We’re Just 140 Years Away From The Climate That Caused A Planet-Wide Extinction

We’re Just 140 Years Away From The Climate That Caused A Planet-Wide Extinction

Humans have pushed atmospheric carbon dioxide to heights unseen in our short (geologically speaking) existence. But give us another few generations, and our geologic impact on the planet will be clear.

New findings released on Wednesday show that at current emissions rates, we’re just five generations away from creating an atmosphere the likes of which hasn’t been seen in 56 million years. The last time carbon dioxide levels were as high as we’re headed for, it helped create one of the greatest die offs in recent Earth history.

The Paleocene–Eocene Thermal Maximum (PETM) is a period of planetary history as ominous as it sounds. Scientists have studied it for years, looking at carbon isotopes, fossils, and other clues buried in the Earth. Their findings show that carbon dioxide spiked rapidly, causing Earth to warm 5-8 degrees Celsius (9-14.4 degrees Fahrenheit). The tropical Atlantic was likely 36 degrees Celsius (96.8 degrees Fahrenheit), up to half of the microscopic foraminifera that inhabit the seas died, animals on land perished or shrunk, and it took 150,000 years for Earth to recover from the shock. It’s not exactly a dream climate and yet it seems to offer the closest analogue to what humans are doing to the climate today.

The new research, published in Geophysical Research Letters, shows just how close we are to reaching the extremes of the PETM and in some ways, how we’ve already surpassed it. Drawing on a suite of studies about when the PETM began and how fast carbon dioxide piled up in the atmosphere, Philip Gingerich, an emeritus professor at the University of Michigan’s earth science department, used models to project human carbon emissions into the future.

While the PETM pulse of carbon dioxide was rapid in geological terms, it pales in comparison to what humans are doing to the atmosphere. Modern rates of emissions are up to 10 times faster than they were during the PETM. But whereas PETM emissions were likely the result of a mix of volcanism, wildfires, and methane seeping out of permafrost and the seafloor, the current situation is almost entirely due to carbon emissions from human activity. And those emissions still climbing, with the world setting new high water for carbon pollution last year. Based on that bleak trend, Gingerich projected emissions into the future and found that in just 140 years, at current rates, we’ll have created the beginning of PETM atmosphere v2.0. At 259 years down the road, we’ll hit peak PETM.

This is a distinctly worst case scenario, which makes it seem unlikely we’ll get to that point. And yet we’ve been living that scenario out since carbon dioxide record keeping began in earnest in 1959, the start date Gingerich used to calculate future trends.

“[It’s] as if we are deliberately and efficiently manufacturing carbon for emission to the atmosphere at a rate that will soon have consequences comparable to major events long ago in earth history,” he told Earther.

As the study helpfully notes, Gingerich’s grandfather was born 140 years ago, while 259 years in past, Ben Franklin was inventing a clock with hours, minutes, and seconds hands. While the world has shown little appetite to wind down emissions, there’s been a lot of talk of how we should, you know, probably do it sooner than later. The new findings are a stark reminder of what’s waiting for our grandkids if it doesn’t.


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