IMPLICATIONS FOR AMMONITE ECOLOGY AND PHYLOGENY FROM CARBON ISOTOPES
To explore this proposition, we compared the stable isotopic ratios of fossilized shell material from planaspiral, scaphitid, and baculitid ammonites as well as contemporaneous benthic mollusks. The physiology of benthic mollusks is generally better understood than that of ammonites, and they serve as a comparison due to their immobile nature relative to free swimming ammonites. Specimens were sourced from the Western Interior Seaway of North America and are Cretaceous (~80-70 Ma) in age. Sample collection for stable isotopic analysis was performed using a computerized micromill or hand drill and analyzed with an isotope ratio mass spectrometer. We observean overlap in the δ13C values of baculitid and planaspiral ammonites, which may be explained by two interpretations. Metabolic rates between the two genera may be similar, implying that our understanding of the ecology of these groups may be incorrect. Alternatively, δ13C variation in ammonites may not reflect differing metabolic rates but rather another physiological factor.Notable similarities in oxygen isotopic (δ18O)values between planaspiral and baculitid ammonites further indicate a shared position in the water columnduring life. Additional data, from scaphitid ammonites and benthic mollusks, will provide a broader framework for comparison.