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DEUTEROSTOMES: ECHINODERMS AND HEMICHORDATES  399










                                                                lateral view   aboral view    oral view
                                                                         Timoroblastus  Permian


                    Echinosphaerites
                     rhombiferan







                                                                lateral view    oral view     lateral view
                                                                         Pentremites         Schizoblastus
                                                                        Carboniferous    Carboniferous-Permian
                     Sphaeronites                            Figure 15.8  Some blastoid genera. Magnifi cation
                     diploporite                             ×0.6 for all. (Redrawn from various sources.)




                                             Pleurocystites
                                             rhombiferan





                     Haplosphaeronis
                      diploporite
             Figure 15.7  Some Ordovician cystoid genera:    (a)                         (b)
             Echinosphaerites and Sphaeronites, (×0.75),
             Haplosphaeronis and Pleurocystites (×1.5).      Figure 15.9  (a) An eocrinoid, and (b) a
             (Based on Treatise on Invertebrate Paleontology,   paracrinoid. (Based on Treatise on Invertebrate
             Part S. Geol. Soc. Am. and Univ. Kansas Press.)  Paleontology, Part S. Geol. Soc. Am. and Univ.
                                                             Kansas Press.)

             a few horizons are packed with blastoids, par-  basal Fissiculata characterized by hydrospire
             ticularly when the diversity of the group       folds, and the Spiraculata with, as the name
             peaked in the Early Carboniferous. Viséan       suggests, well-developed spiracles.
             reefal facies in northern England yield abun-
             dant blastoids, as do the Permian limestones    Eocrinoids
             on the island of Timor where, for example,
             Timoroblastus and Schizoblastus occur.          The eocrinoids were the earliest of the brachi-

               The blastoids first appeared during the        ole-bearing echinoderms. They had a huge
             Silurian, probably evolving from an Ordovi-     range of thecal shapes with primitive hold-
             cian ancestor with brachioles and a reduced     fasts and an irregular to regular arrangement
             number of plates. They initially competed,      of plates (Fig. 15.9a). Sutural pores rather
             ecologically, with the rhombiferan cystoids.    than thecal pores, along the joins between the
             The evolutionary history of the group was       plates, were characteristic of the earliest eocri-
             marked by changes in the shape of the theca     noids; in others there is a total lack of respira-
             and variations in the length of the ambulacra.   tory structures. Eocrinoids differ from the
             Two main groups are recognized: the more        crinoid groups in having biserial brachial
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