Phylogenetic Analysis of Members of the Crenarchaeota in Association
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Genome Size Evolution in the Archaea
Kellner, S., Spang, A., Offre, P., Szollosi, G. J., Petitjean, C., & Williams, T. (2018). Genome size evolution in the Archaea. Emerging Topics in Life Sciences. https://doi.org/10.1042/ETLS20180021 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1042/ETLS20180021 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Portland Press at http://www.emergtoplifesci.org/content/early/2018/11/13/ETLS20180021 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Emerging Topics in Life Sciences (2018) https://doi.org/10.1042/ETLS20180021 Review Article Genome size evolution in the Archaea Siri Kellner1, Anja Spang2,3, Pierre Offre2, Gergely J. Szöllo˝si4,5, Celine Petitjean6 and Tom A. Williams6 1School of Earth Sciences, University of Bristol, Bristol BS8 1TQ, U.K.; 2NIOZ, Royal Netherlands Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, and Utrecht University, P.O. Box 59, NL-1790 AB Den Burg, The Netherlands; 3Department of Cell and Molecular Biology, Science for Life Laboratory, Uppsala University, SE-75123, Uppsala, Sweden; 4MTA-ELTE Lendület Evolutionary Genomics Research Group, 1117 Budapest, Hungary; 5Department of Biological Physics, Eötvös Loránd University, 1117 Budapest, Hungary; 6School of Biological Sciences, University of Bristol, Bristol BS8 1TQ, U.K. -
Emended Descriptions of Genera of the Family Halobacteriaceae
International Journal of Systematic and Evolutionary Microbiology (2009), 59, 637–642 DOI 10.1099/ijs.0.008904-0 Taxonomic Emended descriptions of genera of the family Note Halobacteriaceae Aharon Oren,1 David R. Arahal2 and Antonio Ventosa3 Correspondence 1Institute of Life Sciences, and the Moshe Shilo Minerva Center for Marine Biogeochemistry, Aharon Oren The Hebrew University of Jerusalem, Jerusalem 91904, Israel [email protected] 2Departamento de Microbiologı´a y Ecologı´a and Coleccio´n Espan˜ola de Cultivos Tipo (CECT), Universidad de Valencia, 46100 Burjassot, Valencia, Spain 3Department of Microbiology and Parasitology, Faculty of Pharmacy, University of Sevilla, 41012 Sevilla, Spain The family Halobacteriaceae currently contains 96 species whose names have been validly published, classified in 27 genera (as of September 2008). In recent years, many novel species have been added to the established genera but, in many cases, one or more properties of the novel species do not agree with the published descriptions of the genera. Authors have often failed to provide emended genus descriptions when necessary. Following discussions of the International Committee on Systematics of Prokaryotes Subcommittee on the Taxonomy of Halobacteriaceae, we here propose emended descriptions of the genera Halobacterium, Haloarcula, Halococcus, Haloferax, Halorubrum, Haloterrigena, Natrialba, Halobiforma and Natronorubrum. The family Halobacteriaceae was established by Gibbons rRNA gene sequence-based phylogenetic trees rather than (1974) to accommodate the genera Halobacterium and on true polyphasic taxonomy such as recommended for the Halococcus. At the time of writing (September 2008), the family (Oren et al., 1997). As a result, there are often few, if family contained 96 species whose names have been validly any, phenotypic properties that enable the discrimination published, classified in 27 genera. -
Pan-Genome Analysis and Ancestral State Reconstruction Of
www.nature.com/scientificreports OPEN Pan‑genome analysis and ancestral state reconstruction of class halobacteria: probability of a new super‑order Sonam Gaba1,2, Abha Kumari2, Marnix Medema 3 & Rajeev Kaushik1* Halobacteria, a class of Euryarchaeota are extremely halophilic archaea that can adapt to a wide range of salt concentration generally from 10% NaCl to saturated salt concentration of 32% NaCl. It consists of the orders: Halobacteriales, Haloferaciales and Natriabales. Pan‑genome analysis of class Halobacteria was done to explore the core (300) and variable components (Softcore: 998, Cloud:36531, Shell:11784). The core component revealed genes of replication, transcription, translation and repair, whereas the variable component had a major portion of environmental information processing. The pan‑gene matrix was mapped onto the core‑gene tree to fnd the ancestral (44.8%) and derived genes (55.1%) of the Last Common Ancestor of Halobacteria. A High percentage of derived genes along with presence of transformation and conjugation genes indicate the occurrence of horizontal gene transfer during the evolution of Halobacteria. A Core and pan‑gene tree were also constructed to infer a phylogeny which implicated on the new super‑order comprising of Natrialbales and Halobacteriales. Halobacteria1,2 is a class of phylum Euryarchaeota3 consisting of extremely halophilic archaea found till date and contains three orders namely Halobacteriales4,5 Haloferacales5 and Natrialbales5. Tese microorganisms are able to dwell at wide range of salt concentration generally from 10% NaCl to saturated salt concentration of 32% NaCl6. Halobacteria, as the name suggests were once considered a part of a domain "Bacteria" but with the discovery of the third domain "Archaea" by Carl Woese et al.7, it became part of Archaea. -
The Role of Stress Proteins in Haloarchaea and Their Adaptive Response to Environmental Shifts
biomolecules Review The Role of Stress Proteins in Haloarchaea and Their Adaptive Response to Environmental Shifts Laura Matarredona ,Mónica Camacho, Basilio Zafrilla , María-José Bonete and Julia Esclapez * Agrochemistry and Biochemistry Department, Biochemistry and Molecular Biology Area, Faculty of Science, University of Alicante, Ap 99, 03080 Alicante, Spain; [email protected] (L.M.); [email protected] (M.C.); [email protected] (B.Z.); [email protected] (M.-J.B.) * Correspondence: [email protected]; Tel.: +34-965-903-880 Received: 31 July 2020; Accepted: 24 September 2020; Published: 29 September 2020 Abstract: Over the years, in order to survive in their natural environment, microbial communities have acquired adaptations to nonoptimal growth conditions. These shifts are usually related to stress conditions such as low/high solar radiation, extreme temperatures, oxidative stress, pH variations, changes in salinity, or a high concentration of heavy metals. In addition, climate change is resulting in these stress conditions becoming more significant due to the frequency and intensity of extreme weather events. The most relevant damaging effect of these stressors is protein denaturation. To cope with this effect, organisms have developed different mechanisms, wherein the stress genes play an important role in deciding which of them survive. Each organism has different responses that involve the activation of many genes and molecules as well as downregulation of other genes and pathways. Focused on salinity stress, the archaeal domain encompasses the most significant extremophiles living in high-salinity environments. To have the capacity to withstand this high salinity without losing protein structure and function, the microorganisms have distinct adaptations. -
Mesohaline Responses to Cycles of “Famine Or Feast” in Layered Brines
Int. Assoc. Sedimentol. Spec. Publ. (2011) 43, 315–392 Evaporitic source rocks: mesohaline responses to cycles of “famine or feast” in layered brines JOHN K. WARREN International Master Program in Petroleum Geoscience, Department of Geology, Faculty of Science, Chulalongkorn University, Bangkok, 10330, Thailand. Formerly: Shell Professor in Carbonate Studies, Oil and Gas Research Centre, Sultan Qaboos University, Muscat, Oman (E-mail: [email protected]) ABSTRACT Organic matter in modern saline systems tends to accumulate in bottom sediments beneath a density-stratified mass of saline water where layered hydrologies are subject to oscillations in salinity and brine level. Organic matter is not produced at a constant rate in such systems; rather, it is generated in pulses by a halotolerant community in response to relatively short times of less stressful conditions (brackish to mesohaline) that occur in the upper part of the layered hydrology. Accumulations of organic matter can occur in any layered brine lake or epeiric seaway when an upper less-saline water mass forms on top of nutrient-rich brines, or in wet mudflats wherever waters freshen in and above the uppermost few millimetres of a microbial mat. A flourishing community of halotolerant algae, bacteria and archaeal photosynthesizers drives the resulting biomass bloom. Brine freshening is a time of “feast” characterized by very high levels of organic productivity. In a stratified brine column (oligotrophic and meromictic) the typical producers are planktonic algal or cyanobacterial communities inhabiting the upper mesohaline portion of the stratified water mass. In mesohaline holomictic waters, where light penetrates to the water bottom, the organic-producing layer is typically the upper algal and bacterial portion of a benthic laminated microbialite characterized by elevated numbers of cyanobacteria. -
Salinity Drives Archaeal Distribution Patterns in High Altitude Lake Sediments on the Tibetan Plateau Yongqin Liu 1,2,∗, John C
FEMS Microbiology Ecology, 92, 2016, fiw033 doi: 10.1093/femsec/fiw033 Advance Access Publication Date: 16 February 2016 Research Article RESEARCH ARTICLE Salinity drives archaeal distribution patterns in high altitude lake sediments on the Tibetan Plateau Yongqin Liu 1,2,∗, John C. Priscu3, Jinbo Xiong4, Ralf Conrad5, Trista Vick-Majors3, Haiyan Chu6 and Juzhi Hou1 Downloaded from 1Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Beijing 100101, China, 2CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, China, 3Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, MT 59717, USA, 4Faculty of Marine Sciences, Ningbo University, Ningbo http://femsec.oxfordjournals.org/ 315211, China, 5Max Planck Institute for Terrestrial Microbiology, Marburg 35043, Germany and 6State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China ∗Corresponding author: Institute of Tibetan Plateau, Chinese Academy of Science, No. 16, Lincuo Rd., Beijing 100101, China. Tel: 86-10-84097122; E-mail: [email protected] One sentence summary: We represent a comprehensive investigation of archaeal diversity in the pristine lake sediments across the Tibetan Plateau, and found salinity is the key factor controlling archaeal community diversity and composition. Editor: Dirk Wagner by guest on April 5, 2016 ABSTRACT Archaeal communities and the factors regulating their diversity in high altitude lakes are poorly understood. Here, we provide the first high-throughput sequencing study of Archaea from Tibetan Plateau lake sediments. We analyzed twenty lake sediments from the world’s highest and largest plateau and found diverse archaeal assemblages that clustered into groups dominated by methanogenic Euryarchaeota, Crenarchaeota and Halobacteria/mixed euryarchaeal phylotypes. -
(Gid ) Genes Coding for Putative Trna:M5u-54 Methyltransferases in 355 Bacterial and Archaeal Complete Genomes
Table S1. Taxonomic distribution of the trmA and trmFO (gid ) genes coding for putative tRNA:m5U-54 methyltransferases in 355 bacterial and archaeal complete genomes. Asterisks indicate the presence and the number of putative genes found. Genomes Taxonomic position TrmA Gid Archaea Crenarchaea Aeropyrum pernix_K1 Crenarchaeota; Thermoprotei; Desulfurococcales; Desulfurococcaceae Cenarchaeum symbiosum Crenarchaeota; Thermoprotei; Cenarchaeales; Cenarchaeaceae Pyrobaculum aerophilum_str_IM2 Crenarchaeota; Thermoprotei; Thermoproteales; Thermoproteaceae Sulfolobus acidocaldarius_DSM_639 Crenarchaeota; Thermoprotei; Sulfolobales; Sulfolobaceae Sulfolobus solfataricus Crenarchaeota; Thermoprotei; Sulfolobales; Sulfolobaceae Sulfolobus tokodaii Crenarchaeota; Thermoprotei; Sulfolobales; Sulfolobaceae Euryarchaea Archaeoglobus fulgidus Euryarchaeota; Archaeoglobi; Archaeoglobales; Archaeoglobaceae Haloarcula marismortui_ATCC_43049 Euryarchaeota; Halobacteria; Halobacteriales; Halobacteriaceae; Haloarcula Halobacterium sp Euryarchaeota; Halobacteria; Halobacteriales; Halobacteriaceae; Haloarcula Haloquadratum walsbyi Euryarchaeota; Halobacteria; Halobacteriales; Halobacteriaceae; Haloquadra Methanobacterium thermoautotrophicum Euryarchaeota; Methanobacteria; Methanobacteriales; Methanobacteriaceae Methanococcoides burtonii_DSM_6242 Euryarchaeota; Methanomicrobia; Methanosarcinales; Methanosarcinaceae Methanococcus jannaschii Euryarchaeota; Methanococci; Methanococcales; Methanococcaceae Methanococcus maripaludis_S2 Euryarchaeota; Methanococci; -
Pyrolobus Fumarii Type Strain (1A)
Lawrence Berkeley National Laboratory Recent Work Title Complete genome sequence of the hyperthermophilic chemolithoautotroph Pyrolobus fumarii type strain (1A). Permalink https://escholarship.org/uc/item/89r1s0xt Journal Standards in genomic sciences, 4(3) ISSN 1944-3277 Authors Anderson, Iain Göker, Markus Nolan, Matt et al. Publication Date 2011-07-01 DOI 10.4056/sigs.2014648 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Standards in Genomic Sciences (2011) 4:381-392 DOI:10.4056/sigs.2014648 Complete genome sequence of the hyperthermophilic chemolithoautotroph Pyrolobus fumarii type strain (1AT) Iain Anderson1, Markus Göker2, Matt Nolan1, Susan Lucas1, Nancy Hammon1, Shweta Deshpande1, Jan-Fang Cheng1, Roxanne Tapia1,3, Cliff Han1,3, Lynne Goodwin1,3, Sam Pitluck1, Marcel Huntemann1, Konstantinos Liolios1, Natalia Ivanova1, Ioanna Pagani1, Konstantinos Mavromatis1, Galina Ovchinikova1, Amrita Pati1, Amy Chen4, Krishna Pala- niappan4, Miriam Land1,5, Loren Hauser1,5, Evelyne-Marie Brambilla2, Harald Huber6, Montri Yasawong7, Manfred Rohde7, Stefan Spring2, Birte Abt2, Johannes Sikorski2, Reinhard Wirth6, John C. Detter1,3, Tanja Woyke1, James Bristow1, Jonathan A. Eisen1,8, Victor Markowitz4, Philip Hugenholtz1,9, Nikos C. Kyrpides1, Hans-Peter Klenk2, and Alla Lapidus1* 1 DOE Joint Genome Institute, Walnut Creek, California, USA 2 DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany 3 Los Alamos National Laboratory, Bioscience Division, Los Alamos, -
Freshwater Aquatic Biomes GREENWOOD GUIDES to BIOMES of the WORLD
Freshwater Aquatic Biomes GREENWOOD GUIDES TO BIOMES OF THE WORLD Introduction to Biomes Susan L. Woodward Tropical Forest Biomes Barbara A. Holzman Temperate Forest Biomes Bernd H. Kuennecke Grassland Biomes Susan L. Woodward Desert Biomes Joyce A. Quinn Arctic and Alpine Biomes Joyce A. Quinn Freshwater Aquatic Biomes Richard A. Roth Marine Biomes Susan L. Woodward Freshwater Aquatic BIOMES Richard A. Roth Greenwood Guides to Biomes of the World Susan L. Woodward, General Editor GREENWOOD PRESS Westport, Connecticut • London Library of Congress Cataloging-in-Publication Data Roth, Richard A., 1950– Freshwater aquatic biomes / Richard A. Roth. p. cm.—(Greenwood guides to biomes of the world) Includes bibliographical references and index. ISBN 978-0-313-33840-3 (set : alk. paper)—ISBN 978-0-313-34000-0 (vol. : alk. paper) 1. Freshwater ecology. I. Title. QH541.5.F7R68 2009 577.6—dc22 2008027511 British Library Cataloguing in Publication Data is available. Copyright C 2009 by Richard A. Roth All rights reserved. No portion of this book may be reproduced, by any process or technique, without the express written consent of the publisher. Library of Congress Catalog Card Number: 2008027511 ISBN: 978-0-313-34000-0 (vol.) 978-0-313-33840-3 (set) First published in 2009 Greenwood Press, 88 Post Road West, Westport, CT 06881 An imprint of Greenwood Publishing Group, Inc. www.greenwood.com Printed in the United States of America The paper used in this book complies with the Permanent Paper Standard issued by the National Information Standards Organization (Z39.48–1984). 10987654321 Contents Preface vii How to Use This Book ix The Use of Scientific Names xi Chapter 1. -
Determination of Hydrolytic Enzyme Capabilities of Halophilic Archaea Isolated from Hides and Skins and Their Phenotypic and Phylogenetic Identification by S
33 DETERMinATION OF HYDROLYTic ENZYME CAPABILITIES OF HALOPHILIC ARCHAEA ISOLATED FROM HIDES AND SKins AND THEIR PHENOTYpic AND PHYLOGENETic IDENTIFicATION by S. T. B LG School of Health, Canakkale Onsekiz Mart University, Terzioglu Campus Canakkale, Turkey, 17100. and B. MER ÇL YaPiCi Biology Department, Faculty of Arts and Science, Canakkale ONSEKIZ MART UNIVERSITY, TERZIOGLU CAMPUS, Canakkale, Turkey, 17100. and İsmail Karaboz Basic and Industrial Microbiology Section, Biology Department, Faculty of Science, Ege University, Bornova, İzmi r, Turkey, 35100. ABSTRACT INTRODUCTION This research aims to isolate extremely halophilic archaea The main constituent of the raw hide is protein, mainly from salted hides, to determine the capacities of their collagen (33% w/w), and remainder is moisture and fat. During hydrolytic enzymes, and to identify them by using phenotypic storage of raw hide, collagen’s excessive proteolysis by and molecular methods. Domestic and imported salted hide lysosomal autolysis or proteolytic bacterial enzymes can lead and skin samples obtained from eight different sources were to the disintegration of the structure of collagen fibers.1 used as the research material. 186 extremely halophilic Biodeterioration is among the major causes of impairment of microorganisms were isolated from salted raw hides and aesthetic, functional and other properties of leather and other skins. Some biochemical, antibiotic sensitivity, pH, NaCl, biopolymers or organic materials and the products made from temperature tolerance and quantitative and qualitative them. Due to the fact that prevention of biological degradation hydrolytic enzyme tests were performed on these isolates. In is very important in conservation and processing of leather, our study, taking into account the phenotypic findings of the great effort is being made for decontamination of these research, 34 of 186 isolates were selected. -
Hyperthermophilic Microorganisms - Karl O
EXTREMOPHILES - Vol. I - Hyperthermophilic Microorganisms - Karl O. Stetter HYPERTHERMOPHILIC MICROORGANISMS Karl O. Stetter Universität Regensburg, Lehrstuhl für Mikrobiologie, Universitätsstraße 31, D-93053 Regensburg, Germany Keywords: Thermophilic, hyperthermophile, extremophile, prokaryote, archaea, bacteria, primitive, phylogeny, physiology, autotrophic, heterotrophic, heat stability, protein, nucleic acid, biotechnology, biotope, volcanic, hydrothermal, geothermal, solfataric, abyssal, antarctic, extraterrestrial, Mars Contents 1. Introduction 2. Biotopes of hyperthermophiles 2.1. Terrestrial biotopes 2.2. Marine biotopes 3. Phylogeny of hyperthermophiles 4. Taxonomy of hyperthermophiles 5. Sampling and isolation of hyperthermophiles 6. Strategies of life and environmental adaptations of hyperthermophiles 6.1. General metabolic potentialities 6.2. Physiological properties of the different groups of hyperthermophiles 6.2.1. Terrestrial hyperthermophiles 6.2.2. Marine hyperthermophiles 7. Distribution of species and complexity in hyperthermophilic ecosystems 8. Basis of heat stability and the upper temperature limit for life 9. Conclusions: hyperthermophiles in the history of life Acknowledgments Bibliography Biographical Sketch Summary Hyperthermophilic Archaea and Bacteria with optimal growth temperatures between 80 and 110° C have been isolated from geo- and hydrothermally heated terrestrial and submarineUNESCO environments. Small subunit – rR NAEOLSS sequence comparisons indicate great phylogenetic diversity among the 32genera -
Isolation, Characterization and Phylogenetic Analysis of Halophilic Archaea from a Salt Mine in Central Anatolia (Turkey)
Polish Journal of Microbiology 2012, Vol. 61, No 2, 111–117 ORGINAL PAPER Isolation, Characterization and Phylogenetic Analysis of Halophilic Archaea from a Salt Mine in Central Anatolia (Turkey) EVRIM YILDIZ, BIRGUL OZCAN* AND MAHMUT CALISKAN Mustafa Kemal University, Biology Department, 31040 Hatay-Turkey Received 22 October 2011, revised 2 May 2012, accepted 5 May 2012 Abstract !e haloarchaeal diversity of a salt mine, a natural cave in central Anatolia, was investigated using convential microbiological and molecu- lar biology methods. Eight halophilic archaeal isolates selected based on their colony morphology and whole cell protein profiles were taxonomically classified on the basis of their morphological, physiological, biochemical properties, polar lipid and protein profiles and 16S rDNA sequences. From the 16S rDNA sequences comparisons it was established that the isolates CH2, CH3 and CHC resembled Halorubrum saccharovorum by 98.8%, 98.9% and 99.5%, respectively. !ere was a 99.7% similarity between the isolate CH11 and Halobac- terium noricense and 99.2% between the isolate CHA1 and Haloarcula argentinensis . !e isolate CH8K and CH8B revealed a similarity rate of 99.8% and 99.3% to Halococcus dombrowskii , respectively. It was concluded that the isolates named CH2, CH3 and CHC were clustered in the genus Halorubrum and that CHA1 and CH7 in the genus Haloarcula , CH8K and CH8B in the genus Halococcus and CH11 in the genus Halobacterium . K e y w o r d s: Halophilic archaea, Phylogeny, Taxonomy, Salt mine, Turkey Introduction 2006; 2009; Birbir et al ., 2007). Phylogenetic studies revealed that the halophilic archaeal isolates from Tur- !e increasing interest, in recent years, in micro- key clustered closely to genera Halorubrum , Haloarcula , organisms from hypersaline environments has resulted Natrinema , Halobacterium and Natronococcus (Ozcan in the discovery of several new species and genera et al ., 2007; Birbir et al ., 2007).