Another flat brachiopod from the class Strophomenata that can be found in the Bois d'Arc formation is Strophonella bransoni. It has a rounded to subrectangular shape with a (notably) convex brachial valve and concave pedicle valve. The surface of the valves have many thin costellae decorating it, which stand out in relief somewhat, and on some specimens very fine concentric growth lines can be seen. Amsden's original description for the species indicates that the pedicle valve has a small beak that extends past the hinge line but none of the specimens I found have that portion visible enough for me to confirm. Strophonella bransoni can be distinguished from Stropheodonta gibbera by the smaller degree of convexity to the shell and the stronger, more rounded costellae.
Specimen #2 - This specimen is more intriguing for the epibionts that decorate the shell.
I found the specimen shown on this page in the Bois d'Arc formation (Cravatt member)
near Clarita, OK which is Devonian in age (Lockhovian stage). The Bois
d'Arc overlies the Haragan formation but both are
the same age (Devonian, Lockhovian stage). They are both
roughly correlative to the Helderberg fauna of New York and thus are
contemporaneous with the Coyemans, Kalkberg and New Scotland formations.
"Stratigraphy and Paleontology of the Hunton Group in the Arbuckle
Mountain Region, Part V - Bois d'Arc Articulate Brachiopods " Amsden,
1958, Oklahoma Geological Survey Bulletin 82