Sclerocephalus

Sclerocephalus is an extinct genus of temnospondyl amphibian from the lowermost Permian of Germany with four valid species, including the type species "S. haeuseri". It is one of the most completely preserved and most abundant Palaeozoic tetrapods. "Sclerocephalus" was once thought to be closely related to eryopoid temnospondyls, but it is now thought to be more closely related to archegosauroids. It is the only genus in the family Sclerocephalidae.
Description and lifestyle.
The adults animals reached a body length of ca. 150 cm, and had an elongate trunk and a laterally compressed tail. In some specimens lateral line sulci are retained. These body features suggest an aquatic mode of life, with aquatic larvae that probably breathed with external gills like modern tadpoles, while the adults breathed with lungs. "Sclerocephalus" underwent significant changes during its ontogeny, for example the eyes are much larger and the tail much longer in larvae than in adults. The latest revision, redescription and phylogenetic study of this genus was provided by Schoch & Witzmann (2009).
"Sclerocephalus" was often classified within the deprecated paraphyletic taxa Stegocephalia and Labyrinthodontia, because of a skull that was connected to the shoulder girdle and teeth of labyrinthodont type. The skull had a distinct pineal foramen. Besides the usual row of teeth in the upper and lower jaw, "Sclerocephalus" also had three additional pairs of palatine teeth. From specimens with fossilized stomach content we know the adults mainly fed on fish of the genus "Paramblypterus", but sometimes also on other amphibians (Branchiosaurus, "Micromelerpeton") and even small conspecifics.
Discovery.
The holotype of "Sclerocephalus haeuseri" was described 1847 by the German paleontologist Georg August Goldfuss, who misidentified the fossil as skull of a fish. The famous American vertebrate paleontologist Alfred Romer recognized in 1939 that the fossil amphibians described as "Leptorophus levis" are the larvae of "Sclerocephalus". The most important modern research on "Sclerocephalus" was published by Boy (1988) and Schoch (2000, 2002, 2003, 2009).
A famous locality that yielded numerous excellently preserved fossils of "Sclerocephalus" is Odernheim am Glan in Rhineland-Palatinate (Germany), where the Permian sediments of the Rotliegend have even been named "Stegocephalenkalke" (= Stegocephalia limestones).
Taxonomy.
Krätschmer (2004) questioned the validity of the type species "Sclerocephalus haeuseri", of which the holotype is lost, and considered "Pfarrwaldia jeckenbachensis" as valid name for the neotype designated by Boy (1988). This was refuted in the revision of Schoch & Witzmann (2009), who considered "P. jeckenbachensis" as younger synonym of "S. haeuseri".
The following four species are recognized as valid by Schoch & Witzmann (2009):
Phylogeny.
The phylogenetic relationships of "Sclerocephalus" are uncertain. It was traditionally considered a close relative of the genus "Onchiodon", and both were placed in the family Actinodontidae. Actinodontidae was thought to be closely related to the family Eryopidae, and is now considered a synonym of that group. However, while "Sclerocephalus" shares some similarities with eryopids, it also shares much in common with a group of large-bodied, semiaquatic temnospondyls called Stereospondylomorpha. "Sclerocephalus" and "Onchiodon" are no longer thought to be closely related, and while "Onchiodon" remains a close relative of eryopids, "Sclerocephalus" is often grouped near the genus "Archegosaurus" as a basal stereospondylomorph.
The most commonly accepted phylogeny of temnospondyls (first proposed by Yates and Warren [2000]) divides the group into two different branches called Limnarchia and Euskelia. Limnarchia is a diverse Mesozoic clade that includes Stereospondylomorpha. Euskelia is a smaller Paleozoic clade that includes Eryopidae and the group Dissorophoidea, which may have given rise to modern amphibians. An earlier phylogeny proposed by Boy (1990) takes a different view, combining Eryopidae and Stereospondylomorpha into the group Eryopoidea, with dissorophoids as distant relatives. If this phylogeny is correct, "Sclerocephalus" would be a basal member of Eryopoidea, close to the ancestry of most other stereospondylomorphs.
Schoch & Witzmann (2009) found support for the Eryopoidea clade. They included "Sclerocephalus" in their phylogenetic analysis and found it to nest at the base of Stereospondylomorpha. Below is a cladogram from their study: