Chronology in stratigraphy
https://doi.org/10.24930/1681-9004-2025-25-6-1249-1263
EDN: QVZUPI
Abstract
Research subject. Issues related to the chronological representation of time in stratigraphy are discussed, including the features of biochronological calculation of geological time, the nature of zonal biochronological scales, the dual nature of stratigraphic classifications, the biological basis of chronostratigraphic divisions, as well as the concepts of “chronological
scale” and “chronological classification”.
Material and methods. Conventional approaches to the above issues are analyzed. An attempt is made to reveal the logical sources of disagreement on the issues under discussion and to outline possible compromise solutions.
Results. In order to successfully resolve the abovementioned issues, it is necessary to distinguish the biochronological scale as an instrument for measuring geological time and the geological section – as an object of measurement. Being cycles of paleontological development, peer subdivisions of biochronological scales should be equivalent, but not stratigraphic subdivisions of the same order.
Conclusions. The true chronological scales in stratigraphy are zonal biochronological scales, the construction of which uses the evolutionary sequence of similar events (“existence of species”), which allows us to obtain a scale of order consisting of equivalent (commensurate, equivalent, congruent) divisions – zones. The International Stratigraphic Scale (a summary section of the stratisphere) is, in its essence, a calendar of geological events and dates. The names of the subdivisions of the International Stratigraphic Scale serve as an international chronological language.
Keywords
About the Author
V. V. ChernykhRussian Federation
Valerii V. Chernykh
620110; 15 Academician Vonsovsky st.; Еkaterinburg
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Review
For citations:
Chernykh V.V. Chronology in stratigraphy. LITHOSPHERE (Russia). 2025;25(6):1249-1263. (In Russ.) https://doi.org/10.24930/1681-9004-2025-25-6-1249-1263. EDN: QVZUPI





































