Changes in the Apparent Temperature Optima of the Plankton of Lake Michigan at Chicago, Illinois
Forty years (1937–76) of data from Lake Michigan water intakes at Chicago, Illinois, were examined to explain reported differences in the apparent temperature optima of phytoplankton. The bimodal seasonal plankton distribution, typical at Chicago, still occurs. However, there has been a shift in seasonal periodicity with spring peaks occurring in March from 1957 to 1976 instead of May–June as previously reported for 1937–56. An optimum temperature of 10 °C for the plankton community was observed between 1936 and 1956, while for the last 20 yr an optimum temperature range from 0 to 4 °C was observed. This change in optimum temperature of the plankton community is related to a change in the abundance of the genera Asterionella, Fragilaria, Stephanodiscus, and Tabellaria. Asterionella and Fragilaria were the dominant spring plankton with maximum standing crops observed around 10 °C prior to 1956. Stephanodiscus first increased significantly in 1957 and was the dominant spring plankter through 1976. More recently (1972–76), blue-green algae have increased in numbers. Differences in apparent temperature optima reported are real and are caused by the emergence of cold water species of Stephanodiscus as the dominant spring plankter from 1957 to 1976. Key words: plankton, temperature optima, Lake Michigan