Class Crinoidea is from the Phylum Echinodermata, and first appears abundantly in the fossil record in the Ordovician Period. Crinoids consist of a flexible stem made of interlocking ossicles with a calyx (cup)
attached to the top. Coming off of the cup are arms, which are visible in the pictures below. The focus of this page is the calyx of the crinoids, which are needed for identification, and besides we found quite a few of
them on this year's field trip. Most of the ones shown on this page were found in a Gilmore City rock quarry by the Dordt 2000 Paleontology class, on a field trip taken November 3 and 4, 2000. A description of this
first stop can be found on the web (restricted to Dordt students). The students on the trip were: Greg Le Mahieu, Sharla Zwart, Janna Leusink, Becky Van Ee, and Marissa Moncur, and the professor, Dr. James Mahaffy. We found them in the Gilmore City Formation of the Mississippi Period. Also shown on the page is a calyx found by Florence Mahaffy (wife of Dr. Mahaffy) in the same formation, but a different site on a different date.
A number of the unidentified were identifed with the help of some crinoid experts.
|
|
|
|
|
|
|
|
|
|
|
|
Page modified on Nov. 7, 2006