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CHAPTER 14 NOTES

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Title: CHAPTER 10.4 AND 11 NOTES Author: Heather Krueger Last modified by: Bernal, Nicole Created Date: 12/28/1999 5:34:57 PM Document presentation format – PowerPoint PPT presentation

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Title: CHAPTER 14 NOTES


1
CHAPTER 14 NOTES
HOW LIFE BEGAN?
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Inorganic (nonliving) matter was transformed into
simple organic molecules
  • Miller-Urey experiment (they modeled the ancient
    atmosphere in a reacting chamber, then electrodes
    produced sparks to simulate lightning and after
    one week they found the liquid produced by the
    experiment contained amino acids the building
    blocks of proteins)
  • Eventually these simple organic molecules changed
    into cells with DNA and a nucleus

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FOSSILS
  • Paleontologists are scientists who study fossils
  • The fossil record provides evidence about the
    history of life on Earth and it also shows how
    different groups of organisms, including species,
    have changed over time
  • Most fossils form in sedimentary rock

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FOSSIL DATING
  • RELATIVE VS. RADIOACTIVE

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RELATIVE DATING
  • Determines the age of a fossil by comparing its
    placement with that of fossils in other layers of
    rock
  • Oldest fossils are in lower layers of the rock
  • Draw the picture on your notes which fossil is
    older? _____

B
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RADIOACTIVE DATING
  • The use of half-lives to determine the age of a
    fossil
  • Radioactive decay occurs at a constant rate
    called a HALF-LIFE (the time it takes for half of
    the atoms in a sample to undergo radioactive
    decay)
  • EX. The half-life of Potassium-40 is 1.26
    billion years
  • Ex. The half-life of Carbon-14 is 5730 years
  • Potassium dating is used for rocks that are
    suspected to be billions of years old and carbon
    dating is used for younger fossils (50,000 years)

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EXAMPLE PROBLEM
  • Suppose there are 16 grams of Carbon-14 in a
    living snail shell and 4 grams of Carbon-14 in a
    fossilized snail shell
  • How many half-lives has this fossil gone through?
  • 2
  • What is the age of the fossil if each half-life
    of Carbon-14 takes 5730 years?
  • 5730 X 2 11,460
  • How many grams of Carbon-14 will be left if the
    snail shell goes through one more half-life?
  • 2 grams

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GEOLOGIC TIME SCALE
  • In order to catalog the 4 billion years of life
    on Earth, scientists have created the geologic
    time scale to represent evolutionary time
  • The scale is divided into large time spans called
    ERAS, which is subdivided into PERIODS

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MOST RECENT
GEOLOGIC TIME SCALE
BEGIN
END
OLDEST
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MASS EXTINCTION
  • When majorities of species were eliminated during
    a time period very quickly
  • Ex. Dinosaurs during the Cretaceous mass
    extinction
  • These mass extinctions can have various causes
    volcanoes, change in atmosphere, lands shifting,
    large comet or asteroid, weather changes
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