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Ozone is made in all parts of the atmosphere. It is at its highest concentration in the lower part of the stratosphere. Below the "ozone layer", UV-B intensity is greatly diminished, which will decrease the available energy for certain ionizations of gases. The ozone layer is able to couple radiatively in the infrared, so it can tap heat energy of oxygen and nitrogen. The atmosphere doesn't really care what sort of gases it contains. So it is really hard to arrive at some sort of "effect" that would be interesting / significant...

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The ozone layer that filters ultraviolet radiation originated from


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