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c. Radiocarbon. 2001. The Encyclopedia of World History |
 | | Developed by Willard F. Libby of the University of Chicago, radiocarbon dating is based on the fact that carbon isotope carbon-14 enters the carbon dioxide of the atmosphere with carbon-12, ordinary carbon (c). |
 | | As soon as an organism dies, no further radiocarbon is incorporated into it and the carbon-14 left therein disintegrates at a known rate, only half remaining after 5,730 years. |
 | | The C-14 atoms in radiocarbon samples taken from tiny samples of bone, charcoal, shell, wood, and other organic substances found in archaeological sites are counted by accelerator mass spectrometry, resulting in age determinations that are statistical approximations of the date of the sample. |
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