Friday, June 13, 2025

 

Famous Ice Age ‘puppies’ likely wolf cubs and not dogs, study shows




University of York
Ice Age wolf siblings 

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One of the wolf cub siblings uncovered near Tumat

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Credit: Mietje Germonpré Royal Belgian Institute of Natural Sciences




New analysis of the remains of two ‘puppies’ dating back more than 14,000 years ago has shown that they are most likely wolves, and not related to domestic dogs, as previously suggested.

The genetic analysis also proved that the cubs were sisters at the age of around two months, and like modern day wolves had a mixed diet of meat and plants. Researchers, however, were surprised to see evidence of a wooly rhinoceros as part of their last meals, as this would have been a considerably large animal for a wolf to hunt.

The ‘Tumat Puppies’ are two remarkably well-preserved puppy remains found in northern Siberia, about 40 km from Tumat, the nearest village. One was found in 2011 and the other in 2015 at what’s now called the Syalakh site. 

The puppies were discovered in layers of soil, preserved in ice, alongside the bones of woolly mammoths, some of which showed signs of having been burned and processed by humans. This led scientists to wonder if the site was once used by humans to butcher mammoths, and whether the puppies might have had a connection to people, possibly as early dogs or tamed wolves that hung around humans for food.

There are no visible injuries or signs of attack to the cubs, and so they were likely to have been inside an underground den, resting after their meal, until a potential landslide collapsed their home, trapping the cubs inside. 

A new study, led by the University of York, however, has shown that, based on genetic data from the animals’ gut contents and other chemical ‘fingerprints’ found in their bones, teeth and tissue, that the way they were living, what they were eating, and the environment they existed in, points to the puppies being wolf cubs and not early domesticated dogs.

Both were already eating solid food, including woolly rhinoceros meat and, in one case, a small bird called a wagtail. However, their bodies still showed signs of having nursed, meaning they were likely still getting milk from their mother too.

Despite being found near human-modified mammoth bones, there was no evidence of the cubs consuming mammoth, but the piece of wooly rhinoceros skin found in the stomach of one of the cubs had not been fully digested, suggesting they died not long after their last meal.

It is thought that the wooly rhinoceros may have been a young calf, rather than a fully grown adult, and likely hunted by the adult pack and fed to the cubs, but even if this was the case, a young woolly rhinoceros would have been considerably bigger than prey modern-day wolves typically hunt.

This has led researchers to think that these Pleistocene wolves may have been somewhat bigger than the wolves of today. Previous DNA testing suggests that the cubs most likely belonged to a wolf population that eventually died out and didn’t lead to today’s domestic dogs.

Anne Kathrine Runge, from the University of York’s Department of Archaeology, who analysed the cubs as part of her PhD, said: “It was incredible to find two sisters from this era so well preserved, but even more incredible that we can now tell so much of their story, down to the last meal that they ate.”

The original hypothesis that the Tumat Puppies were dogs is also based on their black fur colour, which was believed to have been a mutation only present in dogs, but the Tumat Puppies challenge that hypothesis as they are not related to modern dogs.

Anne Kathrine added: “Whilst many will be disappointed that these animals are almost certainly wolves and not early domesticated dogs, they have helped us get closer to understanding the environment at the time, how these animals lived, and how remarkably similar wolves from more than 14,000 years ago are to modern day wolves.

“It also means that the mystery of how dogs evolved into the domestic pet we know today deepens, as one of our clues - the black fur colour - may have been a red herring given its presence in wolf cubs from a population that is not related to domestic dogs.”

Tiny fossilised plant remains were discovered in the cubs’ stomachs, indicating that they lived in a diverse environment with a variety of plants and animals to consume, including prairie grasses, leaves from the shrub genus Dryas and willow twigs. This suggests the landscape they inhabited included different types of habitats that could support rich and varied ecosystems.

Dr Nathan Wales, from the University of York’s Department of Archaeology, said: “We know grey wolves have been around as a species for hundreds of thousands of years based on skeletal remains from palaeontological sites, and researchers have done DNA testing of some of those remains to understand how the population changed over time. The soft tissues preserved in the Tumat Puppies, however, gives us access to other ways of investigating wolves and their evolutionary line.

“We can see that their diets were varied, consisting of both animal meat and plant life, much like that of modern wolves, and we have an insight into their breeding behaviours too. The pair were sisters and likely being reared in a den and cared for by their pack - all common characteristics of breeding and raising of offspring in wolves today. 

“Today, litters are often larger than two, and it is possible that the Tumat Puppies had siblings that escaped their fate. There may also be more cubs hidden in the permafrost or lost to erosion.

“The hunting of an animal as large as a wooly rhinoceros, even a baby one, suggests that these wolves are perhaps bigger than the wolves we see today, but still consistent in many ways, because wolves still tend to hunt easy prey while some of the pack is engaged in cub rearing.”

The research findings, however, means that the hunt for the oldest dog - and their place of origin - is still on. 

The research, in collaboration with researchers based in Belgium, Canada, Denmark, Germany, Russia and Sweden is published in the journal Quaternary Research.

 

Triassic reptiles took 10,000 mile trips through “hellish” conditions, study suggests



First study to consider how ancient reptiles dispersed across the Earth after end-Permian mass extinction



University of Birmingham





The forerunners of dinosaurs and crocodiles in the Triassic period were able to migrate across areas of the ancient world deemed completely inhospitable to life, new research suggests.

 

In a paper published in Nature Ecology and Evolution today (11th June), researchers from the University of Birmingham and University of Bristol have used a new method of geographical analysis to infer how these ancestral reptiles, known as archosauromorphs, dispersed following one of the most impactful climate events the Earth has ever seen, the end-Permian mass extinction.

 

The first archosauromorphs, some resembling modern reptiles and many times smaller than familiar dinosaurs, were previously believed to only survive in certain parts of the globe due to extreme heat across the tropics, viewed by many palaeontologists as a dead zone, in the earliest Triassic.

 

By developing a new modelling technique based on landscape reconstructions and evolutionary trees, the team of researchers have been able to discover clues about how these reptiles moved around the world during the Triassic period, following the mass extinction where more than half of land-based animals and 81% of marine life died.

 

The archosauromorphs that survived the extinction event rose to prominence in Earth’s ecosystems in the Triassic, leading to the evolution of dinosaurs. The team now suggest that their later success was in part due to their ability to migrate up to 10,000 miles across the tropical dead zone to access new ecosystems.

 

Dr Joseph Flannery-Sutherland from the University of Birmingham and corresponding author of the study said:

 

“Amid the worst climatic event in Earth’s history, where more species died than at any period since, life still survived. We know that archosauromorphs as a group managed to come out of this event and over the Triassic period became one of the main players in shaping life thereafter.

 

“Gaps in their fossil record have increasingly begun to tell us something about what we weren’t seeing when it comes to these reptiles. Using our modelling system, we have been able to build a picture of what was happening to the archosauromorphs in these gaps and how they dispersed across the ancient world. This is what led us to call our method TARDIS, as we were looking at terrains and routes directed in space-time.

 

“Our results suggest that these reptiles were much hardier to the extreme climate of the Pangaean tropical dead zone, able to endure these hellish conditions to reach the other side of the world. It’s likely that this ability to survive the inhospitable tropics may have conferred an advantage that saw them thrive in the Triassic world.”

 

“The evolution of life has been controlled at times by the environment,” says Professor Michael Benton from the University of Bristol, senior author of the study, “but it is difficult to integrate our limited and uncertain knowledge about the ancient landscape with our limited and uncertain knowledge about the ecology of extinct organisms. But by combining the fossils with reconstructed maps of the ancient world, in the context of evolutionary trees, we provide a way of overcoming these challenges.”

 

Paleontologists from the University of Calgary identify closest-known ancestor to Tyrannosaurs



Khankhuuluu was a precursor to the famous bone-crushing kings of the Cretaceous



University of Calgary

University of Calgary paleontologists identify closest-known ancestor to Tyrannosaurs 

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Darla Zelenitsky, a paleontologist and associate professor in the Faculty of Science, and Jared Voris, a PhD candidate, have identified a new species of dinosaur named Khankhuuluu. They, along with a team of international scientists, have published a paper in the journal, Nature, about the evolution of Tyrannosaurs.

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Credit: Riley Brandt/University of Calgary





Paleontologists have identified a new species of dinosaur, Khankhuuluu, which is being described as the closest-known ancestor to the giant Tyrannosaurs.

The finding by an international team of researchers – led by Jared Voris and Dr. Darla Zelenitsky in the Faculty of Science at the University of Calgary – is published in the journal Nature.

Voris, first author and a PhD candidate in the Department of Earth, Energy, and Environment, says the new species of Tyrannosaur would have lived 86 million years ago and was a medium-sized, fleet-footed predator that evolved after the extinction of other large predatory dinosaurs.

Khankhuuluu was the closest ancestor to the behemoths famously depicted in media like Jurassic Park, the Tyrannosaurs.

“This new species provides us the window into the ascent stage of Tyrannosaur evolution; right when they’re transitioning from small predators to their apex predator form," says Voris.

Khankhuuluu translates from Mongolian to mean “prince of dragons” or “the dragon prince.” The name denotes its place in the lineage of Tyrannosaurs, as Khankhuuluu was the prince before species like Tyrannosaurus rex, the Tyrant Lizard King. As the closest-known ancestor, Khankhuuluu shares many characteristics with its Tyrannosaur descendants – though it lacked some of the more defining features that Tyrannosaurs had. The new species weighed 750 kilograms (about the size of a horse), making it two to three times smaller than its massive descendants.

Khankhuuluu had tiny rudimentary horns that would evolve to be more noticeable in species like Albertosaurus or Gorgosaurus used for mating display or intimidation. It had a long, shallow skull that shows Khankhuuluu didn’t have the ability to crunch through bone like the T. rex. The new species can be defined as a mesopredator, similar to coyotes, meaning it used speed and agility to take down its prey.

The fossils, found in the Bayanshiree Formation in southeastern Mongolia, had been studied in the 1970’s by paleontologist Altangerel Perle. Perle likened the fossils to another medium-sized Tyrannosaur called Alectrosaurus from China. Voris went to Mongolia in 2023 to study fossils at the Institute of Paleontology – and soon realized there were features that differentiated them from the Alectrosaurus.

The discovery also provides more details into Tyrannosaur evolution.

Khankhuuluu, or a closely related species, would have immigrated to North America from Asia around 85 million years ago," explains Zelenitsky, a paleontologist and associate professor in the Department of Earth, Energy and Environment. "Our study provides solid evidence that large Tyrannosaurs first evolved in North America as a result of this immigration event."

The results of the study show the movement of Tyrannosaurs back and forth between Asia and North America was less frequent and less sporadic than previously known. Khankhuuluu is the last known ancestor of Tyrannosaurs found in the Asian fossil record.

The research reveals that the new species, or one of its kin, travelled across a land bridge into North America, where it evolved into the famous apex predator Tyrannosaurs. The fossil record indicates Tyrannosaurs were exclusive to North America for few million years before immigrating to Asia, where the lineage split into two groups. One group branched off to become even bigger apex predators, ultimately evolving into T. rex, and the other group evolved into a medium-sized long-snouted species (dubbed ‘Pinocchio rexes’).

Looking ahead, the next step for researchers is to investigate the earlier ancestors of these apex predators, which are still poorly known.

Darla Zelenitsky, a paleontologist and associate professor in the Faculty of Science, and Jared Voris, a PhD candidate, have identified a new species of dinosaur named Khankhuuluu. They, along with a team of international scientists, have published a paper in the science journal, Nature, about the evolution of Tyrannosaurs.

Credit

Riley Brandt/University of Calgary

 

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




University of Wisconsin-Madison

Fossil coral 

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Fossil coral exposed in a limestone outcrop above present sea level in the Seychelles. 

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Credit: Belinda Dechnik





SEYCHELLES — 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 PhD student Karen Vyverberg at the University of Florida led an international collaboration that included researchers from 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 the 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 will be published June 13 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.

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, policy makers 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.

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.

This research received funding from the National Science Foundation (grant awards 1155495, 1159040, 1934477, 2035080 and 2202913).

View of the coastline on La Digue, Seychelles. Corals can attach directly to the surface of the granite bedrock.

Dr. Andrea Dutton examines a limestone outcrop with fossil corals growing on the granite bedrock on La Digue, Seychelles.

Credit

Belinda Dechnik

 

Bodybuilding in ancient times: How the sea anemone got its back



New insights into the evolution of the back-belly-axis



University of Vienna

Fig. 1: Adult polyp of the sea anemone Nematostella vectensis. 

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Fig. 1: Adult polyp of the sea anemone Nematostella vectensis.

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Credit: Grigory Genikhovich





A new study from the University of Vienna reveals that sea anemones use a molecular mechanism known from bilaterian animals to form their back-to-belly body axis. This mechanism ("BMP shuttling") enables cells to organize themselves during development by interpreting signaling gradients. The findings, published in Science Advances, suggest that this system evolved much earlier than previously assumed and was already present in the common ancestor of cnidarians and bilaterians.

Most animals exhibit bilateral symmetry—a body plan with a head and tail, a back and belly, and left and right sides. This body organization characterizes the vast group known as Bilateria, which includes animals as diverse as vertebrates, insects, molluscs and worms. In contrast, cnidarians, such as jellyfish and sea anemones, are traditionally described as radially symmetric, and indeed jellyfish are. However, the situation is different is the sea anemones: despite superficial radiality, they are bilaterally symmetric – first at the level of gene expression in the embryo and later also anatomically as adults. This raises a fundamental evolutionary question: did bilateral symmetry arise in the common ancestor of Bilateria and Cnidaria, or did it evolve independently in multiple animal lineages? Researchers at the University of Vienna have addressed this question by investigating whether a key developmental mechanism called BMP shuttling is already present in cnidarians.

Shuttling for development

In bilaterian animals, the back-to-belly axis is patterned by a signaling system involving Bone Morphogenetic Proteins (BMPs) and their inhibitor Chordin. BMPs act as molecular messengers, telling embryonic cells where they are and what kind of tissue they should become. In bilaterian embryos, Chordin binds BMPs and blocks their activity in a process called "local Inhibition". At the same time, in some but not all bilaterian embryonic models, Chordin can also transport bound BMPs to other regions in the embryo, where they are released again – a mechanism known as "BMP shuttling". Animals as evolutionary distant as sea urchins, flies and frogs use BMP shuttling, however, until now it was unclear whether they all evolved shuttling independently or inherited it from their last common ancestor some 600 million years ago. Both, local inhibition and BMP shuttling, create a gradient of BMP activity across the embryo. Cells in the early embryo detect this gradient and adopt different fates depending on BMP levels. For example, in vertebrates, the central nervous system forms where BMP signaling is lowest, kidneys will develop at intermediate BMP signaling levels, and the skin of the belly will form in the area of maximum BMP signaling. This way, the body's layout from back to belly is established. To find out whether BMP shuttling by Chordin represents an ancestral mechanism for patterning the back to belly axis, the researchers had to look at bilaterally symmetric animals outside Bilateria – the sea anemones.

An Ancient Blueprint

To test whether sea anemones use  Chordin as a local inhibitor or as a shuttle, the researchers first blocked Chordin production in the embryos of the model sea anemone Nematostella vectensis. In Nematostella, unlike in Bilateria, BMP signaling requires the presence of Chordin, so, without Chordin, BMP signaling ceased and the formation of the second body axis failed. Chordin was then reintroduced into a small part of the embryo to see if it could restore axis formation. BMP signaling resumed—but it was unclear whether this was because Chordin simply blocked BMPs locally, allowing a gradient to form from existing BMP sources, or because it actively transported BMPs to distant parts of the embryo, shaping the gradient more directly. To answer this, two versions of Chordin were tested—one membrane-bound and immobile, the other diffusible. If Chordin acted as a local inhibitor, both, the immobile and the diffusible Chordin would restore BMP signaling on the side of the embryo opposite to the Chordin producing cells. However, only diffusible Chordin can act as a BMP shuttle. The results were clear: Only the diffusible form was able to restore BMP signaling at a distance from its source, demonstrating that Chordin acts as a BMP shuttle in sea anemones—just as it does in flies and frogs. 

A shared strategy across over 600 million years of evolution?

The presence of BMP shuttling in both cnidarians and bilaterians suggests that this molecular mechanism predates their evolutionary divergence some 600-700 million years ago. "Not all Bilateria use Chordin-mediated BMP shuttling, for example, frogs do, but fish don't, however, shuttling seems to pop up over and over again in very distantly related animals making it a good candidate for an ancestral patterning mechanism. The fact that not only bilaterians but also sea anemones use shuttling to shape their body axes, tells us that this mechanism is incredibly ancient," says David Mörsdorf, first author of the study and postdoctoral researcher at the Department of Neurosciences and Developmental Biology at the University of Vienna. "It opens up exciting possibilities for rethinking how body plans evolved in early animals."

Grigory Genikhovich, senior author and group leader at the same department, adds: "We might never be able to exclude the possibility that bilaterians and bilaterally symmetric cnidarians evolved their bilateral body plans independently. However, if the last common ancestor of Cnidaria and Bilateria was a bilaterally symmetric animal, chances are that it used Chordin to shuttle BMPs to make its back-to-belly axis. Our new study showed that." 

(The study was supported by the Austrian Science Fund (FWF), grants P32705 and M3291.)

Fig. 2: Blocked Chordin protein production by microinjection of Chordin MO (left). This effect can be rescued by injecting Chordin mRNA into the Embryo (the descendants of the injected cell are stained orange in the embryo on the right).

Credit

David Mörsdorf, Grigory Genikhovich