Terraformation from Geotechnica by Ladd Allen Doane

The Terraforming of Earth - A Raelian Hypothesis By Marcel Terrusse Up until the mid-sixties the majority of geochemists considered the current atmosphere as the final product of the degassing of the chemical elements forming the Earth's crust. They were convinced that reactions through non-biological processes had determined its current state. Oxygen, for instance, was merely supposed to be the product of the breakdown of water vapor molecules coupled with the release of hydrogen in the environment, resulting in an excess of free oxygen. It was thought that living beings simply “borrowed” gases from the atmosphere and returned them unmodified. However, the atmosphere’s composition deviates considerably from the chemical equilibrium of the steady-state. Almost everything seems to violate the rules of chemical equilibrium. In fact, the atmosphere’s composition is such a curious and incompatible mixture that it could not have formed or persisted by chance.

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