Résumé
Rationale Carbon and nitrogen stable isotope time series performed in continuously growing tissues (hair, tooth enamel) are commonly used to reconstruct the dietary history of modern and ancient animals. Predicting the effects of altitudinal mobility on animal δ13C and δ15N values remains difficult as several variables such as temperature, water availability or soil type can contribute to the isotope composition. Modern references adapted to the region of interest are therefore essential.MethodsBetween June 2015 and July 2018, six free‐ranging domestic horses living in the Mongolian Altaï were fitted with GPS collars. Tail hairs were sampled each year, prepared for sequential C and N isotope analysis using EA‐IRMS. Isotopic variations were compared with altitudinal mobility, and Generalized Additive Mixed (GAMMs) models were used to model the effect of geographic and environmental factors on δ13C and δ15N values.ResultsLess than half of the pasture changes were linked with a significant isotopic shift while numerous isotopic shifts did not correspond to any altitudinal mobility. Similar patterns of δ13C and δ15N variations were observed between the different horses, despite differences in mobility patterns. We propose that water availability as well as seasonal availability of N2 fixing type plants primarily controlled horse hair δ13C and δ15N values, overprinting the influence of altitude.ConclusionsOur study shows that altitudinal mobility is not the main factor that drives the variations in horse tail hair δ13C and δ15N values and that seasonal change in the animal dietary preference also plays an important role. It is therefore risky to interpret variations in δ13C and δ15N values of animal tissues in terms of altitudinal mobility alone, at least in C3–dominated environments.