The Formation of Thermal Proteinoids in Hot Water

Ignat Ignatov, Oleg Mosin


It was demonstrated the formation of thermal proteinogenic microspheres in hot water at increasing the pH value. Proteinogenic microspheres doubled in hot water with increasing the pH up to 6.0. The hot alkaline mineral water with temperature from +65 0C to +95 0C and the pH value from 9 to 11 is more suitable for the origination of life and living matter than other analyzed water samples. In hot mineral waters the local maximums in IR-spectra are more manifested compared to the local maximums obtained in IR-spectra of the same water at a lower temperature. The difference in the local maximums from +20 0C to +95 0C at each +5 0C according to the Student t-criterion makes up p < 0,05.

Keywords: deuterium, hydrosphere, evolution, origin of life, condensation-dehydratation, IR-spectroscopy.

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