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Grazing high and low: Can we detect horse altitudinal mobility using high‐resolution isotope ( δ 13 C and δ 15 N values) time series in tail hair? A case study in the Mongolian Altai
Author(s) -
Lazzerini Nicolas,
Coulon Aurélie,
Simon Laurent,
Marchina Charlotte,
Noost Bayarkhuu,
Lepetz Sébastien,
Zazzo Antoine
Publication year - 2019
Publication title -
rapid communications in mass spectrometry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.528
H-Index - 136
eISSN - 1097-0231
pISSN - 0951-4198
DOI - 10.1002/rcm.8496
Subject(s) - isotope , chemistry , stable isotope ratio , grazing , horse , altitude (triangle) , isotope analysis , isotopes of carbon , δ13c , zoology , pasture , isotopes of nitrogen , nitrogen , environmental chemistry , ecology , biology , total organic carbon , paleontology , mathematics , physics , geometry , quantum mechanics , organic chemistry
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 δ 13 C and δ 15 N 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. Methods Between 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 δ 13 C and δ 15 N values. Results Less 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 δ 13 C and δ 15 N variations were observed between the different horses, despite differences in mobility patterns. We propose that water availability as well as seasonal availability of N 2 fixing type plants primarily controlled horse hair δ 13 C and δ 15 N values, overprinting the influence of altitude. Conclusions Our study shows that altitudinal mobility is not the main factor that drives the variations in horse tail hair δ 13 C and δ 15 N values and that seasonal change in the animal dietary preference also plays an important role. It is therefore risky to interpret variations in δ 13 C and δ 15 N values of animal tissues in terms of altitudinal mobility alone, at least in C 3 –dominated environments.