Neolithisation of the aegean and southeast europe during the 6600-6000 calBC period of rapid climate change

Abstract

In extension of the recently established 'Rapid Climate Change (RCC) Neolithisation Model' (Clare 2013), in the present paper we demonstrate the existence of a remarkable coincidence between the exact (decadel-scale) entry and departure dates of the Neolithic into/from the Aegean (∼6600/6050 calBC) with begin/end of RCC-conditions. IZVLE∞EK - ∞lanek predstavlja razΠiritev nedavno vzpostavljenega modela neolitizacije v povezavi s hitrimi klimatskimi spremembami - T. i. 'Rapid Climate Change (RCC) Neolithisation model' (Clare 2013). V ≠lanku opozorimo na izjemno sovpadanje med natan≠nimi (v merilu desetletij) vstopnimi in izstopnimi datumi za Πirjenje neolitika v/iz Egejskega prostora (∼6600/6050 calBC) in za≠etkom/ koncem razmer hitre klimatske spremembe (RCC).