This paper reviews the, so far available, paleorecords of Vitis sylvestris C.C. Gmel and Vitis vinifera L. from Romania. The study takes into consideration the presence of Vitis pollen from Holocene peat sediment sequences and archaeological context, but also the presence of macrorests from various archaeological sites that date from Neolithic, Chalcolithic, Bronze Age, and La Tène. Both paleobotanical arguments and archaeological discoveries support the theory that places the beggining of viticulture in Romania a few millenia ago, in Neolithic period. Also, written evidences (works of classical authors, epigraphical sources) confirm, indirectly, the presence of grapevine in La Tène period. Occurrences of Vitis vinifera and those of Vitis sylvestris manifest independently of the climate oscillations, being present both through colder and more humid episodes, as well as through drier and warmer events. Probably prehistoric communities have made a constant and deliberate effort, all along the Holocene, to maintain grapevine crops.
Recent excavations at Taraschina, south-eastern Romania, have revealed an extensive Chalcolithic settlement in the heart of the Danube Delta. Based on ceramic data, Taraschina was attributed to the Gumelniţa Culture and dated to the mid 5th millennium BC by radiocarbon dating. Phytolith analysis was conducted at Taraschina in order to reconstruct some activities carried out by the Chalcolithic populations in the Danube Delta. The study was undertaken on the site sediments, as well as on additional deposits sampled around the site by coring. The results show that phytoliths characterizing cereal processing are attested in archaeological deposits, as well as in the surrounding sequence. Our study highlights an important signal of cereal processing in the heart of the Danube Delta, 6000 years ago.
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.
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