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An age could be estimated by measuring the amount of carbon-14 present in the sample and comparing this against an internationally used reference standard.
Plants and animals assimilate carbon 14 from carbon dioxide throughout their lifetimes.
When they die, they stop exchanging carbon with the biosphere and their carbon 14 content then starts to decrease at a rate determined by the law of radioactive decay.
Version was 3.10 which was a Windows standalone program; this is still available above but will not be further developed.
The current version is 4.3 and works with Int Cal13. A variety of different chronological models can be included in the analysis.
The information for such analysis can be entered using the user interface or in the form of text command files. The Int Cal13 and Marine13 data files are bundled with Ox Cal (with the kind permission of the compilers).
Radiocarbon dating is essentially a method designed to measure residual radioactivity.
By knowing how much carbon 14 is left in a sample, the age of the organism when it died can be known.