There are three stages in the evolution of
the present atmosphere.
- The first stage is marked by the loss of primordial atmosphere.
- In the second stage, the hot interior of the earth contributed to the evolution of the atmosphere.
- During the cooling of the earth, gases and water vapour were released from the interior solid earth.
- This started the evolution of the present atmosphere.
- The early atmosphere largely contained water vapour, nitrogen, carbon dioxide, methane, ammonia and very little of free oxygen.
- The process through which the gases were outpoured from the interior is called degassing.
- Continuous volcanic eruptions contributed water vapour and gases to the atmosphere.
- As the earth cooled, the water vapour released started getting condensed.
- The carbon dioxide in the atmosphere got dissolved in rainwater and the temperature further decreased causing more condensation and more rains.
- The rainwater falling onto the surface got collected in the depressions to give rise to oceans.
- The earth’s oceans were formed within 500 million years from the formation of the earth.
- Finally, the composition of the atmosphere was modified by the living world through the process of photosynthesis.
- around 2,500-3,000 million years before the present, the process of photosynthesis got evolved.
- Life was confined to the oceans for a long time. Oceans began to have the contribution of oxygen through the process of photosynthesis.
- Eventually, oceans were saturated with oxygen, and 2,000 million years ago, oxygen began to flood the atmosphere.
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