Zooplankton succession and thermal stratification in the polymictic shallow Muggelsee (Berlin, Germany): a case for the intermediate disturbance hypothesis?
B. Eckert et N. Walz, Zooplankton succession and thermal stratification in the polymictic shallow Muggelsee (Berlin, Germany): a case for the intermediate disturbance hypothesis?, HYDROBIOL, 387, 1998, pp. 199-206
From the end of May to November 1995 the succession of rotifers and cladoce
rans was investigated in Muggelsee with samples taken twice a week. Keratel
la cochlearis was the only rotifer which was found on every sampling day an
d this species also showed the highest abundances. During summer, when freq
uencies of strong wind events were low and water was strongly stratified, t
hree small cladocerans were dominant (Daphnia cucullata, Chydorus sphaericu
s, Eubosmina coregoni). Food supply was the main limiting factor for Kerate
lla spp. and Synchaeta spp. In autumn, however, when the intervals between
strong winds were shorter, rotifers with shorter periods for population dev
elopment prospered. Zooplankton diversity first increased and subsequently
decreased after disturbances. The results do not support the intermediate d
isturbance hypothesis in its present formulation.