A Comprehensive Survey of Soil Acidobacterial Diversity Using Pyrosequencing and Clone Library Analyses
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Genomic Analysis of Family UBA6911 (Group 18 Acidobacteria)
bioRxiv preprint doi: https://doi.org/10.1101/2021.04.09.439258; this version posted April 10, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.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 4.0 International license. 1 2 Genomic analysis of family UBA6911 (Group 18 3 Acidobacteria) expands the metabolic capacities of the 4 phylum and highlights adaptations to terrestrial habitats. 5 6 Archana Yadav1, Jenna C. Borrelli1, Mostafa S. Elshahed1, and Noha H. Youssef1* 7 8 1Department of Microbiology and Molecular Genetics, Oklahoma State University, Stillwater, 9 OK 10 *Correspondence: Noha H. Youssef: [email protected] bioRxiv preprint doi: https://doi.org/10.1101/2021.04.09.439258; this version posted April 10, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.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 4.0 International license. 11 Abstract 12 Approaches for recovering and analyzing genomes belonging to novel, hitherto unexplored 13 bacterial lineages have provided invaluable insights into the metabolic capabilities and 14 ecological roles of yet-uncultured taxa. The phylum Acidobacteria is one of the most prevalent 15 and ecologically successful lineages on earth yet, currently, multiple lineages within this phylum 16 remain unexplored. Here, we utilize genomes recovered from Zodletone spring, an anaerobic 17 sulfide and sulfur-rich spring in southwestern Oklahoma, as well as from multiple disparate soil 18 and non-soil habitats, to examine the metabolic capabilities and ecological role of members of 19 the family UBA6911 (group18) Acidobacteria. -
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 -
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. -
Supplementary Material 16S Rrna Clone Library
Kip et al. Biogeosciences (bg-2011-334) Supplementary Material 16S rRNA clone library To investigate the total bacterial community a clone library based on the 16S rRNA gene was performed of the pool Sphagnum mosses from Andorra peat, next to S. magellanicum some S. falcatulum was present in this pool and both these species were analysed. Both 16S clone libraries showed the presence of Alphaproteobacteria (17%), Verrucomicrobia (13%) and Gammaproteobacteria (2%) and since the distribution of bacterial genera among the two species was comparable an average was made. In total a 180 clones were sequenced and analyzed for the phylogenetic trees see Fig. A1 and A2 The 16S clone libraries showed a very diverse set of bacteria to be present inside or on Sphagnum mosses. Compared to other studies the microbial community in Sphagnum peat soils (Dedysh et al., 2006; Kulichevskaya et al., 2007a; Opelt and Berg, 2004) is comparable to the microbial community found here, inside and attached on the Sphagnum mosses of the Patagonian peatlands. Most of the clones showed sequence similarity to isolates or environmental samples originating from peat ecosystems, of which most of them originate from Siberian acidic peat bogs. This indicated that similar bacterial communities can be found in peatlands in the Northern and Southern hemisphere implying there is no big geographical difference in microbial diversity in peat bogs. Four out of five classes of Proteobacteria were present in the 16S rRNA clone library; Alfa-, Beta-, Gamma and Deltaproteobacteria. 42 % of the clones belonging to the Alphaproteobacteria showed a 96-97% to Acidophaera rubrifaciens, a member of the Rhodospirullales an acidophilic bacteriochlorophyll-producing bacterium isolated from acidic hotsprings and mine drainage (Hiraishi et al., 2000). -
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. -
Glossary Animal Physiology
Limnology 1 Weisse - WS99/00 Glossary Limnology 1 Biological Zonation of a lentic System: Most organisms can be classified on the basis of their typical habitat. Benthos: The community of plants and animals that live permanently in or on the sea bottom. Littoral (intertidal zone): The trophogenic zone along the shore till the compensation depth where NPP occurs. It is rich in species diversity and number - especially algae and higher plants. • Epilittoral: Sedentary organisms of the shoreline; e.g. macrophytes, diatoms, etc. • Profundal: Depths of 180m and deeper. Limnion: Temperature related zonation of the open water body of lentic systems; i.e. summer stratification due to solar radiation produces several trophic zones - see also ecological aspects - depth zones. • Epilimnion: The upper warm and illuminated surface layer of a lake; narrower than the trophogenic zone. • Metalimnion: The transitional zone between epi- and hypolimnion; i.e. the zone of the thermocline. • Hypolimnion: The cool and poorly illuminated bottom layer of a lake, below the thermocline. Nekton: Pelagic animals that are active swimmers; i.e. most of the adult fishes. Pelagial: The environment of the open water of a lake, away from the bottom, and not in close proximity to the shoreline. It is Lower in species number and diversity than the benthos. The pelagial of rivers exhibits a directed and continuos flux (spatial relocation = amountH2O/cross-surface area). Plankton: Passively drifting or weakly swimming organisms in fresh waters; i.e. microscopic plants, eggs, larval stages of the nekton and benthos (such as phyto-plankton, zoo-plankton). • Neuston: The epipelagic zone few centimeters below the waterline; i.e. -
Edaphobacter Modestus Gen. Nov., Sp. Nov., and Edaphobacter Aggregans Sp
International Journal of Systematic and Evolutionary Microbiology (2008), 58, 1114–1122 DOI 10.1099/ijs.0.65303-0 Edaphobacter modestus gen. nov., sp. nov., and Edaphobacter aggregans sp. nov., acidobacteria isolated from alpine and forest soils Isabella H. Koch,1 Frederic Gich,1 Peter F. Dunfield2 and Jo¨rg Overmann1 Correspondence 1Bereich Mikrobiologie, Ludwig-Maximilians-Universita¨t Mu¨nchen, Maria-Ward-Str. 1a, Jo¨rg Overmann D-80638 Mu¨nchen, Germany [email protected] 2Institute of Geological and Nuclear Sciences, Wairakei Research Centre, Wairakei, Private Bag 2000, Taupo, New Zealand The phylum Acidobacteria is currently represented mostly by environmental 16S rRNA gene sequences, and the phylum so far contains only four species with validly published names, Holophaga foetida, Geothrix fermentans, Acidobacterium capsulatum and Terriglobus roseus.In the present study, two novel strains of acidobacteria were isolated. High-throughput enrichments were set up with the MicroDrop technique using an alpine calcareous soil sample and a mixture of polymeric carbon compounds supplemented with signal compounds. This approach yielded a novel, previously unknown acidobacterium, strain Jbg-1T. The second strain, Wbg-1T, was recovered from a co-culture with a methanotrophic bacterium established from calcareous forest soil. Both strains represent members of subdivision 1 of the phylum Acidobacteria and are closely related to each other (98.0 % 16S rRNA gene sequence similarity). At a sequence similarity of 93.8–94.7 %, strains Jbg-1T and Wbg-1T are only distantly related to the closest described relative, Terriglobus roseus KBS 63T, and accordingly are described as members of the novel genus Edaphobacter gen. -
Isolation of an Archaeon at the Prokaryote-Eukaryote Interface 3 4 Authors: 5 Hiroyuki Imachi1*, Masaru K
bioRxiv preprint doi: https://doi.org/10.1101/726976; this version posted August 8, 2019. 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 Title: 2 Isolation of an archaeon at the prokaryote-eukaryote interface 3 4 Authors: 5 Hiroyuki Imachi1*, Masaru K. Nobu2*, Nozomi Nakahara1,3, Yuki Morono4, Miyuki 6 Ogawara1, Yoshihiro Takaki1, Yoshinori Takano5, Katsuyuki Uematsu6, Tetsuro Ikuta7, 7 Motoo Ito4, Yohei Matsui8, Masayuki Miyazaki1, Kazuyoshi Murata9, Yumi Saito1, Sanae 8 Sakai1, Chihong Song9, Eiji Tasumi1, Yuko Yamanaka1, Takashi Yamaguchi3, Yoichi 9 Kamagata2, Hideyuki Tamaki2 and Ken Takai1 10 11 *These authors contributed equally to this work. 12 13 Affiliations: 14 1Institute for Extra-cutting-edge Science and Technology Avant-garde Research (X-star), 15 Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan 16 2Bioproduction Research Institute, National Institute of Advanced Industrial Science and 17 Technology (AIST), Tsukuba, Japan 18 3Department of Civil and Environmental Engineering, Nagaoka University of 19 Technology, Nagaoka, Japan 20 4Kochi Institute for Core Sample Research, X-star, JAMSTEC, Nankoku, Japan 21 5Biogeochemistry Program, Research Institute for Marine Resources Utilization, 22 JAMSTEC, Yokosuka, Japan 23 6Department of Marine and Earth Sciences, Marine Work Japan Ltd, Yokosuka, Japan 24 7Research Institute for Global Change, JAMSTEC, Yokosuka, Japan 25 8Research Institute for Marine Resources Utilization, JAMSTEC, Yokosuka, Japan 26 9National Institute for Physiological Sciences, Okazaki, Japan 27 28 Corresponding authors: 29 Hiroyuki Imachi, E-mail: [email protected] 30 Masaru K. Nobu, E-mail: [email protected] 31 32 33 1 bioRxiv preprint doi: https://doi.org/10.1101/726976; this version posted August 8, 2019. -
Novel Phosphate-Solubilizing Bacteria Enhance Soil Phosphorus Cycling Following Ecological Restoration of Land Degraded by Mining
The ISME Journal (2020) 14:1600–1613 https://doi.org/10.1038/s41396-020-0632-4 ARTICLE Novel phosphate-solubilizing bacteria enhance soil phosphorus cycling following ecological restoration of land degraded by mining 1 2 1 2 2 2 2 Jie-Liang Liang ● Jun Liu ● Pu Jia ● Tao-tao Yang ● Qing-wei Zeng ● Sheng-chang Zhang ● Bin Liao ● 1 1,2 Wen-sheng Shu ● Jin-tian Li Received: 22 October 2019 / Revised: 2 March 2020 / Accepted: 10 March 2020 / Published online: 23 March 2020 © The Author(s) 2020. This article is published with open access Abstract Little is known about the changes in soil microbial phosphorus (P) cycling potential during terrestrial ecosystem management and restoration, although much research aims to enhance soil P cycling. Here, we used metagenomic sequencing to analyse 18 soil microbial communities at a P-deficient degraded mine site in southern China where ecological restoration was implemented using two soil ameliorants and eight plant species. Our results show that the relative abundances of key genes governing soil microbial P-cycling potential were higher at the restored site than at the unrestored site, indicating enhancement of soil P cycling following restoration. The gcd gene, encoding an enzyme that mediates inorganic P solubilization, was 1234567890();,: 1234567890();,: predominant across soil samples and was a major determinant of bioavailable soil P. We reconstructed 39 near-complete bacterial genomes harboring gcd, which represented diverse novel phosphate-solubilizing microbial taxa. Strong correlations were found between the relative abundance of these genomes and bioavailable soil P, suggesting their contributions to the enhancement of soil P cycling. -
Chapter 4: PROKARYOTIC DIVERSITY
Chapter 4: PROKARYOTIC DIVERSITY 1. Prokaryote Habitats, Relationships & Biomes 2. Proteobacteria 3. Gram-negative and Phototropic Non-Proteobacteria 4. Gram-Positive Bacteria 5. Deeply Branching Bacteria 6. Archaea 1. Prokaryote Habitats, Relationships & Biomes Important Metabolic Terminology Oxygen tolerance/usage: aerobic – requires or can use oxygen (O2) anaerobic – does not require or cannot tolerate O2 Energy usage: phototroph – uses light as an energy source • all photosynthetic organisms chemotroph – acquires energy from organic or inorganic molecules • organotrophs – get energy from organic molecules • lithotrophs – get energy from inorganic molecules …more Important Terminology Carbon Source: autotroph – uses CO2 as a carbon source • e.g., photoautotrophs or chemoautotrophs heterotroph – requires an organic carbon source • e.g., chemoheterotroph – gets energy & carbon from organic molecules Oligotrophs require few nutrients, the opposite of eutrophs or copiotrophs Facultative vs Obligate (or Strict): facultative – “able to, but not requiring” • e.g., facultative anaerobes can survive w/ or w/o O2 obligate – “absolutely requires” • e.g., obligate anaerobes cannot survive in O2 Symbiotic Relationships Symbiotic relationships (close, direct interactions) between different organisms in nature are of several types: • e.g., humans have beneficial bacteria in their digestive tracts that also benefit from the food we eat (mutualism) Microbiomes All the microorganisms that inhabit a particular organism or environment (e.g., human or -
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. -
Archaea;Crenarchaeota;Marine;Other;Other Archaea;Crenarchaeota;Miscellaneous;Other;Other Archaea;Crenarchaeota;Soil;Other;Other
Archaea;Crenarchaeota;Marine;Other;Other Archaea;Crenarchaeota;Miscellaneous;Other;Other Archaea;Crenarchaeota;Soil;Other;Other Archaea;Crenarchaeota;South;Other;Other Archaea;Crenarchaeota;terrestrial;Other;Other Archaea;Euryarchaeota;Halobacteria;Halobacteriales;Miscellaneous Archaea;Euryarchaeota;Methanobacteria;Methanobacteriales;Methanobacteriaceae Archaea;Euryarchaeota;Methanomicrobia;Methanocellales;Methanocellaceae Archaea;Euryarchaeota;Methanomicrobia;Methanosarcinales;Methanosarcinaceae Archaea;Euryarchaeota;Thermoplasmata;Thermoplasmatales;Marine Bacteria;Acidobacteria;Acidobacteria;11-24;uncultured Bacteria;Acidobacteria;Acidobacteria;Acidobacteriales;Acidobacteriaceae Bacteria;Acidobacteria;Acidobacteria;BPC102;uncultured Bacteria;Acidobacteria;Acidobacteria;Bryobacter;uncultured Bacteria;Acidobacteria;Acidobacteria;Candidatus;Other Bacteria;Acidobacteria;Acidobacteria;DA023;uncultured Bacteria;Acidobacteria;Acidobacteria;DA023;unidentified Bacteria;Acidobacteria;Acidobacteria;DS-100;uncultured Bacteria;Acidobacteria;Acidobacteria;PAUC26f;uncultured Bacteria;Acidobacteria;Acidobacteria;RB41;uncultured Bacteria;Acidobacteria;Holophagae;32-20;uncultured Bacteria;Acidobacteria;Holophagae;43F-1404R;uncultured Bacteria;Acidobacteria;Holophagae;Holophagales;Holophagaceae Bacteria;Acidobacteria;Holophagae;NS72;uncultured Bacteria;Acidobacteria;Holophagae;SJA-36;uncultured Bacteria;Acidobacteria;Holophagae;Sva0725;uncultured Bacteria;Acidobacteria;Holophagae;iii1-8;uncultured Bacteria;Acidobacteria;RB25;uncultured;Other Bacteria;Actinobacteria;Actinobacteria;Actinobacteridae;Actinomycetales