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  2. Triassic–Jurassic extinction event - Wikipedia

    en.wikipedia.org/wiki/Triassic–Jurassic...

    The cause of the Tr-J extinction event may have been extensive volcanic eruptions in the Central Atlantic Magmatic Province (CAMP), [8] which released large amounts of carbon dioxide into the Earth's atmosphere, [9] [10] causing profound global warming [11] along with ocean acidification. [12]

  3. List of periods and events in climate history - Wikipedia

    en.wikipedia.org/wiki/List_of_periods_and_events...

    Perhaps 30,000 years of volcanic activity form the Deccan Traps in India, or a large meteor impact. 66: Cretaceous–Paleogene boundary and Cretaceous–Paleogene extinction event, extinction of dinosaurs: 55.8: Paleocene–Eocene Thermal Maximum: 53.7: Eocene Thermal Maximum 2: 49: Azolla event may have ended a long warm period 5.3–2.6

  4. Tectonic–climatic interaction - Wikipedia

    en.wikipedia.org/wiki/Tectonic–climatic...

    The climate surrounding the volcano constrains the impact of the eruption. Models of eruptions that treat climatic variables as controls and hold eruption intensity constant predict particulate emissions, such as volcanic ash and other pyroclastic debris ejected into the atmosphere, in the tropics to reach higher altitudes than eruptions in ...

  5. Scientists thought a warming Earth led to the age of the ...

    www.aol.com/scientists-thought-warming-earth-led...

    The extinction has been tied to massive volcanic eruptions that split up Pangaea, the supercontinent made up of all of Earth’s continents. Those eruptions sent ash and volcanic debris into the ...

  6. Chicxulub crater - Wikipedia

    en.wikipedia.org/wiki/Chicxulub_crater

    It is now widely accepted that the devastation and climate disruption resulting from the impact was the primary cause of the Cretaceous–Paleogene extinction event, a mass extinction of 75% of plant and animal species on Earth, including all non-avian dinosaurs. [4]

  7. Climate across Cretaceous–Paleogene boundary - Wikipedia

    en.wikipedia.org/wiki/Climate_across_Cretaceous...

    The Earth's poles were cool and temperate; North America, Europe, Australia, and South America were warm and temperate; equatorial areas were warm; and the climate around the Equator was hot and arid. [citation needed] In the Paleocene, the Earth's climate was much warmer than today's by as much as 15 °C and atmospheric CO 2 was around 500 ...

  8. What is a mass extinction, and why do scientists think we’re ...

    www.aol.com/brief-history-end-world-every...

    When dinosaurs got big. Another period of extreme volcanic activity 201 million years ago marked the end-Triassic mass extinction. It has been linked to the breakup of the Pangea supercontinent ...

  9. Cretaceous–Paleogene extinction event - Wikipedia

    en.wikipedia.org/wiki/Cretaceous–Paleogene...

    Other causal or contributing factors to the extinction may have been the Deccan Traps and other volcanic eruptions, [17] [18] climate change, and sea level change. However, in January 2020, scientists reported that climate-modeling of the extinction event favored the asteroid impact and not volcanism. [19] [20] [21]