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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.
21 paź 2019 · 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.
1 mar 2022 · The Cretaceous-Paleogene (K-Pg) boundary mass extinction event, ~66 million years ago, is one of the most devastating climatic and faunal events in geological history and ended the age of the dinosaurs (Alvarez et al., 1980; Keller, 1988).
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.
30 maj 2018 · The Cretaceous/Palaeogene mass extinction eradicated 76% of species on Earth 1, 2. It was caused by the impact of an asteroid 3, 4 on the Yucatán carbonate platform in the southern Gulf of...
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.
Scientists had agreed that a massive meteorite made impact approximately 66.04 million years ago at the Cretaceous-Paleogene (known as K-Pg) boundary, as identified through a geological record in crust and rock.
