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An Afternoon With Sponges And Algae (Pennsylvanian)


Missourian

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On Saturday afternoon, I returned to a favorite spot in the Pennsylvanian Wyandotte Formation:

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The exposure, south of the Kansas City metro, features sponges and certain enigmatic forms that may be phylloid algae, as well as small crinoid calices and various other things. I last visited in fall 2011. I wanted to return early enough in the season to check out the patches of ground that are usually covered with weeds. Would a lack of vegetation, as well as two and a half years of weathering, expose anything new? Lets find out.

The Wyandotte is made up mostly of the Argentine Limestone:

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About twenty feet is exposed here. Just to the north, the limestone, combined with the overlying Farley Limestone, swells to as much as a hundred feet. This enhanced thickness is due to a reef-like build-up of lime mud bound by blades of phylloid algae. The interesting fossils found at this site may be due to them having grown in favorable conditions along the mound's southern margin.

The Argentine is fossiliferous. Large productid brachiopods can be found. This is Echinaria:

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Edited by Missourian
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Below the Argentine is the Quindaro Shale:

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Normally, this unit is unfossiliferous or sparsely fossiliferous. Here, there is a profusion of sponges, along with coral, bryozoans, brachiopods, crinoids, and a few mollusks including cephalopod, and shark teeth. Typically, only the sponges are well preserved. Most conspicuous are Heliospongia ramosa. I picked up several pieces:

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A few Heliospongia specimens....

Budding branch:

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'Hand' specimen:

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Sectioned and etched:

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Edited by Missourian

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Some Heliospongia formed colonies:

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There were even larger colonies, but I didn't take them home:

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Other twig-like sponges, include Maeandrostia kansasense and possibly Fissispongia, cover the ground in places:

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A few Maeandrostia (along with one Amblysiphonella, lower right, from the underlying Frisbie Member):

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Edited by Missourian

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At the base of the Quindaro is a thin packstone that may be the top of the Frisbie Limestone. This bed is made up of crinoid debris and various other fossils. This piece has a mold of a Petalodus tooth:

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The actual tooth was long gone.

A few inches down, there are thin beds and lenses of limestone that contain certain smooth and segmented plant-like thalli. I was hoping to find some in situ. I found one fragment at the top of the slope and began to dig:

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A found a few fragments with good detail:

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I have many more pieces that I haven't washed off yet.

I figure this is a highly unusual case of phylloid algae preserved in shale. These algae (red Archaeolithophyllum and green codiaceans), are almost always locked away in dense limestone where their morphology is difficult to determine. As mentioned above, the overlying Argentine Limestone is full of them.

Edited by Missourian

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Below the Frisbie is the upper twenty feet of the Liberty Memorial Formation:

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This gray sandy shale contains trace fossils including Conostichus.

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Wonderful report and specimens! Thanks for sharing your trip. :)

Process of identification "mistakes create wisdom".

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thanks for the trip, the sponges and algae are fantastic. :)

"Your serpent of Egypt is bred now of your mud by the operation of your sun; so is your crocodile." Lepidus

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Thanks everyone for the comments.

I cleaned off the remainder of the pieces, but nothing earth-shattering turned up (well, there was a bit of earth shattering to get to them. :) ).

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Excellent report! Your knowledge of the formations in that area is astounding..I still cant be certain of some of the formations I visit :D

That brachiopod is amazing, Ive never seen one that big!

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Excellent report! Your knowledge of the formations in that area is astounding..I still cant be certain of some of the formations I visit :D

That brachiopod is amazing, Ive never seen one that big!

Thanks. Fortunately, our Pennsylvanian units are thin and distinctive enough to make it fairly easy to get ones bearings -- most of the time.

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Did you fit any of the pieces together?

None so far. I guess I'll have to go back and dig some more.

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