TY - JOUR
T1 - A pulse of the Earth
T2 - A 27.5-Myr underlying cycle in coordinated geological events over the last 260 Myr
AU - Rampino, Michael R.
AU - Caldeira, Ken
AU - Zhu, Yuhong
N1 - Funding Information:
Research was partly funded by an NYU Research Challenge Fund Grant. We thank A. Embry, D.V. Kent, C. Koeberl, A. Prokoph, S. Self and 5 anonymous reviewers for helpful information.
Publisher Copyright:
© 2021 China University of Geosciences (Beijing) and Peking University
PY - 2021/11
Y1 - 2021/11
N2 - We performed spectral analyses on the ages of 89 well-dated major geological events of the last 260 Myr from the recent geologic literature. These events include times of marine and non-marine extinctions, major ocean-anoxic events, continental flood-basalt eruptions, sea-level fluctuations, global pulses of intraplate magmatism, and times of changes in seafloor-spreading rates and plate reorganizations. The aggregate of all 89 events shows ten clusters in the last 260 Myr, spaced at an average interval of ~ 26.9 Myr, and Fourier analysis of the data yields a spectral peak at 27.5 Myr at the ≥ 96% confidence level. A shorter period of ~ 8.9 Myr may also be significant in modulating the timing of geologic events. Our results suggest that global geologic events are generally correlated, and seem to come in pulses with an underlying ~ 27.5-Myr cycle. These cyclic pulses of tectonics and climate change may be the result of geophysical processes related to the dynamics of plate tectonics and mantle plumes, or might alternatively be paced by astronomical cycles associated with the Earth's motions in the Solar System and the Galaxy.
AB - We performed spectral analyses on the ages of 89 well-dated major geological events of the last 260 Myr from the recent geologic literature. These events include times of marine and non-marine extinctions, major ocean-anoxic events, continental flood-basalt eruptions, sea-level fluctuations, global pulses of intraplate magmatism, and times of changes in seafloor-spreading rates and plate reorganizations. The aggregate of all 89 events shows ten clusters in the last 260 Myr, spaced at an average interval of ~ 26.9 Myr, and Fourier analysis of the data yields a spectral peak at 27.5 Myr at the ≥ 96% confidence level. A shorter period of ~ 8.9 Myr may also be significant in modulating the timing of geologic events. Our results suggest that global geologic events are generally correlated, and seem to come in pulses with an underlying ~ 27.5-Myr cycle. These cyclic pulses of tectonics and climate change may be the result of geophysical processes related to the dynamics of plate tectonics and mantle plumes, or might alternatively be paced by astronomical cycles associated with the Earth's motions in the Solar System and the Galaxy.
KW - Correlations
KW - Cyclic pulses
KW - Fourier analysis
KW - Global geological events
KW - Tectonics
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U2 - 10.1016/j.gsf.2021.101245
DO - 10.1016/j.gsf.2021.101245
M3 - Article
AN - SCOPUS:85108112142
SN - 1674-9871
VL - 12
JO - Geoscience Frontiers
JF - Geoscience Frontiers
IS - 6
M1 - 101245
ER -