The evolution, of the arcoid bivalves is a consequence of the interaction of three distinct, complementary groups of factors which determine organic form. Arcoid diversity has resulted from the opportunistic realization of possible forms, within a range set by the limitations of ancestral morphology, by characteristic growth patterns, and by the requirements of survival in available environments. Historical, phylogenetic constraints include the evolutionary heritage common to all bivalves, the filibranch gill, a shell microstructure suited to form sturdy hinge teeth, and the initial acquistion of a hinge and a ligament both based on the serial repetition of simple elements. Constructional, morphogenetic constraints include the geometrical limitations of the spiral exoskeleton, the unsuitability of the necessarily weak ligament for either epifaunal or infaunal specialization, and hinge teeth that must remain numerous and similar in form. The principal ecological determinant of arcoid form is that individual taxa be functionally adapted to live as shallow burrowers or as endobyssate or epibyssate nestlers, frequently on physically unstable substrates. This requirement is reflected in the close relationship between the overall proportions of arcoid shells and their habitats, in contrast with the conservatism of their soft-part anatomies. Analysis of the interaction between phylogeny, growth and adaptation provides sufficient explanations for individual arcoid forms, while collectively these determinants of form define the adaptive range of the Arcoida. It also yields insight into patterns of evolution. For instance, the repeated occurrence of close evolutionary convergence between arcoid taxa is as much a function of the limited range of solutions to problems of shell growth as it is of common adaptation to a single environment.