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Cranial morphology of the Carboniferous rhizodontidScrebinodus ornatus(Osteichthyes: Sarcopterygii)

2012/03/27 by Jonathan E. Jeffery · 2 citations
Earth and Planetary Sciences · Environmental Science · #Paleontology and Evolutionary Biology #Ichthyology and Marine Biology #Evolution and Paleontology Studies

paper · doi:10.1080/14772019.2011.595961

openalex publication_date 2012/03/27 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/29

Abstract

Well-preserved material is described of several specimens of Screbinodus ornatus, a small (approximately 1.5 metres long) rhizodontid sarcopterygian, from the Visean (Mississippian, Carboniferous) of Scotland. This species shows numerous ‘typical’ rhizodontid characteristics, such as post-parietals with a median ‘tail’, pectoral lepidotrichia with elongated basal segments, large symphysial tusks on the dentary and a ‘reverse’ overlap relationship between the cleithrum and clavicle. It also shows several characters unknown in other rhizodontids, such as the loss of the extratemporal and subopercular, and the probable exclusion of the postorbital from the orbital margin. A phylogenetic analysis finds that rhizodontids are the sister group to all other members of the tetrapod total group (with the exception of Kenichthys). This confirms that resemblances between derived rhizodontids and digited stem-tetrapods such as Acanthostega (noted by several previous authors) are due to convergence. A second analysis finds that Screbinodus is a derived rhizodontid, and part of a monophyletic Carboniferous radiation.

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