Browsing Radiocarbon, Volume 51, Number 2 (2009) by Authors
Monks and Icon Painters from the Spaso-Andronikov Monastery, MoscowAlexandrovskaya, E. I.; Alexandrovskiy, A. L.; van der Plicht, J.; Kovalyukh, N. N.; Skripkin, V. V. (Department of Geosciences, The University of Arizona, 2009-01-01)In the Monastery of Our Saviour and St. Andronicus in Moscow, skeletal remains of clerics and of (possibly) famous icon painters were discovered. The bones were radiocarbon dated, nd concentrations of trace elements in bone tissues were measured. From tombs 1-4, the 14C dates obtained from human bones (likely monks) and from associated wood date to the 14th-15th centuries AD, as expected. Trace element concentrations indicate signs of fasting. Tomb 5 contained 2 burials; these could belong to the famous icon painters Rublev and Chernyi. Indeed, the bones show high concentrations of lead, zinc, and copper, which is typical for remains of artists and metallurgists. The 14C dates of the 2 skeletons, however, differ by 200 yr, and seem to be too old for Rublev and Chernyi. At this stage, it is not clear if the burials can be assigned to these painters.
The Spread of the Neolithic in the South East European Plain: Radiocarbon Chronology, Subsistence, and EnvironmentDolukhanov, Pavel M.; Shukurov, Anvar; Davison, Kate; Sarson, Graeme; Gerasimenko, Natalia P.; Pashkevich, Galina A.; Vybornov, Aleksandr A.; Kovalyukh, Vikolai N.; Skripkin, V. V.; Zaitseva, Ganna I.; et al. (Department of Geosciences, The University of Arizona, 2009-01-01)Newly available radiocarbon dates show the early signs of pottery-making in the North Caspian area, the Middle-Lower Volga, and the Lower Don at 8-7 kyr cal BC. Stable settlements, as indicated by "coeval subsamples," are recognized in the Middle-Lower Volga (Yelshanian) at 6.8 kyr cal BC and the Caspian Lowland at about 6 kyr cal BC. The ages of the Strumel-Gostyatin, Surskian, and Bug-Dniesterian sites are in the range of 6.6-4.5 kyr BC, overlapping with early farming entities (Starčevo-Krs-Criş and Linear Pottery), whose influence is perceptible in archaeological materials. Likewise, the 14C-dated pollen data show that the spread of early pottery-making coincided with increased precipitation throughout the forest-steppe area.