Researchers found clues in Italian limestone about a Jurassic-era marine extinction caused by volcanic CO2 emissions, paralleling today’s climate change concerns.
Limestone from the Mercato San Severino area in southern Italy provides evidence of historical oceanic oxygen depletion.
Researchers have uncovered a significant hint within Italian limestone that sheds light on a mass marine life extinction from millions of years ago. This finding could also offer insights into how current oceanic conditions might be affected by oxygen depletion and climate change.
“This event, and events like it, are the best analogs we have in Earth’s past for what is to come in the next decades and centuries,” said Michael A. Kipp, an earth and climate science assistant professor at Duke University. Kipp co-authored a study published June 24 in the Proceedings of the National Academy of Sciences that measures oxygen loss in oceans leading to the extinction of marine species 183 million years ago.
During the Jurassic Period, when marine reptiles like ichthyosaurs and plesiosaurs thrived, volcanic activity in modern South Africa released an estimated 20,500 gigatons of carbon dioxide (CO2) over 500,000 years. This heated the oceans, causing them to lose oxygen.
Italian limestone collected from the Mercato San Severino section in southern Italy contains molecular traces of ancient oceanic chemistry. An analysis of these rocks helps explain how early Jurrasic volcanism lead to de-oxygenation of the ocean and mass extinctions. Credit: Mariano Remírez, George Mason University
The result was the suffocation and mass extinction of marine species.
“It’s an analog, but not a perfect one, to predict what will happen to future oxygen loss in oceans from human-made carbon emissions, and the impact that loss will have on marine ecosystems and biodiversity,” said co-author Mariano Remirez, an assistant research professor at George Mason University.
Estimating Ancient Oxygen Levels
Studying limestone sediment that carries chemicals dating back to the time of the volcanic outburst, researchers were able to estimate the change in oxygen levels in ancient oceans. At one point, oxygen was completely depleted in up to 8% of the ancient global seafloor, an area roughly three times the size of the United States.
Since the Industrial Revolution began in the 18th and 19th centuries, human activity has released CO2 emissions equivalent to 12% of what was released during the Jurassic volcanism.
But Kipp said that today’s rapid rate of atmospheric CO2 release is unprecedented in history, making it hard to predict when another mass extinction might occur or how severe it might be.
“We just don’t have anything this severe,” Kipp said. “We go to the most rapid CO2-emitting events we can in history, and they’re still not rapid enough to be a perfect comparison to what we’re going through today. We’re perturbing the system faster than ever before.”
“We have at least quantified the marine oxygen loss during this event, which will help constrain our predictions of what will happen in the future,” Kipp said.
Reference: “Carbonate uranium isotopes record global expansion of marine anoxia during the Toarcian Oceanic Anoxic Event” by Mariano N. Remírez, Geoffrey J. Gilleaudeau, Tian Gan, Michael A. Kipp, François L. H. Tissot, Alan J. Kaufman and Mariano Parente, 24 June 2024, Proceedings of the National Academy of Sciences.
DOI: 10.1073/pnas.2406032121
The study was funded by the Duke University.
