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ABSTRACT The morphology of the petrosal is often employed in mammalian systematics, yet this bone has not been described in detail for a comparative sample of extinct members of Suoidea (the clade encompassing pigs, peccaries and their... more
ABSTRACT The morphology of the petrosal is often employed in mammalian systematics, yet this bone has not been described in detail for a comparative sample of extinct members of Suoidea (the clade encompassing pigs, peccaries and their extinct relatives), a total clade that represents one of the major divisions within Artiodactyla. Here, the petrosal osteology of fossil Suoidea ranging from their early representatives (Late Eocene) up to Late Miocene is described. A sample of petrosal specimens documenting eight genera from the four suoid families (Suidae, Tayassuidae, Sanitheriidae and Palaeochoeridae) has been collected from in situ mechanical preparation, CT-based reconstruction or identification of isolated petrosals. The diagnostic significance of petrosal characters for suoid systematics is assessed by the inclusion of the new petrosals data in a phylogenetic analysis. As in other mammal groups, petrosal characters are shown to be of primary phylogenetic interest. The monophyly of the included families and subfamilies shown by craniodental and postcranial characters is supported by petrosal characters, and the problematic New World suoid Perchoerus is interpreted as the first offshoot of the Suoidea clade. This work allows definition of Suoidea on the basis of petrosal morphological characters and reveals the shaping over time of the peculiar petrosal morphology observed in extant suoids, notably the drastic reduction of the mastoid of this ‘amastoidean’ group, convergently present in hippos.
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... The forehead is broad; the sus orbitari sulci are wide, deep and converge sharply. They originate from deep supra orbital fo-ramina, situated close to the sagittal plane in a posterior position (midline of the orbit's... more
... The forehead is broad; the sus orbitari sulci are wide, deep and converge sharply. They originate from deep supra orbital fo-ramina, situated close to the sagittal plane in a posterior position (midline of the orbit's upper margin). The frontal is thick and domed (Fig. 2B). ...
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Research Interests: Geology and South West
Abstract A new Scolebythidae Eobythus patriciae gen. nov., sp. nov. is described from the Lowermost Eocene amber of the Oise Valley (France). A first attempt at a phylogenetic analysis suggests that the fossil genera Eobythus gen. nov.... more
Abstract A new Scolebythidae Eobythus patriciae gen. nov., sp. nov. is described from the Lowermost Eocene amber of the Oise Valley (France). A first attempt at a phylogenetic analysis suggests that the fossil genera Eobythus gen. nov. and Libanobythus Prentice et ...