Differential kinetic responses of ammonia oxidation and nitrite oxidation to light radiation in the South China Sea
ID:466 View Protection:ATTENDEE Updated Time:2026-08-31 16:41:58 Hits:28 Poster Presentation

Start Time:2027-01-15 19:00(Asia/Shanghai)

Duration:15min

Session:S69 Session 69 - The nitrogen cycle in a changing ocean: from the process level to basin scale » S69PS69-Poster

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Abstract
Ammonia oxidation and nitrite oxidation are the two sequential steps of marine nitrification, and their coupling determines the efficiency of inorganic nitrogen transformation in the euphotic zone. Light is considered a key environmental factor regulating this coupling. However, current understanding of light inhibition relies largely on changes in bulk rates, which cannot reveal whether light alters the substrate utilization kinetics of nitrifying microorganisms, thereby limiting mechanistic understanding of light-regulated coupling between ammonia oxidation and nitrite oxidation.Using 15N stable isotope tracers, we determined the Michaelis–Menten kinetic parameters (Km, Vmax, and α) for ammonia oxidation and nitrite oxidation from matrix incubations with five light intensities and five substrate concentrations in the South China Sea. The two processes exhibited distinct kinetic responses to light. In particular, the responses of Km and α to increasing irradiance differed between ammonia oxidation and nitrite oxidation, suggesting that light influences not only nitrification rates but also the substrate utilization kinetics of the two processes. These findings provide kinetic evidence for the differential effects of light on the two nitrification steps and improve our understanding of environmental regulation of nitrification coupling in the euphotic ocean.
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Speaker
Li Liu
Wenzhou University

Submission Author
Li Liu Wenzhou University
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Important Date
  • Conference Date

    Jan 12

    2027

    to

    Jan 15

    2027

  • Jul 21 2026

    Draft paper submission deadline

  • Jan 15 2027

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University (MEL)
Department of Earth Sciences, National Natural Science Foundation of China (NSFC)
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