So what happened? This is a point of some debate among scientists who study the period, but we have a few compelling pieces of evidence that suggest the problem was not a natural disaster like an asteroid impact or supervolcano. Instead, the proliferation of new life forms, including trees on land and invasive fish in the oceans, may have caused the evolutionary equivalent of a baby bust.
I learned about this while researching my new book, Scatter, Adapt, and Remember: How Humans Will Survive A Mass Extinction. Before we survive, however, we need to understand what destroyed the world in previous eons.
The Devonian was a time when life on Earth was evolving very rapidly. Some paleontologists have called it the "age of fishes," because the seas were filled with huge, rapidly diversifying fish -- some fully plated in armor, and many with long, sharp teeth. Enormous reefs created their own ecosystems that wound in long, sinuous curves across the ocean floors. Most of these reefs were dominated by sponges, and they might have looked a lot smoother than today's coral reef systems. The seas were a big part of continental life too. Massive inland oceans covered large parts of the continents, such as the area we now call the Great Basin in the Americas.
But ocean life wasn't the only game in town. The Devonian was also the period when trees evolved. Plants that had been relatively small and ocean-dependent developed vascular systems, roots, and seeds. This allowed them to grow into giants that survived far from the coastal regions and oceans that had once been the main provenance of Earth's flora. As trees spread all across the continents, their root systems broke up the topsoil and created unprecedented amounts of nutrient runoff into the water -- in some ways similar to runoff from factory farms today. Trees began to change the environment, and then the climate.
There were moments during the Devonian when temperatures fluctuated dramatically, causing sea levels to rise and fall. Paleobotanists believe that the trees may have enriched the atmosphere with so much oxygen that temperatures dropped, causing an ice age that locked up seawater in ice. At that point, sea levels would have fallen and killed off many coastal species. But there were also cycles of hot, greenhouse conditions in which ocean levels rose even as the waters became acidic, killing off all of the reef systems and the lifeforms that depended on them.
New species would be less likely to evolve in habitats where conditions are changing too fast for creatures to adapt to them. Indeed, we are seeing extinctions on Earth for this reason right now: habitat change is causing amphibian dieoffs in the Americas, and ocean acidification is wrecking reef life.
Still, these kinds of climate changes are not enough to explain the dramatic dropoff in species diversity we see at the end of the Devonian period.