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BMC Evolutionary Biology 2008, 8:56                            http://www.biomedcentral.com/1471-2148/8/56




            stitution rate, which ranged from 0.03–1% per lineage per  gesting recent expansion, perhaps after its arrival on the
            My (see refs. in the Discussion). The two markers, with  mainland; however, a no growth scenario could not be
            different substitution rates, yield similar 95% HPD time  rejected statistically. Tajima's D did not support a demo-
            intervals.                                          graphic expansion in either of the balearicus groups sepa-
                                                                rately, or combined. The northeastern range limit of B.
            Although the values reported should be regarded with the  balearicus appears to be the Po River drainage, which may
            caveats mentioned, it is highly improbable that the vicar-  also be the southwestern boundary for B. viridis. Recent
            iant event that separated the African and Sicilian green  mapping of green toad distributions in Italy [38], how-
            toads took place during the Messinian (5.3 Mya), that is,  ever, shows an  apparently continuous range from the
            earlier than the range of dates estimated by this method.  northeast (probable haplotype group of B. v. viridis) to the
            Instead, it is very likely that the Africa-Sicily divergence is  southwest (haplotype group of B. balearicus) across the Po
            post-Messinian. In order to validate the hypothesis pro-  drainage. It is likely that the groups are in contact in that
            posed here and to test competing paleobiogeographic sce-  area; discerning  contacts and possible hybridization
            narios, a formal comparative phylogeographic study  dynamics represent challenging future research topics.
            including more genetic markers and other terrestrial spe-  Indeed, the Po drainage seems to be a biogeographic bor-
            cies in Sicily and North Africa would be necessary. Several  der and/or contact zone between variously related taxa of
            new comparative phylogeographic approaches have been  amphibians and reptiles (for overview [65]: Rana latastii/
            proposed [55-57], each requiring the inclusion of more  R. italica; Hyla arborea/H. intermedia [66]; Bombina varie-
            data for a more reliable  statistical  inference to be  gata/B. pachypus [67]; Rana lessonae/R. bergeri[68]) or, it is
            obtained.                                           considered a "source of genetic variability" [69].

            Historical biogeography of Bufo balearicus          Fossils demonstrate the presence of green toads on the
            The second major result of our study is that green toads  Balearic Islands from the Upper Pleistocene of Mallorca
            from most of the Apennine Peninsula, Corsica, Sardinia  [70], but early human introduction from Corsica was pro-
            and the Balearic Islands represent a separate taxon, which  posed as the source of green toads on these islands [35].
            is different from other Eurasian green toads on the mito-  Our data show toads from Mallorca and Menorca to be
            chondrial and nuclear levels. Three B. balearicus subclades  nested within the mitochondrial clades from the Apen-
            emerged from our mtDNA control region data; the subc-  nine Peninsula and Corsica/Sardinia, and thus corrobo-
            lade on Corsica and Sardinia exhibited basal haplotypes  rate serum albumin data on toads from Mallorca and
            and  the  most substantial structure. These  observations  Corsica that prove them more closely related to each other
            suggest speciation of B. balearicus on these islands around  than to green toads from Palestine,  Africa,  and Greece
            0.9 Mya to 1.8 Mya (Table 3). The earliest green toad fos-  [35]. We cannot locate the exact geographic origin of Bal-
            sils in Italy are known from the Late Miocene from the  earic green  toads with our current data; faster evolving
            northeast (Ravenna Province) and from the Pliocene in  nuclear markers and denser sampling in regions of possi-
            the southeast (Gargano region) of the Apennine Penin-  ble origin are required. Our data also corroborate provi-
            sula [58]. They have also been identified from the Pleis-  sional allozyme data (Lattes, A. 1997, Abstr. 3rd World
            tocene of Corsica and Sardinia [59]. Corsica and Sardinia  Congr.  Herpetol., Prague: p. 123) that associated toads
            had landbridges to  (or were  separated only by narrow  from Corsica, Sardinia and NW-Italy (all from the B. bal-
            marine straits from) the Apennine Peninsula during sev-  earicus range) with a ~0.25 Nei's distance from toads from
            eral geological periods (~18 Mya; 9 Mya; 5.3 Mya [60]).  Vienna based on a UPGMA dendrogram (B. viridis; [71]
            Although a narrow strait may have mostly separated Cor-  quoting Lattes' abstr.).
            sica/Sardinia from Tuscany [61], paleontological [62,63]
            and phylogeographic data  (Discoglossus  [25], isopods  Although Calabria  consisted of  islands until the Pleis-
            [64]) suggest limited early Pleistocene faunal (perhaps  tocene [72], episodic Upper Pleistocene faunal exchange
            oversea) exchange between these islands and the main-  across the Strait of Messina is well documented by the fos-
            land.                                               sil record [72]. While few amphibians crossed the Strait of
                                                                Messina [67], B. balearicus haplotypes have been detected
            This same signature is suggested by our data. The baleari-  in northeastern Sicily (loc. 20).
            cus  clade widespread  on the Apennine Peninsula dis-
            played a mismatch distribution visually, but not    Biogeography of Bufo siculus n. sp
            statistically fitting that expected  for a  population that  Our phylogeographic findings agree with paleogeo-
            underwent a sudden expansion (Figure 3). Similarly, the  graphic and fossil data [72], which suggest a long Plio-
            coalescent simulation program  Fluctuate  estimated a  Pleistocene isolation of Sicily. After their "out of Africa"
            growth  parameter ten times higher for the peninsular  origin, green toads apparently spread across most of Sic-
            group than for the island balearicus clade (Table 2), sug-  ily, where they are well known from the Pleistocene fossil


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