Abstract
The cuticular permeabilities of individual C. b. hungerfordi Lansbury collected over a wide range of salinities were determined. Corixids from low salinity water (0-2000 .mu.mhos.cntdot.cm-1 surface conductivity at 25.degree. C) exhibited low cuticular permeability; those from moderately saline water bodies (7000-11,000 .mu.mhos.cntdot.cm-1) were much more permeable. At higher salinities cuticular permeability was again low, corixids from a lake with a surface conductivity of 16,000 .mu.mhos.cntdot.cm-1 (.apprx. 1/2 that of seawater) had cuticular permeabilities comparable with those of corixids from freshwater lakes. This phenomenon was acclimatory, since permeability decreased over time when corixids from moderately saline lakes were placed into distilled water. The biological reasons for these results are not clear, but apparently cuticular permeability of C. bifida increases as problems of ion regulation diminish, and then begins to decrease, seemingly at the salinity at which it becomes difficult for the corixid to maintain a constant hemolymph osmotic pressure. The biological implications of this phenomenon are discussed.