Based on their compiled data set of ten extinction episodes (four of which had no known extinction rates), Rampino et al. (2020) claimed a 27.5-My period in non-marine-tetrapod extinctions. I reassessed that claim using the Gauss–Vaníček spectral analysis (GVSA), which revealed spectra of extremely low fidelity (mostly << 1) dominated by the Earth’s axial precession, without 99%-significant periods, but with hundreds of 95%-significant periods unrelated to the extinctions and the claimed period. Therefore, the data are physically nonsensical as far as any underlining cyclicity is concerned. The analysis did not reveal the claimed period in any band, at either 99% or 95% significance, so the claimed period is a ghost due to intermediary as...
The claims of periodicity in impact cratering and biological extinction events are controversial. An...
The fossil record is our only direct means for evaluating shifts in biodiversity through Earth’s his...
The decline in species richness from the equator to the poles is referred to as the latitudinal dive...
We re-examine the evidence for a 62 million year (Myr) periodicity in biodiversity throughout the Ph...
We re-examine the evidence for a 62 million year (Myr) periodicity in biodiversity throughout the Ph...
The discipline-wide effort to database the fossil record at the occurrence level has made it possibl...
Reconstructing deep time trends in biodiversity remains a central goal for palaeobiologists, but our...
Time series analysis of fossil biodiversity of marine invertebrates in the Paleobiology Database (PB...
Patterns of last occurrences of fossil species are often used to infer the tempo and timing of mass ...
A Fourier analysis of the magnitudes and timing of the Phanerozoic mass extinctions (MEs) demonstrat...
Time series analysis of fossil biodiversity of marine invertebrates in the Paleobiology Database (PB...
Studies of extinction in the fossil record commonly involve comparisons of taxonomic extinction rate...
The hypothesis that ocean acidification was a proximate trigger of the marine end-Triassic mass exti...
A Fourier analysis of the magnitudes and timing of the Phanerozoic mass extinctions (MEs) demonstrat...
The hypothesis that destructive mass extinctions enable creative evolutionary radiations (creative d...
The claims of periodicity in impact cratering and biological extinction events are controversial. An...
The fossil record is our only direct means for evaluating shifts in biodiversity through Earth’s his...
The decline in species richness from the equator to the poles is referred to as the latitudinal dive...
We re-examine the evidence for a 62 million year (Myr) periodicity in biodiversity throughout the Ph...
We re-examine the evidence for a 62 million year (Myr) periodicity in biodiversity throughout the Ph...
The discipline-wide effort to database the fossil record at the occurrence level has made it possibl...
Reconstructing deep time trends in biodiversity remains a central goal for palaeobiologists, but our...
Time series analysis of fossil biodiversity of marine invertebrates in the Paleobiology Database (PB...
Patterns of last occurrences of fossil species are often used to infer the tempo and timing of mass ...
A Fourier analysis of the magnitudes and timing of the Phanerozoic mass extinctions (MEs) demonstrat...
Time series analysis of fossil biodiversity of marine invertebrates in the Paleobiology Database (PB...
Studies of extinction in the fossil record commonly involve comparisons of taxonomic extinction rate...
The hypothesis that ocean acidification was a proximate trigger of the marine end-Triassic mass exti...
A Fourier analysis of the magnitudes and timing of the Phanerozoic mass extinctions (MEs) demonstrat...
The hypothesis that destructive mass extinctions enable creative evolutionary radiations (creative d...
The claims of periodicity in impact cratering and biological extinction events are controversial. An...
The fossil record is our only direct means for evaluating shifts in biodiversity through Earth’s his...
The decline in species richness from the equator to the poles is referred to as the latitudinal dive...