TRACING MIGRATION PATTERNS AND CLIMATE CHANGE USING ISOTOPE ANALYSES OF PREHISTORIC BISON BONES AND TEETH
Here we present analyses of the stable oxygen, carbon, and nitrogen isotope values of samples of tooth enamel carbonate, bone phosphate, and bone collagen from Late Prehistoric bison jumps in Wyoming. Values for prehistoric bison were compared with corresponding analyses of modern bison from across the Great Plains. We also have analyzed the strontium isotope ratios of a subset of the archaeological samples; the strontium isotope ratios of individuals reflects soil values in their habitat which, in turn, vary depending on the type and age of the bedrock that weathered to form the soil.
The majority of bison at each archaeological site displayed oxygen and carbon isotope ratios that were similar to those of modern bison from the same region (the northern Great Plains). However, a few individual at each site displayed oxygen and/or carbon isotope ratios that differed by up to 5 per mil from the values for modern bison from the same region. Archaeological bison with extreme oxygen and carbon isotope ratios also displayed extreme strontium and nitrogen isotope ratios that differed from the mean values for these proxies at each location. Overall, our results suggest that corresponding analyses of multiple isotopic systems can be used to distinguish between migrant and resident animals, and that 10 to 15% of prehistoric bison in the Northern Great Plain region migrated long distances across different environments.