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FISHES AND BASAL TETRAPODS  435
                                                                    CONODONT ZONES   STAGES








                        Skinnerbukta                    Pseudolonchodina fluegeli  Pterospathodus celloni  Aulacognathus bullatus Pseudooneotodas tricornis Pterospathodus amorphognathoides





                               Ireviken Event  Icriodella discreta  Ozarkodina hassi  O. oldhamensis  O? kentuckyensis  Pranognathos tenuis  Distomodus spp.  Carniodus carnulus  Pterospathodus
                                                                     amorphognathoides
                              Snipklint Primo                                        Telychian
                        Vik     Episode                               Pterospathodus
                                                                         celloni

                        Rytteråker  Malmøykalven                     staurognathoides
                                Secundo
                                                                       Distomodus
                                Episode
                              Sandvika Event
                             Jong Primo Episode                                      Aeronian



                        Solvik  Spirodden                              Distomodus
                                Secundo
                                Episode                               kentuckyensis
                                                                                    Rhuddanian




               Figure 16.6  The use of conodont assemblages in stratigraphy: alternation of primo and secundo
               oceanic states correlated with part of the Lower Silurian succession of the Oslo region, Norway.
               In the stratigraphic column, limestone is shown by a blocky pattern and mudstone by gray.
               (Courtesy of Dick Aldridge.)





             anterior comb-like ramiform elements proba-     linked by tiny muscles. The transition cannot
             bly grasped prey items that were sucked         be followed in fossils because the gill skeleton
             towards the mouth, and the posterior pectini-   of jawless fi shes was not mineralized. Molecu-
             form elements may have chomped the food         lar biologists have even suggested that the
             before swallowing. One the greatest mysteries   origin of jaws was so profound that it must
             in paleontology had been solved.                have been associated with a dramatic genome
                                                             duplication event – but the fossils say no (Box
                                                             16.4).
             JAWS AND FISH EVOLUTION                           Some of the oldest jaw-bearing fi shes were
                                                             the placoderms, such as  Coccosteus (Fig.
             The fi rst jaws
                                                             16.8a), which had an armor of large bony
             The basal vertebrates, including conodonts,     plates over the head and shoulder region, as
             lacked jaws, and jaws probably evolved during   in the ostracoderms, and a more lightly
             the Ordovician. Study of the anatomy of         armored posterior region. They swam by
             modern vertebrates suggests that jaws may       beating this tail region from side to side. The
             have evolved from the strengthening bars of     edges of the jaws did not carry teeth, but
             cartilage or bone between the gill slits, each   instead sharp bony plates that would have
             of which consists of several elements, all      been just as effective in snapping at prey.
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