It’s explained in the exhibit’s section on the Great Dying. About 250 million years ago or so, an enormous volcanic field erupted in what is now Siberia. It spewed lava that burned though limestone and coal beds and filled the atmosphere with carbon dioxide and pollution, possibly for millions of years. That in turn warmed the planet, made the oceans acidic and robbed them of oxygen. More than 90% of species in the oceans died out as did two-thirds of those on land.
There have been other mass extinctions, like the one that wiped out the dinosaurs about 65 million years ago, but this one, at the end of the Permian Period, was mostly caused by too much carbon dioxide rising into the atmosphere. And the Smithsonian notes often in its exhibit that the current warming of the planet is déjà vu all over again.
“We can learn from studying the past,” Wing says. “They’re also the processes that are being observed by Earth scientists today.”
One of them is Curtis Deutsch at the University of Washington, whose research helped inform the Smithsonian curators. “The very same things that caused the Great Dying are happening right now in our ocean today as a result of human activities,” he says, “not to the same degree, but in the same direction.”
Currently, the planet has warmed to almost 2 degrees Fahrenheit on average above what it was before the Industrial Revolution, though at the current rate it could warm several degrees more. The Great Dying saw a warming increase of four or five times that.
But it happened gradually. So Deutsch thought, Why not re-create the hothouse of the Great Dying in a computer, a model that simulates the warming, and see how present-day species in the ocean would fare? He could crank up the carbon dioxide — that would in turn raise temperatures and lower oxygen in the oceans. Then he could watch as parts of the ocean started to become deadly.
“The first thing that happens is that you start to see a local loss of species as they begin to move in response to the climate heating up,” he says. But some parts of the planet were more forgiving. “We discovered something that was kind of surprising and new, I think,” Deutsch explains, “and that is that extinction was very strong everywhere, but it was even stronger near the cold parts of Earth, near the polar oceans, than it was in the warmer tropical oceans.”
It makes sense, he says. Animals that live near the equator can migrate toward the poles to find cooler water, but those that already live in cold, oxygen-rich waters nearer the poles have very little room to run.
Deutsch says the experiment is a window on the future — even the present: Marine species are already migrating. And to Deutsch, that migration looks familiar. “We see responses of marine species to those changes today that look like what we think happened at the end of the Permian,” he says.
The Smithsonian exhibit makes explicit references to the threat from human-caused climate change; it also received funding from industrialist David Koch, who is known for supporting groups that contest the scientific consensus on climate change. Wing, the curator, says making the connection between the Great Dying and what’s happening now is a message that needs to be heard. “We have exceeded the frame of our own history,” he says of the human race. “Because we are so powerful, we are basically a geologic force now as well as a human force.”
This article was condensed from an article in npr.org for Dr. David Jensen
