Radiocarbon dating, also known as carbon-14 dating, is a method used by scientists to determine the age of carbonaceous materials up to about 60,000 years old. This technique is widely used in paleontology, archaeology, and geoscience to date once-living materials.
The principle behind radiocarbon dating is quite simple. Living organisms absorb a constant ratio of carbon isotopes, including the radioactive isotope carbon-14, from the atmosphere. When an organism dies, it stops absorbing carbon-14, and the isotope begins to decay at a known rate, known as its half-life. By measuring the remaining levels of carbon-14 in a sample, scientists can estimate when the organism died.
Radiocarbon dating is particularly useful for dating fossils of plants and animals that lived up to 60,000 years ago. This method has revolutionized our understanding of the timeline of historical and prehistorical events, including the ages of archaeological finds and the timing of ice ages.
Technological advancements have improved the accuracy and scope of radiocarbon dating. Accelerator mass spectrometry (AMS) dating is a modern method that allows for the dating of extremely small samples with more precision, extending the capabilities of radiocarbon dating.
Carbon Isotope Analysis, Half-Life of Carbon-14, Paleontology Dating Methods, Archaeological Dating, Geological Time Measurements, Accelerator Mass Spectrometry (AMS), Carbonaceous Fossil Examination.
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