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BIOLOGY CONCEPTS & CONNECTIONS Fourth Edition Neil A. Campbell • Jane B. Reece • Lawrence G. Mitchell • Martha R. Taylor CHAPTER 15 Tracing Evolutionary History Modules 15.1 – 15.5 From PowerPoint® Lectures for Biology: Concepts & Connections Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings Are Birds Really Dinosaurs with Feathers? • Did birds evolve from dinosaurs? • Evolutionary biologists investigate this question by looking at the fossil record Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings • The fossil of the earliest known bird, Archeaopteryx, was discovered in 1861 • Fossils of dinosaurs with feathers may support the birddinosaur theory Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings EARTH HISTORY AND MACROEVOLUTION 15.1 The fossil record chronicles macroevolution • Macroevolution consists of the major changes in the history of life – The fossil record chronicles these changes, which have helped to devise the geologic time scale Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings Figure 15.1 Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings 15.2 The actual ages of rocks and fossils mark geologic time • The sequence of fossils in rock strata indicates the relative ages of different species • Radiometric dating can gauge the actual ages of fossils Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings 15.3 Continental drift has played a major role in macroevolution • Continental drift is the slow, incessant movement of Earth’s crustal plates on the hot mantle Eurasian Plate North American Plate African Plate Pacific Plate Nazca Plate South American Plate Split developing Indo-Australian Plate Antarctic Plate Edge of one plate being pushed over edge of neighboring plate (zones of violent geologic events) Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings Figure 15.3A Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings India South America MESOZOIC Antarctica PALEOZOIC – Separation of continents caused the isolation and diversification of organisms Eurasia Africa Millions of years ago – Continental mergers triggered extinctions CENOZOIC • This movement has influenced the distribution of organisms and greatly affected the history of life Laurasia Figure 15.3B • Continental drift explains the distribution of lungfishes – Lungfishes evolved when Pangaea was intact Figure 15.3C Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings NORTH AMERICA ASIA EUROPE AFRICA SOUTH AMERICA AUSTRALIA = Living lungfishes = Fossilized lungfishes Figure 15.3D Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings 15.4 Connection: Tectonic trauma imperils local life • Plate tectonics, the movements of Earth’s crustal plates, are also associated with volcanoes and earthquakes – California’s San Andreas fault is a boundary between two crustal plates San Andreas fault San Francisco Santa Cruz Los Angeles Figure 15.4A Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings • By forming new islands, volcanoes can create opportunities for organisms – Example: Galápagos • But volcanic activity can also destroy life – Example: Krakatau Figure 15.4B, C Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings 15.5 Mass extinctions were followed by diversification of life-forms • At the end of the Cretaceous period, many lifeforms disappeared, including the dinosaurs – These mass extinctions may have been a result of an asteroid impact or volcanic activity Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings ? Cretaceous extinctions 90 million years ago 80 70 65 60 Figure 15.5 Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings • Every mass extinction reduced the diversity of life – But each was followed by a rebound in diversity – Mammals filled the void left by the dinosaurs Copyright © 2003 Pearson Education, Inc. publishing as Benjamin Cummings