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WITMER-ANTORBITAL CAVITY OF ARCHOSAURS<br />

max<br />

vom<br />

lat<br />

FIGURE 15. Osteological correlates <strong>of</strong> paranasal pneumaticity. A, Aquila chrysaetos (golden eagle), skull in left lateral (top) and ventral (bottom)<br />

views. B, Alligator mississippiensis, horizontally sectioned skull in dorsal view. Arrows show the course or position <strong>of</strong> pneumatic diverticula.<br />

Shaded structure shows the position <strong>of</strong> the nasolacrimal duct. (B modified from Witmer, 1995b.)<br />

the margin <strong>of</strong> the external antorbital fenestra, <strong>of</strong>ten excavating<br />

a fossa-on the maxilla and lacrimal (Figs. 6B, 15A). A few<br />

avian clades (e.g., owls) have extensive contact between the<br />

maxilla and lacrimal, obliterating the external fenestra (except<br />

the dorsal passage for the nasolacrimal duct) and enclosing the<br />

antorbital sinus. In adult crocodilians, there is no external antorbital<br />

fenestra and hence no comparable fossa. In birds, the<br />

external antorbital fenestra forms morphogenetically as a fontanelle<br />

that never closes (rather than as a hole that opens up<br />

during ontogeny; Witmer, 1995b). The fontanelle <strong>of</strong> embryonic<br />

crocodilians likewise is associated with the air sac and may be<br />

homologized with the external antorbital fenestra, although I<br />

hesitate to apply the latter term as the fontanelle never has the<br />

finished edges <strong>of</strong> a true fenestra.<br />

With regard to the internal antorbital fenestra, birds have an<br />

irregular &d variable opening. Some birds (e.g., Anser anser)<br />

have such a large maxillary contribution that much <strong>of</strong> the medial<br />

wall <strong>of</strong> the antorbital cavity is bony, but, in many other<br />

birds, the maxilla is small and most <strong>of</strong> the internal antorbital<br />

fenestra is closed by the cartilage <strong>of</strong> the nasal capsule. In crocodilians,<br />

the maxillary contribution to the medial wall <strong>of</strong> the<br />

cavity is virtually complete in the comparable (i.e., prechoanal)<br />

region (Fig. 15). Thus, in crocodilians, the internal antorbital<br />

fenestra is small and represented by at least part <strong>of</strong> the aperture<br />

within the maxilla leading to the caviconchal recess and by the<br />

tip <strong>of</strong> the lacrimal. In both clades <strong>of</strong> extant archosaurs, the only<br />

structure that passes through the internal antorbital fenestra is<br />

the pneumatic diverticulum, and, because the internal fenestra<br />

is partially occluded by the nasal cartilages, it is larger in area<br />

than the sinus ostium itself.<br />

The Hypothesis<br />

Based on the correspondences in s<strong>of</strong>t and hard anatomical<br />

attributes in the EPB, we may hypothesize that the bracket ancestor<br />

had a large paranasal air sac with the following characteristics:<br />

(1) it passed laterally from the nasal cavity through<br />

the internal antorbital fenestra to occupy a bony cavity bounded<br />

by primarily the lacrimal, palatine, and especially maxilla; (2)<br />

it excavated fossae within the maxilla; (3) the opening to the<br />

air sac (i.e., the internal antorbital fenestra) was located directly<br />

opposite the primary choana (Osmblska, 1985); (4) the nasolacrimal<br />

canal passed dorsomedially over the air sac; and (5)<br />

the air sac is associated,with the external antorbital fenestra<br />

(based on the presence <strong>of</strong> the latter in birds and the fonticulus<br />

antorbitalis in embryonic crocodilians).<br />

Testing the Hypothesis<br />

Testing will begin with fossil birds, progressing down the<br />

cladogram toward the root and then up again toward crocodilians.<br />

Dinosauria: Theropoda-Previous studies <strong>of</strong> the early evolution<br />

<strong>of</strong> facial pneumaticity in birds suggested that the osteological<br />

correlates <strong>of</strong> the antorbital sinus were present in the<br />

Mesozoic birds Archaeopteryx lithographica, Hesperornis regalis,<br />

Parahesperornis alexi, and Gobipteryx minuta (Witmer<br />

and Martin, 1987; Witmer, 1990). The antorbital cavity <strong>of</strong> hesperornithids<br />

is remarkably modem, and there is good evidence<br />

for maxillary and lacrimal diverticula <strong>of</strong> the antorbital sinus<br />

(KUVP 71012, 2287, YPM 1206, LACM 128317; Fig. 16A;<br />

see Witmer, 1990 for details). The choana was directly opposite

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