THE LATER PREHISTORY OF THE SHAHRIZOR PLAIN, KURDISTAN REGION OF IRAQ: FURTHER INVESTIGATIONS AT GURGA CHIYA AND TEPE MARANI

The Shahrizor Prehistory Project has targeted prehistoric levels of the Late Ubaid and Late Chalcolithic 4 (LC4; Late Middle Uruk) periods at Gurga Chiya (Shahrizor, Kurdistan region of northern Iraq), along with the Halaf period at the adjacent site of Tepe Marani. Excavations at the latter have produced new dietary and environmental data for the sixth millennium B.C. in the region, while at Gurga Chiya part of a burned Late Ubaid tripartite house was excavated. This has yielded a promising archaeobotanical assemblage and established a benchmark ceramic assemblage for the Shahrizor Plain, which is closely comparable to material known from Tell Madhhur in the Hamrin valley. The related series of radiocarbon dates gives significant new insights into the divergent timing of the Late Ubaid and early LC in northern and southern Mesopotamia. In the following occupation horizon, a ceramic assemblage closely aligned to the southern Middle Uruk indicates convergence of material culture with central and southern Iraq as early as the LC4 period. Combined with data for the appearance of Early Uruk elements at sites in the adjacent Qara Dagh region, this hints at long-term co-development of material culture during the fourth millennium B.C. in southeastern Iraqi Kurdistan and central and southern Iraq, potentially questioning the model of expansion or colonialism from the south.

REVISITING TELL BEGUM: A PREHISTORIC SITE IN THE SHAHRIZOR PLAIN, IRAQI KURDISTAN

Tell Begum was previously explored by Iraqi archaeologists in the 1960s when excavations revealed a multi-period site. Among the key finds were Halaf period remains that are relatively rare in the region of the Shahrizor plain and included polychrome ceramics suggesting a local variation of the Halaf culture. Recent investigations and excavations in 2011 and 2013 revealed a 5 hectare site inhabited during the Halaf, Ubaid, Late Chalcolithic, and medieval periods. The Halaf site may have had an area of about 3 hectares, making it a relatively large settlement for that period, although its full extent is unclear. Offsite work revealed the area to have been well watered in the past, with likely neighbouring regions of woodland and abundant shrubs. The heavy sedimentation in the region has partially obscured archaeological remains, including possibly Tell Begum's lower mound. The site, nevertheless, shows continuity of settlement, indicating relative stability in settlement over long timespans.

Tell Sabi Abyad, Syria: Dating of Neolithic Cemeteries

Late Neolithic graves excavated at Tell Sabi Abyad, Syria, have been dated by radiocarbon. This series of 46 human bone dates represents a sequence of cemeteries that is analyzed by Bayesian methodology. The dates show continuous use of the northeastern slope of the mound as a burial ground throughout the Initial Pottery Neolithic to the Halaf period.

Tell Sabi Abyad, Syria: Dating of Neolithic Cemeteries

Late Neolithic graves excavated at Tell Sabi Abyad, Syria, have been dated by radiocarbon. This series of 46 human bone dates represents a sequence of cemeteries that is analyzed by Bayesian methodology. The dates show continuous use of the northeastern slope of the mound as a burial ground throughout the Initial Pottery Neolithic to the Halaf period.

Obsidian as an indicator of inter-regional contacts and exchange: three case-studies from the Halaf period

Obsidian was used to make tools and luxury items which were widely distributed in the ancient Near East. At most sites it is an imported material and, as such, has been used as an indicator of exchange, although little specific detail of the nature of that exchange is available. Even though methods of provenance analysis for obsidian are well established, often only a few samples per site have been analysed. This means there is not enough information to indicate the relative importance of the obsidian from each source, or to establish whether source preference changed through time or whether obsidians from different sources were treated differently. The restriction in numbers analysed is, at least in part, due to the expense and the destructive nature of provenance analysis and problems associated with obtaining sufficient samples. In an attempt to address these problems case-studies examining the obsidian assemblages from three sites of Halaf date will be used to demonstrate the potential of a method of grouping obsidians based on their physical characteristics, including colour; these groupings are confirmed by geochemical analysis. This allows the entire assemblage to be grouped quickly and cost effectively and, if used alongside techno-typological and spatial studies, enables us to begin to confront some of the issues outlined above.