This article summarizes a series of experiments involving low-dose add
itions of phosphorus, nitrogen, and organic carbon, performed to test
hypotheses concerning the oligotrophication of acidified and limed lak
es. Gradual fertilization of a whole lake stimulated productivity, via
chrysophytes and cladoceran zooplankton, through the entire pelagic f
ood chain without causing structural damage to the system. Although P
is considered the primary limiting nutrient for phytoplankton growth i
n acidified and limed lakes, in two out of four lakes we found a close
balance between P and N limitation. In acidified Lake Njupfatet, phyt
oplankton community structure changed depending on the form in which n
itrogen, added together with phosphorus, was supplied. A cyanophyte wa
s favored with ammonium, whereas a dinoflagellate dominated when nitra
te was the nitrogen source. Chrysophytes, the desired ''edible'' phyto
plankton, were only stimulated when organic carbon was added together
with N and P. Many flagellates are mixotrophic and they may have respo
nded to an increase in heterotrophic bacterial growth. Nutrient additi
ons during late summer, when cyanophytes dominated, did not improve th
e growth of any component of the plankton community. Liming of Lake Nj
upfatet resulted in decreases both in phosphorus concentration and in
standing stock of phytoplankton. The phytoplankton community after lim
ing changed markedly, the cyanophytes disappeared, while the zooplankt
on community composition remained typical of acidified lakes. Nutrient
additions during late summer resulted in increased growth of both phy
to- and zooplankton. We argue that controlled nutrient additions may b
e a necessary complement to liming in order to restore acidified lakes
.