Metabolic Versatility of the Nitrite-Oxidizing Bacterium Nitrospira
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Metaproteomics Reveals Differential Modes of Metabolic Coupling Among Ubiquitous Oxygen Minimum Zone Microbes
Metaproteomics reveals differential modes of metabolic coupling among ubiquitous oxygen minimum zone microbes Alyse K. Hawleya, Heather M. Brewerb, Angela D. Norbeckb, Ljiljana Paša-Tolicb, and Steven J. Hallama,c,d,1 aDepartment of Microbiology and Immunology, cGraduate Program in Bioinformatics, and dGenome Sciences and Technology Training Program, University of British Columbia, Vancouver, BC, Canada V6T 1Z3; and bBiological and Computational Sciences Division, Pacific Northwest National Laboratory, Richland, WA 99352 Edited by Edward F. DeLong, Massachusetts Institute of Technology, Cambridge, MA, and approved June 10, 2014 (received for review November 26, 2013) Marine oxygen minimum zones (OMZs) are intrinsic water column transformations in nonsulfidic OMZs, providing evidence for features arising from respiratory oxygen demand during organic a cryptic sulfur cycle with the potential to drive inorganic carbon matter degradation in stratified waters. Currently OMZs are expand- fixation processes (13). Indeed, many of the key microbial players ing due to global climate change with resulting feedback on marine implicated in nitrogen and sulfur transformations in OMZs, in- ecosystem function. Here we use metaproteomics to chart spatial cluding Thaumarchaeota, Nitrospina, Nitrospira, Planctomycetes, and temporal patterns of gene expression along defined redox and SUP05/ARCTIC96BD-19 Gammaproteobacteria have the gradients in a seasonally stratified fjord to better understand metabolic potential for inorganic carbon fixation (14–19), and -
Light-Independent Nitrogen Assimilation in Plant Leaves: Nitrate Incorporation Into Glutamine, Glutamate, Aspartate, and Asparagine Traced by 15N
plants Review Light-Independent Nitrogen Assimilation in Plant Leaves: Nitrate Incorporation into Glutamine, Glutamate, Aspartate, and Asparagine Traced by 15N Tadakatsu Yoneyama 1,* and Akira Suzuki 2,* 1 Department of Applied Biological Chemistry, Graduate School of Agricultural and Life Sciences, University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-8657, Japan 2 Institut Jean-Pierre Bourgin, Institut national de recherche pour l’agriculture, l’alimentation et l’environnement (INRAE), UMR1318, RD10, F-78026 Versailles, France * Correspondence: [email protected] (T.Y.); [email protected] (A.S.) Received: 3 September 2020; Accepted: 29 September 2020; Published: 2 October 2020 Abstract: Although the nitrate assimilation into amino acids in photosynthetic leaf tissues is active under the light, the studies during 1950s and 1970s in the dark nitrate assimilation provided fragmental and variable activities, and the mechanism of reductant supply to nitrate assimilation in darkness remained unclear. 15N tracing experiments unraveled the assimilatory mechanism of nitrogen from nitrate into amino acids in the light and in darkness by the reactions of nitrate and nitrite reductases, glutamine synthetase, glutamate synthase, aspartate aminotransferase, and asparagine synthetase. Nitrogen assimilation in illuminated leaves and non-photosynthetic roots occurs either in the redundant way or in the specific manner regarding the isoforms of nitrogen assimilatory enzymes in their cellular compartments. The electron supplying systems necessary to the enzymatic reactions share in part a similar electron donor system at the expense of carbohydrates in both leaves and roots, but also distinct reducing systems regarding the reactions of Fd-nitrite reductase and Fd-glutamate synthase in the photosynthetic and non-photosynthetic organs. -
Nitrite Reductase 1 Is a Target of Nitric Oxide-Mediated Post-Translational Modifications and Controls Nitrogen Flux and Growth in Arabidopsis
International Journal of Molecular Sciences Article Nitrite Reductase 1 Is a Target of Nitric Oxide-Mediated Post-Translational Modifications and Controls Nitrogen Flux and Growth in Arabidopsis Álvaro Costa-Broseta , MariCruz Castillo and José León * Instituto de Biología Molecular y Celular de Plantas, Consejo Superior de Investigaciones Científicas, Universidad Politécnica de Valencia, 46022 Valencia, Spain; [email protected] (Á.C.-B.); [email protected] (M.C.) * Correspondence: [email protected]; Tel.: +34-963877882 Received: 15 September 2020; Accepted: 29 September 2020; Published: 1 October 2020 Abstract: Plant growth is the result of the coordinated photosynthesis-mediated assimilation of oxidized forms of C, N and S. Nitrate is the predominant N source in soils and its reductive assimilation requires the successive activities of soluble cytosolic NADH-nitrate reductases (NR) and plastid stroma ferredoxin-nitrite reductases (NiR) allowing the conversion of nitrate to nitrite and then to ammonium. However, nitrite, instead of being reduced to ammonium in plastids, can be reduced to nitric oxide (NO) in mitochondria, through a process that is relevant under hypoxic conditions, or in the cytoplasm, through a side-reaction catalyzed by NRs. We use a loss-of-function approach, based on CRISPR/Cas9-mediated genetic edition, and gain-of-function, using transgenic overexpressing HA-tagged Arabidopsis NiR1 to characterize the role of this enzyme in controlling plant growth, and to propose that the NO-related post-translational modifications, by S-nitrosylation of key C residues, might inactivate NiR1 under stress conditions. NiR1 seems to be a key target in regulating nitrogen assimilation and NO homeostasis, being relevant to the control of both plant growth and performance under stress conditions. -
Differential Depth Distribution of Microbial Function and Putative Symbionts Through Sediment-Hosted Aquifers in the Deep Terrestrial Subsurface
ARTICLES https://doi.org/10.1038/s41564-017-0098-y Differential depth distribution of microbial function and putative symbionts through sediment-hosted aquifers in the deep terrestrial subsurface Alexander J. Probst1,5,7, Bethany Ladd2,7, Jessica K. Jarett3, David E. Geller-McGrath1, Christian M. K. Sieber1,3, Joanne B. Emerson1,6, Karthik Anantharaman1, Brian C. Thomas1, Rex R. Malmstrom3, Michaela Stieglmeier4, Andreas Klingl4, Tanja Woyke 3, M. Cathryn Ryan 2* and Jillian F. Banfield 1* An enormous diversity of previously unknown bacteria and archaea has been discovered recently, yet their functional capacities and distributions in the terrestrial subsurface remain uncertain. Here, we continually sampled a CO2-driven geyser (Colorado Plateau, Utah, USA) over its 5-day eruption cycle to test the hypothesis that stratified, sandstone-hosted aquifers sampled over three phases of the eruption cycle have microbial communities that differ both in membership and function. Genome- resolved metagenomics, single-cell genomics and geochemical analyses confirmed this hypothesis and linked microorganisms to groundwater compositions from different depths. Autotrophic Candidatus “Altiarchaeum sp.” and phylogenetically deep- branching nanoarchaea dominate the deepest groundwater. A nanoarchaeon with limited metabolic capacity is inferred to be a potential symbiont of the Ca. “Altiarchaeum”. Candidate Phyla Radiation bacteria are also present in the deepest groundwater and they are relatively abundant in water from intermediate depths. During the recovery phase of the geyser, microaerophilic Fe- and S-oxidizers have high in situ genome replication rates. Autotrophic Sulfurimonas sustained by aerobic sulfide oxidation and with the capacity for N2 fixation dominate the shallow aquifer. Overall, 104 different phylum-level lineages are present in water from these subsurface environments, with uncultivated archaea and bacteria partitioned to the deeper subsurface. -
Revealing the Full Biosphere Structure and Versatile Metabolic Functions In
Chen et al. Genome Biology (2021) 22:207 https://doi.org/10.1186/s13059-021-02408-w RESEARCH Open Access Revealing the full biosphere structure and versatile metabolic functions in the deepest ocean sediment of the Challenger Deep Ping Chen1†, Hui Zhou1,2†, Yanyan Huang3,4†, Zhe Xie5†, Mengjie Zhang1,2†, Yuli Wei5, Jia Li1,2, Yuewei Ma3, Min Luo5, Wenmian Ding3, Junwei Cao5, Tao Jiang1,2, Peng Nan3*, Jiasong Fang5* and Xuan Li1,2* * Correspondence: nanpeng@fudan. edu.cn; [email protected]; lixuan@ Abstract sippe.ac.cn †Ping Chen, Hui Zhou, Yanyan Background: The full biosphere structure and functional exploration of the microbial Huang, Zhe Xie and Mengjie Zhang communities of the Challenger Deep of the Mariana Trench, the deepest known contributed equally to this work. hadal zone on Earth, lag far behind that of other marine realms. 3Ministry of Education Key Laboratory for Biodiversity Science Results: We adopt a deep metagenomics approach to investigate the microbiome and Ecological Engineering, School in the sediment of Challenger Deep, Mariana Trench. We construct 178 of Life Sciences, Fudan University, Shanghai, China metagenome-assembled genomes (MAGs) representing 26 phyla, 16 of which are 5Shanghai Engineering Research reported from hadal sediment for the first time. Based on the MAGs, we find the Center of Hadal Science and microbial community functions are marked by enrichment and prevalence of Technology, College of Marine Sciences, Shanghai Ocean mixotrophy and facultative anaerobic metabolism. The microeukaryotic community is University, Shanghai, China found to be dominated by six fungal groups that are characterized for the first time 1CAS-Key Laboratory of Synthetic in hadal sediment to possess the assimilatory and dissimilatory nitrate/sulfate Biology, CAS Center for Excellence in Molecular Plant Sciences, Institute reduction, and hydrogen sulfide oxidation pathways. -
(Antarctica) Glacial, Basal, and Accretion Ice
CHARACTERIZATION OF ORGANISMS IN VOSTOK (ANTARCTICA) GLACIAL, BASAL, AND ACCRETION ICE Colby J. Gura A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2019 Committee: Scott O. Rogers, Advisor Helen Michaels Paul Morris © 2019 Colby Gura All Rights Reserved iii ABSTRACT Scott O. Rogers, Advisor Chapter 1: Lake Vostok is named for the nearby Vostok Station located at 78°28’S, 106°48’E and at an elevation of 3,488 m. The lake is covered by a glacier that is approximately 4 km thick and comprised of 4 different types of ice: meteoric, basal, type 1 accretion ice, and type 2 accretion ice. Six samples were derived from the glacial, basal, and accretion ice of the 5G ice core (depths of 2,149 m; 3,501 m; 3,520 m; 3,540 m; 3,569 m; and 3,585 m) and prepared through several processes. The RNA and DNA were extracted from ultracentrifugally concentrated meltwater samples. From the extracted RNA, cDNA was synthesized so the samples could be further manipulated. Both the cDNA and the DNA were amplified through polymerase chain reaction. Ion Torrent primers were attached to the DNA and cDNA and then prepared to be sequenced. Following sequencing the sequences were analyzed using BLAST. Python and Biopython were then used to collect more data and organize the data for manual curation and analysis. Chapter 2: As a result of the glacier and its geographic location, Lake Vostok is an extreme and unique environment that is often compared to Jupiter’s ice-covered moon, Europa. -
DNA and RNA-SIP Reveal Nitrospira Spp. As Key Drivers of Nitrification in 2 Groundwater-Fed Biofilters
bioRxiv preprint doi: https://doi.org/10.1101/703868; this version posted July 16, 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 DNA and RNA-SIP reveal Nitrospira spp. as key drivers of nitrification in 2 groundwater-fed biofilters 3 4 Running title: Nitrospira drives nitrification in groundwater-fed biofilters 5 Authors: Arda Gülay1,4*, Jane Fowler1, Karolina Tatari1, Bo Thamdrup3, Hans-Jørgen Albrechtsen1, 6 Waleed Abu Al-Soud2, Søren J. Sørensen2 and Barth F. Smets1* 7 1 Department of Environmental Engineering, Technical University of Denmark, Building 113, Miljøvej, 2800 8 Kgs Lyngby, Denmark. Phone: +45 45251600. FAX: +45 45932850. e-mail: [email protected], jfow@ 9 env.dtu.dk, [email protected], [email protected]* 10 2 Department of Biology, University of Copenhagen, Universitetsparken 15, Building 1, 2100 Copenhagen, 11 Denmark. Phone: +45 35323710. FAX: +45 35322128. e-mail: [email protected], [email protected] 12 3 Nordic Center for Earth Evolution, Department of Biology, University of Southern Denmark, Campusvej 55, 13 5230 Odense, Denmark. Phone: +45 35323710. FAX: +45 35322128. e-mail: [email protected] 14 4 Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, United States, 15 26 Oxford St, Cambridge, MA 02138, Phone: +1 (617)4951564. e-mail: [email protected] 16 17 *Corresponding authors 18 Keywords: Nitrification, comammox, Nitrospira, DNA SIP, RNA SIP 19 bioRxiv preprint doi: https://doi.org/10.1101/703868; this version posted July 16, 2019. -
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. -
The Bacterial Sulfur Cycle in Expanding Dysoxic and Euxinic Marine Waters
Environmental Microbiology (2020) 00(00), 00–00 doi:10.1111/1462-2920.15265 Special Issue Article The bacterial sulfur cycle in expanding dysoxic and euxinic marine waters Daan M. van Vliet ,1 F.A. Bastiaan von Meijenfeldt,2 bacteria, and discuss the probable involvement of Bas E. Dutilh,2 Laura Villanueva,3 uncultivated SAR324 and BS-GSO2 bacteria in sulfur Jaap S. Sinninghe Damsté,3,4 Alfons J.M. Stams1,5 oxidation. Uncultivated Marinimicrobia bacteria with and Irene Sánchez-Andrea 1* a presumed organoheterotrophic metabolism are 1Laboratory of Microbiology, Wageningen University and abundant in DMW. Like SRB, they may use specific Research, Stippeneng 4, 6708WE, Wageningen, molybdoenzymes to conserve energy from the oxida- Netherlands. tion, reduction or disproportionation of sulfur cycle 2Theoretical Biology and Bioinformatics, Science for intermediates such as S0 and thiosulfate, produced Life, Utrecht University, Padualaan 8, 3584 CH, Utrecht, from the oxidation of sulfide. We expect that tailored Netherlands. sampling methods and a renewed focus on cultiva- 3Department of Marine Microbiology and tion will yield deeper insight into sulfur-cycling bacte- Biogeochemistry, Royal Netherlands Institute for Sea ria in DMW. Research (NIOZ), Utrecht University, Landsdiep 4, 1797 SZ, ’t Horntje (Texel), Netherlands. Introduction 4Department of Earth Sciences, Faculty of Geosciences, Oxygen deficiency is a rather common phenomenon in Utrecht University, Princetonlaan 8A, 3584 CB, Utrecht, marine waters caused by microbial aerobic respiration Netherlands. coupled to the degradation of organic matter, combined 5Centre of Biological Engineering, University of Minho, with insufficient supply of oxygen through water circulation Campus de Gualtar, 4710-057 Braga, Portugal. or diffusion (Canfield et al., 2005). -
High Functional Diversity Among Nitrospira Populations That Dominate Rotating Biological Contactor Microbial Communities in a Municipal Wastewater Treatment Plant
The ISME Journal (2020) 14:1857–1872 https://doi.org/10.1038/s41396-020-0650-2 ARTICLE High functional diversity among Nitrospira populations that dominate rotating biological contactor microbial communities in a municipal wastewater treatment plant 1 1 1 1 1 2 Emilie Spasov ● Jackson M. Tsuji ● Laura A. Hug ● Andrew C. Doxey ● Laura A. Sauder ● Wayne J. Parker ● Josh D. Neufeld 1 Received: 18 October 2019 / Revised: 3 March 2020 / Accepted: 30 March 2020 / Published online: 24 April 2020 © The Author(s) 2020. This article is published with open access Abstract Nitrification, the oxidation of ammonia to nitrate via nitrite, is an important process in municipal wastewater treatment plants (WWTPs). Members of the Nitrospira genus that contribute to complete ammonia oxidation (comammox) have only recently been discovered and their relevance to engineered water treatment systems is poorly understood. This study investigated distributions of Nitrospira, ammonia-oxidizing archaea (AOA), and ammonia-oxidizing bacteria (AOB) in biofilm samples collected from tertiary rotating biological contactors (RBCs) of a municipal WWTP in Guelph, Ontario, 1234567890();,: 1234567890();,: Canada. Using quantitative PCR (qPCR), 16S rRNA gene sequencing, and metagenomics, our results demonstrate that Nitrospira species strongly dominate RBC biofilm samples and that comammox Nitrospira outnumber all other nitrifiers. Genome bins recovered from assembled metagenomes reveal multiple populations of comammox Nitrospira with distinct spatial and temporal distributions, including several taxa that are distinct from previously characterized Nitrospira members. Diverse functional profiles imply a high level of niche heterogeneity among comammox Nitrospira, in contrast to the sole detected AOA representative that was previously cultivated and characterized from the same RBC biofilm. -
Indications for Enzymatic Denitriication to N2O at Low Ph in an Ammonia
The ISME Journal (2019) 13:2633–2638 https://doi.org/10.1038/s41396-019-0460-6 BRIEF COMMUNICATION Indications for enzymatic denitrification to N2O at low pH in an ammonia-oxidizing archaeon 1,2 1 3 4 1 4 Man-Young Jung ● Joo-Han Gwak ● Lena Rohe ● Anette Giesemann ● Jong-Geol Kim ● Reinhard Well ● 5 2,6 2,6,7 1 Eugene L. Madsen ● Craig W. Herbold ● Michael Wagner ● Sung-Keun Rhee Received: 19 February 2019 / Revised: 5 May 2019 / Accepted: 27 May 2019 / Published online: 21 June 2019 © The Author(s) 2019. This article is published with open access Abstract Nitrous oxide (N2O) is a key climate change gas and nitrifying microbes living in terrestrial ecosystems contribute significantly to its formation. Many soils are acidic and global change will cause acidification of aquatic and terrestrial ecosystems, but the effect of decreasing pH on N2O formation by nitrifiers is poorly understood. Here, we used isotope-ratio mass spectrometry to investigate the effect of acidification on production of N2O by pure cultures of two ammonia-oxidizing archaea (AOA; Nitrosocosmicus oleophilus and Nitrosotenuis chungbukensis) and an ammonia-oxidizing bacterium (AOB; Nitrosomonas 15 europaea). For all three strains acidification led to increased emission of N2O. However, changes of N site preference (SP) 1234567890();,: 1234567890();,: values within the N2O molecule (as indicators of pathways for N2O formation), caused by decreasing pH, were highly different between the tested AOA and AOB. While acidification decreased the SP value in the AOB strain, SP values increased to a maximum value of 29‰ in N. oleophilus. In addition, 15N-nitrite tracer experiments showed that acidification boosted nitrite transformation into N2O in all strains, but the incorporation rate was different for each ammonia oxidizer. -
Phylogeny of Nitrogenase Structural and Assembly Components Reveals New Insights Into the Origin and Distribution of Nitrogen Fixation Across Bacteria and Archaea
microorganisms Article Phylogeny of Nitrogenase Structural and Assembly Components Reveals New Insights into the Origin and Distribution of Nitrogen Fixation across Bacteria and Archaea Amrit Koirala 1 and Volker S. Brözel 1,2,* 1 Department of Biology and Microbiology, South Dakota State University, Brookings, SD 57006, USA; [email protected] 2 Department of Biochemistry, Genetics and Microbiology, University of Pretoria, Pretoria 0004, South Africa * Correspondence: [email protected]; Tel.: +1-605-688-6144 Abstract: The phylogeny of nitrogenase has only been analyzed using the structural proteins NifHDK. As nifHDKENB has been established as the minimum number of genes necessary for in silico predic- tion of diazotrophy, we present an updated phylogeny of diazotrophs using both structural (NifHDK) and cofactor assembly proteins (NifENB). Annotated Nif sequences were obtained from InterPro from 963 culture-derived genomes. Nif sequences were aligned individually and concatenated to form one NifHDKENB sequence. Phylogenies obtained using PhyML, FastTree, RapidNJ, and ASTRAL from individuals and concatenated protein sequences were compared and analyzed. All six genes were found across the Actinobacteria, Aquificae, Bacteroidetes, Chlorobi, Chloroflexi, Cyanobacteria, Deferribacteres, Firmicutes, Fusobacteria, Nitrospira, Proteobacteria, PVC group, and Spirochaetes, as well as the Euryarchaeota. The phylogenies of individual Nif proteins were very similar to the overall NifHDKENB phylogeny, indicating the assembly proteins have evolved together. Our higher resolution database upheld the three cluster phylogeny, but revealed undocu- Citation: Koirala, A.; Brözel, V.S. mented horizontal gene transfers across phyla. Only 48% of the 325 genera containing all six nif genes Phylogeny of Nitrogenase Structural and Assembly Components Reveals are currently supported by biochemical evidence of diazotrophy.