A detailed study of C-14 dating, coarse fraction, carbonate content, and planktonic foraminifera faunal of twenty-five box cores collected from off northeastern Taiwan. Core conducted locations range from the East China Sea shelf to the southern Okinawa Trough, and the results provide an opportunity to understand the oceanographic conditions of the region where the Kuroshio Current changes flow direction from southward to northeastward. The dominant planktonic foraminifera species in this region are Neogloboquadrina dutertrei, Pulleniatina obliquiloculata, Globigerinoides ruber, and Globigerina bulloides. Distinct patterns in the special distribution of these species reflect the influence of the Kuroshio Current in the area. The concentrations of the planktonic foraminifera indicate that the upwelling center in this area is located close to 25°25'N, 122°25'E.