The Fossil Record Def: the traces or remains of animals or plants from a previous geologic time.
Paleontologist Study fossils to learn about past geologic events,  climates, and evolution.
Most fossils are found in sedimentary rock… Cover a dead object without damaging it. Keep other animals from destroying ā€œpotentialā€ fossils. keichosaurus
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.
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.
Types of Fossilization
Mummification Organisms become dried out. Usually found in desert caves or buried in desert sand. Org doesn’t rot : bacteria need moisture to ā€œwork.ā€
Amber Hardened tree sap. Delicate structures preserved (legs, antennae) DNA has been extracted from these fossils…
Tar Beds Pools of ā€œblack goldā€ 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.
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.
Petrification Mineral-rich groundwater removes & replaces the original mineral with a harder mineral (such as silica, calcite, pyrite). Petrified wood!
Traces of Organisms TRACE FOSSILS such as tracks, footprints, borings, and burrows can provide information about organisms.
Imprints Leaves, stems, shelled creatures, flowers, fish… become stuck in soft clay and leave an imprint which shows the surface features of the organism.
Molds An organism gets buried in soft sediment… … its remains decay, leaving an empty space…a ā€œbubbleā€ of nothing in the shape of the organism A mold retains the   shape & exterior markings   of the org, but tells us zero about the ā€œinsides.ā€
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
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
To Qualify as an Index Fossil: Must be ā€œworld-wide.ā€ Must be distinctive. Must have a ā€œshortā€ life span. Must be numerous! Echioceras: Jurassic Period

The Fossil Record

  • 1.
    The Fossil RecordDef: the traces or remains of animals or plants from a previous geologic time.
  • 2.
    Paleontologist Study fossilsto learn about past geologic events, climates, and evolution.
  • 3.
    Most fossils arefound in sedimentary rock… Cover a dead object without damaging it. Keep other animals from destroying ā€œpotentialā€ fossils. keichosaurus
  • 4.
    No fossils inigneous or metamorphic rocks !? Living things covered with hot, molten lava tend to burn up… … and fossils in metamorphised rocks become pressured/heated beyond recognition.
  • 5.
    Usually, only theHARD parts of an organism are preserved…bones, shells, teeth. Sometimes, only a replica of the organism remains.
  • 6.
    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.
  • 7.
  • 8.
    Mummification Organisms becomedried out. Usually found in desert caves or buried in desert sand. Org doesn’t rot : bacteria need moisture to ā€œwork.ā€
  • 9.
    Amber Hardened treesap. Delicate structures preserved (legs, antennae) DNA has been extracted from these fossils…
  • 10.
    Tar Beds Poolsof ā€œblack goldā€ 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.
  • 11.
    Freezing Low tempsof frozen soil & ice protect & preserve organisms. Org doesn’t rot: bacteria can’t survive freezing temps. Rhinos, mastodons, mammoths found in Alaska & Siberia.
  • 12.
    Petrification Mineral-rich groundwaterremoves & replaces the original mineral with a harder mineral (such as silica, calcite, pyrite). Petrified wood!
  • 13.
    Traces of OrganismsTRACE FOSSILS such as tracks, footprints, borings, and burrows can provide information about organisms.
  • 14.
    Imprints Leaves, stems,shelled creatures, flowers, fish… become stuck in soft clay and leave an imprint which shows the surface features of the organism.
  • 15.
    Molds An organismgets buried in soft sediment… … its remains decay, leaving an empty space…a ā€œbubbleā€ of nothing in the shape of the organism A mold retains the shape & exterior markings of the org, but tells us zero about the ā€œinsides.ā€
  • 16.
    Casts When sandor 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
  • 17.
    Index Fossils Certainfossils are found only in the rock layers of a particular geologic age. These are known as INDEX FOSSILS. Paradoxides :Cambrian Era
  • 18.
    To Qualify asan Index Fossil: Must be ā€œworld-wide.ā€ Must be distinctive. Must have a ā€œshortā€ life span. Must be numerous! Echioceras: Jurassic Period