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After the death of an organism, C-14 decays to N-14. The rate, as for all radioactive decay, is related to the amount of C-14 present at any given time. In principle, any material that still has a sufficient amount of C-14 can be dated, with the date representing the time since the material stopped exchanging carbon with the atmosphere. The illustration below demonstrates how the amount of radioactive C-14 decreases with time. Mouse click the numbers on the slider. Each number is one half-life different in time than the preceding or following one. The daughter product, N-14, is not retained by a specimen because it is a gas and escapes as it forms. |
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