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Chapter 25 Slides Sections 1-3

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• By about 2.7 billion years ago, O 2 began<br />

accumulating in the atmosphere and rusting<br />

iron-rich terrestrial rocks<br />

• This “oxygen revolution” from 2.7 to 2.3 billion<br />

years ago caused the extinction of many<br />

prokaryotic groups<br />

• Some groups survived and adapted using<br />

cellular respiration to harvest energy<br />

AP Biology<br />

© 2011 Pearson Education, Inc.

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