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Journal of Paleontology; September 2009; v. 83; no. 5; p. 794-803; DOI: 10.1666/08-096.1
© 2009 Paleontological Society
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ARTICLE

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







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