TOWARDS A MODEL FOR SPECIATION IN AMMONOIDS: DEVELOPMENTAL TIMING AND ECOLOGICAL SPECIATION MAY PLAY COMPLEMENTARY ROLES IN PROMOTING RAPID DIVERSIFICATION
A case study from the Cretaceous Western Interior Seaway (WIS) of North America illustrates the model. Acanthoceratid ammonites moved into the newly formed WIS during the Cenomanian and underwent a rapid endemic radiation over the next two million years. Here I focus on one WIS acanthoceratid clade, the genus Metoicoceras and its dwarf offshoots. The earliest Metoicoceras species was derived from a species of Plesiacanthoceras; juveniles of the two groups are nearly identical, but diverge in the timing of appearance and disappearance of shell ornament traits during ontogeny. Later species of Metoicoceras also differ largely in the timing of appearance of traits during development. The degree of sympatry between contemporary Metoicoceras species increased as the radiation proceeded while the amount of geographic range symmetry decreased. These patterns suggest that the relative importance of geographic isolation changed during the course of Metoicoceras’ radiation—the initial move into the seaway may have followed an allopatric speciation model, with sympatric speciation driven by developmental changes and ecological divergence increasing in importance as the radiation proceeded.