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IVITMER-ANTORBITAL<br />

Pseudhesperosuchus jachaleri) diverted the primary choana<br />

caudally. Because <strong>of</strong> the fundamental morphogenetic relationship<br />

between the primary choana and antorbital sinus (discussed<br />

above; see also Witmer, 1995b), the entire system shifted<br />

caudally where, encroaching on the orbit and its contents, there<br />

simply was less space available for the antorbital cavity; in<br />

other words, it was constrained by "packing" phenomena. It<br />

turns out, however, that formation <strong>of</strong> a nasopharyngeal duct in<br />

mesoeucrocodilians seems to have had virtually no effect on<br />

the subsequent reduction or enclosure <strong>of</strong> the antorbital cavity,<br />

because forms such as Notosuchus terrestris, Uruguaysuchus<br />

aznarezi, and Araripesuchus gomesii retain an antorbital cavity<br />

similar to that <strong>of</strong> protosuchians. This situation probably results<br />

because the development <strong>of</strong> a nasopharyngeal duct involves the<br />

presence and position <strong>of</strong> the secondary choana, not the primary<br />

choana (Witmer, 1995b); the primary choana (i.e., the rostra1<br />

end <strong>of</strong> the duct) had not moved relative to the antorbital cavity.<br />

In fact, all this is further evidence affirming the causal relationship<br />

<strong>of</strong> primary choana and antorbital sinus.<br />

So, if the initial reduction <strong>of</strong> the antorbital cavity perhaps has<br />

its causal basis in the evolution <strong>of</strong> palatal processes <strong>of</strong> the maxilla,<br />

what factors are involved in the ultimate reduction <strong>of</strong> the<br />

cavity? As discussed earlier, extreme reduction and closure <strong>of</strong><br />

the external antorbital fenestra occurs multiple times in Crocodylomorpha:<br />

once or twice in Thalattosuchia, at least once or<br />

twice among basal metasuchians, and at least once or twice in<br />

Neosuchia. Concomitant internalization <strong>of</strong> the antorbital cavity<br />

occurred clearly at least twice: at least once in Thalattosuchia<br />

and at least once in Neosuchia. In most <strong>of</strong> these cases, closure<br />

<strong>of</strong> the external fenestra can be shown to be associated with<br />

apomorphic flattening <strong>of</strong> the snout. Skull flattening, the other<br />

imuortant concurrent trend mentioned above, has been well<br />

documented by Langston (1973) and especially Busbey (1995).<br />

The biomechanical consequences <strong>of</strong> dorsoventral flattening<br />

are considerable. Flattening the snout (Fig. 38B) moves it away<br />

from the design optimum <strong>of</strong> a cylinder (Fig. 38A), potentially<br />

making it less competent to resist sagittal bending and torsional<br />

loads (Witmer, 1992b). Busbey's (1995) elegant functional analysis<br />

<strong>of</strong> the trend from oreinirostral (tall-snouted) sphenosuchians<br />

and protosuchians to platyrostral (flat-snouted) neosuchians<br />

confirmed these mechanical sequelae and suggested mechanisms<br />

to resist these stresses. In particular, Busbey (1995) noted<br />

that platyrostral taxa show increased cross-sectional area <strong>of</strong><br />

bone through (1) thickening <strong>of</strong> the bones and (2) the development<br />

<strong>of</strong> a secondary palate (interestingly, even an incomplete<br />

secondary palate has biomechanical benefits). Furthermore,<br />

Busbey (1995) was correct in noting that platyrostral skulls<br />

loaded in sagittal bending exhibit stress concentrations at the<br />

caudal end <strong>of</strong> the snout, just in front <strong>of</strong> the orbits. These stress<br />

concentrations are in precisely the position <strong>of</strong> the external antorbital<br />

fenestrae. Therefore, an external fenestra severely decreases<br />

the ability <strong>of</strong> the snout to resist these torsional and<br />

especially sagittal loads, because such a gap or discontinuity<br />

would produce a so-called "open section" (Fig. 38B). In fact,<br />

it would result in the coincidence <strong>of</strong> an open section and a stress<br />

concentration-a potentially catastrophic design. Therefore, I<br />

would suggest (see also Witmer, 1992b) that the ultimate closure<br />

<strong>of</strong> the external fenestra is causally linked to platyrostry as<br />

another mechanism to increase cross-sectional area <strong>of</strong> bone.<br />

Thus, in light <strong>of</strong> the epithelial hypothesis for the function <strong>of</strong><br />

pneumaticity, the evolutionary trends in the snouts <strong>of</strong> crocodylomorphs<br />

support the claim <strong>of</strong> a "struggle" between the conflicting<br />

tendencies <strong>of</strong> pneumatization and maintenance <strong>of</strong> adequate<br />

strength. The caudal shift <strong>of</strong> the primary choana resulting<br />

from the development <strong>of</strong> maxillary palatal processes pushed the<br />

whole pneumatic system caudally and constricted it as it competed<br />

for space with the orbital contents. Nevertheless, the cavity<br />

remained tolerably large in the oreinirostral metasuchians<br />

CAVITY OF ARCHOSAURS<br />

A primitive condition:<br />

cylindrical snout<br />

fen<br />

antorb<br />

ext<br />

"dangerous" derived condition:<br />

dorsoventrally flattened snout<br />

retaining external fenestra<br />

agitta<br />

bending<br />

open cross section<br />

produced by fenestra<br />

fen antorb ext<br />

FIGURE 38. Biomechanical implications <strong>of</strong> platyrostry (flattening <strong>of</strong><br />

the snout). A, the primitive condition (manifested by sphenosuchians,<br />

protosuchians, many basal metasuchians) is to have a much taller, more<br />

cylindrical snout. B, the dorsoventral flattening observed in some clades<br />

(most notably neosuchians) makes the snout particularly susceptible to<br />

failure under sagittal bending andlor torsion. Furthermore, the stress<br />

concentrations resulting from platyrostry are in precisely the locations<br />

<strong>of</strong> the external antorbital fenestra, which would produce an open cross<br />

section further weakening the snout. Ultimate closure <strong>of</strong> the external<br />

antorbital fenestra and internalization <strong>of</strong> the antorbital cavity was probably<br />

largely a biomechanical consequence <strong>of</strong> platyrostry.<br />

such as Araripesuchus gomesii. However, the flattening <strong>of</strong> the<br />

snout produced a biomechanical weak spot at exactly the location<br />

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

external fenestra and internalization <strong>of</strong> the paranasal air sac was<br />

a biomechanical solution to the problem (and nasal rotation was<br />

probably the morphogenetic mechanism accomplishing this closure;<br />

Witmer, 1995b). It would seem that in crocodylomorphs,<br />

the paranasal air sinus "loses" in the metaphorical struggle, and<br />

this is probably a fair conclusion. But, interestingly, in the<br />

broad- but flat-snouted alligatorines, pneumaticity has rebounded,<br />

and the snout is a multi-chambered maze with stout bony<br />

struts at biomechanically predictable locations.<br />

Ornithopoda-Turning to ornithischian dinosaurs, the focus<br />

will be Omithopoda, but most major clades <strong>of</strong> ornithischians

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