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Hundreds evacuated as Guatemalan volcano erupts

Guatemalan authorities said Thursday they were evacuating more than 500 people after Central America’s most active volcano spewed gas and ash.

Residents were moved to shelters from communities near the Fuego volcano, located 35 kilometers (22 miles) from the capital Guatemala City.

“We prefer to leave rather than mourn the death of everyone in the village later,” Celsa Perez, 25, told AFP.

The government suspended local school activities and closed a road linking the south of the country to the colonial city of Antigua, a UNESCO World Heritage Site, disaster coordination agency Conred reported.

There have been several such mass evacuations in recent years because Fuego erupted, including in March of this year.

In 2018, 215 people were killed and a similar number left missing when rivers of lava poured down the volcano’s slopes, devastating a village.

Evacuees remain at a shelter after fleeing their village affected by the eruption of the Fuego volcano
Evacuees remain at a shelter after fleeing their village affected by the eruption of the Fuego volcano.

© 2025 AFP

Wasp lookalikes from 33 million years ago fooled ancient birds too

New fossil shows that precise wasp mimicry in hoverflies evolved far earlier than previously thought—and wasn’t shaped by modern birds.

Děčín, Czech Republic—A newly discovered fossil from the Early Oligocene reveals that hoverflies were already mastering the art of deception 33 million years ago. The fossil, Spilomyia kvaceki, found in the Děčín-Bechlejovice site in the Czech Republic, exhibits a strikingly well-preserved coloration pattern that mimics social wasps with exceptional accuracy.

Given that all previously described fossil mimics displayed only inaccurate resemblance to their hymenopteran models, this specimen provides the first known evidence of accurate wasp mimicry. The species is named in honor of the world-renowned paleobotanist Zlatko Kvaček, who worked in the Faculty of Science, Charles University.

This discovery provides unprecedented insight into the evolution of Batesian mimicry, a survival strategy in which harmless species evolve to imitate more dangerous ones, such as stinging insects. While modern mimicry is typically shaped by passerine birds—the dominant avian insect predators in Europe today—this study published in Current Biology demonstrates that non-passerine birds, such as those from the Coraciimorphae and Apodiformes groups, likely drove the development of accurate mimicry millions of years earlier.

“The fossil‘s detail is extraordinary. It shows that the mimicry of wasps we see in living hoverflies was already fully formed when Europe was dominated by very different kinds of birds,” says the study’s lead researcher Klára Daňková from Faculty of Science at Charles University in Prague.

The study also notes the presence of fossilized Palaeovespa wasps—potential models for the mimic—in the same locality, further supporting the hypothesis of early ecological interactions between mimics and models.

This find not only extends the known history of mimicry in insects but also reshapes our understanding of predator-prey interactions in deep time.

More information: Klára Daňková et al, Highly accurate Batesian mimicry of wasps dates back to the Early Oligocene and was driven by non-passerine birds, Current Biology (2025). DOI: 10.1016/j.cub.2025.02.069

Journal information: Current Biology 

Provided by Charles University 

Discovery of giant planet orbiting tiny star challenges theories on planet formation

Star TOI-6894 is just like many in our galaxy, a small red dwarf, and only ~20% of the mass of our sun. Like many small stars, it is not expected to provide suitable conditions for the formation and hosting of a large planet.

However, an international team of astronomers have found the unmistakable signature of a giant planet, called TOI-6894b, orbiting this tiny star. The work is published in Nature Astronomy.

This system has been discovered as part of a large-scale investigation of TESS (Transiting Exoplanet Survey Satellite) data, looking for giant planets around low-mass stars, led by Dr. Edward Bryant, who completed this work at the University of Warwick and at UCL’s Mullard Space Science Laboratory.

Dr. Edward Bryant, Warwick Astrophysics Prize Fellow and first author said, “I was very excited by this discovery. I originally searched through TESS observations of more than 91,000 low-mass red-dwarf stars looking for giant planets.

“Then, using observations taken with one of the world’s largest telescopes, ESO’s VLT, I discovered TOI-6894b, a giant planet transiting the lowest mass star known to date to host such a planet. We did not expect planets like TOI-6894b to be able to form around stars this low-mass. This discovery will be a cornerstone for understanding the extremes of giant planet formation.”

The planet (TOI-6894b) is a low-density gas giant with a radius a little larger than Saturn’s but with only ~50% of Saturn’s mass. The star (TOI-6894) is the lowest mass star to have a transiting giant planet discovered to date and is just 60% the size of the next smallest star to host such a planet.

Dr. Daniel Bayliss, associate professor at the University of Warwick said, “Most stars in our galaxy are actually small stars exactly like this, with low masses and previously thought to not be able to host gas giant planets. So, the fact that this star hosts a giant planet has big implications for the total number of giant planets we estimate exist in our galaxy.”

A challenge to the leading theory

Dr. Vincent Van Eylen, from UCL’s Mullard Space Science Laboratory, said, “It’s an intriguing discovery. We don’t really understand how a star with so little mass can form such a massive planet. This is one of the goals of the search for more exoplanets. By finding planetary systems different from our solar system, we can test our models and better understand how our own solar system formed.”

The most widely held theory of planet formation is called the core accretion theory. A planetary core forms first through accretion (gradual accumulation of material) and as the core becomes more massive, it eventually attracts gases that form an atmosphere. It then gets massive enough to enter a runaway gas accretion process to become a gas giant.

In this theory, the formation of gas giants is harder around low-mass stars because the amount of gas and dust in a protoplanetary disk around the star (the raw material of planet formation) is too limited to allow a massive enough core to form, and the runaway process to occur.

Yet the existence of TOI-6894b (a giant planet orbiting an extremely low-mass star) suggests this model cannot be completely accurate and alternative theories are needed.

Edward added, “Given the mass of the planet, TOI-6894b could have formed through an intermediate core-accretion process, in which a protoplanet forms and steadily accretes gas without the core becoming massive enough for runaway gas accretion.

“Alternatively, it could have formed because of a gravitationally unstable disk. In some cases, the disk surrounding the star will become unstable due to the gravitational force it exerts on itself. These disks can then fragment, with the gas and dust collapsing to form a planet.”

But the team found that neither theory could completely explain the formation of TOI-6894b from the available data, which leaves the origin of this giant planet as an open question for now.

Atmospheric answers

One avenue to shed light on the mystery of TOI-6894b’s formation is a detailed atmospheric analysis. By measuring the distribution of material within the planet, astronomers can determine the size and structure of the planet’s core, which can tell us whether TOI-6894b formed via accretion or via an unstable disk.

This is not the only interesting feature of TOI-6894b’s atmosphere; it is unusually cold for a gas giant. Most of the gas giants found by exoplanet hunters are hot Jupiters, massive gas giants with temperatures of ~1,000–2,000 Kelvin.

TOI-6894b, by comparison, is just 420 Kelvin. The cool temperature alongside other features of this planet, such as the very deep transits, makes it one of the most promising giant planets for astronomers to characterize with a cool atmosphere.

Professor Amaury Triaud, University of Birmingham, co-author, and member of the SPECULOOS collaboration said, “Based on the stellar irradiation of TOI-6894b, we expect the atmosphere is dominated by methane chemistry, which is exceedingly rare to identify. Temperatures are low enough that atmospheric observations could even show us ammonia, which would be the first time it is found in an exoplanet atmosphere.

“TOI-6894b likely presents a benchmark exoplanet for the study of methane-dominated atmospheres and the best ‘laboratory’ to study a planetary atmosphere containing carbon, nitrogen, and oxygen outside the solar system.”

The atmosphere of TOI-6894b is already scheduled to be observed by the James Webb Space Telescope (JWST) within the next 12 months. This should allow astronomers to determine which, if either, of the possible theories can explain the formation of this unexpected planet.

Co-author Dr. Andrés Jordán, researcher at the Millennium Institute of Astrophysics and professor at Adolfo Ibáñez University, said, “This system provides a new challenge for models of planet formation, and it offers a very interesting target for follow-up observations to characterize its atmosphere.

“This discovery is the result of a systematic program we have been carrying out for several years from Chile and the UK. Our efforts have allowed us to contribute significantly to a better understanding of how often small stars can form giant planets, and we are providing prime targets for follow-up with space-based platforms.”

More information: A transiting giant planet in orbit around a 0.2-solar-mass host star, Nature Astronomy (2025). DOI: 10.1038/s41550-025-02552-4

Journal information: Nature Astronomy 

Provided by University of Warwick 

What if the Big Bang wasn’t the beginning? Research suggests it may have taken place inside a black hole

The Big Bang is often described as the explosive birth of the universe—a singular moment when space, time and matter sprang into existence. But what if this was not the beginning at all? What if our universe emerged from something else—something more familiar and radical at the same time?

In a new paper, published in Physical Review D, my colleagues and I propose a striking alternative. Our calculations suggest the Big Bang was not the start of everything, but rather the outcome of a gravitational crunch or collapse that formed a very massive black hole—followed by a bounce inside it.

This idea, which we call the black hole universe, offers a radically different view of cosmic origins, yet it is grounded entirely in known physics and observations.

Today’s standard cosmological model, based on the Big Bang and cosmic inflation (the idea that the early universe rapidly blew up in size), has been remarkably successful in explaining the structure and evolution of the universe. But it comes at a price: it leaves some of the most fundamental questions unanswered.

For one, the Big Bang model begins with a singularity—a point of infinite density where the laws of physics break down. This is not just a technical glitch; it’s a deep theoretical problem that suggests we don’t really understand the beginning at all.

To explain the universe’s large-scale structure, physicists introduced a brief phase of rapid expansion into the early universe called cosmic inflation, powered by an unknown field with strange properties. Later, to explain the accelerating expansion observed today, they added another “mysterious” component: dark energy.

In short, the standard model of cosmology works well—but only by introducing new ingredients we have never observed directly. Meanwhile, the most basic questions remain open: where did everything come from? Why did it begin this way? And why is the universe so flat, smooth, and large?

New model

Our new model tackles these questions from a different angle—by looking inward instead of outward. Instead of starting with an expanding universe and trying to trace back how it began, we consider what happens when an overly dense collection of matter collapses under gravity.

This is a familiar process: stars collapse into black holes, which are among the most well-understood objects in physics. But what happens inside a black hole, beyond the event horizon from which nothing can escape, remains a mystery.

In 1965, the British physicist Roger Penrose proved that under very general conditions, gravitational collapse must lead to a singularity. This result, extended by the late British physicist Stephen Hawking and others, underpins the idea that singularities—like the one at the Big Bang—are unavoidable.

The idea helped win Penrose a share of the 2020 Nobel prize in physics and inspired Hawking’s global bestseller “A Brief History of Time: From the Big Bang to Black Holes.” But there’s a caveat. These “singularity theorems” rely on “classical physics,” which describes ordinary macroscopic objects. If we include the effects of quantum mechanics, which rules the tiny microcosmos of atoms and particles, as we must at extreme densities, the story may change.

In our new paper, we show that gravitational collapse does not have to end in a singularity. We find an exact analytical solution—a mathematical result with no approximations. Our math shows that as we approach the potential singularity, the size of the universe changes as a (hyperbolic) function of cosmic time.

This simple mathematical solution describes how a collapsing cloud of matter can reach a high-density state and then bounce, rebounding outward into a new expanding phase.

But how come Penrose’s theorems forbid out such outcomes? It’s all down to a rule called the quantum exclusion principle, which states that no two identical particles known as fermions can occupy the same quantum state (such as angular momentum, or “spin”).

And we show that this rule prevents the particles in the collapsing matter from being squeezed indefinitely. As a result, the collapse halts and reverses. The bounce is not only possible—it’s inevitable under the right conditions.

Crucially, this bounce occurs entirely within the framework of general relativity, which applies on large scales such as stars and galaxies, combined with the basic principles of quantum mechanics—no exotic fields, extra dimensions or speculative physics required.

What emerges on the other side of the bounce is a universe remarkably like our own. Even more surprisingly, the rebound naturally produces the two separate phases of accelerated expansion—inflation and dark energy—driven not by a hypothetical fields but by the physics of the bounce itself.

Testable predictions

One of the strengths of this model is that it makes testable predictions. It predicts a small but non-zero amount of positive spatial curvature—meaning the universe is not exactly flat, but slightly curved, like the surface of Earth.

This is simply a relic of the initial small over-density that triggered the collapse. If future observations, such as the ongoing Euclid mission, confirm a small positive curvature, it would be a strong hint that our universe did indeed emerge from such a bounce. It also makes predictions about the current universe’s rate of expansion, something that has already been verified.

This model does more than fix technical problems with standard cosmology. It could also shed new light on other deep mysteries in our understanding of the early universe—such as the origin of supermassive black holes, the nature of dark matter, or the hierarchical formation and evolution of galaxies.

These questions will be explored by future space missions such as Arrakhis, which will study diffuse features such as stellar halos (a spherical structure of stars and globular clusters surrounding galaxies) and satellite galaxies (smaller galaxies that orbit larger ones) that are difficult to detect with traditional telescopes from Earth and will help us understand dark matter and galaxy evolution.

These phenomena might also be linked to relic compact objects—such as black holes—that formed during the collapsing phase and survived the bounce.

The black hole universe also offers a new perspective on our place in the cosmos. In this framework, our entire observable universe lies inside the interior of a black hole formed in some larger “parent” universe.

We are not special, no more than Earth was in the geocentric worldview that led Galileo (the astronomer who suggested Earth revolves around the sun in the 16th and 17th centuries) to be placed under house arrest.

We are not witnessing the birth of everything from nothing, but rather the continuation of a cosmic cycle—one shaped by gravity, quantum mechanics and the deep interconnections between them.

More information: Enrique Gaztañaga et al, Gravitational bounce from the quantum exclusion principle, Physical Review D (2025). DOI: 10.1103/PhysRevD.111.103537. On arXivarxiv.org/html/2505.23877v1

Journal information: Physical Review D  arXiv 

Provided by The Conversation 

New study uncovers brutal punishment and public display of medieval woman on Thames foreshore

In 1991, the remains of a woman were discovered on the early medieval foreshore of the Thames River. The skeletal remains were moved to the London Museum, where they were curated. However, the analysis of the remains and publication of the results would not occur until over two decades later.

An investigation of the remains by Dr. Madeline Mant and her colleagues has now been published in World Archaeology.

The woman’s skeletal remains had been found placed between two sheets of bark, lying on a mat of reeds with moss pads placed on her face, pelvis, and knees.

At the time of excavation, it was noted that she had not been buried in a hole but rather placed on the foreshore where her remains could be viewed by the surrounding communities at high tide.

From the radiocarbon dates taken from the bark sheets, it is known she lived during the early medieval period between 680–810 AD.

When she died, she had been between the ages of 28 and 40. Stable isotope analyses revealed she had been a native of the area, likely having grown up in or near London.

Her diet consisted of terrestrial foods; however, after 5 years old, she experienced a period which led to increased stable nitrogen values.

This could indicate a change in diet, potentially incorporating more meat, or conversely, a period of starvation in which her body resorted to breaking down its fat and protein stores.

Prior to her death, she was subject to a series of brutal beatings and eventual execution.

Two weeks prior to her death, she had experienced two traumatic incidents, leading to over 50 individual signs of injury across her body. The first trauma incident resulted in hairline fractures in both her scapulae (shoulder blades); similar fractures on the scapula and spine are observed as a result of motor vehicle collisions. It is possible that for a 9th-century woman, these injuries were induced by beatings or floggings.

The second suite of injuries occurred on her torso and skull and were likely inflicted using blunt objects or a series of kicks and punches, akin to torture beatings.

A final, precise blow to the left side of her head resulted in her death.

According to Dr. Mant this form of corporal punishment could have been the result of changing law codes during the period. “Early Medieval England was a time of change regarding law codes—the law code of Æthelberht (c. 589–616) did not include corporal punishment, but that of Wihtred of Kent (690–725) outlined specific punishments, for instance, beatings for those who could not pay fines.

“Capital punishments were also included when willed by the king. As time passed, more crimes were associated with the death penalty under King Alfred (871–899). Crimes such as theft, treason, witchcraft, and sorcery could be met with the death penalty, which could be brought about by stoning or drowning.

“The burial treatment of UPT90 sk 1278 lets us know that her body was meant to be visible on the landscape, which could be interpreted as a warning to witnesses. We can tell from the osteobiography of this individual and their burial treatment that they were executed, but the specific offense is impossible to know for certain. We can only infer from the law codes of the period.”

After execution, it was typical to place the remains in liminal or separate spaces, such as in execution cemeteries. However, the remains of UPT90 sk 1278 were placed on the foreshore of the Thames, where her body could be viewed by the surrounding community at high tide.

“Many scholars have examined the burial/placement of bodies in liminal spaces as an indication of the burial being unusual or indicating deviance. Criminal behavior is perceived as deviant; thus, a non-normative burial location could be a contextual clue as to how the individual was perceived during their life. The Thames foreshore could be considered a liminal space, and has been discussed as a symbolic boundary in the broader literature,” explains Dr. Mant.

Despite changing law codes, executions were still relatively rare, with archaeological evidence from execution cemeteries indicating a rate of around one execution per decade. Additionally, these executions are more often associated with men, with a male-to-female sex ratio of execution cemeteries being around 4.5:1.

This makes the remains of UPT90 sk 1278 especially unique for understanding the embodiment of early Medieval law in female bodies and provides insights into the judicial contexts of isolated burials.

More information: Madeleine Mant et al, Evidence for punishment and execution on the foreshore: a unique early medieval burial (680–810 AD) from London, World Archaeology (2025). DOI: 10.1080/00438243.2025.2488739

© 2025 Science X Network

Greenland’s melting ice caps reveal the true extent of climate change

For most of us, first-hand knowledge of Greenland is probably limited to flying over it en route to North America. It’s likely that you’ve heard more about it over the last few months than in the rest of your life combined, but geopolitical debates aside, Greenland is also of vital importance for research into the climate and environment.

In recent decades, this territory—80% of which is covered with ice—has recorded a loss of frozen mass that outpaced previous estimates by 20%. This rapid reduction not only has consequences for Greenland’s 56,000 inhabitants, but also on a global scale, as it affects rising sea levels and the balance of the planet’s climate systems.

Understanding the current dynamics of ice loss and glacier retreat requires a long-term view. This means drawing a line between the changes happening now and the climatic and environmental conditions of thousands of years ago.

We can reconstruct these past dynamics with information from various sources, such as cores extracted from the ice sheet, or by dating the rocks transported and deposited by ancient glaciers. Sediments accumulated in Arctic lakes also provide valuable data for identifying natural and anthropogenic (human-caused) climate variations over time.

Information on ecosystems that are free from human intervention is also essential to understanding their evolution. Data obtained in the field allows us to calculate the thickness of the ice at different times, and to reconstruct its environmental transformations in the face of climatic changes.

As well as providing insight into the past, this data helps to project future scenarios more accurately. Direct observations, combined with tools such as remote sensing and modeling, make it possible to anticipate how ecosystems might evolve in the face of rising temperatures. This integration is key to land use planning and adaptation, and not just in polar regions.

A new coastline

Greenland’s coastline is being redrawn, both by changes in the extent of surface ice and by melting glaciers flowing into the sea. Between 2000 and 2020, the retreat of these glaciers in the Northern Hemisphere has led to an increase of 2,500km in the length of the Arctic coastline. Most of the new ice-free areas can be found in Greenland.

In addition to glacial retreat on land, coastal areas are impacted by a decrease in both the extent and duration of sea ice. This intensifies coastal erosion, with shorelines retreating up to 20 meters per year in some areas.

These transformations have a significant impact on permanently frozen ground (permafrost), which is more exposed to marine storms and the degradation they cause. Melting permafrost not only releases large quantities of greenhouse gases, but also makes coastal areas more vulnerable to rising sea levels.

Arctic changes, global consequences

Scientific research is essential to understanding the ongoing climatic changes that are affecting polar regions such as Greenland.

Phenomena such as retreating glaciers, thawing permafrost and shifting coastlines are all moving fast. These processes not only impact the landscape, they also have a profound effect on local communities. Their wider repercussions are global, impacting the North Atlantic, which in turn influences sea level rise, shifting climate patterns, and the behavior of ocean currents.

Beyond the effects on the natural environment, such as the loss of coastal areas and biodiversity, these transformations have significant social and economic consequences. These include the rising costs of adapting to more frequent and intense storms, which directly threaten territories like Greenland and their inhabitants.

A laboratory in Greenland

In the face of the widespread retreat of polar glaciers and the projected deglaciation of large areas of the Arctic, it is essential to understand how, and how quickly, areas change after ice disappears.

In this context, the GRELARCTIC project continues research carried out in Greenland in recent years, both on postglacial evolution and how it may affect global climate change.

This new research phase will study changes from the depths of inland glaciers all the way to the coastline. It will address key areas such as plant colonization to understand which species settle more rapidly in the areas exposed by ice loss, as well as the evolution of snowpack to analyze annual dynamics and long-term trends, and the way changing river courses impact the environment.

This data is essential for understanding how Arctic ecosystems respond to environmental variations. Greenland does not just reflect climate change: it predicts it. Understanding how this region adapts to a warmer climate offers crucial clues for anticipating transformations in other parts of the planet.

Provided by The Conversation 

This article is republished from The Conversation under a Creative Commons license. Read the original article.

What made Mount Etna’s latest eruption so rare

Mount Etna, the volcano that towers over eastern Sicily, has again captivated the world with a spectacular show, spewing smoke and high into the sky.

But the defining event of Monday’s eruption was the more rare pyroclastic flow from the southwestern crater not visible from a distance.

The volcano is Europe’s most active and the continent’s largest. Etna attracts hikers and backpackers to its slopes while less adventurous tourists can take it in from a distance, most stunningly from the Ionian Sea.

Etna’s latest eruption caused neither injuries nor evacuations, but sent a group of tourists on its flanks running, as captured by video posted on social media with smoke towering in the background.

Authorities emphasized there was no danger to the population, and the pyroclastic flow—a fast-moving mixture of rock fragments, gas and ash—was limited to about 2 kilometers (more than a mile) and didn’t go beyond the Valle del Leone, or Lion Valley, which forms a natural containment area.

Etna has been active recently and this was the 14th episode since mid-March. The most recent pyroclastic flows with significant reach were recorded on Feb. 10, 2022, Oct. 23, 2021, Dec. 13, 2020, and Feb. 11, 2014, Marco Viccaro, president of Italy’s national volcanology association, said Tuesday.

What made Mount Etna's latest eruption so rare
Smoke billows from Mount Etna volcano, Italy, Monday, June 2, 2025. Credit: AP Photo/Giuseppe Distefano

What’s happening now

After a 19-day lull, Etna began to erupt with lively explosive bursts of gas and ash followed by a mild lava flow on the eastern slope followed by a smaller flow to the south.

At around 10 a.m. Monday, Etna exploded with its first major, violent eruption of the year: Lava fountains and a column of ash and gas rose several kilometers (miles) in the air. The event climaxed around 11:23 a.m. when the pyroclastic flow, triggered when magma mixed with snow, traveled 2 kilometers (more than a mile) to the Valle del Leone within a minute.

By late afternoon, scientists said the event had subsided.

Imposing figure

Etna towers around 3,350 meters (around 11,050 feet) above sea level and is 35 kilometers (22 miles) in diameter, although the volcanic activity has changed the mountain’s height over time.

  • What made Mount Etna's latest eruption so rare Smoke billows from Mount Etna volcano, seen from the village of Zafferana Etnea, Italy, Monday, June 2, 2025. Credit: AP Photo/Giuseppe Distefano
  • What made Mount Etna's latest eruption so rare Smoke billows from Mount Etna volcano, Italy, Monday, June 2, 2025. Credit: AP Photo/Giuseppe Distefano
  • What made Mount Etna's latest eruption so rare Smoke billows from Mount Etna volcano, Italy, Monday, June 2, 2025. Credit: AP Photo/Giuseppe Distefano
  • What made Mount Etna's latest eruption so rare Smoke billows from Mount Etna volcano, seen from the village of Zafferana Etnea, Italy, Monday, June 2, 2025. Credit: AP Photo/Giuseppe Distefano
  • What made Mount Etna's latest eruption so rare Smoke billows from Mount Etna volcano, Italy, Monday, June 2, 2025. Credit: AP Photo/Giuseppe Distefano

Occasionally, the airport at Catania, eastern Sicily’s largest city, has to close down for hours or days, when ash in the air makes flying in the area dangerous. An aviation warning was put in place during the latest event, but the airport wasn’t closed.

With Etna’s lava flows largely contained to its uninhabited slopes, life goes in towns and villages elsewhere on the mountain. Among the benefits of the volcano: fertile farmland and tourism.

Deadly past

Inspiring ancient Greek legends, Etna has had scores of known eruptions in its history. An eruption in 396 B.C., has been credited with keeping the army of Carthage at bay.

In 1669, in what has been considered the volcano’s worst known eruption, lava buried a swath of Catania, about 23 kilometers (15 miles) away and devastated dozens of villages. An eruption in 1928 cut off a rail route circling the mountain’s base.

© 2025 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed without permission.

Taking a realistic look at terraforming Mars

A team of researchers with a variety of backgrounds and affiliated with multiple institutions in the U.S. has taken a realistic approach to looking at the question of whether Mars could be terraformed. In their paper published in the journal Nature Astronomy, the group suggests that the time has come to look at the means by which Mars could be terraformed, and then whether such a task should be undertaken.

Over the past century, a host of figures from scientists to science fiction writers have tackled the issue of terraforming Mars—doing things to the planet that would make it habitable for humans. Currently there are two main questions surrounding the issue: Whether it should be done if possible, and whether it is possible at all.

In a new study, researchers argue that the latter issue should be addressed first, because the first issue would be moot if the answer is no. They created an outline of sorts that could be used to begin assessing what it would take to terraform Mars.

Taking a realistic look at terraforming Mars
Thresholds in making Mars suitable for life. Credit: Nature Astronomy (2025). DOI: 10.1038/s41550-025-02548-0

The team suggests any attempt to terraform Mars would almost certainly have to start with an effort to heat the planet. Possible means for doing so include putting solar sails in place or dispersing nanoparticles into the planet’s atmosphere to hold in heat from the sun. Once the planet was heated by approximately 30°C, they suggest, likely over many years, carbon dioxide would be released from the poles, further helping to warm the planet—and making the atmosphere thicker.

Once the planet was heated sufficiently, microbes could be introduced that would produce oxygen. Once that process was complete, the planet could then be tended by adding hardware to monitor and tweak the environment and chemicals and other materials as needed. Eventually, plants and animals could be introduced, and then at some point, human life could be supported.

The researchers acknowledge that it is still not possible to determine whether Mars could be terraformed, but enough is known to begin the process of experimenting here on Earth in ways that could provide answers for Mars. They also note that anything learned along the way could provide valuable lessons in how to clean up our own planet and keep it habitable.

More information: Erika Alden DeBenedictis et al, The case for Mars terraforming research, Nature Astronomy (2025). DOI: 10.1038/s41550-025-02548-0

Journal information: Nature Astronomy 

© 2025 Science X Network

Nearly complete dinosaur skull reveals a new sauropod species from East Asia

A team led by China University of Geosciences has described a new species of sauropod, Jinchuanloong niedu, from a partial skeleton and nearly complete skull found in northwestern China, adding a rare non-neosauropod eusauropod to the Middle Jurassic record of East Asia.

Eusauropods are the clade that includes nearly all long-necked dinosaurs beyond the earliest forms. They became the only surviving sauropod lineage after a global extinction in the late Early Jurassic.

Many later branching forms belong to Neosauropoda, such as the iconic giants Apatosaurus and Brachiosaurus. Several non-neosauropod eusauropods also persisted through the Middle Jurassic, dominating faunas in that interval.

Fossils preserving complete skulls remain rare among non-neosauropod eusauropods, leaving major gaps in the Middle Jurassic fossil record.

In the study, “A new eusauropod (Dinosauria, Sauropodomorpha) from the Middle Jurassic of Gansu, China,” published in Scientific Reports, researchers describe the anatomy and evolutionary placement of a previously unknown specimen.

Recovered from the lower part of the Xinhe Formation in Jinchuan District, Gansu Province, the Jinchuanloong niedu holotype consists of a nearly complete skull with mandible, five articulated cervical vertebrae, and 29 articulated caudal vertebrae. Site sedimentary beds date to the late Bathonian of the Middle Jurassic, around 165 to 168 million years ago.

New dinosaur discovered from a nearly complete skull
Caudal vertebrae of Jinchuanloong niedu (JCMF0132). Credit: Scientific Reports (2025). DOI: 10.1038/s41598-025-03210-5

Detailed anatomical comparisons with other East Asian sauropods revealed a combination of primitive and derived features. Researchers examined the specimen’s cranial and postcranial anatomy through comparative morphological description and scored it in two phylogenetic datasets to evaluate its placement within Eusauropoda.

In both analyses, Jinchuanloong was resolved as a diverged non-neosauropod eusauropod, sister to the clade comprising Turiasauria and Neosauropoda. Unique diagnostic traits include a foramen at the base of the maxillary ascending process, an aperture on the anterodorsal surface of the prefrontal, and a robust postorbital with a height-to-length ratio. Maxillary teeth are described as spoon-like in labial view, a shape shared with taxa such as Shunosaurus and Turiasaurus.

Unfused neural arches in the posterior caudal vertebrae and a large pineal foramen feature suggest a juvenile or subadult individual—something to keep in mind when assessing the estimated body length of approximately 10 meters.

According to the researchers, Jinchuanloong anatomy contributes to broader discussions about Middle Jurassic sauropod diversification and ecological partitioning in East Asia. The near-complete cranial remains offer an exceptional glimpse into the craniofacial evolution of early eusauropods.

“The discovery of Jinchuanloong niedu enriches the diversity of early diverging sauropods and provides additional information to help understand the evolutionary history of sauropods in northwest China,” the authors write.

More information: Ning Li et al, A new eusauropod (Dinosauria, Sauropodomorpha) from the Middle Jurassic of Gansu, China, Scientific Reports (2025). DOI: 10.1038/s41598-025-03210-5

Journal information: Scientific Reports 

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Turkey earthquake: Moment 5.8-magnitude quake rocks popular Rhodes hotel

This is the moment a 5.8-magnitude earthquake which struck in Turkey shakes a hotel in neighbouring Greece.

Footage shows the quake shaking CCTV cameras at the five-star Rodos Palladium hotel on Rhodes Island, in the early hours of 3 June.

The quake struck about 29km north of Rhodes, the largest of the Dodecanese islands near the Turkey border, at around 2.17am (local time) on Tuesday at a depth of 68km, according to the European Mediterranean Seismological Centre

At least one person has died in Turkey, while dozens of people sustained injuries as panicked locals tried to jump off their buildings, according to local reports.