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A Trip Through Geologic Time

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Title: A Trip Through Geologic Time


1
A Trip Through Geologic Time
2
The Fossil Record
  • fossils tell the history of life on earth
  • not all organisms form fossils
  • conditions necessary for fossil formation
  • protected from destruction and decay
  • sediments bury it and become rock
  • hard parts

3
Types of Fossils
  • petrified fossils mineralized copies of
    original bones
  • minerals in water replace original matter
  • parts turned to stone

4
  • molds and casts
  • mold - cavity in the shape of an organism
  • cast - minerals fill in the cavity

5
  • trace fossils
  • footprints, tracks, trails, and burrows
  • coprolites
  • tell about what an organism ate
  • unchanged fossils
  • amber, tar pits

6
Interpreting FossilsRelative Age Dating
  • principle of superposition
  • -younger rock on top of older rock
  • -basis for most relative age dating of fossils

7
Disruption of Layers
  • folding faulting disrupt order of layers
  • erosion removes layers

8
  • Rules for interpreting layers
  • Rock layers are horizontal before they deform
  • A fault or igneous dike did not exist when the
    layers formed, and is younger than the layers it
    cuts across

9
Absolute Dating
  • absolute dates expressed in years
  • Radiometric dating compares amount of
    radioactive isotope present to the amount of
    decay present
  • half-life time it takes for half of isotope to
    decay

10
Isotope Half-Life (Years) Used to Date
Thorium-232 14 billion Very old rocks
Potassium-40 1,300 million Old rocks fossils in them
Carbon-14 5,730 Fossils less than 50,000 years old
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The Geologic Time Scale
  • Geologic Eras
  • Precambrian
  • Paleozoic Era
  • Mesozoic Era
  • Cenozoic Era

13
Precambrian Era The Dawn of Life
  • 4600 mya - 540 mya
  • Earths history begins
  • Seas form from volcanic emissions comet
    impacts.
  • Continents form grow.
  • Oxygen builds up in atmosphere from
    photosynthesizing organisms (stromatolites)

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Paleozoic EraOld Life - Life Comes Ashore
  • 540 mya - 248 mya
  • Age of Invertebrates
  • Began with Cambrian Explosion of new life
    forms, due to preceeding mass extinction.
  • Abundant sea life. First fishes appear, first
    amphibians evolved from fishes, first reptiles
    evolved from amphibians.
  • First terrestrial life (arthropods other
    invertebrates) invades from sea.
  • Carboniferous swamps create coal deposits.
  • Pangaea formed near end of era.

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Mesozoic Era Middle Life - Age of Dinosaurs
  • 248 mya - 65 mya
  • Era of many changes
  • Dinosaurs, birds, mammals all evolved from
    reptiles. Mammals avoid competition
    with/predeation by dinosaurs by being nocturnal
    eating insects.
  • Pangea broke up 200 mya.
  • Flowering plants became dominant plant life.

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Cenozoic Era New Life - Age of Mammals
  • 65 mya present
  • Mammals dominated.
  • Primates, human ancestors, modern humans
    evolved.
  • Land bridge formed between N. S. America,
    disrupted ocean currents triggered Ice Ages -
    sheets of ice advance and recede several times.
  • Alps and Himalaya Mountains form from collisions
    of continents.

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Check These Out!
  • Geologic Time Machine
  • Fossils, Rocks, and Time
  • Ice Age Paleoecology
  • USGS FAQ about Dinosaurs
  • Carbon-14 Dating
  • Paleontology Without Walls
  • Dinosaur Images
  • Paleomapping Project

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The End
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