Carnian
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- For the Carnian Alps, see Carnic Alps.
The Carnian (less commonly, Karnian) is the first stage of the Upper Triassic, Mesozoic. Its boundaries are not characterized by major extinctions or biotic turnovers, but a climatic event (known as the Carnian Pluvial Event) occurred during the Carnian and seems to be associated with important extinctions or radiations.
| Triassic period | ||
|---|---|---|
| Lower/Early Triassic | Middle Triassic | Upper/Late Triassic |
| Induan | Olenekian | Anisian | Ladinian | Carnian | Norian Rhaetian |
Contents |
[edit] Naming
The Carnian was named in 1869 by Mojsisovics. It is unclear if it was named after the Carnic Alps or after the Austrian region of Carinthia (Kärnten in German). The name, however, was firstly used referring to a part of the Hallstatt Limestone cropping out in Austria.
[edit] Dating and subdivisions
There is not an established, standard usage for the Carnian subdivisions, thus, while some authors use a two-substage subdivision:
- Julian
- Tuvalian
others prefer a three-substage organization of the stage as follows:
- Cordevolian
- Julian
- Tuvalian
The Carnian spans from 228.0 */- 2.0 to 216.5 ± 2.0 Ma. These dates are interpolated, because direct radiometric datations of this stage are missing at the moment. Some researchers believe that the Carnian age ended some 10 millions of years before, and this hypothesis is awaiting confirmation by new radiometric datations.
[edit] Definition
The base of the Carnian stage is not yet formally defined. The leading GSSP candidate is at Prati di Stuores/Stuores Wiesen, in Badia Valley, South Tyrol, Italy. The proposed base of the Carnian is at the First Occurrence of the ammonoid Daxatina canadensis. Other possible candidate sections are in Spiti, Indian Himalayas, and at New Pass in Nevada.
[edit] Paleogeography and climate
The paleogeography of the Carnian was basically the same as for the rest of the Triassic. Most continents were merged into the supercontinent Pangaea, and there was a single global ocean, Panthalassa. The global ocean had a western branch at tropical latitudes called Paleo-Tethys. The sediments of Paleo-Tethys now crop out in southeastern Europe, in the Middle East, in the Himalayas, and up to the island of Timor.
The extreme land-sea distribution led to "mega-monsoons", i.e., an atmospheric monsoon regime more intense than the present one.
As for most of the Mesozoic, there were no ice caps. Climate was mostly arid in the tropics, but an episode of wet tropical climate is documented at least in the Paleo-Tethys. This putative climatic event is called the “Carnian Pluvial Event”, its age being between latest early Carnian (Julian) and the beginning of late Carnian (Tuvalian). The nature of this event is still discussed; some scientists believe it is only an artifact, due to the migration of continents of the Tethyan area across the equatorial climatic belt. Following this idea, the apparent shift from arid to humid, and then back to arid climate simply testifies the continents going from southern tropical, to equatorial, and then to northern tropical latitudes.
[edit] Life in the Carnian
[edit] Plants
[edit] Invertebrates
There are a few invertebrates which are typical and characteristic of the Carnian. Among molluscs, the ammonoid genus Trachyceras is exclusive of the lower Carnian (i.e., Julian of the two-substages subdivision, see above). The family tropitidae and the genus Tropites appear at the base of the upper Carnian (Tuvalian). The bivalve genus Halobia, a bottom-dweller of deep sea environments, differentiated from Daonella at the beginning of this age. Scleractinian coral reefs, i.e., reefs with corals of the modern type, became relatively common for the first time in the Carnian.
[edit] Vertebrates
It is unclear whether Dinosaurs originated during the Carnian or even earlier, nevertheless, the oldest well documented dinosaurian assemblage, in the Ischigualasto Formation of Argentina, is most probably late Carnian in age.
Conodonts are present in Triassic marine sediments. Paragondolella polygnathiformis appears at the base of the stage, and is perhaps the most characteristic species. A partial list of Carnian vertebrates is given below.
[edit] Temnospondyli
- Cyclotosaurus
- Metoposaurus
[edit] Ichthyosaurs
- Californosaurus
- Shastasaurus
- Shonisaurus
[edit] Archosauromorphs
[edit] Non-dinosaurian archosaurs
- Palaeorhinus
- Rutiodon
- Doswellia
- Ornithosuchus
- Saurosuchus
- Postosuchus
- Stagonolepis
- Desmatosuchus
- Hesperosuchus
[edit] Dinosaurs
- Azendohsaurus
- Blikanasaurus (considered Norian by some researchers)
- Euskelosaurus (considered Norian by some researchers)
- Guaibasaurus
- Pisanosaurus
- Teyuwasu
[edit] Synapsids
- Placerias
- Exaeretodon
[edit] Classic localities and Lagerstätten
The lower Carnian fauna of the San Cassiano Formation (Dolomites, northern Italy) is studied since the 19th century. Fossiliferous localities are many, and are distributed mostly in the surroundings of Cortina d'Ampezzo and in the high Badia Valley, near the village of San Cassiano, after which the formation was named. This fauna is extremely various, including ammonoids, gastropods, bivalves, echinoderms, calcareous sponge, corals, brachiopods, and a variety of less common fossils. A collection of this fauna is exposed in the “Museo delle Regole”, a museum in Cortina d'Ampezzo.
The Ischigualasto Formation of northwestern Argentina yielded a very important vertebrate association, including the oldest dinosaurian assemblage.
[edit] References
- Gradstein F.M., Ogg J.G. and Smith A.G., 2004, A Geologic Time Scale 2004, Cambridge University Press.
- Broglio Loriga, C., and others, 1999, The Prati di Stuores/Stuores Wiesen section (Dolomites, Italy): a candidate Global Stratotype Section and Point for the Base of the Carnian stage. Rivista Italiana di Paleontologia e Stratigrafia, v. 105, p. 37-78.
