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Mass Extinction Events

Explore the causes, effects, and characteristics of major mass extinction events throughout Earth's history.

Grade 11 Science Earth & Space ScienceMass Extinction
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Multiple ChoiceFill in the BlanksShort AnswerTrue / FalseTextMatching

Standards

HS-LS2-7HS-ESS2-7

Topics

mass extinctionpaleontologygeologybiologyearth science
8 sections · Free to use · Printable
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Mass Extinction Events

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Read each question carefully and answer to the best of your ability. For multiple-choice questions, select the best option. For short answer questions, provide concise and accurate responses.

1. Which of the following is NOT considered one of the 'Big Five' mass extinction events?

a

End-Ordovician Extinction

b

Late Devonian Extinction

c

Paleocene-Eocene Thermal Maximum

d

End-Permian Extinction

2. What is the most widely accepted theory for the cause of the Cretaceous-Paleogene (K-Pg) extinction event?

a

Massive volcanic eruptions

b

A large asteroid impact

c

Significant global warming

d

Rapid sea-level fall

1. The End-Permian extinction event is also known as The Great   due to the severity of species loss.

2. During a mass extinction, the rate of species extinction significantly   the rate of speciation.

3. The formation of large igneous provinces, such as the Siberian Traps, is linked to increased volcanic activity during the   extinction.

1. Briefly explain how climate change can contribute to a mass extinction event.

2. Describe one long-term ecological impact of a mass extinction event on the surviving species and ecosystems.

1. The current rate of extinction is significantly lower than the background extinction rate.

T

True

F

False

2. The Chicxulub impactor is believed to be the primary cause of the extinction of the non-avian dinosaurs.

T

True

F

False

The image below illustrates the timeline of Earth's past mass extinction events.

Timeline of Five Past Mass Extinction Events

Match each extinction event with its primary suspected cause.

1. End-Permian Extinction

 

a. Global cooling and glaciation

2. End-Ordovician Extinction

 

b. Massive volcanic activity (Siberian Traps)

3. K-Pg Extinction

 

c. Asteroid impact