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Seventeen extant populations of Microtus (Terricola) savii have been investigated for correlations of first lower molar shape to climatic variables by means of geometric morphometrics, and controlling for phylogenetic inheritance. Comparative methods revealed that climatic variables and phylogeography provide a very similar contribution to variation in first lower molars morphology, whereas tooth size does not appear to be affected by climatic conditions. Climate‐related changes have been recognized in the anteroconid portion of the tooth. This indicates that molar tooth variation is strongly influenced by climatic conditions, although in a complex way. Calabrian populations, often ascribed to Microtus (Terricola) brachycercus, form a distinct cluster, in agreement with the most recent genetic analyses. © 2010 The Linnean Society of London, Biological Journal of the Linnean Society, 2010, 99 , 632–647.  相似文献   
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The cuticular hydrocarbons (CHCs) of codling moth larvae collected in the field from their host plant species, apple and walnut, were analyzed and compared with the CHCs of fruits from these two phylogenetically distant hosts. The CHC profiles of the larvae consisted solely of n‐alkanes (C23–C31) and differed quantitatively between host populations. Amounts of the CHCs from the walnut‐collected larvae were shifted towards longer‐chain alkanes compared to those from apple‐collected larvae. A similar shift was observed for the CHC profiles of walnut and apple fruits. Analysis of the CHCs of larvae reared on artificial diet, in comparison with hydrocarbons from the diet, confirmed that larval CHCs scarcely reflect hydrocarbons from the food source. This finding indicates that the larval hydrocarbons must be biosynthesized to a large degree by the insect, rather than being gained directly from its diet. Hence, codling moth populations from apple and walnut each synthesize their own CHC profiles, which largely resemble those of their respective host plant, yielding a potential tool of chemical camouflage from certain natural antagonists of the larvae. The findings of the present study, together with recent molecular population analyses, provides evidence for a process that might ultimately lead to sympatric speciation of this herbivore species. © 2010 The Linnean Society of London, Biological Journal of the Linnean Society, 2010, 101 , 376–384.  相似文献   
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Mandibular corpus shape variability was investigated in seven families of both extant and extinct mammalian carnivores using two‐dimensional landmarks and geometric morphometric methods. The landmark configuration represents the position of the fourth premolar relative to the canine and the lower carnassial, plus related features of the corpus profile. Between families, the corpus manifests differences in shape and allometry. Additionally, families differ in the relationship between the angle α (a carnassial trait proxy for hypo‐hypercarnivory) and mandibular corpus shape. When phylogenetic relatedness is taken into account using five different phylogenies as covariates, interspecific scaling is still present but the relationship between α and corpus shape is no longer significant. This suggests that the allometric relationship reflects the physical constraints of mastication, resulting in relatively increased corpus depth with higher loads. In contrast, the angle α is related to corpus curvature and this relationship is phylogenetically constrained by the reduction of the molar battery in large feliforms early during the carnivore radiation. In summary, large fissiped carnivores show extensive functional convergence in mandibular corpus shape although the evolutionary routes leading to such functional convergence are different. © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society, 2008, 154 , 832–845.  相似文献   
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A phylogeny of the 37 known species and subspecies of the micropterous snow fly genus Chionea Dalman is presented using adult morphological characters. The genus contains two major clades: a strictly Palaearctic clade, and a combined Nearctic‐Palaearctic clade with representatives in the Nearctic and Western Palaearctic regions. As there is little congruence between the recovered phylogeny of Chionea and the currently used subgeneric division in Chionea s.s. and Sphaeconophilus Becker, we propose to abandon the use of subgeneric taxa in Chionea. A strictly morphological analysis appears to be insufficient to fully resolve the phylogeny of the genus at the species level, and future molecular work should provide additional evidence for the establishment of relationships among the members of Chionea. The large‐scale historical biogeography of Chionea was analysed using dispersal‐vicariance analysis. The initial distribution area of the genus probably extended in the Eastern Palaearctic, and the Nearctic and the origin of Chionea could be dated in the Late Cretaceous. The various dispersal and vicariance events that led to the major speciation events in the genus are set against major paleogeographic developments. The ancestor of the Western Palaearctic group in the second major clade originated from the Nearctic. The presence of the cold‐adapted Chionea in currently temperate to warm climatic zones in the southern parts of its distribution was analysed using ecological niche modelling. It appears that prolonged periods of climate cooling, as occurred during the Last Glacial Maximum, enabled Chionea to cover large parts of central and southern Europe and reach the southern distribution areas where the genus is present today. A similar biogeographic pattern was less evident in the Nearctic region.  相似文献   
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