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Thus Triassic stratigraphy is mostly based on organisms that lived in lagoons and hypersaline environments, such as Estheria crustaceans.
At the beginning of the Mesozoic Era, Africa was joined with Earth's other continents in Pangaea.
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The Triassic was named in 1834 by Friedrich von Alberti, after the three distinct rock layers (tri meaning "three") that are found throughout Germany and northwestern Europe—red beds, capped by marine limestone, followed by a series of terrestrial mud- and sandstones—called the "Trias".
The Triassic is usually separated into Early, Middle, and Late Triassic Epochs, and the corresponding rocks are referred to as Lower, Middle, or Upper Triassic.The vast supercontinent of Pangaea existed until the mid-Triassic, after which it began to gradually rift into two separate landmasses, Laurasia to the north and Gondwana to the south.The global climate during the Triassic was mostly hot and dry, with deserts spanning much of Pangaea's interior.The Triassic began in the wake of the Permian–Triassic extinction event, which left the earth's biosphere impoverished; it would take well into the middle of this period for life to recover its former diversity.Therapsids and archosaurs were the chief terrestrial vertebrates during this time.Later in the mid-Triassic a similar sea penetrated along the equator from the west.