Page 170 - Introduction to Paleobiology and The Fossil Record
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FOSSIL FORM AND FUNCTION  157


                                     stance phase          swing phase









                          (a)
                                     early stance            mid-stance      late stance

                                                                     muscle
                                                                    moment

                                           GRF                  {
                                                              knee
                                                            moment
                                                              arm
                          (b)                         (c)             (d)










                          (e)                (f)                       (g)

             Figure 6.13  The running stride of Tyrannosaurus rex. (a) The main components of a stride, showing
             the stance phase when the foot touches the ground, and the swing phase. (b–d) Three positions of the
             limb in early stance, mid-stance and late stance, as the body moves forward, and showing the main
             forces, including the ground reaction force (GRF). (e–g) Three alternative postures for the limb, with
             the body held high or low. Read more, and see the movies at http://www.rvc.ac.uk/AboutUs/Staff/
             jhutchinson/ResearchInterests/beyond/Index.cfm. (Courtesy of John Hutchinson.)


                example, fossil reefs may be killed off in      There are some rare examples of arthro-
                a particular crisis, and all the organisms      pods preserved at the ends of their trails.
                that lived together are found in life posi-     The link between trace fossil and producer
                tion; some corals, bryozoans and crinoids       is usually a little less clear: dinosaur foot-
                may be fixed to the substrate in their           prints may be found at certain levels within

                normal growth position, and mobile              a particular geological formation, and the
                organisms like gastropods or trilobites         skeletons of likely producers at other
                may be preserved among the thickets of          levels. The bones of fishes and marine rep-

                benthic sessile organisms. Similarly, a         tiles may be found associated with phos-
                paleosol (see p. 518) may preserve roots        phatic  coprolites (fossil dung) in certain
                and stems of dozens of plants in life posi-     marine beds – it is likely that the copro-
                tion, together with burrows of insects and      lites were dropped by one or other of the
                worms that lived among them. Associa-           associated animals. If a link can be made
                tions of fossils can also be more intimate,     between a trace fossil and its maker, then
                where for example parasites may be found        a great deal of additional paleobiologi-
                attached to their hosts, or fossils of one      cal information can be established (see
                species may be found in the stomach             Chapter 19).
                region of another.                           4  Close study of the body fossils themselves
             3  Associated trace fossils can sometimes be       is also warranted. Skeletal fossils regularly
                linked to their producers, but not always.      preserve evidence of soft tissues and other
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