Page 33 - The Restless Earth Fossils
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32   Fossils


                             A  collector  can  section  a  completely  mineralized  piece  of
                         wood with a rock saw and see even microscopic cellular detail.
                         Bones have a similar porous structure that makes them perfect for
                         permineralization. The phosphate compounds that make up bone
                         may  change  composition  somewhat  by  incorporating  chlorine
                         and/or  fluorine  atoms  rather  than  being  completely  replaced.
                         Iron  sulfides  may  replace  calcium  carbonate  shells  or  other
                         organic materials buried in low-oxygen, ocean-bottom mud, in a
                         process aided by bacteria, to produce fool’s gold, or pyrite. Such
                         fossils truly look like creatures dipped in gold.


                         casts, Molds, and other variations on
                         the theMe

                         Not  all  fossils  become  exact  replicas  of  their  living  model.  In
                         the tree example, the sand and mud around the trunk may have
                         hardened to stone, but all the organic material of the tree ulti-
                         mately decayed completely. This left a hollow cylinder, or mold,
                         that displayed the exact shape and outer detail of the tree trunk.
                         If this natural mold then filled with minerals or more mud before
                         breaking apart or eroding away, a cast of the tree would remain
                         behind. The cast would have the shape and outer texture of the
                         tree but inside it could be pure agate, a form of silicon dioxide.
                         This  kind  of  petrified  fossil  is  also  called  a  pseudomorph,  or
                         “false form.”
                             Shells also make good fossils because they are hard and resis-
                         tant to change. Animals create their shells out of a form of cal-
                         cium  carbonate  called  aragonite.  Aragonite  often  recrystallizes
                         into the more stable form of calcium carbonate called calcite. At
                         other times, shells end up as casts or molds or both.
                             Some popular fossils called trilobites are the casts, molds, and
                         petrified remains of arthropods whose shells were composed of
                         chitin, like modern crabs and insects. A person finding a mold of
                         a trilobite shell can easily make a cast of the animal by pressing
                         some clay into the mold. Because trilobites and other arthropods
                         grow larger by shedding old shells and growing new ones after
                         their  bodies  take  up  water  and  expand,  each  animal  has  the







        RE_Fossils2print.indd   32                                                             3/17/09   8:59:12 AM
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