The phenomenon of formation of prebiological compounds in volcanic processes.

Organic matter has been found in the juvenile ash of seven volcanoes in Kamchatka, the Kurile Islands and Indonesia. Its amount in one eruption is of the order of 1 00 000 tons. This matter constitutes a multicomponent mixture (more than 150 components) of, mainly, high boiling (b.p. over 250 degrees C) organic compounds of a complex structure. These are represented by hydrocarbons of saturated and aromatic nature, and, among them, polycyclic hydrocarbons, amino acids, amino sugars and other heteroatomic molecules, also containing N, O, S and C1. The formation of the above mentioned organic compounds is associated with volcanic processes--with abiogenous synthesis taking place in ash-gas clouds and, possibly, in the entrails of the Earth (hydrocarbons and their heteroatomic derivatives have also been found in volcanic bombs). On the strength of these facts, volcanic phenomena are regarded as the process which serves as the starting point of the chemical evolution from the inanimate to the animate matter.