@article{2993390,
    title = "Long-term trends of land use and demography in Greece: A comparative study",
    author = "Weiberg, E. and Bevan, A. and Kouli, K. and Katsianis, M. and Woodbridge, J. and Bonnier, A. and Engel, M. and Finné, M. and Fyfe, R. and Maniatis, Y. and Palmisano, A. and Panajiotidis, S. and Roberts, C.N. and Shennan, S.",
    journal = "The Holocene",
    year = "2019",
    volume = "29",
    number = "5",
    pages = "742-760",
    publisher = "SAGE Publications Ltd",
    issn = "0959-6836, 1477-0911",
    doi = "10.1177/0959683619826641",
    keywords = "Along Track Scanning Radiometer;  anthropogenic effect;  archaeology;  bioclastic sediment;  bioclimatology;  Bronze Age;  climate conditions;  climate variation;  comparative study;  demography;  land cover;  land use;  landscape;  long-term change;  Neolithic;  pollen;  probability;  radiocarbon dating;  vegetation type, Greece",
    abstract = "This paper offers a comparative study of land use and demographic development in northern and southern Greece from the Neolithic to the Byzantine period. Results from summed probability densities (SPD) of archaeological radiocarbon dates and settlement numbers derived from archaeological site surveys are combined with results from cluster-based analysis of published pollen core assemblages to offer an integrated view of human pressure on the Greek landscape through time. We demonstrate that SPDs offer a useful approach to outline differences between regions and a useful complement to archaeological site surveys, evaluated here especially for the onset of the Neolithic and for the Final Neolithic (FN)/Early Bronze Age (EBA) transition. Pollen analysis highlight differences in vegetation between the two sub-regions, but also several parallel changes. The comparison of land cover dynamics between two sub-regions of Greece further demonstrates the significance of the bioclimatic conditions of core locations and that apparent oppositions between regions may in fact be two sides of the same coin in terms of socio-ecological trajectories. We also assess the balance between anthropogenic and climate-related impacts on vegetation and suggest that climatic variability was as an important factor for vegetation regrowth. Finally, our evidence suggests that the impact of humans on land cover is amplified from the Late Bronze Age (LBA) onwards as more extensive herding and agricultural practices are introduced. © The Author(s) 2019."
}