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Fossils

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Organism is enclosed by material that prevents decay. Example. Ants in amber. Tar pits. How Fossils are Formed. Petrification (Mineral Replacement) ... – PowerPoint PPT presentation

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Title: Fossils


1
Fossils
  • Earth History Part II

2
Fossils
  • Any part, remnant or evidence left by an organism
    in a rock
  • Fossils are found in sedimentary rocks

3
How Fossils are Formed
  • Original Remains
  • Actual unchanged remains
  • Wooly Mammoths
  • Replaced Remains
  • Hard parts have been replaced by minerals
  • Petrified wood

4
How Fossils are Formed
  • 5 ways
  • Molds
  • Casts
  • Refrigeration
  • Encasement
  • Petrification

5
How Fossils are Formed
  • Mold
  • Creature is dissolved completely out of the rock
    leaving a depression
  • Cast
  • New material fills the mold

6
How Fossils are Formed
  • Refrigeration
  • Freezing organism
  • Preserved in ice
  • Wooly Mammoth in glaciers

7
How Fossils are Formed
  • Encasement
  • Organism is enclosed by material that prevents
    decay
  • Example
  • Ants in amber
  • Tar pits

8
How Fossils are Formed
  • Petrification (Mineral Replacement)
  • Mineral crystals replace cells in the organism
  • Example
  • Petrified wood

9
Trace Fossil
  • Evidence of life other than the remains of a
    plant or animal
  • Footprints
  • Tracks
  • Burrows
  • Borings

10
Index Fossil
  • Fossils that are typical of a particular time
    segment of Earths history.

11
3 Characteristics of Index Fossils
  • 1.) Must be easily recognizable. Unique in some
    way so they can easily be told from other similar
    fossils.
  • 2.) Must be widespread in occurrence
    geographically.
  • 3.) Limited in time.
  • 4.) Abundant

12
Key Bed
  • A single rock layer that has the same
    characteristics as an index fossil.
  • Example A large volcanic eruption.

13
Other Uses
  • Fossils are also used to tell us about past
    climates.
  • Fossils and microfossils are also used for
    correlation.

14
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15
Principle of Fossil Succession
  • When fossils are arranged according to their age
    in sedimentary rocks, they show progressive
    changes and different groups of organisms coexist
    at different times.

16
Hiatus location where the rock record is
missing one or more layers
17
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18
Fossil Evidence
  • Direct
  • Actual organism is preserved in some way
  • Indirect
  • A replica or model of the organism shape or an
    activity it made

19
Which ones are direct?
  • Refrigeration
  • Encasement

20
Which ones are indirect?
  • Molds
  • Casts
  • Petrification

21
Direct or indirect?
22
Direct or indirect?
23
Direct or indirect
24
Direct or indirect?
25
Direct or indirect?
26
Direct or indirect?
27
Direct or indirect?
28
Direct or indirect?
29
Direct or indirect?
30
Direct or indirect?
31
Direct or indirect?
32
Direct or indirect?
33
Direct or indirect?
34
K-T Boundary
  • The divisions of the time scale were based on the
    observations that large percentages of animals
    and plants became extinct at certain intervals.
  • The most talked about of these is the extinction
    at the end of the Cretaceous (KT extinction) .
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