A consistent procedure intended for dividing the geological history into periods as well as for recovering space-time principles of the geological time materialization bears on stratotypes of the boundaries and compatibility of geochronological features. The key features are paleontological and isotope-geochronological. The results of the paleontological studies in comparison with those of the isotope geochronometric research demonstrate a specific character of time materialization by organic and inorganic matter and their fundamentally different geochronometric potential. A possibility and necessity to create a planetary geochronological calendar, i.e. an independent theoretical metric of the external control over the results of the event stratigraphy, isotope geochronology and cosmology have been ascertained.

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