How did the buildup of oxygen lead to the formation of the ozone layer?

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The formation of the ozone layer was a critical development in Earth's history, facilitated by the rise of atmospheric oxygen.

The process began approximately two billion years ago as oxygen levels in the atmosphere increased, largely due to the activity of photosynthetic organisms. As these oxygen molecules (O2) accumulated in the upper atmosphere, they were subjected to high-energy solar photons.12

This interaction triggers a process called photodissociation, where the solar radiation breaks the chemical bonds of the O2 molecules, releasing single oxygen atoms. These highly reactive atoms then collide and bond with intact oxygen molecules to form ozone (O3).1

The resulting buildup of ozone created a protective layer in the stratosphere that screens out lethal levels of UVB radiation. This shielding effect was essential for the evolution of life, as it allowed marine organisms to safely migrate from the oceans and colonize land.12