No abstract

Gross and microscopic examination of the Krapina Neanderthal dental remains reveals the presence of artificial grooves along the cemento-enamel junction of 14 teeth representing ten different individuals. The grooves display distinct morphological features including their consistent location (primarily on the mesial and/or distal root walls), their troughlike appearance, striations and/or polishing in the channel, and the ridges of reactive cementum bordering the groove. These grooves occur only on erupted, permanent teeth, and except for a single occurrence on a lower I2, all are located on mandibular or maxillary P4-M3. The morphological nature of the grooves is distinct and has been used to distinguish these grooves from root caries and other pathological or natural causes. Based on the close resemblance between artificial grooves at Krapina and those which have been attributed to toothpick use in other fossil and recent populations, we argue the Krapina Neanderthals were habitually probing the interproximal dental spaces with tools.

No abstract

It has often been reported that the Krapina Neandertal remains bear incised linear striations which appear to be cutmarks. Here, the plausibility of the striations as cutmarks is tested by comparing them to Mousterian butchery marks on large fauna and to cutmarks on modern human skeletons known to have been defleshed with stone tools. The anatomical location, gross appearance, and frequency of occurrence of the striations on the Krapina material do not resemble Mousterian butchery marks on reindeer. The Krapina striations do closely match authenticated cutmarks on 22 modern human skeletons defleshed with stone tools after partial decomposition, preparatory to secondary burial. Data are presented supporting the hypothesis that the striations on the Krapina Neandertal remains are consistent with postmortem processing of corpses with stone tools, probably in preparation for burial of cleaned bones.

One of the most reasonable hypotheses regarding the functional significance of the browridge is that the supraorbital torus forms in response to masticatory stress during development. Oyen, Walker, and Rice (1979) have recently proposed a model that tests this hypothesis: if browridges are functionally related to masticatory stresses on the cranial vault, then changes in the biomechanics of the masticatory system ought to be reflected by changes in the browridge. To test their model they attempted to relate biomechanical discontinuities resulting from tooth eruption to episodes of bone deposition on the supraorbital tori of a developmental series of dry Papio crania. This paper reports on a parallel test of the model on a cross-sectional sample of Australian Aboriginal juvenile crania. This sample showed no relation between tooth eruption and the supraorbital surface morphology thought to be indicative of active bone deposition. It is also demonstrated that no significant relationship between tooth eruption and episodes of bone deposition is shown by the Papio sample. It is concluded that the use of small cross-sectional samples of dry crania does not provide a valid test of the model.