Tectulipora tuberculata, Ernst & Fernández & Fernández-Martínez & Vera, 2013

Ernst, Andrej, Fernández, Luis Pedro, Fernández-Martínez, Esperanza & Vera, Carmen, 2013, ERRATUM volume 34 (4), 2012: 693 - 738. Date of publication: December 28, 2012. Description of a bryozoan fauna from mud mounds of the Lebanza Formation (Lower Devonian) in the Arauz area (Pisuerga-Carrión Province, Cantabrian Zone, NW Spain), Geodiversitas 35 (1), pp. 273-276 : 274-276

publication ID

https://doi.org/ 10.5252/g2013n1a9

persistent identifier

https://treatment.plazi.org/id/9666614E-FF9F-7340-7CBD-6E95FB4808E9

treatment provided by

Marcus

scientific name

Tectulipora tuberculata
status

sp. nov.

Tectulipora tuberculata n. sp.

(Figs 19G, H; 20A-H; Appendix)

ETYMOLOGY. — The species name refers to the presence of abundant large nodes, present both on the branches and superstructure.

HOLOTYPE. — SMF 21.361 View Materials .

PARATYPES. — SMF 21.362- SMF 21.380.

TYPE LOCALITY. — Arauz Sur (Arroyo section), Province of Palencia, NW-Spain (Cantabrian Mountains).

TYPE HORIZON. — Lebanza Formation, Lower Devonian (Pragian).

DIAGNOSIS. — Reticulate colonies, conical, frontal surface exterior; autozooecia arranged in two weakly alternating rows on branches, 4-7 spaced per length of a fenestrule; autozooecial chambers rectangular in mid tangential section, short and relatively high, with moderately short vestibules; axial wall straight; hemisepta absent; terminal diaphragms planar; fenestrules oval to rectangular; superstructure produced by straight high club-shaped median keel, corresponding with underlying branches, outer lamellar skeleton well developed, traversed by small microstyles; large, irregularly sized nodes on reverse colony surface and on the protective superstructure; heterozooecia not observed.

DESCRIPTION

Reticulate colonies, conical, frontal surface exterior. Branches intermediate in width, straight, intermediately spaced, dichotomously divided, joined by straight wide dissepiments. Autozooecia arranged in two weakly alternating rows on branches, having circular apertures with low peristomes, 4-7 spaced per length of a fenestrule. Fenestrules oval to rectangular, varying in size. Straight high clubshaped median keel on obverse side of branches, composed of core of granular skeleton and sheath of laminar skeleton; superstructure corresponding with underlying branches, consisting of laterally expanded laths borne on continuous skeletal sheets from branches and dissepiments.

Internal granular skeleton continuous with obverse keel, nodes, peristome and across dissepiments, 0.015 -0.055 mm thick on the branch reverse wall. Outer lamellar skeleton well developed, 0.055 - 0.170 mm thick on the branch reverse wall, traversed by small microstyles. Reverse colony surface containing large, irregularly sized nodes, 0.03- 0.09 mm in diameter. Similar nodes occurring on the protective superstructure, 0.03-0.05 mm in diameter. Heterozooecia not observed.

Interior description Autozooecial chambers rectangular in mid tangential section, short and relatively high, with moderately short vestibules. Axial wall between autozooecial rows straight in tangential sections, continuing unbroken in superstructure. Hemisepta absent. Terminal diaphragms planar.

COMPARISON Tectulipora tuberculata n. sp. is similar to T. pannosa (Počta, 1894) from the Lower Devonian (Pragian) of Czech Republic and to T. conjunctiva (Hall, 1881) from the Lower Devonian of Canada in general morphology and dimensions of the meshwork, but differs from them in having large nodes on the reverse colony surface. Tectulipora tuberculata n. sp. is also similar to Isotrypa (Tectulipora) sibirica Krasnopeeva subsp. communis Waschurova, 1964 (Waschurova 1964: 100, pl. 21, fig. 3) in general morphology and in the presence of nodes on the reverse colony surface and on the superstructure. However, the latter species has narrower branches (branch width 0.31 vs 0.28-0.49 mm in present material), and smaller fenestrules (fenestrule width 0.23 vs 0.20-0.42 mm and fenestrule length 0.31- 0.54 vs 0.69-1.05 mm in present material).

Published on 29 March 2013.

SMF

Forschungsinstitut und Natur-Museum Senckenberg

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