169 



the climatic changes of the recarring seasons. This factor in 

 the environment of the plankton is thus an ever changing one, 

 but at the same time it runs an annual cycle of the same gen- 

 eral character year after year with ever present minor varia- 

 tions of a seasonal or local origin. The extremes of tempera- 

 ture in bodies of water in this latitude are so divergent that 

 they afford the basis for marked seasonal changes in both the 

 constitution and the quantity of the plankton. Adaptations on 

 the part of the organisms of the plankton to definite tempera- 

 ture limits thus occur. 



Records of the temperature of the air and of the surface 

 and the bottom water have been taken regularly at all stations 

 where quantitative plankton collections were liiade. These 

 are recorded in Table I. The temperatures were taken with a 

 Negretti-Zambra self-recording thermometer from 1894 till May 

 24, 1898, after which time a Hick's self-recording maximum-mini- 

 mu]n thermometer w as used. Under stable conditions no appre- 

 ciable variation was noted in the reading of the thermometers, 

 but at the times of sudden change, as in the mingling waters of 

 a rising flood, readings would sometimes vary as much as four 

 or five degrees at one location and level. 



The temperature of the river water is influenced by a vari- 

 ety of causes in addition to the immediate action of solar heat. 

 The most prouiinent of these are the access of the tributary 

 water from streams, springs, and impounding backwaters. The 

 temperature of tributary streams, such as the Spoon River 

 (Table IV.), is often, though not always, warmer in winter and 

 colder in summer by several degrees than that of the main 

 stream, as a result probably of the greater proportion of spring 

 water and the greater nearness of the same to its subterranean 

 source. A good illustration of this was to be seen along the 

 eastern shore of Quiver Lake, where at low-water stages springs 

 near the water's margin kept up a continuous flow. The tem- 

 perature of the water in summer was 54", while in winter it 

 fell only to 51°. The smaller tributary waters also respond 

 more quickly to fluctuations of temperature than does the river 



