Abstract Metagenomic Analysis of Deep-Branching
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Corynebacterium Sp.|NML98-0116
1 Limnochorda_pilosa~GCF_001544015.1@NZ_AP014924=Bacteria-Firmicutes-Limnochordia-Limnochordales-Limnochordaceae-Limnochorda-Limnochorda_pilosa 0,9635 Ammonifex_degensii|KC4~GCF_000024605.1@NC_013385=Bacteria-Firmicutes-Clostridia-Thermoanaerobacterales-Thermoanaerobacteraceae-Ammonifex-Ammonifex_degensii 0,985 Symbiobacterium_thermophilum|IAM14863~GCF_000009905.1@NC_006177=Bacteria-Firmicutes-Clostridia-Clostridiales-Symbiobacteriaceae-Symbiobacterium-Symbiobacterium_thermophilum Varibaculum_timonense~GCF_900169515.1@NZ_LT827020=Bacteria-Actinobacteria-Actinobacteria-Actinomycetales-Actinomycetaceae-Varibaculum-Varibaculum_timonense 1 Rubrobacter_aplysinae~GCF_001029505.1@NZ_LEKH01000003=Bacteria-Actinobacteria-Rubrobacteria-Rubrobacterales-Rubrobacteraceae-Rubrobacter-Rubrobacter_aplysinae 0,975 Rubrobacter_xylanophilus|DSM9941~GCF_000014185.1@NC_008148=Bacteria-Actinobacteria-Rubrobacteria-Rubrobacterales-Rubrobacteraceae-Rubrobacter-Rubrobacter_xylanophilus 1 Rubrobacter_radiotolerans~GCF_000661895.1@NZ_CP007514=Bacteria-Actinobacteria-Rubrobacteria-Rubrobacterales-Rubrobacteraceae-Rubrobacter-Rubrobacter_radiotolerans Actinobacteria_bacterium_rbg_16_64_13~GCA_001768675.1@MELN01000053=Bacteria-Actinobacteria-unknown_class-unknown_order-unknown_family-unknown_genus-Actinobacteria_bacterium_rbg_16_64_13 1 Actinobacteria_bacterium_13_2_20cm_68_14~GCA_001914705.1@MNDB01000040=Bacteria-Actinobacteria-unknown_class-unknown_order-unknown_family-unknown_genus-Actinobacteria_bacterium_13_2_20cm_68_14 1 0,9803 Thermoleophilum_album~GCF_900108055.1@NZ_FNWJ01000001=Bacteria-Actinobacteria-Thermoleophilia-Thermoleophilales-Thermoleophilaceae-Thermoleophilum-Thermoleophilum_album -
Supporting Information
Supporting Information Lozupone et al. 10.1073/pnas.0807339105 SI Methods nococcus, and Eubacterium grouped with members of other Determining the Environmental Distribution of Sequenced Genomes. named genera with high bootstrap support (Fig. 1A). One To obtain information on the lifestyle of the isolate and its reported member of the Bacteroidetes (Bacteroides capillosus) source, we looked at descriptive information from NCBI grouped firmly within the Firmicutes. This taxonomic error was (www.ncbi.nlm.nih.gov/genomes/lproks.cgi) and other related not surprising because gut isolates have often been classified as publications. We also determined which 16S rRNA-based envi- Bacteroides based on an obligate anaerobe, Gram-negative, ronmental surveys of microbial assemblages deposited near- nonsporulating phenotype alone (6, 7). A more recent 16S identical sequences in GenBank. We first downloaded the gbenv rRNA-based analysis of the genus Clostridium defined phylo- files from the NCBI ftp site on December 31, 2007, and used genetically related clusters (4, 5), and these designations were them to create a BLAST database. These files contain GenBank supported in our phylogenetic analysis of the Clostridium species in the HGMI pipeline. We thus designated these Clostridium records for the ENV database, a component of the nonredun- species, along with the species from other named genera that dant nucleotide database (nt) where 16S rRNA environmental cluster with them in bootstrap supported nodes, as being within survey data are deposited. GenBank records for hits with Ͼ98% these clusters. sequence identity over 400 bp to the 16S rRNA sequence of each of the 67 genomes were parsed to get a list of study titles Annotation of GTs and GHs. -
Crystalline Iron Oxides Stimulate Methanogenic Benzoate Degradation in Marine Sediment-Derived Enrichment Cultures
The ISME Journal https://doi.org/10.1038/s41396-020-00824-7 ARTICLE Crystalline iron oxides stimulate methanogenic benzoate degradation in marine sediment-derived enrichment cultures 1,2 1 3 1,2 1 David A. Aromokeye ● Oluwatobi E. Oni ● Jan Tebben ● Xiuran Yin ● Tim Richter-Heitmann ● 2,4 1 5 5 1 2,3 Jenny Wendt ● Rolf Nimzyk ● Sten Littmann ● Daniela Tienken ● Ajinkya C. Kulkarni ● Susann Henkel ● 2,4 2,4 1,3 2,3,4 1,2 Kai-Uwe Hinrichs ● Marcus Elvert ● Tilmann Harder ● Sabine Kasten ● Michael W. Friedrich Received: 19 May 2020 / Revised: 9 October 2020 / Accepted: 22 October 2020 © The Author(s) 2020. This article is published with open access Abstract Elevated dissolved iron concentrations in the methanic zone are typical geochemical signatures of rapidly accumulating marine sediments. These sediments are often characterized by co-burial of iron oxides with recalcitrant aromatic organic matter of terrigenous origin. Thus far, iron oxides are predicted to either impede organic matter degradation, aiding its preservation, or identified to enhance organic carbon oxidation via direct electron transfer. Here, we investigated the effect of various iron oxide phases with differing crystallinity (magnetite, hematite, and lepidocrocite) during microbial 1234567890();,: 1234567890();,: degradation of the aromatic model compound benzoate in methanic sediments. In slurry incubations with magnetite or hematite, concurrent iron reduction, and methanogenesis were stimulated during accelerated benzoate degradation with methanogenesis as the dominant electron sink. In contrast, with lepidocrocite, benzoate degradation, and methanogenesis were inhibited. These observations were reproducible in sediment-free enrichments, even after five successive transfers. Genes involved in the complete degradation of benzoate were identified in multiple metagenome assembled genomes. -
Table S5. the Information of the Bacteria Annotated in the Soil Community at Species Level
Table S5. The information of the bacteria annotated in the soil community at species level No. Phylum Class Order Family Genus Species The number of contigs Abundance(%) 1 Firmicutes Bacilli Bacillales Bacillaceae Bacillus Bacillus cereus 1749 5.145782459 2 Bacteroidetes Cytophagia Cytophagales Hymenobacteraceae Hymenobacter Hymenobacter sedentarius 1538 4.52499338 3 Gemmatimonadetes Gemmatimonadetes Gemmatimonadales Gemmatimonadaceae Gemmatirosa Gemmatirosa kalamazoonesis 1020 3.000970902 4 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas indica 797 2.344876284 5 Firmicutes Bacilli Lactobacillales Streptococcaceae Lactococcus Lactococcus piscium 542 1.594633558 6 Actinobacteria Thermoleophilia Solirubrobacterales Conexibacteraceae Conexibacter Conexibacter woesei 471 1.385742446 7 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas taxi 430 1.265115184 8 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas wittichii 388 1.141545794 9 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas sp. FARSPH 298 0.876754244 10 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sorangium cellulosum 260 0.764953367 11 Proteobacteria Deltaproteobacteria Myxococcales Polyangiaceae Sorangium Sphingomonas sp. Cra20 260 0.764953367 12 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas panacis 252 0.741416341 -
Microbial and Geochemical Characterization of Wellington Oil Field, Southcentral Kansas, and Potential Applications to Microbial Enhanced Oil Recovery
Microbial and Geochemical Characterization of Wellington Oil Field, Southcentral Kansas, and Potential Applications to Microbial Enhanced Oil Recovery By Breanna L. Huff Submitted to the graduate degree program in Geology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Arts. ________________________________ Jennifer A. Roberts, Chair ________________________________ David A. Fowle, Co-Chair ________________________________ Gwendolyn L. Macpherson ________________________________ Leigh A. Stearns Date Defended: May 12, 2014 The Thesis Committee for Breanna L. Huff certifies that this is the approved version of the following thesis: Microbial and Geochemical Characterization of Wellington Oil Field, Southcentral Kansas, and Potential Applications to Microbial Enhanced Oil Recovery ________________________________ Jennifer A. Roberts, Chairperson Date approved: May 12, 2014 ii Abstract The aqueous geochemistry and microbiology of subsurface environments are intimately linked and in oil reservoir fluids. This interdependence may result in a number of processes including biodegradation of oil, corrosion of pipes, bioclogging of porous media, and biosurfactant production. During production of oil and reinjection of production water, surface exposed fluids are introduced to oxygen and exogenous microbes, both of which may alter reservoir biogeochemistry. In this study, production waters from six wells within the Wellington Field in SE Kansas, which has been water flooded continuously for 60 years, were sampled and analyzed for geochemistry, microbial ecology, microbial biomass, and biosurfactant production to better understand the relationship between the microbiology and oil production in the field. Minor differences in aqueous geochemistry were detected among the five production wells and single injection well, and data analysis and modeling indicate that depth-specific water-rock reactions play a major role in controlling the major ion geochemistry in the field. -
Serpentinicella Alkaliphila Gen. Nov., Sp. Nov., a Novel
International Journal of Systematic and Evolutionary Microbiology (2016), 66, 4464–4470 DOI 10.1099/ijsem.0.001375 Serpentinicella alkaliphila gen. nov., sp. nov., a novel alkaliphilic anaerobic bacterium isolated from the serpentinite-hosted Prony hydrothermal field, New Caledonia. Nan Mei,1 Anne Postec,1 Gael Erauso,1 Manon Joseph,1 Bernard Pelletier,2 Claude Payri,2 Bernard Ollivier1 and Marianne Quem eneur 1 Correspondence 1Aix Marseille Univ, Universite de Toulon, CNRS, IRD, MIO, Marseille, France Marianne Quemeneur 2Centre IRD de Noumea, 101 Promenade Roger Laroque, BP A5 - 98848 Noumea cedex, , New [email protected] Caledonia A novel anaerobic, alkaliphilic, Gram-stain-positive, spore-forming bacterium was isolated from a carbonaceous hydrothermal chimney in Prony Bay, New Caledonia. This bacterium, designated strain 3bT, grew at temperatures from 30 to 43 C (optimum 37 C) and at pH between 7.8 and 10.1 (optimum 9.5). Added NaCl was not required for growth (optimum 0–0.2 %, w/v), but was tolerated at up to 4 %. Yeast extract was required for growth. Strain 3bT utilized crotonate, lactate and pyruvate, but not sugars. Crotonate was dismutated to acetate and butyrate. Lactate was disproportionated to acetate and propionate. Pyruvate was degraded to acetate plus trace amounts of hydrogen. Growth on lactate was improved by the addition of fumarate, which was used as an electron acceptor and converted to succinate. Sulfate, thiosulfate, elemental sulfur, sulfite, nitrate, nitrite, FeCl3, Fe(III)-citrate, Fe(III)-EDTA, chromate, arsenate, selenate and DMSO were not used as terminal electron acceptors. The G+C content of the genomic DNA was 33.2 mol%. -
The Keystone Species of Precambrian Deep Bedrock Biosphere the Supplement Related to This Article Is Available Online at Doi:10.5194/Bgd-12-18103-2015-Supplement
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Biogeosciences Discuss., 12, 18103–18150, 2015 www.biogeosciences-discuss.net/12/18103/2015/ doi:10.5194/bgd-12-18103-2015 BGD © Author(s) 2015. CC Attribution 3.0 License. 12, 18103–18150, 2015 This discussion paper is/has been under review for the journal Biogeosciences (BG). The keystone species Please refer to the corresponding final paper in BG if available. of Precambrian deep bedrock biosphere The keystone species of Precambrian L. Purkamo et al. deep bedrock biosphere belong to Burkholderiales and Clostridiales Title Page Abstract Introduction L. Purkamo1, M. Bomberg1, R. Kietäväinen2, H. Salavirta1, M. Nyyssönen1, M. Nuppunen-Puputti1, L. Ahonen2, I. Kukkonen2,a, and M. Itävaara1 Conclusions References Tables Figures 1VTT Technical Research Centre of Finland Ltd., Espoo, Finland 2Geological Survey of Finland (GTK), Espoo, Finland anow at: University of Helsinki, Helsinki, Finland J I Received: 13 September 2015 – Accepted: 23 October 2015 – Published: 11 November 2015 J I Correspondence to: L. Purkamo (lotta.purkamo@vtt.fi) Back Close Published by Copernicus Publications on behalf of the European Geosciences Union. Full Screen / Esc Printer-friendly Version Interactive Discussion 18103 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract BGD The bacterial and archaeal community composition and the possible carbon assimi- lation processes and energy sources of microbial communities in oligotrophic, deep, 12, 18103–18150, 2015 crystalline bedrock fractures is yet to be resolved. In this study, intrinsic microbial com- 5 munities from six fracture zones from 180–2300 m depths in Outokumpu bedrock were The keystone species characterized using high-throughput amplicon sequencing and metagenomic predic- of Precambrian deep tion. -
Draft Genome Sequence of Dethiobacter Alkaliphilus Strain AHT1T, a Gram-Positive Sulfidogenic Polyextremophile Emily Denise Melton1, Dimitry Y
Melton et al. Standards in Genomic Sciences (2017) 12:57 DOI 10.1186/s40793-017-0268-9 EXTENDED GENOME REPORT Open Access Draft genome sequence of Dethiobacter alkaliphilus strain AHT1T, a gram-positive sulfidogenic polyextremophile Emily Denise Melton1, Dimitry Y. Sorokin2,3, Lex Overmars1, Alla L. Lapidus4, Manoj Pillay6, Natalia Ivanova5, Tijana Glavina del Rio5, Nikos C. Kyrpides5,6,7, Tanja Woyke5 and Gerard Muyzer1* Abstract Dethiobacter alkaliphilus strain AHT1T is an anaerobic, sulfidogenic, moderately salt-tolerant alkaliphilic chemolithotroph isolated from hypersaline soda lake sediments in northeastern Mongolia. It is a Gram-positive bacterium with low GC content, within the phylum Firmicutes. Here we report its draft genome sequence, which consists of 34 contigs with a total sequence length of 3.12 Mbp. D. alkaliphilus strain AHT1T was sequenced by the Joint Genome Institute (JGI) as part of the Community Science Program due to its relevance to bioremediation and biotechnological applications. Keywords: Extreme environment, Soda lake, Sediment, Haloalkaliphilic, Gram-positive, Firmicutes Introduction genome of a haloalkaliphilic Gram-positive sulfur dispro- Soda lakes are formed in environments where high rates portionator within the phylum Firmicutes: Dethiobacter of evaporation lead to the accumulation of soluble carbon- alkaliphilus AHT1T. ate salts due to the lack of dissolved divalent cations. Con- sequently, soda lakes are defined by their high salinity and Organism information stable highly alkaline pH conditions, making them dually Classification and features extreme environments. Soda lakes occur throughout the The haloalkaliphilic anaerobe D. alkaliphilus AHT1T American, European, African, Asian and Australian conti- was isolated from hypersaline soda lake sediments in nents and host a wide variety of Archaea and Bacteria, northeastern Mongolia [10]. -
Draft Genome Sequence of Dethiobacter Alkaliphilus Strain AHT1T, a Gram-Positive Sulfidogenic Polyextremophile
Lawrence Berkeley National Laboratory Recent Work Title Draft genome sequence of Dethiobacter alkaliphilus strain AHT1T, a gram-positive sulfidogenic polyextremophile. Permalink https://escholarship.org/uc/item/7gw7f283 Journal Standards in genomic sciences, 12(1) ISSN 1944-3277 Authors Melton, Emily Denise Sorokin, Dimitry Y Overmars, Lex et al. Publication Date 2017 DOI 10.1186/s40793-017-0268-9 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Melton et al. Standards in Genomic Sciences (2017) 12:57 DOI 10.1186/s40793-017-0268-9 EXTENDED GENOME REPORT Open Access Draft genome sequence of Dethiobacter alkaliphilus strain AHT1T, a gram-positive sulfidogenic polyextremophile Emily Denise Melton1, Dimitry Y. Sorokin2,3, Lex Overmars1, Alla L. Lapidus4, Manoj Pillay6, Natalia Ivanova5, Tijana Glavina del Rio5, Nikos C. Kyrpides5,6,7, Tanja Woyke5 and Gerard Muyzer1* Abstract Dethiobacter alkaliphilus strain AHT1T is an anaerobic, sulfidogenic, moderately salt-tolerant alkaliphilic chemolithotroph isolated from hypersaline soda lake sediments in northeastern Mongolia. It is a Gram-positive bacterium with low GC content, within the phylum Firmicutes. Here we report its draft genome sequence, which consists of 34 contigs with a total sequence length of 3.12 Mbp. D. alkaliphilus strain AHT1T was sequenced by the Joint Genome Institute (JGI) as part of the Community Science Program due to its relevance to bioremediation and biotechnological applications. Keywords: Extreme environment, Soda lake, Sediment, Haloalkaliphilic, Gram-positive, Firmicutes Introduction genome of a haloalkaliphilic Gram-positive sulfur dispro- Soda lakes are formed in environments where high rates portionator within the phylum Firmicutes: Dethiobacter of evaporation lead to the accumulation of soluble carbon- alkaliphilus AHT1T. -
Cv15866 JGI PR CR:JGI Progress Report
15866_JGI_PR_CR:Cover 3/23/09 11:07 AM Page 1 U.S. DEPARTMENT OF ENERGY 2008 Progress Joint Genome Institute Report DOE JGI—powering a sustainable future with the science we need for biofuels, environmental cleanup, and carbon capture. 15866_JGI_PR_CR:Cover 3/23/09 11:07 AM Page 2 DISCLAIMER This document was prepared as an account of work sponsored by the United States Gov- ernment. While this document is believed to contain correct information, neither the United States Govern- ment nor any agency thereof, nor The Regents of the University of California, nor any of their employees, makes any warranty, express or implied, or assumes any legal responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by its trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof, or The Regents of the University of California. The views and opinions of authors expressed herein do not necessarily state or reflect uencing targets of the DOE Joint Genome those of the United States Government or any agency thereof or The Regents of the University of California. The cover depicts various DOE mission-relevant genome seq Institute. This work was performed under the auspices of the US Department of Energy's Office of Science, Biological and Environmental Research Program, and by the University of California, Lawrence Berkeley National Labora- tory under contract No. -
Microbial Diversity in Engineered Haloalkaline Environments Shaped by Shared Geochemical Drivers Observed in Natural Analogues
Microbial Diversity in Engineered Haloalkaline Environments Shaped by Shared Geochemical Drivers Observed in Natural Analogues Talitha C. Santini,a,b,c Lesley A. Warren,d Kathryn E. Kendrad School of Geography, Planning, and Environmental Management, The University of Queensland, Brisbane, QLD, Australiaa; Centre for Mined Land Rehabilitation, The University of Queensland, Brisbane, QLD, Australiab; School of Earth and Environment, The University of Western Australia, Crawley, WA, Australiac; School of Geography and Earth Sciences, McMaster University, Hamilton, Ontario, Canadad Microbial communities in engineered terrestrial haloalkaline environments have been poorly characterized relative to their nat- ural counterparts and are geologically recent in formation, offering opportunities to explore microbial diversity and assembly in dynamic, geochemically comparable contexts. In this study, the microbial community structure and geochemical characteristics Downloaded from of three geographically dispersed bauxite residue environments along a remediation gradient were assessed and subsequently compared with other engineered and natural haloalkaline systems. In bauxite residues, bacterial communities were similar at the phylum level (dominated by Proteobacteria and Firmicutes) to those found in soda lakes, oil sands tailings, and nuclear wastes; however, they differed at lower taxonomic levels, with only 23% of operational taxonomic units (OTUs) shared with other haloalkaline environments. Although being less diverse than natural analogues, -
Diversity and Prevalence of ANTAR Rnas Across Actinobacteria
bioRxiv preprint doi: https://doi.org/10.1101/2020.10.11.335034; this version posted October 11, 2020. 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. Diversity and prevalence of ANTAR RNAs across actinobacteria Dolly Mehta1,2 and Arati Ramesh1,+ 1National Centre for Biological Sciences, Tata Institute of Fundamental Research, GKVK Campus, Bellary Road, Bangalore, India 560065. 2SASTRA University, Tirumalaisamudram, Thanjavur – 613401. +Corresponding Author: Arati Ramesh National Centre for Biological Sciences GKVK Campus, Bellary Road Bangalore, 560065 Tel. 91-80-23666930 e-mail: [email protected] Running title: Identification of ANTAR RNAs across Actinobacteria Keywords: ANTAR protein:RNA regulatory system, structured RNA, actinobacteria 1 bioRxiv preprint doi: https://doi.org/10.1101/2020.10.11.335034; this version posted October 11, 2020. 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. ABSTRACT Computational approaches are often used to predict regulatory RNAs in bacteria, but their success is limited to RNAs that are highly conserved across phyla, in sequence and structure. The ANTAR regulatory system consists of a family of RNAs (the ANTAR-target RNAs) that selectively recruit ANTAR proteins. This protein-RNA complex together regulates genes at the level of translation or transcriptional elongation.