Tending and drive hunting: A density-mediated attrition model can explain age profiles of white-tailed deer at Iroquoian village sites

In a 1993 paper, Noble and Crerar suggested, based on the age and sex distribution of white-tailed deer (Odocoileus virginianus) longbones from four Attawandaron Iroquoian sites around the western end of Lake Ontario, that the contact-period Attawandaron were managing local deer populations, in response to the aboriginal trade in hides. Having observed similar patterns of differential preservation of elements and epiphyseal fusion at nearby Iroquoian sites that are not ascribed to the Attawandaron, and which pre-date the hypothesised trading period, we argue that these patterns may instead relate to bone density and/or vulnerability to taphonomic effects of late-fusing epiphyses. We further support our argument through age profiles based on dental eruption and wear.     

Radiocarbon and U-series dating of the endemic deer Praemegaceros cazioti (Depéret) from “Grotta Juntu”, Sardinia

Radiocarbon and U-series methods (²³⁰Th/U and ²³¹Pa/²³⁵U) for absolute age determination have been applied to some fossil samples from Grotta Juntu, in North Eastern Sardinia (Italy). The remains belong to the endemic deer species Praemegaceros cazioti, which is here represented by an almost complete skeleton. The three dating methods lead to concordant ages of about 7500 years BP, indicating that the skeleton was maintained as closed system after burial. Taking into consideration these results, Praemegaceros cazioti from Grotta Juntu is now the youngest representative of this species in Sardinia.     

Expanding ecomorphological methods: geometric morphometric analysis of Cervidae post-crania

This study presents ecomorphological methods for reconstructing paleohabitats using three-dimensional geometric morphometric analyses of Cervidae (deer and relatives) post-cranial elements. Cervids are often the most abundant taxon in Eurasian Plio-Pleistocene sites, yet their post-cranial remains are rarely utilized in paleoecological reconstructions. Cervids are found in a wide variety of habitats, and thus their ecomorphology spans an appropriate range to serve as a proxy for paleohabitat. Four morphological features are examined in this study; the calcaneus as a whole (n = 122), the medial margin of the patellar surface of the femur (n = 133), the lateral margin of the tibial plateau (n = 136), and the plantar margin of the third phalanx (n = 62). These features were chosen because they represent various aspects of cervid locomotion important for power generation, stability, and substrate interaction. For each feature, canonical variates analyses with cross-validations were used to assess how well landmark configurations distinguish among specimens from different habitat types. Cross-validations returned correct reclassifications rates ranging from 38.9% to 66.3% in a four-habitat system, with resubstitution rates of 55.4% to 79.1% correct. Most habitat groups were found to be significantly different at p < 0.0001 using permutations tests. Variation in these ecomorphological adaptations are explored via visualizations depicting “open” and “closed” habitat types, and hypotheses are presented for cervid functional morphology.