The other day when Allison and I were out in the field, we made a quick stop near Dillsboro, IN to look at an outcrop of what was probably Mount Auburn Member (of the Grant Lake Fm) or the Arnheim Formation. We knew we were not any younger than that because we came across some rather large
Platystrophia ponderosa (
Vinlandostrophia ponderosa)
which are known the make through the Arnheim, yet disappearing before the Waynesville Formation. However we didn't see any of the true diagnostic fossils like
Lapteana or
Retrosirostra carleyi.
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Outcrop of Grant Lake or Arnheim Formation near Dillsboro, Indiana |
We did come across this rather interesting pair of rocks in the float that showed some sort of groove or gutter carved into what must have been a semi-harden marine floor and in this groove was dozens of small
Zygospira brachiopods.
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Groove or gutter filled with the small brachiopod Zygospira |
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Another accumulation of Zygospira from the same locality. The large brachiopod on the bottom right is a Rafinesquina. |
Zygospira are known for adhering themselves to whatever hard substrate they can find. In a
paper by Micheal Sandy (1996), the author describes a specimen from the Waynesville Formation of Ohio where an articulated
crinoid stem is thoroughly encrusted by
Zygospira. There have also been reports by local
trilobite collectors that they have found
Zygospira concentrated around fragments of
Isotelus in mudstone deposits colloquially referred to as butter shales (more on these next week).
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A closer look at one of the accumulations of Zygospira |
Lastly, an interesting note is that on at least one of the blocks we see the dumbbell shaped trace fossil
Diplocraterion generally thought to be the dwelling trace of a crustacean or worm.
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Arrow is pointing to the Diplocraterion trace fossils associated with one of these Zygospira accumulations. |
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