Zanclean

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The Zanclean is the lowest stage or earliest age on the geologic time scale of the Pliocene. It spans the time between 5.332 ± 0.005 Ma (million years ago) and 3.6 ± 0.005 Ma. It is preceded by the Messinian Age of the Miocene Epoch, and followed by the Piacenzian Age.

The Zanclean can be correlated with regionally used stages, such as the Opoitian of New Zealand,[1] and the Tabianian or Dacian of Central Europe. It also corresponds to the late Hemphillian to mid-Blancan North American Land Mammal Ages. In California, the Zanclean roughly corresponds to the middle part of the Delmontian stage.[2]

Definition

The Zanclean Stage was introduced by Giuseppe Seguenza in 1868. It is named after Zancle, the pre-Roman name for the Italian city of Messina on Sicily.

The base of the Zanclean (and the Pliocene Series) lies with the top of magnetic chronozone Cr3 (about 100,000 years before the Thvera normal subchronozone C3n.4n). The base is also close to the extinction level of the calcareous nanoplankton species Triquetrorhabdulus rugosus (the base of biozone CN10b) and the first appearance of nanoplankton Ceratolithus acutus. The GSSP for the Zanclean is in the vicinity of the ruins of the ancient city of Heraclea Minoa on Sicily, Italy.[3]

The top of the Zanclean Stage (the base of the Piacenzian Stage) is at the base of magnetic chronozone C2An (the base of the Gauss chronozone and at the extinction of the planktonic forams Globorotalia margaritae and Pulleniatina primalis.

Events of the Zanclean

References

Notes

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  1. ^ Page Module:Citation/CS1/styles.css has no content.Gradstein FM, Ogg JG, Schmitz MD, Ogg GM, eds. (2012). The Geologic Timescale 2012. Elsevier. pp. 936–937. ISBN 978-0-44-459390-0.
  2. ^ Page Module:Citation/CS1/styles.css has no content.Allaby, Ailsa; Michael Allaby (1999). "Delmontian". A Dictionary of Earth Sciences. Encyclopedia.com. Retrieved 10 Dec 2009. A stage in the Upper Tertiary of the west coast of N. America
  3. ^ Cite error: The named reference Van Couvering was invoked but never defined (see the help page).
  4. ^ Page Module:Citation/CS1/styles.css has no content.Marco Roveri; Adele Bertini; DomenicoCosentino; Agata Di Stefano; Rocco Gennari; Elsa Gliozzi; Francesco Grossi; Silvia Maria Iaccarino; Stefano Lugli; Vinicio Manzi; Marco Tavian (2008). "A high-resolution stratigraphic framework for the latest Messinian events in the Mediterranean area" (PDF). Stratigraphy. 5 (3–4): 323–342, text-figures 1–9. doi:10.29041/strat.05.3.08. Archived from the original (PDF) on January 21, 2012. Retrieved December 10, 2009.
  5. ^ Page Module:Citation/CS1/styles.css has no content.Petuch, Edward J.; Roberts, Charles (18 April 2007). The Geology of the Everglades and Adjacent Areas. CRC Press. ISBN 9781420045598.

Literature

  • Page Template:Smallcaps/styles.css has no content.Castradori, D.; Rio, D.; Hilgen, F.J. & Lourens, L.J.; 1998: The Global Standard Stratotype section and Point (GSSP) of the Piacenzian Stage (Middle Pliocene), Episodes, 21(2): pp 88–93.
  • Page Template:Smallcaps/styles.css has no content.Gradstein, F.M.; Ogg, J.G. & Smith, A.G. (eds.) (2005) A Geologic Time Scale 2004 Cambridge University Press, Cambridge, UK, Template:ISBN.
  • Page Template:Smallcaps/styles.css has no content.Giuseppe Seguenza; 1868: La Formation Zancléenne, ou recherches sur une nouvelle formation tertiaire, Bulletin de la Société Géologique de France, séries 2, 25: 465-485. Template:In lang
  • Page Template:Smallcaps/styles.css has no content.Van Couvering, J.A.; Castradori, D.; Cita, M.B.; Hilgen, F.J. & Rio, D.; 2000: The base of the Zanclean Stage and of the Pliocene Series, Episodes, 23(3): pp 179–187.

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  • Zanclean at the GeoWhen database
  • Neogene timescale, at the website of the subcommission for stratigraphic information of the ICS
  • Neogene timescale at the website of the Norwegian network of offshore records of geology and stratigraphy

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