Today we check in with one of the more unusual members of Paleozoic seafloor
communities:
Conulariida. The "four-sided herringboned ice cream cones" still hold many mysteries (including the mystery of the whereabouts of
George Sinclair's collection; I'd still be interested in knowing more about that!). One of the major
mysteries has been what exactly the soft parts of the animal looked like; if
we knew that, we'd know a lot more about how conulariids are related to other
animals, how they fed, how they looked, etc. It's generally assumed they are
some kind of cnidarian (along with corals, jellyfish, sea anemones, and so
on). Wikipedia has them potentially aligned with Staurozoa, which today is
represented by
stalked jellyfish
(worth looking up if you've never heard of stalked jellyfish).
A cnidarian identity would imply stinging tentacles, but these have never been
firmly identified. Soft parts in general are not particularly well-known for
conulariids, which makes sense because preserving the soft parts of cnidarians
is not something that just happens as a matter of course. (We could use a late Paleozoic
amber-producing coastal forest that was flooded by a storm that dredged up all
kinds of marine organisms.) There were some potential finds in the 1980s, as
discussed in Babcock and Feldman (1986a) and
Sendino et al. (2023)
(see
Figure 30
in Babcock and Feldman 1986b for internal casts and x-ray image of a conulariid's putative guts). Recently,
Sendino et al. (2023) have applied X-ray micro-Computed Tomography (μCT) to a
collection of well-preserved Pennsylvanian-age conulariids from the Wewoka
Formation of Oklahoma and the Finis Shale Member of the Grand Formation of
Texas.
What can μCT see in a conulariid? First off, it can see the concealed end of
one conulariid partially within another conulariid. This is a good sign as a
sanity check because we can confirm it can discern something that obviously
should be there. With that encouraging information in mind, what else is
there?
|
Figure 4
in Sendino et al. (2023); it's always good to see what you *ought* to
see.
CC BY 4.0.
|
Sendino et al. (2023) found "longitudinal bundles" in many of their specimens,
i.e., oriented apex–aperture. The authors interpreted these as muscles for
closing the flaps of the aperture. (This tells us a few things about the
muscular and nervous systems of conulariids.) In some examples there was also
an internal structure they interpreted as a possible gastric cavity. In other
specimens, the internal sediment was clearly replaced, for example by sand, or
contained other fossil material such as forams or a tiny drilled brachiopod.
The internal sediment of some specimens appears to have been disrupted by
later burrowing. A number of the conulariids also show scars from external
attacks (conulariids seem to have been easy targets). The article, which is
freely available, is heavily illustrated with μCT images, followed up by a
series of supplementary files of large images.
In other business: I'll be giving a talk for the Geological Society of Minnesota
on Monday, May 8: "Snorkeling at Shadow Falls: Fossils of Minnesota". Non-members are welcome!
References
Babcock, L. E., and R. M. Feldmann. 1986a.
Devonian and Mississippian conulariids of North America. part A. General
description and Conularia. Annals of the Carnegie Museum 55:349–410.
Babcock, L. E., and R. M. Feldmann. 1986b.
Devonian and Mississippian conulariids of North America. part B.
Paraconularia, Reticulaconularia, new genus, and organisms
rejected from Conulariida. Annals of the Carnegie Museum 55:411–479.
Sendino, C., B. Clark, A. C. Morandini, T. Salge, M. Lowe, and W. Rushlau.
2023.
Internal conulariid structures unveiled using µCT. PalZ (2023). doi:https://doi.org/10.1007/s12542-023-00649-7.