mammal – Page 9 – Nix Illustration

Island Weirdness #53 — Tiny Elephants On Parade Part 5: Western Mediterranean

During the Pleistocene elephants colonized many of the islands in the Mediterranean Sea, with each island independently developing its own unique dwarfed form.

A stylized illustration of an extinct pygmy mammoth. It has long tightly-curved tusks, small ears, and a coat of hair over its body. — Mammuthus lamarmorai

Mammuthus lamarmorai lived on the island of Sardinia during the middle and late Pleistocene, between about 450,000 and 40,000 years ago. Standing around 1.4m tall at the shoulder (4’7″), it was a dwarf form roughly one-third the size of its ancestor, the huge Eurasian steppe mammoth.

Its remains are known only from the west and south of the island. Strangely it appears to be have been absent from the nearby island of Corsica, despite the two being joined as a single landmass a few times during lower sea level periods in the Pleistocene.

It’s not clear why this mini-mammoth disappeared. The date of the earliest human settlement of Sardinia is controversial (ranging from 250,000 to 20,000 years ago), so Mammuthus lamarmorai might never have actually encountered them. Instead it may have struggled to cope with climate changes during the last glacial period towards the end of the Pleistocene, which rapidly turned Sardinia colder and drier.

A stylized illustration of an extinct dwarf elephant. It has long thin tusks and tiny ears, and its body shape resembles a chubby baby elephant. — Palaeoloxodon falconeri

Over on Sicily and Malta (which were also occasionally a single island when sea levels were lower), there were several different species of miniature elephant during the mid-to-late Pleistocene, each with a different body size and occupying its own ecological niche. They were all descendants of the massive straight-tusked elephant (Palaeoloxodon antiquus) but each resulted from independent colonization waves swimming over to the island(s).

Palaeoloxodon falconeri lived during the mid-Pleistocene, about 550,000 years ago, and was both the smallest of the Mediterranean dwarfs and possibly the smallest elephant to ever exist. Just 0.8-1m tall (2’7″-3’3″), it had adult body proportions resembling the juveniles of its ancestors, limbs adapted for running and clambering over rough terrain, and a proportionally enormous brain relative to its body size.

Around 200,000 years ago a sea level drop allowed new colonization from the Italian mainland. If Palaeoloxodon falconeri was still around at that time it likely didn’t survive long with new competition from large herbivores like bison and deer, and being preyed on by newly-arriving large carnivores like wolves, lions, and hyenas.

Another small elephant soon evolved to take its place, although due to the presence of predators it was never able to get nearly so tiny.

A stylized illustration of an extinct dwarf elephant. It has short thick twisting mammoth-like tusks and small ears. — Palaeoloxodon mnaidriensis

Palaeoloxodon mnaidriensis was in fact one of the largest dwarf elephants in the Mediterranean, standing about 1.8-2m tall (5’11”-6’6″), but despite its larger size its limbs still show signs of adaptation for more fast and agile movement. Its tusks also show a lot of variation in shape, with some much more curved and twisted than others.

This elephant had disappeared by about 13,000 years ago, probably due to the climate significantly warming towards the end of the last ice age. Much like Sardinia, the earliest arrival of humans on Sicily and Malta is controversial, and it’s unclear whether they ever encountered Palaeoloxodon mnaidriensis — the earliest definite date for Sicily is about 16,000 years ago, so a human-induced extinction can’t be ruled out entirely.

The subfossil remains of the Siculo-Maltese elephants may have also ended up inspiring legends of the cyclops, as their skulls would have resembled large human ones with the nasal cavity forming a single big “eye socket”.

Island Weirdness #51 — Tainotherium valei

Like much of the Caribbean, Puerto Rico originated as part of a Mesozoic volcanic island arc. While in theory this could have resulted in the region retaining some relict populations of weird Cretaceous species, there’s a major reason this didn’t actually happen: the asteroid impact event 66 million years ago. The proximity to Chicxulub would have been devastating to the proto-Caribbean at the time, with tsunamis as high as 500m (1640′) battering the islands and destroying practically everything that lived there at the time.

Afterwards subsidence in the early Cenozoic submerged many of the islands and drowned whatever was left, so it wasn’t until later tectonic uplifting that land re-emerged and was able to be recolonized by species via rafting and island hopping (or possibly via a short-lived land bridge).

Caviomorph rodents arrived from South America around the start of the Oligocene, about 33 million years ago, and became very successful due to being some of the only land mammals present on many of the islands. The only modern survivors of this lineage are a handful of hutias, but in the past they were much more diverse — and some of them were giants.

Tainotherium valei lived in Puerto Rico during the Late Pleistocene and early Holocene, and while it wasn’t quite the largest of the giant hutias it was still enormous. It’s only known from a single partial leg bone, so its full size is difficult to estimate, but it was probably somewhere around 80cm tall at the shoulder (2’7″) and weighed about 100kg (220lbs) – similar in size to a modern black bear.

And that leg bone is especially unusual, showing anatomical adaptions associated with tree-climbing. This is strange for such a huge heavy mammal, but it may have been an ecological equivalent of something like the giant Malagasy lemurs, a slow-moving animal that climbed up trees to feed and regularly traveled over the ground from one feeding site to another.

During the Pleistocene lower sea levels meant most of the Puerto Rican archipelago was part of a much larger landmass that also included most of the nearby Virgin Islands, and the predominate climate at the time was a dry savanna. As sea levels rose at the start of the Holocene the climate shifted wetter and Puerto Rico became densely forested. This would have been advantageous for a tree-climbing animal like Tainotherium, so it was likely still around when the first humans arrived in around 3000-2000 BCE.

Unfortunately these early settlers appear to have burned large amounts of the forests for the first few centuries of their presence, and such widespread habitat destruction would have driven this giant rodent extinct very quickly.

Island Weirdness #49 — Sloth-Monkeys & Fighting Ibises

Jamaica is the third largest island in the Caribbean, and much like Cuba it originated as part of a Late Cretaceous volcanic island arc. It began to subside during the Eocene and was completely submerged for a large portion of the Cenozoic, then was uplifted again in the early-to-mid Miocene, reaching close to its present-day size around 13 million years ago.

Few land mammals ever colonized the island prior to human influence, and most of the known remains are from rodents. But another group did make it onto Jamaica, and became something especially weird.

A stylized illustration of an extinct titi monkey. It has long soft fur and a very long tail. — Xenothrix mcgregori

Xenothrix mcgregori is a primate only known from fragmentary remains, but what is known of its skeleton shows a unique combination of features for a New World monkey. It had a reduced number of teeth in its jaws, with enlarged molars, and oddly-shaped heavily-built leg bones that resemble those of slow quadrupedal climbers like lorises.

It was probably about 70cm long in total (2’4″), including the tail, and is thought to have lived a lot like a tree sloth, spending most of its time moving slowly around in the trees and possibly even feeding while hanging upside down.

Its anatomy was so ununsual that its evolutionary relationships were a mystery until ancient DNA was recovered from subfossil bones and confirmed it was actually a titi monkey very closely related to the genus Cheracebus. Its ancestors probably arrived on Jamaica in the late Miocene, around 11 million years ago, and it had some close relatives on a couple of other Caribbean islands — the terrestrial Paralouatta on Cuba, and Antillothrix and Insulacebus on Hispaniola — although they likely all independently colonized the Caribbean via different rafting events from South America.

A stylized illustration of an extinct flightless ibis. It has stout legs, and has its wings raised as if threatening to hit something with its heavy club-like arm bones. — Xenicibis xympithecus

Another inhabitant of Jamaica was an equally strange bird.

Xenicibis xympithecus was one of only two lineages of ibis ever known to have become completely flightless (the other being Apteribis from Hawaii).

Around 60cm tall (2′), it had some of the most unique wings of any bird. The hollow bones were thickened, its forearm was proportionally short, and the hand was modified into a large heavy “club” — and blunt-force injuries on some of these birds’ remains suggest that they used their wings as weapons when fighting, clobbering each other with powerful blows.

Radiocarbon dating suggests the Xenothrix monkeys survived well into the Holocene, until around 1100 CE. Since various groups of humans had been present on Jamaica since about 4000 BCE the sloth-monkeys must have coexisted with them for several millennia, and their extinction may have been caused by more of a “slow fuse” of gradual habitat destruction than direct exploitation.

Dating on Xenicibis‘ extinction is less precise, with the youngest known remains being somewhere between 10,000 and 2200 years old. It may have still been around when the earliest humans arrived, but unlike the native monkeys it seems like it didn’t last long beyond that point.

Island Weirdness #47 — Megalocnus rodens

Just 21km south of the Bahamas (13 miles), Cuba is the biggest island in the Caribbean and has a complex geological history. It originated as part of a volcanic island arc in the Late Cretaceous and during its existence in the Cenozoic it was colonized by a richer variety of mammals than the Bahamas ever had, including rodents, the enigmatic solenodons and nesophontes, and ground sloths.

The Caribbean ground sloths were all part of the megalonychid lineage — which eventually reached North America and produced giants — and they arrived on Cuba by the early Miocene, about 20 million years ago.

Megalocnus rodens lived during the Late Pleistocene and Holocene, between about 125,000 and 5000 years ago. It had unusually rodent-like front teeth, and while it was dwarfed compared to its mainland relatives it was actually one of the largest of the Cuban ground sloths — close to the size of a modern black bear, about 80cm tall at the shoulder (2’5″).

Subfossil remains show that Megalocnus survived well into the Holocene, and there’s been speculation that it may even have still been around in the highland forests as late as the time of European colonization in the 1500s.

However, radiocarbon dating of remains has given no dates younger than about 5000-4000 years ago, about 1000 years after the earliest arrival of humans in Cuba.

Island Weirdness #45 — The Pedro González Dwarf Deer

Isla Pedro González is part of the Pearl Islands in the Gulf of Panama, about 48km (30 miles) offshore. It was formed after the end of the last glacial period, as steadily rising sea levels cut it off completely from mainland Panama about 8500 years ago — and isolating the population of deer that lived there.

Although Pedro González is the third largest of the Pearl Islands it’s still fairly tiny, just 6.5km long (4 miles). As a result of this small space, limited available food supplies, and a lack of any large predators, these deer rapidly shrank down into a dwarfed form to survive. By 6000 years ago they were the size of a small dog, just 35-40cm tall at the shoulder (1’2″-1’4″) and weighing less than 10kg (22lbs).

The Pedro González dwarf deer haven’t been given any official scientific name just yet, but since they’re thought to be descendants of brocket deer they’d be a part of the genus Mazama, either as their own separate species or as a subspecies — similar to the larger native deer on nearby Isla San José, which are probably their closest living relatives.

Paleoindian settlers arrived on Pedro González just over 6000 years ago, and we know they hunted and ate the tiny deer because all the known remains come from a preserved trash heap and show signs of human butchering and chewing.

Younger deposits have gradually less and less deer bones, and although those particular settlers had left again by about 5500 years ago the damage was already done — layers from another group of people about 2300 years ago show no deer bones at all, so the dwarf deer had to be already extinct by that time.

Island Weirdness #44 — Tiny Elephants On Parade Part 4: Mammoth-Mimics & Mini-Mammoths

In the cool-temperate climate of Pleistocene Japan one type of small elephant seems to have convergently become somewhat of a mammoth-mimic, with twisting tusks and possibly even a thick coat of hair.

A stylized illustration of an extinct mammoth-like elephant. It has long twisting tusks, small ears, and a speculative coat of long hair. — Palaeoloxodon naumanni

Palaeoloxodon naumanni lived during the late Pleistocene, between about 500,000 and 16,000 years ago. At about 2-2.5m tall at the shoulder (6’6″-8’2″) it was still fairly large, similar in size to the smallest living elephant species — but it was a dwarf in comparison to its immediate ancestors, the absolutely enormous Asian straight-tusked elephant (Palaeoloxodon namadicus).

Actual woolly mammoths (Mammuthus primigenius) were also present in Japan, but the two similar-looking elephants inhabited different environments — Palaeoloxodon naumanni preferred the southern forests, while the true mammoths roamed the colder north.

Humans arrived in Japan around 40,000-30,000 years ago, so Palaeoloxodon naumanni actually coexisted with them for quite some time. Although it was hunted, it seems to have mainly been climate change towards the end of the last glacial maximum that led to its extinction.

A stylized illustration of an extinct pgymy mammoth. It has curving tusks, small ears, and a speculative coat of hair. — Mammuthus exilis

Over on the other side of the Pacific Ocean, at least 60,000 years ago, some huge Columbian mammoths (Mammuthus columbi) swam the 6.5km (4 miles) distance to the ancient island of Santa Rosae — a landmass that today is mostly submerged, with its remaining peaks forming the modern California Channel Islands.

With a lack of large predators and then steadily rising sea levels reducing the available habitat on their new home, the mammoths shrank into a dwarfed species known as the Channel Islands pygmy mammoth (Mammuthus exilis). Standing around 1.75-2m at the shoulder (5’9″-6’6″), they were less than half the size of their ancestors and had only about 10% of the body mass.

The pygmy mammoths survived until about 13,000 years ago, around the same time that early Paleoindians arrived. While they may also have been hunted by humans, the warming post-glacial climate is currently thought to be the main factor in their extinction, changing the types of vegetation on their still-shrinking islands and reducing fresh water sources.

(And if you prefer your pygmy mammoths less speculatively hairy, there’s always the version I did for PBS Eons earlier this year.)

Island Weirdness #32 — Tiny Elephants On Parade Part 3: More Indonesia

It’s finally time for part 2 of the Island Weirdness series!

(If you haven’t seen the previous installments, I suggest starting back at the beginning here.)

We left off last time with the dwarf stegodontids of Flores, but other Indonesian islands also had their own populations of unusually small elephant-relatives — so here’s a few more to start off this month!

A stylized illustration of an extinct dwarf elephant. It has long straight tusks and small ears. — Sinomastodon bumiajuensis

Sinomastodon bumiajuensis lived on the island of Java during the early Pleistocene, about 2-1.5 million years ago. It stood around 2m tall at the shoulder (6’6″), less than half the size of most other Sinomastodon species from mainland Asia. Although it looked convergently similar to modern elephants it was actually a member of the gomphotheres, much more closely related to the weird “shovel-tuskers” than to any living species.

A stylized illustration of an extinct dwarf elephant. It has long gently curving tusks and proportionalyl short legs. — Stegodon semedoensis

Stegodon semedoensis, also from the early Pleistocene of Java about 1.5 million years ago, is only known from a few isolated molar teeth — but the size of those teeth suggest it was one of the smallest known pygmy stegodontids. It was probably no more than 1.2m at the shoulder (3’11”), comparable in size to its close relative Stegodon sondaari over on Flores.

A stylized illustration of an extinct dwarf elephant. It has four straight tusks, two longer ones in its upper jaw and two shorter ones in its lower jaw. — Elephas celebensis

Meanwhile on Sulawesi, Elephas celebensis (sometimes called Stegoloxodon celebensis) was an actual true elephant closely related to the modern Asian elephant. Living during the late Pliocene and early Pleistocene, between about 2.5 million and 800,000 years ago, it was only 1.5m tall (5′) and had a second set of tusks in its lower jaw, a “primitive” feature retained from the gomphothere-like ancestors of modern elephants.

A stylized illustration of an extinct dwarf elephant. It has long curving tusks and small ears. — Stegodon sompoensis

At the same time Sulawesi also had yet another small stegodontid, Stegodon sompoensis, also around 1.5m tall.

Both of these dwarfs lived alongside a larger Stegodon species, as well as giant tortoises and large-tusked pigs.

The cooling climate of the Pleistocene and dropping sea levels eventually connected the islands of western Indonesia to the Sundaland landmass of mainland Asia. Influxes of new predators and competitors — and early humans — probably drove these endemic small elephants to extinction.

Antilohyrax

This is not a deer.

In Africa during the Eocene and Oligocene, the main terrestrial herbivores were a different type of mammal entirely: hyraxes, the close relatives of elephants and manatees. Although their only modern representatives are small climbing rodent-like animals, hyraxes were once a much more diverse and widespread group, filling a variety of ecological niches and ranging from the size of rats up to the size of rhinos.

Antilohyrax pectidens was a mid-sized example of these diverse hyraxes, standing about 50cm tall at the shoulder (1′8″) and living around 34-28 million years ago in Egypt. It had a deer-like snout and long slender limbs adapted for running and leaping, with leg bones incredibly similar in size and proportion to modern springbok.

Its incisor teeth were comb-shaped and resembled those of colugos, so it was probably a similar sort of selective browser eating soft leaves and shoots.

Eons Roundup 3

Some more recent work I’ve done for PBS Eons!

The eurypterids Hibbertopterus and Brachyopterus, from “When Giant Scorpions Swarmed the Seas”
https://www.youtube.com/watch?v=1sQXTXbuLYo

The short-faced bears Plionarctos and Arctotherium, from “The Mystery Behind the Biggest Bears of All Time”
https://www.youtube.com/watch?v=KtsOhmBb92E

The big cats Panthera blytheae and Panthera atrox, from “The Ghostly Origins of the Big Cats”
https://www.youtube.com/watch?v=oPJnqWke5n8

Inticetus

While most modern toothed whales have jaws full of teeth that are all the same simple pointed shape – an adaptation for better holding onto slippery prey – their ancient ancestors had teeth much more like other mammals, with differentiated incisors, canines, and molars.

In-between them were whales like Inticetus vertizi, which lived off the coast of southwestern Peru during the Early Miocene, about 18 million years ago.

At over 3.5m long (11′6″) it was one of the larger known toothed whales around at the time, but it wasn’t the direct ancestor of any living whales. Instead it was more of an evolutionary “cousin” to them, part of an older offshoot lineage that lived alongside the early members of modern toothed whale groups.

Inticetus had a long and unusually wide-based snout, somewhat croc-like in appearance, with sharp pointed teeth at the front and multi-lobed cheek teeth further back. A lack of obvious wear on its back teeth suggests it wasn’t using them to chew up its food, and it may have had a fairly specialized diet – possibly using those back teeth to sieve small prey out of the water in a similar manner to modern lobodontine seals.

An close-up view of Inticetus' jaws, showing the differences in tooth shape from front to back. — Closeup of *Inticetus*‘ jaws

Inticetus-like teeth have also been found in Miocene-aged deposits in the eastern USA, the Atlantic coast of France, and southeast Italy, indicating that this ancient whale lineage was quite widespread.