Malia - Research on the Paleoenvironment
Research into the paleogeographical evolution of Malia's plain began again in 2015, with new studies in the marsh bordering the site of the Minoan city: 11 sediment cores were taken (from a depth of 4 to 8 metres) under the guidance of Laurent Lespez (UPEC-UMR 8591 CNRS) and Maia Pomadère (Université Paris 1-ArScAn), with the collaboration of Jean-François Berger (CNRS-UMR 5600, Lyon) and Arthur Glais (Université de Caen).
Plan du sondage
Malia, topographical plan of the Marsh's outlines. Drawn up by L. Fadin © FSA

These cores are currently the subject of multi-parameter analyses and radiocarbon dating, which will enable researchers to determine how the marsh evolved from the Neolithic period until today. 
Several preliminary observations have, however, already been formulated: the marshy sequences present in the sediment cores confirm that Malia’s marsh was from the middle Neolithic period (6th millennium) a low marsh supplied by freshwater streams. The precise study of sedimentary facies should provide the keys to understanding the impact of unusual hydro-climatic or tectonic events, such as storm flooding, as suggested by a clear change in the rhythm of sedimentation like that which occurred in the middle of the 2nd millennium BC.

These preliminary results still need to be refined and/or confirmed by the results of sedimentological, geochemical or pollen analyses currently in progress.   

M. Pomadère © FSA

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Saili, Petroni plot, Agios Georgios, Corfu

Saili, Petroni plot, Agios Georgios, Corfu. Gorgia Provata (H’ EPKA) reports on the excavation of an agricultural facility dating to the end of the fourth / start of the third century BC.

In the W part of the plot, foundations were located of two parallel walls. To the E Wall 1 was found at depth 11.25m, and was 5.75m long and width 0.75m. 0.55m to the W and parallel was found Wall 12, with maximum surviving length 6.13m...

A collaborative project with the BSA.