Jf. Gillooly et Si. Dodson, Latitudinal patterns in the size distribution and seasonal dynamics of newworld, freshwater cladocerans, LIMN OCEAN, 45(1), 2000, pp. 22-30
Analysis of zooplankton communities in over 1,100 water bodies spanning the
western Hemisphere (77 degrees S, 81 degrees N latitude) revealed latitudi
nal patterns in cladoceran body size and Daphnia seasonal dynamics. The mea
n body length of cladoceran species occurring at different latitudinal inte
rvals was greatest in north temperate regions, declining in size toward the
poles and equator. Thus, mean cladoceran size was greatest in regions wher
e the mean annual surface temperatures of lakes ranged from 6 to 8 degrees
C in both the Northern and Southern Hemispheres. The date of maximum Daphni
a abundance and the period of minimum Daphnia abundance in lakes of North A
merica was positively, linearly related to the latitudinal position of the
lakes. The date of maximum abundance increased with latitude such that Daph
nia peaked during nearly all months of the year depending on latitude, but
usually within the same, narrow temperature range (15-20 degrees C). The pe
riod of minimum Daphnia abundance decreased linearly with latitude such tha
t abundance generally was minimal when water temperatures exceeded 20 degre
es C.