A Middle Eocene Haplorhine Frontal Bone From the Tornillo Basin of Texas, and Its Implications for the Phylogenetic Relationships of Rooneyia and Other Paleogene Primates

Objectives

Here we describe a well-preserved primate frontal bone (TMM 46513-1) recovered from Middle Eocene exposures of the Devil's Graveyard Formation in the Tornillo Basin of Texas. We also discuss the significance of frontal bone morphology for understanding early haplorhine phylogeny.

Materials and Methods

TMM 46513-1 was mechanically prepared, μCT scanned, and compared with a broad array of extant and fossil crown primates. Revised dates for the specimen were provided using ⁴⁰Ar/³⁹Ar geochronology. Dice-CT scans of Saguinus were used to investigate the contents of bony canals found within the frontal bones of many euarchontans.

Results

TMM 46513-1 resembles Rooneyia viejaensis in several key features, including: (1) the presence of a ventral flange on the lateral process of the frontal that intervenes between the posterosuperior orbit and temporal fossa, (2) the presence of a bony canal system (“orbitofrontal canal”) within the frontal that connects a foramen on the posterior aspect of the lateral process (“lateral process foramen”) with the superomedial orbit and the anterior cranial fossa, (3) a metopic suture that is unfused at its rostral end but obliterated at its caudal end, and (4) an anterior cranial fossa that overlaps the posteromedial portions of the orbits.

Conclusions

The lateral segment of the orbitofrontal canal and substantial ventral expansion of the lateral process are features restricted to the Haplorhini among crown primates. The morphological features shared by TMM 46513-1 and Rooneyia suggest that they may be stem haplorhines, but are less consistent with the hypothesis that Rooneyia is a stem anthropoid.