A one year field study of four stations in the Gulf of Bothnia during
1991 showed that the biomass was ca. two times, and primary productivi
ty ca, four times, lower in the north (Bothnian Bay) than in the south
(Bothnian Sea) during the summer. Nutrient addition experiments indic
ated phosphorus limitation of phytoplankton in the Bothnian Bay and th
e coastal areas in the northern Bothnian Sea, but nitrogen limitation
in the open Bothnian Sea. A positive correlation between the phosphate
concentration and the production/biomass ratio of phytoplankton was d
emonstrated, which partly explained the differences in the specific gr
owth rate of the phytoplankton during the summer. Differences in photo
synthetic active radiation between the stations also showed a covariat
ion with the primary productivity. The relative importance of nutrient
or light limitation for photosynthetic carbon fixation could not, how
ever, be conclusively determined from this study. Marked differences i
n phytoplankton species composition from north to south were also obse
rved. The number of dominating species was higher in the Bothnian Sea
than in the Bothnian Bay. The distribution of some species could be ex
plained as due to nutrient availability (e.g. Nodularia spumigena, Aph
anizomenon sp.), while salinity probably limits the distribution of so
me limnic as well as marine species. The potentially toxic phytoplankt
on N. spumigena, Dinophysis acuminata and Chrysochromulina spp. were c
ommon in the Bothnian Sea but not in the Bothnian Bay. The pico- and n
anoplankton biomass during late summer was higher than previously repo
rted due to a revised carbon/volume ratio.