Page 44 - Introduction to Paleobiology and The Fossil Record
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FOSSILS IN TIME AND SPACE  31




                            Section  1                Section  2                Section  3
                         A    B    C                A    B   C                A    B    C











                                   RASC solution                      Maximal range solution
                                  A    B    C                          A    B   C









                      (c)
                Figure 2.4 (Continued)  (c) The RASC method predicts the solution most likely to occur in the
                next section based on previous data. Three sections (1–3) are presented and, based on a majority

                vote, the RASC solution is constructed; since the first two sections are similar they win over the
                third slightly different section. This is different to the maximum range solution that may be
                constructed by other methods. (c, based on Hammer & Harper 2005.)







                                          Foraminifera  Sponges  Corals  Bryozoans  Brachiopods  Bivalves  Gastropods  Nautiloids  Ammonoids  Belemnites  Trilobites  Ostracodes  Crinoids  Echinoids  Graptolites




                                Quaternary
                                Tertiary
                               Cretaceous
                                 Jurassic
                                 Triassic
                                Permian
                             Carboniferous
                               Devonian
                                Silurian
                              Ordovician

                               Cambrian
                            important for          used for zoning      only occasionally or
                            world-wide zoning      and correlation      never, used
                            and correlation        of regions           for zoning and
                                                                        correlation

             Figure 2.5  Approximate stratigraphic ranges through time of the main biostratigraphically useful
             invertebrate fossils groups. (Replotted from various sources.)
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