The Permian-Triassic extinction event, also known as the "Great Dying", was the most severe mass extinction in Earth's history, wiping out an estimated 96% of marine species and 70% of terrestrial vertebrate species. It occurred approximately 252 million years ago, marking the boundary between the Permian and Triassic periods.
There is still ongoing research and debate about the specific causes of the Permian-Triassic extinction event. However, several leading theories include:
The Permian-Triassic extinction event had profound and long-lasting effects on the Earth's biosphere. It led to the collapse of ecosystems, the loss of dominant species, and the reshaping of evolutionary pathways. In the aftermath of the extinction, new groups of organisms emerged and gradually repopulated the planet, setting the stage for the rise of the dinosaurs and other iconic Mesozoic life forms.
To effectively study the Permian-Triassic extinction event, consider the following key points:
By engaging with these study guide points, students can develop a comprehensive understanding of the Permian-Triassic extinction event and its significance in the broader context of Earth's natural history.