Way back in February, I wrote about the fossils my son found. At that time, I promised him I’d do some research and find out what kind of fossils they were. To recap, here’s what they looked like:
Time passed, and he asked other questions, and I got busy studying for a certification test at work (which is why I’ve been so quiet the past few months). But finally, since I’ve had a chance to catch my breath, it’s time to answer a question: what, exactly, are those fossils?
My primary source for this is Identification Guide for Common Fossils of the Cincinnatian. Based on this guide, most of the fossils appear to be Brachiopods, most likely some species of Cincinnetina (since they’re common in the region) – from the pictures in the guide, though, they could be Platystrophia ponderosa. The point is, they’re certainly brachiopods, and they’re around 480 to 440 million years old.
To tell you the truth, my son was disappointed that he didn’t find a Tyrannosaurus Rex. That wouldn’t be particularly likely, however, for a few reasons. The first being that T. Rex didn’t live 440 million years ago, and the second being that if T. Rex did live 440 million years ago in Cincinnati he would have drowned. Because Cincinnati was under water.
So, no Tyrannosaurs here. Certainly not in the strata that was laid down on his brachiopods.
And what, exactly, is a brachiopod?
Well, Wikipedia says that brachiopods are:
…a group of lophotrochozoan animals that have hard “valves” (shells) on the upper and lower surfaces, unlike the left and right arrangement in bivalve molluscs. Brachiopod valves are hinged at the rear end, while the front can be opened for feeding or closed for protection.
“Lophotrochozoan” animals are a clade of bilaterally symmetrical animals with cillia around their middle, if that helps.
Brachiopods are related to mollusks and annelid worms (earthworms and leeches). There are around 330 living species. There were a whole lot more of them back in the past, with the greatest diversity of Brachiopods occurring in the Devonian. The Permo-Triassic mass extinction crushed a lot of that diversity, and it has never fully recovered.
Modern brachiopods feed by sucking water in through their sides, using their cilia to trap particles of food, and then expelling the water and any waste products through the front. They absorb oxygen through their skin, and have colorless blood, and some modern species can live over 30 years (assuming they aren’t eaten).
Case closed, right?
Well, except for this strange little thing:
Uhm. What is that?
I have no idea. I’m pretty sure that’s not a brachiopod. Not unless we’ve got the shell end-on, and it also folded in a pretty dramatic fashion. After some digging, I four possible candidates. Here they are.
1. It’s just a rock. Needless to say, I find that boring. It is the null hypothesis, but I don’t think it’s accurate. after all, the color resembles that of the other fossils in the piece of stone my son found. So, although it’s certainly possible, I don’t think it’s correct.
2. It’s a piece of an Isorophus cincinnatiensis. This might be a reach, because it would make it a fragment of an arm of a 440 million year old echinoderm. Pros for the argument are that it’s from the region, it’s about the right size, and it looks kind of like the arm seen in this picture. Cons for the argument include the fact that it doesn’t look a whole lot like the arm in that picture.
3. It’s a bit of coral. I couldn’t find any pictures of coral that curves like that, but that doesn’t mean they don’t exist.
4. It’s something I can’t identify. Yes, yes, that’s an utterly lame hypothesis. But I’ve got nothing else, and I’m pretty sure it’s some flavor of fossil. So, I’ll probably just leave it at that. Unless someone reading this happens to know what that might be.