Majority

The majority is a mineral found in the terrestrial coat of empirical formula Mg3 (Fe, Al, If) 2 (SiO4) 3.

Under conditions of Pressure and high Temperature, this mineral binds to the oxygen and acts like a sponge and tank of gas essential to the animal life. When the temperature and the pressure decrease, which occurs when the majority is moved by Convection towards the Earth's crust, oxygen is released in the atmosphere, thus taking part in the regulation of the quantity of this gas in the Atmosphère. Studies going back to 2007 suggest that the quantity of oxygen thus controlled by the majority much more important than is initially thought.

References and sources

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