The Permian-Triassic mass extinction is the largest in Earth's history. In the United States, the record of this critical geobiologic interval was long thought to be absent at a major sedimentary hiatus.
Matthew R. Saltzman and Alexa R.C. Sedlacek present new evidence that a more continuous record of the Permian-Triassic boundary extinction event in shallow marine, Bahamas-like carbonate platform deposits of the Confusion Range in western Utah that represent the ancient western margin of Pangaea.