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Triassic period

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from 230 million to 190 million years ago; dinosaurs, marine reptiles; volcanic activity

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Geologists call this time the Mesozoic period and subdivide it into the Cretaceous, Jurassic, and Triassic periods.
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It began some 250 million years ago... in the Triassic period... with land reptiles that moved into the sea.
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Monte San Giorgio became a UNESCO World Heritage Sites in 2003, because it "is the single best known record of marine life in the Middle Triassic period, and records important remains of life on land as well."
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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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Theropods first appeared during the Carnian age of the late Triassic period 231.4 million years ago (Ma) and included the sole large terrestrial carnivores from the Early Jurassic until at least the close of the Cretaceous, about 66 Ma.
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This lizard-like reptile was found in 1965 in the Madygen Formation, Dzailauchou, on the southwest edge of the Fergana valley in Kyrgyzstan, in what was then the Asian part of U.S.S.R. dating to the middle-late Triassic period (about 225 million years ago).
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In the Triassic period some groups of archosaurs (a group that includes crocodiles and dinosaurs) developed bipedalism; among them the dinosaurs, all the early forms and many later groups were habitual or exclusive bipeds; the birds are members of a clade of exclusively bipedal dinosaurs, the Theropods.
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The earliest exposed formations in the area date from the Triassic and early Jurassic periods, and have been named Zerqa and Kurnub formations.
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The era is subdivided into three major periods: the Triassic, Jurassic, and Cretaceous, which are further subdivided into a number of epochs and stages.
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The end of this period is marked by the Triassic-Jurassic extinction event .
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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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Other leading museums in Stuttgart include: The History Museum (Haus der Geschichte, 1987), examining local history, finds, the conflict between modern society and its cultural history State Museum of Natural History Stuttgart (SMNS) in Park Rosenstein housed in Castle Rosenstein (with an emphasis on biology and natural history) and Löwentor Museum (paleontology and geology, home of the Steinheim Skull and many unique fossils from the triassic, jurassic and tertiary periods) The Mercedes-Benz Museum (1936, moved in 2006), now the most visited museum in Stuttgart (440,000 visits per year).
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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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