In-Situ Metatranscriptomic Analyses Reveal the Metabolic Flexibility Of
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Microbial Community Composition and Function Beneath Temperate Trees Exposed to Elevated Atmospheric Carbon Dioxide and Ozone
Oecologia (2002) 131:236–244 DOI 10.1007/s00442-002-0868-x ECOSYSTEMS ECOLOGY Rebecca L. Phillips · Donald R. Zak William E. Holmes · David C. White Microbial community composition and function beneath temperate trees exposed to elevated atmospheric carbon dioxide and ozone Received: 1 August 2001 / Accepted: 13 December 2001 / Published online: 14 February 2002 © Springer-Verlag 2002 Abstract We hypothesized that changes in plant growth activity and microbial metabolism of cellobiose, and that resulting from atmospheric CO2 and O3 enrichment microbial processes under early-successional aspen and would alter the flow of C through soil food webs and birch species were more strongly affected by CO2 and O3 that this effect would vary with tree species. To test this enrichment than those under late-successional maple. idea, we traced the course of C through the soil microbial community using soils from the free-air CO2 and O3 Keywords Soil microorganisms · enrichment site in Rhinelander, Wisconsin. We added Carbon-13-phospholipid fatty acid analysis · either 13C-labeled cellobiose or 13C-labeled N-acetylglu- Elevated carbon dioxide · Elevated ozone · cosamine to soils collected beneath ecologically distinct Soil carbon cycling temperate trees exposed for 3 years to factorial CO2 –1 (ambient and 200 µl l above ambient) and O3 (ambient and 20 µl l–1 above ambient) treatments. For both labeled Introduction substrates, recovery of 13C in microbial respiration increased beneath plants grown under elevated CO2 by Human activity has increased the concentration of CO2 29% compared to ambient; elevated O3 eliminated this and O3 in the earth’s troposphere (Barnola et al. -
A Study on the Phototrophic Microbial Mat Communities of Sulphur Mountain Thermal Springs and Their Association with the Endangered, Endemic Snail Physella Johnsoni
A Study on the Phototrophic Microbial Mat Communities of Sulphur Mountain Thermal Springs and their Association with the Endangered, Endemic Snail Physella johnsoni By Michael Bilyj A thesis submitted to the Faculty of Graduate Studies in partial fulfillment of the requirements for the degree of Master of Science Department of Microbiology Faculty of Science University of Manitoba Winnipeg, Manitoba October 2011 © Copyright 2011, Michael A. Bilyj 1 Abstract The seasonal population fluctuation of anoxygenic phototrophs and the diversity of cyanobacteria at the Sulphur Mountain thermal springs of Banff, Canada were investigated and compared to the drastic population changes of the endangered snail Physella johnsoni. A new species and two strains of Rhodomicrobium were taxonomically characterized in addition to new species of Rhodobacter and Erythromicrobium. Major mat-forming organisms included Thiothrix-like species, oxygenic phototrophs of genera Spirulina, Oscillatoria, and Phormidium and purple nonsulfur bacteria Rhodobacter, Rhodopseudomonas and Rhodomicrobium. Aerobic anoxygenic phototrophs comprised upwards of 9.6 x 104 CFU/cm2 of mat or 18.9% of total aerobic heterotrophic bacterial isolates at certain sites, while maximal purple nonsulfur and purple sulfur bacteria were quantified at 3.2 x 105 and 2.0 x 106 CFU/cm2 of mat, respectively. Photosynthetic activity measurements revealed incredibly productive carbon fixation rates averaging 40.5 mg C/cm2/24 h. A temporal mismatch was observed for mat area and prokaryote-based organics to P. johnsoni population flux in a ―tracking inertia‖ manner. 2 Acknowledgements It is difficult to express sufficient gratitude to my supervisor Dr. Vladimir Yurkov for his unfaltering patience, generosity and motivation throughout this entire degree. -
Chromatic Acclimation and Population Dynamics of Green Sulfur Bacteria Grown with Spectrally Tailored Light
Chromatic acclimation and population dynamics of green sulfur bacteria grown with spectrally tailored light Semion K. Saikin,a,† Yadana Khin,b Joonsuk Huh,a Moataz Hannout,c Yaya Wang,b Farrokh Zare,b Alán Aspuru-Guzik,a Joseph Kuo-Hsiang Tangb,* a Department of Chemistry and Chemical Biology, Harvard University, Cambridge, MA 02138 USA; b School of Chemistry and Biochemistry, Clark University, Worcester, MA 01610-1477 USA, c Department of Physics, Clark University, Worcester, MA 01610-1477 USA To whom correspondence should be addressed: †E-mail: [email protected], Tel: 1-617-496-8221, Fax: 1-617-496-9411 *E-mail: [email protected],Tel: 1-614-316-7886, Fax: 1-508-793-8861 Keywords: photosynthesis, chromatic acclimation, energy transfer, light-harvesting complex, chlorosome, green sulfur bacteria Living organisms have to adjust to their surrounding in order to survive in stressful conditions. We study this mechanism in one of most primitive creatures – photosynthetic green sulfur bacteria. These bacteria absorb photons very efficiently using the chlorosome antenna complexes and perform photosynthesis in extreme low-light environments. How the chlorosomes in green sulfur bacteria are acclimated to the stressful light conditions, for instance, if the spectrum of light is not optimal for absorption, is unknown. Studying Chlorobaculum tepidum cultures with far-red to near-infrared light-emitting diodes, we found that these bacteria react to changes in energy flow by regulating the amount of light- absorbing pigments and the size of the chlorosomes. Surprisingly, our results indicate that the bacteria can survive in near-infrared lights capturing low-frequency photons by the intermediate units of the light-harvesting complex. -
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. -
Chapter 3 the Title and Subtitle of This Chapter Convey a Dual Meaning
3.1. Introduction Chapter 3 The title and subtitle of this chapter convey a dual meaning. At first reading, the subtitle Photosynthetic Reaction might seem to indicate that the topic of the structure, function and organization of Centers: photosynthetic reaction centers is So little time, so much to do exceedingly complex and that there is simply insufficient time or space in this brief article to cover the details. While this is John H. Golbeck certainly the case, the subtitle is Department of Biochemistry additionally meant to convey the idea that there is precious little time after the and absorption of a photon to accomplish the Molecular Biology task of preserving the energy in the form of The Pennsylvania State University stable charge separation. University Park, PA 16802 USA The difficulty is there exists a fundamental physical limitation in the amount of time available so that a photochemically induced excited state can be utilized before the energy is invariably wasted. Indeed, the entire design philosophy of biological reaction centers is centered on overcoming this physical, rather than chemical or biological, limitation. In this chapter, I will outline the problem of conserving the free energy of light-induced charge separation by focusing on the following topics: 3.2. Definition of the problem: the need to stabilize a charge-separated state. 3.3. The bacterial reaction center: how the cofactors and proteins cope with this problem in a model system. 3.4. Review of Marcus theory: what governs the rate of electron transfer in proteins? 3.5. Photosystem II: a variation on a theme of the bacterial reaction center. -
Aerobic Respiration
Life is based on redox • All energy generation in biological systems is due to redox (reduction-oxidation) reactions Aerobic Respiration: + - C6H12O6 + 6 H2O ==> 6 CO2 + 24 H +24 e oxidation electron donor (aka energy source) + - (O2+ 4H + 4e ==> 2H2O) x6 reduction electron acceptor --------------------------------------- C6H12O6 + 6 O2 ==> 6 CO2 + 6 H2O overall reaction (24 electrons) Types of bacterial metabolisms • While eukaryotes only reduce O2 and oxidize organic compounds, prokaryotes can use a variety of electron donors and acceptors, organic and inorganic. - • Aerobic respiration: e acceptor is O2 - • Anaerobic respiration: e acceptor is not O2 • Fermentation: e- donor and acceptor are organic molecules • Chemolithotrophy: e- donor and acceptor are inorganic molecules • Phototrophy: e- donor is light and e- acceptor is either organic or inorganic all microorganisms energy source? chemical light chemotroph phototroph carbon source? carbon source? organic organic CO CO compound 2 compound 2 chemoheterotroph chemoautotroph photoheterotroph photoautotroph e- acceptor? Nitrifying and sulfur- use H O to reduce CO ? oxidizing bacteria 2 2 green non-sulfur and O Other than O 2 2 purple non-sulfur bacteria anoxygenic oxygenic photosynthesis: photosynthesis: green sulfur and most bacteria Organic Inorganic cyanobacteria compound compound purple sulfur bacteria fermentative organism anaerobic respiration: nitrate, sulfate, Fe(III) Aerobic or anaerobic respiration Chemolithotrophy Important molecules Redox Electron Carrier: for example the -
The Vulnerability of Microbial Ecosystems in a Changing Climate: Potential Impact in Shark Bay
life Review The Vulnerability of Microbial Ecosystems in a Changing Climate: Potential Impact in Shark Bay Max Reinold 1,2, Hon Lun Wong 1,2, Fraser I. MacLeod 1,2, Julia Meltzer 1,2, April Thompson 1,2 and Brendan P. Burns 1,2,* 1 School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney 2052, Australia 2 Australian Centre for Astrobiology, The University of New South Wales, Sydney 2052, Australia * Correspondence: [email protected]; Tel.: +612-9385-3659; Fax: +612-9385-1591 Received: 30 July 2019; Accepted: 28 August 2019; Published: 2 September 2019 Abstract: The potential impact of climate change on eukaryotes, including humans, has been relatively well described. In contrast, the contribution and susceptibility of microorganisms to a changing climate have, until recently, received relatively less attention. In this review, the importance of microorganisms in the climate change discourse is highlighted. Microorganisms are responsible for approximately half of all primary production on earth, support all forms of macroscopic life whether directly or indirectly, and often persist in “extreme” environments where most other life are excluded. In short, microorganisms are the life support system of the biosphere and therefore must be included in decision making regarding climate change. Any effects climate change will have on microorganisms will inevitably impact higher eukaryotes and the activity of microbial communities in turn can contribute to or alleviate the severity of the changing climate. It is of vital importance that unique, fragile, microbial ecosystems are a focus of research efforts so that their resilience to extreme weather events and climate change are thoroughly understood and that conservation efforts can be implemented as a response. -
Evolution of the 3-Hydroxypropionate Bicycle and Recent Transfer of Anoxygenic Photosynthesis Into the Chloroflexi
Evolution of the 3-hydroxypropionate bicycle and recent transfer of anoxygenic photosynthesis into the Chloroflexi Patrick M. Shiha,b,1, Lewis M. Wardc, and Woodward W. Fischerc,1 aFeedstocks Division, Joint BioEnergy Institute, Emeryville, CA 94608; bEnvironmental Genomics and Systems Biology Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720; and cDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125 Edited by Bob B. Buchanan, University of California, Berkeley, CA, and approved August 21, 2017 (received for review June 14, 2017) Various lines of evidence from both comparative biology and the provide a hard geological constraint on these analyses, the timing geologic record make it clear that the biochemical machinery for of these evolutionary events remains relative, thus highlighting anoxygenic photosynthesis was present on early Earth and provided the uncertainty in our understanding of when and how anoxy- the evolutionary stock from which oxygenic photosynthesis evolved genic photosynthesis may have originated. ca. 2.3 billion years ago. However, the taxonomic identity of these A less recognized alternative is that anoxygenic photosynthesis early anoxygenic phototrophs is uncertain, including whether or not might have been acquired in modern bacterial clades relatively they remain extant. Several phototrophic bacterial clades are thought recently. This possibility is supported by the observation that to have evolved before oxygenic photosynthesis emerged, including anoxygenic photosynthesis often sits within a derived position in the Chloroflexi, a phylum common across a wide range of modern the phyla in which it is found (3). Moreover, it is increasingly environments. Although Chloroflexi have traditionally been thought being recognized that horizontal gene transfer (HGT) has likely to be an ancient phototrophic lineage, genomics has revealed a much played a major role in the distribution of phototrophy (8–10). -
1 Temperature and Carbon Assimilation Regulate The
Temperature and Carbon Assimilation Regulate the Chlorosome Biogenesis in Green Sulfur Bacteria Joseph Kuo-Hsiang Tang1,*, Semion K. Saikin2, Sai Venkatesh Pingali3, Miriam M. Enriquez4, Joonsuk Huh2, Harry A. Frank4, Volker S. Urban3, Alán Aspuru-Guzik2 1School of Chemistry and Biochemistry, Clark University, Worcester, MA 01610 USA, 2Department of Chemistry and Chemical Biology, Harvard University, Cambridge, MA 02138 USA, 3Center for Structural Molecular Biology, Biology and Soft Matter Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831 USA, 4Department of Chemistry, University of Connecticut, Storrs, CT 06269 USA Running title: Metabolic regulation of chlorosome *To whom correspondence should be addressed: Tel: 1-614-316-7886, Fax: 1-508-793-8861, E-mail: [email protected] Abstract Green photosynthetic bacteria adjust the structure and functionality of the chlorosome – the light absorbing antenna complex – in response to environmental stress factors. The chlorosome is a natural self-assembled aggregate of bacteriochlorophyll (BChl) molecules. In this study we report the regulation of the biogenesis of the Chlorobaculum tepidum chlorosome by carbon assimilation in conjunction with temperature changes. Our studies indicate that the carbon source and thermal stress culture of Cba. tepidum grows slower and incorporates less BChl c in the chlorosome. Compared with the chlorosome from other cultural conditions we investigated, the chlorosome from the carbon source and thermal stress culture displays: (a) smaller cross- sectional radius and overall size; (b) simplified BChl c homologues with smaller side chains; (c) blue-shifted Qy absorption maxima and (d) a sigmoid-shaped circular dichroism (CD) spectra. Using a theoretical model we analyze how the observed spectral modifications can be associated with structural changes of BChl aggregates inside the chlorosome. -
The Reaction Center of Green Sulfur Bacteria1
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Elsevier - Publisher Connector Biochimica et Biophysica Acta 1507 (2001) 260^277 www.bba-direct.com Review The reaction center of green sulfur bacteria1 G. Hauska a;*, T. Schoedl a, Herve¨ Remigy b, G. Tsiotis c a Lehrstuhl fu«r Zellbiologie und P£anzenphysiologie, Fakulta«tfu«r Biologie und Vorklinische Medizin, Universita«t Regensburg, 93040 Regenburg, Germany b Biozentrum, M.E. Mu«ller Institute of Microscopic Structural Biology, University of Basel, CH-4056 Basel, Switzerland c Division of Biochemistry, Department of Chemistry, University of Crete, 71409 Heraklion, Greece Received 9 April 2001; received in revised form 13 June 2001; accepted 5 July 2001 Abstract The composition of the P840-reaction center complex (RC), energy and electron transfer within the RC, as well as its topographical organization and interaction with other components in the membrane of green sulfur bacteria are presented, and compared to the FeS-type reaction centers of Photosystem I and of Heliobacteria. The core of the RC is homodimeric, since pscA is the only gene found in the genome of Chlorobium tepidum which resembles the genes psaA and -B for the heterodimeric core of Photosystem I. Functionally intact RC can be isolated from several species of green sulfur bacteria. It is generally composed of five subunits, PscA^D plus the BChl a-protein FMO. Functional cores, with PscA and PscB only, can be isolated from Prostecochloris aestuarii. The PscA-dimer binds P840, a special pair of BChl a-molecules, the primary electron acceptor A0, which is a Chl a-derivative and FeS-center FX. -
Assessing the Chemistry and Bioavailability of Dissolved Organic Matter from Glaciers and Rock Glaciers
RESEARCH ARTICLE Assessing the Chemistry and Bioavailability of Dissolved 10.1029/2018JG004874 Organic Matter From Glaciers and Rock Glaciers Special Section: Timothy Fegel1,2 , Claudia M. Boot1,3 , Corey D. Broeckling4, Jill S. Baron1,5 , Biogeochemistry of Natural 1,6 Organic Matter and Ed K. Hall 1Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, CO, USA, 2Rocky Mountain Research 3 Key Points: Station, U.S. Forest Service, Fort Collins, CO, USA, Department of Chemistry, Colorado State University, Fort Collins, • Both glaciers and rock glaciers CO, USA, 4Proteomics and Metabolomics Facility, Colorado State University, Fort Collins, CO, USA, 5U.S. Geological supply highly bioavailable sources of Survey, Reston, VA, USA, 6Department of Ecosystem Science and Sustainability, Colorado State University, Fort Collins, organic matter to alpine headwaters CO, USA in Colorado • Bioavailability of organic matter released from glaciers is greater than that of rock glaciers in the Rocky Abstract As glaciers thaw in response to warming, they release dissolved organic matter (DOM) to Mountains alpine lakes and streams. The United States contains an abundance of both alpine glaciers and rock • ‐ The use of GC MS for ecosystem glaciers. Differences in DOM composition and bioavailability between glacier types, like rock and ice metabolomics represents a novel approach for examining complex glaciers, remain undefined. To assess differences in glacier and rock glacier DOM we evaluated organic matter pools bioavailability and molecular composition of DOM from four alpine catchments each with a glacier and a rock glacier at their headwaters. We assessed bioavailability of DOM by incubating each DOM source Supporting Information: with a common microbial community and evaluated chemical characteristics of DOM before and after • Supporting Information S1 • Data Set S1 incubation using untargeted gas chromatography–mass spectrometry‐based metabolomics. -
Photosynthetic Reaction Centre of Chloroflexus Aurantiacus
Volume 232, number 2, 364-368 FEB 05888 May 1988 Photosynthetic reaction centre of Chloroflexus aurantiacus Primary structure of M-subunit Yu.A. Ovchinnikovt, N.G. Abdulaev, B.E. Shmuckler, A.A. Zargarov, M.A. Kutuzov, I.N. Telezhinskaya, N.B. Levina and A.S. Zolotarev Shemyakin Institute of Bioorganic Chemistry, USSR Academy of Sciences, ul. Miklukho-Maklaya 16110, 117871 GSP Moscow V-437, USSR Received 24 March 1988 The M-subunit primary structure of the reaction centre (RC) from ChloroJexus auruntiacus composed of 306 amino acid residues has been determined by parallel analysis of the protein and corresponding DNA. The blocked N-terminus as well as replacement of the essential histidine liganding Mg of an accessory bacteriochlorophyll in purple bacteria by leucine distinguishes the M-subunit of Chloroflexus RC from that of purple bacteria. Photosynthesis; Reaction center; Subunit structure; Amino acid sequence; Nucleotide sequence; (Chloroflexus aurantiacus) 1. INTRODUCTION Chloroflexus RC to be homologous to the M- subunit of the purple bacteria. This paper presents The reaction centre (RC) is a protein-pigment the primary structure and tentative folding of the complex where the primary events of light energy polypeptide chain of the Chloroflexus RC M- conversion into chemical energy occur. The reac- subunit. tion centre of filamentous green bacterium Chloroflexus aurantiacus, the smallest RC known 2. MATERIALS AND METHODS today, consists of two protein subunits [l]. The primary structure of one subunit has been recently Experimental procedures applied for separation of highly determined in this laboratory by parallel analysis purified preparation of Chlorofexus RC, cleavage of the pro- of the protein and corresponding DNA [2].