Journal of Paleontology; September 2009; v. 83; no. 5;
p. 794-803; DOI: 10.1666/08-096.1
© 2009 Paleontological Society
A NEW AGELACRINITID EDRIOASTEROID ATTACHED TO A LARGE HARDGROUND CLAST FROM THE MCKENZIE MEMBER OF THE MIFFLINTOWN MEMBER (SILURIAN) OF PENNSYLVANIA
COLIN D. SUMRALL1,
CARLTON E. BRETT2 and
MICHAEL L. McKINNEY1
1 Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, 37996
2 Carlton E. Brett, Department of Geology, University of Cincinnati, Ohio 45221
A new agelacrinitid edrioasteroid, Multiplexidiscus mckenziensis n. gen., n. sp. is described from the middle Silurian upper McKenzie Shale Member of the Mifflintown Formation of Pennsylvania. These edrioasteroids were attached to a large hardground clast that was reworked and flipped during a storm event. The occurrence of edrioasteroids in a near shore, perhaps in sub-normal salinity, is unusual for echinoderms. The edrioasteroids show a dispersed spatial distribution and weak thecal orientation. Multiplexidiscus differs from other agelacrinid edrioasteroids in the presence of a complex pattern of ambulacral cover plates combined with nearly straight paedomorphic ambulacra.
Key Words: Edrioasteroidea Silurian New York McKenzie Mifflintown
Copyright © 2009 by Paleontological Society