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      Nitrogen-fixing populations of Planctomycetes and Proteobacteria are abundant in surface ocean metagenomes

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          Abstract

          Nitrogen fixation in the surface ocean impacts global marine nitrogen bioavailability and thus microbial primary productivity. Until now, cyanobacterial populations have been viewed as the main suppliers of bioavailable nitrogen in this habitat. Although PCR amplicon surveys targeting the nitrogenase reductase gene have revealed the existence of diverse non-cyanobacterial diazotrophic populations, subsequent quantitative PCR surveys suggest that they generally occur in low abundance. Here, we use state-of-the-art metagenomic assembly and binning strategies to recover nearly one thousand non-redundant microbial population genomes from the TARA Oceans metagenomes. Among these, we provide the first genomic evidence for non-cyanobacterial diazotrophs inhabiting surface waters of the open ocean, which correspond to lineages within the Proteobacteria and, most strikingly, the Planctomycetes. Members of the latter phylum are prevalent in aquatic systems, but have never been linked to nitrogen fixation previously. Moreover, using genome-wide quantitative read recruitment, we demonstrate that the discovered diazotrophs were not only widespread but also remarkably abundant (up to 0.3% of metagenomic reads for a single population) in both the Pacific Ocean and the Atlantic Ocean northwest. Our results extend decades of PCR-based gene surveys, and substantiate the importance of heterotrophic bacteria in the fixation of nitrogen in the surface ocean.

          Abstract

          Recovery of population genomes from surface ocean samples identified non-cyanobacterial diazotrophs that were widespread and abundant, including Proteobacteria and Planctomycetes, indicating their importance for nitrogen fixation in this environment.

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          Most cited references48

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          Processes and patterns of oceanic nutrient limitation

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            Fast algorithms for large-scale genome alignment and comparison.

            We describe a suffix-tree algorithm that can align the entire genome sequences of eukaryotic and prokaryotic organisms with minimal use of computer time and memory. The new system, MUMmer 2, runs three times faster while using one-third as much memory as the original MUMmer system. It has been used successfully to align the entire human and mouse genomes to each other, and to align numerous smaller eukaryotic and prokaryotic genomes. A new module permits the alignment of multiple DNA sequence fragments, which has proven valuable in the comparison of incomplete genome sequences. We also describe a method to align more distantly related genomes by detecting protein sequence homology. This extension to MUMmer aligns two genomes after translating the sequence in all six reading frames, extracts all matching protein sequences and then clusters together matches. This method has been applied to both incomplete and complete genome sequences in order to detect regions of conserved synteny, in which multiple proteins from one organism are found in the same order and orientation in another. The system code is being made freely available by the authors.
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              Biogeochemical Controls and Feedbacks on Ocean Primary Production

              Changes in oceanic primary production, linked to changes in the network of global biogeochemical cycles, have profoundly influenced the geochemistry of Earth for over 3 billion years. In the contemporary ocean, photosynthetic carbon fixation by marine phytoplankton leads to formation of approximately 45 gigatons of organic carbon per annum, of which 16 gigatons are exported to the ocean interior. Changes in the magnitude of total and export production can strongly influence atmospheric CO2 levels (and hence climate) on geological time scales, as well as set upper bounds for sustainable fisheries harvest. The two fluxes are critically dependent on geophysical processes that determine mixed-layer depth, nutrient fluxes to and within the ocean, and food-web structure. Because the average turnover time of phytoplankton carbon in the ocean is on the order of a week or less, total and export production are extremely sensitive to external forcing and consequently are seldom in steady state. Elucidating the biogeochemical controls and feedbacks on primary production is essential to understanding how oceanic biota responded to and affected natural climatic variability in the geological past, and will respond to anthropogenically influenced changes in coming decades. One of the most crucial feedbacks results from changes in radiative forcing on the hydrological cycle, which influences the aeolian iron flux and, in turn, affects nitrogen fixation and primary production in the oceans.
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                Author and article information

                Contributors
                tomodelmont@gmail.com
                meren@uchicago.edu
                Journal
                Nat Microbiol
                Nat Microbiol
                Nature Microbiology
                Nature Publishing Group UK (London )
                2058-5276
                11 June 2018
                11 June 2018
                2018
                : 3
                : 7
                : 804-813
                Affiliations
                [1 ]ISNI 0000 0004 1936 7822, GRID grid.170205.1, Department of Medicine, , University of Chicago, ; Chicago, IL USA
                [2 ]ISNI 0000 0000 8809 1613, GRID grid.7372.1, Warwick Medical School, , University of Warwick, ; Coventry, UK
                [3 ]ISNI 0000 0004 1936 7822, GRID grid.170205.1, Graduate Program in the Biophysical Sciences, , University of Chicago, ; Chicago, IL USA
                [4 ]ISNI 0000 0001 2188 0957, GRID grid.410445.0, Hawaii Institute of Marine Biology, , University of Hawaii at Manoa, ; Kaneohe, HI USA
                [5 ]ISNI 0000 0001 0695 7223, GRID grid.267468.9, School of Freshwater Sciences, , University of Wisconsin-Milwaukee, ; Milwaukee, WI USA
                [6 ]ISNI 0000000122931605, GRID grid.5590.9, Department of Microbiology, , Radboud University, ; Nijmegen, The Netherlands
                [7 ]ISNI 000000012169920X, GRID grid.144532.5, Josephine Bay Paul Center, , Marine Biological Laboratory, ; Woods Hole, MA USA
                [8 ]ISNI 0000 0004 1936 7822, GRID grid.170205.1, Committee on Microbiology, , University of Chicago, ; Chicago, IL USA
                Author information
                http://orcid.org/0000-0001-7053-7848
                http://orcid.org/0000-0001-9013-4827
                Article
                176
                10.1038/s41564-018-0176-9
                6792437
                29891866
                c2088b78-7ae1-44aa-af4c-0f0c2ca684e1
                © The Author(s) 2018

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 25 May 2017
                : 15 May 2018
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                © The Author(s) 2018

                microbial ecology,metagenomics,marine microbiology,bacterial genomics

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