Cacops

C. woehri holotype

Cacops aspidephorus is the most famous dissorophid, in part due to a majority of its skeleton having been known for over a century.[1] Over 50 specimens have been found in the Cacops Bone Bed in Baylor County, Texas,[1] which is now flooded by the dammed Lake Kemp.[6] However, many of the specimens are covered in calcite, which penetrates the bone tissue, resulting in poor preservation.[3] "Trematopsis seltini" from the Vale Formation of Texas was originally described as a trematopid by Olson (1956)[7] but was later synonymized with Cacops aspidephorus by Milner (1985).[8]

Cacops morrisi is named in honor of Tony Morris, who discovered one of its two specimens.[3] Many specimens have been found in the Dolese Brothers Limestone Quarry, near Richards Spur, Oklahoma.[5] Cacops morrisi has a skull that differs from C. aspidephorus in having a snout that is slightly longer than its post-orbital region, a shorter distance between the orbit and the temporal emargination, and uncinate processes of the ribs.[3][5]

Cacops woehri is named in honor of Daniel Woehr, who is an amateur collector of fossils. Specimens have been found in the Dolese Brothers Limestone Quarry, near Richards Spur, Oklahoma.[2][4] Cacops woehri differs from C. aspidephorus and C. morrisi in many attributes, including a more shallow skull, more dorsally located orbits, and a narrow opening of its tympanic embayment. The contribution of the postparietals to the skull roof also appears to be shorter in C. woehri than in C. morrisi, while the occipital flanges are proportionately larger in C. woehri. More notable differences distinguishable from C. morrisi include: absence of lateral exposure of ectopterygoid in juveniles, absence of tusk-like teeth on the anterior margin of the interpterygoid vacuities, and the quadratojugal lacking an anterior process.[2] The teeth of C. woehri are also not recurved as in C. aspidephorus and C. morrisi, showing instead a distinct lingual curvature. Because of the different skull shape, it is theorized that this specific taxon may have had a different ecology than its sister taxa, possibly with a different prey spectrum.[2] This suggests that there could have been different functional demands for the dissorophoids found at the Oklahoma locality.[4]

Restoration of C. aspidephorus

American paleontologist Samuel W. Williston used the details of the species Cacops aspidephorus to first describe its features.[1] He noted: "The creature as mounted presents an almost absurd appearance, with its large head and pectoral region, absence of neck, and short tail" (pg. 279), reflected in the name Cacops (from Greek kakos "bad, ugly" and ops "face, look"). 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.[2][3][5][4] Features that distinguish Cacops from other dissorophids include a large dorsal process of the quadrate and a shortened posterior skull.[9]

The skull is very box-like and its cheeks aligned almost at a right angle to the skull table. The external cranial ornamentation 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. 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. Cacops has fewer, but larger, teeth than in most other dissorophids.[5] The palatal dentition consists of recurved tusks larger than the marginal teeth and minute, strongly recurved teeth that cover most of the palatal surface.[3]

Cacops was a medium-sized dissorophid, being smaller than later dissorophids from Eurasia such as Kamacops. Like other dissorophids, Cacops had osteoderms associated with the vertebral column. Internal osteoderms are fused to the neural spines, while external osteoderms overlapped adjacent positions with a ventral flange that inserted between successive internal osteoderms.[10][11] The osteoderms are associated with only the first 15 vertebrae, beginning at the axis. They are relatively narrow, especially posteriorly, and are subrectangular in dorsal profile, except for the first osteoderm which is more triangular.[5] The osteoderms also have dermal pitting on their dorsal surfaces. 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.