Abstract
A macroevolutionary model is developed to account for the “adaptive radiation”; of cheilostome bryozoans that commenced in the Cenomanian after a long phase of low diversity. Living cheilostome species possess one of two types of larvae; planktotrophic (cyphonautes) larvae of relatively long duration, and brooded non‐planktotrophic (coronate) larvae of short duration. Planktotrophic larvae characterize the paraphyletic “malacostegans”; from which “advanced”; cheilostomes with non‐planktotrophic larvae are thought to have evolved monophyletically. Research on other marine invertebrates suggests that gene flow within and between populations is likely to be poorer in species having non‐planktotrophic larvae, and hence the frequency of allopatric and quasi‐sympatric speciation may be greater. Skeletal evidence of larval brooding in the cheilostomes first appears in the late Albian, immediately before their adaptive radiation, and the evolution of non‐planktotrophy with associated increase in speciation rate is proposed to have triggered this radiation.