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2009, Science
A unique finding of wild flax fibers from a series of Upper Paleolithic layers at Dzudzuana Cave, located in the foothills of the Caucasus, Georgia, indicates that prehistoric hunter-gatherers were making cords for hafting stone tools, weaving baskets, or sewing garments. ...
Science, 2009
Citation Kvavadze, Eliso, Ofer Bar-Yosef, Anna Belfer-Cohen, Elisabetta Boaretto, Nino Jakeli, Zinovi Matskevich, and Tengiz Meshveliani. 2009. 30,000 Years old wild flax fibers - Testimony for fabricating prehistoric linen. Science 325(5946): 1359.
UISPP — Liège, 2012
In our article we deal with three Upper Paleolithic cave sites, which are located in Upper Imereti region just in few km from each other (2-6 km). These are already well-known sites-Ortvala Klde, Dzudzuana Cave and newly discovered Bondi Cave. The landscapes, where these caves are situated, are the similar. All of them are located in parallel gorges. The distance between the gorges is 4-8 km. According to pollen analysis and obtained dating, the environment around these caves was the similar. The inhabitants of Dzudzuana and Bondi caves were hunting mostly on bisons and equses. At the same time the Neanderthals and the Modern humans of Ortvala Klde traditionally were extracting the Capra caucasuica (95 %). The industry of Bondi and Dzudzuana caves is more or less similar but there are differences as well-the microliths are dominated in the material of Dzudzuana. The blade and bladelet oriented technology are represented in both sites. The blade technology is represented in Ortvala Klde as well, but there are some orignacian features which are better represented in this cave than in other above-mentioned sites. Coexistence of Aurignacian and Gravettian features is one of the characters of Upper Paleolithic of Western Georgia. In Bondi and Dzudzuana caves there were discovered the most ancient flax and colored fibers dated from 35000-34000. Perhaps the differences between those contemporary sites can be explained by different economical activities of different groups, or by distribution of the habitat areas between them. Thème I ASIE
The late Pleistocene expansion of anatomically modern humans (AMHs) into Eurasia and the concurrent demise of the Neanderthals appears to be a complex and regionally variable process. The southern Caucasus region, with its rich cave-sites, has recently provided important results regarding this process. In this paper we report on the results of fieldwork in Bondi Cave, Western Georgia, providing a new radiocarbon chronology, stratigraphic observations, analyses of lithic technology and provenance, faunal and floral remains as well as paleoenvironmental data. The cave includes Middle Palaeolithic (ca, 45,000 ka cal. BP) cultural horizons and a long Upper Palaeolithic sequence (ca. 40,000e27,000 cal. BP from layer V to IV). A modern human tooth was found in layer Vb. We estimate its age at 39,000 e35,800 Cal BP (95.4%), based on the Bayesian age model we built. If the context of the tooth is reliable, as we think it is, this would make it the oldest morphologically modern human in the Caucasus. Upper Palaeolithic hunting of tur and bison, as well as the collection of various plants including flax is attested. Mobile Upper Palaeolithic foragers inhabited the cave in generally cold and dry periods, but a mosaic of environments, including forests and meadows, was nonetheless available to them. The archaeological sequence of Bondi and adjacent sites indicates a substantial time gap between the Middle and Upper Palaeolithic occupations, thus disproving Neanderthal-AMH interaction in this area and lending support to a replacement scenario in the southern Caucasus, assuming of course that the Early Upper Palaeolithic (EUP) is related to the arrival of AMHs.
Global cooling during the Last Glacial Maximum (LGM) posed significant challenges to peoples living in northern Eurasia. Using micromorphology, pollen and non-pollen palynomorphs (NPP), and faunal analyses , this study reconstructs the local paleoenvironmental contexts of repeated ephemeral occupations at Shizitan 29 in Shanxi Province, North China, across the LGM, from ca. 28 to 18 Ka cal BP, followed by a gap until a final occupation ca.13.5 Ka cal BP. Among the significant finds at Shizitan 29 are remains of 285 hearths and a rich lithic assemblage that contains the earliest radiocarbon-dated evidence for microblades in China, appearing first in Layer 7. The environmental data show that the low mountains and tributary river valleys of the Yellow River in the Loess Plateau provided abundant sources of water and food in spite of environmental fluctuations. Microblade-producing groups repeatedly visiting this locality survived severe climate change by making use of fire, selective herbivore hunting, processing plant foods with grinding stones, and symbolic ornamentation such as ostrich shell beads. NPP data also indicate the potential presence of flax and other fiber processing. The Shizitan 29 data demonstrate how humans adapted to challenging local conditions throughout the LGM, allowing them to stay within this northerly region without migrating to warmer southern latitudes.
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