The (conventional) radiocarbon age of a sample is
where is the activity of the sample’s carbon and that of the reference standard; it uses the half-life of years (mean life years), normalises the activities for the isotopic fractionation of carbon (), and counts years before AD 1950 (BP, “before present”). A calibration curve gives the radiocarbon age of samples of known calendar age; read backwards, it converts a radiocarbon age into a range of calendar ages (cal BP).