Page 450 - Introduction to Paleobiology and The Fossil Record
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FISHES AND BASAL TETRAPODS  437






                                                                                                  Sarcopterygii


                 100
                  90                        Conodonta                       Placodermi
                  80
                Number of families  60  Cephalochordata  Petromyzontida  Heterostraci  Galeaspida  Osteostraci  Chondrichthyes  Actinopterygii
                  70
                  50
                  40
                  30
                  20
                  10  Tunicata   Myxinoidea           Anaspida  Thelodonti             Acanthodii
                  0
                                           Stem                            Gnathostomes         Crown










                                                                              Duplication





               Figure 16.7  Phylogeny of the basal fishes. One major genome duplication event was apparently

               associated with the origin of jaws. When the fossil groups (open lines) are omitted, there is a

               large morphological and genomic leap from jawless lampreys and hagfishes; when the fossil
               groups are included, as here, the transition appear much more gradual. The timing of the genome
               duplication events is uncertain, and falls within the area of the gray box. The number of families
               within each living and fossil group is shown by the shaded vertical bars. (Courtesy of Phil
               Donoghue.)




             spaced rows on their undersides (Fig. 16.8b).   lobefins, the sarcopterygians, that had thick,


             Acanthodians are often found preserved in       muscular, limb-like fins. Today, the lobefi ns
             vast numbers in the rock layers, so they prob-  are rare, being represented by only three

             ably swam in huge shoals in open water,         species of lungfishes and the rare coelacanth.
             perhaps feeding on small arthropods and         The coelacanth Latimeria is a famous “living
             plankton. They escaped predators by rapid       fossil”. Until 1938, coelacanths were only
             darting from side to side in their shoals, and   known as Devonian to Cretaceous fossils, but
             perhaps their exceptional spininess made them   in 1938 the world was astounded to hear that
             diffi cult to swallow.                           a living coelacanth had been fi shed  out  of
                                                             deep waters off East Africa, and more have
                                                             been caught since then.
             Bony fi shes: ray fi ns and lobefi ns
                                                               The ray fins of the Devonian include Chei-

             The osteichthyans, or bony fi shes,  also  ap -  rolepis (Fig. 16.8c), which had a fl exible body
             peared in the Devonian. There are two groups:   covered with small scales and a plated head.
             (i) those with ray-like fi ns, the actinopteryg-  This was an active predator that may have fed
             ians, ancestors of most fishes today from carp   on acanthodians. The Devonian lobefi ns

             to salmon, and seahorse to tuna; and (ii) the   include both lungfi shes  and  “rhipidistians”.
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