Steneosaurus

Steneosaurus
Temporal range: 183–142 Ma
Toarcian - Berriasian
Steneosaurus bollensis, Holzmaden Germany
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Sauropsida
Infraclass: Archosauromorpha
(unranked): Mesoeucrocodylia
Suborder: Thalattosuchia
Family: Teleosauridae
Genus: Steneosaurus
Geoffroy, 1825
Species
  • S. baroni
  • S. bollensis
  • S. boutilieri
  • S. brevior
  • S. edwardsi
  • S. gracilirostris
  • S. heberti
  • S. jugleri
  • S. larteti
  • S. leedsi
  • S. megarhinus
  • S. megistorhynchus (type)
  • S. obtusidens
  • S. priscus
Synonyms

Steneosaurus is an extinct genus of teleosaurid crocodyliform from the Early Jurassic to Early Cretaceous (Toarcian to Berriasian). Fossil specimens have been found in England, France, Germany, Switzerland and Morocco.

Contents

Species

Species in this genus are traditionally classed into two skull groups: longirostrine (long, narrow jaws) and brevirostrine (short, broad jaws).

Longirostrine

Brevirostrine

Evolutionary relationships

A recent phylogenetic analysis into the evolutionary relationships of Thalattosuchia did not support the monophyly of Steneosaurus, as the genera Machimosaurus and Teleosaurus both fell within Steneosaurus.[2]

Niche partitioning

Steneosaurus priscus is one of five thalattosuchian species known from the Mörnsheim Formation (Solnhofen limestone, early Tithonian) of Bavaria, Germany. Steneosaurus was the only teleosaurid known from this Formation, co-existing with four metriorhynchid species from the genera Dakosaurus and Geosaurus. It has been hypothesised that niche partitioning enabled several species of crocodyliforms to co-exist.[3]

From the semi-aquatic Oker locality in Lower Saxony, Germany (Kimmeridgian-age) two genera of teleosaurids (Steneosaurus and Machimosaurus) are known, in addition to the neosuchian genera Goniopholis and Theriosuchus.[4] Steneosaurus and Machimosaurus are also found together in the same Tithonian-age deposits of western France.[5]

See also

External links

References

  1. ^ Andrews CW. 1913. A descriptive catalogue of the marine reptiles of the Oxford Clay, Part Two. London: British Museum (Natural History), 206 pp.
  2. ^ Mueller-Töwe IJ. 2005. Phylogenetic relationships of the Thalattosuchia. Zitteliana A45: 211–213.
  3. ^ Andrade MB, Young MT. 2008. High diversity of thalattosuchian crocodylians and the niche partition in the Solnhofen Sea. The 56th Symposium of Vertebrate Palaeontology and Comparative Anatomy
  4. ^ Karl H-V, Gröning E, Brauckmann C, Schwarz D, Knötschke N.2006. The Late Jurassic crocodiles of the Langenberg near Oker, Lower Saxony (Germany), and description of related materials (with remarks on the history of quarrying the “Langenberg Limestone” and “Obernkirchen Sandstone”). Clausthaler Geowissenschaften 5: 59-77.
  5. ^ Billon-Bruyat J-P, Mazin J-M, Buffetaut E, Tong H, Abit D. 2001. New occurrence of vertebrate remains in the latest Jurassic of western France (Oléron island, Charente-Maritime). 6th European Workshop on Vertebrate Palaeontology - Florence and Montevarchi (Italy) - September 19–22, 2001 Abstract Booklet, p. 19