convergent evolution – Nix Illustration

Ictitherium

Ictitherium ebu* was a hyena that lived in what is now Kenya during the late Miocene and early Pliocene, around 7-5 million years ago. It was part of an early branch of the hyaenids known as ictitheres, dog-like hyenas found across Miocene Africa and Eurasia that occupied similar ecological niches to modern canids.

(*alternatively classified as Hyaenictitherium ebu by some studies)

It was similar in size to the modern aardwolf, standing about 50cm tall at the shoulder (~1’8″) – but it had proportionally longer legs, giving it a build convergently similar to the present-day maned wolf. Despite these long limbs it wasn’t a fast runner, with its joint anatomy instead suggesting it was adapted for efficient walking, pouncing on prey, and looking over the tall grasses of its savanna woodland habitat.

Polysacos

Polysacos vickersianum was a marine mollusc that lived during the early Carboniferous, around 345 million years ago, in what is now Indiana, USA.

It was part of a group known as multiplacophorans, which are usually considered to be close relatives of modern chitons — but may instead represent a much earlier branch of the aculiferan lineage that convergently evolved chiton-like anatomical features.

About 2.5cm long (~1″), Polysacos had seventeen shell plates surrounded by a fringe of long spines with concave upper surfaces. Like the modern chitons it resembled it was probably a grazer that scraped up algae from hard rocky surfaces.

Ptychotherates

Ptychotherates bucculentus was a herrerasaurian dinosaur that lived during the Late Triassic, about 205 million years ago, in what is now New Mexico, USA.

Probably around 2m long (~6’6″), it had a short deep skull and massive cheekbones – unusual features for an early saurischian, and convergently similar to those of some later theropods.

Along with its close relatives Tawa, Chindesaurus, and Daemonosaurus (a grouping collectively known as “morphoraptorans”) it represents one of the latest-surviving known herrerasaurians, suggesting that these early-diverging carnivorous dinosaurs persisted in low-latitude regions until much closer to the end of the Triassic than previously thought.

Xenocranium

Xenocranium pileorivale lived during the late Eocene, about 35 million years ago, in what is now the Midwestern and Mountain states regions of the USA.

Despite its very mole-like appearance, this little mammal was a member of an extinct lineage known as palaeanodonts — and its closest living relatives are actually pangolins.

Around 15cm long (~6″), Xenocranium was highly adapted for a subterranean burrowing lifestyle, with an upturned shovel-shaped snout bearing a pad of thickened skin, and short powerful limbs with large digging claws. Its eyes were very reduced, functionally blind, and may not have even been visible in life. Its sense of hearing was also specialized for the sort of low-frequency sounds that carry well through the ground.

It was probably a head-lift digger, using upward motions of its snout and downward strokes with its forelimbs to excavate tunnels while foraging for worms and underground insects.

Ubaghsicystis

Ubaghsicystis segurae was an echinoderm that lived during the mid Cambrian, about 506-497 million years ago, in what is now Spain. Similar fossils are also known from Morocco, Mexico and Canada, suggesting this genus was quite widespread in marine continental shelf habitats at the time.

It was part of an extinct group known as eocrinoids, which were the earliest known echinoderms to develop stalked bodies and specialized feeding appendages — but despite the name and similar body plan, their resemblance to crinoids was due to convergent evolution rather than any direct relation.

Its globular body was only about 5mm in diameter (~0.2″), with a long stalk at least twice that length ending in a small disc that attached it to the substrate. The upper half of its body was dotted with small holes (called epispires) that probably served a respiratory function, and unlike most other eocrinoids it seems to have had just two slender flexible feeding appendages.

It would have been a suspension feeder, using tube feet to catch food particles floating around in the water, then move it down to its mouth positioned at the base of the two “arms”.

Poposaurus

Despite its incredible resemblance to theropod dinosaurs, Poposaurus gracilis was actually a pseudosuchian more closely related to crocodilians than to dinosaurs.

Living in what is now North America during the Late Triassic, about 237-216 million years ago, Poposaurus grew to around 4.5m long (~15′) with roughly half of that length taken up by just its long tail. With its sharp-toothed jaws, small arms, bipedal locomotion, and counterbalancing tail, it convergently evolved the same sort of body plan and ecology as carnivorous theropods – which were still in their early days at the time, and wouldn’t really become the dominant terrestrial predators until after the end-Triassic extinction.

Unlike most other pseudosuchians Poposaurus lacked bony osteoderm armor, seems to have been capable of a digitigrade posture, and its claws were flattened and somewhat hoof-like, all adaptations that suggest it was built for running after fast-moving prey.

Duonychus

Duonychus tsogtbaatari was a therizinosaurid dinosaur living in what is now the Gobi Desert in southern Mongolia during the Late Cretaceous, around 96-90 million years ago.

Like other therizinosaurids it would have been a chunky-bodied herbivore with a small beaked head atop a long neck, long rake-like claws on its hands, stout legs, and a rather short tail. But it was rather small compared to most of its close relatives, estimated at about 3m long (~9’10”), with its known fossil remains including several vertebrae, partial ribs and pelvis, and a set of nearly-complete arms and hands.

Its hands had only two well-developed fingers, with a small splint-like vestigial third finger, an anatomical condition convergently seen in some other theropod groups but previously unknown in therizinosaurids. One of its long curved claws also preserved a rare example of a thick keratinous sheath, showing that in life the claw was over 40% longer than its bony core.

Duonychus’ elbow and finger joints had a fairly limited range of motion – more similar to the forearms of Tyrannosaurus than other therizinosaurids – but its claws were able to flex almost 90° at the tips of its fingers, which may have given it the ability to reach out and grab onto foliage with a very strong and precise grip.

Thrinacodus gracia

Thrinacodus gracia* was a stem–elasmobranch – a cartilaginous fish related to modern sharks and rays – living in what is now Montana, USA during the mid-Carboniferous around 324 million years ago.

* previously known as Thrinacoselache gracia

Although the cartilaginous skeletons of chondrichthyans rarely preserve, the exceptional preservation conditions of the Bear Gulch Limestone fossil deposits mean we do actually have full-body soft tissue impressions of this species. It was about 1m long (3’3″) with an unusually slender eel-like body, a pointed snout, no dorsal fins, and an elongated tapering tail.

Preserved gut contents show that Thrinacodus gracia preyed on shrimp-like crustaceans and smaller cartilaginous fish such as Falcatus and Harpagofututor. It would have inhabited a shallow tropical bay environment, and may have had a similar sort of lifestyle to the modern eels it resembled, hiding in crevices or burrowing into sediment and ambushing passing prey.

Dorypterus

Dorypterus hoffmanni was a stem–actinopterygian fish that lived during the late Permian, around 259-254 million years ago, in shallow warm lagoons covering what is now northwestern Europe.

About 13cm long (~5″), it had a tall narrow disc-shaped body convergently similar to modern reef fish, and it was mostly scaleless with only a few scales on its underside, below its pectoral fins, and along the top of its tail. It also appears to have been toothless, and probably used its large scissor-like jaws to snip off mouthfuls of soft food such as algae.

But its most distinctive feature was its highly elongated pennant-like dorsal fin, which may be an example of sexual dimorphism – fossils of short-finned individuals have also been found, and although they were originally named as a separate species (Dorypterus althausi) they probably actually represent female D. hoffmani.

Allenypterus

Allenypterus montanus was an unusual early coelacanth that lived during the late Carboniferous, around 324 million years ago, in a tropical bay covering what is now central Montana, USA.

Up to about 15cm long (~6″), its tapering tadpole-like body plan somewhat resembled that of modern knifefishes and featherbacks, with the top part of its tail fin highly elongated into a ribbon-like shape and the rest of its tail fins being vestigial. The distinctive humped shape of its back was also much more pronounced in larger, more mature individuals.

It was probably a fairly slow swimmer, and preserved gut contents suggest it mainly ate small soft-bodied prey.

Its closest known relative seems to have been the eel-like Holopterygius – but since around 60 million years and different continents separated them both, this suggests the existence of a whole ghost lineage of other tapering coelacanths yet to be discovered.