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The History of Life on Earth

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CHAPTER 20 The History of Life on Earth Chapter 20: The History of Life on Earth The History of Life on Earth How Do We Know that Earth Is Ancient? – PowerPoint PPT presentation

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Title: The History of Life on Earth


1
CHAPTER 20 The History of Life on Earth
2
Chapter 20 The History of Life on Earth
  • The History of Life on Earth
  • How Do We Know that Earth Is Ancient?
  • How Has Earth Changed over Time?
  • The Fossil Record
  • Life in the Remote Past

3
Chapter 20 The History of Life on Earth
  • Rates of Evolutionary Change
  • Patterns of Evolutionary Change
  • The Future of Evolution

4
The History of Life on Earth
  • Changes that take effect during the lifetimes of
    species constitute microevolution.
  • Those that involve the appearance of new species
    and evolutionary lineages are called
    macroevolution.
  • 4

5
How Do We Know that Earth is Ancient?
  • The relative ages of rock layers in Earths crust
    can be determined from their positions relative
    to one another and from their embedded fossils.
  • 5

6
How Do We Know that Earth is Ancient?
  • Radioisotopes supplied the key for assigning
    absolute ages to rocks.
  • 6

7
How Do We Know that Earth is Ancient?
  • Earths geological history is divided into eras
    and periods.
  • The boundaries between these units are based on
    differences between their fossil biotas.
  • Review Table 20.1
  • 7

8
Table 20.1
table 20-01-2.jpg
  • Table 20.1

9
How Has Earth Changed over Time?
  • Unidirectional physical changes on Earth include
    gradual cooling and weakening of the forces that
    cause continental drift.
  • 9

10
How Has Earth Changed over Time?
  • Earths early atmosphere lacked free oxygen.
  • Oxygen accumulated after prokaryotes evolved the
    ability to use water as a source of hydrogen ions
    in photosynthesis.
  • Increasing atmospheric oxygen allowed evolution
    of eukaryotes and multicellular organisms.
  • Review Figure 20.2
  • 10

11
20.2
figure 20-02.jpg
  • Figure 20.2

12
How Has Earth Changed over Time?
  • Throughout Earths history the continents have
    shifted, sometimes separating, at other times
    colliding.
  • Review Figures 20.10, 20.11, 20.13, 20.15
  • 12

13
20.10
figure 20-10.jpg
  • Figure 20.10

14
20.11
figure 20-11.jpg
  • Figure 20.11

15
20.13
figure 20-13.jpg
  • Figure 20.13

16
20.15
figure 20-15.jpg
  • Figure 20.15

17
How Has Earth Changed over Time?
  • Rapid climate change, massive volcanism, and
    major shifts in sea levels and ocean currents
    have all had dramatic effects on the evolution of
    life on Earth.
  • Review Figures 20.3, 20.4
  • 17

18
20.3
figure 20-03.jpg
  • Figure 20.3

19
20.4
figure 20-04.jpg
  • Figure 20.4

20
How Has Earth Changed over Time?
  • External events, such as meteorite collisions,
    also have changed conditions on Earth.
  • A meteorite may have caused the abrupt mass
    extinction at the end of the Cretaceous period.
  • 20

21
The Fossil Record
  • Much of what we know about the history of life on
    Earth comes from the study of fossils.
  • 21

22
The Fossil Record
  • The fossil record, although incomplete, reveals
    broad patterns in the evolution of life.
  • About 300,000 fossil species have been described.
  • 22

23
The Fossil Record
  • Fossils show that many evolutionary changes are
    gradual, but an incomplete record can falsely
    suggest or conceal times of rapid change.
  • Review Figure 20.7, 20.8
  • 23

24
20.7
figure 20-07.jpg
  • Figure 20.7

25
20.8 Part 1
figure 20-08a.jpg
  • Figure 20.8 Part 1

26
20.8 Part 2
figure 20-08b.jpg
  • Figure 20.8 Part 2

27
20.8 Part 3
figure 20-08c.jpg
  • Figure 20.8 Part 3

28
Life in the Remote Past
  • The fossil record for Precambrian times is
    fragmentary, but fossils from Australia show that
    many lineages that evolved then may not have left
    living descendants.
  • 28

29
Life in the Remote Past
  • Diversity exploded during the Cambrian period.
  • Review Figure 20.10
  • 29

30
Life in the Remote Past
  • Geographic differentiation of biotas increased
    during the Mesozoic era.
  • 30

31
Life in the Remote Past
  • The modern biota evolved during the Cenozoic era.
  • 31

32
Rates of Evolutionary Change
  • Rates of evolutionary change have been very
    uneven.
  • 32

33
Rates of Evolutionary Change
  • Rapid rates of evolution occur when changes to
    the physical or biological environment create
    conditions that favor new traits.
  • Review Figure 20.16
  • 33

34
20.16
figure 20-16.jpg
  • Figure 20.16

35
Patterns of Evolutionary Change
  • Truly novel features of organisms have evolved
    infrequently.
  • Most evolutionary changes are the result of
    modifications of already existing structures.
  • 35

36
Patterns of Evolutionary Change
  • Three major faunas have dominated animal life on
    Earth.
  • Review Figure 20.17
  • 36

37
20.17
figure 20-17.jpg
  • Figure 20.17

38
Patterns of Evolutionary Change
  • Over evolutionary time, organisms have increased
    in size and complexity.
  • Predation rates have also increased, resulting in
    the evolution of better defenses among prey
    species.
  • Review Figure 20.18
  • 38

39
20.18
figure 20-18.jpg
  • Figure 20.18

40
The Future of Evolution
  • The agents of evolution continue to operate
    today, but human intervention, both deliberate
    and inadvertent, now plays an unprecedented role
    in the history of life.
  • 40
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