The Sixth Mass Extinction Will Be Like Nothing in Earth's History
The sixth mass extinction — the one that seven billion humans are sadly doing their utmost to trigger at this very moment — is shaping up to be like nothing our planet has ever seen. That’s the conclusion of a sweeping new analysis, which compared marine fossil records from Earth’s five previous mass extinction events to what’s happening in the oceans right now.
“There is no past event that looks biologically like what’s happening today,” lead study author Jonathan Payne, of Stanford University, told Gizmodo. Unlike the past, Payne said, “processes like warming and ocean acidification are not the dominant cause of threat in the modern ocean”.
Instead, the dominant threat is people. It’s the nets, harpoons, and trawlers that are systematically emptying the oceans of fish and other marine life forms. Whereas the mass extinctions of the past tended to target organisms in certain environments, the sixth mass extinction is poised to hit the biggest animals the hardest. And that could have have profound implications for how our planet’s future unfolds.
A palaeontologist by training, Payne and his research group started compiling data on modern marine organisms several years back, in order to study how body size and ecological traits have changed over evolutionary time. Payne, who has studied the End Permian extinction event, which wiped out more than 95 per cent of all marine species 250 million years ago, soon realised that his dataset — comprising living and extinct members of nearly 2500 marine genera — could serve another purpose.
“We thought the data we had would allow us to examine extinction in the modern in a way that would be very comparable to the fossil record,” Payne said. “Our hope was that we might be able to identify past events that biologically were most similar to the extinction threat the oceans are facing today.”
So that’s exactly what the researchers did. By comparing the extinction threat faced by modern marine genera (as indicated by their official conservation status) with their ancestral counterparts, Payne and his colleagues discovered that modern extinction threat is more strongly associated with body size. Larger animals face a greater risk of disappearing than smaller animals.
In past mass extinction events, body size didn’t matter that much. Instead, it was an organism’s habitat that dictated its fate. Animals that lived in the open ocean, or pelagic zone, went extinct at a higher rate than benthic creatures living on the seafloor.
This difference in “extinction selectivity” can be explained by different drivers. During the End Permian, changes in ocean chemistry triggered by microbes, volcanoes, or some combination of the two are thought to have created a toxic environment for most marine life. At the end of the Cretaceous period, an enormous asteroid impact followed by supervolcano eruptions sent plumes of dust into the sky, choking out sunlight and cutting off the energy supply at the bottom of the food chain. In both cases, organisms that lived in more isolated, sheltered environments away from the ocean’s surface fared better.
Today, the dominant driver of marine extinction is people, and people aren’t terribly selective about what environments they pluck animals from. We go for the biggest game, fishing down the food web and removing top predators. Within species, too, we tend to hunt the largest individuals, which is why North Atlantic cod and Chesapeake oysters were historically much larger. “In a sense, we’re driving evolution ,” Payne said.
There are a few big caveats to the analysis. For the sake of comparison, Payne and his co-authors only analysed marine genera that have fossil counterparts, which means certain soft-bodied organisms that don’t preserve well (like octopods) were excluded. What’s more, they only looked at organisms whose extinction risk has been assessed by the International Union for the Conservation of Nature (IUCN). That creates a rather serious bias toward big, charismatic groups: fish, sea turtles, marine mammals, and the like. There are countless species of marine invertebrates that we simply don’t have enough data on to do a proper threat assessment.
Perhaps most problematically, the study excluded corals, which are currently in the midst of a catastrophic, global die-off. As habitat for roughly a quarter of all marine species, the loss of coral reefs due to global warming and ocean acidification would undoubtedly be a major blow to the health of the oceans overall.
Even considering these omissions, the pattern the authors uncovered implies that the trajectory of the sixth mass extinction could be unique. The loss of large animals tends to cause what ecologists call a “tropic cascade”, which is essentially a ripple effect down the food chain. Larger organisms also play an outsized role in global nutrient cycling: whale faeces fertilises the oceans with iron, for instance, while salmon migrations bring nitrogen and phosphorus upstream and even onto the land.
It’s unclear whether the loss of these ecosystem services will make it harder for marine life to recover, but it’s certainly a possibility. The study minces no words to this point: “the preferential removal of the largest animals from the modern oceans, unprecedented in the history of animal life, may disrupt ecosystems for millions of years.”
There is, however, a bright spot: things haven’t got too terrible yet. In Payne’s dataset, there is only one genus that has actually gone extinct in the past 500 years. While more species have gone extinct, and some genera are too poorly studied to be sure, we’re at best on the precipice of a sixth mass extinction. We can still turn this sinking ship around.
“We have the opportunity to totally avert this, if we make the right decisions,” Payne said. “Even on the land, where we have lost a bunch of large species, almost everything at the genus level is still here.”
“To claim we’re in a sixth mass extinction is something very enormous,” he continued. “It is a possibility. It is not the reality yet.”