Geological and paleontological evidence of eaely cambrian hydrothermal type ecosystems (kyzyl-tashtyg pyrite ore field, tyva)
Geological history of hydrothermal type ecosystems is of special interest to study the regularities of the evolutionary process. This article presents geological and paleontological evidence of early cambrian ecosystems hydrothermal type of tumattayginskaya formation of pyrite Kyzyl-Tashtyg ore field, Tuva.