47 Under the (Ancient) Sea: Marine Life from the Coastal to Great Plains (Posters)

Friday, 8 April 2022
1:30 PM - 5:30 PM
Junior Ballroom B


ENVIRONMENTAL AND ECOLOGICAL ANALYZATION OF MIDDLE CHESTERIAN CRINOIDS

Paper number: 47-17
Program: Theme Sessions
Time: 1:30 PM – 5:30 PM


Authors


Abstract

The Mississippian Period was a peak of crinoid diversity during the Paleozoic, with genera radiating into new environmental niches. Eucladid crinoids expanded during this time and diverged into many specialized morphs adapted to varying water turbidities and tiering levels. An outcrop near Princeton, Kentucky has yielded abundant articulated and semi-articulated crinoid specimens collected over many years as they weathered out of the Middle Chesterian Glen Dean Formation. Using systematic taxonomy, six crinoid species have been tentatively identified: Dasciocrinus florialis (Yandell and Shumard), Phacelocrinus decabrachiatus (Hall), Phacelocrinus longidactylus (McChesney), Phacelocrinus sp., Phanocrinus maniformis (Yandell and Shumard), and Zeacrinites sp. Other noticeable fauna includes blastoids, brachiopods, and fenestrated bryozoa. The morphologies of these crinoids have been used to reconstruct possible relationships between members of the benthic community in this filter-feeder dominated Mississippian ecosystem. Specifically, traits such as fan density and branching patterns were analyzed to determine the most probable environments, tiering, and optimal turbidity for individual species and the collective faunal community. This kind of study shows the benefits of using biological traits as evidence for environmental and ecological conclusions when outcrops have been extremely weathered and degraded.

Geological Society of America Abstracts with Programs. Vol. 54, No. 4

doi: 10.1130/abs/2022NC-374990

© Copyright 2022 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.