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Island colonists are often assumed to experience higher levels of phenotypic diversification than continental taxa. However, empirical evidence has uncovered exceptions to this ‘island effect’. Here, we tested this pattern using the geckos of the genus Pristurus from continental Arabia and Africa and the Socotra Archipelago. Using a recently published phylogeny and an extensive morphological dataset, we explore the differences in phenotypic evolution between Socotran and continental taxa. Moreover, we reconstructed ancestral habitat occupancy to examine if ecological specialization is correlated with morphological change, comparing phenotypic disparity and trait evolution between habitats. We found a heterogeneous outcome of island colonization. Namely, only one of the three colonization events resulted in a body size increase. However, in general, Socotran species do not present higher levels or rates of morphological diversification than continental groups. Instead, habitat specialization explains better the body size and shape evolution in Pristurus . Particularly, the colonization of ground habitats appears as the main driver of morphological change, producing the highest disparity and evolutionary rates. Additionally, arboreal species show very similar body size and head proportions. These results reveal a determinant role of ecological mechanisms in morphological evolution and corroborate the complexity of ecomorphological dynamics in continent–island systems.

The shape of the tree of life is the result of shifting diversification rates, and identifying the factors driving these shifts is one of the main aims in evolutionary biology. Various biotic and abiotic factors have been proposed to have an impact on mammal diversification, such as climatic and tectonic changes, the acquisition of new traits, and expansion into new ecosystems or landmasses. We used phylogenetic comparative methods to quantify the influence of potential drivers on diversification patterns in extant squirrels (Sciuridae, Rodentia). We conducted a multilayer approach, comparing diversification rates among squirrel lineages depending on their degree of biome specialisation, biogeographic realm occupancy, locomotion adaptations, and presence in mountainous regions. We generated the most complete phylogeny of squirrels to date, encompassing almost 80% of the extant species, and applied multiple and binary state‐dependent diversification models. All the traits examined showed an influence on diversification rates. The biome specialist lineages showed the highest speciation rates, suggesting a major role of bioclimatic specialisation on macroevolutionary patterns. A single major event, the Miocene–Pleistocene radiation of terrestrial‐adapted lineages in North America, left a signal that was recovered in two of our analyses. Both the Nearctic lineages and the terrestrial‐adapted lineages showed high speciation rates, highlighting the fact that that major evolutionary episodes may produce confounding effects in state‐dependent diversification models. Ancestral reconstructions showed that cold and warm intervals in Earth’s history had different effects on squirrels’ diversification, depending on their climatic affinities. Tropical and arboreal squirrels evolved predominantly in the warm intervals, while terrestrial and cold‐adapted squirrels radiated in the cold intervals. Our findings suggest that, while global climatic shifts are key for the speciation processes in mammalian lineages, lineage‐specific ecological adaptations are critical modulators of the responses of lineages to such environmental shifts, in an interplay that ultimately affects their diversification patterns.

The study of deep-time ecological dynamics has the ability to inform conservation decisions by anticipating the behavior of ecosystems millions of years into the future. Using network analysis and an exceptional fossil dataset spanning the past 21 million years, we show that mammalian ecological assemblages undergo long periods of functional stasis, notwithstanding high taxonomic volatility due to dispersal, speciation, and extinction. Higher functional richness and diversity promoted the persistence of functional faunas despite species extinction risk being indistinguishable among these different faunas. These findings, and the large mismatch between functional and taxonomic successions, indicate that although safeguarding functional diversity may or may not minimize species losses, it would certainly enhance the persistence of ecosystem functioning in the face of future disturbances.

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The study of how long-term changes affect metacommunities is a relevant topic, that involves the evaluation of connections among biological assemblages across different spatio-temporal scales, in order to fully understand links between global changes and macroevolutionary patterns. We applied multivariate statistical analyses and diversity tests using a large data matrix of rodent fossil sites in order to analyse long-term faunal changes. Late Miocene rodent faunas from southwestern Europe were classified into metacommunities, presumably sharing ecological affinities, which followed temporal and environmental non-random assembly and disassembly patterns. Metacommunity dynamics of these faunas were driven by environmental changes associated with temperature variability, but there was also some influence from the aridity shifts described for this region during the late Miocene. Additionally, while variations in the structure of rodent assemblages were directly influenced by global climatic changes in the southern province, the northern sites showed a pattern of climatic influence mediated by diversity-dependent processes.

We developed new quantitative palaeoclimatic inference models based on the body-size structure of mammal faunas from the Old World tropics and applied them to the Somosaguas fossil site (middle Miocene, central Iberian Peninsula). Twenty-six mammal species have been described at this site, including proboscideans, ungulates, carnivores, insectivores, lagomorphs and rodents. Our analyses were based on multivariate and bivariate regression models correlating climatic data and body-size structure of 63 modern mammal assemblages from Sub-Saharan Africa and the Indian subcontinent. The results showed an average temperature of the coldest month higher than 26°C for the Somosaguas fossil site, a mean annual thermal amplitude around 10°C, a drought length of 10 months, and an annual total precipitation greater than 200 mm per year, which are climate conditions typical of an ecotonal zone between the savanna and desert biomes. These results are congruent with the aridity peaks described over the middle Aragonian of Spain and particularly in the local biozone E, which includes Somosaguas. The aridity increase detected in this biozone is associated with the Middle Miocene Global Cooling Event. The environment of Somosaguas around 14 Ma was similar to the current environment in the Sahel region of North Africa, the Horn of Africa, the boundary area between the Kalahari and the Namib in Southern Africa, south-central Arabia, or eastern Pakistan and northwestern India. The distribution of modern vegetation in these regions follows a complex mosaic of plant communities, dominated by scattered xerophilous shrublands, semidesert grasslands, and vegetation linked to seasonal watercourses and ponds.