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Permian period

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from 280 million to 230 million years ago; reptiles

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The layers span around 27 million years of the Permian period; and it preserves fossils dating back to the Carboniferous period.
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Some 50 million years later, near the end of the Permian period, volcanic activity would burn the carbonaceous matter, releasing the carbon dioxide and acidic components, creating a sudden greenhouse gas effect that warmed the oceans and released methane from the ocean beds, all leading towards the Permian–Triassic extinction event, killing 90% of the species on Earth.
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The Permian spanned from 299 to 252 million years ago and was the last period of the Paleozoic Era.
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Marine extinction intensity during the Phanerozoic % Millions of years ago (H) K–Pg Tr–J P–Tr Cap Late D O–S The Permian–Triassic (P–Tr or P–T) extinction event, colloquially known as the Great Dying, the End-Permian Extinction or the Great Permian Extinction, occurred about 252 Ma (million years) ago, forming the boundary between the Permian and Triassic geologic periods, as well as between the Paleozoic and Mesozoic eras.
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Dinosaurs diverged from their archosaur ancestors approximately 230 million years ago during the Middle to Late Triassic period, roughly 20 million years after the Permian-Triassic extinction event wiped out an estimated 95% of all life on Earth.
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