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What dinosaur fossils could teach us about cancer

When you think of dinosaurs, you might imagine towering predators or gentle giants roaming prehistoric landscapes. But what if these ancient creatures could teach us about one of humanity’s most persistent challenges: cancer?

In a new study, my team and I explored how fossilized soft tissues, preserved for tens of millions of years, could reveal new insights into ancient proteins that might one day help the study of cancer.

For decades, dinosaur research has focused on bones, which are much more likely to be preserved. But bones alone can’t tell the full story of how these animals lived, or how they died. Advances in technology, like paleoproteomics (the study of ancient proteins) are now allowing scientists to analyze delicate fragments of soft tissues preserved in fossils.

In 2016, I read an article about the discovery of a new fossil in Romania with a tumor in its jaw. Those remains were from a dinosaur called Telmatosaurus transsylvanicus, a duck-billed, plant-eating “marsh bird”. The specimen had lived between 66-70 million years ago in the Hateg Basin in present-day Romania.

I was fascinated by what we might learn from this. Although there were a handful of previous reports of cancers in other dinosaur bones, and previous findings of soft tissues like blood vessels in fossils, no one had ever described soft tissues in an ancient tumor.

To understand more, my team went to Romania and collected the specimen. We brought it back, and made a tiny hole into it with a drill the width of a human hair, taking a minuscule sample.

Then we mounted it onto a powerful microscope, called a scanning electron microscope. Inside it, we saw images of blood cells, which contain proteins.

In the original Jurassic Park film, the scientists create or clone dinosaurs from ancient genetic material. But in reality over millions of years the DNA is completely broken down.

Proteins however, unlike DNA, can be remarkably stable over time. Research has shown that they can persist in fossils for millions of years under the right conditions, acting as molecular time capsules. Studying these proteins can help us reconstruct biological processes, including diseases like cancer, that affected dinosaurs.

Cancer’s deep evolutionary roots

Cancer is often seen as a modern plague, but it has ancient origins. Large, long-lived animals, from elephants to whales, are a paradox. Their size and longevity should make them cancer-prone, yet many have evolved remarkable defenses.

Elephants, for example, carry extra copies of the TP53 gene, a tumor suppressor. Bowhead whales which can live for over 200 years, have ultra-efficient DNA repair mechanisms and damage to DNA is the root cause of cancer. Dinosaurs, as some of the largest animals to ever exist, probably faced similar problems.

My team’s research builds on growing evidence that dinosaurs weren’t immune to cancer. Fossilized tumors have been found in species like Tyrannosaurus rex and Telmatosaurus, ranging from benign growths to aggressive cancers. My team is aiming to uncover the molecular tools dinosaurs used to suppress tumors in the future.

Bones tell us about anatomy, but soft tissues hold the keys to biology. In my team’s study, the red blood cell-like structures we found in Telmatosaurus fossils represent gateways to understanding the dinosaur’s physiology.

Proteins preserved in these tissues could reveal how dinosaurs managed oxidative stress which is linked to cancer, inflammation, or even immune responses to cancer. For instance, certain proteins might indicate mechanisms for detecting and destroying faulty cells before tumors can form.

This work also highlights a need for a critical shift in paleontology: to preserve soft tissues, not just skeletons. Museums and researchers often prioritize intact bones, but fragments of fossilized skin, blood vessels, or cells can harbor molecular secrets. As technology advances, these overlooked specimens could become invaluable for studying disease evolution

Bridging past and present

The link between dinosaurs and humans might seem distant, but evolution often repurposes ancient biological tools. Modern oncology already draws inspiration from nature and many chemotherapies come from plants or trees. The drug trabectedin, for example, used to treat soft-tissue sarcoma, comes from a marine organism called the sea squirt.

Expanding our search to extinct species could open a library of evolutionary solutions. If we can identify cancer-suppressing or cancer-promoting proteins in dinosaurs, these molecules might inspire new lessons about human cancers.

It’s taken nearly a decade to get this far. Like so much work, this research underscores the importance of patience and we’re not there yet. A real breakthrough might come when advances in research allows us to study ancient proteins in detail, tracking how cancer mechanisms evolved over millions of years.

Bridging paleontology and oncology is not only uncovering ancient history. We’re potentially writing a new chapter in the fight against cancer.

Provided by The Conversation 

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

A Lake Mead’s worth of water has vanished from the ground: Could Las Vegas suffer?

The water beneath our feet that we use to bathe, drink and water crops is vanishing faster than ever in the Colorado River Basin, according to a new study.

From Arizona State University researchers, the study of satellite images has found that an amount of water comparable to Lake Mead has been lost from the ground in the period studied from April 2002 to October 2024. That’s roughly twice as fast as water on the surface.

For Jay Famiglietti, a study co-author who pioneered the practice of using satellites to study groundwater at ASU, the loss of 27.8 million acre-feet of groundwater should be a wake-up call for everyone from decision-makers to regular citizens who call the West home.

“Groundwater is a trans-generational resource,” Famiglietti said. “If we want our great-great-great-grandchildren to eat, then it’s time to think more holistically about the water that we use and what kind of protection it needs.”

While it’s true that Las Vegas relies on surface water from Lake Mead for 90% of its supply, that’s an increasingly limited resource it shares with six other states, Native American tribes and parts of Mexico.

And the overuse of groundwater—especially highlighted in Arizona—could prove to be a major problem as conflicts between water users flare in the future, causing more of a reliance on Colorado River surface water.

“Groundwater is key to our economic vitality,” Famiglietti said, “yet it remains sort of spottedly managed. Even where it is being managed, it’s unclear how effective the management will be.”

Spotlight on Arizona

The worst offender, by far, is Arizona when it comes to Colorado River Basin states.

Its $1.4 billion agricultural industry is largely propped up by groundwater, and only 18% of the state’s groundwater is subject to regulation and management, according to the study.

Under the state’s Groundwater Management Act of 1980, seven so-called “active management areas” exist in mostly urban areas, slowly weaning water users off of groundwater and onto surface water. The most recently designated one is the Wilcox basin east of Tucson, which officials approved last December.

A huge help to that mission came with the completion of the Central Arizona Project in the ’90s. Meant to stop over-reliance on groundwater, the 336-mile pipeline transports water from Lake Havasu to a distribution point near Tucson.

In a statement, the Arizona Department of Water Resources acknowledged the findings of the study as issues its water managers have long thought about.

“Protecting groundwater supplies throughout the state—both within the mainstem and outside the mainstem Colorado River Basin—is a major reason why Arizona is taking steps to expand its Groundwater Management Act protections to threatened regions,” a department spokesperson said.

Southern Nevada’s tie to groundwater

Though not highlighted in the study, the Las Vegas Valley Water District manages four groundwater-dependent delivery systems in the region: Blue Diamond, Kyle Canyon, Searchlight and Jean.

Continuous—sometimes hourly—monitoring of the aquifers that residents and businesses rely on in each of those systems helps water managers keep a close eye. All four of those aquifers’ levels tend to be responsive to rainfall, as well as snowmelt from the Spring Mountains.

Since 2020, the water district board has had a moratorium in place because of low aquifer levels, preventing any new connection hookups for the two wells that serve the neighborhoods near Red Rock Canyon.

In all four systems, water users are well acquainted with conservation rules that change depending on water levels, said Colby Pellegrino, deputy general manager of resources at the Southern Nevada Water Authority.

“We have gotten to the point where we have to say, ‘Hey, now is the time when you need to stop outdoor watering,'” Pellegrino said.

A ticking clock for 2027

Unanswered questions linger as Nevada and its neighbor states continue to negotiate throughout the next year.

Whatever they decide, the study’s authors are pushing for negotiators to consider groundwater and its stress on the entire Colorado River system in tense, ongoing interstate water negotiations to update each state’s river allocation by the end of 2026.

Karem Abdelmohsen, an ASU postdoctoral student who is the study’s lead author, said he and Famiglietti shared the results with Arizona water managers, who seemed receptive.

“The main message is that we are giving a lot of attention to surface water along the Colorado River, but groundwater needs a lot of attention as it is getting depleted in huge amounts,” Abdelmohsen said. “We need to slow down and give a chance for nature to refill our aquifers.”

It remains to be seen what approach Arizona officials will take to save its productive agricultural industry, though none seem to have floated the idea of building more diversions from the river.

Still, signs like this study point to more cuts for everyone involved as human-caused climate change and other factors dry up the Colorado River Basin.

“There’s no indication that Arizona is going to try and get more water from the Colorado River based upon what’s happening with their local groundwater,” said Pellegrino, of the Southern Nevada Water Authority.

“They’ve got to figure out, just like everyone else, what does our post-2026 operating regime look like?”

2025 Las Vegas Review-Journal. Distributed by Tribune Content Agency, LLC.

China’s Everest obsession: How tourism and climate change are transforming the mountain

“To the discerning eye, other mountains are visible—giants between 23,000 and 26,000 feet high. Not one of their slenderer heads even reaches their chief’s shoulder. Beside Everest they escape notice, such is the preeminence of the greatest,” George Mallory, 1922.

The climbing season on Mount Everest peaks in late May and early June every year. Extreme weather patterns at this location and altitude mean the main climbing season is remarkably short, perhaps only a few weeks between the winter freeze and monsoon storms.

Even within that time, the precise location of the jetstream that accelerates wind speeds at the summit creates pinchpoints of ideal climbing conditions, leading to images of long queues of mountaineers at particularly challenging points such as the Hillary Step—named after one of the two men who first climbed Everest on May 29, 1953.

In the 30 years after Edmund Hillary and Sherpa Tenzing Norgay first stood at the summit, only 150 men and women matched their feat. But since then, the number of climbers has sky-rocketed. In 2019, a record 877 people summited the mountain, and in 2024 ascents were only just shy of this.

Rebecca Stephens, the first British woman to climb Everest in 1993, has described how the “global obsession with the world’s highest mountain is shaping its future and the future of the people who work on it.”

Stephens said her ascent in 1993, when there was only one commercial expedition on the mountain, felt like a watershed moment. Since then, commercial expeditions have mushroomed on Everest’s southern base camp on the Khumbu glacier (altitude: 5,364 meters), which now boasts a wide range of facilities including coffee shops and party tents.

The explosion of interest in climbing Everest has been aided by the fact that, despite its altitude and dangers, it is far from the most difficult high-altitude mountain. A member of the Tibet Mountaineering Association who had summited five times told me, on a good day, Everest was “very straightforward”—and that climbing Denali in Alaska (North America’s tallest peak) had been much more difficult.

By the end of 2024, there had been 12,884 ascents and 335 deaths on Everest, a survival rate of 97.4%. But the so-called “death zone” above 8,000 meters, combined with avalanches, extreme weather and frostbite, will always present significant hazards to the people who visit these slopes.

This climbing season, a Scottish former marine described quitting his attempt 800 meters below the summit after encountering two dead climbers. Meanwhile, four other ex-British special forces soldiers including UK government minister Alastair Carns, used xenon gas and hypoxia training to travel to Everest and summit in under a week—leading to concerns that this could further increase the number of people attempting to scale the increasingly crowded mountain.

But while images of high-altitude queues and stories of occasional fatalities hog the headlines, most visitors to Everest do not attempt to climb it. And by far the majority of these tourists are on the “other side of Everest,” in China-administered Tibet.

China’s “economic miracle”, combined with its desire to develop peripheral regions, has meant that Qomolangma (the Tibetan name for Everest) is now easily accessible, with tarmacked roads all the way to the northern base camp at Rongbuk (altitude: 5,150 meters).

From having lower numbers of visitors than the Nepalese side 20 years ago, the Tibetan side of Everest now welcomes more than half a million tourists a year—the vast majority from mainland China. Short Chinese holidays mean most of these visits are whistlestop trips that also take in the nearby high-altitude cities of Lhasa and Shigatse. Because of the lack of altitude acclimatization time, many tourists carry oxygen bottles or wear oxygen backpacks during their visits.

Retracing the earliest routes

To better understand the impact of tourism on Everest, I visited the Tibetan side in June 2024 as a guest of Linsheng Zhong, professor of human and tourism geography at China’s Institute of Geographical Sciences and Natural Resources Research.

The date of our visit was significant, being a century since the disappearance of early Everest adventurers George Mallory and Sandy Irvine on June 8, 1924. We set out to examine both the human and environmental changes that have occurred over the intervening hundred years—using century-old journals and photographs as a baseline.

As geographers rather than high-altitude mountaineers, our aim was to retrace some of the reconnaissance routes used by the British in the 1920s—a time when Nepal was closed to foreign visitors. Between 1921 and 1924, three expeditions organized by the Royal Geographical Society and the Alpine Club visited Tibet with the aim of being the first recorded people to climb Mount Everest. None, as far as we know, reached the top—and the remains of the two leaders of the final expedition, Mallory and Irvine, were only discovered on Everest many years later.

While the vistas are equally spectacular today, climate change has had a significant impact on glaciers throughout the region. Recent scientific estimates suggest that there has been between a 26% and 28% reduction in the glaciers surrounding Everest between the 1970s and 2010.

In 1921, the leader of the first expedition, Charles Howard-Bury, camped just below the Langma pass—the highest but most direct easterly route to Everest—and photographed “a peak of black rock with a glacier just below it.” It is apparent from this “slider” comparison, using a photograph I took from the same spot, how much this hanging glacier has retreated over the past century.

The human impact on Everest

Everest’s permanent northern base camp at Rongbuk in Tibet now welcomes up to 3,000 visitors a day in high season. Tourists are initially disgorged into a regimented tented village—modern versions of Tibetan yak herder accommodation.

Some of these jet-black tents, made from thick yak hair which breathes when dry and is waterproof when wet, provide simple (but heated and oxygenated) accommodation for the hardier tourists who want to be at the mountain early for the best photo opportunities.

Wandering up the astroturf lining the central boulevard, we meet a range of souvenir sellers before reaching the “world’s highest post office” and a circular plaza commemorating the various scientific and political achievements of the region. The near-landscape is largely brown: when he was here, Mallory described the contrast between the rain-shadowed “monotonously dreary, stony wastes” of Rongbuk with the beauty of the snowy mountains looming above.

Today, a boardwalk takes tourists marginally further to Rongbuk monastery—founded in 1902 and rebuilt after being damaged during the Chinese Cultural Revolution—and a final viewpoint of the north face of Everest. A yellow sandstone band is clearly visible just below the summit—evidence that this mighty mountain was once at the bottom of the ocean.

The mood on our trip was a sharp contrast to my visit in November 2007, when our Tibetan guide had been keen to evade any security checkpoints (albeit to maximize his personal profit, rather than any ethical standpoint). With only a few thousand annual, mostly international, visitors, the facilities back then were very limited, beyond a warning to tourists to proceed no further or face significant fines—and a shiny new sign proclaiming mobile phone coverage.

However, we were able to walk to the snout of the Rongbuk glacier, a jumble of shattered sandstone rocks at the terminal moraine. Today, tourists cannot go far beyond the monastery and are corralled on new boardwalks.

Tourism has brought rapid economic change to this region of the Tibetan plateau—including diversifying from traditional livelihoods. Central government efforts to reduce overgrazing in the fragile ecosystem have led to a system of payments to traditional herders—and a drop in livestock numbers from a peak of nearly 1 million in 2008 to below 700,000 today.

In contrast, the permanent human population of the Qomolangma National Nature Preserve (the protected area that includes the Tibetan side of Everest) has more than doubled since the 1950s to more than 120,000 people, with especially accelerated growth over the last decade coinciding with the rise in tourism. The Pang La pass which crosses into the Rongbuk valley, described as “desolate” by English mountaineer Alan Hinkes in the 1980s, is now festooned with souvenir shops and mobile coffee baristas.

Concern about the environmental impacts of these tourists led to the introduction of a fleet of electric buses in 2019, with visitors instructed to park their vehicles in the small town of Tashi Dzom before taking a 30-minute electric bus ride to the northern Everest base camp.

Now there are plans to move the bus transfer station to a gleaming new park center closer to the main highway, to save tourists having to drive the numerous switchbacks over the Pang La pass to Tashi Dzom, then negotiate traffic jams and parking challenges nearer the peak.

This is partly to cope with another western import to China: the concept of the “road trip.” For Chinese car enthusiasts, the 5,000-kilometer Route 318 from Shanghai to the foot of Everest is now one of their most popular long-distance drives.

“The most beautiful valley in the world’

We visited the east and north faces of Everest in Tibet armed with photographs and accounts from those three early British expeditions more than a century ago—the first recorded attempts to climb the world’s highest mountain.

The first (1921) expedition led by Howard-Bury, an army lieutenant-colonel, botanist and future Conservative MP, was a detailed scientific and topographical survey of the area. In their attempts to find a route to the summit, approaches via the northern (Rongbuk) and eastern (Kama) valleys were reconnoitered.

Although less visited than the Khumbu base camp in Nepal or the Rongbuk base camp in Tibet, the eastern approach to Everest via the Kama valley is a wonderful trek with unobstructed views of the immense eastern face of Everest. Howard-Bury described the allure of the valley which remains today: “We had not been able to gather much information locally about Mount Everest. A few of the shepherds said that they had heard that there was a great mountain in the next valley to the south … They called this the Kama valley, and little did we realize at the time that in it, we were going to find one of the most beautiful valleys in the world.”

The valley is accessed from the settlement of Kharta, a small-but-booming town on the banks of the Bong Chu-Arun river. Just below Kharta, the river enters a steep gorge, dropping from nearly 4,000m to 2,000m as it enters Nepal. Today, the Kama valley route is becoming popular with Chinese trekkers, although there are very limited facilities to deal with their impact on the area—notably, the human and plastic waste.

The 1921 expedition selected Kharta as the location of its second base camp after several months of exploration at Rongbuk. All were relieved to find such an amenable climate and greenery after the dry and cold of the Tibetan plateau.

With the help of the dzongpen (village head) and a local fixer, they rented a farmhouse where many of the photos from the expedition were later developed. Located in a grove of poplar and willow with small streams trickling along its boundary, we also visited this farmhouse—now owned by a Tibetan farmer who cheerily showed us around and introduced the three generations of his family.

The British expeditions’ investigations of the Kama valley are of particular interest as this valley sits on the climatic boundary between drier and wetter areas to the north and south of the Himalayan range. Howard-Bury described thick mists coming up the Kama valley each evening, providing significant moisture to the region: “As usual, in the evening, the clouds came up and enveloped us in a thick mist … When we started the following morning, there was still a thick Scotch mist which made the vegetation very wet … On the opposite side of the valley were immense black cliffs descending sheer for many thousand feet.”

Still evident today, this precipitation, combined with great variations in altitude and temperature, supports a profusion of plants—as well as animal life that our predecessors described as “extraordinarily tame.” Now as then, in summer, the hillsides are covered with the yellow, white and pink flowers of rhododendrons and azaleas, and huge juniper trees grow in the lower valley. Howard-Bury described spending “the whole afternoon lying among the rhododendrons at 15,000 feet—admiring the beautiful glimpses of these mighty peaks revealed by occasional breaks among the fleecy clouds.”

Adorned with prayer flags, the high passes are still used by local people as portals to the sacred Kama valley. In 1921, when he crossed the Langma pass to enter this “sanctuary,” Mallory wrote that the grumblings of his previously stubborn porters had suddenly transformed into “great friendliness” and “splendid marching”—such that they were “undepressed with the gloomy circumstance of again encamping in the rain.”

Descending into the Kama valley, Howard-Bury effused: “To the west, our gaze encountered a most wonderful amphitheater of peaks and glaciers. Three great glaciers almost met in the deep green valley that lay at our feet. One of these glaciers evidently came down from Mount Everest.”

While the topography here remains largely unchanged, the very significant reduction in the volume of the central glacier is evident in these comparison images:

In 1921, the expedition wrote that the outflow from the Kangshung glacier (which descends from Everest) had to “hurl itself into a great ice cavern” in order to flow under the Kandoshang glacier (from Makalu, the world’s fifth-highest peak) and become the Kama river. Today, as a result of glacial retreat, that ice cavern is no longer present and the main stream from the Kangshung glacier flows unimpeded along the snout of the Kangdoshang glacier.

Further up the valley, the 1921 expedition established another base camp in the high meadows towards the head of the valley at Pethang Ringmo, which, as well as a final camp stop for trekking groups today, remains an important grazing area for migratory yak herders. These herders were important sources of information for the early explorers, but today there is some evidence of overgrazing.

Howard-Bury commented: “We found ourselves among pleasant grassy meadows—it was a most delightfully sunny spot at 16,400 feet, right under the gigantic and marvelously beautiful cliffs of Chomolönzo—now all powdered over with the fresh snow of the night before and only separated from us by the Kangshung glacier, here about a mile wide. Great avalanches thunder down its sides all day long with a terrifying sound.”

A century later, avalanches continue to show us this is a dynamic landscape in a state of constant flux. Often, we would glimpse the rapid tumbling of ice and snow in a long white cloud, rushing down the steep couloirs seconds before the terrifying sound reaches you—reminding us of one of the major threats to climbers.

At the head of the Kama valley, the Kangshung face of Everest is perhaps the most impressive of all the sides of the mountain, towering some two miles above the glacier below. Both the north-east (Tibetan) and south-east (Nepalese) ridges—the most popular routes to the summit—are clearly visible from here. The Kangshung face itself was not climbed successfully until an assault by an American team in 1983, and the first British ascent of Everest without oxygen by Stephen Venables in 1988.

While initially, the mountains and peaks look remarkably similar to the 1920s, the drop in the level of the glacier quickly becomes apparent. The ordered glacial flow has been replaced by rocky detritus and numerous perched lakes, leaving a lunar-like landscape.

During his first visit, and despite having spent much of his life in the mountains of Europe, Mallory wrote that he was in awe of the vista here: “Perhaps the astonishing charm and beauty here lie in the complications half-hidden behind a mask of apparent simplicity, so that one’s eye never tires of following up the lines of the great arêtes, of following down the arms pushed out from their great shoulders, and of following along the broken edge of the hanging glacier covering the upper half of this eastern face of Everest.”

While Everest was the prize sought by all the expeditions, the sight of the Makalu massif, dominating the Kama valley to the south, appears to have had a greater impact on both the climbers. Howard-Bury claimed it was by “far the more beautiful mountain of the two,” while Mallory “saw a scene of magnificence and splendor even more remarkable than the facts suggest.”

He wrote: “Among all the mountains I have seen, and, if we may judge by photographs, all that ever have been seen, Makalu is incomparable for its spectacular and rugged grandeur. It was significant to us that the astonishing precipices rising above us on the far side of the glacier as we looked across from our camp—a terrific awe-inspiring sweep of snow-bound rocks—were the sides not so much of an individual mountain, but rather of a gigantic bastion or outwork defending Makalu.”

In fact, according to Howard-Bury, “the shepherds would insist that Makalu was the higher of the two mountains, and would not believe us when we said that Mount Everest was the higher.”

The future of the Everest region

This historical comparison of hundred-year-old images and quotes represents both the enduring mountains but also the rapid changes that the Himalayas now face. Forces of tourism on one hand and climate change on the other are posing huge challenges for these marginal environments.

Our research shows that tourist and climbing activity is having significant impacts on the region. The causes are both directly at the mountain but also at home, particularly in the damage that all of our consumptive lifestyles are having on Himalayan glaciers.

Of course, these activities have also brought much-needed development opportunities to local populations, and the residents of both the Nepalese and Tibetan sides are generally much better off than populations in less-visited areas of their respective countries.

The expected redesignation of the Qomolangma National Nature Preserve as a national park in the current Chinese central government plan may bring opportunities for further management locally as the crowds continue to grow. However, we also identified a shortfall in protecting the significant cultural heritage and longstanding spiritual relationship to the mountain, which is often eclipsed by its physical size.

Perhaps a more balanced relationship to the mountain and its people is required, one that reevaluates our rather unhealthy obsession with just one peak. Reading the accounts from the 1920s, one is aware that there was a deep reverence for the region—not only from local people but also from its British visitors.

In the intervening years, summit bids on the Tibetan side have historically been much lower than in Nepal. Closed to outsiders for much of the latter half of the last century, Tibetan ascents briefly became more popular in the 1990s and 2000s, with a few well-organized commercial operators. But closures in 2008 during Olympic preparations, and again during the COVID pandemic from 2020 to 2023, once again meant a much-reduced number of attempts.

Combined with less reliance on foreign exchange, China has been able to exert much more control on the climbing industry, and in 2024 did not charge a permit fee at all, preferring to ensure climbers were appropriately experienced. There may be merit in this approach, as no one was killed on the Tibetan side in 2024, as opposed to the eight climbers who perished on the southern side.

But on both sides of the mountain, it is highly unlikely that our global obsession with Everest will wane. As longtime chronicler Alan Arnette notes, the mountain has an “immutable attraction that is oddly perverse.” So, it is important we continue to monitor the changes in this dynamic landscape wrought by both its visitors and climate change.

To counter the rising commercialization of both mountaineering and mountain tourism requires, above all, greater respect for our mountains and the people who reside on them. According to Lakhpa Puti Sherpa, president of the Nepal Mountain Academy, notes: “The Himalayan mountains are holy spots—and we, the Sherpas, worship them. Before climbing any mountain, we worship it, begging apologies on having to step on it on the top, and asking to absolve the sin we are going to incur from this particular violence.”

Provided by The Conversation 

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

Frozen, thawed: How Arendelle’s glacier would fare under modern climate change

As a glaciologist who thinks about ice a lot, rewatching the movie Frozen umpteen times with my six-year-old daughter provides ample opportunity for my imagination to run wild. The movie is set in the fictional kingdom of Arendelle, which is modeled on a fjord landscape, complete with a large glacier at the head of Arenfjord. Ice unsurprisingly plays a very prominent role in the story. Yet this glacier receives very little attention.

Glaciers are receding across the world at an unprecedented rate. And on more than one occasion I have wondered how Arendelle’s glacier might have fared since the time of Frozen.

To add some scientific rigor to this thought experiment, it is useful to approximate a real geographical location. Arendelle is inspired by the fjords of western Norway, a region where most of the glaciers flow from the Jostedalsbreen ice cap, the largest ice mass in mainland Europe.

We can also approximate the date. Based on various clues, including the clothing and technology on show, it appears the events in Frozen take place one July in the mid-19th century. This means the glacier is depicted towards the end of the Little Ice Age, a cool period lasting several centuries during which most Northern Hemisphere glaciers expanded to their largest size in recent history.

In the movie, the glacier plunges from a high elevation plateau into the fjord below and looks steep and crevassed at the front. This implies a healthy, advancing glacier, in a similar condition to the many outlet glaciers of Jostedalsbreen that reached their Little Ice Age maximum positions around this time.

The short-term health of Arendelle’s glacier may have been further boosted by the unseasonal summer snowfall and cold temperatures that Elsa’s powers unleashed on the kingdom.

Real glaciers are shrinking fast

The fate of the fictional glacier since the Little Ice Age would have been less positive, as demonstrated by the very real glaciers of Jostedalsbreen. This period has been characterized by accelerated climate warming, causing widespread glacier retreat and thinning.

Since Elsa’s time, the real glaciers it’s based on have shrunk by about a fifth. Individual glaciers have retreated several kilometers at rates of up to 20 meters per year. This makes it likely that, without any further help from Elsa, Arendelle’s glacier would have retreated onto land within decades of the time of the film.

In the late 1980s and early 1990s, an increase in winter snowfall in western Norway meant most major glaciers in the region began to advance up to a few hundred meters. The Arendelle glacier might therefore have grown again for a time, although probably not enough for the glacier to re-enter the fjord. While there are other explanations, the more imaginative mind might consider the possibility that a descendent of Elsa was responsible for this period of increased snowfall.

Since the early 2000s, those same glaciers have shrunk significantly, retreating by up to 70 meters per year. That’s largely because higher air temperatures mean more ice is melting in summer. Several of Jostedalsbreen’s glaciers have retreated almost back onto the plateau, while others are disconnecting from the larger ice bodies that have been nourishing them for centuries.

What would Arendelle’s glacier look like today?

Retreat of this scale means the fictional glacier today might look something like Briksdalsbreen, now just a small tongue spilling over from the plateau ice behind. Indeed, it is quite possible that in 2025, designated by the UN as the International Year of Glaciers’ Preservation, Arendelle’s glacier would no longer have been visible from Arendelle Castle.

So, if Arendelle’s glacier were real, it would be a shadow of its 19th-century self—much like its real-life Norwegian equivalents. By 2050, approximately 200 years after the time of Frozen, the glacier would probably have retreated onto the plateau. The ice cap would also have thinned considerably and might even be in the early stages of terminal break up.

However, while this is one potential scenario for Jostedalsbreen in the 21st century, it is by no means certain. Climate scientists agree that concerted action is needed to reduce greenhouse gas emissions to limit warming.

Magic helped Arendelle once. This time, it’ll take real-world action to ensure the real glaciers have a fighting chance of still being around by the time Frozen 3 is finally released.

Provided by The Conversation 

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

New T-Rex ancestor discovered in drawers of Mongolian institute

Misidentified bones that languished in the drawers of a Mongolian institute for 50 years belong to a new species of tyrannosaur that rewrites the family history of the mighty T-Rex, scientists said Wednesday.

This slender ancestor of the massive Tyrannosaurus Rex was around four meters (13 feet) long and weighed three quarters of a tonne, according to a new study in the journal Nature.

“It would have been the size of a very large horse,” study co-author Darla Zelenitsky of Canada’s University of Calgary told AFP.

The fossils were first dug up in southeastern Mongolia in the early 1970s but at the time were identified as belonging to a different tyrannosaur, Alectrosaurus.

For half a century, the fossils sat in the drawers at the Institute of Paleontology of the Mongolian Academy of Sciences in the capital Ulaanbaatar.

Then Ph.D. student Jared Voris, who was on a trip to Mongolia, started looking through the drawers and noticed something was wrong, Zelenitsky said.

It turned out the fossils were well-preserved, partial skeletons of two different individuals of a completely new species.

“It is quite possible that discoveries like this are sitting in other museums that just have not been recognized,” Zelenitsky added.

‘Messy’ family history

They named the new species Khankhuuluu mongoliensis, which roughly means the dragon prince of Mongolia because it is smaller than the “king” T-Rex.

The dragon prince of Mongolia
Graphic on a newly identified dinosaur species, found in Mongolia and believed to be an ancestor of the Tyrannosaurus rex.

Zelenitsky said the discovery “helped us clarify a lot about the family history of the tyrannosaur group because it was really messy previously”.

The T-Rex represented the end of the family line.

It was the apex predator in North America until 66 million years ago, when an asteroid bigger than Mount Everest slammed into the Gulf of Mexico.

Three quarters of life on Earth was wiped out, including all the dinosaurs that did not evolve into birds.

Around 20 million years earlier, Khankhuuluu—or another closely related family member—is now believed to have migrated from Asia to North America using the land bridge that once connected Siberia and Alaska.

This led to tyrannosaurs evolving across North America.

Then one of these species is thought to have crossed back over to Asia, where two tyrannosaur subgroups emerged.

One was much smaller, weighing under a tonne, and was nicknamed Pinocchio rex for its long snout.

The other subgroup was huge and included behemoths like the Tarbosaurus, which was only a little smaller than the T-Rex.

One of the gigantic dinosaurs then left Asia again for North America, eventually giving rise to the T-Rex, which dominated for just two million years—until the asteroid struck.

More information: Jared T. Voris et al, A new Mongolian tyrannosauroid and the evolution of Eutyrannosauria, Nature (2025). DOI: 10.1038/s41586-025-08964-6.

Journal information: Nature 

© 2025 AFP

Fossil corals point to possibly steeper sea level rise under a warming world

Coastal planners take heed: Newly uncovered evidence from fossil corals found on an island chain in the Indian Ocean suggests that sea levels could rise even more steeply in our warming world than previously thought.

“This is not good news for us as we head into the future,” says Andrea Dutton, a professor of geoscience at the University of Wisconsin–Madison. Dutton and her Ph.D. student Karen Vyverberg at the University of Florida led an international collaboration that included researchers from the University of Sydney, University of Minnesota Twin Cities, Victoria University of Wellington and University of Massachusetts Amherst who analyzed fossilized corals discovered in the Seychelles islands.

These particular fossils provided an exceptional opportunity for researchers to reconstruct past sea levels. That’s in part because they’re remnants of coral species that only live in shallows very near the sea surface. Their tropical location also means they were far away from any past ice sheets, which have a more pronounced effect on local sea levels.

By determining the ages of two dozen fossil corals from various elevations on the islands and analyzing the sediments around the fossils, the team gathered a wealth of insights. The findings were published in the journal Science Advances.

First, the team was able to confirm the timing of peak global sea levels to between 122 and 123,000 years ago. That was during a period known as the Last Interglacial, when global temperatures were actually very similar to what they are now. Such a precise date gives us a better understanding of the relationship between global climate and sea levels.

Fossil corals point to possibly steeper sea level rise under a warming world
View of the coastline on La Digue, Seychelles. Corals can attach directly to the surface of the granite bedrock. Credit: Belinda Dechnik

Perhaps more importantly, though, the researchers discovered that there were three distinct periods of sudden and sharp sea-level rise over the 6,000 years leading up to peak sea levels during the Last Interglacial.

These abrupt pulses of sea-level rise were punctuated by periods of falling seas, and Dutton says they point to times when the polar ice sheets in Greenland and Antarctica—thousands of miles away from the Seychelles islands—were changing rapidly.

“That says there’s potential for this very rapid, dynamic change in both ice sheet volume and sea level change,” says Dutton. “This is hugely important for coastal planners, policymakers and those in the business of risk management.”

These rises and falls in sea level that the team documented also point to a key difference between the present and the Last Interglacial, which is sometimes used as a model for understanding how the current and future climate could affect ice sheets and sea levels due to the similar temperatures between the two time periods.

“These swings suggest that the polar ice sheets were growing and shrinking out of phase with each other as a result of temperature changes in the two hemispheres that were also not aligned,” says Dutton.

“So even though sea level rose at least several meters higher than present during this past warm period, if temperature rises simultaneously in both hemispheres as it is today, then we can expect future sea level rise to be even greater than it was back then.”

The researchers made one more sobering observation: One of the sharp pulses of sea-level rise they identified occurred at about the same time that the last remnants of a massive ice sheet in North America were likely collapsing, according to evidence collected by other teams working in the Atlantic Ocean.

Fossil corals point to possibly steeper sea level rise under a warming world
Dr. Andrea Dutton examines a limestone outcrop with fossil corals growing on the granite bedrock on La Digue, Seychelles. Credit: Belinda Dechnik

While there’s no large North American ice sheet today, Dutton says this finding has important implications for understanding the dynamics of other present-day ice sheets. That’s because most scientists have not previously considered a North American ice sheet as a major factor in sea-level dynamics during the Last Interglacial.

“But if ice was still present in North America several thousand years into this past warm period, then some of the rise we’ve documented would have required more meltwater from another ice sheet, such as Antarctica,” says Dutton.

“This would suggest that Antarctica was even more sensitive to warming than we previously recognized, because the full extent of sea-level rise flowing from the continent was masked by a remnant ice sheet in North America.”

In its totality, Dutton says the new evidence, thanks to fossilized corals from thousands of years ago, suggests that sea levels could rise even faster and higher thanks to climate change than current projections indicate.

“We could be looking at upward of 10 meters of global average sea-level rise in the future just based on the amount of warming that has already occurred,” she says.

The good news, as Dutton sees it, is that society has the means to blunt the impact of climate change on sea levels.

“The more we do to draw down our greenhouse gas emissions, and the faster we do so, could prevent the worst scenarios from becoming our lived reality,” Dutton says.

More information: Karen Vyverberg et al, Episodic reef growth in the Last Interglacial driven by competing influence of polar ice sheets to sea-level rise, Science Advances (2025). DOI: 10.1126/sciadv.adu3701www.science.org/doi/10.1126/sciadv.adu3701

Journal information: Science Advances 

Provided by University of Wisconsin-Madison 

How the disappearance of mastodons still threatens native South American forests

Ten thousand years ago, mastodons vanished from South America. With them, an ecologically vital function also disappeared: the dispersal of seeds from large-fruited plants. A new study led by the University of O’Higgins, Chile, with key contributions from IPHES-CERCA, demonstrates for the first time—based on direct fossil evidence—that these extinct elephant relatives regularly consumed fruit and were essential allies of many tree species.

Their loss was not only zoological; it was also botanical, ecological, and evolutionary. Some plant species that relied on mastodons for seed dispersal are now critically endangered.

The research, published in Nature Ecology & Evolution, presents the first solid evidence of frugivory in Notiomastodon platensis, a South American Pleistocene mastodon.

The findings are based on a multiproxy analysis of 96 fossil teeth collected over a span of more than 1,500 kilometers, from Los Vilos to Chiloé Island in southern Chile. Nearly half of the specimens come from the emblematic site of Lake Tagua Tagua, an ancient lake basin rich in Pleistocene fauna, located in the present-day O’Higgins Region.

The study was led by Erwin González-Guarda, researcher at the University of O’Higgins and associate at IPHES-CERCA, alongside an international team that includes IPHES-CERCA researchers Florent Rivals, a paleodiet specialist; Carlos Tornero and Iván Ramírez-Pedraza, experts in stable isotopes and paleoenvironmental reconstruction; and Alia Petermann-Pichincura. The study was carried out in collaboration with the Universitat Rovira i Virgili (URV) and the Universitat Autònoma de Barcelona (UAB), where Carlos Tornero is professor in the Department of Prehistory.

An ecological hypothesis finally proven

In 1982, biologist Daniel Janzen and paleontologist Paul Martin proposed a revolutionary idea: many tropical plants developed large, sweet, and colorful fruits to attract large animals—such as mastodons, native horses, or giant ground sloths—that would serve as seed dispersers. Known as the “neotropical anachronisms hypothesis,” this theory remained unconfirmed for more than 40 years. Now, the study led by González-Guarda provides direct fossil evidence that validates it.

To understand the lifestyle of this mastodon, the team employed various techniques: isotopic analysis, microscopic dental wear studies, and fossil calculus analysis.

“We found starch residues and plant tissues typical of fleshy fruits, such as those of the Chilean palm (Jubaea chilensis),” explains Florent Rivals, ICREA research professor at IPHES-CERCA and an expert in paleodiet. “This directly confirms that these animals frequently consumed fruit and played a role in forest regeneration.”

The forgotten role of large seed dispersers

“Through stable isotope analysis, we were able to reconstruct the animals’ environment and diet with great precision,” notes Iván Ramírez-Pedraza. The data point to a forested ecosystem rich in fruit resources, where mastodons traveled long distances and dispersed seeds along the way. That ecological function remains unreplaced.

“Dental chemistry gives us a direct window into the past,” says Carlos Tornero. “By combining different lines of evidence, we’ve been able to robustly confirm their frugivory and the key role they played in these ecosystems.”

A future threatened by an incomplete past

The extinction of mastodons broke a co-evolutionary alliance that had lasted for millennia. The researchers applied a machine learning model to compare the current conservation status of megafauna-dependent plants across different South American regions. The results are alarming: in central Chile, 40% of these species are now threatened—a rate four times higher than in tropical regions where animals such as tapirs or monkeys still act as alternative seed dispersers.

“Where that ecological relationship between plants and animals has been entirely severed, the consequences remain visible even thousands of years later,” says study co-author Andrea P. Loayza.

Species like the gomortega (Gomortega keule), the Chilean palm, and the monkey puzzle tree (Araucaria araucana) now survive in small, fragmented populations with low genetic diversity. They are living remnants of an extinct interaction.

Beyond its fossil discoveries, the study sends a clear message: understanding the past is essential to addressing today’s ecological crises. “Paleontology isn’t just about telling old stories,” concludes Florent Rivals. “It helps us recognize what we’ve lost—and what we still have a chance to save.”

More information: Erwin González-Guarda et al, Fossil evidence of proboscidean frugivory and its lasting impact on South American ecosystems, Nature Ecology & Evolution (2025). DOI: 10.1038/s41559-025-02713-8

Journal information: Nature Ecology & Evolution 

Provided by Autonomous University of Barcelona 

Two-million-year-old teeth transform theory of prehistoric human evolution

The enamel that forms the outer layer of our teeth might seem like an unlikely place to find clues about evolution. But it tells us more than you’d think about the relationships between our fossil ancestors and relatives.

In our new study, published in the Journal of Human Evolution, we highlight a different aspect of enamel.

In fact, we highlight its absence.

Specifically, we show that tiny, shallow pits in fossil teeth may not be signs of malnutrition or disease. Instead, they may carry surprising evolutionary significance.

You might be wondering why this matters.

Well, for people like me who try to figure out how humans evolved and how all our ancestors and relatives were related to each other, teeth are very important. And having a new marker to look out for on fossil teeth could give us a new tool to help fit together our family tree.

Uniform, circular and shallow

These pits were first identified in the South African species Paranthropus robustus, a close relative of our own genus Homo. They are highly consistent in shape and size: uniform, circular and shallow.

Initially, we thought the pits might be unique to P. robustus. But our latest research shows this kind of pitting also occurs in other Paranthropus species in eastern Africa. We even found it in some Australopithecus individuals, a genus that may have given rise to both Homo and Paranthropus.

The enamel pits have commonly been assumed to be defects resulting from stresses such as illness or malnutrition during childhood. However, their remarkable consistency across species, time and geography suggests these enamel pits may be something more interesting.

The pitting is subtle, regularly spaced, and often clustered in specific regions of the tooth crown. It appears without any other signs of damage or abnormality.

Two million years of evolution

We looked at fossil teeth from hominins (humans and our closest extinct relatives) from the Omo Valley in Ethiopia, where we can see traces of more than two million years of human evolution, as well as comparisons with sites in southern Africa (Drimolen, Swartkrans and Kromdraai).

The Omo collection includes teeth attributed to Paranthropus, Australopithecus and Homo, the three most recent and well-known hominin genera. This allowed us to track the telltale pitting across different branches of our evolutionary tree.

What we found was unexpected. The uniform pitting appears regularly in both eastern and southern Africa Paranthropus, and also in the earliest eastern African Australopithecus teeth dating back around 3 million years. But among southern Africa Australopithecus and our own genus, Homo, the uniform pitting was notably absent.

Teeth from Paranthropus robustus skulls found in South African caves provided evidence for migratory patterns
Teeth from Paranthropus robustus skulls found in South African caves provided evidence for migratory patterns (PA)

A defect … or just a trait?

If the uniform pitting were caused by stress or disease, we might expect it to correlate with tooth size and enamel thickness, and to affect both front and back teeth. But it doesn’t.

What’s more, stress-related defects typically form horizontal bands. They usually affect all teeth developing at the time of the stress, but this is not what we see with this pitting.

We think this pitting probably has a developmental and genetic origin. It may have emerged as a byproduct of changes in how enamel was formed in these species. It might even have some unknown functional purpose.

In any case, we suggest these uniform, circular pits should be viewed as a trait rather than a defect.

A modern comparison

Further support for the idea of a genetic origin comes from comparisons with a rare condition in humans today called amelogenesis imperfecta, which affects enamel formation.

About one in 1,000 people today have amelogenesis imperfecta. By contrast, the uniform pitting we have seen appears in up to half of Paranthropus individuals.

Although it likely has a genetic basis, we argue the even pitting is too common to be considered a harmful disorder. What’s more, it persisted at similar frequencies for millions of years.

Paranthropus enamel pitting
Paranthropus enamel pitting (Journal of Human Evolution)

A new evolutionary marker

If this uniform pitting really does have a genetic origin, we may be able to use it to trace evolutionary relationships.

We already use subtle tooth features such as enamel thickness, cusp shape, and wear patterns to help identify species. The uniform pitting may be an additional diagnostic tool.

For example, our findings support the idea that Paranthropus is a “monophyletic group”, meaning all its species descend from a (relatively) recent common ancestor, rather than evolving seperatly from different Australopithecus taxa.

And we did not find this pitting in the southern Africa species Australopithecus africanus, despite a large sample of more than 500 teeth. However, it does appear in the earliest Omo Australopithecus specimens.

So perhaps the pitting could also help pinpoint from where Paranthropus branched off on its own evolutionary path.

An intriguing case

One especially intriguing case is Homo floresiensis, the so-called “hobbit” species from Indonesia. Based on published images, their teeth appear to show similar pitting.

If confirmed, this could suggest an evolutionary history more closely tied to earlier Australopithecus species than to Homo. However, H. floresiensis also shows potential skeletal and dental pathologies, so more research is needed before drawing such conclusions.

More research is also needed to fully understand the processes behind the uniform pitting before it can be used routinely in taxonomic work. But our research shows it is likely a heritable characteristic, one not found in any living primates studied to date, nor in our own genus Homo (rare cases of amelogenesis imperfecta aside).

As such, it offers an exciting new tool for exploring evolutionary relationships among fossil hominins.

Fossilised stomach reveals sauropod dinosaur’s final meal

Since the late 19th century, sauropod dinosaurs (long-necks like Brontosaurus and Brachiosaurus) have been almost universally regarded as herbivores, or plant eaters.

However, until recently, no direct evidence – in the form of fossilised gut contents – had been found to support this.

I was one of the palaeontologists on a dinosaur dig in outback Queensland, Australia, that unearthed “Judy”: an exceptional sauropod specimen with the fossilised remains of its last meal in its abdomen.

In a new paper published in Current Biology, we describe these gut contents while also revealing that Judy is the most complete sauropod, and the first with fossilised skin, ever found in Australia.

Remarkably preserved, Judy helps to shed light on the feeding habits of the largest land-living animals of all time.

Plant-eating land behemoths

Sauropod dinosaurs dominated Earth’s landscapes for the entire 130 million years of the Jurassic and Cretaceous periods. Along with many other species, they died out in the mass extinction event at the end of the Cretaceous 66 million years ago.

Ever since the first reasonably complete sauropod skeletons were found in the 1870s, the hypothesis that they were herbivores has rarely been contested. Simply put, it is hard to envisage sauropods eating anything other than plants.

Their relatively simple teeth were not adapted for tearing flesh or crushing bone. Their small brains and ponderous pace would have prevented them from outsmarting or outpacing most potential prey.

Some of the many plant fossils found within Judy’s gut contents, including conifer bracts (B) and a seed fern seed pod (C)
Some of the many plant fossils found within Judy’s gut contents, including conifer bracts (B) and a seed fern seed pod (C) (2025: Current Biology)

And to sustain their huge bodies, sauropods would have had to eat regularly and often, necessitating an abundant and reliable food source – plants.

Although the general body plan of sauropods seems pretty uniform – stocky, on all fours, with long necks – these behemoths did vary when we look more closely.

Some had squared-off snouts with tiny, rapidly replaced teeth confined to the front of the mouth. Others had rounded snouts, with much more robust teeth, arranged in a row that extended farther back in the mouth. Neck length varied greatly (with some necks up to 15 metres long), as did neck flexibility. In addition, a few of them had taller shoulders than hips.

Absolute size varied too – some were less enormous than others. All of these factors would have constrained how high above ground each species could feed and which plants they could reach.

Food in the belly

Sauropod discoveries are becoming more regular in outback Queensland, thanks largely to the Australian Age of Dinosaurs Museum in Winton.

In 2017, I helped the museum unearth a roughly 95-million-year-old sauropod, nicknamed Judy after the museum’s co-founder Judy Elliott.

We soon realised this find was extraordinary. Besides being the most complete sauropod skeleton and skin ever found in Australia, Judy’s belly region hosted a strange rock layer. It was about two square metres in area and ten centimetres thick on average, chock-full of fossil plants.

The fact that this plant-rich layer was confined to Judy’s abdomen and located on the inside surface of the fossil skin, made us wonder – had we unearthed the remains of Judy’s last meal or meals?

If so, we knew we had something special on our hands: the first sauropod gut contents ever found.

Multi-level feeding

Analysis of Judy’s skeleton, which was prepared out of the surrounding rock by volunteers in the museum’s laboratory, enabled us to classify her as a Diamantinasaurus matildae.

We scanned portions of Judy’s gut contents with X-rays at the Australian Synchrotron in Melbourne and at CSIRO in Perth, and with neutrons at Australia’s Nuclear Science and Technology Organisation in Sydney.

This enabled us to digitally visualise the plants – which were preserved as voids within the rock – without destroying them.

We did destructively sample some small portions of the gut contents to figure out their chemical make-up, along with the skin and surrounding rock.

This revealed the gut contents were turned to stone by microbes in an acidic environment (stomach juices, perhaps), with minerals likely derived from the decomposition of Judy’s own body tissues.

Small portion of Judy’s skin, showing approximately hexagonal scales covered in tiny lumps (termed papillae)
Small portion of Judy’s skin, showing approximately hexagonal scales covered in tiny lumps (termed papillae) (2025: Current Biology)

Judy’s gut contents confirm that sauropods ate their greens but barely chewed them – their gut flora did most of the digestive work.

Most importantly, we can tell Judy ate bracts from conifers (relatives of modern monkey puzzle trees and redwoods), seed pods from extinct seed ferns, and leaves from angiosperms (flowering plants) just before she died.

Conifers then, as now, would have been huge, implying Judy fed well above ground level. By contrast, flowering plants were mostly low-growing in the mid-Cretaceous.

Based on other specimens (especially teeth), scientists previously thought Diamantinasaurus browsed plants relatively high off the ground. The conifer bracts in Judy’s belly support this.

However, Judy was not fully grown when she died, and the angiosperms in her belly imply lower-level feeding, as well. It seems likely, then, that the diets of some sauropods changed slightly as they grew. Nevertheless, they were lifelong vegetarians.

Judy’s skin and gut contents are now on display at the Australian Age of Dinosaurs Museum in Winton. I’m not sure how I’d feel about having the remains of my last meal publicly exhibited for all to see posthumously, but if it helped the cause of science, I think I’d be OK with it.

Early apes evolved in tropical forests disturbed by fires and volcanoes, fossil find suggests

Great apes began to diverge from other primates about 25 million years ago, according to eastern African fossil records. Though it would take another 20 million or so years for upright-walking hominins to appear, understanding the habitats of early apes helps clarify how environments drove the evolution of our distant ancestors.

Venanzio Munyaka and colleagues excavated and analyzed fossils from an approximately 20-million-year-old early Miocene site in western Kenya called Koru 16. The now-extinct Tinderet Volcano repeatedly blanketed the area in ash, preserving it for millions of years, and today, the site hosts fossils from an array of plants and animals. Their study is published in the journal Paleoceanography and Paleoclimatology.

Many prior studies focused on the area around Koru 16: The first primate fossils from the site were discovered in 1927, and famed anthropologist Louis Leakey led multiple digs there.

As part of the new research, scientists uncovered fossils of approximately 1,000 leaves and many vertebrates at two subsites between 2013 and 2023. The specimens included those of a new type of large-bodied ape and two other previously known ape species, bringing the total number of vertebrate species discovered at the site to 25.

By examining the shapes of fossilized leaves, the geochemistry of fossilized soils (paleosols), and the distribution and density of fossil tree stumps, the researchers determined that the Koru 16 site was likely located within a warm, wet forest, with rainfall amounts similar to those of modern-day tropical and seasonal African forests.

However, the ancient ecosystem likely hosted more deciduous plants than do modern tropical forests. The vertebrate fossils the researchers analyzed were consistent with apes, pythons, and rodents that might have lived in such an environment.

The researchers suggest that this ancient forest environment—which was interspersed with open areas and frequently disturbed by fires, floods, or volcanic eruptions—played a role in shaping the course of evolution for early apes.

More information: Venanzio Munyaka et al, Insights on the Paleoclimate and Paleoecology of an Early Miocene Hominoid Site: A Multiproxy Study From Koru, Western Kenya, Paleoceanography and Paleoclimatology (2025). DOI: 10.1029/2025PA005152

Journal information: Paleoceanography and Paleoclimatology 

Provided by Eos

This story is republished courtesy of Eos, hosted by the American Geophysical Union. Read the original story here.