Archaeothyris

Description

Archaeothyris was 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 size & shape, it did possess a pair of enlarged canines, suggesting that it was a carnivore.

''Archaeothyris'''s legs were articulated laterally at its pelvis and shoulders, which gave it a sprawling stance. The first toe is smaller than the second.

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 includes mammals).

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

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). Nova Scotia at this time was a coal forest. The "trees" (actually giant club mosses) were very tall, some, such as Lepidodendron, up to 50 m tall. Archaeothyris and the other early amniotes lived in the moist vegetation on the forest ground, together with the more terrestrially adapted labyrinthodont amphibians.

References

References

1. Reisz, R., 1972. [https://www.researchgate.net/publication/38430531_Pelycosaurian_reptiles_from_the_Middle_Pennsylvanian_of_North_America Pelycosaurian reptiles from the middle Pennsylvanian of North America. Harvard University].
2. Reisz, R., 1972. [https://www.researchgate.net/publication/38430531_Pelycosaurian_reptiles_from_the_Middle_Pennsylvanian_of_North_America Pelycosaurian reptiles from the middle Pennsylvanian of North America. Harvard University].
3. 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. [http://findarticles.com/p/articles/mi_qa3721/is_200711/ai_n21137484/?tag=content;col1 article]
4. "Archaeothyris florensis".
5. (1999). "The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals". Marshall Editions.
6. Benson, R.J.. (2012). "Interrelationships of basal synapsids: cranial and postcranial morphological partitions suggest different topologies". Journal of Systematic Palaeontology.
7. 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