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The formal division of the Quaternary is the responsibility of the IUGS International Commission on Stratigraphy's (ICS) Subcommission on Quaternary Stratigraphy (SQS), in partnership with the International Union for Quaternary Research's (INQUA) Commission on Stratigraphy and Chronology (SACCOM).
The table provides a correlation of chronostratigraphical subdivisions of late Cenozoic geological time, spanning the last 2.7 million years. The timescale of the correlation table is based on the internationally-recognised formal time subdivisions: the Phanerozoic Eon; the Cenozoic Era; the Quaternary System or Period; the Pleistocene and Holocene Series, and finally the Early/Lower, Middle, Late/Upper Pleistocene Subseries. At present the subseries divisions of the Pleistocene are not formalised. Series, and thereby systems, are formally-defined based on Global Stratotype Section and Points (GSSP) of which two have been ratified within the last 2.7 million years.
Previous versions of the chart were published as Gibbard et al. 2004, 2005 and Gibbard & Cohen, 2008.

The following sites produce up to date stratigraphical charts for all divisions of geological time
This chart, Tabla Cronoestratigráfica del Cuaternario de la Península Ibérica, is produced by AEQUA
For download is a high-resolution jpeg version (1.0 Mb). This is version 2, the earlier version, published in 2007 (1.3 Mb), is available here.

A new 2009 Geologic Time Scale chart by the Geological Society of America is published in GSA Today.
this page is maintained by P.L. Gibbard and K.M. Cohen