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18  INTRODUCTION TO PALEOBIOLOGY AND THE FOSSIL RECORD


                      cooperation of many people. The spectacular     and private funding sources must have con-
                      Burgess Shale fauna (Gould 1989; Briggs         tributed hundreds of thousands of dollars to
                      et al. 1994) was found by the geologist Charles   the continuing work of collecting, describing
                      Walcott in 1909. The discovery was partly by    and interpreting the extraordinary Burgess
                      chance: the story is told of how Walcott and    Shale animals.
                      his wife were riding through the Canadian         The Burgess Shale is a dramatic and unusual
                      Rockies, and her horse supposedly stumbled      example. Most paleontological research is
                      on a slab of shale bearing beautifully pre-     more mundane: researchers and students may
                      served examples of  Marrella splendens, the     spend endless hours splitting slabs, excavating
                      “lace crab”. During fi ve  subsequent  fi eld     trenches and picking over sediment from
                      seasons, Walcott collected over 60,000 speci-   deep-sea cores under the microscope in order
                      mens, now housed in the National Museum         to recover the fossils of interest. Laboratory
                      of Natural History, Washington, DC. The         preparation may also be tedious and long-
                      extensive researches of Walcott, together with   winded. Successful researchers in paleontol-
                      those of many workers since, have docu-         ogy, as in any other discipline, need endless
                      mented a previously unknown assemblage of       patience and stamina.
                      remarkable soft-bodied animals. The success       Modern paleontological expeditions go all
                      of the work depended on new technology          over the world, and require careful negotia-
                      in the form of high-resolution microscopes,     tion, planning and fund-raising. A typical
                      scanning electron microscopes, X-ray photog-    expedition might cost anything from
                      raphy and computers to enable three-dimen-      US$20,000 to $100,000, and fi eld paleontol-
                      sional reconstructions of fl attened fossils. In   ogists have to spend a great deal of time plan-
                      addition, the work was only possible because    ning how to raise that funding from government
                      of the input of thousands of hours of time in   science programs, private agencies such as the
                      skilled preparation of the delicate fossils, and   National Geographic Society and the Jurassic
                      in the production of detailed drawings and      Foundation, or from alumni and other spon-

                      descriptions. In total, a variety of government   sors. A typical high-profile example has been





                               Box 1.4  Giant dinosaurs from Madagascar


                        How do you go about finding a new fossil species, and then telling the world about it? As an example,
                        we choose a recent dinosaur discovery from the Late Cretaceous of Madagascar, and tell the story
                        step by step. Isolated dinosaur fossils had been collected by British and French expeditions in the
                        1880s, but a major collecting effort was needed to see what was really there. Since 1993, a team,
                        led by David Krause of SUNY-Stony Brook, has traveled to Madagascar for nine fi eld seasons with
                        funding from the US National Science Foundation and the National Geographic Society. Their work

                        has brought to light some remarkable new finds of birds, mammals, crocodiles and dinosaurs from
                        the Upper Cretaceous.
                           One of the major discoveries on the 1998 expedition was a nearly complete skeleton of a titanosau-
                        rian sauropod. These giant plant-eating dinosaurs were known particularly from South America and
                        India, though they have a global distribution, and isolated bones had been reported from Madagascar
                        in 1896. The new fossil was found on a hillside in rocks of the Maevarano Formation, dated at about
                        70 million years old, in the Mahajanga Basin. The landscape is rough and exposed, and the bones were
                        excavated under a burning sun. The fi rst hint of discovery was a series of articulated tail vertebrae, but
                        as the team reported, “The more we dug into the hillside, the more bones we found”. Almost every
                        bone in the skeleton was preserved, from the tip of the nose, to the tip of the tail. The bones were exca-
                        vated and carefully wrapped in plaster jackets for transport back to the United States.
                           Back in the laboratory, the bones were cleaned up and laid out (Fig. 1.12). Kristi Curry Rogers
                        worked on the giant bones for her PhD dissertation that she completed at SUNY-Stony Brook in
                        2001. Kristi, and her colleague Cathy Forster, named the new sauropod Rapetosaurus krausei in
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