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TAPHONOMY AND THE QUALITY OF THE FOSSIL RECORD  63












                                                              preservation
                                                              of soft parts in
                                            pyritization      carbonate
                                           high


                                                                         (d)
                  (b)                 Rate of
                                       burial



                                           low                       phosphatization
                                             low                 high
                                                      Organic
                                        (a)           content










                  (e)                                                   (c)
             Figure 3.3  The conditions for exceptional preservation. (a) The rate of burial and organic content are
             key controls on the nature of mineralization of organic matter in fossils. Pyritization (high rate of
             burial, low organic content) may preserve entirely soft-bodied worms, as in an example from the Early
             Devonian Hunsrückschiefer of Germany (b). Phosphatization (low rate of burial, high organic content)
             may preserve trilobite limbs such as this example of Agnostides from the Cambrian of Sweden (c). Soft
             parts may be preserved in carbonate (high rate of burial, high organic content), such as polyps in a
             colonial coral, Favosites, from the Early Silurian of Canada (d). If decay never starts, small animals
             may be preserved organically and without loss of material, such as a fly in amber from the Early

             Tertiary of the Baltic region (e). (a, based on Allison 1988; b, courtesy of Phil Wilby; c–e, courtesy of
             Derek Briggs.)


             and some chemical (bioerosion, corrosion and    noids, where the ligaments holding the sepa-
             dissolution).                                   rate skeletal elements together decay rapidly.
               Skeletons that are made from several parts    In trilobites and vertebrates, normal aerobic
             may become  disarticulated, separated into      or anaerobic bacterial decay may take weeks
             their component parts. For example, the mul-    or months to remove all connective tissues.
             tielement skeletons of armored worms and          Skeletons may also become  fragmented,
             vertebrates may be broken up by scavengers      that is, individual shells, bones or pieces of
             and by wave and current activity on the seabed   woody tissue break up into smaller pieces
             (Fig. 3.6a). Disarticulation happens only after   (Fig. 3.6b), usually along lines of weakness.
             the scavenging or decay of connective tissues   Fragmentation may be caused by predators
             that hold the skeleton together. This may       and scavengers such as hyenas that break
             occur within a few hours in the case of cri-    bones, or such as crabs that use their claws to
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