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This comprehensive science passage introduces middle school students to the topic of mass extinctions, aligning with NGSS standards MS-ESS1-4 and MS-LS4-1. Students will learn what mass extinctions are, the mechanisms behind the 'Big Five' historic events, and the scientific evidence used to understand them, such as the iridium layer and fossil record gaps. The passage explains cause-and-effect relationships, including volcanic eruptions, asteroid impacts, and climate change, and discusses the long-term recovery of life on Earth. It also raises awareness about the current biodiversity crisis and human contributions to a possible sixth mass extinction. Activities include comprehension questions, writing prompts, and graphic organizers to reinforce learning. Audio integration ensures accessibility for diverse learners. This resource is ideal for building understanding of Earth's history, systems thinking, and scientific inquiry.
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The five major mass extinction events in Earth's history
Mass extinctions are periods in Earth's history when a significant portion of living species disappears in a geologically short time. These catastrophic events have dramatically altered the course of life on our planet. Scientists have identified five major mass extinctions, each causing the loss of at least 75% of all species within a few million years. Understanding these events helps us learn how ecosystems respond to rapid changes and what might threaten biodiversity today.
The Mechanisms Behind Mass Extinctions Mass extinctions occur due to powerful forces that disrupt Earth's ecosystems. For example, the Permian-Triassic extinction, the most severe, wiped out 90-96% of marine species and 70% of land species about 252 million years ago. Huge volcanic eruptions in the Siberian Traps released enormous amounts of gases, leading to climate change and changes in ocean chemistry. Another cause is asteroid impact. The Chicxulub crater in Mexico marks where an asteroid struck Earth 66 million years ago, triggering the Cretaceous-Paleogene extinction that ended the age of dinosaurs. Both volcanic activity and impacts can block sunlight, cool temperatures, and poison the environment, setting off a chain reaction that collapses food webs.
Evidence and Recovery After Extinction Scientists use several lines of evidence to study mass extinctions. One clue is a thin layer of iridium—a rare element from asteroids—found worldwide in rocks from the time of the dinosaur extinction. Another is the presence of shocked quartz, which forms under the intense pressure of an impact. The fossil record shows sudden gaps or changes in species diversity after these events. After a mass extinction, recovery takes millions of years. Surviving lineages slowly diversify, leading to the evolution of new species and reshaped ecosystems. For example, mammals became the dominant land animals after the dinosaurs disappeared.
The Ongoing Biodiversity Crisis Today, scientists warn that we may be living through a sixth mass extinction, driven by human activities. Habitat destruction, pollution, climate change, and overhunting are causing species to vanish at rates much faster than the normal background rate. This rapid loss of biodiversity threatens the stability of ecosystems and the services they provide, including clean air, water, and food. Understanding past mass extinctions may help us prevent future losses and protect Earth's living systems.
Interesting Fact: After the Permian-Triassic extinction, it took about 10 million years for Earth's biodiversity to recover to pre-extinction levels.
What is a mass extinction?
A period when many species disappear in a short timeA slow change in climate over millions of yearsA single species going extinctNew species forming quickly
How many major mass extinctions have occurred in Earth's history?
FiveTenTwoOne
What is one main cause of the Permian-Triassic extinction?