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Penniretepora oculata

Penniretepora oculata

(Moore, 1929)

GBIF:226325038

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Descriptions(3)

Figure 19 A-E; Appendix 1929 Pinnatopora oculata Moore, p. 125 - 126, pl. 15, figs. 4, 5, 9. 1930 Pinnatopora oculata Moore, 1929; Warthin, p. 38, pl. 3, fig. 5.
Ernst, Andrej, Claussen, Anna Lene, Seuss, Barbara, Wyse Jackson, Patrick N. (2022): Stenolaemate bryozoans from the Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA. Palaeontologia Electronica (a 15) 25 (2): 1-56, DOI: 10.26879/1174, URL: http://dx.doi.org/10.26879/1174
Remarks. Penniretepora oculata (Moore, 1929) is similar to P. rossica Shishova, 1959, from the Upper Carboniferous (Gzhelian) of Russia but differs in having narrower branches (main branch width 0.27 – 0.49 mm vs. 0.45 – 0.50 mm in P. rossica) and smaller apertures (aperture width 0.05 – 0.08 mm vs. 0.09 – 0.12 mm in P. rossica). Penniretepora oculata differs from P. mariae (Shishova, 1959) from the Upper Carboniferous (Gzhelian) of Russia in possessing large widely spaced nodes on branches instead of a narrow keel with a row of small closely spaced nodes in P. mariae. Furthermore, lateral branches in Penniretepora oculata are spaced wider than in P. mariae (distance between branch centres 0.68 – 1.00 mm vs. 0.67 – 0.71 in P. mariae). Occurrence. Pennsylvanian of Oklahoma, USA. Upper Graham Formation, Pennsylvanian (Virgilian); Texas, USA. Graham Formation, Pennsylvanian (Virgilian); TXV- 200 (" Spillway section at Lost Creek Lake "), Texas, USA.
Ernst, Andrej, Claussen, Anna Lene, Seuss, Barbara, Wyse Jackson, Patrick N. (2022): Stenolaemate bryozoans from the Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA. Palaeontologia Electronica (a 15) 25 (2): 1-56, DOI: 10.26879/1174, URL: http://dx.doi.org/10.26879/1174
Material. SNSB-BSPG 2020 XCI 31, SNSB-BSPG 2020 XCI 51, SNSB-BSPG 2020 XCI 92, SNSB-BSPG 2020 XCI 94, SNSB-BSPG 2020 XCI 95, SNSB-BSPG 2020 XCI 96, SNSB-BSPG 2020 XCI 124. Exterior description. Pinnate colonies consisting of straight main branches with frequent lateral branches. Main branches 0.27 – 0.49 mm wide, lateral branches 0.19 – 0.30 mm wide, diverging at angles 68 – 81 ° from main branches, spaced 0.68 – 1.00 mm from centre to centre. Autozooecia having oval apertures, arranged in two rows both on main and lateral branches; regularly one aperture at the base of each lateral branch and one aperture between two neighbouring lateral branches. Median keels low, straight, containing widely spaced elliptical nodes. Interior description. Autozooecial chambers arranged in alternating order in one row on branches, trapezoid to roughly pentagonal in mid-tangential section both on main and secondary branches, relatively long, inflated, with moderately long vestibules. Axial wall strongly undulating from base to crest. Hemisepta absent. Extrazooecial skeleton moderately developed, traversed by abundant microstylets; microstylets with distinct hyaline cores and dark laminated sheaths, diverging from inner hyaline skeleton, regularly spaced across entire colony surface, 0.010 – 0.015 mm in diameter. Reverse side containing longitudinal rows of microstylets. Nanozooecia present.
Ernst, Andrej, Claussen, Anna Lene, Seuss, Barbara, Wyse Jackson, Patrick N. (2022): Stenolaemate bryozoans from the Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA. Palaeontologia Electronica (a 15) 25 (2): 1-56, DOI: 10.26879/1174, URL: http://dx.doi.org/10.26879/1174

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FIGURE 19. Penniretepora oculata Moore, 1929 (A–E): A, B – branch fragment with autozooecial apertures divided by keel with nodes (XCI 124); C, D – tangential section showing autozooecial chambers (XCI 96); E – tangential section showing autozooecial apertures (arrow: nanozooecium) (XCI 96).

Imageimage/png© Ernst, Andrej;Claussen, Anna Lene;Seuss, Barbara;Wyse Jackson, Patrick N.Ernst, Andrej;Claussen, Anna Lene;Seuss, Barbara;Wyse Jackson, Patrick N.

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Source Information

Stenolaemate bryozoans from the Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA

checklist

This dataset contains the digitized treatments in Plazi based on the original journal article Ernst, Andrej, Claussen, Anna Lene, Seuss, Barbara, Wyse Jackson, Patrick N. (2022): Stenolaemate bryozoans from the Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA. Palaeontologia Electronica (a 15) 25 (2): 1-56, DOI: 10.26879/1174, URL: http://dx.doi.org/10.26879/1174

ABSTRACT

An exceptionally well-preserved bryozoan fauna has been described from the Finis Shale Member, Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA. Nineteen bryozoan species (four cystoporates, one trepostome, two rhabdomesine cryptostomes, and 12 fenestrates) have been identified in two profiles which cut the most vertical range, at the level of the outcrop-base, of the Finis Shale. Two species are new: a trepostome Dyscritella felixi n. sp. and a fenestrate Laxifenestella texana n. sp. The fauna was studied on a combined basis of external and internal morphology, using a SEM and thin sections, respectively. Bryozoans from the Finis Shale Member exhibit a variety of growth forms from encrusting unilaminar, erect ramose, erect reticulate robust, and erect reticulate delicate, to erect pinnate morphologies. The erect growth forms clearly dominate, and bryozoans become more robust in the upper level of the profiles. The distribution pattern of bryozoan growth forms indicates gradual shallowing in the profiles supporting the assumption of a transgressive-regressive cycle in the Finis Shale. Bryozoan richness, abundance, and α-diversity increase toward the top of the profiles. Palaeobiogeographic relations of the Finis Shale bryozoans are mostly restricted to the American realm, with some connections to the Pennsylvanian of Europe.

Andrej Ernst. Institut für Geologie, Universität Hamburg, Bundesstr. 55, 20146 Hamburg, Germany. Andrej.Ernst@uni-hamburg.de

Anna Lene Claussen. GeoZentrum Nordbayern, Friedrich-Alexander University Erlangen-Nürnberg (FAU), Loewenichstrasse 28, D-91054 Erlangen, Germany. anna.lene.claussen@fau.de

Barbara Seuss. GeoZentrum Nordbayern, Friedrich-Alexander University Erlangen-Nürnberg (FAU), Loewenichstrasse 28, D-91054 Erlangen, Germany. barbara.seuss@fau.de

Patrick N. Wyse Jackson. Department of Geology, Trinity College, Dublin 2, Ireland. wysjcknp@tcd.ie

http://zoobank.org/ A4A07D50-3DDB-4E45-A255-1ECCF45F147A

Keywords: Finis Shale; cyclothem; North American Midcontinent; morphology; taxonomy; ecology

Submission: 1 July 2021. Acceptance: 29 April 2022.

Ernst A, Claussen A L, Seuss B, Wyse Jackson P N, felipe (2022). Stenolaemate bryozoans from the Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA. Plazi.org taxonomic treatments database. Checklist dataset https://doi.org/10.15468/baaezv accessed via GBIF.org on 2026-06-15.

CC0Published 5/31/2022View dataset
GBIF Usage Key
226325038
Dataset Key
77c06bea-bbd5-46af-8ef1-f434aa25c6a8
Origin
source
Backbone Key
10728915
Taxon ID
03C387F19A3D39592C16030DF1934866.taxon
Last Crawled
6/9/2026
Last Interpreted
6/9/2026