AnimaliaNot EvaluatedacceptedspeciesAccepted
Penniretepora flexistriata

Penniretepora flexistriata

Richards, 1959

GBIF:226325039

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Descriptions(3)

Figure 18 D-J; Appendix 1959 Penniretepora flexistriata Richards, p. 1116, text-figs. A 7, A 8. 1980 Penniretepora flexistriata Richards, 1959; Simonsen and Cuffey, p. 23 - 24, figs. 3 K, 4 K, 5 K, 6 K, 7 K.
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 flexistriata Richards, 1959, is similar to P. cyclotriangulata Shishova, 1959, from the Upper Carboniferous (Moscovian) of Russia but differs from it in having narrower lateral branches (lateral branch width 0.12 – 0.24 mm vs. 0.20 – 0.25 mm in P. cyclotriangulata) and smaller apertures (aperture width 0.06 – 0.08 mm vs. 0.15 – 0.20 mm in P. cyclotriangulata). Occurrence. Lower Virgilian to upper Wolfcampian; Kansas, 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 82, SNSB-BSPG 2020 XCI 83, SNSB-BSPG 2020 XCI 84, SNSB-BSPG 2020 XCI 85, SNSB-BSPG 2020 XCI 91, SNSB-BSPG 2020 XCI 93, SNSB-BSPG 2020 XCI 121, SNSB-BSPG 2020 XCI 122, SNSB-BSPG 2020 XCI 123. Exterior description. Pinnate colonies consisting of straight main branches with frequent lateral branches. Main branches 0.22 – 0.43 mm wide, lateral branches 0.12 – 0.24 mm wide, diverging at angles 59 – 82 ° from main branches, spaced 0.59 – 0.85 mm from centre to centre. Autozooecia having circular apertures with stellate structure, 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, undulating, nodes absent. Interior description. Autozooecial chambers arranged in two alternating rows on branches, triangular to pentagonal or trapezoid in mid-tangential section both on main and secondary branches, short, inflated, with moderately long vestibules. Axial wall strongly undulating to zigzag from base to crest. Hemisepta absent. Apertural pore present, positioned proximally to the autozooecial aperture, 0.02 – 0.03 mm in diameter. Extrazooecial skeleton moderately developed, traversed by abundant microstylets; microstylets without hyaline core, regularly spaced across entire colony surface, 0.005 – 0.008 mm in diameter. Coarse longitudinal striation developed both on main and lateral branches.
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 18. Septopora blanda Moore, 1929 (A–C): A, B – tangential section showing autozooecial apertures and chambers, and cyclozooecia (arrows) (XCI 47); C – tangential section showing autozooecial chambers and cyclozooecia (XCI 54). Penniretepora flexistriata Richards, 1959 (D–J): D–F – colony fragments with autozooecial apertures with apertural pores (arrows) and stellate structures, divided by low undulating keel (D: (XCI 121), E–F: (XCI 122); G – autozooecial aperture with apertural pore (arrow) and stellate structure (XCI 123); H, I – thin section showing autozooecial chambers (XCI 83); J – thin section showing autozooecial apertures with apertural pore (arrow) (XCI 82).

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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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
226325039
Dataset Key
77c06bea-bbd5-46af-8ef1-f434aa25c6a8
Origin
source
Backbone Key
4979836
Taxon ID
03C387F19A0339592E8003B7F7204B06.taxon
Last Crawled
6/9/2026
Last Interpreted
6/9/2026