H. Hummell et al., A COMPARATIVE-STUDY ON THE RELATION BETWEEN COPPER AND CONDITION IN MARINE BIVALVES AND THE RELATION WITH COPPER IN THE SEDIMENT, Aquatic toxicology, 38(1-3), 1997, pp. 165-181
The relation between condition and copper concentration was assessed i
n three bivalve species (the Baltic clam Macoma balthica, the cockle C
erastoderma edule and the mussel Mytilus edulis) from several Dutch an
d French estuaries. In general, the copper concentration in the bivalv
es was negatively related to condition. The slope of this relation was
strongest in the Baltic clam M. balthica, with an almost inversely pr
oportional change of Cu concentration at a change of condition, indica
ting an almost constant Cu content (body burden) per individual, i.e.
no elimination or accumulation of Cu. In the mussel M. edulis, the slo
pe of this relation was absent or the weakest, with an almost uniform
Cu concentration at a change of condition, indicating an almost propor
tional elimination (or accumulation) of Cu at a decrease (or increase)
of the condition. Thus in Baltic clams the copper body burden is kept
at an almost constant level, whereas in mussels the copper concentrat
ion is almost constant. In Baltic clams, but not in mussels and cockle
s, spatial differences were related to copper concentrations in the se
diment. It is discussed that mussels maintain a homeostatic Cu concent
ration within a short time-period (days; copper highly exchangeable by
complexation to metallothioneins), whereas the Cu concentration in Ba
ltic clams is more slowly regulated (several weeks; fossilization of c
opper in mineral granules) and remains on an average in (partitioning)
equilibrium with the Cu concentration in the sediment. Therefore, the
Baltic clam is a better indicator of sediment copper pollution than t
he commonly used mussel. In addition, the observed differences between
species were compared with differences in their life-strategies. The
Cu concentration in the sediment is strongly related to the silt fract
ion (<16 mu m) of the sediment.