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    Describe process carbon dating

    He first noted that the cells of all living things contain atoms taken in from the organism's environment, including carbon; all organic compounds contain carbon.

    Most carbon consists of the isotopes carbon 12 and carbon 13, which are very stable.

    This is how carbon dating works: Carbon is a naturally abundant element found in the atmosphere, in the earth, in the oceans, and in every living creature.

    C-12 is by far the most common isotope, while only about one in a trillion carbon atoms is C-14.

    Isotopes of a particular element have the same number of protons in their nucleus, but different numbers of neutrons.

    This means that although they are very similar chemically, they have different masses.

    It takes another 5,730 for half of the remainder to decay, and then another 5,730 for half of what's left then to decay and so on.

    This procedure of radiocarbon dating has been widely adopted and is considered accurate enough for practical use to study remains up to 50,000 years old.

    Because atmospheric carbon 14 arises at about the same rate that the atom decays, Earth's levels of carbon 14 have remained fairly constant.

    Once an organism is dead, however, no new carbon is actively absorbed by its tissues, and its carbon 14 gradually decays.

    C-14 is produced in the upper atmosphere when nitrogen-14 (N-14) is altered through the effects of cosmic radiation bombardment (a proton is displaced by a neutron effectively changing the nitrogen atom into a carbon isotope).

    The new isotope is called "radiocarbon" because it is radioactive, though it is not dangerous.

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