In temperate latitudes sheep have a seasonal reproductive behaviour, which imposes strong constraints on husbandry in terms of work organization and availability of animal products. During the last 50 years, researchers have focused on understanding the mechanisms driving small ruminants' reproduction cycles and finding ways to control them. This characteristic is inherited from their wild ancestor. However, the history of its evolution over the 10 millennia that separates present day European sheep from their Near Eastern ancestors' remains to be written. This perspective echoes archaeologists' current attempts at reconstructing ancient pastoral societies' socio-economical organization. Information related to birth seasonality may be retrieved directly from archaeological sheep teeth. The methodology consists of reconstructing the seasonal cycle record in sheep molars, through sequential analysis of the stable oxygen isotope composition (δ 18 O) of enamel. Because the timing of tooth development is fixed within a species, inter-individual variability in this parameter reflects birth seasonality. A review of the data obtained from 10 European archaeological sites dated from the 6th to the 3rd millennia BC is provided. The results demonstrate a restricted breeding season for sheep: births occurred over a period of 3 to 4 months, from late winter to early summer at latitudes 43°N to 48°N, while a later onset was observed at a higher latitude (59°N). All conclusions concurred with currently held expectations based on present day sheep physiology, which, aside from the historical significance, contributes to the reinforcing of the methodological basis of the approach. Further study in this area will permit regional variability attributable to technical choices, within global schemes, to be fully reported.

During the course of the diffusion of Neolithic agropastoral societies across Europe, animal husbandry was adapted to local constraints and resources, involving changes in practices, as well as in animal physiology. As a result, the timing of animal breeding was impacted, with consequences on the organization of agro-pastoral tasks and the seasonal availability of animal productions. Past sheep birth seasonality can be investigated through the reconstruction of the seasonal cycle recorded in molars, based on the sequential analysis of stable oxygen isotope ratios (δ 18 O) in enamel. Modern sheep serve as comparative material to define the season of birth. In the present study, we provide new reference values for winter births in the sheep third molar (M3) using data from the modern Kemenez sheep herd. The dataset also includes paired upper and lower M3s in order to test the comparability of results obtained from both teeth. Results show a moderate shift in the isotopic record between upper and lower M3s. The consecutive difference in the assessment of the timing of birth is one month, on average. Additionally, we provide a new set of results for sheep from Nova Nadezhda (Bulgaria, early sixth millennium BC), combining upper and lower molars, in order to expand data relating to the earliest stages of the introduction of sheep to Europe. At Nova Nadezhda, sheep were born in late winter and spring, and the pattern of birth distribution does not indicate the control of sheep reproduction by separating males from females. When compared to previously published results at other Neolithic and Chalcolithic sites in the Balkans, corrected for the shift between upper and lower M3s, no latitudinal and chronological trend is observed between the Southern Balkans, Northern Balkans and Hungarian plains over the early sixth to the second half of the fifth millennia BC. This apparent uniformity for the length (3-4 months) and timing of the birth period could be challenged in the future by enlarged datasets.

Abstract

International audienceThe Molène archipelago appears to be particularly rich in Neolithic and Bronze Age remains and an exceptional concentration of megaliths has been brought to light. Several settlements are confirmed by dry-stone structures or by shell middens. These data give precious indications on the occupation chronology of the area. Moreover they allow us, for the first time in Brittany, to reconstruct everyday life during the late Prehistoric period.A prerequisite to this reconstruction was a better understanding of the evolution of the environment during this period, which locally implies a better knowledge of paleogeographic changes related to Holocene sea-level rise as well as on floral and faunal resources. The results obtained through paleogeographic reconstructions show that the archipelago since 4500 BC was already disconnected from the mainland. The megalithic monuments must therefore have been erected and used by islanders present on the archipelago from the middle of the 5th to the 2nd millennium BC. The distribution of the megalithic tombs reveals landscape occupation strategies which respond to both cultural choices and natural constraints. Throughout the entire period, geographic isolation has continued to increase, although it did not imply strong cultural specificities. Nevertheless, the increasing remoteness of the islands has fostered the search for livelihoods based on the intense exploitation of coastal resources. Despite their focus on the sea, these people did not neglect what inland areas could offer as evidenced by the early agro-pastoral practices in the archipelago

Évolution des paysages et occupation humaine en mer d'Iroise (Finistère, Bretagne) du Néolithique à l'Âge du Bronze Landscapes evolution and human settlement in the Iroise Sea (Finistère, Brittany, France) during Neolithic and Bronze Age