Titlebook: Geological Evolution of the Earth During the Precambrian; Lazarus J. Salop Book 1983 Springer-Verlag Berlin Heidelberg 1983 Cambrian.Geolo

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most Eocambrian (the Lower Vendian). The Epiprotozoic was recognized as an erathem (era) in the Precambrian in my paper in 1964 (Salop 1964). This erathem could also be called the Katangan or Adelaidean according to the typical strata of Equatorial Africa or Southern Australia.

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The Neoprotozoic,mmonly occur in the same localities, and sometimes build up common extensive rock sequences (complexes or supergroups). At the same time, they are also characterized by stratigraphic or angular unconformities, locally of significant magnitude; the intrusive magmatism also separates these sub-erathems at places.

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The Epiprotozoic,most Eocambrian (the Lower Vendian). The Epiprotozoic was recognized as an erathem (era) in the Precambrian in my paper in 1964 (Salop 1964). This erathem could also be called the Katangan or Adelaidean according to the typical strata of Equatorial Africa or Southern Australia.

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The Epiprotozoic,e termination of the Katangan orogeny of the first order (680–650 m.y.). Thus, the formations examined constitute a separate stage in geologic evolution of the planet and its duration ( ~ 350 m.y.) is more than that of the Paleozoic Era (330 m.y.). Nevertheless, this large Precambrian unit was not p