The technique is based on comparing the levels of <SUP>14</SUP>C and <SUP>12</SUP>C isotopes in the sample. When the sample was living, the ratio of <SUP>14</SUP>C to <SUP>12</SUP>C in the material is the same as in the atmosphere. But after death the <SUP>14</SUP>C isotope decays into N-14, while <SUP>12</SUP>C does not. The loss in <SUP>14</SUP>C is then used to estimate how long ago the sample died, which is typically the same as how long the sample existed. | The technique is based on comparing the levels of <SUP>14</SUP>C and <SUP>12</SUP>C isotopes in the sample. When the sample was living, the ratio of <SUP>14</SUP>C to <SUP>12</SUP>C in the material is the same as in the atmosphere. But after death the <SUP>14</SUP>C isotope decays into N-14, while <SUP>12</SUP>C does not. The loss in <SUP>14</SUP>C is then used to estimate how long ago the sample died, which is typically the same as how long the sample existed. |