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The Postglacial record of environmental history from Lago di Pergusa, SicilyDipartimnento di Biologia Vegetale, Università di Roma ‘La Sapienza’, P.le Aldo Moro 5, 00185 Roma, Italy; laura.sadori{at}uniiomal.it
ENEA, C.R. Casaccia, C.P. 2400, Roma, Italy Lacustrine sedimients from Lago di Pergusa in central Sicily provide a Postglacial record of environmental change in the Mediterranean. Magnetic susceptibility measurements, lithofacies characterization and pollen analysis were carried out anid integrated to obtain a better reconstruction of the past 11000 years. The chronoogy is provided by AMS radiocarbon dates on macrofossils or bulk sediment, and by a tephra correlative with a late-Holocene explosion from the Etna volcano. The transition period related to the present interglacial reafforestation, characterized by increasing humidity, started about 10700 years BP. The onset of the wettest conditions of the Postglacial occurred at about 9000 years BP and lasted until about 7200 years BP. Then a trend towards aridification began. leading to very dry conditions at about 3000 years BP. An unquestionable human impact on vegetation is found from 2800 years BP, although earlier land use cannot be excluded. As the climate had already induced change in the vegetation, the well-known human occupancy during the last three millennia did not produce strong effects on the environment.
Key Words: Lacustrine sediments • lithology • palynology • palaeoecology • climiiatic change • tephra • central • Mediterranean • Holocene
The Holocene, Vol. 11, No. 6,
655-671 (2001) This article has been cited by other articles:
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