Summary

Linda Trueb Cranial Osteology of the Hylid Frog…

The pseudobasal process abruptly increases in size. At the level of the prootic foramen (Fig. 16) the medial branch of the pterygoid diverges from the posterior ramus and is closely applied to the medial surface of the pseudobasal process. The otic process extends along the medial surface of the squamosal from the dorsolateral edge of the pseudobasal process, and then expands medially to meet the bony edge of the otic capsule and form the crista parotica.
Source: Gutenberg

Linda Trueb Cranial Osteology of the Hylid Frog…

Compared to hylids not having integumentary-cranial co-ossification, the dermal roofing bones of Smilisca baudini are extensive, and the skull is well-ossified internally. In contrast to most casque-headed hylids (those having integumentary-cranial co-ossification) , the dermal roofing bones are much less extensive, the dermal sphenethmoid (see Trueb, 1966, p. 563) is absent, and internal ossification is less extensive.
2. The solum nasi is not ossified; the septum nasi is ossified only posteriorly, and the olfactory eminence is supported by the cartilaginous solum nasi and the bony prevomer.
Source: Gutenberg

Linda Trueb Cranial Osteology of the Hylid Frog…

Posteriorly the cartilage is associated with the pterygoid, where it is known as the pterygoid process (pter. proc., Fig. 14) .
Planum antorbitale.—The anterior terminus of the planum antorbitale (pla. ant.) lies medial to the ventrolateral part of the nasal and lateral to the internal nares (Fig. 12) . It abruptly expands dorsally along the medial face of the nasal to join the tectum nasi dorsolaterally; somewhat posteriorly the planum antorbitale joins [Pg 22] the anterior maxillary process ventrally at the posterior margin of the internal nares.
Source: Gutenberg

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