Ankyrin Domains Across the Tree of Life
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Spatio-Temporal Study of Microbiology in the Stratified Oxic-Hypoxic-Euxinic, Freshwater- To-Hypersaline Ursu Lake
Spatio-temporal insights into microbiology of the freshwater-to- hypersaline, oxic-hypoxic-euxinic waters of Ursu Lake Baricz, A., Chiriac, C. M., Andrei, A-., Bulzu, P-A., Levei, E. A., Cadar, O., Battes, K. P., Cîmpean, M., enila, M., Cristea, A., Muntean, V., Alexe, M., Coman, C., Szekeres, E. K., Sicora, C. I., Ionescu, A., Blain, D., O’Neill, W. K., Edwards, J., ... Banciu, H. L. (2020). Spatio-temporal insights into microbiology of the freshwater-to- hypersaline, oxic-hypoxic-euxinic waters of Ursu Lake. Environmental Microbiology. https://doi.org/10.1111/1462-2920.14909, https://doi.org/10.1111/1462-2920.14909 Published in: Environmental Microbiology Document Version: Peer reviewed version Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights Copyright 2019 Wiley. This work is made available online in accordance with the publisher’s policies. Please refer to any applicable terms of use of the publisher. General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. -
Journal of Clinical Microbiology
JOURNAL OF CLINICAL MICROBIOLOGY Volume 45 September 2007 No. 9 MINIREVIEW 16S rRNA Gene Sequencing for Bacterial Identification in J. Michael Janda and Sharon L. 2761–2764 the Diagnostic Laboratory: Pluses, Perils, and Pitfalls Abbott BACTERIOLOGY Is the Volume of Blood Cultured Still a Significant Factor in Emilio Bouza, Dolores Sousa, 2765–2769 the Diagnosis of Bloodstream Infections? Marta Rodrı´guez-Cre´ixems, Juan Garcı´a Lechuz, and Patricia Mun˜oz Reclassification of Phenotypically Identified Staphylococcus Takashi Sasaki, Ken Kikuchi, 2770–2778 intermedius Strains Yoshikazu Tanaka, Namiko Takahashi, Shinichi Kamata, and Keiichi Hiramatsu Evaluation of Gen-Probe APTIMA-Based Neisseria Erik Munson, Vivian Boyd, Jolanta 2793–2797 gonorrhoeae and Chlamydia trachomatis Confirmatory Testing Czarnecka, Judy Griep, Brian Lund, in a Metropolitan Setting of High Disease Prevalence Nancy Schaal, and Jeanne E. Hryciuk Convenient Test Using a Combination of Chelating Agents Soo-Young Kim, Seong Geun Hong, 2798–2801 for Detection of Metallo--Lactamases in the Clinical Ellen S. Moland, and Kenneth S. Laboratory Thomson Molecular Characterization of Vancomycin-Resistant Bo Zheng, Haruyoshi Tomita, Yong 2813–2818 Enterococcus faecium Isolates from Mainland China Hong Xiao, Shan Wang, Yun Li, and Yasuyoshi Ike Bacteriology of Moderate-to-Severe Diabetic Foot Infections Diane M. Citron, Ellie J. C. 2819–2828 and In Vitro Activity of Antimicrobial Agents Goldstein, C. Vreni Merriam, Benjamin A. Lipsky, and Murray A. Abramson Outbreak of Pseudomonas -
Westchester County Restaurants
RESTAURANTS THAT ARE ENOUGH TO MAKE YOU SICK: AN ANALYSIS OF UNSANITARY CONDITIONS AT NEW YORK CITY AND WESTCHESTER COUNTY RESTAURANTS STATE SENATOR JEFF KLEIN RANKING MINORITY MEMBER CONSUMER PROTECTION COMMITTEE RESTAURANTS ENOUGH TO MAKE YOU SICK: AN ANALYSIS OF UNSANITARY CONDITIONS AT NEW YORK CITY AND WESTCHESTER COUNTY RESTAURANT S How Consumers Are At Risk There is little reason why eating a meal in a restaurant should be any more dangerous than eating a meal in your own home. The volume and variety of foods prepared in a restaurant kitchen makes sanitation more critical, but the basic rules of cleanliness, temperature control and pest control are universal. The major difference is that the restaurant patron cannot usually see the kitchen where his or her meal is prepared. These unseen risks are present and they can pose a serious threat to the public. Worse, they may go undetected and unaddressed for extended periods of time. Although inspections are the first step toward catching these problems before they become public health hazards, many problems linger long after they have been cited by inspectors because restaurants can continue to operate with ongoing violations, with no warning to consumers. Many of the violations we have looked at, and many of the most common violations, are easily correctable, and if eradicated, greatly reduce the probability of an outbreak of food borne illness. By simply ensuring that potentially hazardous foods are properly stored, that they do not come into contact with other ready-to-eat foods, and ensuring that employees wash their hand or change their gloves after handling such foods would almost eliminate the risks posed by these foods. -
NC10 Phylum Anaerobs? Methanotrophs? Where Can I Find Them?
NC10 phylum Anaerobs? Methanotrophs? Where can I find them? Beate Kraft Microbial Diversity 2012 Abstract Methylomirabilis oxyfera, the only cultured member of the NC10 phylum performs the newly discovered pathway of NO-dismutation. In this study different habitats were screened for the presence of member of this phylum and the diversity of the sequences obtained was analyzed. Furthermore enrichment cultures for nitrite reduction coupled to methane oxidation were set up. Indeed, the presence of NC10 seems to be associated with nitrite and methane rich fresh water environments. Introduction Recently a new nitrite reduction pathway, NO-dismutation, coupled to methane oxidation has been discovered (Ettwig et al. 2010). In NO-dismutation nitrite is oxidized to NO as in denitrification but then NO dimutated into N2 and O2 instead of being further reduced to N2O. The generated oxygen is then used for methane oxidation. The organism responsible for this process is Methylomirabils oxfera. It is the only cultured member of the candidate phylum NC10. Fig 1: Pathway of NO-dismutation (from Ettwig et al. 2010) It remains open if other members of the NC10 phylum share the same metabolism and respiratory pathway or if they are metabolically more diverse. 16S sequences that fall into the NC10 phylum have been found in mainly oxygen limited freshwater habitats such as lakes including lake sediments, rice paddy soils, wastewater sludge and ditches (Deutzmann and Schink 2011, Luesken et a.l 2011). Their occurrence apparently seem to be correlated with the presence of methane and nitrite in the habitat. This would suggest a similar respiratory pathway as in Methylomirabilis oxyfera. -
Yu-Chen Ling and John W. Moreau
Microbial Distribution and Activity in a Coastal Acid Sulfate Soil System Introduction: Bioremediation in Yu-Chen Ling and John W. Moreau coastal acid sulfate soil systems Method A Coastal acid sulfate soil (CASS) systems were School of Earth Sciences, University of Melbourne, Melbourne, VIC 3010, Australia formed when people drained the coastal area Microbial distribution controlled by environmental parameters Microbial activity showed two patterns exposing the soil to the air. Drainage makes iron Microbial structures can be grouped into three zones based on the highest similarity between samples (Fig. 4). Abundant populations, such as Deltaproteobacteria, kept constant activity across tidal cycling, whereas rare sulfides oxidize and release acidity to the These three zones were consistent with their geological background (Fig. 5). Zone 1: Organic horizon, had the populations changed activity response to environmental variations. Activity = cDNA/DNA environment, low pH pore water further dissolved lowest pH value. Zone 2: surface tidal zone, was influenced the most by tidal activity. Zone 3: Sulfuric zone, Abundant populations: the heavy metals. The acidity and toxic metals then Method A Deltaproteobacteria Deltaproteobacteria this area got neutralized the most. contaminate coastal and nearby ecosystems and Method B 1.5 cause environmental problems, such as fish kills, 1.5 decreased rice yields, release of greenhouse gases, Chloroflexi and construction damage. In Australia, there is Gammaproteobacteria Gammaproteobacteria about a $10 billion “legacy” from acid sulfate soils, Chloroflexi even though Australia is only occupied by around 1.0 1.0 Cyanobacteria,@ Acidobacteria Acidobacteria Alphaproteobacteria 18% of the global acid sulfate soils. Chloroplast Zetaproteobacteria Rare populations: Alphaproteobacteria Method A log(RNA(%)+1) Zetaproteobacteria log(RNA(%)+1) Method C Method B 0.5 0.5 Cyanobacteria,@ Bacteroidetes Chloroplast Firmicutes Firmicutes Bacteroidetes Planctomycetes Planctomycetes Ac8nobacteria Fig. -
Bacteria Clostridia Bacilli Eukaryota CFB Group
AM935842.1.1361 uncultured Burkholderiales bacterium Class Betaproteobacteria AY283260.1.1552 Alcaligenes sp. PCNB−2 Class Betaproteobacteria AM934953.1.1374 uncultured Burkholderiales bacterium Class Betaproteobacteria AJ581593.1.1460 uncultured betaAM936569.1.1351 proteobacterium uncultured Class Betaproteobacteria Derxia sp. Class Betaproteobacteria AJ581621.1.1418 uncultured beta proteobacterium Class Betaproteobacteria DQ248272.1.1498 uncultured soil bacterium soil uncultured DQ248272.1.1498 DQ248235.1.1498 uncultured soil bacterium RS49 DQ248270.1.1496 uncultured soil bacterium DQ256489.1.1211 Variovorax paradoxus Class Betaproteobacteria Class paradoxus Variovorax DQ256489.1.1211 AF523053.1.1486 uncultured Comamonadaceae bacterium Class Betaproteobacteria AY706442.1.1396 uncultured bacterium uncultured AY706442.1.1396 AJ536763.1.1422 uncultured bacterium CS000359.1.1530 Variovorax paradoxus Class Betaproteobacteria Class paradoxus Variovorax CS000359.1.1530 AY168733.1.1411 uncultured bacterium AJ009470.1.1526 uncultured bacterium SJA−62 Class Betaproteobacteria Class SJA−62 bacterium uncultured AJ009470.1.1526 AY212561.1.1433 uncultured bacterium D16212.1.1457 Rhodoferax fermentans Class Betaproteobacteria Class fermentans Rhodoferax D16212.1.1457 AY957894.1.1546 uncultured bacterium AJ581620.1.1452 uncultured beta proteobacterium Class Betaproteobacteria RS76 AY625146.1.1498 uncultured bacterium RS65 DQ316832.1.1269 uncultured beta proteobacterium Class Betaproteobacteria DQ404909.1.1513 uncultured bacterium uncultured DQ404909.1.1513 AB021341.1.1466 bacterium rM6 AJ487020.1.1500 uncultured bacterium uncultured AJ487020.1.1500 RS7 RS86RC AF364862.1.1425 bacterium BA128 Class Betaproteobacteria AY957931.1.1529 uncultured bacterium uncultured AY957931.1.1529 CP000884.723807.725332 Delftia acidovorans SPH−1 Class Betaproteobacteria AY957923.1.1520 uncultured bacterium uncultured AY957923.1.1520 RS18 AY957918.1.1527 uncultured bacterium uncultured AY957918.1.1527 AY945883.1.1500 uncultured bacterium AF526940.1.1489 uncultured Ralstonia sp. -
The Phylogenetic Composition and Structure of Soil Microbial Communities Shifts in Response to Elevated Carbon Dioxide
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Minnesota Digital Conservancy The ISME Journal (2012) 6, 259–272 & 2012 International Society for Microbial Ecology All rights reserved 1751-7362/12 www.nature.com/ismej ORIGINAL ARTICLE The phylogenetic composition and structure of soil microbial communities shifts in response to elevated carbon dioxide Zhili He1, Yvette Piceno2, Ye Deng1, Meiying Xu1,3, Zhenmei Lu1,4, Todd DeSantis2, Gary Andersen2, Sarah E Hobbie5, Peter B Reich6 and Jizhong Zhou1,2 1Institute for Environmental Genomics, Department of Botany and Microbiology, University of Oklahoma, Norman, OK, USA; 2Ecology Department, Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, USA; 3Guangdong Provincial Key Laboratory of Microbial Culture Collection and Application, Guangdong Institute of Microbiology, Guangzhou, China; 4College of Life Sciences, Zhejiang University, Hangzhou, China; 5Department of Ecology, Evolution, and Behavior, St Paul, MN, USA and 6Department of Forest Resources, University of Minnesota, St Paul, MN, USA One of the major factors associated with global change is the ever-increasing concentration of atmospheric CO2. Although the stimulating effects of elevated CO2 (eCO2) on plant growth and primary productivity have been established, its impacts on the diversity and function of soil microbial communities are poorly understood. In this study, phylogenetic microarrays (PhyloChip) were used to comprehensively survey the richness, composition and structure of soil microbial communities in a grassland experiment subjected to two CO2 conditions (ambient, 368 p.p.m., versus elevated, 560 p.p.m.) for 10 years. The richness based on the detected number of operational taxonomic units (OTUs) significantly decreased under eCO2. -
Being Aquifex Aeolicus: Untangling a Hyperthermophile's Checkered Past
GBE Being Aquifex aeolicus: Untangling a Hyperthermophile’s Checkered Past Robert J.M. Eveleigh1,2, Conor J. Meehan1,2,JohnM.Archibald1, and Robert G. Beiko2,* 1Department of Biochemistry and Molecular Biology, Dalhousie University, Halifax, Nova Scotia, Canada 2Faculty of Computer Science, Dalhousie University, Halifax, Nova Scotia, Canada *Corresponding author: E-mail: [email protected]. Accepted: November 22, 2013 Abstract Lateral gene transfer (LGT) is an important factor contributing to the evolution of prokaryotic genomes. The Aquificae are a hyper- thermophilic bacterial group whose genes show affiliations to many other lineages, including the hyperthermophilic Thermotogae, the Proteobacteria, and the Archaea. Previous phylogenomic analyses focused on Aquifex aeolicus identified Thermotogae and Downloaded from Aquificae either as successive early branches or sisters in a rooted bacterial phylogeny, but many phylogenies and cellular traits have suggested a stronger affiliation with the Epsilonproteobacteria. Different scenarios for the evolution of the Aquificae yield different phylogenetic predictions. Here, we outline these scenarios and consider the fit of the available data, including three sequenced Aquificae genomes, to different sets of predictions. Evidence from phylogenetic profiles and trees suggests that the Epsilonproteobacteria have the strongest affinities with the three Aquificae analyzed. However, this pattern is shown by only a http://gbe.oxfordjournals.org/ minority of encoded proteins, and the Archaea, many lineages of thermophilic bacteria, and members of genus Clostridium and class Deltaproteobacteria also show strong connections to the Aquificae. The phylogenetic affiliations of different functional subsystems showed strong biases: Most but not all genes implicated in the core translational apparatus tended to group Aquificae with Thermotogae, whereas a wide range of metabolic and cellular processes strongly supported the link between Aquificae and Epsilonproteobacteria. -
Genomic Analysis of Helicobacter Himalayensis Sp. Nov. Isolated from Marmota Himalayana
Genomic analysis of Helicobacter himalayensis sp. nov. isolated from Marmota himalayana Shouhui Hu Peking University Shougang Hospital Lina Niu Hainan Medical University Lei Wu Peking University Shougang Hospital Xiaoxue Zhu Peking University Shougang Hospital Yu Cai Peking University Shougang Hospital Dong Jin Chinese Center for Disease Control and Prevention Linlin Yan Peking University Shougang Hospital Fan Zhao ( [email protected] ) Peking University Shougang Hospital https://orcid.org/0000-0002-8164-5016 Research article Keywords: Helicobacter, Comparative genomics, Helicobacter himalayensis, Virulence factor Posted Date: December 1st, 2020 DOI: https://doi.org/10.21203/rs.3.rs-55448/v3 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published on November 23rd, 2020. See the published version at https://doi.org/10.1186/s12864-020-07245-y. Page 1/18 Abstract Background: Helicobacter himalayensis was isolated from Marmota himalayana in the Qinghai-Tibet Plateau, China, and is a new non-H. pylori species, with unclear taxonomy, phylogeny, and pathogenicity. Results: A comparative genomic analysis was performed between the H. himalayensis type strain 80(YS1)T and other the genomes of Helicobacter species present in the National Center for Biotechnology Information (NCBI) database to explore the molecular evolution and potential pathogenicity of H. himalayensis. H. himalayensis 80(YS1)T formed a clade with H. cinaedi and H. hepaticus that was phylogenetically distant from H. pylori. The H. himalayensis genome showed extensive collinearity with H. hepaticus and H. cinaedi. However, it also revealed a low degree of genome collinearity with H. -
R Graphics Output
883 | Desulfovibrio vulgaris | DvMF_2825 298701 | Desulfovibrio | DA2_3337 1121434 | Halodesulfovibrio aestuarii | AULY01000007_gene1045 207559 | Desulfovibrio alaskensis | Dde_0991 935942 | Desulfonatronum lacustre | KI912608_gene2193 159290 | Desulfonatronum | JPIK01000018_gene1259 1121448 | Desulfovibrio gigas | DGI_0655 1121445 | Desulfovibrio desulfuricans | ATUZ01000018_gene2316 525146 | Desulfovibrio desulfuricans | Ddes_0159 665942 | Desulfovibrio | HMPREF1022_02168 457398 | Desulfovibrio | HMPREF0326_00453 363253 | Lawsonia intracellularis | LI0397 882 | Desulfovibrio vulgaris | DVU_0784 1121413 | Desulfonatronovibrio hydrogenovorans | JMKT01000008_gene1463 555779 | Desulfonatronospira thiodismutans | Dthio_PD0935 690850 | Desulfovibrio africanus | Desaf_1578 643562 | Pseudodesulfovibrio aespoeensis | Daes_3115 1322246 | Pseudodesulfovibrio piezophilus | BN4_12523 641491 | Desulfovibrio desulfuricans | DND132_2573 1121440 | Desulfovibrio aminophilus | AUMA01000002_gene2198 1121456 | Desulfovibrio longus | ATVA01000018_gene290 526222 | Desulfovibrio salexigens | Desal_3460 1121451 | Desulfovibrio hydrothermalis | DESAM_21057 1121447 | Desulfovibrio frigidus | JONL01000008_gene3531 1121441 | Desulfovibrio bastinii | AUCX01000006_gene918 1121439 | Desulfovibrio alkalitolerans | dsat_0220 941449 | Desulfovibrio | dsx2_0067 1307759 | Desulfovibrio | JOMJ01000003_gene2163 1121406 | Desulfocurvus vexinensis | JAEX01000012_gene687 1304872 | Desulfovibrio magneticus | JAGC01000003_gene2904 573370 | Desulfovibrio magneticus | DMR_04750 -
Helicobacter Cinaedi Induced Typhlocolitis in Rag-2-Deficient Mice
Helicobacter cinaedi Induced Typhlocolitis in Rag-2-Deficient Mice The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Shen, Zeli; Feng, Yan; Rickman, Barry and Fox, James G. “ Helicobacter Cinaedi Induced Typhlocolitis in Rag-2-Deficient Mice .” Helicobacter 20, no. 2 (November 2014): 146–155 © 2014 John Wiley & Sons Ltd As Published http://dx.doi.org/10.1111/hel.12179 Publisher Wiley Blackwell Version Author's final manuscript Citable link http://hdl.handle.net/1721.1/109464 Terms of Use Creative Commons Attribution-Noncommercial-Share Alike Detailed Terms http://creativecommons.org/licenses/by-nc-sa/4.0/ HHS Public Access Author manuscript Author Manuscript Author ManuscriptHelicobacter Author Manuscript. Author manuscript; Author Manuscript available in PMC 2016 April 01. Published in final edited form as: Helicobacter. 2015 April ; 20(2): 146–155. doi:10.1111/hel.12179. Helicobacter cinaedi Induced Typhlocolitis in Rag-2-Deficient Mice Zeli Shen, Yan Feng, Barry Rickman, and James G. Fox Division of Comparative Medicine, Massachusetts Institute of Technology, Cambridge, MA 02139, USA Abstract Background—Helicobacter cinaedi, an enterohepatic helicobacter species (EHS), is an important human pathogen and is associated with a wide range of diseases, especially in immunocompromised patients. It has been convincingly demonstrated that innate immune response to certain pathogenic enteric bacteria is sufficient to initiate colitis and colon carcinogenesis in recombinase-activating gene (Rag)-2-deficient mice model. To better understand the mechanisms of human IBD and its association with development of colon cancer, we investigated whether H. cinaedi could induce pathological changes noted with murine enterohepatic helicobacter infections in the Rag2−/− mouse model. -
The Environment, Diversity and Activity of Microbial Communities in Submarine Freshwater Springs in the Dead Sea
The environment, diversity and activity of microbial communities in submarine freshwater springs in the Dead Sea Dissertation Zur Erlangung des Grades eines Doktors der Naturwissenschaften - Dr. rer. nat. - dem Fachbereich Geowissenschaften der Universität Bremen vorgelegt an Stefan Häusler Bremen, April 2014 Die vorliegende Arbeit wurde in der Zeit von November 2010 bis April 2014 am Max- Planck-Institut für Marine Mikrobiologie in Bremen angefertigt. 1. Gutachter: Prof. Dr. Marcel M.M. Kuypers 2. Gutachter: Prof. Dr. Thorsten Dittmar Datum des Promotionskolloquiums: 16. Mai 2014 Contents Summary 1 Zusammenfassung 3 Chapter 1 7 Introduction 7 Motivation and objectives 23 Overview of enclosed manuscripts 35 Chapter 2 39 Microbial and chemical characterization of underwater fresh water springs in the Dead Sea Chapter 3 105 Microenvironments of reduced salinity harbor biofilms in Dead Sea underwater springs Chapter 4 125 Spatial distribution of diatom and cyanobacterial microbial mats in the Dead Sea is determined by response to rapid salinity fluctuations Chapter 5 153 Sulfate reduction and sulfide oxidation in extremely steep salinity gradients formed by freshwater springs emerging into the Dead Sea Chapter 6 189 Conclusions and perspectives Contributed work 201 Acknowledgements 211 Summary Summary The Dead Sea, located at the border between Jordan, Israel and the Palestinian authority is one of the most hypersaline lakes on earth. Its waters contain a total dissolved salt concentration of up to 348 g L-1, which is about 10 times higher than regular sea water. The lake is characterized by elevated concentrations of divalent cations (~2 M Mg2+ and ~0.5 M Ca2+), which, in addition to the high salinity, form an extreme environment where only highly adapted microorganisms can survive.