Sheffield and Sumrall—Generic revision of North American Holocystitidae
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Figure 4.
(1) Gomphocystites indianensis Miller, 1889, a nonholocystitid
diploporitan from the Silurian of North America. Note the long, spiraling ambulacra. Brachiole facets are borne from the left side of the ambulacra only. True diplopores situated within shallow, elliptical peripores are clearly seen in this image (FMNH 19708). (2) Middle Silurian Eucystis specimen from the Bainbridge Formation of Missouri. Oral area pictured shows five multibranching ambulacra extending across the orals and proximal thecal plates and ending in various numbers of large brachiole facets (CMCIP 53630). Scale bars = 1 cm.
strongly from holocystitids. It has a typical oral plate–bearing oral area but lacks O7, and plates O2 and O5 are not in contact with the peristomial opening. The recumbent ambulacra are long and spiraling and wrap around the theca, but they bear brachiole facets only on the left side and seem to be borne on floor plates that are restricted to the left side. They also bear true diplopores instead of the humatipores of holocystitids. The only other known Silurian diploporitan from North
America is a recently discovered and undescribed species of Eucystis from Wenlock-age strata of the Bainbridge Group of Missouri (Sheffield and Sumrall, 2015b). These specimens (Fig. 4.2) share strong morphological similarities with Eucystis from the Ordovician Baltican and peri-Gondwanan faunas. Like their Baltican and peri-Gondwanan counterparts, these speci- mens have five multibranching ambulacra extending across the orals and proximal thecal plates without underlying floor plates. These food grooves each end in a brachiole facet. The diplopores
are simple, and the theca bears an unusually large holdfast that flares slightly at the attachment surface (whether this flaring is characteristic of this taxon or was formed around an unusually large bioclast is unclear). However, these specimens share a similar, slightly clockwise rotation of the oral plates with respect to the ambulacra with Holocystites and
Glyptosphaerites.Itis clear, from strong morphological deviations, that neither Gomphocystites nor these recently discovered eucystitid speci- mens are closely related tomembers of Holocystitidae. Details of the relationships between these taxa are pending phylogenetic analyses that are currently in progress.
Previous phylogenetic analysis.—An evolutionary hypothesis of the Holocystitidae was proposed by Frest et al. (2011), based on assumed trends in peristomial morphology. A second ana- lysis based on a stratocladistic model is not discussed here. The resulting phylogeny (Fig. 5) shows a complicated evolutionary history with drastic changes in the oral area of the diploporitans from an inferred hypothetical ancestor to the more derived taxa (Table 1). Holocystites and Trematocystis are depicted as grades of organization at nodes rather than as monophyletic groupings of taxa. Frest et al. (2011) drew the conclusion that more- derived holocystitids trended toward a reduced number of plates
Figure 5. A proposed evolutionary hypothesis proposed by Frest et al. (2011), based on changes within peristomial morphology; note that Holocystitinae, Holocystites, and Trematocystis are all paraphyletic. This analysis interpreted a trend toward a reduction in oral plates in advanced holocystitids, such as Pentacystis, whose species were described as having vestigial or absent oral plates. Figure modified from Frest et al. (2011).
within the oral area. As mentioned in the preceding, the number of plates observed was affected by taphonomy and specimen preparation and is, therefore, not based on the evolutionary history of the taxa involved. Further, Paul (1971) and Frest et al. (2011) misidentified an oral plate (O7) as a facetal plate, which influenced their interpretations. Some of the characters within their analysis were based on counting the numbers of plates present in proposed taxa. However, characters based on the number of plates present in the absence of a clear understanding of which homologous elements are present and absent among taxa are not properly constructed because the alternate states are not derived from a single character transformation.
Materials and methods
Repositories and institutional abbreviations.—All taxa studied for this analysis, alongwith their locality and age information, are listed in Table 2. All specimens are housed in research collections from the following museums or institutions: CincinnatiMuseum Center (CMCIP), Field Museum of Natural History (FMNH; UC), TheUniversity of Iowa (SUI),Miami University (MUMG), and Yale Peabody Museum (YPM). Brightonicystis was not examined for this study because of a lack of available material.
Systematic paleontology
Subphylum Blastozoa Sprinkle, 1973 Class Diploporita Müller, 1854
Superfamily Sphaeronitida Neumayr, 1889 Family Holocystitidae Miller, 1889
Type genus.—Holocystites Hall, 1861
Other genera.—Trematocystis Jaekel, 1899; Pentacystis Paul, 1971; Pustulocystis Paul, 1971; Brightonicystis Paul, 1971; Paulicystis Frest and Strimple, 2011 in Frest et al., 2011.
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