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https://www.youtube.com/watch?v=3Y4eLFNYrKE
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On the unforgiving landscape of North Greenland, temperatures drop and sunlight barely penetrates through the polar winter. It was here, however, that an international team of scientists found <a href="https://www.earth.com/news/predatory-worms-were-terror-beasts-half-a-billion-years-ago/#google_vignette" target="_blank" rel="noreferrer noopener">evidence of sea monsters</a> that would change our understanding of ocean life in the past.



This video captures the discovery of Timorebestia fossils that had been hidden for more than 500 million years in the Sirius Passet formation. The "terror beasts," as they are called, are a hidden chapter in the evolutionary history of <a href="https://www.earth.com" target="_blank" rel="noreferrer noopener">Earth</a>, showing that sophisticated predator-prey interactions occurred much earlier than previously envisioned.



Dr. Jakob Vinther and his research team at the <a href="https://www.bristol.ac.uk/" target="_blank" rel="noreferrer noopener">University of Bristol</a>, in collaboration with researchers at the <a href="https://eng.kopri.re.kr/" target="_blank" rel="noreferrer noopener">Korean Polar Research Institute</a>, braved extreme weather conditions at 82.5 north latitude to locate these giant creatures. Using sophisticated electron microprobe analysis, they revealed the detailed anatomy of the animals, including their muscle and nerve tissues.



The find upsets the traditional timeline of sea predators. Although we've long appreciated that Cambrian oceans were at one time ruled by <a href="https://www.youtube.com/watch?v=jWI3-UgA3_o&amp;list=PL1QLQMW9MWDwpkFOnvgAmu7wT6rZmYqdJ&amp;index=19" target="_blank" rel="noreferrer noopener">arthropods</a>, these discoveries indicate that relatives of arrow worms were first to dominate the seas. These worms were building sophisticated food webs several million years before other predator groups arose.



Each fossil is a story of ancient hunger, with fossil stomach contents revealing these meter-long beasts dined on heavily armored arthropods regularly, cementing their place as the ocean's first apex predators.



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Worms dominated seas before dinosaurs

https://www.youtube.com/watch?v=3Y4eLFNYrKE On the unforgiving landscape of North Greenland, temperatures drop and sunlight barely penetrates through the polar winter. It was here, however, that an international team of scientists found evidence of sea monsters that would change our understanding of ocean life in the past. This video captures the discovery of Timorebestia fossils that had been hidden for more than 500 million years in the Sirius Passet formation. The "terror beasts," as they are called, are a hidden chapter in the evolutionary history of Earth, showing that sophisticated...

For many people, mornings don’t really begin until the first sip of coffee. That drink doesn’t just wake the body - it flips a switch in the mind. Researchers at Bielefeld University and the University of Warwick wanted to know why coffee feels so uplifting in the morning compared with the afternoon.



The team followed young adults in Germany for several weeks. Each person tracked their mood and reported whether they had consumed caffeine in the last 90 minutes. 



The results were clear. <a href="https://www.earth.com/news/drinking-coffee-may-reduce-frailty-in-aging-adults/">Coffee</a> and other caffeinated drinks boosted happiness and enthusiasm. The effect was strongest within two and a half hours of waking. Later in the day, the effect weakened.



<h2 class="wp-block-heading" id="h-morning-coffee-resets-our-mood">Morning coffee resets our mood</h2>



<a href="https://www.earth.com/news/coffee-helps-bacteria-resist-antibiotics-in-your-gut/">Caffeine</a> didn’t only improve positive feelings. It also reduced negative ones like sadness and being upset. But that change was smaller and less reliable. Unlike the morning lift in happiness, this effect didn’t depend on the time of day.



The difference may lie in how caffeine works. It blocks adenosine receptors in the brain. This lifts energy and increases dopamine activity. 



Dopamine is tied to alertness and mood. Together, these changes explain why the morning cup feels like such a mental reset.



<h2 class="wp-block-heading" id="h-do-people-react-differently">Do people react differently?</h2>



The team expected to see differences based on mental health, anxiety, or caffeine habits. But they didn’t. 



"We were somewhat surprised to find no differences between individuals with varying levels of caffeine consumption or differing degrees of depressive symptoms, anxiety, or sleep problems," noted Justin Hachenberger from <a href="https://www.uni-bielefeld.de" target="_blank" rel="noreferrer noopener">Bielefeld University</a>.



"The links between caffeine intake and positive or negative emotions were fairly consistent across all groups."



This result suggests that caffeine’s emotional effects are widely shared. People who react badly to caffeine may avoid it, so they were not strongly represented in the study. 



<h2 class="wp-block-heading" id="h-the-withdrawal-question">The withdrawal question</h2>



Scientists also debated whether the morning boost is real or simply relief from overnight withdrawal. 



"<a href="https://www.earth.com/news/coffee-may-help-you-live-longer-if-you-drink-it-this-way/">Caffeine</a> works by blocking adenosine receptors, which can increase dopamine activity in key brain regions - an effect that studies have linked to improved mood and greater alertness," explained Professor Anu Realo from the <a href="https://warwick.ac.uk" target="_blank" rel="noreferrer noopener">University of Warwick</a>.



"Even people with moderate caffeine consumption can experience mild withdrawal symptoms that disappear with the first cup of coffee or tea in the morning." 



In other words, coffee may feel good not only because of brain chemistry but also because it takes away the drag of going without caffeine during sleep.



<h2 class="wp-block-heading" id="h-mood-changes-depend-on-coffee-use">Mood changes depend on coffee use</h2>



The research showed that tiredness and social setting also change how caffeine feels. When people were more tired than usual, <a href="https://www.earth.com/news/can-caffeine-slow-down-aging-yeast-may-hold-the-answer/">caffeine</a> gave them a bigger mood boost. 



When people were around others, the effect weakened. Social interactions may have already shaped mood, leaving caffeine less noticeable.



Negative feelings like worry didn’t shift much. Researchers think these emotions are tied to long-term stress or life events. That makes them harder to change with one drink. Positive emotions, on the other hand, respond more quickly to stimulation.



<h2 class="wp-block-heading" id="h-global-link-between-coffee-and-mood">Global link between coffee and mood </h2>



"Around 80 percent of adults worldwide consume caffeinated beverages, and the use of such stimulating substances dates far back in human history," said Professor Sakari Lemola from Bielefeld University, the study’s senior author. 



"Even wild animals consume caffeine; bees and bumblebees prefer nectar from plants that contain caffeine."



Coffee is more than a drink. It is part of daily routines across cultures. Yet researchers warn against drinking too much. High doses can disturb sleep and increase dependence. Over time, stopping suddenly can trigger headaches, irritability, and fatigue.



<h2 class="wp-block-heading" id="h-mood-boost-from-morning-coffee">Mood boost from morning coffee</h2>



The study shows caffeine works best early in the day. It makes people feel happier, more awake, and more enthusiastic. But the effect doesn’t grow stronger with each cup. It fades as the day goes on.



For most people, moderation is the key. That first cup can brighten the morning, but too much can backfire. 



Coffee may not solve deeper worries or stress, but it can lift the mood enough to start the day with energy.



The study is published in the journal <a href="https://www.nature.com/articles/s41598-025-14317-0" target="_blank" rel="noreferrer noopener">Scientific Reports</a>.



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Mood boost: How coffee makes us happier in the morning

For many people, mornings don’t really begin until the first...

In 2024, the world’s climate continued to break records, with greenhouse gas concentrations and global temperatures reaching unprecedented highs.



The oceans absorbed more heat than ever before. Sea levels climbed to their highest point on record, and glaciers shed more ice than in any prior year.



This year’s State of the Climate report, published by the <a href="https://www.ametsoc.org/ams/">American Meteorological Society</a>, brought together 589 scientists from 58 countries. 



The experts used data from satellites, weather stations, ocean buoys, and ice-core records. For decades, this report has been the go-to snapshot of Earth’s climate - tracking key changes and <a href="https://www.earth.com/news/2024-confirmed-as-earths-hottest-year-in-recorded-history/">extreme events</a> across the globe.



<h2 class="wp-block-heading" id="h-greenhouse-gases-hit-highest-levels">Greenhouse gases hit highest levels</h2>



Carbon dioxide, methane, and nitrous oxide all set new records in 2024. Average CO2 levels reached 422.8 parts per million, up 52% from pre-industrial times. The jump from 2023 matched the fastest increase seen in the past 60 years.



Fossil fuel burning and agriculture remain the biggest sources. Rising greenhouse gases are locking in more heat, driving stronger feedback loops like higher water vapor in the <a href="https://www.earth.com/news/climate-extremes-in-2024-what-have-we-learned/">atmosphere</a> and changes in how land stores carbon.



<h2 class="wp-block-heading" id="h-heat-breaks-climate-records-again">Heat breaks climate records again</h2>



For the second year in a row, the planet broke its surface temperature record. Readings were up to 0.72°C (1.30°F) above the 1991-2020 average. 



A strong El Niño that began in mid-2023 and ended in spring 2024 helped push temperatures higher.



Heat extremes weren’t limited to the tropics. Europe, Asia, and South America saw their hottest years yet. Heatwaves lasted longer and struck at times of year when they used to be rare.



<h2 class="wp-block-heading" id="h-extreme-rain-and-drought">Extreme rain and drought</h2>



Warmer air holds more moisture, and in 2024 it showed. The atmosphere carried record levels of water vapor. One in five areas on Earth hit all-time highs, double the share from 2023.



Heavy rain events set records too. Dubai saw 250 mm in one day - three times its yearly average. While some places were drowning, others faced persistent droughts and extreme heat.



<h2 class="wp-block-heading" id="h-ocean-heating-breaks-climate-records">Ocean heating breaks climate records</h2>



From January through June, sea surface temperatures refused to budge from record-breaking highs. 



The global average edged past the 2023 mark by 0.06°C (0.11°F) - a small number on paper, but significant in climate terms. A potent El Niño, layered on top of decades of steady warming, drove the surge.



Vast stretches of ocean endured marine heatwaves - bleaching coral reefs, pushing fish into new territories, and unsettling entire food webs. On average, the seas sweltered through 100 heatwave days in 2024, while cold spells were rare - just nine days across the year.



<h2 class="wp-block-heading" id="h-sea-levels-keep-rising">Sea levels keep rising</h2>



Oceans absorb over 90% of excess heat from greenhouse gases. In 2024, heat content down to 2,000 meters (6,562 feet) reached its highest ever. 



Global sea level hit a new high for the 13th year straight - over 10 centimeters (3.94 inches) above 1993 levels.



Warmer water expands, and melting ice from Greenland, Antarctica, and glaciers adds more volume. The result is higher flood risks and saltwater intrusion into freshwater supplies.



<h2 class="wp-block-heading" id="h-record-heat-at-the-poles">Record heat at the poles</h2>



The Arctic experienced its second-warmest year on record, with autumn setting an all-time high for temperatures.



In August, parts of the North American Arctic endured record high temperatures, and Norway topped 30°C (86°F) in September for the first time that late in the year.



Antarctica’s sea ice stayed far below average. Minimum and maximum extents were the second lowest ever recorded, continuing a run of poor ice years since 2016.



For the second consecutive year, all 58 reference glaciers lost ice in 2024. It was the worst year for glacier loss in the 55-year record. Venezuela lost its last glacier. In Colombia, the Conejeras Glacier vanished completely.



These losses threaten water supplies for farming, hydropower, and drinking water in many mountain regions.



<h2 class="wp-block-heading" id="h-storms-bring-destruction">Storms bring destruction</h2>



There were 82 named tropical cyclones in 2024, fewer than average but still deadly. Hurricane Helene flooded parts of the U.S., killing more than 200 people. 



Hurricane Milton hit Florida less than two weeks later - setting a state record for the shortest gap between two major hurricanes.



In Asia, Super Typhoon Yagi tore through China and Vietnam, leaving more than 800 dead. Many storms intensified unusually quickly, fueled by warmer <a href="https://www.earth.com/news/astonishing-global-heat-in-january-2025-defied-climate-expectations/">ocean</a> waters.



<h2 class="wp-block-heading" id="h-our-changing-climate-reality">Our changing climate reality</h2>



“The State of the Climate report is an annual scientific landmark,” said American Meteorological Society President David J. Stensrud. 



"It is a truly global effort, in which hundreds of researchers from universities, government agencies, and more come together to provide a careful, rigorously peer-reviewed report on our planet’s climate."



"High-quality observations and findings from all over the world are incorporated, underscoring the vital importance of observations to monitor, and climate science to understand, our <a href="https://www.earth.com/news/earth-is-just-three-years-away-from-dangerous-carbon-milestone/">environment</a>." 



According to Stensrud, the results affirm the reality of our changing climate, as global temperatures continue to reach record highs.



The research is published in the <a href="https://www.ametsoc.org/ams/publications/bulletin-of-the-american-meteorological-society-bams/state-of-the-climate/" target="_blank" rel="noreferrer noopener">Bulletin of the American Meteorological Society</a>.



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State of the Climate 2024: Record heat and rising seas

In 2024, the world’s climate continued to break records, with...

If you live around Naples, you know the ground breathes. Streets crack, the harbor silts up, steam curls from the earth, and swarms of small quakes rattle windows. All that action comes from Campi Flegrei, a wide “supervolcano” caldera that last erupted in 1538.



For years, many scientists have read these signals as classic signs of magma on the move. But two recent studies - one in March 2023 and another in May 2025 - have reshaped the picture.



Together, they tell a story that is both sobering and surprisingly hopeful: Campi Flegrei is still dangerous, but some of its most disruptive <a href="https://www.earth.com/news/volcano-eruptions-alerts-shear-wave-signals-discovered-that-could-transform-early-warning-systems/">behavior may be managed</a>.



<h2 class="wp-block-heading" id="h-studying-campi-flegrei-in-2023">Studying Campi Flegrei in 2023</h2>



The <a href="https://pubs.geoscienceworld.org/gsa/geology/article/51/4/397/620796/Discriminating-carbon-dioxide-sources-during" target="_blank" rel="noreferrer noopener">2023 paper</a> focused on carbon dioxide (CO₂), a gas that volcanoes <a href="https://www.earth.com/news/volcanic-cooling-not-warming-caused-a-major-mass-extinction/">release in large amounts</a>. CO₂ matters because it often increases when magma rises and starts to degas, which can precede eruptions. 



At the Campi Flegrei caldera, CO₂ measurements at the <a href="https://www.researchgate.net/figure/a-Geologic-map-of-the-Solfatara-Pisciarelli-area-from-this-study-UTM-projection_fig2_351100327" target="_blank" rel="noreferrer noopener">Solfatara-Pisciarelli zone</a> rose during the current unrest (which began in 2005), reaching roughly 4,000-5,000 tons per day - among the highest volcanic CO₂ fluxes on Earth. 



If one looked only at that trend, one might conclude that magma was moving upward and a countdown to an eruption had begun.



The authors investigated further. They examined gases such as nitrogen and helium alongside CO₂ and compared the real data to what their models predicted if magma degassing were the only driver. 



The numbers did not line up. 



Beginning in 2005, the gas ratios drifted away from the “<a href="https://www.earth.com/news/the-sun-affects-magma-formation-deep-within-the-earth/">pure magma</a>” pattern, matching two surface indicators: hydrothermal temperatures and the steady ground uplift known locally as bradyseism.



<h2 class="wp-block-heading" id="h-where-was-the-gas-coming-from">Where was the gas coming from?</h2>



What was adding CO₂ if not just magma? The 2023 study pointed to a second source: <a href="https://www.earth.com/news/plants-and-trees-predict-volcano-eruptions-when-viewed-from-space-satellites/">the hydrothermal system</a> heating the rocks themselves. 



In plain language, hot, reactive fluids were <a href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/decarbonation" target="_blank" rel="noreferrer noopener">decarbonating calcite</a> (a carbonate-rich mineral) in the shallow reservoir rocks and releasing additional CO₂. The team estimated that this non-magmatic source contributed about 20-40% of total CO₂. 



That finding did not make the volcano harmless - far from it - but it did change how scientists interpret gas alarms.



A spike in CO₂ at Campi Flegrei does not automatically mean magma is surging. Sometimes it means the hydrothermal system is getting hotter and more pressurized, which can still be hazardous but in a different way.



<h2 class="wp-block-heading" id="h-studying-campi-flegrei-in-2025">Studying Campi Flegrei in 2025</h2>



Fast forward 14 months to May 2025. A second group of scientists <a href="https://www.science.org/doi/10.1126/sciadv.adt2067" target="_blank" rel="noreferrer noopener">published a study</a> that asked a bigger question: what, exactly, is driving the recent bursts of earthquakes and the dramatic rise and fall of the ground? 



They pulled together two major episodes of unrest - 1982-1984 and 2011-2024 - then compared the patterns of uplift, seismicity, and subsurface imaging. 



In the lab, they simulated the rocks above the caldera using a setup like a moka pot, the stovetop espresso maker. 



A heated lower chamber (representing a <a href="https://www.earth.com/news/geothermal-energy-is-cheap-and-clean-and-having-its-moment/">geothermal reservoir</a>) pushed fluid into a cracked “lid” made of Campi Flegrei-like materials. The result of all that detective work was a new model with a crucial twist.



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2024/12/supervolcano_campi-flegrei_location-satellite-view_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2024/12/supervolcano_campi-flegrei_location-satellite-view_1s.webp" alt="Satellite view Phlegraean Fields and Solfatara crater showing a massive caldera supervolcano named Campi Flegrei west of Naples, Italy. It is part of the Campanian volcanic arc, which includes Mount Vesuvius. Credit: Geology" class="wp-image-1982065"/></a><figcaption class="wp-element-caption">Satellite view Phlegraean Fields and Solfatara crater showing a massive caldera supervolcano named Campi Flegrei west of Naples, Italy. It is part of the Campanian volcanic arc, which includes Mount Vesuvius. Click image to enlarge. Credit: Geology</figcaption></figure>



<h2 class="wp-block-heading" id="h-how-supervolcano-pressure-builds">How supervolcano pressure builds</h2>



The central actor behind the building pressure inside Campi Flegrei is not a blob of rising magma in the upper crust; it is a capped geothermal reservoir sitting beneath the town of Pozzuoli. The caprock above it is fibrous and “self-healing,” which means cracks can seal up quickly. 



When the lid seals, water and steam trapped below it build pressure. Pressure builds until the rocks fracture, the water flashes to steam, producing a burst of shaking and noise - a pattern residents report. 



Interestingly, the <a href="https://www.earth.com/news/volcanic-tremors-can-now-be-detected-to-forecast-eruptions/">earthquakes in these sequences</a> tend to start shallow and then deepen over time, which is the opposite of what you would expect if magma or its gases were pushing upward from depth. 



After big episodes, the land actually sinks a bit, consistent with fluids discharging and pressure dropping.



<h2 class="wp-block-heading" id="h-why-does-any-of-this-matter">Why does any of this matter?</h2>



Here is the hopeful part. If the main driver of unrest is pressure in a closed, fluid-filled reservoir, then you can manage the fuel. 



You cannot turn off the “burner” heating the system - the deep magmatic heat source - but you can reduce the amount of water available to pressurize the reservoir. 



The researchers propose practical steps: restore and maintain surface-water channels so heavy rains do not funnel into the system; monitor and control <a href="https://www.earth.com/news/groundwater-has-a-vital-role-in-ecosystem-survival/" target="_blank" rel="noreferrer noopener">groundwater levels</a>; and, where appropriate, relieve pressure by withdrawing fluids through wells. 



Think of it like tending a radiator: keep the system from clogging or overfilling, and bleed off pressure before it blows a gasket.



<h2 class="wp-block-heading" id="h-campi-flegrei-eruption-risk">Campi Flegrei eruption risk</h2>



What does that mean for eruption risk? It does not mean Campi Flegrei is safe. A <a href="https://www.nhm.ac.uk/discover/what-is-a-supervolcano.html" target="_blank" rel="noreferrer noopener">supervolcano caldera</a> with Campi Flegrei’s eruptive history still sits atop a large population. Magma is still present at depth. 



The 2023 work showed that the hydrothermal system has been heating and releasing CO₂ in ways that track with ground uplift, while the 2025 work argues that pressure in the sealed geothermal reservoir can trigger swarms of shallow quakes and potentially steam-driven explosions (phreatic blasts). 



Both of those issues can be destructive, even without lava.



The new approach does not “turn off” a magmatic eruption if deep melt intrudes; it aims to prevent or reduce the kind of fluid-pressure crises that have damaged buildings and frightened residents for decades.



<h2 class="wp-block-heading" id="h-shifting-focus-and-mindset">Shifting focus and mindset</h2>



The key takeaway is a shift in mindset. For decades, <a href="https://www.usgs.gov/observatories/cvo/science/volcano-monitoring" target="_blank" rel="noreferrer noopener">volcano monitoring</a> focused on watching and warning: measure gases, track quakes, map ground motion, and be ready to evacuate. That is still essential. 



But if groundwater and surface runoff are a big part of the problem, civil engineers and geoscientists can work together on prevention.



They can unclog centuries-old drainage canals, divert stormwater, measure groundwater levels like a cardiologist tracking blood pressure, and - where science and policy align - use wells as pressure valves. 



None of this is a silver bullet for Campi Flegrei, or anywhere else. It requires careful design, community buy-in, and constant monitoring. 



But this appears to be a rare case in which a supervolcano’s most pressing threat is not an unstoppable magma surge; it is a pressure system that we might learn to regulate.



The full 2023 study was published in the journal <a href="https://pubs.geoscienceworld.org/gsa/geology/article/51/4/397/620796/Discriminating-carbon-dioxide-sources-during" target="_blank" rel="noreferrer noopener">Geology</a>.



The full 2025 study was published in the journal <a href="https://www.science.org/doi/10.1126/sciadv.adt2067" target="_blank" rel="noreferrer noopener">Science Advances</a>.



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Supervolcano shows signs of waking up, which is not a good thing, but scientists have a plan

If you live around Naples, you know the ground breathes....

Extreme heat pushes the heart to work harder. On humid days, that strain can quickly shift from tolerable to dangerous - and a new analysis shows just how steeply the risk of weather-related heart problems rises.



Researchers in Dhaka, Bangladesh report that the chance of a cardiovascular emergency visit rises sixfold on days that are both extremely <a href="https://www.earth.com/news/astonishing-global-heat-in-january-2025-defied-climate-expectations/">hot</a> and very humid, compared with hot days when the air is much drier.



<h2 class="wp-block-heading" id="h-how-humidity-makes-heat-worse">How humidity makes heat worse</h2>



First author Mostafijur Rahman, an assistant professor of environmental health sciences at the Celia Scott Weatherhead School of Public Health (<a href="https://sph.tulane.edu/" target="_blank" rel="noreferrer noopener">SPH</a>) and Tropical Medicine at <a href="https://sph.tulane.edu/trmd/home" target="_blank" rel="noreferrer noopener">Tulane</a> University, led the research with collaborators in Bangladesh and the United States.



Humidity matters because sweat must evaporate to cool the body, and water-laden air stalls evaporation. The resulting strain raises body <a href="https://www.earth.com/news/more-heat-cleaner-air-the-surprising-ozone-connection/">temperature</a>, increases skin blood flow, and can load the heart with extra work that some people cannot sustain.



As humidity climbs, the same thermometer reading feels much hotter to the body. That mismatch helps explain why ordinary heat advisories sometimes fail to capture the real risk for people with heart disease.



“These findings show we need to consider heat and humidity together when we discuss any kind of climate change policy,” said Rahman, who noted that the size of the effect surprised the team.



<h2 class="wp-block-heading" id="h-heart-risks-intensified-by-high-humidity">Heart risks intensified by high humidity</h2>



The researchers counted 340,758 emergency department visits for heart conditions during the hot months from 2014 to 2019 and matched those days to weather records. 



Heat alone raised risk on low humidity days, but risk jumped far higher on the muggiest days when relative humidity exceeded roughly 82 percent.



High heat in the analysis was defined as above 84 degrees Fahrenheit, which raised heart related emergency visits even without intense humidity. There was no separate link between humidity alone and heart emergencies, yet humidity amplified heat <a href="https://www.earth.com/news/extreme-temperatures-are-killing-thousands-across-india/">effects</a> across age and sex groups.



“Hopefully governments will be spurred to develop systems to warn cities of dangerous heat and humidity. We know extreme heat can have a negative health impact, but I never expected such a dramatic increase in risk when high humidity is also factored in,” said Rahman.



The pattern is consistent with clinical experience. When sweat fails to evaporate, the heart must move more blood toward the skin for cooling, while dehydration and electrolyte loss further stress the system.



<h2 class="wp-block-heading" id="h-humidity-and-public-health-warnings">Humidity and public health warnings</h2>



Hot extremes are becoming more frequent and more intense as the planet warms, and that trend is evident with every additional 0.9 degrees Fahrenheit of global warming, according to the Intergovernmental Panel on Climate Change (<a href="https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_SPM.pdf" target="_blank" rel="noreferrer noopener">IPCC</a>).



Independent research also links moist summer air to higher rates of heart, coronary, and stroke hospitalizations in older adults in the United States, even after accounting for temperature. 



A long-term analysis of about 63 million Medicare beneficiaries found higher cardiovascular hospitalization risks with higher summer-specific humidity.



Laboratory and field <a href="https://pmc.ncbi.nlm.nih.gov/articles/PMC10231239/" target="_blank" rel="noreferrer noopener">studies</a> add biological context. They show that humid heat undermines sweat evaporation and raises the physiologic load on the heart, validating the Dhaka pattern.



These threads point to one conclusion. Health systems and public warnings need to treat humidity as a co-equal driver of heat danger, not just a background variable.



<h2 class="wp-block-heading" id="h-access-to-cooling-matters">Access to cooling matters</h2>



Dhaka’s results are particularly relevant in places where home air conditioning is rare. Recent national survey <a href="https://www.seforall.org/taxonomy/term/38" target="_blank" rel="noreferrer noopener">reporting</a> in Bangladesh shows that only about 2.28 percent of households owned an air conditioner in 2023, a small rise from 1.6 percent in 2021.



Global analyses identify Bangladesh among countries with large populations at high risk due to a lack of access to affordable, sustainable cooling. Those gaps create exposure that individuals cannot easily avoid during multi day hot spells.



“There are billions around the world, from Southeast Asia to Africa, who are directly impacted by rising temperatures but have little access to air conditioning,” said Rahman. 



Equity is central here. The people least able to afford cooling often live and work in buildings and neighborhoods that trap heat, and they may have the most to lose from heart strain.



<h2 class="wp-block-heading" id="h-adapting-to-heat-and-humidity">Adapting to heat and humidity</h2>



Clinicians already flag combined heat and humidity as a risk for people with heart disease, heart failure, high blood pressure, prior stroke, and older age. 



Public guidance now acknowledges that humid heat can drive blood pressure swings and raise hospitalizations for those with cardiovascular conditions.



City agencies should tune heat warnings to humidity, not just temperature thresholds. Emergency managers could extend hours for cooling centers, stagger outdoor work schedules, and coordinate hydration and medication checks with community groups.



Individuals should plan around the weather forecast on humid <a href="https://www.earth.com/news/earth-is-just-three-years-away-from-dangerous-carbon-milestone/">hot</a> days. Small steps such as shortening exertion, spacing outdoor tasks, and favoring shaded or air conditioned spaces can spare the heart avoidable stress.



Health systems can prepare for surges. Hospitals and ambulance services can adjust staffing based on heat and humidity forecasts, which now provide advance warning of the most extreme events.



<h2 class="wp-block-heading" id="h-heart-risks-of-humidity-are-clear">Heart risks of humidity are clear</h2>



The Dhaka study is observational, and it uses outdoor weather to represent exposure, which cannot capture every indoor environment or personal behavior. 



Even so, the same day link between humid heat and heart emergencies aligns with physiology and persisted across sensitivity tests in the analysis.



Public agencies should incorporate humidity explicitly in heat alert systems. Common composites such as the <a href="https://journals.ametsoc.org/view/journals/apme/61/10/JAMC-D-22-0021.1.xml" target="_blank" rel="noreferrer noopener">heat index</a> were not designed for extreme combinations of temperature and humidity, and updated methods could improve their performance.



The Dhaka data highlight a simple truth: on hot, muggy days, the heart works overtime, and treating humidity as a key hazard in planning can save lives.



The study is published in the journal <a href="https://www.sciencedirect.com/science/article/pii/S0048969725018601?via%3Dihub" target="_blank" rel="noreferrer noopener">Science of The Total Environment</a>.



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Extreme heat and humidity sharply raise heart risks

Extreme heat pushes the heart to work harder. On humid...

River otters have roamed the shores and inlets of Chesapeake Bay for a long time. But there’s still a lot we don’t know about how they interact with their environment. What do they eat? Where do they hang out? And oddly enough - where do they go to the bathroom?



To answer these questions, researchers in Maryland spent nearly a year observing river otters and collecting data on their habits. 



The team, based at the <a href="https://serc.si.edu/" target="_blank" rel="noreferrer noopener">Smithsonian Environmental Research Center</a> (SERC), analyzed scat samples and habitat use to better understand the otters’ diet, behavior, and exposure to parasites.



Study senior author Dr. Katrina Lohan is a parasite ecologist and head of the Coastal Disease Ecology Laboratory at SERC.



“River otters in the Chesapeake Bay eat a wide range of animals, including those that live in the water and on land. <a href="https://www.earth.com/news/parasites-help-worker-ants-live-much-longer-lives/">Parasites</a>, too, are crucial parts of their diet,” said Dr. Lohan. "We also found that river otters use manmade structures for latrines or choose areas with specific characteristics.”



<h2 class="wp-block-heading" id="h-otter-poop-on-the-dock">Otter poop on the dock</h2>



It all started with an email. A colleague spotted some odd, watery scat on a dock and sent a message to Dr. Lohan. Inside the scat was a bright red worm. 



Cameras later confirmed that the dock had become a favorite toilet spot for a local river otter. This was the beginning of a full-scale study.



Graduate researcher Calli Wise took the lead on collecting samples. Over 11 months, she gathered scat from 18 active otter latrines. On average, each latrine held about 28 scat piles.



“Scats usually smelled strongly of fish and were full of scales or <a href="https://www.earth.com/news/new-invasive-crustacean-species-discovered-in-the-mediterranean/">crustacean</a> shells,” Wise said. “We wore gloves and used sterile tools and tubes to collect scat samples, to avoid contamination with other DNA.”



<h2 class="wp-block-heading" id="h-otter-toilets-are-social-hotspots">Otter toilets are social hotspots</h2>



The latrines aren’t just toilets. Otters use them to mark territory with urine and feces, but they’re also social spaces. 



Otters gather there to eat, play, and rest. The latrines often show signs of repeated use: flattened grass, worn vegetation, and nearby cover.



Most were located near the shoreline. The researchers found that otters liked areas with woody debris and easy access to the water. 



Some latrines stood out. Five were found directly on man-made features like docks, boardwalks, or stairs leading to the water.



<h2 class="wp-block-heading" id="h-what-the-otter-poop-reveals">What the otter poop reveals</h2>



The team used two main methods to analyze the samples: metabarcoding, which identifies DNA fragments, and traditional microscopy. Both approaches helped piece together what the otters had been eating - and what else they might be spreading.



“We collected most scats in the summer, when river otter diet is likely diverse,” Wise said. “We found evidence of invasive species like common carp and white river <a href="https://www.earth.com/news/bright-coloration-in-crayfish-does-not-serve-an-evolutionary-purpose/">crayfish</a> in river otters’ diet.”



The otters also ate American blue crabs, other fish, and crustaceans. Occasionally, they even consumed <a href="https://www.earth.com/news/how-ducks-balance-water-pressure-while-diving/">ducks</a> or <a href="https://www.earth.com/news/over-40-of-amphibians-face-extinction-due-to-escalating-climate-threats/">amphibians</a>.



But diet was just one layer. The scat also showed which parasites the otters were exposed to - either through their prey or directly. Most parasites infected teleost fish, the primary type of fish eaten by otters. A few may have infected the otters themselves.



“It is possible that river otters, like other top predators, wouldn’t be able to find enough food to eat without parasites,” noted Dr. Lohan.



<h2 class="wp-block-heading" id="h-why-parasites-might-be-a-good-thing">Why parasites might be a good thing</h2>



The researchers couldn’t identify every parasite. Gaps in DNA databases made some sequences impossible to match. They also couldn’t link poop to specific otters, so individual diets remain a mystery.



Still, the findings suggest otters might be playing an even bigger role in the ecosystem than we thought.



“Since so many of the parasites are actually infecting otters’ prey, it could mean that river otters are culling sick individuals from the populations they are preying upon,” explained Dr. Lohan.



Removing infected animals could reduce the spread of disease and even affect the gene pool of prey species. Sick animals don’t get to reproduce if they’re eaten. There’s also a potential connection to human health.



“Some of the parasites that infect river otters could potentially also infect humans, who also are mammals,” said Dr. Lohan. “Thus, we could use river otters as ‘disease sentinels,’ and study them to learn about what public health threats occur in certain areas.”



This study opens new questions about how river otters influence, and are influenced by, their environment. Their poop tells stories about what they eat, where they go, what parasites they host, and what role they might play in managing disease in coastal ecosystems.



And in Chesapeake Bay, it turns out those stories often start at a latrine - sometimes even on a dock.



The full study was published in the journal <a href="https://www.frontiersin.org/journals/mammal-science/articles/10.3389/fmamm.2025.1620318/full">Frontiers in Mammal Science</a>.



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What river otter poop reveals about life in Chesapeake Bay

River otters have roamed the shores and inlets of Chesapeake...

Sometimes, a white dwarf isn’t just a white dwarf. What seems ordinary at first glance can have a much more dramatic origin. That’s what astronomers discovered when they took a closer look at a star called WD 0525+526.



This compact, Earth-sized star appeared to be typical - but it wasn’t. Scientists found that it’s actually the aftermath of a stellar collision: two stars that crashed together and merged into one.



<h2 class="wp-block-heading" id="h-white-dwarf-with-a-violent-history">White dwarf with a violent history </h2>



White dwarfs mark the final stage of life for stars like our Sun. These stellar remnants are incredibly compact. One can pack more mass than the <a href="https://www.earth.com/news/team-creates-video-showing-the-sun-in-gamma-rays-over-a-14-year-period/">Sun</a> into a body no bigger than our planet. Most white dwarfs are born when a single star burns through its fuel and collapses.



But there’s another, rarer path. Sometimes two stars - often in a close <a href="https://www.earth.com/news/first-binary-star-system-d9-found-near-supermassive-black-hole-sagittarius-a-milky-way/">binary system</a> - collide and merge. The result is an ultra-massive white dwarf. That’s what happened with WD 0525+526, and this is the first time scientists have confirmed a merger origin based on ultraviolet evidence.



“It's a discovery that underlines things may be different from what they appear to us at first glance,” said Boris Gaensicke, principal investigator of the Hubble program at the <a href="https://warwick.ac.uk/" target="_blank" rel="noreferrer noopener">University of Warwick</a>. 



“Until now, this appeared as a normal white dwarf, but Hubble's ultraviolet vision revealed that it had a very different history from what we would have guessed.”



<h2 class="wp-block-heading" id="h-white-dwarf-transformed-by-a-merger">White dwarf transformed by a merger </h2>



Located 128 light-years from Earth, WD 0525+526 is 20% more massive than the Sun. Visually, it looks like any other white dwarf. But scientists used NASA’s Hubble Space Telescope and its ultraviolet capabilities to peer deeper into the star’s composition.



<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://youtu.be/nyWuLSIoosk?si=LgE0ox4Vv6Ojgx-Q
</div><figcaption class="wp-element-caption">Astronomers using NASA’s Hubble Space Telescope have found a rare ultra massive white dwarf formed from a stellar merger.</figcaption></figure>



The ultraviolet spectrum revealed something unexpected: <a href="https://www.earth.com/news/webb-finds-largest-amount-of-carbon-ever-seen-in-a-planet-forming-disk/">carbon</a> in the star’s atmosphere. Normally, white dwarfs formed from a single star have atmospheres made up of hydrogen and helium. Their carbon and oxygen are buried in the core, hidden under thick atmospheric layers.



Mergers, however, change the outcome. When two white dwarfs - or one and another type of star - crash into each other, the resulting explosion can strip away much of that outer hydrogen and <a href="https://www.earth.com/news/global-helium-supply-running-low-race-is-on-to-prevent-the-next-shortage/">helium</a>. What’s left is a thinner atmosphere, where carbon can leak up from the core and become visible.



<h2 class="wp-block-heading" id="h-detecting-carbon-in-the-star-s-atmosphere">Detecting carbon in the star's atmosphere</h2>



WD 0525+526 is hotter and more massive than the handful of other known merger-born white dwarfs. At nearly 21,000 kelvins (around 37,000 degrees Fahrenheit), it’s too hot for convection - the usual process that stirs carbon up into a white dwarf’s outer layers.



So how did the carbon get there? The researchers think a more subtle mechanism called semi-convection is at play. It’s a gentler process, but still powerful enough to pull a small trace of carbon to the surface.



What’s truly remarkable is how little carbon is in this star’s atmosphere - about 100,000 times less than what’s been observed in other merger remnants. This made it nearly impossible to spot without the right tools.



“Hubble's Cosmic Origins Spectrograph is the only instrument that can obtain the superb quality ultraviolet spectroscopy that was required to detect the carbon in the atmosphere of this white dwarf,” said study lead author Snehalata Sahu from the University of Warwick.



<h2 class="wp-block-heading" id="h-hidden-white-dwarf-mergers">Hidden white dwarf mergers </h2>



The discovery builds on a 2019 study using ESA’s <a href="https://www.earth.com/news/gaia-reveals-moons-around-hundreds-of-asteroids/">Gaia mission</a>, which identified a group of unusually blue white dwarfs. Some of those were later confirmed as the products of mergers. WD 0525+526 is now the hottest and most massive member of that group.



Because carbon in ultra-hot white dwarfs is easier to detect in ultraviolet than visible light, it’s possible many more of these cosmic collision survivors are out there - hiding in the data, waiting to be found.



“We would like to extend our research on this topic by exploring how common carbon white dwarfs are among similar white dwarfs, and how many stellar mergers are hiding among the normal white dwarf family,” said study co-author Antoine Bedrad.



“That will be an important contribution to our understanding of white dwarf binaries, and the pathways to <a href="https://www.earth.com/news/the-true-nature-of-dark-matter-may-be-revealed-in-a-supernova/">supernova</a> explosions.”



The research is published in the journal <a href="https://www.nature.com/articles/s41550-025-02590-y" target="_blank" rel="noreferrer noopener">Nature Astronomy</a>.



Image Credit: NASA, ESA, STScI, Ralf Crawford (STScI)



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Hubble spots a white dwarf created in a violent star collision

Sometimes, a white dwarf isn’t just a white dwarf. What...

Millions of adults will lose at least one permanent tooth, and many will lose several more as the years go by. In the United States alone, an estimated 178 million people are missing at least one tooth, which explains why dentures and titanium implants replacements are so common.



Dentistry is now aiming for something better, a living replacement that feels and functions like the original. The idea is not science fiction anymore, and it is moving from animal studies toward carefully designed human trials.



<a href="https://dental.tufts.edu/people/faculty/pamela-yelick" target="_blank" rel="noreferrer noopener">Pamela C. Yelick</a> of <a href="https://dental.tufts.edu/" target="_blank" rel="noreferrer noopener">Tufts University</a> School of Dental Medicine leads one of the teams moving this vision toward the clinic. A recent study from her and colleague <a href="https://dental.tufts.edu/people/faculty/weibo-zhang" target="_blank" rel="noreferrer noopener">Weibo Zhang</a> have pushed the conversation onto the main stage.



<h2 class="wp-block-heading" id="h-dentures-as-tooth-replacements">Dentures as tooth replacements</h2>



Tooth loss is not rare, and the burden rises with age worldwide. About 7 percent of people 20 or older have complete tooth loss, and that figure reaches 23 percent for those 60 or older.



Modern implants are anchored directly to the jaw through osseointegration, a concept that traces back to Per Ingvar Brånemark’s mid twentieth century work with titanium and bone. 



The history matters because it explains why implants are stable, and also why they do not feel like natural teeth.



Natural teeth are suspended in the socket by the periodontal ligament, which provides sensation and micro movement control that <a href="https://www.earth.com/news/scientists-successfully-grow-human-teeth-in-a-laboratory-for-the-first-time/">implants</a> lack. That difference shows up as reduced tactile sensitivity with implants compared with natural teeth.



Load also travels differently through an implant than through a tooth root cushioned by ligament fibers. Over time, that can contribute to bone loss around the fixture and biological complications that sometimes lead to failure.



<h2 class="wp-block-heading" id="h-two-routes-to-living-teeth">Two routes to living teeth</h2>



One route grows a replacement as a tissue, using a scaffold that guides cells to assemble into a tooth. 



In a recent large animal <a href="https://pubmed.ncbi.nlm.nih.gov/39729491/" target="_blank" rel="noreferrer noopener">study</a>, researchers used decellularized tooth bud scaffolds seeded with human dental pulp cells, porcine dental epithelial cells, and endothelial cells. 



They then implanted these constructs into adult minipig jaws where they formed tooth like tissues including periodontal ligament. 



The other route tries to spark tooth development in place by presenting the right developmental signals to adult cells. 



<a href="https://pubmed.ncbi.nlm.nih.gov/40120109/" target="_blank" rel="noreferrer noopener">Teams</a> mapping the choreography of early human tooth formation are building a playbook that identifies the epithelial and mesenchymal cues needed to kick off organized growth.



<h2 class="wp-block-heading" id="h-tooth-roots-and-ligaments">Tooth roots and ligaments</h2>



The scaffold approach matters because the emerging structures were not inert. 



They developed <a href="https://www.earth.com/news/dental-pulp-stem-cells-from-extracted-wisdom-teeth-can-treat-multiple-diseases/">tooth</a> supporting ligament and mineralized tissues in the socket and progressed over a period of months, which brings the approach closer to human scale.



“Even creating a tooth root that you could put an artificial crown on, with living dental pulp in the middle, secured by periodontal ligaments instead of being screwed into the jaw, could be a huge improvement to a person’s oral health and in turn, systemic health,” said Yelick.



<h2 class="wp-block-heading" id="h-protein-helps-tooth-replacement">Protein helps tooth replacement</h2>



A separate line of work targets a specific protein, <a href="https://pmc.ncbi.nlm.nih.gov/articles/PMC7880588/" target="_blank" rel="noreferrer noopener">USAG-1</a>, that suppresses tooth formation. Blocking USAG-1 in mice rescued missing teeth caused by different genetic problems, and the same strategy produced new incisors in ferrets, which share a human-like replacement pattern.



“Moreover, a single administration was enough to generate a whole tooth,” stated <a href="https://toregem.co.jp/en/about" target="_blank" rel="noreferrer noopener">Katsu Takahashi</a>, whose group <a href="https://www.kyoto-u.ac.jp/en/research-news/2021-03-31" target="_blank" rel="noreferrer noopener">reported</a> the antibody treatment while at <a href="https://www.kyoto-u.ac.jp/en" target="_blank" rel="noreferrer noopener">Kyoto University</a>.



A humanized anti USAG-1 antibody has been advanced by industry collaborators, with investigators reporting that a phase 1 protocol has been finalized and preparations for future studies are underway. 



That marks the shift from animal proof of concept to testing for safety, dosing, and early signals of activity in people.



Financing updates from partners indicate plans to run the first in human study and to prepare for subsequent pediatric trials if early results support it. 



The initial clinical focus is congenital tooth agenesis in young children, where a therapy that triggers tooth development could change lifelong care. 



<h2 class="wp-block-heading" id="h-what-would-count-as-success">What would count as success</h2>



A living <a href="https://www.earth.com/news/tooth-enamel-analysis-suggests-early-eurasians-were-multiple-species-paranthropus-robustus/">tooth</a> would restore ligament mediated sensation, which helps people modulate bite force and detect grit or high spots. It would also reconnect to bone through tissues that are built to bear chewing loads.



Those features could reduce pain and bone loss around a replacement compared with a rigid post. 



They could also lengthen functional life compared with today’s devices, which often need repair or replacement after years of wear.



<h2 class="wp-block-heading" id="h-what-about-cost-and-complexity">What about cost and complexity</h2>



Cell based therapies will only reach clinics if they can be produced reliably and priced within reach of today’s prosthetic options. 



Sourcing compatible epithelial cells at the right developmental stage is a known challenge, and that is why teams built their scaffolds around young pig tooth buds while they refine ways to recruit a patient’s own cells.



Work with induced pluripotent stem cells (<a href="https://pmc.ncbi.nlm.nih.gov/articles/PMC9065891/" target="_blank" rel="noreferrer noopener">iPSC</a>s) is also moving forward, including efforts to make enamel forming cells and repair enamel defects. 



As methods improve, the main questions will be safety, quality control, and whether costs can compete with implant dentistry.



<h2 class="wp-block-heading" id="h-tooth-replacement-and-future-tech">Tooth replacement and future tech</h2>



An atlas of human fetal tooth development now details epithelial subpopulations and their signaling to mesenchyme. 



That resource gives researchers the specific factors and timing likely needed to nudge adult cells toward making a new tooth unit.



If those cues can be delivered precisely, either by a staged therapy in the jaw or by organoid-like constructs that finish maturing in the socket, dentists could one day replace a lost tooth with a living one that integrates, remodels, and feels like it belongs.



The study is published in <a href="https://academic.oup.com/stcltm/article/14/2/szae076/7933795" target="_blank" rel="noreferrer noopener">Stem Cells Translational Medicine</a>.



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The end of dentures: Science is about to help you regrow your own teeth

Millions of adults will lose at least one permanent tooth,...

On May 12, 2008, central China was hit by one of the deadliest earthquakes in recent memory. The magnitude 7.9 Wenchuan Earthquake struck along the edge of the Tibetan Plateau, triggering violent landslides across the steep slopes of the Longmen Shan - known as the Dragon’s Gate Mountains.



The disaster killed more than 69,000 people, but nearly a third of those deaths weren't from shaking alone. They came from geohazards - including more than 60,000 landslides that came tumbling down the mountains in the hours and days that followed.



Now, after nearly two decades of research, scientists at <a href="https://www.ucsb.edu/" target="_blank" rel="noreferrer noopener">UC Santa Barbara</a> and the University of Southern California say the story of that earthquake still isn’t over. Their recent study shows that the debris shaken loose by the quake is still working its way through the region’s rivers. 



The team tracked how sediment surged into the Min River and how it changed the river’s behavior - possibly for decades. And their work could help answer a deeper question: Do earthquakes build mountains, or wear them down?



<h2 class="wp-block-heading" id="h-a-river-loaded-with-debris">A river loaded with debris</h2>



When the quake hit, millions of tons of rock and soil collapsed into nearby streams. Much of it ended up in the Min River, which runs through the Longmen Mountains. The river became a conveyor belt for that debris.



Geologists call this "<a href="https://www.earth.com/news/rivers-show-widespread-change-from-human-activity/">sediment flux</a>" - the amount of material a river carries. It shows up in two forms. The first is suspended sediment, fine particles carried in the water, easy to measure. The second is bedload - coarser stuff like gravel and boulders that roll or bounce along the bottom. That’s harder to track.



“Before our work, people mostly focused on the sediment of very fine size,” said Gen Li, an assistant professor in UC Santa Barbara’s Department of Earth Science.



Suspended sediment is routinely measured by agencies around the world. But bedload? That’s trickier. You can’t collect it with a bottle. And during an event like the Wenchuan Earthquake, there's suddenly a lot of it.



Scientists have long suspected that this surge in bedload plays a big role in <a href="https://www.earth.com/news/mega-tsunamis-triggered-by-earthquakes-could-wipe-part-of-us-off-the-map/">post-quake flooding</a>. The idea is simple: if a riverbed fills with debris, the channel gets shallower. Then, when a flood comes, it spills over more easily. But proving this has been a challenge.



<h2 class="wp-block-heading" id="h-how-a-dam-became-a-natural-lab">How a dam became a natural lab</h2>



Back in 2001, the Sichuan Provincial Electric Power Company started building the Zipingpu Dam. By 2006, the reservoir began filling, just 20 kilometers downstream from where the Wenchuan Earthquake would later strike. It was an unintentional stroke of luck for science.



That dam turned into the perfect sediment trap. Shortly after the quake, Li and his collaborators - including researchers from the <a href="http://www.cjh.com.cn/eng/" target="_blank" rel="noreferrer noopener">Chinese Bureau of Hydrology</a> - began surveying it.



Daily data already existed for suspended sediment. What the scientists needed was the rest of the picture. They set out, year after year, using sonar to map the floor of the reservoir. 



Each expedition added a new layer to their data. Over time, they could measure how much total sediment had built up. From there, they did the math. Total sediment minus suspended sediment equals bedload.



<h2 class="wp-block-heading" id="h-when-earthquake-effects-last-a-decade">When earthquake effects last a decade</h2>



After the quake, the amount of total sediment in the Min River grew sixfold. But the real shock came with the bedload, which had increased 20 times. That is not normal. Bedload usually makes up about 20% of sediment in a mountain river. Here, it made up 65 percent.



The result didn’t surprise co-author Josh West. He had suspected that sediment flux would spike after a <a href="https://www.earth.com/news/can-we-detect-major-earthquakes-months-in-advance/">major earthquake</a>, especially in the form of increased bedload.



What did surprise the team was how long it lasted. The elevated sediment flow didn’t return to normal after a few years. It stayed high for at least a decade.



“In fact, from the data we’ve collected so far, there’s no evidence yet of the total sediment flux declining back to background levels,” West said.



“Usually, we think the influence from earthquakes may last, at most, a few years after the main shock,” said Professor Li. “But this data shows that this is not true.”



<h2 class="wp-block-heading" id="h-earthquakes-set-off-a-chain-reaction">Earthquakes set off a chain reaction </h2>



The study adds weight to a growing idea among scientists: the danger from <a href="https://www.earth.com/news/natural-disasters-are-on-the-rise-but-hazard-plans-are-inadequate/">natural disasters</a> doesn’t stop once the main event ends. Earthquakes can set off a chain reaction. One disaster leads to another.



“Earthquake-triggered landslides are a great example,” West said. “As we prepare for natural disasters, we often think of them as being discrete events. But what’s left out of that is the longer tail that follows.”



In other words, rebuilding too quickly - or rebuilding in the same way, in the same place - can be risky. The land has changed. Riverbeds are higher and <a href="https://www.earth.com/news/earthquakes-and-flood-zones-hidden-risks-in-the-pacific-northwest/">flood zones</a> are different. What was once a safe 10-year floodplain may now be a ticking time bomb.



<h2 class="wp-block-heading" id="h-do-earthquakes-build-mountains">Do earthquakes build mountains?</h2>



Earthquakes are thought to push up mountain ranges. But they also cause <a href="https://www.earth.com/news/landslide-predictions-could-become-94-percent-more-accurate/">landslides</a> that scrape them back down. So which effect wins?



Professor Li looked into this in an earlier study. He used satellite images to estimate that the Wenchuan Earthquake caused about three cubic kilometers of material to slide off the Longmen Mountains. “That is around half of the sediment flux of all the rivers in the world over one year,” he said.



Li also looked at how much rock the quake pushed upward. Turns out, it was about the same. That means the quake may have added and removed equal amounts of mass. Whether the mountain grows or shrinks depends on what happens next.



If the river can carry all that debris away quickly, the mountain stays tall. If the debris piles up and clogs the system, the mountain starts to erode. So far, the Min River has flushed out about 10% of the landslide debris over ten years.



“The fact that the pace was sustained for ten years was a surprise on its own,” West said. But predicting what happens in the next few decades is harder. Watersheds evolve and landscapes shift. The balance is fragile.



<h2 class="wp-block-heading" id="h-many-questions-remain">Many questions remain</h2>



Professor Li is now investigating why this particular river carried so much bedload. The 2015 Gorkha Earthquake in Nepal, for instance, didn’t trigger the same kind of sediment surge in Himalayan rivers. This suggests other factors are at play.



The rock itself might be the key. Its type, texture, and how it breaks apart all affect how much debris a quake generates. The size of the grains also matters. And how those grains move downstream is still being modeled.



Li’s team is now studying these patterns in more detail - using field data and computer models to understand how sediment flows over time.



“It’s very satisfying to have been able to quantify something that we’ve struggled to quantify before and that has a wide range of relevance, from hazards to long-term consequences for understanding the evolution of topography over long periods of time," said West.



The full study was published in the journal <a href="https://www.nature.com/articles/s41586-025-09354-8" target="_blank" rel="noreferrer noopener">Nature</a>.



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How earthquakes move mountains - and what comes next

On May 12, 2008, central China was hit by one...

Researchers analyzing images from the James Webb Space Telescope report 300 unusually bright objects that vanish from bluer filters yet appear in redder ones, a classic signature used to flag very distant systems.



Some of these sources almost certainly belong to a closer crowd wearing heavy dust. Others could sit far back in cosmic time, where our current playbook for how <a href="https://www.earth.com/news/oxygen-detected-in-most-distant-galaxy-yet-cosmic-dawn-jades-gs-z14-0/">galaxies</a> grow gets stressed.



The research was led by Liu Bangzheng “Tom” Sun and Haojing Yan in the Department of Physics and Astronomy at the University of Missouri (<a href="https://physics.missouri.edu/news/campus-and-community-outreach" target="_blank" rel="noreferrer noopener">UM</a>).



<h2 class="wp-block-heading" id="h-jwst-finds-300-bright-objects">JWST finds 300 bright objects</h2>



The <a href="https://iopscience.iop.org/article/10.3847/1538-4357/addbe0" target="_blank" rel="noreferrer noopener">study</a> sifted public JWST images across four deep fields and cataloged 300 very bright “dropouts,” then focused on 137 objects that also have mid infrared measurements, a combination that helps rule in or rule out distant candidates.



Their modeling shows that most of these luminous dropouts are nearby in cosmic terms, likely at redshift z ≈ 1–4, while a nontrivial slice could be truly distant at z greater than 6, a mix that demands careful follow up.



“These mysterious objects are candidate galaxies in the early <a href="https://www.earth.com/news/milky-way-galaxy-may-be-inside-a-giant-void-in-the-universe-explains-hubble-tension/">universe</a>, meaning they could be very early galaxies,” said Haojing Yan, co-author of the study.



<h2 class="wp-block-heading" id="h-redshift-and-early-galaxies">Redshift and early galaxies</h2>



As light travels for billions of years, its wavelength stretches to the red end of the spectrum, a shift that pushes early galaxies out of optical reach and into the infrared. 



JWST’s Near Infrared Camera, <a href="https://jwst-docs.stsci.edu/jwst-near-infrared-camera" target="_blank" rel="noreferrer noopener">NIRCam</a>, is purpose built for that stretch to observe redshifts and sees from 0.6 to 5.0 microns.



The Mid Infrared Instrument (<a href="https://jwst-docs.stsci.edu/jwst-mid-infrared-instrument" target="_blank" rel="noreferrer noopener">MIRI</a>) extends that reach to roughly 5 to 28 microns, giving astronomers an extra set of eyes that can be decisive when red colors come from dust instead of distance.



The broader context is moving quickly. <a href="https://arxiv.org/abs/2405.18485" target="_blank" rel="noreferrer noopener">Spectroscopy</a> with JWST has now been locked in galaxies beyond redshift 14, showing that luminous systems were present only about 290 million years after the Big Bang.



“As the light from these early <a href="https://www.earth.com/image/hundreds-of-galaxies-illuminate-the-early-universe/">galaxies</a> travels through space, it stretches into longer wavelengths, shifting from visible light into infrared,” said Yan, explaining redshift.



<h2 class="wp-block-heading" id="h-high-redshift-dropout-technique">High-redshift dropout technique</h2>



The team used the “dropout technique,” which flags an abrupt loss of flux blueward of the <a href="https://adsabs.harvard.edu/full/1995AJ....110.2519S" target="_blank" rel="noreferrer noopener">Lyman break</a> and a clear detection just redward of that break, a method pioneered in the 1990s and refined ever since.



“It detects high-redshift galaxies by looking for objects that appear in redder wavelengths but vanish in bluer ones,” said Bangzheng “Tom” Sun, referring to the dropout signature tied to absorption by neutral hydrogen.



Color cuts are only the start. The team estimated photometric redshifts using three independent spectral energy distribution fitting tools, including Le Phare and EAZY, to weigh high redshift solutions against dusty, lower redshift impostors.



Spectroscopy remains the gold standard. It breaks a galaxy’s light into its component wavelengths and nails down spectroscopic redshift when emission lines are identified, which is why the authors call for more follow up.



<h2 class="wp-block-heading" id="h-one-extreme-bright-galaxy">One extreme bright galaxy</h2>



Among the sample sits a known source in the CEERS field at <a href="https://arxiv.org/abs/1507.02679" target="_blank" rel="noreferrer noopener">redshift z = 8.68</a>, originally identified from ground based Keck data because its infrared color hinted at strong oxygen emission, then studied repeatedly with JWST.



Later <a href="https://arxiv.org/abs/2303.08918" target="_blank" rel="noreferrer noopener">observations</a> revealed active black hole signatures in the same redshift neighborhood, including broad H beta emission that points to an accreting nucleus embedded in a vigorously star forming host.



That kind of source shows how a single, very bright object can be luminous for multiple reasons, from intense star formation to an active nucleus, and why mid infrared measurements help disentangle the power sources.



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/08/potential-early-galaxies_300-observations_uds-field_JWST_UMissouri_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/08/potential-early-galaxies_300-observations_uds-field_JWST_UMissouri_1s.webp" alt="Graphic showing the mysterious objects with very high redshift, possibly early galaxies in the universe, that the University of Missouri researchers identified in their study. Credit: JWST/Bangzheng “Tom” Sun/University of Missouri" class="wp-image-1982072"/></a><figcaption class="wp-element-caption">Graphic showing the mysterious objects with very high redshift, possibly early galaxies in the universe, that the University of Missouri researchers identified in their study. Click image to enlarge. Credit: JWST/Bangzheng “Tom” Sun/University of Missouri</figcaption></figure>



<h2 class="wp-block-heading" id="h-early-galaxies-and-high-redshift">Early galaxies and high-redshift</h2>



The headline is not that every bright dropout is ancient, but that some probably are, and the brightest of those could stress current models if confirmed. 



Theoretical <a href="https://ui.adsabs.harvard.edu/abs/2023MNRAS.522.3986F/abstract" target="_blank" rel="noreferrer noopener">work</a> has shown that it is possible to reproduce many luminous early galaxies by dialing up star formation efficiency in massive halos at high density, yet the very brightest systems remain a challenge.



“Even if only a few of these objects are confirmed to be in the early <a href="https://www.earth.com/news/massive-black-hole-pushes-the-boundaries-of-whats-possible/">universe</a>, they will force us to modify the existing theories of galaxy formation,” said Yan.



Sun and Yan emphasize that spectroscopy will deliver the final word, since dusty galaxies at modest redshift can mimic the same colors that signal extreme distance. 



That caution is well placed, given how often the Lyman break can be confused with a strong Balmer break in redder, older systems.



The study is published in <a href="https://iopscience.iop.org/article/10.3847/1538-4357/addbe0" target="_blank" rel="noreferrer noopener">The Astrophysical Journal</a>.



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Mysterious bright objects found in space might be very early galaxies, or something else entirely

Researchers analyzing images from the James Webb Space Telescope report...

<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=Ow3JH03PqEQ
</div><figcaption class="wp-element-caption">New York is the site of the world's oldest forest.</figcaption></figure>



<h2 class="wp-block-heading" id="h-385-million-year-old-trees-discovered">385-million-year-old trees discovered</h2>



Scientists have uncovered something extraordinary just two hours north of New York City. The <a href="https://www.earth.com/news/worlds-oldest-forest-discovered-close-to-new-york-city/" target="_blank" rel="noreferrer noopener">world's oldest forest</a>, dating back 385 million years, offers a window into how Earth's first complex forests shaped our planet's atmosphere.



Located near <a href="https://townofcairo.com/" target="_blank" rel="noreferrer noopener">Cairo, New York</a>, in Greene County, these weren't merely primitive plants struggling to survive. These were sophisticated trees with root systems remarkably similar to modern forests. This ancient woodland predates dinosaurs by 140 million years.



<h2 class="wp-block-heading" id="h-the-cairo-forest-discovery">The Cairo forest discovery</h2>



385 million years ago, upstate New York was a tropical paradise near the equator. Thanks to continental drift, this ancient forest has traveled thousands of miles to its current location.



The fossil forest sits in an abandoned quarry, roughly half the size of a football field. This represents just a slice of what was likely a massive forest system stretching from New York into Pennsylvania.



Charles Ver Straeten, curator of sedimentary rocks at the <a href="https://www.nysm.nysed.gov/" target="_blank" rel="noreferrer noopener">New York State Museum</a>, made the discovery in 2009. While scouting the former highway department property, his trained eye spotted wandering patterns in the stone that looked like marine features.



<h2 class="wp-block-heading" id="h-revolutionary-age-and-preservation">Revolutionary age and preservation</h2>



The site contains 385-million-year-old rocks with fossilized woody roots forming horizontal patterns up to 18 feet (5.5 meters) wide. As Christopher Berry, a paleobotanist at Cardiff University, explains: "You are walking through the roots of ancient trees."



This discovery pushes back advanced tree evolution by millions of years. The research, published in <a href="https://www.cell.com/current-biology/home" target="_blank" rel="noreferrer noopener">Current Biology</a> in December 2019, fundamentally changes our understanding of when complex forests first emerged.



Researchers believe a massive flood buried the forest floor, creating perfect fossilization conditions. Over millions of years, sediment hardened into rock, preserving these root patterns like nature's time capsule.



<h2 class="wp-block-heading" id="h-meet-archaeopteris-the-first-modern-tree">Meet Archaeopteris: the first modern tree</h2>



The star of this ancient forest is Archaeopteris – not to be confused with the feathered dinosaur Archaeopteryx. This tree was far older and more revolutionary.



William Stein from <a href="https://www.binghamton.edu/" target="_blank" rel="noreferrer noopener">Binghamton University</a> describes the roots as "strikingly modern, essentially what you'd see outside in my yard right now." These weren't simple root systems you'd expect from ancient plants.



Some fossilized roots are six inches (15 centimeters) in diameter, forming 36-foot-wide (11-meter) patterns. These giants grew up to 65 feet (20 meters) tall with five-foot-diameter (1.5-meter) trunks.



<h2 class="wp-block-heading" id="h-climate-changing-impact">Climate-changing impact</h2>



These trees fundamentally changed Earth's environment. Kevin Boyce, a Stanford University geoscientist, explains how their deep roots triggered "weathering," chemical reactions that pulled carbon dioxide from the atmosphere.



This process dropped atmospheric CO2 levels from 10-15 times higher than today to roughly modern concentrations. These ancient trees helped create atmospheric conditions that made complex life possible.



<h2 class="wp-block-heading" id="h-ancient-forest-ecosystem">Ancient forest ecosystem</h2>



The forest was remarkably diverse. Scientists identified Eospermatopteris, palm tree-like plants with short roots that reached 30 feet (9 meters) tall but lacked woody structure. The forest also housed cladoxylopsids and a mysterious third species still being studied.



All reproduced through spores rather than seeds – millions of years before seeds evolved. This tropical environment had no grass, flowers, or flying insects, just towering trees creating Earth's first complex forest canopy.



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



Before this finding, the Gilboa forest, located 25 miles (40 kilometers) away, held the "oldest forest" title. Cairo's trees are 2-3 million years older, showing that complex forest ecosystems developed much faster than scientists believed possible.



Patricia Gensel, a <a href="https://www.unc.edu/" target="_blank" rel="noreferrer noopener">University of North Carolina</a> paleobotanist, notes: "The size of those root systems is really changing the picture. Even 20 years ago, researchers assumed trees with such complex root systems didn't evolve so early."



The Cairo site presents three unique root systems, suggesting Devonian period forests were diverse ecosystems with different trees occupying different environmental niches, much like today's forests.



<h2 class="wp-block-heading" id="h-modern-preservation-efforts">Modern preservation efforts</h2>



In 2022, New York State Senator Michelle Hinchey secured a $170,000 grant for the town of Cairo to construct specialized fencing around the fossil forest site. The town plans to conduct a feasibility study exploring the possibility of creating an educational center and working lab on-site.



Joe Hasenkopf, chair of the Cairo Planning Board, hopes to partner with educational institutions to create a research facility serving scientists, students, and the public.



<h2 class="wp-block-heading" id="h-lessons-for-today-s-climate">Lessons for today's climate</h2>



Why does a 385-million-year-old forest matter today? It shows how dramatically forests can change Earth's climate. These ancient woodlands created the atmospheric conditions supporting complex life.



Understanding how prehistoric forests transformed the planet helps us appreciate modern forests' critical role in addressing climate change. Forests remain Earth's most effective carbon capture systems.



These prehistoric trees changed Earth's atmosphere by pulling massive amounts of carbon dioxide from the air. As we face modern climate challenges, this ancient forest reminds us of trees' incredible power to transform our planet's environment.



The next time you walk through a forest, remember you're experiencing an ecosystem whose blueprint was established 385 million years ago in upstate New York. These ancient pioneers didn't just survive – they thrived and changed the world forever.



The full study was published in the journal Current Biology.



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Earth's oldest forest found in the United States

https://www.youtube.com/watch?v=Ow3JH03PqEQ New York is the site of the world's oldest...

<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=Veg4HmmRVZY
</div><figcaption class="wp-element-caption">Our bodies hits two 'aging cliffs' at these ages.</figcaption></figure>



<h2 class="wp-block-heading" id="h-scientists-map-exact-ages-when-your-body-rapidly-ages">Scientists Map Exact Ages When Your Body Rapidly Ages</h2>



Scientists have <a href="https://www.earth.com/news/human-bodies-begin-breaking-down-two-very-precise-ages/#google_vignette">discovered that aging</a> isn't the gradual, steady process many assume it to be. Instead, researchers from Stanford Medicine have found that our bodies undergo dramatic molecular changes at two specific ages: 44 and 60. This research, published in Nature Aging, reveals that aging happens in sudden bursts rather than smooth transitions.



<h2 class="wp-block-heading" id="h-two-waves-of-rapid-aging">Two waves of rapid aging</h2>



The Stanford study tracked over 135,000 different molecules and microbes in 108 participants aged 25 to 75 over several years. Results showed that 81% of all molecules studied exhibited non-linear changes, meaning they shifted dramatically at certain ages rather than changing gradually over time.



Michael Snyder, chair of genetics at Stanford School of Medicine and the study's senior author, noted significant findings. "We're not just changing gradually over time; there are some really dramatic changes. It turns out the mid-40s is a time of dramatic change, as is the early 60s. And that's true no matter what class of molecules you look at."



The first wave of changes occurs around age 44, affecting molecules related to alcohol metabolism, caffeine processing, lipid <a href="https://www.earth.com/news/age-related-changes-in-metabolism-dont-match-our-expectations/" target="_blank" rel="noreferrer noopener">metabolism</a>, <a href="https://www.earth.com/news/heart-disease-remains-the-leading-cause-of-death-worldwide/" target="_blank" rel="noreferrer noopener">cardiovascular disease</a>, and skin and muscle function. The second wave hits around age 60, involving changes in carbohydrate metabolism, immune regulation, kidney function, and again cardiovascular and muscle health.



<h2 class="wp-block-heading" id="h-what-happens-during-these-aging-bursts">What happens during these aging bursts</h2>



During the mid-40s transformation, researchers observed significant changes in how the body processes alcohol and fats. This period often coincides with increased stress levels in many people's lives, potentially contributing to lifestyle factors that accelerate these molecular shifts.



"It's possible some of these changes could be tied to lifestyle or behavioral factors that cluster at these age groups, rather than being driven by biological factors," Snyder explained. For instance, alcohol metabolism dysfunction might result from increased consumption during the typically stressful mid-40s period.



The changes at age 60 are perhaps less surprising, as this is when many age-related diseases begin to manifest more prominently. The molecular shifts affect immune function and kidney health, both critical for maintaining overall wellness as we enter our senior years.



<h2 class="wp-block-heading" id="h-latest-research-confirms-aging-patterns">Latest research confirms aging patterns</h2>



Recent 2025 studies have validated these findings. Research examining tissue samples from 76 people found similar aging patterns, noting an "inflection point" between ages 45 and 55.



Scientists discovered that blood vessels, particularly the aorta, age fastest among all body tissues. This vascular aging may drive aging in other body parts, highlighting cardiovascular health's central role in the aging process.



<h2 class="wp-block-heading" id="h-cellular-changes-and-microbiome-shifts">Cellular changes and microbiome shifts</h2>



The Stanford research revealed that these aging bursts affect our microbiome – the trillions of bacteria, viruses, and fungi living in and on our bodies. These microbial communities undergo substantial shifts during both aging periods, potentially affecting everything from digestion to immune function.



Additionally, researchers found that protein production and gene expression begin to fall out of sync as we age. This breakdown in cellular communication becomes especially pronounced during the two aging waves, contributing to the accumulation of damaged proteins associated with diseases such as <a href="https://www.earth.com/news/alzheimers-may-not-be-brain-disorder-important-data-was-fabricated/" target="_blank" rel="noreferrer noopener">Alzheimer's</a>.



<h2 class="wp-block-heading" id="h-health-implications-and-longevity-considerations">Health implications and longevity considerations</h2>



Understanding these aging patterns has important implications for healthcare strategies. Research suggests that people should pay particular attention to their health during their 40s and 60s, when these dramatic molecular changes occur.



Snyder emphasized the importance of proactive health measures. "I'm a big believer that we should try to adjust our lifestyles while we're still healthy," he noted. This might include increasing exercise to protect heart health and maintain muscle mass, or reducing alcohol consumption in the 40s as the body's ability to metabolize it declines.



<h2 class="wp-block-heading" id="h-new-approaches-to-anti-aging-treatment">New approaches to anti-aging treatment</h2>



Aging research has seen notable advances in 2025. Harvard Medical School scientists developed chemical cocktails that reverse cellular aging without genetic modification. These six combinations restored aged cells to youthfulness in under a week, offering safer alternatives to gene therapy.



Researchers identified new biomarkers like "InflammAge," a saliva-based test measuring chronic inflammation associated with aging. This non-invasive approach could change how we monitor aging and intervention.



<h2 class="wp-block-heading" id="h-future-directions-in-aging-research">Future directions in aging research</h2>



Emerging technologies including artificial intelligence, cellular reprogramming, and senolytic therapies, are opening new possibilities for extending healthspan. Companies develop treatments targeting aging's fundamental mechanisms rather than just managing age-related diseases.



The Stanford findings provide a roadmap for implementing preventive measures. Rather than waiting for symptoms, people can prepare for and potentially mitigate these predictable aging waves.



As aging understanding evolves, one thing becomes clear: aging isn't inevitable decline, but specific biological events we may learn to prevent or reverse. The key is recognizing when these transitions occur and taking proactive health steps during vulnerable periods.



The study was published in the journal <a href="https://www.nature.com/nataging" target="_blank" rel="noreferrer noopener">Nature Aging</a>.



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Scientists discover we age in bursts

https://www.youtube.com/watch?v=Veg4HmmRVZY Our bodies hits two 'aging cliffs' at these ages....

<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=PqlF0XKzHY4
</div><figcaption class="wp-element-caption">The hidden science behind tickling.</figcaption></figure>



<h2 class="wp-block-heading" id="h-scientists-discover-the-brain-s-tickling-command-center">Scientists discover the brain's 'tickling command center'</h2>



Researchers have finally solved one of humanity's most enduring mysteries: why we can't <a href="https://www.earth.com/news/after-centuries-of-debate-we-still-dont-know-how-tickling-works/" target="_blank" rel="noreferrer noopener">tickle</a> ourselves and what makes some people incredibly ticklish while others barely react? Recent scientific discoveries are revolutionizing our understanding of this peculiar human behavior.



<h2 class="wp-block-heading" id="h-breakthrough-discovery-in-the-brain">Breakthrough discovery in the brain</h2>



In 2023, Dr. Michael Brecht's team at <a href="https://www.hu-berlin.de/en" target="_blank" rel="noreferrer noopener">Humboldt University</a>-<a href="https://www.hu-berlin.de/en" target="_blank" rel="noreferrer noopener">Berlin</a> made a major discovery published in the <a href="https://www.cell.com/iscience/fulltext/S2589-0042(22)01991-5" target="_blank" rel="noreferrer noopener">journal Neuron</a>. They identified the brain's actual "tickling command center" – specific neurons in a region called the periaqueductal gray that control both tickling responses and play behavior.



When researchers used cutting-edge optogenetic technology to shut down these neurons in laboratory rats, something remarkable happened. The animals completely lost their ability to be tickled or engage in playful behavior.



"We found that global blockade of the rat periaqueductal gray with either muscimol or lidocaine interfered with ticklishness and play," the research team reported in their study.



<h2 class="wp-block-heading" id="h-two-types-of-tickling-revealed">Two types of tickling revealed</h2>



What we call "tickling" is two completely different phenomena, according to the latest research. Light tickling – that feathery sensation that makes you want to scratch – is essentially your body's sophisticated bug detection system. This alerts you to potential insects or parasites on your skin.



Deep tickling – the kind that makes you laugh uncontrollably – involves complex brain circuits and is fundamentally social. You literally cannot tickle yourself with this type of stimulation.



<h2 class="wp-block-heading" id="h-why-self-tickling-is-impossible">Why self-tickling is impossible</h2>



Your cerebellum acts like a prediction machine, recent findings show. When you move your own hand to touch yourself, your brain generates precise predictions about what you will feel and then cancels out the tickling sensation through neural inhibition.



When someone else tickles you, your brain can't predict their movements, so the full tickling response activates. It's like your brain's way of distinguishing between self and others.



<h2 class="wp-block-heading" id="h-individual-differences-explained">Individual differences explained</h2>



Individual differences in ticklishness depend on genetics, psychology, and even trust. Dr. Xinzhong Dong at <a href="https://www.jhu.edu/" target="_blank" rel="noreferrer noopener">Johns Hopkins University</a> notes that people with denser nerve endings tend to be more sensitive.



Psychological factors matter just as much. You respond more strongly when tickled by people you trust, and anxiety completely shuts down tickling responses. This explains why the same physical stimulus can produce completely different reactions depending on who's doing the tickling.



<h2 class="wp-block-heading" id="h-controlling-your-ticklishness">Controlling your ticklishness</h2>



Science offers answers for controlling your ticklishness. You can reduce tickling sensitivity through systematic desensitization – gradual exposure in controlled settings.



Dr. Konstantina Kilteni's 2025 research, published in <a href="https://www.science.org/doi/10.1126/sciadv.adt0350" target="_blank" rel="noreferrer noopener">Science Advances</a>, reveals another technique: place your hand on the tickler's hand. This allows your brain to partially predict the sensations, reducing the tickling response by up to 90 percent.



"Your brain is essentially learning to override its own reflexes," Kilteni explained in her review of tickling research.



<h2 class="wp-block-heading" id="h-evolutionary-purpose-discovered">Evolutionary purpose discovered</h2>



From an evolutionary perspective, tickling serves vital functions according to <a href="https://www.umd.edu" target="_blank" rel="noreferrer noopener">University of Maryland</a> researcher Dr. Robert Provine's extensive studies. It trains our defense reflexes for vulnerable body areas and facilitates social bonding between family members.



Tickling-induced laughter is actually one of the first forms of communication between infants and caregivers. "Tickle involves a neurological self/nonself discrimination, providing the most primitive social scenario," Provine noted in his research.



<h2 class="wp-block-heading" id="h-clinical-applications-emerge">Clinical applications emerge</h2>



Research shows people with autism spectrum disorder perceive touches as more ticklish than people without the condition. Investigating this difference could provide insight into brain differences and help advance autism research.



People with schizophrenia tend to experience self-touches similarly to external tickles, allowing them to essentially tickle themselves. This suggests altered sensory prediction mechanisms in the condition.



<h2 class="wp-block-heading" id="h-animal-research-reveals-universal-nature">Animal research reveals universal nature</h2>



Scientists have discovered that many species beyond humans are ticklish. Rats emit ultrasonic "laughs" when tickled, while chimpanzees, gorillas, and orangutans all respond to tickling stimulation.



This widespread occurrence across species suggests that tickling serves fundamental biological and social functions that evolved long before humans developed complex language and culture.



<h2 class="wp-block-heading" id="h-future-research-directions">Future research directions</h2>



Dr. Kilteni argues that tickling research deserves more scientific attention. "It is a complex interplay of motor, social, neurological, developmental, and evolutionary aspects," she stated in her recent review.



New haptic technologies and advanced research methodologies now permit scientists to investigate tickle sensation with unprecedented precision. Standardized experimental methods using mechanical tickling devices ensure consistent results across studies.



Recent findings published in Science Advances show that tickling research is opening new doors in neuroscience, potentially leading to a better understanding of social behavior, sensory processing, and neurological conditions.



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Scientists solve the mystery of tickling

https://www.youtube.com/watch?v=PqlF0XKzHY4 The hidden science behind tickling. Scientists discover the brain's...

<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=elr4948_uOU
</div><figcaption class="wp-element-caption">Dr. Ronald Mallett from the University of Connecticut reveals secret mission to create working time travel device.</figcaption></figure>



<h2 class="wp-block-heading" id="h-could-an-equation-truly-bend-time-a-physicist-s-decades-long-quest-to-rewrite-reality">Could an equation truly bend time? A physicist's decades-long quest to rewrite reality</h2>



Imagine the impossible: stepping back through time in a time machine, not in fantasy, but through a scientific endeavor driven by profound personal loss. For <a href="https://www.earth.com/news/astrophysicist-says-hes-cracked-the-equation-for-time-travel/" target="_blank" rel="noreferrer noopener">Dr. Ronald Mallett</a>, a distinguished astrophysicist and professor emeritus at the <a href="https://uconn.edu/">University of Connecticut</a>, this deeply human longing has fueled a lifelong mission. He claims to have discovered the equation that could unlock temporal displacement, pushing boundaries once deemed purely science fiction.



<h2 class="wp-block-heading" id="h-a-profound-grief-that-forged-a-vision">A profound grief that forged a vision</h2>



Mallett's extraordinary pursuit began with devastating tragedy in 1955. At merely 10 years old, he endured his father Boyd's sudden death—a television repairman whose passion for science had ignited a similar spark in his young son. Boyd Mallett, only 33, succumbed to a heart attack, leaving behind a grief-stricken child searching for solace.



That solace came through H.G. Wells' The Time Machine. Within its pages, Mallett found a captivating concept: "Time is only a kind of Space." These words transformed from a literary phrase into a guiding principle, becoming the driving force behind his unwavering commitment to unraveling time's fundamental mysteries.



<h2 class="wp-block-heading" id="h-from-humble-beginnings-to-academic-heights">From humble beginnings to academic heights</h2>



Mallett's journey was far from straightforward. After serving in the Air Force during the Vietnam War era, he utilized the GI Bill for higher education, earning his Ph.D. in physics from Pennsylvania State University in 1973 at the age of 28.



In 1975, he made history as the first African American professor in the University of Connecticut's physics department, achieving full professorship in 1987 before retiring in 2024 as professor emeritus.



Throughout these successful academic years, Mallett harbored his radical ambition as a closely guarded secret. "I kept my time travel goal a secret," he confessed. "I worried people would think I was nuts." His public research centered on black holes, serving as a "cover story" while he quietly developed his revolutionary time travel theory.



<h2 class="wp-block-heading" id="h-the-breakthrough-moment">The breakthrough moment</h2>



His pivotal insight arrived while hospitalized for a heart condition—a profound irony given his father's heart attack started this journey. The breakthrough was elegantly simple yet revolutionary: "If gravity can bend time, and light can create gravity, then light can bend time."



"It turns out that black holes can create a gravitational field that could lead to the creation of time loops that could allow us to go back in time," he explained.



<h2 class="wp-block-heading" id="h-the-blueprint-for-a-temporal-vortex">The blueprint for a temporal vortex</h2>



Mallett's vision for a functioning time machine replicates spacetime-warping phenomena around black holes. He offers a compelling analogy: "Picture a cup of coffee. Stir it with a spoon, and the coffee swirls. A spinning black hole does the same to spacetime."



In Einstein's general relativity, the universe is a dynamic fabric woven from space and time. Massive objects like black holes warp this fabric—an effect we perceive as gravity. Mallett theorizes that an intense, continuous, circulating beam of light from a ring of powerful lasers could replicate this gravitational torsion, effectively twisting time into a loop.



This "time loop" would theoretically allow information—or perhaps matter—to travel backward in time. He detailed this mathematical concept in his 2006 autobiography, Time Traveler: A Scientist's Personal Mission to Make Time Travel a Reality.



<h2 class="wp-block-heading" id="h-published-research-and-recognition">Published research and recognition</h2>



His work, published in respected journals including <a href="https://www.sciencedirect.com/journal/physics-letters-a" target="_blank" rel="noreferrer noopener">Physics Letters A</a> and <a href="https://link.springer.com/journal/10701" target="_blank" rel="noreferrer noopener">Foundations of Physics</a>, suggests circulating laser light could generate gravitational fields potent enough to create closed timelike curves, enabling time travel for data.



Mallett's research has gained worldwide media attention, featured on <a href="https://www.thisamericanlife.org/" target="_blank" rel="noreferrer noopener">National Public Radio's This American Life</a>, the <a href="https://www.history.com/" target="_blank" rel="noreferrer noopener">History Channel</a>, and <a href="https://www.today.com/" target="_blank" rel="noreferrer noopener">NBC's Today Show</a>. The widespread interest reflects both his compelling personal story and rigorous scientific approach.



<h2 class="wp-block-heading" id="h-the-galactic-hurdles-and-persistent-skepticism">The galactic hurdles and persistent skepticism</h2>



While Mallett's equations captivate imagination, the path to reality faces immense obstacles. The energy requirement is staggering—Mallett acknowledges needing "galactic amounts of energy," far beyond current technological capabilities.



There's also a poignant limitation: even if realized, his machine could only send information back to when it was first activated, meaning it couldn't transport him to 1955 to prevent his father's death.



The scientific community remains skeptical. Physicists Ken Olum and Allen Everett argue that Mallett's proposed laser ring would need to be larger than the observable universe to achieve the necessary spacetime distortion. They invoke Stephen Hawking's chronology protection conjecture, suggesting physics may prevent macroscopic time travel.



Astrophysicist Paul Sutter has voiced doubts about Mallett's underlying mathematics, while science writer Brian Clegg finds the concept intriguing enough to warrant experimental investigation.



<h2 class="wp-block-heading" id="h-a-legacy-that-transcends-time">A legacy that transcends time</h2>



Now approaching 80, Dr. Mallett remains steadfast. "I believe my work will show time travel is possible," he asserts. "Future generations will build on it in ways we can't yet imagine."



His equations, though yet to physically bend time, have bent our collective imagination. Ongoing public interest, evidenced by his continued media appearances and Spike Lee's film adaptation of his memoir, underscores his ideas' profound impact.



More than a scientific pursuit, Mallett's story testifies to human resilience, intellectual courage, and hope's enduring power. Whether his theoretical time machine ever materializes, his legacy is immeasurable—inspiring countless individuals to challenge conventional limits and perceive time not as an unyielding barrier, but as a boundless frontier awaiting exploration.







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Retired professor claims he solved time travel

https://www.youtube.com/watch?v=elr4948_uOU Dr. Ronald Mallett from the University of Connecticut reveals...

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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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https://youtu.be/XYgiPzmNBTU?si=eFYY7gPHU1JznLvU
</div></figure>



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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https://youtu.be/Ug657J67iEo?si=w96YjGMsg939LD_3
</div></figure>



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 the <a href="https://www.esa.int/">European Space Agency</a> features Nushagak Bay, a large estuary in southwest Alaska. Nushagak runs mainly north to south and exits in Bristol Bay, a large body of water in the Bering Sea.



"The bay is primarily fed by the Nushagak River, which begins in the Alaska Range and flows southwest approximately 450 km. The bay is also fed by several additional rivers including the Wood, Igushik, Snake and Weary rivers," says ESA.



"The dark colors of the Nushagak River are most likely due to tannins or lignins (chemical substances found in plants). Tannins and lignins from roots, leaves, seeds, bark and soil can leach into the water and give it a brown or even black colour. The sediments then flow southwards where it is mixed with the bluer waters of the bay."



Video/ Image Credit: ESA



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

Nushagak Bay in southwest Alaska

[sendtonews key="0ynNMYkMKa-2340414-12187" 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.acs.org/">American Chemical Society</a> (ACS) reveals that proteins on flu viruses are actually flexible, tilting and waving in a “breath-like” motion. According to the experts, these proteins could be used to better defend against the flu.



"The main antigenic targets of influenza virus are two surface glycoproteins, hemagglutinin (HA) and neuraminidase (NA). Whereas the structural and dynamical properties of both glycoproteins have been studied previously, the understanding of their plasticity in the whole-virion context is fragmented," wrote the researchers.



To investigate, the team conducted detailed simulations of the influenza A H1N1 virion, or the swine flu. The experts concluded that the visualizations show many new vulnerable states of flu viruses, which could improve future vaccines and antiviral drugs.



Video/ Image 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.

Flu viruses are more flexible than expected

[sendtonews key="G9bUoxcjr4-2511624-12187" 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> features Lake Trasimeno, which is located west of Perugia in central Italy. It is the fourth largest lake in the country. While Trasimeno’s water level varies, it has a maximum depth of approximately six meters.&nbsp;



"In this Copernicus Sentinel-2 image, captured on 6 August 2022, the lake’s emerald green colour is likely due to the presence of phytoplankton. Streaks in the water, particularly visible in the west, indicate the presence of soil and sediments which have been stirred up by winds. Dark colored waters in the southern part of the lake indicate a presence of submerged and floating macrophytes (aquatic plants) as well as algae," says ESA.



"Surrounded by hills on three sides, Trasimeno is subject to heavy storms created by winds, especially from the north and west. There are three islets in the lake: Maggiore, Minore and Polvese (the largest). The lake’s shores are sparsely inhabited with only two popular villages: Castiglione del Lago and Passignano sul Trasimeno."



"Italy is experiencing its worst drought in 70 years which has affected drinking water supplies, hydroelectric power and agricultural production. High temperatures, hot winds and lack of rainfall are the main causes of drought in the Umbrian region which saw Lake Trasimeno’s drop 1.3 m, reaching the limit of the hydrometric zero in July 2022."



Video/Image Credit: ESA&nbsp;



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

Lake Trasimeno in Central Italy

[sendtonews key="3upvlAaHgO-2256633-12187" 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.acs.org/">American Chemical Society</a> describes a new self-powered nanosensor that can instantly detect mercury contamination with the tap of a finger.&nbsp;



The oxidized form of mercury can be harmful when it is ingested through contaminated water or food. This makes it necessary for experts to develop sensors that can quickly and accurately detect the presence of mercury.&nbsp;



Zong-Hong Lin and colleagues have now created a triboelectric nanosensor (TENS) that can detect mercury by simply by touching a sample. According to the researchers, their TENS could serve as the basis for similar devices to safely and remotely monitor other pollutants.



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.

Detecting mercury contamination with the tap of a finger

[sendtonews key="LvS8v8bp9z-2564889-12187" 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> features Kainji Lake, a reservoir on the Niger River.



In 1968, Kainji Lake was created by the construction of the Kainji Dam. The Niger River, the third longest in Africa, enters the lake in the north.&nbsp;



According to <a href="https://www.earth.com/news/rivers-in-the-american-west-are-a-lifesaving-resource-for-birds/">ESA</a>, the creation of the lake submerged Foge Island and the town of Bussa and permanently flooded other riverine settlements, leaving around 50,000 people displaced.&nbsp;



Large parts of Foge Island are temporarily exposed during low water tides, and the land is often used by migrating fishermen. Kainji Dam is a dam across the Niger River in Niger State of Central Nigeria. 



Wild mammals occur at relatively low densities due to illegal hunting. Lake Kainji has suffered a dramatic decline as a fishery due to the high numbers of artisanal and subsistence fisherfolk using the lake. It has been suggested that a period of closure, together with controlled fishing rights may help improve fish stocks.



Kainji Lake National Park is the oldest of its kind in Nigeria. The park contains three distinct areas: a part of the Kainji Lake, the Borgu Game Reserve to the west of the lake, and the Zugurma Game Reserve to the southeast. The park is home to around 65 mammal species, 350 bird species, and 30 species of reptiles and amphibians. 



Video/ Image Credit: European Space Agency&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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Kainji Lake in north central Nigeria

[sendtonews key="iuA5mpp3jv-1641775-12187" type="single"] Today’s Video of the Day from the...

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