The post discusses the end-Permian mass extinction and its implications for current and future biodiversity. It highlights that while many factors can trigger extinctions, once they begin, they follow a similar rapid course. Unlike the quick K-T extinction event, the end-Permian extinction unfolded over an extended period, primarily linked to long-term volcanic activity of the Siberian Traps, which increased stress on the biosphere. The conversation also includes reflections on current extinction rates, conservation efforts, and the resilience of life in the face of environmental collapse, emphasizing research into refugia and the potential for life to rebound post-extinction. The need for conservation is underlined as crucial for protecting remaining biodiversity and allowing ecosystems to adapt to changing conditions.