Growing up in Ancient Sardinia: Infant-toddler dietary changes revealed by the novel use of hydrogen isotopes (δ2H).

Detailed information about the lives and deaths of children in antiquity is often in short supply. Childhood dietary histories are, however, recorded and maintained in the teeth of both juveniles and adults. Primary tooth dentinal collagen does not turn over, preserving a sequential record of dietary changes. The use of nitrogen (δ15N) and carbon (δ13C) isotope values of incrementally sampled dentin are used in the study of breastfeeding practices but evidence for the addition of weaning foods, both in terms of mode and, particularly, duration, has remained analytically inaccessible to date. Here, we demonstrate how the novel use hydrogen isotope (δ2H) values of sequentially micro-sampled dentin collagen, measured from individuals excavated from a Punic cemetery, in Sardinia, Italy, can serve as a proxy for weaning food type and duration in ancient childhood diet. The weaning rate and age, based on the decline in δ15N and δ13C values of permanent first molars and the concomitant increase in δ2H, appears to be broadly similar among six individuals. Hydrogen isotopes vary systematically from a low value soon after birth, rising through early childhood. The early post-birth values can be explained by the influence of 2H-depleted lipids from mother's breastmilk and the later δ2H rise is consistent with, among other things, a substantial portion of boiled foodstuffs, such as the higher δ2H values observed in porridge. Overall δ2H in dentin shows great promise to elucidate infant and childhood feeding practices, and especially the introduction of supplementary foods during the weaning process.

Prehistoric funerary complexity in northern Iberia studied by using dental morphology.

During the Neolithic Age and afterwards, several funerary practices coexisted in the northeast of the Iberian Peninsula from the Mediterranean to the Atlantic. According to archaeological data, there was a coexistence of sepulchral caves and megalithic monuments at the end of the Neolithic, following the dominance of open-air pit burials during the Middle Neolithic. The aim of this work is to analyze the biological relationships between individuals representing those cultures, based on their dental morphology - the first such attempt. This study presents data of 156 individuals from this period, and will allow elucidate the population dynamics including the role of migrations and other factors. The results indicate that there were no significant differences between the groups living in Atlantic and Mediterranean areas. Moreover, pairwise comparisons for each trait only show two significant results. This lack of differences could be related to trade activities between the two basins, which would contribute to individual exchanges between groups. Furthermore, according to biological affinities, trade activities along the Mediterranean Sea had a more marked influence over the Catalan populations than those from the Atlantic basin. There are no biological differences between groups representing the open-air pit culture and the sepulchral caves in each area. Finally, the megalithic groups from the Atlantic basin differ the most from the surrounding populations. This could be indicative of a slightly different biological origin of the people related to this culture.

A case of bilateral macrodontia of mandibular second premolars from a Chalcolithic context in the Iberian Peninsula.

Isolated macrodontia, consisting of the gigantism of a single tooth, is an extremely rare condition. Only 16 cases of isolated macrodontia of mandibular second premolars have been reported to date. Although the aetiology of this phenomenon remains unknown, many authors have related it to the control of the apoptotic process, leading to the patterning and size of dental cusps. There is not a clear genetic inheritance pattern since only two of those 16 cases correspond to close relatives. To our knowledge, there have been no reports of isolated macrodontia of mandibular second premolars in archaeological remains. Cova del Pantà de Foix site is a Chalcolithic sepulchral cave situated in the North-East of the Iberian Peninsula in which the remains of at least 30 individuals were recovered. Most of these individuals show several signs of environmental stressors. The current study presents the first case of isolated bilateral macrodontia of mandibular premolars from an archaeological context, corresponding to a young male individual discovered in this site. This condition could be the last consequence of environmental factors epigenetically affecting apoptosis processes in early tooth development and a possible genetic predisposition to show a shape-deviation in the dentition.

The emergence of mesolithic cemeteries in SW Europe: insights from the El Collado (Oliva, Valencia, Spain) radiocarbon record.

Located on the Iberian Mediterranean coast, El Collado is an open-air site where a rescue excavation was conducted over two seasons in 1987 and 1988. The archaeological work excavated a surface area of 143 m2 where 14 burials were discovered, providing skeletal remains from 15 individuals. We have obtained AMS dates for 10 of the 15 individuals by means of the direct dating of human bones. The ranges of the probability distribution of the calibrated dates suggest that the cemetery was used during a long period of time (781-1020 years at a probability of 95.4%). The new dates consequently set back the chrono-cultural attribution of the cemetery from the initial proposal of Late Mesolithic to an older date in the Early Mesolithic. Therefore, El Collado becomes the oldest known cemetery in the Iberian Peninsula, earlier than the numerous Mesolithic funerary contexts documented on the Atlantic façade such as the Portuguese shell-middens in the Muge and Sado Estuaries or the funerary sites on the northern Iberian coast.