Cyanoprokaryote assemblages of eight very productive Brazilian lakes are de
scribed and the main driving forces of their dominance are considered. Rela
tive abundance of blue-greens is shown to have been positively related to t
emperature, but not to pH or total-P and to have been negatively associated
with light, mixing, NO3, but not with NH4, total N or total N/total P rati
o. Both heterocytic and non-heterocytic groups were negatively related to N
O3. However, if Cylindrospermopsis species are considered as non-N-2-fixing
organisms (only 10% of the filaments carried heterocytes), the lakes could
be considered as dominated by non-N-2-fixing populations during most of th
e years. In this new scenario, non-N-2-fixing were dominant in NO3 (but not
NH4) deficient lakes and in both NO3 and NH4 deficient conditions. Assembl
ages S, S-n, H, M, X-1, as groups of descriptor species of systems having s
imilar features as proposed by Reynolds (1997: Ecology Institute, Oldenburg
), were representative of warm, shallow, turbid, enriched and frequently mi
xed lakes. We propose to move some species from Z (picoplancton of oligotro
phic lakes) to X-1 assemblage (nanoplankton of eutrophic lakes) and we comm
ent on Microcystis species of M assemblage from mixed shallow lakes in rela
tion to L-m assemblage of end-summer in temperate lakes. S and S-n assembla
ges, which comprise species which are good-light antennae, were the best re
presented group in these generally turbid and shallow lakes.