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The imagery on this page is the basis for a paper entitled The anatomy of Herpetotherium cf. fugax COPE, 1873, a metatherian from the Oligocene of North America, by I. Horovitz, S. Ladevèze, C. Argot, T.E. Macrini, T. Martin, J.J. Hooker, C. Kurz, C. de Muizon, and M.R. Sánchez-Villagra (2008, Palaeontographica Abteilung A 284:109-141). The Summary is as follows:
The recent discovery of well preserved specimens of Herpetotherium cf. fugax Cope, 1873 in the Early Oligocene White River Formation of Wyoming has allowed a better understanding of its morphology, phylogenetic position, and locomotor adaptations. We describe in detail its enamel microstructure, petrosal morphology, cranial endocast, and postcranial skeleton.
The molar enamel consists of radial enamel with a thick layer of prismless external enamel which represents the plesiomorphic marsupial condition. Prisms describe a single turn from 45° to 0° inclination on their way from the enamel dentine junction (EDJ) to the outer enamel surface. Interprismatic matrix is oriented perpendicular to the EDJ. Enamel tubules occur within the prisms.
Many features of the auditory region of Herpetotherium highlight a close relationship with Marsupialia (understood as the crown group within Metatheria) and some characters clearly distinguish it from the ancestral condition of Marsupialia. The reconstruction of the osseous inner ear shows that Herpetotherium has less cochlear turns (and therefore is more primitive) than the hypothetical ancestor of Marsupialia. The bony labyrinth exhibits a peculiar feature of the lateral and posterior semicircular canals that form a second crus commune, as in certain basal marsupials.
The cranial endocast of Herpetotherium has relatively large olfactory bulb casts, relatively small and lissencephalic cerebral hemisphere casts, a relatively large cerebellar cast, and relatively large subarcuate fossae suggesting presence of large paraflocculi. It is unclear if a rhinal fissure was present on the endocast because the lateral surfaces are incomplete. Herpetotherium has a small endocranial volume relative to skull length in comparison to extant marsupials.
The articular relationship of astragalus and calcaneum is more primitive than in living marsupials, with the sustentacular facet of the calcaneum directed practically medially in its anterior end as in other basal metatherians excluded from crown group Marsupialia. In the latter, in contrast, this facet presents the derived condition of being directed dorsally.
The morphology of the hind limb suggests terrestrial locomotor habits. Some of these characters are a deep intertrochanteric fossa, a femur that is almost as deep as it is wide in its distal end, a sharp tibial crest, and a rather sagittally restricted upper ankle joint.
About the Species
This specimen was collected 18.4 meters above the Chadronian/Orellan North American Land Mammal Age Boundary (Eocene/Oligocene boundary), section 33, Township 32 North, Range 70 West in Wyoming. It was scanned using a Micro-CT-Scan RayScan 200 at the Fachhochschule Aalen, Arbeitsgruppe Metallguss, Germany. It was made available to DigiMorph by Dr. Ted Macrini of the American Museum of Natural History. Funding for additional image processing was provided by a National Science Foundation Digital Libraries Initiative grant to Dr. Timothy Rowe of The University of Texas at Austin. Endocast image processing by Ted Macrini and petrosal image processing by Thomas Schmelzle (Munich) and Sandrine Ladevèze (see Additional Imagery).
About this Specimen
The specimen was scanned using a Micro-CT-Scan RayScan 200 at the Fachhochschule Aalen, Arbeitsgruppe Metallguss, Germany. The interslice spacing is approximately 0.03197 mm and the interpixel spacing is 0.0331 mm.
About the Scan
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