[Earlier steps of the soil ecosystem evolution].

Fossil soils are known since early Praecambrian, long before the occurrence of higher terrestrial plants on the Earth. Primeval biocoenoses on the land and in continental water bodies were floating and bottom prokaryotic mats and films which produced the majority of biomass and with regard to specific productivity were not inferior to any other photosynthetics. Before the occurrence of higher plants, erosion was very strong, resulting in flat relief, absence of permanent streams, domination of wandering rivers and surface runoff; all water bodies were muddy. When floods occurred, which was quite so often, clay particles of muddy water streams isolated bottom-mats from the light and then their considerable part perished. The result was not soil as a uniform bioinert body but rather a "puff pie" consisted of layers of unoxidized charred organic matter and clay prolayers. The burial of unoxidized organic matter contributed to enrichment of the atmosphere with oxygen. Worms and arthropods, which came out to the land and continental water bodies during Cambrian period, mixed up the organic matter with mineral components strengthening the process of soil forming considerably. Soils of the modern type appeared after higher plants expanded in Devonian and displaced bottom-mats in shallow waters. The soil fauna that existed at this time was not so different from the modern one with regard to its evolutionary level.