Rhabdomeson Young & Young, 1874

Ernst, Andrej, Wyse Jackson, Patrick N. & Aretz, Markus, 2015, Bryozoan fauna from the Mississippian (Visean) of Roque Redonde (Montagne Noire, southern France), Geodiversitas 37 (2), pp. 151-213 : 176-178

publication ID

https://doi.org/ 10.5252/g2015n2a2

publication LSID

urn:lsid:zoobank.org:pub:BA9B2FF0-9D3B-44AF-894F-419DE5AE4C13

DOI

https://doi.org/10.5281/zenodo.10526191

persistent identifier

https://treatment.plazi.org/id/038D87E1-F749-FFB4-A291-FA20E69BFA74

treatment provided by

Felipe

scientific name

Rhabdomeson Young & Young, 1874
status

 

Genus Rhabdomeson Young & Young, 1874 View in CoL

Coeloconus Ulrich, 1889: 298 .

TYPE SPECIES. — Rhabdomeson progracile Wyse Jackson & Bancroft, 1995 by subsequent designation of Wyse Jackson & Bancroft (1995) ( ICZN Opinion 1854; ICZN 1996). Lower Carboniferous, Mississippian (Visean-Serpukhovian); Britain and Ireland.

DIAGNOSIS. — Rhabdomesid with delicate dendroid colony with irregularly dichotomizing branches. Autozooecia regularly budding around central axial cylinder in an annual or spiral manner. Hemisepta common. Autozooecial apertures elliptical, pyriform or rhombic, closely spaced, arranged in quincunx on colony surface; of constant or variable dimensions around branch. Stylets abundant and structurally diverse (after Wyse Jackson and Bancroft, 1995).

OCCURRENCE. — Middle Devonian to Upper Permian; worldwide.

COMPARISON

Rhabdomeson Young & Young, 1874 View in CoL differs from other rhabdomesines in the presence of a central axial cylinder, from Silenella Gorjunova, 1992 View in CoL in absence of aktinotostyles, from Pseudorhabdomeson Gorjunova, 2002 View in CoL in having a rounded axial tube instead of a polygonal one and in the presence of differentiated styles instead of aktinotostyles.

Rhabdomeson progracile Wyse Jackson & Bancroft, 1995 View in CoL ( Fig. 19 View FIG A-F; Appendix)

For synonymy see Wyse Jackson & Bancroft (1995: 30, 31).

MATERIAL. — SMF 21.872- SMF 21.883.

OCCURRENCE. — Carboniferous, Mississippian (Visean-Serpukhovian); Britain, Ireland. Carboniferous, Mississippian (upper Visean); Roque Redonde (Montagne Noire, southern France).

DESCRIPTION

Branched colonies with narrow axial cylinder. Branches 0.60- 1.63 mm in diameter. Axial cylinder circular to polygonal, 0.1- 0.2 mm in diameter. Autozooecia budding in a spiral pattern diverging at angles of 27-40° from the axial cylinder, arranged 10-14 in the first row around the axial cylinder, hexagonal to rhomboid in transverse in the endozone. Autozooecial apertures oval, arranged in regular diagonal rows. Macroacanthostyles large, long, 4 arranged around each aperture building a regular hexagonal pattern. Microacanthostyles small, 1-2 arranged between macroacanthostyles. Paurostyles scattered on the colony surface. Superior hemisepta small, blunt, positioned at distal end of the autozooecia, visible only in occasional sections; inferior hemisepta absent. Diaphragms absent.

COMPARISON

Rhabdomeson progracile Wyse Jackson & Bancroft, 1995 View in CoL is similar to R. regularis Nekhoroshev, 1932 View in CoL , and R. spinosum Morozova, 1955 View in CoL , in terms of size, and in the positioning of a solitary prominent acanthostyle situated proximally of autozooecial apertures. R. progracile View in CoL differs from R. regularis View in CoL in having larger hemisepta and wider autozooecial apertures, and from R. spinosum View in CoL in acanthostyles that are smaller and a wider exozone ( Wyse Jackson & Bancroft 1995: 34).

SMF

Forschungsinstitut und Natur-Museum Senckenberg

Kingdom

Animalia

Phylum

Bryozoa

Class

Stenolaemata

Order

Cryptostomida

Family

Rhabdomesidae

Loc

Rhabdomeson Young & Young, 1874

Ernst, Andrej, Wyse Jackson, Patrick N. & Aretz, Markus 2015
2015
Loc

Coeloconus

ULRICH E. O. 1889: 298
1889
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