Bluemarblewest

History of earth

  • Earth is formed
    4540 BCE

    Earth is formed

    Dust that had been floating around in space begain to collect together. Because these particles have gravity the collection of dust grew and grew until it formed our earth.
  • First forms of life
    3800 BCE

    First forms of life

    RNA molecules are the first signs of life and are able to self replicate in nature.
  • 1st Multicellular Life
    3500 BCE

    1st Multicellular Life

    The fist example of multicellular organisms is cyanobacteria. Though this is the first example of a multicellular organism, multicellular organisms have evolved independent of each other at least 46 times.
  • Oxygen enters atmosphere
    2500 BCE

    Oxygen enters atmosphere

    Cyanobacteria started production oxygen and over millions of years the buildup of oxygen in the atmosphere made the earth more sustainable.
  • 1st Eukaryotes
    2100 BCE

    1st Eukaryotes

    The earliest know eukaryotes are acritarchs. These are also the most common fossils of the late Proterozoic.
  • End Ordovician Extinction
    439 BCE

    End Ordovician Extinction

    About 85% of all marine life went extinct. The two main causes of this are the cooling of the earth and lowering of the sea level.
  • Late Devonian Extinction
    367 BCE

    Late Devonian Extinction

    Around 75% of all life died. The lack of oxygen in the sea resulted in almost all marine life dieing and reefs did not recover until almost 100 million years later.
  • Pangaea forms
    270 BCE

    Pangaea forms

    Pangaea was a supercontinent that was surrounded by the ocean Panthalassa. This supercontinent spanned the early Permian period until the early Jurassic period.
  • End Permian Extinction
    245 BCE

    End Permian Extinction

    Almost all marine life died and 70% of terrestrial vertebrates died. It is the only mass extinction of insects know to have happened.
  • End Triassic Extinction
    208 BCE

    End Triassic Extinction

    This wiped out nearly half of all life. The possible reasons for this is either climate change or an impact.
  • Pangaea Begains to Break Apart
    200 BCE

    Pangaea Begains to Break Apart

    Because of the constant movement of tectonic plates the supercontinent Pangaea begain to break apart 200 million years ago.
  • End Cretaceous
    65 BCE

    End Cretaceous

    This extinction killed the dinosaurs. It is thought to be caused by a meteor impact which led to climate change.