Before crusteacean invertibrates radiated from one organism residing in the era of the proteriozoic period, as the phylogenetic tree theory states. It is widely predicted that the vulnerable troposphere of the Ediacaran era with an irregular crust morphology was the result of layering the earth surface with silica and magnetite, small air layers of cooling pockets consisting of the carbon dioxide and inorganic mineral composite items of tourmaline, gneiss material and the formation of a particular organic substance of carbon spheres that are thought to be residual airbourne materials of methane and carbon dioxide. The way tourmaline is deposited is from the very same way iron, berylium and manganese came to the surface as igneus movement. Of course the layering of certain chemicals is quite vast with the formation of sandstone and carbon spheres created spontaneously from on-earth eruptions of primarily condensed oxides.