Age Determination of Fossil Bones from the Vindija Neanderthal Site in Croatia
Issue Date
2001-01-01Keywords
CarnivoraFissipeda
Homo sapiens neanderthalensis
Ursidae
Ursus
Vindija Cave
Hominidae
Homo
Homo sapiens
Primates
amino acids
racemization
Th U
anthropology
cave environment
Theria
Eutheria
terrestrial environment
Croatia
organic acids
Southern Europe
Mammalia
archaeological sites
biostratigraphy
Chordata
Tetrapoda
Vertebrata
biochemistry
Pleistocene
upper Pleistocene
organic compounds
Europe
bones
Cenozoic
charcoal
Quaternary
C 14
carbon
dates
isotopes
radioactive isotopes
absolute age
Metadata
Show full item recordCitation
Wild, E. M., Paunovic, M., Rabeder, G., Steffan, I., & Steier, P. (2001). Age determination of fossil bones from the Vindija Neanderthal site in Croatia. Radiocarbon, 43(2B), 1021-1028.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
Vindija cave in Croatia is famous for the Neanderthal bones found in layer G of its sediment profile. Radiocarbon dating has been performed mainly on this layer due to the great interest in its fossils. In addition to Neanderthal remains, the sediment in layer G contains bones from the cave bear. Cave bear bones are found also in other layers of the sediment profile and offer the possibility of studying the bears' evolutionary mode. Therefore, we tried to determine the time span covered by the entire profile. The U/Th age determination method was applied to cave bear bones from different layers of the profile. For the younger part of the profile, the U/Th ages were compared with the results of the 14C and the amino-acid racemization method. The agreement of the different methods indicates that closed-system behavior can be assumed for the fossil bones from Vindija cave. From this finding it may be deduced that bones from the lower sediment layers are also closed systems and that the U/Th ages of these layers are reliable. This conclusion is corroborated by the stratigraphy of the cave profile.Type
Proceedingstext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200041680