“…Therefore, by matching tissue‐specific isotopic signatures to terrestrially delineated isotopic landscapes called isoscapes, stable isotopes have been successfully used to determine the overwintering or breeding areas of many terrestrial birds (Haché, Hobson, Villard, & Bayne, ; Hobson, ). Isoscapes of δ 2 H are generated as a result of predictable, regionally generalized patterns of precipitation (Bowen, Wassenaar, & Hobson, ; Mehl, Alisauskas, Hobson, & Merkel, ) and have proven useful for inferring the terrestrial overwintering grounds of various migrant bird species (Haché et al., ; Hénaux, Powell, Vrtiska, & Hobson, ; Hobson, Bowen, Wassenaar, Ferrand, & Lormee, ; Yerkes et al., ). Unlike deuterium, δ 13 C and δ 15 N isoscapes are generated by landscape‐scale processes related to nitrogen cycling in the soil (δ 15 N) and the plant types present (δ 13 C) (Bond & Jones, ; Rubenstein & Hobson, ).…”