Sphinctozoans
Sphinctozoans are sponges that grow as a series of
chambers, one on top of the next. Most are aspiculate, including the living
representative Vaceletia crypta. However, a few Mesozoic forms contain triradiate
calcareous spicules embedded in the body wall. This suggests an evolutionary
relationship with the Calcarea.
On the other hand, soft parts of V. crypta indicate that it shares a common
ancestor with the ceractinomorph
demosponges.
The sphinctozoan growth form has probably evolved independently
within the Calcarea and the Demospongia, making the grouping
polyphyletic.
Thus, they cannot be thought of as a natural evolutionary group.
Fossil "sphinctozoan" families for which
calcarean or demosponge affinities
cannot be determined are known from the Cambrian to the Cretaceous.
Sources:
Reitner, J. 1990. Polyphyletic origin of the "Sphinctozoans". In Rutzler, K. (ed.), New Perspectives in Sponge Biology, Proceedings of the Third International Conference on the Biology of Sponges (Woods Hole). pp. 33-42. Smithsonian Institution Press, Washington, DC.
Vacelet, J. 1985. Coralline sponges and the evolution of the Porifera. In Conway Morris, S., J. D. George, R. Gibson, and H. M. Platt (eds.), The Origins and Relationships of Lower Invertebrates. pp. 1-13. Clarendon Press, Oxford.