Platychoerops richardsoni
Platychoerops richardsoni
Summary
Platychoerops richardsoni was one of the largest known plesiadapids, a group of Palaeogene euarchontan mammals close to the broader primate radiation but not equivalent to modern primates. Its dentition had moved well beyond a simple insect-eating pattern: the premolars became strongly molar-like and the cheek teeth developed tall relief, numerous crests and crenulated enamel, greatly increasing the area available for breaking down plant food.
That dental architecture points to a predominantly herbivorous animal. The strongly crested molars are consistent with substantial leaf processing, while fruit and other plant tissues may also have formed part of the diet; these are functional inferences from the teeth. The enlarged anterior incisor would have been important in acquiring or cropping food, giving the animal a feeding apparatus unlike that of any living primate.
The London Clay type is an incomplete palate preserving upper P4 and molars, and the species is known chiefly through cranial and dental material. Its postcranial anatomy is too poorly documented to state confidently whether P. richardsoni itself was arboreal, scansorial or mainly terrestrial, even though arboreal habits occur elsewhere among plesiadapiforms.
Quick Identification
Look for: a comparatively large plesiadapid cheek tooth with a high-relief, strongly crested crown and crenulated enamel; where a premolar is present, P4/p4 is unusually molar-like rather than simple and pointed. In a lower p4, check for a distinct paraconid, a metaconid nearly as large as the protoconid and a clear trigonid basin. Size and the full cusp pattern still need specialist comparison for a species-level identification.
Diagnostic Features
- The cheek teeth are very large for a plesiadapid; P. richardsoni is significantly larger dentally than P. daubrei.
- The lower p4 is strongly molarised and reaches at least about 80% of the occlusal area of m2.
- Lower p4 bears a distinct molar-like paraconid rather than a simple premolar cutting cusp.
- On p4 the metaconid approaches the protoconid in size and the two help enclose a distinct trigonid basin.
- Upper P4 has at least an incipient molar-type paraconule, while the molars have high crown relief and distinctly crenulated enamel.
Fossil Details
Recorded Fossil Sites
No fossil-site occurrences have yet been recorded for this species.
References
- Boyer, D. M.; Costeur, L.; Lipman, Y. (2012). Earliest record of Platychoerops (Primates, Plesiadapidae), a new species from Mouras Quarry, Mont de Berru, France. American Journal of Physical Anthropology, 149(3), 329–346 View reference
- Gingerich, P. D. (1976). Cranial Anatomy and Evolution of Early Tertiary Plesiadapidae (Mammalia, Primates). University of Michigan Papers on Paleontology, 15, 1–141. Museum of Paleontology, The University of Michigan View reference
- Lydekker, R. (1885). Note on the Generic Identity of the Genus Esthonyx, Cope, with Platychoerops, Charlesworth (=Miolophus, Owen). Geological Magazine, 2(8), 360–361 View reference
- Silcox, M. T.; Bloch, J. I.; Boyer, D. M.; Chester, S. G. B.; López-Torres, S. (2017). The evolutionary radiation of plesiadapiforms. Evolutionary Anthropology, 26(2), 74–94 View reference
- Smith, T.; Smith, R. (2003). Terrestrial mammals as biostratigraphic indicators in upper Paleocene–lower Eocene marine deposits of the southern North Sea Basin. Causes and Consequences of Globally Warm Climates in the Early Paleogene, 513–520. Geological Society of America, Boulder, Colorado View reference