Detection of Survival and Proliferation of Sulfate Reducers Under
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Multiple Lateral Transfers of Dissimilatory Sulfite Reductase
JOURNAL OF BACTERIOLOGY, Oct. 2001, p. 6028–6035 Vol. 183, No. 20 0021-9193/01/$04.00ϩ0 DOI: 10.1128/JB.183.20.6028–6035.2001 Copyright © 2001, American Society for Microbiology. All Rights Reserved. Multiple Lateral Transfers of Dissimilatory Sulfite Reductase Genes between Major Lineages of Sulfate-Reducing Prokaryotes MICHAEL KLEIN,1 MICHAEL FRIEDRICH,2 ANDREW J. ROGER,3 PHILIP HUGENHOLTZ,4 SUSAN FISHBAIN,5 1 4 6 1 HEIKE ABICHT, LINDA L. BLACKALL, DAVID A. STAHL, AND MICHAEL WAGNER * 1 Lehrstuhl fu¨r Mikrobiologie, Technische Universita¨t Mu¨nchen, D-85350 Freising, and Department of Biogeochemistry, Max Planck Downloaded from Institute for Terrestrial Microbiology, D-35043-Marburg,2 Germany; Department of Biochemistry and Molecular Biology, Dalhousie University, Halifax, Nova Scotia B3H 4H7, Canada3; Advanced Wastewater Management Centre, Department of Microbiology and Parasitology, The University of Queensland, Brisbane 4072, Queensland, Australia4; Department of Civil Engineering, Northwestern University, Evanston, Illinois 60208-31095; and Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington 98195-27006 Received 26 February 2001/Accepted 3 July 2001 http://jb.asm.org/ A large fragment of the dissimilatory sulfite reductase genes (dsrAB) was PCR amplified and fully sequenced from 30 reference strains representing all recognized lineages of sulfate-reducing bacteria. In addition, the sequence of the dsrAB gene homologs of the sulfite reducer Desulfitobacterium dehalogenans was determined. In contrast to previous reports, comparative analysis of all available DsrAB sequences produced a tree topology partially inconsistent with the corresponding 16S rRNA phylogeny. For example, the DsrAB sequences of -several Desulfotomaculum species (low G؉C gram-positive division) and two members of the genus Thermode sulfobacterium (a separate bacterial division) were monophyletic with ␦-proteobacterial DsrAB sequences. -
Table 1. Overview of Reactions Examined in This Study. ΔG Values Were Obtained from Thauer Et Al., 1977
Supplemental Information: Table 1. Overview of reactions examined in this study. ΔG values were obtained from Thauer et al., 1977. No. Equation ∆G°' (kJ/reaction)* Acetogenic reactions – – – + 1 Propionate + 3 H2O → Acetate + HCO3 + 3 H2 + H +76.1 Sulfate-reducing reactions – 2– – – – + 2 Propionate + 0.75 SO4 → Acetate + 0.75 HS + HCO3 + 0.25 H –37.8 2– + – 3 4 H2 + SO4 + H → HS + 4 H2O –151.9 – 2– – – 4 Acetate + SO4 → 2 HCO3 + HS –47.6 Methanogenic reactions – – + 5 4 H2 + HCO3 + H → CH4 + 3 H2O –135.6 – – 6 Acetate + H2O → CH4 + HCO3 –31.0 Syntrophic propionate conversion – – – + 1+5 Propionate + 0.75 H2O → Acetate + 0.75 CH4 + 0.25 HCO3 + 0.25 H –25.6 Complete propionate conversion by SRB – 2– – – + 2+4 Propionate + 1.75 SO4 → 1.75 HS + 3 HCO3 + 0.25 H –85.4 Complete propionate conversion by syntrophs and methanogens 1+5+6 Propionate– + 1.75 H O → 1.75 CH + 1.25 HCO – + 0.25 H+ –56.6 2 4 3 1 Table S2. Overview of all enrichment slurries fed with propionate and the total amounts of the reactants consumed and products formed during the enrichment period. The enrichment slurries consisted of sediment from either the sulfate zone (SZ), sulfate-methane transition zone (SMTZ) or methane zone (MZ) and were incubated at 25°C or 10°C, with 3 mM, 20 mM or without (-) sulfate amendments along the study. The slurries P1/P2, P3/P4, P5/P6, P7/P8 from each sediment zone are biological replicates. Slurries with * are presented in the propionate conversion graphs and used for molecular analysis. -
Microbial Fe(III) Oxide Reduction Potential in Chocolate Pots Hot Spring, Yellowstone National Park N
Geobiology (2016), 14, 255–275 DOI: 10.1111/gbi.12173 Microbial Fe(III) oxide reduction potential in Chocolate Pots hot spring, Yellowstone National Park N. W. FORTNEY,1 S. HE,1 B. J. CONVERSE,1 B. L. BEARD,1 C. M. JOHNSON,1 E. S. BOYD2 ANDE.E.RODEN1 1Department of Geoscience, NASA Astrobiology Institute, University of Wisconsin-Madison, Madison, WI, USA 2Department of Microbiology and Immunology, NASA Astrobiology Institute, Montana State University, Bozeman, MT, USA ABSTRACT Chocolate Pots hot springs (CP) is a unique, circumneutral pH, iron-rich, geothermal feature in Yellowstone National Park. Prior research at CP has focused on photosynthetically driven Fe(II) oxidation as a model for mineralization of microbial mats and deposition of Archean banded iron formations. However, geochemical and stable Fe isotopic data have suggested that dissimilatory microbial iron reduction (DIR) may be active within CP deposits. In this study, the potential for microbial reduction of native CP Fe(III) oxides was inves- tigated, using a combination of cultivation dependent and independent approaches, to assess the potential involvement of DIR in Fe redox cycling and associated stable Fe isotope fractionation in the CP hot springs. Endogenous microbial communities were able to reduce native CP Fe(III) oxides, as documented by most probable number enumerations and enrichment culture studies. Enrichment cultures demonstrated sus- tained DIR driven by oxidation of acetate, lactate, and H2. Inhibitor studies and molecular analyses indicate that sulfate reduction did not contribute to observed rates of DIR in the enrichment cultures through abi- otic reaction pathways. Enrichment cultures produced isotopically light Fe(II) during DIR relative to the bulk solid-phase Fe(III) oxides. -
Prokaryotic Community Structure and Activity of Sulfate Reducers in Production Water from High-Temperature Oil Reservoirs with and Without Nitrate Treatment
Prokaryotic community structure and activity of sulfate reducers in production water from high-temperature oil reservoirs with and without nitrate treatment Dr. Antje Gittel Dept. of Biological Sciences, Aarhus University ISMOS 2 Aarhus 2009 Introduction Hypothesis Results Conclusions Offshore oil production systems Separation Oil Gas Water Production Injection ~80 degC 50-60 degC Reservoir ISMOS 2, June 2009 Antje Gittel Introduction Hypothesis Results Conclusions Characteristics of the study sites Norway Halfdan • Injection of sulfate-rich seawater Denmark • High loads of organic carbon compounds in the reservoir Dan Enrichment of sulfate -reducing prokaryotes Danish Underground Consortium, Maersk Oil (SRP ) that produce H 2S Souring, plugging, biocorrosion, toxicity, ..... • Strategy to control SRP activity at Halfdan: Addition of nitrate to the injection water ISMOS 2, June 2009 Antje Gittel Introduction Hypothesis Results Conclusions Principles of SRP inhibition by nitrate addition (i) Stimulation of heterothrophic nitrate- reducing bacteria (hNRB ) that hNRB outcompete SRP for electron donors (ii) Activity of nitrate -reducing, sulfide - oxidizing bacteria (NR-SOB ) resulting in SRP NR-SOB a decreasing net production of H2S (iii) Increase in redox potential by the production of nitrite and nitrous oxides and thereby and inhibition of SRP ISMOS 2, June 2009 Antje Gittel Introduction Hypothesis Results Conclusions Compared to an untreated oil field (Dan), nitrate addition to the injection water at Halfdan stimulates the growth of hNRB and/or NR-SOB , resulting in: 1) A general change in the prokaryotic community composition, i.e. • Presence of competitive hNRB and NR-SOB and/or • Presence of SRP that are able to reduce nitrate instead of sulfate 2) A decrease in SRP abundance and activity and 3) A reduced net sulfide production. -
Supplementary Information for Microbial Electrochemical Systems Outperform Fixed-Bed Biofilters for Cleaning-Up Urban Wastewater
Electronic Supplementary Material (ESI) for Environmental Science: Water Research & Technology. This journal is © The Royal Society of Chemistry 2016 Supplementary information for Microbial Electrochemical Systems outperform fixed-bed biofilters for cleaning-up urban wastewater AUTHORS: Arantxa Aguirre-Sierraa, Tristano Bacchetti De Gregorisb, Antonio Berná, Juan José Salasc, Carlos Aragónc, Abraham Esteve-Núñezab* Fig.1S Total nitrogen (A), ammonia (B) and nitrate (C) influent and effluent average values of the coke and the gravel biofilters. Error bars represent 95% confidence interval. Fig. 2S Influent and effluent COD (A) and BOD5 (B) average values of the hybrid biofilter and the hybrid polarized biofilter. Error bars represent 95% confidence interval. Fig. 3S Redox potential measured in the coke and the gravel biofilters Fig. 4S Rarefaction curves calculated for each sample based on the OTU computations. Fig. 5S Correspondence analysis biplot of classes’ distribution from pyrosequencing analysis. Fig. 6S. Relative abundance of classes of the category ‘other’ at class level. Table 1S Influent pre-treated wastewater and effluents characteristics. Averages ± SD HRT (d) 4.0 3.4 1.7 0.8 0.5 Influent COD (mg L-1) 246 ± 114 330 ± 107 457 ± 92 318 ± 143 393 ± 101 -1 BOD5 (mg L ) 136 ± 86 235 ± 36 268 ± 81 176 ± 127 213 ± 112 TN (mg L-1) 45.0 ± 17.4 60.6 ± 7.5 57.7 ± 3.9 43.7 ± 16.5 54.8 ± 10.1 -1 NH4-N (mg L ) 32.7 ± 18.7 51.6 ± 6.5 49.0 ± 2.3 36.6 ± 15.9 47.0 ± 8.8 -1 NO3-N (mg L ) 2.3 ± 3.6 1.0 ± 1.6 0.8 ± 0.6 1.5 ± 2.0 0.9 ± 0.6 TP (mg -
Microbial Diversity Under Extreme Euxinia: Mahoney Lake, Canada V
Geobiology (2012), 10, 223–235 DOI: 10.1111/j.1472-4669.2012.00317.x Microbial diversity under extreme euxinia: Mahoney Lake, Canada V. KLEPAC-CERAJ,1,2 C. A. HAYES,3 W. P. GILHOOLY,4 T. W. LYONS,5 R. KOLTER2 AND A. PEARSON3 1Department of Molecular Genetics, Forsyth Institute, Cambridge, MA, USA 2Department of Microbiology and Molecular Genetics, Harvard Medical School, Boston, MA, USA 3Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA 4Department of Earth and Planetary Sciences, Washington University, Saint Louis, MO, USA 5Department of Earth Sciences, University of California, Riverside, CA, USA ABSTRACT Mahoney Lake, British Columbia, Canada, is a stratified, 15-m deep saline lake with a euxinic (anoxic, sulfidic) hypolimnion. A dense plate of phototrophic purple sulfur bacteria is found at the chemocline, but to date the rest of the Mahoney Lake microbial ecosystem has been underexamined. In particular, the microbial community that resides in the aphotic hypolimnion and ⁄ or in the lake sediments is unknown, and it is unclear whether the sulfate reducers that supply sulfide for phototrophy live only within, or also below, the plate. Here we profiled distribu- tions of 16S rRNA genes using gene clone libraries and PhyloChip microarrays. Both approaches suggest that microbial diversity is greatest in the hypolimnion (8 m) and sediments. Diversity is lowest in the photosynthetic plate (7 m). Shallower depths (5 m, 7 m) are rich in Actinobacteria, Alphaproteobacteria, and Gammaproteo- bacteria, while deeper depths (8 m, sediments) are rich in Crenarchaeota, Natronoanaerobium, and Verrucomi- crobia. The heterogeneous distribution of Deltaproteobacteria and Epsilonproteobacteria between 7 and 8 m is consistent with metabolisms involving sulfur intermediates in the chemocline, but complete sulfate reduction in the hypolimnion. -
Isolation and Characterization of a Thermophilic Sulfate-Reducing Bacterium, Desuvotomaculum Themosapovorans Sp
- INTERNATIONALJOURNAL OF SYSTEMATICBACTERIOLOGY, Apr. 1995, p. 218-221 Vol. 45, No. 2 0020-7713/95/$04.00+0 Copyright O 1995, International Union of Microbiological Societies Isolation and Characterization of a Thermophilic Sulfate-Reducing Bacterium, Desuvotomaculum themosapovorans sp. nov. MARIE-LAURE FARDEAU,1,''' BERNARD OLLIVIER: BHARAT K. C. PATEL?3 PREM DWIVEDI? MICHEL RAGOT? AND JEAN-LOUIS GARCIA' Laboratoire de Chimie Bactérienne, Centre National de la Recherche ScieiitiJque, 13277 Marseille cedex 9, and Laboratoire de Microbiologie ORSTOM, Université de Provence, 13331 Marseille cedex 3, France, and Faculty of Science and Technology, Crifith University, Biisbane, Queensland 4111, Australia3 Strain MLFT (T = type strain), a new thermophilic, spore-forming sulfate-reducing bacterium, was char- acterized and was found to be phenotypically, genotypically, and phylogenetically related to the genus Desul- fotornaculurn. This organism was isolated from a butyrate enrichment culture that had been inoculated with a mixed compost containing rice hulls and peanut shells. The optimum temperature for growth was 50°C. The G+C content of the DNA was 51.2 mol%. Strain MLFT incompletely oxidized pyruvate, butyrate, and butanol to acetate and presumably CO,. It used long-chain fatty acids and propanediols. We observed phenotypic and phylogenetic differences between strain MLFT and other thermophilic Desulfotornaculum species that also oxidize long-chain fatty acids. On the basis of our results, we propose that strain MLFT is a member of a new species, Desulfotornaculum tliermosapovorarzs. In environments where conditions for the survival of the The organisms wcre cultivated under strictly anoxic conditions at 55°C. The basal strictly anaerobic sulfate-reducing bacteria are not provided medium contained (per liter of distilled water) 1.0 g of NH,Cl, 0.15 g of continuously, the sporulating species of the genus Desulfo- CaCI,. -
Desulfotomaculum Arcticum Sp. Nov., a Novel Spore-Forming, Moderately
International Journal of Systematic and Evolutionary Microbiology (2006), 56, 687–690 DOI 10.1099/ijs.0.64058-0 Desulfotomaculum arcticum sp. nov., a novel spore-forming, moderately thermophilic, sulfate- reducing bacterium isolated from a permanently cold fjord sediment of Svalbard Verona Vandieken,1 Christian Knoblauch2 and Bo Barker Jørgensen1 Correspondence 1Max-Planck-Institute for Marine Microbiology, Celsiusstr. 1, 28359 Bremen, Germany Verona Vandieken 2University of Hamburg, Institute of Soil Science, Allende-Platz 2, 20146 Hamburg, Germany [email protected] Strain 15T is a novel spore-forming, sulfate-reducing bacterium isolated from a permanently cold fjord sediment of Svalbard. Sulfate could be replaced by sulfite or thiosulfate. Hydrogen, formate, lactate, propionate, butyrate, hexanoate, methanol, ethanol, propanol, butanol, pyruvate, malate, succinate, fumarate, proline, alanine and glycine were used as electron donors in the presence of sulfate. Growth occurred with pyruvate as sole substrate. Optimal growth was observed at T pH 7?1–7?5 and concentrations of 1–1?5 % NaCl and 0?4 % MgCl2. Strain 15 grew between 26 and 46?5 6C and optimal growth occurred at 44 6C. Therefore, strain 15T apparently cannot grow at in situ temperatures of Arctic sediments from where it was isolated, and it was proposed that it was present in the sediment in the form of spores. The DNA G+C content was 48?9 mol%. Strain 15T was most closely related to Desulfotomaculum thermosapovorans MLFT (93?5% 16S rRNA gene sequence similarity). Strain 15T represents a novel species, for which the name Desulfotomaculum arcticum sp. nov. is proposed. The type strain is strain 15T (=DSM 17038T=JCM 12923T). -
Distribution of Sulfate-Reducing Communities from Estuarine to Marine Bay Waters Yannick Colin, M
Distribution of Sulfate-Reducing Communities from Estuarine to Marine Bay Waters Yannick Colin, M. Goñi-Urriza, C. Gassie, E. Carlier, M. Monperrus, R. Guyoneaud To cite this version: Yannick Colin, M. Goñi-Urriza, C. Gassie, E. Carlier, M. Monperrus, et al.. Distribution of Sulfate- Reducing Communities from Estuarine to Marine Bay Waters. Microbial Ecology, Springer Verlag, 2017, 73 (1), pp.39-49. 10.1007/s00248-016-0842-5. hal-01499135 HAL Id: hal-01499135 https://hal.archives-ouvertes.fr/hal-01499135 Submitted on 26 Sep 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - ShareAlike| 4.0 International License Microb Ecol (2017) 73:39–49 DOI 10.1007/s00248-016-0842-5 MICROBIOLOGY OF AQUATIC SYSTEMS Distribution of Sulfate-Reducing Communities from Estuarine to Marine Bay Waters Yannick Colin 1,2 & Marisol Goñi-Urriza1 & Claire Gassie1 & Elisabeth Carlier 1 & Mathilde Monperrus3 & Rémy Guyoneaud1 Received: 23 May 2016 /Accepted: 17 August 2016 /Published online: 31 August 2016 # Springer Science+Business Media New York 2016 Abstract Estuaries are highly dynamic ecosystems in which gradient. The concentration of cultured sulfidogenic microor- freshwater and seawater mix together. -
Phylogenetic and Functional Characterization of Symbiotic Bacteria in Gutless Marine Worms (Annelida, Oligochaeta)
Phylogenetic and functional characterization of symbiotic bacteria in gutless marine worms (Annelida, Oligochaeta) Dissertation zur Erlangung des Grades eines Doktors der Naturwissenschaften -Dr. rer. nat.- dem Fachbereich Biologie/Chemie der Universität Bremen vorgelegt von Anna Blazejak Oktober 2005 Die vorliegende Arbeit wurde in der Zeit vom März 2002 bis Oktober 2005 am Max-Planck-Institut für Marine Mikrobiologie in Bremen angefertigt. 1. Gutachter: Prof. Dr. Rudolf Amann 2. Gutachter: Prof. Dr. Ulrich Fischer Tag des Promotionskolloquiums: 22. November 2005 Contents Summary ………………………………………………………………………………….… 1 Zusammenfassung ………………………………………………………………………… 2 Part I: Combined Presentation of Results A Introduction .…………………………………………………………………… 4 1 Definition and characteristics of symbiosis ...……………………………………. 4 2 Chemoautotrophic symbioses ..…………………………………………………… 6 2.1 Habitats of chemoautotrophic symbioses .………………………………… 8 2.2 Diversity of hosts harboring chemoautotrophic bacteria ………………… 10 2.2.1 Phylogenetic diversity of chemoautotrophic symbionts …………… 11 3 Symbiotic associations in gutless oligochaetes ………………………………… 13 3.1 Biogeography and phylogeny of the hosts …..……………………………. 13 3.2 The environment …..…………………………………………………………. 14 3.3 Structure of the symbiosis ………..…………………………………………. 16 3.4 Transmission of the symbionts ………..……………………………………. 18 3.5 Molecular characterization of the symbionts …..………………………….. 19 3.6 Function of the symbionts in gutless oligochaetes ..…..…………………. 20 4 Goals of this thesis …….………………………………………………………….. -
Tree Scale: 1 D Bacteria P Desulfobacterota C Jdfr-97 O Jdfr-97 F Jdfr-97 G Jdfr-97 S Jdfr-97 Sp002010915 WGS ID MTPG01
d Bacteria p Desulfobacterota c Thermodesulfobacteria o Thermodesulfobacteriales f Thermodesulfobacteriaceae g Thermodesulfobacterium s Thermodesulfobacterium commune WGS ID JQLF01 d Bacteria p Desulfobacterota c Thermodesulfobacteria o Thermodesulfobacteriales f Thermodesulfobacteriaceae g Thermosulfurimonas s Thermosulfurimonas dismutans WGS ID LWLG01 d Bacteria p Desulfobacterota c Desulfofervidia o Desulfofervidales f DG-60 g DG-60 s DG-60 sp001304365 WGS ID LJNA01 ID WGS sp001304365 DG-60 s DG-60 g DG-60 f Desulfofervidales o Desulfofervidia c Desulfobacterota p Bacteria d d Bacteria p Desulfobacterota c Desulfofervidia o Desulfofervidales f Desulfofervidaceae g Desulfofervidus s Desulfofervidus auxilii RS GCF 001577525 1 001577525 GCF RS auxilii Desulfofervidus s Desulfofervidus g Desulfofervidaceae f Desulfofervidales o Desulfofervidia c Desulfobacterota p Bacteria d d Bacteria p Desulfobacterota c Thermodesulfobacteria o Thermodesulfobacteriales f Thermodesulfatatoraceae g Thermodesulfatator s Thermodesulfatator atlanticus WGS ID ATXH01 d Bacteria p Desulfobacterota c Desulfobacteria o Desulfatiglandales f NaphS2 g 4484-190-2 s 4484-190-2 sp002050025 WGS ID MVDB01 ID WGS sp002050025 4484-190-2 s 4484-190-2 g NaphS2 f Desulfatiglandales o Desulfobacteria c Desulfobacterota p Bacteria d d Bacteria p Desulfobacterota c Thermodesulfobacteria o Thermodesulfobacteriales f Thermodesulfobacteriaceae g QOAM01 s QOAM01 sp003978075 WGS ID QOAM01 d Bacteria p Desulfobacterota c BSN033 o UBA8473 f UBA8473 g UBA8473 s UBA8473 sp002782605 WGS -
Impacts of Desulfobacterales and Chromatiales on Sulfate Reduction in The
bioRxiv preprint doi: https://doi.org/10.1101/2020.08.16.252635; this version posted November 6, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Impacts of Desulfobacterales and Chromatiales on sulfate reduction in the 2 subtropical mangrove ecosystem as revealed by SMDB analysis 3 Shuming Mo 1, †, Jinhui Li 1, †, Bin Li 2, Ran Yu 1, Shiqing Nie 1, Zufan Zhang 1, Jianping 4 Liao 3, Qiong Jiang 1, Bing Yan 2, *, and Chengjian Jiang 1, 2 * 5 1 State Key Laboratory for Conservation and Utilization of Subtropical Agro- 6 bioresources, Guangxi Research Center for Microbial and Enzyme Engineering 7 Technology, College of Life Science and Technology, Guangxi University, Nanning 8 530004, China. 9 2 Guangxi Key Lab of Mangrove Conservation and Utilization, Guangxi Mangrove 10 Research Center, Guangxi Academy of Sciences, Beihai 536000, China. 11 3 School of Computer and Information Engineering, Nanning Normal University, 12 Nanning 530299, China. 13 † These authors contributed equally to this work. 14 *: Corresponding Author: 15 Tel: +86-771-3270736; Fax: +86-771-3237873 16 Email: [email protected] (CJ); [email protected] (BY) 17 1 bioRxiv preprint doi: https://doi.org/10.1101/2020.08.16.252635; this version posted November 6, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.