BOOKS | 2016
Edited by Corien Wiersma, Dimitris Agnousiotis, Evangelia Karimali, Wietske Prummel & H. Reinder Reinders
Gronigen
2016
This volume is devoted to Magoúla Pavlína, a Middle Bronze Age site in the municipality of Almirós (Thessalía, Greece). Immediately after the magoúla was brought under cultivation and ploughed for the first time, in 1996, the site was surveyed and a sample of ceramics, lithics, molluscs and bone material was collected.
Karine Rivière
In 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 Sobotkova
In 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.
Traunmüller, S.
Gnomon 88.5 (2016): 470-472
Traunmüller, S., Review of: K. Müller, Gournia. Ein urbanes Zentrum der Spätbronzezeit (Berlin 2013), Gnomon 88.5 (2016): 470-472
Hartmut, M.
Gnomon 88.7 (2016): 629-633
Hartmut, M., Review of: V. Karageorghis & E. Raptou, Necropoleis at Palaepaphos from the End of the Late Bronze Age to the Cypro-Archaic Period (Nicosia 2014), Gnomon 88.7 (2016): 629-633
Lee Clare-Bernhard Weninger
In 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.
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This paper focuses on the influence of conflict and violence on Neolithisation and Neolithic dispersal in the Eastern Mediterranean.
Krzyszkowska, O.
Journal of Hellenic Studies 136 (2016): 266-267
Krzyszkowska, O., Review of: G. Dionisio, A. M. Jasink & J. Weingarten, Minoan Cushion Seals: Innovation in Form, Style, and Use in Bronze Age Glyptic (Rome 2014), Journal of Hellenic Studies 136 (2016): 266-267
Kotsonas, A.
Journal of Hellenic Studies 136 (2016): 268-269
Kotsonas, A., Review of: F. Gaignerot-Driessen & J. Driessen (eds), Cretan Cities: Formation and Transformation, Aegis. Actes de colloques 7 (Louvain 2015), Journal of Hellenic Studies 136 (2016): 268-269
Edited by Ernst Pernicka, Sinan Ünlüsöy & Stephan W. E. Blum
Bonn
Troy has been of outstanding importance for EBA archaeology ever since the discovery and excavation of the site by Heinrich Schliemann. Partly due to the paucity of archaeological research on EBA Anatolia, Troy has long been considered as the only key site for Western Anatolia and the Northern Aegean.
Edited by Nikolaos Chr. Stampolidis
Athens
In 2016 the Museum of Cycladic Art celebrated 30 years of creative presence with an exhibition entitled “Cycladic Society 5,000 Years Ago”, opened from early December 2016 to late March 2017.
Nikos Mourtzas & Eleni Kolaiti
In M. Ghilardi, F. Leandri, J. Bloemendal, L. Lespez & S. Fachard (eds) 2016. Géoarchélogie des îles de Mediterranée, Paris: 119-135.
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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 Chalkioti
In 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.
Burçin Erdoğu
In M. Ghilardi, F. Leandri, J. Bloemendal, L. Lespez & S. Fachard (eds) 2016. Géoarchélogie des îles de Mediterranée, Paris: 89-94.
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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.
Alan Simmons & Rolfe D. Mandel
In M. Ghilardi, F. Leandri, J. Bloemendal, L. Lespez & S. Fachard (eds) 2016. Géoarchélogie des îles de Mediterranée, Paris: 57-72.
This paper summarizes the arguments for the association of cultural remains with pygmy hippopotami, specifically focusing on the site’s stratigraphic sequence, chronology, and formation processes. These data are consistent with the hypothesis that the remains of the pygmy hippopotami are in direct association with cultural features and artifacts that comprise the site’s two primary archaeological strata.
Thomas P. Leppard & Suzanne E. Pillar Birch
In M. Ghilardi, F. Leandri, J. Bloemendal, L. Lespez & S. Fachard (eds) 2016. Géoarchélogie des îles de Mediterranée, Paris: 47-56.
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We consider the insular ecology of Capra hircus and suggest that its introduction into Quercus-dominated Mediterranean environments would have resulted in dramatically increased predation on plant genera that were not adapted for ovicaprid herbivory. This would have driven a series of corresponding changes, including the sheet erosion of topsoils and ecological release in competitor taxa. These changes – possibly including localized extinctions – may possibly have been more substantial than those effected via direct human agency.