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The Atmosphere

History (continued).

The evolution of green plants and the presence of oxygen
in the atmosphere produced further changes.

Ammonia and methane would have reacted with oxygen
producing carbon dioxide and water (from methane)
and nitrogen and water from ammonia.
Ammonia would also have decomposed in the presence of
strong ultraviolet light from the sun, giving more nitrogen and hydrogen.

Nitrifying bacteria acted on ammonia to produce nitrates for plant growth,
and denitrifying bacteria added nitrogen to the atmosphere (nitrogen cycle).
The proportion of nitrogen in the atmosphere steadily increased.

The increase in oxygen and the presence of the ozone layer in
the atmosphere allowed new and more complex life forms to evolve.

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