EGU24-4027, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-4027
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

N2O Assimilation, a New N2O Sink and Organic Nitrogen Source in Aquatic Ecosystems

Guangbo Li1 and Qixing Ji2
Guangbo Li and Qixing Ji
  • 1Division of Emerging Interdisciplinary Areas, Academy of Interdisciplinary Studies, The Hong Kong University of Science and Technology, Hong Kong, China
  • 2Earth, Ocean and Atmospheric Sciences Thrust, Function Hub, The Hong Kong University of Science and Technology (Guangzhou), Guangzhou, China

Nitrous oxide (N2O) is a strong greenhouse gas with ozone layer destruction ability, and its atmospheric concentration has been increasing rapidly due to anthropogenic activities. N2O reduction to dinitrogen (N2), the last step of denitrification, was recognized as the only biological N2O sink. Recently, diazotrophic N2O assimilation to organic nitrogen in biomass by nitrogenase has been discovered in the eastern South Pacific Ocean and cultured diazotroph Crocosphaera and Trichodesmium. N2O assimilation to organic nitrogen is thermodynamically more favored than N2 fixation in higher N2O concentration and cooler environments, but the distribution and detailed mechanism of this new N2O sink are still unclear. We applied isotopic tracing experiments to validate and measure N2O assimilation and built an enzymatic kinetics model for a mechanistic explanation. Cultured diazotroph Crocosphaera (WH8501) and Trichodesmium (IMS101) both showed evident N2O assimilation rates of 0.751 nM N h-1 for Crocosphaera at [N2O]/[N2] = 0.0075, 0.690 nM N h-1 for Trichodesmium at [N2O]/[N2] = 0.01, and 0.481 nM N h-1 for Trichodesmium at [N2O]/[N2] = 0.0005. Although N2O assimilation was assumed to be carried out by nitrogenase, it was asynchronous with the diel rhythmicity of N2 fixation. Field samples from the Pearl River Estuary did not demonstrate the presence of N2O assimilation. Since N2 fixation was absent as well, the isotopic tracer 46N2O barely introduced influences on nitrogen isotopic composition compared to photosynthesis and remineralization, indicating that N2O assimilation is an insignificant N2O sink in eutrophic estuarine waters. Our enzymatic kinetic model revealed that N2 rather than N2O dominated the overall growth rates of cultured diazotrophs. The model indicated the [N2O]/[N2] required for the presence of N2O assimilation in isotopic tracing experiments and explained the absence of this process under natural N2 concentration environments. The insights from this study may suggest new engineering methods to control N2O emissions.

How to cite: Li, G. and Ji, Q.: N2O Assimilation, a New N2O Sink and Organic Nitrogen Source in Aquatic Ecosystems, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-4027, https://doi.org/10.5194/egusphere-egu24-4027, 2024.