Cellular Polyamine Catalogues of the Five Classes of the Phylum Proteobacteria: Distributions of Homospermidine Within the Class
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The 2014 Golden Gate National Parks Bioblitz - Data Management and the Event Species List Achieving a Quality Dataset from a Large Scale Event
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science The 2014 Golden Gate National Parks BioBlitz - Data Management and the Event Species List Achieving a Quality Dataset from a Large Scale Event Natural Resource Report NPS/GOGA/NRR—2016/1147 ON THIS PAGE Photograph of BioBlitz participants conducting data entry into iNaturalist. Photograph courtesy of the National Park Service. ON THE COVER Photograph of BioBlitz participants collecting aquatic species data in the Presidio of San Francisco. Photograph courtesy of National Park Service. The 2014 Golden Gate National Parks BioBlitz - Data Management and the Event Species List Achieving a Quality Dataset from a Large Scale Event Natural Resource Report NPS/GOGA/NRR—2016/1147 Elizabeth Edson1, Michelle O’Herron1, Alison Forrestel2, Daniel George3 1Golden Gate Parks Conservancy Building 201 Fort Mason San Francisco, CA 94129 2National Park Service. Golden Gate National Recreation Area Fort Cronkhite, Bldg. 1061 Sausalito, CA 94965 3National Park Service. San Francisco Bay Area Network Inventory & Monitoring Program Manager Fort Cronkhite, Bldg. 1063 Sausalito, CA 94965 March 2016 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service. -
Inactivation of CRISPR-Cas Systems by Anti-CRISPR Proteins in Diverse Bacterial Species April Pawluk1, Raymond H.J
LETTERS PUBLISHED: 13 JUNE 2016 | ARTICLE NUMBER: 16085 | DOI: 10.1038/NMICROBIOL.2016.85 Inactivation of CRISPR-Cas systems by anti-CRISPR proteins in diverse bacterial species April Pawluk1, Raymond H.J. Staals2, Corinda Taylor2, Bridget N.J. Watson2, Senjuti Saha3, Peter C. Fineran2, Karen L. Maxwell4* and Alan R. Davidson1,3* CRISPR-Cas systems provide sequence-specific adaptive immu- MGE-encoded mechanisms that inhibit CRISPR-Cas systems. In nity against foreign nucleic acids1,2. They are present in approxi- support of this hypothesis, phages infecting Pseudomonas aeruginosa mately half of all sequenced prokaryotes3 and are expected to were found to encode diverse families of proteins that inhibit constitute a major barrier to horizontal gene transfer. We pre- the CRISPR-Cas systems of their host through several distinct viously described nine distinct families of proteins encoded in mechanisms4,5,17,18. However, homologues of these anti-CRISPR Pseudomonas phage genomes that inhibit CRISPR-Cas function4,5. proteins were found only within the Pseudomonas genus. Here, We have developed a bioinformatic approach that enabled us to we describe a bioinformatic approach that allowed us to identify discover additional anti-CRISPR proteins encoded in phages five novel families of functional anti-CRISPR proteins encoded in and other mobile genetic elements of diverse bacterial phages and other putative MGEs in species spanning the diversity species. We show that five previously undiscovered families of Proteobacteria. of anti-CRISPRs inhibit the type I-F CRISPR-Cas systems of The nine previously characterized anti-CRISPR protein families both Pseudomonas aeruginosa and Pectobacterium atrosepticum, possess no common sequence motifs, so we used genomic context to and a dual specificity anti-CRISPR inactivates both type I-F search for novel anti-CRISPR genes. -
Table 1. Overview of Reactions Examined in This Study. ΔG Values Were Obtained from Thauer Et Al., 1977
Supplemental Information: Table 1. Overview of reactions examined in this study. ΔG values were obtained from Thauer et al., 1977. No. Equation ∆G°' (kJ/reaction)* Acetogenic reactions – – – + 1 Propionate + 3 H2O → Acetate + HCO3 + 3 H2 + H +76.1 Sulfate-reducing reactions – 2– – – – + 2 Propionate + 0.75 SO4 → Acetate + 0.75 HS + HCO3 + 0.25 H –37.8 2– + – 3 4 H2 + SO4 + H → HS + 4 H2O –151.9 – 2– – – 4 Acetate + SO4 → 2 HCO3 + HS –47.6 Methanogenic reactions – – + 5 4 H2 + HCO3 + H → CH4 + 3 H2O –135.6 – – 6 Acetate + H2O → CH4 + HCO3 –31.0 Syntrophic propionate conversion – – – + 1+5 Propionate + 0.75 H2O → Acetate + 0.75 CH4 + 0.25 HCO3 + 0.25 H –25.6 Complete propionate conversion by SRB – 2– – – + 2+4 Propionate + 1.75 SO4 → 1.75 HS + 3 HCO3 + 0.25 H –85.4 Complete propionate conversion by syntrophs and methanogens 1+5+6 Propionate– + 1.75 H O → 1.75 CH + 1.25 HCO – + 0.25 H+ –56.6 2 4 3 1 Table S2. Overview of all enrichment slurries fed with propionate and the total amounts of the reactants consumed and products formed during the enrichment period. The enrichment slurries consisted of sediment from either the sulfate zone (SZ), sulfate-methane transition zone (SMTZ) or methane zone (MZ) and were incubated at 25°C or 10°C, with 3 mM, 20 mM or without (-) sulfate amendments along the study. The slurries P1/P2, P3/P4, P5/P6, P7/P8 from each sediment zone are biological replicates. Slurries with * are presented in the propionate conversion graphs and used for molecular analysis. -
Detection of a Bacterial Group Within the Phylum Chloroflexi And
Microbes Environ. Vol. 21, No. 3, 154–162, 2006 http://wwwsoc.nii.ac.jp/jsme2/ Detection of a Bacterial Group within the Phylum Chloroflexi and Reductive-Dehalogenase-Homologous Genes in Pentachlorobenzene- Dechlorinating Estuarine Sediment from the Arakawa River, Japan KYOSUKE SANTOH1, ATSUSHI KOUZUMA1, RYOKO ISHIZEKI2, KENICHI IWATA1, MINORU SHIMURA3, TOSHIO HAYAKAWA3, TOSHIHIRO HOAKI4, HIDEAKI NOJIRI1, TOSHIO OMORI2, HISAKAZU YAMANE1 and HIROSHI HABE1*† 1 Biotechnology Research Center, The University of Tokyo, 1–1–1 Yayoi, Bunkyo-ku, Tokyo 113–8657, Japan 2 Department of Industrial Chemistry, Faculty of Engineering, Shibaura Institute of Technology, Minato-ku, Tokyo 108–8548, Japan 3 Environmental Biotechnology Laboratory, Railway Technical Research Institute, 2–8–38 Hikari-cho, Kokubunji-shi, Tokyo 185–8540, Japan 4 Technology Research Center, Taisei Corporation, 344–1 Nase, Totsuka-ku, Yokohama 245–0051, Japan (Received April 21, 2006—Accepted June 12, 2006) We enriched a pentachlorobenzene (pentaCB)-dechlorinating microbial consortium from an estuarine-sedi- ment sample obtained from the mouth of the Arakawa River. The sediment was incubated together with a mix- ture of four electron donors and pentaCB, and after five months of incubation, the microbial community structure was analyzed. Both DGGE and clone library analyses showed that the most expansive phylogenetic group within the consortium was affiliated with the phylum Chloroflexi, which includes Dehalococcoides-like bacteria. PCR using a degenerate primer set targeting conserved regions in reductive-dehalogenase-homologous (rdh) genes from Dehalococcoides species revealed that DNA fragments (approximately 1.5–1.7 kb) of rdh genes were am- plified from genomic DNA of the consortium. The deduced amino acid sequences of the rdh genes shared sever- al characteristics of reductive dehalogenases. -
(Batch Learning Self-Organizing Maps), to the Microbiome Analysis of Ticks
Title A novel approach, based on BLSOMs (Batch Learning Self-Organizing Maps), to the microbiome analysis of ticks Nakao, Ryo; Abe, Takashi; Nijhof, Ard M; Yamamoto, Seigo; Jongejan, Frans; Ikemura, Toshimichi; Sugimoto, Author(s) Chihiro The ISME Journal, 7(5), 1003-1015 Citation https://doi.org/10.1038/ismej.2012.171 Issue Date 2013-03 Doc URL http://hdl.handle.net/2115/53167 Type article (author version) File Information ISME_Nakao.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP A novel approach, based on BLSOMs (Batch Learning Self-Organizing Maps), to the microbiome analysis of ticks Ryo Nakao1,a, Takashi Abe2,3,a, Ard M. Nijhof4, Seigo Yamamoto5, Frans Jongejan6,7, Toshimichi Ikemura2, Chihiro Sugimoto1 1Division of Collaboration and Education, Research Center for Zoonosis Control, Hokkaido University, Kita-20, Nishi-10, Kita-ku, Sapporo, Hokkaido 001-0020, Japan 2Nagahama Institute of Bio-Science and Technology, Nagahama, Shiga 526-0829, Japan 3Graduate School of Science & Technology, Niigata University, 8050, Igarashi 2-no-cho, Nishi- ku, Niigata 950-2181, Japan 4Institute for Parasitology and Tropical Veterinary Medicine, Freie Universität Berlin, Königsweg 67, 14163 Berlin, Germany 5Miyazaki Prefectural Institute for Public Health and Environment, 2-3-2 Gakuen Kibanadai Nishi, Miyazaki 889-2155, Japan 6Utrecht Centre for Tick-borne Diseases (UCTD), Department of Infectious Diseases and Immunology, Faculty of Veterinary Medicine, Utrecht University, Yalelaan 1, 3584 CL Utrecht, The Netherlands 7Department of Veterinary Tropical Diseases, Faculty of Veterinary Science, University of Pretoria, Private Bag X04, 0110 Onderstepoort, South Africa aThese authors contributed equally to this work. Keywords: BLSOMs/emerging diseases/metagenomics/microbiomes/symbionts/ticks Running title: Tick microbiomes revealed by BLSOMs Subject category: Microbe-microbe and microbe-host interactions Abstract Ticks transmit a variety of viral, bacterial and protozoal pathogens, which are often zoonotic. -
Novel Bacterial Diversity in an Anchialine Blue Hole On
NOVEL BACTERIAL DIVERSITY IN AN ANCHIALINE BLUE HOLE ON ABACO ISLAND, BAHAMAS A Thesis by BRETT CHRISTOPHER GONZALEZ Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2010 Major Subject: Wildlife and Fisheries Sciences NOVEL BACTERIAL DIVERSITY IN AN ANCHIALINE BLUE HOLE ON ABACO ISLAND, BAHAMAS A Thesis by BRETT CHRISTOPHER GONZALEZ Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Approved by: Chair of Committee, Thomas Iliffe Committee Members, Robin Brinkmeyer Daniel Thornton Head of Department, Thomas Lacher, Jr. December 2010 Major Subject: Wildlife and Fisheries Sciences iii ABSTRACT Novel Bacterial Diversity in an Anchialine Blue Hole on Abaco Island, Bahamas. (December 2010) Brett Christopher Gonzalez, B.S., Texas A&M University at Galveston Chair of Advisory Committee: Dr. Thomas Iliffe Anchialine blue holes found in the interior of the Bahama Islands have distinct fresh and salt water layers, with vertical mixing, and dysoxic to anoxic conditions below the halocline. Scientific cave diving exploration and microbiological investigations of Cherokee Road Extension Blue Hole on Abaco Island have provided detailed information about the water chemistry of the vertically stratified water column. Hydrologic parameters measured suggest that circulation of seawater is occurring deep within the platform. Dense microbial assemblages which occurred as mats on the cave walls below the halocline were investigated through construction of 16S rRNA clone libraries, finding representatives across several bacterial lineages including Chlorobium and OP8. -
Geomicrobiological Processes in Extreme Environments: a Review
202 Articles by Hailiang Dong1, 2 and Bingsong Yu1,3 Geomicrobiological processes in extreme environments: A review 1 Geomicrobiology Laboratory, China University of Geosciences, Beijing, 100083, China. 2 Department of Geology, Miami University, Oxford, OH, 45056, USA. Email: [email protected] 3 School of Earth Sciences, China University of Geosciences, Beijing, 100083, China. The last decade has seen an extraordinary growth of and Mancinelli, 2001). These unique conditions have selected Geomicrobiology. Microorganisms have been studied in unique microorganisms and novel metabolic functions. Readers are directed to recent review papers (Kieft and Phelps, 1997; Pedersen, numerous extreme environments on Earth, ranging from 1997; Krumholz, 2000; Pedersen, 2000; Rothschild and crystalline rocks from the deep subsurface, ancient Mancinelli, 2001; Amend and Teske, 2005; Fredrickson and Balk- sedimentary rocks and hypersaline lakes, to dry deserts will, 2006). A recent study suggests the importance of pressure in the origination of life and biomolecules (Sharma et al., 2002). In and deep-ocean hydrothermal vent systems. In light of this short review and in light of some most recent developments, this recent progress, we review several currently active we focus on two specific aspects: novel metabolic functions and research frontiers: deep continental subsurface micro- energy sources. biology, microbial ecology in saline lakes, microbial Some metabolic functions of continental subsurface formation of dolomite, geomicrobiology in dry deserts, microorganisms fossil DNA and its use in recovery of paleoenviron- Because of the unique geochemical, hydrological, and geological mental conditions, and geomicrobiology of oceans. conditions of the deep subsurface, microorganisms from these envi- Throughout this article we emphasize geomicrobiological ronments are different from surface organisms in their metabolic processes in these extreme environments. -
Downloaded 13 April 2017); Using Diamond
bioRxiv preprint doi: https://doi.org/10.1101/347021; this version posted June 14, 2018. 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 2 3 4 5 Re-evaluating the salty divide: phylogenetic specificity of 6 transitions between marine and freshwater systems 7 8 9 10 Sara F. Pavera, Daniel J. Muratorea, Ryan J. Newtonb, Maureen L. Colemana# 11 a 12 Department of the Geophysical Sciences, University of Chicago, Chicago, Illinois, USA 13 b School of Freshwater Sciences, University of Wisconsin Milwaukee, Milwaukee, Wisconsin, USA 14 15 Running title: Marine-freshwater phylogenetic specificity 16 17 #Address correspondence to Maureen Coleman, [email protected] 18 bioRxiv preprint doi: https://doi.org/10.1101/347021; this version posted June 14, 2018. 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. 19 Abstract 20 Marine and freshwater microbial communities are phylogenetically distinct and transitions 21 between habitat types are thought to be infrequent. We compared the phylogenetic diversity of 22 marine and freshwater microorganisms and identified specific lineages exhibiting notably high or 23 low similarity between marine and freshwater ecosystems using a meta-analysis of 16S rRNA 24 gene tag-sequencing datasets. As expected, marine and freshwater microbial communities 25 differed in the relative abundance of major phyla and contained habitat-specific lineages; at the 26 same time, however, many shared taxa were observed in both environments. 27 Betaproteobacteria and Alphaproteobacteria sequences had the highest similarity between 28 marine and freshwater sample pairs. -
Microbial Fe(III) Oxide Reduction Potential in Chocolate Pots Hot Spring, Yellowstone National Park N
Geobiology (2016), 14, 255–275 DOI: 10.1111/gbi.12173 Microbial Fe(III) oxide reduction potential in Chocolate Pots hot spring, Yellowstone National Park N. W. FORTNEY,1 S. HE,1 B. J. CONVERSE,1 B. L. BEARD,1 C. M. JOHNSON,1 E. S. BOYD2 ANDE.E.RODEN1 1Department of Geoscience, NASA Astrobiology Institute, University of Wisconsin-Madison, Madison, WI, USA 2Department of Microbiology and Immunology, NASA Astrobiology Institute, Montana State University, Bozeman, MT, USA ABSTRACT Chocolate Pots hot springs (CP) is a unique, circumneutral pH, iron-rich, geothermal feature in Yellowstone National Park. Prior research at CP has focused on photosynthetically driven Fe(II) oxidation as a model for mineralization of microbial mats and deposition of Archean banded iron formations. However, geochemical and stable Fe isotopic data have suggested that dissimilatory microbial iron reduction (DIR) may be active within CP deposits. In this study, the potential for microbial reduction of native CP Fe(III) oxides was inves- tigated, using a combination of cultivation dependent and independent approaches, to assess the potential involvement of DIR in Fe redox cycling and associated stable Fe isotope fractionation in the CP hot springs. Endogenous microbial communities were able to reduce native CP Fe(III) oxides, as documented by most probable number enumerations and enrichment culture studies. Enrichment cultures demonstrated sus- tained DIR driven by oxidation of acetate, lactate, and H2. Inhibitor studies and molecular analyses indicate that sulfate reduction did not contribute to observed rates of DIR in the enrichment cultures through abi- otic reaction pathways. Enrichment cultures produced isotopically light Fe(II) during DIR relative to the bulk solid-phase Fe(III) oxides. -
Supplementary Information for Microbial Electrochemical Systems Outperform Fixed-Bed Biofilters for Cleaning-Up Urban Wastewater
Electronic Supplementary Material (ESI) for Environmental Science: Water Research & Technology. This journal is © The Royal Society of Chemistry 2016 Supplementary information for Microbial Electrochemical Systems outperform fixed-bed biofilters for cleaning-up urban wastewater AUTHORS: Arantxa Aguirre-Sierraa, Tristano Bacchetti De Gregorisb, Antonio Berná, Juan José Salasc, Carlos Aragónc, Abraham Esteve-Núñezab* Fig.1S Total nitrogen (A), ammonia (B) and nitrate (C) influent and effluent average values of the coke and the gravel biofilters. Error bars represent 95% confidence interval. Fig. 2S Influent and effluent COD (A) and BOD5 (B) average values of the hybrid biofilter and the hybrid polarized biofilter. Error bars represent 95% confidence interval. Fig. 3S Redox potential measured in the coke and the gravel biofilters Fig. 4S Rarefaction curves calculated for each sample based on the OTU computations. Fig. 5S Correspondence analysis biplot of classes’ distribution from pyrosequencing analysis. Fig. 6S. Relative abundance of classes of the category ‘other’ at class level. Table 1S Influent pre-treated wastewater and effluents characteristics. Averages ± SD HRT (d) 4.0 3.4 1.7 0.8 0.5 Influent COD (mg L-1) 246 ± 114 330 ± 107 457 ± 92 318 ± 143 393 ± 101 -1 BOD5 (mg L ) 136 ± 86 235 ± 36 268 ± 81 176 ± 127 213 ± 112 TN (mg L-1) 45.0 ± 17.4 60.6 ± 7.5 57.7 ± 3.9 43.7 ± 16.5 54.8 ± 10.1 -1 NH4-N (mg L ) 32.7 ± 18.7 51.6 ± 6.5 49.0 ± 2.3 36.6 ± 15.9 47.0 ± 8.8 -1 NO3-N (mg L ) 2.3 ± 3.6 1.0 ± 1.6 0.8 ± 0.6 1.5 ± 2.0 0.9 ± 0.6 TP (mg -
1 Microbial Transformations of Organic Chemicals in Produced Fluid From
Microbial transformations of organic chemicals in produced fluid from hydraulically fractured natural-gas wells Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Morgan V. Evans Graduate Program in Environmental Science The Ohio State University 2019 Dissertation Committee Professor Paula Mouser, Advisor Professor Gil Bohrer, Co-Advisor Professor Matthew Sullivan, Member Professor Ilham El-Monier, Member Professor Natalie Hull, Member 1 Copyrighted by Morgan Volker Evans 2019 2 Abstract Hydraulic fracturing and horizontal drilling technologies have greatly improved the production of oil and natural-gas from previously inaccessible non-permeable rock formations. Fluids comprised of water, chemicals, and proppant (e.g., sand) are injected at high pressures during hydraulic fracturing, and these fluids mix with formation porewaters and return to the surface with the hydrocarbon resource. Despite the addition of biocides during operations and the brine-level salinities of the formation porewaters, microorganisms have been identified in input, flowback (days to weeks after hydraulic fracturing occurs), and produced fluids (months to years after hydraulic fracturing occurs). Microorganisms in the hydraulically fractured system may have deleterious effects on well infrastructure and hydrocarbon recovery efficiency. The reduction of oxidized sulfur compounds (e.g., sulfate, thiosulfate) to sulfide has been associated with both well corrosion and souring of natural-gas, and proliferation of microorganisms during operations may lead to biomass clogging of the newly created fractures in the shale formation culminating in reduced hydrocarbon recovery. Consequently, it is important to elucidate microbial metabolisms in the hydraulically fractured ecosystem. -
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.