Showing posts with label mammoth. Show all posts
Showing posts with label mammoth. Show all posts

Sunday, 14 December 2025

Prehistoric Mammal Discoveries 2025

Image
Computer reconstruction of the skeleton of the Miocene
 right whale Megabalaena, published this year
As another year draws to a close, it's time to take another dash through the mammalian palaeontological findings of the last twelve months. As always, this will be a rapid survey of some discoveries that I find particularly interesting without any detailed discussion, but hopefully covering as wide a range of prehistoric mammals as I can.

Large Herbivores

Land mammals don't come much larger than mammoths, and such animals, and their mastodon relatives, have shaped the world around them through their mere presence and the food they chose to eat. A study on southern mammoths (Mammuthus meridionalis) uncovered at a million-year-old site in northern Spain showed that the climate at the time was already Mediterranean, a warm gap within the Ice Ages, causing them to feed more on grasslands than trees. While hyenas had fed on some of the carcasses, they were not alone, as the evidence also shows clear signs of butchering with stone tools.

Elsewhere, a new study found that the South American gomphothere, Notiomastodon, which had entered the continent when the Panama Land Bridge formed, had a diet rich in fruit. When they went extinct as the climate warmed 10,000 years ago, their disappearance spelt trouble for the plants with large, fleshy fruit that had relied on them for seed dispersal.

But if Spain had a reasonably modern Mediterranean climate one million years ago, that obviously didn't last. Although we know they must have existed earlier, until this year, the oldest known cold-adapted mammals from Spain dated to no more 190,000 years ago, during the second-to-last Ice Age. This year, however, a reindeer tooth was described from the country that could date back as far as 300,000 years, during the Ice Age prior to that - it's the most southerly known reindeer fossil ever discovered. 

On the subject of deer, a new analysis of the DNA of the Toronto Subway deer (Torontoceros hypogaeus) discovered during the construction of the eponymous transport system suggested that, while undeniably a distinct species, it might be more closely related to the living white-tailed deer than previously thought. It lived in open habitats, and was driven to extinction at least partly by the spread of the forests that now cover the area.

Studies of isotope ratios in the short-legged hippo-shaped rhinceros Teleoceras from Nebraska showed that they lived in much in the same areas throughout their lives, not migrating, or even moving as far as we would expect when they reached adulthood and left their parents. This may have been because they relied on habitats with plenty of water to wallow in, and they just couldn't find them elsewhere. Over in eastern Siberia, the longest ever fossilised horn from a woolly rhino (Coelodonta antiquitatis) was described; it was over 164 cm (65 inches) long, far larger than those of any living rhino.

Fossils are not necessarily of things like bones and horns, however. This year, the oldest known fossilised cowpat was described from 20 million-year-old deposits, also in Nebraska. At least it looks like a cowpat - it's about the right size and shape, and it's obviously dung - but cows didn't exist that far back, and, honestly, neither did anything closely related to them. So, probably a ruminant of some sort, but what kind will likely always remain a mystery.

Carnivores

Europe is devoid of big cats today, unless you count the occasional lynx. This was not always so, however, and a publication this year expanded the range of the European jaguar (Panthera gombazagoensis) to Poland and to Suffolk in England between 700,000 and 350,000 years ago. Another large cat, the famous sabretooth Smilodon fatalis, was discovered further south than ever before - in Uruguay

We already knew about leopards (the modern species) in the Pyrenees during the Ice Ages, but their fossils are rare. A new study of their overall distribution and history showed that they became steadily larger as the Pleistocene wore on, and also that males and females were more similar in size than in living members of their species. Moreover, they showed a preference for mountainous habitats, and their body shape shifted towards that of modern snow leopards prior to their local extinction.

The largest mammalian carnivore during the Ice Ages in North America was the giant short-faced bear (Arctodus simus), with some individuals estimated to have weighed up to 950 kg (2,000 lbs). However, some fossils were significantly smaller than this and had been suggested to represent a distinct subspecies. Genetic analysis this year was unable to find any significant differences between the larger and smaller specimens except for one: all the large ones were male, and the small ones female...

And, well, yes, I should probably mention this, since it was all over the news. This year, a company claimed to have returned the dire wolf (Aenocyon dirus) from extinction, in the form of three, rather cute, white puppies. Almost nobody outside the company with any expertise agrees that this is really what they have done, simply adding a few dire wolf-like genes to what are rather obviously grey wolves.

Cetaceans are also carnivores, although descended from creatures that were not. An analysis of the skull of the very primitive dolphin-sized Protocetus showed that it had already developed the large brain that cetaceans are known for today but, more importantly, that it still had a keen sense of smell. Modern whales and dolphins have no use for smell but Protocetus likely spent at least some of its time on land, giving it a very different lifestyle.

Among more recognisable whales, Idiophorus is either the most primitive known sperm whale or a close relative of their last common ancestor. Recovered from Miocene age deposits in Patagonia, it had a long snout shaped like a wine bottle (so hardly like a modern sperm whale) and was around 6.6 metres (22 feet) in length. The key fossil was thoroughly re-examined this year for the first time since it was uncovered in the 19th century, revealing that it was a deadly predator feeding on relatively large vertebrate prey, unlike other known sperm whale species living in the area at the time. 

At the other end of the Americas, and a few million years earlier, Fucaia was a Canadian whale belonging to a now-extinct group. Analysis of a well-preserved fossil this year showed that, like Idiophorus, it was an agile and active predator, although, partly because it was rather smaller, its hunting style was probably most like that of a modern sea lion. Despite this, its closest living relatives include the toothless krill-feeding baleen whales.

Other Placentals

Glyptodonts were gigantic relatives of armadillos, their heavy armour plating making them the mammalian equivalent of tanks. A study this year provided the first analysis of damage to that armour in three South American species, adding to those already performed on more common ones. It also confirmed that, like certain dinosaurs, they likely did wallop each other with the clubs on their tails, likely while competing for mates or territory.

Ground sloths have a long evolutionary history, much larger relatives of the small(ish) tree-dwelling animals that are their only remaining close relatives. A new analysis shows how they gradually increased in size as the climate shifted, but that, probably to the surprise of few people, it was not climate change that eventually drove them to extinction, but the arrival of humans. 

Look at any reconstruction of a ground sloth, and it will inevitably show a large, somewhat shaggy animal. But it had been argued that, like elephants and rhinos, the largest ground sloths may not have had much fur at all, being so big that they did not lose much body heat anyway. It was a minority view, but geochemical analyses and simulations published this year seem to put the nail in its coffin. Given the relatively cool environments in which they lived, the simulations suggest that even the largest species would have needed a pelt of fur 10mm (0.4 inches) thick, and some would have needed fur three to five times that long. This, despite the fact that palaeothermometric analysis in the same study showed that they had unusually low body temperatures for their size.

Several studies this year took a look at the development of increasing brain size during primate evolution - primarily monkeys and apes. They did not all come to the same conclusions, which, while they don't necessarily contradict one another, either, suggests that there was probably a lot going on rather than one single answer. One study pinpoints visual processing as the main factor, with visual parts of the brain becoming disproportionately large before the rest caught up, something that would make sense for an animal that had to navigate through tree branches.

Another points to socialisation, with parts of the brain responsible for some of our most complex behaviour starting to enlarge early on. A third points out that brain enlargement correlates, to some extent, with the elongation of our thumbs (which are obviously very different from those of most non-primates), implying that fine manipulation of objects may have been another key element in the drive for greater intelligence.

Going further back in time, another study this year challenged the traditional view of primates originating in tropical jungles. Instead, it suggests that the very first primates appeared in cold and temperate habitats in the north, the changeable climates of such areas promoting the evolution and dispersal that allowed them to reach the tropics later on.

Among the rodents, analysis of a new fossil and comparison to others already known shed light on the origins of the group that includes the gophers. The fossil belongs to an unusually large relative of the ancestor of gophers and kangaroo rats, and seems to have already been a skilled digger. This supports existing theories that the ancestral gopher looked like, and had a similar lifestyle to, today's pocket mice.

An unusually complete fossil free-tailed bat found north of Marseilles in France dates back over 30 million years to the Early Oligocene. The shape of the wings and muscular anchors in the body shows that it was fast and capable of sustained flight, probably catching insects in the air as it flew over what was then a large lake.

Conoryctes was a medium-sized burrowing mammal living in North America just 3 million years after the extinction of the non-avian dinosaurs. It's probably a placental mammal, but it has been argued that it may actually be an early relative that's simply closer to true placentals than to marsupials. A study of the microscopic structure of its bones shows that it must have grown rapidly, reaching adult body size in a single year and that it would have been weaned at about the age we would expect for a true placental of its size. So even if, by some chance, it wasn't literally a placental mammal, it lived very much like one.

Marsupials and More

The best-known and distinctive marsupial species are probably the kangaroos and wallabies. All but one living species belong to a subfamily that spread through Australia starting around 11 million years ago. The oldest known fossil belonging to this subfamily belongs to Dorcopsoides, which may hold some clues as to why the group became so succesful on their home continent. A new analysis published this year found that it was a more efficient hopper than had previously been thought, suggesting that it was already adapted to open environments, something that was just starting to become more common at the time, as the Australian outback began to dry out. 

It may have helped that, as another new analysis of the wear patterns on their teeth showed, Ice Age kangaroos had a wider diet than was apparent from their anatomy alone. On the downside, if they were adaptable, the fact that so many kangaroo species went extinct around 40,000 years ago is probably not primarily due to the change towards a colder climate...

While fairly detailed DNA analysis is possible for mammoths and other Ice Age animals preserved in permafrost, it is much harder for animals of similar age in warmer climates. A new study this year therefore used the molecular structure of collagen from sinews and other tissue to confirm the relationships between some of the marsupials that went extinct in the last 100,000 years. Perhaps the most significant finding was that the closest living relative of the extinct carnivorous marsupial lion Thylacoleo may be the koala, rather than it being an earlier relative of the koala-wombat common ancestor.

On the subject of carnivorous marsupials, these were at least as prominent in South America in prehistoric times, dominated in particular by the large sparassodonts. A new analysis of the skulls of South American marsupials this year showed that, while most had similarly shaped (elongated) brains to modern marsupials, that of the sabretooth marsupial Thylacosmilus was more rounded, due to its shorter, cat-like face. More significantly, revised estimates of its body weight showed that its brain was smaller than previously thought, in the range of some of its earliest ancestors, its size having evolved less than expected.

Similar analysis of an armbone belonging to the mysterious mammal Kryorectes confirmed that it was, as previously thought, a monotreme. Living alongside Australian dinosaurs a whopping 106 million years ago - 40% further back in time than Tyrannosaurus rex - the study also showed that it was probably a semiaquatic burrowing animal. The platypus lifestyle may be truly ancient. 

Finally, the multituberculates were neither placental, marsupial, nor monotreme but a fourth grouping that survived well into the Age of Mammals. An analysis this year of their habitats and distribution across North America suggested that, at least on that continent, they were restricted to damp temperate forests dominated by redwoods and swamp cypress and that they finally disappeared when those forests dramatically declined as the world cooled at the end of the Eocene. This contradicts the popular theory that it was competition with newly arrived rodents that killed them off, since they were apparently living elsewhere at the time.


Synapsida is taking a break for the holiday period and will return on the 4th January

[Image from Yanaka et al. 2025, available under CC-BY-4.0]

Sunday, 5 January 2025

Miniature Mediterranean Mammoths

Image
Insular dwarfism is a phenomenon that has occurred many times throughout evolution. What happens is that a population of some large animal becomes trapped on an island, out of contact with its mainland kin., Because the island has a limited size, it also has a limited amount of food on it, and this is a problem for a large animal that needs plenty to eat,

If the island is particularly small, of course, the animals in question are likely to die out, if not immediately, then dwindling over a few generations until they lack the genetic diversity to sustain themselves. On the other hand, if the island is a large one (such as, say, Britain) then there may not be a problem at all, and nothing happens beyond the usual genetic drift between isolated populations. 

Sunday, 15 December 2024

Prehistoric Mammal Discoveries 2024

Image
Zalamdalestes
I have reached the end of another year and that means it's time for what has become a tradition on this blog over the last eight years: a look back at some of the discoveries about fossil mammals made in 2024 that didn't make into the regular posts. As usual, this will be a quick whistle-stop tour of mammalian palaeontology, hopefully focusing on some of the more interesting findings. Like any field of science, it has not been standing still.

Large Herbivores

Woolly mammoths (Mammuthus primigenius) are among the best-known of all prehistorical mammals to the general public and, aided by the fact that some lived recently enough to be preserved in permafrost, they are also amongst the best-studied. But there is still more to learn about the details of their lives and habits. A study published this year looked at the detailed isotopic composition of a fossil mammoth that had died about 12,000 BC in Alaska, showing that she was female, and had migrated over 1000 km (600 miles) during her lifetime, having originally been born in the Yukon. The area in which she died was popular with mammoths, but also with humans - she may have died peacefully, but the presence of people where mammoths congregated may not be a coincidence.

Sunday, 17 December 2023

Prehistoric Mammal Discoveries 2023

Image
Potamotherium
It's the last post of the year for 2023, and that means it's time once again to take a brief look at discoveries from the last year in the world of fossil mammals that didn't make it into this blog. Because, while dinosaurs are undoubtedly popular, the study of prehistoric mammals is also a major field, aided by that, being (mostly) relatively recent they tend to be more numerous and better preserved. Of course, everyone's heard of woolly mammoths and sabretooth cats but there's plenty more out there and, if I'm going to zip through them at speed today, I'm also going to try and cover as wide a range as possible. So, let's get going...

Sunday, 15 December 2019

Prehistoric Mammal Discoveries of 2019

Image
Nehalaennia, an 8 million-year-old rorqual
from the Netherlands, first described this year
As the year - and decade - approach their inevitable conclusion, it's time again to look back at a few palaeontological findings of 2019 that didn't, for whatever reason, make it into the regular Synapsida posts. As always, there is no theme to this list, just a sample of what seemed interesting linked only by when it happened to be published.

Sunday, 17 December 2017

Prehistoric Mammal Discoveries of 2017

Image
Albertocetus meffordorum, the post-cranial anatomy of which
was described for the first time this year.
At the end of each year, I do a slightly different post to wrap up the blog for the season. The format of these has changed over the years, and this year, again, it's time to do something slightly different from previous occasions. Not that there haven't been some interesting new species discovered this last year, with, to my mind, the Skywalker gibbon (Hoolock tianxing) being the stand-out example. This was announced early in the year, having been discovered in the Chinese/Myamar border region by a group of researchers who were fans of a certain science fiction franchise ("tianxing" literally translates to "sky-walker" in Standard Chinese), and is likely already endangered.

But this year, instead of discussing just how many new kinds of bat we discovered in the last twelve months, I'm going to note that my posts on fossil mammals tend to be more popular than those on the living sort, and take a look at a partial assortment of scientific papers published on this subject in the last year that, for various reasons, didn't end up in my regular blog posts. So here goes.

Sunday, 17 April 2016

Pliocene (Pt 10): Before There Were Zebras

Image
At the dawn of the Pliocene, Africa, like Europe, was a much wetter place than it is today. As a result, it was also much greener, a place of lusher vegetation, and the animals that fed on it. While that likely made little difference to the heart of the Congo jungle and to the more tropical reaches of West Africa, which are about as green as they're going to get, elsewhere the changes would have be obvious to any putative time traveller.

The biggest difference was likely in the north, where the even the very heart of what is now the Sahara Desert was likely covered in arid scrubland - hardly hospitable, but a significant improvement over baking hot dune-fields. By one estimate, moist savannah and open woodland stretched as far north as 21°, covering what are now countries like Chad, Sudan, and Mauritania. Further east, Somalia would also have been covered by woodland, rather than its current dry grasslands, and, at the opposite end of the continent, there may have been small forests in what are now the Namib Desert and the Kalahari.

It didn't last, of course. Around 3 million years ago, as the world fell irrevocably into the long autumn of the late Pliocene, Africa became not only cooler, but drier. And, if the generally cooler climate did not make too much difference to a continent sitting on the equator, the loss of rain certainly did. It's at this time that the Sahara, and the other deserts we are familiar with today, began to form, and the wildlife had to either adapt to that fact, or die. What was good news for voles in Europe, promoting the tougher grasses on which they thrive, was bad news further south, where the grass gave way to open sand.

Sunday, 21 April 2013

Pleistocene (Pt 8): Mammoths v. Mastodons

Image
American mastodons
The arrival of the first mammoths in North America was a significant turning point in the development of the local wildlife. It's so important that this date, 1.9 million years ago, marks the beginning of the first of just two 'land mammal stages' that define North American wildlife during the Ice Ages. It used to also mark the beginning of the Pleistocene itself, but for various reasons, that's now been shifted a little further back.

The mammoths in question arrived from Asia, crossing over the Bering land bridge, the recurring appearance and disappearance of which greatly influenced North American wildlife during this time. They were southern mammoths (Mammuthus meridionalis), the dominant species of mammoth in Asia at the time, but they quickly evolved into a home-grown American animal: the Columbian mammoth (Mammuthus columbi).

It used to be thought that, even ignoring any late-surviving southern mammoths, there were at least two different species of mammoth living in North America in the early to mid Pleistocene. We're now pretty confident that they're all just examples of Columbian mammoth. Nonetheless, you will often see references to the "Imperial mammoth" (Mammuthus imperator). Perhaps the biggest elephant that has ever lived - they were about thirteen feet tall at the shoulder - these were probably just really big Columbian mammoths. Not that that's anything to sneeze at, mind you.

Saturday, 23 February 2013

Pleistocene (Pt 7): Meanwhile, Across the Atlantic...

Image
Columbian mammoth
(It's likely that the real animal was hairier than the one in
this reconstruction, but it shows the tusks effectively)
Over the last five parts of this series I have described the history of Pleistocene Europe, describing some of the ways that the animal life of the continent changed over those thousands of millennia, and looking at a few particular animals in more detail. But one doesn't need a degree in zoology to notice that today, the wildlife of North America, for example, is different to that of Europe. North America has coyotes, raccoons, cougars, armadillos, and pronghorn antelope, to name just a few animals that are simply absent in Europe. (Or, in the case of raccoons, were absent until somebody made the mistake of releasing some of the furry nuisances in 1930s Germany).

It's hardly surprising that that continent also had different wildlife during the Pleistocene. One notable difference, for instance, is that we humans weren't there. Obviously, neither Columbus nor Leif Ericsson were genuinely the first person to discover America. But even whichever long-lost group of Native Americans was actually the first to discover the great western continent, they did so long, long, after the first Europeans discovered Europe. While Europe had at least some species of human inhabiting it for about two-thirds of the Pleistocene, nobody reached America until the epoch was all but over.

Sunday, 7 October 2012

Pleistocene (Pt 4): Time of the Woolly Mammoths

Image
The second-to-last Ice Age ended around 0.13 million years ago, a full 95% of the way through the Pleistocene. As I've described in Part 3, it was just one of a series of Ice Ages stretching back nearly two million years, and separated by relatively warm 'interglacials'. For much of this time, European wildlife had had a distinctly 'African' flavour, with lions, hyenas, hippos, and elephants, among others, inhabiting the continent alongside the ancestors of more familiar European animals.

Such animals prospered during the warmer gaps between the Ice Ages, and this, the last full interglacial, was no exception. The phrase 'hippos in the Thames' is often used when talking about this time, and its perfectly accurate. The climate of the day was, if anything, slightly warmer than it is now, with the ice retreating far into the Arctic. All that melting ice had to go somewhere, of course, and the sites of modern day coastal cities such as Amsterdam and Copenhagen would have been underwater. On land, much of the northern continent was covered by dense oak forests, a green wilderness yet to be cleared to make way for farmland or towns.

Sunday, 26 August 2012

Pleistocene (Pt 3): Ice Ages and Interglacials

Image
Life-size reconstruction of a steppe mammoth
(compared with a 3-year old human)

When the Pleistocene began, Europe's climate was much the same as it is today, and the general shape of the continent would also have been instantly recognisable from space. The animals however, were different, many of them being ones we would now associate with Africa - rhinos, elephants, hyenas, and cheetahs, among others. In part 2, I described how that began to change 1.8 million years ago (which, incidentally, was once defined as the beginning of the Pleistocene - see part 1 for why that changed).

This was a time of cooler weather, as the Ice Ages began to dawn. Forests retreated in the face of advancing tundra, and musk oxen, bison, and (strangely) European hippos began to make their appearance. The cold snap was prolonged, and, so far as we can tell, the fauna of Europe remained relatively stable for the next 600,000 years. That's still a very long time - if we go back to my analogy where we get just one minute to watch the events of a decade, with the whole of written history thereby spread out into a nine hour spectacular, this phase of European history would last a full six weeks.

1.2 million years ago, half way through the Pleistocene, the climate changed again, and mammals (and other animals) were forced to adapt. However, the change wasn't towards yet colder weather, but back towards a warmer, more pleasant climate. The forests grew back, with all their dense undergrowth in attendance, and the harsh steppe-lands retreated into the north. As had been the case at the dawn of the Pleistocene, European weather would have been much as it is now.

Sunday, 29 July 2012

Pleistocene (Pt 2): Europe at the Dawn of the Ice Ages

Image
Pachycrocuta brevirostris, a European hyena
The Pleistocene is the time of the Ice Ages, when great ice sheets rolled across much of the northern hemisphere. Nothing much lived on the ice sheets themselves, just as there is very little today in the heart of Greenland. But, as we've seen, not only were their wide bands of tundra and pine forest reaching across much of today's 'western' world (and, of course, a fair chunk of the Orient), but the ice ages weren't continuous; there were many warm gaps between them.

The mammals of the Pleistocene include what are surely the most familiar fossil mammals to most people, the ones we generally think of when we think of 'after the dinosaurs'. For this was the time of the mammoths and sabretooths. They're familiar to us because, aside from the tiny sliver of warm weather we currently live in, the Pleistocene is the most recent, and therefore the best preserved and the most easily analysed, of all the epochs of the Age of Mammals. It's been the setting for a number of films, books, and TV series - to name just two, the Ice Age cartoons, and the Earth's Children series.

Yet, when we think seriously about Pleistocene animals, there are a couple of important points to bear in mind.