Dans ce travail, l’évolution de la zone interne du delta du Danube est appréhendée à partir de travaux géoarchéologiques et géomorphologiques réalisés dans le district de Mila 23, suite à la découverte de la plus vieille occupation humaine (énéolithique/chalcolithique) du delta dans les années 90. Les travaux sur site et hors site ont permis de préciser les stades précoces de l’évolution du delta entre 5 600 et 4 000 ans cal. av. J.-C. Celui-ci évolue comme un delta lagunaire en eau douce, s’épandant dans un large lagon séparé de la mer par la ride de Letea-Caraorman. La remontée rapide du niveau lagunaire, sous l’effet de la remontée eustatique et peut-être d’une surcote liée à un événement humide, ont conduit à une submersion partielle du site et probablement à son abandon vers 4 450 ans cal. av. J.-C.

The article presents the palaeobotanical investigations of a remarkable discovery from the Early Chalcolithic settlement of Isaiia–Balta Popii (Romania), a multi-layered site. The excavation of a dwelling brought to light a rather rare finding, meaning a medium sized ceramic vessel having deposited inside two objects of burnt clay: an anthropomorphic figurine depicting pregnancy attributes and a small cone. Given the special character of the deposition, several samples from the vessel and near it were collected for phytolith analysis. Our results highlighted a ritual plant deposition: Elongate dendritic and Blocky morphotypes suggest that cereals and probably Artemisia seem to have been used for this purpose. These plants are known, aside from their practical uses, as powerful symbols, used through the ages in magic practices. All of these facts are strong arguments to interpret this find as a result of a ritual related to fertility involving both feminine and masculine symbols and plant use.

Early Neolithic communities penetrated in southwestern Transylvania and were established in the Mureș Valley where they found suitable territories for domestic animal herds and probably plant cultivation. The present study tries to answer questions related to the beginnings of the neolithisation in this area, from an interdisciplinary perspective, valuing archeozoologically and archeobotanically the Starčevo-Criș site of Soimuș-Teleghi (Hunedoara County), dating to the 7th–6th millennium BC. Animal skeletal remains and phytoliths are the proxies analysed in this paper, offering data about the palaeoeconomy and palaeoenvironment of the Early Neolithic settlement. In the archaeozoological samples, the remains coming from domestic mammals are the most frequent, being identified as cattle (Bos taurus), sheep/goat (Ovis aries/Capra hircus), pig (Sus domesticus), and dog (Canis familiaris). The fact that pig remains are almost absent in the samples is significant, suggesting a mobility of the evaluated communities. The skeletal remains of wild mammal species are rare, belonging to red deer (Cervus elaphus), roe deer (Capreolus capreolus), aurochs (Bos primigenius), wild boar (Sus scrofa), and polecat (Mustela putorius). The strong dominance of grasses is attested through the phytoliths’ assemblages. ELONGATE DENDRITIC phytoliths are well represented. This morphotype, which originates from the inflorescence or the husk of Poaceae, is most likely derived from cultivated plants (cereals such as wheat, barley, etc.). Archaeozoological and archaeobotanical data resulting from this study suggest an open environment around the Early Neolithic settlement, where communities of the Starčevo-Criș culture mainly raised herds of cattle and sheep/goat. Sporadically, hunting and gathering molluscs were practised by the inhabitants, as indicated by archaeozoological results.

Situated in the northern part of Dobrogea which belonged to Scythia Minor province, Ibida was the largest fortification in this region during Roman-Byzantine times, between the 4th and 6th centuries. This study investigates the usefulness of multidisciplinary analysis on the territory of Ibida fortress by integrating faunal data and phytolith records in relation to soil characteristics to understand past human–environmental interactions. One of the four soil profiles excavated within the fortress territory was sampled for phytolith analysis indicated the domination of grasses. The habitation phase corresponding to the Roman-Byzantine period was identified at 1.65 m depth on the Slava Rusă floodplain. This was the richest level in artefacts and elongate dendritic phytoliths, also suggesting an important accumulation of grass spikelets in the cultural layer. This could be explained either by the presence of cereals in the dwelling level or by the presence of non-cereal grasses used for animal fodder. The faunal remains were collected from various archaeological contexts (i.e. intramuros, wall and extramuros). The identification of numerous cattle and sheep/goat remains and the soil characteristics more likely suggest a pastoral use of the land from fortress proximity, where the cultivation of cereals seems to play a less important role.

The paper analyzes the archaeobotanical and archaeozoological remains originating from the middle Holocene (i.e. Chalcolithic site of Poduri-Dealul Ghindaru, in Eastern Romania, Bacău County). Poduri-Dealul Ghindaru site is the only tell settlement known in the area of existence of the Cucuteni culture, with inhabitation levels from Neolithic to the Bronze Age. In order to better understand the diet components of the prehistoric inhabitation belonging to the Cucuteni A and Cucuteni B phases, we follow evidence from archaeozoology, carpology, and palynology. For the carpological taxa, we calculate their ubiquity, diversity, and edibility score. The two sets of taxa are then compared in their similarity. Palynological data record the presence of cereal grains in all samples. We present the archaeozoological taxa with their quantification values and we calculate for the Cucuteni A and B phases, and in comparison with the Bronze Age sample, their richness, Shannon–Weaver diversity index and equitability. A correspondence analysis is carried out in order to compare the exploitation strategies for the three assemblages. For the archaeobotanical data, we find that the Cucuteni A phase is dominated by anthropogenic activity indicators and a heavy reliance on cereals. The Cucuteni B phase seems to be characterized by a restriction of human activity. The archaeozoological data highlight a preference for large mammals (cattle, dear, boar) during Cucuteni A and BA and smaller mammals during Cucuteni B (sheep/goat, pig, hare). We conclude that although the subsistence strategies remain similar, the dietary components change during the Cucuteni A and B phases, probably in response to environmental changes.