Using Polymerase Chain Reaction (PCR) Melting Profile and Protein Fingerprint Profile Analyses to Identify Methanothermobacter Marburgensis DX01

Total Page:16

File Type:pdf, Size:1020Kb

Using Polymerase Chain Reaction (PCR) Melting Profile and Protein Fingerprint Profile Analyses to Identify Methanothermobacter Marburgensis DX01 African Journal of Microbiology Research Vol. 5(26) pp. 4555-4561, 16 November, 2011 Available online at http://www.academicjournals.org/AJMR ISSN 1996-0808 ©2011 Academic Journals DOI: 10.5897/AJMR11.586 Full Length Research Paper Using polymerase chain reaction (PCR) melting profile and protein fingerprint profile analyses to identify Methanothermobacter marburgensis DX01 Xia Ding1*, Xiao-Jue Peng1, Wen-Zhuo Li1, Yao-Hui Cai2 and Wei-Jun Yang3 1College of Life Sciences, Nanchang University, Nanchang, Jiangxi, 330031, China. 2Jiangxi Academy of Agricultural Sciences, Nanchang, Jiangxi, 330000, China. 3College of Life Sciences, Zhejiang University, Hangzhou, Zhejiang, 310058, China. Accepted 17 October, 2011 A thermophilic new strain of Methanothermobacter marburgensis DX01, with a different morphology from M. thermautotrophicus delta H, was isolated from a hot spring in China. To provide further molecular evidence to identify the methanogen M. marburgensis DX01, polymerase chain reaction melting profile (PCR MP) technique and protein fingerprint profiling were performed. Both DNA and protein fingerprint profiles showed significant differences between M. marburgensis DX01 and M. thermautotrophicus delta H. In addition, five interesting DNA fragments obtained from PCR MP of the DX01 strain were excised and sequenced. We found that all five DNA fragments were unique to M. marburgensis DX01. Expression of induced proteins in M. marburgensis DX01 was analyzed by protein fingerprint profiling and a protein that was more highly expressed at 70°C was excised and identified by N-terminal amino acid sequencing. We found that the up-regulated protein was Methyl-coenzyme M reductase І, which was 97.6% amino acid sequence identity with that of M. thermautotrophicus delta H. These studies may provide clues for a better understanding of the new isolate of thermophilic M. marburgensis. Key words: Methanothermobacter, polymerase chain reaction (PCR) melting profile, protein fingerprint profile analyses. INTRODUCTION There are a large number of extremely thermophilic anaerobic digesters, digested sludge and hot springs. organisms in the archaeal domain (de Poorter et al., Although these strains were assigned to a single species, 2007; Schill et al., 1996). The thermophilic species of there are still certain differences between the strains. Methanothermobacter are able to produce their energy With the development of new taxonomy techniques, from the oxidation of H2 and reduction of CO2 to methane various taxonomic subdivisions of Methanothermobacter (Valentine, 2007). Growth of Methanothermobacter is into separate species have been proposed. In 2001, characterized by a requirement for gaseous energy and Methanothermobacter was redefined as carbon sources and low biomass. In addition, Methanothermobacter defluvii, Methanothermobacter Methanothermobacter is thermophilic and strictly marburgensis, Methanothermobacter thermautotrophicus, anaerobic (Farhoud et al., 2005; Schill et al., 1996). Methanothermobacter thermoflexus, Currently, over ten Methanothermobacter strains have Methanothermobacter thermophilus and been found in a number of environments, including Methanothermobacter wolfeii, as cited in the second edition of the Bergey’s Manual of Systematic Bacteriology and published in the validation list no. 85. Over the past 20 years, a large number of DNA-based *Corresponding author. E-mail:[email protected]. Tel: +86 techniques have been introduced into the field of 791 3969163. Fax: +86 7913. microbial characterization and taxonomy. These include 4556 Afr. J. Microbiol. Res. restriction endonuclease analysis, molecular NiCl2∙6H2O 0.025 g; NaSeO3∙6 H2O 0.0003 g). After adjustment to hybridization, and PCR amplification; most of these pH 7.0, the medium was prepared and sterilized under a strictly anaerobic H2 and CO2 atmosphere (80:20). techniques use PCR for detection of fragments (Dnyaneshwar et al., 2006; Frias-Lopez et al., 2008; Krawczyk et al., 2006; Lopez-Ribot et al., 2000; Pandya Electron microscopy (EM) at different growth temperature et al., 2009). These genomic fingerprinting methods were Strains were grown to late exponential phase at different incubation developed to detect DNA sequence polymorphisms by temperatures (50, 60, 65 and 70°C). The electronic graph was using general principles such as restriction fragment performed using electron microscopy (EM). length polymorphisms (RFLPs) (Botstein et al., 1980), random amplification of polymorphic DNA (RAPD) (Williams et al., 1990), or repetitive element PCR (rep- DNA extraction PCR) (Georghiou et al., 1994). Chromosomal DNA was obtained using previously described Nowadays, physiological characterization, phylogenetic methods (Jarrell et al., 1992). Total DNA was quantified on a analysis of the 16S rRNA, DNA-DNA hybridization, Genova UV/visible spectrophotometer at 260 nm. analysis of the GC percentage, antigenic fingerprinting, and plasmid and phage typing have all been used for Ligation mediated PCR performed at low denaturation type strains of Methanothermobacter (Wasserfallen et al., temperatures (PCR melting profiles) 2000). The performance and convenience of the PCR melting profile (PCR MP) technique, which is based on The PCR melting profile (PCR MP) was performed according to using low denaturation temperatures during ligation previously described methods (Masny and Plucienniczak, 2003). mediated PCR (LM PCR) of bacterial DNA, demonstrates Briefly, genomic DNA was digested with HindIII. Digested DNA was ligated with two oligonucleotides forming an adaptor: POWIE 5'- that PCR MP is a rapid method that offers good CTCACTCTCACCAACGTCGAC-3' and HINLIG 5'- discriminatory power (Krawczyk et al., 2009; Krawczyk et AGCTGTCGACGTTGG-3'. The ligation products were used in the al., 2007; Krawczyk et al., 2006; Masny and next round of PCR as an amplification template with primer Plucienniczak, 2003; Mueller et al., 2001; Ngoc et al., POWAGCTT 5'-CTCACTCTCACCAACGTCGACAGCTT-3'. PCRs 2008). were performed by incubating the samples for 2 min at 72°C to A new thermophilic archaea M. marburgensis DX01 release unligated HINLIG oligonucleotides, followed by the addition of 1 µl of Taq DNA polymerase (2.5 U/μl). The reaction mixture was was isolated from a hot spring in China (Ding et al., incubated for an additional 5 min at 72°C to fill in the single- 2010). The isolate showed some distinct phenotypic stranded ends and create amplicons, after which the samples were characteristics in pellet color and morphology. Previously, initially denatured at (80 + x) °C for 1 min, followed by 21 cycles of M. marburgensis and M. thermautotrophicus were denaturation at (80 + x) °C for 40 s, with annealing and elongation thought to belong to the same species: at 72°C for 2 min (where x is a digit between 0 and 8, and is constant for a single PCR reaction). Methanobacterium thermoautotrophicum. Strain delta H was a type strain. The two species exhibited extremely similar physiological characteristics. However, DNA-DNA Comparison of PCR MPs of two strains hybridization studies revealed they lacked similarity in The products of PCR MPs were separated by 2% agarose gels. sequence (Wasserfallen et al., 2000). The differences Electrophoresis was performed in 1·Tris–acetate–EDTA buffer at 50 between the two species in genomic sequence and V. Gels were stained by ethidium bromide. Interesting DNA protein expression were still unknown. Additionally, it was fragments were recovered from the agarose gel using the Agarose not known whether the new DX10 strain possessed Gel DNA Fragment Recovery Kit (TaKaRa, Dalian, China). unique genes. In the present study, to provide further Recovered PCR product was ligated into the pUCm-T vector (TaKaRa, Dalian, China) and transformed into E. coli DH5α cells. molecular evidence of the difference between the strains, The cloning procedure was conducted according to the PCR MP and protein fingerprint profiles were used to manufacturer’s instructions. Sequencing reactions were run on an create a more complete picture of the variation in Applied Biosystems 3730 sequencer (Invitrogen, Shanhai, China). genomes and protein expression to fingerprint a novel methanogen strain DX01. N-terminal protein sequencing MATERIALS AND METHODS Purified proteins from the fractions were first separated by SDS- PAGE and then transferred via electroblot onto PVDF membranes. Culturing Protein bands on the PVDF membrane were visualized by staining with G-250 Coomassie stain solution, after which protein bands of Methanothermobacter strains were grown in anaerobic medium interest with the correct molecular weight were cleaved and the N- using the Hungate technique (Balch et al., 1979). The culture terminal amino acid sequence was determined on the Procise- -1 medium contained (L ): MgCl2·6H2O, 0.1 g; NaCl 0.6 g; K2HPO4, Protein Sequencing System (Applied Biosystems) using the 1.5 g; NH4Cl, 1.5 g; sodium cysteine 0.5 g; NaHCO3, 1.0 g; sodium manufacturer’s pulse-liquid Edman degradation chemistry cycles. resazurin 0.001 g; trace element solution 10 ml (MgSO ∙7H O 3 g; 4 2 MnSO4∙4H2O 0.5 g; NaCl 10 g; FeSO4∙7H2O 0.1 g; CoCl2∙6H2O 0.1 Cloning and nucleotide sequencing g; CaCl2∙2H2O 0.1 g; ZnSO4∙7H2O 0.1 g; CuSO4 0.01 g; KAl(SO4)2∙12H2O 0.01 g; H3BO3 0.01 g; Na2MoO4∙2H2O 0.01 g; Degenerate primers (5'-ATG ATA TGG CAC AAT ACT A-3' and 5'- Ding et al. 4557 Figure 1. Morphology of M. marburgensis DX01. (a) Color of the cell pellet. (b) Electron microscopy of cells grown at 50°C (A, E), 60°C (B, F), 65°C
Recommended publications
  • Can Methanogens Grow in a Perchlorate Environment on Mars? T.A
    72nd Annual Meteoritical Society Meeting (2009) 5136.pdf CAN METHANOGENS GROW IN A PERCHLORATE ENVIRONMENT ON MARS? T.A. Kral1,2, T. Goodhart1, K.L. Howe2 and P. Gavin2. 1Department of Biological Sciences, University of Arkansas, Fayetteville, AR 72701, 2Arkansas Cen- ter for Space and Planetary Sciences, University of Arkansas, Fayetteville, AR 72701. [email protected]. Introduction: We have been studying methanogens as a model for life on Mars for a number of years now. Methanogens are microorganism in the domain Archaea that use carbon diox- ide as a carbon source, molecular hydrogen as an energy source, produce methane as a by-product of metabolism, and have been shown to grow on a Mars soil simulant, JSC Mars-1 (1). The relatively recent discovery of methane in the Martian atmosphere has added relevance to these types of studies (2). In 2008, The Mars Phoenix Lander discovered perchlorate at its landing site in concentrations of approximately 1.0wt% (3). Because of perchlo- rate’s powerful oxidizing property, many believed that the chances for extant life on the planet had decreased. Methods: The research reported here was designed to de- termine if methanogens could grow in the presence of three dif- ferent perchlorate salts. The methanogens tested were Methanothermobacter wolfeii, Methanosarcina barkeri, Metha- nobacterium formicicum and Methanococcus maripaludis. Stan- dard growth media were prepared containing 0, 0.1, 0.5 and 1.0wt% magnesium perchlorate, sodium perchlorate, or potas- sium perchlorate. Organisms were inoculated into their respective media followed by incubation at each organism’s optimal growth temperature. Methane production, commonly used to measure methanogen growth, was measured by gas chromatography of headspace samples.
    [Show full text]
  • Bacteria and Archaea - Aharon Oren
    PHYLOGENETIC TREE OF LIFE - Bacteria And Archaea - Aharon Oren BACTERIA AND ARCHAEA Aharon Oren The Institute of Life Sciences, The Hebrew University of Jerusalem, Jerusalem, Israel. Keywords: Archaea, Bacteria, Bacteriological Code, Bergey‟s Manual, Nomenclature, Phylogenetic tree, Polyphasic taxonomy, Prokaryotes, 16S rRNA, Taxonomy, Species concept, Systematics Contents 1. Prokaryotes: The unseen majority 2. The species concept for the Prokaryotes 3. Bacteria and Archaea, the two domains of the prokaryotic world 4. The differences between Bacteria and Archaea 5. The Prokaryotes – a taxonomic overview 5.1. General considerations 5.2. The phyla of Bacteria 5.3. The phyla of Archaea 6. Prokaryotes: The uncultured majority Glossary Bibliography Biographical sketch Summary With an estimated number of 4-6x1030 cells, the prokaryotes are the most numerous organisms on earth. They inhabited our planet long before the eukaryotes evolved, and metabolically they are the most diverse group. Compared to the number of eukaryotic taxa the number of prokaryote genera and species described is surprisingly small. A little over 9,000 different species of prokaryotes have been named, and classified in nearly 2,000 genera. The naming of prokaryotes is regulated by the International Code of Nomenclature of Prokaryotes. Internationally approved rules for naming species exist, but there is no universally accepted species concept for the prokaryotes. For the description of new representatives a polyphasic approach is used, which includes determination of numerous phenotypic and genotypic properties. If necessary, the genomes of related strains are compared by DNA-DNA hybridization or full or partial genome sequence comparison. Since the 1970s comparative sequence analysis of small- subunit ribosomal RNA has revolutionized our views of prokaryote taxonomy.
    [Show full text]
  • Fmicb-11-00948 May 15, 2020 Time: 16:54 # 1
    UvA-DARE (Digital Academic Repository) Stromatolites as Biosignatures of Atmospheric Oxygenation Carbonate Biomineralization and UV-C Resilience in a Geitlerinema sp. - Dominated Culture Popall, R.M.; Bolhuis, H.; Muyzer, G.; Sánchez-Román, M. DOI 10.3389/fmicb.2020.00948 Publication date 2020 Document Version Final published version Published in Frontiers in Microbiology License CC BY Link to publication Citation for published version (APA): Popall, R. M., Bolhuis, H., Muyzer, G., & Sánchez-Román, M. (2020). Stromatolites as Biosignatures of Atmospheric Oxygenation: Carbonate Biomineralization and UV-C Resilience in a Geitlerinema sp. - Dominated Culture. Frontiers in Microbiology, 11, [948]. https://doi.org/10.3389/fmicb.2020.00948 General rights It is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), other than for strictly personal, individual use, unless the work is under an open content license (like Creative Commons). Disclaimer/Complaints regulations If you believe that digital publication of certain material infringes any of your rights or (privacy) interests, please let the Library know, stating your reasons. In case of a legitimate complaint, the Library will make the material inaccessible and/or remove it from the website. Please Ask the Library: https://uba.uva.nl/en/contact, or a letter to: Library of the University of Amsterdam, Secretariat, Singel 425, 1012 WP Amsterdam, The Netherlands. You will be contacted as soon as possible. UvA-DARE is a service provided by the library of the University of Amsterdam (https://dare.uva.nl) Download date:05 Oct 2021 fmicb-11-00948 May 15, 2020 Time: 16:54 # 1 ORIGINAL RESEARCH published: 19 May 2020 doi: 10.3389/fmicb.2020.00948 Stromatolites as Biosignatures of Atmospheric Oxygenation: Carbonate Biomineralization and UV-C Resilience in a Geitlerinema sp.
    [Show full text]
  • Protein Complexing in a Methanogen Suggests Electron Bifurcation and Electron Delivery from Formate to Heterodisulfide Reductase
    Protein complexing in a methanogen suggests electron bifurcation and electron delivery from formate to heterodisulfide reductase Kyle C. Costaa,b, Phoebe M. Wonga, Tiansong Wanga,c, Thomas J. Liea, Jeremy A. Dodswortha,b,1, Ingrid Swansona, June A. Burna, Murray Hackettc, and John A. Leigha,b,2 aDepartment of Microbiology, bNational Science Foundation Integrative Graduate Education Research Traineeship Program in Astrobiology, and cDepartment of Chemical Engineering, University of Washington, Seattle, WA 98195 Edited by William Metcalf, University of Illinois, Urbana, IL, and accepted by the Editorial Board May 6, 2010 (received for review March 19, 2010) In methanogenic Archaea, the final step of methanogenesis gen- Most methanogens can use H2 as the electron donor, and many fi erates methane and a heterodisul de of coenzyme M and co- can also use formate. Reduced coenzyme F420 (F420H2)isarequired fi enzyme B (CoM-S-S-CoB). Reduction of this heterodisul de by intermediate, and can be generated from H2 by F420-reducing hy- fi heterodisul de reductase to regenerate HS-CoM and HS-CoB is an drogenase (Fru) or by a cycle involving the enzymes H2-dependent Nat Rev Micro- exergonic process. Thauer et al. [Thauer, et al. 2008 methylene-H4MPT dehydrogenase and F420-dependent methylene- biol – 6:579 591] recently suggested that in hydrogenotrophic metha- H4MPT dehydrogenase (2). When formate is the electron donor, fi nogens the energy of heterodisul de reduction powers the most it is oxidized to CO2 by a formate dehydrogenase (Fdh) that endergonic reaction in the pathway, catalyzed by the formylmetha- yields F420H2. nofuran dehydrogenase, via flavin-based electron bifurcation.
    [Show full text]
  • Geochemical Cycles on Present-Day Earth @Methanojen 2019 Sagan Exoplanet Summer Workshop “Astrobiology for Astronomers” July 15, 2019
    Geochemical Cycles on Present-Day Earth @methanoJen www.JenniferGlass.com 2019 Sagan Exoplanet Summer Workshop “AstroBiology for Astronomers” July 15, 2019 Artwork by Sam Walton On Earth, O2 and CH4 have no significant abiotic sources N2 78.08% O2 20.95% Ar 0.93% CO2 0.0407% Ne 0.0018% He 0.000524% CH4 0.00018% I. Modern Cycle Biological Methanogenesis 4H2 + CO2 CH4 + 2H2O 0-120°C no O2 46 Fe-S clusters in first enzyme: FWD NicKel cofactor F430 in last Wagner et al., 2016, Science enzyme (MCR) ABiotic Methane Production 4H2 + CO2 CH4 + 2H2O “Fischer- Tropsch 3H + CO CH + H O Process” 2 4 2 150–300 °C Abiotic reactions are sluggish at low temperatures without mineral catalysts (Seewald et al. 2006, McCollom 2016) Methane production is overwhelmingly Biological “Abiotic methane production estimates from serpentinization ranging between approximately 1/30th and 1/150th the present biotic flux appear reasonable for modern Earth.” - Arney et al., 2018, Astrobiology Serpentinization: Source of Hydrogen olivine water serpentine hydrogen Biological methane emissions to the atmosphere Lyu Z, Shao N, Akinyemi T, Whitman WB (2018) Methanogenesis. Current Biology 28: R727-R732 Methane cycling prior to release to atmosphere Dean JF, Middelburg JJ, Röckmann T., Aerts R, Blauw LG, Egger M, et al (2018). Methane feedbacks to the global climate system in a warmer world. Reviews of Geophysics, 56, 207–250. The major sinks for atmospheric methane is photolytic destruction, which depends on OH radicals Modern methane’s atmospheric lifetime is ~10 years May not go quite as fast in atmosphere without oxygen Natural Methane Sources and Sinks (Tg yr-1) Tropo- Geological spheric OH sources Soil oxidation Wet- Fresh- lands Hydrates waters Anthropogenic Methane Sources and Sinks (Tg yr-1) Biomass Landfills & Rice Rumi- Termites Fossil nants burning waste fuels Tropo- Geological spheric OH sources Soil oxidation Wet- Fresh- lands Hydrates waters MicroBial methane makers: Euryarchaeota Bacteria Archaea Eukaryotes Castelle & Banfield 2018 Cell Sorokin et al.
    [Show full text]
  • Effect of N on Biological Methanation in a Continuous Stirred-Tank
    fermentation Article Effect of N2 on Biological Methanation in a Continuous Stirred-Tank Reactor with Methanothermobacter marburgensis Marc Philippe Hoffarth *,†, Timo Broeker and Jan Schneider Institute for Food Technology.NRW (ILT.NRW), Ostwestfalen-Lippe University of Applied Sciences and Arts, 32657 Lemgo, Germany * Correspondence: [email protected]; Tel.: +49-5261-7025769 † Current address: Ostwestfalen-Lippe University of Applied Sciences and Arts, Campusallee 12, 32657 Lemgo, Germany. Received: 20 May 2019; Accepted: 28 June 2019 ; Published: 2 July 2019 Abstract: In this contribution, the effect of the presence of a presumed inert gas like N2 in the feed gas on the biological methanation of hydrogen and carbon dioxide with Methanothermobacter marburgensis was investigated. N2 can be found as a component besides CO2 in possible feed gases like mine gas, weak gas, or steel mill gas. To determine whether there is an effect on the biological methanation of CO2 and H2 from renewable sources or not, the process was investigated using feed gases containing CO2,H2, and N2 in different ratios, depending on the CO2 content. A possible effect can be a lowered conversion rate of CO2 and H2 to CH4. Feed gases containing up to 47% N2 were investigated. The conversion of hydrogen and carbon dioxide was possible with a conversion rate of up to 91% but was limited by the amount of H2 when feeding a stoichiometric ratio of 4:1 and not by adding N2 to the feed gas. Keywords: biological methanation; CSTR; Methanothermobacter marburgensis; methane; carbon dioxide; dinitrogen; hydrogen; power-to-gas 1. Introduction Today’s demand for energy all over the world makes it necessary to reduce the use of fossil energy sources to a minimum.
    [Show full text]
  • Genome-Centric View of Carbon Processing in Thawing Permafrost Ben J
    ARTICLE https://doi.org/10.1038/s41586-018-0338-1 Genome-centric view of carbon processing in thawing permafrost Ben J. Woodcroft1,10, Caitlin M. Singleton1,10, Joel A. Boyd1, Paul N. Evans1, Joanne B. Emerson2,9, Ahmed A. F. Zayed2, Robert D. Hoelzle1, Timothy O. Lamberton1, Carmody K. McCalley3, Suzanne B. Hodgkins4, Rachel M. Wilson4, Samuel O. Purvine5, Carrie D. Nicora5, Changsheng Li6, Steve Frolking6, Jeffrey P. Chanton4, Patrick M. Crill7, Scott R. Saleska8, Virginia I. Rich2 & Gene W. Tyson1* As global temperatures rise, large amounts of carbon sequestered in permafrost are becoming available for microbial degradation. Accurate prediction of carbon gas emissions from thawing permafrost is limited by our understanding of these microbial communities. Here we use metagenomic sequencing of 214 samples from a permafrost thaw gradient to recover 1,529 metagenome-assembled genomes, including many from phyla with poor genomic representation. These genomes reflect the diversity of this complex ecosystem, with genus-level representatives for more than sixty per cent of the community. Meta-omic analysis revealed key populations involved in the degradation of organic matter, including bacteria whose genomes encode a previously undescribed fungal pathway for xylose degradation. Microbial and geochemical data highlight lineages that correlate with the production of greenhouse gases and indicate novel syntrophic relationships. Our findings link changing biogeochemistry to specific microbial lineages involved in carbon processing, and provide key information for predicting the effects of climate change on permafrost systems. Permafrost thaw induced by climate change is predicted to make up to measurements were taken at each site from four active layer depths 174 Pg of near-surface carbon (less than 3 m below the surface) avail- (near surface, mid, deep and extra-deep; 1–51 cm; Fig.
    [Show full text]
  • User's Guide: Manual for Metaxa2.2
    User's guide: Manual for Metaxa2.2 This is a guide on how to install and use the software utility Metaxa2, version 2.2. The software is written for Unix-like platforms, and should work on nearly all Linux-based systems, as well as macOS. Contents of this manual 1. Detailed installation instructions 2. Changes from previous versions of Metaxa 3. Usage and commands 4. Output files 5. Metaxa2 Taxonomic Traversal Tool 6. Metaxa2 Diversity Tools 7. Metaxa2 Database Builder 8. The Metaxa2 Database Repository 9. Internal changes in Metaxa2 10. Running the analysis steps of Metaxa2 separately 11. ‘Undocumented’ features 12. License information 1. Detailed installation instructions The README.txt file bundled with the script provides a quick installation guide. In order to install certain packages, you might need to have superuser privileges. For installation on Mac, you have to install the Apple Xcode Command Line Tools package, if that is not already installed, in order to compile the required programs. Please talk to your system administrator if you are unsure about these steps. Note that the package is mandatory and that you should not proceed unless these criteria are fulfilled. [If you don’t have superuser privileges on your machine: Create a directory within your user directory, e.g. /home/user/bin/, and store all required binaries there. By adding this directory to your PATH, any software placed in the directory will behave as if installed for all users using superuser privileges. If you use the bash shell, you can add a bin directory to your PATH, by adding the line “export PATH=$PATH:$HOME/bin/:.” to the file .profile in your home directory.
    [Show full text]
  • Application for Approval to Import Into Containment Any New Organism That
    ER-AN-02N 10/02 Application for approval to import into FORM 2N containment any new organism that is not genetically modified, under Section 40 of the Page 1 Hazardous Substances and New Organisms Act 1996 FORM NO2N Application for approval to IMPORT INTO CONTAINMENT ANY NEW ORGANISM THAT IS NOT GENETICALLY MODIFIED under section 40 of the Hazardous Substances and New Organisms Act 1996 Application Title: Importation of extremophilic microorganisms from geothermal sites for research purposes Applicant Organisation: Institute of Geological & Nuclear Sciences ERMA Office use only Application Code: Formally received:____/____/____ ERMA NZ Contact: Initial Fee Paid: $ Application Status: ER-AN-02N 10/02 Application for approval to import into FORM 2N containment any new organism that is not genetically modified, under Section 40 of the Page 2 Hazardous Substances and New Organisms Act 1996 IMPORTANT 1. An associated User Guide is available for this form. You should read the User Guide before completing this form. If you need further guidance in completing this form please contact ERMA New Zealand. 2. This application form covers importation into containment of any new organism that is not genetically modified, under section 40 of the Act. 3. If you are making an application to import into containment a genetically modified organism you should complete Form NO2G, instead of this form (Form NO2N). 4. This form, together with form NO2G, replaces all previous versions of Form 2. Older versions should not now be used. You should periodically check with ERMA New Zealand or on the ERMA New Zealand web site for new versions of this form.
    [Show full text]
  • Post-Transcriptional Modification Characterizing and Mapping of Archaea Trnas Using Liquid Chromatography with Tandem Mass Spectrometry
    Post-transcriptional Modification Characterizing and Mapping of Archaea tRNAs Using Liquid Chromatography with Tandem Mass Spectrometry A dissertation submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of Doctor of Philosophy (PhD) in the Department of Chemistry of the McMicken College of Arts and Sciences by Ningxi Yu M. Sc. Chemistry, Central China Normal University, 2012 B. Eng. Wuhan Institute of Technology, 2009 October 2018 Committee Chair: Patrick A. Limbach, Ph.D i Abstract This dissertation is focused on exploring the transfer RNA modification profiles in archaea. Transfer RNA (tRNA) plays a key role in decoding the genetic information on messenger RNA (mRNA), and the post-transcriptional modification within tRNAs shape the decoding strategies in different organisms. Bacteria have been extensively studied in term of types and positions of tRNA modifications, and a few eukaryotic organisms have also been investigated. However, our knowledge of tRNA modifications in archaea is still limited. While the modifications in multiple archaeal organisms have been identified, the only sets of tRNA sequences whose modification have been localized to particular tRNAs is from Haloferax volcanii. To improve our understanding of archaeal tRNA modification profiles and decoding strategies, I have used liquid chromatography and tandem mass spectrometry to localize post-transcriptional modifications of selected archaeal organisms. A computational tool has been developed for MS/MS data interpretation and RNA sequence annotation. By using this tool, the modifications were localized to tRNA sequences from five archaeal organisms. Among the five selected organisms, the modifications in the anticodon of Methanocaldococcus jannaschii tRNAs have been fully identified, and the first compilation of modified tRNA sequences of this archaea have been generated.
    [Show full text]
  • Unraveling the Microbiome of a Thermophilic Biogas Plant By
    Maus et al. Biotechnol Biofuels (2016) 9:171 DOI 10.1186/s13068-016-0581-3 Biotechnology for Biofuels RESEARCH Open Access Unraveling the microbiome of a thermophilic biogas plant by metagenome and metatranscriptome analysis complemented by characterization of bacterial and archaeal isolates Irena Maus1, Daniela E. Koeck2, Katharina G. Cibis3, Sarah Hahnke4, Yong S. Kim5, Thomas Langer4, Jana Kreubel3, Marcel Erhard6, Andreas Bremges1,7, Sandra Off5, Yvonne Stolze1, Sebastian Jaenicke8, Alexander Goesmann8, Alexander Sczyrba1,7, Paul Scherer5, Helmut König3, Wolfgang H. Schwarz2, Vladimir V. Zverlov2, Wolfgang Liebl2, Alfred Pühler1, Andreas Schlüter1 and Michael Klocke4* Abstract Background: One of the most promising technologies to sustainably produce energy and to mitigate greenhouse gas emissions from combustion of fossil energy carriers is the anaerobic digestion and biomethanation of organic raw material and waste towards biogas by highly diverse microbial consortia. In this context, the microbial systems ecol- ogy of thermophilic industrial-scale biogas plants is poorly understood. Results: The microbial community structure of an exemplary thermophilic biogas plant was analyzed by a com- prehensive approach comprising the analysis of the microbial metagenome and metatranscriptome comple- mented by the cultivation of hydrolytic and acido-/acetogenic Bacteria as well as methanogenic Archaea. Analysis of metagenome-derived 16S rRNA gene sequences revealed that the bacterial genera Defluviitoga (5.5 %), Halocella (3.5 %), Clostridium
    [Show full text]
  • Temperature and Inoculum Origin Influence the Performance of Ex-Situ Biological Hydrogen Methanation
    molecules Article Temperature and Inoculum Origin Influence the Performance of Ex-Situ Biological Hydrogen Methanation Noémie Figeac 1,2, Eric Trably 1, Nicolas Bernet 1 , Jean-Philippe Delgenès 1 and Renaud Escudié 1,* 1 INRAE, University of Montpellier, LBE, 102 Avenue des Etangs, 11100 Narbonne, France; noemie.fi[email protected] (N.F.); [email protected] (E.T.); [email protected] (N.B.); [email protected] (J.-P.D.) 2 French Environment and Energy Management Agency, 20 Avenue du Grésillé- BP 90406, CEDEX 01, 49004 Angers, France * Correspondence: [email protected]; Tel.: +33-4684-251-73 Received: 22 October 2020; Accepted: 29 November 2020; Published: 1 December 2020 Abstract: The conversion of H2 into methane can be carried out by microorganisms in a process so-called biomethanation. In ex-situ biomethanation H2 and CO2 gas are exogenous to the system. One of the main limitations of the biomethanation process is the low gas-liquid transfer rate and solubility of H2 which are strongly influenced by the temperature. Hydrogenotrophic methanogens that are responsible for the biomethanation reaction are also very sensitive to temperature variations. The aim of this work was to evaluate the impact of temperature on batch biomethanation process in mixed culture. The performances of mesophilic and thermophilic inocula were assessed at 4 temperatures (24, 35, 55 and 65 ◦C). A negative impact of the low temperature (24 ◦C) was observed on microbial kinetics. Although methane production rate was higher at 55 and 65 ◦C (respectively 290 55 and 309 109 mL CH /L.day for the mesophilic inoculum) than at 24 and ± ± 4 35 C (respectively 156 41 and 253 51 mL CH /L.day), the instability of the system substantially ◦ ± ± 4 increased, likely because of a strong dominance of only Methanothermobacter species.
    [Show full text]