Let's start with a pair of photos, one of typical Platteville Formation fossils and the same for the Decorah Shale:
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Welcome to the Ordovician! Hope you like brachiopods! |
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...or bryozoans and crinoids |
No points for guessing which is which. The first photo shows natural molds and casts in the Platteville, while the second shows the well-shredded fossils of the thin limestone beds of the Decorah. Now try this one:
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No peeking! |
Despite the preservation, this piece is from the Platteville. Specifically, it comes from a bed about halfway up the Mifflin Member. Somehow this bed managed to escape the worst of the heartbreak of dolomitization, at least in a small area. Little glimpses like this show a richer picture of the Platteville fauna than we get from the natural molds and casts. (The tiny crinoid columnals are an interesting touch, as is the relative scarcity of bryozoans.)
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They're in there. It's a proper hash. |
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The strophomenids might be a little smaller, too. |
There are also snails,
ostracodes, and some elongate triangular things. Some of these are probably small nautiloids, others might be
hyoliths.
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The example near the center bottom of the photo is one I suspect is a hyolith. |
There are a lot of subtleties to the rocks and faunal assemblages once you start looking!
(Also, having found a decent place to see the Glenwood up close, I've added a couple of photos to the
old post.)
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