How do scientists use carbon-14 to date formerly living material?

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Scientists use carbon-14 dating to determine the age of organic materials by measuring the decay of the radioactive isotope carbon-14.12

Carbon-14 is continuously produced in the atmosphere by cosmic rays and enters the carbon cycle, where it is absorbed by plants and subsequently consumed by animals. While an organism is alive, it maintains a stable ratio of carbon-14 to stable carbon isotopes because it is constantly replenishing its supply through food and air.132

Upon death, an organism ceases to intake carbon, and the carbon-14 in its tissues begins to decrease at a constant rate due to radioactive decay, with a half-life of 5,730 ± 40 years. By using an accelerator mass spectrometer to measure the remaining proportion of carbon-14, scientists can estimate how long ago the organism died. Because atmospheric carbon-14 levels have fluctuated over time, researchers often calibrate these raw dates using data from sources like dendrochronology to improve accuracy.1324