“…Differences in the isotopic signature of dietary items require differences in isotopic fractionation, which can result from physical processes (e.g., geographic 2 H gradients) [9,45,46,88], metabolic pathways (e.g., C 3 vs. C 4 plant δ 13 C) [9,12,43], trophic level (e.g., plant vs. consumer δ 15 N) [9,40,44], or biome (e.g., marine vs. terrestrial δ 13 C and δ 15 N) [9,[40][41][42]. Once diet has been established, that information can then be used to answer a wide range of ecological questions, including what resources are used by different species [13,[89][90][91], where individuals move to acquire those resources [92][93][94][95], how energy and nutrients move among trophic levels [34,35,96,97], and how communities and biomes are linked by the flow of energy and nutrients [42,[98][99][100]. The diversity and novelty of these applications contribute to the great popularity of stable isotope-based diet reconstruction methods.…”