Abstract
Palynological studies of the Leffe Basin lacustrine deposits (Lombard Pre‐Alps, Italy) reveal a succession of deciduous mesophytic arboreal communities, coniferous forests and brief phases of withdrawal of arboreal taxa. The pollen record can be easily correlated with a previous pollen diagram by Lona (1950). However, contrary to his interpretation, we believe that the cyclicity shown by vegetation dynamics cannot be correlated with the major glacial events that occurred in the Southern Alps, but perhaps with interglacial‐glacial cycles of moderate amplitude.