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R R Ackermann

Publications and source records attributed to R R Ackermann.

3 recordsLinked to original sources

Inferring Plio-Pleistocene southern African biochronology from facial affinities in Parapapio and other fossil papionins.

Buried in the same South African cave deposits as Australopithecus, fossil papionins have been referred to Parapapio (Pp. whitei, Pp. broomi, Pp. jonesi, Pp. antiquus), Papio (P. izodi, P. angusticeps, P. h. robinsoni), Theropithecus (e.g., T. darti), Gorgopithecus, or Dinopithecus on the basis of postcanine tooth size and descriptive morphology of the muzzle. The morphological patterns of variation that these papionins demonstrate can help to place the Australopithecus fossils into a biochronological context and provide valuable information for reconstructing regional Plio-Pleistocene turnover. To document these patterns of variation across fossil-bearing sites, we explore morphometric affinities within Parapapio, and between Parapapio and other Plio-Pleistocene taxa (Dinopithecus ingens, Papio angusticeps, Papio izodi, and Theropithecus darti) by analyzing a sample of interlandmark distances derived from 3-D coordinate data of the most complete fossil papionin specimens available. Bivariate and multivariate analyses show that Pp. whitei exhibits as much variation between sites and between individuals as Pp. broomi and Pp. whitei combined. Diversity in Parapapio at Makapansgat and Sterkfontein may suggest substantial time depth to the caves. Theropithecus darti, Dinopithecus ingens, Papio angusticeps, Pp. whitei from Bolt's Farm (BF 43), and Pp. jonesi from Sterkfontein (STS 565) differ considerably from one another. Other Parapapio specimens across sites form a separate cluster with P. izodi from Taung, suggesting a Pliocene age for this site.

Africa, Southern↗

Phenotypic covariance structure in tamarins (genus Saguinus): a comparison of variation patterns using matrix correlation and common principal component analysis.

Constancy of variation/covariation structure among populations is frequently assumed in order to measure the differential selective forces which have caused population differentiation through evolutionary time. Following Steppan ([1997] Evolution 51:571-594), this assumption is examined among closely related tamarin species (genus Saguinus), using two distinct approaches applied to the task of evaluating similarity in patterns of morphological variation: common principal component analysis and matrix correlations. While the results of these analyses may appear contradictory, closer examination reveals them as complementary, highlighting the wisdom of combined methodologies. Overall, the results reveal a close relationship among the morphologically based variance structures of the tamarin species a relationship whose pattern is consistent with the pattern of phylogenetic relatedness as found via a molecular genetic study. More specifically, both methodological approaches provide some support for divergence of S. geoffroyi and S. oedipus (with regards to their patterns of morphological variation) from other tamarin species. This suggests that variance/covariance structure may have diverged through evolutionary time in the tamarin lineage, placing assumptions of constancy in doubt.

Analysis of Variance↗

Three-dimensional imaging in forensic anthropology: a test study using the Macintosh.

Forensic anthropologists have unique, albeit usually fleeting, access to modern skeletal remains. By constructing a database of three-dimensional images, such remains can be accessed long after the remains are gone. A method is proposed which uses Macintosh hardware and NIH Image software to preserve remains digitally through red-blue three-dimensional imaging techniques. Additionally, the qualitative and quantitative accuracy of these images is assessed. By creating this type of forensic database, anthropologists can address issues such as populational variance, thereby using modern forensic skeletal remains to explore some of the fundamental issues within anthropology.

Bone and Bones↗