Causes of Mass Extinctions
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Causes of Mass Extinctions

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@IllustriousHawkSEye

Questions and Answers

What is a common characteristic of species that are more vulnerable to extinction?

Ecological specialization

What is believed to have caused the Permian-Triassic Extinction?

Climate change and associated ocean acidification, along with massive volcanic eruptions

What percentage of marine species went extinct during the Permian-Triassic Extinction?

96%

What is believed to have caused the K-Pg Extinction?

<p>A massive asteroid impact, global wildfires, and massive volcanic eruptions</p> Signup and view all the answers

What is a potential effect of a large asteroid impact?

<p>Global cooling</p> Signup and view all the answers

What is a characteristic of massive volcanic eruptions that can contribute to mass extinctions?

<p>Release of massive amounts of toxic gases</p> Signup and view all the answers

Which of the following is an example of a massive volcanic eruption that contributed to a mass extinction?

<p>Siberian Traps</p> Signup and view all the answers

What is the name of the asteroid impact that is believed to have contributed to the K-Pg Extinction?

<p>Chicxulub asteroid impact</p> Signup and view all the answers

Study Notes

Causes of Extinction

  • Multiple factors contribute to mass extinctions, including:
    • Environmental stressors (e.g., climate change, sea-level changes)
    • Evolutionary factors (e.g., species competition, adaptation)
    • Random events (e.g., asteroid impacts, volcanic eruptions)
  • Species vulnerability plays a crucial role in mass extinctions, with species that are:
    • Ecologically specialized
    • Geographically restricted
    • Having low population sizes
    • Being evolutionary novelties being more prone to extinction

Permian-Triassic Extinction (PT Extinction)

  • Also known as the "Great Dying"
  • Occurred around 252 million years ago
  • Causes:
    • Massive volcanic eruptions in Siberia (Siberian Traps)
    • Climate change and associated ocean acidification
    • Possible asteroid impact
  • Effects:
    • 96% of marine species and 70% of terrestrial species went extinct
    • Most families of life were severely impacted or went extinct
    • Recovery took millions of years

K-Pg Extinction (Cretaceous-Paleogene Extinction)

  • Occurred around 65 million years ago
  • Causes:
    • Asteroid impact (Chicxulub asteroid impact)
    • Global wildfires
    • Massive volcanic eruptions (Deccan Traps)
  • Effects:
    • 75% of species, including non-avian dinosaurs, went extinct
    • Marks the end of the Cretaceous period and the beginning of the Paleogene period

Asteroid Impacts

  • Large asteroid impacts can cause massive destruction and global cooling, leading to mass extinctions
  • Examples:
    • Chicxulub asteroid impact (K-Pg Extinction)
    • Vredefort impact ( Possible contributor to the Permian-Triassic Extinction)
  • Effects:
    • Shock waves and tsunamis
    • Global firestorms
    • Long-term climate disruption

Massive Volcanic Eruptions

  • Large-scale volcanic eruptions can release massive amounts of toxic gases, causing global cooling and acid rain, which can lead to mass extinctions
  • Examples:
    • Siberian Traps (Permian-Triassic Extinction)
    • Deccan Traps (K-Pg Extinction)
  • Effects:
    • Global cooling
    • Acid rain
    • Reduced sunlight
    • Disruption of food chains

Causes of Extinction

  • Multiple factors contribute to mass extinctions, including environmental stressors, evolutionary factors, and random events.
  • Species vulnerability plays a crucial role in mass extinctions, especially for species that are ecologically specialized, geographically restricted, have low population sizes, or are evolutionary novelties.

Permian-Triassic Extinction (PT Extinction)

  • Occurred around 252 million years ago and is also known as the "Great Dying".
  • Massive volcanic eruptions in Siberia (Siberian Traps) and climate change with associated ocean acidification were the likely causes.
  • Possible asteroid impact also contributed to the extinction.
  • 96% of marine species and 70% of terrestrial species went extinct, with most families of life severely impacted or gone extinct.
  • Recovery took millions of years.

K-Pg Extinction (Cretaceous-Paleogene Extinction)

  • Occurred around 65 million years ago.
  • The Chicxulub asteroid impact, global wildfires, and massive volcanic eruptions (Deccan Traps) were the likely causes.
  • 75% of species, including non-avian dinosaurs, went extinct, marking the end of the Cretaceous period and the beginning of the Paleogene period.

Asteroid Impacts

  • Large asteroid impacts can cause massive destruction and global cooling, leading to mass extinctions.
  • Examples include the Chicxulub asteroid impact (K-Pg Extinction) and the Vredefort impact (possible contributor to the Permian-Triassic Extinction).
  • Effects include shock waves and tsunamis, global firestorms, and long-term climate disruption.

Massive Volcanic Eruptions

  • Large-scale volcanic eruptions can release massive amounts of toxic gases, causing global cooling and acid rain, which can lead to mass extinctions.
  • Examples include the Siberian Traps (Permian-Triassic Extinction) and the Deccan Traps (K-Pg Extinction).
  • Effects include global cooling, acid rain, reduced sunlight, and disruption of food chains.

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Description

Explore the multiple factors that contribute to mass extinctions, including environmental stressors, evolutionary factors, and random events. Learn how species vulnerability plays a crucial role in these events.

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