Episodes

Vol. 28 No.3 September 2005

Journal of International Geoscience

Published by the International Union of Geological sciences


by Kenitiro Suguio1,2, Aleth谷a Ernandes Martins Sallun2, and Em赤lio A. A. Soares2,3

Quaternary: ※Quo Vadis§?

1 Centro de P車s-Graduação, Pesquisa e Extensão (CEPPE), Universidade Guarulhos (UnG), Praça Tereza Cristina, 01 每 Guarulhos 每 SP 每 Brazil每 07023-070. e-mail: kenitirosuguio@hotmail.com
2 Programa de P車s-Graduação em Geologia Sedimentar - Instituto de Geoci那ncias, Universidade de São Paulo, Rua do Lago, 562 每 São Paulo每SP 每 Brazil 每 05508-080. e-mail: aletheamartins@hotmail.com
3 Departamento de Geoci那ncias, Universidade Federal do Amazonas, Av. Gal. Rodrigo O.J. Ramos, 3000, Manaus 每 AM 每Brazil - 69077-000 e-mail:easoares@usp.br

Abstract

The Quaternary, like the long-abandoned terms Primary, Secondary and Tertiary, is a very ambiguous word, whose chronological meaning is not very well defined. Its usage spread very quickly, perhaps due to its more-or-less close relationship with the human history and with the latest glaciations. However, the oldest of human fossil record, according to recent discoveries in Africa (Djourab Desert in Tchad), is about 7 million years old, rather than 2 million years as suggested by fossils at Olduvai. Moreover, for some time now, it has been known that the first Quaternary-type glaciations occurred in several regions of the Earth between 2.5 and 3 million years ago, that is prior to the Pliocene-Pleistocene limit at 1.81 million years ago, as determined by the GSSP. These facts have led some researchers, mostly from the International Union of Geological Sciences (IUGS), and from the International Association for Quaternary Research (INQUA), to suggest changes in the subdivision of the Neocenozoic. Certainly, discussions on this subject will be raised at many scientific meetings in the near future until almost unanimous agreement can be attained. Some additional suggestions are presented here, as a contribution to resolution of these nomenclatorial issues.  

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