Chapter 17-1: The Fossil Record - PowerPoint PPT Presentation

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Chapter 17-1: The Fossil Record

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Chapter 17-1: The Fossil Record Essential Questions: What is the fossil record? What is the difference between relative dating & radioactive dating? – PowerPoint PPT presentation

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Title: Chapter 17-1: The Fossil Record


1
Chapter 17-1 The Fossil Record
  • Essential Questions
  • What is the fossil record?
  • What is the difference between relative dating
    radioactive dating?
  • What are the main divisions of geologic time
    scale?

2
  • Half of a Half of a Half . . .
  • Some forms of chemical elements are unstablethat
    is, they break down into other substances. Like
    the decay of leftovers in your refrigerator, this
    breakdown takes place over time. Unlike those
    leftovers, however, the breakdown of unstable
    forms of an element progresses in a very orderly
    wayby decaying into halves.

3
  • 1. Using your ruler, draw a line 24 cm in length
    on a sheet of paper. Make a mark at the halfway
    point (12 cm).
  • 2. Then, divide this 12-cm segment in half,
    making a mark at 6 cm. Continue in this way,
    dividing each progressively smaller segment in
    half (ignoring all of the other segments) until
    it becomes too small to accurately measure.
  • 3. Now count each progressively smaller
    half- segment. How many segments did you count?

4
  • Fossils ancient life
  • Paleontologist study fossils
  • Fossil record
  • Provides evidence of history of life on Earth
  • Shows how different organisms have changed over
    time
  • 99 of species that have lived on Earth now
    extinct

5
  • How fossils form

6
  • Interpreting fossil evidence
  • Relative dating
  • Position of sediment beds relative to each other
    gives relative ages

7
  • Radioactive dating
  • Isotope form of element with different numbers
    of neutrons
  • Ex C12 C14 2 extra neutrons in C14
  • While a sample is losing neutrons, its
    radioactive
  • Amount of time for ½ of isotopes in sample to
    revert to stable form is its half-life
  • For C14 ? 5440 years
  • If we look at of C14 C12
  • Ex 25 C14 75 C12
  • 2? 10,880 years old
  • Other isotopes decay more slowly
  • Potassium ? 1.3 billion years

8
  • Geologic time scale
  • Eras and periods defined by major changes in the
    fossil record
  • Divisions are not
  • even amounts
  • Ex Precambrian
  • era about
  • 90 of Earths
  • history
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