The nutrient budget, phytoplankton primary production and sedimentatio
n rate were studied weekly in the large (270 km(2)) and shallow (mean
depth 2.8 m) eutrophic Lake Vortsjarv in 1995. The annual external loa
ding was 7.7 gm(-2) y(-1) of total nitrogen (TN) and 0.2 gm(-2) y(-1)
of total phosphorus (TP), including 7% of both inputs as direct atmosp
heric precipitation. The external budget revealed a retention of 53% o
f TN and 28% of TP annual input. About 80% of the total loss of nitrog
en was accounted for by denitrification (3.3 gm(-2) y(-1)) and only 20
% was buried into the sediment. Wind-induced sediment resuspension pla
yed the major role in the upward nutrient flux formation and, thus, in
the formation of the temporal pattern of nutrient concentration durin
g the ice-free season. Other fluxes as the external loading or new sed
imentation of autochthonous production were overcome and masked by the
powerful resuspension - sedimentation cycle, exceeding the former by
one or two orders of magnitude. The intensity of upward flux of nutrie
nts (mainly caused by resuspension) increased in accordance to decreas
ing water level in autumn and correlated with the weekly average wind
speed. The summer population of filamentous blue-greens dominated by L
imnothrix redekei was light-limited until the minima of TN:TP ratio (<
10) and DIN:TN ratio (similar to 0) in July initiated a clear peak of
N-2-fixing algae (Aphanizomenon gracile, Anabaena spp.) which lasted u
ntil September.