Goniocladia grahamensis Moore, 1929

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), pp. 1-56 : 11

publication ID

https://doi.org/ 10.26879/1174

publication LSID

lsid:zoobank.org:pub:A4A07D50-3DDB-4E45-A255-1ECCF45F147A

DOI

https://doi.org/10.5281/zenodo.11032506

persistent identifier

https://treatment.plazi.org/id/03C387F1-9A16-3972-2C03-0258F0184F44

treatment provided by

Felipe

scientific name

Goniocladia grahamensis Moore, 1929
status

 

Goniocladia grahamensis Moore, 1929 View in CoL

Figure 6 View FIGURE 6 C-E; Appendix

1929 Goniocladia grahamensis Moore , p.

154-156, pl. 18, figs. 1-3, 8-11.

Material. SNSB-BSPG 2020 XCI 100.

Description. Reticulate colonies consisting of anastomosing bifoliate branches. Branches 0.54– 0.70 mm wide. Fenestrules oval to polygonal, 1.00– 1.36 mm wide and 2.32–2.66 mm long. Autozooecia budding in 2–3 rows from each side of thin mesotheca, opening on both sides of the sharp median carina. Lunaria present, horseshoe-shaped, directed toward fenestrule. Numerous microstylets on the colony surface, 0.008 –0.011 mm in diameter.

Remarks. Goniocladia grahamensis Moore, 1929 , differs from G. subpulchra Schulga-Nesterenko, 1955 , from the Gzhelian of the Russian Platform, and from G. tenuis Schulga-Nesterenko, 1933 , from the Gzhelian of Russia, in having smaller fenestrules (fenestrule width 1.00– 1.36 mm vs. 1.25–2.00 in G. subpulchra and 1.75–2.00 mm in G. tenuis ; fenestrule length 2.32–2.66 mm vs. 3.25–4.25 mm in G. subpulchra and 3.15–4.70 mm in G. tenuis ).

Occurrence. Upper Graham Formation, Pennsylvanian (Virgilian); Texas, USA. Graham Formation, Pennsylvanian (Virgilian); TXV-200 (“Spillway section at Lost Creek Lake”), Texas, USA.

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