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The History of Life

The History of Life

Assessment

Presentation

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Science

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6th - 8th Grade

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Practice Problem

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Medium

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NGSS
MS-LS4-1, MS-ESS1-4, HS-PS1-8

+1

Standards-aligned

Created by

Barbara White

Used 12+ times

FREE Resource

13 Slides • 22 Questions

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The History of Life

Middle School
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Learning Objectives
  • Analyze the fossil record to find patterns of existence, diversity, extinction, and change.

  • Explain how rock layers and fossils help build the geologic time scale.

  • Use superposition for relative dating and absolute dating for a numerical age.

  • Recognize transitional fossils as evidence for the evolution and complexity of life.

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Key Vocabulary

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Fossil

Preserved remains or traces of ancient organisms, providing valuable evidence of past life on Earth.

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Fossil Record

The complete history of life on Earth as documented by the discovery and study of fossils.

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Rock Strata

Distinct layers of sedimentary rock that have been deposited over very long periods of time.

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Relative Dating

The method of determining the age of a fossil by comparing its placement with other fossils.

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Absolute Dating

A technique used to determine the specific age of a fossil, often using radioactive elements.

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Law of Superposition

This principle states that in undisturbed rock layers, the oldest rocks are always at the bottom.

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Key Vocabulary

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Radioactive Decay

The process where an unstable atom loses energy by emitting radiation to become stable.

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Half-Life

The time required for one-half of the atoms of a radioactive isotope to decay.

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Geologic Time Scale

A model that shows the major events in Earth’s history and the evolution of life.

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Extinction

The complete and permanent disappearance of a species from Earth, leaving no living members behind.

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Diversity

The wide variety of life forms that exist in an ecosystem or on the planet.

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Anatomical Complexity

The level of detail and organization in an organism's body structure, from simple to complex.

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What Are Fossils?

Body Fossils

  • These fossils are formed from the actual preserved parts of an ancient organism.

  • Hard parts like bones, teeth, and shells are the most common types of body fossils.

  • They are more likely to be preserved because they do not decay as easily.

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Trace Fossils

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  • These fossils preserve evidence of an organism’s activities rather than its actual remains.

  • Examples include footprints, burrows, nests, and impressions left in the mud or sand.

  • They show how an ancient organism lived and moved in its environment.

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Multiple Choice

What is the main difference between body fossils and trace fossils?

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Body fossils are the preserved parts of an organism, while trace fossils are evidence of its activities.

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Body fossils are only found in stone, while trace fossils are found in mud or sand.

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Body fossils show how an organism moved, while trace fossils show what it looked like.

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Body fossils come from animals, while trace fossils come from plants.

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Multiple Choice

Why are bones, teeth, and shells the most common types of body fossils?

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They are hard parts that are less likely to decay over time.

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They are much larger than an organism's soft parts.

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They are usually found in groups rather than by themselves.

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They provide more information than evidence of an organism's activities.

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Multiple Choice

If a scientist finds many sets of fossilized footprints from the same animal species all heading in the same direction, what is the most logical conclusion to draw?

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The organism likely lived in a group or herd.

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The organism had hard bones and teeth that were preserved.

3

The organism was a plant that left an impression in the mud.

4

The organism was quickly buried after it died.

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Relative Dating: The Principle of Superposition

  • Relative dating compares rock layer ages without giving a specific numerical date.

  • The principle of superposition says lower rock layers are older than upper layers.

  • Fossils found in deeper rock layers are older than those in upper layers.

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Multiple Choice

Which statement best describes the principle of superposition?

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Lower rock layers are older than upper layers.

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Upper rock layers are older than lower layers.

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All rock layers are the exact same age.

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Only rock layers with fossils have an age.

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Multiple Choice

What is the primary role of the principle of superposition in relative dating?

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It provides the exact numerical age of the rock layers.

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It allows for the comparison of rock layer ages without a specific date.

3

It identifies the specific types of fossils found in rock layers.

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It explains how the rock layers were originally formed.

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Multiple Choice

A scientist discovers a fossil in a deep rock layer and a different fossil in a layer much closer to the surface. Based on this discovery, what is the most logical conclusion?

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The fossil found near the surface is older.

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The fossil found in the deeper layer is older.

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Both fossils are from the same time period.

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The exact age of both fossils can be determined.

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Reading Rock Strata: Cross-Cutting

  • Scientists use rules like cross-cutting to find the relative age of rock strata.

  • Any feature that cuts across rock layers is younger than the layers it crosses.

  • For instance, a fault is younger than the rock strata it breaks through.

  • This helps uncover the history of geological events and life in the rocks.

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Multiple Choice

According to the principle of cross-cutting, what is true about a feature that cuts across several rock layers?

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The feature is younger than the rock layers.

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The feature is older than the rock layers.

3

The feature is the same age as the rock layers.

4

The feature's age cannot be compared to the layers.

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Multiple Choice

Why do scientists use principles like cross-cutting?

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To find the exact age of a rock in years.

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To determine the relative order of geological events.

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To identify the specific types of fossils in a layer.

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To measure the thickness of each rock stratum.

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Multiple Choice

A geologist observes a series of horizontal rock strata that are all broken and shifted by a fault line. Which of the following is the most logical conclusion?

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The fault is the youngest feature.

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The top rock layer is the youngest feature.

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The fault and the rock layers are all the same age.

4

The bottom rock layer is younger than the fault.

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Absolute Dating: A Radioactive Clock

  • Absolute dating provides a precise, numerical age for rocks and fossils.

  • It uses the decay of unstable radioactive isotopes into stable elements.

  • The decay rate is measured in a constant unit called a half-life.

  • Scientists use 235U for old rocks and 14C for recent organic remains.

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Multiple Choice

What is the main purpose of absolute dating?

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It provides a specific, numerical age for a rock or fossil.

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It compares the age of one rock layer to another.

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It identifies the types of minerals present in a rock.

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It determines where a fossil was originally located.

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Multiple Choice

What feature of radioactive decay makes it a reliable 'clock' for determining the age of rocks?

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The decay of unstable isotopes happens at a constant, predictable rate.

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All radioactive isotopes decay completely within a few years.

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The color of the rock changes as the isotopes decay.

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Only fossils, not rocks, contain radioactive isotopes.

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Multiple Choice

A scientist finds that exactly half of the original Uranium-235 in a rock sample has decayed. What is the most logical conclusion the scientist can draw?

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The rock has existed for one half-life of Uranium-235.

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The rock is too old to be dated using Uranium-235.

3

All of the original Uranium-235 is now gone.

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The rock must be younger than one half-life of Uranium-235.

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The Geologic Time Scale

  • The geologic time scale organizes Earth’s entire 4.6-billion-year history in a model.

  • ​It is created by analyzing rock strata and the worldwide fossil record.

  • Scientists use it to place major events like mass extinctions in order.

  • It is divided into eras like the Paleozoic, Mesozoic, and Cenozoic.

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Multiple Choice

What is the main purpose of the geologic time scale?

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To organize Earth’s 4.6-billion-year history in a model

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To predict when future volcanoes will erupt

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To find the location of precious metals in rock layers

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To show how the continents have moved over time

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Multiple Choice

How do scientists create the divisions, such as eras, within the geologic time scale?

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By analyzing rock strata and the fossils they contain

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By measuring the Earth's distance from the sun

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By studying the behavior of modern-day animals

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By reading historical records written by humans

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Multiple Choice

A paleontologist discovers a new fossil in a rock layer just above a layer containing fossils of a known, extinct dinosaur species. What can the paleontologist conclude about the new fossil?

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It belongs to plant species if the current era.

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It belongs to the extinct species of mammals.

3

The new fossil belongs to the paleozoic era.

4

The new fossil belongs to the whales.

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Patterns in the Fossil Record

  • The fossil record is the ordered collection of all fossils found.

  • It provides evidence for the history of life on our planet.

  • The record shows how life has changed and become more diverse over time.

  • It also shows when widespread extinctions of different species have occurred due to sudden decrease in fossil abundance.

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Multiple Choice

What is the primary purpose of the fossil record?

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To provide evidence for the history of life on our planet.

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To show how rocks and minerals are formed.

3

To predict the movement of Earth's continents.

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To map the locations of ancient rivers.

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Multiple Choice

What is a major trend that the fossil record shows about life over time?

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Life on Earth has changed and become more diverse.

2

Life on Earth has remained exactly the same.

3

All species that ever lived exist today.

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The oldest fossils are the most complex ones.

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Multiple Choice

Imagine scientists find a rock layer rich with many different fossils, but the layer directly above it has very few fossils. What is the best conclusion supported by this evidence?

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A widespread extinction event likely occurred.

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The animals all migrated to a new environment.

3

The conditions for fossilization improved.

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The older species quickly evolved into new ones.

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Transitional Fossils: Evidence of Change

  • The fossil record shows evidence of major evolutionary changes and increasing life complexity.

  • Transitional fossils show features of both ancestral groups and their modern descendants.

  • These special fossils provide a snapshot of evolution as it is happening.

  • For example, tetrapod fossils show a mix of fish traits and limb structures.

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Multiple Choice

What is the key characteristic of a transitional fossil?

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It is a fossil of an animal that is now extinct.

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It is always the oldest fossil found in a rock layer.

3

It shows features of both an ancestral group and a descendant group.

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It is a fossil that has been perfectly preserved in ice.

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Multiple Choice

What is the primary importance of transitional fossils to scientists?

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They only show animals that have gone extinct.

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They provide evidence for how life has changed over time.

3

They are much more common than other types of fossils.

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They only show the evolution of fish.

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Multiple Choice

A scientist finds a fossil that has both fish-like features and the first bone structure of a limb. What conclusion does this evidence support?

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It was a type of fish that could not swim well.

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It was likely an ancestor of modern four-limbed animals.

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It lived on land and in the water at the same time.

4

It was an animal that did not change for millions of years.

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Common Misconceptions

Misconception

Correction

Every dead organism becomes a fossil.

Fossilization is a very rare event that requires specific conditions.

Carbon-14 dating can be used to age any fossil.

Carbon-14 dating is only effective for recent organic remains.

Humans and dinosaurs lived at the same time.

Dinosaurs became extinct 66 million years before humans appeared.

A fossil's age is found by dating the fossil itself.

A fossil's age is found by dating the surrounding rock layers.

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Summary
  • The fossil record shows patterns of life, extinction, and change over time.

  • The geologic time scale is built by dating rock strata and fossils.

  • Relative dating orders events chronologically; absolute dating provides a numerical age.

  • Transitional fossils show evolution, and consistent scientific laws explain Earth’s history.

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Poll

On a scale of 1-4, how confident are you about interpreting the fossil record to understand Earth's history?

1 (Not confident at all)

2 (A little confident)

3 (Mostly confident)

4 (Very confident)

pattern-tertiary
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The History of Life

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