Earlier this year, astronomers alerted the world to a startling possibility: based on initial calculations, it appeared that a recently discovered asteroid known as 2024 YR4 had a not-zero chance of colliding with Earth in 2032. At 174–220 feet wide, the space rock has the potential to destroy a sizable city in less than a decade’s time. In this case, however, “not-zero” never amounted to anything higher than a three percent probability. And after gathering additional information from an array of terrestrial observatories as well as the James Webb Space Telescope, experts concluded in March that 2024 YR4 didn’t pose any direct threat to the planet.
But just because Earth was spared doesn’t mean our moon is safe. Based on the most recent calculations, the chance that the asteroid has a 2032 date with the lunar surface is higher than it ever was for us.
“The probability that asteroid 2024 YR4 will strike the Moon on 22 December 2032 is now approximately 4 percent, and this probability was still slowly rising as the asteroid faded out of view,” the European Space Agency said in its most recent update.
Okay, so it’s not that much more likely than 2024 YR4’s highest probability for Earth. But a 96-percent likelihood of missing the moon leaves room for the space rock to defy the odds. Astronomers will now need to wait until its orbit sends it around the sun in mid-2028 to begin conducting further observations.
So what happens if 2024 YR4 really does collide with the moon? That’s a great question—one that even the experts can’t answer at the moment.
“No one knows what the exact effects would be,” admitted ESA Planetary Defense Office director Richard Moissl. “It is a very rare event for an asteroid this large to impact the Moon—and it is rarer still that we know about it in advance.”
Moissl added the collision “would certainly leave a new crater on the surface,” but it’s not currently possible to accurately predict how much material would eject into space, and whether Earth’s gravitational pull would catch any of it. That said, there isn’t a major worry that an asteroid of 2024 YR’s size would result in lunar armageddon. Moissl also explained that while the impact would likely be visible from Earth, astronomers remain “excited by the prospect of observing and analyzing it.”
If you’re still uneasy about errant asteroids hurtling towards us, take comfort in knowing that international space agencies are working to improve our early detection capabilities and plan for worst-case scenarios. The ESA, for example, is currently planning to launch its Near-Earth Object Mission in the Infrared (NEOMIR) satellite in the early 2030s. NEOMIR is designed to position itself at the first Sun-Earth Lagrange Point, one of five locations where the planet’s gravitational forces and the satellite’s orbit interact to allow for a stable observation point. Once there, the array will be able to scan for unknown asteroids larger than 197-feet-wide that are potentially en route to Earth. This will provide governments and agencies much more time to identify, analyze, and plan for space emergencies.
“NEOMIR would have detected asteroid 2024 YR4 about a month earlier than ground-based telescopes did,” Moissl explained. “This would have given astronomers more time to study the asteroid’s trajectory and allowed them to much sooner rule out any chance of Earth impact in 2032.”
Utah State University physicist Jenny Whiteley’s Northern Utah home has recently given her and her family occasional glimpses of colorful auroras in the night sky.
“We’ve seen vibrant greens and purples, with moving, vertical white shafts of light,” says Whiteley, a doctoral student in USU’s Department of Physics. “It was fascinating to see the electrons trace out magnetic field lines above the Earth, which are always there but only visible under certain — and in our location — rare conditions.”
The ability to explain physical phenomena following mathematical logic is what attracts Whiteley to the study of physics.
“It’s amazing to me that mathematical expressions can be constructed to successfully replicate the physical behavior we see around us,” she says.
Whiteley, who is one of five USU graduate students selected this time last year for a 2024-2025 Utah NASA Space Grant Consortium Fellowship Award, is studying radiation-induced conductivity in the Materials Physics Group led by USU physics professor J.R. Dennison.
The lab’s team members perform ground-based testing of electrical charging and electron transport properties of both conducting and insulating materials, emphasizing studies of electron emission, conductivity, luminescence and electrostatic discharge.
The lab’s research is supported by NASA, the Air Force Office of Scientific Research and private aerospace companies.
“Among the topics studied in Dr. Dennison’s lab is how various materials behave in response to harsh conditions, such as space,” Whiteley says.
The space community, she notes, is highly focused on hazards posed to spacecraft and aircraft by static electricity, radiation and extreme temperatures.
Whiteley, who earned both bachelor’s and master’s degrees from USU, in 2021 and 2023, respectively, has spent much of the past year analyzing data from Idaho State University’s Idaho Accelerator Center (IAC) in Pocatello collected by previous group members.
“Dr. Dennison and his students have studied how to measure conductivity in highly insulating materials, such as polymers used in spacecraft,” she says.
Whiteley is preparing to conduct tests similar to those at the IAC, using much smaller and more compact instrumentation, here at Utah State.
“The USU Materials Physics Group now has instrumentation that can test radiation-induced conductivity in materials accurately and efficiently at a lower cost than the previously used method,” she says.
“Working with the new instrumentation will be fun,” Whiteley says. “I am looking forward to the hands-on aspects of this work, where we’ll set up experiments and determine how to collect data.”
The materials she and group members are testing, she points out, are insulators.
“By definition, they don’t conduct,” Whiteley says. “But because of the atomic level interaction between the radiation and the material, we sometimes get a surprise: conductivity. It is important to quantify this behavior to those choosing materials because of specific insulating properties so they aren’t caught unawares once ambient conditions change.”
The stakes are high, she says, as NASA and other space agencies plan for increasingly longer space missions. Spacecraft must endure grueling conditions.
Dennison says Whiteley, who was one of USU’s 2020 Goldwater Scholars, is among the most inquisitive scholars he’s ever met.
“Jenny is an ideal candidate to pursue a challenging research endeavor, because she’s naturally curious and never gives up,” he says. “She asks lots of questions, reads and listens to other scholars. She genuinely wants to understand difficult concepts and isn’t afraid of failure.”
That last quality, Dennison says, makes Whiteley an effective teacher as well as a researcher. Whiteley says one of the best parts of teaching is helping others move beyond bewilderment to confident comprehension.
“Teaching has given me the opportunity to internalize concepts at a much deeper level than what I understood when I took the class myself,” she says. “I really enjoy helping others who are overwhelmed by the physics concepts or by the volume of material hurled at them. It’s quite fun to help a student go from ‘I’m so confused” to ‘maybe I’ve got this.’”
On June 30, 1908, an asteroid about 65 meters wide collided with Earth’s atmosphere and exploded several miles above Siberia; the force of the blast flattened and burned millions of trees over an area of more than 2,000 square kilometers. Today, the anniversary of the Tunguska blast has become World Asteroid Day: a science holiday co-founded by a rock music legend and an Apollo astronaut.
In 2015, Apollo 9 lunar module pilot Rusty Schweickart helped launch World Asteroid Day with astrophysicist and Queen guitarist Brian May. The United Nations officially recognized the event a year later in 2016. Earlier this month, Arizona senator Mark Kelly – also a former astronaut – introduced a Senate resolution that, if passed, would officially recognize June 30 as World Asteroid Day in the U.S.
I spoke with Kevin Schindler, resident historian at Lowell Observatory in Arizona, about the origins of World Asteroid Day, the history of planetary defense, and what asteroids can reveal about the history of our Solar System.
Discovering the Danger from Outer Space
Around 200 years ago, in the 1830s, geologists began to study fossils and figure out that several mass extinctions had wiped out whole ecosystems of species on Earth in the distant past.
“In recent decades, they realized that those weren’t necessarily caused by something on Earth, but by something impacting from space – like the Cretaceous Tertiary boundary,” says Schindler.
An artist’s impression of a giant meteor impact.
NASA Goddard
In the 1960s, geologist Walter Alvarez discovered a thin layer of black clay in rocks around the world. Below the black line, the rocks were rich in fossils; above it, they were nearly barren. The same layer of black clay showed up all around in the world: in rock outcroppings in Italy and New Zealand, and in samples from the floor of the Pacific Ocean. And it clearly marked a deadly before-and-after moment in Earth’s history – one that happened around 66 million years ago.
Alvarez suspected that the black clay was something alien; it contained bizarrely large amounts of an element called iridium, which is vanishingly rare here on Earth but more common in asteroids. He began to realize that an asteroid or comet may have slammed into our planet 66 million years ago, kicking off a mass extinction and scattering iridium-rich black dust over the planet like a burial shroud.
The pieces came together in 1978 when geophysicists Glen Penfield and Antonio Camargo discovered the outline of a crater hundreds of kilometers wide at the edge of Mexico’s Yucatan Peninsula. Its center lies at the bottom of the Gulf of Mexico. Penfield and Camargo named the crater for one of the communities that now lies within its boundaries: Chicxulub Pueblo.
Other craters – smaller but still impressive – also make it obvious that our planet has had more than a few run-ins with meteors during its long history.
“And while there’s not as much debris floating around in our Solar System as when it was newly-formed, there’s still stuff out there,” says Schindler. “And it’s inevitable that at some point that stuff will come back and get us again.”
NASA’s Asteroid Watch tracks known asteroids and comets in the Solar System, while observatories … More like Lowell scan the skies for more.
NASA
From Deep Impact to DART
So we’ve known almost 60 years that asteroids and comets could threaten life on Earth.
“In the 1980s and 1990s, there was a search to look for bodies that specifically could impact Earth,” says Schindler. “Phase one of all this started with, ‘okay, let’s look for these bodies that could hit us,’ and then a couple decades later is when we got to phase two, ‘what can we do about it if we do find these things?’”
Strangely enough, it was a pair of high-budget, low-scientific-accuracy Hollywood blockbusters that really brought planetary defense to public attention, according to Schindler. The summer of 1998 featured not just one but two movies about humanity trying to save itself from extinction by blowing up an incoming chunk of space rock. In Armageddon, a wildly-improbable effort by a team of offshore drillers saves Earth from an asteroid impact; in Deep Impact, a similarly-improbable effort fails to save Earth from a comet (so the summer ends in a cinematic tie).
Two men in a space suit using a piece of machinery in a scene from the film ‘Deep Impact’, 1998. … More (Photo by Paramount Pictures/Getty Images)
Getty Images
“The good thing about those movies is that, even though they’re not scientifically accurate in every way, they certainly built awareness enough to where lawmakers said, you know, we should put some money aside to study this stuff more,” says Schindler. “Hollywood, in some ways, has helped the cause to learn more.”
And, as science fiction often does, Deep Impact and Armageddon provided thought experiments (albeit not super-accurate ones, to put it mildly) for the ideas that would eventually become actual efforts at planetary defense. According to Schindler, theoretical ideas about whether we could destroy an incoming meteor eventually shifted to ideas about just nudging the deadly object off-course.
“This is just something that’s really been developed in the last decade or so and – I wouldn’t say culminated, but really became well-known with the mission that went up to deflect the moon of an asteroid to see if it was possible,” says Schindler.
Artist rendering of the NASA Double Asteroid Redirection Test (DART) space probe approaching the … More asteroid Didymos and its minor-planet-moon Dimorphos. The DART spacecraft aims to collide with Dimorphos in autumn 2022 in order to study the effect of an impact with near-Earth objects. Created on September 13, 2021. (Illustration by Nicholas Forder/Future Publishing via Getty Images)
Future Publishing via Getty Images
That mission was NASA’s Double Asteroid Redirection Test, or DART, in which an intrepid little spacecraft flew 7 million miles to crash into the asteroid Dimorphos and knock it off-course. Dimorphos is actually a mini-moon that orbits another, larger asteroid called Didymos. Astronomers at Lowell carefully measured Dimorphos’s orbital path around its parent asteroid before and after the impact – and they saw evidence that DART had succeeded in knocking Dimorphos into a different orbit.
It’s a long, long way from deflecting one tiny asteroid moonlet onto a different path around its parent asteroid to deflecting something the size of the Chicxulub impactor – or even Tunguska – as it’s barreling toward Earth. But the consensus seems to be that DART was a good start.
“The biggest thing, I think, was that it is possible. This was a very controlled initial step,” says Schindler. “This was certainly promising enough that we should keep doing these tests in different sizes of body and different compositions, because depending on what it’s made of, a body might react differently to something impacting it.”
Fossils of the Early Solar System
This illustration depicts the 140-mile-wide (226-kilometer-wide) asteroid Psyche, which lies in the … More main asteroid belt between Mars and Jupiter.
NASA
Meanwhile, Schindler and World Asteroid Day also want the public to know that asteroids are more than potential threats: they’re an orbiting treasure trove of information about the history of our Solar System and even the origins of life.
Most asteroids are chunks of rock that coalesced early in our Solar System’s history but never grew massive enough to become planets; they’re like the seeds of planets that might have been. Others are the debris left behind by collisions between objects in those chaotic early days of the Solar System, when planets were forming and gas giants migrated, scattering lesser objects in their wake.
“They tell us what the early composition was and what a chaotic time it was in the early part of our Solar System,” says Schindler.
Those clues are written not just in the chemical and physical makeup of asteroids, but in their orbital paths around the Sun. By studying and modelling how those paths have changed over the years, scientists can reconstruct how asteroids and planets may have interacted. The orbits of modern asteroids are like the “footprints” of planet formation, migrating gas giants, and long-ago collisions.
Today, NASA’s Lucy mission is exploring the asteroid belt, getting up close and personal with several of these objects. Meanwhile, NASA’s OSIRIS-APEX mission is on its way to study the asteroid Apophis, which will pass close (but not too close!) to Earth in 2029.
The surface of asteroid Bennu, as seen by OSIRIS-REX in late 2020, is strewn with boulders.
NASA
“And now we are studying planetary systems around other stars. Better understanding our Solar System, we can now look at others and see how typical we are,” says Schindler. “You don’t know that without knowing your own Solar System pretty well, so it really has helped us to learn about, sort of, our heritage, I guess.”
World Asteroid Day
World Asteroid Day aims to tie all of those things together, promoting awareness of planetary defense but also of the immense scientific value – and maybe monetary value, eventually – of asteroids.
At Lowell Observatory, that awareness is hard to escape; the observatory stands just an hour’s drive from Meteor Crater – which is exactly what the name suggests, a 213-meter-deep, 1200-meter-wide crater where an object about the size of a Boeing 747 slammed into the desert floor around 50,000 years ago.
“The proximity of Lowell Observatory, where we’re studying bodies in space, and Meteor crater, where we’ve seen the result of one of those bodies hitting Earth – how convenient is that? We’re looking at both ends of it, from when it’s still up in space to the final product if something like this hits.”
When humans burst into laughter together, moods lift almost automatically. New research shows that a similar boost happens in our closest cousins.
An international team led by Indiana University scientists has discovered that bonobos become more upbeat after hearing the giggles of their companions. This finding pushes the evolutionary history of positive emotions back millions of years.
Laughter changed ape choices
To explore laughter’s influence, the researchers designed a cognitive-bias test often used in animal psychology to gauge optimism or pessimism.
First, they trained bonobos at the Ape Initiative in Des Moines, Iowa, to recognize two kinds of boxes: black ones that always contained a delicious snack and white ones that were always empty.
Once the apes consistently chose black and ignored white, the experimenters introduced a third, ambiguous gray box. They then played one of two sounds: recorded bonobo laughter or a neutral control noise.
“We know that other apes, like chimpanzees, have contagious laughter during play,” said lead author Sasha Winkler, a primatologist at Duke University. “We were wondering if that behavior could be explained by positive emotions produced from the sound itself.”
If the bonobos felt a surge of good feeling after hearing laughter, the team expected them to treat the uncertain gray box as if it were the rewarding black one.
That is exactly what happened. “Think of it like the rose-colored glasses effect,” Winkler said. “The bonobos were much more likely to approach the gray boxes after hearing laughter, treating them like the rewarded boxes, and indicating a more optimistic expectation of finding a treat.”
Tracing optimism to our ancestors
This study is the first experimental proof that great-ape laughter can shift mood and cognition the way human laughter does.
“The tendency to behave more optimistically after hearing laughter suggests that the sound alone induced a positive emotional state in bonobos,” said senior author Erica Cartmill, the director of Indiana University’s Cognitive Science Program.
“This is the first study of which we’re aware to measure a positive affect shift in nonhuman primates from a brief experimental intervention.”
Great apes – bonobos, chimpanzees, gorillas, orangutans – all emit play calls that acoustically resemble human chuckles. Earlier work tied those sounds to a common evolutionary origin. The new findings add a cognitive twist.
“Our results suggest that laughter in other apes shares not only phylogenetic and behavioral similarities with human laughter but also perhaps some of the same cognitive-emotional underpinnings,” Winkler noted.
“This emotional contagion appears to have been present in the primate lineage long before the evolution of language.”
Laughter, empathy, and apes
Emotional contagion is often described as a foundational element of empathy – the capacity to share another’s feelings. As Winkler put it, “studies like ours can help to untangle the evolutionary building blocks of empathy, communication, and cooperation in humans.”
By revealing that a simple vocal cue can brighten outlooks in bonobos, the research suggests that the mechanisms linking social sound to positive mood were already in place in a common ancestor millions of years ago.
Cartmill added that the work answers a long-standing bias in emotion research. “Our emotions influence many aspects of cognition, including memory, attention, and decision-making, but research has historically focused on negative emotions with clear behavioral correlates, like fear and aggression.”
“We wanted to better understand the relationship between positive affect and cognition in our closest living relatives.”
Kanzi and the future of empathy
The experiments involved four bonobos, including the celebrated language-using ape Kanzi, who recently passed away.
“I feel incredibly grateful to have had the opportunity to work with Kanzi while he was still alive,” Winkler said.
“We hope this brings greater public awareness of the remarkable similarities between us and bonobos, who are an endangered species. We have so much to learn from these incredible animals.”
Future studies will test whether laughter exerts similar cognitive effects in chimpanzees and other primates. They will also explore how social context – for example, hearing laughs from friends versus strangers – modulates optimism.
For now, the discovery that bonobo giggles brighten expectations highlights a shared emotional heritage and hints that a simple laugh has been boosting group spirits since long before humans walked the Earth.
The study is published in the journal Nature Scientific Reports.
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In June last year, astronomers scanning the sky from the remote deserts of Western Australia picked up a sudden, blinding burst of radio energy. The signal was so powerful, it temporarily outshone every other radio source in the sky, according to a report of CNN.
At first, the team at Curtin University believed they had discovered something extraordinary — perhaps a new type of astronomical object or an ultra-rare fast radio burst (FRB) from within our galaxy.
“We were really excited,” Dr. Clancy James, associate professor at Curtin’s Institute of Radio Astronomy, told CNN. “It looked like we had found an unknown object near Earth.” The data came from the ASKAP telescope, an advanced array of 36 large antennas spread across the Wajarri Yamaji Country in Western Australia. This setup is usually used to detect FRBs — intense, millisecond-long bursts of radio energy from distant galaxies, potentially caused by exotic phenomena like magnetars, the ultra-magnetic remains of dead stars.
These bursts are not only puzzling but also powerful tools for mapping the “missing” matter in the universe. But this particular signal wasn’t behaving like a normal FRB.
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Unlike typical FRBs that originate billions of light-years away, this burst appeared to be shockingly close — just 4,500 kilometers (2,800 miles) from Earth. When the team zoomed into the data, the image became blurry — a telltale sign the source was much closer than expected.After sifting through satellite databases, the astronomers matched the source to Relay 2, a long-defunct U.S. communications satellite launched in 1964. Relay 2 had been orbiting silently since its instruments failed in 1967.But this sparked an even more bizarre question: Could a dead satellite suddenly burst back to life?
A Flash from the Past The leading theory is an electrostatic discharge — a burst of energy caused by a buildup of electric charge on the satellite’s surface, similar to the shock you get from touching a doorknob after walking on carpet. When the charge releases, it can emit a sharp flash of radio energy.
While these discharges are common and often harmless, the intensity and brevity of this one — just 30 nanoseconds long — was unprecedented. In fact, it was 2,000 to 3,000 times brighter than any other signal the ASKAP instrument typically detects.
Another possibility, though less likely, is that a micrometeorite no larger than a grain of sand slammed into Relay 2 at extreme speed, causing a burst of plasma and radio waves. However, the team estimates there’s only about a 1% chance that was the cause.
Why This Matters Although this turned out to be a human-made source, the discovery underscores a major challenge in space research: the interference of space junk with astronomical observations. With over 22,000 satellites launched since the dawn of the space age — and thousands no longer functional — Earth’s orbit is becoming a crowded and unpredictable place.
Signals like the one from Relay 2 could easily be mistaken for cosmic phenomena, especially as ground-based observatories like ASKAP and upcoming arrays such as SKA-Low (Square Kilometre Array) continue to scan the skies for fast, faint signals.
While this unexpected “zombie signal” turned out to be from a defunct satellite, it opens up new possibilities for using radio telescopes to monitor aging spacecraft for signs of unusual activity.
Fieldwork at an exposed fossilized Caribbean reef located in the Dominican Republic
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Credit: Sean Mattson
When we think of fossils, giant prehistoric creatures like dinosaurs may come to mind. But the fossil record also holds the remains of smaller organisms, such as fish and corals, that tell us about our oceans’ past.
Scientists at the Smithsonian Tropical Research Institute (STRI) recently studied exposed fossilized coral reefs from Panama’s Bocas del Toro Province and the Dominican Republic, comparing them with nearby modern reefs. These exceptionally well-preserved reefs date back 7,000 years, offering a unique window into what Caribbean reefs looked like before human impact. Within the fine sediments of these ancient reefs, the team discovered thousands of tiny fish ear bones and shark scales, allowing them to reconstruct entire ancient fish communities.
The results revealed a dramatic shift in fish communities over time: sharks have declined by 75% and human-targeted fish have become 22% smaller. But the real surprise came from the prey fish species — those eaten by predators like sharks. These have doubled in abundance and grown 17% larger on modern reefs. This study provides the first historical evidence for the “predator release effect” — where removing top predators allows their prey to flourish. Whilst scientists have long predicted such an effect, evidence for it was scarce without knowing what reefs looked like before human impact. Remarkably, the tiniest reef fish that shelter in coral crevices, showed no change in size or abundance over millennia. Their stability suggests a remarkable resilience to the multitude of changes occurring on reefs at higher layers of the food chain.
To compare fossilized and modern reefs, scientists collected, quantified and measured thousands of skeletal remains, including the tiny tooth-like scales that give shark skin a sandpapery texture, called dermal denticles.
To study the abundance and size of prey fish and small coral reef-sheltered fish (also known as cryptobenthic fishes), they also examined fish otoliths — the calcium carbonate structures found in fishes’ inner ears. Because otoliths grow in layers, scientists can estimate a fish’s size at death. In total, the team examined 807 denticles and 5,724 otoliths.
The behavior of some organisms can also leave a fossil record. In this study, scientists measured the frequency and size of damselfish bite marks on coral branches from both fossilized and modern reefs. They found that the number of bites has increased in modern reefs — also indicating the rise in prey fish populations.
These results illustrate an important change in food webs of modern Caribbean reefs: with fewer sharks and other predatory fish to control the population of exposed prey fishes, they have become bigger and more abundant, reflecting release from predation. On the other hand, small reef-sheltered fish remained unchanged in size and abundance over thousands of years, suggesting that the degradation of water quality and habitat in the region did not drive the changes in community structure.
This study demonstrates the power of the fossil record for future conservation. By revealing what reefs looked like before intensive human fishing, these 7,000-year-old fossils provide the missing baseline critical to understand the food webs of pre-human coral reefs, and document which elements of reefs changed and which are resilient.
This research, published in the Proceedings of the National Academy of Sciences, PNAS, was a collaboration among scientists from the Smithsonian Tropical Research Institute (STRI), the Sistema Nacional de Investigación (SENACYT) in Panama, the Marine Science Institute at the University of Texas at Austin, the Center for Biodiversity Outcomes at Arizona State University, the Graduate School of Oceanography at the University of Rhode Island, The Nature Conservancy, the Biodiversity Research Center at Academia Sinica in Taiwan, the Department of Earth & Environmental Sciences at Boston College, and the Cotsen Institute of Archaeology and Department of Anthropology at the University of California, Los Angeles.
Journal
Proceedings of the National Academy of Sciences
Article Publication Date
30-Jun-2025
Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.
Washed foraminifera being picked for computer tomography and geochemical analysis
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Credit: University of Southampton
27 June 2025
UNDER EMBARGO UNTIL 20:00 UK TIME (15:00 U.S. EASTERN TIME) ON MONDAY JUNE 30, 2025
Scientists at the University of Southampton have developed a new way of analysing fossils allowing them to see how creatures from millions of years ago were shaped by their environment on a day-to-day basis for the first time.
The research published today [30 June] in Proceedings of the National Academy of Sciences could revolutionise our understanding of how character traits driven by environmental changes shaped evolutionary history and life on earth.
It could help scientists to understand how much of a species’ evolutionary journey is down to ‘nature vs nurture’.
Researchers from the University of Southampton studied the fossilised remains of prehistoric plankton using high-resolution 3D scanning, like a medical CT scan, to examine tiny fossil shells about the size of a grain of sand.
These plankton, called foraminifera or ‘forams’ for short, are tiny floating seashells that still live in the ocean today. Their shells are made of calcium carbonate and grow every few days by adding a new chamber to their shell in a spiralling pattern.
These chambers act a little like the rings of a tree trunk, providing a permanent record of the growth and lived environment of forams over time.
The shells’ chemical composition also tells us about the conditions the organism lived in, including the chemistry, depth and temperature of the water.
“The fossil record provides the most powerful evidence of biodiversity change on Earth, but it traditionally does so at a scale of thousands and millions of years,” says Dr Anieke Brombacher, lead author of the paper how carried out the research at the University of Southampton and now works at the National Oceanography Centre.
“These fossils however act a bit like chapter summaries of a species’ evolutionary story. This new way of analysing them lets us read the pages within each chapter – allowing us to see how individual organisms adapted to their changing environment, not over the course of generations but within an individual life span at day-to-day resolution.”
The key advance the researchers developed was to combine highly advanced CT scanning with chemical analysis by laser ablation techniques. This combination of methods meant the team was able to ‘zoom in’ and ‘read’ the individual pages of those chapters to reveal how the forams grew and estimate the environment they experienced while growing.
The growth rates of all three species were similar at low temperatures, but one species grew much faster in higher temperatures despite reaching the same average size.
“If you’re a foram, temperature appears to be a bigger determinant of your growth rate than even how old you are,” says Dr Brombacher.
“Temperatures change throughout the depth of the ocean water column so being able to optimise growth at different temperatures would have allowed each foram to live in a greater variety of habitats.”
James Mulqueeney a PhD researcher from the University of Southampton and co-author of the study said: “We also found that of the two species with similar environmental sensitivities, one was able to reach the same size but with a thinner shell, indicating a lower energetic cost and potential evolutionary advantage.”
Researchers say the same analysis techniques could be applied to other creatures which preserve their environmental and lifespan information including ammonoids, corals and bivalves like clams, oysters and mussels.
“This sort of data is routine in how we study adaptation in modern populations but has only now been gathered for fossils. By bringing together experts and facilities across the University of Southampton, we’ve been able to make progress on a foundational question in biology that wouldn’t have been possible within a single discipline,” says Prof Thomas Ezard, supervising author on the paper from the University of Southampton.
The research is part of a wider project which aims to scale up the analysis across a wider sample of two thousand plankton specimens to determine if a species’ adaptive flexibility is likely to lead it to diverge into separate, distinct species over time.
Detecting environmentally dependent developmental plasticity in fossilised individuals is published in Proceedings of the National Academy of Sciences and is available online.
The study was funded by the Natural Environment Research Council (NERC).
Ends
Contact
Steve Williams, Media Manager, University of Southampton, press@soton.ac.uk or 023 8059 3212.
Notes for editors
Detecting environmentally dependent developmental plasticity in fossilised individuals will be published in Proceedings of the National Academy of Sciences. An advanced copy is available upon request.
For Interviews with Prof Thomas Ezard please contact Steve Williams, Media Manager, University of Southampton press@soton.ac.uk or 023 8059 3212.
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All images and videos should be credited to University of Southampton
Additional information
The University of Southampton drives original thinking, turns knowledge into action and impact, and creates solutions to the world’s challenges. We are among the top 100 institutions globally (QS World University Rankings 2025). Our academics are leaders in their fields, forging links with high-profile international businesses and organisations, and inspiring a 22,000-strong community of exceptional students, from over 135 countries worldwide. Through our high-quality education, the University helps students on a journey of discovery to realise their potential and join our global network of over 200,000 alumni. www.southampton.ac.uk
Detecting environmentally dependent developmental plasticity in fossilized individuals
Article Publication Date
4-Jul-2025
COI Statement
None declared
Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.
The ocean around Antarctica is rapidly getting saltier at the same time as sea ice is retreating at a record pace. Since 2015, the frozen continent has lost sea ice similar to the size of Greenland. That ice hasn’t returned, marking the largest global environmental change during the past decade.
This finding caught us off guard – melting ice typically makes the ocean fresher. But new satellite data shows the opposite is happening, and that’s a big problem. Saltier water at the ocean surface behaves differently than fresher seawater by drawing up heat from the deep ocean and making it harder for sea ice to regrow.
The loss of Antarctic sea ice has global consequences. Less sea ice means less habitat for penguins and other ice-dwelling species. More of the heat stored in the ocean is released into the atmosphere when ice melts, increasing the number and intensity of storms and accelerating global warming. This brings heatwaves on land and melts even more of the Antarctic ice sheet, which raises sea levels globally.
Our new study has revealed that the Southern Ocean is changing, but in a different way to what we expected. We may have passed a tipping point and entered a new state defined by persistent sea ice decline, sustained by a newly discovered feedback loop.
The Southern Ocean surrounds Antarctica, which is fringed by sea ice.Nasa
A surprising discovery
Monitoring the Southern Ocean is no small task. It’s one of the most remote and stormy places on Earth, and is covered in darkness for several months a year. Thanks to new European Space Agency satellites and underwater robots which stay below the ocean surface measuring temperature and salinity, we can now observe what is happening in real time.
Our team at the University of Southampton worked with colleagues at the Barcelona Expert Centre and the European Space Agency to develop new algorithms to track ocean surface conditions in polar regions from satellites. By combining satellite observations with data from underwater robots, we built a 15-year picture of changes in ocean salinity, temperature and sea ice.
What we found was astonishing. Around 2015, surface salinity in the Southern Ocean began rising sharply – just as sea ice extent started to crash. This reversal was completely unexpected. For decades, the surface had been getting fresher and colder, helping sea ice expand.
The annual summer minimum extent of Antarctic sea ice dropped precipitously in 2015.NOAA Climate.gov/National Snow and Ice Data Center
To understand why this matters, it helps to think of the Southern Ocean as a series of layers. Normally, the cold, fresh surface water sits on top of warmer, saltier water deep below. This layering (or stratification, as scientists call it) traps heat in the ocean depths, keeping surface waters cool and helping sea ice to form.
Saltier water is denser and therefore heavier. So, when surface waters become saltier, they sink more readily, stirring the ocean’s layers and allowing heat from the deep to rise. This upward heat flux can melt sea ice from below, even during winter, making it harder for ice to reform. This vertical circulation also draws up more salt from deeper layers, reinforcing the cycle.
A powerful feedback loop is created: more salinity brings more heat to the surface, which melts more ice, which then allows more heat to be absorbed from the Sun. My colleagues and I saw these processes first hand in 2016-2017 with the return of the Maud Rise polynya, which is a gaping hole in the sea ice that is nearly four times the size of Wales and last appeared in the 1970s.
What happens in Antarctica doesn’t stay there
Losing Antarctic sea ice is a planetary problem. Sea ice acts like a giant mirror reflecting sunlight back into space. Without it, more energy stays in the Earth system, speeding up global warming, intensifying storms and driving sea level rise in coastal cities worldwide.
Wildlife also suffers. Emperor penguins rely on sea ice to breed and raise their chicks. Tiny krill – shrimp-like crustaceans which form the foundation of the Antarctic food chain as food for whales and seals – feed on algae that grow beneath the ice. Without that ice, entire ecosystems start to unravel.
What’s happening at the bottom of the world is rippling outward, reshaping weather systems, ocean currents and life on land and sea.
Feedback loops are accelerating the loss of Antarctic sea ice.University of Southampton
Antarctica is no longer the stable, frozen continent we once believed it to be. It is changing rapidly, and in ways that current climate models didn’t foresee. Until recently, those models assumed a warming world would increase precipitation and ice-melting, freshening surface waters and helping keep Antarctic sea ice relatively stable. That assumption no longer holds.
Our findings show that the salinity of surface water is rising, the ocean’s layered structure is breaking down and sea ice is declining faster than expected. If we don’t update our scientific models, we risk being caught off guard by changes we could have prepared for. Indeed, the ultimate driver of the 2015 salinity increase remains uncertain, underscoring the need for scientists to revise their perspective on the Antarctic system and highlighting the urgency of further research.
We need to keep watching, yet ongoing satellite and ocean monitoring is threatened by funding cuts. This research offers us an early warning signal, a planetary thermometer and a strategic tool for tracking a rapidly shifting climate. Without accurate, continuous data, it will be impossible to adapt to the changes in store.
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This article is republished from The Conversation under a Creative Commons license. Read the original article.
Alessandro Silvano is a Natural Environment Research Council (United Kingdom Research and Innovation) Independent Research Fellow.
NASA’s Perseverance rover is digging deeper into Mars’ geologic past as it begins grinding into Red Planet rock surfaces to expose material that could hold clues to the planet’s ancient environment and habitability.
Earlier this month, the Perseverance rover used its abrasion tool to scrape away the top layer of a rocky Martian outcrop nicknamed “Kenmore,” revealing a fresh surface for close-up analysis of the rock’s composition and history. The procedure, which involves a combination of mechanical grinding and gas-blast cleaning, allows scientists to study rock interiors that haven’t been altered by wind, radiation or dust over billions of years.
“Kenmore was a weird, uncooperative rock,” Ken Farley, Perseverance’s deputy project scientist, said in a statement. “Visually, it looked fine — the sort of rock we could get a good abrasion on and perhaps, if the science was right, perform a sample collection. But during abrasion, it vibrated all over the place and small chunks broke off. Fortunately, we managed to get just far enough below the surface to move forward with an analysis.”
The recent abrasion marks a shift in the rover’s focus from primarily scouting and sampling to more detailed in-situ science. Compared to its predecessors, Perseverance uses an advanced abrading bit and gaseous Dust Removal Tool, or gDRT, which applies five puffs of nitrogen to clear samples in a way that poses less risk of contamination. For comparison, earlier rovers used a brush instead to sweep debris, or tailings, out of the way.
(Image credit: NASA/JPL-Caltech)
After an abrasion is complete, Perseverance’s science instruments are deployed to investigate the exposed rock. The rover’s WATSON (Wide Angle Topographic Sensor for Operations and Engineering) imager snaps close-up photos, while its SuperCam uses laser pulses to analyze the composition of vaporized material with one spectrometer and study visible and infrared light reflected from the freshly exposed surface with another.
“The tailings showed us that this rock contains clay minerals, which contain water as hydroxide molecules bound with iron and magnesium — relatively typical of ancient Mars clay minerals.” Cathy Quantin-Nataf, SuperCam team member, said in the statement. “The abrasion spectra gave us the chemical composition of the rock, showing enhancements in iron and magnesium.”
Perseverance also relies on its SHERLOC (Scanning Habitable Environments with Raman & Luminescence for Organics & Chemicals) and PIXL (Planetary Instrument for X-ray Lithochemistry) instruments to help determine mineral content, chemical composition and potential signs of past water activity or even microbial life. In fact, not only did these tools find further evidence of clay, they also detected feldspar — a mineral common in Earth’s crust as well as on the moon and other rocky planets. The team also found, for the first time, manganese hydroxide in the observed specimens.
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“The data we obtain now from rocks like Kenmore will help future missions so they don’t have to think about weird, uncooperative rocks,” Farley said. “Instead, they’ll have a much better idea whether you can easily drive over it, sample it, separate the hydrogen and oxygen contained inside for fuel, or if it would be suitable to use as construction material for a habitat.”
The work is being carried out in Mars’ Jezero Crater, a 28-mile-wide (45-kilometer-wide) basin that once hosted a river delta and lake. Scientists believe the region contains some of the best-preserved records of Mars’ wet past, making it a prime location to search for biosignatures, or indicators of ancient life. Kenmore represents the 30th Martian rock that Perseverance has studied in such fine detail.
Perseverance is also continuing to collect rock core samples, which are being sealed in tubes and stored for a possible future return to Earth through the planned Mars Sample Return (MSR) campaign — though the Trump administration’s recently released FY 2026 NASA budget proposal suggests cutting the MSR program altogether.
As cities rapidly grow, expanding by an area almost double the size of France by 2030, natural spaces are being replaced by buildings and roads. This massive urban spread is hitting wildlife hard, wiping out their homes, cranking up temperatures, and creating dangerous concrete jungles.
It’s a tough situation for many animals on the move. Cities can be tempting with easy food and fewer natural predators, but they also come with deadly risks like traffic and lost pathways.
While past studies used cameras or sound to monitor urban wildlife, a new Yale study takes a different approach by analyzing environmental DNA (eDNA) from soil in 21 Detroit parks during winter and summer to uncover how mammal diversity changes with the seasons in urban landscapes.
The study aimed to understand how human activity shapes mammal communities in urban areas. By sampling environmental DNA (eDNA) from soil across 21 Detroit parks, researchers uncovered subtle, park-specific shifts in species composition, influenced by both natural and human-related factors, and larger parks supported greater biodiversity.
eDNA revealed seasonal changes and human presence effects on urban wildlife. These insights offer a promising tool for more adaptive and informed urban biodiversity planning, helping cities better balance green space with growing human footprints.
Measuring the effects of natural events on wildlife
Researchers analyzed soil samples from 21 urban parks in Detroit, Michigan, during February and July 2023. They detected DNA from 23 mammal species, including humans. They confirmed these results using iNaturalist wildlife sightings.
The DNA samples revealed seasonal shifts in mammal presence. Hibernators like groundhogs and muskrats were absent in winter samples, reflecting seasonal behaviors. During winter, animals were more clustered, likely due to resource competition and limited movement.
In summer, eDNA patterns revealed that mammals were more dispersed across landscapes, with fewer cross-species interactions due to abundant resources. Larger parks supported wider-ranging species, and coyotes appeared only in parks over 14.4 hectares.
Human DNA made up about one-third of all samples, highlighting constant human presence. Domesticated animal DNA (from cats, dogs, pigs, and cattle) reinforced the idea that urban parks are shared socio-ecological spaces.
Human presence influenced wildlife makeup, generalist and human-tolerant mammals thrived in busier areas, while more sensitive species were less commonly detected.
To protect urban biodiversity, especially wide-ranging species, researchers recommend expanding green spaces and building wildlife corridors that link parks together.
As cities continue to grow, these connected landscapes could be key to maintaining resilient ecosystems that support both nature and human well-being.
Journal Reference
Jane Hallam and Nyeema C. Harris. Network dynamics revealed from eDNA highlight seasonal variation in urban mammal communities. Journal of Animal Ecology. DOI: 10.1111/1365-2656.70082