Page 370 - Introduction to Paleobiology and The Fossil Record
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SPIRALIANS 2: MOLLUSKS  357


                        shell aperture
                                                               Eras       Periods
                                                                        Quaternary
                      gonad                                                 Pliocene
                                   kidney                                Neogene  Miocene
                                  anus                        Cenozoic
                                       water–sediment interface        Tertiary  Oligocene
                                                                             Eocene
                   gut           mantle cavity                           Paleogene  Paleocene
                                mantle
                                                                           Cretaceous
                 head
                                                                 Mesozoic   Jurassic
                                                                             Triassic
                               foot                                         Permian
                                                                         Upper  Carboniferous
                                                                            Devonian
             (a)                                                Paleozoic
                                                                            Silurian
                  gape
                                                                         Lower  Ordovician
                                              rostrum
                                                                            Cambrian
                                                                                      Monoplacophora  Diplacophora  Helcionellida  Bivalvia  Rostroconchia  Tergomyonia  Cephalopoda  Polyplacophora  Gastropoda  Scaphopoda  Aplacophora



                  anterior                    posterior
                  (b)
             Figure 13.25  (a) Scaphopod morphology and      Figure 13.26  Stratigraphic range of the main
             (b) rostroconch morphology.                     mollusk groups.



             benthos of the Paleozoic, although many more    neogastropods, and with a further diversifi ca-
             localized, often nearshore, assemblages were    tion of mesogastropods (Fig. 13.26).
             dominated by mollusks.                            The cephalopods evolved through the
               During the Paleozoic, bivalves were           development of a chambered shell with a sip-
             common in nearshore environments, often         huncle, which gave them considerable control
             associated   with   lingulide  brachiopods,     over attitude and buoyancy; this system was
             although the class also inhabited a range of    refi ned in the nautiloid groups. The evolution
             deeper-water clastic environments; and by the   of complex folded sutures in the ammonoids,
             Late Paleozoic bivalves had invaded a variety   the exploitation of a pelagic larval stage and
             of carbonate environments. However, at the      a marginal position for the siphuncle appar-
             end of the Paleozoic, the appearance of more    ently set the agenda for the further radiation
             typical bivalves in shallow-water belts may     of the group during the Mesozoic.
             have displaced the Paleozoic associations         Throughout the Phanerozoic, the fl eshy
             seaward. During the Late Mesozoic and Ceno-     mollusks provided a source of nutrition for
             zoic the significant radiation of infaunal       many groups of predators. The evolution of

             taxa may have been a response to increased      the phylum was probably in part infl uenced
             predation.                                      by the development of predator–prey rela-
               The majority of Paleozoic gastropods were     tionships and minimization of predator
             Eogastropoda that commonly dominated            success. Thick armored shells were developed
             shallow-water marine environments and some      in some groups while the evolution of deep-
             carbonate reef settings. The Mesozoic, however,   infaunal life modes was also part of a defen-
             was dominated by the Mesogastropoda, which      sive strategy. Predation and the development
             grazed on algal-coated hard substrates. The     of avoidance strategies, together with the
             Cenozoic, marks the acme of the group with      so-called arms race, had an important infl u-
             the radiation of the siphonal carnivorous       ence on molluskan evolution. Predators
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