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This is Baptanodon, an ichthyosaur which lived during the middle and late parts of the Jurassic Period about 165-155 million years ago. During this time, the central part of North America was covered with a body of saltwater known as the Sundance Sea, and Baptanodon was one of the creatures that swam in this inland ocean. It measured 20 feet long, it had freakishly huge eyes, and, as far as I have been able to learn so far, it had small teeth only in the front half of its mouth while the rear half was completely toothless. The presence of grooves running along the sides of its jaws indicate that it probably had lips and the teeth would not have been visible when the mouth was closed.
Baptanodon was closely related to the European ichthyosaur Ophthalmosaurus. In fact, for a while it was believed that Ophthalmosaurus and Baptanodon might be the same animal. However, phylogenic studies indicate that they are indeed separate.
Baptanodon shared its habitat with numerous other forms of marine life including oysters, ammonites, belemnites, hybodont sharks, as well as the 20 foot long plesiosaur Pantosaurus and the 25 foot long pliosaur Megalneusaurus.
This drawing was made on printer paper with No.2 pencil, Crayola colored pencils, and Prismacolor colored pencils.
Baptanodon. © Jason R. Abdale. August 12, 2020.
Many people, usually un-informed talking heads that appear on populist nature documentaries who want to make claims that will grab your attention, will say that sharks have remained unchanged since the time of the dinosaurs. It’s wrong. The Mesozoic Era, the age of the dinosaurs, was a time of great transition for sharks. Sharks had existed on Earth for millions of years before the first dinosaurs appeared, ever since the Devonian Period when creatures like Cladoselache swam in the oceans around 370 million years ago. However, these were very primitive sharks that bore only a slight resemblance to most of the sharks that are found in the oceans today. The closest visual comparisons that we have for many prehistoric species are those that are found in very deep water, even though these sharks are still thoroughly modern in their genetics and evolutionary history. Sharks that are described as “modern” by biologists and paleontologists appeared towards the end of the Mesozoic Era during the late Cretaceous Period. Examples of prehistoric “modern sharks” are Cretoxyrhina and Squalicorax, both of which look like many shark species that are alive today.
During the Mesozoic Era, new shark forms emerged that could be described as transitional, a sort of in-between stage between the primitive sharks of the Paleozoic Era and the modern sharks of the very late Mesozoic. The most recognizable of these transitional species were a group of sharks called the “hybodonts”. Part of the reason why the hybodonts are regarded by many as THE shark group of the dinosaur age is because they lasted for such a long time. The hybodonts first emerged during the Carboniferous Period and they stuck around until the very end of the Cretaceous – that’s a LONG time! The hybodonts, therefore, existed throughout the entire duration of the Mesozoic Era. No wonder that they are considered the archetypal Mesozoic shark. Another reason for their status as the sharks that most people think of as dinosaur-age sharks is that they were widespread. Hybodont sharks existed all over the world during the Mesozoic, and they appeared to have existed in every aquatic niche: freshwater, brackish, and saltwater. Perhaps, like modern-day Bull Sharks, they had the ability to migrate in and out of water with different salinity levels without suffering adverse effects.
The most well-known of all of the hybodont sharks is its eponymous member Hybodus, a genus composed of several species which survived and thrived during the dinosaur age. It measured 6 feet long, and it occupied marine habitats around the world, although it is especially known from fossils found in Europe. Below is a drawing that I made of it based upon numerous fossils and scientific articles that I found. I noticed that the profile of the creature looked remarkably similar to a modern-day Blunt-Nosed Six-Gill Shark (Hexanchus griseus), with its rounded blunt nose and the characteristic humped back. Hybodus’ pectoral fins were surprisingly small and convex along the posterior edge, looking similar to the pectoral fins on numerous species of bottom-dwelling sharks. I get the impression that Hybodus was somewhat lethargic and spent much of its time cruising near the sea bottom, but that’s just my guess. The drawing was made with No. 2 pencil.
Keep your pencils sharp.
This is a drawing of Lonchidion, a hybodont shark from the Mesozoic Era. There were at least eleven different species, one of which was found in the Hell Creek Formation. I won’t get into all of the particulars regarding this genus or the Hell Creek species in particular (L. selachos). Their size depended upon the species, some being very small. Lonchidion selachos may have been three feet long, judging by the size of its dorsal spines. The drawing is based upon the preserved remains of other hybodont sharks, because specimens from the Hell Creek Formation consist mostly of teeth, well-preserved specimens of any Lonchidion species are very rare, and as far as I am aware, they looked more or less like other well-known hybodonts.
Hybodont sharks are identified by their large dorsal fin spines as well as the four large spines atop their heads, which are really overly-enlarged denticle scales found all over the rest of the body. Hybodonts first appeared during the Carboniferous Period, but it was during the Jurassic that they came into their own. However, by the Cretaceous Period, they were being replaced by so-called “modern” sharks very similar to the ones we see today. Lonchidion was one of the last surviving members of its kind before the whole hybodont group (the few species that remained, anyway) was completely wiped out at the end of the Mesozoic Era 65 million years ago.
Let’s change from dinosaurs to some other prehistoric life. Here are two prehistoric sharks. The large gray one on top is called Cretoxyrhina mantelli, more commonly known as the Ginsu Shark. The smaller blue one underneath is called Squalicorax falcatus, more commonly known as the Crow Shark. These two species are only a handful of prehistoric animals that have common names ascribed to them – most paleo-critters have only their scientific names.
Both of these prehistoric sharks lived in what was called the Niobrara Sea, also called the Western Interior Sea, which covered the central third of North America during the late Cretaceous Period. Both of these sharks are classified as being lamniform sharks, also known as mackerel sharks. This is the same group which includes the Mako and the Great White. “Modern” sharks first appeared on Earth towards the end of the Mesozoic Era, and both of these species are good examples of early modern sharks.
Cretoxyrhina was a large twenty-foot shark. It lasted from 100-82 MYA, and it was probably the top predator in its environment during that time. However, during the Cretaceous Period, a new group of marine carnivores appeared called mosasaurs. These creatures were literally oceanic lizards – in fact, their closest relatives are today’s monitor lizards, like the ten-foot Komodo Dragon. But mosasaurs got much bigger than this, with some reaching over forty feet long. The mososaurs out-competed this large shark for food and drove it into extinction.
The smaller Crow Shark appears to have been much more versatile. It evolved into several different species, some measuring six feet long, while others reached as high as sixteen feet in length.
One of the things that you’ll immediately notice about this drawing is that it’s in color. I very rarely make color drawings – I usually just stick to grayscale. The reason why is because I haven’t really gotten the knack for making illustrations in color yet. I’ve been working in black-and-white for a long time, and I dare say (at the risk of tooting my own horn) that I’ve gotten pretty good at it. I don’t like using color because it washes out all of the texture and detail. Well, it’s a learning process. I’m sure that I’ll get the hang of it sooner or later.
Keep your pencils sharp.