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SOCIETY OF VERTEBRATE PALEONTOLOGY, MEMOIR 3<br />

FIGURE 30. Albertosaurus libratus. A, stereophotographs <strong>of</strong> left maxilla <strong>of</strong> RTMP 83.35.100 in lateral view. B, same in medial view. C,<br />

Interpretive drawing <strong>of</strong> A. Arrow points to the promaxillary fenestra concealed behind the ascending ramus. D, interpretive drawing <strong>of</strong> B. Arrow<br />

passes through the caudal fenestra in the maxillary antrum, between the postantral and interfenestral struts. E, drawing <strong>of</strong> the same specimen in<br />

oblique rostrodorsomedial view. Arrow at right passes from the antorbital cavity through the promaxillary fenestra into the promaxillary recess.<br />

Arrow at left passes through the caudal fenestra in the maxillary antrum. Curved arrows point into the interalveolar pneumatic recesses.<br />

internalization <strong>of</strong> the antorbital cavity. An isolated maxilla <strong>of</strong><br />

T. pusillus (BMNH 48260) has ample space for an internalized<br />

antorbital cavity between the lateral wall <strong>of</strong> the nasal cavity and<br />

the tooth-bearing portion. A maxillary groove was not observed<br />

in any more derived neosuchians, and its absence may correlate<br />

with complete closure <strong>of</strong> the external antorbital fenestra.<br />

Goniopholidids have an unusual feature aptly termed the<br />

"maxillary depression" by Buffetaut (1982, 1986). In Goniopholis<br />

sirnus (BMNH 41098), this depression is completely<br />

within the maxilla, just dorsal to the tooth row, and, although<br />

somewhat subdivided by two low septae, does not open medially.<br />

Buffetaut (1982) identified a small foramen between the<br />

lacrimal and maxilla in this specimen and in Eutretauranosuchus<br />

delfsi that he regarded as the antorbital fenestra. Although<br />

he suggested that the foramen was associated with the maxillary<br />

depression, I could not confirm the presence <strong>of</strong> this foramen in<br />

BMNH 41098, and it is not clear how such a foramen would<br />

relate to the depression. In any case, the maxillary depression<br />

is an unusual feature <strong>of</strong> problematic function.<br />

All higher neosuchians (i.e., Dyrosauridae, Bernissartia fagesii,<br />

Eusuchia) have completely closed the external antorbital<br />

fenestra (Norell and Clark, 1990). Given their similarity to extant<br />

eusuchians, the extinct higher neosuchians presumably internalized<br />

the antorbital cavity in a similar manner, although<br />

appropriate material was not available to confirm this for all<br />

taxa.<br />

Conclusions<br />

Having examined in detail all <strong>of</strong> the major clades <strong>of</strong> archosaurs,<br />

it is possible to infer the presence <strong>of</strong> an epithelial air sac<br />

within the antorbital cavities <strong>of</strong> all Archosauria with very little<br />

speculation (a level I inference). Whereas previous hypotheses<br />

failed to implicate the antorbital fenestrae and fossa in housing<br />

a gland or jaw muscle, these bony structures are, in fact, inti-<br />

mately (almost certainly causally) related to the presence <strong>of</strong> an<br />

epithelial air sac. In other words, all <strong>of</strong> the osteological correlates<br />

<strong>of</strong> the air sinus that were observed in extant birds and<br />

crocodilians (the extant phylogenetic bracket) were observed in<br />

virtually all clades <strong>of</strong> extinct archosaurs. For example, the internal<br />

antorbital fenestra is the bony aperture through which the<br />

epithelial diverticulum passes. The antorbital fossae are pneumatic<br />

fossae excavated by the air sac. The external antorbital<br />

fenestra develops as a fontanelle around the paranasal air sac.<br />

Thus the original hypothesis survives the congruence test, and<br />

the avian antorbital sinus is indeed homologous to the caviconchal<br />

sinus <strong>of</strong> crocodilians. Therefore, given that the osteological<br />

correlates are indeed causally associated with the air sac, all<br />

extinct archosaurs possessed a homologous paranasal air sinus,<br />

unless it was apomorphically lost. The term developed for birds<br />

for the epithelial diverticulum-the antorbital sinus (Witmer,<br />

1987b, 1990)-may be applied to all archosaurs, reserving the<br />

designation "antorbital cavity" for the bony space (Witmer,<br />

1994).<br />

Given the above conclusions, closure <strong>of</strong> the external antorbital<br />

fenestra is a derived condition. Although a large antorbital<br />

cavity and a prominent external fenestra remain important features<br />

<strong>of</strong> Archosauria as a whole, the external antorbital fenestra<br />

independently closes in at least ten different clades: a number<br />

<strong>of</strong> crocodylomorphs clades, a few birds (e.g., some owls), Stegosauridae,<br />

Ankylosauria, Hadrosauridae, most Pachycephalosauria,<br />

Psittacosauridae, some Ceratopsidae. In almost all <strong>of</strong><br />

these taxa, there is evidence that the antorbital cavity is still<br />

present, just internalized.<br />

ACCESSORY CAVITIES AS COMPELLING<br />

MORPHOLOGICAL EVIDENCE FOR<br />

PARANASAL PNEUMATICITY<br />

Accessory cavities are recesses located in the bones surrounding<br />

the antorbital cavity (e.g., lacrimal, maxilla, nasal,

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