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Collaborative metabolisms of urea and cyanate degradation in marine anammox bacterial culture.


ABSTRACT: Anammox process greatly contributes to nitrogen loss occurring in oceanic oxygen minimum zones (OMZs), where the availability of NH4+ is scarce as compared with NO2-. Remineralization of organic nitrogen compounds including urea and cyanate (OCN-) into NH4+ has been believed as an NH4+ source of the anammox process in oxygen minimum zones. However, urea- or OCN-- dependent anammox has not been well examined due to the lack of marine anammox bacterial culture. In the present study, urea and OCN- degradation in a marine anammox bacterial consortium were investigated based on 15N-tracer experiments and metagenomic analysis. Although a marine anammox bacterium, Candidatus Scalindua sp., itself was incapable of urea and OCN- degradation, urea was anoxically decomposed to NH4+ by the coexisting ureolytic bacteria (Rhizobiaceae, Nitrosomonadaceae, and/or Thalassopiraceae bacteria), whereas OCN- was abiotically degraded to NH4+. The produced NH4+ was subsequently utilized in the anammox process. The activity of the urea degradation increased under microaerobic condition (ca. 32-42 μM dissolved O2, DO), and the contribution of the anammox process to the total nitrogen loss also increased up to 33.3% at 32 μM DO. Urea-dependent anammox activities were further examined in a fluid thioglycolate media with a vertical gradient of O2 concentration, and the active collaborative metabolism of the urea degradation and anammox was detected at the lower oxycline (21 μM DO).

SUBMITTER: Oshiki M 

PROVIDER: S-EPMC10833080 | biostudies-literature | 2024 Jan

REPOSITORIES: biostudies-literature

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Collaborative metabolisms of urea and cyanate degradation in marine anammox bacterial culture.

Oshiki Mamoru M   Morimoto Emi E   Kobayashi Kanae K   Satoh Hisashi H   Okabe Satoshi S  

ISME communications 20240110 1


Anammox process greatly contributes to nitrogen loss occurring in oceanic oxygen minimum zones (OMZs), where the availability of NH<sub>4</sub><sup>+</sup> is scarce as compared with NO<sub>2</sub><sup>-</sup>. Remineralization of organic nitrogen compounds including urea and cyanate (OCN<sup>-</sup>) into NH<sub>4</sub><sup>+</sup> has been believed as an NH<sub>4</sub><sup>+</sup> source of the anammox process in oxygen minimum zones. However, urea- or OCN<sup>-</sup>- dependent anammox has no  ...[more]

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