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Long-term erosion and subsidence cause dramatic alterations in the physical and ecological features of oceanic islands. Although oceanic islands have been extensively used as models for the study of speciation, little attention has been given to investigating evolutionary patterns in old volcanic islands that have suffered severe climatic degradation. The spider genus Dysdera has diversified across the Canary Islands and has evolved endemisms in the low-elevation, xeric eastern islands, which sharply contrast with the younger, higher, and more humid western islands. A combined phylogenetic analysis of seven mitochondrial and nuclear genes reveals that the eastern Canaries were colonized twice, although only one lineage underwent in situ diversification. Origins of the speciose lineage remain obscure, but probably preceded diversification of present-day Iberian and North African species. A second colonization of the eastern Canaries from North Africa has occurred in more recent times. Molecular analyses reveal several instances of geographically coherent cryptic lineages further supported by morphometric evidence. Analyses of diversification rates suggest deceleration of diversification over the course of time, and this is compatible with increasing extinction rates due to drastic yet continuous ecological changes. Extinction may also explain incongruent patterns of morphological differentiation and species coexistence. Despite a general trend towards community impoverishment, there is also evidence for recent speciation events linked to ecological shifts, which may illustrate the origins of nonspeciose relic lineages on islands. © 2008 The Linnean Society of London, Biological Journal of the Linnean Society, 2008, 94, 589–615.

Invertebrate communities in volcanic habitats of different ages on the islands of La Palma and El Hierro were studied using standardized trapping and searching techniques. A variety of graphical and numerical approaches were used to analyse relationships among the sites. Young, barren lava flows constitute aeolian ecosystems with a fauna of generalized detritivores and predators, especially collembolans, earwigs, thysamirans and crickets. Surface samples have many individuals and low diversity; those from caves have smaller numbers but similar taxonomic composition. Vegetated surface habitats have richer communities, with diverse herbivores and predators but largely without the pioneer ‘lavicolous’ species. Caves with high humidity and stable temperature contain mainly specialized troglobitic species, but if there are both dry and humid sections lavicoles may also be present. Divergence into distinct epigean and hypogean communities results from both abiotic and biotic processes, including erosion and plant succession. While these occur mainly on the surface they also affect caves, increasing humidity and providing insulation from variations in external environmental conditions; the process is considered as a form of ‘maturation’ of the caves. Various models of succession are considered, which might help to account for the disappearance of lavicoles from mature epigean and hypogean communities.