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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