Page 273 - Introduction to Paleobiology and The Fossil Record
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Chapter 11






                      The basal metazoans:


                      sponges and corals









                        Key points

                        •  Parazoans are a grade of organization within the metazoans composed of multicellular
                            complexes with few cell types and lacking variation in tissue or organs; the sponges
                            (Phylum Porifera) are typical parazoans that lack a gut.
                        •  Sponges are almost entirely fi lter-feeding members of the sessile benthos. The group
                            contains a variety of grades of functional organization that cut across the traditional
                            classification of the phylum.

                        •  Sponge reefs were dominated, during most of the Phanerozoic, by calcareous grades
                            developed convergently across the phylum; siliceous sponges were important reef build-
                            ers mainly during the Mesozoic.
                        •  Stromatoporoids are a grade of organization within the Porifera with a secondary cal-
                            careous skeleton, important in reefs during the mid-Paleozoic and mid-Mesozoic.
                        •  Archaeocyaths are Cambrian organisms of sponge grade. They were mainly solitary but
                            developed a branching, modular growth mode and successfully built reefs in often
                            turbulent and unstable environments.
                        •  Reef-type structures were already present in the Late Precambrian hosting large, robust,
                            colonial organisms.
                        •  The cnidarians are the simplest of the higher metazoans with a radial diploblastic body
                            plan and stinging cells or cnidoblasts. The phylum includes sea anemones, jellyfi sh and
                            hydra together with the corals.
                        •  The Paleozoic rugose and tabulate corals displayed a wide range of growth modes often
                            related to environments; neither group was a dominant reef builder.
                        •  The scleractinians radiated during the Mesozoic with zooxanthellate forms dominating
                            biological reefs. Scleractinian-like morphs in Paleozoic faunas arose several times inde-
                            pendently from anemones with scleractinian-type polyps.
                        •  Reef development through time has waxed and waned, dominated at different times by
                            different groups of reef-building organisms.
                        •  Coloniality within the metazoans has evolved many times; one hypothesis suggests that
                            a Precambrian colonial organism may have been a source for the bilaterians.
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