Search

Strontium isotopes (Sr-87/Sr-86) provide valuable information to help reconstruct past mobility. For the analysis of archaeological tooth enamel to provide a direct assessment of mobility, a comparison to the baseline Sr-87/Sr-86 in a region is required. In this study, a large-scale Sr-87/Sr-86 baseline of Portugal is created based on 151 paired plant and soil leachate samples combined with previously published data (20 additional plant and 33 additional soil leachate sites). Spatial patterns of Sr-87/Sr-86 are evident, following Portugal's geology and terrain, with higher Sr-87/Sr-86 in the granite dominated north and further inland. Influences from sea spray are observed along the coastal regions of the country. The bioavailable strontium range for Portugal is 0.70575-0.73487, and paired plant-soil leachate site measurements show a strong positive relationship. Empirical Bayesian Kriging (EBK) alongside mean Sr-87/Sr-86 per geological unit are used to provide predictive surfaces for bioavailable Sr-87/Sr-86. We find that the addition of archaeological site-specific measurements is required in archaeological mobility studies to ensure local-scale Sr-87/Sr-86 variation is captured, illustrated in this study using the Late Middle Neolithic to Early Bronze Age site of Perdigoes. The bioavailable strontium isoscape for Portugal provides a baseline map for future archaeological and palaeoecological studies in this region and contributes to the global efforts to map strontium isotope variability. ARC Discovery Project DP160100811 Grant agreement number 948913 info:eu-repo/semantics/publishedVersion

Your dentist can tell a lot about your health and daily habits just by looking at your teeth. But did you know that archaeological scientists have discovered that there is a lot more information hidden in teeth? We can study the chemical composition of teeth and can find out what types of food a person ate, and even where that food was growing. When we find teeth in archaeological sites, a method called isotope analysis can be used to reconstruct the movements and diets of people, even when no written records are available. In this article, we will discuss what our teeth are made of and how isotope analysis can be used to learn more about ancient people. We will then look at an archaeological site in France, where children discovered bones and teeth on the playground behind their kindergarten.

This paper collates previously published data from incremental isotopic studies performed on faunal remains found within the modern boundaries of the United Kingdom (UK). The dataset represents a complete collection of zooarchaeological incremental data from the UK, consisting of 1,092 data points, obtained from 152 faunal specimens from 20 archaeological sites, dating from 7960 BC to AD 1300. 59 of these values are from incrementally sampled dentine and present stable carbon and nitrogen isotope ratios (

During the early medieval period (5th–9th century CE), the North Sea coastal societies were involved in long distance maritime trade relations, which resulted in a pronounced mobility of individuals throughout the North Sea area. This work presents the first isotope data from human remains on diet and mobility from early medieval Belgian coastal populations. A total of 23 out of 51 excavated individuals from the archaeological site of Koksijde, Belgium (7th–8th century AD), was selected for isotope and elemental analyses (δ13Ccol, δ15N, δ18OP, δ13Cap, δ18OC, 87Sr/86Sr and [Sr]). The high δ15N values of part of the individuals buried at Koksijde indicate that high trophic level ranked fish was included in their diets, suggesting an intensive exploitation of marine food sources. The δ18O values are not compatible with the predicted ‘local’ values while the strontium isotope ratios have values close to that of seawater (0.7092). Either the actual oxygen isotope values in early medieval Belgium are offset by 1 or2‰ compared to the current meteoric water predictions, or the population came from somewhere else. Whether or not this was linked to the population's mobility is difficult to assess based on their δ18O and 87Sr/86Sr values. Nonetheless, the study of the population at Koksijde provides new insights into the lives of the early medieval coastal Belgian societies.

International audience; The burial mound of Le Tumulus des Sables, southwest France, contains archaeological artefacts spanning from the Neolithic to the Iron Age. Human remains have been found throughout the burial mound, however their highly fragmented state complicates the association between the burial mound structure and the archaeological material. Radiocarbon dating and isotopic analyses of human teeth have been used to investigate the chronology, diet and mobility of the occupants. Radiocarbon dating shows that the site was used for burials from the Neolithic to Iron Age, consistent with the range of archaeological artefacts recovered. δ 13 C and δ 15 N values (from dentine collagen) suggest a predominately terrestrial diet for the population, unchanging through time. 87 Sr/ 86 Sr (on enamel and dentine) and δ 18 O (on enamel) values are consistent with occupation of the surrounding region, with one individual having a δ 18 O value consistent with a childhood spent elsewhere, in a colder climate region. These results showcase the complex reuse of this burial mound by a mostly local population over a period of about 2000 years.

Strontium isotope ratios (87Sr/86Sr) of archaeological samples (teeth and bones) can be used to track mobility and migration across geologically distinct landscapes. However, traditional interpolation algorithms and classification approaches used to generate Sr isoscapes are often limited in predicting multiscale 87Sr/86Sr patterning. Here we investigate the suitability of plant samples and soil leachates from the IRHUM database ( www.irhumdatabase.com ) to create a bioavailable 87Sr/86Sr map using a novel geostatistical framework. First, we generated an 87Sr/86Sr map by classifying 87Sr/86Sr values into five geologically-representative isotope groups using cluster analysis. The isotope groups were then used as a covariate in kriging to integrate prior geological knowledge of Sr cycling with the information contained in the bioavailable dataset and enhance 87Sr/86Sr predictions. Our approach couples the strengths of classification and geostatistical methods to generate more accurate 87Sr/86Sr predictions (Root Mean Squared Error = 0.0029) with an estimate of spatial uncertainty based on lithology and sample density. This bioavailable Sr isoscape is applicable for provenance studies in France, and the method is transferable to other areas with high sampling density. While our method is a step forward in generating accurate 87Sr/86Sr isoscapes, the remaining uncertainty also demonstrates that fine-modelling of 87Sr/86Sr variability is challenging and requires more than geological maps for accurately predicting 87Sr/86Sr variations across the landscape. Future efforts should focus on increasing sampling density and developing predictive models to further quantify and predict the processes that lead to 87Sr/86Sr variability.

Rationale Oxygen isotope ratios (δ18 O values) of fish otoliths (ear bones) are valuable geochemical tracers of water conditions and thermal life history. Delta Smelt (Hypomesus transpacificus) are osmerid forage fish endemic to the San Francisco Estuary, California, USA, that are on the verge of extinction. These fish exhibit a complex life history that allows them to survive in a dynamic estuarine environment; however, a rapidly warming climate threatens this thermally sensitive species. Here we quantify the accuracy and precision of using δ18 O values in otoliths to reconstruct the thermal life histories of Delta Smelt. Methods Delta Smelt were reared for 360 days using three different water sources with different ambient δ18 Owater values (-8.75‰, -5.28‰, and -4.06‰) and different water temperatures (16.4°C, 16.7°C, 18.7°C, and 20.5°C). Samples were collected after 170 days (n = 28) and 360 days (n = 14) post-hatch. In situ δ18 O values were measured from the core of the otolith to the dorsal edge using secondary ion mass spectrometry (SIMS) to reconstruct temporally resolved thermal life histories. Results The δ18 Ootolith values for Delta Smelt varied as a linear inverse function of water temperature: 1000 ln α = 18.39 (±0.43, 1SE)(103 TK-1 ) - 34.56 (±1.49, 1SE) and δ18 Ootolith(VPDB) - δ18 Owater (VPDB) = 31.34(±0.09, 1SE) - 0.19(±0.01, 1SE) × T ° C. When the ambient δ18 Owater value is known, this species-specific temperature-dependent oxygen isotope fractionation model facilitated the accurate (0.25°C) and precise (±0.37°C, 2σ) reconstruction of the water temperature experienced by the fish. In contrast, the use of existing general fractionation equations resulted in inaccurate temperature reconstructions. Conclusions The species-specific δ18 Ootolith fractionation equation allowed for accurate and precise reconstructions of water temperatures experienced by Delta Smelt. Characterization of ambient δ18 Owater values remains a critical next step for reconstructing thermal life histories of wild Delta Smelt. This tool will provide new insights into habitat utilization, potential thermal refugia, and resilience to future warming for this critically endangered fish.

International audience; Neanderthals had complex land use patterns, adapting to diversified landscapes and climates. Over the past decade, considerable progress has been made in reconstructing the chronology, land use and subsistence patterns, and occupation types of sites in the Rhône Valley, southeast France. In this study, Neanderthal mobility at the site of Payre is investigated by combining information from lithic procurement analysis (“chaîne evolutive” and “chaîne opératoire” concepts) and strontium isotope analysis of teeth (childhood foraging area), from two units (F and G). Both units date to the transition from Marine Isotope Stage (MIS) 8 to MIS 7, and show similar environmental conditions, but represent contrasting occupation durations. Level Gb (unit G) represents a long-term year-round use, in contrast to short-term seasonal use of the cave in level Fb (unit F). For both levels, lithic material and food were generally collected from a local to semi-local region. However, in level Gb, lithic materials were mainly collected from colluviums and food collected in the valley, whereas in level Fb, lithic procurement focused primarily on alluvial deposits and food was collected from higher elevation plateaus. These procurement or exchange patterns might be related to flint availability, knapping advantages of alluvial flint or occupation duration. The site of Payre is located in a flint rich circulation corridor and the movement of groups or exchanges between groups were organized along a north-south axis on the plateaus or towards the east following the river. The ridges were widely used as they are rich in flint, whereas the Rhône Valley is not an important source of lithic raw materials. Compared to other western European Middle Palaeolithic sites, these results indicate that procurement strategies have a moderate link with occupation types and duration, and with lithic technology. The Sr isotope ratios broadly match the proposed foraging areas, with the Rhône Valley being predominantly used in unit G and the ridges and limestone plateaus in unit F. While lithic reconstructions and childhood foraging are not directly related this suggests that the three analysed Neanderthals spend their childhood in the same general area and supports the idea of mobile Neanderthals in the Rhône Valley and neighbouring higher elevation plateaus. The combination of reconstructing lithic raw material sources, provisioning strategies, and strontium isotope analyses provides new details on how Neanderthals at Payre practised land use and mobility in the Early Middle Palaeolithic.

Elemental records in teeth reveal prehistoric seasons of Neanderthal birth, weaning, childhood illness, and neurotoxic exposures., Scholars endeavor to understand the relationship between human evolution and climate change. This is particularly germane for Neanderthals, who survived extreme Eurasian environmental variation and glaciations, mysteriously going extinct during a cool interglacial stage. Here, we integrate weekly records of climate, tooth growth, and metal exposure in two Neanderthals and one modern human from southeastern France. The Neanderthals inhabited cooler and more seasonal periods than the modern human, evincing childhood developmental stress during wintertime. In one instance, this stress may have included skeletal mobilization of elemental stores and weight loss; this individual was born in the spring and appears to have weaned 2.5 years later. Both Neanderthals were exposed to lead at least twice during the deep winter and/or early spring. This multidisciplinary approach elucidates direct relationships between ancient environments and hominin paleobiology.