Eksino, on the island of Gökçeada (Imbros) in the Northeast Aegean, is a new open-air site with evidence of Palaeolithic cultural remains. Stone tools collected by an initial survey have clarified an assessment of the site from the Lower Palaeolithic, and brought to light new evidence from the Middle Palaeolithic as well as transition to the Upper Palaeolithic. Eksino is probably one of the most significant Lower Palaeolithic tool collections in the North Aegean, and finds such as chopper or chopping tools and Acheulean bifacial handaxes from the site show that the North Aegean may be another possible dispersal route from hominids to Europe via the East and Northeast Mediterranean during the Lower Palaeolithic. Middle Palaeolithic finds are frequent in the site and finds resemble the typical Mousterian type which is characterized by discoidal cores, Levallois cores and flakes, scrapers, denticulates, notches and points. Upper Palaeolithic finds are rare in the site, and a bifacial leaf point and large crescent-shaped backed pieces made on blades may reveal the presence of the Middle-Upper Palaeolithic transition on the island. This new data from Palaeolithic Gökçeada is likely to fill key geographic gaps associated with the initial dispersal of hominins through the northeast Aegean islands.
The 8.2 ka BP event is one of the most proeminent and abrupt climatic events of the Holocene, showing generally drier and colder conditions for ca. 160 years, but there are also variations in climatic impacts by region. Dating and archaeological evidence indicates that the impact of the climate event varies by region, from large‑scale site abandonment to continued occupation and local adaptation. The dating evidence from Uğurlu on the Island of Gökçeada, Northeast Aegean, shows that there is a clear hiatus in 14C dates between ca. 8220 and 8000 cal BP, corresponding to the 8.2 ka BP climate event. This paper presents dating and archaeological evidence from Uğurlu and discusses the consequences of evidence in terms of the 8.2 ka BP climate event.
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