1 D13. Paleontology, Phylogenetic/Morphological Patterns: Invertebrates

Sunday, 22 October 2017
8:00 AM - 12:00 PM
Room 604

THE CONVOLUTED HISTORY OF PARACRINOIDS AND RHIPIDOCYSTIDS (BLASTOZOAN ECHINODERMS) DURING THE ORDOVICIAN RADIATION

Paper number: 1-12
Program: Technical Sessions
Time: 10:45 AM – 11:00 AM

Authors

Abstract

Paracrinoids (about 24 genera) and rhipidocystids (6 genera) are derived blastozoan echinoderms forming part of the Ordovician Radiation. They lack the pentameral symmetry and organized plate circlets that characterize many other early stemmed echinoderms, replacing them with two different types of bilateral symmetry. Lens-shaped paracrinoids appear to be flattened in the BC–DE plane, in contrast to rhipidocystids that are flattened in the A–CD plane. Paracrinoids were thought to be a well-defined mostly Late Ordovician class when monographed in 1975, but new discoveries in western Laurentia expanded both their stratigraphic range downward to the Early Ordovician and their morphologic diversity. Rhipidocystids also have recently expanded from Middle to Late Ordovician with a new taxon from Laurentia.

Thecal shapes range from globular to ovoid to lens-shaped in paracrinoids, and are strongly flattened in rhipidocystids. Plates in rhipidocystids and some paracrinoids are polygonal, thin, and smooth; in other paracrinoids, plates are either ridged with covered respiratory slits or surface pores between radiating ridges, or concave with respiratory pores on the raised sutures or in plate centers. The mouth can either be central on the summit opposite the stem facet (most rhipidocystids and early paracrinoids) or tilted off the summit with the periproct opposite the stem facet (most later paracrinoids). 2-5 recumbent or erect ambulacra can radiate from the mouth, with either erect biserial brachioles or uniserial ‘pinnules’ attached to the ambulacra.

Various workers in the late 20th Century, such as Frest and Rozhnov, suggested a sister-group relationship between the two groups, but exactly what synapomorphies link the two groups as a clade remain elusive. We suggest the search for phylogenetic linkage focus on peristomal bordering plates, hydropore–gonopore–periproct arrangement, the 3-plate basal circlet, and proximal stem morphology. These features are likely to be relatively stable compared to highly variable features such as thecal plate number, respiratory structures, and ambulacral system arrangement.

Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-302126

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