Monticulipora d’Orbigny, 1850

Ernst, Andrej & Carrera, Marcelo G., 2022, A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera, Geodiversitas 44 (20), pp. 563-601 : 570

publication ID

https://doi.org/ 10.5252/geodiversitas2022v44a20

publication LSID

urn:lsid:zoobank.org:pub:5EC74771-0B7B-494D-ADC8-79BECD097A3A

DOI

https://doi.org/10.5281/zenodo.6723053

persistent identifier

https://treatment.plazi.org/id/865C87FD-FFAB-FFE9-3995-FC424BE4F99E

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scientific name

Monticulipora d’Orbigny, 1850
status

 

Genus Monticulipora d’Orbigny, 1850 View in CoL

TYPE SPECIES. — Monticulipora mammulata d’Orbigny, 1850 View in CoL by original designation. Upper Ordovician (Cincinnatian); North America .

DIAGNOSIS. — Colonies encrusting, hemispherical, massive, frondose or ramose. Autozooecial apertures polygonal. Cystiphragms and planar diaphragms generally occur throughout the zooecia. Acanthostyles are commonly short, generally limited to thick-walled zones and are the best developed in monticules or can be rare or absent. Intermonticular mesozooecia are common to lacking, polygonal in cross section and contain planar, closely spaced diaphragms. Autozooecial walls laminated throughout the colonies. Monticules are marked by thickened zooecial and mesozooecia walls and increased concentrations of enlarged acanthostyles, often with a central cluster of mesozooecia surrounded by enlarged zooecia.

OCCURRENCE. — Middle Ordovician to Lower Silurian, worldwide.

COMPARISON

Monticulipora d’Orbigny, 1850 differs from Prasopora Nicholson & Etheridge, 1877 by having less abundant mesozooecia, polygonal autozooecial apertures, serrated instead of amalgamated wall structure, and usually less abundant cystiphragms.

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF