THE SALINE LAKES OF SASKATCHEWAN

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Abstract
Sixty lakes in central and southern Saskatchewan were investigated during the years 1938 to 1943. Most of these are saline and lie within the aspen parkland. A few freshwater lakes from the adjacent forest zone were included for comparison. Physical and chemical studies included observation of depth, temperature, dissolved oxygen, light penetration, and the mineral constituents of the water. The plankton was sampled with nets and traps, bottom organisms with an Ekman dredge, and the fish with gill nets and seines. In the first two years the survey covered all the main lakes in the southern part of the province. In the last three, more intensive studies were made in selected lakes.Most of the lakes have between 300 and 30,000 p.p.m. of total solids but Little Manitou Lake has 120,000 p.p.m. The salts are mostly sulphates of magnesium or sodium with little chlorides. Seasonal, annual, and long-term variations in salinity are discussed. Most of the lakes are shallow and only those of moderate depth show thermal stratification. High salinity affects the course of circulation. Light penetration is low in the shallow lakes but none is excessively turbid.The phytoplankton, dominated by the blue-green algae, is mostly composed of euryhaline species. Higher aquatic plants are widespread but absent from Little Manitou Lake. Cosmopolitan species of halophytes grow around the saline lakes. Rotifers are abundant with Pedalia and Brachionus dominant in the more saline water. The Entomostraca thrive in all salinities. The brine shrimp, Artemia salina, is found only in Little Manitou Lake. Chironomid larvae, amphipods, and mollusca dominate the bottom fauna. The relation of the quantity of bottom organisms to salinity is discussed.Twenty-six species of fish are found. Several species tolerate a salinity of 15,000 p.p.m. but only the nine-spined stickleback, Pungitius pungitius, occurs in 20,000 p.p.m. The saline lakes produce much game fish and about 5% of the commercial catch of the province. Fish planting and the results of three experiments in fish culture are recorded.These lakes may be classified as saline eutrophic. Salinity is the dominant influence and it is also an expression of the climatic and physiographic factors that were responsible for the formation of the lakes. The saline lakes of Saskatchewan are much like those in the steppes of western Siberia.

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