Defining climate's role in ecosystem evolution: Clues from late quaternary mammals

Mammalian communities alter their taxonomic composition through time as the species composing them change their biogeographic range, become extinct, or evolve into new species. When taxonomic compositions change through these processes, inevitably the links between taxa and communities change too, resulting in evolution from one ecosystem into the next. Late Quaternary examples suggest that on a timescale encompassing a few thousand to a few hundred thousand years (the “multi‐millennial timescale"), climatic change is perhaps the most important driver of ecosystem evolution because it periodically forces biogeographic changes and extinction. Climatic change over this timescale, which essentially slips between “geological time”; and “ecological time”;, is not very closely in phase with population‐level evolution of a species analyzed for this study, the meadow vole Microtus pennsylvanicus; therefore climatic oscillations on the multi‐millennial timescale may not stimulate speciation much. Instead, speciation may contribute to ecosystem evolution independent of climatic change and over a longer time scale.