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Radio carbon dating is done by estimating in specimen the
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Ratio of amount of still present
Radiocarbon dating relies on a simple natural phenomenon. As the earth's upper is bombarded by cosmic radiation, atmospheric nitrogen is broken down into an unstable isotope of carbon-carbon (C-14).
The unstable isotope is brought to earth by atmospheric activity, such as storms, and becomes fixed in the biosphere. Because it reacts identically to C-12 and C-13, C-14 attached to complex organic molecules through photosynthesis in plants and becomes their molecular makeup. Animals eating those plants in turn absorb carbon as well as stable isotopes. This process of ingesting continues as long as the plant or animal remains alive.
The within an organism is continually decaying into stable carbon isotopes, but organism is absorbing more during its life, the ratio of to remains about same as the ratio in the atmosphere. Where the organism dies, the ratio of C-14 within its carcass begins to gradually decrease.
The unstable isotope is brought to earth by atmospheric activity, such as storms, and becomes fixed in the biosphere. Because it reacts identically to C-12 and C-13, C-14 attached to complex organic molecules through photosynthesis in plants and becomes their molecular makeup. Animals eating those plants in turn absorb carbon as well as stable isotopes. This process of ingesting continues as long as the plant or animal remains alive.
The within an organism is continually decaying into stable carbon isotopes, but organism is absorbing more during its life, the ratio of to remains about same as the ratio in the atmosphere. Where the organism dies, the ratio of C-14 within its carcass begins to gradually decrease.
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