M. Kazantzaki, C. Athanassas, Y. Bassiakos & E. TsakalosIn E. Photos-Jones, Y. Bassiakos, E. Filippaki, A. Hein, I. Karatasios, V. Kilikoglou & E. Kouloumpi (eds), 2016. Proceedings of the 6th Symposium of the Hellenic Society for Archaeometry (Bar International Series 2780), Oxford: 207-214.
It is to be noted here that it is the first time that such old luminescence ages have been reported for Greek coastal sediments. This paper presents preliminary luminescence dating results with special focus on the performance of the PIRIR290 methodology. Palaeoenvironmental implications of the obtained PIRIR290 ages are also discussed.
Catherine PerlèsQuaternary International 407 (July 2016): 45-58
The long Upper Palaeolithic and Mesolithic sequence of Franchthi Cave is often quoted for the importance of its marine resources. The first coastal resources to be exploited, from the very beginning of the Upper Palaeolithic, were ornamental shell species. Fish was captured since at least the 13th millennium cal BC, and Franchthi is well known for the episode of intense tuna fishing in the Upper Mesolithic (8th millennium cal BC).
Arthur Glais, José Antonio López-Sáez, Laurent Lespez & Robert DavidsonQuaternary International 403 (June 2016): 237-250
Palynological and sedimentological investigations carried out around the tell of Dikili Tash (Eastern Macedonia, Greece), one of the oldest Neolithic sites in Europe, improve our understanding of the evolution of the paleoenvironment from the Late Pleistocene to the Neolithic period (6500–3200 cal BC in this region).
Third millennium B.C. anthropomorphic marble sculpture from the Aegean Cyclades, the so-called Early Cycladic figures and figurines, have fascinated art aficionados and scholars alike for over a century. This has led to a tremendous amount of aesthetic appreciation and monetary value for the aforementioned artifacts.
The socio-economic processes during the Late Neolithic in northern Greece have been given little attention compared to earlier phases of this period. However, several studies suggest interesting phenomena such as shifts in settlement patterns and ceramic production, possibly entailing processes of intense group interactions and increasing territorialization.
Karine RivièreIn C. Müller & M. Heintz (eds) 2016. Transitions historiques. Colloques de la Maison de l’Archéologie et de l’Ethnologie, René Ginouvés 12, Paris: 57-67.
Scholars have established a classical chronology for the study of Greek history from the 14th down to the end of the 6th century BC. It distinguishes three movements, the Mycenaean period, a set of centuries to which diverse names are given, and the Archaic period.
Adela SobotkovaIn M. Manoledakis (ed.) 2016. The Black Sea in the Light of New Archaeological Data and Theoretical Approaches. Proceedings of the 2nd International Workshop on the Black Sea in Antiquity Held in Thessaloniki, 18-20 September 2015, Oxford: 77-87.
Mobile lifestyle is frequently used to explain lacunae in archaeological evidence, such as the absence of permanent and long-term occupations in the archaeological record of 1st millennium BC Thrace. In this paper, I investigate the feasibility of Iron Age nomadic pastoralism, defined as an economic activity in which the whole community moves along with the herds.
Lee Clare-Bernhard WeningerIn M. Reindel, K. Bartl, F. Lüth & N. Benecke (eds) 2016. Palaeoenvironment and the Development of Early Settlements. Proceedings of the International Conferences at Şanliurfa 2012 and Aqaba 2013, Halle/Saale: 29-49.
The history of the Ayia Irini promontory is closely linked to seismic activity and the successive changes in Relative Sea Level from the Late Neolithic to the Hellenistic period. After an occupation period of approximately 500 years, it was suddenly abandoned in 2000 BC, when the RSL rose from -5.0 ± 0.10 m to -3.60 ± 0.30 m.
Areti ChalkiotiIn M. Ghilardi, F. Leandri, J. Bloemendal, L. Lespez & S. Fachard (eds) 2016. Géoarchélogie des îles de Mediterranée, Paris: 109-118.
This contribution aims to reconstruct the past coastal landscapes of the island of Lemnos, Northeast Aegean Sea, Greece, for the last 20 000 years. It is based on recent publications which estimate the fluctuations in sea-level and ice volume through past glacial cycles, as well as sea-level reconstructions derived from borehole stratigraphies.
During the low sea level of the Last Glacial Maximum the island of Gökçeada, together with all of the North Aegean Islands, was connected to the mainland. Gökçeada, together with Lemnos, became an island probably just after the Younger Dryas, and they were connected by an isthmus. Around 7000-6500 cal. BC, sea level was 20 m lower than today and the separate island of Gökçeada lay close to the Gelibolu Peninsula.