Wildfires leave behind loss and ruin - charred homes, scorched forests, communities upended. Yet even in those blackened remnants, Professor Pei Chiu sees an overlooked resource with climate potential.&nbsp;



In his lab at the<a href="https://www.udel.edu/" target="_blank" rel="noreferrer noopener"> University of Delaware</a>, Professor Chiu studies “char,” the carbon-rich residue produced when biomass burns without much oxygen. His team has probed both naturally produced <a href="https://www.earth.com/news/wildfire-risk-is-rapidly-rising-across-the-southern-u-s/">wildfire</a> char and its artificial cousin, biochar.



The researchers uncovered a surprising role of chars: they can help starve methane-producing microbes and tilt microbial communities toward pathways that generate far less climate damage.



<h2 class="wp-block-heading" id="h-why-wildfire-char-is-everywhere">Why wildfire char is everywhere</h2>



Char forms whenever organic matter is heated at high temperatures with limited <a href="https://www.earth.com/news/dark-oxygen-discovery-deep-ocean-rocks-upends-centuries-of-scientific-beliefs/">oxygen</a>. In nature, that’s wildfires; in industry, it’s pyrolysis, the controlled heating of leftover biomass such as wood chips, corn stalks, rice husks, and other agricultural residues.&nbsp;



Commercial “biochar” is already used to improve soils, blend into compost, and filter stormwater. 



Wildfire char, by contrast, is scattered by the ton across burned landscapes and gradually worked into soils by wind, rain, and <a href="https://www.earth.com/news/plant-roots-could-be-key-to-fighting-climate-change/">roots</a>.



<h2 class="wp-block-heading" id="h-chars-that-behave-like-batteries">Chars that behave like batteries</h2>



Several years ago, Chiu’s group noticed something striking: chars made by pyrolysis behaved like tiny rechargeable batteries. They could store and release electrons - a property the team calls electron storage capacity (ESC).&nbsp;



That matters because <a href="https://www.earth.com/news/microbes-aquificales-discovered-in-hot-springs-breathe-oxygen-and-sulfur-at-same-time/">microbes</a> make a living moving electrons around. In oxygen-rich settings, they “breathe” oxygen to accept electrons as they break down sugars. In oxygen-poor places - think landfills, manure pits, waterlogged soils, rice paddies, <a href="https://www.earth.com/news/wetlands-are-a-hidden-source-of-rising-methane-emissions/">wetlands</a>, or the guts of anaerobic digesters - other organisms take over.&nbsp;



Among the most consequential are methanogens, microbes that churn out <a href="https://www.earth.com/news/microbes-have-emerged-as-major-source-of-methane-emissions/">methane</a>, a heat-trapping gas roughly 85 times more potent than CO₂ over the short term and responsible for about a third of current warming.



Chiu’s team showed that char gives many common soil microbes an alternative “breath.” In essence, char can stand in for oxygen as an electron sink, letting beneficial microbes keep metabolizing without ceding the field to methanogens. When that happens, methane production drops.



<h2 class="wp-block-heading" id="h-what-wildfires-have-to-do-with-it">What wildfires have to do with it</h2>



Wildfire char has been part of Earth’s carbon cycle for millions of years. That longevity led Chiu to a simple hypothesis: if char has been embedded in soils for eons, microbes likely evolved ways to use it.&nbsp;



Across a range of chars - those born in wildfires and those made in kilns - the team measured substantial ESC, enough to change who thrives in oxygen-limited environments.&nbsp;



<h2 class="wp-block-heading" id="h-how-much-charge-are-we-talking-about">How much “charge” are we talking about?</h2>



The numbers are eye-opening. In lab tests, a single gram of char - about a quarter teaspoon - could hold on the order of 10²¹ electrons. Scale that to real-world biomass and the potential grows fast.&nbsp;



U.S. agriculture alone generates roughly 140 million dry tons of crop residues each year (with corn stover and wheat straw leading the way), while forestry adds 60–70 million dry tons more.&nbsp;



Collectively, Chiu noted, chars represent an immense rechargeable, bioavailable reservoir of electrons - he likens it to a “trillion-trillion-trillion” (10³⁶) electrons injected into the global biogeochemical cycle annually.



<h2 class="wp-block-heading" id="h-turning-down-methane-naturally">Turning down methane - naturally</h2>



In controlled experiments, all wildfire chars and plant-based biochars tested suppressed methane formation.&nbsp;



The mechanism is elegant: by giving char-“breathing” microbes a competitive edge, the material helps outcompete methanogens, which still produce more than 50% of global methane today.&nbsp;



Unlike a chemical additive that’s used once and gone, char can be reused by microbes repeatedly, serving as a long-lived electron buffer in soils, sediments, and engineered systems.



<h2 class="wp-block-heading" id="h-cleaner-water-healthier-soils">Cleaner water, healthier soils</h2>



Steering electrons through char doesn’t only curb methane. The same microbial pathways can keep arsenic from mobilizing into drinking water or crops and can remove nitrate and perchlorate from stormwater and groundwater.&nbsp;



That dovetails with biochar’s existing uses in filtration and <a href="https://www.earth.com/news/planting-diverse-crops-traps-carbon-and-boosts-soil-health/">soil health</a>, suggesting one material can deliver multiple environmental services at once.



None of this minimizes the devastation of wildfires, which destroy ecosystems, businesses, and lives. But Chiu argues there’s value in learning from what’s left behind.&nbsp;



Wildfire char’s electron-trading ability points to a sustainable lever for <a href="https://www.earth.com/news/climate-mitigation-strategies-may-be-endangering-biodiversity/">climate mitigation</a> and pollution control - one built on microbes already common in nature and on carbon materials produced at massive scales, whether by accident (fires) or design (pyrolysis).



<h2 class="wp-block-heading" id="h-why-the-urgency-and-the-hope">Why the urgency - and the hope</h2>



CO₂ rightly dominates climate discussions, but it lingers for 50 to 200 years. Methane is different: far stronger in the near term and with an atmospheric lifetime of about 12 years. That makes near-term methane cuts an unusually fast-acting climate lever.&nbsp;



“If we can find ways to reduce methane, we could see the impact within our lifetimes,” said Professor Chiu.



That promise keeps his team pushing on the basic science: How exactly do microbes “breathe” a solid? How do different chars - from different fires, feedstocks, or kiln settings - shift ESC and microbial behavior?&nbsp;



And how can this knowledge be scaled into landfill covers, livestock waste systems, wetlands restoration, or post-fire land management so that nature’s own electron economy helps dial down a powerful greenhouse gas?



Char, in other words, may be the rare wildfire remnant that points forward.



Study co-authors include doctoral student Jiwon Choi and former graduate student Danhui Xin (now at the <a href="https://www.sccwrp.org/" target="_blank" rel="noreferrer noopener">Southern California Coastal Water Research Project</a>).



The research is published in the journal <a href="https://pubs.acs.org/doi/10.1021/acs.est.5c05709" target="_blank" rel="noreferrer noopener">Environmental Science &amp; Technology</a>.



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From ashes to action: Wildfire char holds a hidden climate solution

Wildfires leave behind loss and ruin - charred homes, scorched forests, communities upended. Yet even in those blackened remnants, Professor Pei Chiu sees an overlooked resource with climate potential.&nbsp; In his lab at the University of Delaware, Professor Chiu studies “char,” the carbon-rich residue produced when biomass burns without much oxygen. His team has probed both naturally produced wildfire char and its artificial cousin, biochar. The researchers uncovered a surprising role of chars: they can help starve methane-producing microbes and tilt microbial communities toward pathways that generate...

The Mediterranean has long been a crossroads of trade and tourism, yet its deepest pocket, the Calypso Deep, seemed beyond the reach of day-to-day pollution. 



That hope ended earlier this year when researchers reported plastic bags, glass shards, and crumpled cans resting 16,770 feet beneath the waves in the <a href="https://en.wikipedia.org/wiki/Ionian_Sea" target="_blank" rel="noreferrer noopener">Ionian Sea</a>.



Their survey logged hundreds of items on the trench floor. By any measure, it is one of the densest concentrations of trash ever recorded in the <a href="https://www.earth.com/news/deep-ocean-buffet-big-fish-are-surprisingly-reliant-on-the-twilight-zone/">dark zone</a> of the ocean.



The discovery arrives as global attention continues to focus on <a href="https://www.earth.com/news/surprise-study-some-scientists-call-for-halting-ocean-plastic-cleanup-efforts/">plastic waste</a>. 



Videos of snagged sea turtles and bottle-strewn beaches have already ignited public concern, but those images barely hint at what sinks far below the reach of sunlight.



Now evidence from Calypso Deep shows that even the <a href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/calypso" target="_blank" rel="noreferrer noopener">Mediterranean’s farthest recesses</a> are filling up.



<h2 class="wp-block-heading" id="h-calypso-deep-is-full-of-plastic-waste">Calypso Deep is full of plastic waste</h2>



The team used the submersible <a href="https://en.wikipedia.org/wiki/DSV_Limiting_Factor" target="_blank" rel="noreferrer noopener">Limiting Factor</a> to reach the bottom of a kidney-shaped trench roughly 12.4 miles long and 3.1 miles across. 



During a 43-minute trek near the seafloor of the Calypso Deep, cameras captured thousands of objects per square mile, mostly plastic waste discarded by humans.



A single straight-line pass of 2,130 feet was enough to confirm that human trash blankets large stretches of the basin. Most pieces were flexible plastics; glass, metal, and paper rounded out the list. 



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/03/marine-trash_Calypso-Deep-region_Mediterranean_study-map_UBarcelona_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/03/marine-trash_Calypso-Deep-region_Mediterranean_study-map_UBarcelona_1s.webp" alt="(A) General location of the Calypso Deep (box) in the Ionian Sea. PP: Peloponnese Peninsula. (B) Close up and general bathymetry of Calypso Deep (box) and surrounding area. For depth ranges, see color scale. (C) Detailed bathymetry of Calypso Deep with depth contours in meters. The position of the deepest point is indicated by the white dot, while the dive area is indicated by the red dot. Credit: University of Barcelona" class="wp-image-1976573"/></a><figcaption class="wp-element-caption">(A) General location of the Calypso Deep (box) in the Ionian Sea. PP: Peloponnese Peninsula. (B) Close up and general bathymetry of Calypso Deep (box) and surrounding area. For depth ranges, see color scale. (C) Detailed bathymetry of Calypso Deep with depth contours in meters. The position of the deepest point is indicated by the white dot, while the dive area is indicated by the red dot. Click image to enlarge. Credit: University of Barcelona</figcaption></figure>



Even without animals caught on camera, the piles raise alarms because deep-sea communities recover slowly from disturbance.



Calypso Deep lies about 37 miles west of the Peloponnese coast inside the Hellenic Trench, a zone of steep, stepped walls prone to earthquakes. 



<h2 class="wp-block-heading" id="h-plastic-waste-rides-currents">Plastic waste rides currents</h2>



Weak currents, usually under 0.8 inches per second and rarely reaching 7 inches per second, let debris settle instead of sweeping it away.



“It comes from various sources, both terrestrial and marine. It could have arrived by various routes, including long-distance transport by ocean currents or direct dumping,” explains <a href="https://web.ub.edu/en/web/directori/?accio=SEL&amp;id=v759w8s35bo5v72r&amp;lang=ca" target="_blank" rel="noreferrer noopener">Miquel Canals</a>, professor at the Department of Earth and Ocean Dynamics at the University of Barcelona.



“Some light waste, such as plastics, comes from the coast and escapes to Calypso Deep, just about 37 miles away. Certain plastics, <a href="https://www.earth.com/news/plastic-bag-bans-have-drastically-reduced-ocean-pollution/">like bags</a>, drift just above the seabed until they are partially or completely buried or break down into smaller fragments," Canals continued.



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/03/marine-trash_Calypso-Deep-region_Mediterranean_litter-photos_UBarcelona_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/03/marine-trash_Calypso-Deep-region_Mediterranean_litter-photos_UBarcelona_1s.webp" alt="Examples of identified litter items with category attribution per material type (cf. Table 2). (A) Plastic bag, J3. (B) Plastic heavy-duty sack, J36. (C) Plastic sheet, J67. (D) Plastic food container made of hard plastic, J225. (E) Plastic heavy-duty sack, J36. (F) Plastic bag, J3 (G) Cups and lids of hard plastic, J227. (H) Plastic rope &gt; 1 cm in diameter, J49. (I) Paper cartons/Tetrapak (non-milk), J151. (J) Metal drink can, J175. (K) Glass bottle. Note sediment shadow with side scouring downwards of the bottle J200. (L) Plastic drink bottle. Credit: University of Barcelona" class="wp-image-1976569"/></a><figcaption class="wp-element-caption">Examples of identified litter items with category attribution per material type. (A) Plastic bag, J3. (B) Plastic heavy-duty sack, J36. (C) Plastic sheet, J67. (D) Plastic food container made of hard plastic, J225. (E) Plastic heavy-duty sack, J36. (F) Plastic bag, J3 (G) Cups and lids of hard plastic, J227. (H) Plastic rope &gt; 1 cm in diameter, J49. (I) Paper cartons/Tetrapak (non-milk), J151. (J) Metal drink can, J175. (K) Glass bottle. Note sediment shadow with side scouring downwards of the bottle J200. (L) Plastic drink bottle. Click image to enlarge. Credit: University of Barcelona</figcaption></figure>



Rivers, wind, and ship traffic all feed the stream of refuse heading offshore. As algae and other organisms cling to floating polymers, the added weight turns buoyant scraps into sinking hazards. The trench’s closed shape then locks the pieces in place.



<h2 class="wp-block-heading" id="h-calypso-deep-as-a-plastic-graveyard">Calypso Deep as a plastic graveyard</h2>



Surface eddies often corral floating trash into the trench. When these eddies form over the Calypso Trench, some debris slowly falls to the bottom, aided by degradation and ballasting processes that increase its density. 



Surface currents can also carry debris northward from the Adriatic Sea through the Strait of Otranto and from waters off northwestern Greece. 



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/03/marine-trash_Calypso-Deep-region_Mediterranean_3D-model_UBarcelona_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/03/marine-trash_Calypso-Deep-region_Mediterranean_3D-model_UBarcelona_1s.webp" alt="(A) 3D model generated from a subset of video frames by reference to a litter item of known size shown in B. The white dashed line in A represents the camera frames along the Deep Submergence Vehicle (DSV) Limiting Factor moving path, whereas the red dashed line represents the frames counted between two items identified on the seabed. (B) Accumulation of litter items in the inner Calypso Deep with a litter item of known size (12 cm) used as a reference for 3D model generation. Credit: University of Barcelona" class="wp-image-1976567"/></a><figcaption class="wp-element-caption">(A) 3D model generated from a subset of video frames by reference to a litter item of known size shown in B. The white dashed line in A represents the camera frames along the Deep Submergence Vehicle (DSV) Limiting Factor moving path, whereas the red dashed line represents the frames counted between two items identified on the seabed. (B) Accumulation of litter items in the inner Calypso Deep with a litter item of known size (12 cm) used as a reference for 3D model generation. Click image to enlarge. Credit: University of Barcelona</figcaption></figure>



The same circular flows that drive marine life cycles are now channeling waste into permanent graveyards at the very bottom of Earth's deepest bodies of water.



<a href="https://web.ub.edu/ca/web/actualitat/w/a-sea-of-rubbish-ocean-floor-landfills-?" target="_blank" rel="noreferrer noopener">Earlier work in 2021</a> showed the Strait of Messina carrying the world’s heaviest load of undersea garbage, confirming that the Mediterranean is especially at risk.



“We have also found evidence of boats dumping bags of rubbish, indicated by piles of assorted waste followed by an almost straight furrow," said Canals, expressing his frustration.



That is why the bottom of the Calypso Deep is littered with humans' plastic waste, and also why the problem will do nothing but continue to worsen.



"Unfortunately, when it comes to the Mediterranean, it is fair to say that ‘not a single inch of it is clean.’”



<h2 class="wp-block-heading" id="h-where-do-we-go-from-here">Where do we go from here?</h2>



Unlike beaches and coastlines, the <a href="https://www.earth.com/news/99-percent-of-the-deep-ocean-floor-has-still-never-been-seen-by-humans/">ocean floor</a> remains largely out of sight, making it difficult to build social and political momentum for its conservation. 



Yet what settles at the bottom can influence marine life, food webs, fisheries, climate feedback loops, and even geological stability.



<a href="https://www.earth.com/news/the-mediterranean-nearly-lost-all-of-its-water-6-million-years-ago/">The Mediterranean</a> is an enclosed sea, surrounded by humanity, with intense maritime traffic and widespread fishing activity.



“Scientists, communicators, journalists, influencers - everyone with a platform - must work together. The problem is vast, even if it is not directly visible, and we cannot ignore it," Canals implored.



The trail of refuse from shorelines to Calypso Deep underlines a plain truth: plastics and other debris do not vanish once tossed aside. They ride currents, sink in stages, and ultimately collect in the planet’s most secluded hollows. 



The evidence provided by this research should galvanize global efforts - especially in the Mediterranean - to curb dumping, particularly of plastics, in line with the pending <a href="https://www.globalplasticlaws.org/un-global-plastics-treaty" target="_blank" rel="noreferrer noopener">UN Global Plastics Treaty</a>.



From the North Atlantic’s first recorded litter in 1975 to the record densities documented across the Mediterranean today, the pattern remains the same - human waste reaches everywhere water flows.



We must do more, we must do better, and we must do it now.



-----



Thanks to the leaders of this research team - Miquel Canals of the <a href="https://web.ub.edu/en/" target="_blank" rel="noreferrer noopener">University of Barcelona</a>, Georg Hanke of the European Commission’s <a href="https://commission.europa.eu/about/departments-and-executive-agencies/joint-research-centre_en" target="_blank" rel="noreferrer noopener">Joint Research Centre</a>, François Galgani of <a href="https://www.ifremer.fr/en" target="_blank" rel="noreferrer noopener">IFREMER</a>, and Victor Vescovo of <a href="https://caladanoceanic.com/" target="_blank" rel="noreferrer noopener">Caladan Oceanic</a>



The full study was published in the journal <a href="https://www.sciencedirect.com/science/article/pii/S0025326X25000852">Marine Pollution Bulletin</a>.



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Disturbing discovery made on the deepest parts of the seafloor: "Not a single inch of it is clean"

The Mediterranean has long been a crossroads of trade and...

In 2022, the underwater Hunga volcano exploded, blasting ash 37 miles into the sky - the largest volcanic plume ever captured by satellites. What followed offered researchers a rare chance to see how the ocean floor responds to sudden, massive disruption.



Months later, scientists from around the world headed to the location of the eruption on a research vessel.



Onboard the ship, undergraduate student Marcus Chaknova discovered something unexpected: thick layers of <a href="https://www.earth.com/news/fire-and-ice-volcanic-ash-plays-a-surprising-role-in-cloud-formation/">volcanic ash</a> coating the seafloor. The ash had suffocated deep-sea ecosystems that rely on fragile chemical exchanges to survive.



<h2 class="wp-block-heading" id="h-underwater-eruptions-usually-go-unseen">Underwater eruptions usually go unseen</h2>



“This was an extremely rare opportunity,” Chaknova explained. “Observing the mass movement of underwater sediment is something that hasn't been studied much.”



Now a graduate student in Earth Sciences at the <a href="https://www.uoregon.edu/" target="_blank" rel="noreferrer noopener">University of Oregon</a>, Chaknova led a study that analyzed what the underwater eruption left behind.



Working with Professor Thomas Giachetti and 16 other experts from around the world, he became the lead author on a study that looked at how volcanic ash travels - and what it does to life underwater.



“We had scientists from every single time zone you could think of,” Chaknova said. His project needed expertise from the fields of marine biology, geochemistry, and micropaleontology.



<h2 class="wp-block-heading" id="h-tracking-ash-from-the-volcano">Tracking ash from the volcano </h2>



The first step was to confirm that the underwater ash had indeed come from <a href="https://www.earth.com/news/new-clues-about-the-hunga-tonga-hunga-haapai-eruption/">Hunga</a>, located about 40 miles from <a href="https://www.bbc.com/news/world-asia-pacific-16197014" target="_blank" rel="noreferrer noopener">Tonga's</a> main island in the South Pacific. 



After an eruption, it can take weeks or even months for ash to fall through the water and settle on the ocean floor. As it drifts, wind and currents push it farther from the eruption site.



"One grain of sediment will take weeks or months to reach the bottom of the ocean. It's like a leaf falling from a tree. Because of the wind, it might end up somewhere completely different," Giachetti explained.



Back in the lab, Chaknova matched the ash samples to those found near the volcano. The grains were varied - some jagged and sharp, others rounded and smooth. 



In some places, the sediment was more than a meter thick. Most of it was made up of very fine particles, around the width of a human hair.



<h2 class="wp-block-heading" id="h-what-the-eruption-left-behind">What the eruption left behind</h2>



Chaknova discovered that much of the ash came from the volcano’s caldera walls and was carried away by fast-moving underwater flows - something like underwater avalanches.



Those flows were so powerful they damaged submarine cables and carved small canyons into the seafloor. The researchers even used the timing of power loss from those broken cables to calculate how fast the ash surged.



Using computer models, Chaknova plans to simulate how the ash moved and where it went. Giachetti said this research could change how scientists think about sediment movement in the oceans.



<h2 class="wp-block-heading" id="h-deep-sea-life-suffocated">Deep-sea life suffocated</h2>



The underwater <a href="https://www.earth.com/news/tonga-volcanic-eruption-had-a-much-more-devastating-impact-than-we-knew/">eruption</a> didn’t just leave a geological footprint; it disrupted entire ecosystems.



In the deep sea, where sunlight doesn’t reach, life depends on <a href="https://www.earth.com/news/how-can-deep-ocean-microbes-survive-without-sunlight/">chemosynthesis</a> - organisms use chemicals like methane or ammonia from hydrothermal vents, instead of sunlight, to produce energy.



Roughly 90% of marine life lives on the seafloor, according to the <a href="https://www.worldwildlife.org/" target="_blank" rel="noreferrer noopener">World Wide Fund for Nature</a>. After the eruption, much of that life was buried in thick sediment.



Some creatures like worms and anemones can survive brief burials, but this sudden wave of ash was too much. 



Many deep-sea species are suspension feeders. They grab tiny particles of food from the water and filter them through their gills.



"With all the displaced sediment, these organisms are only grabbing sediment," Chaknova continued. "That's going to clog their gills, it's going to clog their intestines, and that's going to have a dramatic effect on their ability to create energy."



<h2 class="wp-block-heading" id="h-fallout-from-the-underwater-eruption">Fallout from the underwater eruption </h2>



Chaknova’s early findings also show that ash made it all the way to Tonga’s coral reefs. At first, it caused a short-lived plankton bloom at the surface. 



But as the ash settled, it threatened coral ecosystems that support larger marine life. When coral suffers, everything above it in the food chain is affected.



On top of the environmental consequences, the eruption of this underwater volcano also affected livelihoods for Tonga residents.



Fishing is a way of life in Tonga. According to the <a href="https://www.worldbank.org/ext/en/home" target="_blank" rel="noreferrer noopener">World Bank</a>, about 82% of households rely on reef fishing in some way for income. Marine tourism accounts for more than 7% of Tonga’s GDP.



“Although this eruption occurred on the seafloor, there is a chain of both positive and negative effects,” Chaknova explained.



“The negative effects go farther than just losing power or Wi-Fi from submarine cables. This is some people’s livelihood. They need fish for food. Fishing is incredibly important for the economic and food security of Tonga.”



<h2 class="wp-block-heading" id="h-warning-for-deep-sea-mining">Warning for deep-sea mining</h2>



The study also has bigger implications. As the world turns toward clean energy, demand is growing for metals like copper and cobalt - many of which sit in potato-sized nodules beneath the ocean floor.



Private companies have approached small Pacific nations, including Tonga, with offers to mine these resources.



"The area where we collected the sediment is within the Kingdom of Tonga, and we found that they are very rich in minerals," Chaknova said. 



"A lot of companies are interested in collecting these minerals, and so this area that belongs to the Kingdom of Tonga will be up for bid, in coming years, for <a href="https://www.earth.com/news/deep-sea-mining-impacts-marine-life-for-decades/">deep-sea mining</a>."



While commercial mining hasn’t started yet, researchers are urging caution. The plumes of sediment created by mining could be just as harmful as those created by volcanic eruptions - clogging gills, burying habitats, and destroying fragile ecosystems.



Chaknova’s work provides some of the only real-world data we have on what that kind of disturbance could look like. 



The research gives scientists and policymakers a better understanding of what’s at stake - and what might be lost if we move forward without enough knowledge.



The full study was published in the journal <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GC011629" target="_blank" rel="noreferrer noopener">Geochemistry, Geophysics, Geosystems</a>.



Image Credit: <a href="https://www.noaa.gov" target="_blank" rel="noreferrer noopener">NOAA</a>



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Massive underwater eruption layered coral reefs with ash and suffocated marine life

In 2022, the underwater Hunga volcano exploded, blasting ash 37...

Suffering with autism spectrum disorder (ASD) or attention‑deficit/hyperactivity disorder (ADHD) as a child is difficult enough. Now, scientists tell us that those who suffer from ASD and ADHD also face higher vulnerability to common plastic pollutants.



A recent study found that their bodies detoxify <a href="https://www.niehs.nih.gov/health/topics/agents/sya-bpa" target="_blank" rel="noreferrer noopener">bisphenol A (BPA)</a> less efficiently than neurotypical peers, increasing the time their tissues are exposed to this chemical.



<a href="https://orcid.org/0000-0001-6148-2363" target="_blank" rel="noreferrer noopener">Dr. T. Peter Stein</a> of <a href="https://som.rowan.edu/" target="_blank" rel="noreferrer noopener">Rowan‑Virtua School</a> of Osteopathic Medicine led the study. Researchers measured urine glucuronidation, the liver process that adds a sugar molecule to BPA so it can be excreted.&nbsp;



Children with ASD and ADHD had reduced BPA detoxification efficiency compared to the control group. 



<a href="https://pubmed.ncbi.nlm.nih.gov/28770280/" target="_blank" rel="noreferrer noopener">BPA glucuronidation</a> was about 11% lower in the ASD group and 17% lower in those with ADHD, while differences in <a href="https://pmc.ncbi.nlm.nih.gov/articles/PMC5842715/" target="_blank" rel="noreferrer noopener">phthalate DEHP</a> detoxification followed the same trend but were not statistically significant.



Children with ASD and ADHD often have weaker detox systems, leaving them exposed to BPA in the body longer. 



That doesn’t guarantee illness from BPA but raises concern. Stein noted that this was the “first hard biochemical evidence” linking impaired BPA clearance to <a href="https://www.epa.gov/americaschildrenenvironment/health-neurodevelopmental-disorders" target="_blank" rel="noreferrer noopener">neurodevelopmental disorders</a>.



<h2 class="wp-block-heading" id="h-understanding-asd-and-adhd">Understanding ASD and ADHD</h2>



<a href="https://www.psychiatry.org/patients-families/autism/what-is-autism-spectrum-disorder" target="_blank" rel="noreferrer noopener">Individuals with ASD</a> often face challenges in social communication and exhibit restricted or repetitive behaviors. 



They might have difficulty interpreting social cues, maintaining eye contact, or adjusting to changes in routine. 



Sensory sensitivities - such as heightened responses to light, sound, or textures - are also common. ASD presents across a wide spectrum, so the degree and nature of symptoms can vary greatly from person to person.



In contrast, ADHD primarily involves persistent patterns of inattention, hyperactivity, and impulsivity that interfere with daily functioning. 



<a href="https://www.nimh.nih.gov/health/topics/attention-deficit-hyperactivity-disorder-adhd" target="_blank" rel="noreferrer noopener">People with ADHD</a> may struggle to focus, stay organized, or complete tasks, often acting without thinking or having trouble sitting still. 



While ADHD and ASD are separate diagnoses, they can co-occur, and some traits overlap - such as difficulties with executive function and emotional regulation.



<h2 class="wp-block-heading" id="h-bpa-exposure-in-children">BPA exposure in children</h2>



<a href="https://www.sciencedirect.com/topics/biochemistry-genetics-and-molecular-biology/glucuronidation" target="_blank" rel="noreferrer noopener">Glucuronidation</a> converts toxins like BPA into water‑soluble compounds that exit via urine. In this study, mass spectrometry tracked both bound and unbound BPA. 



A lower percentage of detoxification indicated less efficient excretion. Stein’s team confirmed the effect held true even when accounting for urine strength using creatinine levels.



Of twelve detox pathways tested, only BPA and DEHP stood out, suggesting a specific vulnerability rather than a broad weakness. 



Comparing results with metabolomic profiles, ASD and ADHD children showed unique patterns tied to BPA metabolism that controls did not share.



<h2 class="wp-block-heading" id="h-bpa-detox-with-adhd-and-asd">BPA detox with ADHD and ASD</h2>



BPA and DEHP act as <a href="https://www.niehs.nih.gov/health/topics/agents/endocrine" target="_blank" rel="noreferrer noopener">endocrine disruptors</a>, interfering with hormone signals. If detoxification is compromised, these chemicals linger longer in the body during critical phases of brain development. 



Though genetic vulnerability may play a role, this adds a measurable biological mechanism to the environmental risk picture.



Sterile in lab animals, DEHP affects neurodevelopment via epigenetic changes such as DNA methylation. A recent <a href="https://www.biorxiv.org/content/10.1101/2025.03.03.641339" target="_blank" rel="noreferrer noopener">analysis</a> of prenatal exposure in 847 Australian children linked DEHP levels to later ASD and ADHD symptoms. 



<a href="https://www.nature.com/scitable/topicpage/the-role-of-methylation-in-gene-expression-1070/" target="_blank" rel="noreferrer noopener">Methylation</a> in key genes and neural cell networks showed mediation effects between 21% and 80%. These epigenetic footprints reinforce the idea that plastics can affect neurodevelopment through non-genetic pathways.



<h2 class="wp-block-heading" id="h-evidence-of-environmental-links">Evidence of environmental links</h2>



This study builds on a large body of research connecting neurodevelopmental disorders to environmental pollutants. 



<a href="https://www.ncbi.nlm.nih.gov/books/NBK201995/" target="_blank" rel="noreferrer noopener">Epidemiological studies</a> have associated prenatal exposure to air pollution, flame retardants, and pesticides with elevated ASD and ADHD risk. 



The common thread in these findings is timing; exposure during pregnancy and early life seems to matter most.



Regulatory bodies have long debated what constitutes a “safe” exposure level for these chemicals. 



The <a href="https://www.fda.gov/food/food-packaging-other-substances-come-contact-food-information-consumers/bisphenol-bpa-use-food-contact-application" target="_blank" rel="noreferrer noopener">U.S. Food and Drug Administration</a> and the <a href="https://www.efsa.europa.eu/en/topics/topic/bisphenol" target="_blank" rel="noreferrer noopener">European Food Safety Authority</a> have reviewed BPA safety multiple times, but the growing evidence suggests current thresholds may not be low enough for sensitive populations, especially children with neurodevelopmental conditions.



<h2 class="wp-block-heading" id="h-what-does-all-of-this-mean">What does all of this mean?</h2>



This study doesn’t claim BPA or DEHP cause <a href="https://www.earth.com/news/children-with-autism-benefit-from-learning-multiple-languages/">autism</a> or ADHD. But it does show that children with these conditions often metabolize these chemicals less efficiently. 



Because BPA exposure is widespread (found in everything from food can liners to thermal paper) this raises questions about safety thresholds for all kids, not just those with ASD or <a href="https://www.earth.com/news/autism-and-adhd-disorders-directly-linked-amount-of-time-kids-spend-on-screens/">ADHD</a>.



Reducing reliance on BPA and phthalates in daily life (choosing glass or stainless steel containers, fresh food over cans, and avoiding receipts) can help limit exposure. 



Policy swings already reflect this concern: several countries are phasing out DEHP and tightening BPA regulations.



<h2 class="wp-block-heading" id="h-bpa-plastics-and-the-future">BPA, plastics, and the future</h2>



Future studies could investigate whether impaired detoxification is present from birth or develops over time. Longitudinal tracking of exposure, detox pathway function, and neurodevelopment could help answer this. 



Researchers also recommend examining genetic variants in detox enzymes, which might identify individuals most at risk.



On the epigenetic side, researchers are starting to connect prenatal chemical exposure to long‑term <a href="https://www.earth.com/news/is-your-dna-information-safe-scientists-warn-of-cyber-threats/">DNA</a> changes in specific brain regions, pointing to windows of vulnerability. 



That knowledge could eventually guide nurse‑led intervention, dietary changes, or policies to protect early brain development.



Children with ASD and ADHD are at a double vulnerability: genetic and developmental differences and a slower ability to clear everyday pollutants. 



While this study doesn’t offer advice on treatment or diagnosis, it certainly does ask parents and policymakers to seriously consider chemical exposure in early childhood and pregnancy as a significant factor in neurodevelopment.



The study is published in <a href="https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0289841" target="_blank" rel="noreferrer noopener">PLOS ONE</a>.



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Scientists link a common chemical in plastics to autism and ADHD in children

Suffering with autism spectrum disorder (ASD) or attention‑deficit/hyperactivity disorder (ADHD)...

Every year, humanity tallies its carbon emissions, but it rarely considers how the planet itself bears that burden. A new study flips the script by treating Earth as a stressed material rather than a passive scoreboard.



A team led by Matthias Jonas of the International Institute for Applied Systems Analysis (<a href="https://iiasa.ac.at/" target="_blank" rel="noreferrer noopener">IIASA</a>) converted gigatons of emissions into units engineers use to test bridges. 



The researchers borrowed tools from rheology, the science of how substances deform. Their <a href="https://www.sciencedirect.com/science/article/pii/S0048969725015633?via%3Dihub" target="_blank" rel="noreferrer noopener">numbers</a> suggest the carbon‑climate <a href="https://www.earth.com/news/ancient-societies-used-mixed-strategies-to-survive-climate-change/">system</a> is already flexing beyond its natural range.



<h2 class="wp-block-heading" id="h-earth-feels-stress-from-carbon-pollution">Earth feels stress from carbon pollution</h2>



Instead of tonnes, the team measured atmospheric pressure in <a href="https://www.noaa.gov/jetstream/atmosphere/air-pressure" target="_blank" rel="noreferrer noopener">pascals</a>, the metric engineers apply to describe a push on a square meter of surface. They model Earth as a <a href="https://www.sciencedirect.com/science/article/abs/pii/0019103567900061" target="_blank" rel="noreferrer noopener">Maxwell body</a>, a simple combination of elastic and viscous parts that stretch and flow when forced.



In that picture, accumulated emissions create stress while expansion of the air column and slower absorption of carbon by land and sea show up as strain. The ratio of the two reveals how quickly the global fabric is wearing thin.



“We wanted to see how the entire <a href="https://www.earth.com/news/tree-species-face-unprecedented-climate-shifts-across-their-ranges/">Earth</a> system stretches and strains under that burden,” explained Jonas. 



By calculating the change from 1850 to 2021, the team uncovered hidden thresholds invisible in the usual mass‑balance charts.



<h2 class="wp-block-heading" id="h-even-low-stress-reshapes-earth">Even low stress reshapes Earth</h2>



The calculations show that by 2021 humanity was injecting between 12.8 and 15.5 pascals per year of extra energy per unit volume, a value Jonas calls <a href="https://www.sciencedirect.com/science/article/pii/S0048969725015633" target="_blank" rel="noreferrer noopener">stress power</a>. 



Spread over every cubic yard of air, water, and soil, that push compares to the force of a light breeze yet persists nonstop.



Such steady pressure, tiny at any single point, becomes enormous once multiplied across the oceans and atmosphere. Earth’s natural buffers can accommodate only so much before their response time slows.



Jonas compares the phenomenon to leaving a garden hose on low all night; the gentle trickle still floods the yard by morning. In the same way, low but unrelenting stress alters <a href="https://www.earth.com/news/plant-roots-could-be-key-to-fighting-climate-change/">atmospheric</a> volume and ocean chemistry alike.



<h2 class="wp-block-heading" id="h-weakening-of-earth-s-natural-systems">Weakening of Earth’s natural systems </h2>



The study charts delay time, the lag between a pulse of emissions and the planet’s structural response. That metric peaked in the early 1900s, revealing that land and ocean sinks began to lose agility far sooner than expected.



For their mid‑range <a href="https://bg.copernicus.org/articles/21/3903/2024/" target="_blank" rel="noreferrer noopener">estimate</a>, the tipping year is 1932 - almost two decades after the Model T rolled off assembly lines. 



After that point, the land‑ocean system no longer recovered in step with stress, it merely absorbed the hit and carried scars forward.



“Even if we hit our emissions targets, the weakening of Earth’s natural systems could still leave us facing major disruptions sooner than expected,” noted Jonas.



<h2 class="wp-block-heading" id="h-growing-strain-makes-climate-action-urgent">Growing strain makes climate action urgent</h2>



Carbon dioxide output topped 40.9 billion tons in <a href="https://www.globalcarbonproject.org/carbonbudget/22/files/GCP_CarbonBudget_2022.pdf" target="_blank" rel="noreferrer noopener">2022</a>, a record that nudged stress power up another notch. As emissions grow roughly 0.5 percent per year, the energy injected into the planet’s framework rises even if temperature targets appear on paper.



Delay also magnifies costs, because infrastructure built for a cooler baseline may degrade faster under compounded thermal and mechanical strain. Counting only temperature ignores those hidden maintenance bills.



The <a href="https://www.ipcc.ch/2022/04/04/ipcc-ar6-wgiii-pressrelease/">Intergovernmental Panel on Climate Change</a> warns that to keep global warming close to 2.7 °F, greenhouse gas emissions must peak before 2025 and decline by 43 percent by 2030.



Jonas’ numbers imply that every year of delay increases baseline stress, meaning future cuts must be steeper just to arrest further strain on the planet.



<h2 class="wp-block-heading" id="h-natural-sinks-are-losing-their-strength">Natural sinks are losing their strength</h2>



Natural <a href="https://www.climate.gov/news-features/feed/landmark-study-indicates-weakening-ocean-carbon-sink" target="_blank" rel="noreferrer noopener">sinks</a> still sponge up about half of human CO₂, but their efficiency is waning, especially in the Southern Ocean and tropical forests. In 2023, extreme heat left land vegetation absorbing almost no net carbon according to global monitoring.



<a href="https://www.earth.com/news/more-than-3500-animal-species-are-directly-threatened-by-climate-change/">Ocean</a> uptake has slowed by as much as four percent in the past decade, while land sink efficiency has swung in and out of negative territory during major droughts. 



The strain analysis corroborates those field observations by showing the ocean side of the equation weakening faster than the terrestrial side.



In the model, the damping constant linked to ocean uptake falls 30 percent between 1850 and today, a sign that heat and acidity may already be reshaping marine chemistry. The land constant declines, too, but at a gentler pace.



<h2 class="wp-block-heading" id="h-past-stress-and-future-climate-risks">Past stress and future climate risks</h2>



Because stress power grows with cumulative emissions, simply hitting net‑zero late in the century will not reset the clock. The strain frozen into the system can persist for decades, lengthening the time before sinks regain strength.



Carbon‑removal schemes therefore act less like an optional extra and more like a structural repair kit, needed to relieve pressure already baked in. Yet large‑scale removal is not ready at the speed or cost required.



If nations wait for the alarm of higher temperatures alone, they may overlook mechanical fatigue building under the surface. Jonas likens the risk to pushing a steel beam until microscopic cracks race ahead of visible bending.



<h2 class="wp-block-heading" id="h-earth-stress-and-hidden-damage">Earth stress and hidden damage</h2>



The authors hope to weave their rheology framework into coupled climate models so that fatigue dynamics appear alongside temperature and precipitation outputs. 



The goal is to identify regions where local shocks, from dieback to ice‑shelf loss, propagate globally.



The researchers also plan to refine sink parameters with satellite and autonomous buoy data, reducing uncertainty in the damping constants. 



Better bounds will reveal whether the 1930s shift was a global threshold or the first of several steps.



Ultimately, the approach offers another yardstick for progress: a direct readout of how quickly Earth relaxes once stress is reduced. Watching that number fall may prove as motivating as any temperature curve.



The study is published in the journal <a href="https://www.sciencedirect.com/science/article/pii/S0048969725015633?via%3Dihub" target="_blank" rel="noreferrer noopener">Science of the Total Environment</a>.



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Earth faces hidden mechanical stress from carbon emissions

Every year, humanity tallies its carbon emissions, but it rarely...

Climate change is rapidly melting glaciers. While rising seas and disappearing ice dominate the headlines, something more ominous may be stirring beneath the surface. 



Dormant volcanoes - sealed under ice for millennia - could soon awaken. And when they do, the eruptions may be anything but ordinary: they could strike suddenly and with explosive force.



This isn’t just a theory. Scientists studied volcanoes in Chile’s Andes mountains. The research showed that melting glaciers can spark volcanic activity. 



Antarctica hides hundreds of <a href="https://www.earth.com/news/earths-orbit-may-trigger-massive-volcanic-eruptions/">volcanoes</a> under its ice. If this pattern holds, those volcanoes may start to stir too. The warning is clear. As glaciers vanish, the ground may soon roar.



<h2 class="wp-block-heading" id="h-volcanoes-responding-to-melting-glaciers">Volcanoes responding to melting glaciers </h2>



Scientists in Iceland began investigating the connection between melting glaciers and increased volcanic activity as early as the 1970s.



This latest study shows that volcanoes in large continental regions may respond in the same way. The findings could reshape how we predict volcanic <a href="https://www.earth.com/news/ancient-mantle-plume-created-a-60-million-year-volcanic-trail-from-iceland-to-ireland/">eruptions</a>.



Beyond Chile, volcanoes in North America, New Zealand, and Russia may also face this hidden threat.



Many volcanoes once thought harmless may no longer stay quiet. As glaciers melt, the risk rises. Scientists are beginning to ask what else could be lying in wait.



<h2 class="wp-block-heading" id="h-how-ice-suppressed-volcanoes">How ice suppressed volcanoes</h2>



Researchers from the <a href="https://www.wisc.edu" target="_blank" rel="noreferrer noopener">University of Wisconsin-Madison</a> led this work. They joined forces with scientists from other U.S. universities. The team focused on six volcanoes in southern Chile.



Among these volcanoes was the now quiet Mocho-Choshuenco. Long ago, it sat beneath the thick Patagonian Ice Sheet.



The scientists collected rocks and studied them closely. They used argon dating to find the exact age of past <a href="https://www.earth.com/news/fresh-lava-from-deep-earth-mantle-pulses-burst-onto-land-where-new-ocean-is-forming/">eruptions</a>. 



The researchers also examined crystals in the rocks to see what had happened beneath the surface.



The story was clear: when glaciers were thick, they pressed down hard on the volcanoes. That pressure locked magma underground.



<h2 class="wp-block-heading" id="h-melting-glaciers-unlock-eruptions">Melting glaciers unlock eruptions</h2>



During the last ice age, from about 26,000 to 18,000 years ago, glaciers covered the land. They acted like a giant lid, holding back eruptions.



But no glacier lasts forever. As the ice melted quickly near the end of the ice age, everything changed.



The crust beneath the volcanoes began to relax. Magma, once trapped, found space to expand. Gases inside the magma bubbled and grew. Soon, pressure built up too much. The volcanoes erupted in dramatic fashion.



These eruptions shaped the land and left scars that remain today. The cause was simple. The melting glaciers had removed the pressure that kept the magma in check.



<h2 class="wp-block-heading" id="h-glacier-melt-raises-volcano-risks">Glacier melt raises volcano risks</h2>



Pablo Moreno-Yaeger from the University of Wisconsin-Madison presented this study. His warning was sharp and direct.



“Glaciers tend to suppress the volume of eruptions from the volcanoes beneath them. But as glaciers retreat due to climate change, our findings suggest these <a href="https://www.earth.com/news/scientists-discover-why-stealthy-volcanoes-erupt-without-warning/">volcanoes</a> go on to erupt more frequently and more explosively," said Moreno-Yaeger.



"The key requirement for increased explosivity is initially having a very thick glacial coverage over a magma chamber, and the trigger point is when these glaciers start to retreat, releasing pressure - which is currently happening in places like Antarctica.”



Moreno-Yaeger pointed out that this risk is not limited to Iceland. Volcanoes under thick ice in Antarctica and other parts of the world could behave the same way.



<h2 class="wp-block-heading" id="h-magma-shifts-slowly-but-danger-grows">Magma shifts slowly but danger grows</h2>



Volcanoes do not react overnight. Even as ice melts fast, magma builds pressure slowly. These changes often take centuries.



However, in geological terms, this is still fast. Scientists have enough time to watch carefully. They can look for signs like moving magma or shifting gases. With close monitoring, future eruptions might be predicted before disaster strikes.



But the clock has already started ticking. Glaciers are melting now, and some volcanoes are likely already changing deep below the surface.



<h2 class="wp-block-heading" id="h-eruptions-also-change-earth-s-climate">Eruptions also change Earth’s climate</h2>



Volcanic eruptions do more than shake the ground. They can also change the planet’s temperature.



When volcanoes erupt, they send aerosols into the atmosphere. These tiny particles block sunlight and cool Earth for a short time. After Mount Pinatubo erupted in 1991, the planet cooled by about 0.5 degrees Celsius.



Cooling the planet might sound like a good thing, but it does not last. If several volcanoes erupt within a short time, the story flips again.



<h2 class="wp-block-heading" id="h-glaciers-and-volcanoes-may-fuel-a-loop">Glaciers and volcanoes may fuel a loop</h2>



“Over time the cumulative effect of multiple eruptions can contribute to long-term global warming because of a buildup of greenhouse gases,” said Moreno-Yaeger. 



“This creates a positive feedback loop, where melting glaciers trigger eruptions, and the eruptions in turn could contribute to further warming and melting.”



This loop works like a trap. Melting glaciers cause eruptions, which release greenhouse gases. Those gases warm the planet more, causing more glaciers to melt.



This cycle could spiral out of control if left unchecked. This is no longer just about melting ice. It is about a whole chain of disasters feeding each other.



The study received funding from the <a href="https://www.nsf.gov" target="_blank" rel="noreferrer noopener">National Science Foundation</a>. 



The team presented their research at the <a href="https://conf.goldschmidt.info/goldschmidt/2025/meetingapp.cgi" target="_blank" rel="noreferrer noopener">Goldschmidt Conference</a> in Prague on July 8, 2025.



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Melting glaciers may awaken sleeping volcanoes

Climate change is rapidly melting glaciers. While rising seas and...

Ships have long connected the world’s economies. They bring goods and people across seas and rivers. But their impact on the environment goes beyond the fuel they burn. 



A new study from <a href="https://www.chalmers.se/en/" target="_blank" rel="noreferrer noopener">Chalmers University of Technology</a> has uncovered a surprising threat linked to ship movement itself. 



This research reveals how ships stir up methane emissions, a potent <a href="https://www.earth.com/news/cutting-super-pollutants-could-quickly-cool-the-planet/">greenhouse gas</a>, simply by traveling through shallow waters.



The findings are both alarming and unexpected. They show that methane emissions in busy shipping lanes are twenty times higher than in undisturbed waters nearby. This means that global methane estimates may have been far too low for many years.



Methane has always been a cause for concern among climate scientists. It traps heat far more effectively than carbon dioxide. Despite its powerful effects, methane emissions from ship movements have been mostly ignored.



<h2 class="wp-block-heading" id="h-methane-escapes-as-ships-pass">Methane escapes as ships pass</h2>



Amanda Nylund, a researcher at <a href="https://www.chalmers.se/en/" target="_blank" rel="noreferrer noopener">Chalmers University of Technology</a> and the Swedish Meteorological and Hydrological Institute (<a href="https://www.smhi.se/en" target="_blank" rel="noreferrer noopener">SMHI</a>), explains how these <a href="https://www.earth.com/news/dairy-farms-can-join-the-climate-fight-by-trapping-methane/">emissions</a> occur.



"Our measurements show that ship passages trigger clear pulses of high methane fluxes from the water to the atmosphere," she said. 



"This is caused by pressure changes and mixing of the water mass. Even if the pulses are short, the total amount during a day is significant."



This new finding changes how we think about emissions from ships. Previously, the main concern involved ships that run on liquefied natural gas, or LNG.



In this case, however, the methane has no connection to the fuel used by ships. Instead, it comes from the seafloor itself, disturbed by ship traffic. This means that all ships, regardless of their fuel, can cause these emissions.



<h2 class="wp-block-heading" id="h-shallow-seas-emit-more-gas">Shallow seas emit more gas</h2>



The study focused on shallow marine environments rich in organic matter. These areas have oxygen-free sediments, ideal for producing <a href="https://www.earth.com/news/cutting-methane-emissions-could-quickly-slow-global-warming/">methane</a>.



Methane in such regions builds up naturally within the seafloor. In many cases, it slowly escapes in small bubbles or leaks through cracks into the water above.



But when a ship passes through, the story changes. The passing vessel causes sudden pressure changes at the seafloor. This triggers methane to burst out from the sediments in large amounts.



The effect grows stronger when combined with the mixing action from the ship’s wake. This mixing allows methane to travel more quickly from the water to the surface, where it escapes into the air.



As ships pass repeatedly throughout the day, the methane pulses accumulate into significant emissions.



<h2 class="wp-block-heading" id="h-methane-link-found-by-chance">Methane link found by chance</h2>



The research team stumbled upon this phenomenon by accident. They were conducting unrelated measurements in Neva Bay, part of the Baltic Sea, when they noticed strange methane spikes.



This accidental finding became the starting point for a new line of inquiry. Their work has now been published in Nature Communications Earth &amp; Environment.



Johan Mellqvist is a professor of Optical Remote Sensing at Chalmers. His group made the unexpected discovery that forms the basis for the new results.



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/07/ships_methane-leaks-discovery_illustration_credit-Chalmers-University_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/07/ships_methane-leaks-discovery_illustration_credit-Chalmers-University_1s.webp" alt="A Chalmers-led study shows that ship passages can trigger clear pulses of high methane fluxes from the water to the atmosphere. Credit: Chalmers University of Technology and Amanda Nylund" class="wp-image-1976785"/></a><figcaption class="wp-element-caption">A Chalmers-led study shows that ship passages can trigger clear pulses of high methane fluxes from the water to the atmosphere. Click image to enlarge. Credit: Chalmers University of Technology and Amanda Nylund</figcaption></figure>



"The discovery of the hitherto unknown impact of ships is important for improving global estimates of <a href="https://www.earth.com/news/top-10-global-methane-emissions-hotspots-spotted-by-satellites/">methane</a> emissions, not least considering that nine of the world's ten largest ports are located in waters with similar conditions as Neva Bay," he said. 



This finding holds global significance because many of the world's busiest ports are in shallow waters similar to Neva Bay.



<h2 class="wp-block-heading" id="h-smaller-ships-bigger-leaks">Smaller ships, bigger leaks</h2>



The study analyzed emissions from different ship types. Large cruise ships and container ships produced the highest and most frequent methane releases.



Surprisingly, smaller ropax vessels, which transport both passengers and cargo, also caused major emissions. These vessels, though smaller than cruise or container ships, had high methane release rates.



Interestingly, larger bulk carriers showed lower methane emissions than expected. This challenges the assumption that bigger ships always cause greater emissions.



Researchers believe that ship design may influence these results.



"A possible explanation for the high emissions of ropax vessels is that they have double propellers," says Rickard Bensow, Professor of Hydrodynamics, Chalmers, and responsible for the study's modeling of ship traffic.



<h2 class="wp-block-heading" id="h-big-ports-hide-methane-risks">Big ports hide methane risks</h2>



The findings suggest a need for urgent changes in how methane emissions of ships are monitored and reported. The authors stress that more attention must be given to coastal areas where natural and human activities interact.



The researchers now plan to expand their investigation to include large ports in river deltas - these locations likely face similar methane risks.



"The next step is to estimate how large these effects can be globally," said Ida-Maja Hassellöv, a professor of Maritime Environmental Science. She will lead the follow-up project that will start this autumn.



"Major ports in China, Singapore, and South Korea, as well as European ports such as Rotterdam, Antwerp, and river systems in Germany, have similar conditions to the Neva Bay," she said. "It is very likely that we underestimate methane emissions there as well." 



<h2 class="wp-block-heading" id="h-shipping-rules-could-tighten">Shipping rules could tighten</h2>



This research could reshape how the world calculates methane emissions. Current models may leave out critical methane sources hidden beneath the waves.



If similar emissions are found in other shallow ports worldwide, it may prompt major changes in global climate strategies. It could also affect shipping regulations, urging stronger controls on ship routes and port operations in sensitive areas.



This surprising discovery proves that hidden climate risks can emerge from unexpected places. Ships do not just carry cargo and passengers - they may also be pushing greenhouse gases into the air, one wave at a time.



The study is published in the journal <a href="https://www.nature.com/articles/s43247-025-02344-8" target="_blank" rel="noreferrer noopener">Nature Communications Earth &amp; Environment</a>.



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Ships moving in shallow waters cause huge hidden methane leaks

Ships have long connected the world’s economies. They bring goods...

It started with a single ice shelf photo. On November 28, 1966, an American military plane flew over the Antarctic Peninsula, just south of Chile. A photographer onboard - likely from the U.S. Navy - snapped an image of the <a href="https://www.earth.com/wp-content/uploads/2025/07/wordie-ice-shelf_old-photos_collapse_sea-level-rise_Credit-Mads-Domgaard_1m.jpg" target="_blank" rel="noreferrer noopener">Wordie Ice Shelf</a>.



At the time, no one knew that the ice shelf he photographed would almost completely collapse just 30 years later.



That image became the first in a long series of data points that are now helping researchers understand how and why ice shelves collapse - and what it could mean for our future.



<h2 class="wp-block-heading" id="h-from-archives-to-data-that-matters">From archives to data that matters</h2>



Scientists at the <a href="https://www.ku.dk/en">University of Copenhagen</a> used that photo, along with hundreds more taken between 1966 and 1969, to reconstruct a detailed, time-lapsed view of the early stages of the Wordie Ice Shelf’s collapse. 



The study merges the historical aerial photos with modern satellite data to track the long-term changes in the ice shelf's size, shape, and behavior.



For the first time, this research documents the collapse of an ice shelf not as a sudden event, but as a long, <a href="https://www.earth.com/news/giant-icebergs-are-not-the-main-threat-to-antarcticas-stability/">evolving process</a>. That shift in understanding matters.



“We have identified several signs of incipient ice shelf collapse that we expect will be observed in other ice shelves," explained postdoc <a href="https://scholar.google.com/citations?user=jhKkns4AAAAJ&amp;hl=da" target="_blank" rel="noreferrer noopener">Mads Dømgaard</a> from the Department of Geosciences and Natural Resource Management, who is lead author of the study.



"Perhaps more importantly, the dataset has given us a multitude of pinning points that can reveal how far advanced a collapse is. It's a completely new tool that we can use to do reality checks on ice shelves that are at risk of collapsing or already in the process of collapsing.”



<h2 class="wp-block-heading" id="h-ripple-effects-of-the-ice-shelf-collapse">Ripple effects of the ice shelf collapse</h2>



The collapse of Wordie was relatively small in scale. It led to only millimeters of <a href="https://www.earth.com/news/coastal-cities-will-spend-over-3-trillion-dollars-damages-from-sea-level-rise/">sea level rise</a>. But it acted like a cork being popped. Without the support of the ice shelf, glaciers behind it were free to slide into the sea more easily.



That’s a major problem with larger ice shelves. Ronne and Ross - the two largest in <a href="https://www.earth.com/news/antarcticas-melting-ice-shelves-threaten-global-sea-levels/">Antarctica</a> - hold back glaciers with enough ice to raise global sea levels by up to five meters.



While Antarctica may feel far away, its <a href="https://www.earth.com/news/melting-ice-in-antarctica-could-wake-sleeping-volcanoes/">melting ice</a> doesn’t just affect the Southern Hemisphere. Because of how gravity influences ocean distribution, ice loss in Antarctica leads to sea level rise in the Northern Hemisphere - including in places like Denmark.



<h2 class="wp-block-heading" id="h-what-really-caused-the-collapse">What really caused the collapse?</h2>



To analyze the old images, researchers used a method called structure-from-motion photogrammetry. It stitches together overlapping photos to create detailed 3D models of the ice shelf’s surface, thickness, and movement over time.



They discovered something unexpected. Previous assumptions pointed to warmer air and the formation of <a href="https://www.earth.com/news/meltwater-lakes-ice-shelves-bend/">meltwater lakes</a> as the main culprits behind Wordie's collapse. But the evidence from the current study tells a different story.



“Our findings show that the primary driver of Wordie's collapse is <a href="https://www.earth.com/news/pacific-ocean-temperatures-highest-in-650-years-greatly-harming-coral-reefs/">rising sea temperatures</a>, which have generated the melting beneath the floating ice shelf,” said Dømgaard.



In other words, it’s not what’s happening on top of the ice that matters most - it’s what’s happening below.



<h2 class="wp-block-heading" id="h-surprising-pace-of-ice-shelf-collapse">Surprising pace of ice shelf collapse</h2>



The study also challenges the common assumption that ice shelf collapses <a href="https://www.earth.com/news/ice-sheet-fracture-sets-a-speed-record-in-antarctica/">happen quickly</a>.



"The tentative conclusion from our findings is that ice shelf collapse may be slower than we thought," said <a href="https://scholar.google.com/citations?user=bCPIXH8AAAAJ&amp;hl=en" target="_blank" rel="noreferrer noopener">Anders Anker Bjørk</a>, assistant professor at the Department of Geosciences and Natural Resource Management.



"This means that the risk of a very rapid development of violent sea level rise from melting in Antarctica is slightly lower, based on knowledge from studies like this one."



That sounds like good news, but it comes with a catch. According to Bjørk, the data shows a collapse process that is even more protracted than previously assumed.



"And this longer process will make it harder to reverse the trend once it has started. This is an unambiguous signal to prioritise halting greenhouse gas emissions now, rather than sometime in the future," noted Bjørk.



The findings are a reminder that even slow-moving changes can carry enormous consequences. Understanding how ice shelves collapse gives us a chance to act - not later, but now - while we still have the choice to shape what happens next.



-----



Featured image credit: The Wordie Ice Shelf has undergone a total collapse since <a href="https://www.earth.com/wp-content/uploads/2025/07/wordie-ice-shelf_old-photos_collapse_sea-level-rise_Credit-Mads-Domgaard_1m.jpg">first photographed November 1966</a>. Credit: Mads Dømgaard



The full study was published in the journal <a href="https://www.nature.com/articles/s41467-025-59293-1" target="_blank" rel="noreferrer noopener">Nature Communications</a>.



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Old photos help scientists predict ice shelf collapse and sea level rise

It started with a single ice shelf photo. On November...

A new review pulls together decades of research on tire wear particles (TWPs) - the tiny bits that break off tires and get washed away. It turns out wind and rain can sweep huge amounts of these fragments off highways and straight into nearby streams and ponds.



In heavy-traffic zones, TWPs can make up 50 to 90 percent of all <a href="https://www.earth.com/news/car-tires-are-a-big-source-of-microplastics-pollution-but-what-about-mountain-bikes/">microplastics</a> that run off roads during rainfall. When soils are included, nearly 45 percent of microplastics found on land or in freshwater environments can be traced to tire abrasion.



Concentrations recorded in field samples vary wildly - from just 0.00001 mg per liter to an astonishing 10,000 mg per liter. These extremes highlight the presence of localized hotspots.



<h2 class="wp-block-heading" id="h-tires-release-a-toxic-mix">Tires release a toxic mix</h2>



When it comes to tires, speed and grip matter more than ecological impact. The review lists 2,456 different chemicals in tire rubber - and lab tests show that at least 144 of them can leach out.



Prominent among them are hexamethoxymethyl-melamine, dibutyl phthalate, and the antioxidant 6-PPD, which transforms into its highly toxic quinone derivative. 



Manufacturers embed <a href="https://www.earth.com/news/heavy-metal-pollution-threatens-marine-life-and-human-health/">heavy metals</a> - like zinc, manganese, cadmium, and lead - into the polymer matrix as vulcanizing agents and fillers.



Hans-Peter Grossart of the <a href="https://www.igb-berlin.de/en">Leibniz Institute of Freshwater Ecology and Inland Fisheries</a> is a co-author of the study.



“During the leaching process, tire abrasion releases more chemicals than thermoplastics such as PE. We also assume that more substances are leached out than we already know,” he said.



<h2 class="wp-block-heading" id="h-tire-dust-disrupts-ecosystems">Tire dust disrupts ecosystems</h2>



Laboratory exposure studies reveal that tire particles and their leachates prompt oxidative stress, DNA damage, immune suppression, and developmental defects in a wide array of aquatic organisms. Affected species show reduced feeding, stunted growth, and lower reproductive success.



Scaling up, the review links these individual ailments to shifts in community composition, which in turn disrupt nutrient cycles and diminish biodiversity. 



Changes in microbial and algal communities could also disrupt how carbon and nitrogen cycle through the environment - processes that are key to <a href="https://www.earth.com/news/it-took-200-million-years-for-earth-to-get-its-oxygen/">oxygen</a> production and clean water.



<h2 class="wp-block-heading" id="h-warming-worsens-toxic-effects">Warming worsens toxic effects</h2>



Rising temperatures and freshwater acidification are likely to make the ecological impact of tire particles even worse.



Higher temperatures accelerate chemical reactions, increasing the rate at which additives leach from particles, while lower pH can heighten metal solubility and bioavailability.



Grossart cautioned that these environmental shifts will likely exacerbate the effects of tire wear and its leaching by altering its toxicity and its interactive effects on microbial activity, <a href="https://www.earth.com/news/climate-change-is-draining-nutrients-from-the-oceans-surface/">nutrient</a> cycling, and the resilience of ecosystems.



<h2 class="wp-block-heading" id="h-tire-dust-sinks-near-roads">Tire dust sinks near roads</h2>



Studies indicate that wind can spread tire wear particles over a wide area. However, most fragments fall near their release points and accumulate along road verges, drainage ditches, and sediment beds.



The researchers estimate that only about two percent of tire particles carried by rivers reach the sea. That means capturing them earlier - at the watershed level - could have a big impact.



The review calls for physical barriers and improved drainage systems to trap particles before they reach natural waterways.



<h2 class="wp-block-heading" id="h-drivers-play-a-role-too">Drivers play a role too</h2>



The researchers suggest that tire manufacturers should explore alternative formulations with fewer hazardous additives.



They also urge urban planners to improve the separation between road surfaces and water bodies. Yet drivers also hold part of the solution.



“Effective reduction strategies involve the development of alternative tire manufacturers, and a better demarcation of roads and wastewater from natural areas," Grossart said. "Ultimately, everyone can make their own contribution with a prudent driving style.” 



<h2 class="wp-block-heading" id="h-calls-for-tire-pollution-limits">Calls for tire pollution limits</h2>



Despite the mounting evidence, major knowledge gaps persist. Standardized field protocols are rare, hindering cross-study comparisons, and most of the thousands of tire-derived chemicals remain untested for toxicity.



The review urges cross-disciplinary collaborations to develop real-world monitoring networks and predictive models. These tools would help regulators set science-based limits for TWP emissions.



The review highlights TWPs as a major but overlooked source of freshwater pollution, based on volume and chemical complexity.



Without concerted action - from product redesign to traffic management - the dust generated by every mile driven will continue to seep into <a href="https://www.earth.com/news/major-plastic-pollution-lurks-beneath-the-surface-of-rivers/">rivers</a> and lakes, carrying with it a suite of toxins that ecosystems must somehow absorb.



The review is published in the <a href="https://www.sciencedirect.com/science/article/abs/pii/S0301479725020353?via%3Dihub">Journal of Environmental Management</a>. 



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Tire particles flood freshwater with toxic microplastics

A new review pulls together decades of research on tire...

Coral reefs are in trouble. As oceans warm and environments shift, the vibrant ecosystems built by corals are turning pale and dying off. 



While scientists have known for years that coral bleaching is linked to the loss of symbiotic algae, they’ve never been able to watch the process unfold at the cellular level in realtime - until now.



<h2 class="wp-block-heading" id="h-underwater-microscope-for-studying-coral">Underwater microscope for studying coral</h2>



Researchers at the <a href="https://scripps.ucsd.edu/">Scripps Institution of Oceanography at UC San Diego</a> have created a handheld underwater microscope. The device makes it possible to study coral photosynthesis right where it happens - in the ocean, inside living coral tissue - without causing any damage.



The team named the device the Benthic Underwater Microscope imaging PAM - BUMP, for short.



The Jaffe Lab for Underwater Imaging at Scripps Oceanography built the microscope with support from the U.S. National Science Foundation.



The tool combines imaging with a light-based technique known as pulse amplitude modulated (PAM) fluorometry to measure how efficiently tiny algae inside corals are <a href="https://www.earth.com/news/the-fate-of-coral-reefs-lies-in-the-hands-of-their-tiny-inhabitants/">photosynthesizing</a>.



<h2 class="wp-block-heading" id="h-coral-depends-on-glowing-algae">Coral depends on glowing algae</h2>



The algae, called <a href="https://www.earth.com/news/symbiosis-will-help-some-corals-survive-in-a-warming-world/">symbionts</a>, are essential for coral survival. They live within coral tissue and convert sunlight, water, and carbon dioxide into sugars and oxygen.



The coral, in turn, uses that energy to grow and build reefs. But when stressed by warming seas or pollution, corals eject these algae. Without them, corals appear white and slowly starve - known as the bleaching effect.



The BUMP microscope makes it possible to monitor this relationship in real-time and in natural environments - something that couldn’t be done before.



<h2 class="wp-block-heading" id="h-a-huge-technological-leap">A huge technological leap</h2>



“This microscope is a huge technological leap in the field of coral health assessment,” said study lead author Or Ben-Zvi, a postdoctoral researcher at Scripps Oceanography. 



“Coral reefs are rapidly declining, losing their photosynthetic symbiotic algae in the process known as <a href="https://www.earth.com/news/the-worlds-largest-coral-bleaching-event-is-now-underway/">coral bleaching</a>."



"We now have a tool that allows us to examine these microalgae within the coral tissue, noninvasively and in their natural environment.”



The microscope is small enough to fit in a carry-on suitcase. It’s light enough for a diver to bring to the seafloor without a ship’s help. 



Controlled with a touchscreen and powered by a battery pack, the microscope uses focused LED lights and high-magnification lenses to capture vivid images and videos. It also creates detailed 3D scans and maps photosynthesis in high resolution.



<h2 class="wp-block-heading" id="h-microscope-reveals-corals-inner-glow">Microscope reveals corals’ inner glow</h2>



At just 10 micrometers wide - one-tenth the width of a human hair - coral symbionts are invisible to the naked eye. But when corals are viewed under the microscope, the <a href="https://www.earth.com/news/marine-algae-genes-chlorophyll-boost-crop-yields-land-plants/">algae</a> glow red due to chlorophyll, the pigment that powers <a href="https://www.earth.com/news/key-to-life-on-earth-photosynthesis-begins-on-the-quantum-level-with-a-single-photon/">photosynthesis</a>. 



PAM technology measures this glow to calculate how efficiently the algae are converting light into energy. Other glowing areas, like cyan and green patches, come from fluorescent proteins that the coral produces, often around its mouth and tentacles. 



The images help researchers “see” coral health without touching or harming them. "We get a lot of information about their health without the need to interrupt nature,” said Ben-Zvi. 



“It's similar to a nurse who takes your pulse and tells you how well you're doing. We're checking the coral's pulse without giving them a shot or doing an intrusive procedure on them.”



<h2 class="wp-block-heading" id="h-observing-corals-at-unseen-scales">Observing corals at unseen scales</h2>



Ben-Zvi and her colleagues tested the microscope at coral hotspots around the world - including Hawaii, the Red Sea, and <a href="https://www.earth.com/news/coral-reefs-in-some-parts-of-the-world-actually-benefit-from-warming-el-nino-events/">Palmyra Atoll</a> - in collaboration with the Smith Lab at Scripps Oceanography. 



What they saw surprised them. Corals weren’t passive. They moved constantly, changing shape, reacting to particles, and even behaving in ways that looked like fighting or kissing.



Ben-Zvi observed coral polyps contracting their tentacles, possibly trying to remove or capture something floating by.



“The more time we spend with this microscope, the more we hope to learn about corals and why they do what they do under certain conditions,” she said. 



“We are visualizing photosynthesis, something that was previously unseen at the scales we are examining, and that feels like magic.”



<h2 class="wp-block-heading" id="h-early-detection-of-coral-stress">Early detection of coral stress</h2>



Corals face serious threats from climate change, and once bleaching begins, it can be hard to stop. But this microscope might help researchers catch problems earlier.



“The microscope facilitates previously unavailable, underwater observations of <a href="https://www.earth.com/news/what-grazing-halos-and-parrotfish-reveal-about-coral-reef-health/">coral health</a>, a breakthrough made possible thanks to the National Science Foundation and its critical investment in technology development,” said Jules Jaffe, a research oceanographer at Scripps and co-author of the study. 



Without continued federal funding, scientific research is at risk. In this case, however, support from <a href="https://www.nsf.gov/">NSF</a> enabled the team to build a device that helps solve the physiological mystery of coral bleaching and, ultimately, inform efforts to reverse it.



By detecting signs of stress before the coral reaches the tipping point, the researchers hope to create better strategies for protecting reefs from events like marine heatwaves.



<h2 class="wp-block-heading" id="h-studying-kelp-and-ocean-algae">Studying kelp and ocean algae</h2>



The potential doesn’t stop with corals. Scientists at Scripps Oceanography are already using the BUMP microscope to study other tiny marine life that rely on photosynthesis, including baby kelp off the coast of California.



“Since photosynthesis in the ocean is important for life on earth, a host of other applications are imaginable with this tool, including right here off the coast of San Diego,” said Jaffe.



In short, the BUMP microscope gives scientists something they’ve never had before: a new way to look at life underwater - close up, in motion, and alive. And with this new perspective, scientists are hoping to find better ways to protect some of the most fragile ecosystems on the planet.



The full study was published in the journal <a href="https://besjournals.onlinelibrary.wiley.com/doi/10.1111/2041-210X.70078">Methods in Ecology and Evolution</a>.



About the image: The photo features the coral&nbsp;Stylophora pistillata&nbsp;taken with the new micrsope, BUMP. Each polyp has a mouth and a set of tentacles, and the red dots are individual microalgae residing inside the coral tissue. Credit: Or Ben-Zvi



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Microscope reveals coral health in unprecedented detail

Coral reefs are in trouble. As oceans warm and environments...

We hear about minerals all the time. Lithium, cobalt, nickel, graphite, and rare earth elements appear in the news almost every week.



These minerals power phones, <a href="https://www.earth.com/news/dirty-power-the-hidden-climate-cost-of-electric-vehicles/">electric cars</a>, and military equipment. Countries want them, companies want them, and the competition for the minerals keeps growing.



While leaders plan and companies race, some scientists study a different part of the story. They ask questions about where these minerals come from and how they move underground.



Geologist Zachary Burton works on these questions. He studies natural processes instead of using drills or machines.



<h2 class="wp-block-heading" id="h-rare-earth-elements-are-hard-to-find">Rare earth elements are hard to find</h2>



"Rare earth elements aren't technically rare - they are somewhat ubiquitous at very low concentrations - but highly concentrated, economically attractive deposits are indeed rare and hard to find," Burton explained.



In the Department of Earth Sciences at <a href="https://www.montana.edu/">Montana State University</a>, Burton has been studying these elements for almost 15 years.



The problem is simple. Scientists do not fully understand how these minerals move or gather in one place.



"That's in large part because we don't even know many fundamental scientific processes of why they concentrate in certain areas and how they're moving around," Burton said.



<h2 class="wp-block-heading" id="h-a-desert-deep-in-antarctica">A desert deep in Antarctica</h2>



Burton recently studied these minerals in a very cold place: <a href="https://www.earth.com/news/antarctica-is-experiencing-rapid-plant-growth-concerning-scientists/">Antarctica</a>'s McMurdo Dry Valleys. This part of Antarctica is dry, windy, and extremely cold. It has unusual landscapes that look similar to other planets.



Burton’s team investigated how rare earth minerals move in this polar desert. They focused on salt ponds in the area, including Don Juan Pond, VXE-6 Pond, and Brine Pond Number 1.



The team found something intriguing. In Don Juan Pond, mineral levels were low in the center - likely because chemicals had washed them away.



However, minerals had gathered underground in two specific spots: one about 10 to 12 centimeters deep (roughly 4 to 5 inches) west of Don Juan Pond, and another about 4 to 7 centimeters deep (around 1.5 to 2.75 inches) beneath VXE-6 Pond.



<h2 class="wp-block-heading" id="h-freezing-and-melting-moves-minerals">Freezing and melting moves minerals</h2>



The places with more minerals had another feature. The soil there contained clay-like <a href="https://www.earth.com/news/rare-meteorites-provide-a-window-into-the-early-solar-system/">materials</a>. These formed through chemical changes.



The reason for this process was clear. Water froze and melted many times. The ponds also changed in size. These actions moved the minerals.



Water carried the minerals. When the water froze, the minerals stayed behind in the soil. This cycle repeated many times. Over the years, minerals gathered just below the surface.



Burton explained that similar things can happen in other cold areas. He pointed to Greenland and Ukraine, two places that are often in the news for their mineral resources.



"Rare earths are an area that's been relatively neglected these past decades in terms of scientific research, but now - with these critical minerals constantly making headlines - there's a whole lot to be learned in terms of where deposits are," he said.



<h2 class="wp-block-heading" id="h-from-antarctica-to-other-planets">From Antarctica to other planets</h2>



Burton’s research is not only about Earth. It also connects to space. The Dry Valleys in Antarctica are similar to places on <a href="https://www.earth.com/news/new-plan-terraform-mars-nanoparticles-would-make-it-habitable-for-humans/">Mars</a>. That makes them a good place to study processes that might also happen on other planets. 



Space agencies, such as NASA, need to find resources beyond Earth. Burton’s work may help them plan future missions.



The study also included diagrams that showed how minerals move underground. Water flows below the surface, freezes, and leaves minerals behind. These findings may guide future work in space.



<h2 class="wp-block-heading" id="h-rare-mineral-movement-in-hot-deserts">Rare mineral movement in hot deserts</h2>



Burton’s projects also focus on dry areas in the United States. He studies how minerals move in places like Nevada, Utah, and California’s <a href="https://www.earth.com/news/desert-lichen-may-offer-clues-to-life-beyond-earth/">Mojave Desert</a>. 



These regions are hot, dry, and full of desert basins. The goal is to understand how rare earth elements and lithium move and collect in such places.



Burton described the work as difficult but exciting. "It's a challenge and a scramble, but also very exciting, because there's a lot more for the world to learn in these areas."



<h2 class="wp-block-heading" id="h-a-new-frontier-for-geology">A new frontier for geology</h2>



Montana State University is now focusing more on this type of research. Alison Harmon, vice president for research and economic development at the university, said these studies matter.



"This will be an area where MSU can make an important contribution to national security and economic development in Montana and beyond," said Harmon.



Burton’s research shows that minerals do not stay in one spot forever. Water, ice, and time keep moving them around. By studying how this happens, researchers can learn more about Earth’s resources and even about resources on other worlds.



The study is published in the journal <a href="https://www.sciencedirect.com/science/article/pii/S0165232X25001661?via%3Dihub" target="_blank" rel="noreferrer noopener">Cold Regions Science and Technology</a>.



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Water and ice may reveal where rare earth elements are hiding

We hear about minerals all the time. Lithium, cobalt, nickel,...

Antarctica’s surrounding ocean has lost sea ice equal to the size of Greenland since 2015. That’s not just a startling statistic - it marks one of the fastest environmental shifts happening anywhere on Earth today.



For decades, the belief was simple: melting ice made the ocean surface fresher, which helped new ice form. But recent findings show the ocean is behaving differently - and that shift could have far-reaching consequences.



<h2 class="wp-block-heading" id="h-a-puzzling-change-in-ocean-salinity">A puzzling change in ocean salinity</h2>



A team of researchers from the <a href="https://www.southampton.ac.uk/">University of Southampton</a>, working with collaborators in Spain, analyzed <a href="https://www.earth.com/news/human-induced-changes-in-ocean-salinity-threaten-biodiversity-and-marine-ecosystems/">ocean salinity</a> data using instruments aboard the European Space Agency’s SMOS satellite. 



The analysis revealed a clear shift: surface waters south of 50° S latitude are becoming saltier. This shift marks a break from a long-standing trend. 



Since the 1980s, surface waters in the Southern Ocean had been cooling and freshening - conditions that helped sea ice expand. That trend has now reversed.



“The discovery was unexpected because <a href="https://www.earth.com/news/antarcticas-melting-ice-shelves-threaten-global-sea-levels/">melting ice</a> should freshen the ocean, not make it saltier,” said Dr. Alessandro Silvano, lead author of the study published this week. “Yet SMOS satellite data reveal the opposite is occurring, and this is deeply troubling.”



<h2 class="wp-block-heading" id="h-saltier-waters-less-ice">Saltier waters, less ice</h2>



When the ocean’s surface is fresh and cold, it floats on top of warmer, saltier water deep below. This layering keeps the heat trapped underneath, allowing ice to grow and stay intact.



“But now the saltier surface waters are enabling heat from deeper down to rise more readily,” Dr. Silvano explained. “This upward flow of warmer water melts sea ice from beneath, making it significantly harder for ice to reform.”



The consequences are already visible. <a href="https://www.earth.com/news/rapid-antarctic-sea-ice-loss-is-causing-severe-storms-around-the-world/">Antarctic sea ice</a> has dropped sharply. Even more concerning, a large patch of open water - the Maud Rise polynya - has reappeared in the Weddell Sea. It hadn’t been seen since the 1970s.



“The return of the <a href="https://www.earth.com/news/massive-hole-polynya-the-size-of-switzerland-appeared-in-the-antarctica-sea-ice/">Maud Rise polynya</a> highlights just how abnormal the current situation is,” said Dr. Silvano. “If this trend of higher salinity and reduced ice persists, it could lead to lasting changes in the Southern Ocean, with consequences for the rest of the world.”



<h2 class="wp-block-heading" id="h-monitoring-the-ocean-from-space">Monitoring the ocean from space</h2>



Studying the Southern Ocean isn’t easy. It’s isolated, violent, and dark for much of the year. That’s why satellite technology is so essential.



To overcome the challenges, scientists at the University of Southampton and the Barcelona Expert Centre built new algorithms to measure changes in surface salinity more accurately from space. The effort was part of ESA’s Earth Observation FutureEO program.



“This is yet another example of how crucial sea-surface salinity measurements from space are,” said Roberto Sabia, ESA Earth Observation Ocean Scientist. 



“This novel regional product has been devised to overcome the conventional limitations of salinity retrieval at high latitudes, an area where seawater density is largely controlled by salinity.”



By combining satellite data with instruments in the ocean, the team built a 15-year dataset tracking changes in salinity, temperature, and ice cover in the Southern Ocean.



<h2 class="wp-block-heading" id="h-a-dangerous-feedback-loop">A dangerous feedback loop</h2>



The findings challenge previous assumptions about how the ocean and climate interact. For years, <a href="https://www.earth.com/news/climate-models-underestimate-sea-ice-melt-and-global-warming/">climate models</a> predicted that warming would lead to more ice melt and freshening at the surface, which would help balance things out. That’s no longer the case.



“Our new study has revealed that the Southern Ocean is changing, but in a different way to what we expected,” said Dr. Silvano.



“We might be closer to passing a tipping point than expected and we have potentially entered a new state defined by persistent sea ice decline, sustained by a newly discovered feedback loop.”



The feedback loop works like this: warmer, saltier surface water melts ice from below. Less ice means more exposed ocean. That exposed water absorbs more heat, driving even more melting.



<h2 class="wp-block-heading" id="h-the-global-ripple-effect">The global ripple effect</h2>



The loss of Antarctic sea ice isn’t just a local problem. It’s linked to more heat escaping from the ocean into the air. That fuels stronger storms and speeds up global warming. The result is more extreme weather, more melting of the Antarctic ice sheet, and faster sea level rise.



There’s also a direct threat to wildlife. Penguins, seals, and other species that rely on sea ice for survival are losing their habitat.



These shifts are happening faster - and differently - than climate models predicted. Scientists are now questioning long-held assumptions about how warming should affect ocean layering and ice stability.



“These findings show that we still have gaps in our understanding of ocean and climate dynamics,” said co-author Alberto Naveira Garabato. “Continuous satellite and in-situ monitoring is essential if we want to track and predict these critical changes.”



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Antarctica’s waters are getting saltier - and it could transform Earth's climate

Antarctica’s surrounding ocean has lost sea ice equal to the...

How did life on Earth begin? People have been asking that for ages. The answers remain scattered across rocks, oceans, and ancient landscapes. One clue hides in an essential ingredient for life - phosphorus.



Phosphorus is everywhere in living things. It holds together DNA and RNA. It forms the framework of cell membranes. No life can grow or function without it. 



Yet, phosphorus mostly stays trapped in rocks. It hides inside phosphate minerals, which barely dissolve in water. That raises an old and puzzling question: how did early Earth get enough phosphorus to <a href="https://www.earth.com/news/scientists-discover-one-simple-rule-that-explains-all-life-on-earth-bioregions/">spark</a> life?



Yuya Tsukamoto and Takeshi Kakegawa from <a href="https://www.tohoku.ac.jp/en/" target="_blank" rel="noreferrer noopener">Tohoku University</a> took that question seriously. They decided to look where most people wouldn’t - deep under the sea, in rocks that are billions of years old.



<h2 class="wp-block-heading" id="h-key-element-for-life-on-earth">Key element for life on Earth</h2>



The researchers focused on the Pilbara Craton in Western Australia, which holds some of the oldest known seafloor rocks. 



The rocks are an astonishing 3.455 billion years old. The team's discovery wasn’t subtle. It jumped out from the data.



"We analyzed 3.455-billion-year-old basaltic seafloor rocks in drill core samples recovered from the Pilbara Craton, Western Australia, discovering that P was significantly leached from the hydrothermally altered rocks compared to the least altered rocks," explained Tsukamoto.



He noted that further mineralogical analyses indicated that phosphate minerals had undergone dissolution in rocks where P was depleted. 



Simply put, hot fluids moved through these rocks and pulled phosphorus out. That phosphorus didn’t just disappear. It entered the surrounding seawater, turning parts of the ocean into phosphorus-rich zones.



<h2 class="wp-block-heading" id="h-tracking-the-source-of-phosphorus">Tracking the source of phosphorus </h2>



The rocks alone didn’t tell the whole story. The team wanted to understand what made this phosphorus release possible. They uncovered two kinds of hydrothermal fluids that shaped this <a href="https://www.earth.com/news/third-state-of-existence-beyond-life-and-death-confirmed-by-scientists/">process</a>.



One type was hot, rich in sulfur, and capable of breaking down minerals quickly. The other was more surprising - mildly acidic to alkaline fluids at lower temperatures. 



These fluids were common in the Archean era because Earth’s atmosphere back then was filled with carbon dioxide. That unique atmosphere made these fluids react in unexpected ways with the rocks.



The result? Massive amounts of dissolved phosphate in the water. The numbers were shocking. These fluids could carry up to 2 millimolar phosphate - nearly 1,000 times higher than what’s found in modern seawater.



Suddenly, early <a href="https://www.earth.com/news/luca-last-universal-common-ancestor-progenitor-all-life-on-earth/">Earth</a> wasn’t a barren place. Its oceans were filled with phosphorus.



<h2 class="wp-block-heading" id="h-earth-s-oceans-held-elements-for-life">Earth’s oceans held elements for life</h2>



This wasn’t just a chemistry experiment. The results changed how scientists think about early Earth. The researchers calculated how much phosphorus these underwater systems could release. 



The findings were stunning. The amount of phosphorus released into the oceans by these hydrothermal systems could match, or even exceed, the amount entering modern oceans through rivers and weathering of land rocks.



"Importantly, this study provides direct evidence that submarine hydrothermal activity leached P from seafloor basaltic rocks and quantifies the potential P flux from these hydrothermal systems to the early ocean," adds Tsukamoto.



Imagine ancient oceans filled with nutrients. These phosphorus-rich waters may have supported some of Earth’s earliest microbial life. 



The ancient communities didn’t need a vast, lush <a href="https://www.earth.com/news/rocks-reveal-the-turning-point-when-oxygen-changed-earth-forever/">planet</a>. It only needed these hidden underwater environments to get started.



<h2 class="wp-block-heading" id="h-hot-springs-and-hidden-worlds-on-land">Hot springs and hidden worlds on land</h2>



The study also pointed to something beyond the oceans - hot springs on land. Hydrothermal systems aren’t just found under the sea. They exist on land too, in places like hot springs.



These environments might have also released phosphorus on early Earth. That means life’s building blocks weren’t limited to deep-sea vents. They could have existed in steaming pools on land.



This opens the door for more discoveries. Scientists now plan to study how phosphate behaves in rocks across different periods of Earth’s history. By tracing phosphorus through time, they hope to unlock new chapters of Earth’s story.



The message is clear: Life’s ingredients may have come from places on Earth we’ve only just begun to explore. Deep beneath the waves, within rocks touched by ancient fluids, the story of life may have quietly begun.



The study is published in the journal <a href="https://www.sciencedirect.com/science/article/abs/pii/S0016703725003266?via%3Dihub" target="_blank" rel="noreferrer noopener">Geochimica et Cosmochimica Acta</a>.



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Earth may have always held the key ingredients for life

How did life on Earth begin? People have been asking...

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=WXXGGiynIjs
</div><figcaption class="wp-element-caption">Greenland is not sinking. In fact, it is the opposite.</figcaption></figure>



<h2 class="wp-block-heading" id="h-a-contrasting-climate-response">A contrasting climate response</h2>



Most coastal towns are <a href="https://www.earth.com/news/sinking-land-will-intensify-the-effects-of-rising-sea-levels/" target="_blank" rel="noreferrer noopener">preparing for higher sea levels</a>, but <a href="https://www.earth.com/news/greenland-no-longer-has-to-worry-about-rising-sea-levels/" target="_blank" rel="noreferrer noopener">Greenland presents</a> a different scenario during climate change. The ground there is rising at a remarkable rate. Over the past decade, some areas have lifted about 20 centimeters, which translates to roughly 2 meters per century. This rate significantly exceeds current projections for sea level rise.



<h2 class="wp-block-heading" id="h-geological-rebound-process-through-climate-change">Geological rebound process through climate change</h2>



The mechanism behind this phenomenon is straightforward. As the ice sheet melts, the immense weight is removed from the bedrock, causing the land to rebound upward. This process resembles the way compressed material springs back when pressure is released.



<h2 class="wp-block-heading" id="h-scientific-monitoring-networks">Scientific monitoring networks</h2>



Researchers at the <a href="https://www.dtu.dk/english/" target="_blank" rel="noreferrer noopener">Technical University of Denmark</a> are documenting this uplift using the GNET network, consisting of 61 GPS stations positioned around Greenland's coast. These sensors can detect movement with millimeter precision, providing detailed measurements of the ongoing changes.



The data reveal that current uplift rates exceed the gradual rebound occurring since the last ice age ended approximately 12,000 years ago. This acceleration corresponds directly with increased ice sheet melting rates.



<h2 class="wp-block-heading" id="h-coastal-transformation">Coastal Transformation</h2>



This uplift is actively reshaping Greenland's coastline. New islands and rocky formations, called "skerries," are emerging as previously submerged land surfaces rise above the water level. This represents a notable contrast to global concerns about rising seas.



The study, published in Geophysical Research Letters, demonstrates the varied regional impacts of climate change. While many locations face rising water levels, Greenland's bedrock is literally rising above the surrounding seas.



The full study was recently published in <a href="https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2023GL104851" target="_blank" rel="noreferrer noopener">Geophysical Research Letters</a>.



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Greenland's ground rises while coasts worldwide face higher seas

https://www.youtube.com/watch?v=WXXGGiynIjs Greenland is not sinking. In fact, it is the...

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=DSM3EVeGHJU
</div><figcaption class="wp-element-caption">Companies like MindStudio help companies train their employees to implement the latest AI Agent building platform.</figcaption></figure>



<h2 class="wp-block-heading" id="h-ai-agent-training-transforms-the-workplace-fear-factor-into-a-competitive-advantage">AI agent training transforms the workplace 'fear factor' into a competitive advantage</h2>



Organizations that offer comprehensive artificial intelligence training to their workers find remarkable value that extends well beyond basic <a href="https://www.earth.com/news/mind-wandering-might-be-more-productive-than-you-think/" target="_blank" rel="noreferrer noopener">productivity improvements</a>. Emerging research demonstrates that carefully crafted AI training programs <a href="https://www.earth.com/news/ai-does-not-replace-human-creativity-but-enhances-it/" target="_blank" rel="noreferrer noopener">enhance</a> corporate performance, lower operational costs, and dramatically improve employee psychological well-being by turning workplace uncertainty into professional empowerment.



<h2 class="wp-block-heading" id="h-addressing-the-widespread-ai-anxiety-crisis-among-us">Addressing the widespread 'AI anxiety' crisis among us</h2>



A staggering 53% of employees expressed concern that the use of AI tools to automate work tasks could make them appear disposable to their employers, according to <a href="https://www.microsoft.com/" target="_blank" rel="noreferrer noopener">Microsoft</a>'s 2024 workplace survey. Such pervasive worry about being substituted by machines has caused what researchers have termed "AI technostress" – a psychological state that can result in occupational burnout and poorer mental well-being.



Data published in <a href="https://www.nature.com/palcomms/" target="_blank" rel="noreferrer noopener">Humanities and Social Sciences Communications</a> showed that belief in AI learning ability was a moderator in the link between technology adoption and work pressure, and higher confidence significantly lowered negative psychological responses. Workers provided ample training to become competent with AI software have significantly lower stress.



Companies like <a href="https://www.mindstudio.ai/" target="_blank" rel="noreferrer noopener">MindStudio</a> have platforms for building what are known as "AI Agents". In essence, AI Agents are simply tools that employees can build for themselves or their teams quickly and inexpensively. MindStudio will even train entire companies, from the CEO on down, at no cost. By letting MindStudio empower employees, companies avoid hiring more IT staff, buying more software, and implementing solutions to problems that do not exist.



MindStudio even has partners locally for companies, like <a href="http://www.dominnus.com" target="_blank" rel="noreferrer noopener">Dominnus</a> with offices in the Carolinas, California, and Denver, to help build AI Agents and support employees as they become resident AI experts for their organization. The training provided by MindStudio is applicable across other AI Agent building platforms as well.



<h2 class="wp-block-heading" id="h-revolutionary-productivity-through-focused-learning">Revolutionary productivity through focused learning</h2>



Organizations that implement large-scale AI training programs achieve dramatic outcomes. Employees performed tasks significantly better when they utilized AI support compared to when they didn't, according to <a href="https://www.nngroup.com/" target="_blank" rel="noreferrer noopener">Nielsen Norman Group</a> research findings. Their study documented productivity increases of 66% for a variety of professional tasks.



Federal Reserve Bank of St. Louis research finds workers record 33% higher productivity in time working with generative AI tools. The benefit is equivalent to 5.4% of work time savings for AI users – around 2.2 hours per week for full-time workers.



<h2 class="wp-block-heading" id="h-psychological-well-being-benefits-through-ai-competence">Psychological well-being benefits through AI competence</h2>



The emotional transformation when employees are provided with proper technology training is a fundamental transformation from fear to professional confidence. A survey of 600 employees across industries, carried out by ScienceDirect, proved that AI capabilities strengthen work environment commitment and improve job satisfaction.



A <a href="https://www.lut.fi/en" target="_blank" rel="noreferrer noopener">LUT University</a> study discovered that AI adoption has no direct effect on workers' well-being but does so indirectly through working conditions like task optimization and safety protocols. Strategically deployed AI that involves correct training can actually increase workplace mental well-being.



<h2 class="wp-block-heading" id="h-from-replacement-anxiety-to-partnership-confidence">From 'replacement anxiety' to 'partnership confidence'</h2>



Although 35% of those interviewed in recent McKinsey studies were concerned about workforce displacement, firms with large-scale training initiatives witness such fears dissipate quickly. The World Economic Forum found that two out of three respondents believe AI competencies will enhance their career prospects and job marketability.



This shift from fear to trust has measurable implications for job satisfaction. Applied Sciences research indicates AI can create tailored wellness programs based on individual employee requirements.



<h2 class="wp-block-heading" id="h-financial-benefits-of-increased-retention">Financial benefits of increased retention</h2>



The mental health advantages of AI learning have a direct impact on organizational bottom lines in the form of a positive feedback cycle with high retention of employees. Recent ROI research validates that artificial intelligence learning has a beneficial impact on employee turnover and satisfaction levels.



PriceWaterhouseCoopers' research documents 20% to 30% improvements in productivity, market speed, and revenue in organizations that attempt systematic AI adoption through comprehensive training.



<h2 class="wp-block-heading" id="h-environmental-advantages-of-ai-enabled-teams">Environmental advantages of AI-enabled teams</h2>



AI training has unforeseen environmental benefits as it makes the work environment more efficient. According to a study in Scientific Reports, the carbon footprint in writing and illustrating work is significantly lower when AI performs it compared to humans. AI software produces 130 to 1,500 times less CO2 equivalent per page of text created than human authors.



In addition, AI-driven remote work functionality significantly reduces environmental impact. Research by Cornell University and Microsoft indicates that remote workers reduce greenhouse gas emissions by up to 54% by not commuting daily to offices. Hybrid workers working remotely two to four days a week can reduce their carbon footprint by 11% to 29%.



<h2 class="wp-block-heading" id="h-cumulative-organizational-advantages">Cumulative organizational advantages</h2>



The compounding gains of better mental well-being, reduced turnover, increased productivity, and environmental benefits flow to enterprises from the pairing. McKinsey analysis estimates the long-term AI potential at $4.4 trillion in incremental productivity growth opportunity from business use cases.



As of now, 75% of knowledge workers globally utilize generative AI, mirroring widespread adoption patterns. Organizations that provide organized training and assistance see the most favorable results in productivity, worker satisfaction, and ecological sustainability.



The research overwhelmingly indicates that companies that invest in proper AI education, like that offered through <a href="https://www.mindstudio.ai" target="_blank" rel="noreferrer noopener">MindStudio</a>, establish win-win scenarios where employees are both more empowered and less stressed, and companies enjoy the gains of increased productivity, reduced turnover, and improved mental health outcomes throughout their workforce.



For more on MindStudio's free AI training for companies, visit the website's of MindStudio and Dominnus from the links below.



The research was published across a variety of peer-reviewed journals, including <a href="https://www.nature.com/palcomms/" target="_blank" rel="noreferrer noopener">Humanities and Social Sciences Communications</a>, <a href="https://www.frontiersin.org/journals/artificial-intelligence" target="_blank" rel="noreferrer noopener">Frontiers in Artificial Intelligence</a>, and <a href="https://www.mdpi.com/journal/applsci">Applied Sciences</a>.



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MindStudio.AI: <a href="https://www.mindstudio.ai" target="_blank" rel="noreferrer noopener">https://www.mindstudio.ai</a>



Dominnus: <a href="https://www.dominnus.com" target="_blank" rel="noreferrer noopener">https://www.dominnus.com</a>

AI agent training boosts mental health and profits

https://www.youtube.com/watch?v=DSM3EVeGHJU Companies like MindStudio help companies train their employees to...

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=0HDXqTGEmi4
</div><figcaption class="wp-element-caption">Scientists give plants superpowers against bacterial disease</figcaption></figure>



<h2 class="wp-block-heading" id="h-a-natural-solution-to-disease-through-crop-modification">A natural solution to disease through crop modification.</h2>



The agricultural industry stands at a crossroads between productivity and environmental responsibility, and crop modification often carries a negative connotation. While chemical pesticides have long been the go-to solution for crop protection, their harmful effects on ecosystems and human health have prompted scientists to seek alternatives. The recent breakthrough by <a href="https://www.southampton.ac.uk/" target="_blank" rel="noreferrer noopener">University of Southampton</a> researchers offers a promising path forward through the precise manipulation of plant-associated microbial communities.



<h2 class="wp-block-heading" id="h-the-science-behind-microbial-partnerships">The science behind microbial partnerships</h2>



Plants naturally harbor diverse ecosystems of bacteria, fungi, and other microorganisms that function as biological allies. These microscopic partners contribute to disease resistance, nutrient absorption, and stress tolerance. However, until now, scientists lacked the tools to deliberately reshape these communities to enhance crop protection.



The Southampton team's approach centered on <a href="https://www.earth.com/news/engineered-plant-microbiomes-the-future-of-crop-protection/" target="_blank" rel="noreferrer noopener">modifying lignin biosynthesis genes in rice plants</a>. This strategic intervention altered the plant's metabolic output, creating conditions that favored beneficial bacterial populations while suppressing harmful ones. The result was a living defense system embedded within the plant itself.



<h2 class="wp-block-heading" id="h-implications-for-global-food-security">Implications for global food security</h2>



The successful demonstration against Xanthomonas oryzae, the pathogen responsible for bacterial blight in rice, represents more than a laboratory achievement. Rice feeds nearly half the world's population, and bacterial blight causes devastating crop losses annually. Traditional control methods rely heavily on pesticides that contaminate soil and water systems.



<h2 class="wp-block-heading" id="h-looking-beyond-disease-resistance">Looking Beyond Disease Resistance</h2>



While disease protection represents the immediate application, the research framework opens doors to broader agricultural improvements. Future developments could engineer microbiomes to enhance nutrient uptake, reducing dependence on synthetic fertilizers. This dual benefit addresses both crop productivity and environmental sustainability.



<h2 class="wp-block-heading" id="h-the-path-forward">The path forward</h2>



As this technology advances from laboratory to field applications, it promises to reshape sustainable agriculture. The ability to program plants with their own biological defense systems could herald a new era where crops protect themselves naturally, reducing chemical inputs while maintaining yields necessary for global food security.



The study is published in the journal&nbsp;<a href="http://dx.doi.org/10.1038/s41467-023-44335-3" target="_blank" rel="noreferrer noopener">Nature Communications</a>.



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Revolutionizing agriculture through microbiome engineering

https://www.youtube.com/watch?v=0HDXqTGEmi4 Scientists give plants superpowers against bacterial disease A natural...

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=prrq8Ql81zk
</div><figcaption class="wp-element-caption">Acid rain and a crisis solved.</figcaption></figure>



<h2 class="wp-block-heading" id="h-why-don-t-we-ever-hear-about-acid-rain-anymore-the-environmental-crisis-that-was-solved">Why don't we ever hear about "acid rain" anymore? The environmental crisis that was solved</h2>



Remember the 1980s when acid rain dominated headlines? Dire warnings about rain eating buildings, killing fish, and destroying forests filled every news cycle. Then, almost like magic, acid rain vanished from public discourse. What happened? Did we actually solve one of the late 20th century's most pressing environmental challenges?



The answer might surprise you. Unlike many environmental issues that drag on indefinitely, acid rain represents one of modern history's most successful ecological recovery stories. It's a tale of science, politics, and technology working together to tackle what seemed impossible.



<h2 class="wp-block-heading">What was acid rain?</h2>



Acid rain isn't regular rain having a bad day – it's precipitation that became significantly more acidic due to air pollution. When power plants, factories, and vehicles burn fossil fuels, they release sulfur dioxide (SO2) and nitrogen oxides (NOx) into the atmosphere.



<h2 class="wp-block-heading">The science behind it</h2>



Think of acid rain as nature's chemistry experiment gone wrong. These compounds react with water, oxygen, and other chemicals to form sulfuric and nitric acids. When mixed with water vapor in clouds, they create precipitation with dangerously low pH levels.



While clean rain has a pH of about 5.6, acid rain could drop as low as 4.2 to 4.4 – roughly as acidic as tomato juice or coffee. According to US Geological Survey documentation, Scottish chemist Angus Smith first coined "acid rain" in 1872, but it didn't become a household phrase until the 1960s and 1970s when Swedish scientist Svante Odén documented its devastating effects on Scandinavian lakes and European forests.



<h2 class="wp-block-heading">The crisis at its peak</h2>



During the height of public concern, environmental damage was both widespread and visible. This wasn't some abstract future threat – people could see destruction happening in real-time.



<h2 class="wp-block-heading">Environmental devastation</h2>



The most dramatic impacts were impossible to ignore. Research documented by the Adirondack Lakes Survey Corporation and the New York State Department of Environmental Conservation shows that in the Adirondack Mountains, more than 200 lakes became so acidic they couldn't support fish life. The Adirondack Council reports that 409 lakes once supported brook trout, but many lost their fish populations due to acid rain.



By 1976, when scientists cataloged all acidified lakes in the Adirondack Park, researchers found that half of the lakes over 2,000 feet above sea level had no fish, according to studies published in environmental journals. The acidification process worked like a slow-motion disaster. As acid rain fell into watersheds, it gradually lowered pH levels. Fish couldn't survive in acidic water, and their food sources died off too.



Trees at high elevations showed stress directly linked to acid rain. It weakened them by leaching nutrients and making them susceptible to disease. Historical records show Germany's Black Forest saw nearly half its trees damaged by the mid-1980s.



<h2 class="wp-block-heading">Economic impact</h2>



Acid rain wasn't just environmental – it was expensive. Acidic precipitation corroded infrastructure, buildings, and monuments. Historic stone structures deteriorated at accelerated rates. Tourism suffered as lakes became fishless and forests declined. EPA economic analyses from the period documented repair costs mounting into billions annually.



<h2 class="wp-block-heading">The solution: government action and technology</h2>



Transformation from crisis to success required unprecedented cooperation between governments, industries, and environmental groups.



<h2 class="wp-block-heading">The Clean Air Act of 1990</h2>



The turning point came with the Clean Air Act Amendments of 1990, signed by President George H.W. Bush. This represented a fundamentally new approach to environmental regulation, as documented in EPA historical records.



<h2 class="wp-block-heading">Cap-and-trade success</h2>



Instead of mandating specific technologies, the 1990 amendments introduced something revolutionary: a cap-and-trade system for sulfur dioxide emissions. EPA program documentation shows this market-based approach set overall limits but allowed companies to trade emission allowances.



The genius was harnessing market forces to find cost-effective pollution reduction. Companies reducing emissions cheaply could sell excess allowances to those facing higher costs. Research published in environmental economics journals and EPA progress reports shows this resulted in dramatic SO2 reduction at a fraction of projected costs.



<h2 class="wp-block-heading">Technology advances</h2>



Policy provided the framework, but technology made reductions possible. Studies in atmospheric science journals document the widespread adoption of flue gas desulfurization systems ("scrubbers") that removed sulfur dioxide before it reached the atmosphere. By the 2000s, new installations could remove over 95% of SO2 emissions, according to EPA technical reports.



The push coincided with cleaner energy development. Natural gas produces fewer sulfur compounds than coal. Wind and solar, emerging in the 1990s, captured growing market share, reducing reliance on high-sulfur coal.



<h2 class="wp-block-heading" id="h-why-we-don-t-hear-about-it-today">Why we don't hear about it today</h2>



Why did acid rain disappear from headlines? Simple: the problem was largely solved.



<h2 class="wp-block-heading">Success doesn't make news</h2>



There's an old journalism saying: "If it bleeds, it leads." Environmental success stories don't generate urgency like crisis reporting. Media attention shifted to other challenges: climate change, plastic pollution, and biodiversity loss. There's only so much environmental anxiety the public can absorb, and newer concerns replaced acid rain.



<h2 class="wp-block-heading">Mission accomplished</h2>



The primary reason is beautifully simple: interventions worked. EPA monitoring data shows sulfur dioxide emissions dropped over 90% since 1990. Academic research published in environmental science journals confirms pH levels in formerly affected areas returned closer to normal. This represents one of history's most dramatic environmental recoveries. Studies by the Adirondack Lakes Survey Corporation show fishless lakes now support healthy populations. Forests recovered, and building damage slowed dramatically.



<h2 class="wp-block-heading" id="h-is-it-really-gone">Is it really gone?</h2>



The crisis is largely resolved, but monitoring data shows the problem isn't completely eliminated – it's managed to acceptable levels. Some areas still experience occasional events during high pollution periods. International environmental research indicates that rapidly industrializing Asian countries face similar problems to what we experienced decades ago, though they're implementing successful strategies.



EPA research shows nitrogen oxide emissions proved more challenging than sulfur dioxide, coming from vehicles and mobile sources. Climate science studies suggest changing weather patterns add complexity to how acid rain forms and falls.



<h2 class="wp-block-heading">What this teaches us</h2>



The acid rain experience proves that seemingly intractable environmental problems can be solved with scientific understanding, political will, and technological innovation. Environmental monitoring data shows recovery speed was remarkable – within a decade, measurable improvements appeared in air quality and ecosystem health.



Success came from bipartisan support across party lines. Policy analysis studies show the market-based approach appealed to those preferring economic incentives while achieving environmental goals. This support created lasting policy surviving political changes.



<h2 class="wp-block-heading">Conclusion</h2>



Acid rain's disappearance from public consciousness represents environmental science's greatest success stories. Through effective regulation, technological innovation, and international cooperation, we transformed an overwhelming crisis into a manageable challenge.



Today's silence isn't because we forgot – it's because we solved it. The 1990 Clean Air Act, combined with technology and energy market changes, reduced acid rain emissions over 90%, according to comprehensive EPA data analysis.



This success offers hope for current challenges. It proves complex problems can be solved when science, policy, and technology work together. As we face climate change and plastic pollution, acid rain reminds us that dramatic positive change is possible.



Next time someone asks whether environmental regulations work, remember acid rain. It's proof that sometimes, we get it right.



<hr class="wp-block-separator has-alpha-channel-opacity"/>



Sources: This article draws from EPA official documentation and progress reports, peer-reviewed research published in environmental and atmospheric science journals, historical data from the Adirondack Lakes Survey Corporation, New York State Department of Environmental Conservation records, US Geological Survey publications, policy analysis studies, and environmental monitoring data collected over three decades.



<h2 class="wp-block-heading">Frequently Asked Questions</h2>



1. Is acid rain completely gone? No, but EPA monitoring shows it's reduced to manageable levels. US sulfur dioxide emissions dropped over 90% since 1990, making acid rain much less severe than the 1980s crisis.



2. How long did solving take? Environmental monitoring data shows significant improvements began within 5-10 years of 1990s emission controls. Full ecosystem recovery took longer – some areas need 20-30 years for complete recovery.



3. What made the solution successful? Clear scientific understanding, visible damage motivating action, bipartisan support, available technology, and innovative market-based policies like cap-and-trade.



4. Do other countries have acid rain problems? Yes, particularly rapidly industrializing Asian countries. However, international environmental research shows many implement similar successful control strategies.



5. Could acid rain return? Potentially, if regulations weaken or we return to high-sulfur coal without controls, though effects would take years to become severe according to environmental projections.



6. Can you recommend any teaching tools on the subject of "acid rain"? The United States Environmental Protection Agency produced a wonderful teacher's guide for ages 14 and under that you can find on the EPA website here: <a href="https://www.epa.gov/sites/default/files/2017-03/documents/teachersguide.pdf" target="_blank" rel="noreferrer noopener">https://www.epa.gov/sites/default/files/2017-03/documents/teachersguide.pdf</a>



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The environmental problem we actually solved

https://www.youtube.com/watch?v=prrq8Ql81zk Acid rain and a crisis solved. Why don't we...

Green,Ecoduct,Over,An,Empty,Highway,During,Sunset.

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A new long-term study in Monkton, Vermont, reveals that wildlife tunnels significantly reduce amphibian road mortality during seasonal migrations. 



Frogs and salamanders often cross roads to reach breeding ponds each spring, but many are killed by vehicles. 



Researchers from the <a href="https://www.uvm.edu/" target="_blank" rel="noreferrer noopener">University of Vermont</a>, in collaboration with local citizens and the Vermont Agency of Natural Resources, installed two underpass tunnels in 2015. 



Over a 12-year monitoring period, they observed an 80.2% reduction in amphibian deaths, and up to 94% for non-climbing species like salamanders. 



The study used a before-after-control-impact design and documented more than 5,200 amphibians, highlighting the tunnels’ effectiveness even in nearby buffer zones.



Funded at $342,397 - far cheaper than wildlife crossings for large mammals - the project showcased the power of community-led conservation.



Local groups initiated the effort after observing mass amphibian deaths. Wildlife cameras later captured over 2,200 amphibians using a tunnel in just one spring, along with other species like raccoons and bobcats, indicating wider ecosystem benefits.



This marks the first peer-reviewed, long-term data set in the northeastern U.S. confirming amphibian-specific underpasses work. 



The study urges transportation departments to incorporate these designs into road planning and highlights how community action, thoughtful infrastructure, and persistence can make a real difference for biodiversity.



The full study was published in the <a href="https://linkinghub.elsevier.com/retrieve/pii/S1617138125000780" target="_blank" rel="noreferrer noopener">Journal for Nature Conservation</a>.



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Wildlife tunnels save millions of amphibians

https://youtu.be/XYgiPzmNBTU?si=eFYY7gPHU1JznLvU A new long-term study in Monkton, Vermont, reveals that...

Scientists are transforming chocolate into a functional food by infusing it with probiotics and prebiotics, aiming to create a treat that satisfies cravings while supporting gut health. 



The challenge lies in maintaining chocolate's beloved texture and flavor while adding health benefits.



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Probiotics - beneficial microbes that balance gut bacteria and aid digestion - are typically fragile and can be destroyed by stomach acid or processing. 



Prebiotics act as food for these microbes, helping them thrive. Together, they form "synbiotics," a powerful health combination.



Researchers Smriti Gaur and Shubhi Singh from India's Jaypee Institute of Information Technology took an innovative approach, using natural prebiotics like corn and honey instead of complex processing methods. 



They created five chocolate varieties: a control and four synbiotic versions containing different combinations of prebiotics, probiotics (Lactobacillus strains), and flavor enhancers (cinnamon or orange).



Laboratory simulations of human digestion showed the probiotics remained viable for over five hours, suggesting they could survive long enough to benefit gut health.



Taste tests were positive, with researchers particularly enjoying the orange-flavored variety, describing it as having "vibrant citrus notes" complementing the "rich cocoa" with a "luxurious" texture.



This research represents just the beginning. With further refinement of strains, textures, and flavors, chocolate could evolve beyond mere indulgence to become a functional food that nourishes while it delights.



The study is published in the journal <a href="https://pubs.acs.org/doi/10.1021/acsfoodscitech.4c00741" target="_blank" rel="noreferrer noopener">ACS Food Science &amp; Technology</a>.

Is chocolate the next nutritional powerhouse?

Scientists are transforming chocolate into a functional food by infusing...

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Today’s Video of the Day from <a href="https://www.igb.illinois.edu/">Carl R. Woese Institute for Genomic Biology</a> reveals how scientists can modify common crops like soybean, rice, and wheat to protect them from heat stress.



“We need to double crop production by 2050 to feed a growing global population, and not only are we not on track to do that, but climate change is further complicating things,” said Amanda Cavanagh, a lecturer at the University of Essex. 



The study is part of Realizing Increased Photosynthetic Efficiency (RIPE), an international research project that aims to develop food crops that turn the sun’s energy into food more efficiently.



“Using an engineering approach we designed multiple alternative metabolic pathways to photorespiration. Testing them in the field showed increases in productivity which led Amanda to significantly move the project forward by showing our engineered plants can withstand pretty extreme temperature stress,” said study co-author and RIPE researcher Paul South.&nbsp;



“As the climate changes and temperature stresses increase the pressure on our global food supply, farmers will need every tool available including engineering approaches like the synthetic biology used here to maintain safe and productive harvests.”



The experts tested plants modified to have more efficient photorespiration to see if they were better adapted to warmer temperatures.&nbsp;



The team found that the engineered plants produced 26 percent more biomass than the wild-type plants exposed to the same temperatures, and had 15 percent less yield loss under the higher temperatures.



Video Credit: Amanda Nguyen/University of Illinois



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Designing crops that can beat the heat

[sendtonews key="QGPzYnXEtN-1712599-12187" type="single"] Today’s Video of the Day from Carl...

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> describes the first comprehensive estimate of carbon density in the Saharan, Sahel, and Sudanian zones of Africa. In an effort to measure the amount of carbon stored across these drylands, a team of scientists used high-resolution satellite images and artificial intelligence to map nearly 10 billion individual trees. 



"The high spatial resolution (50 cm) combined with AI and field measurements used in this study is key to improving tree inventories in drylands," said Pierre Hiernaux, a French researcher working for NASA. "The ever-increasing availability of very high-resolution satellite imagery will make it possible to assess carbon pools and their dynamics at the individual tree level on a global scale."



"This study is exceptional because it is pioneering a type of approach that will revolutionize the monitoring of trees and forests on a global scale: in the short term, it will be possible to map the world's trees from the centre of the Amazon to our schoolyards," said <a href="https://www.inrae.fr/en">INRAE</a> researcher Jean-Pierre Wigneron.



"Many fields of application will become much more efficient and accurate, such as tracking carbon stocks, biodiversity, monitoring logging and protection against illegal forest degradation, in near real time.”



Video Credit: NASA Goddard&nbsp;



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Remote sensing will revolutionize the way we monitor trees

[sendtonews key="EjmSP20gQK-2593093-12187" type="single"] Today's Video of the Day from NASA...

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Lesotho: Africa's "Kingdom in the Sky" Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features northwest Lesotho in South Africa.



According to ESA, Lesotho is the only nation in the world that lies completely above 1,000 m in elevation. The country is famous for its tall mountains and narrow valleys, and is known as Africa's "Kingdom in the Sky."



Out of a population of around two million people, about 80 percent live in rural areas. More than 75 percent of these people are engaged in <a href="https://www.earth.com/news/climate-change-will-have-a-global-impact-on-agriculture/">agriculture</a>, including rainfed cereal production and animal grazing.&nbsp;



ESA reports that the country’s agricultural system faces a growing number of issues, with climate-related vulnerabilities such as drought, floods and extreme temperatures occurring more frequently. 



Diamonds are amongst the minerals found in the mountains. Indeed, Lesotho can truly be called the Kingdom in the Sky. Beautiful, culturally rich, safe, affordable, and easily accessible from Durban and Johannesburg, mountainous Lesotho is a vastly underrated travel destination. the Kingdom of Lesotho (Sotho: 'Muso oa Lesotho) is an enclaved country in southern Africa. It is just over 30,000 km2 (11,583 sq mi) in size and has a population of around 2 million.



Video Credit: ESA&nbsp;&nbsp;



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Lesotho: Africa's "Kingdom in the Sky"

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> features a visual dataset of.methane emissions from wetlands across the globe. Atmospheric methane levels have reached record highs in recent years, and wetlands are a major source of these emissions.&nbsp;



"Methane is an important greenhouse gas that contributes substantially to global warming. On a molecule by molecule basis, methane is much more efficient at trapping heat than carbon dioxide, the main driver of warming," says NASA.



"Though human activities, including agriculture, oil and natural gas production and use, and waste disposal, collectively contribute the majority of methane to the atmosphere, about a third of total methane emissions comes from wetlands."&nbsp;



According to NASA, understanding methane emissions from wetlands and other natural sources is critically important for scientists and policymakers who are working to combat climate change by reducing emissions from human activities.



Video Credit: NASA Goddard



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Wetlands are a major source of methane emissions

[sendtonews key="f8fukm28Vz-2491833-12187" type="single"] Today's Video of the Day from NASA...

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Today’s Video of the Day from <a href="https://earthobservatory.nasa.gov/">NASA Earth Observatory</a> reveals the evolution of the Columbia Glacier in southeastern Alaska. Columbia is among the fastest shrinking glaciers in the world, and the video documents its rapid retreat over the years.&nbsp;



Columbia Glacier is a large, multi-branched calving glacier that flows out of the Chugach Mountains to the Prince William Sound.&nbsp;



According to USGS, Columbia had a long history of stability prior to 1980, with a length 41 miles, and small, short-lived advances or retreats.



In the years since 1980, however, satellite images have captured Columbia’s alarming retreat. By using false-color images, scientists can distinguish between snow and ice, open water, vegetation, and rocky debris on the glacier’s surface.



The series of false-color images featured in today's video were acquired over the span of 35 years. You can see that by 2021, the glacier’s main branch had retreated about 15 miles from its initial position.



The Columbia Glacier has also lost more than 50 percent of its volume, mostly due to calving. <a href="https://www.earth.com/video/nasa-reveals-3d-visual-of-an-atmospheric-river/">NASA</a> reports that while climate change likely started the retreat, mechanical processes kept the disintegration going.



The NASA images are provided by Jesse Allen, Robert Simmon, Joshua Stevens, and Lauren Dauphin using data from Landsat satellites, from the U.S. Geological Survey, and data from MODIS on NASA’s Terra satellite. The structure of Columbia’s moraine played a large role in the stability of the glacier before 1980. 



Like other tidewater glaciers, the Columbia built up a moraine over time, and the mixture of ice and rock functioned like a dam keeping out the sea. It was supported on one end by the shoreline and by the underwater terminal moraine at the other.



Video Credit: NASA Earth Observatory/&nbsp; NASA’s Scientific Visualization Studio



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The rapid retreat of the Columbia Glacier

[sendtonews key="0879czfG3k-1785905-12187" type="single"] Today’s Video of the Day from NASA...

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> describes how record-breaking heat expressed itself around the world in 2022.



Scientists have determined that 2022 was the 5th warmest year since 1880. Furthermore, the last nine consecutive years have been the warmest on record.



From devastating floods and wildfires to natural disasters like Hurricane Ian, 2022 showed us yet again how a warming climate affects people across the globe.&nbsp;



"As we look back at 20:22 and years past, we see that each year we better understand the challenges we face and how important it is to meet them," says NASA.



Video/ Image Credit: NASA Goddard



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2022 illustrated the consequences of a warming climate

[sendtonews key="3UUsNkFOuS-2487333-12187" type="single"] Today's Video of the Day from NASA...

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Satellites reveal how Earth's systems are interconnected Today’s Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> describes Earth’s interconnected systems, and how this network is affected by rising temperatures.&nbsp;



During 2020, average global temperatures matched the hottest year on record. The hurricane season was also record-breaking, with many of the storms intensifying at extraordinary speeds. Hot water in the ocean is fuel for hurricanes. The satellite data shows that it's all one interconnected system showing how Satellites reveal how Earth's systems are interconnected.



According to NASA, dust swept up from Northern Africa plays a major role in the formation of hurricanes, and is also a key source of fertilization in the Amazon rainforest. As a result of<a href="https://www.earth.com/news/seagrass-wasting-disease-is-fueled-by-climate-change/"> climate</a> change, dust plumes are expected to decline, which will have an effect on vegetation far away.&nbsp;



Images from Earth-observing satellites show how the world’s plant life is affected by natural disasters, fires, and deforestation. Satellites also reveal how widespread changes in vegetation impact waterways,&nbsp; the climate, air quality. Satellites communicate by using radio waves to send signals to the antennas on the Earth. "Earth From Space" is a groundbreaking two-hour special that reveals a spectacular new space-based vision of our planet. 



Video Credit: NASA Goddard&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Satellites reveal how Earth's systems are interconnected

[sendtonews key="JbW4VsY53O-1632195-12187" type="single"] Satellites reveal how Earth's systems are interconnected...

Today’s Video of the Day from the <a href="https://welcome.miami.edu/">University of Miami</a> Rosenstiel School of Marine and Atmospheric Science explores how changes in water temperatures have affected tiger shark habitats and movements in the North Atlantic Ocean. The study reveals that rising temperatures have caused the sharks to shift toward the poles over the past 40 years.



“Tiger shark annual migrations have expanded poleward, paralleling rising water temperatures,” explained study lead author Neil Hammerschlag. “These results have consequences for tiger shark conservation, since shifts in their movements outside of marine protected areas may leave them more vulnerable to commercial fishing.”



The researchers analyzed nine years of tracking data from satellite-tagged tiger sharks, combined with four decades of conventional tag and recapture data provided by National Oceanic and Atmospheric Administration (NOAA) Cooperative Shark Tagging Program.



The experts found that during the last decade of record heat, for every one-degree Celsius increase in water temperatures, tiger sharks migrated further poleward by over 400 kilometers. They also migrated two weeks earlier than usual to waters off the northeastern coast of the United States.



“Given their role as apex predators, these changes to tiger shark movements may alter predator-prey interactions, leading to ecological imbalances, and more frequent encounters with humans,” concluded Professor Hammerschlag.



Video Credit: University of Miami Rosenstiel School of Marine and Atmospheric Science



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Tiger sharks are shifting poleward as temperatures rise

Today’s Video of the Day from the University of Miami...

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> is focused on the melt ponds that emerge during the spring and summer on the Greenland Ice Sheet, which is the largest ice mass in the northern hemisphere.



"Melt ponds are vast pools of open water that form on both sea ice and ice sheets and are visible as turquoise-blue pools of water in this Copernicus Sentinel-2 image," says ESA.



"When snow and ice melts atop glaciers, water flows in channels and streams and collects in depressions on the surface. These melt ponds can speed up the melting of the surrounding ice since they greatly reduce the ice’s ability to reflect sunlight."



"This can create a positive feedback where an increasing number of melt ponds absorb more heat which causes ice cover to melt even faster."



According to ESA, Greenland has been hit with a late-season heatwave that began in early September. This caused the type of melt event that usually occurs in the middle of summer.



"In a recent paper published in Nature Climate Change, scientists found that major sea-level rise from the melting of the Greenland ice cap is now ‘inevitable’ even if the burning of fossil fuels were to halt overnight," says ESA. "Using satellite observations of Greenland ice loss and ice cap from 2000 to 2019, the team found the losses will lead to a minimum rise of 27 cm regardless of climate change."



Video Credit: ESA&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Melt ponds on the Greenland Ice Sheet

[sendtonews key="qARzJPSabQ-2270617-12187" type="single"] Today’s Video of the Day from the...

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> describes how Earth is unique in our solar system for its ability to sustain liquid water on its surface. But now, the water cycle is shifting as the climate warms, and scientists must find ways to predict how these changes will affect water availability.



Overall, 96 percent of Earth's water is saltwater, and nearly all of freshwater is found in ice and groundwater. These sources of water are linked as it passes through solid, liquid and gas phases.



In a warmer climate, the water cycle will be transformed. It will be easier for water to evaporate and form clouds, and storms will become more frequent and intense. Some regions will get too much water, while others will be left without enough water. In addition, soil moisture will be lost - which threatens food security.



Scientists are using satellite data from over the last 40 years to track changes that are happening in the water cycle. This will ultimately help us prepare for extreme events and better manage our water resources, according to ESA.



Video Credit: ESA



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Tracking changes in Earth's water cycle

[sendtonews key="fxH3eJHEkQ-2010196-12187" type="single"] Today’s Video of the Day from the...

Saturn,-,High,Resolution,3d,Images,Presents,Planets,Of,The

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard Space Flight Center</a> features images of Saturn from NASA’s Hubble Space Telescope. The photographs capture the start of the mysterious "spoke season" on Saturn - when unexplained features appear on its rings. 



According to NASA, both the cause of the spokes and their seasonal variability have yet to be fully explained by planetary scientists.



"Like Earth, Saturn is tilted on its axis and therefore has four seasons, though because of Saturn's much larger orbit, each season lasts approximately seven Earth years. Equinox occurs when the rings are tilted edge-on to the Sun," explains NASA.



"The spokes disappear when it is near summer or winter solstice on Saturn. (When the Sun appears to reach either its highest or lowest latitude in the northern or southern hemisphere of a planet.) As the autumnal equinox of Saturn's northern hemisphere on May 6, 2025, draws near, the spokes are expected to become increasingly prominent and observable."



Experts believe that the spokes may be a product of the planet's variable magnetic field. When magnetic fields interact with solar wind, an electrically charged environment is created. This phenomenon is visible on Earth as the northern lights.&nbsp;



"Scientists think that the smallest, dust-sized icy ring particles can become charged as well, which temporarily levitates those particles above the rest of the larger icy particles and boulders in the rings," says NASA.



The spokes were first observed in the early 1980s by NASA's Voyager mission. Depending on the angle of the rings, the spokes can appear dark or light.



"Thanks to Hubble's OPAL program, which is building an archive of data on the outer solar system planets, we will have longer dedicated time to study Saturn’s spokes this season than ever before," said NASA senior planetary scientist Amy Simon, head of the Hubble Outer Planet Atmospheres Legacy (OPAL) program.



"Despite years of excellent observations by the Cassini mission, the precise beginning and duration of the spoke season is still unpredictable, rather like predicting the first storm during hurricane season."



Video Credit: NASA Goddard&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Mysterious "spoke season" captured on Saturn

[sendtonews key="Ccjk8KEMzv-2550719-12187" type="single"] Today's Video of the Day from NASA...

Closeup,Of,Fresh,Green,The,Napier,Bush,Grass,As,Animal

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Today’s Video of the Day from <a href="http://www.ntu.edu.sg/">NTU Singapore</a> reveals that some plants can remove toxic heavy metals from soil.&nbsp;



The researchers analyzed samples of various tropical plant species to test for levels of heavy metals and metalloids. The study showed that there are existing plants with high levels of these contaminants, which means that these species are great candidates for drawing pollutants out of the soil.&nbsp;



Among the plants examined in the study, 12 species had accumulated several types of heavy metals and metalloids. These plants are widely available, including species that are native to Singapore.



“In a small nation like Singapore, land may be repurposed to support new development plans, so it is important that we have a green and sustainable way to remediate land that is contaminated," said Professor Lam Yeng Ming.



"We set out to uncover how to better make use of tropical plants to do phytoremediation and through advanced characterization techniques, we showed how some of these tropical plant species can be an environmentally friendly and literally a 'green' way to remove contaminants in soil."&nbsp;



"Phytoremediation also has benefits of cost effectiveness, simplicity of management, aesthetic advantages, and long-term applicability and sustainability. The strategy prevents erosion and metal leaching by stabilizing or accumulating heavy metals, so that helps reduce the risk of contaminant spread.”



Video Credit: NTU Singapore



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

Plants help remove heavy metals from contaminated soil

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Today’s Video of the Day from the <a href="https://www.acs.org/">American Chemical Society</a> describes why herbicides are not as effective in killing weeds anymore. In the 20th century, chemical companies developed thousands of herbicides. The most commonly used herbicide was glyphosate, which was introduced in 1974.



Over the past few decades, dozens of species of weeds have evolved resistance to glyphosate. Depending on the site of action, the part of the plant that an herbicide interacts with, weeds may even be resistant to herbicides that have not been developed yet.&nbsp;



With increasing resistance to glyphosate and other herbicides, weeds are - once again - becoming a major concern for farmers.&nbsp;



Video Credit: American Chemical Society&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

Weeds are becoming increasingly resistant to herbicides

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Today’s Video of the Day from the <a href="https://www.jpl.nasa.gov/">NASA Jet Propulsion Laboratory</a> (JPL) describes a dust storm on Mars that was nearly twice the size of the United States. As the storm covered the southern hemisphere of the planet, some of NASA’s explorers had to delay their normal activities.



NASA’s Insight lander put itself in a "safe mode" for 11 days to conserve battery power because solar power was disrupted by the dust. The Ingenuity Mars Helicopter postponed flights until conditions improved.



"A fleet of NASA orbiters monitor Martian dust storms like this one and serve as lifelines to Earth by relaying data from the rovers and lander on the ground back to the team. This includes the Mars Reconnaissance Orbiter, MAVEN, and Odyssey," reports JPL.



"Dust storms like this recent one start close to the ground and are spread by wind as they rise – warming the cold Martian atmosphere."



The images in the video were captured by NASA’s Curiosity as the dust rolled in. A fleet of orbiters monitored the dust storm from above, relaying data from Mars’ explorers back to scientists on Earth.



Video &amp; Image Credit: NASA/JPL-Caltech/ASU/MSSS



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

NASA monitors giant dust storms on Mars

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