Estimation of N and N₂O cycling processes using the information of bacterial functional genes in the East Sea
- 1Department of Marine Science, Incheon National University, Incheon, South Korea (hyoryeonkim@inu.ac.kr, kmsy0227@inu.ac.kr, ilnamkim@inu.ac.kr)
- 2Marine Environmental Research Division, National Institute of Fisheries Science, Busan, South Korea (lim900@korea.kr)
- 3Fisheries Resources and Environment Research Division, East Sea Fisheries Research Institute, National Institute of Fisheries Science, Gangneung, South Korea (hkjung85@korea.kr)
Marine nitrogen (N) cycle plays important roles in controlling marine ecosystem and biogeochemistry, as it is well known as a limiting element for marine productivity and significantly influences on the carbon and phosphorus cycles in the marine environment. Also, nitrous oxide (N₂O) production via marine N cycling is regarding as climate interaction with a big concern owing to its significant warming potential in the atmosphere. The East Sea (ES) is a semi-enclosed marginal sea, but frequently referred to as a miniature ocean as it shows multiple ocean dynamic processes. Recently, a number of studies reported that the ES is rapidly changing due to anthropogenic perturbations. Given that understanding of the ES’s biogeochemical cycles under such a condition is apparently urgent, we have little knowledge about particularly N cycling and N₂O production mechanisms to date. At present, the application of metagenomics approaches is widely used for understanding marine N cycle as an important means. Here, using the information of bacterial functional genes, we for the first time investigate (1) N cycling processes and (2) N2O production pathways during June and October 2021 at three different depths (0m, 150m, and 750m) of the ES.
How to cite: Kim, H.-R., Lim, J.-H., Jung, H.-K., Kim, S.-Y., and Kim, I.-N.: Estimation of N and N₂O cycling processes using the information of bacterial functional genes in the East Sea, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-4899, https://doi.org/10.5194/egusphere-egu23-4899, 2023.