Reteporidra NICKLES & BASSLER, 1900

Ernst, Andrej, Tolokonnikova, Zoya & Yarahmadzahi, Hamed, 2012, Upper Devonian (Frasnian) Bryozoa from the Shishtu 1 Formation of Niaz area (eastern Tabas, central Iran), Revue de Paléobiologie 31 (1), pp. 1-14 : 6

publication ID

0253-6730

DOI

https://doi.org/10.5281/zenodo.6448224

persistent identifier

https://treatment.plazi.org/id/59452E7C-FFAC-FF99-FF75-FAF563EED25B

treatment provided by

Carolina

scientific name

Reteporidra NICKLES & BASSLER, 1900
status

 

[= Reteporidra NICKLES & BASSLER, 1900 View in CoL ]

Type species: Fenestella cinctuta HALL, 1884 . Middle Devonian (Erian); Canada and USA.

Diagnosis: Fan-shaped colonies, some with heavy extrazooidal calcification covering proximal portion of colony; branches broad, strongly sinuous, bifurcating, branch spacing and anastomoses at intermediate distance; keels and superstructure absent; autozooecia arranged in 2-8 rows on branches, large-end intermediate-sized, elongate perpendicular to curved obverse surface, chambers nearly circular oval in tangential section deep in endozone, elongate oval in shallower endozone; transverse wall at high angle to reverse wall; hemisepta and diaphragms absent; elevated peristome present in well preserved specimens. Tubes connecting the endozonal zooecial chambers with the obverse surface present, few or abundant, varying in size. Autozooecial walls of thick granular material may be lined by laminar skeleton in both the distal tube and the inflated chamber; reverse wall flat or minimally curved transversely, longitudinal ridges on reverse side minimally developed; extrazooidal skeleton finely laminated, traversed by closely spaced small microstyles, a gently sloped median keel commonly present on reverse surface, locally forming cystose structures bridging fenestrules where broad expanse of extrazooidal skeleton is deposited as continuous sheet over multiple branches.

Remarks: Anastomopora SIMPSON, 1897 differs from the similar genus Reteporina D’ ORBIGNY, 1849 in having more than 2 rows of autozooecia on branches. Both genera possess exozonal tubes, which number and size are variable in different species.

Stratigraphic and geographic range: Lower-Late Devonian; North America, Europe, Asia (Carboniferous and Permian species referred to the genus Reteporidra , do not belong to the Anastomopora ).

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