Fossil range: Early Permian
Cacops aspidephorus skeleton.
Scientific classification



(Unranked) :









  • C. aspidephorus

Cacops is an extinct genus of dissorophid amphibians that is known from the Early Permian of Texas. It was about 40 cm (16 inches) long, with a heavily built skull and an enormous otic notch enclosed with a bony bar; indicating an enormous eardrum. Edwin Colbert suggests that perhaps it was a nocturnal animal like modern frogs. The body was short, and the back was protected by a double row of armour plates. The legs were strong and indicate a terrestrial animal, and the tail was short.


American paleontologist Samuel Wendell Williston used the details of the species Cacops aspidephorus to first describe its features. However, because of the poor preservation of specimens collected from the Cacops Bone Bed in Texas, other researchers who collected specimens from other localities have described many of Cacops’ features with more certainty.


The skull is very box-like and its cheeks aligned almost at a right angle to the skull table. The external cranial ornament is noticeable on the skull table and on top of the ridges that border the numerous depressions. One significant ontogenetic change in Cacops is a more evenly distributed ornamentation in the adults. Another important feature of the skull is the tip of the snout, which has a teardrop shaped internarial fontanelle, evident in both adult and juvenile specimens.[5] Like other dissorophids, the temporal region of Cacops’ skull was dominated by the tympanic embayment, which likely housed a large tympanum. Marginal teeth are recurved and thinner than in other temnospondyls. The palatal dentition consists both of recurved tusks larger than the marginal teeth and strong recurved teeth that cover most of the palatal surface.

Vertebra and OsteodermsEdit

Cacops was about 40 cm long. There is a change in shape and height of the presacral neural spine as you proceed posteriorly along the vertebral column. There are two sacral vertebrae and the pleurocentrum of the first sacral vertebrae is noticeably smaller that the rest. All internal osteoderms are fused to the neural spines.[5][6] The osteoderms are associated with only the first 15 vertebrae, beginning at the axis. The lateral margin of each osteoderm can either be bluntly pointed or rounded. The osteoderms also have dermal pitting, each varying in size and depth. The distributions of these pits are not random, but rather found along the raised edges of the midsagittal groove and often in the groove as well. The ventral surface of both series of osteoderms does not have either grooves or pitting.


References Edit

  • Colbert, E. H., (1969), Evolution of the Vertebrates, John Wiley & Sons Inc (2nd ed.)
Mantell's Iguanodon restoration

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