Mystery Fossil

The Mystery Microfossil
"Heimbrock's Wedges with Ridges"

Here's a mystery fossil that has been the first such specimen anyone has ever seen, including many renowned paleontolgists. It is still not known what type of animal this fossil represents. It is a microfossil ranging in size from 0.5 mm to 2 mm long. It has been found at only one site. The site is in Northern Kentucky. It is likely to be a phosphatic mold because it is only found in the phosphatic "Cyclora Fossil Hash" layers of the site from the Middle to Upper Arnheim Formation of the Cincinnatian (Upper Ordovician). The mystery fossil is abundant in a couple of fossil hash layers on that site. A 2, 3 or 4-plate specimen can be found on every rock you pick up and samples of the gritty soil taken home in bag and cleaned will yield dozens of single and double plate specimens.

If you have any thoughts on what this mystery fossil may be, or would like me to mail you a few samples for analysis, please Email me at billheim@xfossils.com .

Bill Heimbrock
Dry Dredgers
1621 Westwood Ave
Cincinnati, OH 45214
(513) 921-2335

T A B L E O F C O N T E N T S

General Description of Exterior Structure
Some Four-plate Specimens
Speculation on the Identity of the Mystery Fossil
Description of Layer Containing the Mystery Fossil

Pictures of 3, 4, and 6-plate specimens
See a stereo image of a 4-plate specimen
Click here to see THIN SECTIONS of the Mystery Fossil!
The Pelecypod Hinge Teeth Hypothesis
New Photos of Lyrodesma dentations resembling Mystery Fossil! (NEW)
Possible Evidence of Secondary Phosphatization and Origin of the Nodules in the Mystery Fossil (NEW)
Roger Cuffey's list of possible suspects
Emails with Paleontologists discussing the Mystery Fossil

The Exterior Structure

There seems to always be an end that is open, exposing grit, nodules and possible bridges between the plate sides. It is always the same end that is open. The opposite side of each plate is a mirror image of the first side. One "facing" side of each plate has the high end of the ridges on the left and the other side has the high end of the ridges on the right. We can refer to the facing sides as the "high on left" side and the "high on right" side. It seems to me that the open end (the end with guts showing) is always on the "high side" of the ridges. This leads me to wonder if the open side of each specimen is incomplete, perhaps because the shell becomes too thin to be preserved. When there are two plates stuck together, both plates have their ridges oriented the same way. They are usually closer to each other on the wide, thin end as shown below.

There appears to be grit and nodules between attached plates. This may have been material belonging to the living animal. Some plates appear to be slightly bowed in one direction as shown above, while others appear to be relatively flat.

Some plates are much wider than others, as if serving the purpose of two normal plates. These have an additional curved bottom as shown above. Perhaps this curved around another body part to which it attached. It is possible that this wide plate is complete, while all the narrower plates you find are simply broken versions of this wide, complete plate.

Four Plate Specimens

Here is a four-plate specimen in matrix. In this example, some of the plates are equidistant to each other for the entire length of the plate. There is black material between the plates with a few light colored objects bridging the plates.

Here is another four-plate specimen in which the plates are offset from each other. The fourth plate is broken (right). Note the nodules hanging out the left side of each plate.
Photo compliments of Colin Sumrall, Cincinnati Museum Center.

Specimen 13
Shows how the plates fit together. This appears to be a juvenile specimen. It is smaller than most and the ridges form a sine-wave curve as illustrated at right.

Click Here for More Pictures of 3, 4, and 6-plate specimens!

Speculation on the Identity of the Mystery Fossil

I have shown it to many experts and no one as recognized it or are even sure what class it is in. Some people have ruled out Echinoderm because, when broken, it doesn't exhibit a stereom structure of pores. It could be a Cirrepedia, but experts have ruled out Machaeridian. The problem there is that the shell of a Machaeridian is thin. This mystery microfossil is thick, but may well be a mold. It could be an Operculum (foot plate) of a gastropod. The problem is that there is no gastropod in this layer the right size to have this sized operculum. Another problem is that the ridges look the same on both sides. An operculum would not have ornamentation on both sides. It could be a part from an Ordovician fish. Again, the problem is that the ridges look the same on both sides, which is uncharacteristic of fish parts.

I have thought that perhaps this mystery fossil could be a bryozoan colony internal mold. The abundant bryozoans from this site are preserved as internal molds. In this form, the zooids form rods. The overlying mesh pattern is removed. The mystery plates could be where the phosphates have melded the zooids together. Phosphates have been found at this site oozing into and out of any opening available.

Another good possibility is that of pelecypod hinge teeth. The Upper Ordovician clam, Lyrodesma, has teeth that closely resemble the multiple plate specimens of our mystery fossil. In this case, each mystery plate would be the external mold of phosphates between the individual teeth of a single valve.

Click Here for a detailed description of my pelecypod hinge teeth hypothesis .

Click Here for some photos of Possible Evidence of Secondary Phosphatization and Origin of the Nodules in the Mystery Fossil

Description of Layer Containing the Mystery Fossil

The mystery fossil comes from a layer in the middle of the Arnheim Formation in the Cincinnatian Series of Northern Kentucky. It can be described as "fossil hash with Cyclora gastropods". This 1 foot layer consists of sandstones and loose sand material. The sandstone is comprised of a reddish brown gritty matrix filled with tiny gastropods, pelecypods, bryozoans, annelid worm tubes, cyclocystoid plates and other unidentified plates which all appear as white dots in the matrix when first coming across such rock.

The gastropods and bryozoans are white to yellow in color. The gastropods appear to have a coating of brownish/blackish material, perhaps contributing to their yellowish coloring. The mystery plates, similarly, vary in color from white to yellow and possess a brownish black grit coating.

The quantity of Cyclcocystoid plates in this "fossil hash" is astounding. They are very abundant and ubiquitous throughout this layer. The "mystery fossil" is also ubiquitous in this layer but only slightly abundant. One specimen of the "mystery fossil" can be found on the surface of almost every rock in the layer.

Other types material found in this sand and matrix include a conodont and a scolecodont. Some crinoid stem and cup plates are also found. Echinoderm material has the stereom structure filled with phosphates, which can be seen when broken or dissolved in acid.

Removal of samples of the loose sand surrounding the "fossil hash" rocks has yielded many specimens of the mystery fossil free from matrix. Almost half of the specimens found are double-plate specimens. A couple of three-plate specimens have been found loose, but many more three-plate examples have been found imbedded in the surface of the rocks. To date, 20 four-plate specimen have been found on the surface of rocks.

The layer containing this fossil hash is just above a one-foot-thick limestone hard layer consisting almost entirely of Rafinesquina Brachiopod fragments. Similar layers of badly fragmented Rafinesquina can be found above the "fossil hash" layer.

Other layers above the "fossil hash" layer include shale with zones of very abundant Zygospira Brachiopods. There are other gastropod zones consisting of larger specimens including Cyclonema . Fragments of the trilobites Isotelus and Flexicalymene have been found in these shale layers as well as one complete Flexicalymene.One such shale layer of abundant Zygospira Brachiopods exists immediately above the "fossil hash" layer.

Here's a group picture showing just how common these mystery fossil are. They were picked out of the sand with a tweezers.