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    This house was built partly from recycled diapers

    Meet the house that diapers built.

    Researchers have designed and erected a house that has shredded, disposable diapers mixed into its concrete and mortar. A single-story home of about 36 square meters can pack nearly 2 cubic meters of used diapers into its floors, columns and walls, the team reports May 18 in Scientific Reports.

    Using recycled diapers as composite building materials would not only shrink landfill waste but also could make such homes more affordable, the team says, a particular need in developing countries like Indonesia where the demand for low-cost housing far outstrips the supply.

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    Indonesia’s urban population has increased by about 4 percent per year in the last three decades, and more of its people are moving to urban centers. Over two-thirds of Indonesians are expected to live in urban areas by 2025, says environmental engineer Siswanti Zuraida of the University of Kitakyushu in Japan. That population boom is putting a heavy strain on both housing demand and waste management, says Zuraida, who is originally from Indonesia. Used disposable diapers mostly pile up in landfills or get incinerated, adding to a growing waste problem.

    The materials used to build a house, meanwhile, particularly those needed to shore up its structural integrity, are often the biggest barrier to making homes affordable. So researchers have previously examined the possibility of using a wide variety of unconventional materials that could also save costs. These materials included many that would otherwise pile up as waste, such as the husks of rice grains or fly ash, the fine residue left over from the combustion of pulverized coal. Disposable diapers, as it happens, contain a lot of potentially useful building material, such as wood pulp, cotton, rayon and plastic.

    Zuraida and colleagues assessed how much of the sand, gravel and other traditional building materials used in mortar and concrete could be replaced by diapers — washed, dried, sterilized and shredded — without reducing the strength of the structures. They created six different samples of concrete and mortar by mixing different proportions of diaper material with cement, sand, gravel and water. Crushing the samples in a machine let the researchers test how much weight each could bear.

    The team then went on to design — and then build — a small, single-story, two-bedroom, one-bathroom home based on the maximum amount of diaper waste they calculated they could use. Recycled diapers could replace up to 27 percent of the traditional materials used in load-bearing structural components like columns and beams without losing significant strength, the team found. For buildings with more floors, that fraction is somewhat less: A three-story home could use up to 10 percent disposable diapers in its load-bearing structures, the team calculated. As for nonstructural components like wall partitions or garden paving blocks, shredded diapers could replace up to 40 percent of the sand.

    Despite the need for more affordable housing, there are significant hitches that stand in the way of adopting diapers or other low-impact nonconventional materials, Zuraida says.

    Diapers’ plastic components would have to be separated from the organic fibers, a complicated recycling process currently available only in developed nations. And Indonesia’s building regulations restrict construction materials to concrete, bricks, wood and ceramics — materials that also bear a high cost in terms of carbon emissions.

    “Thinking about how to use waste for other purposes is an excellent idea,” says chemist Christof Schröfl of Technische Universität Dresden in Germany. But there may be limits on the ultimate environmental friendliness of repurposing used diapers in buildings, he says, due to the existing challenges of separating and sanitizing diapers in waste. “It’s maybe worthwhile to start thinking about ways to replace single-use diapers” with something less frequently disposed of. More

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    Soil microbes that survived tough climates can help young trees do the same

    Microbial stress can be a boon for young trees.

    Saplings grown in soil microbes that have experienced drought, cold or heat are more likely to survive when faced with those same conditions, researchers report in the May 26 Science. And follow-up tests suggest that the microbes’ protective relationship with trees may linger beyond initial planting.   

    The team’s findings could aid massive tree planting efforts by giving new saplings the best chance of survival over the long run, says Ian Sanders, a plant and fungal ecologist at the University of Lausanne in Switzerland. “If you can control which microbes are put onto tree saplings in a nursery, you can probably help to determine whether they’re going to survive or not when they’re transplanted to the field.”

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    As climate change pushes global temperatures ever higher, many species must either adapt to new conditions or follow their ideal climate to new places (SN: 1/25/23). While forests’ ranges have changed as Earth’s climate has warmed and cooled over hundreds of millions of years, the pace of current climate change is too fast for trees to keep up (SN: 4/1/20).

    Trees live a long time, and they don’t move or evolve very quickly, says Richard Lankau, a forest ecologist at the University of Wisconsin–Madison. They do have close relationships with fast-adapting soil microbes, including fungi, which can help plants survive stressful conditions.

    But it was unclear whether microbes that had previously survived various climates and stresses might give inexperienced baby trees encountering a changing climate a leg up. With friends in the soil, “trees might have more tools in their toolkit than we give them credit for” to survive tough conditions, Lankau says.

    For the study, Lankau and fellow ecologists Cassandra Allsup and Isabelle George — both also at UW–Madison — collected soil from 12 spots in Wisconsin and Illinois that varied in temperature and amount of rain. The team then used the soils to plant an abundance of 12 native tree species, including white oak (Quercus alba) and silver maple (Acer saccharinum). Overall, “we had thousands of plants we were monitoring,” Allsup says.

    Those saplings grew in the soils in a greenhouse for two months before being transplanted in one of two field sites — one warm and one cold. To simulate drought, some trees in each spot were placed under transparent plastic sheets that blocked direct rainfall.

    One site in northern Wisconsin was at the northern edge of the trees’ range and represented how trees might take root in a new area that’s getting warm enough for them to grow. There, trees planted in soil containing cold-adapted microbes better survived Wisconsin’s frigid winter temperatures. Plants that faced drought in addition to the cold, on the other hand, didn’t have the same benefit.

    The other location, set up in central Illinois, was designed to represent a region where the climate is getting too hot or dry for the tree species to tolerate. Saplings grown in soil with microbes from arid spots were more likely to survive a lack of rain. But those grown in soils with heat-tolerant microbes were only slightly more likely to survive when they received normal rainfall. 

    Some fungi, including this jack-o’-lantern mushroom (Omphalotus illudens), have a close relationship with trees. That connection could help saplings expand their range amid changing climate.Cassandra Allsup

    Resident species already living in the area didn’t outcompete all of the transplanted microbes. Newly introduced fungi persisted in the soil for three years, a sign that any protective effects might last at least that long, the team found. 

    It’s still unclear which microbes best aid the trees. Analyses of microbes living in the soil hinted that fungi that live inside plant roots may better help trees survive drought. Cold-adapted soils seem to have fewer fungal species. But soils also contain bacteria, archaea and protists, Sanders says. “We don’t know what it is yet that seems to affect the plant survival in these changing climates.”

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    Determining which microbes are the important ones and whether there are specific conditions that best suit the soil is next up on the list, Allsup says. For example, can dry-adapted soil from Iowa help when planting trees in Illinois? “We need to think more about soils and combinations and [transplant] success… to actually save the forest.”

    One caution, Sanders says, is that transporting microbes from one place to another en masse could bring the bad along with the good. Some microbes might be pathogens in the new place where they’re transplanted. “That’s also a big danger.”  More

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    There’s good and bad news with California’s electric vehicle program

    A worldwide gearshift from fossil fuel–powered cars to electric vehicles could significantly reduce the amount of carbon dioxide that humans emit to the atmosphere. But current strategies for vehicle electrification can also shift some pollution to communities already suffering under higher economic, health and environmental burdens, researchers warn.

    California, which leads the United States by a mile when it comes to EV adoption, offers a window into this evolving problem. The state is aggressively seeking to reduce its carbon footprint and has made substantial increases in wind and solar power generation as well as in the promotion of electric vehicle purchases. One tool the state has used is the California Clean Vehicle Rebate Project, or CVRP, which kicked off in 2010 and offers consumers money back for the purchase or lease of new EVs.

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    Now, an analysis of the CVRP’s impact on the state’s air quality from 2010 to 2021 reveals both good and bad news, researchers report May 3 in PLOS Climate.

    To assess the impact of the CVRP on a community and statewide level, the team developed a computer model that incorporates data on where the rebates went, how much additional electricity would be required to power those vehicles, which of the state’s electric generating units would provide that power and how much pollution they might produce.

    The team then overlapped these data with a mapping tool called CalEnviroScreen that identifies which of the state’s more than 8,000 census tracts — county subdivisions used in population assessments — are the most vulnerable to pollution. That vulnerability measure is based not only on exposure to pollutants such as power plant emissions and unsafe water but also on factors such as income, education level, access to health care and linguistic isolation.

    The good news is that the CVRP is responsible for making a dent in the state’s overall CO2 emissions, reducing them by about 280,000 metric tons per year on average, says environmental scientist Jaye Mejía-Duwan of the University of California, Berkeley. In 2020, transportation in California produced about 160 million tons of CO2, about 40 percent of the total 370 million tons of CO2 emitted by the state that year.

    The program has also reduced the state’s overall emissions of other types of air-polluting gases, including sulfur dioxide and several nitrogen oxide gases collectively called NOx.

    The bad news is that the most disadvantaged communities in the state didn’t see the same overall improvement in air quality, Mejía-Duwan and colleagues found. Those communities didn’t have the same decreases in sulfur dioxide and NOx gases — and in fact saw an increase in one type of air pollution, tiny particulates known as PM2.5 (SN: 7/30/20). “These particles are small enough to penetrate deep into the lungs and cross over into the bloodstream,” increasing the risk of cancer, cardiovascular problems and cognitive decline, Mejía-Duwan says.  

    Where the power is

    California uses a computer model called CalEnviroScreen, currently in its fourth version, to determine levels of vulnerability to the impacts of pollution. The most disadvantaged communities (darker blue) are determined by both pollutant exposure and socioeconomic factors. The state’s electricity-generating units (EGUs, circles) are disproportionately located in the most disadvantaged communities. That reveals how increasing electrification, which includes power generated by nonrenewable sources, could increase pollution in many of the most disadvantaged communities.

    Pollution impact by community

    J. Mejía-Duwan, M. Hino and K. J. Mach/PLOS Climate 2023

    J. Mejía-Duwan, M. Hino and K. J. Mach/PLOS Climate 2023

    That increase may be indirectly related to putting more EVs on the road. Although electric vehicles themselves don’t produce PM2.5 from their tailpipes, increased electricity generation, if it’s not fossil fuel–free, can. Renewable resources, including rooftop solar cells, supplied about half of California’s electricity in 2022. But natural gas–fired power plants still provide a hefty chunk of the state’s power.

    “Electric vehicles are often incorrectly referred to as ‘zero-emission vehicles,’ but they’re only as clean as the underlying electric grid from which the energy is sourced,” Mejía-Duwan says. The most disadvantaged 25 percent of the state’s communities also contain 50 percent of the power plants, the team found.

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    EVs also tend to be relatively heavy due to their hefty batteries. And “heavier vehicles can produce as much if not more particulate matter” than equivalently sized fossil fuel-powered cars, due to brake, tire or road wear, Mejía-Duwan says.

    Increasing the cleanliness of the electric grid would help, as would changes to the management of the state’s generated power, the researchers say. California’s solar, wind and hydroelectric energy production has grown rapidly. But the battery technology to store and use that energy later lags behind. Most of that energy is generated during the day, so some researchers have suggested plugging in electric vehicles while it’s light out to take advantage of the daytime glut of electricity — and then using the vehicles to help power houses at nighttime (SN: 12/22/21).

    But, clever as that idea is, it doesn’t address the underlying factors behind these inequities. Since 2010, the CVRP has provided over 400,000 rebates for EVs of up to $7,500, depending on income. Yet, as it turns out, those rebates have disproportionately gone to the least disadvantaged communities. “That’s a major driver of these inequities,” Mejía-Duwan says.

    Changing that isn’t an easy fix. The state has tried several ways to address the issue, such as by imposing an income cap on eligibility.

    But those efforts have had little effect, particularly given strong barriers that stand in the way of the adoption of EVs by people in disadvantaged communities. One roadblock is that prospective EV buyers must have enough money for a down payment, and then fill out forms and be able to wait several months for the rebate money. Another is that car manufacturers are trending toward producing larger, more expensive EVs. Chevrolet, for example, announced in April that its most affordable EV, the Bolt, will be discontinued as the company pivots to producing electric SUVs.

    There’s also a lack of equitable access to vehicle charging infrastructure. And then there are subtler but no less insidious issues, such as “a lack of sufficient multicultural and multilingual outreach about EVs, plus the fact that people of color and minoritized communities report facing discrimination at dealerships,” Mejía-Duwan says.

    These findings echo and support researchers’ longtime concerns about how current programs to encourage vehicle electrification will disproportionately impact people. “It’s not a surprise,” says Román Partida-López, senior legal counsel for transportation equity at The Greenlining Institute, a nonprofit organization based in Oakland, Calif. “What [California] is doing is a move in the right direction, but it’s not enough.”

    California and other states pursuing aggressive zero-emissions policies need to shift their thinking, Partida-López says, to be more intentional about targeting their efforts toward the communities experiencing the greatest impacts (SN: 12/14/22). Rebates, in particular, are known to be an inequitable approach, he says, because they “assume you have the money up front to be able to put down a down payment of several thousand dollars.”

    A better strategy to reduce the barriers to EV adoption, he says, would be to provide other types of incentives, such as vouchers that low-income households could use at the time of purchase as well as accessible financing programs.

    After all, making EVs accessible to everyone is going to be essential to the big picture of transitioning to zero emissions (SN: 1/27/23). “We’re not going to meet any of those goals unless we center equity” in program designs, Partida-López says. “The focus has always been, ‘How do we transform the market?’ We need to change the narrative to ‘How are we going to focus on the people most impacted, to help with this transition?’”

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    In one lake deep under Antarctica’s ice, microbes feast on ancient carbon

    How microbes survive in lakes far beneath Antarctica’s ice sheet has been a mystery. Now scientists have figured out what’s on the menu for microbes in one buried lake in West Antarctica.

    The lake’s bacteria and other microbial inhabitants get by on carbon that seawater left behind thousands of years ago, researchers report in the April AGU Advances. The find adds to existing evidence that, during a period of warming about 6,000 years ago, the ice sheet in West Antarctica was smaller than it is today. That allowed seawater to deposit nutrients in what is now a lake bed buried under hundreds of meters of ice.

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    This study is among the first to provide evidence from beneath the ice that the ice sheet was smaller in the not-so-distant past, geologically speaking, before growing back to its modern size, says Greg Balco, a geochemist at the Berkeley Geochronology Center in California.

    Understanding how the ice sheet changed during past periods of warming is crucial to predicting Antarctica’s future as the world continues to warm due to human-caused climate change, says Balco, who was not involved in the new study.

    Hundreds of lakes pool under Antarctica’s massive ice sheet, the result of the underside of the ice ever-so-slowly melting due to heat from the Earth’s interior. The lakes tend to be pitch-black, near freezing and are almost all isolated from the outside world.

    These less-than-ideal conditions should make them hostile to life. “If I were a microbe, I wouldn’t want to live in the cold, dark depths where I haven’t seen the sun or a new nutrient in thousands of years,” says Ryan Venturelli, a paleoglaciologist at the Colorado School of Mines in Golden. Yet billions of microbes — and even some animals — have found a way to thrive in these subglacial waterbodies (SN: 4/21/23).

    As the last glacial period came to a close, starting around 15,000 years ago, ice sheets around the world retreated. Computer simulations have predicted that as the climate warmed, the ice sheet in West Antarctica may have shrunk to an even smaller size than it is today. But working out what a smaller ice sheet might have looked like isn’t easy since most of the evidence for it is now locked under ice, Balco says.

    In 2018, Venturelli joined a team of about 30 scientists headed to a remote corner of West Antarctica to drill for the past. The journey took them to Lake Mercer: a body of subglacial water that today sits 150 kilometers from the sea.

    It took the expedition over a week of using a hot-water drill 24 hours a day to pierce through just over a kilometer of ice to reach the lake. “There was a lot of cheering and high-fiving” when the drill finally made it through, Venturelli recalls. Lake Mercer is only the second subglacial lake in the world that scientists have ever managed to reach.

    Paleoglaciologist Ryan Venturelli holds a tube of sediment collected from the bed of Lake Mercer. Carbon in this sediment core reveals that the lake was connected to the ocean 6,000 years ago.Billy Collins

    The team collected and analyzed lake water and sediment samples from the lake bed. This work revealed traces of 6,000-year-old carbon-14, a form of the element that’s made in the atmosphere and then falls to Earth. For that carbon to get past the ice, the lake would have had to have contact with the outside world. 

    The researchers didn’t spot any telltale signs of ancient photosynthesizing plankton, suggesting that the area wasn’t open ocean when the carbon settled in the sediment. Instead, seawater carrying the carbon must have come to the lake. That means that ocean water had to have flowed under the ice about 250 kilometers farther inland than it does today, the researchers say. 

    “There’s no other way to get carbon-14 in there,” Balco says. “You can’t push it through ice. Organisms can’t tunnel through. The only way for it to get it there is for ocean water to get under the ice sheet.”

    Seawater does flow under the ice today — but not as far inland as the lake’s location. So the edge of the ice shelf was probably closer to Lake Mercer several thousand years ago. That suggests, the team says, that the ice sheet over West Antarctica was probably smaller back then.

    Microorganisms living in this area 6,000 years ago would have feasted on the inflow from the ocean. And their descendants still seem to as well. The researchers found traces of carbon-14 in the water samples as well as in the sediment, suggesting the microbes are recycling the ancient carbon deposited in the lake bed as food.

    The new study emphasizes how much information is waiting to be found in Antarctica’s hidden lakes, Venturelli says. “There are about 675 lakes under the ice sheet, and we’ve only sampled two,” she says. “I would very much like to drill into every single one of them.” More

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    Satellite data reveal nearly 20,000 previously unknown deep-sea mountains

    The number of known mountains in Earth’s oceans has roughly doubled. Global satellite observations have revealed nearly 20,000 previously unknown seamounts, researchers report in the April Earth and Space Science.

    Just as mountains tower over Earth’s surface, seamounts also rise above the ocean floor. The tallest mountain on Earth, as measured from base to peak, is Mauna Kea, which is part of the Hawaiian-Emperor Seamount Chain.

    These underwater edifices are often hot spots of marine biodiversity (SN: 10/7/16). That’s in part because their craggy walls — formed from volcanic activity — provide a plethora of habitats. Seamounts also promote upwelling of nutrient-rich water, which distributes beneficial compounds like nitrates and phosphates throughout the water column. They’re like “stirring rods in the ocean,” says David Sandwell, a geophysicist at the Scripps Institution of Oceanography at the University of California, San Diego.

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    More than 24,600 seamounts have been previously mapped. One common way of finding these hidden mountains is to ping the seafloor with sonar (SN: 4/16/21). But that’s an expensive, time-intensive process that requires a ship. Only about 20 percent of the ocean has been mapped that way, says Scripps earth scientist Julie Gevorgian. “There are a lot of gaps.”

    So Gevorgian, Sandwell and their colleagues turned to satellite observations, which provide global coverage of the world’s oceans, to take a census of seamounts.

    The team pored over satellite measurements of the height of the sea surface. The researchers looked for centimeter-scale bumps caused by the gravitational influence of a seamount. Because rock is denser than water, the presence of a seamount slightly changes the Earth’s gravitational field at that spot. “There’s an extra gravitational attraction,” Sandwell says, that causes water to pile up above the seamount.

    Using that technique, the team spotted 19,325 previously unknown seamounts. The researchers compared some of their observations with sonar maps of the seafloor to confirm that the newly discovered seamounts were likely real. Most of the newly discovered underwater mountains are on the small side — between roughly 700 and 2,500 meters tall, the researchers estimate.

    However, it’s possible that some could pose a risk to mariners. “There’s a point when they’re shallow enough that they’re within the depth range of submarines,” says David Clague, a marine geologist at the Monterey Bay Aquarium Research Institute in Moss Landing, Calif., who was not involved in the research. In 2021, the USS Connecticut, a nuclear submarine, ran into an uncharted seamount in the South China Sea. The vessel is still undergoing repairs at a shipyard in Washington state. More

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    Thawing permafrost may unleash industrial pollution across the Arctic

    As the Arctic’s icebound ground warms, it may unleash toxic substances across the region.

    By the end of the century, the thaw threatens to destabilize facilities at more than 2,000 industrial sites, such as mines and pipelines, and further compromise more than 5,000 already contaminated areas, researchers report March 28 in Nature Communications.

    Those numbers come from the first comprehensive study to pinpoint where Arctic permafrost thaw could release industrial pollutants. But there are probably even more contaminated areas that we don’t know about, says permafrost researcher Moritz Langer of the Alfred Wegener Institute in Potsdam, Germany. “We only see the tip of the iceberg.”

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    Toxic substances released from these locations could jeopardize fish and other animals living in Arctic waterways, as well as the health of people who depend on them.

    Permafrost is any soil, sediment or rock that remains frozen for at least two years. Step on the ground in the Arctic and chances are that permafrost lies underfoot. For decades, people have treated the frozen earth as staunch and largely immobile. Industries constructed infrastructure atop its firmness, and within it they buried their refuse and sludge. In some places, scientists and others have used permafrost to store radioactive waste.

    But the Arctic is warming nearly four times as fast as the rest of the planet as a result of climate change, and as much as 65 percent of the region’s permafrost may disappear by 2100 (SN: 8/11/22).

    That could release some worrisome things, says climate scientist Kimberley Miner of NASA’s Jet Propulsion Laboratory in Pasadena, Calif., who wasn’t involved in the study. In 2021, Miner and her colleagues warned that the thawing of Arctic permafrost could release antibiotic-resistant bacteria, viruses and radioactive waste from nuclear-testing programs into the environment.

    Keen to identify where the warming could spread industrial pollutants, Langer and his colleagues first analyzed the range of Arctic permafrost and whereabouts of industrial infrastructure. They identified about 4,500 sites — including oil fields, mines and abandoned military installations — in places where permafrost probably exists. Next, the team used contamination data from Alaska and Canada — regions with accessible records — and found that as of January 2021, about 3,600 contaminated locations occupy the two regions. These include waste areas and places where pollutants were accidentally released.

    Realistically, these numbers are probably deflated, Langer says, because many incidents of contamination have probably gone undocumented.

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    Focusing on Alaska, the researchers found that diesel, gasoline and related petrochemicals make up about half of the pollutants reported. Lead, arsenic and mercury — substances toxic to fish, people and other organisms — were reported too. But in many cases, the type of pollutant was not documented. “That’s a big problem,” Langer says, in part because it makes understanding the risks of a particular leak or spill much harder.

    Using the locations of industrial sites and North American contamination data, Langer and colleagues extrapolated where industrial contamination and permafrost might coexist across the entirety of the Arctic, finding 13,000 to 20,000 such sites may exist today. Then, they used computer simulations to investigate the impact of current and future levels of climate change.

    Today, there may already be a risk of permafrost degrading at about 1,000 of the known industrial sites and 2,200 to 4,800 of the known and estimated contaminated locations, they found.

    In a low-emissions scenario in which warming rises by up to 2 degrees Celsius above preindustrial levels by the end of the century, those numbers increase to more than 2,100 industrial sites and 5,600 to 10,000 contaminated areas. An increase of about 4.3 degrees C would probably affect almost all the known and projected locations.

    “We’re going to need to think about keeping [pollutants] where they need to be,” Miner says, “not just leaving them on the landscape where we feel like.”

    The new findings are probably conservative, Langer says, partly because the analysis didn’t consider that infrastructure itself can warm the ground. What’s more, even if it doesn’t fully thaw, “warming of the permafrost causes quite a bit of problem,” says civil engineer Guy Doré of Université Laval in Quebec City, who wasn’t involved in the study. Permafrost that warms from –5° C to –2° C can lose half of its load-bearing capacity, he says, destabilizing infrastructure.

    Today, no international regulations mandate industries in the Arctic to document the substances they use and store, or what happens to them. Without that information, Langer says, it’ll be difficult to assess and manage the growing risk of contamination.

    He plans to visit decades-old oil drilling facilities in Canada to study how the changing permafrost has affected the containment of drilling fluids. “That’s the next step,” he says, “to understand better how [industrial contaminants] spread into the landscape.” More

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    Ultrasound reveals trees’ drought-survival secrets

    The tissues of living trees may hold the secrets of why some can recover after drought and others die. But those tissues are challenging to assess in mature forests. After all, 90-year-old trees can’t travel to the lab to get an imaging scan. So most studies of the impacts of drought on plants are done in the lab and on younger trees — or by gouging cores out of mature trees.

    Barbara Beikircher, an ecophysiologist at the University of Innsbruck in Austria, and colleagues came up with a different approach: They brought the lab to the trees.

    In the Kranzberg Forest outside Munich, the team outfitted stands of mature spruce and beech trees with rugged, waterproof ultrasound sensors. Some of the stands had been covered by roofs to block the summer rain, creating artificial drought conditions.

    Researchers outfitted stands of mature spruce and beech trees with ultrasound sensors and electrical probes to figure how the species cope with long dry spells.University of Innsbruck

    Five years of monitoring revealed that beeches (Fagus sylvatica) are more drought-resilient than spruces (Picea abies), the team reported in the December Plant Biology. Delving into the underlying mechanisms explained this difference.

    Drought-stressed trees produced more ultrasound signals than trees exposed to summer rains. Those faint acoustic waves were bouncing off air bubbles called embolisms deep within the trees’ vasculature. Surface tension keeps water moving through a tree’s thousands of tiny vessels — evaporation from pores in leaves drives water up the trunk (SN: 9/6/22). But if there’s insufficient water in the soil, this upward pull can generate embolisms that clog vessels. In the experiments, spruces pinged much more than beeches, suggesting they had far more embolisms.

    That’s despite the fact that beeches appear to be less conservative with their water management, at least aboveground. Trees can prevent embolisms by closing the pores on their leaves, but there’s a trade-off. Doing so cuts off the supply of the carbon dioxide that drives photosynthesis, which makes the carbohydrates and sugars that trees need to live and grow. In dry conditions, trees face an impossible choice “between starving and dying of thirst,” Beikircher says.

    Beeches suffered fewer embolisms than the spruce, even though they kept their pores open longer than the conifers did. Perhaps that’s because beeches have roots that extend into deeper, wetter soil as well as more robust water reserves, Beikircher says. Another set of experiments after the researchers relieved the drought suggests that’s the case.

    At the end of the experiment, the team drenched the soil. All the trees recovered well by most measures: Rates of photosynthesis in the previously parched trees caught up to the rates of trees in the control groups and embolisms filled with water.

    But when Beikircher measured the trees’ resistance to an electrical current, an indication of moisture levels deep within trunks, the spruces’ water reserves were still depleted. One season of rain was not enough to help these trees fully recover. It’s unclear whether spruces can replenish their reserves after prolonged drought or how long that might take.

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    Species that can withstand drought conditions and recover more quickly may become more populous in future forests as climate change causes droughts to become more frequent and intense (SN: 3/10/22). That means the compositions of the trees that make up the world’s temperate forests could change as the climate warms, with uncertain consequences for the other plants and animals in these ecosystems.

    Beikircher plans to test whether a more diverse forest could help drought-sensitive species like the spruce survive. Deep-rooted beeches interspersed with spruces might help increase moisture in the soil’s upper levels by wicking water up to where spruce roots are, she says. More

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    A massive cavern beneath a West Antarctic glacier is teeming with life

    The coastal plain of the Kamb Ice Stream, a West Antarctic glacier, hardly seems like a coast at all. Stand in this place, 800 kilometers from the South Pole, and you see nothing but flat ice extending in every direction. The ice is some 700 meters thick and stretches for hundreds of kilometers off the coastline, floating on the water. On clear summer days, the ice reflects the sunlight with such ferocity that it inflicts sunburn in the insides of your nostrils. It might seem hard to believe, but hidden beneath this ice is a muddy tidal marsh, where a burbling river wends its way into the ocean.

    Until recently, no human had ever glimpsed that secret landscape. Scientists had merely inferred its existence from the faint reflections of radar and seismic waves. But in the closing days of 2021, a team of scientists from New Zealand melted a narrow hole through the glacier’s ice and lowered in a camera. They had hoped that their hole would intersect with the river, which they believed had melted a channel up into the ice — a vast water-filled cavity, nearly tall enough to hold the Empire State Building and half as long as Manhattan. On December 29, Craig Stevens finally got his first look inside. It is a moment that he will always remember.

    Stevens is a physical oceanographer with New Zealand’s National Institute of Water and Atmospheric Research in Wellington. He spent 90 anxious minutes that day in Antarctica with his head buried ostrich-style under a thick down jacket to block the sunlight that would otherwise obscure his computer monitor. There, he watched live video from the camera as it descended into the hole. Icy circular walls scrolled past, reminiscent of a cosmic wormhole. Suddenly, at a depth of 502 meters, the walls widened out.

    Stevens shouted for a colleague to halt the winch lowering the camera. He stared at the screen as the camera rotated idly on its cable. Its floodlights raked across a ceiling of glacial ice — a startling sight — scalloped into delicate crests and waves. It resembled the dreamy undulations that might take millennia to form in a limestone cavern.

    The Kamb Ice Stream is located on the coast of West Antarctica and flows into the Ross Ice Shelf, a slab of floating ice hundreds of meters thick. The site of the newly discovered cavern is shown as a yellow box.A. WHITEFORD ET AL/JOURNAL OF GEOPHYSICAL RESEARCH: EARTH SURFACE 2022

    “The interior of a cathedral,” says Stevens. A cathedral not only in beauty, but also in size. As the winch restarted, the camera journeyed downward for another half hour, through 242 meters of sunless water. Bits of reflective silt stirred up by currents streamed back down like snowflakes through the black void.

    Stevens and his colleagues spent the next two weeks lowering instruments into the void. Their observations revealed that this coastal river has melted a massive, steep-walled cavern cutting as far as 350 meters up into the overlying ice. The cavern extends for at least 10 kilometers and appears to be boring inland, farther upstream, into the ice sheet with each passing year.

    This cavity offers researchers a window into the network of subglacial rivers and lakes that extends hundreds of kilometers inland in this part of West Antarctica. It’s an otherworldly environment that humans have barely explored and is laden with evidence of Antarctica’s warm, distant past, when it was still inhabited by a few stunted trees.

    Researchers got their first glimpse into the hidden landscape in late 2021, when they drilled through 500 meters of ice and lowered in instruments to observe the cavern below (borehole shown).C. STEVENS/NIWA (CC BY-ND)

    One of the biggest surprises came as the camera reached bottom that day. Stevens gazed in disbelief as dozens of orange blurs swam and darted on his monitor — evidence that this place, roughly 500 kilometers from the open, sunlit ocean, is nonetheless bustling with marine animals.

    Seeing them was “just complete shock,” says Huw Horgan, a glaciologist formerly at the Victoria University of Wellington who led the drilling expedition.

    Horgan, who recently moved to ETH Zurich, wants to know how much water is flowing through the cavern and how its growth will impact the Kamb Ice Stream over time. Kamb is unlikely to fall apart anytime soon; this part of West Antarctica is not immediately threatened by climate change. But the cavern might still offer clues to how subglacial water could affect more vulnerable glaciers.

    What’s beneath Antarctica’s ice sheet?

    Scientists have long surmised that a veneer of liquid water sits beneath much of the ice sheet covering Antarctica. This water forms as the bottom of the ice slowly melts, several penny-thicknesses per year, due to heat seeping from the Earth’s interior. In 2007, Helen Amanda Fricker, a glaciologist at the Scripps Institution of Oceanography in La Jolla, Calif., reported evidence that this water pools into large lakes beneath the ice and can flood quickly from one lake to another (SN: 6/17/06, p. 382).

    Fricker was looking at data from NASA’s Ice, Cloud and Land Elevation Satellite, or ICESat, which measures the height of the ice surface by reflecting a laser off of it. The surface at several spots in West Antarctica seemed to bob up and down, rising and falling by as much as nine meters over a couple of years. She interpreted these active spots as subglacial lakes. As they filled and then spilled out their water, the overlying ice rose and fell. Fricker’s team and several others eventually found over 350 of these lakes scattered around Antarctica, including a couple dozen beneath Kamb and its neighboring glacier, the Whillans Ice Stream.

    The lakes provoked great interest because they were expected to harbor life and might provide insights about what sorts of organisms could survive on other worlds — deep within the ice-covered moons of Jupiter and Saturn, for instance. The layers of sediment in Antarctica’s lakes might also offer glimpses into the continent’s ancient climate, ecosystems and ice cover. Teams funded by Russia, the United Kingdom and the United States attempted to drill into subglacial lakes. In 2013, the U.S.-led team succeeded, melting through 800 meters of ice and tapping into a reservoir called Subglacial Lake Whillans. It was teeming with microbes, 130,000 cells per milliliter of lake water (SN: 9/20/14, p. 10).

    Horgan helped map Lake Whillans before drilling began. But by the time the lake was breached, he and others were becoming intrigued with another facet of the subglacial landscape — the rivers thought to carry water from one lake to another, and eventually to the ocean.

    Finding these hidden rivers requires complicated guesswork. Their flow paths are influenced not only by the subglacial topography, but also by differences in the thickness of the overlying ice. Water moves from places where the ice is thick (and the pressure high) to places where it is thinner (and the pressure lower) — meaning that rivers can sometimes run uphill.

    By 2015, scientists had mapped the likely paths of several dozen subglacial rivers. But drilling into them still seemed farfetched. The rivers are narrow targets and their exact locations often uncertain. But around that time, Horgan got a lucky break.

    While examining a satellite photo of the Kamb Ice Stream, he noticed a wrinkle in the pixelated tapestry of the image. The wrinkle resembled a long, shallow trough in the surface of the ice, as if the ice had sagged from melting beneath. The trough sat several kilometers from the hypothetical path of one subglacial river. Horgan believed that it marked the spot where that river flowed over the coastal plain and spilled into the ice-covered sea.

    In 2016, while visiting the area for an unrelated research project, Horgan and his companions detoured briefly to the surface trough to take radar measurements. Sure enough, they found a void under the ice, filled with liquid water. Horgan began making plans to study it more closely. He would return twice in the next few years, once to map the river in detail and a second time to drill into it. What he found greatly exceeded his expectations.

    Scientists map a subglacial landscape

    Horgan and graduate student Arran Whiteford of the Victoria University of Wellington visited the lower Kamb Ice Stream to map the river in December 2019.

    After weeks on the Antarctic ice sheet, they’d grown accustomed to its monotonous flat landscape, their perception sensitized to even tiny ups and downs. In this context, the surface trough “looked like this massive chasm,” Whiteford says, “like an amphitheater” — even though it slanted no more dramatically than a rolling cornfield in Iowa.

    It was a week of scientific drudgery, towing the ice-penetrating radar behind a snowmobile along a series of straight, parallel lines that crisscrossed the trough to map the shape of the river channel under the ice.

    Horgan and Whiteford worked up to 12 hours per day, occasionally trading positions. One person drove the snowmobile, straining his thumb on the throttle to maintain a constant 8 kilometers per hour. Two sleds hissed along behind. One held a transmitter that fired radar waves into the glacier below; the other held an antenna that received the signal reflected back off the bottom of the ice. The second person rode on the sled with the antenna, his eyes on a bouncing laptop screen making sure that the radar was functioning.

    Researchers deploy instruments through a borehole into the water-filled cavern hidden beneath the Kamb Ice Stream.H. HORGAN

    Each evening they huddled in their tent, reviewing their radar traces. The river channel appeared far more dramatic than the gentle dip atop the ice suggested. Below their boots sat a vast water-filled cavern with steep sides like a train tunnel, 200 meters to a kilometer wide and cutting as much as 50 percent of the way up through the glacier. The more they looked, the more it resembled a river. “It kind of meanders downstream,” Whiteford says.

    All told, Whiteford made two weeklong visits to the trough, snowmobiling over from another camp 50 kilometers away. The first time he was accompanied by Horgan, and the second time by another graduate student, Martin Forbes.

    After returning home to New Zealand in January 2020, Whiteford examined a series of old satellite images. They showed that the surface trough — and hence, the cavern — had begun forming at least 35 years before, starting with a blip at the very mouth of the river, where it ran into the ocean. That blip had gradually lengthened, reaching progressively farther inland, or upstream. Whiteford and Horgan reported the observations in late 2022 in the Journal of Geophysical Research: Earth Surface — along with their theory about how the cavern formed.

    In other parts of Antarctica where the ice sheet protrudes off the coastline, scientists have found that the ice’s underside is often insulated from the ocean heat by a buoyant layer of colder, fresher meltwater. That protective layer is sometimes only a couple of meters thick. But Horgan and Whiteford suspect that the turbulence of the subglacial river flowing into the ocean stirs up that protective layer, causing seawater — a few tenths of a degree warmer than the subglacial water — to swirl up into contact with the ice. This causes an area of concentrated melt right at the river’s mouth, creating a small cavity where warm seawater can intrude further.

    In this way, says Horgan, the focal point of melting is “stepping back over time.” And the cavern gradually burrows farther upstream into the ice.

    Whiteford used a different set of satellite measurements — which measured the rate at which the ice’s surface sank over time — to determine how quickly the ice was melting in the cavern below. Based on this, he estimated that in the upstream end of the cavern, the ice (currently 350 to 500 meters thick over the channel) was melting and thinning 35 meters per year. That’s an astronomical rate. It’s 135 times what has been measured 50 kilometers southwest of the cavern, where the ice floats on the ocean. The water temperature is probably similar at both locations. But the turbulence caused by the river transfers the water’s heat far more efficiently into the ice.

    Horgan thinks that the cavern at Kamb also owes its dramatic height to another factor. Glaciers in this part of West Antarctica generally flow several hundred meters per year. So the melt caused by a flowing river beneath, over years or decades, would normally be spread out over a long swath of ice. This would erode a shallow channel rather than a deep cleft. But Kamb is an oddball. Around 150 years ago, it stopped moving almost entirely due to the cyclical interplay of melting and freezing at its base. It now creeps forward only about 10 meters per year. The melting is thus concentrated, year after year, in almost the same spot.

    Back in 2020, all of this was still conjecture. But if Horgan and his colleagues could return, drill into the cavern and lower instruments into it, they could confirm how it formed. By studying the water, sediment and microbes flowing out of it, they could also learn a lot about Antarctica’s vast subglacial landscape.

    The West Antarctic Ice Sheet covers an area three times the size of the Colorado River drainage basin, which sprawls across Arizona, Utah, Colorado and parts of four other states. To date, humans have observed only a tiny swath of this underworld, smaller than a basketball court — represented by several dozen narrow boreholes scattered across the region, where scientists have grabbed a bit of mud from the bottom or sometimes lowered in a camera.

    Horgan was eager to explore more. With New Zealand already melting boreholes through ice floating on the ocean, drilling into this coastal river seemed like a natural next step.

    How did the hidden cavern form?

    On December 4, 2021, a pair of caterpillar-tracked PistenBullys arrived at the place where Horgan and Whiteford had visited two years before. The tractors had traveled for 16 days from New Zealand’s Scott Base on the edge of the continent, growling across a thousand kilometers of floating ice as they towed a convoy of sleds packed with 90 metric tons of food, fuel and scientific gear. The convoy lumbered around to the upstream end of the valley and stopped.

    Workers erected a tent the size of a small aircraft hangar, and inside it, assembled a series of water heaters, pumps and a kilometer of hose — a machine called a hot water drill. Using shovels and a small mechanized scooper, they dumped 54 tons of snow into a tank and melted it. The workers then jetted that hot water through the hose, using it to melt a narrow hole, no wider than a dinner plate, through 500 meters of ice — and down through the domed ceiling of the cavern.

    The sight of animals inside the cavern generated instant excitement among Horgan, Stevens and the other people at camp. But those first images were blurry, leaving people unsure of what the orange, bumblebee-sized critters actually were.

    Workers next lowered an instrument down the borehole to measure the water temperature and salinity inside the cavern. They found the top 50 meters of water colder and fresher than what lay below — confirming that seawater was flowing in along the bottom and a more buoyant mixture of saltwater and freshwater was flowing out along the top. The cavern, says Stevens, “is operating quite like an estuary.”

    But those measurements also presented a mystery: The water in the top of the cavern was only about 1 percent less salty than the seawater in its bottom, suggesting that the amount of freshwater flowing in through the river was “quite small,” says Stevens. It’s akin to a shallow creek that a young kid might splash around in. He and Horgan doubted that the turbulence caused by this small flow, even over 35 years, could melt the entire cavern — roughly a cubic kilometer of ice.

    A likely answer came from a set of samples collected from the floor of the cavern. Gavin Dunbar, a sedimentologist at the Victoria University of Wellington, lowered a hollow plastic cylinder down the hole in hopes of retrieving a core. As he and graduate student Linda Balfoort hoisted the cylinder back up, they found it streaked and filled with chocolaty mud — a strange sight in this world of pure white, where not a speck of rock or dirt can be seen for hundreds of kilometers.

    As Dunbar and Balfoort X-rayed and analyzed the cores months later, back in New Zealand, their peculiarities became obvious: They were unlike anything that Dunbar had ever encountered in this part of the world.

    Every core that Dunbar had ever seen from the seafloors near this part of Antarctica consisted of a chaotic jumble of sand, silt and gravel — a material called diamict, formed as the ice sheet advances and retreats over the seafloor, plowing and mixing it like a rototiller. But in these cores, Dunbar and Balfoort saw distinct layers. Bands of coarse, gravely material were interspersed with layers of fine, silty mud.

    That alternating pattern resembled samples from steep seafloor canyons off the coast of New Zealand, where earthquakes sometimes trigger underwater landslides that sweep for many kilometers downhill. Each flood deposits a single layer of chunky material.

    Dunbar believes that something similar happened under the Kamb Ice Stream, possibly in the last few decades. A series of fast-moving torrents gushed through the river channel carrying big gravelly chunks from somewhere upstream that later settled on the cavern floor. “Each of these [coarse layers] represents minutes to hours of sediment deposition” that occurred during a single flood, he says. And the fine, silty layers would have been laid down over years or decades in between the floods, when the river flowed languidly along.

    These subglacial floods could explain how this small river carved such a large cavern, Stevens says. Those floods could have been 100 to 1,000 times as large as the flow rates that were measured during the 2021–22 field season.

    No one knows when those events happened, but scientists using satellites to study subglacial lakes have spotted at least one candidate. In 2013, a lake 20 kilometers upstream from the cavern, called KT3, disgorged an estimated 60 million cubic meters of water — enough to fill 24,000 Olympic-sized swimming pools.

    Scientists would love to know whether that flood actually passed through this cavern. “Connecting this upstream to the lake system would be extremely cool,” says Matthew Siegfried, a glaciologist at the Colorado School of Mines in Golden, who coauthored one of the reports documenting the 2013 flood.

    Studying the outflow of this river could also answer other questions about the subglacial landscape upstream. “The vast majority of our knowledge of subglacial lakes comes from surface observations from space,” Siegfried says. But those satellite records, of ice bobbing up and down, permit only indirect estimates of how much water is flowing through. It’s possible, for example, that a lot of water passes through the lakes even when the ice above isn’t moving.

    Scientists could also learn about the subglacial landscape by studying the sediment washed downstream. When Dunbar and his colleagues examined the coarse material from their cores, they found it full of microscopic fossils: glassy shells of marine diatoms, needly spicules of sea sponges, and notched and spiky pollen grains of southern beech trees. These fossils represent the remains of a warmer world, 15 million to 20 million years ago, when a few stands of stunted, shrubby trees still clung to parts of Antarctica. Back then, the West Antarctic basin held a sea rather than an ice sheet, and this detritus settled on its muddy bottom. These old marine deposits underlie much of the West Antarctic Ice Sheet, and the few boreholes drilled so far suggest that the mix of fossils differs from one place to another. Those mixes could provide clues to how the flow of rivers changes over time.

    To uncover the nuance of what’s happening in the cavern “is mind-blowingly cool,” says Christina Hulbe, a glaciologist at the University of Otago in Dunedin, New Zealand, who has studied this region of Antarctica for nearly 30 years. “That’s the outlet for a massively big river system, if you think about it.”

    By studying the water, scientists could estimate the amount of organic carbon and other nutrients flowing out of the river into the ice-covered ocean. The landscape beneath the ice sheet appears to be rich in nutrients that might sustain oases of life in an otherwise famished biological desert.

    Scientists unveil an oasis of life

    Even as the cavern penetrates farther into the Kamb Ice Stream, it does not necessarily threaten the glacier’s stability. This part of the West Antarctic coastline is not considered vulnerable, because its shallow bed shields it from the deep, warm ocean currents that are causing rapid ice loss in other regions. But subglacial rivers pour out at many other points along the coastline, including some — like Thwaites Glacier, roughly 1,100 kilometers northeast of Kamb — where the ice is retreating rapidly (SN: 3/11/23, p. 8).

    Thwaites and nearby glaciers have collectively shed over 2,000 cubic kilometers of ice since 1992. They could eventually raise global sea levels by 2.3 meters if they collapse. Remote sensing studies have documented over a dozen low, squat shield volcanoes beneath this part of the ice sheet. The elevated geothermal heat flow, even from inactive volcanoes, is thought to cause high levels of melting under the ice sheet. That melting produces large amounts of subglacial water, which could render these glaciers even more vulnerable to human-caused climate change.

    Horgan believes that what scientists learn at Kamb could improve our understanding of how subglacial rivers impact those other, rapidly changing coastlines of Antarctica.

    But the most evocative discovery made at Kamb — in purely human terms — may be the blurry, orangish animals seen swarming near the bottom of the cavern. Stevens captured some clearer images a few days later and tentatively identified them as shrimp­like marine crustaceans called amphipods. To see so many of them here, Stevens says, “we really hadn’t expected that.”

    [embedded content]
    Video from a camera lowered into a hidden cavern beneath the Kamb Ice Stream showed animals, perhaps amphipods, swimming about. They may subsist in part on nutrients transported by a subglacial river.

    Microbes like those previously found under the ice sheet in Subglacial Lake Whillans are known to eke out a living even in harsh conditions. But animals are a different matter. The deepest seafloors on Earth sit only 10 or 11 kilometers from sunlight, and animal life in those places is generally scarce. But the animals in the cavern are thriving 500 kilometers from the nearest daylight, cut off from the photosynthesis that fuels most life on Earth.

    The amphipods and their supporting ecosystem must be subsisting on some other food source. But what? Observations in the Kamb ice cavern, combined with those at two other remote boreholes drilled in recent years, offer some tantalizing hints.

    In 2015, researchers pierced the ice at another site 250 kilometers from the cavern, where the Whillans Ice Stream lifts off its bed and floats. In that location, a thin sliver of seawater, just 10 meters deep, sits beneath 760 meters of ice. A remotely operated vehicle, or ROV, sent down the hole captured images of fish and amphipods.

    John Priscu, a microbial ecologist at Montana State University in Bozeman who was involved in the drilling at the site, believes that the glacier itself is sustaining this ecosystem. The bottom 10 meters of ice is packed with mud that had frozen onto the belly of the glacier many kilometers upstream. The mud had been dragged to its present location as the glacier oozed forward, 400 meters per year. As the ROV navigated about, bits of that muddy debris constantly rained down, released as the ice’s underside slowly melted. That debris is rich in organic matter — the rotting remains of diatoms and other phytoplankton that sank to the bottom millions of years ago when the world was warmer.

    “Those amphipods are swarming to the particulate matter,” Priscu says. “They’re sensing the organic matter falling out of that basal ice.” Or perhaps they may be eating the bacteria that live on those organics.

    Because the Kamb Ice Stream is barely moving, the supply of dirty ice moving toward the sea is small. But the river flowing into the ice cavern may deliver the same subglacial nutrients that are found in dirty ice. After all, the water’s journey through a series of subglacial lakes down to the river’s mouth may take years or decades. Throughout that time, the river absorbs nutrients from the organic-rich subglacial sediments.

    Indeed, when scientists drilled into Subglacial Lake Whillans in 2013, they found its water honey-colored — chock-full of life-sustaining iron, ammonium and organics. “What these lakes are pumping out may be a concentrated source of nutrients” for ecosystems along the dark coastline, says Trista Vick-Majors, a microbial ecologist at Michigan Technological University in Houghton who was involved in the drilling at Lake Whillans. She has estimated that the subglacial rivers flowing out from under Kamb and its neighboring glaciers may deliver 56,000 tons of organic carbon and other nutrients to this section of the coastline every year.

    More recently, in December 2019, a team from New Zealand led by Horgan and Hulbe drilled through the ice just 50 kilometers from the Kamb cavern, in a place where the Kamb Ice Stream floats on the ocean. There’s no dirty ice there and no nearby river outlets. The area resembled a famished seafloor desert; it was populated by single-celled microbes with little to eat, and few signs of animals were seen — only a few burrowing traces on the muddy bottom. Priscu sees this location as an exception that proves the point: Subglacial nutrients are the crucial energy source in this dark world under the floating ice, whether they are dragged forward on the undersides of glaciers or spilled out through subglacial rivers.

    The mud and water samples collected from the Kamb ice cavern may provide a new opportunity to test that theory. Craig Cary, a microbial ecologist at the University of Waikato in New Zealand, is analyzing DNA from those samples. He hopes to determine whether the microbes in the cavern belong to taxonomic groups that are known to subsist on ammonium, methane, hydrogen or other sources of chemical energy that originate from the subglacial sediments. That might reveal whether such sources support enough microbial growth to feed the animals observed there.

    The team also needs to measure the flow rate of the subglacial river that spills into the cavern, since that determines the nutrient supply. Stevens continues to monitor this thanks to a set of instruments left behind in the cavern.

    At the end of the trip, scientists including Craig Stewart (right) and Andrew Mullen (center) lowered instruments (a current meter is shown) into the cavern so they could continue monitoring it from afar.C. STEVENS/NIWA

    As people were packing up camp on January 11, 2022, workers pumped more hot water into the borehole, widening it to more than 35 centimeters — and creating a dangerous pitfall. Stevens and his colleagues donned climbing harnesses, clipped into safety ropes and approached the hole one last time. They lowered a series of cylinders the size of caulking guns down the hole. These devices continue to measure the temperature, salinity and water currents inside the cavern, sending the data 500 meters up a cable to a transmitter that beams it home via satellite once a day. That data will reveal how the river’s flow changes over time. With luck, the instruments might even detect a subglacial flood gushing through.

    “That would just be outstanding,” Horgan says. For many years, he had to content himself with seeing these rivers and lakes dimly, through the outlines of water on radar and satellite images. This is “one of the first times we’ve got to stand at a river mouth and observe it.” More