Syllabus Edition

First teaching 2024

First exams 2026

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Mass Extinctions (HL) (DP IB Environmental Systems & Societies (ESS))

Revision Note

Alistair Marjot

Expertise

Biology & Environmental Systems and Societies

Mass Extinctions

What is a mass extinction?

  • Mass extinction is a widespread and rapid decrease in the diversity of life on Earth

    • It happens when a significant proportion of Earth's species die off in a relatively short period of time

    • At least 75% of species are wiped out in a mass extinction event

  • There have been five major mass extinctions in Earth's history

    • Each has significantly reshaped life on the planet

The five major mass extinctions

1. Ordovician-Silurian Extinction (approx. 444 million years ago)

  • This was the first mass extinction

  • It mainly affected marine life, as most species lived in the oceans at the time

    • Around 85% of marine species became extinct

    • Possible causes include:

      • Climate change (glaciation and global cooling)

      • Sea level drop, which reduced habitat space for marine species

2. Late Devonian Extinction (approx. 375 million years ago)

  • This event took place over millions of years and impacted marine ecosystems

    • 75% of all species died out, including many species of corals and fish

    • Possible causes include:

      • Volcanic activity, leading to climate change

      • Decreased oxygen levels in oceans (hypoxia)

3. Permian-Triassic Extinction (approx. 252 million years ago)

  • Known as the 'Great Dying', it was the most severe mass extinction.

    • 96% of marine species and around 70% of land species became extinct

    • Possible causes include:

      • Massive volcanic eruptions in what is now Siberia

      • The volcanic activity released huge amounts of carbon dioxide, causing global warming and ocean acidification

      • Some scientists suggest this event was made worse by methane gas being released from melting ice

4. Triassic-Jurassic Extinction (approx. 201 million years ago)

  • This extinction was followed by the dominance of dinosaurs

    • Around 80% of all species died out

    • Possible causes include:

      • Volcanic activity linked to the breakup of the supercontinent Pangaea

      • Resulting climate changes and sea-level rises

5. Cretaceous-Paleogene Extinction (approx. 66 million years ago)

  • This is the most famous mass extinction, known for the extinction of the dinosaurs

    • Around 75% of species became extinct, including all non-avian dinosaurs, pterosaurs, and ammonites

    • Possible causes include:

      • A large meteorite impact in what is now the Yucatán Peninsula in Mexico (Chicxulub crater)

      • This caused fires, tsunamis, and dust clouds that blocked out sunlight, disrupting the climate

      • Massive volcanic activity in India, causing short-term global cooling and acid rain, may have contributed

What causes mass extinctions?

Tectonic plate movements

  • Tectonic plates are large slabs of Earth's crust that move over time, reshaping continents and oceans

  • When plates move, they can cause habitat loss by altering land masses and changing ecosystems.

    • Formation of supercontinents like Pangaea combined previously separated land masses, reducing coastal areas and shallow seas, which are rich in biodiversity

    • This led to widespread species loss, particularly in marine environments

  • Plate movements can also trigger volcanic activity and earthquakes

    • These events can significantly impact life by destroying habitats and releasing gases into the atmosphere

Super-volcanic eruptions

  • Super-volcanoes release massive amounts of ash, lava, and gases (such as sulphur dioxide and carbon dioxide) into the atmosphere

  • This can block sunlight, leading to a temporary cooling of the Earth known as a 'volcanic winter'

    • The reduced sunlight can cause plants to die off, disrupting food chains and leading to the collapse of entire ecosystems

    • The Siberian Traps eruptions at the end of the Permian period released enough gases and ash to cause global temperatures to plummet and acidify the oceans

Climate changes

  • Mass extinctions can be caused by both global cooling (ice ages) and global warming (greenhouse effects)

  • Global cooling can reduce biodiversity by shrinking marine habitats and lowering temperatures beyond the tolerance of many species

    • The Ordovician-Silurian extinction was triggered by an ice age, which reduced shallow marine habitats

  • Global warming can lead to increased temperatures, habitat destruction, and ocean acidification

    • Warming can cause polar ice caps to melt, raising sea levels and altering ecosystems

Sea-level changes

  • Fluctuating sea levels can drastically reduce or expand habitats, particularly for marine species

  • Sea-level decline can expose shallow seas and coastal habitats, reducing the space available for organisms that rely on these environments

    • This is particularly destructive to coral reefs, mangroves, and other coastal ecosystems, which are biodiversity hotspots

  • Sea-level rise can flood terrestrial areas, displacing land species and altering ecosystems

Meteorite impact

  • Large meteorites or asteroids crashing into Earth can cause massive destruction on a global scale

  • Upon impact, meteorites create shockwaves and fires, but the more long-term damage comes from dust and debris thrown into the atmosphere

    • This debris can block sunlight for months or even years

    • This cools the planet and disrupts photosynthesis, leading to a breakdown of food chains

Rapid speciation after mass extinctions

  • Speciation is the process by which new species evolve

    • After a mass extinction, many ecological niches become available due to the extinction of species

    • Surviving species often undergo rapid evolution to fill these empty niches

    • This is the reason why periods of rapid speciation frequently follow mass extinctions

      • For example, after the Cretaceous-Paleogene extinction, mammals diversified and evolved into many new species, leading to the eventual rise of humans

The sixth mass extinction (anthropogenic extinction)

  • Anthropogenic means caused by humans

  • Scientists believe a sixth mass extinction has begun, driven by human activities including:

    • Habitat destruction, such as deforestation and urbanisation

    • Climate change caused by burning fossil fuels is altering habitats and weather patterns

    • Overfishing, hunting, and pollution (e.g. plastic pollution, pesticides) are further threats to biodiversity

Examiner Tip

Make sure you are able to explain how different factors (volcanic eruptions, sea-level changes, etc.) contribute to mass extinctions.

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Alistair Marjot

Author: Alistair Marjot

Expertise: Biology & Environmental Systems and Societies

Alistair graduated from Oxford University with a degree in Biological Sciences. He has taught GCSE/IGCSE Biology, as well as Biology and Environmental Systems & Societies for the International Baccalaureate Diploma Programme. While teaching in Oxford, Alistair completed his MA Education as Head of Department for Environmental Systems & Societies. Alistair has continued to pursue his interests in ecology and environmental science, recently gaining an MSc in Wildlife Biology & Conservation with Edinburgh Napier University.