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      Oxygen at Nanomolar Levels Reversibly Suppresses Process Rates and Gene Expression in Anammox and Denitrification in the Oxygen Minimum Zone off Northern Chile

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          ABSTRACT

          A major percentage (20 to 40%) of global marine fixed-nitrogen loss occurs in oxygen minimum zones (OMZs). Concentrations of O 2 and the sensitivity of the anaerobic N 2-producing processes of anammox and denitrification determine where this loss occurs. We studied experimentally how O 2 at nanomolar levels affects anammox and denitrification rates and the transcription of nitrogen cycle genes in the anoxic OMZ off Chile. Rates of anammox and denitrification were reversibly suppressed, most likely at the enzyme level. Fifty percent inhibition of N 2 and N 2O production by denitrification was achieved at 205 and 297 nM O 2, respectively, whereas anammox was 50% inhibited at 886 nM O 2. Coupled metatranscriptomic analysis revealed that transcripts encoding nitrous oxide reductase ( nosZ), nitrite reductase ( nirS), and nitric oxide reductase ( norB) decreased in relative abundance above 200 nM O 2. This O 2 concentration did not suppress the transcription of other dissimilatory nitrogen cycle genes, including nitrate reductase ( narG), hydrazine oxidoreductase ( hzo), and nitrite reductase ( nirK). However, taxonomic characterization of transcripts suggested inhibition of narG transcription in gammaproteobacteria, whereas the transcription of anammox narG, whose gene product is likely used to oxidatively replenish electrons for carbon fixation, was not inhibited. The taxonomic composition of transcripts differed among denitrification enzymes, suggesting that distinct groups of microorganisms mediate different steps of denitrification. Sulfide addition (1 µM) did not affect anammox or O 2 inhibition kinetics but strongly stimulated N 2O production by denitrification. These results identify new O 2 thresholds for delimiting marine nitrogen loss and highlight the utility of integrating biogeochemical and metatranscriptomic analyses.

          IMPORTANCE

          The removal of fixed nitrogen via anammox and denitrification associated with low O 2 concentrations in oceanic oxygen minimum zones (OMZ) is a major sink in oceanic N budgets, yet the sensitivity and dynamics of these processes with respect to O 2 are poorly known. The present study elucidated how nanomolar O 2 concentrations affected nitrogen removal rates and expression of key nitrogen cycle genes in water from the eastern South Pacific OMZ, applying state-of-the-art 15N techniques and metatranscriptomics. Rates of both denitrification and anammox responded rapidly and reversibly to changes in O 2, but denitrification was more O 2 sensitive than anammox. The transcription of key nitrogen cycle genes did not respond as clearly to O 2, although expression of some of these genes decreased. Quantifying O 2 sensitivity of these processes is essential for predicting through which pathways and in which environments, from wastewater treatment to the open oceans, nitrogen removal may occur.

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          Most cited references61

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          Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis

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            Cell biology and molecular basis of denitrification.

            W Zumft (1997)
            Denitrification is a distinct means of energy conservation, making use of N oxides as terminal electron acceptors for cellular bioenergetics under anaerobic, microaerophilic, and occasionally aerobic conditions. The process is an essential branch of the global N cycle, reversing dinitrogen fixation, and is associated with chemolithotrophic, phototrophic, diazotrophic, or organotrophic metabolism but generally not with obligately anaerobic life. Discovered more than a century ago and believed to be exclusively a bacterial trait, denitrification has now been found in halophilic and hyperthermophilic archaea and in the mitochondria of fungi, raising evolutionarily intriguing vistas. Important advances in the biochemical characterization of denitrification and the underlying genetics have been achieved with Pseudomonas stutzeri, Pseudomonas aeruginosa, Paracoccus denitrificans, Ralstonia eutropha, and Rhodobacter sphaeroides. Pseudomonads represent one of the largest assemblies of the denitrifying bacteria within a single genus, favoring their use as model organisms. Around 50 genes are required within a single bacterium to encode the core structures of the denitrification apparatus. Much of the denitrification process of gram-negative bacteria has been found confined to the periplasm, whereas the topology and enzymology of the gram-positive bacteria are less well established. The activation and enzymatic transformation of N oxides is based on the redox chemistry of Fe, Cu, and Mo. Biochemical breakthroughs have included the X-ray structures of the two types of respiratory nitrite reductases and the isolation of the novel enzymes nitric oxide reductase and nitrous oxide reductase, as well as their structural characterization by indirect spectroscopic means. This revealed unexpected relationships among denitrification enzymes and respiratory oxygen reductases. Denitrification is intimately related to fundamental cellular processes that include primary and secondary transport, protein translocation, cytochrome c biogenesis, anaerobic gene regulation, metalloprotein assembly, and the biosynthesis of the cofactors molybdopterin and heme D1. An important class of regulators for the anaerobic expression of the denitrification apparatus are transcription factors of the greater FNR family. Nitrate and nitric oxide, in addition to being respiratory substrates, have been identified as signaling molecules for the induction of distinct N oxide-metabolizing enzymes.
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              Global patterns of marine nitrogen fixation and denitrification

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                Author and article information

                Journal
                mBio
                MBio
                mbio
                mbio
                mBio
                mBio
                American Society of Microbiology (1752 N St., N.W., Washington, DC )
                2150-7511
                28 October 2014
                Nov-Dec 2014
                : 5
                : 6
                : e01966-14
                Affiliations
                [ a ]Department of Bioscience, Aarhus University, Silkeborg, Denmark
                [ b ]Arctic Research Centre, Aarhus University, Aarhus, Denmark
                [ c ]School of Biology, Georgia Institute of Technology, Atlanta, Georgia, USA
                [ d ]Department of Biology and Nordic Center for Earth Evolution (NordCEE), University of Southern Denmark, Odense, Denmark
                [ e ]Department of Bioscience, Aarhus University, Aarhus, Denmark
                [ f ]Departamento de Oceanografía & Instituto Mileno de Oceanografía, Universidad de Concepción, Concepción, Chile
                [ g ]Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA
                [ h ]Department of Oceanography, University of Hawai’i, Mānoa, Hawai’i, USA
                Author notes
                Address correspondence to Tage Dalsgaard, tda@ 123456dmu.dk .

                Editor Douglas G. Capone, University of Southern California

                This article is a direct contribution from a Fellow of the American Academy of Microbiology.

                Author information
                http://orcid.org/0000-0003-2604-6499
                Article
                mBio01966-14
                10.1128/mBio.01966-14
                4217175
                25352619
                6b592e5b-dda5-4a5f-aec1-c1600b71db38
                Copyright © 2014 Dalsgaard et al.

                This is an open-access article distributed under the terms of the Creative Commons Attribution-Noncommercial-ShareAlike 3.0 Unported license, which permits unrestricted noncommercial use, distribution, and reproduction in any medium, provided the original author and source are credited.

                History
                : 17 September 2014
                : 23 September 2014
                Page count
                Pages: 14
                Categories
                Research Article
                Custom metadata
                November/December 2014

                Life sciences
                Life sciences

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