“…The stable isotope ratios of sulfur ( 34 S/ 32 S, reported as δ 34 S), for example, can be combined with δ 13 C to help distinguish among primary producers in marine food webs (Connolly et al, 2004), and to identify foraging ranges and spatial distribution across populations (e.g., Giménez et al, 2018b; Wilson et al, 2012), between sexes, and among ages (e.g., Louis et al, 2021; Niño‐Torres et al, 2006). The stable isotope ratios of oxygen ( 18 O/ 16 O, reported as δ 18 O) are potentially useful to distinguish habitat use (e.g., Drago et al, 2020) and movements across areas with strong salinity gradients (e.g., Gauffier et al, 2020; Matthews et al, 2016). The stable isotope ratios of strontium ( 87 Sr/ 86 Sr ratios, reported as 87 Sr) vary regionally according to oceanographic factors and have been used to investigate movements patterns in mysticetes (e.g., Vighi et al, 2019).…”