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Study Shows Mercury Levels in Arctic Wildlife Could Rise for Centuries

Study Shows Mercury Levels in Arctic Wildlife Could Rise for Centuries

New York Times13-06-2025
Levels of mercury in Arctic wildlife could continue to rise significantly even as countries curb their emissions, a new study suggests.
Researchers analyzed more than 700 samples of fish, mammals and peat collected across Greenland over the past 40 years and found evidence that the mercury in them was distributed by ocean currents.
The finding, published this week in the journal Nature Communications, helps explain why levels of mercury contamination have continued increasing in the Arctic even as global emissions have begun to plateau.
'We got a lot of surprises when we analyzed the data,' said Jens Sondergaard, a senior ecological science researcher at Aarhus University in Denmark and lead author of the study. 'It's a really striking trend.'
Exposure to high concentrations of mercury, a potent neurotoxin, can lead to neurological and other health-related effects and the study confirms that mercury emitted today could continue posing a large threat to humans and wildlife in the region for centuries.
eBy analyzing mercury isotopes, a unique kind of chemical signature that can be matched like a fingerprint, the researchers traced the spread of mercury contamination to the patterns of ocean currents around Greenland. Previous research has shown that mercury can persist in oceans for more than 300 years.
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Astronomers Found the Most Self-Destructive Planet in the Sky
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Stars often whip their planets with solar winds and radiation, pull them ever closer with gravity and sear them with heat. But a newfound planet exerts an unexpectedly strong—and ultimately self-destructive—influence on its star in return. The star HIP 67522 is slightly larger than our sun and shines roughly 408 light-years away in the Scorpius-Centaurus star cluster. It's 17 million years old, a youngster by stellar standards, and has two orbiting planets that are even younger. The innermost of these two planets, a Jupiter-size gas giant called HIP 67522 b, orbits HIP 67522 at a distance of less than 12 times the star's radius—almost seven times closer than Mercury's distance from the sun in our Solar System. This in-your-face proximity, combined with HIP 67522's volatile teenage nature, has created a spectacle astronomers have never seen before: a planet that triggers powerful flares on the surface of its host star, leading to the planet's own slow destruction. 'In a way, we got lucky,' says Ekaterina Ilin, an astrophysicist at the Netherlands Institute for Radio Astronomy (ASTRON), who led the study on the HIP 67522 system, published on Wednesday in Nature. 'We took all the star-planet systems that we knew of and just went ahead looking for flares—sudden intense bursts of radiation coming from the star's surface.' Parsing through the data gathered by two space-based telescopes, NASA's TESS (Transiting Exoplanet Survey Satellite) and the European Space Agency's CHEOPS (Characterizing Exoplanet Satellite), Ilin's team noticed that HIP 67522's flares seemed to be synchronized with its closest planet's orbital period. And those flares were gigantic—'thousands of times more energetic than anything the sun can produce,' Ilin says. On supporting science journalism If you're enjoying this article, consider supporting our award-winning journalism by subscribing. By purchasing a subscription you are helping to ensure the future of impactful stories about the discoveries and ideas shaping our world today. The orbiting gas giant likely sparks these powerful flares by perturbing the star's strong magnetic field lines as it passes by in its orbit. This sends waves of energy downward along the lines—and when those waves meet the star's surface, a flare bursts out. The star's magnetic loops are 'almost like a spring waiting to be let go,' Ilin says. 'The planet's just giving it this last push.' Based on the team's observations, HIP 67522 b triggers a flare once every Earth day or two. And this action has severe consequences for the planet itself: Ilin estimates the unlucky gas giant gets six times more radiation than it would if it wasn't triggering flares and blasting away its own atmosphere. At this pace, Ilin's team says, HIP 67522 b will shrink from Jupiter's size to Neptune's in about 100 million years. 'Flaring might cut the lifetime of the planet's atmosphere in half,' she says. Researchers had suspected this type of star-planet interplay might occur, but they had never previously seen it, says Antoine Strugarek, an astrophysicist at the French Alternative Energies and Atomic Energy Commission's (CEA's) center CEA Paris-Saclay, who was not involved in the new study. 'This is the first time we see very convincing evidence such interaction has been actually detected,' he says. Ilin says it's too early to draw far-reaching conclusions from this first example of the phenomenon. As a next step, she says, researchers can compare HIP 67522 b with the other planet in the system, which orbits a bit farther from the star, to calculate how much mass the more closely orbiting world is actually losing through this process compared with the more distant one, which is likely only hit with random flares. Another unanswered question is exactly how the flare triggering works. 'Is it a wave [of magnetic energy] that propagates from the planet?' Ilin wonders. She suggests that what happens could be similar to an effect that has been seen on the sun: smaller solar flares sometimes perturb nearby magnetic loops and tip them over the edge to snap and produce a larger flare. But perhaps the most important question is how common the newly observed phenomenon is. For now, Ilin wants to focus on finding more systems where planets induce stellar flares that scientists can study. 'Once we figure out how it works, we can turn it into a planet-detection technique,' she says. Instead of searching for the planets themselves, researchers could look for stars that flare following a certain pattern—suggesting they, too, might have planets with a self-destructive bent.

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Around 252 million years ago, life on Earth suffered its most catastrophic blow to date: a mass extinction event known as the 'Great Dying' that wiped out around 90% of life. What followed has long puzzled scientists. The planet became lethally hot and remained so for 5 million years. A team of international researchers say they have now figured out why using a vast trove of fossils — and it all revolves around tropical forests. Their findings, published Wednesday in the journal Nature Communications, may help solve a mystery, but they also spell out a dire warning for the future as humans continue to heat up the planet by burning fossil fuels. The Great Dying was the worst of the five mass extinction events that have punctuated Earth's history, and it marked the end of the Permian geological period. It has been attributed to a period of volcanic activity in a region known as the Siberian Traps, which released huge amounts of carbon and other planet-heating gases into the atmosphere, causing intense global warming. Enormous numbers of marine and land-based plants and animals died, ecosystems collapsed and oceans acidified. What has been less clear, however, is why it got so hot and why 'super greenhouse' conditions persisted for so long, even after volcanic activity ceased. 'The level of warming is far beyond any other event,' said Zhen Xu, a study author and a research fellow at the School of Earth and Environment at the University of Leeds. Some theories revolve around the ocean and the idea that extreme heat wiped out carbon-absorbing plankton, or changed the ocean's chemical composition to make it less effective at storing carbon. But scientists from the University of Leeds in England and the China University of Geosciences thought the answer may lie in a climate tipping point: the collapse of tropical forests. The Great Dying extinction event is unique 'because it's the only one in which the plants all die off,' said Benjamin Mills, a study author and a professor of Earth system evolution at the University of Leeds. To test the theory, they used an archive of fossil data in China that has been put together over decades by three generations of Chinese geologists. They analyzed the fossils and rock formations to get clues about climate conditions in the past, allowing them to reconstruct maps of plants and trees living on each part of the planet before, during and after the extinction event. 'Nobody's ever made maps like these before,' Mills told CNN. The results confirmed their hypothesis, showing that the loss of vegetation during the mass extinction event significantly reduced the planet's ability to store carbon, meaning very high levels remained in the atmosphere. Forests are a vital climate buffer as they suck up and store planet-heating carbon. They also play a crucial role in 'silicate weathering,' a chemical process involving rocks and rainwater — a key way of removing carbon from the atmosphere. Tree and plant roots help this process by breaking up rock and allowing fresh water and air to reach it. Once the forests die, 'you're changing the carbon cycle,' Mills said, referring to the way carbon moves around the Earth, between the atmosphere, land, oceans and living organisms. Michael Benton, a professor of paleontology at the University of Bristol, who was not involved in the study, said the research shows 'the absence of forests really impacts the regular oxygen-carbon cycles and suppresses carbon burial and so high levels of CO2 remain in the atmosphere over prolonged periods,' he told CNN. It highlights 'a threshold effect,' he added, where the loss of forests becomes 'irreversible on ecological time scales.' Global politics currently revolve around the idea that if carbon dioxide levels can be controlled, damage can be reversed. 'But at the threshold, it then becomes hard for life to recover,' Benton said. This is a key takeaway from the study, Mills said. It shows what might happen if rapid global warming causes the planet's rainforests to collapse in the future — a tipping point scientists are very concerned about. Even if humans stop pumping out planet-heating pollution altogether, the Earth may not cool. In fact, warming could accelerate, he said. There is a sliver of hope: The rainforests that currently carpet the tropics may be more resilient to high temperatures than those that existed before the Great Dying. This is the question the scientists are tackling next. This study is still a warning, Mills said. 'There is a tipping point there. If you warm tropical forests too much, then we have a very good record of what happens. And it's extremely bad.'

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