sixth mass extinction

There's a lot of talk these days about how greenhouse gases could spark a "mass extinction" on earth. Mass extinctions are episodes in the history of life on Earth during which unusually large numbers of species die off. They stand in contrast to the background rate of extinction, which occurs even when the diversity of life is increasing. Scientists recognize five major mass extinctions in the Earth’s history. The extinctions are measured in terms of large groups of related species, called families.

The five mass extinction episodes occurred because of major changes in the prevailing ecological conditions brought about by climate change, cataclysmic volcanic eruptions, or collisions with giant meteors. The sixth mass extinction appears to be in progress now, and the main cause is environmental change brought about by human activities.

  • 440M Years Ago - Late Ordovician Episode: 20-50% of Families Died Out - Tropical areas are hit hardest.
  • 360M Years Ago - Late Devonian Episode: 20-30% of Families Died Out - Many fish and marine invertebrates die out.
  • 250M Years Ago - End of Permian Episode: 50% of Families Died Out - Greatest mass extinction ever.
  • 213M Years Ago - Late Triassic Episode: 20-35% of Families Died Out - Dinosaurs and mammals had just recently evolved; both live through this extinction.
  • 66M Years Ago - Late Cretaceous Episode: 15% of Families Died Out - Dinosaurs become extinct, possibly caused by a metorite colliding with the Earth. Mammals and fishes begin to proliferate. 65 million years after this mass extinction, early humans evolve.