Asphyxiation killed off a lot of marine species 252 million years ago
A massive series of volcanic eruptions in Earth’s distant past left ocean creatures gasping for breath. Greenhouse gases emitted by the volcanoes dramatically lowered oxygen levels in the oceans, a deadly scenario that may have been the main culprit in the Great Dying, researchers report.
Earth scientist Justin Penn of the University of Washington in Seattle and colleagues mapped out just how hot the oceans got at the time of the greatest mass extinction on Earth, about 252 million years ago, at the end of the Permian Period. From those climate simulations, the team investigated where the hot water led to ocean anoxia, dangerously low concentrations of dissolved oxygen.
Then, the team combined those data with the oxygen requirements of modern ocean dwellers. The scientists determined that hypoxia — a lack of sufficient oxygen for species’ metabolic needs — could have been the primary culprit behind the die-off. The research, published in the Dec. 7 Science, also predicts that the effects of hypoxia would have been worst at polar latitudes, and available fossil data support that result.
“Anoxia has been invoked as a primary kill mechanism for the marine extinctions for 20 years,” says Lee Kump, a geochemist at Penn State who wrote a commentary on the finding in the same issue of Science. But what’s unique about this study is the inclusion of how that anoxia affects organisms living in different ecological niches within the oceans, he says.
In the Great Dying, as many as 90 percent of all marine species and 70 percent of terrestrial vertebrate species died off. Massive volcanic eruptions, discharging in pulses that began about 300,000 years before the onset of the extinction event, were almost certainly the trigger for the Great Dying (SN: 9/19/15, p. 10).
But how, exactly, those eruptions led to the die-off isn’t clear. There are many ways that the volcanoes could have made Earth untenable. The volcanoes emitted large bursts of carbon dioxide and methane, powerful greenhouse gases that rapidly and dramatically increased temperatures on land and sea. The eruptions may also have punched holes in the ozone layer, allowing ultraviolet radiation to blast the planet and perhaps sterilize plants on land (SN Online: 2/12/18).
Oceans took the largest hit. Ocean temperatures increased at least 10 degrees Celsius at the tropics, and ocean acidification or hypoxia might have struck a killing blow for many creatures.
To identify a leading culprit, Penn and his colleagues decided to take a look at the animals themselves. Or rather, at modern stand-ins for long-extinct species. The team determined where in the ocean oxygen supply would have fallen below oxygen demand — for feeding, reproduction and defense — for various creatures.
The tropics suffered, the researchers found, but many species there have adaptations that enable them to survive warming waters and lower-oxygen conditions. The worst of the death toll from lack of oxygen would have happened at high latitudes, where creatures have no such adaptations, and have nowhere to go.
The team also scoured through a huge online database of fossils, the Paleobiology Database, to look for geographic patterns in extinction. To the researchers’ surprise, the fossils suggested that species suffered more at the poles than in the tropics too. Such a pattern hadn’t previously been reported, says biological oceanographer Curtis Deutsch, also of the University of Washington and a coauthor on the study. “No one had ever described a latitude difference,” he says. The similarities between the fossil record and model data were “uncanny,” he says.
The team also considered the role of ocean acidification. But acidification, it turns out, would have had the biggest impact at the tropics, not the poles. “It’s not proof, but a strong indication that the underlying mechanism was this oxygen loss,” Deutsch says.
Whether more creatures actually died at the poles at the end of the Permian isn’t wholly clear. Fossil records can be patchy, Deutsch acknowledges, and thus present an incomplete picture. But, he notes, the apparently higher risk of death at the high latitudes appeared in many different types of species, from vertebrates such as fish to shelled creatures such as mollusks.
One of the most surprising findings of the new study is that geographic pattern of extinction intensity, Kump says. He applauds the “novel and sophisticated” approach that the researchers took to examining hypoxia as the primary culprit, although he notes that volcanic gases probably made the oceans toxic to oxygen-breathers in other ways as well, including by adding hydrogen sulfide and carbon dioxide to the water.
Still, he says, the new research is “the most comprehensive analysis of a kill mechanism and its physiological impacts that’s been done so far. It’s really an advance forward.”
J.L. Penn et al. Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction. Science. Vol. 362, December 7, 2018, p. 1130. doi:10.1026/aat1327.
L. Kump. Climate change and marine mass extinction. Science. Vol. 362, December 7, 2018, p. 1113. doi:10.1126/science.aav7479.
C. Gramling. Ancient ozone holes may have sterilized forests 252 million years ago. Science News Online, February 12, 2018.
T. Sumner. Volcanic activity convicted in Permian extinction. Science News. Vol. 188, September 19, 2015, p. 10.
D. Powell. Calcium offers clues in mass extinction. Science News Online, June 14, 2012.
A. Witze. Gassy volcanoes tied to mass extinction. Science News. Vol. 179, January 15, 2011, p. 12.
N. Moreira. Last Gasp: Toxic gas could explain great extinction. Science News. Vol. 167, May 28, 2005, p. 339.