Page 64 - The Restless Earth Fossils
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Marking turning points in evolution  63


                          western Colorado yield fossil insects and leaves. In 2002, volun-
                          teers  helped  the  Denver  Museum  of  Nature  and  Science,  Utah
                          State Parks, and the U.S. Bureau of Land Management personnel
                          excavate more than 300 square feet (28 square meters) of Green
                          River Formation leaf and insect fossils to line the walls of a new
                          museum  in  Vernal,  Utah.  The  work  also  discovered  new  speci-
                          mens to illustrate the Parachute Creek Atlas Project—an Eocene
                          fossil  plant  record  that  complements  work  done  on  “flashier”
                          vertebrate species.


                          Mass extinctions: liFe on the edge
                          oF disaster

                          The fossils associated with the Paleozoic, Mesozoic, and Cenozoic
                          Eras stand out by their differences. Paleontologists can see those
                          dramatic  differences  in  the  rock.  The  boundary  between  the
                          Mesozoic and Cenozoic Eras—the marker for the end of the reign
                          of dinosaurs—is a seam of clay that can be covered by the width
                          of a human hand. In the late 1970s, geochemist Lewis Alvarez and
                          his father, Walter, a geologist and geophysicist, collected samples
                          from the boundary layer exposed near Gubbio, Italy, where it is
                          sandwiched  between  layers  of  pink  limestone.  They  found  that
                          the layer contained a very high concentration of iridium, an ele-
                          ment usually rare on Earth, but common in meteors and aster-
                          oids—the  leftover  debris  of  planet  building  during  the  birth  of
                          the solar system. Also present were deformed particles of quartz
                          called shocked quartz that result from the impacts of meteors
                          with the Earth.
                             Other  scientists  found  these  same  features  at  sites  all  over
                          the  world.  Radiometric  studies  dated  the  layer  to  65.5  million
                          years old—precisely the age of the Cretaceous-Tertiary boundary
                          (abbreviated as the KT boundary) as determined by other meth-
                          ods. Alvarez calculated that an object the size of Mount Everest
                          must have struck the Earth to leave a worldwide trace of this mag-
                          nitude. That would have left a crater some 110 miles (180 km)
                          wide. No one was aware of a crater that size until the early 1990s,









        RE_Fossils2print.indd   63                                                             3/17/09   9:00:08 AM
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