Biogeochemistry
Carbon dating is a scientific method used to determine the age of an artifact or organic material by measuring the amount of carbon-14 it contains. This technique relies on the principle that living organisms absorb carbon from their environment, including a small amount of the radioactive isotope carbon-14. After death, the carbon-14 begins to decay at a known rate, allowing scientists to estimate the time elapsed since the organism's death, making it a crucial tool in biogeochemical studies for understanding past environmental conditions and changes.
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