A window on the past: how carbon dating works

1

Cosmic rays batter the upper atmosphere and send cascades of neutrons through the air

Neutrons

Nitrogen

2

These strike atoms of nitrogen, the main component of Earth’s atmosphere, and transform some of them into carbon-14

Two extra

neutrons

Carbon-14

Has six protons and eight neutrons in its nucleus, which makes it unstable, so that it decays radioactively into an atom of nitrogen. Most of the carbon in our bodies and the world has six protons and six neutrons

3

Carbon-14 atoms combine with oxygen to create radioactive carbon dioxide that is absorbed by plants, which are then eaten by animals

4

When an organism dies, it stops absorbing carbon-14 and its existing store slowly decays

5

By measuring its radioactivity, its carbon-14 content can be estimated and the date of its time of death can be measured

1

Cosmic rays batter the upper atmosphere and send cascades of neutrons through the air

Carbon-14

Has six protons and eight neutrons in its nucleus, which makes it unstable, so that it decays radioactively into an atom of nitrogen. Most of the carbon in our bodies and the world has six protons and six neutrons

Neutrons

Nitrogen

Two extra

neutrons

2

These strike atoms of nitrogen, the main component of Earth’s atmosphere, and transform some of them into carbon-14

3

Carbon-14 atoms combine with oxygen to create radioactive carbon dioxide that is absorbed by plants, which are then eaten by animals

4

When an organism dies, it stops absorbing carbon-14 and its existing store slowly decays

5

By measuring its radioactivity, its carbon-14 content can be estimated and the date of its time of death can be measured