Paul—Testing for homologies in echinoderms
plates. In paracrinoids, both the flooring plates of the main ambulacra and the erect pinnules are uniserial. The flooring plates are again modified first pinnulars but are uniserial simply because pinnules only arise from one side of the ambulacra. Pinnular facets are confined to single flooring plates. More derived ambulacral structures occur where biserial brachioles arise from facets on single flooring plates in a simple biserial arrangement. A variety of ambulacral structures occurs in ‘cystoids.’ Lack of detailed knowledge of such structures in many Cambrian ‘cystoids’ makes it difficult to decide which are likely to be plesiomorphic. Details of any transitions between biserial and uniserial structures are uncertain. Many ambulacral structures conform to the ideal design for
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Bell, B.M., 1976a, Phylogenetic implications of ontogenetic development in the class Edrioasteroidea (Echinodermata): Journal of Paleontology, v. 50, p. 1001–1019.
Bell, B.M., 1976b,Astudy of North American Edrioasteroidea: New York State Museum, Memoir v. 21, p. 1–447.
Billings, E., 1854, On some new genera and species of Cystidea from the Trenton Limestone: Canadian Journal, v. 2, p. 215–219, 250–253, 268–274.
Billings, E., 1858, Figures and descriptions of Canadian organic remains: Decade 3: Ottawa, Canada, Geological Survey of Canada, 102 p.
Bockelie, J.F., 1978, Variability of ambulacral structures in some diploporite cystoids: Thalassia Jugoslavica, v. 12 (for 1976), p. 31–39.
Bockelie, J.F., 1979a, Celticystis n. gen., a gomphocystitid cystoid from the Silurian of Sweden: Geologiska Föreningens i Stockholm Förhandlingar, v. 101, p. 157–166.
Bockelie, J.F., 1979b, Taxonomy, functional morphology and palaeoecology of the Ordovician cystoid family Hemicosmitidae: Palaeontology, v. 22, p. 363–406.
an efficient filter and match similar structures in modern crinoids. For this and other reasons, ‘cystoids’ probably possessed extensions of the water vascular system in their ambulacra. Cover plates of main ambulacral grooves may not have
opened in life, whereas those of brachioles and pinnules must have done so. There is no evidence for any musculature to open cover plates in either main ambulacral grooves or brachioles and pinnules. The simplest way to open cover plates is by erecting underlying tube feet—another reason for believing extensions of the water vascular system occurred in the ‘cystoid’ ambula- cra. The complete absence of cover plates in the food grooves of Lichenoides and sphaeronitid diploporites is particularly puzzling.
Acknowledgments
I am grateful to A.B. Smith for providing key references and being an inspirational colleague for many years now. S. Zamora, Geological Survey, Spain, kindly provided the original of Figure 13. S. Zamora and I.A. Rahman also furnished some key references. A. Smith and B. Lefebvre produced thorough and thought-provoking reviews of the original manuscript. I amalso indebted to Y. Makhlouf and B. Lefebvre, University Claud Bernard, Lyon, for latex moulds of some critical diploporites originally described by J. Chauvel and J. Barrande, respectively.
Accessibility of supplementary data
Data available from the Dryad Digital Repositary:
http://doi.org/ 10.5061/ dryad.n2d7d.
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