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After a living organism dies, it stops taking in carbon-14, which is a radioactive isotope of carbon found in the atmosphere. The carbon-14 that was present in its tissues begins to decay at a known rate, with a half-life of about 5,730 years. As time passes, the levels of carbon-14 in the organism decrease, allowing scientists to estimate the time since death through radiocarbon dating. This process provides valuable information about the age of archaeological and geological samples.

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