T98 Perspectives on Multi-Element Skeleton Taphonomy: Case Studies, Approaches, and Advances
Monday, 2 November 2015
8:00 AM - 12:00 PM
Room 319/320
A GIANT PTERYGOTID EURYPTERID FROM THE EARLY ORDOVICIAN FEZOUATA BIOTA OF MOROCCO
Paper number: T98-8
Program: Technical Sessions
Time: 9:45 AM – 10:00 AM
Authors
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Peter Van RoyYale University, New Haven, CT
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Derek BriggsYale University, New Haven, CT
Abstract
The assignment of the Moroccan eurypterid to Pterygotidae infers a large ghost range for all eurypterid clades into the Lower Ordovician. This suggests either an explosive radiation of eurypterids during the earliest Ordovician, or an origin sometime during the Cambrian; the latter notion may be supported by the presence of chasmataspidid fossils in the late Cambrian of Texas. The new taxon also reveals that large body size evolved in pterygotids long before the first appearance of large armored placoderms. The co-occurrence of traditional Cambrian faunal elements such as anomalocaridids with Paleozoic faunal elements like eurypterids in the Lower Ordovician further underscores that the turnover between the Cambrian an Paleozoic Evolutionary Faunas was a considerably more protracted and complex affair than previously considered; as a consequence, the distinction between these evolutionary faunas may not be as clear as thought. The Fezouata fauna comprises a complex, multi-tiered ecosystem with multiple large predatory species, showing that such ecosystems evolved early in the Great Ordovician Biodiversification Event.