Page 72 - Introduction to Paleobiology and The Fossil Record
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TAPHONOMY AND THE QUALITY OF THE FOSSIL RECORD  59




                                                    dead organism




                                                  potential body fossil
                                   immediate burial                 decay and transport


                         complete preservation                      only hard parts
                         (rare)                                        left
                                                                       burial



                     preserved      recrystallized         material               material
                     unaltered
                                                           removed                added




                                    e.g. aragonite
                                      calcite
                                                                      mineral    sediment/   molecular
                                          partial        complete       into      mineral   replacement
                                                                       pores       infill



                                                        natural
                                                        mould


                                             natural cast                        internal cast

             Figure 3.1  How a dead bivalve becomes a fossil. The sequence of stages between the death of the
             organism and its preservation in various ways.


             and others in plants, and chitin, collagen        Decay processes exist because dead organ-
             and keratin in animals, which may exist in      isms are valuable sources of food for other
             isolation or in association with mineralized    organisms. When large animals feed on dead
             tissues.                                        plant or animal tissues, the process is termed
                                                             scavenging, and when microbes, such as fungi
                                                             or bacteria, transform tissues of the dead
             Decay
                                                             organism, the process is termed decay. Well-
             Decay processes typically operate from the      known examples of scavengers are hyenas
             moment of death until either the organism       and vultures, both of which strip the fl esh
             disappears completely, or until it is mineral-  from large animal carcasses. After these large

             ized, though mineralization does not always     scavengers have had their fill, smaller animals,
             halt decay. If mineralization occurs early, then   such as meat-eating beetles, may continue the
             a great deal of detail of both hard and soft    process of defleshing. In many cases, all fl esh

             parts may be preserved, so-called exceptional   is removed in a day or so. Decay is dependent
             preservation (see below). If mineralization     on three factors.
             occurs late, as is usually the case, decay pro-   The first factor controlling decay is the

             cesses will have removed or replaced all soft   supply of oxygen. In  aerobic (oxygen-rich)
             tissues and may also affect many of the hard    situations, microbes break down the organic
             tissues.                                        carbon of a dead animal or plant by convert-
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