Genomic Analysis of Family UBA6911 (Group 18 Acidobacteria)
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Draft Genome Sequence of Acidobacteria Group 1 Acidipila Sp
GENOME SEQUENCES crossm Draft Genome Sequence of Acidobacteria Group 1 Acidipila sp. Strain EB88, Isolated from Forest Soil Luiz A. Domeignoz-Horta,a Kristen M. DeAngelis,a Grace Poldb aDepartment of Microbiology, University of Massachusetts, Amherst, Massachusetts, USA bGraduate Program in Organismic and Evolutionary Biology, University of Massachusetts, Amherst, Massachusetts, USA ABSTRACT Here, we present the genome sequence of a member of the group I Acidobacteria, Acidipila sp. strain EB88, which was isolated from temperate forest soil. Like many other members of its class, its genome contains evidence of the potential to utilize a broad range of sugars. roup I Acidobacteria are abundant members of acidic-soil microbial communities G(1), typically characterized by slow growth, heterotrophy, and the production of copious extracellular polysaccharides (2). Within this group, members of the genus Acidipila are characterized as acidophilic heterotrophs that use sugars as favored growth substrates (3, 4). Acidipila sp. strain EB88 was isolated from the Ͻ0.8-m size fraction of a deciduous forest mineral soil slurry plated onto VL45 plus glucose-yeast extract (GYE) medium (5). It was selected for sequencing based on the paucity of cultivated group I Acidobacteria, its peculiar bright-red waxy colonies on solid medium, and its undetectable growth in liquid medium unless a solid substrate, such as sand, is added. DNA was prepared for sequencing by repeatedly freeze-thawing 9-day-old biomass scraped from pH 5 R2A medium and extracted using the Qiagen genomic DNA protocol. Sequencing at UMass Worcester using the PacBio RS II sequencer resulted in 476,266 filtered reads, with a mean length of 3,208 bp. -
Novel Bacterial Lineages Associated with Boreal Moss Species Hannah
bioRxiv preprint doi: https://doi.org/10.1101/219659; this version posted November 16, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 1 Novel bacterial lineages associated with boreal moss species 2 Hannah Holland-Moritz1,2*, Julia Stuart3, Lily R. Lewis4, Samantha Miller3, Michelle C. Mack3, Stuart 3 F. McDaniel4, Noah Fierer1,2* 4 Affiliations: 5 1Cooperative Institute for Research in Environmental Sciences, University of Colorado at Boulder, 6 Boulder, CO, USA 7 2Department of Ecology and Evolutionary Biology, University of Colorado at Boulder, Boulder, CO, 8 USA 9 3Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ USA 10 4Department of Biology, University of Florida, Gainesville, FL 32611-8525, USA 11 *Corresponding Author 12 13 Abstract 14 Mosses are critical components of boreal ecosystems where they typically account for a large 15 proportion of net primary productivity and harbor diverse bacterial communities that can be the major 16 source of biologically-fixed nitrogen in these ecosystems. Despite their ecological importance, we have 17 limited understanding of how microbial communities vary across boreal moss species and the extent to 18 which local environmental conditions may influence the composition of these bacterial communities. 19 We used marker gene sequencing to analyze bacterial communities associated with eight boreal moss 20 species collected near Fairbanks, AK USA. We found that host identity was more important than site in 21 determining bacterial community composition and that mosses harbor diverse lineages of potential N2- 22 fixers as well as an abundance of novel taxa assigned to understudied bacterial phyla (including 23 candidate phylum WPS-2). -
Global Metagenomic Survey Reveals a New Bacterial Candidate Phylum in Geothermal Springs
ARTICLE Received 13 Aug 2015 | Accepted 7 Dec 2015 | Published 27 Jan 2016 DOI: 10.1038/ncomms10476 OPEN Global metagenomic survey reveals a new bacterial candidate phylum in geothermal springs Emiley A. Eloe-Fadrosh1, David Paez-Espino1, Jessica Jarett1, Peter F. Dunfield2, Brian P. Hedlund3, Anne E. Dekas4, Stephen E. Grasby5, Allyson L. Brady6, Hailiang Dong7, Brandon R. Briggs8, Wen-Jun Li9, Danielle Goudeau1, Rex Malmstrom1, Amrita Pati1, Jennifer Pett-Ridge4, Edward M. Rubin1,10, Tanja Woyke1, Nikos C. Kyrpides1 & Natalia N. Ivanova1 Analysis of the increasing wealth of metagenomic data collected from diverse environments can lead to the discovery of novel branches on the tree of life. Here we analyse 5.2 Tb of metagenomic data collected globally to discover a novel bacterial phylum (‘Candidatus Kryptonia’) found exclusively in high-temperature pH-neutral geothermal springs. This lineage had remained hidden as a taxonomic ‘blind spot’ because of mismatches in the primers commonly used for ribosomal gene surveys. Genome reconstruction from metagenomic data combined with single-cell genomics results in several high-quality genomes representing four genera from the new phylum. Metabolic reconstruction indicates a heterotrophic lifestyle with conspicuous nutritional deficiencies, suggesting the need for metabolic complementarity with other microbes. Co-occurrence patterns identifies a number of putative partners, including an uncultured Armatimonadetes lineage. The discovery of Kryptonia within previously studied geothermal springs underscores the importance of globally sampled metagenomic data in detection of microbial novelty, and highlights the extraordinary diversity of microbial life still awaiting discovery. 1 Department of Energy Joint Genome Institute, Walnut Creek, California 94598, USA. 2 Department of Biological Sciences, University of Calgary, Calgary, Alberta T2N 1N4, Canada. -
Table S4. Phylogenetic Distribution of Bacterial and Archaea Genomes in Groups A, B, C, D, and X
Table S4. Phylogenetic distribution of bacterial and archaea genomes in groups A, B, C, D, and X. Group A a: Total number of genomes in the taxon b: Number of group A genomes in the taxon c: Percentage of group A genomes in the taxon a b c cellular organisms 5007 2974 59.4 |__ Bacteria 4769 2935 61.5 | |__ Proteobacteria 1854 1570 84.7 | | |__ Gammaproteobacteria 711 631 88.7 | | | |__ Enterobacterales 112 97 86.6 | | | | |__ Enterobacteriaceae 41 32 78.0 | | | | | |__ unclassified Enterobacteriaceae 13 7 53.8 | | | | |__ Erwiniaceae 30 28 93.3 | | | | | |__ Erwinia 10 10 100.0 | | | | | |__ Buchnera 8 8 100.0 | | | | | | |__ Buchnera aphidicola 8 8 100.0 | | | | | |__ Pantoea 8 8 100.0 | | | | |__ Yersiniaceae 14 14 100.0 | | | | | |__ Serratia 8 8 100.0 | | | | |__ Morganellaceae 13 10 76.9 | | | | |__ Pectobacteriaceae 8 8 100.0 | | | |__ Alteromonadales 94 94 100.0 | | | | |__ Alteromonadaceae 34 34 100.0 | | | | | |__ Marinobacter 12 12 100.0 | | | | |__ Shewanellaceae 17 17 100.0 | | | | | |__ Shewanella 17 17 100.0 | | | | |__ Pseudoalteromonadaceae 16 16 100.0 | | | | | |__ Pseudoalteromonas 15 15 100.0 | | | | |__ Idiomarinaceae 9 9 100.0 | | | | | |__ Idiomarina 9 9 100.0 | | | | |__ Colwelliaceae 6 6 100.0 | | | |__ Pseudomonadales 81 81 100.0 | | | | |__ Moraxellaceae 41 41 100.0 | | | | | |__ Acinetobacter 25 25 100.0 | | | | | |__ Psychrobacter 8 8 100.0 | | | | | |__ Moraxella 6 6 100.0 | | | | |__ Pseudomonadaceae 40 40 100.0 | | | | | |__ Pseudomonas 38 38 100.0 | | | |__ Oceanospirillales 73 72 98.6 | | | | |__ Oceanospirillaceae -
Coupled Reductive and Oxidative Sulfur Cycling in the Phototrophic Plate of a Meromictic Lake T
Geobiology (2014), 12, 451–468 DOI: 10.1111/gbi.12092 Coupled reductive and oxidative sulfur cycling in the phototrophic plate of a meromictic lake T. L. HAMILTON,1 R. J. BOVEE,2 V. THIEL,3 S. R. SATTIN,2 W. MOHR,2 I. SCHAPERDOTH,1 K. VOGL,3 W. P. GILHOOLY III,4 T. W. LYONS,5 L. P. TOMSHO,3 S. C. SCHUSTER,3,6 J. OVERMANN,7 D. A. BRYANT,3,6,8 A. PEARSON2 AND J. L. MACALADY1 1Department of Geosciences, Penn State Astrobiology Research Center (PSARC), The Pennsylvania State University, University Park, PA, USA 2Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA 3Department of Biochemistry and Molecular Biology, The Pennsylvania State University, University Park, PA, USA 4Department of Earth Sciences, Indiana University-Purdue University Indianapolis, Indianapolis, IN, USA 5Department of Earth Sciences, University of California, Riverside, CA, USA 6Singapore Center for Environmental Life Sciences Engineering, Nanyang Technological University, Nanyang, Singapore 7Leibniz-Institut DSMZ-Deutsche Sammlung von Mikroorganismen und Zellkulturen, Braunschweig, Germany 8Department of Chemistry and Biochemistry, Montana State University, Bozeman, MT, USA ABSTRACT Mahoney Lake represents an extreme meromictic model system and is a valuable site for examining the organisms and processes that sustain photic zone euxinia (PZE). A single population of purple sulfur bacte- ria (PSB) living in a dense phototrophic plate in the chemocline is responsible for most of the primary pro- duction in Mahoney Lake. Here, we present metagenomic data from this phototrophic plate – including the genome of the major PSB, as obtained from both a highly enriched culture and from the metagenomic data – as well as evidence for multiple other taxa that contribute to the oxidative sulfur cycle and to sulfate reduction. -
Yu-Chen Ling and John W. Moreau
Microbial Distribution and Activity in a Coastal Acid Sulfate Soil System Introduction: Bioremediation in Yu-Chen Ling and John W. Moreau coastal acid sulfate soil systems Method A Coastal acid sulfate soil (CASS) systems were School of Earth Sciences, University of Melbourne, Melbourne, VIC 3010, Australia formed when people drained the coastal area Microbial distribution controlled by environmental parameters Microbial activity showed two patterns exposing the soil to the air. Drainage makes iron Microbial structures can be grouped into three zones based on the highest similarity between samples (Fig. 4). Abundant populations, such as Deltaproteobacteria, kept constant activity across tidal cycling, whereas rare sulfides oxidize and release acidity to the These three zones were consistent with their geological background (Fig. 5). Zone 1: Organic horizon, had the populations changed activity response to environmental variations. Activity = cDNA/DNA environment, low pH pore water further dissolved lowest pH value. Zone 2: surface tidal zone, was influenced the most by tidal activity. Zone 3: Sulfuric zone, Abundant populations: the heavy metals. The acidity and toxic metals then Method A Deltaproteobacteria Deltaproteobacteria this area got neutralized the most. contaminate coastal and nearby ecosystems and Method B 1.5 cause environmental problems, such as fish kills, 1.5 decreased rice yields, release of greenhouse gases, Chloroflexi and construction damage. In Australia, there is Gammaproteobacteria Gammaproteobacteria about a $10 billion “legacy” from acid sulfate soils, Chloroflexi even though Australia is only occupied by around 1.0 1.0 Cyanobacteria,@ Acidobacteria Acidobacteria Alphaproteobacteria 18% of the global acid sulfate soils. Chloroplast Zetaproteobacteria Rare populations: Alphaproteobacteria Method A log(RNA(%)+1) Zetaproteobacteria log(RNA(%)+1) Method C Method B 0.5 0.5 Cyanobacteria,@ Bacteroidetes Chloroplast Firmicutes Firmicutes Bacteroidetes Planctomycetes Planctomycetes Ac8nobacteria Fig. -
MIAMI UNIVERSITY the Graduate School Certificate for Approving The
MIAMI UNIVERSITY The Graduate School Certificate for Approving the Dissertation We hereby approve the Dissertation of Qiuyuan Huang Candidate for the Degree: Doctor of Philosophy _______________________________________ Hailiang Dong, Director ________________________________________ Yildirim Dilek, Reader ________________________________________ Jonathan Levy, Reader ______________________________________ Chuanlun Zhang, External examiner ______________________________________ Annette Bollmann, Graduate School Representative ABSTRACT GEOMICROBIAL INVESTIGATIONS ON EXTREME ENVIRONMENTS: LINKING GEOCHEMISTRY TO MICROBIAL ECOLOGY IN TERRESTRIAL HOT SPRINGS AND SALINE LAKES by Qiuyuan Huang Terrestrial hot springs and saline lakes represent two extreme environments for microbial life and constitute an important part of global ecosystems that affect the biogeochemical cycling of life-essential elements. Despite the advances in our understanding of microbial ecology in the past decade, important questions remain regarding the link between microbial diversity and geochemical factors under these extreme conditions. This dissertation first investigates a series of hot springs with wide ranges of temperature (26-92oC) and pH (3.72-8.2) from the Tibetan Plateau in China and the Philippines. Within each region, microbial diversity and geochemical conditions were studied using an integrated approach with 16S rRNA molecular phylogeny and a suite of geochemical analyses. In Tibetan springs, the microbial community was dominated by archaeal phylum Thaumarchaeota -
Archaeal Distribution and Abundance in Water Masses of the Arctic Ocean, Pacific Sector
Vol. 69: 101–112, 2013 AQUATIC MICROBIAL ECOLOGY Published online April 30 doi: 10.3354/ame01624 Aquat Microb Ecol FREEREE ACCESSCCESS Archaeal distribution and abundance in water masses of the Arctic Ocean, Pacific sector Chie Amano-Sato1, Shohei Akiyama1, Masao Uchida2, Koji Shimada3, Motoo Utsumi1,* 1University of Tsukuba, Tennodai, Tsukuba, Ibaraki 305-8572, Japan 2National Institute for Environmental Studies, Onogawa, Tsukuba, Ibaraki 305-8506, Japan 3Tokyo University of Marine Science and Technology, Konan, Minato-ku, Tokyo 108-8477, Japan ABSTRACT: Marine planktonic Archaea have been recently recognized as an ecologically impor- tant component of marine prokaryotic biomass in the world’s oceans. Their abundance and meta- bolism are closely connected with marine geochemical cycling. We evaluated the distribution of planktonic Archaea in the Pacific sector of the Arctic Ocean using fluorescence in situ hybridiza- tion (FISH) with catalyzed reporter deposition (CARD-FISH) and performed statistical analyses using data for archaeal abundance and geochemical variables. The relative abundance of Thaum - archaeota generally increased with depth, and euryarchaeal abundance was the lowest of all planktonic prokaryotes. Multiple regression analysis showed that the thaumarchaeal relative abundance was negatively correlated with ammonium and dissolved oxygen concentrations and chlorophyll fluorescence. Canonical correspondence analysis showed that archaeal distributions differed with oceanographic water masses; in particular, Thaumarchaeota were abundant from the halocline layer to deep water, where salinity was higher and most nutrients were depleted. However, at several stations on the East Siberian Sea side of the study area and along the North- wind Ridge, Thaumarchaeota and Bacteria were proportionally very abundant at the bottom in association with higher nutrient conditions. -
Insights Into Archaeal Evolution and Symbiosis from the Genomes of a Nanoarchaeon and Its Inferred Crenarchaeal Host from Obsidian Pool, Yellowstone National Park
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Microbiology Publications and Other Works Microbiology 4-22-2013 Insights into archaeal evolution and symbiosis from the genomes of a nanoarchaeon and its inferred crenarchaeal host from Obsidian Pool, Yellowstone National Park Mircea Podar University of Tennessee - Knoxville, [email protected] Kira S. Makarova National Institutes of Health David E. Graham University of Tennessee - Knoxville, [email protected] Yuri I. Wolf National Institutes of Health Eugene V. Koonin National Institutes of Health See next page for additional authors Follow this and additional works at: https://trace.tennessee.edu/utk_micrpubs Part of the Microbiology Commons Recommended Citation Biology Direct 2013, 8:9 doi:10.1186/1745-6150-8-9 This Article is brought to you for free and open access by the Microbiology at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Microbiology Publications and Other Works by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. Authors Mircea Podar, Kira S. Makarova, David E. Graham, Yuri I. Wolf, Eugene V. Koonin, and Anna-Louise Reysenbach This article is available at TRACE: Tennessee Research and Creative Exchange: https://trace.tennessee.edu/ utk_micrpubs/44 Podar et al. Biology Direct 2013, 8:9 http://www.biology-direct.com/content/8/1/9 RESEARCH Open Access Insights into archaeal evolution and symbiosis from the genomes of a nanoarchaeon and its inferred crenarchaeal host from Obsidian Pool, Yellowstone National Park Mircea Podar1,2*, Kira S Makarova3, David E Graham1,2, Yuri I Wolf3, Eugene V Koonin3 and Anna-Louise Reysenbach4 Abstract Background: A single cultured marine organism, Nanoarchaeum equitans, represents the Nanoarchaeota branch of symbiotic Archaea, with a highly reduced genome and unusual features such as multiple split genes. -
Oceans of Archaea Abundant Oceanic Crenarchaeota Appear to Derive from Thermophilic Ancestors That Invaded Low-Temperature Marine Environments
Oceans of Archaea Abundant oceanic Crenarchaeota appear to derive from thermophilic ancestors that invaded low-temperature marine environments Edward F. DeLong arth’s microbiota is remarkably per- karyotes), Archaea, and Bacteria. Although al- vasive, thriving at extremely high ternative taxonomic schemes have been recently temperature, low and high pH, high proposed, whole-genome and other analyses E salinity, and low water availability. tend to support Woese’s three-domain concept. One lineage of microbial life in par- Well-known and cultivated archaea generally ticular, the Archaea, is especially adept at ex- fall into several major phenotypic groupings: ploiting environmental extremes. Despite their these include extreme halophiles, methanogens, success in these challenging habitats, the Ar- and extreme thermophiles and thermoacido- chaea may now also be viewed as a philes. Early on, extremely halo- cosmopolitan lot. These microbes philic archaea (haloarchaea) were exist in a wide variety of terres- first noticed as bright-red colonies trial, freshwater, and marine habi- Archaea exist in growing on salted fish or hides. tats, sometimes in very high abun- a wide variety For many years, halophilic isolates dance. The oceanic Marine Group of terrestrial, from salterns, salt deposits, and I Crenarchaeota, for example, ri- freshwater, and landlocked seas provided excellent val total bacterial biomass in wa- marine habitats, model systems for studying adap- ters below 100 m. These wide- tations to high salinity. It was only spread Archaea appear to derive sometimes in much later, however, that it was from thermophilic ancestors that very high realized that these salt-loving invaded diverse low-temperature abundance “bacteria” are actually members environments. -
Open Thweattetd1.Pdf
The Pennsylvania State University The Graduate School CHARACTERIZATION OF PIGMENT BIOSYNTHESIS AND LIGHT-HARVESTING COMPLEXES OF SELECTED ANOXYGENIC PHOTOTROPHIC BACTERIA A Dissertation in Biochemistry, Microbiology, and Molecular Biology and Astrobiology by Jennifer L. Thweatt 2019 Jennifer L. Thweatt Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy December 2019 ii The dissertation of Jennifer L. Thweatt was reviewed and approved* by the following: Donald A. Bryant Ernest C. Pollard Professor in Biotechnology and Professor of Biochemistry and Molecular Biology Dissertation Advisor Chair of Committee Squire J. Booker Howard Hughes Medical Investigator Professor of Chemistry and Professor of Biochemistry and Molecular Biology Eberly Distinguished Chair in Science John H. Golbeck Professor of Biochemistry and Biophysics Professor of Chemistry Jennifer L. Macalady Associate Professor of Geosciences Timothy I. Miyashiro Assistant Professor of Biochemistry and Molecular Biology Wendy Hanna-Rose Professor of Biochemistry and Molecular Biology Department Head, Biochemistry and Molecular Biology *Signatures are on file in the Graduate School iii ABSTRACT This dissertation describes work on pigment biosynthesis and the light-harvesting apparatus of two classes of anoxygenic phototrophic bacteria, namely the green bacteria and a newly isolated purple sulfur bacterium. Green bacteria are introduced in Chapter 1 and include chlorophototrophic members of the phyla Chlorobi, Chloroflexi, and Acidobacteria. The green bacteria are defined by their use of chlorosomes for light harvesting. Chlorosomes contain thousands of unique chlorin molecules, known as bacteriochlorophyll (BChl) c, d, e, or f, which are arranged in supramolecular aggregates. Additionally, all green bacteria can synthesize BChl a, the and green members of the phyla Chlorobi and Acidobacteria can synthesize chlorophyll (Chl) a. -
Supplementary Material the Metallochaperone Encoding Gene Hypa Is Widely Distributed Among Pathogenic Aeromonas Spp
Supplementary material The Metallochaperone Encoding Gene hypA Is Widely Distributed among Pathogenic Aeromonas spp. and Its Expression Is Increased under Acidic pH and within Macrophages. Ana Fernández-Bravo, Loida López-Fernández*, Maria José Figueras*. Unit of Microbiology, Department of Basic Health Sciences, Faculty of Medicine and Health Sciences, IISPV, University Rovira i Virgili, Reus, Spain. *Correspondence: Dr. Maria José Figueras, [email protected]; Dr. Loida López-Fernández, [email protected] Figure S1. Phylogenetic tree constructed with 25 species of Aeromonas based on sequences of the protein HypA by the Maximum- Likelihood algorithm (model JTT+G). Numbers at nodes denote the level of bootstrap based on 1000 replicates; only values greater than 50% are shown. Scale bar, base substitutions per site. 1 Table S1. Genetic analyses and diversity of hypA presence at strain-level in 143 genomes from 36 different species from the genus Aeromonas. T indicates type strain. Accesion number HypA Rate of hypA Species Strain Identified (NCBI) (genome) Re-identification Presence presence (%) CECT 4199 T A. allosaccharophila NZ_CDBR00000000.1 - Yes BVH88 A. allosaccharophila NZ_CDCB00000000.1 A. allosaccharophila Yes A. allosaccharophila 4/4 Z9-6 A. allosaccharophila NZ_NXBS00000000.1 A. allosaccharophila Yes (100) TTU2014- A. allosaccharophila NZ_CDCB00000000.1 A. allosaccharophila Yes 159ASC CECT 4227 T A. bestiarum NZ_CDDA00000000.1 - Yes A. bestiarum 2/2 CA23 Aeromonas sp. NZ_CP023818.1 A. bestiarum Yes 100 CECT 7113 T A. bivalvium NZ_CDBT00000000.1 - No ZJ19-2 A.bivalvium NZ_NXBQ00000000.1 A.bivalvium No 3/3 A. bivalvium 100 ZJ20-2 A.bivalvium NZ_NXBX00000000.1 A.bivalvium No CECT 838 T A.