A Palaeoecological Perspective on the Environmental Impact of Prehistoric Societies in Europe with Emphasis on Greece and the Southern Balkans
摘要
Here, we provide an overview on the environmental impact of Europe’s first farmers, focusing on the vegetation[aut]Vegetation shifts that occurred in the southern BalkansBalkan/s during the Neolithisation[aut]Neolithisation. First, we draw on recent methodological developments in palaeoecology[aut]Palaeoecology that contribute to tighten its linkages with archaeology. We start highlighting the importance of highly precise and accurate lake sediment chronologies to enhance comparison with dendrochronologically dated archaeological settlements[aut]Settlement. Then, we assess modern pollen-vegetation relationships to better interpret the fossil pollen records[aut]Pollen record. The results reveal (i) an overall good match between the main vegetation[aut]Vegetation types of the southern BalkansBalkan/s and their soil pollen[aut]Pollen assemblages, and (ii) that pollen[aut]Pollen assemblages from lake[aut]Lake surface samples reflect reliably the surrounding vegetation[aut]Vegetation. Afterwards, we summarise our latest results from the region. In Limni ZazariLimni Zazari (GreeceGreece), continuous pollen records[aut]Pollen record of cereals[aut]Arable farmingcereal and ruderal plants[aut]Ruderal (plants, vegetation) allow dating early farming[aut]Arable farmingfarming activities around 6250 BC. At Ploča Mičov GradPloča Mičov Grad (Lake OhridLake Ohrid, North MacedoniaNorth Macedonia), pollen[aut]Pollen evidence of cereals and weeds[aut]Weed place the onset of the Neolithic at 5500–5100 BC, i.e. significantly earlier than the tree-ring inferred age of the settlement[aut]Settlement. Current efforts aim at producing new palaeoecological records, refining the available ones, and adding palaeoclimatic[aut]Palaeoclimate reconstructions[aut]PalaeoclimateClimate that allow determining which role climate[aut]Climateclimate variability played in the Neolithisation[aut]Neolithisation.