Planctomycetes and Methanotrophic Verrucomicrobia

Total Page:16

File Type:pdf, Size:1020Kb

Planctomycetes and Methanotrophic Verrucomicrobia PDF hosted at the Radboud Repository of the Radboud University Nijmegen The following full text is a publisher's version. For additional information about this publication click this link. http://hdl.handle.net/2066/149508 Please be advised that this information was generated on 2021-10-08 and may be subject to change. Cell biology of anammox Planctomycetes and methanotrophic Verrucomicrobia The cell envelope of anammox Planctomycetes Muriel van Teeseling Cell biology of anammox Planctomycetes and methanotrophic Verrucomicrobia Part i The cell envelope of anammox Planctomycetes Muriel van Teeseling Muriel van Teeseling (2015) Cell biology of anammox Planctomycetes and methanotrophic Verrucomicrobia. PhD thesis, Radboud University Nijmegen. This PhD project was financially supported by ERC AG 232937. Printing of this thesis was financially supported by SIAM gravitation grant 024002002 and by the Netherlands Society of Medical Microbiology (NVMM) and the Royal Netherlands Society for Microbiology (KNVM). Cover: Freeze‐fractured Methylacidimicrobium fagopyrum cell by Muriel van Teeseling. Print: Gildeprint Drukkerijen, Enschede, the Netherlands. ISBN: 978‐94‐6233‐163‐1. Cell biology of anammox Planctomycetes and methanotrophic Verrucomicrobia Proefschrift ter verkrijging van de graad van doctor aan de Radboud Universiteit Nijmegen op gezag van de rector magnificus, volgens besluit van het college van decanen in het openbaar te verdedigen op woensdag 13 januari 2016 om 14.30 uur precies door Muriël Caroline Frieda van Teeseling geboren op 25 december 1986 te Naarden Promotor Prof. dr. ir. M.S.M. Jetten Copromotor dr. L. van Niftrik Manuscriptcommissie Prof. dr. C. Mariani Prof. dr. W. Bitter (Vrije Universiteit Amsterdam) Prof. dr. S‐V. Albers (Albert‐Ludwigs‐Universität Freiburg, Duitsland) Contents Summary 3 (i) Samenvatting 5 (i) Chapter 1 General introduction 9 (i) Chapter 2 A new addition to the cell plan of anammox bacteria: 25 (i) Kuenenia stuttgartiensis has a protein surface layer (S‐layer) as outermost layer of the cell Chapter 3 The abundant protein Kustd1878 of the anammox 49 (i) Planctomycete Kuenenia stuttgartiensis is a pore‐forming outer membrane protein Chapter 4 Lipopolysaccharides in Planctomycetes: present or absent? 67 (i) Chapter 5 Anammox Planctomycetes have a peptidoglycan cell wall 89 (i) Chapter 6 Integration and Outlook 103 (i) References 121 (i) Acknowledgements 147 (i) Curriculum vitae 153 (i) Publication list 154 (i) 1 (i) 2 (i) Summary Anammox bacteria perform anaerobic ammonium oxidation and play an important role in the biological nitrogen cycle. They are applied to efficiently remove ammonium and nitrite from wastewater via a biochemically highly interesting mechanism involving hydrazine as intermediate and dinitrogen gas as end product. Anammox bacteria are also of particular interest to cell biologists. They belong to the Planctomycetes, a phylum characterized by a unique cell organization. Most Planctomycetes have two compartments, of which the innermost was interpreted as an intracytoplasmic compartment. Anammox bacteria have a third compartment that acts as a prokaryotic organelle in which the anammox reaction takes place. The anammox cell thus consists of the following compartments (from the outside inwards): the paryphoplasm, the riboplasm and the anammoxosome. An interesting aspect of all Planctomycetes is the cell envelope, which was proposed to lack peptidoglycan and an outer membrane. This is striking since almost all bacteria contain peptidoglycan in their cell envelope. Furthermore all bacteria classified as Gram‐negative additionally contain an outer membrane surrounding the peptidoglycan layer. Especially for anammox bacteria, many questions about the cell envelope remain, such as: Which components does the cell envelope contain? What are the characteristics of the outermost membrane (previously defined as a cytoplasmic membrane)? The research presented in this part of the thesis therefore aims to elucidate which components constitute the cell envelope of the model anammox species Kuenenia stuttgartiensis. With the new results we were able to answer the question if, as was postulated, this organism truly forms an exception to the Gram‐negative cell plan. Chapter 1 provides an introduction into bacterial cell (envelope) organization, (anammox) Planctomycetes and their cell biology. The results of chapter 2 show that a new layer was discovered as the outermost structure of the K. stuttgartiensis cell. This so‐called surface layer (S‐layer) consists of proteins and forms a symmetrical pattern. The S‐layer was characterized via freeze‐etching followed by transmission electron microscopy (TEM). Enrichment of this S‐layer led to the identification of the glycoprotein that builds this structure: Kustd1514. Two main glycan components were retrieved from Kustd1514 and their composition was elucidated via mass spectrometry coupled to liquid chromatography in combination with monosaccharide analysis. Immunogold localization using an antibody generated against Kustd1514 verified that this protein indeed forms the observed S‐layer. To investigate if the outermost membrane has characteristics of an outer membrane, most notably lipopolysaccharide (LPS) as specific lipids and outer membrane proteins (OMPs) as specific proteins, chapter 3 and chapter 4 describe in‐depth investigations of this membrane. The purification and characterization of a specific OMP, Kustd1878, are described in chapter 3. The structure of Kustd1878 was investigated via bioinformatics, suggesting the protein has an OMP‐specific ß‐barrel structure. Pore‐forming function, a typical characteristic of OMPs, was verified by membrane bilayer assays. Immunogold localization using an antibody generated against the purified protein furthermore suggested the presence of this protein in the outermost membrane of K. stuttgartiensis that can best be described as an outer membrane. 3 (i) Chapter 4 aims at elucidating if LPS, the main component of the outer leaflet of outer membranes, is present in K. stuttgartiensis and the two non‐anammox Planctomycetes Planctopirus limnophila and Rhodopirellula baltica. Genes necessary for the synthesis of lipid A, the part of the LPS that is anchored in the membrane, were identified in the genome of all three species and in the transcriptome of K. stuttgartiensis. Gel electrophoresis indicated the presence of LPS in all three species and polymyxin B, an antibiotic that disrupts the outer membrane upon binding to LPS, caused disruption of the membranes of R. baltica and to a lesser extent of K. stuttgartiensis and P. limnophila. However, the LPS components KDO and lipid A were not detected in K. stuttgartiensis via mass spectrometry methods. Therefore, the presence of LPS in the three Planctomycetes species seems plausible, but additional experiments are needed for further verification. In chapter 5 the proposed absence of peptidoglycan in anammox bacteria was revisited. Cryo‐TEM of vitreous sections identified a layer in between the cytoplasmic and outermost membrane in K. stuttgartiensis. When using a peptidoglycan isolation protocol, characteristic sacculi were observed. These sacculi disintegrated upon treatment with lysozyme, an agent that cleaves the sugar backbone of peptidoglycan. In addition, the presence of peptidoglycan was demonstrated in growing cultures by fluorescent probes that are built in during peptidoglycan synthesis. The presence of peptidoglycan in K. stuttgartiensis was ultimately proven when muropeptide analysis showed the composition of the sacculi to be typical for Gram‐negative peptidoglycan. Based on the results of the previous chapters, chapter 6 reaches the conclusion that (anammox) Planctomycetes can best be interpreted as Gram‐negative bacteria. This chapter furthermore gives an overview of the cell envelope of anammox bacteria, and describes key questions and associated hypotheses and experiments in order to come to a thorough understanding of the cell biology of (anammox) Planctomycetes. 4 (i) Samenvatting Anammoxbacteriën voeren anaërobe ammonium‐oxidatie uit en spelen een belangrijke rol in de biologische stikstofcyclus. Ze worden toegepast om op efficiënte wijze ammonium en nitriet uit afvalwater te verwijderen via een biochemisch zeer interessant mechanisme met hydrazine als tussenproduct en stikstofgas als eindproduct. Anammoxbacteriën zijn daarnaast bijzonder interessant voor celbiologen. Ze behoren tot de Planctomyceten, een phylum dat door een unieke celorganisatie gekarakteriseerd wordt. De meeste Planctomyceten hebben twee compartimenten waarvan de binnenste werd beschouwd als een intracytoplasmatisch compartiment. Anammoxbacteriën hebben daarnaast een derde compartiment dat functioneert als prokaryoot organel waarin de anammoxreactie plaatsvindt. Anammoxbacteriën bestaan dus uit de volgende compartimenten (van buiten naar binnen): het paryphoplasma, het riboplasma en het anammoxosoom. Een interessant aspect van alle Planctomyceten is de celenvelop, waarvan men aannam dat hierin zowel peptidoglycaan als een buitenmembraan ontbrak. Dit is opvallend aangezien bijna alle bacteriën peptidoglycaan bevatten in hun celenvelop. Daarnaast hebben alle bacteriën die als Gram‐negatief worden geklassificeerd een peptidoglycaan omringende buitenmembraan. In het bijzonder voor anammoxbacteriën zijn er nog veel open vragen over de celenvelop, zoals: Uit welke componenten bestaat de celenvelop? Wat zijn de karakteristieken van de buitenste membraan (dat voorheen als cytoplasmatisch
Recommended publications
  • ORGANIC GEOCHEMISTRY: CHALLENGES for the 21St CENTURY
    ORGANIC GEOCHEMISTRY: CHALLENGES FOR THE 21st CENTURY VOL. 2 Book of Abstracts of the Communications presented to the 22nd International Meeting on Organic Geochemistry Seville – Spain. September 12 -16, 2005 Editors: F.J. González-Vila, J.A. González-Pérez and G. Almendros Equipo de trabajo: Rocío González Vázquez Antonio Terán Rodíguez José Mª de la Rosa Arranz Maquetación: Rocío González Vázquez Fotomecánica e impresión: Akron Gráfica, Sevilla © 22nd IMOG, Sevilla 2005 Depósito legal: SE-61181-2005 I.S.B.N.: 84-689-3661-8 COMMITTEES INVOLVED IN THE ORGANIZATION OF THE 22 IMOG 2005 Chairman: Francisco J. GONZÁLEZ-VILA Vice-Chairman: José A. GONZÁLEZ-PÉREZ Consejo Superior de Investigaciones Científicas (CSIC) Instituto de Recursos Naturales y Agrobiología de Sevilla (IRNAS) Scientific Committee Francisco J. GONZÁLEZ-VILA (Chairman) IRNAS-CSIC, Spain Gonzalo ALMENDROS Claude LARGEAU CCMA-CSIC, Spain ENSC, France Pim van BERGEN José C. del RÍO SHELL Global Solutions, The Netherlands IRNAS-CSIC, Spain Jørgen A. BOJESEN-KOEFOED Jürgen RULLKÖTTER GEUS, Denmark ICBM, Germany Chris CORNFORD Stefan SCHOUTEN IGI, UK NIOZ, The Netherlands Gary ISAKSEN Eugenio VAZ dos SANTOS NETO EXXONMOBIL, USA PETROBRAS RD, Brazil Local Committee José Ramón de ANDRÉS IGME, Spain Mª Carmen DORRONSORO Mª Enriqueta ARIAS Universidad del País Vasco Universidad de Alcalá Antonio GUERRERO Tomasz BOSKI Universidad de Sevilla Universidad do Algarve, Faro, Portugal Juan LLAMAS Ignacio BRISSON ETSI Minas de Madrid Repsol YPF Albert PERMANYER Juan COTA Universidad de Barcelona Universidad de Sevilla EAOG Board Richard L. PATIENCE (Chairman) Sylvie DERENNE (Secretary) Ger W. van GRAAS (Treasurer) Walter MICHAELIS (Awards) Francisco J. GONZALEZ-VILA (Newsletter) C.
    [Show full text]
  • Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-Rich, Geothermal Spring 2 3 Lewis M
    bioRxiv preprint doi: https://doi.org/10.1101/428698; this version posted September 27, 2018. 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 Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-rich, Geothermal Spring 2 3 Lewis M. Ward1,2,3*, Airi Idei4, Mayuko Nakagawa2,5, Yuichiro Ueno2,5,6, Woodward W. 4 Fischer3, Shawn E. McGlynn2* 5 6 1. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138 USA 7 2. Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo, 152-8550, Japan 8 3. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 9 91125 USA 10 4. Department of Biological Sciences, Tokyo Metropolitan University, Hachioji, Tokyo 192-0397, 11 Japan 12 5. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, 13 152-8551, Japan 14 6. Department of Subsurface Geobiological Analysis and Research, Japan Agency for Marine-Earth 15 Science and Technology, Natsushima-cho, Yokosuka 237-0061, Japan 16 Correspondence: [email protected] or [email protected] 17 18 Abstract 19 Hydrothermal systems, including terrestrial hot springs, contain diverse and systematic 20 arrays of geochemical conditions that vary over short spatial scales due to progressive interaction 21 between the reducing hydrothermal fluids, the oxygenated atmosphere, and in some cases 22 seawater. At Jinata Onsen, on Shikinejima Island, Japan, an intertidal, anoxic, iron- and 23 hydrogen-rich hot spring mixes with the oxygenated atmosphere and sulfate-rich seawater over 24 short spatial scales, creating an enormous range of redox environments over a distance ~10 m.
    [Show full text]
  • Nicole Kube Phd
    Leibniz-Institut für Meereswissenschaften The integration of microalgae photobioreactors in a recirculation system for low water discharge mariculture Dissertation zur Erlangung des Doktorgrades der Mathematisch-Naturwissenschaftlichen Fakultät an der Christian-Albrechts-Universität zu Kiel vorgelegt von Nicole Kube Kiel, 2006 Referentin: Prof. Dr. Karin Lochte Koreferent: Prof. Dr. Dr. h.c. Harald Rosenthal Tag der mündlichen Prüfung: Zum Druck genehmigt: Kiel, den Der Dekan Foreword The manuscripts included in this thesis are prepared for submission to peer- reviewed journals as listed below: Wecker B., Kube N., Bischoff A.A., Waller U. (2006). MARE – Marine Artificial Recirculated Ecosystem: feasibility and modelling of a novel integrated recirculation system. (manuscript) Kube N., Bischoff A.A., Wecker B., Waller U. Cultivation of microalgae using a continuous photobioreactor system based on dissolved nutrients of a recirculation system for low water discharge mariculture (manuscript) Kube N. And Rosenthal H. Ozonation and foam fractionation used for the removal of bacteria and parti- cles in a marine recirculation system for microalgae cultivation (manuscript) Kube N., Bischoff A.A., Blümel M., Wecker B., Waller U. MARE – Marine Artificial Recirulated Ecosystem II: Influence on the nitrogen cycle in a marine recirculation system with low water discharge by cultivat- ing detritivorous organisms and phototrophic microalgae. (manuscript) This thesis has been realised with the help of several collegues. The contributions in particular
    [Show full text]
  • Nutrient Control Design Manual: State of Technology Review Report,” Were
    United States Office of Research and EPA/600/R‐09/012 Environmental Protection Development January 2009 Agency Washington, DC 20460 Nutrient Control Design Manual State of Technology Review Report EPA/600/R‐09/012 January 2009 Nutrient Control Design Manual State of Technology Review Report by The Cadmus Group, Inc 57 Water Street Watertown, MA 02472 Scientific, Technical, Research, Engineering, and Modeling Support (STREAMS) Task Order 68 Contract No. EP‐C‐05‐058 George T. Moore, Task Order Manager United States Environmental Protection Agency Office of Research and Development / National Risk Management Research Laboratory 26 West Martin Luther King Drive, Mail Code 445 Cincinnati, Ohio, 45268 Notice This document was prepared by The Cadmus Group, Inc. (Cadmus) under EPA Contract No. EP‐C‐ 05‐058, Task Order 68. The Cadmus Team was lead by Patricia Hertzler and Laura Dufresne with Senior Advisors Clifford Randall, Emeritus Professor of Civil and Environmental Engineering at Virginia Tech and Director of the Occoquan Watershed Monitoring Program; James Barnard, Global Practice and Technology Leader at Black & Veatch; David Stensel, Professor of Civil and Environmental Engineering at the University of Washington; and Jeanette Brown, Executive Director of the Stamford Water Pollution Control Authority and Adjunct Professor of Environmental Engineering at Manhattan College. Disclaimer The views expressed in this document are those of the individual authors and do not necessarily, reflect the views and policies of the U.S. Environmental Protection Agency (EPA). Mention of trade names or commercial products does not constitute endorsement or recommendation for use. This document has been reviewed in accordance with EPA’s peer and administrative review policies and approved for publication.
    [Show full text]
  • Metagenomic Analysis Reveals Rapid Development of Soil Biota on Fresh Volcanic Ash Hokyung Song1, Dorsaf Kerfahi2, Koichi Takahashi3, Sophie L
    www.nature.com/scientificreports OPEN Metagenomic analysis reveals rapid development of soil biota on fresh volcanic ash Hokyung Song1, Dorsaf Kerfahi2, Koichi Takahashi3, Sophie L. Nixon1, Binu M. Tripathi4, Hyoki Kim5, Ryunosuke Tateno6* & Jonathan Adams7* Little is known of the earliest stages of soil biota development of volcanic ash, and how rapidly it can proceed. We investigated the potential for soil biota development during the frst 3 years, using outdoor mesocosms of sterile, freshly fallen volcanic ash from the Sakurajima volcano, Japan. Mesocosms were positioned in a range of climates across Japan and compared over 3 years, against the developed soils of surrounding natural ecosystems. DNA was extracted from mesocosms and community composition assessed using 16S rRNA gene sequences. Metagenome sequences were obtained using shotgun metagenome sequencing. While at 12 months there was insufcient DNA for sequencing, by 24 months and 36 months, the ash-soil metagenomes already showed a similar diversity of functional genes to the developed soils, with a similar range of functions. In a surprising contrast with our hypotheses, we found that the developing ash-soil community already showed a similar gene function diversity, phylum diversity and overall relative abundances of kingdoms of life when compared to developed forest soils. The ash mesocosms also did not show any increased relative abundance of genes associated with autotrophy (rbc, coxL), nor increased relative abundance of genes that are associated with acquisition of nutrients from abiotic sources (nifH). Although gene identities and taxonomic afnities in the developing ash-soils are to some extent distinct from the natural vegetation soils, it is surprising that so many of the key components of a soil community develop already by the 24-month stage.
    [Show full text]
  • University of Southampton Research Repository Eprints Soton
    University of Southampton Research Repository ePrints Soton Copyright © and Moral Rights for this thesis are retained by the author and/or other copyright owners. A copy can be downloaded for personal non-commercial research or study, without prior permission or charge. This thesis cannot be reproduced or quoted extensively from without first obtaining permission in writing from the copyright holder/s. The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the copyright holders. When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given e.g. AUTHOR (year of submission) "Full thesis title", University of Southampton, name of the University School or Department, PhD Thesis, pagination http://eprints.soton.ac.uk UNIVERSITY OF SOUTHAMPTON FACULTY OF ENGINEERING , SCIENCE AND MATHEMATICS School of Ocean and Earth Science The role of microbial populations in the cycling of iron and manganese from marine aggregates by Sergio Balzano Thesis for the degree of Doctor of Phylosophy June 2009 BIOTRACS Bio-transformations of trace elements in aquatic systems THIS THESIS WAS COMPLETED USING FRAMEWORK 6 FUNDING FROM THE EUROPEAN UNION. RESEARCH DG HUMAN RESOURCES AND MOBILITY PROJECT NO: 514262 UNIVERSITY OF SOUTHAMPTON ABSTRACT FACULTY OF ENGINEERING, SCIENCE AND MATHEMATICS SCHOOL OF OCEAN AND EARTH SCIENCES Doctor of philosophy THE ROLE OF MICROBIAL PROCESSES IN MARINE AGGREGATES ON THE CYCLING OF IRON AND MANGANESE By Sergio Balzano Marine aggregates play an important role in the cycling of carbon, nutrients and trace metals.
    [Show full text]
  • Aquatic Microbial Ecology 55:1
    Vol. 55: 1–16, 2009 AQUATIC MICROBIAL ECOLOGY Printed April 2009 doi: 10.3354/ame01277 Aquat Microb Ecol Published online March 18, 2009 OPENPEN ACCESSCCESS FEATURE ARTICLE Vertical diversity of bacteria in an oxygen-stratified humic lake, evaluated using DNA and phospholipid analyses Sami Taipale1, 2, Roger I. Jones2, Marja Tiirola2,* 1University of Washington, Civil and Environmental Engineering, Box 352700, 201 More Hall, Seattle, Washington 98195, USA 2Department of Biological and Environmental Science, PO Box 35, 40014 University of Jyväskylä, Finland ABSTRACT: Microbes play a particularly important role in the food web in lakes with high dissolved organic carbon content. The bacterial community of a polyhumic lake, Mekkojärvi, was studied using DNA techniques and phospholipid fatty acid (PLFA) analysis during the mid-summer period of water column strati- fication. According to the 16S rRNA gene clone libraries and length heterogeneity analysis (LH-PCR), heterotrophic bacteria dominated only in the oxic epilimnion, in which various Actinobacteria (mostly cluster acI-B) and Betaproteobacteria (especially Poly- nucleobacter subcluster PnecC) were common. Se- quences assigned to heterotrophic, methylotrophic, photoautotrophic, and chemoautotrophic genera were all abundant in the oxic-anoxic boundary layer. Methylobacter and Methylophilus were dominant Mekkojärvi, in southern Finland, is one of countless small, genera among methylotrophic bacteria. Sequences humic lakes around the boreal zone; inset: sampling the brown water rich in DOC. assigned to the photoautotrophic green sulfur bac- Photos: Sami Taipale terium Chlorobium sp. dominated in the anoxic water column, in which the microbial PLFA biomass was 6 times higher than in the oxic surface layer. All PLFA- profiles were dominated by 16 monounsaturated fatty INTRODUCTION acids typical of Gram-negative bacteria, whereas iso- and anteiso-branched PLFAs typical of Actinobacteria Microbial foodwebs of humic (dystrophic) lakes were present only in minor proportions.
    [Show full text]
  • 7.014 Lectures 16 &17: the Biosphere & Carbon and Energy Metabolism
    MIT Department of Biology 7.014 Introductory Biology, Spring 2005 7.014 Lectures 16 &17: The Biosphere & Carbon and Energy Metabolism Simplified Summary of Microbial Metabolism The metabolism of different types of organisms drives the biogeochemical cycles of the biosphere. Balanced oxidation and reduction reactions keep the system from “running down”. All living organisms can be ordered into two groups1, autotrophs and heterotrophs, according to what they use as their carbon source. Within these groups the metabolism of organisms can be further classified according to their source of energy and electrons. Autotrophs: Those organisms get their energy from light (photoautotrophs) or reduced inorganic compounds (chemoautotrophs), and their carbon from CO2 through one of the following processes: Photosynthesis (aerobic) — Light energy used to reduce CO2 to organic carbon using H2O as a source of electrons. O2 evolved from splitting H2O. (Plants, algae, cyanobacteria) Bacterial Photosynthesis (anaerobic) — Light energy used to reduce CO2 to organic carbon (same as photosynthesis). H2S is used as the electron donor instead of H2O. (e.g. purple sulfur bacteria) Chemosynthesis (aerobic) — Energy from the oxidation of inorganic molecules is used to reduce CO2 to organic carbon (bacteria only). -2 e.g. sulfur oxidizing bacteria H2S → S → SO4 + - • nitrifying bacteria NH4 → NO2 → NO3 iron oxidizing bacteria Fe+2 → Fe+3 methane oxidizing bacteria (methanotrophs) CH4 → CO2 Heterotrophs: These organisms get their energy and carbon from organic compounds (supplied by autotrophs through the food web) through one or more of the following processes: Aerobic Respiration (aerobic) ⎯ Oxidation of organic compounds to CO2 and H2O, yielding energy for biological work.
    [Show full text]
  • Difference Between Chemoorganotrophic and Obligate Autotroph
    Difference Between Chemoorganotrophic And Obligate Autotroph Cary underbidding misanthropically. Ulric often demise parlous when conjugated Ford mollycoddles indistinctly and domes her cyma. Lew often descants unfeignedly when isocheimic Tedie turn-offs designedly and Judaizing her accentors. No mechanism for anaerobic metabolism in conjunction with a common when algae, along the catabolism ofaromatic compounds provide evidence was a difference between trees inferred with the four genera have a consensus approach to The physiological characteristics of use different types of bacteria and their interactions. CO2 stimulates the chemoorganotrophic growth of both ammonia oxidizers and the. Chemoorganotrophic Definition of Chemoorganotrophic by. While Acidithiobacillus ferrooxidans growing on FeSO4 would depict an obligate aerobe. A fundamental metabolic distinction is between autotrophs and heterotrophs. Cthe intermediate steps of autotroph and only select multiple curvature and to safely place in each student need to a membrane that can be essentially the deep. The facultative autotroph also oxidizes a ridicule of organic compounds such. Bacterial Metabolism Medical Microbiology NCBI Bookshelf. Interestingly the amount cure the carboxylase in M capsulatus in chemostat culture. Facultative autotroph Can reproduce as autotroph if they must first better as. Learning Objectives Differentiate photoautotrophs from photoheterotrophs. Electron Transport Chain. Ecology of Cyanobacteria II Their Diversity in Space faculty Time. A Photographic Atlas for the Microbiology Laboratory. 5 Algae Biology LibreTexts. MB302 Oregon State University. Autotroph t-trf An organism that manufactures its own value from inorganic substances such high carbon dioxide and ammonia Most autotrophs such clean green plants certain algae and photosynthetic bacteria use ticket for energy. Ment was achieved by comparison by the labour count helpless the pervert of Thiobacillus A2 obtained on.
    [Show full text]
  • Control Factors of the Marine Nitrogen Cycle
    Control factors of the marine nitrogen cycle The role of meiofauna, macrofauna, oxygen and aggregates Stefano Bonaglia Academic dissertation for the Degree of Doctor of Philosophy in Geochemistry at Stockholm University to be publicly defended on Wednesday 29 April 2015 at 13.00 in Nordenskiöldsalen, Geovetenskapens hus, Svante Arrhenius väg 12. Abstract The ocean is the most extended biome present on our planet. Recent decades have seen a dramatic increase in the number and gravity of threats impacting the ocean, including discharge of pollutants, cultural eutrophication and spread of alien species. It is essential therefore to understand how different impacts may affect the marine realm, its life forms and biogeochemical cycles. The marine nitrogen cycle is of particular importance because nitrogen is the limiting factor in the ocean and a better understanding of its reaction mechanisms and regulation is indispensable. Furthermore, new nitrogen pathways have continuously been described. The scope of this project was to better constrain cause-effect mechanisms of microbially mediated nitrogen pathways, and how these can be affected by biotic and abiotic factors. This thesis demonstrates that meiofauna, the most abundant animal group inhabiting the world’s seafloors, considerably alters nitrogen cycling by enhancing nitrogen loss from the system. In contrast, larger fauna such as the polychaete Marenzelleria spp. enhance nitrogen retention, when they invade eutrophic Baltic Sea sediments. Sediment anoxia, caused by nutrient excess, has negative consequences for ecosystem processes such as nitrogen removal because it stops nitrification, which in turn limits both denitrification and anammox. This was the case of Himmerfjärden and Byfjord, two estuarine systems affected by anthropogenic activities, such as treated sewage discharges.
    [Show full text]
  • Changes and Other Important Stuff
    1/23/2012 Changes and other Important Stuff • Rm change – Maury 112 – Geology Lab • web page is not really on Collab – http://www.evsc.virginia.edu/~alm7d/523 • [email protected] • reading assignment: above/handouts/papers Krumbein and Dyer – This Planet is Alive CO2 Organic Matter 1 1/23/2012 Microbial Ecology Living with the unseen majority The Microbe is so very small You cannot make him out at all, But many sanguine people hope To see him through a microscope. His jointed tongue that lies beneath A hundred curious rows of teeth; His seven tufted tails with lots Of lovely pink and purple spots, On each of which a pattern stands, Composed of forty separate bands; His eyebrows of a tender green; All these have never yet been seen-- But Scientists, who ought to know, Assure us that they must be so.... Oh! let us never, never doubt What nobody is sure about! (Hillaire Beloc) Wodzinski’s Basic Laws of Bacteriology From about 1967 Mills’ corollaries to Wodzinski’s laws 1. Bacteria are very small 1a. But there are a LOT of them 1b. And they grow VERY fast 2. Bacteria are our friends 2a. As long as you hang out with the right crowd 2b. And even your friends can play jokes on you 3. Bacteria always have the last word 3a. RIGHT! 2 1/23/2012 10 – 100 μm ≈ 1 μm BACTERIA ARE SMALL : a typical (large) rod- shaped bacterium 0.5μm x 2μm bacterium has a volume of ca. 0.393μm3. (same as a cube 0.732μm on a side) If we tried to pack those cubes into another cube that is 1 cm3, the cube will hold about 2.5 x 1012 cells.
    [Show full text]
  • Distribution and Diversity of Bacterial Chemolithotrophs in Marine and Freshwater Sediments Lisa M
    The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library 5-2006 Distribution and Diversity of Bacterial Chemolithotrophs in Marine and Freshwater Sediments Lisa M. Nigro Follow this and additional works at: http://digitalcommons.library.umaine.edu/etd Part of the Environmental Microbiology and Microbial Ecology Commons, and the Marine Biology Commons Recommended Citation Nigro, Lisa M., "Distribution and Diversity of Bacterial Chemolithotrophs in Marine and Freshwater Sediments" (2006). Electronic Theses and Dissertations. 517. http://digitalcommons.library.umaine.edu/etd/517 This Open-Access Thesis is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. DISTRIBUTION AND DIVERSITY OF BACTERIAL CHEMOLITHOTROPHS IN MARINE AND FRESHWATER SEDIMENTS By Lisa M. Nigro B.S. Rutgers University, 2001 A THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science (in Microbiology) The Graduate School The University of Maine May, 2006 Advisory Committee: Dr. Gary M. King, Professor of Microbiology and Oceanography, Advisor Dr. Jean MacRae, Assistant Professor of Environmental Engineering Dr. Bryan Dail, Assistant Professor of Soil Microbiology LIBRARY RIGHTS STATEMENT In presenting this thesis in partial fulfillment of the requirements for an advanced degree at The University of Maine, I agree that the Library shall make it freely available for inspection. I further agree that permission for “fair use” copying of this thesis for scholarly purposes may be granted by the Librarian. It is understood that any copying or publication of this thesis for financial gain shall not be allowed without my written permission.
    [Show full text]