Paleontology
Carbon dating is a scientific method used to determine the age of an organic material by measuring the amount of carbon-14 it contains. This technique relies on the principle of radioactive decay, where carbon-14, a radioactive isotope of carbon, decays over time at a known rate. By comparing the ratio of carbon-14 to stable carbon isotopes in a sample, scientists can estimate the time since the organism died, which is crucial for understanding the timeline of early life forms.
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