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  1. The extinction occurred at the end of the Cretaceous Period, about 65.5 million years ago. Who became extinct? In addition to the non-avian dinosaurs, vertebrates that were lost at the end of the Cretaceous include the flying pterosaurs, and the mosasaurs, plesiosaurs and ichthyosaurs of the oceans.

  2. Researchers report that the Cretaceous Chicxulub asteroid impact that resulted in the extinction of non-avian dinosaurs 66 million years ago, also rapidly acidified the oceans producing ecological collapse and long-lasting effects on the climate, and was a key reason for end-Cretaceous mass extinction.

  3. 1 wrz 2022 · The impact ejected magma, debris and vapors into the atmosphere, ignited wildfires and sent towering tsunamis across the globe. A period of intense cold and darkness followed an initial heatwave, as aerosols and particulates blocked out the sun. Sulfates from the atmosphere acidified the oceans.

  4. 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.

  5. The researchers say it is the first direct evidence that the Cretaceous-Paleogene extinction event 66 million years ago coincided with a sharp drop in the pH levels of the oceans — which indicates a rise in ocean acidity.

  6. 11 gru 2014 · The Deccan Traps flood basalts in India represent over a million cubic kilometers of erupted lava. These massive eruptions occurred around the same time as the end-Cretaceous mass extinction some 65 million years ago, which famously wiped out all nonavian dinosaurs.

  7. 19 lis 2016 · One of the most phenomenal events in the history of Phanerozoic life was the end-Cretaceous (K-Pg) mass extinction, occurring 66.04 Ma ago (Vandenberghe et al. 2012; Husson et al. 2014 for recent calibrations), an event that has been important for the subsequent evolutionary and ecological history of the continental and marine biota.

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