Unit 10 Lesson 2 What Was Ancient Earth Like? Copyright Houghton Mifflin Harcourt Publishing Company

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3 How Rocks and Fossils Tell a Story Sedimentary rock forms in layers. Many sedimentary rocks contain fossils. The oldest rock layers are at the bottom, and the youngest rock layers are at the top. The relative age of a layer of rock is the age of that layer when compared to other layers.

4 How Rocks and Fossils Tell a Story Fossils form when sediment buries dead organisms. The fossil record is made up of all the fossils in Earth s rock layers. The fossil record contains information about Earth s history and the history of life on Earth.

5 C.W 10.2 : Q1

6 C.W 10.2 : Q2

7 How Rocks and Fossils Tell a Story Over time, the movement of Earth s crust can cause layers of rock to become tilted. It can also lift rocks formed in the ocean to above sea level. The rock layers of the Grand Canyon were tilted and lifted millions of years ago.

8 Divisions in Time Scientists developed the geologic time scale to divide Earth s history into manageable units. The fossils each unit contains define it.

9 Divisions in Time Large tree ferns were common during the late Paleozoic Era. The large coal deposits in the eastern United States formed from plants like these. Trilobites were so common that the earliest part of the Paleozoic Era is called the Age of Trilobites.

10 Divisions in Time Trees that produce seeds in cones appeared at the beginning of the Mesozoic Era. The middle and end of this era is known as the Age of Dinosaurs. Large animals, such as Stegosaurus, lived during this time.

11 Divisions in Time Flowering plants, such as grasses, and saber-toothed cats existed during the Ice Age.

12 Divisions in Time

13 Divisions in Time Index fossils help identify a very short period of Earth s history and must meet four requirements. 1.The organisms from which they formed lived during a short period of Earth s history. 2.The organisms must have had large populations so that many fossils formed. 3.The fossils must be widespread 4.The fossils must be easily recognized.

14 Big Changes on Earth Fossils tell how life on Earth has changed over time. Fossils also tell how Earth s continents and landforms have changed. Scientists have found fossils of a Mesosaurus a small, lizard-like reptile that lived in fresh water on both sides of the Atlantic Ocean.

15 Big Changes on Earth Mesosaurus was too small to have been able to swim across the Atlantic. At the end of the Paleozoic Era, all of Earth s masses were joined. These masses began to break apart during the Mesozoic Era. The single landmass (Pangea) explains how Mesosaurus could move across land.

16 Big Changes on Earth The landmasses breaking apart supports the idea of continental drift, and helps scientists understand the movement of Earth s plates.

17 Big Changes on Earth

18 Changing Environments Fossils provide clues about changing environments. Finding a fossil sea snail at the top of a mountain would lead to the conclusion that the environment has changed.

19 Changing Environments

20 Changing Environments Fossils of plants and animals at La Brea Tar Pits, in Los Angeles, California, show that the climate has not changed much in the last 40,000 years.

21 Changing Environments Falls of the Ohio is a state park in Indiana where summers are hot and winters are cold and snowy. Fossils of coral, clams, and other organisms that lived in shallow, warm, tropical seas show how the climate has changed in the last 380 million years.

22 The Great Die Offs Several times in history, many species became extinct at once. These large events, caused by climate change, are called mass extinctions. Worldwide volcanic eruptions blow large amounts of ash and dust into the air, blocking sunlight so plants can t grow. Other plants die as ash settles on them and smothers them.

23 The Great Die Offs At the end of the Mesozoic Era, an asteroid sent huge amounts of dust into the air, blocking sunlight and changing the climate. These changes may have led to the extinction of many organisms, including dinosaurs.

24 The Great Die Offs

25 The Great Die Offs

26 The Great Die Offs Effects: Drought _ Dust and ash in air _ Results: - Lack of sunlight causes plant to die and animals too.(2) -Plants and animals die -Habitats are destroyed and organisms too. Cause: - Meteor impact -Too much rain

Earth History. What is the Earth s time scale? Geological time Scale. Pre-Cambrian. FOUR Eras

Earth History. What is the Earth s time scale? Geological time Scale. Pre-Cambrian. FOUR Eras The Earth is 4.6 billion years old! Earth History Mrs. Burkey ESS Cy Creek HS 17-18 If the Earth formed at midnight 6:00 am First life appears 10:00 pm First animals/plants on land 11:59 pm First humans