This paper presents a pilot study designed to test the use of oxygen isotopes for investigating aspects of early herding practices in the Neolithic of western Asia, using the site of Çatalhöyük in central Anatolia as a case study. Time‐sequenced δ 18 O values in dental enamel of archaeological sheep are assessed for post‐depositional diagenetic effects and compared with seasonal δ 18 O meteoric water values in the region today. The evidence is used to indicate the environmental conditions in which individual sheep spent their first year, enabling management of breeding and birthing seasons, and movement to seasonal pastures, to be investigated.
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Henton et al. (2009) studied this question.
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