Page 290 - Introduction to Paleobiology and The Fossil Record
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THE BASAL METAZOANS: SPONGES AND CORALS  277




                                          tentacles
                                                   mouth and gullet
                                                                       tentacles


                                     polyp wall
                                                                    mesentery
                                     mesentery
                                     basal
                                     infolding                        septum or
                                     over                             scleroseptum
                                     septum
                                     basal plate
                                     (a)
                                       tentacles
                                                            tentacles


                                                                         abandoned
                                                                         corallite







                                      (b)















                                       (c)


                                                        (d)

               Figure 11.18  Main cnidarian body plans: (a) generalized scleractinian polyp, (b) generalized part

               of scleractinian coral colony, (c) living anemone, and (d) living jellyfish. (From various sources.)




             include freshwater and colonial forms together   phylum. Hydrozoans reproduce either sexu-

             with the fire corals and most kinds of “jelly-   ally or by asexual budding; the polyp stage is

             fish”. There are over 3000 living species        asexual and the medusoid normally sexual.
             inhabiting water depths up to 8000 m, mainly    The scyphozoans are mainly free-swimming

             in marine environments. Supposed hydrozo-       medusae or jellyfish often inhabiting open-
             ans have been recorded from the Late Precam-    ocean environments. Some elements of the
             brian Ediacara fauna (see p. 242), where        Ediacara fauna may be scyphozoans, for
             genera such as Eoporpita and Ovatoscutum        example  Conomedusites and  Corumbella;
             may be the oldest sessile members of the        however many of the best-preserved fossil
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