Sulfuricurvum Kujiense Type Strain (YK-1T)
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Niche Differentiation Among Sulfur-Oxidizing Bacterial Populations in Cave Waters
The ISME Journal (2008) 2, 590–601 & 2008 International Society for Microbial Ecology All rights reserved 1751-7362/08 $30.00 www.nature.com/ismej ORIGINAL ARTICLE Niche differentiation among sulfur-oxidizing bacterial populations in cave waters Jennifer L Macalady1, Sharmishtha Dattagupta1, Irene Schaperdoth1, Daniel S Jones1, Greg K Druschel2 and Danielle Eastman2 1Department of Geosciences, Pennsylvania State University, Pennsylvania, PA, USA and 2Department of Geology, University of Vermont, Burlington, VT, USA The sulfidic Frasassi cave system affords a unique opportunity to investigate niche relationships among sulfur-oxidizing bacteria, including epsilonproteobacterial clades with no cultivated representatives. Oxygen and sulfide concentrations in the cave waters range over more than two orders of magnitude as a result of seasonally and spatially variable dilution of the sulfidic groundwater. A full-cycle rRNA approach was used to quantify dominant populations in biofilms collected in both diluted and undiluted zones. Sulfide concentration profiles within biofilms were obtained in situ using microelectrode voltammetry. Populations in rock-attached streamers depended on the sulfide/oxygen supply ratio of bulk water (r ¼ 0.97; Po0.0001). Filamentous epsilonproteobacteria dominated at high sulfide to oxygen ratios (4150), whereas Thiothrix dominated at low ratios (o75). In contrast, Beggiatoa was the dominant group in biofilms at the sediment–water interface regardless of sulfide and oxygen concentrations or supply ratio. Our results -
Laboratory of Marine Environmental Microbiology
Division of Applied Biosciences, Graduate School of Agriculture, Kyoto University 12/09/2017 Laboratory of Marine Environmental Microbiology Professor:Shigeki SAWAYAMA, Associate professor:Satoshi NAKAGAWA This laboratory is doing researches on microalgal productions of ω-3 fatty acids, carotenoids and third-generation biofuels by genetic engineering. ω-3 Fatty acids and carotenoids have physiological functions and are used for dietary supplements. We are also searching novel and useful fungi from marine environments. In addition, we have studied ecophysiology and evolution of ‘earth-eating’ microorganisms inhabiting various extreme marine environments such as deep-sea hydrothermal fields. ω-3 Fatty acids, carotenoids and biofuel production using microalgae Chlorella spp. produce ω-3 fatty acids and Dunaliella spp. produce β-carotene known as a vitamin A pre-cursor. We are doing researches on molecular biology of these microalgae to produce useful compounds. Dunaliella salina Marine fungi and methanogens Fungi producing large amount of enzymes are widely used for fermentation industries. We are conducting research on screening of novel marine fungi. We are also studying ecological roles of methanogens in aquatic environments. Marine fungus with melon flavor Microbial ecophysiology and evolution in extreme marine environments. Rich microbial ecosystems exist in deep-sea and oceanic sediments, and even in rock deep inside Earth’s crust, where not long ago it was thought that life could not exist. We have studied ecophysiology and evolution of microorganisms inhabiting extreme marine environments. ©JAMSTEC DSV Shinkai6500 Key words Microalgae, ω-3 Fatty acid, Carotenoid, Biofuel, Fungi, Yeast, Methanogen, Deep-sea vents, Symbiosis, Extremophiles Research Achievements 2017 Overexpression of DnaJ-like chaperone enhances carotenoid synthesis in Chlamydomonas reinhardtii. -
Pdf Circulation
Western Washington University Western CEDAR Biology Faculty and Staff ubP lications Biology 8-28-2017 Community Structure of Lithotrophically-Driven Hydrothermal Microbial Mats from the Mariana Arc and Back-Arc Kevin W. Hager Western Washington University Heather Fullerton Western Washington University David A. Butterfield University of Washington Craig L. Moyer Western Washington University, [email protected] Follow this and additional works at: https://cedar.wwu.edu/biology_facpubs Part of the Biology Commons, and the Environmental Microbiology and Microbial Ecology Commons Recommended Citation Hager KW, Fullerton H, Butterfield DA and Moyer CL (2017) Community Structure of Lithotrophically-Driven Hydrothermal Microbial Mats from the Mariana Arc and Back-Arc. Front. Microbiol. 8:1578. doi: 10.3389/fmicb.2017.01578 This Article is brought to you for free and open access by the Biology at Western CEDAR. It has been accepted for inclusion in Biology Faculty and Staff ubP lications by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. ORIGINAL RESEARCH published: 28 August 2017 doi: 10.3389/fmicb.2017.01578 Community Structure of Lithotrophically-Driven Hydrothermal Microbial Mats from the Mariana Arc and Back-Arc Kevin W. Hager 1†, Heather Fullerton 1†, David A. Butterfield 2 and Craig L. Moyer 1* 1 Department of Biology, Western Washington University, Bellingham, WA, United States, 2 National Oceanic and Atmospheric Administration Pacific Marine Environmental Lab, Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, Seattle, WA, United States Edited by: Jesse G. Dillon, California State University, Long The Mariana region exhibits a rich array of hydrothermal venting conditions in a complex Beach, United States geological setting, which provides a natural laboratory to study the influence of local Reviewed by: environmental conditions on microbial community structure as well as large-scale Gilberto E. -
Metagenomic Insights Into S(0) Precipitation in a Terrestrial Subsurface Lithoautotrophic Ecosystem
ORIGINAL RESEARCH ARTICLE published: 08 January 2015 doi: 10.3389/fmicb.2014.00756 Metagenomic insights into S(0) precipitation in a terrestrial subsurface lithoautotrophic ecosystem Trinity L. Hamilton 1*, Daniel S. Jones 1,2, Irene Schaperdoth 1 and Jennifer L. Macalady 1* 1 Department of Geosciences, Penn State Astrobiology Research Center, The Pennsylvania State University, University Park, PA, USA 2 Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA Edited by: The Frasassi and Acquasanta Terme cave systems in Italy host isolated lithoautotrophic John R. Spear, Colorado School of ecosystems characterized by sulfur-oxidizing biofilms with up to 50% S(0) by mass. Mines, USA The net contributions of microbial taxa in the biofilms to production and consumption Reviewed by: of S(0) are poorly understood and have implications for understanding the formation Matthew Schrenk, Michigan State University, USA of geological sulfur deposits as well as the ecological niches of sulfur-oxidizing John R. Spear, Colorado School of autotrophs. Filamentous Epsilonproteobacteria are among the principal biofilm architects Mines, USA in Frasassi and Acquasanta Terme streams, colonizing high-sulfide, low-oxygen niches Takuro Nunoura, Japan Agency for relative to other major biofilm-forming populations. Metagenomic sequencing of eight Marine-Earth Science & Technology, Japan biofilm samples indicated the presence of diverse and abundant Epsilonproteobacteria. *Correspondence: Populations of Sulfurovum-like organisms were the most abundant Epsilonproteobacteria Trinity L. Hamilton and Jennifer L. regardless of differences in biofilm morphology, temperature, or water chemistry. After Macalady, Department of assembling and binning the metagenomic data, we retrieved four nearly-complete Geosciences, Penn State genomes of Sulfurovum-like organisms as well as a Sulfuricurvum spp. -
The Pennsylvania State University
The Pennsylvania State University The Graduate School College of Earth and Mineral Sciences CULTURE-DEPENDENT AND INDEPENDENT STUDIES OF SULFUR OXIDIZING BACTERIA FROM THE FRASASSI CAVES A Thesis in Geosciences by Leah E. Tsao © 2014 Leah E. Tsao Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science December 2014 The thesis of Leah E. Tsao was reviewed and approved* by the following: Jennifer L. Macalady Associate Professor of Geosciences Thesis Adviser Katherine H. Freeman Professor of Geosciences Christopher H. House Professor of Geosciences Demian Saffer Professor of Geosciences Interim Associate Head of the Department of Geosciences *Signatures are on file in the Graduate School. ii ABSTRACT The Frasassi Caves (Italy) are developed in calcium carbonate rocks and contain sulfide from groundwater and oxygen from both the cave atmosphere and downward percolating meteoric water. The presence of sulfide and oxygen allows for both the abiotic and biotic formation of sulfuric acid, which subsequently reacts with calcium carbonate cave walls to enlarge the cave. While the contribution of abiotic processes on cave development has been studied, less research has focused on microbial contributions through the complete oxidation of reduced sulfur sources. I used culture-dependent and culture-independent methods to study the metabolic properties of Thiobacillus baregensis, a dominant sulfur oxidizing bacterium in sulfidic streams within the cave system, and a novel strain of Sulfuricurvum kujiense (Sulfuricurvum sp. strain Frasassi), the first Epsilonproteobacterium successfully cultured from the Frasassi Caves. Since T. baregensis is abundant and capable of completely oxidizing multiple reduced sulfur sources, it is likely to contribute to cave development. -
An Oligarchic Microbial Assemblage in the Anoxic Bottom Waters of a Volcanic Subglacial Lake
The ISME Journal (2009) 3, 486–497 & 2009 International Society for Microbial Ecology All rights reserved 1751-7362/09 $32.00 www.nature.com/ismej ORIGINAL ARTICLE An oligarchic microbial assemblage in the anoxic bottom waters of a volcanic subglacial lake Eric Gaidos1,2, Viggo Marteinsson3, Thorsteinn Thorsteinsson4, Tomas Jo´hannesson5, A´ rni Rafn Ru´ narsson3, Andri Stefansson6, Brian Glazer7, Brian Lanoil8,11, Mark Skidmore9, Sukkyun Han8, Mary Miller10, Antje Rusch1 and Wilson Foo8 1Department of Geology and Geophysics, University of Hawaii at Manoa, Honolulu, HI, USA; 2NASA Astrobiology Institute, Mountain View, CA, USA; 3MATIS-Prokaria, Reykjavı´k, Iceland; 4Hydrological Service, National Energy Authority, Reykjavı´k, Iceland; 5Icelandic Meteorological Office, Reykjavı´k, Iceland; 6Science Institute, University of Iceland, Reykjavı´k, Iceland; 7Department of Oceanography, University of Hawaii, Honolulu, HI, USA; 8Department of Environmental Sciences, University of California at Riverside, Riverside, CA, USA; 9Department of Earth Sciences, Montana State University, Bozeman, MT, USA and 10Department of Microbiology and Immunology, University of Texas Medical Branch, Galveston, TX, USA In 2006, we sampled the anoxic bottom waters of a volcanic lake beneath the Vatnajo¨ kull ice cap (Iceland). The sample contained 5 Â 105 cells per ml, and whole-cell fluorescent in situ hybridization (FISH) and PCR with domain-specific probes showed these to be essentially all bacteria, with no detectable archaea. Pyrosequencing of the V6 hypervariable region of the 16S ribosomal RNA gene, Sanger sequencing of a clone library and FISH-based enumeration of four major phylotypes revealed that the assemblage was dominated by a few groups of putative chemotrophic bacteria whose closest cultivated relatives use sulfide, sulfur or hydrogen as electron donors, and oxygen, sulfate or CO2 as electron acceptors. -
Coupled Carbon, Sulfur, and Nitrogen Cycles Mediated by Microorganisms in the Water Column of a Shallow-Water Hydrothermal Ecosystem
fmicb-09-02718 November 10, 2018 Time: 13:43 # 1 ORIGINAL RESEARCH published: 13 November 2018 doi: 10.3389/fmicb.2018.02718 Coupled Carbon, Sulfur, and Nitrogen Cycles Mediated by Microorganisms in the Water Column of a Shallow-Water Hydrothermal Ecosystem Yufang Li1,2†, Kai Tang1,2†, Lianbao Zhang1,2, Zihao Zhao3, Xiabing Xie1, Chen-Tung Arthur Chen4, Deli Wang1,2, Nianzhi Jiao1,2 and Yao Zhang1,2* 1 State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, China, 2 College of Ocean and Earth Sciences, Xiamen University, Xiamen, China, 3 Department of Limnology and Bio-Oceanography, University of Vienna, Vienna, Austria, 4 Department of Oceanography, National Sun Yat-sen University, Kaohsiung, Taiwan Shallow-water hydrothermal vent ecosystems are distinctly different from deep-sea vents, as other than geothermal, sunlight is one of their primary sources of energy, so their resulting microbial communities differ to some extent. Yet compared with deep- Edited by: sea systems, less is known about the active microbial community in shallow-water Osvaldo Ulloa, Universidad de Concepción, Chile ecosystems. Thus, we studied the community compositions, their metabolic pathways, Reviewed by: and possible coupling of microbially driven biogeochemical cycles in a shallow- Luisa I. Falcon, water hydrothermal vent system off Kueishantao Islet, Taiwan, using high-throughput Universidad Nacional Autónoma de México, Mexico 16S rRNA sequences and metatranscriptome analyses. Gammaproteobacteria and Alejandro A. Murillo, Epsilonbacteraeota -
Exploring the Taxonomical and Functional Profile of As Burgas Hot Spring Focusing on Thermostable Β-Galactosidases
www.nature.com/scientificreports OPEN Exploring the taxonomical and functional profle of As Burgas hot spring focusing on thermostable β‑galactosidases María‑Eugenia DeCastro1, Michael P. Doane2,4, Elizabeth Ann Dinsdale2,3, Esther Rodríguez‑Belmonte1 & María‑Isabel González‑Siso1* In the present study we investigate the microbial community inhabiting As Burgas geothermal spring, located in Ourense (Galicia, Spain). The approximately 23 Gbp of Illumina sequences generated for each replicate revealed a complex microbial community dominated by Bacteria in which Proteobacteria and Aquifcae were the two prevalent phyla. An association between the two most prevalent genera, Thermus and Hydrogenobacter, was suggested by the relationship of their metabolism. The high relative abundance of sequences involved in the Calvin–Benson cycle and the reductive TCA cycle unveils the dominance of an autotrophic population. Important pathways from the nitrogen and sulfur cycle are potentially taking place in As Burgas hot spring. In the assembled reads, two complete ORFs matching GH2 beta‑galactosidases were found. To assess their functional characterization, the two ORFs were cloned and overexpressed in E. coli. The pTsbg enzyme had activity towards o‑Nitrophenyl‑β‑d‑galactopyranoside (ONPG) and p‑Nitrophenyl‑ β‑d‑fucopyranoside, with high thermal stability and showing maximal activity at 85 °C and pH 6, nevertheless the enzyme failed to hydrolyze lactose. The other enzyme, Tsbg, was unable to hydrolyze even ONPG or lactose. This fnding highlights the challenge of fnding novel active enzymes based only on their sequence. Termophiles, growing optimally at temperatures over 55 °C, are found in hot environments such as fumaroles, hydrothermal vents, hot springs, or deserts1–4. -
Comparative Genomic Analysis of the Class Epsilonproteobacteria and Proposed Reclassification to Epsilonbacteraeota (Phyl. Nov.)
fmicb-08-00682 April 20, 2017 Time: 17:21 # 1 ORIGINAL RESEARCH published: 24 April 2017 doi: 10.3389/fmicb.2017.00682 Comparative Genomic Analysis of the Class Epsilonproteobacteria and Proposed Reclassification to Epsilonbacteraeota (phyl. nov.) David W. Waite1, Inka Vanwonterghem1, Christian Rinke1, Donovan H. Parks1, Ying Zhang2, Ken Takai3, Stefan M. Sievert4, Jörg Simon5, Barbara J. Campbell6, Thomas E. Hanson7, Tanja Woyke8, Martin G. Klotz9,10 and Philip Hugenholtz1* 1 Australian Centre for Ecogenomics, School of Chemistry and Molecular Biosciences, The University of Queensland, St Lucia, QLD, Australia, 2 Department of Cell and Molecular Biology, College of the Environment and Life Sciences, University of Rhode Island, Kingston, RI, USA, 3 Department of Subsurface Geobiological Analysis and Research, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan, 4 Department of Biology, Woods Hole Oceanographic Institution, Woods Hole, MA, USA, 5 Microbial Energy Conversion and Biotechnology, Department of Biology, Technische Universität Darmstadt, Darmstadt, Germany, 6 Department of Biological Sciences, Life Science Facility, Clemson University, Clemson, SC, USA, 7 School of Marine Science and Policy, College of Earth, Ocean, and Environment, Delaware Biotechnology Institute, University of Delaware, Newark, DE, USA, 8 Department of Energy, Joint Genome Institute, Walnut Edited by: Creek, CA, USA, 9 Department of Biology and School of Earth and Environmental Sciences, Queens College of the City Svetlana N. Dedysh, University -
Insight Into the Evolution of Microbial Metabolism from the Deep- 2 Branching Bacterium, Thermovibrio Ammonificans 3 4 5 Donato Giovannelli1,2,3,4*, Stefan M
1 Insight into the evolution of microbial metabolism from the deep- 2 branching bacterium, Thermovibrio ammonificans 3 4 5 Donato Giovannelli1,2,3,4*, Stefan M. Sievert5, Michael Hügler6, Stephanie Markert7, Dörte Becher8, 6 Thomas Schweder 8, and Costantino Vetriani1,9* 7 8 9 1Institute of Earth, Ocean and Atmospheric Sciences, Rutgers University, New Brunswick, NJ 08901, 10 USA 11 2Institute of Marine Science, National Research Council of Italy, ISMAR-CNR, 60100, Ancona, Italy 12 3Program in Interdisciplinary Studies, Institute for Advanced Studies, Princeton, NJ 08540, USA 13 4Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo 152-8551, Japan 14 5Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 15 6DVGW-Technologiezentrum Wasser (TZW), Karlsruhe, Germany 16 7Pharmaceutical Biotechnology, Institute of Pharmacy, Ernst-Moritz-Arndt-University Greifswald, 17 17487 Greifswald, Germany 18 8Institute for Microbiology, Ernst-Moritz-Arndt-University Greifswald, 17487 Greifswald, Germany 19 9Department of Biochemistry and Microbiology, Rutgers University, New Brunswick, NJ 08901, USA 20 21 *Correspondence to: 22 Costantino Vetriani 23 Department of Biochemistry and Microbiology 24 and Institute of Earth, Ocean and Atmospheric Sciences 25 Rutgers University 26 71 Dudley Rd 27 New Brunswick, NJ 08901, USA 28 +1 (848) 932-3379 29 [email protected] 30 31 Donato Giovannelli 32 Institute of Earth, Ocean and Atmospheric Sciences 33 Rutgers University 34 71 Dudley Rd 35 New Brunswick, NJ 08901, USA 36 +1 (848) 932-3378 37 [email protected] 38 39 40 Abstract 41 Anaerobic thermophiles inhabit relic environments that resemble the early Earth. However, the 42 lineage of these modern organisms co-evolved with our planet. -
Microbial Diversity and Evidence of Sulfur- and Ammonium-Based Chemolithotrophy in Movile Cave
The ISME Journal (2009) 3, 1093–1104 & 2009 International Society for Microbial Ecology All rights reserved 1751-7362/09 $32.00 www.nature.com/ismej ORIGINAL ARTICLE Life without light: microbial diversity and evidence of sulfur- and ammonium-based chemolithotrophy in Movile Cave Yin Chen1,5, Liqin Wu2,5, Rich Boden1, Alexandra Hillebrand3, Deepak Kumaresan1, He´le`ne Moussard1, Mihai Baciu4, Yahai Lu2 and J Colin Murrell1 1Department of Biological Sciences, University of Warwick, Coventry, UK; 2College of Resources and Environmental Sciences, China Agricultural University, Beijing, China; 3Institute of Speleology ‘Emil Racovita’, Bucharest, Romania and 4The Group of Underwater and Speleological Exploration, Bucharest, Romania Microbial diversity in Movile Cave (Romania) was studied using bacterial and archaeal 16S rRNA gene sequence and functional gene analyses, including ribulose-1,5-bisphosphate carboxylase/ oxygenase (RuBisCO), soxB (sulfate thioesterase/thiohydrolase) and amoA (ammonia monoox- ygenase). Sulfur oxidizers from both Gammaproteobacteria and Betaproteobacteria were detected in 16S rRNA, soxB and RuBisCO gene libraries. DNA-based stable-isotope probing analyses using 13 C-bicarbonate showed that Thiobacillus spp. were most active in assimilating CO2 and also implied that ammonia and nitrite oxidizers were active during incubations. Nitrosomonas spp. were detected in both 16S rRNA and amoA gene libraries from the ‘heavy’ DNA and sequences related to nitrite- oxidizing bacteria Nitrospira and Candidatus ‘Nitrotoga’ were also detected in the ‘heavy’ DNA, which suggests that ammonia/nitrite oxidation may be another major primary production process in this unique ecosystem. A significant number of sequences associated with known methylotrophs from the Betaproteobacteria were obtained, including Methylotenera, Methylophilus and Methylo- vorus, supporting the view that cycling of one-carbon compounds may be an important process within Movile Cave. -
Microorganisms from Deep-Sea Hydrothermal Vents
Marine Life Science & Technology (2021) 3:204–230 https://doi.org/10.1007/s42995-020-00086-4 REVIEW Microorganisms from deep‑sea hydrothermal vents Xiang Zeng1,3 · Karine Alain2,3 · Zongze Shao1,3 Received: 23 June 2020 / Accepted: 17 November 2020 / Published online: 22 January 2021 © Ocean University of China 2021 Abstract With a rich variety of chemical energy sources and steep physical and chemical gradients, hydrothermal vent systems ofer a range of habitats to support microbial life. Cultivation-dependent and independent studies have led to an emerging view that diverse microorganisms in deep-sea hydrothermal vents live their chemolithoautotrophic, heterotrophic, or mixotrophic life with versatile metabolic strategies. Biogeochemical processes are mediated by microorganisms, and notably, processes involving or coupling the carbon, sulfur, hydrogen, nitrogen, and metal cycles in these unique ecosystems. Here, we review the taxonomic and physiological diversity of microbial prokaryotic life from cosmopolitan to endemic taxa and emphasize their signifcant roles in the biogeochemical processes in deep-sea hydrothermal vents. According to the physiology of the targeted taxa and their needs inferred from meta-omics data, the media for selective cultivation can be designed with a wide range of physicochemical conditions such as temperature, pH, hydrostatic pressure, electron donors and acceptors, carbon sources, nitrogen sources, and growth factors. The application of novel cultivation techniques with real-time monitoring of microbial diversity and metabolic substrates and products are also recommended. Keywords Deep-sea hydrothermal vents · Cultivation · Diversity · Biogeochemical cycle Introduction hydrothermal plumes (∼2 °C), low-temperature hydrother- mal fuids (∼5–100 °C), high-temperature hydrothermal The discovery of deep-sea hydrothermal vents in the late fuids (∼150–400 °C), sulfde rock, basalt, and pelagic and 1970s expanded our knowledge of the extent of life on Earth metalliferous sediments.