Latent periodicity in the phanerozoic isotope age-curves of delta(34)S
, delta(13)C, and Sr-87/Sr-86 was established by spectral analysis met
hod. The most representative periods are 1200-1500 Myr and 550-570 Myr
that are trends and cycles with periods 200 and 150 Myr for curves de
lta(34)S and delta(13)C. Spectral composition of the curve Sr-87/Sr-86
differs from the curves mentioned above. Extremums of harmonics for t
he periods found coincide on time scale with boundaries of the stages
of reorganization plate kinematics.