The study of fish concentrations and sediment inventories in 19 European high mountain lakes (40-67 degrees N) shows that a fraction of organochlorine compounds (OCs), the less volatile compounds (LVC; subcooled liquid vapor pressure < or = 10(-2.5) Pa), are trapped in the higher locations. This general trend is not significantly influenced by possible local sources. Compound distribution is related to average air temperatures. The phase-change pseudoenthalpies calculated from the sediment inventories closely match the summed theoretical volatilization and dissolution enthalpies. This fractionation effect is responsible for the accumulation of high concentrations of the LVC, the more persistent and toxic according to literature data, in organisms inhabiting sites far from the locations of synthesis or use.

No abstract

Minnows have recently been introduced into the mountain lakes of southern Norway. In Øvre Heimdalsvatn, an intensively studied lake, the minnow population has increased rapidly during the last decade. Studies were performed on feeding habits, habitat preferences, age, growth, energy content, densities, parasites, predation and spawning activities. Several aspects were found to be different from other studies, e.g. higher age of sexual maturation, lower growth rate, no feeding on plants, and low infection of parasites. The interaction with the only other fish, the brown trout, is discussed in relation to the minnow population. In 1978 the minnows constituted little more than 10% of production and food consumption of the trout population, and only limited food competition and predation was documented. Increasing competition is likely with a greater minnow population.

Energy pathways of a natural brown trout Salmo trutta population were constructed. The main subjects taken into account were: the biomass, calorific values and production of the population, natural mortality and annual yield, energy intake, calorific values and composition of the food, efficiency of food absorption, spawning and migration of young trout. The specific energy value of trout increased with increasing weight of the fish. An energy decrease of almost 50% was demonstrated for the spawning trout of both sexes, and the calorific values prior to spawning were not reached before the next summer. Energy intake was estimated to 6.87, 10.31, 8.42 and 9.15 kcal m−2 lake surface for the years 1969, 1970, 1971 and 1972 respectively. Although a great number of food items were found in the trout stomachs, the four groups Gammarus lacustris, Lepidurus arcticus, Trichoptera and Chironomidae accounted for 2/3 of the total consumption. The efficiency of food absorption varied between 42 and 53%. The mean age of trout entering the lake from the nursery streams was ca. 3 yr. The annual amount of this immigration was estimated to be 0.28 and 0.24 kcal m−2 lake surface for 1969 and 1970 respectively. Annual production of trout in the take was estimated to be 1.46 and 2.66 kcal m−2 respectively for the same years. For both these years balance was found between biomass at the beginning of the year plus immigration of young and total production, minus catch by man, natural mortality and spawning on the one hand and biomass at the end of the year on the other hand.

No abstract