Following isopycnic sedimentation in density gradients of colloidal silica (Ludox AM), zooplankton segregated into 3 broad bands of increasing density which included, respectively, fish eggs, invertebrates, and fish larvae. The zone of fish eggs was contaminated with Sagitta spp. and the zone of fish larvae was overlapped partially by mysids and euphausids. We have sought to minimize contamination through modifications of the silica gradients which might shift banding densities of the ichthyoplankton or of the contaminating invertebrates. Density shifts in fact occurred in different commercial formulations of silica sols and in gradients modified by small amounts of polymers, osmotica or charged small molecules.
Sagitta were specifically shifted out of the zone of fish eggs by the addition of I% w/v dextran sulfate or in a silica sol composed of very small particles of silica (Naleoag 1115). Fish larvae were shifted to higher densities by the addition of I% w/v trimetaphosphate or I% w/v dextran sulfate. Additions of I% w/v polyvinyl alcohol, and of I0 mM glycine, and potassium phosphate had intermediate effects. The same banding densities of plankton in silica gradients were reached in less than IO h at one gravity, independent of the immediate pretreatment of the sample.