The primate genus Theropithecus is represented at various Plio-Pleistocene sites including the Pliocene site of Makapansgat (2.9 mya), the early Pleistocene cave of Swartkrans (1.8 mya), the late Pleistocene deposits from Elandsfontein (700,000 ka) and by extant gelada baboons from Ethiopia. To examine how diet has changed over time in this genus, dental microwear features of Theropithecus darti (n=2), Theropithecus danieli (n=8), Theropithecus gelada (n=2) Theropithecus oswaldi (n=1) Parapapio whitei (n=14), Papio robinsoni (n=16) and Papio ursinus (n=13) were examined under low-magnification (35x) using light refractive technology. Although there is a significant relationship between small pits and fine scratches, Analysis of Variance followed by Tukey’s post-hoc tests failed to demonstrate significant groupings. However, bivariate analyses suggest that as scratch count increases, pit count decreases. The results suggest that there is much dietary variation in modern and extinct gelada baboons, but that extant Theropithecus relies somewhat more on grassland resources than did their extinct counterparts.

The primate genus Theropithecus is represented at various Plio-Pleistocene sites including the Pliocene site of Makapansgat (2.9 mya), the early Pleistocene cave of Swartkrans (1.8 mya), the late Pleistocene deposits from Elandsfontein (700,000 ka) and by extant gelada baboons from Ethiopia. To examine how diet has changed over time in this genus, dental microwear features of Theropithecus darti (n=2), Theropithecus danieli (n=8), Theropithecus gelada (n=2) Theropithecus oswaldi (n=1) Parapapio whitei (n=14), Papio robinsoni (n=16) and Papio ursinus (n=13) were examined under low-magnification (35x) using light refractive technology. Although there is a significant relationship between small pits and fine scratches, Analysis of Variance followed by Tukey’s post-hoc tests failed to demonstrate significant groupings. However, bivariate analyses suggest that as scratch count increases, pit count decreases. The results suggest that there is much dietary variation in modern and extinct gelada baboons, but that extant Theropithecus relies somewhat more on grassland resources than did their extinct counterparts.

No / Microwear patterns and formation processes are examined in modern browsing and grazing Gotland sheep from Denmark. Clear differences in microwear patterning are identified between Gotland sheep, which included a high proportion of leaves, bark and twigs of deciduous trees and shrubs in their diet, and those which primarily had access to graze species, with the browsing group exhibiting enamel surfaces dominated by pitted microwear features, the grazers a predominance of striations. Analysis of abrasives in dung suggests that these trends can be attributed to higher levels of soil ingestion in the grazing population and are a consequence both of grassland management practices and height of feeding within the vegetation canopy. These findings question previous interpretations of microwear patterning in browsing and grazing ungulates, which have equated striated enamel features with the ingestion of high levels of opal phytoliths, and thus have significant implications for palaeodietary reconstruction in such species, both within archaeological and palaeontological contexts. To address further the implications of these results, comparison is made between the Gotland sheep and modern grazing and fodder-fed sheep and goats from elsewhere in Europe. It is concluded that dental microwear analysis has the potential to address questions relating to grassland management practices and the use of certain fodders, such as leafy-hay, but that it may ultimately prove more difficult to distinguish `fresh¿ browsing sheep from some grazing populations, specifically those in which levels of soil ingestion are reduced.

The purpose of this study is to identify the currently supported diet and dietary niches of the Malagasy subfossil and extant lemurs. The study was conducted partially in Tsinjoarivo and Antananarivo, Madagascar in the summer of 2013. Samples were analyzed and microwear determined that the dietary niches were aligned with current literature. Grit accumulation occurs more frequently in disturbed habitats and on lower canopy levels, which suggests that human manipulation of environment can impact the dental microwear of living primates.

Cercopithecines are common in hominid producing deposits and are a useful proxy for determining the ecological context of the early hominids. For this study, dental microwear is examined through low-magnification stereomicroscopy and used to reconstruct the diets of sampled primates. Those from the earliest sites, predominantly Parapapio, are primarily frugivorous while the incidence of gramnivory increases in the later Dinopithecus, Gorgopithecus, and Papio individuals denoting a general cooling and drying trend over the South African Plio-Pleistocene with a distinct pulse between 1.9-1.8 million years ago (mya). Australopithecus is reconstructed as a primary gramnivore which indicates that hominids adapted early in their evolution to expanding grasslands.

Reconstructing diet in Andean populations is complicated by ecological complexity and by large-scale population movements and trade networks during the period of imperial rule. It is therefore more difficult to reconstruct dietary patterns within these contexts. Previous multi-isotopic analysis of the skeletal population from the Inca site of Machu Picchu indicates marked variation in dietary composition both early and late in life. However, these data are limited in their specificity due to overlap in isotopic signals from different resource types. I compare existing isotopic data to enamel macro- and microwear data to more accurately profile diet composition in a Machu Picchu skeletal population subset. Results suggest there is little to no dietary variation between sexes and age groups. Results also reveal the role that maize played in the diet of this non-elite population, which may prove useful in more accurately estimating consumed food resources in this and other Andean populations.

The craniodental morphology of the early Pliocene ursid Agriotherium africanum has been studied extensively to reveal aspects of its dietary ecology. Results suggest that this large-bodied, long-legged, short-faced African native primarily consumed vertebrate matter. While many carnivoran families exhibit a clear functional relationship between craniodental form and performance on the one hand, and dietary behavior on the other, this is not always the case with Ursidae. Because of uncertainties regarding the appropriateness of using craniodental form to investigate ursid diets, questions still linger about the dietary ecology of Ag. africanum. Here, we report on a dental microwear texture analysis of six Ag. africanum lower second molars from the South African fossil site of Langebaanweg. Results support morphological evidence that suggests a diet focused on vertebrate soft tissue and bone. Unfortunately, results cannot clarify questions about mode of acquisition.

Throughout the past, bioarchaeologists have been concerned with identifying subsistence strategies of past populations and when subsistence strategies have transitioned from foraging to agriculture practices. Specifically, one area of major concentration has been examining the transition from foraging to agriculture in the southeast of the present day United States. The present study examines the transition of subsistence practices in prehistoric Tennessee utilizing dental microwear texture analysis. This study examined a total of 49 individuals from Archaic and Mississippian sites. These were compared temporally by comparing Archaic microwear signatures to Mississippian microwear signatures, and geographically, through the comparison of each site in relation to its geographic location. Non-parametric Mann-Whitney U tests were utilized to determine if statistical significant differences existed between the Archaic and Mississippian groups analyzed, and to determine if statistical significant differences existed based on geographic location. Due to the small sample size utilized in the study, it must be stated that the results are preliminary and further testing using dental microwear texture analysis needs to be undertaken in order to better understand the results.

This study utilizes stable isotope and dental microwear analyses to elucidate diet and subsistence practices of indigenous Muchik peoples interred at two sites in the Lambayeque region of northern Peru: La Capilla Santa María Magdalena De Eten (CSMME) (n=17) and La Capilla Del Niño Serranito (CNS) (n=18). Burials at CNS date to the Early Colonial Period (A.D. 1533-1620), while burials at CSMME date to the Mid- to Late-Colonial Period (A.D. 1625-1760). Dental microwear and stable isotope investigations reveal a highly correlated dietary profile across both sites, which suggests consistent subsistence practices across the Colonial Period, insofar as can be measured using these techniques. However, there is significant differences between CNS and CSMME in dental microwear features indicating the foods consumed by all members at each site—since sex and age are not significantly different between the two sites—is perhaps attributable to the influence of Spanish colonial rule to the degree to which these dental microwear features capture larger patterns in these two populations. Although samples sizes are limited, at CNS, the frequency of fine scratches and small pits increase with age and coarse scratches decrease between childhood and adolescence, indicative of transitions in diet or the use of the teeth during the maturation. Further, statistical inquiry found no significant dental microwear differences between site, age, or sex in the studied populations.

The evolutionary history of the South African papionins is a useful analog for the emergence of hominids in South Africa. However, the taxonomic relationships of the papionins are unclear. This study uses low-magnification stereomicroscopy to examine dental microwear and uses the microwear signals to explore the existing classification of these papionins. The results from the species and site level analyses are equivocal. However, the genera and time period results show clear evidence for a dietary change between the extinct and extant forms of Papio and Parapapio. This adds an additional tool for distinguishing these two groups. The dietary changes witnessed in the papionins are likely found in the hominids from the Plio-Pleistocene. Using the papionin analog, hominid dietary evolution may be explored.