The uptake of dissolved trace metals, such as zinc and cadmium, by cru
staceans can often be explained in terms of physicochemical changes be
yond the physiological control of the crustacean itself. Thus, uptake
rates increase with dissolved metal concentration of exposure. Further
more, at a given metal concentration, changes in uptake rates of zinc
and cadmium can typically be explained by changes in the concentration
(availability) of the hydrated free metal ion, for example as affecte
d physicochemically by salinity change or the presence of metal-chelat
ing agents. Nevertheless, some crustaceans appear able to counteract t
o varying degrees such physicochemical effects by what appear to be ph
ysiological responses, for example, to low salinity. Such responses va
ry interspecifically, and cast light on the mechanisms of trace metal
uptake by crustaceans.