The Fossil Record

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    The Fossil Record - Presentation Transcript

    1. The Fossil Record Def: the traces or remains of animals or plants from a previous geologic time.
    2. Paleontologist
      • Study fossils to learn about past geologic events, climates, and evolution.
    3. Most fossils are found in sedimentary rock…
      • Cover a dead object without damaging it.
      • Keep other animals from destroying “potential” fossils.
      keichosaurus
    4. No fossils in igneous or metamorphic rocks !?
      • Living things covered with hot, molten lava tend to burn up…
      • … and fossils in metamorphised rocks become pressured/heated beyond recognition.
      • Usually, only the HARD parts of an organism are preserved…bones, shells, teeth.
      • Sometimes, only a replica of the organism remains.
    5. Normally…
      • Dead plants & animals are usually eaten by other animals or decomposed by bacteria before they can become fossils.
      • Only dead orgs that get buried quickly by sediment stand a chance of getting preserved as fossils.
    6. Types of Fossilization
    7. Mummification
      • Organisms become dried out.
      • Usually found in desert caves or buried in desert sand.
      • Org doesn’t rot : bacteria need moisture to “work.”
    8. Amber
      • Hardened tree sap.
      • Delicate structures preserved (legs, antennae)
      • DNA has been extracted from these fossils…
    9. Tar Beds
      • Pools of “black gold” at the Earth’s surface usually covered by water.
      • Animals come to drink, get stuck in the tar, and get sucked in…
      La Brea Tar Pits in L.A.
    10. Freezing
      • Low temps of frozen soil & ice protect & preserve organisms.
      • Org doesn’t rot: bacteria can’t survive freezing temps.
      • Rhinos, mastodons, mammoths found in Alaska & Siberia.
    11. Petrification
      • Mineral-rich groundwater removes & replaces the original mineral with a harder mineral (such as silica, calcite, pyrite).
      • Petrified wood!
    12. Traces of Organisms
      • TRACE FOSSILS such as tracks, footprints, borings, and burrows can provide information about organisms.
    13. Imprints
      • Leaves, stems, shelled creatures, flowers, fish… become stuck in soft clay and leave an imprint which shows the surface features of the organism.
    14. Molds
      • An organism gets buried in soft sediment…
      • … its remains decay, leaving an empty space…a “bubble” of nothing in the shape of the organism
      • A mold retains the shape & exterior markings of the org, but tells us zero about the “insides.”
    15. Casts
      • When sand or mud gets inside a mold & hardens, a cast is formed.
      • A cast is a replica of the outer surface of the original org.
      Montana Rhinos
    16. Index Fossils
      • Certain fossils are found only in the rock layers of a particular geologic age.
      • These are known as INDEX FOSSILS.
      Paradoxides :Cambrian Era
    17. To Qualify as an Index Fossil:
      • Must be “world-wide.”
      • Must be distinctive.
      • Must have a “short” life span.
      • Must be numerous!
      Echioceras: Jurassic Period
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