Page 43 - The Restless Earth Fossils
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42   Fossils


                         and at a great expense, and showed and admired with as much
                         pleasure as a child’s rattle or a hobby-horse is shown and admired
                         by himself and his playfellows, because it is pretty; and this has
                         been done by thousands who have never paid the least regard to
                         that  wonderful order and regularity with which Nature has dis-
                         posed of these singular productions, and assigned to each class its
                         particular stratum.”
                             Smith  became  obsessed  with  an  idea:  He  would  create  a
                         map that would show in complete detail the inner structure of
                         England. In essence, it would be a geological road map that would
                         reveal details like those that had so impressed Hutton. Smith’s
                         project would take nearly twenty years to complete. It would cost
                         him dearly both in money and good health. But in the end, he
                         created an enormous 8-foot-by-6-foot (2.4 m by 1.8 m) detailed,
                         full-color map that would change the way people thought about
                         the world. He provided a book whose layered pages of rock and
                         stone contained “letters” of distinctive fossils that spoke about
                         past times and vast mineral and energy treasures to those who
                         could read them. And although his map only outlined the geo-
                         logical  “innards”  of  England,  other  scientists  found  the  same
                         layers—and some of the same fossils—all over the world. Fossils
                         especially useful for marking distinct points in geological time are
                         called index fossils.


                         What MaKes a good index Fossil?
                         Index fossils should: (1) be easy to find, but unique to particular
                         layers of rock; and (2) change gradually over time with a well-
                         defined  sequence  of  forms.  The  shells  of  various  invertebrate
                         animals  often  make  good  index  fossils  because  they  belong  to
                         relatively  small  creatures  that  reproduce  in  large  numbers,  fos-
                         silize readily, and possess ridges, pores, spines, and other distinc-
                         tive markings. Some examples include ammonites and baculites:
                         squidlike mollusks that floated in ancient seas and preyed on fish,
                         clams, worms, and trilobites. Ammonites possessed coiled shells
                         and baculites created straight shells not unlike skinny ice cream








        RE_Fossils2print.indd   42                                                             3/17/09   8:59:30 AM
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