Page 28 - The Restless Earth Fossils
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the tortuous road to Fossilhood  27


                          mining  the  famous  La  Brea  tar  pit  traps  in  the  center  of  Los
                          Angeles, California. Many insects, birds, turtles, and plant parts
                          also found their way into the tar. Quick burial and low oxygen
                          preserved their remains intact—in this case for tens of thousands
                          of years.

                          carBonization: Fossil “road Kill”

                          A  paleontologist  visiting  Douglas  Pass,  Colorado,  high  in  the
                          Rocky Mountains, may use her rock hammer to pop apart a thick
                          slab  of  shale  and  find  the  dark  brown  image  of  a  Macginitiea
                          (sycamore) leaf or a fossil cranefly. A musty smell reminds her
                          of  fish  and  rotting  vegetation  on  a  lakeshore.  The  leaf  or  the
                          insect has been carbonized: partially decayed, wrapped in slime,
                          crushed, and heated.
                             Herbert  W.  Meyer,  a  paleontologist  with  the  U.S.  National
                          Park Service, has studied this process in some detail at famous
                          fossil beds (the site of ancient lakes) near Florissant, Colorado.
                          The layers of shale at Florissant and Douglas Pass, as well as other
                          locations in Utah and Wyoming, alternate with the ash from vol-
                          canic eruptions. Many of the early workers at these sites assumed
                          that animals and plants in the lakes died and were preserved in
                          mass dying events during volcanic eruptions, but careful studies
                          have shown that much of this preservation happened in the peri-
                          ods between these violent events. “The thin shale layers formed
                          slowly  over  many  decades,”  says  Meyer,  “whereas  the  layers  of
                          volcanic ash accumulated much more rapidly.”
                             Images taken of Florissant fossils with a scanning electron
                          microscope  have  shown  that  leaves  and  delicate  insect  wings
                          are covered with a thin layer of billions of tiny plant cells called
                          diatoms. Growing abundantly in lake water enriched with silica
                          from  volcanic  ash,  these  diatoms  and  bacteria  covered  dead
                          insects,  fish,  and  leaves  floating  on  or  in  the  lake  with  a  thin
                          film  that  is  almost  like  plastic  wrap.  This  film  helped  preserve
                          the  organisms  long  enough  to  be  buried  by  successive  layers
                          of  silt  and  volcanic  ash.  The  weight  of  these  layers  ultimately










        RE_Fossils2print.indd   27                                                             3/17/09   8:58:56 AM
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