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  2. Cretaceous–Paleogene extinction event - Wikipedia

    en.wikipedia.org/wiki/CretaceousPaleogene...

    The Cretaceous–Paleogene (K–Pg) extinction event, [a] also known as the K–T extinction, [b] was the mass extinction of three-quarters of the plant and animal species on Earth [2] [3] approximately 66 million years ago. The event caused the extinction of all non-avian dinosaurs.

  3. Timeline of Cretaceous–Paleogene extinction event research

    en.wikipedia.org/wiki/Timeline_of_Cretaceous...

    Because the estimated date of the object's impact and the Cretaceous–Paleogene boundary (K–Pg boundary) coincide, there is now a scientific consensus that this impact was the Cretaceous–Paleogene extinction event which caused the death of most of the planet's non-avian dinosaurs and many other species.

  4. Ankylosauridae - Wikipedia

    en.wikipedia.org/wiki/Ankylosauridae

    Ankylosauridae (/ ˌ æ ŋ k ɪ l oʊ ˈ s ɔː r ɪ d iː /) is a family of armored dinosaurs within Ankylosauria, and is the sister group to Nodosauridae.The oldest known ankylosaurids date to around 122 million years ago and went extinct 66 million years ago during the Cretaceous–Paleogene extinction event. [1]

  5. Template:Extinction events graphical timeline - Wikipedia

    en.wikipedia.org/wiki/Template:Extinction_events...

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Pages for logged out editors learn more

  6. Cretaceous Terrestrial Revolution - Wikipedia

    en.wikipedia.org/wiki/Cretaceous_Terrestrial...

    The Cretaceous Terrestrial Revolution (abbreviated KTR), also known as the Angiosperm Terrestrial Revolution (ATR) by authors who consider it to have lasted into the Palaeogene, [1] describes the intense floral diversification of flowering plants (angiosperms) and the coevolution of pollinating insects, as well as the subsequent faunal radiation of frugivorous, nectarivorous and insectivorous ...

  7. Maastrichtian - Wikipedia

    en.wikipedia.org/wiki/Maastrichtian

    The Cretaceous–Paleogene extinction event (formerly known as the Cretaceous–Tertiary extinction event) [a] occurred at the end of this age. [3] In this mass extinction , many commonly recognized groups such as non-avian dinosaurs , plesiosaurs and mosasaurs , as well as many other lesser-known groups, died out.

  8. Cretaceous - Wikipedia

    en.wikipedia.org/wiki/Cretaceous

    The Cretaceous (along with the Mesozoic) ended with the Cretaceous–Paleogene extinction event, a large mass extinction in which many groups, including non-avian dinosaurs, pterosaurs, and large marine reptiles, died out, widely thought to have been caused by the impact of a large asteroid that formed the Chicxulub crater in the Gulf of Mexico.

  9. Paleobiota of the Hell Creek Formation - Wikipedia

    en.wikipedia.org/wiki/Paleobiota_of_the_Hell...

    A Presbyornithid, it is notable for being one of the few birds known to have survived the Cretaceous–Paleogene extinction event. "Unnamed enantiornithine B" [90] Unnamed Montana [90] YPM 57823, a partial coracoid [90] An unnamed enantiornithean. [90] "Unnamed hesperornithiform A" [90] Unnamed Montana; UCMP 13355, a tarsometatarsus