In the Phanerozoic 17 global events took place, which were characterized by
intense basaltic magmatism, active formation of uranium deposits, accumula
tion of marine radioactive uraniferous black shales, increase in the enviro
nment radioactivity, and, as a result, mass extinction of old fauna and app
earance of new species of organisms.
The greatest events (V-C, D-C, J-K) occurred every 216-217 Ma, i.e., every
galactic year. During this period, similar events took place every ca. 30 M
a.
The proposed periodic system includes three large periods (galactic years)
and seven series of similar events.