Platygonus cf. marplatensis Reig, 1952
publication ID |
https://doi.org/ 10.5194/fr-24-65-2021 |
persistent identifier |
https://treatment.plazi.org/id/03AB87E6-C41C-2E32-FF6E-6FA6FC55FC7C |
treatment provided by |
Felipe |
scientific name |
Platygonus cf. marplatensis Reig, 1952 |
status |
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Platygonus cf. marplatensis Reig, 1952
Material examined
Portion of vertical ramus of a left hemimandible with m3 partially preserved ( Selenogonus narinoensis Stirton, 1947 , holotype MGN 931 ( IGM p002118)) ( Fig. 1a, b View Figure 1 ) .
Occurrence
Dark-green fine-grained sandstone exposed in Cocha Verde, Toequerres highway, Tangua Municipality, Nariaeo Department, Colombia. Late Pliocene or Pleistocene (sic Stirton, 1947, p. 322) ( Fig. 2 View Figure 2 ).
Description
This mandible corresponds to a large specimen. It has a shallow but sharply outlined masseteric fossa and a deep internal temporal fossa. The angular process projects forward to the middle part of m3, and its lower edge is slightly projecting laterally outwards. The lower border of the horizontal ramus is sharply hooked (accentuated) distally. The mandibular condyle is located behind the posterior edge of the vertical mandibular ramus. The coronoid process ascends behind m3.
The lower molar 3 only preserves the distal pair of main cusps (hypoconid and entoconid) and the third lobe, which has a well-developed single cusp, and a pair of smaller accessory cusps both located labially and lingually. Despite its incompleteness, a mesodont and bunolophodont dental morphology is observed.
Measurements
See Table 1.
IGM |
Geological Institute, Mongolian Academy of Sciences |
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