Archaeothyris

Archaeothyris
Temporal range: Late Carboniferous, 306 Ma
↓
Life restoration of Archaeothyris
Scientific classification
Kingdom:Animalia
Phylum:Chordata
Family:†Ophiacodontidae
Genus:†Archaeothyris
Reisz, 1972
Type species
†Archaeothyris florensis
Reisz, 1972

Archaeothyris is an extinct genus of ophiacodontid synapsids that lived during the Late Carboniferous and is known from Nova Scotia. Dated to 306 million years ago, Archaeothyris, along with a more poorly known synapsid called Echinerpeton, are the oldest undisputed synapsids known.[1] Protoclepsydrops also from Nova Scotia is slightly older but is known by very fragmentary materials.[2]

Archaeothyris florensis

Description

Skull reconstruction of A. florensis

Archaeothyris was also more advanced than the early sauropsids, having strong jaws that could open wider than those of the early reptiles. While its sharp teeth were all of the same shape, it did possess a pair of enlarged canines, suggesting that it was a carnivore.[3]

Classification

Archaeothyris belonged to the family Ophiacodontidae, a group of early pelycosaurs that evolved early in the Late Carboniferous. It was one of the earliest and most basal synapsids (the group which include mammals).

Below is a cladogram modified from the analysis of Benson (2012):[4]

 

 

Tseajaia campi

 
 

Limnoscelis paludis

 
Amniota

 

 

Captorhinus spp.

 
 

Protorothyris archeri

 
 
Synapsida

 

 

Caseasauria

 
 

 

Ianthodon schultzei

 
 

 

Edaphosauridae

 
 

Sphenacodontia

 
 
 
 
 

 

Varanopidae

 
Ophiacodontidae

 

Archaeothyris florensis

 
 

 

Varanosaurus acutirostris

 
 

 

Ophiacodon spp.

 
 

Stereophallodon ciscoensis

 
 
 
 
 
 
 
 

Discovery and paleoecology

Fossils of Archaeothyris were first described in 1972 from the Joggins fossil cliffs, the same locality in which the early reptiles Hylonomus and Petrolacosaurus (both of which resemble Archaeothyris) were found.

Archaeothyris lived in what is now Nova Scotia, about 306 million years ago in the Carboniferous Period (Pennsylvanian).[5] Nova Scotia at this time was a swamp, similar to today's Everglades in Florida. The "trees" (actually giant club mosses) were very tall, some, such as Lepidodendron, up to 50 metres (164 ft) tall. Archaeothyris and the other early amniotes lived in the moist vegetation on the forest ground, together with the more terrestrially adapted labyrinthodont amphibians.

See also

References

  1. ↑ Falcon-Lang, H.J., Benton, M.J. & Stimson, M. (2007): Ecology of early reptiles inferred from Lower Pennsylvanian trackways. Journal of the Geological Society, London, 164; no. 6; pp 1113-1118. article
  2. ↑ "Archaeothyris florensis". Palaeocritti. Retrieved 13 December 2014.
  3. ↑ Palmer, D., ed. (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. p. 186. ISBN 1-84028-152-9.
  4. ↑ Benson, R.J. (2012). "Interrelationships of basal synapsids: cranial and postcranial morphological partitions suggest different topologies". Journal of Systematic Palaeontology. in press (4): 601. doi:10.1080/14772019.2011.631042.
  5. ↑ Hess J.C., Lippolt H.J. (1986): 40Ar/39Ar ages of tonstein and tuff sanidines: new calibration points for the improvement of the Upper Carboniferous time scale. Chem Geol no 59: pp 143–154

Further reading

  • Kemp, T. S. (2005). The Origin & Evolution of Mammals. Oxford: Oxford University Press. ISBN 0-19-850761-5.
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