Dissolved and particulate thorium-234, particulate organic carbon in the upper 150 m of water columns from five stations in the Prydz Bay, the Southern Ocean were determined during the 22nd Chinese National Antarctic Research Expedition (from November 2005 to March 2006). The disequilibria between thorium-234 and its parent uranium-238 in upper layer was used to derive the averaged residence time of thorium-234, which decreased along with the latitude to the south and a minimum value, 1~8 d for particulate thorium-234 and 29~48 d for dissolved thorium-234, appeared at the medium latitude station, and the export fluxes of thorium-234 were calculated too and a maximum value, 0.35~0.63 Bq/(m3·d) for the particulate thorium-234 and 0.44~0.65 Bq/(m3·d) for the dissolved thorium-234, appeared at the same station. The export fluxes of particulate organic carbon at different water columns were derived by two methods with irreversible scavenging model, and the averaged values were 104.7 mmol/ (m2·d) (E method) and 120.6 mmol/(m2·d) (B method), respectively, indicating that a relatively high new production would exist in summer in the Prydz Bay where it will play a potential significant role in sequestering the absorption CO2 to deeper ocean. Dissolved and particulate thorium-234, particulate organic carbon in the upper 150 m of water columns from five stations in the Prydz Bay, the southern Ocean were determined during the 22nd Chinese National Antarctic Research Expedition (from November 2005 to March 2006). The disequilibria between thorium-234 and its parent uranium-238 in upper layer was used to derive the averaged residence time of thorium-234, which decreased along with the latitude to the south and a minimum value, 1 to 8 days for particulate thorium-234 and 29 to 48 d for dissolved thorium-234, at the medium latitude station, and the export fluxes of thorium-234 were calculated too and a maximum value, 0.35 to 0.63 Bq / (m3 · d) for the particulate thorium-234 and 0.44-0.65 Bq / (m3 · d) for the dissolved thorium-234, at the same station. The export fluxes of particulate organic carbon at different water columns were derived by two methods with irreversible scavenging model, and the averaged values ​​were 104.7 mmol / (m2 · d) (E method) and 120.6 mmol / (m2 · d) (B method), respectively, indicating that a relatively high new production would exist in summer in the Prydz Bay where it will play a potential significant role in sequestering the absorption CO2 to deeper ocean.