Delft University of Technology Desulfonatronospira Sulfatiphila Sp
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The Eastern Nebraska Salt Marsh Microbiome Is Well Adapted to an Alkaline and Extreme Saline Environment
life Article The Eastern Nebraska Salt Marsh Microbiome Is Well Adapted to an Alkaline and Extreme Saline Environment Sierra R. Athen, Shivangi Dubey and John A. Kyndt * College of Science and Technology, Bellevue University, Bellevue, NE 68005, USA; [email protected] (S.R.A.); [email protected] (S.D.) * Correspondence: [email protected] Abstract: The Eastern Nebraska Salt Marshes contain a unique, alkaline, and saline wetland area that is a remnant of prehistoric oceans that once covered this area. The microbial composition of these salt marshes, identified by metagenomic sequencing, appears to be different from well-studied coastal salt marshes as it contains bacterial genera that have only been found in cold-adapted, alkaline, saline environments. For example, Rubribacterium was only isolated before from an Eastern Siberian soda lake, but appears to be one of the most abundant bacteria present at the time of sampling of the Eastern Nebraska Salt Marshes. Further enrichment, followed by genome sequencing and metagenomic binning, revealed the presence of several halophilic, alkalophilic bacteria that play important roles in sulfur and carbon cycling, as well as in nitrogen fixation within this ecosystem. Photosynthetic sulfur bacteria, belonging to Prosthecochloris and Marichromatium, and chemotrophic sulfur bacteria of the genera Sulfurimonas, Arcobacter, and Thiomicrospira produce valuable oxidized sulfur compounds for algal and plant growth, while alkaliphilic, sulfur-reducing bacteria belonging to Sulfurospirillum help balance the sulfur cycle. This metagenome-based study provides a baseline to understand the complex, but balanced, syntrophic microbial interactions that occur in this unique Citation: Athen, S.R.; Dubey, S.; inland salt marsh environment. -
The Microbial Sulfur Cycle at Extremely Haloalkaline Conditions of Soda Lakes
REVIEW ARTICLE published: 21 March 2011 doi: 10.3389/fmicb.2011.00044 The microbial sulfur cycle at extremely haloalkaline conditions of soda lakes Dimitry Y. Sorokin1,2*, J. Gijs Kuenen 2 and Gerard Muyzer 2 1 Winogradsky Institute of Microbiology, Russian Academy of Sciences, Moscow, Russia 2 Department of Biotechnology, Delft University of Technology, Delft, Netherlands Edited by: Soda lakes represent a unique ecosystem with extremely high pH (up to 11) and salinity (up to Martin G. Klotz, University of Louisville, saturation) due to the presence of high concentrations of sodium carbonate in brines. Despite USA these double extreme conditions, most of the lakes are highly productive and contain a fully Reviewed by: Aharon Oren, The Hebrew University functional microbial system. The microbial sulfur cycle is among the most active in soda lakes. of Jerusalem, Israel One of the explanations for that is high-energy efficiency of dissimilatory conversions of inorganic Yanhe Ma, Institute of Microbiology sulfur compounds, both oxidative and reductive, sufficient to cope with costly life at double Chinese Academy of Sciences, China extreme conditions. The oxidative part of the sulfur cycle is driven by chemolithoautotrophic *Correspondence: haloalkaliphilic sulfur-oxidizing bacteria (SOB), which are unique for soda lakes. The haloalkaliphilic Dimitry Y. Sorokin, Winogradsky Institute of Microbiology, Russian SOB are present in the surface sediment layer of various soda lakes at high numbers of up to Academy of Sciences, Prospect 60-let 106 viable cells/cm3. The culturable forms are so far represented by four novel genera within the Octyabrya 7/2, 117312 Moscow, Russia Gammaproteobacteria, including the genera Thioalkalivibrio, Thioalkalimicrobium, Thioalkalispira, e-mail: [email protected]; and Thioalkalibacter. -
Uva-DARE (Digital Academic Repository)
UvA-DARE (Digital Academic Repository) Culturable diversity of lithotrophic haloalkaliphilic sulfate-reducing bacteria in soda lakes and the description of Desulfonatronum thioautotrophicum sp. nov., Desulfonatronum thiosulfatophilum sp. nov., Desulfonatronovibrio thiodismutans sp. nov., and Desulfonatronovibrio magnus sp. nov. Sorokin, D.Y.; Tourova, T.P.; Kolganova, T.V.; Detkova, E.N.; Galinski, E.A.; Muyzer, G. DOI 10.1007/s00792-011-0370-7 Publication date 2011 Document Version Final published version Published in Extremophiles Link to publication Citation for published version (APA): Sorokin, D. Y., Tourova, T. P., Kolganova, T. V., Detkova, E. N., Galinski, E. A., & Muyzer, G. (2011). Culturable diversity of lithotrophic haloalkaliphilic sulfate-reducing bacteria in soda lakes and the description of Desulfonatronum thioautotrophicum sp. nov., Desulfonatronum thiosulfatophilum sp. nov., Desulfonatronovibrio thiodismutans sp. nov., and Desulfonatronovibrio magnus sp. nov. Extremophiles, 15(3), 391-401. https://doi.org/10.1007/s00792-011-0370-7 General rights It is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), other than for strictly personal, individual use, unless the work is under an open content license (like Creative Commons). Disclaimer/Complaints regulations If you believe that digital publication of certain material infringes any of your rights or (privacy) interests, please let the Library know, stating your reasons. In case of a legitimate complaint, the Library will make the material inaccessible and/or remove it from the website. Please Ask the Library: https://uba.uva.nl/en/contact, or a letter to:UvA-DARE Library is of a servicethe University provided by of the Amsterdam, library of the UniversitySecretariat, of Amsterdam Singel 425, (https 1012://dare.uva.nl) WP Amsterdam, The Netherlands. -
'Candidatus Desulfonatronobulbus Propionicus': a First Haloalkaliphilic
Delft University of Technology ‘Candidatus Desulfonatronobulbus propionicus’ a first haloalkaliphilic member of the order Syntrophobacterales from soda lakes Sorokin, D. Y.; Chernyh, N. A. DOI 10.1007/s00792-016-0881-3 Publication date 2016 Document Version Accepted author manuscript Published in Extremophiles: life under extreme conditions Citation (APA) Sorokin, D. Y., & Chernyh, N. A. (2016). ‘Candidatus Desulfonatronobulbus propionicus’: a first haloalkaliphilic member of the order Syntrophobacterales from soda lakes. Extremophiles: life under extreme conditions, 20(6), 895-901. https://doi.org/10.1007/s00792-016-0881-3 Important note To cite this publication, please use the final published version (if applicable). Please check the document version above. Copyright Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons. Takedown policy Please contact us and provide details if you believe this document breaches copyrights. We will remove access to the work immediately and investigate your claim. This work is downloaded from Delft University of Technology. For technical reasons the number of authors shown on this cover page is limited to a maximum of 10. Extremophiles DOI 10.1007/s00792-016-0881-3 ORIGINAL PAPER ‘Candidatus Desulfonatronobulbus propionicus’: a first haloalkaliphilic member of the order Syntrophobacterales from soda lakes D. Y. Sorokin1,2 · N. A. Chernyh1 Received: 23 August 2016 / Accepted: 4 October 2016 © Springer Japan 2016 Abstract Propionate can be directly oxidized anaerobi- from its members at the genus level. -
Desulfonatronovibrio Halophilus Sp. Nov., a Novel Moderately Halophilic Sulfate-Reducing Bacterium from Hypersaline Chloride–Sulfate Lakes in Central Asia
Extremophiles (2012) 16:411–417 DOI 10.1007/s00792-012-0440-5 ORIGINAL PAPER Desulfonatronovibrio halophilus sp. nov., a novel moderately halophilic sulfate-reducing bacterium from hypersaline chloride–sulfate lakes in Central Asia D. Y. Sorokin • T. P. Tourova • B. Abbas • M. V. Suhacheva • G. Muyzer Received: 10 February 2012 / Accepted: 22 March 2012 / Published online: 10 April 2012 Ó The Author(s) 2012. This article is published with open access at Springerlink.com Abstract Four strains of lithotrophic sulfate-reducing soda lakes. The isolates utilized formate, H2 and pyruvate as bacteria (SRB) have been enriched and isolated from electron donors and sulfate, sulfite and thiosulfate as electron anoxic sediments of hypersaline chloride–sulfate lakes in acceptors. In contrast to the described species of the genus the Kulunda Steppe (Altai, Russia) at 2 M NaCl and pH Desulfonatronovibrio, the salt lake isolates could only tolerate 7.5. According to the 16S rRNA gene sequence analysis, high pH (up to pH 9.4), while they grow optimally at a neutral the isolates were closely related to each other and belonged pH. They belonged to the moderate halophiles growing to the genus Desulfonatronovibrio, which, so far, included between 0.2 and 2 M NaCl with an optimum at 0.5 M. On the only obligately alkaliphilic members found exclusively in basis of their distinct phenotype and phylogeny, the described halophilic SRB are proposed to form a novel species within the genus Desulfonatronovibrio, D. halophilus (type strain T T T Communicated by A. Oren. HTR1 = DSM24312 = UNIQEM U802 ). The GenBank/EMBL accession numbers of the 16S rRNA gene Keywords Sulfate-reducing bacteria (SRB) Á sequences of the HTR strains are GQ922847, HQ157562, HQ157563 and JN408678; the dsrAB gene sequences of (halo)alkaliphilic SRB Desulfonatronovibrio Á Hypersaline lakes Á Halophilic obtained in this study are JQ519392-JQ519396. -
A Species of Magnetotactic Deltaproteobacterium Was Detected
A species of magnetotactic deltaproteobacterium was detected at the highest abundance during an algal bloom Hongmiao Pan, Yi Dong, Zhaojie Teng, Jinhua Li, Wenyan Zhang, Tian Xiao, Long-Fei Wu To cite this version: Hongmiao Pan, Yi Dong, Zhaojie Teng, Jinhua Li, Wenyan Zhang, et al.. A species of magneto- tactic deltaproteobacterium was detected at the highest abundance during an algal bloom. FEMS Microbiology Letters, Wiley-Blackwell, 2019, 366 (22), 10.1093/femsle/fnz253. hal-02448980 HAL Id: hal-02448980 https://hal-amu.archives-ouvertes.fr/hal-02448980 Submitted on 22 Jan 2020 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. A species of magnetotactic deltaproteobacterium was detected at the highest abundance during an algal bloom Hongmiao Pan1,2,3,5, Yi Dong1,2,3,5, Zhaojie Teng1, Jinhua Li2,4,5, Wenyan Zhang1,2,3,5, Tian Xiao1,2,3,5*, Long-Fei Wu5,6 1 CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China 2 Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China 3 Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China 4 Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China. -
Microbial Ecology of Halo-Alkaliphilic Sulfur Bacteria
Microbial Ecology of Halo-Alkaliphilic Sulfur Bacteria Microbial Ecology of Halo-Alkaliphilic Sulfur Bacteria Proefschrift ter verkrijging van de graad van doctor aan de Technische Universiteit Delft, op gezag van de Rector Magnificus prof. dr. ir. J.T. Fokkema, voorzitter van het College van Promoties in het openbaar te verdedigen op dinsdag 16 oktober 2007 te 10:00 uur door Mirjam Josephine FOTI Master degree in Biology, Universita` degli Studi di Milano, Italy Geboren te Milaan (Italië) Dit proefschrift is goedgekeurd door de promotor: Prof. dr. J.G. Kuenen Toegevoegd promotor: Dr. G. Muyzer Samenstelling commissie: Rector Magnificus Technische Universiteit Delft, voorzitter Prof. dr. J. G. Kuenen Technische Universiteit Delft, promotor Dr. G. Muyzer Technische Universiteit Delft, toegevoegd promotor Prof. dr. S. de Vries Technische Universiteit Delft Prof. dr. ir. A. J. M. Stams Wageningen U R Prof. dr. ir. A. J. H. Janssen Wageningen U R Prof. dr. B. E. Jones University of Leicester, UK Dr. D. Yu. Sorokin Institute of Microbiology, RAS, Russia This study was carried out in the Environmental Biotechnology group of the Department of Biotechnology at the Delft University of Technology, The Netherlands. This work was financially supported by the Dutch technology Foundation (STW) by the contract WBC 5939, Paques B.V. and Shell Global Solutions Int. B.V. ISBN: 978-90-9022281-3 Table of contents Chapter 1 7 General introduction Chapter 2 29 Genetic diversity and biogeography of haloalkaliphilic sulfur-oxidizing bacteria belonging to the -
Microbiological Study of the Anaerobic Corrosion of Iron
Microbiological study of the anaerobic corrosion of iron Dissertation zur Erlangung des Grades eines Doktors der Naturwissenschaften - Dr. rer. nat.- dem Fachbereich Biologie/Chemie der Universität Bremen vorgelegt von Dinh Thuy Hang aus Hanoi Bremen 2003 Die Untersuchungen zur vorliegenden Doktorarbeit wurden am Max Planck Institut für Marine Mikrobiologie in Bremen gurchgeführt. 1. Gutachter: Prof. Dr. Friedrich Widdel, Universität Bremen 2. Gutachter: Prof. Dr. Heribert Cypionka, Universität Oldenburg Tag des Promotionskolloquiums: 27. Juni 2003 To my parents Table of content Abbreviations Summary 1 Part I. Biocorrosion of iron: an overview of the literature and results of the present study A Overview of the literature 4 1. Introductory remarks on economic significance and principal reactions during corrosion 4 2. Aerobic microbial corrosion 6 3. Anaerobic microbial corrosion 7 3.1 Anaerobic corrosion by sulfate-reducing bacteria (SRB) 7 3.1.1 Physiology and phylogeny of SRB 8 3.1.2 Hydrogenases in SRB 10 3.1.3 Mechanism of corrosion mediated by SRB 12 3.2 Corrosion by anaerobic microorganisms other than SRB 17 3.2.1 Corrosion by methanogenic archaea 17 3.2.2 Corrosion by Fe(III)-reducing bacteria 18 3.2.3 Corrosion by nitrate-reducing bacteria 19 4. Goals of the present work 19 B Results of the present study 1. Anaerobic corrosion by sulfate-reducing bacteria (SRB) 22 1.1 Enrichment of SRB with metallic iron (Fe) as the only source of electrons 22 1.2 Molecular analysis of bacterial communities in the enrichment cultures 23 1.3 Isolation and characterization of SRB from the enrichment cultures 24 1.4 In situ identification of SRB in the enrichment cultures with metallic iron 26 1.5 Study of corrosion by the new isolates of SRB 27 1.5.1 Capability of sulfate reduction with metallic iron 27 1.5.2 Rate of sulfate reduction with metallic iron 29 1.5.3 Hydrogenase activity and accelerated hydrogen formation with metallic iron 30 1.5.4 Analyses of the corroding iron surface 32 2. -
Qinghai Lake
MIAMI UNIVERSITY The Graduate School CERTIFICATE FOR APPROVING THE DISSERTATION We hereby approve the Dissertation of Hongchen Jiang Candidate for the Degree Doctor of Philosophy ________________________________________________________ Dr. Hailiang Dong, Director ________________________________________________________ Dr. Chuanlun Zhang, Reader ________________________________________________________ Dr. Yildirim Dilek, Reader ________________________________________________________ Dr. Jonathan Levy, Reader ________________________________________________________ Dr. Q. Quinn Li, Graduate School Representative ABSTRACT GEOMICROBIOLOGICAL STUDIES OF SALINE LAKES ON THE TIBETAN PLATEAU, NW CHINA: LINKING GEOLOGICAL AND MICROBIAL PROCESSES By Hongchen Jiang Lakes constitute an important part of the global ecosystem as habitats in these environments play an important role in biogeochemical cycles of life-essential elements. The cycles of carbon, nitrogen and sulfur in these ecosystems are intimately linked to global phenomena such as climate change. Microorganisms are at the base of the food chain in these environments and drive the cycling of carbon and nitrogen in water columns and the sediments. Despite many studies on microbial ecology of lake ecosystems, significant gaps exist in our knowledge of how microbial and geological processes interact with each other. In this dissertation, I have studied the ecology and biogeochemistry of lakes on the Tibetan Plateau, NW China. The Tibetan lakes are pristine and stable with multiple environmental gradients (among which are salinity, pH, and ammonia concentration). These characteristics allow an assessment of mutual interactions of microorganisms and geochemical conditions in these lakes. Two lakes were chosen for this project: Lake Chaka and Qinghai Lake. These two lakes have contrasting salinity and pH: slightly saline (12 g/L) and alkaline (9.3) for Qinghai Lake and hypersaline (325 g/L) but neutral pH (7.4) for Chaka Lake. -
Magnetotactic Bacteria from Extreme Environments
Life 2013, 3, 295-307; doi:10.3390/life3020295 OPEN ACCESS life ISSN 2075-1729 www.mdpi.com/ journal/life Review Magnetotactic Bacteria from Extreme Environments Dennis A. Bazylinski 1,* and Christopher T. Lefèvre 2 1 University of Nevada at Las Vegas, School of Life Sciences, Las Vegas, Nevada, 89154-4004, USA 2 CEA Cadarache/CNRS/Aix-Marseille Université, UMR7265 Service de Biologie Végétale et de Microbiologie Environnementale, Laboratoire de Bioénergétique Cellulaire, 13108, Saint-Paul-lez-Durance, France; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +001-702-895-2053; Fax: +001-702-895-3956. Received: 14 February 2013; in revised form: 13 March 2013 / Accepted: 13 March 2013 / Published: 26 March 2013 Abstract: Magnetotactic bacteria (MTB) represent a diverse collection of motile prokaryotes that biomineralize intracellular, membrane-bounded, tens-of-nanometer-sized crystals of a magnetic mineral called magnetosomes. Magnetosome minerals consist of either magnetite (Fe3O4) or greigite (Fe3S4) and FDXVHFHOOVWRDOLJQDORQJWKH(DUWK¶VJHRPDJQHWLFILHOGOLQHV as they swim, a trait called magnetotaxis. MTB are known to mainly inhabit the oxic±anoxic interface (OAI) in water columns or sediments of aquatic habitats and it is currently thought that magnetosomes function as a means of making chemotaxis more efficient in locating and maintaining an optimal position for growth and survival at the OAI. Known cultured and uncultured MTB are phylogenetically associated with the Alpha-, Gamma- and Deltaproteobacteria classes of the phylum Proteobacteria, the Nitrospirae phylum and the candidate division OP3, part of the Planctomycetes-Verrucomicrobia-Chlamydiae (PVC) bacterial superphylum. MTB are generally thought to be ubiquitous in aquatic environments as they are cosmopolitan in distribution and have been found in every continent although for years MTB were thought to be restricted to habitats with pH values near neutral and at ambient temperature. -
Microbial Diversity in a Permanently Cold and Alkaline Environment in Greenland
Microbial diversity in a permanently cold and alkaline environment in Greenland Glaring, Mikkel Andreas; Vester, Jan Kjølhede; Lylloff, Jeanette Eva; Abu Al-Soud, Waleed; Sørensen, Søren Johannes; Stougaard, Peter Published in: PLoS ONE DOI: 10.1371/journal.pone.0124863 Publication date: 2015 Document version Publisher's PDF, also known as Version of record Document license: CC BY Citation for published version (APA): Glaring, M. A., Vester, J. K., Lylloff, J. E., Abu Al-Soud, W., Sørensen, S. J., & Stougaard, P. (2015). Microbial diversity in a permanently cold and alkaline environment in Greenland. PLoS ONE, 10(4), [e0124863]. https://doi.org/10.1371/journal.pone.0124863 Download date: 28. Sep. 2021 RESEARCH ARTICLE Microbial Diversity in a Permanently Cold and Alkaline Environment in Greenland Mikkel A. Glaring1, Jan K. Vester1, Jeanette E. Lylloff1, Waleed Abu Al-Soud2,Søren J. Sørensen2, Peter Stougaard1* 1 Department of Plant and Environmental Sciences, University of Copenhagen, Frederiksberg, Denmark, 2 Department of Biology, University of Copenhagen, Copenhagen, Denmark * [email protected] Abstract The submarine ikaite columns located in the Ikka Fjord in Southern Greenland represent a unique, permanently cold (less than 6°C) and alkaline (above pH 10) environment and are home to a microbial community adapted to these extreme conditions. The bacterial and ar- chaeal community inhabiting the ikaite columns and surrounding fjord was characterised by OPEN ACCESS high-throughput pyrosequencing of 16S rRNA genes. Analysis of the ikaite community struc- Citation: Glaring MA, Vester JK, Lylloff JE, Abu ture revealed the presence of a diverse bacterial community, both in the column interior and Al-Soud W, Sørensen SJ, Stougaard P (2015) Microbial Diversity in a Permanently Cold and at the surface, and very few archaea. -
Metagenomic Identification of Active Methanogens and Methanotrophs in Serpentinite Springs of the Voltri Massif, Italy
Metagenomic identification of active methanogens and methanotrophs in serpentinite springs of the Voltri Massif, Italy William J. Brazelton1, Christopher N. Thornton1, Alex Hyer1, Katrina I. Twing2, August A. Longino1, Susan Q. Lang3,4, Marvin D. Lilley5, Gretchen L. Früh-Green4 and Matthew O. Schrenk2 1 Department of Biology, University of Utah, Salt Lake City, UT, United States 2 Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, United States 3 Department of Earth and Ocean Sciences, University of South Carolina, Columbia, SC, United States 4 Department of Earth Sciences, ETH Zurich, Zurich, Switzerland 5 School of Oceanography, University of Washington, Seattle, WA, United States ABSTRACT The production of hydrogen and methane by geochemical reactions associated with the serpentinization of ultramafic rocks can potentially support subsurface micro- bial ecosystems independent of the photosynthetic biosphere. Methanogenic and methanotrophic microorganisms are abundant in marine hydrothermal systems heavily influenced by serpentinization, but evidence for methane-cycling archaea and bacteria in continental serpentinite springs has been limited. This report provides metage- nomic and experimental evidence for active methanogenesis and methanotrophy by microbial communities in serpentinite springs of the Voltri Massif, Italy. Methanogens belonging to family Methanobacteriaceae and methanotrophic bacteria belonging to family Methylococcaceae were heavily enriched in three ultrabasic springs (pH 12). Metagenomic data also suggest the potential for hydrogen oxidation, hydrogen pro- duction, carbon fixation, fermentation, and organic acid metabolism in the ultrabasic Submitted 22 July 2016 springs. The predicted metabolic capabilities are consistent with an active subsurface Accepted 27 December 2016 ecosystem supported by energy and carbon liberated by geochemical reactions within Published 26 January 2017 the serpentinite rocks of the Voltri Massif.