Chih-An Huh a,), Chih-Chieh Su a,b

Sedimentation dynamics in the East China Sea was investigated based on profiles and inventories of 210Pb, 137Cs andex 239,240Pu in sediment cores collected from various settings in this marginal sea. The derived sedimentation rates vary by two orders of magnitude, from;2 to 0.02 cm yry1, and generally decrease southward along the inner shelf and eastward offshore. This pattern is consistent with the dispersal of Yangtze River-derived sediments by the current and tidal systems. y2 y1.The weighted mean sedimentation rate over the shelf ca. 0.3 g cm yr appears to be higher than fluvial inputs from the y2 y1.Yangtze River and Taiwan 0.14 g cm yr. The discrepancy can be reduced by considering the effect of sediment .mixing which renders sedimentation rates overestimated and the possibility of additional sediment input from the Yellow River’s dispersal system. Spatial variations of the observed nuclide inventories in sediments suggest extensive sediment redistribution, boundary scavenging of 210Pb, and large inputs of 137Cs and 239,240Pu from Yangtze River’s drainage basin