Browsing the "Triassic" Category

The Triassic period is a division of earth’s history spanning from around 252 to 201 million years ago, and during which global faunas were radically reorganised in the wake of the Permian mass extinction. The climate of the Triassic was typically arid and hot. During this period, the supercontinent of Pangaea began to gradually break apart, opening the Tethys Ocean. Recovery from the Permian mass extinction lasted up to 10 million years. In the oceans, surviving invertebrates including corals, cephalopods (such as ammonites) and echinoderms began to diversify. Marine reptiles became abundant and reached colossal sizes by the end of the Triassic. On land, archosaurs, a group of reptiles including crocodilians and dinosaurs, began to flourish. Mammal-like reptiles, on the other hand, became smaller and less diverse. The end Triassic is also characterised by a mass extinction event. Around 76% of all species, including the conodonts (a successful group of jawless fish), many archosaurs (with the notable exception of dinosaurs) and large amphibians were wiped out.

Cretaceous

Episode 174: A History of Dinosaurs in 50 Fossils

Published on April 15th, 2026 | by Sophie Pollard

Prof. Paul Barrett of the Natural History Museum, London, recently authored A History of Dinosaurs in 50 Fossils. We took this as an opportunity to get an overview of what we really know about dinosaurs and [&hellip... Read More


Mesozoic

Episode 173: Petrified Forest

Published on March 17th, 2026 | by Emily Keeble

Petrified Forest National Park in northeastern Arizona, USA is a hub for Triassic palaeontology and has exposures representing 20 million years of the Late Triassic Chinle Formation. Visitors marvel at the colourful fossilised trees from which [&hellip... Read More


Mesozoic

Episode 145: Scleromochlus

Published on October 5th, 2022 | by Liz Martin-Silverstone

Scleromochlus is an animal that has been known for over 100 years, and has been frequently suggested as being an ancestor to pterosaurs. It hails from the Late Triassic of Scotland, and there are fewer than [&hellip... Read More


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