Osgoodicystis Frest & Strimple, 2011
publication ID |
https://doi.org/10.4202/app.01212.2024 |
persistent identifier |
https://treatment.plazi.org/id/911087C6-FFE2-FFCB-FCD6-C899C976FBD5 |
treatment provided by |
Felipe |
scientific name |
Osgoodicystis Frest & Strimple |
status |
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Genus Osgoodicystis Frest & Strimple in Frest et al.,
2011 Type species: Osgoodicystis bissetti Frest & Strimple in Frest et al.,
2011, by original designation, from the Lewisburg and Massie formations, Sheinwoodian (lower Silurian), SE Indiana, USA.
Species included: Type species and Holocystites wykoffi Miller, 1891 .
Emended diagnosis.—Holocystitids with six narrow orals; with five food grooves along oral sutures (simplified from Frest and Strimple in Frest et al. 2011: 92).
Remarks.—In Osgoodicystis ( Figs. 12A View Fig , 13 View Fig , 14 View Fig ) the thecal outline may be cylindrical or inverted pyriform (Frest and Strimple in Frest et al. 2011: 19, fig. 13). The thecal plates are always smooth with buried humatipores. The mouth is rounded with a reduced oral circlet ( Fig. 13 View Fig ) even though all six oral plates are present. Oral pores are present in the oral plates ( Fig. 13A View Fig 1 View Fig ). The five ambulacral facets are confined to individual facetal plates and arranged in the same manner as in Pentacystis . The food grooves pass along the sutures between orals ( Fig. 14 View Fig ). The theca has a relatively large attachment area.
Stratigraphic and geographic range.—Sheinwoodian (lower Silurian), Indiana, USA. Osgoodicystis ranges from the lower limestone of the Lewisburg Formation into the base of the Massie Formation ( Frest et al. 2011: 14, fig. 10; Brett et al. 2012).
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