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1996 McGUIRE-SYSTEMATICS OF CROTAPHYTID LIZARDS 9<br />

debate concerning crotaphytids has been whether or<br />

not Garnbelia should be synonymized with Crota-<br />

phytus (Smith, 1946; Robison and Tanner, 1962;<br />

Weiner and Smith, 1965; Montanucci, 1969, 1978;<br />

Montanucci et al., 1975; Tanner and Banta, 1977).<br />

Nevertheless, very little character evidence has been<br />

presented supporting the monophyly of Crotaphy-<br />

tidae. Etheridge and de Queiroz (1988) recognized<br />

crotaphytids as a monophyletic group on the basis<br />

of a unique combination of derived, yet highly ho-<br />

moplastic features: the presence of posterior cora-<br />

coid fenestrae and female gravid coloration, and the<br />

absence of postfrontal bones and a middorsal scale<br />

row. Frost and Etheridge (1 989) considered crota-<br />

phytids to be monophyletic on the basis of three<br />

reversals: presence of palatine teeth, posterior cor-<br />

acoid fenestrae, and ribs on the third cervical ver-<br />

tebra (the last ofwhich is only infrequently observed<br />

in crotaphytids). In each of these analyses, character<br />

support for Crotaphytidae was dependent upon its<br />

placement within the ingroup topology. The follow-<br />

ing is a list of synapomorphies of Crotaphytidae<br />

recognized in this study: presence of black oral pig-<br />

mentation (reversed within Crotaphytus), presence<br />

of a posterolaterally projecting jugal-ectopterygoid<br />

tubercle immediately posterior to the maxillary tooth<br />

row, presence of posterior coracoid fenestrae, the<br />

tympanic crest of the retroarticular process of the<br />

mandible curves posterodorsally, the parietal and<br />

frontal strongly overlap the medial process of the<br />

postorbital, the supratemporal lies in a groove along<br />

the ventral or ventrolateral border of the supratem-<br />

poral process of the parietal (reversed in most G.<br />

silus or convergent in Crotaphytus and other Garn-<br />

belia), presence of palatine teeth, and contact of the<br />

prefrontal and jugal in the anterolateral border of<br />

the orbit.<br />

The terminal taxa utilized in this study include<br />

the currently recognized species of Crotaphyrus (C.<br />

antiquus, C. bicinctores, C. collaris, C. dickersonae,<br />

C. grismeri, C. insularis, C. reticulatus, and C. ves-<br />

tigium) and Garnbelia (G. coronat, G. silus, and G.<br />

wislizenii). Over the course of this study, it was de-<br />

termined that at least one and probably two addi-<br />

tional species should be recognized. These include<br />

two taxa currently recognized as subspecies, C. c.<br />

nebrius and G. bv. copei (see taxonomic accounts for<br />

data supporting the elevation of these taxa to full<br />

species). These species were also included in the<br />

analysis.<br />

Another population of Gambelia that may even-<br />

tually prove to be a full species is the population of<br />

G. ivislizenii on Isla Tiburon in the Gulf of Califor-<br />

nia. The four osteological specimens examined in<br />

this study lacked autotomic fracture planes in the<br />

caudal vertebrae. Fracture planes are present in all<br />

other G. \clislizenii (n = 19) and G. silus (n = 5)<br />

specimens examined, although they appeared to be<br />

fused in three of ten G. copei. Unfortunately, no<br />

osteological specimens were available from adjacent<br />

Sonora and it could not be determined ifthe absence<br />

of fracture planes is confined to this insular popu-<br />

lation. If this population proves to be a separate<br />

species, it may be the only endemic reptile or am-<br />

phibian on Isla Tiburon, a land-bridge island that<br />

supports an extensive herpetofauna.<br />

The remaining subspecies of Crotaphytus collaris<br />

and Gambelia nislizenii were not treated as separate<br />

terminal taxa because no evidence has been pre-<br />

sented, nor has any been discovered over the course<br />

of this investigation, suggesting that these forms are<br />

discrete evolutionary entities. Rather, they are pat-<br />

tern or convenience classes (Frost et al., 1992), color<br />

morphs largely consistent over an extensive area,<br />

but grading smoothly into other color morphs at<br />

their boundaries.<br />

Etheridge and de Queiroz (1988) and Frost and<br />

Etheridge (1 989) provided evidence for the mono-<br />

phyly of nine suprageneric groups (elevated to fam-<br />

ilies in the latter study) within Iguania. Interfamilial<br />

resolution was elusive and their strict consensus tree<br />

(at the familial level) was an unresolved polytomy.<br />

However, they were able to substantially reduce the<br />

number of equally parsimonious interfamilial to-<br />

pologies as depicted in their 12 unrooted trees with<br />

rooting points (Fig. I). Thus, despite the continuing<br />

lack of unambiguous interfamilial resolution, the<br />

outgroup situation has improved considerably. In<br />

this analysis, characters were considered to be po-<br />

larized only when the polarity assessment was con-<br />

sistent with all 12 unrooted trees.<br />

For each of the eight remaining iguanian families,<br />

exemplars were examined for the purpose of char-<br />

acter polarization. The choice of exemplars was<br />

based whenever possible on the results of recent<br />

intrafamilial phylogenetic analyses. Thus, basal lin-<br />

eages have been proposed for clades within the fam-<br />

ilies Phrynosomatidae (Presch, 1969; Montanucci,<br />

1987; Etheridge and de Queiroz, 1 988; de Queiroz,<br />

1989, 1992; Wiens, 1993a, 1993b), Tropiduridae

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