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Journal of Paleontology 91(4):767–780
from four columns of interambulacral plates to two (Fig. 4). Furthermore, this character seems to have been widespread, as crenulate tubercles are known in Permian archaeocidarids from Timor (Wanner, 1841, fig. 2.1), Pakistan (Waagen, 1985), and Hungary (Mihály, 1980). The discovery of archaeocidarids with crenulate tubercles allows for a better understanding of the probable last common ancestor of the euechinoids and cidaroids. That the innovation of crenulate tubercles likely preceded the evolution of a perignathic girdle and the reduction of interambulacral plating to two columns indicates that the evolution of crenulate tubercles probably preceded the last common ancestor of euechinoids and cidaroids, and thus this last common ancestor likely bore crenulate tubercles. It is, of course, possible that the Archaeocidaridae indet. described herein is a separate lineage of archaeocidarids, which conver- gently evolved crenulate tubercles that are not homologous to those of the miocidarids. The ideal way to test this hypothesis would be through phylogenetic analyses. The material described herein, however, is too incomplete to incorporate into a quantitative phylogenetic analysis as the specimens described herein are composed solely of disarticulated material, with numerous characters that would need to be coded as unknown. Furthermore, these unknown data are not random, given that the taxon’s interambulacral plates and spines are the only morpho- logical features that are preserved. Nonrandom preservation, and subsequent nonrandom missing characters, can introduce systematic bias into the topological placement of taxa in cladograms (Sansom and Wills, 2013). This can be a particularly serious problem with respect to determining the phylogenetic placement of taxa near the crown group–stem group transition, as crown group taxa with many missing characters can appear to be members of the stem group (e.g., Sansom et al., 2010). That the indeterminate archaeocidarid described herein had more than two columns of interambulacral plates indicates it is likely a member of the stem group. We hope, however, to test the hypotheses of character evolution put forth herein in a rigorous phylogenetic context with the discovery of more complete specimens in the future.
Conclusions
The Permian echinoid fauna described here expands upon pre- viously known echinoid diversity in the Permian and sheds light on the Paleozoic divergence of crown group echinoids. This is one of the most diverse faunas of echinoids known from the Permian and indicates that a number of major families, the Archaeocidaridae, Proterocidaridae, and the Miocidaridae, coexisted in reefal environments adjacent to the Delaware Basin. The presence of Eotiaris guadalupensis in reefal environ- ments, similar to those inhabited by the European Eotiaris keyserlingi, may indicate that stem group cidaroids originated and preferentially thrived in these reefal environments. Further- more, the presence of crenulate tubercles on the indeterminate archaeocidarid indicates that crenulate tubercles evolved in archaeocidarids, likely before the reduction in interambulacral columns fromfour to two and the evolution of the first perignathic girdle. Crenulate tuberclesmay thus be plesiomorphicwith respect to the echinoid crown group.
Acknowledgments
This work was funded by National Science Foundation Grant IOS1240626. The authors thank S. Wing, M. Florence, D. Levin, J. Strotman, and K. Hollis at the USNM; A. Molineux at the Texas Memorial Museum, Austin, Texas; J. Cuvelier at the Université Lille; Y. Candela at the National Museums Scotland; and T. Ewin at the Natural History Museum, London, for providing access to specimens and specimen numbers. Furthermore, N. den Ouden provided access to specimens at Naturalis Biodiversity Center, Leiden, and S. Donovan provided the photograph in Figure 2.1. S. Zamora was instrumental in arranging the plates, and his suggestion of a black background improved the clarity of the photos. JRT acknowledges a student grant from the Palaeontological Association, which covered costs for the Progress in Echinoderm Palaeontology meeting in Zaragoza, Spain, from which this volume has been produced. Finally, we thank A. Kroh and L. Zachos, our reviewers, for their instructive comments, which helped to refine the manuscript.
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