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Episodes Vol. 28 No.3 September 2005 Journal of International Geoscience Published by the International Union of Geological sciences |
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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 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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