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Radiocarbon dating involves determining the age of an ancient fossil or specimen by measuring its carbon-14 content. After death the amount of carbon-14 in the organic specimen decreases very regularly as the molecules decay.
The researchers have developed the first direct method for dating pottery by examining animal fats preserved inside the ceramic walls. Archaeologists have long-dated sites by the visual appearance of pottery fragments found around the site. Ceramics, however, have a long and stable lifespan.
For radiocarbon dating to be possible, the material must once have been part of a living organism. This means that things like stone, metal and pottery cannot usually be directly dated by this means unless there is some organic material embedded or left as a residue.
Until this century, relative dating was the only technique for identifying the age of a truly ancient object. By examining the object's relation to layers of deposits in the area, and by comparing the object to others found at the site, archaeologists can estimate when the object arrived at the site.
Today's knowledge of fossil ages comes primarily from radiometric dating, also known as radioactive dating. Radiometric dating relies on the properties of isotopes. These are chemical elements, like carbon or uranium, that are identical except for one key feature -- the number of neutrons in their nucleus.
As a rule, carbon dates are younger than calendar dates: a bone carbon-dated to 10,000 years is around 11,000 years old, and 20,000 carbon years roughly equates to 24,000 calendar years. The problem, says Brock Ramsey, is that tree rings provide a direct record that only goes as far back as about 14,000 years.
Scientists combine several well-tested techniques to find out the ages of fossils. The most important are Relative Dating, in which fossils and layers of rock are placed in order from older to younger, and Radiometric Dating, which allows the actual ages of certain types of rock to be calculated.
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