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- W43398785 abstract "The Cretaceous System/Period is the last major subdivision of Mesozoic time. Established by JJ d'Omalius d'Halloy in 1822, the Cretaceous and was divided into Upper and Lower series/epochs by WD Conybeare and William Phillips that same year. Cretaceous rocks are currently assigned to 12 stage/age-level subdivisions, the combination of which represent an interval estimated to lie between 145.0 and 66.0 Ma. This is the longest single system/period of the Phanerozoic and Cretaceous rocks are found on all continents. Palaeogeographically, the Cretaceous represents the time during which Pangaea continued to fragment and continental plates began to move into their current positions. Prominent tectonic features of Cretaceous time include the rifting of Laurasia to form the northern and southern embayments of the proto-Atlantic Ocean, the joining of these embayments into a single north–south-trending Atlantic Ocean Basin, and the rifting of the southern supercontinent of Gondwana into South America, Antarctica, India, and Australia." @default.
- W43398785 created "2016-06-24" @default.
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- W43398785 date "2014-01-01" @default.
- W43398785 modified "2023-09-25" @default.
- W43398785 title "Overview of the Cretaceous Period☆" @default.
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- W43398785 doi "https://doi.org/10.1016/b978-0-12-409548-9.09376-3" @default.
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