中文摘要：

对东海陆架外黑潮区颗粒有机碳（POC）和生物硅（bSiO2）的研究表明：台湾东北部黑潮主流真光层（100m）POC和bSi02的平均浓度分别为3．31μmol／L和0．68μmol／L；^234Th／^238U不平衡法获得POC和bSi02的输出通量分别为3．7mmol／（m^2·d）和1．6mmol／（m^2·d）．黑潮沿东海陆架北进过程中，POC和bSiO2的含量及输出通量均呈增加趋势．位于日本西南的黑潮主流中，POC和bSiO2的平均浓度分别为3．85μmol／L和2．63μmol／L，输出通量分别为6．7mmol／（m^2·d）和4．0mmol／（m^2·d）．黑潮与陆架水形成的锋面区，POC和bSiO2浓度均高于黑潮主流．

英文摘要：

To reveal the primary characteristics of the POC and biogenic silica （bSiO2 ） in the Kuroshio, as well as their export from the euphoric zone, POC, bSiO2 and 234Th were examined. The average con- centrations of POC and bSiOz were 3.31 μmol/L and 0.68 μmol/L in the main Kuroshio stream to north- east Taiwan respectively, corresponding to their respective export fluxes of 3.7 retool/（ m2 d ） and 1.6 mmol/（m2 d）. Along the flow of Kuroshio northwards, the concentrations of both POC and bSiO2 increased to a varying degree. To southwest Japan, the contents of POC and bSiO2 increased up to 3.85 μmol/L and 2.63 μmol/L respectively. The export fluxes of POC increased to 6. 7 retool/（ m2 d）, accompanying the bSiO2 flux of 4.0 mmol/（ m2 d）. The average concentrations of POC and bSiO2 in the Kuroshio frontal zone were higher than the values in the main stream.