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  • Permian-Triassic Extinction Event: Dividing the Paleozoic and Mesozoic Eras
    The event that marks the division of the Paleozoic and Mesozoic eras is the Permian-Triassic extinction event, also known as the "Great Dying".

    This event, which occurred approximately 252 million years ago, was the most severe known extinction event in Earth's history, with an estimated 90% of marine species and 70% of terrestrial vertebrate species going extinct.

    The event is thought to have been caused by a combination of factors, including:

    * Volcanic eruptions: Massive volcanic eruptions in Siberia released vast amounts of greenhouse gases, causing global warming and ocean acidification.

    * Climate change: The rapid warming caused by volcanic eruptions led to widespread environmental changes, including ocean anoxia (lack of oxygen) and shifts in ocean currents.

    * Asteroid impact: Some scientists theorize that an asteroid impact may have contributed to the extinction event, but evidence for this is less clear.

    The Permian-Triassic extinction event drastically changed the biosphere, paving the way for the rise of dinosaurs and other Mesozoic life forms.

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