Diversification and biodiversity dynamics of hot and cold spots

The determinants that shape the distribution of diversity of life on Earth have been long discussed and many mechanisms underlying its formation have been proposed. Yet connecting the biogeography of hot and cold spots of diversication and current biodiversity patterns to the microevolutionary processes remains largely unexplored. Here, we combine a landscape genetics model based on demographic stochasticity with a speciation model that can be interpreted as a model of the evolution of premating incompatibility or assortative mating to map diversication rates in a spatial context. We show that landscape structure and the intensity and directionality of gene ow strongly inuence the formation of hot and cold spots and its connection to patterns in species richness. Specically, hot and cold spots form in landscapes in which gene ow is suciently strongly structured that the metacommunity nearly breaks up into several disconnected metacommunities. In such a landscape structure, speciation hot spots originate in the center or in the periphery of the landscape depending on whether the direction of gene ow is from the periphery to the center or viceversa, respectively. However, for any given level of gene ow intensity, diversication rates are approximately twice higher in the center than in the periphery of the landscape. These results suggest that sinks may form diversication hot spots with higher probability than sources, in particular, those sinks surrounded by highly diversied sources in dierent locations of the landscape. Joining mechanistically microevolutionary and macroevolutionary processes on landscapes present many fascinating challenges and opportunities to connect the biogeography of diversication with biodiversity dynamics.