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By knowing how much carbon 14 is left in a sample, the age of the organism when it died can be known.
Archaeology and other human sciences use radiocarbon dating to prove or disprove theories.
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.
The impact of the radiocarbon dating technique on modern man has made it one of the most significant discoveries of the 20th century.
Standard errors are also reported in a radiocarbon dating result, hence the “±” values.
These values have been derived through statistical means.
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American Chemical Society National Historic Chemical Landmarks.