Loss of 10 radionuclides by Mytdus edulis was studled near its salinity minimum in the Bothnian Sea (northern Baltic Sea) by labelling mussels in the laboratory and then allowing them to depurate during a 10 mo period in the field at 2 locations: one with normal temperatures, the other with temperatures 8 to 10 C" above normal. During winter, the clearest effect of heating was accelerated loss of silver. Also zinc was apparently lost more rapidly in warm water, whereas none of the remaining nuclides showed loss rates significantly different from zero at either temperature. At normal temperatures during spring and summer all analysed elements were lost faster than in the heated winter experiment despite similar average temperature conditions. It is concluded that temperature differences play only a minor role In the observed seasonal effect on long-term loss rates. Food availabhty appears to be a key factor. Loss rates are apparently faster than in full-salinity waters. Possible reasons for this are discussed. Plutonium to americium ratlos decreased during depuration. The pluton~un~ fraction lost after 300d was estimated to be twice the corresponding fraction of americium. Europium to americium ratios remained unchanged during all seasons and temperatures. whereas cerium to americium ratios decreased to half during the initial loss phase, after which they remained unaltered. It is concluded that europium behaved as an ideal analogue to americium in this experiment.