EVIDENCE OF NICHE CONSERVATISM OVER PLEISTOCENE GLACIAL-INTERGLACIAL CYCLES FOR ANCIENT MAMMALS DURING THE PLEISTOCENE OF EUROPE
To determine mammal ecology, stable carbon and oxygen isotope values from the tooth enamel of large mammals were examined. The analysis of δ13C and δ18O values obtained from the teeth of fossil mammals has proven extremely useful for ascertaining mammal (paleo)ecology. Hundreds of isotope samples were obtained and compared to previously published data from sites in Central and Western Europe. Results show that C3 plants dominated the Pleistocene landscape of Europe as they do today. Horses (Equus sp.), red deer (Cervus elaphus), and bovids (i.e., Bos primigenius and Bison sp.) commonly displayed the most positive δ13C values and maintained a regular ecological relationship when present together at a locality. Consistently, the most negative δ13C values were displayed by individuals in the cave bear lineage (i.e., Ursus spelaeus, Ursus deningeri), and suggest herbivory. For oxygen, canids (Canis sp.) generally displayed the most positive δ18O values, which may relate to obtaining water from a different source than the other analyzed taxa. Overall, the data show limited isotopic differences over time and between localities implying that species maintained their ecology. These data support the tested hypothesis as well as the concept of niche conservatism in Pleistocene European mammals.