ABSTRACT ZELDES, BENJAMIN. Leveraging Extreme
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Developing a Genetic Manipulation System for the Antarctic Archaeon, Halorubrum Lacusprofundi: Investigating Acetamidase Gene Function
www.nature.com/scientificreports OPEN Developing a genetic manipulation system for the Antarctic archaeon, Halorubrum lacusprofundi: Received: 27 May 2016 Accepted: 16 September 2016 investigating acetamidase gene Published: 06 October 2016 function Y. Liao1, T. J. Williams1, J. C. Walsh2,3, M. Ji1, A. Poljak4, P. M. G. Curmi2, I. G. Duggin3 & R. Cavicchioli1 No systems have been reported for genetic manipulation of cold-adapted Archaea. Halorubrum lacusprofundi is an important member of Deep Lake, Antarctica (~10% of the population), and is amendable to laboratory cultivation. Here we report the development of a shuttle-vector and targeted gene-knockout system for this species. To investigate the function of acetamidase/formamidase genes, a class of genes not experimentally studied in Archaea, the acetamidase gene, amd3, was disrupted. The wild-type grew on acetamide as a sole source of carbon and nitrogen, but the mutant did not. Acetamidase/formamidase genes were found to form three distinct clades within a broad distribution of Archaea and Bacteria. Genes were present within lineages characterized by aerobic growth in low nutrient environments (e.g. haloarchaea, Starkeya) but absent from lineages containing anaerobes or facultative anaerobes (e.g. methanogens, Epsilonproteobacteria) or parasites of animals and plants (e.g. Chlamydiae). While acetamide is not a well characterized natural substrate, the build-up of plastic pollutants in the environment provides a potential source of introduced acetamide. In view of the extent and pattern of distribution of acetamidase/formamidase sequences within Archaea and Bacteria, we speculate that acetamide from plastics may promote the selection of amd/fmd genes in an increasing number of environmental microorganisms. -
Microbial Desulfurization of Three Different Coals from Indonesia, China and Korea in Varying Growth Medium
Korean J. Chem. Eng., 30(3), 680-687 (2013) DOI: 10.1007/s11814-012-0168-z INVITED REVIEW PAPER Microbial desulfurization of three different coals from Indonesia, China and Korea in varying growth medium Dong-Jin Kim*, Chandra Sekhar Gahan*,**,†, Chandrika Akilan***, Seo-Yun Choi*, and Byoung-Gon Kim* *Mineral Resource Research Division, Korea Institute of Geoscience and Mineral Resources (KIGAM), Gwahang-ro 92, Yuseong-gu, Daejeon 305-350, Korea **SRM Research Institute, SRM University, Kattankulathur - 603 203, Kancheepuram District, Chennai, Tamil Nadu, India ***Faculty of Minerals and Energy, School of Chemical and Mathematical Sciences, Murdoch University, 90 South Street, Murdoch, 6150, Western Australia (Received 23 April 2012 • accepted 2 October 2012) Abstract−Shake flask studies on microbial desulfurization of three different coal samples (Indonesian lignite, Chinese lignite and Korean anthracite) were performed to optimize the best suitable growth medium. Among the three different growth mediums (basal salt medium, basal salt medium supplemented with 9 g/L Fe and basal salt medium supple- mented with 2.5% S0) tested, the basal salt medium was found to be the best, considering process dynamics and eco- nomical factors. The extent of pyrite oxidation was highest with 95% in the experiments with Korean anthracite in basal salt medium supplemented with 9 g/L Fe, while the lowest pyrite oxidation of 70-71% was observed in the experiments with Indonesian and Chinese Lignite’s in only basal salt medium. The microbial sulfur removal in the experiments with basal salt medium supplemented with 9 g/L Fe for all the three coal samples was between 94-97%, while the experiments on basal salt medium supplemented with 2.5% S0 for all the coal samples were relatively much lower ranging between 27-48%. -
Differences in Lateral Gene Transfer in Hypersaline Versus Thermal Environments Matthew E Rhodes1*, John R Spear2, Aharon Oren3 and Christopher H House1
Rhodes et al. BMC Evolutionary Biology 2011, 11:199 http://www.biomedcentral.com/1471-2148/11/199 RESEARCH ARTICLE Open Access Differences in lateral gene transfer in hypersaline versus thermal environments Matthew E Rhodes1*, John R Spear2, Aharon Oren3 and Christopher H House1 Abstract Background: The role of lateral gene transfer (LGT) in the evolution of microorganisms is only beginning to be understood. While most LGT events occur between closely related individuals, inter-phylum and inter-domain LGT events are not uncommon. These distant transfer events offer potentially greater fitness advantages and it is for this reason that these “long distance” LGT events may have significantly impacted the evolution of microbes. One mechanism driving distant LGT events is microbial transformation. Theoretically, transformative events can occur between any two species provided that the DNA of one enters the habitat of the other. Two categories of microorganisms that are well-known for LGT are the thermophiles and halophiles. Results: We identified potential inter-class LGT events into both a thermophilic class of Archaea (Thermoprotei) and a halophilic class of Archaea (Halobacteria). We then categorized these LGT genes as originating in thermophiles and halophiles respectively. While more than 68% of transfer events into Thermoprotei taxa originated in other thermophiles, less than 11% of transfer events into Halobacteria taxa originated in other halophiles. Conclusions: Our results suggest that there is a fundamental difference between LGT in thermophiles and halophiles. We theorize that the difference lies in the different natures of the environments. While DNA degrades rapidly in thermal environments due to temperature-driven denaturization, hypersaline environments are adept at preserving DNA. -
Resolution of Carbon Metabolism and Sulfur-Oxidation Pathways of Metallosphaera Cuprina Ar-4 Via Comparative Proteomics
JOURNAL OF PROTEOMICS 109 (2014) 276– 289 Available online at www.sciencedirect.com ScienceDirect www.elsevier.com/locate/jprot Resolution of carbon metabolism and sulfur-oxidation pathways of Metallosphaera cuprina Ar-4 via comparative proteomics Cheng-Ying Jianga, Li-Jun Liua, Xu Guoa, Xiao-Yan Youa, Shuang-Jiang Liua,c,⁎, Ansgar Poetschb,⁎⁎ aState Key Laboratory of Microbial Resources, Institute of Microbiology, Chinese Academy of Sciences, Beijing, PR China bPlant Biochemistry, Ruhr University Bochum, Bochum, Germany cEnvrionmental Microbiology and Biotechnology Research Center, Institute of Microbiology, Chinese Academy of Sciences, Beijing, PR China ARTICLE INFO ABSTRACT Article history: Metallosphaera cuprina is able to grow either heterotrophically on organics or autotrophically Received 16 March 2014 on CO2 with reduced sulfur compounds as electron donor. These traits endowed the species Accepted 6 July 2014 desirable for application in biomining. In order to obtain a global overview of physiological Available online 14 July 2014 adaptations on the proteome level, proteomes of cytoplasmic and membrane fractions from cells grown autotrophically on CO2 plus sulfur or heterotrophically on yeast extract Keywords: were compared. 169 proteins were found to change their abundance depending on growth Quantitative proteomics condition. The proteins with increased abundance under autotrophic growth displayed Bioleaching candidate enzymes/proteins of M. cuprina for fixing CO2 through the previously identified Autotrophy 3-hydroxypropionate/4-hydroxybutyrate cycle and for oxidizing elemental sulfur as energy Heterotrophy source. The main enzymes/proteins involved in semi- and non-phosphorylating Entner– Industrial microbiology Doudoroff (ED) pathway and TCA cycle were less abundant under autotrophic growth. Also Extremophile some transporter proteins and proteins of amino acid metabolism changed their abundances, suggesting pivotal roles for growth under the respective conditions. -
A Survey of Carbon Fixation Pathways Through a Quantitative Lens
Journal of Experimental Botany, Vol. 63, No. 6, pp. 2325–2342, 2012 doi:10.1093/jxb/err417 Advance Access publication 26 December, 2011 REVIEW PAPER A survey of carbon fixation pathways through a quantitative lens Arren Bar-Even, Elad Noor and Ron Milo* Department of Plant Sciences, The Weizmann Institute of Science, Rehovot 76100, Israel * To whom correspondence should be addressed. E-mail: [email protected] Received 15 August 2011; Revised 4 November 2011; Accepted 8 November 2011 Downloaded from Abstract While the reductive pentose phosphate cycle is responsible for the fixation of most of the carbon in the biosphere, it http://jxb.oxfordjournals.org/ has several natural substitutes. In fact, due to the characterization of three new carbon fixation pathways in the last decade, the diversity of known metabolic solutions for autotrophic growth has doubled. In this review, the different pathways are analysed and compared according to various criteria, trying to connect each of the different metabolic alternatives to suitable environments or metabolic goals. The different roles of carbon fixation are discussed; in addition to sustaining autotrophic growth it can also be used for energy conservation and as an electron sink for the recycling of reduced electron carriers. Our main focus in this review is on thermodynamic and kinetic aspects, including thermodynamically challenging reactions, the ATP requirement of each pathway, energetic constraints on carbon fixation, and factors that are expected to limit the rate of the pathways. Finally, possible metabolic structures at Weizmann Institute of Science on July 3, 2016 of yet unknown carbon fixation pathways are suggested and discussed. -
Exploring the Microbial Biotransformation of Extraterrestrial
www.nature.com/scientificreports OPEN Exploring the microbial biotransformation of extraterrestrial material on nanometer scale Tetyana Milojevic1*, Denise Kölbl1, Ludovic Ferrière 2, Mihaela Albu 3, Adrienne Kish4, Roberta L. Flemming5, Christian Koeberl2,9, Amir Blazevic1, Ziga Zebec 1,6, Simon K.-M. R. Rittmann 6, Christa Schleper 6, Marc Pignitter7, Veronika Somoza7, Mario P. Schimak8 & Alexandra N. Rupert 5 Exploration of microbial-meteorite redox interactions highlights the possibility of bioprocessing of extraterrestrial metal resources and reveals specifc microbial fngerprints left on extraterrestrial material. In the present study, we provide our observations on a microbial-meteorite nanoscale interface of the metal respiring thermoacidophile Metallosphaera sedula. M. sedula colonizes the stony meteorite Northwest Africa 1172 (NWA 1172; an H5 ordinary chondrite) and releases free soluble metals, with Ni ions as the most solubilized. We show the redox route of Ni ions, originating from the metallic Ni° of the meteorite grains and leading to released soluble Ni2+. Nanoscale resolution ultrastructural studies of meteorite grown M. sedula coupled to electron energy loss spectroscopy (EELS) points to the redox processing of Fe-bearing meteorite material. Our investigations validate the ability of M. sedula to perform the biotransformation of meteorite minerals, unravel microbial fngerprints left on meteorite material, and provide the next step towards an understanding of meteorite biogeochemistry. Our fndings will serve in defning mineralogical and morphological criteria for the identifcation of metal-containing microfossils. Te ability of chemolithotrophic microorganisms to catalyze redox transformations of metals is an exquisite tool for energy transduction between a mineral body and a living entity. Te diferent types of meteorites from diverse parental bodies (asteroids, Moon, or Mars) represent exceptional metal-bearing substrates that have experienced an exposure to multiple extreme conditions during their interstellar or interplanetary travel. -
ABSTRACT AUERNIK, KATHRYNE SHERLOCK. Functional Genomics Analysis of Metal Mobilization by the Extremely Thermoacidophilic Archa
ABSTRACT AUERNIK, KATHRYNE SHERLOCK. Functional Genomics Analysis of Metal Mobilization by the Extremely Thermoacidophilic Archaeon Metallosphaera sedula. (Under the direction of Dr. Robert Kelly.) Biomining processes recovering base, strategic and precious metals have predominantly utilized mesophilic bacteria, but relatively low yields have impacted wider application of this biotechnology. However, the use of high temperature microorganisms offers great potential to increase metal mobilization rates. Metallosphaera sedula (Mse) is an extremely thermoacidophilic archaeon with bioleaching capabilities, although little is known about the physiology of this microorganism. To better characterize Mse, its genome was sequenced and a whole genome oligonucleotide microarray was constructed for transcriptional response analysis. The physiological and bioenergetic complexities of Mse bioleaching were studied focusing on iron oxidation, sulfur oxidation, and growth modes (heterotrophy, autotrophy, and mixotrophy). The transcriptomes corresponding to each of these elements were examined for clues to the mechanisms by which Mse oxidizes inorganic energy sources (i.e. metal sulfides) and fixes CO2. Quinol/terminal oxidases important for maintaining intracellular pH and contributing to ATP generation via proton pumping were stimulated by different energy sources. The soxABCDD’L genome locus (Msed_0285-Msed_0291) was stimulated in the presence of reduced inorganic sulfur compounds (RISCs) and H2, while the soxNL-CbsABA cluster (Msed_0500-Msed_0504) was induced by Fe(II). Two similar copies of the SoxB/CoxI-like cytochrome oxidase subunit, foxAA’ (Msed_0484/Msed_0485) were implicated in fox cluster oxidation of Fe(II), as well as other energy sources. The doxBCE locus (Msed_2030-Msed2032) did not respond uniformly to either Fe(II) or RISCs, but was up-regulated in the presence of chalcopyrite (CuFeS2). -
Calditol-Linked Membrane Lipids Are Required for Acid Tolerance in Sulfolobus Acidocaldarius
Calditol-linked membrane lipids are required for acid tolerance in Sulfolobus acidocaldarius Zhirui Zenga,1, Xiao-Lei Liub,1, Jeremy H. Weia, Roger E. Summonsc, and Paula V. Welandera,2 aDepartment of Earth System Science, Stanford University, Stanford, CA 94305; bDepartment of Geology and Geophysics, University of Oklahoma, Norman, OK 73019; and cDepartment of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139 Edited by Katherine H. Freeman, Pennsylvania State University, University Park, PA, and approved November 7, 2018 (received for review August 14, 2018) Archaea have many unique physiological features of which the lipid and sea-surface temperatures in the Mesozoic and early Cenozoic, composition of their cellular membranes is the most striking. and the geologic history of archaea in ancient sediments (13, 14). Archaeal ether-linked isoprenoidal membranes can occur as bilayers However, deciphering the evolutionary implications of archaeal or monolayers, possess diverse polar head groups, and a multiplicity lipid biosynthesis, as well as being able to properly interpret ar- of ring structures in the isoprenoidal cores. These lipid structures chaeal lipid biomarkers, requires a full understanding of the are proposed to provide protection from the extreme temperature, biosynthetic pathways and the physiological roles of these various pH, salinity, and nutrient-starved conditions that many archaea structures in extant archaea. inhabit. However, many questions remain regarding the synthesis Studies of archaeal membrane lipid synthesis have revealed and physiological role of some of the more complex archaeal lipids. distinct proteins and biochemical reactions, but several open In this study, we identify a radical S-adenosylmethionine (SAM) questions remain (4, 15). -
Diversity of Archaea Domain in Cuatro Cienegas Basin: Archaean Domes
bioRxiv preprint doi: https://doi.org/10.1101/766709; this version posted September 12, 2019. 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 Diversity of Archaea Domain in Cuatro Cienegas Basin: Archaean Domes 2 3 Medina-Chávez Nahui Olin1, Viladomat-Jasso Mariette2, Olmedo-Álvarez Gabriela3, Eguiarte Luis 4 E2, Souza Valeria2, De la Torre-Zavala Susana1,4 5 6 1Universidad Autónoma de Nuevo León, Facultad de Ciencias Biológicas, Instituto de 7 Biotecnología. Av. Pedro de Alba S/N Ciudad Universitaria. San Nicolás de los Garza, Nuevo León, 8 México. C.P. 66455. 9 2Instituto de Ecología, UNAM, Circuito Exterior S/N anexo Jardín Botánico exterior. Ciudad 10 Universitaria, Ciudad de México, C.P. 04500 11 3Departamento de Ingeniería Genética, Centro de Investigación y de Estudios Avanzados del I.P.N. 12 Campus Guanajuato, AP 629 Irapuato, Guanajuato 36500, México 13 14 4Correspondence should be addressed to Susana De la Torre-Zavala; 15 [email protected]. 16 17 18 19 20 21 22 1 bioRxiv preprint doi: https://doi.org/10.1101/766709; this version posted September 12, 2019. 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. 23 Abstract 24 Herein we describe the Archaea diversity in a shallow pond in the Cuatro Ciénegas Basin (CCB), 25 Northeast Mexico, with fluctuating hypersaline conditions containing elastic microbial mats that 26 can form small domes where their anoxic inside reminds us of the characteristics of the Archaean 27 Eon, rich in methane and sulfur gases; thus, we named this site the Archaean Domes (AD). -
Extremophiles-Basic Concepts
CONTENTS CONTENTS EXTREMOPHILES Extremophiles - Volume 1 No. of Pages: 396 ISBN: 978-1-905839-93-3 (eBook) ISBN: 978-1-84826-993-4 (Print Volume) Extremophiles - Volume 2 No. of Pages: 392 ISBN: 978-1-905839-94-0 (eBook) ISBN: 978-1-84826-994-1 (Print Volume) Extremophiles - Volume 3 No. of Pages: 364 ISBN: 978-1-905839-95-7 (eBook) ISBN: 978-1-84826-995-8 (Print Volume) For more information of e-book and Print Volume(s) order, please click here Or contact : [email protected] ©Encyclopedia of Life Support Systems (EOLSS) EXTREMOPHILES CONTENTS VOLUME I Extremophiles: Basic Concepts 1 Charles Gerday, Laboratory of Biochemistry, University of Liège, Belgium 1. Introduction 2. Effects of Extreme Conditions on Cellular Components 2.1. Membrane Structure 2.2. Nucleic Acids 2.2.1. Introduction 2.2.2. Desoxyribonucleic Acids 2.2.3. Ribonucleic Acids 2.3. Proteins 2.3.1. Introduction 2.3.2. Thermophilic Proteins 2.3.2.1. Enthalpically Driven Stabilization Factors: 2.3.2.2. Entropically Driven Stabilization Factors: 2.3.3. Psychrophilic Proteins 2.3.4. Halophilic Proteins 2.3.5. Piezophilic Proteins 2.3.5.1. Interaction with Other Proteins and Ligands: 2.3.5.2. Substrate Binding and Catalytic Efficiency: 2.3.6. Alkaliphilic Proteins 2.3.7. Acidophilic Proteins 3. Conclusions Extremophiles: Overview of the Biotopes 43 Michael Gross, University of London, London, UK 1. Introduction 2. Extreme Temperatures 2.1. Terrestrial Hot Springs 2.2. Hot Springs on the Ocean Floor and Black Smokers 2.3. Life at Low Temperatures 3. High Pressure 3.1. -
4 Metabolic and Taxonomic Diversification in Continental Magmatic Hydrothermal Systems
Maximiliano J. Amenabar, Matthew R. Urschel, and Eric S. Boyd 4 Metabolic and taxonomic diversification in continental magmatic hydrothermal systems 4.1 Introduction Hydrothermal systems integrate geological processes from the deep crust to the Earth’s surface yielding an extensive array of spring types with an extraordinary diversity of geochemical compositions. Such geochemical diversity selects for unique metabolic properties expressed through novel enzymes and functional characteristics that are tailored to the specific conditions of their local environment. This dynamic interaction between geochemical variation and biology has played out over evolu- tionary time to engender tightly coupled and efficient biogeochemical cycles. The timescales by which these evolutionary events took place, however, are typically in- accessible for direct observation. This inaccessibility impedes experimentation aimed at understanding the causative principles of linked biological and geological change unless alternative approaches are used. A successful approach that is commonly used in geological studies involves comparative analysis of spatial variations to test ideas about temporal changes that occur over inaccessible (i.e. geological) timescales. The same approach can be used to examine the links between biology and environment with the aim of reconstructing the sequence of evolutionary events that resulted in the diversity of organisms that inhabit modern day hydrothermal environments and the mechanisms by which this sequence of events occurred. By combining molecu- lar biological and geochemical analyses with robust phylogenetic frameworks using approaches commonly referred to as phylogenetic ecology [1, 2], it is now possible to take advantage of variation within the present – the distribution of biodiversity and metabolic strategies across geochemical gradients – to recognize the extent of diversity and the reasons that it exists. -
The Distribution and Evolution of Small Non-Coding Rnas in Archaea in Light of New Archaeal Phyla
THE DISTRIBUTION AND EVOLUTION OF SMALL NON-CODING RNAS IN ARCHAEA IN LIGHT OF NEW ARCHAEAL PHYLA A thesis submitted in partial fulfilment of the requirements for the Degree of Master of Science in Biological Sciences at the University of Canterbury by Laura A.A. Grundy University of Canterbury 2016 Table of Contents Table of Contents...................................................................................................... 2 Acknowledgements ................................................................................................... 4 Abstract..................................................................................................................... 5 Chapter One - Introduction ..................................................................................... 6 Overview ............................................................................................................... 6 The Archaeal Domain of Life ................................................................................. 6 Metagenomics and the Availability of Genomic Data ......................................... 6 The History of Archaeal Taxa ............................................................................ 7 Archaeal Similarities to the Bacteria and Eukaryotes......................................... 9 Small Non-Coding RNA....................................................................................... 10 RNA................................................................................................................