Tag: lepidosauria

Almost-Living Fossils Month #23 – Enamel-Armored Lizards

The glyptosaurines were a group of lizards that first appeared in the Late Cretaceous, about 85 million years ago. They were an early branch of the anguid lineage, originating in North America, and had heavily armored bodies covered in bony osteoderms – superficially similar to those of modern beaded lizards, but structurally much more complex with the outermost layer formed from a unique enamel-like substance called osteodermine.

They were some of the few lizards to survived through the end-Cretaceous extinction 66 million years ago (which killed off over 80% of the lizard species known at the time) and went on to become quite successful in the warm climates of the early Cenozoic.

They spread across to Europe and Asia and developed much larger body sizes, going from small 10cm-long (4″) forms in the Early Paleocene (~65 mya) to over 60cm long (2′) by the mid-Eocene (~40 mya). In North America and Europe they became common enough that they were probably important parts of the local ecosystems, and their widespread distribution suggests they were able to adapt to a variety of different habitats and environmental niches.

Their teeth resembled those of modern omnivorous lizards like blue-tongued skinks, suggesting they had a similar generalist diet – although their strong jaws have also been proposed to be specializations for crushing hard-shelled invertebrates such as snails.

Helodermoides tuberculatus here was one of the largest glyptosaurines, about 65cm long (2′2″). It lived during the Late Eocene and Early Oligocene (~34-33 mya) in the northwestern and midwestern United States, with fossils known from Montana, Wyoming, and Nebraska.

One fossil shows evidence of having lost part of its tail, probably dropping it in a self-defense behavior to escape a predator. However, unlike the regenerating tails of many other lizards, the osteoderms of Helodermoides instead seem to have formed a thick rounded bony cap over the wound, preventing any significant regrowth and leaving its tail permanently stumpy.

During the Late Eocene and Early Oligocene the glyptosaurines began to disappear, probably struggling to cope with cooling and drying climates, and their last definite fossils date to about 30 million years ago. Possible fragmentary remains from as late as the Early Miocene of Central Europe (~16 mya) may indicate that a few isolated late-surviving members of the group persisted on for a while longer, but if they did hang on that long they were probably finished off by further sharp temperature drops in the mid-Miocene.

Almost-Living Fossils Month #14 – Ancient Snakes

While the evolutionary origin of snakes is still rather poorly understood, one very early branch of their lineage – known as the madtsoiids – were a particularly long-lived group.

Originating back in the mid-Cretaceous (~100 mya), these “primitive” snakes were found mostly in the southern continents of Gondwana (known from South America, Africa, India, and Australia), but a few also spread into Europe. They were either some of the earliest true snakes or perhaps ophidians very closely related to them, and may have retained small hindlimbs that were slightly more well-developed than the vestigal ones of some modern snakes.

They ranged in length from under 1m (3′3″) to at least 7m (23′), with biggest of them rivaling some of the very largest living snakes in size.

They would have been similar to pythons, non-venomous and relying on constriction to kill their prey, although they had less flexible skulls than their modern relatives and couldn’t easily swallow animals much larger than their own heads. At least some of the Cretaceous species would have preyed on smaller dinosaurs, with one fossil even preserving a mid-sized madtsoiid in a sauropod nest alongside a hatchling.

Although the madtsoiids survived the end-Cretaceous extinction quite well and kept going throughout most of their range for the first half of the Cenozoic, most of them eventually disappeared in the Eocene-Oligocene extinction about 33 million years ago.

Aside from a single possible Late Olgiocene/Early Miocene record from South America (~29-21 mya), after that point the madtsoiids were found only in Australia, where they persisted almost into modern times.

Wonambi naracoortensis was one of the last of the Australian madtsoiids, living from the mid-Miocene (~11 mya) to at least the Late Pleistocene (~40,000 years ago). It was also one of the larger members of the group, 5-6m long (16′5″-19′8″), and seems to have been an ambush predator that lurked around waterholes to catch drinking animals.

The last madtsoiids went extinct at the same time as many of the other Australian megafauna, and it’s not clear exactly what caused them to die out. Humans had arrived in Australia about 20,000 years earlier, and hunting – either directly targeting the large snakes, or simply gradually reducing their available prey – combined with a changing climate may have been too much for them to handle.

Barbaturex

Barbaturex morrisoni, a large herbivorous lizard which lived about 40-37 million years ago during the Eocene. Known from Myanmar in Southeast Asia, it’s estimated to have reached lengths of 1.4-1.8m (4′7″-5′10″) and was closely related to modern spiny-tailed lizards.

It had a row of bony knobs along the edges of its lower jaw, which may have supported some sort of display structure. I’ve given it some fleshy double-dewlaps here, and a spiky tail similar to its relatives, but since it’s only known from fragmentary fossils these features are pretty speculative.

Surprisingly Barbaturex was much bigger than a lot of the herbivorous ungulate mammals around at the time, and was also larger than most of the local carnivores – a very different situation to modern ecosystems, where even the biggest plant-eating lizards are still smaller than ungulates.

Titanoboa

Titanoboa cerrejonensis, a boine snake from the Mid-to-Late Paleocene of Colombia, South America (~60-58 mya). Estimated to have reached lengths of up to 12-14m (39-46′) it was one of the largest known snakes of all time, about twice the length of the biggest modern anacondas and pythons. It was probably able to reach such a huge size due to a combination of factors – mainly a very warm climate and the absence of large terrestrial predators immediately following the K-Pg extinction a few million years earlier.

Despite frequently being depicted eating dyrosaurid crocodiles, the anatomy of Titanoboa’s skull suggests it primarily fed on fish. Considering that some of the fish in its tropical riverine habitat were some of the largest available prey in the area, reaching around 3m in length (10′), a piscivorous diet would actually make a lot of sense for a such a big snake.

Unsolved Paleo Mysteries Month #12 – Muddled Mosasaurs

Numerous groups of reptiles have “returned to the water” and become aquatic over the last three hundred million years, but tracing their direct ancestry can be surprisingly difficult. Highly modified and specialized anatomy, lack of transitional forms, and similar features convergently evolving multiple times can all obscure relationships, making it hard to properly classify them.

We’re only just starting to figure out the true origin of turtles (they’re probably archosauromorphs), and they’re a marine reptile group with living members.

Some of the completely extinct ones are even more uncertain. For example: mosasaurs. (Represented here by the eponymous Mosasaurus.)

While some semi-aquatic early mosasaurs are known, and they seem to be closely related to aigialosaurs and dolichosaurs, their exact placement within the squamates is a lot less clear. Traditionally they were regarded as the sister group to snakes, but some studies have found them to be closer to monitor lizards instead, and others have even placed them as much more basal scleroglossans. Their classification in phylogenetic analyses is “highly unstable”, changing depending on what other reptile groups are included, so there’s no real current consensus.

(And even if they are most closely related to snakes, that doesn’t necessarily help much – the exact origin and evolution of snakes is still very poorly known, too!)