Two years after opening, Uŋčí Makhá Park can be considered a paleontological gem in the Twin Cities. With its Magnolia Member bedding planes, side cuts through the Magnolia and Carimona, easy access, and lack of vehicle traffic, it's nigh-on perfect for getting in touch with St. Paul as it was about 454–453 million years ago. It's kind of like our own Carnegie Quarry wall, except it's tiny marine invertebrates rather than dinosaurs, it probably wasn't planned, and you can walk right out over it. It's always fun to get to spend time there for work, and like last year, I got the opportunity to assist with a training session for Mississippi National River & Recreation Area seasonals there. Then, of course, I just had to make a quick return trip later to follow up on some things we'd seen.
It had been raining much of the previous three days, so the water level in the excavated channel was higher than I'd ever seen it, precluding access from some areas. On the other hand, a constant mist was keeping the surfaces of the rocks and fossils wet, which can bring out things that aren't as visible when dry; it was an even trade, I'd say.
Fossils just look a little different wet, y'know? |
The winter, such as it was, had almost no snow and little precipitation of any kind, but the temperature was still usually below freezing, and there was still groundwater to freeze and thaw things. The Carimona is still weathering faster than the Platteville. Fossils are flaking off in places, but on the other hand new fossils are being exposed and weathering is enhancing the exposure of others. Generally I've had a hard time relocating fossils between visits, but that's more a matter of the "Where's Waldo"-like nature of the bedding planes. Here's a couple that we saw before:
The annulated nautiloid; compare to
2022. By checking
Kolata (2021)
I think this is Monomuchites rather than Anaspyroceras, as
the annulations are more closely spaced and a bit crisper. |
The big knobbly burrow; compare to
2023. This one looks like it's suffering more, although some of that could
be sediment deposits obscuring the features. |
Horn corals
Something I noticed this time is that horn corals seem to show up only in the lower part of the Magnolia here.
Spot the three corals! (Bonus: and the small partially dissected
orthocone.) |
Brachiopods
There are of course too many brachiopods here to photograph them all, but here are a few interesting occurrences.
Taphonomy! Here's an odd little patch of bedding plane exposure where
the shells are not laying flat, but are stacked sideways. |
Bivalves
Bivalves are starting to become easier to find, probably due to improving search image.
In this case, the bivalve has become invisible, but we can still tell it
was there. |
What? Another ex-bivalve? Don't you have any bivalves that are still
there? |
It's not a bulbous Vanuexmia-type, but it'll do. Note the optical
illusion; this is actually concave, not convex. |
Nautiloids
It was a good day for spotting nautiloids, even if most of them were partial molds and casts of small orthocones.
Like this happy little fellow (actually, this one probably has the best
preservation). |
There was some variety, though:
Only a little bit is exposed, but this is clearly more in the
Cameroceras/Endoceras mold. |
This orthocone falls somewhere between the previous two in size. It's
pretty vanilla, probably something in the Cartersoceras/Proteoceras
vein. |
This one has a subtle bulge partway through. Several Platteville
nautiloids do that, but the slender build and relatively thick chambers
suggest we're dealing with Whitfieldoceras mumiaforme. |
Nautiloid diversity here is fairly significant, around 8 or so taxa at minimum: at least one and probably two annulated forms (Anaspyroceras and Monomuchites), a spiral form (Plectoceras), a fat curved form (Beloitoceras), a bulging form (Whitfieldoceras), at least one fairly large unornamented orthocone, at least one great big orthocone, and at least one finger-sized orthocone.
Gastropods
One day I'll have to guesstimate the snail diversity here, although it's hard with the preservation we get here.
This may look like nautiloid chambers, but note the way each "chamber"
bulges. This is actually a high-spired snail, probably something like a
large Hormotoma. |
No particular reason except I liked it. You've got a
Lophospira-type screw snail on the left and a cross-section
through a spiral galaxy on the right. |
Trilobites
Because of their habit of generally being smallish and only leaving being
small parts of the whole, trilobites can be hard to spot; I often only find
them after the fact in photos of other things. There are exceptions,
though.
Hey! Another chunk of an Isotelus! |
Ostracodes
Here's a better Eoleperditia than before. (Again with the optical
illusions—this is concave; note the other shadows.) |
Echinoderms
The stars this time were the echinoderms. The most exciting find was made by one of the participants, who observed these little objects in the Carimona:
The group of small equant light-colored objects arranged in an array. |
There's really only one thing this could be: part of the arm of a small sea star such as Hudsonaster (compare to the photos here). This is not something you see every day!
The Carimona is good for crinoids, too, with lots of columnals.
Lots of columnals; where's the rest of the crinoid? |
The Platteville here is less echinoderm-rich, mostly with just the odd columnal here and there, but we did have the partial stem in 2023, and I saw this when I returned after the session this year:
This set of arms is just barely at the surface. I wish the calyx was
there! |
Trace fossils
Under the overcast, damp conditions, the burrows really popped. A lot of them are dark, on the order of a finger in thickness, and have a wrinkly texture; I feel even more strongly now that these were lined burrows and the lining collapsed. For convenience, I've been thinking of them as basically Palaeosynapta.
Here's a pretty representative example. |
In general the Platteville burrows here are dark against the lighter yellow-gray rock, whereas the Carimona burrows are about the same color as the surrounding medium to dark gray rock, or a bit lighter.
When you know where you're going. |
When you realize you forgot something. |
Others
Of course, there were a few things I haven't identified.
It's the
Carimona Brown Thing
again! |
References
Kolata, D. R. 2021. Fossils of the Upper Ordovician Platteville Formation in
the upper Midwest USA: an overview. Illinois State Geological Survey, Prairie
Research Institute, University of Illinois at Urbana-Champaign, Champaign,
Illinois. Bulletin 108.
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