From eons to epochs: multifractal geological time and the compound multifractal-Poisson process
Abstract
Geological time is punctuated by events that define biostrata and the Geological Time Scale's (GTS) hierarchy of eons, eras, periods, epochs, ages. Paleotemperatures and macroevolution rates, have already indicated that the range ? 1 Myr to (at least) several hundred Myrs is a scaling (hence hierarchical) megaclimate regime. We apply analysis techniques including Haar fluctuations, structure functions, trace moment and extended self-similarity to the temporal density of the boundary events (?(t)) of two global and four zonal series. We show that ?(t) itself is a new paleoindicator and we determine the fundamental multifractal exponents characterizing the mean fluctuations, the intermittency and the degree of multifractality. The strong intermittency allows us to show that the (largest) megaclimate scale is at least ? 0.5 Gyr. We find that the tail of the probability distribution of the intervals (gaps) between boundaries is also scaling with an exponent q
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| Título según WOS: | From eons to epochs: multifractal geological time and the compound multifractal-Poisson process |
| Título según SCOPUS: | From eons to epochs: multifractal geological time and the compound multifractal - Poisson process |
| Título de la Revista: | Earth and Planetary Science Letters |
| Volumen: | 669 |
| Editorial: | Elsevier B.V. |
| Fecha de publicación: | 2025 |
| Idioma: | English |
| DOI: |
10.1016/j.epsl.2025.119460 |
| Notas: | ISI, SCOPUS |