Anterior dental loading and root morphology in Neanderthals

Distinguer les incisives et canines des Néanderthaliens de celles des hommes modernes peut représenter un défi dans le cas de dents isolées trouvées dans des collections de musée, ou provenant de contextes stratigraphiques perturbés. De plus, la morphologie de la couronne ne peut être utilisée dans le cas de dents fortement usées. Une étude préliminaire basée sur des échantillons limités et des mesures linéaires (Bailey, 2005) propose que la longueur des racines dentaires à elle seule permet de discriminer taxonomiquement les Néanderthaliens des hommes modernes du Paléolithique supérieur et actuels. Cette thèse teste cette hypothèse pour un échantillon de Néanderthaliens et d'hommes modernes, plus large géographiquement et chronologiquement, en utilisant la micro-tomographie. En plus de l'intérêt taxonomique d'explorer la taille et la forme des racines, nous discutons les implications fonctionnelles de la morphologie racinaire des dents antérieures dans le contexte de l'hypothèse des " dents-utilisées-comme-des-outils ", et des activités para-masticatrices. La première partie a été publiée comme suit : Le Cabec, A., Kupczik, K., Gunz, P., Braga, J., and Hublin, J.J. (2012). Long Anterior Mandibular Tooth Roots in Neanderthals Are Not the Result of their Large Jaws. Journal of Human Evolution, pp. 63, 667-681. DOI: 10.1016/j. jhevol.2012.07.003. Cette partie valide la longueur des racines dentaires en tant qu'outil taxonomique pour distinguer les Néanderthaliens tardifs des hommes modernes du Paléolithique Supérieur et récents. En dépit de l'absence de corrélation entre la taille des racines et la taille de la symphyse mentonnière, les Néanderthaliens ont de grandes racines, pour la taille de leurs mâchoires. Il est alors proposé que les courtes racines des hommes modernes récents résulteraient d'une allométrie négative. La seconde partie a été publiée comme suit : Le Cabec, A., Gunz, P., Kupczik, K., Braga, J. and Hublin, J.J. (2013). Anterior Tooth Root Morphology and Size in Neanderthals: Taxonomic and Functional Implications. Journal of Human Evolution, 64, pp. 169-193. DOI: 10.1016/j. jhevol.2012.08.011. La morphologie racinaire est étudiée à travers un large échantillon d'hominidés fossiles et actuels, couvrant une large période chronologique et une vaste zone géographique. Les plus grandes longueurs racinaires observées chez les Néanderthaliens peuvent avoir résulté de la rétention d'une condition ancestrale. L'attribution taxonomique débattue de certains spécimens est discutée à la lumière de la morphologie racinaire des dents antérieures et montre que la longueur racinaire seule ne devrait pas être considérée comme suffisante pour une diagnose taxonomique. La fréquente présence d'hypercémentose et sa distribution non-homogène autour de l'apex racinaire pour les dents antérieures des Néanderthaliens pourrait refléter le régime de charge exercé sur les dents antérieures, probablement utilisées comme une troisième main.Distinguishing Neanderthal and modern human incisors and canines can be challenging in the case of isolated teeth found in museum collections, or from unclear stratigraphic contexts. In addition, the crown morphology cannot be used in the case of heavily worn teeth. A preliminary study based on limited samples and linear measurements (Bailey, 2005) proposed that root length alone can taxonomically discriminate Neanderthals from Upper Paleolithic and extant modern humans. This thesis investigates whether this remains true for a broader chronological and geographical sample of Neanderthals and modern humans, using micro-computed tomography. In addition to the taxonomic interest of investigating root size and shape, we discuss the functional implications of the anterior root morphology in the context of the 'teeth-as-tools' hypothesis and of para-masticatory activities. The first part was published as: Le Cabec, A., Kupczik, K., Gunz, P., Braga, J., and Hublin, J.J. (2012). Long Anterior Mandibular Tooth Roots in Neanderthals Are Not the Result of their Large Jaws. Journal of Human Evolution, 63, pp. 667-681. DOI: 10.1016/j.jhevol.2012.07.003. This part validates root length as a taxonomical tool to distinguish late Neanderthals from Upper Paleolithic and recent modern humans. Despite the absence of correlation between root size and symphyseal size, Neanderthals have large roots for the size of their jaws. It is hypothesized that the short roots of extant modern humans result from a negative allometry. The second part was published as: Le Cabec, A., Gunz, P., Kupczik, K., Braga, J. and Hublin, J.J. (2013). Anterior Tooth Root Morphology and Size in Neanderthals: Taxonomic and Functional Implications. Journal of Human Evolution, 64, pp. 169-193. DOI: 10.1016/j. jhevol.2012.08.011. Root morphology is explored across a chronologically and geographically large sample of fossil and extant hominids. Longer roots in Neanderthals may have resulted from the retention of an ancestral condition. The debated taxonomic attribution of some specimens is discussed in light of anterior tooth root morphology and shows that root length alone should not be sufficient for taxonomic diagnosis. The frequent presence of hypercementosis and its non-homogeneous distribution around the root apex in Neanderthal anterior teeth could reflect the loading regime exerted on the front teeth, likely used as a third hand

Disentangling isolated dental remains of Asian Pleistocene hominins and pongines

International audienceScholars have debated the taxonomic identity of isolated primate teeth from the Asian Pleis-tocene for over a century, which is complicated by morphological and metric convergence between orangutan (Pongo) and hominin (Homo) molariform teeth. Like Homo erectus, Pongo once showed considerable dental variation and a wide distribution throughout mainland and insular Asia. In order to clarify the utility of isolated dental remains to document the presence of hominins during Asian prehistory, we examined enamel thickness, enamel-den-tine junction shape, and crown development in 33 molars from G. H. R. von Koenigswald's Chinese Apothecary collection (11 Sinanthropus officinalis [= Homo erectus], 21 "Heman-thropus peii," and 1 "Hemanthropus peii" or Pongo) and 7 molars from Sangiran dome (either Homo erectus or Pongo). All fossil teeth were imaged with non-destructive conventional and/or synchrotron micro-computed tomography. These were compared to H. erectus teeth from Zhoukoudian, Sangiran and Trinil, and a large comparative sample of fossil Pongo, recent Pongo, and recent human teeth. We find that Homo and Pongo molars overlap substantially in relative enamel thickness; molar enamel-dentine junction shape is more distinctive, with Pongo showing relatively shorter dentine horns and wider crowns than Homo. Long-period line periodicity values are significantly greater in Pongo than in H. erec-tus, leading to longer crown formation times in the former. Most of the sample originally assigned to S. officinalis and H. erectus shows greater affinity to Pongo than to the hominin comparative sample. Moreover, enamel thickness, enamel-dentine junction shape, and a long-period line periodicity value in the "Hemanthropus peii" sample are indistinguishable from fossil Pongo. These results underscore the need for additional recovery and study of associated dentitions prior to erecting new taxa from isolated teeth

The Neanderthal teeth from Marillac (Charente, Southwestern France): Morphology, comparisons and paleobiology

Few European sites have yielded human dental remains safely dated to the end of MIS 4/beginning of MIS 3. One of those sites is Marillac (Southwestern France), a collapsed karstic cave where archeological excavations (1967–1980) conducted by B. Vandermeersch unearthed numerous faunal and human remains, as well as a few Mousterian Quina tools. The Marillac sinkhole was occasionally used by humans to process the carcasses of different prey, but there is no evidence for a residential use of the site, nor have any hearths been found. Rare carnivore bones were also discovered, demonstrating that the sinkhole was seasonally used, not only by Neanderthals, but also by predators across several millennia. The lithostratigraphic units containing the human remains were dated to ∼60 kyr. The fossils consisted of numerous fragments of skulls and jaws, isolated teeth and several post-cranial bones, many of them with traces of perimortem manipulations. For those already published, their morphological characteristics and chronostratigraphic context allowed their attribution to Neanderthals. This paper analyzes sixteen unpublished human teeth (fourteen permanent and two deciduous) by investigating the external morphology and metrical variation with respect to other Neanderthal remains and a sample from modern populations. We also investigate their enamel thickness distribution in 2D and 3D, the enamel-dentine junction morphology (using geometric morphometrics) of one molar and two premolars, the roots and the possible expression of taurodontism, as well as pathologies and developmental defects. The anterior tooth use and paramasticatory activities are also discussed. Morphological and structural alterations were found on several teeth, and interpreted in light of human behavior (tooth-pick) and carnivores' actions (partial digestion). The data are interpreted in the context of the available information for the Eurasian Neanderthals

New fossils from Jebel Irhoud, Morocco and the pan-African origin of Homo sapiens

Fossil evidence points to an African origin of Homo sapiens from a group called either H. heidelbergensis or H. rhodesiensis. However, the exact place and time of emergence of H. sapiens remain obscure because the fossil record is scarce and the chronological age of many key specimens remains uncertain. In particular, it is unclear whether the present day ‘modern’ morphology rapidly emerged approximately 200 thousand years ago (ka) among earlier representatives of H. sapiens1 or evolved gradually over the last 400 thousand years2. Here we report newly discovered human fossils from Jebel Irhoud, Morocco, and interpret the affinities of the hominins from this site with other archaic and recent human groups. We identified a mosaic of features including facial, mandibular and dental morphology that aligns the Jebel Irhoud material with early or recent anatomically modern humans and more primitive neurocranial and endocranial morphology. In combination with an age of 315?±?34 thousand years (as determined by thermoluminescence dating)3, this evidence makes Jebel Irhoud the oldest and richest African Middle Stone Age hominin site that documents early stages of the H. sapiens clade in which key features of modern morphology were established. Furthermore, it shows that the evolutionary processes behind the emergence of H. sapiens involved the whole African continent

Régime de charge et morphologie racinaire des dents antérieures chez les Néanderthaliens

TOULOUSE3-BU Sciences (315552104) / SudocSudocFranceF

Direct correspondence of 2D and 3D developmental information.

<p>Matching of the incremental pattern between the standardized developmental slice of the ULC of STS2 and the 3D models of its EDJ and OES. Retzius lines or accentuated lines in the enamel on the 2D virtual slice allows the matching of a stress on the EDJ and OES. The number of long-period lines is indicated in square brackets between the major stress events highlighted on the 2D and 3D models, providing a quantitative overview of the time elapsed between stress. The long-period line count was performed on a high resolution image of the 2D slice to ensure a high definition of the growth lines. Further developmental information for this individual may be found in [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0123019#pone.0123019.ref061" target="_blank">61</a>]. File name: Figure_9.tif.</p

Synchrotron X-ray fluorescence mapping of Ca, Sr and Zn at the neonatal line in human deciduous teeth reflects changing perinatal physiology

Objectives: Our first objective was to review the evidence describing the appearance and microstructure of theneonatal line in human deciduous teeth and to link this with known changes in neonatal physiology occurring atand around birth. A second objective was to explore ways to improve identification of the neonatal line bymapping the pre- and postnatal distribution of Ca, Sr and Zn in deciduous cuspal enamel and superimposingthese maps onto transmitted light micrographs that included a clear true section of the neonatal line.Materials and methods: We used synchrotron X-ray fluorescence to map elemental distributions in pre- andpostnatal enamel and dentine. Two deciduous canines and 5 deciduous molars were scanned with an X-ray beammonochromatised to 17.0 keV at either 10.0, 2.5 or 1.0 μm resolution and 10 ms integration time.Results: Calcium maps distinguished enamel and dentine but did not clearly demarcate tissues formed pre- orpostnatally. Strontium maps reflected presumed pre- and postnatal maternal serum levels and what are likely tobe diet-dependent regions of Sr enrichment or depletion. Prenatal Zn maps, particularly for dentine, mirrorelevated levels in the fetus and in colostrum during the first few days of life.Conclusions: The neonatal line, enamel dentine junction and surface enamel were all Zn-rich. Within the neonatalline Zn may be associated with increased crystallinity but also with caries resistance, both of which havebeen reported previously. Elemental mapping may improve the identification of ambiguous NNLs and so beuseful in forensic and archaeological studies

Accessing Developmental Information of Fossil Hominin Teeth Using New Synchrotron Microtomography-Based Visualization Techniques of Dental Surfaces and Interfaces

<div><p>Quantification of dental long-period growth lines (Retzius lines in enamel and Andresen lines in dentine) and matching of stress patterns (internal accentuated lines and hypoplasias) are used in determining crown formation time and age at death in juvenile fossil hominins. They yield the chronology employed for inferences of life history. Synchrotron virtual histology has been demonstrated as a non-destructive alternative to conventional invasive approaches. Nevertheless, fossil teeth are sometimes poorly preserved or physically inaccessible, preventing observation of the external expression of incremental lines (perikymata and periradicular bands). Here we present a new approach combining synchrotron virtual histology and high quality three-dimensional rendering of dental surfaces and internal interfaces. We illustrate this approach with seventeen permanent fossil hominin teeth. The outer enamel surface and enamel-dentine junction (EDJ) were segmented by capturing the phase contrast fringes at the structural interfaces. Three-dimensional models were rendered with Phong’s algorithm, and a combination of directional colored lights to enhance surface topography and the pattern of subtle variations in tissue density. The process reveals perikymata and linear enamel hypoplasias on the entire crown surface, including unerupted teeth. Using this method, highly detailed stress patterns at the EDJ allow precise matching of teeth within an individual’s dentition when virtual histology is not sufficient. We highlight that taphonomical altered enamel can in particular cases yield artificial subdivisions of perikymata when imaged using X-ray microtomography with insufficient resolution. This may complicate assessments of developmental time, although this can be circumvented by a careful analysis of external and internal structures in parallel. We further present new crown formation times for two unerupted canines from South African Australopiths, which were found to form over a rather surprisingly long time (> 4.5 years). This approach provides tools for maximizing the recovery of developmental information in teeth, especially in the most difficult cases.</p></div

Exceptionally high δ15N values in collagen single amino acids confirm Neandertals as high-trophic level carnivores

Isotope and archeological analyses of Paleolithic food webs have suggested that Neandertal subsistence relied mainly on the consumption of large herbivores. This conclusion was primarily based on elevated nitrogen isotope ratios in Neandertal bone collagen and has been significantly debated. This discussion relies on the observation that similar high nitrogen isotopes values could also be the result of the consumption of mammoths, young animals, putrid meat, cooked food, freshwater fish, carnivores, or mushrooms. Recently, compound-specific C and N isotope analyses of bone collagen amino acids have been demonstrated to add significantly more information about trophic levels and aquatic food consumption. We undertook single amino acid C and N isotope analysis on two Neandertals, which were characterized by exceptionally high N isotope ratios in their bulk bone or tooth collagen. We report here both C and N isotope ratios on single amino acids of collagen samples for these two Neandertals and associated fauna. The samples come from two sites dating to the Middle to Upper Paleolithic transition period (Les Cottés and Grotte du Renne, France). Our results reinforce the interpretation of Neandertal dietary adaptations as successful top-level carnivores, even after the arrival of modern humans in Europe. They also demonstrate that high δ15N values of bone collagen can solely be explained by mammal meat consumption, as supported by archeological and zooarcheological evidence, without necessarily invoking explanations including the processing of food (cooking, fermenting), the consumption of mammoths or young mammals, or additional (freshwater fish, mushrooms) dietary protein sources