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- W2087695220 abstract "Krassilov, Valentin 1978 04 IS: Organic evolution and natural stratigraphical classifcation. Typological stratigraphy persisted up to the early 1940's. when it gave way to gradualistic concepts. Because world-wide periodicity of evolutionary events and their functional relations to crustal disturbances were denied, it was decided to define geological time divisions by a set of time-planes marked by agreed reference points. Actually, evolution is discontinuous at the molecular, population, species and community levels. Evolution of the whole biosphere depends on periodicity of tectonic and climatic events which add to general environmental instability and alter adaptive strategies. The perception of geological time is derived from the succession of unique litho- and biosphere events which Serve as a base of natural stratigraphical classification. Correlation is based on the parallelism of cliseres and chronoclines. Their homotaxial members are recognized as coenozones and phenozones. Standard stratigraphical boundaries are materialized in local boundaries defined by historical events of high ‘confidence level’. Nominotypes designated for nomenclatural procedures need not coincide with the boundary reference points; otherwise they would hamper further development of stratigraphical classification." @default.
- W2087695220 created "2016-06-24" @default.
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- W2087695220 date "1978-04-01" @default.
- W2087695220 modified "2023-09-26" @default.
- W2087695220 title "Organic evolution and natural stratigraphical classification" @default.
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- W2087695220 doi "https://doi.org/10.1111/j.1502-3931.1978.tb01292.x" @default.
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