The subject of this note is the chronology of the site of Khirokitia in Cyprus in the light of four recent radiocarbon determinations. Khirokitia has remained one of the most extensively uncovered prehistoric sites in the Levant since its initial excavation over thirty years ago (Dikaios 1953). The fourth millennium BC date then estimated for the site by Dikaios was revised markedly upwards to the mid-sixth millennium following the submission of samples for radiocarbon dating (Dikaios 1962). The fourth millennium estimate had assumed a stratigraphical continuity between the pre-dominantly aceramic occupation of the site and the appearance of well-made pottery in its upper-most levels. Since the radiocarbon samples were taken from aceramic contexts, Dikaios subsequently concluded that the pottery was the product of a re-occupation of the site in the fourth millennium bc, a date based on the ceramic parallels with and the radiocarbon dates from the site at Sotira (Dikaios 1962, 194).

This conclusion is borne out by a re-examination of the published evidence and, less conclusively perhaps because of its limited nature, by the evidence of a small sounding at the site undertaken by the author in 1972 (Stanley Price and Christou 1973). The four main aims of this 2 m square sounding included further observation of the aceramic-ceramic stratigraphy and the collection of additional radiocarbon samples in an attempt to determine the duration of the aceramic occupation.