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Massive underwater eruption may preview deep-sea mining destruction 

Massive underwater eruption may preview deep-sea mining destruction 


This article was originally published on ARS Techica - Science. You can read the original article HERE

Image of an undersea vent, with lots of white material on one side of the vent, and grey sediment surrounding it. No animals are visible.
Enlarge / Following the 2022 Hunga volcano eruption, a nearby hydrothermal vent was seen coated with a white mat of bacteria and surrounded by a thick layer of ash. The vent usually supports animal life that survives using chemical energy from the vent fluid, but those creatures were almost entirely wiped out.

In January 2022, a placid patch of the ocean’s surface near the islands of Tonga suddenly exploded with activity. After a month or so of activity, an underwater eruption of unprecedented scale from the Hunga volcano blasted ash up through the water column and more than 30 miles into the air, where it quickly spread out in a billowing plume spanning hundreds of miles.

The blast was so powerful that it rang Earth like a bell; it produced a shockwave that circled the globe multiple times and released a sonic boom heard as far away as Alaska. The eruption also triggered a tsunami that affected coastlines across the Pacific Ocean and made waves recorded in Japan, North and South America, and Antarctica.

Quite by surprise, scientists discovered that the eruption also had an underwater aftermath, recently described in a paper published in the journal Nature Communications Earth and Environment.

The Tahi Moana hydrothermal vent field, pictured here, was observed covered by up to six inches of ash in some places. Some snails and mussels in this region managed to survive the eruption and its aftermath.
The Tahi Moana hydrothermal vent field, pictured here, was observed covered by up to six inches of ash in some places. Some snails and mussels in this region managed to survive the eruption and its aftermath.

As part of a fortuitously timed expedition, a team of researchers set sail to the Lau Basin––a large underwater area surrounding Tonga where two tectonic plates meet––in April 2022. They aimed to study creatures around deep-sea hot springs. But when they arrived, they found the region strewn with the creatures’ remains instead.

“We didn’t expect to see much, if any, fallout from the eruption because it was a few months later, around a hundred miles away, and more than a mile deep,” said Shawn Arellano, an associate professor at Western Washington University who jointly led the expedition with Roxanne Beinart, an associate professor at The University of Rhode Island. “So we were really surprised by the level of the impact we saw.”

Looking through the eyes of an underwater robot, they saw a blanket of ash up to five feet thick covering the ocean floor––a never-before-seen phenomenon. Local populations of animals, including vulnerable mussels and snails on the Red List of endangered species, were wiped out, either buried alive or unable to acclimate to their dramatically altered conditions.

Before (top) and after (bottom) photos of the same area show how thickly ash was deposited following the eruption.
Enlarge / Before (top) and after (bottom) photos of the same area show how thickly ash was deposited following the eruption.

Similar catastrophic events appear in the fossil record, but scientists seldom have a chance to gather real time observations.

“There are very few modern examples of observations of ash deposition in the ocean,” Beinart said. “But there are many cases where scientists are looking at similar events in the fossil record and trying to piece together what happened.” The team’s observations offer a rare window into the process’s first stages.

Thousands to millions of years from now, perhaps scientists will study fossils of the creatures buried by the Hunga eruption.

Sink or swim?

Their original goal of studying the ecosystem largely dashed, the team quickly pivoted to investigate the eruption’s underwater aftermath. One of their more immediate findings counters long-standing ideas about how some creatures fare following similar events.

The fossil record suggests that crabs and other crustaceans are typically wiped out when their environment is suddenly inundated with ash. Scientists reason that the animals’ respiratory systems likely become clogged. However, Beinart and Arellano’s team noticed that crustaceans seemed to survive the Hunga eruption just fine and were scuttling across the ash that had entombed so many other animals. The team is still working out why crustaceans managed so well, contrary to expectations.

The team also collected more larvae of vent animals than expected. Arellano speculates that a new sampling system could have allowed them to gather more, or the event could have triggered the animals to spawn––something that’s known to occasionally happen following storms or other major disruptions.

“Or it could just be normal for this area,” Arellano said. “There haven’t been a lot of collections in this area before, so we don’t really have a baseline we can compare with.”

Adult Alviniconcha snails.
Enlarge / Adult Alviniconcha snails.
Dexter Davis (Western Washington University)

Among the samples the team collected, Arellano made the first documented observation of Alviniconcha snail larvae. Though these snails grow into animals that are dominant, foundational species at hydrothermal vents across the Western Pacific and Indian Oceans, no one had ever seen their larvae before. These creatures host chemosynthetic bacteria in their tissues that provide the bulk of their nutrition via chemicals in hydrothermal vent fluid.

Back on land, Beinart’s lab is now studying post-eruption changes in the genetic diversity in host animals and the bacteria that provide their energy. She had explored the region before and didn’t see a major shift in the animals’ genetic diversity. However, some strains of bacteria at the worst-hit sites are now missing, which could put animals that rely on them at risk.

“We did see some types of bacteria still present in the environment, but we don’t know whether they’re able to reproduce or they’re just in a dormant stage, waiting to attach to a host animal,” Beinart said. The bacteria must be able to survive on their own for at least some length of time because they aren’t found in the larvae of vent animals––only the full-grown ones. “The biological components for recovery are there, but we have no idea if they’ll actually be able to bounce back.”

Not much is known about the animal larvae the team found, but scientists think they probably settle on bare rocks like those the adults live on. Those hard surfaces are now covered in ash. It’s unclear whether that will spell the creatures’ collective doom.

Troubled waters

Beyond any lessons in ecology, the team’s observations may also preview the potential aftermath of deep-sea mining. Some mining methods kick plumes of sediment up into the water column, where it later settles on the surrounding seafloor.

Some Alviniconcha snails flank a hydrothermal vent chimney.
Enlarge / Some Alviniconcha snails flank a hydrothermal vent chimney.

“The mass-mortality of seafloor life following 2022 Hunga Volcano eruption, a result of the smothering by redistributed sediments and volcanic ash, provides a unique perspective of the damage that can be done to deep-sea communities following seafloor disturbance events,” said Sarah Seabrook, a marine biogeochemist at New Zealand’s National Institute of Water and Atmospheric Research, who was not involved in the study. “It provides a natural analogue for the potential impacts of activities such as deep-sea mining and bottom trawling, which are correlated to the removal and redistribution of sediment on the seafloor.” 

It’s not a 1:1 comparison––mining efforts probably won’t target active vents, and some of the locations that will likely be targeted are already naturally covered in sediment. But scientists currently have extremely little information about how deep-sea animals respond to disturbances in general, so the new observations help fill a major gap.

“A lot of the mining that’s being considered is in the Western Pacific, like the area we studied, which is a totally different geological setting than the Eastern Pacific, where a lot of the work about the recovery of vent ecosystems is happening,” Beinart said. The Eastern Pacific is a naturally more active area because tectonic plates there are spreading apart more quickly, which makes eruptions more common. Animals there have likely adapted to more frequent changes. It’s probably not valid to assume creatures in the Western Pacific will be able to similarly recover, “so this is a useful tool to understand how Western Pacific communities, which adapted under different conditions, can deal with dramatic change,” Beinart said.

Perhaps unsurprisingly, the expedition’s serendipitous observations opened up more questions than they answered.

“We saw some evidence of potential recovery––some animals, though smaller populations, and active reproduction along with lots of larvae,” Arellano said. “But what we don’t know is how things have gone from there.” Perhaps the animals can settle on the sediment after all. Or the sediment may have been cleared away from the area by deep-sea currents.

So far, no one has been back to make any follow-up observations. Beinart secured funding for a sequel expedition, but it likely won’t occur until 2026. “We’re potentially missing lots of major shifts or milestones while we wait to go back,” Beinart says. “Who knows what we’ll see when we finally return?”

Ashley writes about space for a contractor for NASA's Goddard Space Flight Center by day and freelances as an environmental writer. She holds master's degrees in space studies from The University of North Dakota and science writing from The Johns Hopkins University. She writes most of her articles with one of her toddlers on her lap. 

This article was originally published by ARS Techica - Science. We only curate news from sources that align with the core values of our intended conservative audience. If you like the news you read here we encourage you to utilize the original sources for even more great news and opinions you can trust!

Read Original Article HERE



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