In subtropical Hawaiian waters, about 80 % of total chlorophyll and about 60 % of C, N. P, and Si occur in the <5 km fraction. This predominance of chlorophyll in the <5 pm fraction prevails throughout the photic zone in extensive areas of the North Central Pacific Ocean. Sinking rates of various constituents reveal vertical, size-related, and daynight differences. In the deep chlorophyll layer, sinking rates were lower than those in the upper mixed layer. Flux estimates indicated that sedimentation accounted for about 7 % of daily photosynthet~c carbon production, and that particles >20 pm accounted for most of the mlcroparticulate C, N, P, and Si flux. Calculations showed that constituent turnover rates from sedimentary loss alone are < l % of other biological rate processes influencing the concentrations of these constituents (e.g. growth rate). These findings indicate that sedimentation losses from the photic zone resulting from the sinking of intact phytoplankton and/or suspended microparticulates are of comparatively minor importance to the time-dependent changes of phytoplankton biomass in subtropical waters.