Tomorrow is the day to see tons of fossils at the Museum of Discovery. Come out and see what Arkansas has to offer in fossils. We have a far more diverse array of fossils than most people realize. Here are a few dinosaurs you will see.
Here are some casts of Allosaurus bones, a foot and a humerus. Allosaurus itself didn’t live here, but its descendant, Acrocanthosaurus, did.
Here is an ischium of an Apatosaur, which did not live here either. But its titanosaur relatives did.
Here are some hands and claws of Allosaurus and Utahraptor, a giant version of Velociraptor.
Not interested in dinosaurs? How about a Smilodon, one of the biggest and most iconic of mammalian predators?
Of course, what I have shown the past few days is only a few things that the University of Arkansas Earth Sciences Department is bringing. The Anthropology Department will also be there with their own fossils. The Arkansas Geological Survey will be there with a cast of the dinosaur, “Arkansaurus” and more. The Virtual Fossil Museum will be present with more than virtual fossils. Not to be outdone, the Museum of Discovery will have a collection of dinosaur skulls on display, which will be part of an upcoming dinosaur exhibit which you won’t want to miss.
The National Fossil Day event at the Museum of Discovery is almost here.Here are a few more things you might see at the event. Here is a cast of a coelacanth, a lobe-finned fish that is closely related to the fish that started the trek onto land, and a mesosaur, an early reptile before reptiles and mammals went their separate ways.
Want something with a bite to it? How about some teeth? Like Megalodon teeth, and a nodosaurid dinosaur, and how about the tooth of a giant ground sloth? What about primitive horse and rhino teeth?
Lots more to see. Come out and have a look. Bring your fossils and compare.
Here are some brachiopods you will see at the National Fossil Day event. They look much like clams, but are unrelated.
Here are some bryozoans, which look like they should be related to coral, but are thought to be more related to brachiopods because they share the same odd feeding structure.
Speaking of corals…
One of the common fossils you can find in Arkansas are cephalopods, which are all the squids, octopuses, and in terms of fossils, ammonoids. Arkansas has some very large ones. If one goes to Northeast Arkansas and looks in the Fayetteville Shale, one can find ammonoids with shells several feet long. Here is a preview of some of the fossils you will see Saturday.
Come back tomorrow for more fossil previews. Come to the museum to see much, much more.
National Fossil Day is October 15th, but the Museum of Discovery, in conjunction with the Earth Science and Anthropology departments at the University of Arkansas at Little Rock (UALR), the Arkansas Geological Survey, the Arkansas State University Museum, the Virtual Fossil Museum, and others (including of course, me) will be putting on an exhibit on October 11th. If you are in the neighborhood, please stop in. there is much to do and see for everyone from toddlers to grandparents and professional researchers.
This week I will be sharing a few photos of the collections at the UALR Earth Science Department as a preview of things you will see. We will start with echinoderms today. These include crinoids, sea urchins, starfish, and an array of others.
So were you able to figure out what Monday’s fossil was. Congratulations to Herman Diaz for not only correctly identifying it, but the relative that lived in Arkansas as well. If you want to see it in person, along with much more, come out to the National Fossil Day event at the Museum of Discovery in Little Rock.
This is the foot of Allosaurus fragilis, which means “different delicate reptile”. It has gone by a lot of names. Depending on the researcher you ask, Antrodemus, Creosaurus, Labrosaurus, Epanterias, and Saurophaganax are all just versions of Allosaurus.
Because of this, it can be difficult to say just how big Allosaurus was. The most famous specimen called “Big Al” is actually on the small side, measuring only about 7.5 m (25 ft), whereas the American Museum of Natural History has a specimen that is almost 10 m (33 ft.). The fossil called Epanterias is a good 12 m (40 ft.). Thus, Allosaurus may have been essentially the same length as Tyrannosaurus rex, although it was more lightly built, so it would not have weighed as much. We should keep in mind though, that every species has a fairly wide range of sizes, so even when we can measure a bunch of living specimens, stating an average size has to come with wide error bars, so take these measurements with a grain of salt.
Allosaurus itself never lived in Arkansas. But a close relative of it did. Acrocanthosaurus is classified as a Carcharodontosaurid, which is a group that is generally considered to by descended from earlier allosaurs. Allosaurus himself lived in the late Jurassic Period, whereas Acrocanthosaurus lived in the early to middle Cretaceous, so the timing lines up with what we know. No bones of Acrocanthosaurus have ever been found in Arkansas, although they have been found in Texas and Oklahoma. What we do have in Arkansas is their tracks. A large trackway was found in Howard County in 2011. This trackway was mostly footprints of large sauropods such as Sauroposeidon, but it also contained theropod trackways, which were identified as being from Acrocanthosaurus.
Acrocanthosaurus was as big as the biggest allosaurs and was known for unusually long spines on the vertebra, especially over the ribcage. Why did it have the spines? While they weren’t as tall as Spinosaurus, but they were longer than would be necessary for strictly muscle attachment, so the best explanation was that it formed part of a display to make it look bigger and more impressive. It was the biggest predator around, so it likely was not for defense, but to intimidate rivals and impress potential mates.
As the biggest predator around, it preyed upon the main herbivores of the day, which in this case were probably juvenile or elderly sauropods (the healthy adults were likely immune from predation simply on account of size). The skulls were more lightly built than tyrannosaurs, so they probably did not munch through bone like tyrannosaurs. They were apparently more selective in their eating. This would have made them very popular with the scavengers of the time as they would have left more behind.
Were you able to identify Monday’s fossil? Allie Valtakis was. Find out after the picture what it is. I hope it doesn’t make your weekend too crappy.
These two things are coprolites, otherwise known as fossil poop. Always a hit with kids when I show them in schools, but I always get the same questions. Do they smell? Will I get poop on my hands if I touch it? Most are tentatively reassured when I inform them that to be considered a coprolite, the poop has to be replaced with mineral. After a long period of time, there isn’t any actual poop left.
Coprolites can be quite informative. Coprolites preserve traces of what the animal that left it ate, so they can be useful for looking at the diet of prehistoric animals. Karen Chin, a curator at the Colorado University Museum at Boulder, is the leading expert on coprolites, particularly dinosaur coprolites. She found wood In some coprolites found in the Two Medicine Formation in Wyoming, which is unusual for two reasons. One, most coprolites are from carnivores, so herbivore coprolites are relatively rare. Secondly, most herbivores don’t eat wood except as a last resort when no other food sources are available. She was able to tentatively attribute these coprolites to the hadrosaur called Maiasaura (mainly due to the size and content of the coprolites, and the abundance of maiasaur bones in the area), making this the first dinosaur known to eat wood, as well as giving a unexpected perspective on the lifestyles of these “duck-billed” dinosaurs.
Probably the most famous coprolites known are also from the Two Medicine Formation and were also studied by Dr. Chin. They were uncommonly large and clearly from a carnivore. The only known carnivore from that formation big enough to create such a ponderous poop was Tyrannosaurus rex himself.
These coprolites told a fascinating story. The coprolites were readily identified as being from a carnivore due to elevated levels of phosphorus, which results from eating a high protein (i.e. meat) diet. The coprolites contained numerous bone chips, indicating that T. rex was not a dainty eater. T. rex had a massively built skull with powerful jaws, providing T. rex with the most powerful bite of any terrestrial animal. It put these jaws to use chomping through a carcass, bone and all. If one compares the thick, broad teeth of a tyrannosaur with the flatter, blade-like teeth and lighter skull of an allosaur, it is clear they had fundamentally different niches and eating styles.
There was bigger surprise found in the tyrannosaur coprolites. Dr. Chin found traces of undigested muscle. Obviously, it was not original muscle left in the coprolites, but mineralized remains. Why is this important? Modern reptiles have a slow metabolism. Food takes a long time to go through the digestive tract. As a result, digestion is phenomenally thorough. Crocodilians can take the enamel off teeth. Mammals, on the other hand, have notoriously inefficient digestive tracts. It is not uncommon to find recognizable bits left in the feces. Because of the elevated metabolism, food simply passes through too quickly for digestion to be complete. Meat is far easier to digest than plant matter, so carnivores, even mammalian carnivores, typically do a good job of digestion. To have traces of undigested muscle in the coprolite of a T. rex means that either the tyrannosaur was terribly sick with a bad case of the runs, or more likely, tyrannosaurs had short digestive times and a high metabolism to go along with it. It is possible to have thorough digestion with a high metabolism, but it is much harder to have incomplete digestion in a carnivore with a low metabolism.
Thus, coprolites not only tell us about the diet of extinct animals, they can also tell us about their physiology.
On the preservation side of things, one may ask how something as soft and squishy as a poop can fossilize. The answer to that is not easily. The vast majority of poops get washed away. But fecal material does have some advantages that help them get mineralized. As I stated earlier, carnivore feces is enriched in phosphorus. Phosphorus is an important nutrient, eagerly sought after by many organisms because it is not all that common in the environment, making it what is known as a limiting resource.
The other advantage is that feces is mostly made of bacteria, not really waste products. Our intestines are populated with microbes without which we can’t digest our food very well. The richer foods we eat, the more the microbes can grow and meat is a very rich food source.So why is having bacteria in the feces an advantage? Because the waste products they give off during their metabolic processes cause minerals to precipitate around them. Those bacteria are in a phenomenally rich food source in the poop, so they are growing like crazy, which means they are also precipitating minerals like crazy. In effect, they fossilize the poop while they are trying to eat it. If the poop can stay together, is not disturbed, and there is sufficient water around to allow the continued growth of the microbes, you will get a coprolite. The problem with this of course, is that poops are rarely left alone. Other animals eat them, dung beetles carry them off, they get stepped on and spread about, and rain washes them away.
If you have a kid interested in learning more about coprolites, I recommend the book Dino Dung, by Karen Chin. The book is written for elementary school kids, but is packed with a lot of good information on the study of coprolites and provides a great introduction to the study of fossil poop.