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We evaluate local versus distant land‐use models at Neolithic Çatalhöyük, central Anatolia, using strontium isotope analysis of sheep tooth enamel and charred plant remains. Interpretation of strontium in sheep tooth sequences is constrained by previous oxygen isotope work, which largely excludes summer movement to the mountains but cannot distinguish between herding on the plain and the closest upland‐zone, Neogene limestone terraces. We establish a baseline contrast in modern plant strontium values between the plain and terraces and infer predominant herding on the plain from seven sheep tooth sequences. Archaeobotanical plant strontium values exclude the use of the terraces for cultivation and foraging. Relatively local crop and sheep management, plausibly intensive and integrated to some degree, given limited dry ground, appears likely on the basis of this pilot study.

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 δ18O values in dental enamel of archaeological sheep are assessed for post‐depositional diagenetic effects and compared with seasonal δ18O 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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The hunting of Gazella subgutturosa was a dominant practice for Epipalaeolithic and early Neolithic hunter-gatherers in the east Jordan steppe. The seasonal mobility of this taxon in the Levant is poorly understood, especially for early prehistory when herd movements would have influenced hunter-gatherer use of the steppes. This paper proposes four patterns of seasonal herd mobility for G. subgutturosa centred on Jordan's Azraq Basin. The four patterns are modelled using oxygen, carbon and strontium stable isotopes. Seasonal environmental signatures of each are understood through carbon and strontium isotopic variation in sixty modern plant specimens collected from twelve selected locations in north Jordan, published data on oxygen isotopes in local precipitation, and the adaptive behaviour of G. subgutturosa. The integrated isotopic datasets provide clear discriminatory markers for each proposed mobility pattern. Results will be applied in future to isotopic data from archaeological gazelle teeth from the Azraq Basin.

The aim of this article is to examine the isotopic characterisation of domestic animals as it relates to birthing location and seasonality, diet, pasturing pattern, foddering and climatic conditions of herding and to determine variation between these aspects of cattle and caprine husbandry of the Neolithic Linearbandkultur (LBK) and Trichterbecherkultur (TRB) communities from Kopydłowo in Kujavia-one of the major centres of early farming in the European lowlands. Carbon and nitrogen stable isotope analysis was undertaken on faunal bone collagen; carbon, oxygen and strontium isotope ratios were measured from tooth enamel. Isotopic signatures may have been caused by different strategies of management of herds of these animal species. Different and more widely distributed carbon, nitrogen and strontium isotopic data for TRB cattle in comparison with its LBK counterparts is indicative of the exploitation of increasingly diverse ecological zones and more varied pastoral practises. The distribution of oxygen isotope values on caprine tooth made it possible to recognise herding seasonality. Irrespective of the chronology, cattle, sheep and goats kept by the inhabitants had C 3 plantbased diet.

In the northeast Jordan steppe, gazelle were of considerable economic importance to human groups during the Epipalaeolithic and Neolithic. An influential model argues that gazelle herds migrated through the region and were only seasonally available to hunters. This study tests that model, asking whether gazelle were indeed highly seasonally mobile during these time frames, or whether they could have remained more local, adapted to periodically resource-rich habitats, and thus been available to hunters throughout the year. Interpretation of animal location, diet and season, through stable isotope analyses and microwear studies of archaeological gazelle teeth from ten chronologically and spatially varied sites, suggests herds did not migrate. Rather, gazelle appear to have had relatively local year round habitats in the steppe during the Epipalaeolithic at least, while possibly ranging further and becoming more mobile in the Neolithic.