Hispanodorcas orientalis Bouvrain and Bonis, 1988
publication ID |
https://doi.org/ 10.4202/app.2011.0013 |
persistent identifier |
https://treatment.plazi.org/id/060F2E7D-8F7D-7B64-0072-D450FC44942A |
treatment provided by |
Felipe |
scientific name |
Hispanodorcas orientalis Bouvrain and Bonis, 1988 |
status |
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Hispanodorcas orientalis Bouvrain and Bonis, 1988
Fig. 2 View Fig .
Holotype: partial skull with horncores and associated parts of maxillae and mandible, LGPUT DKO−4 ( Fig. 2 View Fig ; Bouvrain and Bonis 1988: figs. 1, 2).
Type locality: Dytiko−3, Axios Valley, Greece.
Type horizon: Late Turolian (MN13; Koufos 2006), Late Miocene.
Diagnosis.—As in Bouvrain and Bonis (1988).
Differential diagnosis.— H. orientalis differs from other members of the genus in its slightly smaller size, as well as its more transversely compressed and more strongly distally diverging horncores, with the latter bearing a blunt anterior keel ( Fig. 2 View Fig ). It additionally differs from H. torrubiae in having shorter horncores without transverse ridges.
Remarks.—Contrary to Bouvrain and Bonis (1988), I suggest that the anterior surface of the horncore of H. orientalis is marked by a moderately developed, proximally blunt and anteromedially descending keel ( Fig. 2B View Fig ). The lateral groove on the horncore of H. orientalis is much less developed than in the holotype of H. torrubiae , appearing only on the proximal third of the horncore as part of the characteristic shallow depression developed along the entire anterolateral surface ( Bouvrain and Bonis 1988: figs. 1, 2; Fig. 2A View Fig ). The upper third of the posterior surface of the horncore of H. orientalis shows a rather deep, longitudinal furrow with sharp, keel−like edges, similar to the condition seen in H. torrubiae ( Thomas et al. 1982: 214) .
Geographic and stratigraphic range.—Late Turolian (Late
Miocene) of Greece.
LGPUT |
Laboratory of Geology and Palaeontology |
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