Task activity and anterior tooth grooving in prehistoric California indians.

Abraded grooves have been observed on the anterior teeth of all the adults in a small population of prehistoric California Indians. These dental effects show considerable variety, appearing on maxillary and mandibular teeth, on approximal and occulusal surfaces, and either isolated or bilaterally aligned. Although many of the grooves are indistinguishable from those reported for other prehistoric populations, their variety illustrates the limited applicability of etiological hypotheses previously proposed to account for such effects. It is suggested that the grooves represent traces of a task activity involving the pulling of fibrous materials across the teeth.     

Interproximal grooving in the Atapuerca-SH hominid dentitions

The dental sample recovered from the Sima de los Huesos (SH) Middle Pleistocene cave site of the Sierra de Atapuerca (Spain) includes 296 specimens. Interproximal wear grooves have been observed in 20 maxillary and mandibular posterior teeth belonging to at least five of the 32 individuals identified so far in the SH hypodigm. Interproximal grooving affected only the adults, and at an age between 25 and 40 years. The appearance, morphology, and location pattern of the SH wear grooves are similar to those reported in other fossil hominids and in more recent human populations. Two alternative proposals, the toothpicking and the fiber or sinew processing hypotheses, compete for explaining the formation of this anomalous wear. The characteristics observed in the wear grooves of the SH teeth are compatible only with the habitual probing of interdental spaces by means of hard and inflexible objects. Dietary grit may also have contributed to the abrasion of the root walls during the motion of the dental probes. Am. J. Phys. Anthropol. 102:369–376, 1997. © 1997 Wiley-Liss, Inc.     

The Incidence of Enamel Hypoplasia among the Krapina Neandertals

Developmental defects of teeth often appear as a record of metabolic disturbances during growth. One defect in particular, enamel hypoplasia, has been described among recent prehistoric human populations, but few analyses have been made of fossil hominids. This study describes the enamel quality of the dental remains of the Krapina Neandertals. Of the 18 individuals represented by dental arch fragments, 13 showed evidence of one or more teeth with enamel defects described as hypoplasia. This was a high frequency of occurrence when compared to Bronze and Copper Age populations in Central Europe or Woodland and Mississippian populations in North America. The reason for the higher incidence among the Neandertals is not fully explainable given the data available. However, there is a suggestion that fluorosis could be a factor that reduced the expression of enamel hypoplasia in the European populations.     

秦岭野生大熊猫牙齿的形态机能

大熊猫(Ailuropoda melanoleuca)是国家一级保护动物,被誉为国宝.牙齿作为大熊猫消化器官之一,相对于其他动物而言,大熊猫牙齿有其自身的构造特点.以往学者和专家对大熊猫牙齿形态的研究侧重于为大熊猫的种群分类寻找根据(Dvadi,1869; Milne-Edwards,1870;王将克,1974),更多关注牙齿在大熊猫进化、演变过程中的意义(王令红等,1982;黄万波,1993).研究的齿位大多局限于臼齿(张鹤宇和刘理,1959),所得结果或数据并不详细和全面.此外,还有一些学者对大熊猫牙齿釉质的超微组织结构进行研究(赵资奎等,1984 ).     

Toothpicking and Periodontal Disease in a Neanderthal Specimen from Cova Foradà Site (Valencia,Spain)

We present a Neanderthal maxilla (CF-1) from Cova Foradà site (Oliva, Valencia, Spain) with periodontal disease and evidence of attempts to alleviate pain with the use of a toothpick. Two interproximal grooves have been found on the distal surfaces of the upper left Pm³ and M¹ of CF-1 maxilla. The location, morphology and size of the grooves coincide with other interproximal grooves found on the teeth of other fossil specimens. Heavy dental wear and periodontal disease would have caused the Cova Foradà Neanderthal specimen pain and discomfort, which the individual attempted to mitigate using some kind of dental probe.     

Brief communication: Identification reassessment of the isolated tooth Krapina D58 through occlusal fingerprint analysis

High variability in the dentition of Homo can create uncertainties in the correct identification of isolated teeth. For instance, standard tooth identification criteria cannot determine with absolute certainty if an isolated tooth is a second or third maxillary molar. In this contribution, using occlusal fingerprint analysis, we reassess the identification of Krapina D58 (Homo neanderthalensis), which is catalogued as a third maxillary molar. We have hypothesized that the presence/absence of the distal occlusal wear facets can be used to differentiate second from third maxillary molars. The results obtained confirm our hypothesis, showing a significant difference between second and third maxillary molars. In particular we note the complete absence of Facets 7 and 10 in all third molars included in this analysis. The presence of these facets in Krapina D58 eliminates the possibility that it is a third maxillary molar. Consequently it should be reclassified as a second molar. Although this method is limited by the degree of dental wear (i.e., unworn teeth cannot be analyzed) and to individual molars in full occlusion, it can be used for tooth identification when other common criteria are not sufficient to discriminate between second and third maxillary molars. Am J Phys Anthropol 143:306–312, 2010. © 2010 Wiley‐Liss, Inc.     

Brief communication: Subvertical grooves on interproximal wear facets from the El Sidrón (Asturias,Spain) Neandertal dental sample

The distribution of subvertical grooves on interproximal wear dental facets from the El Sidrón (Asturias, Spain) Neandertals is described and analyzed. Out of 93 teeth, 64.5% present subvertical grooves, including a high frequency (50%) on the anterior dentition. Contrary to some studies, subvertical grooves from adjacent facets perfectly overlap each other and do not interdigitate, probably forming small channels. Both the facet and the groove surface share the same polished appearance, suggesting a common origin. Statistical analyses reveal that the number of grooves is neither dependent on the degree of occlusal wear, nor on the position on the tooth or the individual's age. However, facet width is an important factor determining the number of subvertical grooves. The etiology of subvertical grooves formation on Neandertal teeth remains unclear. Am J Phys Anthropol, 2010. © 2010 Wiley‐Liss, Inc.     

A reassessment of the purported venom delivery system of the bird-like raptor <Emphasis Type="Italic">Sinornithosaurus</Emphasis>

Gong and colleagues recently described unusual traits in the dromaeosaurid Sinornithosaurus that were interpreted as the first evidence of a venomous dinosaur. This interpretation was based on extremely elongated maxillary teeth, morphologically similar to those present in poisonous snakes; labial grooves on maxillary and dentary tooth crowns; and an additional ornamented depression in the lateral surface of the maxillary bone (subfenestral fossa). A reappraisal of each of these morphological traits is provided here in light of comparisons with other theropod dinosaurs and previous discussions for inferring poisonous capabilities in fossil taxa. We fail to recognize unambiguous evidence supporting the presence of a venom delivery system in Sinornithosaurus. For example, the extremely elongated teeth seem to be a taphonomic artifact due to the displacement of teeth outside the alveoli; the labial grooves are present in a wide variety of theropods; and no strong evidence for the lodging of a venomous gland is recognized. In contrast, the cranial and dental anatomy of Sinornithosaurus is congruent with that of other dromaeosaurids. The weak support for a venomous Sinornithosaurus renders unlikely the ecological model proposed by Gong and colleagues for this predatory dinosaur.     

Substitution of the dental root by aquatic invertebrate skeletons in animals and man

The biocompatibility of mammal bone with aragonite and calcite skeletons of aquatic invertebrates (Corals, Molluscs) led us, after animal experimentation, to implant in humans artificial dental roots derived from such invertebrates. These roots, incorporated but not resorbed, serve as supports for a prosthetic crown; they are equipped to isolate the root from the buccal cavity and to ensure shock absorbtion during mastication. The greater ease of implanting artificial teeth and their excellent acceptance will in many cases modify the strategy of current dental treatment.     

Dental Caries in the Elderly

Studies in the United States and other countries have shown that there is continued caries activity with advancing age. These studies, however, do not elaborate on the nature of the dental caries nor its anatomical location on the tooth. It has been assumed that dental caries occur on the coronal portion of retained teeth and that recurrent decay around existing restorations represents the major form of the disease. In addition to continued coronal caries activity in adults, the problem of carious lesions occurring on the exposed roots of teeth has been identified in a number of recent surveys. The exposure of the root surface to the oral cavity is a consequence of the apical migration of the periodontal attachment through periodontal disease and dental treatment which renders this part of the tooth at risk of the dental caries process. However, there are several distinct differences between coronal and root caries. The continued occurrence of coronal caries in adults and the projected increase m the prevalence of root caries suggests an expanded role for the restorative and preventive services for the older adult patient. Although the techniques relating to coronal caries are well-established, those relating to root caries are just beginning to be explored and developed. Many of the principles, materials and philosophies which have proved to be effective for coronal caries are not equally efficacious when the tooth root is involved. This area represents a fertile field for research and development in the older adult patient.     

Bone breakage in the Krapina hominid collection

The fragmentary condition of the Krapina Neandertal remains has been offered as one line of evidence for the hypothesis that these hominids were the victims of cannibals seeking marrow and brains. Two other hypotheses regarding the causes of the framentation have been raised: a substantial portion of the breakage in the Krapina collection is attributable to excavation damage; and the rest of the breakage is attributable to sedimentary pressure and to natural rock falls that occurred during the site's prehistory. The purpose of this paper is report on tests of these three hypotheses concerning the cause of breakage in the Krapina material. Microscopic inspection of all Krapina hominid specimens showed that 23% of the material was inadvertantly broken during excavation or during quarrying that took place at the end of the last century. The morphology of the prehistoric breakage is inconsistent with the cannibalism hypothesis and supports the hypothesis that prehistoric breakage was caused by sedimentary pressure and/or roof falls.     

Somatic variation in living, wild ring-tailed lemurs (Lemur catta)

While understanding somatic variability among wild primates can provide insight into natural patterns of developmental plasticity, published data for living populations are rare. Here we provide such information for two distinct wild populations of Lemur catta. Variants observed include microtia, athelia, and female virilization. Dental variants observed include individuals with supernumerary teeth, rotated teeth, maxillary incisor agenesis, and severe malocclusion. There was a sex bias in incisor agenesis, with 5 of 7 examples (71%) found in males. The frequency of dental variants in our sample is lower than that seen in many other lemuriformes, as well as other primates. This may be a product of their less derived dental formula and/or their relatively fast dental development. Amassing such data is a critical first step to assess if wild primate populations are exhibiting normal variability or are being affected by potential inbreeding and/or environmental effects.     

中国直立人牙齿特征变异及其演化意义

以往研究发现,中国直立人化石呈现较大的形态变异。对于这种变异程度及造成变异的原因,在古人类学界有不同的认识。有学者提出在直立人阶段,中国古人类已经呈现明显的区域性差异,但也有人认为这些差异似乎没有规律性。近年,本文作者采用不同方法对若干地点的中国直立人牙齿特征及其变异进行了系列研究,取得了一些新的发现和认识。本文在回顾总结这些研究的基础上,结合对其它一些地点中国直立人牙齿特征的观测对比,对中国直立人牙齿特征表现特点及变异作了进一步的分析。本研究发现,中国直立人牙齿特征具有较大的变异范围。这些变异似可分为两种主要类型,元谋、建始、郧县梅铺、和县牙齿呈现出较多的原始特点,代表一种原始类型;周口店、沂源等地点的标本特征相对进步,表现出更多的典型直立人特征。其它一些地点的直立人化石呈现出混合或中间状态。值得注意的是部分呈现出原始牙齿特征类型的中国直立人的生存年代相对较晚,其牙齿特征的原始性与生存时代不具有对应关系。作者认为中国直立人牙齿特征类型反映了更新世早期和中期不同直立人群的演化状态。原始类型牙齿特征的形成不仅与演化时序性和地理分布有关,还在一定程度上反映了一些中国直立人群的演化隔离。     

Krapina, “Classic” Neanderthals,and the evolution of the European face

Except for the front end of the dental arch, tooth size remained at approximately the same level throughout the Middle Pleistocene. The Krapina Neanderthals at the end of the last interglacial differed from Homo erectus only in having larger front teeth. From that time on, tooth size in populations at the northern edge of the area of human occupation in the Old World has reduced approximately in proportion to the time elapsed. The “Classic” Neanderthals of western Europe, in fact, have teeth that are 15% smaller than those of the earlier Krapina Neanderthals and only 5% larger than the early Upper Palaeolithic. Reduction since the early Upper Palaeolithic has proceeded another full 20%. It is suggested that the development of heated stone cooking in the Mousterian, originally for the purpose of thawing frozen food, reduced the forces of selection that had previously maintained tooth size during the Middle Pleistocene. The operation of the Probable Mutation Effect, then produced the observed reductions.     

The late Neandertal supraorbital fossils from Vindija Cave,Croatia: a biased sample?

The late Neandertal sample from Vindija (Croatia) has been described as transitional between the earlier Central European Neandertals from Krapina (Croatia) and modern humans. However, the morphological differences indicating this transition may rather be the result of different sex and/or age compositions between the samples. This study tests the hypothesis that the metric differences between the Krapina and Vindija supraorbital samples are due to sampling bias. We focus upon the supraorbital region because past studies have posited this region as particularly indicative of the Vindija sample's transitional nature. Furthermore, the supraorbital region varies significantly with both age and sex.We analyzed four chords and two derived indices of supraorbital torus form as defined by Smith & Ranyard (1980, Am. J. phys. Anthrop.93, pp. 589-610). For each variable, we analyzed relative sample bias of the Krapina and Vindija samples using three sampling methods. In order to test the hypothesis that the Vindija sample contains an over-representation of females and/or young while the Krapina sample is normal or also female/young biased, we determined the probability of drawing a sample of the same size as and with a mean equal to or less than Vindija's from a Krapina-based population. In order to test the hypothesis that the Vindija sample is female/young biased while the Krapina sample is male/old biased, we determined the probability of drawing a sample of the same size as and with a mean equal or less than Vindija's from a generated population whose mean is halfway between Krapina's and Vindija's. Finally, in order to test the hypothesis that the Vindija sample is normal while the Krapina sample contains an over-representation of males and/or old, we determined the probability of drawing a sample of the same size as and with a mean equal to or greater than Krapina's from a Vindija-based population. Unless we assume that the Vindija sample is female/young and the Krapina sample is male/old biased, our results falsify the hypothesis that the metric differences between the Krapina and Vindija samples are due to sample bias.     

Krapina 1: a juvenile Neandertal from the early late Pleistocene of Croatia

The juvenile A Skull from Krapina, Croatia (Krapina 1) has been the subject of considerable debate since B. Skerlj first suggested that it might not be a Neandertal. Although widely known by its original designation, the Krapina A Skull was recatalogued, along with all of the Krapina hominids, in the 1980's (Radovcic, et al., [1988]. The Krapina Hominids: An Illustrated Catalog of Skeletal Collection. Zagreb; Mladost). It is now catalogued as Krapina 1 in the archives of the Hrvatski Prirodoslovni Muzej, Zagreb, Croatia. We present a detailed, morphometric analysis of this specimen, comparing it to other Krapina specimens, juvenile late Pleistocene hominids (including Neandertals), and subadult recent humans. This analysis demonstrates that Krapina 1 possesses morphological features that are primitive retentions; others that represent derived Neandertal specializations; and still others that are typical for all European late Pleistocene humans. Morphological features associated with the browridges are intermediate between Neandertal and early modern European form. Nevertheless, a thorough analysis of the morphology of this specimen, in ontogenetic and regional contexts, leads to the conclusion that it cannot be excluded from the Neandertal range of variation. We conclude that the most parsimonious explanation for this 130 ka specimen is that it should be regarded as a Neandertal.     

Ancient teeth and modern human origins: an expanded comparison of African Plio-Pleistocene and recent world dental samples

Previous research by the first author revealed that, relative to other modern peoples, sub-Saharan Africans exhibit the highest frequencies of ancestral (or plesiomorphic) dental traits and, thus, appear to be least derived dentally from an ancestral hominin state. This determination, in conjunction with various other lines of dental morphological evidence, was interpreted to be supportive of an African origin for modern humans. The present investigation expands upon this work by using: 1) direct observations of fossil hominin teeth, rather than data gleaned from published sources, 2) a single morphological scoring system (the Arizona State University Dental Anthropology System) with consistent trait breakpoints, and 3) data from larger and more varied modern human comparative samples. As before, a multivariate distance statistic, the mean measure of divergence, was used to assess diachronic phenetic affinities among the Plio-Pleistocene hominins and modern humans. The present study also employed principal components analysis on dental trait frequencies across samples. Both methods yielded similar results, which support the previous findings; that is, of all modern human samples, sub-Saharan Africans again exhibit the closest phenetic similarity to various African Plio-Pleistocene hominins-through their shared prevalence of morphologically complex crown and root traits. The fact that sub-Saharan Africans express these apparently plesiomorphic characters, along with additional information on their affinity to other modern populations, evident intra-population heterogeneity, and a world-wide dental cline emanating from the sub-continent, provides further evidence that is consistent with an African origin model.