The paleoanthropology of Greece

European paleoanthropology and paleolithic archeology were already well‐established by the early twentieth century. The human fossil record from this continent is the longest known and perhaps most intensively studied. Nonetheless, important gaps remain to this day in the map of Pleistocene Europe; perhaps the most glaring of these is located in the southeastern corner of the continent. This region's record is critical for addressing questions about the course of human evolution in Europe because its geographic position lends it a dual role: on one hand, it encompasses a frequently hypothesized dispersal corridor from Africa into Europe for both archaic and early modern humans; on the other, as one of the three Mediterranean peninsulas, it acted as a refugium for plant, animal, and, most likely, human populations during glacial conditions. This article is a review of the paleoanthopological record of Greece, one of the least known in Europe.     

Le Moustérien de Grèce à la lumière des récentes recherches

Thanks to recent research and the re-evaluation of the archaeological material coming from older research, the Mousterian of Greece has started to become better known. Aside the surface findings, which testify the presence of Mousterian throughout the entire continental Greece, only five Middle Paleolithic sites have been excavated. Almost every remnant has been dated to the last ice age. All lithics belong to the “typical” Mousterian, while the Quina Mousterian has not been certainly testified. The Levallois method is almost always present, more or less frequent, but always dominated by non-Levallois methods. The recurrent variations, mostly centripetal, have been more frequently used. The “Micromousterian” of Asprochaliko is the only lithic assemblage from which the Levallois method is absent.