Carbon and nitrogen dynamics in the Sea of Japan (SOJ) are rapidly changing. Here, we investigated the carbon and nitrogen isotope ratios of particulate organic matter (δ 13 C POM and δ 15 N POM , respectively) at a depth of [?] 100 m in the southern part of the SOJ from 2016 to 2021. Both δ 13 C POM and δ 15 N POM showed multimodal distributions and were divided into four classes (I-IV) using the Gaussian mixed model. Most of the samples were categorized into class II (n = 441), with the mean ± standard deviation (SD) of δ 13 C POM and δ 15 N POM being -23.7 ± 1.2 1.2 δ 15 N POM (-2.1 ± 0.8 class III by low δ 13 C POM (-27.1 ± 1.0 δ 13 C POM (-20.7 ± 0.8 34). Using the generalized linear model (GLM), temperature and chlorophyll-a concentration were found to positively impact δ 13 C POM in addition to sampling depth, latitude, salinity, and nitrate concentration, supporting the hypothesis that active photosynthesis and phytoplankton growth elevated δ 13 C POM . The mean δ 15 N POM value suggests that primary production mainly originates from nitrate in the SOJ. The δ 15 N POM variation, however, was explained by temperature and salinity but not by nitrate concentration in the GLM approach, which suggests that the Rayleigh distillation model was not observed in the SOJ. This suggests that primary production is supported by various nitrogenous sources from the Changjiang, Kuroshio, and atmospheric depositions in the SOJ.