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McGUIRE-SYSTEMATICS OF CROTAPHYTID LIZARDS 6 3 Fig. 4 1. -Decay index analysis: The number that is not enclosed in parentheses indicates the number ofadditional steps that must be considered before the node is no longer supported. The num- ber in parenthesesrepresents the number ofcqually parsimonious trees discovered when the given number of additonal steps are permitted. The results of this analysis agree with those of Etheridge and de Queiroz (1 988), Frost and Ether- idge (1 989), and virtually every other study that has considered the systematics of this group in that Cro- taphyfus and Gambelia are found to be sister taxa. The intrageneric relationships also are largely con- sistent with previous hypotheses with some notable exceptions. A major distinction between this anal- ysis and all previous studies is the complete repre- sentation of species included here, several of which were undiscovered or were not known to be distinct lineages at the times of the previous analyses. G. copei agree with those of the bootstrap analysis in suggesting that a number of clades (nodes D, F. G, H, G. wislizenii G. coronat and K) are relatively unstable. Particularly well-supported clades appear to be stems B (Garnbelia), E (Crotaphyrus), and L (C. insularis + C. vesrigiurn). The allozyme and morphology data sets are not entirely consistent with one another in that the allo- G. silus zyme data suggest that C. dickersonae shares a common ancestor with C. collaris, C. nebrius, and C. '. reficulatus, whereas the morphological data suggest that C. dickersonae is more closely related to C. vesrigium and C. bicincrores. The much smaller allo- C. collaris zyme data set (ten characters) seems to contain less phylogenetic signal than does the morphology data C. antiquus set. For example, the differential between the observed g, and the critical g, value for random data C. nebrius is substantially greater for the morphological data set than it is for the allozyme data set (criterion C. dickersonae suggested by J. Huelsenbeck as noted in Wiens [1995]). Nevertheless, because the topology of the C. grismeri single most parsimonious tree is unaffected by the inclusion or exclusion of the allozyme data, the rel- C. bicinclores ative phylogenetic informativeness of the allozyme data is not a critical issue. However, the bootstrap C. vestigium results for both the morphology-only and combined analyses should be considered when evaluating topology robustness for the single most parsimonious C. insularis tree. DISCUSSION A phenetic analysis (Ward's Minimum Variance Cluster Analysis; Wishan, 1968) of unspecified morphological data performed by Smith and Tanner (1972) provided the first estimate of interspecific relationships within Crotaphytus (exclusive of C. reticulatus). They concluded that there were two clusters of taxa within their study group, the collaris complex, composed of C. collaris populations, and the western complex, composed of C. bicinctores, C. vestigiurn, C. insularis, and C. dickersonae. The two clusters are consistent with the results presented here, as both groups appear to be monophyletic. Smith and Tanner (1 974) performed another phe-

BULLETIN CARNEGIE MUSEUM OF NATURAL HISTORY NO. 32 insularis vestigium bicinctores reticularus dickersonae nebrius collaris Fig. 42.-The single tree discovered by Monfanucci et al. (1 975) in their analysis of crotaphytid relationships. netic analysis of Crotaphytus relationships (again without considering Crotaphytus reticulatus). The Ward's Minimum Variance Cluster Analysis (Wis- hart, 1968) employed morphometric and color pat- tern data. Their results were consistent with those oftheir 1972 study, although they were more specific in their assessment of relationships in this later anal- ysis. They discussed the interspecific relationships of the western complex species and recognized two pairs ofsister taxa, (C. dickersonae + C. bicinctores) and (C. vestigium + C. insularis). Their tree indi- cates that they were unsure whether the western complex was monophyletic or if (C. bicinctores + C. dickersonae) was actually the sister taxon of C. collaris (= the collaris complex). Their phyletic tree suggested Gambelia (= G. wislizenii) to be the sister taxon of Crotaphytus, and C. reticulatus to be the sister taxon of the remainder of Crotaphytus. How- ever, data were not presented for these species and it is therefore unclear how these conclusions were reached. The phylogenetic conclusions of this anal- ysis agree in most respects with those of the present study except in the placement of C. dickersonae. which was found to be the sister taxon of C. grismeri, C. bicinctores, C. vestigium, and C. insularis in this analysis. Montanucci et al. (1975) performed the first cla- distic analysis of Crotaphytus, utilizing 12 allozyme, discrete morphological, and morphometric char- acters. Their analysis of these data (using the Wagner program, Kluge and Fams, 1969) resulted in the tree depicted in Figure 42. This tree is similar to those discovered here in the placement of C. bi- cinctores as the sister taxon of (C. vestigium + C. insularis). However, their tree differs from the trees discovered here in the placement of C. dickrsonae as the sister taxon of (C. nebrius + C. collaris), in the placement of C. reticulatus as the sister taxon of this group, and in placing (C. bicinctores (C. ves- tigium + C. insularis)) as the sister taxon of (C. reticulatus (C. dickersonae (C. nebrius + C, collar- is))). As with the previous analyses, several taxa could not be included, such as C. grismeri (not yet recognized as a distinct lineage) and C. antiquus (yet to be discovered). Few comparisons can be drawn between the re- sults of this analysis and those of previous studies regarding the phylogenetic relationships of Garn- belia. Those previous workers who recognized G. silus as a distinct species generally assumed it to be the sister taxon of G. wislizenii. Only Norell (1989) attempted to elucidate the phylogenetic relation- ships of Gambelia and he was primarily interested in the position of G. coronaf. Although Norell (1 989) described a number of useful characters, he was un- able to provide phylogenetic resolution. A distinc- tion between this analysis and several others relates to the evolution of G. silus. Some previous workers suggested that G. silus may have evolved as recently as 11,000 years ago by peripheral isolation (Mon- tanucci, 1967, 1970; Tollestrup, 1979), although Montanucci (1970) also entertained the possibility that G. silus entered the valley much earlier. Re- gardless of the timing of the event, Montanucci (1 970) suggested that differences between G. silus and G. wislizenii are examples of derived character states in G. silus rather than derived characteristics of G. wislizenii. However, most of these features, such as the presence of territoriality, a truncated snout, and sexual dimorphism wherein males are larger than females, are more parsimoniously inter- preted as plesiomorphic retentions in G. silus. This interpretation is consistent with that of Tollestrup (1983), at least with respect to the loss of territori- ality in G. tvislizenii. Thus, it appears that G. silw is a relatively plesiomorphic taxon and not a re- cently derived offshoot of G. wislizenii. It may seem counterintuitive that a narrowly dis- tributed peripheral species such as Gambelia silus would be relatively plesiomorphic in comparison with a wide-ranging taxon such as G. wislizenii (plus its sister taxon, G. copei). However, there are ex-

BULLETIN CARNEGIE MUSEUM OF NATURAL HISTORY NO. 32<br />

insularis<br />

vestigium<br />

bicinctores<br />

reticularus<br />

dickersonae<br />

nebrius<br />

collaris<br />

Fig. 42.-The single tree discovered by Monfanucci et al. (1 975)<br />

in their analysis of crotaphytid relationships.<br />

netic analysis of Crotaphytus relationships (again<br />

without considering Crotaphytus reticulatus). The<br />

Ward's Minimum Variance Cluster Analysis (Wis-<br />

hart, 1968) employed morphometric and color pat-<br />

tern data. Their results were consistent with those<br />

oftheir 1972 study, although they were more specific<br />

in their assessment of relationships in this later anal-<br />

ysis. They discussed the interspecific relationships<br />

of the western complex species and recognized two<br />

pairs ofsister taxa, (C. dickersonae + C. bicinctores)<br />

and (C. vestigium + C. insularis). Their tree indi-<br />

cates that they were unsure whether the western<br />

complex was monophyletic or if (C. bicinctores +<br />

C. dickersonae) was actually the sister taxon of C.<br />

collaris (= the collaris complex). Their phyletic tree<br />

suggested Gambelia (= G. wislizenii) to be the sister<br />

taxon of Crotaphytus, and C. reticulatus to be the<br />

sister taxon of the remainder of Crotaphytus. How-<br />

ever, data were not presented for these species and<br />

it is therefore unclear how these conclusions were<br />

reached. The phylogenetic conclusions of this anal-<br />

ysis agree in most respects with those of the present<br />

study except in the placement of C. dickersonae.<br />

which was found to be the sister taxon of C. grismeri,<br />

C. bicinctores, C. vestigium, and C. insularis in this<br />

analysis.<br />

Montanucci et al. (1975) performed the first cla-<br />

distic analysis of Crotaphytus, utilizing 12 allozyme,<br />

discrete morphological, and morphometric char-<br />

acters. Their analysis of these data (using the Wagner<br />

program, Kluge and Fams, 1969) resulted in the<br />

tree depicted in Figure 42. This tree is similar to<br />

those discovered here in the placement of C. bi-<br />

cinctores as the sister taxon of (C. vestigium + C.<br />

insularis). However, their tree differs from the trees<br />

discovered here in the placement of C. dickrsonae<br />

as the sister taxon of (C. nebrius + C. collaris), in<br />

the placement of C. reticulatus as the sister taxon<br />

of this group, and in placing (C. bicinctores (C. ves-<br />

tigium + C. insularis)) as the sister taxon of (C.<br />

reticulatus (C. dickersonae (C. nebrius + C, collar-<br />

is))). As with the previous analyses, several taxa<br />

could not be included, such as C. grismeri (not yet<br />

recognized as a distinct lineage) and C. antiquus (yet<br />

to be discovered).<br />

Few comparisons can be drawn between the re-<br />

sults of this analysis and those of previous studies<br />

regarding the phylogenetic relationships of Garn-<br />

belia. Those previous workers who recognized G.<br />

silus as a distinct species generally assumed it to be<br />

the sister taxon of G. wislizenii. Only Norell (1989)<br />

attempted to elucidate the phylogenetic relation-<br />

ships of Gambelia and he was primarily interested<br />

in the position of G. coronaf. Although Norell (1 989)<br />

described a number of useful characters, he was un-<br />

able to provide phylogenetic resolution. A distinc-<br />

tion between this analysis and several others relates<br />

to the evolution of G. silus. Some previous workers<br />

suggested that G. silus may have evolved as recently<br />

as 11,000 years ago by peripheral isolation (Mon-<br />

tanucci, 1967, 1970; Tollestrup, 1979), although<br />

Montanucci (1970) also entertained the possibility<br />

that G. silus entered the valley much earlier. Re-<br />

gardless of the timing of the event, Montanucci<br />

(1 970) suggested that differences between G. silus<br />

and G. wislizenii are examples of derived character<br />

states in G. silus rather than derived characteristics<br />

of G. wislizenii. However, most of these features,<br />

such as the presence of territoriality, a truncated<br />

snout, and sexual dimorphism wherein males are<br />

larger than females, are more parsimoniously inter-<br />

preted as plesiomorphic retentions in G. silus. This<br />

interpretation is consistent with that of Tollestrup<br />

(1983), at least with respect to the loss of territori-<br />

ality in G. tvislizenii. Thus, it appears that G. silw<br />

is a relatively plesiomorphic taxon and not a re-<br />

cently derived offshoot of G. wislizenii.<br />

It may seem counterintuitive that a narrowly dis-<br />

tributed peripheral species such as Gambelia silus<br />

would be relatively plesiomorphic in comparison<br />

with a wide-ranging taxon such as G. wislizenii (plus<br />

its sister taxon, G. copei). However, there are ex-

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