TY - JOUR
T1 - The earliest securely-dated hominin artefact in Anatolia?
AU - Maddy, D.
AU - Schreve, D.
AU - Demir, T.
AU - Veldkamp, A.
AU - Wijbrans, J.R.
AU - van Gorp, W.
AU - van Hinsbergen, D.J.J.
AU - Dekkers, M.J.
AU - Scaife, R.
AU - Schoorl, J.M.
AU - Stemerdink, C.
AU - Schriek, T.
PY - 2015
Y1 - 2015
N2 - Anatolia lies at the gateway from Asia into Europe and has frequently been favoured as a route for Early Pleistocene hominin dispersal. Although early hominins are known to have occupied Turkey, with numerous finds of Lower Palaeolithic artefacts documented, the chronology of their dispersal has little reliable stratigraphical or geochronological constraint, sites are rare, and the region's hominin history remains poorly understood as a result. Here, we present a Palaeolithic artefact, a hard-hammer flake, from fluvial sediments associated with the Early Pleistocene Gediz River of Western Turkey. This previously documented buried river terrace sequence provides a clear stratigraphical context for the find and affords opportunities for independent age estimation using the numerous basaltic lava flows that emanated from nearby volcanic necks and aperiodically encroached onto the contemporary valley floors. New
AB - Anatolia lies at the gateway from Asia into Europe and has frequently been favoured as a route for Early Pleistocene hominin dispersal. Although early hominins are known to have occupied Turkey, with numerous finds of Lower Palaeolithic artefacts documented, the chronology of their dispersal has little reliable stratigraphical or geochronological constraint, sites are rare, and the region's hominin history remains poorly understood as a result. Here, we present a Palaeolithic artefact, a hard-hammer flake, from fluvial sediments associated with the Early Pleistocene Gediz River of Western Turkey. This previously documented buried river terrace sequence provides a clear stratigraphical context for the find and affords opportunities for independent age estimation using the numerous basaltic lava flows that emanated from nearby volcanic necks and aperiodically encroached onto the contemporary valley floors. New
U2 - 10.1016/j.quascirev.2014.11.021
DO - 10.1016/j.quascirev.2014.11.021
M3 - Article
SN - 0277-3791
SP - 68
EP - 75
JO - Quaternary Science Reviews
JF - Quaternary Science Reviews
IS - 109
ER -