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Cystodictya formosa

Cystodictya formosa

Moore, 1929

GBIF:226325009

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Descriptions(4)

Description. Bifoliate branches, 0.67 – 1.07 mm wide and 0.40 – 0.92 mm thick. Mesotheca 0.008 – 0.010 mm thick, granular. Autozooecia tubular, teardrop-shaped at their bases, trapezoidal to semicircular in transverse quadrate in cross-section, recumbent on the mesotheca for a relatively short distance, then bending upwards at low angles in exozone and intersecting the surface almost perpendicularly. Diaphragms lacking; long proximolateral hemisepta at zooecial bend present. Autozooecial apertures circular to oval, arranged in 4 – 6 alternating rows on the colony surface. Lunaria distinct, horseshoe-shaped. Vesicular skeleton well-developed, covered in exozone by thick stereom. Vesicles small, rectangular in tangential section, with rounded roofs, completely separating autozooecia in exozone in 1 – 2 rows. Autozooecial walls granular, 0.008 – 0.010 mm thick in endozone. Stereom well developed, 0.13 – 0.18 mm thick, consisting of laminated material, completely separating autozooecia in exozone.
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
Figures 5 C-G, 6 A-B; Appendix 1929 Cystodictya formosa Moore, p. 150 - 151, pl. 18, figs. 4, 12, 13. 1929 Cystodictya formosa var. robusta Moore, p. 151, pl. 18, figs. 14, 29, 31. 1929 Cystodictya formosa var. striata Moore, p. 153, pl. 18, figs. 20 - 22.
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. Moore (1929) established several varieties of the species Cystodictya formosa from the Graham Formation of Texas. Of these varieties, Cystodictya formosa var. robusta and C. formosa var. striata differ only in the branch width and thickness from the species C. formosa Moore, 1929. The differences in the branch width and thickness are indeed minimal and do not exceed normal variation within an assemblage from a restricted biotope (branch width 0.96 mm for C. formosa, 1.15 mm for C. formosa var. robusta, and 1.1 mm for C. formosa var. striata; branch thickness 0.72 mm for C. formosa, 1.3 mm for C. formosa var. robusta, and 0.72 mm for C. formosa var. striata, as given by Moore (1929). Cystodictya formosa Moore, 1929, differs from C. modesta Moore, 1929, in possessing thicker and wider branches as well as in larger and wider spaced autozooecial apertures (aperture width 0.10 – 0.18 mm vs. 0.057 – 0.085 mm in C. modesta). Occurrence. 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 23 a, b, SNSB-BSPG 2020 XCI 27, SNSB-BSPG 2020 XCI 28, SNSB-BSPG 2020 XCI 33, SNSB-BSPG 2020 XCI 99.
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 5. Eridopora beilensis Perkins and Perry in Perkins et al., 1962 (A–B): A – tangential thin section showing autozooecial apertures and vesicles (XCI 36); B – longitudinal thin section of a colony on echinoderm fragment showing autozooecial chambers and vesicles (XCI 59a). Cystodictya formosa Moore, 1929 (C–G): C, D – branch fragment with autozooecial apertures and lunaria (XCI 99); E–F: tangential thin section showing autozooecial apertures with lunaria (XCI 23a); G – deep tangential section showing autozooecial chambers with hemisepta and vesicular skeleton (XCI 23a).

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
226325009
Dataset Key
77c06bea-bbd5-46af-8ef1-f434aa25c6a8
Origin
source
Backbone Key
8785613
Taxon ID
03C387F19A1439722C210178F7904E84.taxon
Last Crawled
6/9/2026
Last Interpreted
6/9/2026