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I'd look up the wikipedia first. But here's a short answer.

Carbon-14 is naturally found in the atmosphere in the form of heavy CO2. The reason for this has to do with neutron flux from the sun hitting nitrogen in the upper atmosphere - whatever. The concentration of heavy CO2 in the atmosphere is relatively stable.

When a plant is alive, it takes up CO2 from the atmosphere and inevitably gets some heavy CO2 as well, and so it incorporates that C14 into its biomass. The concentration of C14 in the plant, as it is alive, stays in equilibrium with the concentration of C14 in the atmosphere.

But when the plant dies, it stops respirating, and it stops taking CO2 in from the atmosphere. The C14 it does have in it continues to decompose according to a very predictable exponential decay rule. So ~14,000years after the plant dies, about half of its C14 has decayed.

So you're a paleontologist 14,000 years from now, and you see a fossilized plant. You measure the amount of C14 in the plant, and you find that its concentration is about half the atmospheric level. Therefor you assume the plant died about 14,000 years earlier.

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16y ago

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