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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