“…The 87 Sr/ 86 Sr signature is not fractionated as it moves from the bedrock, soil, plants and animals in an ecosystem (Aberg, 1995;Blum et al, 2000), so the strontium consumed and imbibed by an individual will reflect the strontium isotope signatures in the geologic regions in which the plants, animals and water originated (see Bentley, 2006). Strontium then substitutes for calcium in hydroxyapatite in enamel and bone (Carr et al, 1962;Dolphin and Eve, 1963;Hodges et al, 1950;Kulp and Schulert, 1962). Since bone is continually remodeling, bone strontium isotope signatures reflect the place of residence during the period of bone formation before death.…”