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Permian-Triassic Extinction Overview

Oct 18, 2024

The Great Dying: Permian-Triassic Extinction

Overview

  • Occurred about 252 million years ago.
  • Known as the greatest mass extinction event on Earth.
  • Affected 96% of marine species and 70% of terrestrial vertebrates.

Pre-Extinction Earth Conditions

  • Atmosphere: Oxygen levels at 23%, CO2 at 900 ppm.
  • Temperature: Average surface temperature was 16°C.
  • Sea Levels: 60 meters below present levels.
  • Climate Variance: Earth was transitioning out of an ice age.

Formation of Pangea

  • Led to vast desert formation on Earth due to rain clouds not reaching inland.
  • Two major deserts formed on Pangea.

Reptilian Dominance

  • Early Permian saw rise of reptiles like Dimetrodons.
  • Adaptation to the dry desert environment.

Extinction Event

  • Occurred over 150,000 years.
  • No single cause identified; multiple factors likely involved.

Possible Causes

Volcanic Activity: The Siberian Traps

  • Located in Siberia, Russia.
  • One of the largest known volcanic eruptions.
  • Eruptions lasted over 2 million years.

Effects of the Eruptions

  • Lava Coverage: Enough to cover an area the size of the mainland United States.
  • Ash and Gas Release: Led to global volcanic ash fallout.
  • Sulfur Dioxide: Mixed with water, causing acid rain.

Environmental Consequences

  • Deforestation: Volcanic ash and acid rain destroyed vegetation.
  • Carbon Dioxide Surge: Levels increased to 2000 ppm, leading to a 5°C rise in global temperatures.
  • Marine Life: Oceans warmed, became oxygen-deprived, destabilizing marine ecosystems.

Methane Release

  • Methane hydrate deposits melted, releasing methane, a potent greenhouse gas.
  • Resulted in an additional 6°C temperature rise.

Resulting Environmental Catastrophe

  • Overall temperature increased by 11°C.
  • 93% of Earth’s biodiversity went extinct.
  • Earth’s average temperature stabilized at 42°C.
  • Near-runaway greenhouse effect scenario.

Recovery and Aftermath

  • Siberian eruptions continued for 500,000 years.
  • Earth's recovery took millions of years:
    • 2 million years for temperature normalization.
    • 5 million years for vegetation return.
    • 10 million years for biodiversity recovery.
  • Dinosaurs rose as dominant species in the Triassic period.

Conclusion

  • The Great Dying was initiated by a chain of events starting with a massive volcanic eruption, leading to catastrophic environmental changes and mass extinction.