The end-Triassic extinction along with the end-Permian and end-Cretaceous events are the most severe mass extinctions in the past 270 million years. The exact mechanisms of the end-Triassic extinction have long been debated, but most prominent: carbon dioxide surfaced by volcanic eruptions built up over many millennia, raising temperatures to unsustainable levels for many creatures, and acidifying ocean waters. But a new paper in the Proceedings of...
