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So, if we measure the rate of beta decay in an organic sample, we can measure how old the sample is.
The decay rate of radioactive elements is described in terms of half-life.
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Radiocarbon doesn’t work well on objects much older than twenty thousand years for such objects have small amounts of C-14 left in them.
But no one actually knows the starting point conditions when things began to form to figure out its age. Stipp, “Excess Radiogenic Argon in Young Subaerial Basalts From Auckland Volcanic Field, New Zealand,” 33 (1969): 1485-1520). Carbon-14 is mostly used to date once-living things (organic material).Living organisms are continually integrating C-14 into their bodies from the cosmic rays in the atmosphere along with other carbon Isotopes.The half-life of an atom is the amount of time it takes for half of the atoms in a sample to decay.The half-life of C, it can only give dates in the thousands-of-year range and not millions.