cretaceous$17599$ - translation to ελληνικό
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cretaceous$17599$ - translation to ελληνικό

LAST & 3RD PERIOD OF THE MESOZOIC ERA, 145-66 MILLION YEARS AGO
Cretaceous period; Cretaceous Period; Cretaceous System; Cretacious; Cretacous; Cretaceous Age; Middle Cretaceous; Creataceous; Cretaceous Africa; Cretacious Era; Cretacaeous; Early-Late Cretaceous; Cretaceous (geology); Early Late Cretaceous; Cretaceous system; Climate of the Cretaceous; Cretaceous era
  • ''[[Scipionyx]]'', a [[theropod]] dinosaur from the Early Cretaceous of Italy
  • Derasmosaurus pietraroiae]]'', a rhyncocephalian from the late Early Cretaceous of Italy
  • isotherm]]s
  • The impact of a [[meteorite]] or [[comet]] is today widely accepted as the main reason for the [[Cretaceous–Paleogene extinction event]].
  • Map of North America During the Late Cretaceous
  • Dutch Limburg]], by Dutch geologist [[Pieter Harting]] (1866)
  • ''[[Philydrosaurus]]'', a choristodere from the Early Cretaceous of China

cretaceous      
adj. γυψώδης

Ορισμός

cretaceous

Βικιπαίδεια

Cretaceous

The Cretaceous (IPA: krih-TAY-shəs) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin creta, "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation Kreide.

The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth by the end of the Cretaceous, coincident with the decline and extinction of previously widespread gymnosperm groups.

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. The end of the Cretaceous is defined by the abrupt Cretaceous–Paleogene boundary (K–Pg boundary), a geologic signature associated with the mass extinction that lies between the Mesozoic and Cenozoic Eras.