Growth rates of populations of the freshwater pearl mussel, Margaritifera margaritifera (L., 1758), in northwestern Spain were analysed based on measurements of annual annuli and using two nonlinear functions for length-at-age data sets: von Bertalanffy's growth model and a hyperbolic function. These populations reach the smallest maximum shell length (90.5 mm) and have the shortest life-span (35 years) and the highest growth rate (k in von Bertalanffy's model >0.1·year–1, on average) known for this species. The two models were similar in performance and were well fitted (around 99%) to shell-length-at-age data, although the hyperbolic function appears to be applicable only from 6 years of age. The growth rate (either k or k' from the hyperbolic function) showed a large and significant variation across populations, both among and within drainages.

The allozyme data base of Arntzen & García-París (1995) on midwife toads (Alytes, Discoglossidae) is reanalysed considering each locus as a discrete character. The phylogeny thus inferred differs from the one obtained with genetic distances in the position of A. dickhilleni from the Betic region – it appears that its sister species is the widespread A. obstetricans, not the Mallorcan endemic A. muletensis. This phylogenetic hypothesis agrees with the taxonomic treatment of the genus based on morphology. A testable biogeographic hypothesis is proposed to account for the diversification of midwife toads in Iberia and the Balearics. The postulated underlying geological changes were the spread of inland saline lakes that divided Iberia (16 mY B.P.), the emergence and break-up of the Betic orogen (14 mY), and the formation of the Betic Strait (8 mY). Dispersal over sea channels or during the Messinian Crisis (6 mY) are deemed unlikely on the basis of ecological and biogeographical data.

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Abstract. Vicariance on a microplate dispersed by the formation of the Western Mediterranean is the probable origin of Melanopsis etrusca Villa in Brot, the only melanopsid (Gastopoda: Melanopsidae) living in the Italian Peninsula. It is distantly related to extant melanopsids in Iberia and Morocco, and is restricted to thermal springs in the Maremma of southern Tuscany. This area was an island throughout the Miocene, inferred to have become detached geographically from the Corso—Sardinian block. Alternative explanations conflict with geological, paleontological, ecological and systematic evidence. In the geologically young Italian Peninsula fossil freshwater melanopsids are known only from Lower Pleistocene sites located around the area occupied by living populations. Their similarity to extant specimens supports the hypothesis that they represent the same lineage, having expanded its range during a brief, favourable period. Introduction of M. etrusca by humans, birds or wind is most improbable given its distinctness, similarity to local fossils, and inability for passive dispersal. Long‐distance dispersal along brackish lagoons during the late Messinian conflicts with the inferred inability of melanopsids living there to colonize freshwater habitats. Indeed, there are ecological, phylogenetic and geological reasons against invoking the Messinian salinity crisis in order to explain the distribution of most taxa. Other freshwater taxa show distribution patterns similar to that of living and fossil melanopsids. However, congruent area cladograms or generalized tracks may not constitute reliable evaluators of biogeographical hypotheses. The detection of vicariance, as that of any other cause, requires robust reconstructions of the past. By pointing at areas of endemism that deserve urgent action, biogeography can provide a contribution to conservation.