Dissimilatory Nitrate Reduction to Ammonium and Responsible Microbes in Japanese Rice Paddy Soil

  • Nojiri Yosuke
    Graduate School of Agricultural and Life Sciences, The University of Tokyo
  • Kaneko Yuka
    Graduate School of Agricultural and Life Sciences, The University of Tokyo
  • Azegami Yoichi
    Graduate School of Agricultural and Life Sciences, The University of Tokyo
  • Shiratori Yutaka
    Niigata Agricultural Research Institute
  • Ohte Nobuhito
    Graduate School of Informatics, Kyoto University
  • Senoo Keishi
    Graduate School of Agricultural and Life Sciences, The University of Tokyo Collaborative Research Institute for Innovative Microbiology, The University of Tokyo
  • Otsuka Shigeto
    Graduate School of Agricultural and Life Sciences, The University of Tokyo Collaborative Research Institute for Innovative Microbiology, The University of Tokyo
  • Isobe Kazuo
    Graduate School of Agricultural and Life Sciences, The University of Tokyo

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Abstract

<p>Nitrification–denitrification processes in the nitrogen cycle have been extensively examined in rice paddy soils. Nitrate is generally depleted in the reduced soil layer below the thin oxidized layer at the surface, and this may be attributed to high denitrification activity. In the present study, we investigated dissimilatory nitrate reduction to ammonium (DNRA), which competes with denitrification for nitrate, in order to challenge the conventional view of nitrogen cycling in paddy soils. We performed paddy soil microcosm experiments using 15N tracer analyses to assess DNRA and denitrification rates and conducted clone library analyses of transcripts of nitrite reductase genes (nrfA, nirS, and nirK) in order to identify the microbial populations carrying out these processes. The results obtained showed that DNRA occurred to a similar extent to denitrification and appeared to be enhanced by a nitrate limitation relative to organic carbon. We also demonstrated that different microbial taxa were responsible for these distinct processes. Based on these results and previous field observations, nitrate produced by nitrification within the surface oxidized layer may be reduced not only to gaseous N2 via denitrification, but also to NH4+ via DNRA, within the reduced layer. The present results also indicate that DNRA reduces N loss through denitrification and nitrate leaching and provides ammonium to rice roots in rice paddy fields.</p>

Journal

  • Microbes and Environments

    Microbes and Environments 35 (4), n/a-, 2020

    Japanese Society of Microbial Ecology / Japanese Society of Soil Microbiology / Taiwan Society of Microbial Ecology / Japanese Society of Plant Microbe Interactions / Japanese Society for Extremophiles

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