliation(s)
- Vengadesh Perumal Natarajan
- State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong UniversityShanghai, China; State Key Laboratory of Ocean Engineering, Shanghai Jiao Tong UniversityShanghai, China
| | - Xinxu Zhang
- Guangdong Provincial Key Laboratory of Marine Biology, Marine Biology Institute, Shantou University Shantou, China
| | - Yuki Morono
- Geomicrobiology Group, Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology Kochi, Japan
| | - Fumio Inagaki
- Geomicrobiology Group, Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology Kochi, Japan
| | - Fengping Wang
- State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong UniversityShanghai, China; State Key Laboratory of Ocean Engineering, Shanghai Jiao Tong UniversityShanghai, China
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13
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Li W, Wang MM, Wang XG, Cheng XL, Guo JJ, Bian XM, Cai L. Fungal communities in sediments of subtropical Chinese seas as estimated by DNA metabarcoding. Sci Rep 2016; 6:26528. [PMID: 27198490 PMCID: PMC4873734 DOI: 10.1038/srep26528] [Citation(s) in RCA: 33] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/26/2016] [Accepted: 05/04/2016] [Indexed: 12/04/2022] Open
Abstract
Ribosomal RNA internal transcribed spacer-1 (ITS1) metabarcoding was used to investigate the distribution patterns of fungal communities and the factors influencing these patterns in subtropical Chinese seas, including the southern and northern Yellow Sea and the Bohai Sea. These seas were found to harbor high levels of fungal diversity, with 816 operational taxonomic units (OTUs) that span 130 known genera, 36 orders, 14 classes and 5 phyla. Ascomycota was the most abundant phylum, containing 72.18% and 79.61% of all OTUs and sequences, respectively, followed by Basidiomycota (19.98%, 18.64%), Zygomycota (1.10%, 0.11%), Chytridiomycota (0.25%, 0.04%) and Rozellomycota (0.12%, 0.006%). The compositions of fungal communities across these three sea regions were found to be vary, which may be attributed to sediment source, geographical distance, latitude and some environmental factors such as the temperature and salinity of bottom water, water depth, total nitrogen, and the ratio of total organic carbon to nitrogen. Among these environmental factors, the temperature of bottom water is the most important driver that governs the distribution patterns of fungal communities across the sampled seas. Our data also suggest that the cold-water mass of the Yellow Sea likely balances competitive relationships between fungal taxa rather than increasing species richness levels.
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Affiliation(s)
- Wei Li
- College of Marine Life Sciences, Ocean University of China, Qingdao 266003, China
| | - Meng Meng Wang
- College of Marine Life Sciences, Ocean University of China, Qingdao 266003, China
| | - Xi Guang Wang
- Institute of Agricultural Information, Chinese Academy of Agricultural Sciences, Beijing 100081, China
| | - Xiao Li Cheng
- College of Marine Life Sciences, Ocean University of China, Qingdao 266003, China
- State Key Laboratory of Mycology, Institute of Microbiology, Chinese Academy of Sciences, Beijing 100101, China
| | - Jia Jia Guo
- College of Marine Life Sciences, Ocean University of China, Qingdao 266003, China
| | - Xiao Meng Bian
- College of Marine Life Sciences, Ocean University of China, Qingdao 266003, China
| | - Lei Cai
- State Key Laboratory of Mycology, Institute of Microbiology, Chinese Academy of Sciences, Beijing 100101, China
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14
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Complementary Microorganisms in Highly Corrosive Biofilms from an Offshore Oil Production Facility. Appl Environ Microbiol 2016; 82:2545-2554. [PMID: 26896143 DOI: 10.1128/aem.03842-15] [Citation(s) in RCA: 97] [Impact Index Per Article: 12.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/26/2015] [Accepted: 02/11/2016] [Indexed: 11/20/2022] Open
Abstract
Offshore oil production facilities are frequently victims of internal piping corrosion, potentially leading to human and environmental risks and significant economic losses. Microbially influenced corrosion (MIC) is believed to be an important factor in this major problem for the petroleum industry. However, knowledge of the microbial communities and metabolic processes leading to corrosion is still limited. Therefore, the microbial communities from three anaerobic biofilms recovered from the inside of a steel pipe exhibiting high corrosion rates, iron oxide deposits, and substantial amounts of sulfur, which are characteristic of MIC, were analyzed in detail. Bacterial and archaeal community structures were investigated by automated ribosomal intergenic spacer analysis, multigenic (16S rRNA and functional genes) high-throughput Illumina MiSeq sequencing, and quantitative PCR analysis. The microbial community analysis indicated that bacteria, particularly Desulfovibrio species, dominated the biofilm microbial communities. However, other bacteria, such as Pelobacter, Pseudomonas, and Geotoga, as well as various methanogenic archaea, previously detected in oil facilities were also detected. The microbial taxa and functional genes identified suggested that the biofilm communities harbored the potential for a number of different but complementary metabolic processes and that MIC in oil facilities likely involves a range of microbial metabolisms such as sulfate, iron, and elemental sulfur reduction. Furthermore, extreme corrosion leading to leakage and exposure of the biofilms to the external environment modify the microbial community structure by promoting the growth of aerobic hydrocarbon-degrading organisms.
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15
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Warren LA, Kendra KE, Brady AL, Slater GF. Sulfur Biogeochemistry of an Oil Sands Composite Tailings Deposit. Front Microbiol 2016; 6:1533. [PMID: 26869997 PMCID: PMC4737920 DOI: 10.3389/fmicb.2015.01533] [Citation(s) in RCA: 22] [Impact Index Per Article: 2.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/01/2015] [Accepted: 12/21/2015] [Indexed: 11/13/2022] Open
Abstract
Composite tailings (CT), an engineered, alkaline, saline mixture of oil sands tailings (FFT), processed sand and gypsum (CaSO4; 1 kg CaSO4 per m3 FFT) are used as a dry reclamation strategy in the Alberta Oil Sands Region (AOSR). It is estimated that 9.6 × 108 m3 of CT are either in, or awaiting emplacement in surface pits within the AOSR, highlighting their potential global importance in sulfur cycling. Here, in the first CT sulfur biogeochemistry investigation, integrated geochemical, pyrosequencing and lipid analyses identified high aqueous concentrations of ∑H2S (>300 μM) and highly altered sulfur compounds composition; low cell biomass (3.3 × 106– 6.0 × 106 cells g−1) and modest bacterial diversity (H' range between 1.4 and 1.9) across 5 depths spanning 34 m of an in situ CT deposit. Pyrosequence results identified a total of 29,719 bacterial 16S rRNA gene sequences, representing 131 OTUs spanning19 phyla including 7 candidate divisions, not reported in oil sands tailings pond studies to date. Legacy FFT common phyla, notably, gamma and beta Proteobacteria, Firmicutes, Actinobacteria, and Chloroflexi were represented. However, overall CT microbial diversity and PLFA values were low relative to other contexts. The identified known sulfate/sulfur reducing bacteria constituted at most 2% of the abundance; however, over 90% of the 131 OTUs identified are capable of sulfur metabolism. While PCR biases caution against overinterpretation of pyrosequence surveys, bacterial sequence results identified here, align with phospholipid fatty acid (PLFA) and geochemical results. The highest bacterial diversities were associated with the depth of highest porewater [∑H2S] (22–24 m) and joint porewater co-occurrence of Fe2+ and ∑H2S (6–8 m). Three distinct bacterial community structure depths corresponded to CT porewater regions of (1) shallow evident Fe(II) (<6 m), (2) co-occurring Fe(II) and ∑H2S (6–8 m) and (3) extensive ∑H2S (6–34 m) (UniFrac). Candidate divisions GNO2, NKB19 and Spam were present only at 6–8 m associated with co-occurring [Fe(II)] and [∑H2S]. Collectively, results indicate that CT materials are differentiated from other sulfur rich environments by modestly diverse, low abundance, but highly sulfur active and more enigmatic communities (7 candidate divisions present within the 19 phyla identified).
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Affiliation(s)
- Lesley A Warren
- School of Geography and Earth Sciences, McMaster University Hamilton ON, Canada
| | - Kathryn E Kendra
- School of Geography and Earth Sciences, McMaster University Hamilton ON, Canada
| | - Allyson L Brady
- School of Geography and Earth Sciences, McMaster University Hamilton ON, Canada
| | - Greg F Slater
- School of Geography and Earth Sciences, McMaster University Hamilton ON, Canada
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16
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Wong HL, Ahmed-Cox A, Burns BP. Molecular Ecology of Hypersaline Microbial Mats: Current Insights and New Directions. Microorganisms 2016; 4:microorganisms4010006. [PMID: 27681900 PMCID: PMC5029511 DOI: 10.3390/microorganisms4010006] [Citation(s) in RCA: 26] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/07/2015] [Revised: 12/08/2015] [Accepted: 12/15/2015] [Indexed: 11/17/2022] Open
Abstract
Microbial mats are unique geobiological ecosystems that form as a result of complex communities of microorganisms interacting with each other and their physical environment. Both the microorganisms present and the network of metabolic interactions govern ecosystem function therein. These systems are often found in a range of extreme environments, and those found in elevated salinity have been particularly well studied. The purpose of this review is to briefly describe the molecular ecology of select model hypersaline mat systems (Guerrero Negro, Shark Bay, S’Avall, and Kiritimati Atoll), and any potentially modulating effects caused by salinity to community structure. In addition, we discuss several emerging issues in the field (linking function to newly discovered phyla and microbial dark matter), which illustrate the changing paradigm that is seen as technology has rapidly advanced in the study of these extreme and evolutionally significant ecosystems.
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Affiliation(s)
- Hon Lun Wong
- School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney 2052, Australia.
- Australian Centre for Astrobiology, University of New South Wales, Sydney 2052, Australia.
| | - Aria Ahmed-Cox
- School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney 2052, Australia.
| | - Brendan Paul Burns
- School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney 2052, Australia.
- Australian Centre for Astrobiology, University of New South Wales, Sydney 2052, Australia.
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17
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Oni OE, Schmidt F, Miyatake T, Kasten S, Witt M, Hinrichs KU, Friedrich MW. Microbial Communities and Organic Matter Composition in Surface and Subsurface Sediments of the Helgoland Mud Area, North Sea. Front Microbiol 2015; 6:1290. [PMID: 26635758 PMCID: PMC4658423 DOI: 10.3389/fmicb.2015.01290] [Citation(s) in RCA: 57] [Impact Index Per Article: 6.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/29/2015] [Accepted: 11/04/2015] [Indexed: 01/05/2023] Open
Abstract
The role of microorganisms in the cycling of sedimentary organic carbon is a crucial one. To better understand relationships between molecular composition of a potentially bioavailable fraction of organic matter and microbial populations, bacterial and archaeal communities were characterized using pyrosequencing-based 16S rRNA gene analysis in surface (top 30 cm) and subsurface/deeper sediments (30-530 cm) of the Helgoland mud area, North Sea. Fourier Transform Ion Cyclotron Resonance Mass Spectrometry (FT-ICR MS) was used to characterize a potentially bioavailable organic matter fraction (hot-water extractable organic matter, WE-OM). Algal polymer-associated microbial populations such as members of the Gammaproteobacteria, Bacteroidetes, and Verrucomicrobia were dominant in surface sediments while members of the Chloroflexi (Dehalococcoidales and candidate order GIF9) and Miscellaneous Crenarchaeota Groups (MCG), both of which are linked to degradation of more recalcitrant, aromatic compounds and detrital proteins, were dominant in subsurface sediments. Microbial populations dominant in subsurface sediments (Chloroflexi, members of MCG, and Thermoplasmata) showed strong correlations to total organic carbon (TOC) content. Changes of WE-OM with sediment depth reveal molecular transformations from oxygen-rich [high oxygen to carbon (O/C), low hydrogen to carbon (H/C) ratios] aromatic compounds and highly unsaturated compounds toward compounds with lower O/C and higher H/C ratios. The observed molecular changes were most pronounced in organic compounds containing only CHO atoms. Our data thus, highlights classes of sedimentary organic compounds that may serve as microbial energy sources in methanic marine subsurface environments.
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Affiliation(s)
- Oluwatobi E Oni
- Department of Microbial Ecophysiology, University of Bremen Bremen, Germany ; MARUM-Center for Marine Environmental Sciences, University of Bremen Bremen, Germany ; International Max-Planck Research School for Marine Microbiology Bremen, Germany
| | - Frauke Schmidt
- MARUM-Center for Marine Environmental Sciences, University of Bremen Bremen, Germany
| | - Tetsuro Miyatake
- Department of Microbial Ecophysiology, University of Bremen Bremen, Germany
| | - Sabine Kasten
- MARUM-Center for Marine Environmental Sciences, University of Bremen Bremen, Germany ; Department of Marine Geochemistry, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Bremerhaven, Germany
| | | | - Kai-Uwe Hinrichs
- MARUM-Center for Marine Environmental Sciences, University of Bremen Bremen, Germany
| | - Michael W Friedrich
- Department of Microbial Ecophysiology, University of Bremen Bremen, Germany ; MARUM-Center for Marine Environmental Sciences, University of Bremen Bremen, Germany
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18
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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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19
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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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20
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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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21
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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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22
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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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23
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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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24
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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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25
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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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26
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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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27
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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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28
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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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29
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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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30
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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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31
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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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32
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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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33
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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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34
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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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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 9969=9969-- bqjm] [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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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 5417=7636-- tabb] [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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37
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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-- ntbd] [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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38
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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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|
39
|
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 rlike (select (case when (7991=6814) then 0x31302e313132382f61656d2e30303134372d3135 else 0x28 end))-- awkz] [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
|
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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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 (8714=1632) then null else ctxsys.drithsx.sn(1,8714) 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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43
|
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
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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))] [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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46
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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))] [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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|
47
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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 8053=(select (case when (8053=6425) then 8053 else (select 6425 union select 9502) end))-- fyqk] [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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|
48
|
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-- boza] [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 rlike (select (case when (3247=9761) then 0x31302e313132382f61656d2e30303134372d3135 else 0x28 end))] [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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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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|