ICS Subcommission on Quaternary Stratigraphy

 

The Subcommission on Quaternary Stratigraphy (SQS) is a constituent body of the International Commission on Stratigraphy (ICS), the largest scientific organisation within the International Union of Geological Sciences (IUGS). It is also the only body concerned with stratigraphy on a global scale for the whole geological column. Its most important major objective is the establishment of a standard, globally-applicable stratigraphical scale, which it seeks to achieve through the co-ordinated contributions of a network of Subcommissions and Working Groups with a specific, limited mandate.
The SQS exists to promote and co-ordinate international co-operation and integration by applying the statutary scientific goals of the ICS to the Quaternary - the most recent geological system, the last 2.6 Ma:

* the establishment and publication of a standard and global geological time-scale for the Quaternary and the preparation and publication of global correlation charts,
* the unification of regional chronostratigraphical nomenclature by organising and documenting stratigraphical units on a global scale,
* the promotion of education in stratigraphical methods, and the dissemination of stratigraphical knowledge,
* the evaluation of new stratigraphical methods and their integration into a multidisciplinary stratigraphy, and
* the definition of principles of stratigraphical classification, terminology and procedure and their publication in guides and glossaries.

The scientific activities are carried out through projects, websites, publications and meetings, particularly through close co-operation with our sister organisation the International Union of Quaternary Research (INQUA), as well as through collaboration with other organisations.
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Information and features

Subcommission

Glacier

Other information

  • A 'Fresh Start' - new negotiations began between INQUA + ICS on the classification of the Quaternary and its relation to Tertiary, Neogene, etc. at the International Geological Congess in Oslo, August 2008. click to enlarge
  • discussion
  • The Argentinian Stratigraphic Committee has decided to maintain the use of Tertiary and Quaternary Systems/Periods within the Cenozoic Erathem/Era. Tertiary includes the Paleogene and Neogene Subsystems/Subperiods. The base of the Quaternary is at Vrica, Italy, as accepted by IUGS. The decision of the Argentinian Stratigraphic Committee and its fundamentals are given in the following publication: Riccardi, A.C., 2007. Terciario y Cuaternario: definición y posición. Revista de la Asociación Geológica Argentina 62: 485-487.
  • The geologic time scale: USGS holds firm. "The gross Cenozoic stratigraphy of the continental USA lends itself to a division into Tertiary and Quaternary rocks." (Andrew Alden 2007).

anthropocene

  • Sequence map of HOLOCENE coastal deposits of Belgium - Belgian Geological Survey. Details in ENGLISH, NEDERLANDS.pdf
GTS
  • ICS VOTE on QUATERNARY and move of Pleistocene boundary to 2.6 Ma - 14.4.07.
  • Group photo of March 2004 meeting here.


iugs

esfs Earth Sciences for Society - an International Year of Planet Earth. Organised under the auspices of The International Union of Geological Sciences (IUGS) which represents about 250,000 Earth scientists in 117 countries.




INQUA

  • INQUA XIX Congress, Bern, Switzerland 2011

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  • INQUA Subcommission on European Quaternary Stratigraphy (INQUA-SEQS) website .
  • INQUA Subcommission on Asian Quaternary Stratigraphy (INQUA-SAQS) website .

This site is supported by Wiley / Blackwell Quaternary Journals. Read more.


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anse du brick
Anse du brick, Normandy, France - raised beach (Eemian), and slope deposits (Weichselian).



Other photographs:
top of page: Laminated interglacial - early glacial lacustrine sediments at Pianico, Northern Italy (late Middle Pleistocene, ?Marine Isotope Stage 11).
below: Blomstrandbreen (glacier) - Svalbard.



Subcommission on Quaternary Stratigraphy,
International Commission on Stratigraphy
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