1. Living organisms accumulate carbon-14, a radioactive isotope, along with stable carbon-12
2. After the organism dies, no more carbon-12 or carbon-14 is added
3. Carbon-14 decays at a constant rate, leaving the organism as nitrogen
4. During any 5730-year period, the amount of carbon-14 in the organism divides in half
5. By determining the amount of carbon-14 in a fossil, scientists can estimate when the organism lived