ИСТИНА

We have repeatedly shown that the process of such transmutation takes place in the aquatic environment in the presence of appropriate isotopes and the presence of syntrophic microbiological associations. The characteristic feature of such transmutation is self-limiting and self-control: the process starts to be inhibited when a large amount of toxins (as metabolic products) are released and when the local environment is depleted with the necessary isotopic components. Under laboratory conditions, these factors can be controlled and corrected by periodical adding of appropriate chemical components. Under natural conditions, a sufficiently long time is needed to re-launch the transmutation process, during which a natural self-purification of the near environment from toxins takes place and the necessary isotopic composition is restored. Such a self-similar process justifies the periodicity of iron synthesis and the formation of thin layers of this element. The paper considers the dynamics of this process and shows that it can be used for the local geological chronology.