1. Studies carried out in Lake Baikal in late spring (late May-early J
une) 1991 showed marked differences in the species composition and abu
ndance of phytoplankton in different regions of the lake. The south an
d north basins were characterized by small forms of algae. The middle
basin, Maloe More and the shallow waters of the Selenga had species wi
th large cells including Aulacoseira islandica subsp. helvetica, Dinob
ryon cylindricum and D. divergens. 2. Areas of high biomass were corre
lated with shallow waters and river inputs. This was especially appare
nt in the region of the Selenga delta. The vertical distribution of ph
ytoplankton indicated the non-synchronous start of the spring homother
my throughout the lake. Phytoplankton were concentrated in the upper 1
00 m layer with subsurface maxima resulting from the sinking of large
algae. 3. The concentration of phytoplankton biomass in general at thi
s time characterized the lake as moderately productive.