Novel Arsenic Hyper-Resistant Bacteria from an Extreme Environment
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Raman and Infrared Spectroscopy of Arsenates of the Roselite and Fairfeldite Mineral Subgroups
This may be the author’s version of a work that was submitted/accepted for publication in the following source: Frost, Ray (2009) Raman and infrared spectroscopy of arsenates of the roselite and fair- feldite mineral subgroups. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy, 71(5), pp. 1788-1794. This file was downloaded from: https://eprints.qut.edu.au/17596/ c Copyright 2009 Elsevier Reproduced in accordance with the copyright policy of the publisher. Notice: Please note that this document may not be the Version of Record (i.e. published version) of the work. Author manuscript versions (as Sub- mitted for peer review or as Accepted for publication after peer review) can be identified by an absence of publisher branding and/or typeset appear- ance. If there is any doubt, please refer to the published source. https://doi.org/10.1016/j.saa.2008.06.039 QUT Digital Repository: http://eprints.qut.edu.au/ Frost, Ray L. (2009) Raman and infrared spectroscopy of arsenates of the roselite and fairfieldite mineral subgroups. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy, 71(5). pp. 1788-1794. © Copyright 2009 Elsevier Raman and infrared spectroscopy of arsenates of the roselite and fairfieldite mineral subgroups Ray L. Frost• Inorganic Materials Research Program, School of Physical and Chemical Sciences, Queensland University of Technology, GPO Box 2434, Brisbane Queensland 4001, Australia. Abstract Raman spectroscopy complimented with infrared spectroscopy has been used to determine the molecular structure of the roselite arsenate minerals of the roselite and 2+ fairfieldite subgroups of formula Ca2B(AsO4)2.2H2O (where B may be Co, Fe , Mg, 2- Mn, Ni, Zn). -
Mineralogy and Crystal Structure of Bouazzerite from Bou Azzer, Anti-Atlas, Morocco: Bi-As-Fe Nanoclusters Containing Fe3+ in Trigonal Prismatic Coordination
American Mineralogist, Volume 92, pages 1630–1639, 2007 Mineralogy and crystal structure of bouazzerite from Bou Azzer, Anti-Atlas, Morocco: Bi-As-Fe nanoclusters containing Fe3+ in trigonal prismatic coordination JOËL BRUGGER,1,* NICOLAS MEISSER,2 SERGEY KRIVOVICHEV,3 THOMAS ARMBRUSTER,4 AND GEORGES FAVREAU5 1Department of Geology and Geophysics, Adelaide University, North Terrace, SA-5001 Adelaide, Australia and South Australian Museum, North Terrace, SA-5000 Adelaide, Australia 2Musée Géologique Cantonal and Laboratoire des Rayons-X, Institut de Minéralogie et Géochimie, UNIL-Anthropole, CH-1015 Lausanne- Dorigny, Switzerland 3Department of Crystallography, St. Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia 4Laboratorium für chemische und mineralogische Kristallographie, Universität Bern, Freiestrasse 3, CH-3012 Bern, Switzerland 5421 Avenue Jean Monnet, 13090 Aix-en-Provence, France ABSTRACT Bouazzerite, Bi6(Mg,Co)11Fe14[AsO4]18O12(OH)4(H2O)86, is a new mineral occurring in “Filon 7” at the Bou Azzer mine, Anti-Atlas, Morocco. Bouazzerite is associated with quartz, chalcopyrite, native gold, erythrite, talmessite/roselite-beta, Cr-bearing yukonite, alumopharmacosiderite, powellite, and a blue-green earthy copper arsenate related to geminite. The mineral results from the weathering of a Va- riscan hydrothermal As-Co-Ni-Ag-Au vein. The Bou Azzer mine and the similarly named district have produced many outstanding mineral specimens, including the world’s best erythrite and roselite. Bouazzerite forms monoclinic prismatic {021} crystals up to 0.5 mm in length. It has a pale 3 apple green color, a colorless streak, and is translucent with adamantine luster. dcalc is 2.81(2) g/cm (from X-ray structure refi nement). -
Metagenomics Analysis Reveals the Microbial Communities
diversity Article Metagenomics Analysis Reveals the Microbial Communities, Antimicrobial Resistance Gene Diversity and Potential Pathogen Transmission Risk of Two Different Landfills in China Shan Wan 1,†, Min Xia 2,†, Jie Tao 1, Yanjun Pang 1, Fugen Yu 1,* , Jun Wu 3,* and Shanping Chen 2,* 1 State Key Laboratory of Pharmaceutical Biotechnology, School of Life Sciences, Nanjing University, Nanjing 210023, China; [email protected] (S.W.); [email protected] (J.T.); [email protected] (Y.P.) 2 Shanghai Environmental Sanitation Engineering Design Institute Co., Ltd., Shanghai 200232, China; [email protected] 3 State Key Laboratory of Pollution Control and Resource Reuse, School of Environment, Nanjing University, Nanjing 210023, China * Correspondence: [email protected] (F.Y.); [email protected] (J.W.); [email protected] (S.C.) † There authors contribute equally to this work. Abstract: In this study, we used a metagenomic approach to analyze microbial communities, antibiotic resistance gene diversity, and human pathogenic bacterium composition in two typical Citation: Wan, S.; Xia, M.; Tao, J.; landfills in China. Results showed that the phyla Proteobacteria, Bacteroidetes, and Actinobacte- Pang, Y.; Yu, F.; Wu, J.; Chen, S. ria were predominant in the two landfills, and archaea and fungi were also detected. The genera Metagenomics Analysis Reveals the Methanoculleus, Lysobacter, and Pseudomonas were predominantly present in all samples. sul2, sul1, Microbial Communities, tetX, and adeF were the four most abundant antibiotic resistance genes. Sixty-nine bacterial pathogens Antimicrobial Resistance Gene were identified from the two landfills, with Klebsiella pneumoniae, Bordetella pertussis, Pseudomonas Diversity and Potential Pathogen aeruginosa, and Bacillus cereus as the major pathogenic microorganisms, indicating the existence of Transmission Risk of Two Different potential environmental risk in landfills. -
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NEW MINERAL NAMES Fleischerite. Itoite C, FnoNnrr, lNo H. SrnuNz. Fleischerit und Itoit, zwei neue Germanium-Mineralien von Tsumeb. Neues Johrb. Mineral., Montash' 1960, 132-142 (English summary)' The minerals were found in the upper oxidation zone of the Tsumeb Mine, associated with cerussite, mimetite, and altered tennantite, also as a crust on plumbojarosite and mimetite on dolomite. A preliminary description of fleischerite (unnamed) was given by Frondel and Ito in Am. Minual 42,747 (1957). Fleischerite occurs as white to pale rose fibrous aggregates, with silky luster. Analysis 11'35, by Jun Ito gave PbO 63.34, GeO 818, GazOr 0.86, Fe:Or 005, SOr 1506, HrO+ HsO- 0.21, insol. 0.56, stm99.61/6, corresponding to Pb3Ge{(OH)4(SOrr'4HrO. Oscillation, rotation, and Laue photographs show fleischerite to be hexagonal, space group probably P$fmmc, o0 8.89, c010.86L Z:Z.Indexed r-ray powder data are given; the strongest lines are 3.619 (10), 2.635 (8), 3.437 (6) , 2.214 (6) , 1.889 (6). No cleavagewas observed. G. 4.2-4.4 (measured),4.59 (calcd.) Hardness low. Optically uniaxial, pos., ,?s e 1.776,u 1.747. Not fluorescentunder UV light, becomes rose-violet when irradiated with *-rays. DTA study showed a distinct endothermal effect at 263", a weak endothermal effect at 314", and a small exothermal effect at 463". When heated and observed under the micro- scope becomes turbid at l7 5-200" , inverts to an isotropic phase at 4650. When ground for a long time in an agate mortar, inverts to itoite by loss of water and oxidation of Ge{ to Ge++. -
Austinite Cazn(Aso4)(OH) C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Orthorhombic
Austinite CaZn(AsO4)(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 222. As enantiomorphous bladed crystals exhibiting {011}, {111}, {111}, {010} and several other forms, sometimes forming scepters. Also as radially fibrous crusts and nodules. Twinning: Left- and right-handed individuals joined on (100), with (010) and (001) coincident. Physical Properties: Cleavage: Good on {011}. Tenacity: Brittle. Hardness = 4–4.5 D(meas.) = 4.13 D(calc.) = [4.31] Optical Properties: Translucent to transparent. Color: Colorless, white to pale yellowish white, green. Luster: Subadamantine to silky in aggregates. Optical Class: Biaxial (+). Orientation: X = a; Y = c; Z = b. Dispersion: r> v,weak. α = 1.759(3) β = 1.763(3) γ = 1.783(3) 2V(meas.) = ∼45◦ Cell Data: Space Group: P 212121. a = 7.505–7.509 b = 9.037–9.046 c = 5.921–5.934 Z=4 X-ray Powder Pattern: Gold Hill, Utah, USA. 3.171 (10), 2.801 (10), 2.637 (10), 1.616 (9), 1.509 (7), 2.529 (6), 5.781 (5) Chemistry: (1) (2) (3) (1) (2) (3) P2O5 0.1 0.90 CaO 19.2 21.33 21.45 As2O5 42.7 42.85 43.96 H2O 3.6 [3.45] 3.45 FeO 0.49 insol. 2.4 CuO 0.88 Total 100.5 [100.00] 100.00 ZnO 32.5 30.10 31.14 (1) Gold Hill, Utah, USA; insoluble is quartz, some adamite adhering. (2) Kamariza mine, Greece; by electron microprobe, H2O by difference; corresponding to Ca1.00(Zn0.96Cu0.03 Fe0.01)Σ=1.00[(As0.97P0.03)Σ=1.00O4](OH). -
New Mineral Names*
American Mineralogist, Volume 66, pages 1274-1280, 1981 NEW MINERAL NAMES* MICHAEL FLEISCHER AND LOUIS J. CABRI Cyanophillite* ar~ 3.350(50)(110), 3.:208(50)(020), 3.080 (80)(111), 2.781(100) (221,111), 2.750(70)(112), 1.721 (60). Kurt Walenta (1981) Cyanophillite, a new mineral from the Clara ~olor1ess to white, luster vitreous. Cleavages {010}, {OOI}, Mine, near Oberwolfach, Central Black Forest. Chem. der {OIl} good, not easily observed. Hardness about 5. Optically Erde, 40, 195-200 (in German). biaxial positive, ns ex= 1.713, /3 = 1.730, )' = 1.748, 2V +88° (89° Analyses gave CuO 36.3, 32.5; Ah03 8.5, -; Sb203 36.5, 38.3; calc.). Material with Zn:Mg = 1:1 is biaxial, neg., ns. ex= 1.689, H20 19.8; sum 101.1%, corresponding to 10CuO . 2Ah03 . 3Sb2 /3 = 1.707, )' = 1.727, 2V ~ 85°. 03 . 25H20. The mineral is dissolved readily by cold 1:1 HCI, The mineral occurs as coatings and small crystals, largest partly dissolved by 1: 1 HN03. Loss of weight when heated (%) dimension about 1 mm; on prosperite, adamite, and austinite 110° 3.4, 150° 9.5, 200° 19.8%. At 250° the mineral is decomposed from Tsumeb, Namibia. Forms observed {010}, {001}, {Oil}, also and turns black. {IOO}very small. X-ray study shows the mineral to be orthorhombic, space The name is for Robert I. Gait, Curator of Mineralogy, Royal group Pmmb, a = 11.82, b = 10.80, c = 9.64A, Z = 1, D 3.10 Ontario Museum, Toronto. Type material is at the Royal Ontario meas., 3.12 calc. -
Talmessite from the Uriya Deposit at the Kiura Mining Area, Oita Prefecture, Japan
116 Journal ofM. Mineralogical Ohnishi, N. Shimobayashi, and Petrological S. Kishi, Sciences, M. Tanabe Volume and 108, S. pageKobayashi 116─ 120, 2013 LETTER Talmessite from the Uriya deposit at the Kiura mining area, Oita Prefecture, Japan * ** *** Masayuki OHNISHI , Norimasa SHIMOBAYASHI , Shigetomo KISHI , † § Mitsuo TANABE and Shoichi KOBAYASHI * 12-43 Takehana Ougi-cho, Yamashina-ku, Kyoto 607-8082, Japan **Department of Geology and Mineralogy, Graduate School of Science, Kyoto University, Kitashirakawa Oiwake-cho, Sakyo-ku, Kyoto 606-8502, Japan *** Kamisaibara Junior High School, 1320 Kamisaibara, Kagamino-cho, Tomada-gun, Okayama 708-0601, Japan † 2058-3 Niimi, Niimi, Okayama 718-0011, Japan § Department of Applied Science, Faculty of Science, Okayama University of Science, 1-1 Ridai-cho, Kita-ku, Okayama 700-0005, Japan Talmessite was found in veinlets (approximately 1 mm wide) cutting into massive limonite in the oxidized zone of the Uriya deposit, Kiura mining area, Oita Prefecture, Japan. It occurs as aggregates of granular crystals up to 10 μm in diameter and as botryoidal aggregates up to 0.5 mm in diameter, in association with arseniosiderite, and aragonite. The talmessite is white to colorless, transparent, and has a vitreous luster. The unit-cell parame- ters refined from powder X-ray diffraction patterns are a = 5.905(3), b = 6.989(3), c = 5.567(4) Å, α = 96.99(3), β = 108.97(4), γ = 108.15(4)°, and Z = 1. Electron microprobe analyses gave the empirical formula Ca2.15(Mg0.84 Mn0.05Zn0.02Fe0.01Co0.01Ni0.01)∑0.94(AsO4)1.91·2H2O on the basis of total cations = 5 apfu (water content calculated as 2 H2O pfu). -
Crystal Structure Determination of Karibibite, an Fe3+ Arsenite, Using Electron Diffraction Tomography
Mineralogical Magazine, October 2017, Vol. 81(5), pp. 1191–1202 Crystal structure determination of karibibite, an Fe3+ arsenite, using electron diffraction tomography 1,*,§ 2,3 4 1 1,5 FERNANDO COLOMBO ,ENRICO MUGNAIOLI ,ORIOL VALLCORBA ,ALBERTO GARCÍA ,ALEJANDRO R. GOÑI 1 AND JORDI RIUS 1 Institut de Ciencià de Materials de Barcelona (ICMAB-CSIC), Campus UAB, E-08193 Bellaterra, Catalonia, Spain 2 Dipartimento di Scienze Fisiche, della Terra e dell’Ambiente. Università degli Studi di Siena. Via Laterino 8, 53100, Siena, Italy 3 Centre for Nanotechnology Innovation@NEST, Istituto Italiano di Tecnologia, Piazza San Silvestro 12, 56127, Pisa, Italy 4 Experiments Division - MSPD Beamline (BL04. ALBA Synchrotron Light Source – CELLS. Crta BP 1413 Km 3.3, 08290 Cerdanyola del Valles,̀ Barcelona, Spain 5 ICREA, Passeig Lluís Companys 23, 08010 Barcelona, Spain [Received 13 February 2016; Accepted 17 October 2016; Associate Editor: Anthony Kampf] ABSTRACT 3þ 3+ 3þ The crystal structure of karibibite, Fe3 (As O2)4(As2 O5)(OH), from the Urucum mine (Minas Gerais, σ Brazil), was solved and refined from electron diffraction tomography data [R1 = 18.8% for F >4 (F)] and further confirmed by synchrotron X-ray diffraction and density functional theory (DFT) calculations. The mineral is orthorhombic, space group Pnma and unit-cell parameters (synchrotron X-ray diffraction) are a = 7.2558(3), b = 27.992(1), c = 6.5243 (3) Å, V = 1325.10(8) Å3, Z = 4. The crystal structure of karibibbite 3+ consists of bands of Fe O6 octahedra running along a framed by two chains of AsO3 trigonal pyramids at each side, and along c by As2O5 dimers above and below. -
Arenimonas Halophila Sp. Nov., Isolated from Soil
TAXONOMIC DESCRIPTION Kanjanasuntree et al., Int J Syst Evol Microbiol 2018;68:2188–2193 DOI 10.1099/ijsem.0.002801 Arenimonas halophila sp. nov., isolated from soil Rungravee Kanjanasuntree,1 Jong-Hwa Kim,1 Jung-Hoon Yoon,2 Ampaitip Sukhoom,3 Duangporn Kantachote3 and Wonyong Kim1,* Abstract A Gram-staining-negative, aerobic, non-motile, rod-shaped bacterium, designated CAU 1453T, was isolated from soil and its taxonomic position was investigated using a polyphasic approach. Strain CAU 1453T grew optimally at 30 C and at pH 6.5 in the presence of 1 % (w/v) NaCl. Phylogenetic analysis based on the 16S rRNA gene sequences revealed that CAU 1453T represented a member of the genus Arenimonas and was most closely related to Arenimonas donghaensis KACC 11381T (97.2 % similarity). T CAU 1453 contained ubiquinone-8 (Q-8) as the predominant isoprenoid quinone and iso-C15 : 0 and iso-C16 : 0 as the major cellular fatty acids. The polar lipids consisted of diphosphatidylglycerol, a phosphoglycolipid, an aminophospholipid, two unidentified phospholipids and two unidentified glycolipids. CAU 1453T showed low DNA–DNA relatedness with the most closely related strain, A. donghaensis KACC 11381T (26.5 %). The DNA G+C content was 67.3 mol%. On the basis of phenotypic, chemotaxonomic and phylogenetic data, CAU 1453T represents a novel species of the genus Arenimonas, for which the name Arenimonas halophila sp. nov. is proposed. The type strain is CAU 1453T (=KCTC 62235T=NBRC 113093T). The genus Arenimonas, a member of the family Xantho- CAU 1453T was isolated from soil by the dilution plating monadaceae in the class Gammaproteobacteria was pro- method using marine agar 2216 (MA; Difco) [14]. -
Lithotectonic Setting Necessary for Formation of a Uranium-Rich, Solution-Collapse Breccia-Pipe Province, Grand Canyon Region, Arizona
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Lithotectonic Setting Necessary for Formation of a Uranium-Rich, Solution-Collapse Breccia-Pipe Province, Grand Canyon Region, Arizona by Karen J. Wenrich 1 & Hoyt B. Sutphin 1 Open-File Report 89-0173 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature, U.S. Geological Survey Box 25046, MS 905 Denver Federal Center Denver, CO 80225 1989 CONTENTS Page Abstract.............................................................. 1 Introduction.......................................................... 2 Structural control of breccia pipes................................... 6 Alignment of breccia pipes....................................... 6 Joints in the Mississippian Redwall Limestone.................... 6 Joints in the overlying Permian strata........................... 8 The relationship of the breccia pipe ring fracture to the joints.......................................................... 8 Breccia pipes exposed in Redwall Limestone caves................. 9 Mineralization of the breccia pipes................................... 9 Mineralization and paragenesis................................... 9 Deposition of early carbonates and sulfates................. 9 Deposition of Ni-Co-As-Fe-S-bearing minerals................ 13 Deposition of Cu-Pb-Zn sulfides............................. 16 Deposition of uraninite and Cu-Fe sulfides.................. 16 Remobilization and deposition of ore metals -
Wendwilsonite Ca2(Mg, Co)(Aso4)2 • 2H2O C 2001-2005 Mineral Data Publishing, Version 1
Wendwilsonite Ca2(Mg, Co)(AsO4)2 • 2H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Crystals are stout prismatic, elongated along [100], showing {011}, {111}, {010}, {110}, to 6 mm. Twinning: On {100} as twin and composition plane; lamellar structure k{010}, {011}, {111} visible optically. Physical Properties: Cleavage: Perfect on {010}. Fracture: Uneven. Hardness = 3–4 D(meas.) = 3.52(8) D(calc.) = 3.57 Optical Properties: Transparent. Color: Pale to intense pink, may be red, commonly color zoned. Streak: Pale pink. Luster: Vitreous. Optical Class: Biaxial (–). Pleochroism: X = violet-pink; Y = rose-pink; Z = colorless. Orientation: Y = b; Z ∧ c =92◦. Dispersion: r< v. Absorption: X ≥Y > Z. α = 1.694(3) β = 1.703(3) γ = 1.713(3) 2V(meas.) = 87(2)◦ Cell Data: Space Group: P 21/c. a = 5.806(1) b = 12.912(2) c = 5.623(2) β = 107◦24(1)0 Z=2 X-ray Powder Pattern: Bou Azzer, Morocco; close to roselite. 2.994 (100), 2.766 (80), 3.226 (60), 5.085 (50), 3.356 (40), 2.592 (40), 3.397 (30) Chemistry: (1) (2) As2O5 55.8 52.76 CoO 2.6 8.60 MgO 7.7 4.63 CaO 26.4 25.74 H2O 7.4 8.27 Total 99.9 100.00 (1) Bou Azzer, Morocco; by electron microprobe, H2O by the Penfield method; corresponding to • • Ca2.03(Mg0.82Co0.15)Σ=0.97(AsO4)2.09 1.77H2O. (2) Ca2(Mg, Co)(AsO4)2 2H2O with Mg:Co = 1:1. -
Unveiling Bacterial Interactions Through Multidimensional Scaling and Dynamics Modeling Received: 06 May 2015 Pedro Dorado-Morales1, Cristina Vilanova1, Carlos P
www.nature.com/scientificreports OPEN Unveiling Bacterial Interactions through Multidimensional Scaling and Dynamics Modeling Received: 06 May 2015 Pedro Dorado-Morales1, Cristina Vilanova1, Carlos P. Garay3, Jose Manuel Martí3 Accepted: 17 November 2015 & Manuel Porcar1,2 Published: 16 December 2015 We propose a new strategy to identify and visualize bacterial consortia by conducting replicated culturing of environmental samples coupled with high-throughput sequencing and multidimensional scaling analysis, followed by identification of bacteria-bacteria correlations and interactions. We conducted a proof of concept assay with pine-tree resin-based media in ten replicates, which allowed detecting and visualizing dynamical bacterial associations in the form of statistically significant and yet biologically relevant bacterial consortia. There is a growing interest on disentangling the complexity of microbial interactions in order to both optimize reactions performed by natural consortia and to pave the way towards the development of synthetic consor- tia with improved biotechnological properties1,2. Despite the enormous amount of metagenomic data on both natural and artificial microbial ecosystems, bacterial consortia are not necessarily deduced from those data. In fact, the flexibility of the bacterial interactions, the lack of replicated assays and/or biases associated with differ- ent DNA isolation technologies and taxonomic bioinformatics tools hamper the clear identification of bacterial consortia. We propose here a holistic approach aiming at identifying bacterial interactions in laboratory-selected microbial complex cultures. The method requires multi-replicated taxonomic data on independent subcultures, and high-throughput sequencing-based taxonomic data. From this data matrix, randomness of replicates can be verified, linear correlations can be visualized and interactions can emerge from statistical correlations.