Archaeologists utilize several methods to analyze data from the past. One scientific tool helps to analyze the radioactive decay of chemical elements found in plant and animal remains, pottery, and even rocks. Radiocarbon dating, also known as carbon-14 dating, has developed into one of the most important radioisotope dating methods archaeologists employ. This scientific tool, first developed by Willard F. Libby in the late 1940s, began with the discovery of the isotopic carbon-14 atom. Following this discovery, scientists began to ponder ways to utilize carbon-14 to date previously living organisms. Since scientists knew that living organisms absorb carbon-14 at a constant rate while alive, they started to formulate a process to measure C-14 to C-12 ratios in dead organisms. This procedure made it possible for scientists to age an organism using this carbon ratio. To ensure the formula was correct, they began to perform experimental trials of radiocarbon dating to test its accuracy, and while testing, discovered several methods of carbon 14 dating that yielded accurate results including the Geiger counting method, liquid scintillation method, and AMS dating method. These three methods have significantly improved the accuracy of assigning dates to past events and artifacts, dating as far back as 70,000 years. Using and describing the techniques, procedures, and applications, the anthropological school of thought for carbon-14 dating will be derived. Although this method has drawbacks and critics, carbon-14 dating has shaped and influenced the historical classification artifacts to the point that archaeologists, geologists, and anthropologists now have the ability to construct the world’s history by filling in some of the many blank dates in the chronology of the history of our human world and by substantiating and revising other dates.
The foundation of radiocarbon dating began with
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