“What interested us was how long it took life to recover afterward,” said William Foster, a professor of geosciences at the University of Texas at Austin and the lead author of a new study about the Great Dying, published in the journal PLOS ONE on Wednesday. “Because not only was this the worst mass-extinction event, but recovery took millions of years.”

Foster wanted to know: Did the recovery of life on Earth take so long after the Great Dying because the extinction event itself was so cataclysmic? Or was something else going on?

To find out, he and his colleagues traveled to the Dolomites, a mountain range in northeastern Italy that’s known for its long geologic record of the Triassic, the period that came just after the Permian, which was capped by the Great Dying. The team examined marine invertebrate fossils, and from that work produced the most continuous dataset ever collected from the region.

The fossils they found showed that there were two additional extinction events in the recovery period after the Great Dying—not so major as to be deemed “mass extinctions,” but bad enough to slow the recuperation of life on Earth. Foster and his colleagues found that during that 10 million year recovery period marine invertebrates peaked then died off two times in association with carbon isotope shifts, which correlated with volcanic pulses from the Siberian Traps. In other words, just as life seemed to be bouncing back from the Great Dying, another extinction event derailed it—twice.

“This is not only interesting from an evolutionary point of view,” Foster says, “but also because those environmental conditions that life had to adapt to, to survive back then, are similar to those predicted for future climate warming scenarios.”

Similar, maybe, but not the identical. And thank goodness for that.

The volcanic eruptions that marked the start of the Great Dying were absolutely monstrous. The entire area of what is now China was covered in some 40 feet of lava. Those same volcanoes released a huge amount of gas, which set off the atmospheric deoxygenation that led to dramatic climate change. For context, it’s borderline ridiculous to compare the magnitude of this event to the 1883 eruption of Krakatoa, one of the deadliest and most violent volcanic eruptions in recorded history. “Krakatoa is very, very, very small compared to what happened at the Siberian Traps,” Foster said. Krakatoa killed some 36,000 people.

The magnitude of the volcanic eruptions 252 million years ago may be difficult to comprehend today, but what’s happening to the atmosphere is familiar.

“This is what makes it so interesting,” Foster told me, “Because you have this huge volcanic eruption that releases all these gases, and then you look at what’s happening today [with climate change] and they’re all the same gases. They’re causing the same effects. So we can say, ‘This is what it did in the past and this is what we might be looking at for the future.’”