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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...
21 paź 2019 · By examining plankton fossils, researchers have found the first ever evidence that ocean acidity is tied to the Cretaceous-Paleogene extinction event.
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.
1 wrz 2022 · The cause of the Cretaceous-Tertiary (K-T) extinction or Cretaceous-Paleogene (KPg) extinction, as it is interchangeably called, has been hotly debated within the scientific community. However, most experts agree that one particular event is an important, if not complete, cause.
11 maj 2016 · The end-Cretaceous mass extinction ranks among the most severe extinctions of all time; however, patterns of extinction and recovery remain incompletely understood. In particular, it is unclear how severe the extinction was, how rapid the recovery was and how sampling biases might affect our understanding of these processes.
6 lut 2009 · The long-term effects of mass extinctions on spatial and evolutionary dynamics have been poorly studied. Here we show that the evolutionary consequences of the end-Cretaceous [Cretaceous/Paleogene (K/Pg)] mass extinction persist in present-day biogeography.
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.