STABLE ISOTOPE ECOLOGY AND DIETARY MODELING OF MAMMALIAN MEGAFAUNA FROM THE MIDDLE IRVINGTONIAN FAIRMEAD LANDFILL LOCALITY, CHOWCHILLA, CA
We used stable isotope values of carnivore and herbivore tooth enamel to investigate paleodietary and paleoecological patterns. δ13C values of tooth enamel are controlled by diet and can be used to investigate resource usage and partitioning among and between taxa. In large mammals δ18O ratios are controlled by drinking water, and by proxy, climate. Ontogenetic serial tooth δ18O and δ13C reveal seasonal trends in resource usage, from which we can infer patterns of forage availability.
Fairmead Landfill δ13C values are consistent with an environment dominated by C3 vegetation. Platygonus and Camelops had the lowest and highest δ13C, respectively. Camelops exhibited the most variable δ13C among herbivores, though several other taxa are represented by single individuals, thus lacking dietary ranges. Among carnivores, Homotherium had the lowest δ13C values (-13.5‰) and Canis latrans the highest (-10.7‰). In addition to population level analysis (ANOVA, t-tests) we also used the Bayesian mixing model Stable Isotope Analysis in R (SIAR) to model carnivore diets against potential herbivore prey. Both canids and felids show generalist dietary patterns, however felids on average consumed Mammuthus than Canis dirus.
We serially sampled teeth from four taxa to investigate seasonality and temporal resource usage among megafauna. Equus, Camelops and Tetrameryx show little variation in δ13C suggesting little turnover in Fairmead’s floral community, on a seasonal scale. We also report a serial sampled Homotherium canine and a calculated growth rate of 3.4 mm/year; a growth rate intermediate between Smilodon and modern pantherine felids.