The system through which an atmosphere can renew itself is called ecological succession.
Ecological succession is the system through which the shape of an organic network evolves over time. Two distinct kinds of succession—number primary and number secondary—have been distinguished.
Primary succession happens in basically useless regions areas wherein the soil is incapable of maintaining existence due to such elements as lava flows, newly shaped sand dunes, or rocks left from a retreating glacier.
Secondary succession happens in regions in which a network that formerly existed has been removed; it's typified by smaller-scale disturbances that don't get rid of all existence and vitamins from the environment.
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