Carnian

For the Carnian Alps, see Carnic Alps.
System/
Period		 Series/
Epoch		 Stage/
Age		 Age (Ma)
Jurassic Lower/
Early		 Hettangian younger
Triassic Upper/
Late		 Rhaetian 201.3–208.5
Norian 208.5–~228
Carnian ~228–~235
Mid/
Middle		 Ladinian ~235–~242
Anisian ~242–247.2
Lower/
Early		 Olenekian 247.2–251.2
Induan 251.2–252.2
Permian Lopingian Changhsingian older
Subdivision of the Triassic system
according to the IUGS, as of July 2012.

The Carnian (less commonly, Karnian) is the lowermost stage of the Upper Triassic series (or earliest age of the Late Triassic epoch). It lasted from about ~228 to ~235 million years ago (Ma).[1] The Carnian is preceded by the Ladinian and is followed by the Norian. 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 biotic radiations.

Stratigraphic definitions

Alluvial plain red clays of the Travenanzes formation, upper Carnian, the Dolomites, northern Italy
Brotheotrachyceras brotheus from the San Cassiano Formation, Val Badia, Dolomites, Southern Alps. This ammonoid is an index fossil for the lower Carnian

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 first used referring to a part of the Hallstatt Limestone cropping out in Austria.

The base of the Carnian stage is defined as the place in the stratigraphic record where the ammonite species Daxatina canadensis first appears. The global reference profile for the base is located at the Stuores-Wiesen near Badia in the Val Badia in the region of South Tyrol, Italy.[2]

The top of the Carnian (the base of the Norian) is at the bases of the ammonite biozones of Klamathites macrolobatus or Stikinoceras kerri and the conodont biozones of Metapolygnathus communisti or Metaolygnathus primitius.

Dating and subdivisions

There is no established, standard usage for the Carnian subdivisions, thus, while in some regional stratigraphies a two-substage subdivision is common:

others prefer a three-substage organization of the stage as follows:

The Carnian spans from 228.0 ± 2.0 to 216.5 ± 2.0 Ma in the proposed geologic time scale by Gradstein et al. (2004). These dates are interpolated, because direct radiometric dates for this stage were missing when that time scale was compiled. Recently, Upper Carnian beds in southern Italy yielded an age of 230.91 ± 0.33 Ma. The age and duration of the Carnian need thus to be reconsidered.

Biostratigraphy

In the Tethys domain, the Carnian stage contains six ammonite biozones:

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.

Life

In the marine realm, the Carnian saw the first abundant occurrences of calcareous nannoplankton, a morphological group including the Coccolithophores.

Invertebrates

There are a few invertebrates which are typical and characteristic of the Carnian. Among molluscs, the ammonoid genus Trachyceras is exclusive to 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.

Vertebrates

The earliest dinosaur Eoraptor originated slightly before the Carnian stage began around 230 Ma. The oldest well documented dinosaurian assemblage, in the Ischigualasto Formation of Argentina, is most probably late Carnian in age.

In this stage the archosaurs became the dominant faunas in the world, evolving into groups such as the phytosaurs, rhynchosaurs, aetosaurs, and rauisuchians. The first dinosaurs also appeared in this stage, and though at the time they were small and insignificant, they diversified rapidly and would dominate the fauna for the rest of the Mesozoic. On the other hand, the therapsids, which included the ancestors of mammals, decreased in both size and diversity, and would remain relatively small until the extinction of the dinosaurs.

Conodonts were present in Triassic marine sediments. Paragondolella polygnathiformis appeared at the base of the Carnian stage, and is perhaps the most characteristic species. A partial list of Carnian vertebrates is given below.

Many Carnian vertebrates are found in Santa Maria Formation rocks of the Paleorrota geopark.

Temnospondyls

Temnospondyls of the Carnian
Taxa Presence Location Description Images
All Across Europe
Cyclotosaurus
Metoposaurus
Australia
Europe and North America

†Ichthyosaurs

Ichthyosaurs of the Carnian
Taxa Presence Location Description Images
Californosaurus
Cymbospondylus
Shastasaurus
Shonisaurus

†Archosauromorphs (non-archosaurian)

Non-Archosaurian Archosauromorphs of the Carnian
Taxa Presence Location Description Images
Paleorrota, Brazil.
Hyperodapedon
Tanystropheus
Trilophosaurus

†Crurotarsans (non-crocodylomorphan)

†Non-crocodylomorph Crurotarsans of the Carnian
Taxa Presence Location Description Images
Desmatosuchus
Doswellia
Ornithosuchus
Paleorhinus
Postosuchus
Rutiodon
Saurosuchus
Stagonolepis

Crocodylomorphs

Crocodylomorphs of the Carnian
Taxa Presence Location Description Images
Hesperosuchus

†Ornithodirans (non-dinosaurian)

†Non-Dinosaurian Ornithodira of the Carnian
Taxa Presence Location Description Images
Silesia, Poland
Silesaurus
Agudo, Rio Grande do Sul, Brazil

Dinosaurs

†Dinosaurs of the Carnian
Taxa Presence Location Description Images
Disputed: considered Norian by some researchers. Lesotho
Eoraptor
Guaibasaurus
Herrerasaurus
Panphagia
Pisanosaurus
Staurikosaurus
Argentina
Disputed: considered Norian by some researchers. Lesotho, South Africa, Zimbabwe
Paleorrota, Brazil.
Argentina
Ischigualasto Formation, San Juan, Argentina A small, lightly built dinosaur approximately 1 m (3 ft 3 in) in length and 30 cm (12 in) in height. It was bipedal and, like all ornithischians, was probably exclusively herbivorous.
  • Saturnalia
 Paleorrota, Rio Grande do Sul, Brazil. May have been a primitive sauropodomorph, probably grew to about 1.5 meters (5 ft) long.
Paleorrota, Rio Grande do Sul, Brazil.

†Therapsids (non-mammalian)

†Non-mammalian Therapsids of the Carnian
Taxa Presence Location Description Images
Paleorrota, Brazil.
Exaeretodon
Placerias

Mammalia

Mammalia of the Carnian
Taxa Presence Location Discussion Images
Tecovas formation, Texas, USA Some writers consider Adelobasileus to be a mammal,[3] while those who limit Mammalia to the crown group do not include this genus. In any case, Adelobasileus is thought to be either the common ancestor of all modern mammals or else a close relative of that ancestor.
Adelobasileus

†Thalattosaurians

Thalattosauria of the Carnian
Taxa Presence Location Description Images
Falang Formation, Guizhou, China A relatively large thalattosaurian, more than 4 meters long.
Miodentosaurus

Classic localities and lagerstätten

The lower Carnian fauna of the San Cassiano Formation (Dolomites, northern Italy) has been 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 diverse, 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.

See also

References

Notes

  1. ↑ According to Gradstein et al. (2004). Brack et al. (2005) give 235 to 226 Ma
  2. ↑ The GSSP was established by Broglio Loriga et al. (1999)
  3. ↑ Lucas and Luo (1993).

Literature

External links

Triassic Period
Lower/Early Triassic Middle Triassic Upper/Late Triassic
Induan |Olenekian Anisian | Ladinian Carnian | Norian
Rhaetian

Coordinates: 46°31′37″N 11°55′49″E / 46.5269°N 11.9303°E