Jones Marc E H
Research Department of Cell and Developmental Biology, Anatomy Building, UCL, University College London, London WCIE 6BT, UK.
J Morphol. 2008 Aug;269(8):945-66. doi: 10.1002/jmor.10634.
The Rhynchocephalia are a group of small diapsid reptiles that were globally distributed during the early Mesozoic. By contrast, the only extant representatives, Sphenodon punctatus and S. guntheri (Tuatara), are restricted to New Zealand off-shore islands. The Rhynchocephalia are widely considered to be morphologically uniform but research over the past 30 years has revealed unexpected phenotypic and taxonomic diversity. Phylogenetically "basal taxa" generally possess relatively simple conical or columnar teeth whereas more derived taxa possessed stouter flanged teeth and sophisticated shearing mechanisms: orthal in some (e.g., Clevosaurus hudsoni) and propalinal in others (e.g., S. punctatus). This variation in feeding apparatus suggests a wide range of feeding niches were exploited by rhynchocephalians. The relationship of skull shape to skull length, phylogenetic grouping, habit, and characters relating to the feeding apparatus are explored here with geometric morphometric analysis on two-dimensional landmarks. Principle components analysis demonstrates that there are significant differences between phylogenetic groups. In particular, Sphenodon differs significantly from all well known fossil taxa including the most phylogenetically basal forms. Therefore, it is not justifiable to use Sphenodon as a solitary outgroup when studying skull shape and feeding strategy in squamates; rhynchocephalian fossil taxa also need to be considered. There are also significant differences between the skull shapes of aquatic taxa and those of terrestrial taxa. Of the observed variation in skull shape, most variation is subsumed by variation in dentary tooth base shape, the type of jaw movement employed (e.g., orthal vs. propalinal) and the number of palatal tooth rows. By comparison, the presence or absence of flanges, dentary tooth number and palatal tooth row orientation subsume much less. Skull length was also found to be a poor descriptor of overall skull shape. Compared to basal rhynchocephalians members of more derived terrestrial radiations possess an enlarged postorbital area, a high parietal, and a jaw joint positioned ventral to the tooth row. Modification of these features is closely associated with increased biting performance and thus access to novel food items. Some of these same trends are apparent during Sphenodon ontogeny where skull growth is allometric and there is evidence for ontogenetic variation in diet.
喙头目是一类小型双孔亚纲爬行动物,在中生代早期曾分布于全球。相比之下,现存的唯一代表物种,斑点楔齿蜥(Sphenodon punctatus)和冈氏楔齿蜥(S. guntheri)(喙头蜥),仅分布于新西兰近海岛屿。人们普遍认为喙头目在形态上较为一致,但过去30年的研究揭示了意想不到的表型和分类多样性。从系统发育角度来看,“基群分类单元”通常具有相对简单的圆锥形或柱状牙齿,而更进化的分类单元则具有更粗壮的带凸缘牙齿和复杂的剪切机制:一些是直向运动(如哈氏锯颌龙Clevosaurus hudsoni),另一些是推进式运动(如斑点楔齿蜥S. punctatus)。这种摄食器官的差异表明喙头目利用了广泛的摄食生态位。本文通过对二维地标进行几何形态测量分析,探讨了头骨形状与头骨长度、系统发育分组、习性以及与摄食器官相关特征之间的关系。主成分分析表明,不同系统发育组之间存在显著差异。特别是,楔齿蜥与所有已知的化石分类单元,包括系统发育上最原始的类群,都有显著差异。因此,在研究有鳞目动物的头骨形状和摄食策略时,仅将楔齿蜥作为单独的外类群是不合理的;喙头目化石分类单元也需要考虑在内。水生类群和陆生类群的头骨形状之间也存在显著差异。在观察到的头骨形状变化中,大多数变化都包含在齿骨齿基部形状的变化、所采用的颌骨运动类型(如直向运动与推进式运动)以及腭齿列的数量之中。相比之下,凸缘的有无、齿骨齿数和腭齿列方向所包含的变化要少得多。研究还发现,头骨长度并不能很好地描述整体头骨形状。与原始喙头目相比,更进化的陆生辐射类群的成员具有扩大的眶后区域、高高的顶骨以及位于齿列腹侧的颌关节。这些特征的改变与咬合力的增强密切相关,从而能够获取新的食物种类。在楔齿蜥的个体发育过程中也出现了一些相同的趋势,其头骨生长呈异速生长,并且有证据表明其饮食存在个体发育上的差异。