Analytical evidence of enamel hypomineralisation on permanent and primary molars amongst past populations /631/181/19/2471 /692/699 /123 article

Molar Incisor Hypomineralisation (MIH) and Hypomineralised Second Primary Molars (HSPM) involve prevalent qualitative structural developmental anomalies of tooth enamel affecting the first permanent molars (and often incisors) and the second primary molars, respectively. These demarcated hypomineralised lesions of enamel manifest as white-cream or yellow-brown opacities, with possible post-eruptive localised loss of enamel. Aetiological hypotheses have involved contemporary life factors (i.e. environmental pollutant exposure or early childhood medications) in contrast to factors not limited to a specific time period (i.e. hypoxia at birth or genetic predisposition). Evidence of MIH in ancient populations would reinforce aetiological factors present for many centuries. By means of microtomographic and X-ray fluorescence analyses the present study provides evidence that (i) two archaeological specimens: "S407" (Sains-en-Gohelle, France, 12th-16th centuries) and "B335" (Beauvais, France, 15th-18th centuries) were MIH-affected, and (ii) one individual "S323" was affected by HSPM and MIH (Sains-en-Gohelle, France, 7th-11th centuries)

The human remains from the Lumentxa cave (Lekeitio, Biscay, Northern Iberian Peninsula): Paleobiology, Taphonomy and Chronology

Lumentxa is a classic site in Basque Prehistory, excavated in three different phases during the 20th century, which has yielded evidence of both Pleistocene and Holocene occupations. In this article, we present a detailed study of the human remains from this site including paleobiological, taphonomic, biomechanical and chronological perspectives. The human assemblage comprises of a minimum number of seven individuals: three subadult and four adults, with both sexes represented, although part of the human collection is currently lost. We have obtained C14 dates from 4 of these 7 individuals indicating a prolonged funerary use of the cave from the Early Neolithic until the Bronze Age. We observed some biases in the skeletal representation which could be due to differences in the excavation methods between field seasons and/or the action of carnivores, the latter being evident in at least three of the individuals. The taphonomic modifications are typical off those found in the post-abandonment phases in cave funerary contexts. The relatively low number of individuals compared with other sites in the region and extended timespan over which the remains were deposited suggest that the cave was used only sporadically for funerary purposes. We report the first biomechanical data for a Neolithic individual from the Iberian Peninsula, which show greatest overall similarity to the Neolithic sample from France and Italy. Finally, the broad time period covered by the direct dates and the more complex taphonomic history than was previously assumed for such sites indicate that caution is warranted when assigning sepulchral caves to cultural periods in the Western Pyrenees when no direct 14C dates have been obtained

Diagnostic guide enabling distinction between taphonomic stains and enamel hypomineralisation in an archeological context

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Stratégies de subsistance et analyse culturelle de populations néolithiques de Ligurie : approche par l'étude isotopique (13C et 15N) des restes osseux

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Stratégies de subsistance et analyse culturelle de populations néolithiques de Ligurie: Approche par l’étude isotopique (δ13C et δ15N) des restes osseux

For the last ten millennia humans have learned how to manage and produce their own food resources. In Liguria, the exploitation of the marine and coastal environment as well as the acquisition and use of agriculture and pastoralism at the time of Neolithisation (i.e. 6th millennia BC) are evidenced by both archaeological and palaeoenvironmental studies. However, it is difficult, using these methods, to determine the relative contributions to human diets made by foods from these difference sources, especially throughout the Neolithic period. The presence of human burials and animal remains from various sites from this region allows the use of isotopic methods, and in particular the study of the δ13C and δ15N values of bone collagen, which provides information on the sources of dietary protein. This method is able to determine the relative importance of marine foods in the diets of the early Neolithic agriculturalists and pastoralists, as well as indicate dietary differences between contemporary populations. Two coastal Neolithic sites were the subject of our study: Pendimoun (France) and Arene Candide (Italy). The results show, contrary to expectations, the absence of regular consumption of marine resources and the food differences within the populations