Page 427 - Introduction to Paleobiology and The Fossil Record
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414  INTRODUCTION TO PALEOBIOLOGY AND THE FOSSIL RECORD


                      marine snow, a bonding material composed        ognized in the class Graptolithina, but only
                      of organic debris and mucus; this seems         two, the Dendroidea and Graptoloidea have
                      less likely because the synrhabdosomes are      important geological records. The patterns of
                      remarkably symmetric, which suggests they       evolution linking these groups are uncertain
                      grew that way. About six orders are now rec-    (Box 15.9).






                                 Box 15.9 The fi rst graptolites: a cryptic Cambrian dimension?


                        By the Ordovician, the graptolites were represented by a number of well-defi ned groups including
                        the familiar dendroids and graptoloids and the less well-known camaroids, crustoids, dithecoids and
                        tuboids. It has long been a mystery where these diverse groups came from because the Cambrian
                        record was virtually non-existent. Barrie Rickards and Peter Durman (2006) have reassessed all the
                        possible ancestors, Cambrian specimens that have been variably assigned to graptolites, hydroids or
                        algae from the Middle and Upper Cambrian. They reassigned some of these cryptic Cambrian speci-
                        mens to the rhabdopleurids and excluded a number of them from the graptolites. The graptolites
                        and rhabdopleurids therefore probably shared a common ancestor in the Early Cambrian (Fig.
                        15.22). The rhabdopleurids are remarkable animals; Cambrian forms are virtually identical to
                        modern rhabdopleurids, making them true living fossils. The common ancestor to the graptolites
                        and rhabdopleurids was probably a solitary, worm-like animal, equipped with a lophophore, and


                        living in pseudocolonial filter-feeding clumps on the seafloor. Thus the graptolites, which dominated
                        the Early Paleozoic water column, started out as rather anonymous benthic filter feeders in the

                        shadow of the more obvious early arthropods, crinoids and mollusks of the Cambrian evolutionary
                        fauna.

                                      Carboniferous  Rhabdopleurids                Dendroids





                                      Devonian                                             Graptoloids

                                                                    Tuboids

                                      Silurian               Crustoids      Dithecoids


                                      Ordovician      Camaroids




                                      Cambrian








                        Figure 15.22  Generalized phylogenetic model for rhabdopleurid and graptolite evolution. (From
                        Rickards & Durman 2006.)
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