“…Within the terrestrial ecosystem, it can distinguish C 3 from C 4 plant sources; on the other hand, the nitrogen isotopic signature (δ 15 N) is useful for determining the trophic level of the analyzed individual(s) [ 1 , 2 , 18 , 19 ]. It would be worth analyzing coeval plant and animal specimens along with human samples in order to better interpret the ecological context and to evaluate possible variations of the isotopic values due to specific agriculture and breeding practices, and/or to the analyzed sites’ geographical location and ecology [ 20 , 21 , 22 , 23 , 24 , 25 , 26 , 27 , 28 , 29 , 30 ].…”