The basic theory of turbulence is reviewed, especially as it applies t
o the smallest scales, in the parameter range typical of the ocean abo
ve the thermocline but away from the direct effect of surface waves. T
he main time and length scales are defined, and related to the environ
ment experienced by particles in the size range of plankton. Two probl
ems are analysed in some detail to illustrate the application of the t
heory: the differential concentration of almost neutrally buoyant part
icles, and the size of the sensory and feeding horizon of current feed
ers.