Two marine bivalve shells were collected from the eastern and western coastal regions of Korea, respectively. Stable oxygen and carbon isotope profiles are constructed using the incremental sampling along the axis of maximum growth to provide the continuous ${delta}^{18}$O and ${delta}^{13}$C records, which register the physical, biological and chemical properties of seawater where the organisms live. Cycles in the ${delta}^{18}$O profiles are interpreted as annual along with the identification of annual growth bands; the maximum ${delta}^{18}$O values correspond with the coldest temperature of seawater whereas the minimum ${delta}^{18}$O values with the warmest temperature. The primary control on the amplitude of the ${delta}^{18}$O profiles is seasonal variation of seawater temperature. The offset of the baseline between ${delta}^{18}$O values of the two specimens is attributed to differences in both temperature and seawater ${delta}^{18}$O values between two localities. The ${delta}^{13}$C profiles show the similar seasonality of carbon cycling associated with phytoplankton productivity. The offset in the ${delta}^{13}$C profiles between two specimens may be, as in the case of oxygen isotope profile, attributed to the different ${delta}^{13}$C value of the seawater DIC (dissolved inorganic carbon) between the western coast and the eastern coast. Relationships between the shell isotopic composition and the coastal water properties of shell growth are readily interpreted from the ${delta}^{18}$O-${delta}^{13}$C pair diagram of the shell isotope data, similar to the use of salinity-${delta}^{18}$O diagram for identifying water masses. The preliminary stable isotope results of this study suggest that mollusk shell isotope geochemistry may be useful to monitor the properties of water masses in the coastal and inner shelf setting around Korea and improve the interpretation of paleoceanography, provided the fossil mollusks are well preserved.