Sediments from Lago di Mezzano, central Italy: a record of Lateglacial/Holocene climatic variations and anthropogenic impact

Microscopic, geochemical and pollen analysis of sediment samples of a Lateg lacial/Horocene profile from Lago di Mezzano, a maar lake in central Italy, reveals evidence of significant climatic and human-induced environmental c hanges. Time control is provided by a combination of varve chronology and r adiocarbon dating. The well-known Lateglacial climatic variations, a warmer interstadial and the Younger Dryas cold phase are clearly represented in a ll the parameters. During the interval between 9200 and 5600 cal. BP of the Holocene climatic optimum, annually laminated, organic-rich diatom gyttja was deposited. Two periods of diminished total organic carbon are identifie d within this interval. The first one (P1) ranges from 8200 to 7800 cal. BP while the second (P2) is centred around 6500 cal. BP. During P1, a predomi nance of diatoms (Stephanodiscus parvus and S. minutulus) over other algae (represented by the total organic carbon content) is observed. The timing o f this period coincides with the early- to mid-Holocene climatic transition , reported from ice cores and lake sediments (Stager and Mayewski, 1997). P 2 is characterized by a decrease in all biogenic parameters including bioge nic opal, organic carbon as well as arboreal pollen. From 5000 cal. BP to d ate, the sediment pattern changes coincide with the mid-Holocene climatic d eterioration. In addition to these natural variations, human impact has bee n recorded and recognized from sedimentological features such as turbidites and charcoal, as well as from reduced arboreal pollen content. Two Middle Bronze Age (3700 cal. BP and 3300 cal. BP), Etruscan/early Roman (2500 cal. BP), Longobardic (AD 900) and 'modern settlements' (since no 1700) have be en distinguished on the basis of these data.