The present literature on biologically mediated fluxes from the benthi
c nepheloid layer (BNL) across the sediment-water interface into the s
ediment and vice versa is reviewed. The processes involved are categor
ised according to direct bioresuspension and biodeposition, i.e. direc
t interception of the animal with particles, and those effects, which
are indirectly created by benthic organisms, e.g., changes of physical
properties in the sediments, constructions like tubes and pits and th
e corresponding changes in hydrodynamic conditions. It is concluded th
at benthic organisms significantly increase the flux of particles acro
ss the interface and that the physically created fluxes are easily mod
ified by a factor of 2 and more.