Abstract
AbstractAimUntil recently, complete information on global reptile distributions has not been widely available. Here, we provide the first comprehensive climate impact assessment for reptiles on a global scale.LocationGlobal, excluding Antarctica.Time period1995, 2050 and 2080.Major taxa studiedReptiles.MethodsWe modelled the distribution of 6296 reptile species and assessed potential global and realmâspecific changes in species richness, the change in global species richness across climate space, and speciesâspecific changes in range extent, overlap and position under future climate change. To assess the future climatic impact on 3768 rangeârestricted species, which could not be modelled, we compared the future change in climatic conditions between both modelled and nonâmodelled species.ResultsReptile richness was projected to decline significantly over time, globally but also for most zoogeographical realms, with the greatest decreases in Brazil, Australia and South Africa. Species richness was highest in warm and moist regions, with these regions being projected to shift further towards climate extremes in the future. Range extents were projected to decline considerably in the future, with a low overlap between current and future ranges. Shifts in range centroids differed among realms and taxa, with a dominant global poleward shift. Nonâmodelled species were significantly stronger affected by projected climatic changes than modelled species.Main conclusionsWith ongoing future climate change, reptile richness is likely to decrease significantly across most parts of the world. This effect, in addition to considerable impacts on species range extent, overlap and position, was visible across lizards, snakes and turtles alike. Together with other anthropogenic impacts, such as habitat loss and harvesting of species, this is a cause for concern. Given the historical lack of global reptile distributions, this calls for a reâassessment of global reptile conservation efforts, with a specific focus on anticipated future climate change.
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