Fossils: Evidence of Past Life — Reading Comprehension

Premium Resource

Grades

Standards

MS-ESS1-4
MS-LS4-1

About This Reader

This comprehensive informational passage introduces middle school students to the fascinating world of fossils, in alignment with NGSS standards MS-ESS1-4 and MS-LS4-1. Students will learn what fossils are, how they form through the process of fossilization, and the different types such as body fossils, trace fossils, molds, casts, and preserved remains. The passage delves into why fossilization is rare, the limitations of the fossil record, and how scientists use fossils to reconstruct ancient environments, understand evolution, and track continental changes. Real-world applications and cause-and-effect relationships are highlighted, encouraging scientific thinking about how evidence builds our knowledge of Earth's past. Integrated audio features support diverse learners, and engaging activities such as quizzes, writing prompts, and graphic organizers foster deeper understanding. The passage is also available in Spanish and a simplified version, making it accessible to all learners.

CONTENT PREVIEW

Fossils at the Geological Museum, Tsukuba 7 — Fossils at the Geological Museum, by Syced / Wikimedia Commons

Fossils are the preserved remains, traces, or imprints of ancient living things, providing direct evidence of life that existed millions of years ago. Scientists use fossils to answer important questions about how life and Earth have changed over time. Without fossils, much of Earth's biological history would remain a mystery. The study of fossils, known as paleontology, allows us to reconstruct past environments and understand the process of evolution.

How Fossils Form: The Mechanism of Fossilization

Fossilization is a rare process that requires specific conditions. When an organism dies, it must be buried quickly by sediment, such as mud or sand, to protect it from decay and scavengers. Over time, minerals in groundwater replace the organic material or fill the empty spaces within the remains. This process, called permineralization, results in a fossil. Only about 1% of all organisms that ever lived become fossils because fossilization requires rapid burial and the presence of hard parts like bones, teeth, or shells. Soft tissues usually decay before fossilization can occur, which is why they are rarely preserved.

Types of Fossils and Their Significance

There are several types of fossils, each offering unique information. Body fossils are preserved parts of organisms, such as bones, teeth, or shells. Trace fossils are indirect signs of life, including footprints, burrows, and coprolites (fossilized feces). Molds and casts are impressions left by organisms; a mold is a hollow imprint, while a cast forms when the mold is filled with minerals. Preserved remains are rare fossils where the whole organism is trapped in substances like amber, ice, or tar, keeping it almost unchanged. Each type helps scientists understand different aspects of ancient life, from anatomy to behavior.

The Fossil Record: Insights and Limitations

The fossil record is the collection of all known fossils and their placement in rock layers. Although the fossil record is incomplete due to the rarity of fossilization and geological changes, it still provides powerful evidence of evolution, extinction, and patterns of life on Earth. Fossils reveal how species have changed, adapted, or disappeared over millions of years. They show us what ancient environments were like, how climates shifted, and even how continents moved. For example, similar fossils found on different continents support the theory of continental drift.

Overall, fossils are crucial for understanding Earth's history. By studying them, scientists can trace the origins of life, environmental changes, and the processes driving evolution. New fossil discoveries continue to fill gaps in our knowledge and inspire new scientific questions.

Interesting Fact:
Less than one percent of all organisms that ever lived have been preserved as fossils, making each discovery valuable for understanding our planet's past.

What is a fossil?

A preserved remain or trace of ancient lifeA living animalA type of rock only found in mountainsA type of plant found in the rainforest

Which field of science studies fossils?

BotanyPaleontologyMeteorologyGeology

What is the first step in the fossilization process described in the passage?

The organism is buried quickly by sedimentMinerals replace the organic materialThe organism decays completelyThe fossil is placed in a museum

What is a trace fossil?

A fossil made of mineralsA fossil showing activity or behavior, like footprintsA preserved boneA rare type of plant fossil

In the passage, what does 'permineralization' mean?

When minerals fill in or replace the material of an organismWhen a plant grows in a mineral-rich soilWhen water washes fossils awayWhen only soft parts are preserved

Which of the following best describes why fossilization is rare?

Most organisms are eaten or decay before they can be buried and fossilizedAll animals become fossils after they dieOnly plants can be fossilizedFossilization happens every day

What can fossils tell scientists about Earth's history?

They reveal ancient environments, evolution, and continental movementThey show how to make rocksThey predict weather patternsThey describe modern animal behaviors

True or False: All organisms that ever lived have become fossils.

TrueFalse

True or False: Preserved remains are fossils where the whole organism is trapped in amber, ice, or tar.

TrueFalse

How does the fossil record help support the theory of continental drift?

Similar fossils are found on different continents, showing they were once connectedFossils are only found in oceansFossils can only be found in AntarcticaContinents have never moved