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The most useful method for dating the remains of plants and animals that lived within the last 50,000 years is radiocarbon dating (carbon-14 dating). This technique measures the decay of carbon-14 isotopes in organic materials, allowing scientists to determine the age of samples up to about 50,000 years old. It is widely used in Archaeology and Paleontology to date organic remains, such as bones and wood, providing valuable insights into past environments and ecosystems.

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