Messinian

System/
Period
Series/
Epoch
Stage/
Age
Age (Ma)
Quaternary Pleistocene Gelasian younger
Neogene Pliocene Piacenzian 3.600–2.58
Zanclean 5.333–3.600
Miocene Messinian 7.246–5.333
Tortonian 11.62–7.246
Serravallian 13.82–11.62
Langhian 15.97–13.82
Burdigalian 20.44–15.97
Aquitanian 23.03–20.44
Paleogene Oligocene Chattian older
Subdivision of the Neogene Period
according to the IUGS, [v2014/02].

The Messinian is in the geologic timescale the last age or uppermost stage of the Miocene. It spans the time between 7.246 ± 0.005 Ma and 5.332 ± 0.005 Ma (million years ago). It follows the Tortonian and is followed by the Zanclean, the first age of the Pliocene.

The Messinian overlaps the Turolian European Land Mammal Mega Zone (more precise MN 12 and 13) and the Pontian Central European Paratethys stage. It also overlaps the late Huayquerian and early Montehermosan South American Land Mammal Ages, and falls inside the more extensive Hemphillian North American Land Mammal Age.

During the Messinian, around 6 million years ago, the Messinian salinity crisis took place, which brought about repeated desiccations of the Mediterranean Sea.

Definition

Messinian gypsum and clay deposits in the Sorbas basin near Sorbas, southern Spain. Evaporite deposits of Messinian age are common throughout the Mediterranean.

The Messinian was introduced by Swiss stratigrapher Karl Mayer-Eymar in 1867.[1] Its name comes from the Italian city of Messina on Sicily, where the Messinian evaporite deposit is of the same age.

The base of the Messinian is at the first appearance of the planktonic foram species Globorotalia conomiozea and is stratigraphically in the middle of magnetic chronozone C3Br.1r. The Global Boundary Stratotype Section and Point for the Messinian is located in a section at Oued Akrech, near the Moroccan capital Rabat.[2]

The top of the Messinian (the base of the Zanclean stage and Pliocene series) lies with the top of magnetic chronozone Cr3 (about 100,000 years before the Thvera normal subchronozone C3n.4n). The top 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.

References

Notes

  1. Mayer-Eymar, Karl (1867) Catalogue systématique et descriptif des fossiles des terrains tertiaires qui se trouvent du Musée fédéral de Zürich (Zürich, Switzerland: Librairie Schabelitz, 1867), page 13. From page 13: "Dans ces circonstances, je crois qu'il m'est permis comme créateur d'une classification conséquente et logique de proposer pour l'étage en question un nom qui lui convient en tous points. Ce nom est celui d'Etage messinien." (In these circumstances, I think that I am permitted as the creator of a consistent and logical classification to propose for the stage in question a name that suits it in every way. That name is that of the Messinian stage.)
  2. This GSSP was established by Hilgen et al. (2000)

Sources

External links

Wikimedia Commons has media related to Messinian.
Wikisource has original works on the topic: Cenozoic#Neogene


Neogene Period
Miocene Pliocene
Aquitanian | Burdigalian
Langhian | Serravallian
Tortonian | Messinian
Zanclean | Piacenzian

Coordinates: 33°56′13″N 6°48′45″W / 33.9369°N 6.8125°W / 33.9369; -6.8125

This article is issued from Wikipedia - version of the 11/22/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.