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.

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Prehistoric quarries in America are poorly understood and thus problematical to take into account when making inferences about past behavior. A microwear analysis of Clovis blades from the 2000 Texas A&M University excavations at the Gault site (41BL323), located in southern Bell County, Texas, provided a window into this problem. Texas A&M excavations on the site produced an extraordinarily large number of Clovis artifacts in two bounded geologic units, 3a and 3b. Included in the artifact types are blades, specialized elongate flakes associated with a core and blade technology. In conducting a microwear analysis of the Clovis blades from Gault, I proposed the following questions: (1) were the Clovis blades utilized at Gault?; (2) is there a difference in the use-wear patterns of Clovis blades from the geological units 3a and 3b?; and (3) is Gault, as a quarry/workshop site, a place to just obtain raw materials or did it also serve as a craft site? Observations from experiments, stereomicroscope analysis, compound microscope analysis, and SEM/EDS analysis led to answers for two research questions: (1) blades were used at Gault and (2) there is a difference between Clovis units 3a and 3b. Eight Clovis 3a blades, or 3.0% of the total Clovis 3a blade/blade fragment population (n=264), exhibit use-wear. Six Clovis 3b blades, 3.3% of the total Clovis 3b blade/blade fragment population (n=182), exhibit use-wear. In general, Clovis 3b blades were used on harder contact materials (wood to bone) than those in Clovis Unit 3a (softer contact materials similar to grass, sinew, and rawhide). The function(s) of quarries and quarry-related workshops were interpreted by William Henry Holmes as a place to obtain raw materials, while Kirk Bryan interpreted them as a place to bring other materials to work in craft activities. Following the microwear analysis of Clovis blades/blade fragments at Gault, I compared Gault to three other Paleoindian quarry-workshop sites (Wells Creek, Dutchess Quarry, and West Athens Hill). My intent is to provide supplemental data for the consideration when applying Holmes’ and Bryan’s respective hypotheses.

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No description available.

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.

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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.