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  2. 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]

  3. 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 ...

  4. 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 non-avian 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

  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. Year Without a Summer - Wikipedia

    en.wikipedia.org/wiki/Year_Without_a_Summer

    This eruption was the largest in at least 1,300 years (after the hypothesized eruption causing the volcanic winter of 536); its effect on the climate may have been exacerbated by the 1814 eruption of Mayon in the Philippines. The significant amount of volcanic ash and gases released into the atmosphere blocked sunlight, leading to global cooling.

  7. Extinction event - Wikipedia

    en.wikipedia.org/wiki/Extinction_event

    The scientific consensus is that the main cause of the End-Permian extinction event was the large amount of carbon dioxide emitted by the volcanic eruptions that created the Siberian Traps, which elevated global temperatures. The formation of large igneous provinces by flood basalt events could have:

  8. After 66 million years, scientists discover there wasn’t just ...

    www.aol.com/66-million-years-scientists-discover...

    A six-mile-long asteroid, which struck Earth 66 million years ago, wiped out the dinosaurs and more than half of all life on Earth.The impact left a 124-mile-wide crater underneath the Gulf of ...

  9. 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]