ABSTRACT
The problem of establishing the provenance of carpets of artistic and historical importance is well known. We have addressed this by investigating whether there is sufficient geographical variation in the stable isotopes in wool (namely C, N and S) between key areas of Turkey to be able to recognize the different regions where carpets were made. Here we report results from modern wool samples taken from the winter growth of sheep in 2003/2004 from 13 carpet-producing sites. Although each site has a characteristic composition, most sites cannot be distinguished from each other, and the overall isotopic pattern is unexpectedly complicated. Thus in Western Turkey there is no sign of sea-spray effects in the delta34S values for sites close (10 km) to the sea, while, in the Konya Basin (Central Turkey), the delta34S values vary significantly between nearby sites. Two 'urban' settlements where sheep are now raised have dramatically higher delta15N values. It is nevertheless possible that certain production centers may have distinct signatures, and further work will compare carpets from known sources with the currently produced wool values. The results also provide additional insight into the natural variation found in archaeological faunal isotopic values, e.g. in bone collagen.
