RadiocarbonDatierung

RadiocarbonDatierung, also known as carbon-14 dating, is a scientific method used to determine the age of organic materials. It relies on the decay of carbon-14, a radioactive isotope of carbon. Living organisms absorb carbon from their environment, including small amounts of carbon-14. Once an organism dies, it no longer absorbs carbon, and the carbon-14 within its tissues begins to decay at a predictable rate. This rate is measured by its half-life, which is approximately 5,730 years. By measuring the remaining amount of carbon-14 in a sample and comparing it to the amount of stable carbon isotopes, scientists can calculate how long ago the organism died. This technique is effective for dating materials up to around 50,000 years old. Radiocarbon dating has been instrumental in various fields, including archaeology, paleontology, and geology, providing crucial insights into past events and the timeline of life on Earth. Calibration curves are used to refine the dates obtained, accounting for variations in atmospheric carbon-14 levels over time.