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The “Problem of the quaternary” and the taxonomic rank of the late cenozoic in the international stratigraphic scale

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Abstract

An international scientific conflict has arisen around the International Stratigraphic Scale, the main document that regulates the rules of reading of geological records and, hence, concerns all Earth sciences. The matter of debate is the geological time scale of 2004, developed by the International Commission on Stratigraphy, where the Quaternary system was abandoned. This ICS decision triggered a protest among Quaternary geologists, members of INQUA, and became the subject of much controversy. This article provides a comprehensive analysis of the Quaternary problem and proposes a reasonable scientific solution that may be appropriate for both parties.

The subject of Late Cenozoic geology is discussed: glaciations, human evolution, and recent deposits. In contrast to Charles Lyell’s definition of the Plio-Pleistocene according to the percentage of modern mollusk species, it is defined here as a blanket formation, which is correlative to the topography and consists of mapped stratogens hosting fossils of modern biogeocenoses. Features of the description of the Plio-Pleistocene in terms of gravitational orbital tuning are considered. Four paleogeographic phases of modern environment evolution are recognized and ranked as stages: (1) The Messinian evolutionary explosion involved the appearance of many biogeocenoses and the bipedal walking of our extinct ancestors armed with sticks. It was a consequence of the Early Greenland (7.6 Ma BP) and Patagonian (6.7 Ma BP) hyperglaciations. (2) The Zanclean age is marked by climatic and hydrological but not evolutionary boundaries. (3) The appearance of the Villafranchian animal assemblage and Australopithecus, who used stones as weapon: 4.0–3.6 Ma BP. Orogeny and isolation of the Arctic Ocean changed the global climate dramatically. (4) The sexual revolution became the third evolutionary jump: the appearance of the first woman, “Eve”, and the genus Homo with her: 1.9 Ma BP.

According to the current view, the Plio-Pleistocene, as defined by Lyell, consists of nineteen chronozones, four stages and two series. Hence, it is a true system, Pliocene-Pleistocene = Hologene, with a GSSP at 7.6 Ma BP, complying with all rules of scientific stratigraphical subdivision, rather than the mere beginning of the archaic Quaternary pseudo system with GSSPs at 1.8 or 2.6 Ma BP

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  1. Research Center for Interdisciplinary Environmental Cooperation, nab. Kutuzova 14, St Petersburg, 191187, Russia

    V. A. Zubakov

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Original Russian Text © V.A. Zubakov, 2011, published in Stratigrafiya. Geologicheskaya Korrelyatsiya, 2011, Vol. 19, No. 1, pp. 108–125.

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Zubakov, V.A. The “Problem of the quaternary” and the taxonomic rank of the late cenozoic in the international stratigraphic scale. Stratigr. Geol. Correl. 19, 108–124 (2011). https://doi.org/10.1134/S086959381005103X

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