engleski

Palaeoenvironmental and Archaeological Implications of a Sediment Core from Polje Cepic, Istria, Croatia

Palaeoenvironmental and archaeological records provide an invaluable framework for land and water management in karstic areas of the Mediterranean realm. We present the results from analyses carried out on three segments of a sediment core extracted in 2004 from a portion of Polje Cepic (Istria. Croatia), a tectono-karstic depression covered in water until artificial drainage took place in 1932. We used bulk sediment analyses, pollen analysis and radiocarbon dating to assess the possible contribution of people to the progressive siltation of the lake, and compared our results with recent archaeological discoveries made on the polje margins. The dating of the sequence points to the presence of a predominantly wet landscape at the coring location since at least 7000 years cal BP. The comcideuce of cereal type pollen grains with several open-air archaeological sites indicates that small-scale agricultural practices possibly developed around the polje in Neolithic times, ca 6500 years cal BP. Concentrations of charcoal in the sedunent core at this time suggest the use of fire clearance as part of the agricultural practice. During the Bronze and Iron Ages, the possible intensification of forest clearance and agricultural practices is indicated by: (1) an increase in the number and type of archaeological sites found around the polje: (2) a more open plant landscape in the upper part of the analysed sequence: and (3) a three-fold increase in the sedimentation rate. possibly starting as early as 4000 years cal BP Wetter climate conditions and higher erosion of the surrounding slopes probably led to the progressive siltation of the lake. Finally, in 1932 the lake was artificially drained and Istria lost its largest natural basin of fresh water.

Holocene. Lake sediments; Geoarchaeology. Palynology. Mediterranean karst.

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