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Evolution and Change

Feb 11, 2016

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Marjan Goodarzi

Evolution and Change. Chapter Fourteen: Earth and Life History. 14.1 Evidence from Rocks 14.2 How Earth Changes 14.3 Natural Selection. Investigation 14B. Interpreting the Fossil Record. How do scientists analyze the fossil record?. 14.3 Life History. - PowerPoint PPT Presentation
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Page 1: Evolution and Change
Page 2: Evolution and Change

Evolution and Change

Page 3: Evolution and Change

Chapter Fourteen: Earth and LifeHistory

• 14.1 Evidence from Rocks

• 14.2 How Earth Changes

• 14.3 Natural Selection

Page 4: Evolution and Change

Investigation 14B

• How do scientists analyze the fossil record?

Interpreting the Fossil Record

Page 5: Evolution and Change

14.3 Life History• Scientists have

developed a model of the history of life on Earth called the geologic time scale.

• Paleontologists divide the geologic time scale into blocks of time called eras and periods.

Page 6: Evolution and Change
Page 7: Evolution and Change

14.3 Life History• The Precambrian era lasted from Earth’s

formation 4.6 billion years ago until 542 million years ago (mya).

• The first cells appeared in the Precambrian era.

Page 8: Evolution and Change

14.3 Life History• The Paleozoic era

lasted from 542 to 251 mya.

• Paleozoic is a Greek word meaning “ancient life.”

• Rocks dated from the Paleozoic era contain fossils of trilobites, snails, clams, and corals.

Page 9: Evolution and Change

14.3 Life History• The Mesozoic era lasted from 251 to 65

mya. (Mesozoic is a Greek word meaning “middle life.”)

• This era is often called the Age of Reptiles.

Page 10: Evolution and Change

14.3 Life History• The Cenozoic era began 65 mya and is still

going on. • Cenozoic means “recent life.” • Fossils from the Cenozoic era are closest to

Earth’s surface, making them easier to find.

Page 11: Evolution and Change

14.3 Mass extinctions• Mass extinctions are

periods of large-scale extinction.

• They seem to be part of the evolutionary process because after each, new life forms emerge.

Asteroids may have played a part in previous mass extinctions.

Page 12: Evolution and Change

14.3 Absolute dating• Absolute dating is a

method of estimating the age of a fossil in years.

• Absolute dating requires the use of a natural “clock.”

• That clock is the radioactive decay of certain naturally-occurring elements like carbon.

Page 13: Evolution and Change

14.3 Absolute dating• Half-life is the amount of

time it takes for half of the unstable atoms in a sample to decay.

• In a sample of uranium-238, it takes 4.5 billion years for half of the uranium atoms to transform into lead atoms.

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Paleontology Connection

• Something drastic happened about 65 million years ago—the fossil evidence is clear.

Mass Extinctions: Devastation and Opportunity

Page 16: Evolution and Change

Activity

• Scientists use absolute dating to estimate the age of a fossil in years.

• Absolute dating uses the decay of radioactive elements as a natural “clock.”

Radioactivity and Half-Life