A Fresh Water Diet-Derived 14C Reservoir Effect at the Stone Age Sites in the Iron Gates Gorge
Issue Date
2001-01-01Keywords
Danube ValleyIron Gates Gorge
Romania
Schela Cladovei archaeological site
Ungulata
fresh water environment
Mesolithic
nitrogen
N 15 N 14
Neolithic
Stone Age
Hominidae
Homo
Primates
artifacts
diet
calibration
Theria
Eutheria
collagen
Southern Europe
Mammalia
archaeology
isotope ratios
Holocene
Chordata
Tetrapoda
Vertebrata
proteins
organic compounds
Europe
bones
Cenozoic
Quaternary
C 14
carbon
dates
isotopes
radioactive isotopes
stable isotopes
absolute age
geochemistry
Metadata
Show full item recordCitation
Cook, G. T., Bonsall, C., Hedges, R. E. M., McSweeney, K., Boronean, V., & Pettitt, P. B. (2001). A freshwater diet-derived 14C reservoir effect at the Stone Age sites in the Iron Gates gorge. Radiocarbon, 43(2A), 453-460.Journal
RadiocarbonDescription
From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.Additional Links
http://radiocarbon.webhost.uits.arizona.edu/Abstract
Human bones from single inhumation burials and artifacts made from terrestrial mammal (ungulate) bone found in direct association with the skeletons were obtained from the Stone Age site of Schela Cladovei situated just below the Iron Gates Gorge of the River Danube. The results of stable isotope analyses of the human bone collagen are consistent with a heavy dependence on aquatic protein while radiocarbon dating of the samples reveals an offset of 300-500 years between the two sample types, indicating a freshwater reservoir effect in the human bone samples. Since protein consumption is by far the major source of nitrogen in the human diet we have assumed a linear relationship between delta-15N and the level of aquatic protein in each individual's diet and derived a calibration for 14C age offset versus delta-15N which has been applied to a series of results from the site at Lepenski Vir within the gorge. The corrected 14C ages (7310-6720 BP) are now consistent with the previous 14C age measurements made on charcoal from related contexts (7360-6560 BP). In addition, the data indicate a change from a primarily aquatic to a mixed terrestrial/aquatic diet around 7100 BP and this may be argued as supporting a shift from Mesolithic to Neolithic. This study also has wider implications for the accurate dating of human bone samples when the possibility exists of an aquatic component in the dietary protein and strongly implies that delta-15N analysis should be undertaken routinely when dating human bones.Type
Proceedingstext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200038327