Italy’s pale and towering Dolomite Mountains are an offshoot of the more extensive Alps, and are famous for their snowy colored exterior, bounty of fossils, and rich history. These mountains used to ...

The Triassic is one of the most important periods in the evolution of life on Earth. After one of the greatest mass extinctions 252 million years ago, not only the dinosaurs but also many other ...

If this increase continues at the same rate, we will reach the level of emissions that caused the Permian-Triassic mass extinction in around 2,700 years—a much faster timescale than the Permian ...

Terrestrial ecosystems underwent extreme shifts in composition, following extensive degassing associated with the Siberian Traps near the Permian–Triassic boundary (PTB). These climatic perturbations ...

Ancient frog relatives survived the aftermath of the largest mass extinction of species by feeding on freshwater prey that evaded terrestrial predators, academics have found. Ancient frog ...

With just a few words, AI models can be prompted to create a story, an image, or even a short film. But according to Weber Wong, these models are all “made by non-creatives for other non ...

This is a well-written important paper on the recovery of fauna and flora following the end-Permian extinction event in several continental sites in northern China. The convincing conclusion, a rapid ...

Some of our staff support projects on the ground, while others provide technical and operational expertise from our regional offices, including our UK headquarters. In addition to our Fauna & Flora ...

For more than 120 years, Fauna & Flora has been working with its partners around the world to protect threatened plant and animal species. Every year, our people work across hundreds of project sites, ...

This significant new study is built around a remarkable fossil of a new genus and species of armoured marine reptile from the Early Triassic of China. More importantly, this paper also adds to our ...

It has long been recognized that terrestrial floras underwent major and long-lasting changes during the Permian and Triassic, some of which have been attributed to the end-Permian mass extinction.