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VARIABILITY IN LAND SNAILS      817

            (Shimizu & Ueshima, 2000; Davison, 2002; Teshima   According to autocorrelation statistics for shell
            et al., 2003).                                   shape similarity (Fig. 5A, B), no spatial structure for
              Similar events may also be described for Sicilian  all western and central populations (0–125 km) is
            Marmorana: there was a morphological gradient of  illustrated by fluctuations around 0 values. Notably,
            characters related to globularity (shell shape index  the analysis confirmed patchy shell shape distribu-
            ShH/MaxD) (Fig. 3); laboratory studies have shown  tion (flat to globular) in this geographic area. The
            that flat keeled and globular snails mate and produce  sudden increase in significant positive values over
            viable offspring (Rensch, 1937) and that the different  the scale of 125 km is in line with the observation
            populations have similar genitalia. Although the  that, along the Sicilian northern mountain chain
            present data do not allow us to confirm the hypothesis  (Madonie Mountains), only globular shapes are
            of introgression by hybridization, it is noteworthy  present and cluster in a monophyletic assemblage
            that intermediate shapes are present where extreme  (clade 3). The sharp drop to significant negative
            shapes (globular and flat) are in close contact. Thus,  values, over the scale of 200 km, for shell shape and
            the co-presence of globular, intermediate and flat  mtDNA sequence correlograms, is in line with the
            shells in single lineages could be a consequence of a  large gap separating the limestone Iblean plateau
            parapatric pattern of populations and/or of a process  and the northern and western side of the calcareous
            of speciation in re. It is noteworthy that the popula-  Sicilian northern mountain chain. Moreover, with
            tion distribution observed in the field over large areas  respect to the mtDNA sequence correlogram, geo-
            of Sicily effectively confirmed a parapatric pattern of  graphic isolation events are illustrated by highly
            distribution.                                    positive values for very close neighbouring popula-
              Regarding genitalia, changes as sharp as those  tions  (0–25 km),  abruptly  decreasing  to  lower
            observed in shells were not observed. Sicilian Mar-  values for more distant populations (50 km). Hence,
            morana show a multiple scale variation pattern   the spatial pattern of distance shows that highly
            (Fiorentino et al., 2008) consistent with the scenarios  morphologically  differentiated  populations  are
            proposed in other studies: genital variance may be  genetically close when geographically close. The
            selectively controlled to maintain function (Baminger  progressive decline over the approximate distance
            & Haase, 2000), such as strong control of the number  range 0–250 km is consistent with a model of isola-
            of allosperm (Lind, 1973; Haase & Baur, 1995) or  tion by distance, a pattern already recognized in
            differences in the number of sperm transferred   other groups of land snails (Madec et al., 2003). In
            (Locher & Baur, 1997; Baur, Locher & Baur, 1998).  a group largely affected by limited and aggregated
            However, DFA and ANOVA significantly distinguished  distribution due to low vagility, dispersion capacity,
            MP specimens (Monte Pellegrino), a lineage signifi-  and obligatory constraint to calcareous rock habi-
            cantly distinct and diversified in the phylogram  tats, vicariance and isolation by distance therefore
            (Fig. 6B).                                       presumably played a key role in diversification pro-
                                                             cesses.  Plio-Pleistocene  paleogeographic  changes
                                                             (involving sea level changes and leading to the
                     PHYLOGENETIC RELATIONSHIPS              current geomorphological setting of Sicily) and
            CO I and 16S sequence data suggest that the mor-  overall postglacial land expansion during the Pleis-
            phological characters used in the taxonomy of the  tocene (Agnesi et al., 2000) may have created isola-
            Sicilian Marmorana to define the five recognized   tion by distance and may both have played major
            species do not reflect phylogenetic relationships.  roles in establishing the present spatial structure of
            Indeed, mitochondrial based reconstructions (Fig. 6B)  genetic and morphological variation in this area of
            identify several supported subclusters not related to  distribution.
            shell shape but well correlated with geographic dis-  Basal relationships are not sufficiently resolved in
            tribution (Fig. 6A). For example, in central-eastern  the analysis for the amplified fragments to provide
            and eastern Sicily, where both shell shapes are wide-  sufficient information to detect relationships at this
            spread, inferred topologies group together globular,  level. Increasing the number of characters may lessen
            flat and intermediate shapes (clade 2 and 4). By  such problems, assuming similar evolutionary pat-
            contrast, the phylogenetic assemblage coherent with  terns of additional nucleotides (Berbee, Carmean &
            shell morphotypes is represented by the cluster  Winka, 2000). On the other hand, if the observed lack
            including populations of the Sicilian northern moun-  of phylogenetic resolution reflects rapid radiation, no
            tain chain (Madonie Mountains), a geographic area in  amount of data would improve resolution. The
            which only globular shapes are found (clade 3). The  general understanding of phylogenetic relationships
            only exceptions to this phylogeographic pattern are  in the genus Marmorana, acquired in the present
            the ‘M. muralis’ cluster (discussed below) and the  study, suggests that further study with nuclear
            unresolved lineages of Caccamo and San Fratello.  markers would be worthwhile.

            © 2008 The Linnean Society of London, Biological Journal of the Linnean Society, 2008, 94, 809–823


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