The palynological study of the lacustrine sediments from Lagaccione, a maar
-lake near Lago di Bolsena in central Italy, has provided a palaeoenvironme
ntal record for the last 100,000 years. The chronology of the sequence is b
ased on sixteen radiocarbon dates and a tephra layer at the base of the St
Germain II s.l. The pollen record, starting during the St Germain I forest
phase and ending about 3000 years ago, shows that remarkable changes occurr
ed in the floristic composition, in the structure of the vegetation and in
the plant biomass, including also long-lasting periods of open woodlands, o
ften with an appreciable floristic diversity, during the last pleniglacial.
Three new vegetational oscillations (Etruria I, Etruria II and Etruria III
), characterized by a well-defined vegetation composition and dynamics, hav
e been recognized after the St Germain I forest phase and before the middle
pleniglacial interstadials. New evidence has been obtained for a significa
nt diffusion of deciduous trees in the Italian peninsula during the late-gl
acial. (C) 1999 Elsevier Science B.V. All rights reserved.