Wordian
| System/ Period |
Series/ Epoch |
Stage/ Age |
Age (Ma) |
|---|---|---|---|
| Triassic | Lower/ Early |
Induan | younger |
| Permian | Lopingian | Changhsingian | 252.2–254.1 |
| Wuchiapingian | 254.1–259.8 | ||
| Guadalupian | Capitanian | 259.8–265.1 | |
| Wordian | 265.1–268.8 | ||
| Roadian | 268.8–272.3 | ||
| Cisuralian | Kungurian | 272.3–283.5 | |
| Artinskian | 283.5–290.1 | ||
| Sakmarian | 290.1–295.0 | ||
| Asselian | 295.0–298.9 | ||
| Carboniferous | Pennsylvanian | Gzhelian | older |
| Subdivision of the Permian system according to the ICS (Geologic Time Scale 2013).[1] | |||
In the geologic timescale, the Wordian is an age or stage of the Permian. It is the middle of three subdivisions of the Guadalupian epoch or series. The Wordian lasted between 268.8 and 265.1 million years ago (Ma). It was preceded by the Roadian and followed by the Capitanian.[2]
Stratigraphy
The Wordian stage was introduced into scientific literature by Johan August Udden in 1916 and was named after the Word Formation of the North American Permian Basin. The Capitanian was first used as a stratigraphic subdivision of the Guadalupian in 1961,[3] when both names were still only used regionally in the southern US. The stage was added to the internationally used ISC timescale in 2001.[4]
The base of the Wordian stage is defined as the place in the stratigraphic record where fossils of conodont species Jinogondolella aserrata first appear. The global reference profile for this stratigraphic boundary is located at Getaway Ledge in the Guadalupe Mountains of Texas.
The top of the Wordian (the base of the Capitanian stage) is defined as the place in the stratigraphic record where the conodont species Jinogondolella postserrata first appears.
The Wordian stage was part of the time in which the Zechstein was deposited in Europe.
Biostratigraphy
The Wordian spans the entire conodont biozone of Jinogondolella aserrata. It contains two fusulinid biozones:
- Zone of Afganella tereshkovae
- Zone of Neoschwagerina tenuis
Biodiversity
Olson’s Extinction, a worldwide loss of terrestrial vertebrate life occurred during the Early Guadalupian (Roadian, Wordian).[5]
References
Notes
- ↑ "Chronostratigraphic chart 2013". ICS. Retrieved 27 March 2013.
- ↑ See Gradstein et al. (2004) for a detailed geologic timescale
- ↑ Glenister & Furnish (1961)
- ↑ The current ICS' subdivision of the Guadalupian epoch/series was first proposed by Glenister et al. (1999)
- ↑ Sahney, S. & Benton, M.J. (2008). "Recovery from the most profound mass extinction of all time" (PDF). Proceedings of the Royal Society: Biological. 275 (1636): 759–65. doi:10.1098/rspb.2007.1370. PMC 2596898
. PMID 18198148.
Literature
- Glenister, B.F. & Furnish, W.M.; 1961: The Permian ammonoids of Australia, Journal of Paleontology 35(4), pp 673–736.
- Glenister, B.F.; Wardlaw, B.R.; Lambert, L.L.; Spinosa, C.; Bowring, S.A.; Erwin, D.H.; Menning, M. & Wilde, G.L.; 1999: Proposal of Guadalupian and Component Roadian, Wordian and Capitanian Stages as International Standards for the Middle Permian Series, Permophiles 34: pp 3–11.
- Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press
External links
- GeoWhen Database - Wordian
- Upper Paleozoic stratigraphic chart at the website of the subcommission for stratigraphic information of the ICS
| Preceded by Proterozoic Eon | Phanerozoic Eon | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Paleozoic Era | Mesozoic Era | Cenozoic Era | ||||||||||
| Cambrian | Ordovician | Silurian | Devonian | Carboniferous | Permian | Triassic | Jurassic | Cretaceous | Paleogene | Neogene | 4ry | |
