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<br />392 <br /> <br />COPEIA, 2001, NO.2 <br /> <br /> <br />energy matrix. Relative warps are principal com- <br />ponents of this space, and describe the major <br />trends in shape variation within the overall sam- <br />ple (Rohlf, 1993). Various forms of RWA can be <br />obtained by varying the exponential weight for <br />the bending energy metric (0:) between zero <br />and one. When 0: > 0, geometrically small-scale <br />variation is given less weight than large scale var- <br />iation. This has the effect of reducing the <br />weight given to regions having more landmarks <br />relative to that given to regions having fewer <br />(and hence more widely spaced) landmarks. We <br />used 0: = 1 because we were intereste i in mor- <br />phometric differences at a larger scale. In ad- <br />dition, we were looking for shape variation in <br />regions other than the nuchal hump, which <br />comprised 40% (10/25) of our landmarks (Fig. <br />1). It also corresponds to the relative warp anal- <br />ysis of Bookstein (l989b, 1991; see Bookstein, <br />1996:146-147). As noted by Rohlf et al. (1996), <br />the value of 0: has no effect on most of the anal- <br />yses employed herein because it merely scales <br />the partial warps. The results of most multivar- <br />iate analyses (e.g., MANOVA, CVA, for exam- <br />ple) are scale free. For our analysis, mean <br />shape-coordinate forms were calculated for all <br />13 samples, with the grand mean as the tangent <br />configuration. <br />We also compared patterns of morphological <br />shape variation in G. robusta and G. CYPha by de- <br />riving taxonomic distances among the five sym- <br />patric populations only, based upon population <br />means for relative warp axes one and two, de- <br />rived from GLS-superimposed specimens. Both <br />matrices were compared against a matrix of geo- <br />graphic distances derived from latitude-longi- <br />tude values and against one another using two- <br />way Mantel tests. <br /> <br />RESULTS <br /> <br />Body size and shape variation in Gila CYPha.-Cen- <br />troid size varied significantly among popula- <br />tions (Fs.142 = 7.33; P < 0.0001) with Little Col- <br />orado River specimens significantly larger than <br />all other groups (Student-Neuman-Keuls test). <br />All shape coordinate pairs showed significant <br />differences among populations (all MANOVA, <br />P < 0.0001), and the overall MANOVA was also <br />significant (Wilks' A = 0.002; X2240 = 743.47; P <br />< 0.0001). Variation can be most clearly seen <br />by examining shape coordinate plots among <br />samples (Appendix 1). Three aspects are em- <br />phasized: shape of the nuchal hump; relative <br />size of the head; and dimensions of the caudal <br />peduncle. The nuchal hump is relatively more <br />pronounced and anteriorly projected in Little <br />Colorado River G. CYPha (Appendix ID), where- <br /> <br />CV2 <br /> <br />@ <br /> <br /> <br />2 <br /> <br />G <br /> <br />e <br /> <br />2 <br /> <br />CV1 <br /> <br />8 <br /> <br />@ <br /> <br />@ <br /> <br />Fig. 2. Shape variation among six Gila typha pop- <br />ulations based on the first two variates derived from <br />a canonical analysis of shape coordinates. Population <br />abbreviations follow Table 1. Circles represent 95% <br />confidence intervals for the group mean. <br /> <br /> <br />as specimens from Cataract Canyon (Appendix <br />IB) have a relatively slight hump. The position <br />of the three landmarks bounding the opercu- <br />lum (LMs 16, 18 and 19; Fig. 1) indicate that <br />specimens from Cataract Canyon have relatively <br />larger heads than do those from the Little Col- <br />orado River, whereas all other populations are <br />intermediate. Finally, there is significant varia- <br />tion in lengths and depths of the caudal pedun- <br />cle, with specimens from Cataract Canyon hav- <br />ing peduncles that are relatively shorter in <br />length but that taper in depth from anterior to <br />posterior, particularly when compared to those <br />from Black Rocks Canyon (Appendix lA), West- <br />water Canyon (Appendix IE), or Yampa River <br />(Appendix IF). Desolation Canyon individuals <br />(Appendix lC) have peduncles that are uni- <br />formly deeper and non tapering than all others. <br />Other aspects of shape variation are found in <br />the distance from pectoral to pelvic fins (LMs <br />2-20), which is reduced in the Little Colorado <br />River population. Fish from this population also <br />have the longest anal fin base, which is reduced <br />in specimens from Cataract Canyon. Also, Des- <br />olation Canyon individuals have shallowest body <br />depths. <br />A canonical variate analysis of shape coordi- <br />nates resulted in three statistically significant <br />variates (of five), accounting for 95.9% of the <br />among-population variation (P < 0.0001; Fig. <br />2). Again, Little Colorado specimens were well <br />separated from the other five populations. All <br />Mahalanobis D2 distances were also significant <br />(P < 0.0001) and demonstrated a high degree <br />of among-sample variation. Classification results <br />were significantly different from chance, with <br /> <br />