Crassigyrinus

Crassigyrinus


Crassigyrinus
Temporal range: Early Carboniferous
Life restoration of Crassigyrinus scoticus
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Class: Amphibia
Order: "Ichthyostegalia"
Family: Watson, 1929
Species
  • C. scoticus Watson, 1926 (type)
Crassigyrinus

Crassigyrinus (meaning "thick tadpole") is an extinct genus of carnivorous stem tetrapod from the Early Carboniferous of Scotland and possibly Greer, West Virginia.[1] The type specimen was originally described as Macromerium scoticum and lacked a complete skull. With subsequent discoveries, Crassigyrinus is now known from three skulls, one of which is in articulation with a fairly complete skeleton, and a couple of incomplete lower jaws. Crassigyrinus grew up to 2 meters in length, coupled with tiny limbs and unusually large jaws. Crassigyrinus is taxonomically enigmatic, having confused paleontologists for decades with its apparent fish-like and tetrapod features.[2] It was traditionally placed within the group Labyrinthodontia along with many other early tetrapods. Some paleontologists have even considered it as the most basal Crown group tetrapod, while others hesitate to even place it within the Tetrapoda superclass. Crassigyrinus had unusually large jaws, enabling it to eat other animals it could catch and swallow. It had two rows of sharp teeth in its jaws, the second row having a pair of fangs. Crassigyrinus had large eyes, suggesting that it was either nocturnal, or lived in very murky water.

Description

Crassigyrinus had a streamlined body up to 2 meters in length. Its limbs were tiny and virtually useless, implying that the animal was almost completely aquatic. Crassigyrinus had unusually large jaws, equipped with two rows of sharp teeth, the second row having a pair of palatal fangs. Studies have shown that Crassigyrinus may have been able to open its mouth as wide as 60 degrees, which further suggest that it was a powerful predator with a strong bite.[2] This strongly suggests that it was ideally suited for catching fish, and the animal was probably a fast-moving predator.

Several thickened bony ridges ran along the dorsal midline of the snout and between the eyes, and several paleontologists have suggested that they helped the skull to withstand stress when the animal bit prey. Crassigyrinus had large eyes, suggesting that it was either nocturnal, or lived in very murky water.[3] It possessed large otic (spiracular) notches, probably accommodating a spiracle rather than a tympanic membrane. [4]

Its peculiar stunted forelimbs were tiny and the humerus was only 35 mm long (the whole animal was about 1.5 m long). Various foramina on the humeral surfaces are very similar to those seen in Ichthyostega, Acanthostega, and lobe-finned fishes like Eusthenopteron.[5][6] The hindlimbs were much larger than the forelimbs, and in the pelvis the ilium lacked a bony connection to the vertebral column (a classic feature of aquatic tetrapods). The tail only known from a few vertebrae fragments, is assumed to have been long and laterally compressed.[2]

References

  1. ^ Godfrey, S. J. 1988. Isolated tetrapod remains from the Carboniferous of West Virginia. Kirtlandia 43, 27-36.
  2. ^ a b c Chapter on Crassigyrinus] from Gaining ground: the origin and evolution of tetrapods, by Jennifer A. Clack, Indiana University Press 2002, from Google Books
  3. ^ Palmer, D., ed (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. p. 51. ISBN 1-84028-152-9. 
  4. ^ Benton, 2005. Vertebrate Palaeontology 3rd edition. Blackwell Publishing
  5. ^ Panchen, A. L. 1985. On the amphibian Crassigyrinus scoticus Watson from the Carboniferous of Scotland. Philosophical Transactions of the Royal Society of London B 309, 505-568.
  6. ^ Panchen, A. L. 1991. The early tetrapods: classification and the shapes of cladograms. In Schultze, H.-P. & Trueb, L. (eds) Origins of the Higher Groups of Tetrapods, Controversy and Consensus. Comstock/Cornell University Press (Ithaca and London), pp. 110-144.



Wikimedia Foundation. 2010.

Игры ⚽ Нужно сделать НИР?

Look at other dictionaries:

  • Crassigyrinus — scoticus Zeitraum Unter und Oberkarbon 325 bis 318 Mio. Jahre Fundorte Schottland S …   Deutsch Wikipedia

  • Crassigyrinus — Saltar a navegación, búsqueda ? Crassigyrinus Rango fósil: Carbonífero …   Wikipedia Español

  • Crassigyrinus — Crassigyrinus …   Wikipédia en Français

  • Crassigyrinus — …   Википедия

  • Crassygyrinus scoticus — Crassigyrinus Lebendrekonstruktion von Crassigyrinus scoticus Zeitraum Karbon ca. 325 318 Mio. Jahre Fossilfundorte Schottland …   Deutsch Wikipedia

  • Крассигиринус — ? † Крассигиринус …   Википедия

  • Temnospondyli — Temnospondyls Temporal range: Early Carboniferous Early Cretaceous, 330–120 Ma Possible descendant taxon Lissamphibia survives to present …   Wikipedia

  • List of Prehistoric Park episodes — This is a list of episodes from Prehistoric Park .Episode 1: T. rex Returns Montana, 65 million years ago, late Cretaceous. Genera encountered: * Ornithomimus (13 brought back) * Tyrannosaurus (identified as Tyrannosaurus rex , 2 brought back) *… …   Wikipedia

  • Karbon (Geologie) — < Devon | K a r b o n | Perm > vor 359,2–299 Millionen Jahren Atmosphärischer O2 Anteil (Durchschnitt über Periodendauer) ca. 32,5 Vol %[1] (163 % des heutigen Niveaus) …   Deutsch Wikipedia

  • Karbonzeit — < Devon | K a r b o n | Perm > vor 359,2–299 Millionen Jahren Atmosphärischer O2 Anteil (Durchschnitt über Periodendauer) ca. 32,5 Vol %[1] (163 % des heutigen Niveaus) …   Deutsch Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”