Abstract
Spectrum decomposition of the angular measurements of fossil tooth enamel fragments using an automated simulated annealing (SA) procedure shows that the mix CO2- radicals generated by laboratory irradiation is significantly different to that of the natural sample. The naturally irradiated sample contains about 10% of non-oriented CO2- radicals and a mix of 35:65 orthorhombic to axial CO2- radicals. In contrast, laboratory irradiation generated about 40% of non-oriented radicals and a large amount of orthorhombic CO2- radicals, while we failed to detect any axial CO2- radicals. The results indicate that geological aging of the sample incurs various annealing and transfer processes; their precise nature is yet unknown. Nevertheless, the understanding of the formation and transfer processes that leads to the observed mix of CO2- radicals in fossil tooth enamel is essential for the reliable application of ESR dating.
Original language | English |
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Pages (from-to) | 1798-1808 |
Number of pages | 11 |
Journal | Applied Radiation and Isotopes |
Volume | 68 |
Issue number | 9 |
DOIs | |
Publication status | Published - Sept 2010 |