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  • Computer-simulated concentration profiles; File format; File name; File size; Microsensor concentration profiles; Uniform resource locator/link to file  (1)
  • Daily cycle  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Klawonn, Isabell; Eichner, Meri J; Wilson, Samuel T; Moradi, Nasrollah; Thamdrup, Bo; Kümmel, Steffen; Gehre, Matthias; Khalili, Arzhang; Grossart, Hans-Peter; Karl, David Michael; Ploug, Helle (2020): Distinct nitrogen cycling and steep chemical gradients in Trichodesmium colonies. The ISME Journal, 14(2), 399-412, https://doi.org/10.1038/s41396-019-0514-9
    Publication Date: 2023-01-13
    Description: Trichodesmium is an important dinitrogen (N~2~)-fixing cyanobacterium in marine ecosystems. Recent nucleic acid analyses indicate that Trichodesmium colonies with their diverse epibionts support various nitrogen (N) transformations beyond N~2~-fixation. However, rates of these transformations and concentration gradients of N-compounds in Trichodesmium colonies remain largely unresolved. We combined isotope-tracer incubations, micro-profiling, and numeric modelling to explore carbon fixation, N-cycling processes, as well as oxygen, ammonium and nitrate concentration gradients in individual field-sampled Trichodesmium colonies. Colonies were net-autotrophic, with carbon and N~2~-fixation occurring mostly at day-time. Ten percent of the fixed N was released as ammonium after 12-hour incubations. Nitrification was not detectable but nitrate consumption was high when nitrate was added. The consumed nitrate was partly reduced to ammonium, while denitrification was insignificant. Thus, the potential N-transformation network was characterized by fixed N gain and recycling processes rather than denitrification. Oxygen concentrations within colonies were 60–200% air-saturation. Moreover, our modelling predicted steep concentration gradients, with up to 6-fold higher ammonium concentrations, and nitrate depletion in the colony centre compared to the ambient seawater. These gradients created a chemically heterogeneous microenvironment, presumably facilitating diverse microbial metabolisms in millimetre-sized Trichodesmium colonies.
    Keywords: Computer-simulated concentration profiles; File format; File name; File size; Microsensor concentration profiles; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-10-26
    Description: © The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Inomura, K., Deutsch, C., Wilson, S. T., Masuda, T., Lawrenz, E., Lenka, B., Sobotka, R., Gauglitz, J. M., Saito, M. A., Prášil, O., & Follows, M. J. Quantifying oxygen management and temperature and light dependencies of nitrogen fixation by Crocosphaera watsonii. Msphere, 4(6), (2019): e00531-19, doi: 10.1128/msphere.00531-19.
    Description: Crocosphaera is a major dinitrogen (N2)-fixing microorganism, providing bioavailable nitrogen (N) to marine ecosystems. The N2-fixing enzyme nitrogenase is deactivated by oxygen (O2), which is abundant in marine environments. Using a cellular scale model of Crocosphaera sp. and laboratory data, we quantify the role of three O2 management strategies by Crocosphaera sp.: size adjustment, reduced O2 diffusivity, and respiratory protection. Our model predicts that Crocosphaera cells increase their size under high O2. Using transmission electron microscopy, we show that starch granules and thylakoid membranes are located near the cytoplasmic membranes, forming a barrier for O2. The model indicates a critical role for respiration in protecting the rate of N2 fixation. Moreover, the rise in respiration rates and the decline in ambient O2 with temperature strengthen this mechanism in warmer water, providing a physiological rationale for the observed niche of Crocosphaera at temperatures exceeding 20°C. Our new measurements of the sensitivity to light intensity show that the rate of N2 fixation reaches saturation at a lower light intensity (∼100 μmol m−2 s−1) than photosynthesis and that both are similarly inhibited by light intensities of 〉500 μmol m−2 s−1. This suggests an explanation for the maximum population of Crocosphaera occurring slightly below the ocean surface.
    Description: We thank Stephanie Dutkiewicz and Sallie W. Chisholm for useful discussion, Martin Lukeš for technical assistance for the N2 fixation measurement, and the members of Writing and Communication Center at MIT for their advice on writing. This research was supported by the Japan Student Service Organization (JASSO) (grant L11171020001 to K.I.), the Gordon and Betty Moore Foundation (grant GBMF 3775 to C.D. and grant GBMF 3778 to M.J.F.), the U.S. National Science Foundation (grant OCE-1756524 to S.T.W., grant OCE-1558702 to M.J.F., and grant OCE-PRF 1421196 to J.M.G), the Simons Foundation (Simons Postdoctoral Fellowship in Marine Microbial Ecology award 544338 to K.I., Simons Collaboration on Ocean Processes and Ecology award 329108 to M.J.F., Simons Collaboration on Computational BIOgeochemical Modeling of Marine EcosystemS [CBIOMES] award 549931 to M.J.F.), the Czech Science Foundation (GAČR) (grant 16-15467S to O.P.), and the National Sustainability Programme (NPU) (grant LO1416 Algatech plus to O.P.).
    Keywords: Crocosphaera ; Carbon ; Cell flux model ; Daily cycle ; Iron ; Light ; Nitrogen ; Nitrogen fixation ; Oxygen ; Photosynthesis ; Temperature
    Repository Name: Woods Hole Open Access Server
    Type: Article
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