Here is a fossil oyster shell from the Duck Creek formation that I found as float in the creek gravels. It belongs to the Genera
Gryphaea Texigryphaea and is somewhat narrow with two undulations on the left valve (all
Gryphaea Texigryphaea type oysters have a convex left valve and flat to concave right valve). As is often typical for oysters there are a number of seemingly overlapping growth lines that are hardly ever regular or flat. In profile the left valve is strongly recurved to nearly coiled over the right valve and angles off to one side a little. The interior of the valve is smooth and I don't see any obvious muscle attachment scars. The specimen I show below is missing it's right valve.
I am not familiar enough with the
Gryphaea Texigryphea to ID this down to the species level. The excellent website
North Texas Fossils lists
two possible species for the Duck Creek formation:
Gryphea corrugata (Say) and
Gryphea washitaensis (Hill). I found another reference on Google Books in "The Lower Cretaceous Gryphaeas of the Texas Region" by Hill and Vaughan, USGS 1898. Even using the illustrations in that book I have a hard time deciding what I found as both species appear to be very similar looking to me. Indeed, the Authors have the same problem with specimens found in the Duck Creek formation (pg. 62) and postulate that the two species interbred with each other. So at this point I am going to call it
Gryphaea Texigryphaea corrugata as that seems to be the most common species and also the "parent" species from which
G. T. washitaensis developed.
Update 6/6/16: A vigilant reader pointed out that the genera
Gryphaea is restricted to Europe and that the equivalent in the Cretaceous of Texas/Oklahoma is
Texigryphea. He also recommended an old issue of
"Oklahoma Geology Notes", Vol 35, No. 2 which has an paper by Robert Fay titled "The Type Species of
Mortoniceras and the Holotype Specimens of the Lower Cretaceous
Texigryphaea of the Southwestern United States". It has some helpful information and a key that may be used to ID specimens of
Texigryphaea. The link above takes you directly to the paper but if you click here you can go to the
Oklahoma Geological Survey site and look through all 74 volumes (up to winter of 2014). There are a lot of good publications and information on their website.
Left valve top
Left profile
Right profile
Interior of left valve
Ventral view
Dorsal view
The above specimen comes from the Duck Creek formation which is Cretaceous (Albian stage) in age.
Compare
G.
T. corrugata to a few other species from the lower Cretaceous of Texas:
Texigryphaea navia,
Texigryphaea marcoui and
Ilymatogyra arietina
No comments:
Post a Comment