Spinofenestella Termier & Termier, 1971

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 : 182

publication ID

https://doi.org/ 10.5252/g2015n2a2

publication LSID

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

persistent identifier

https://treatment.plazi.org/id/038D87E1-F74F-FF8C-A1D3-FD65E6D6FEC8

treatment provided by

Felipe

scientific name

Spinofenestella Termier & Termier, 1971
status

 

Genus Spinofenestella Termier & Termier, 1971 View in CoL

Alternifenestella Termier & Termier, 1971: 42 View in CoL .

TYPE SPECIES. — Fenestella spinosa Condra, 1902 by original designation. Lower Permian (Wolfcampian) ; North America .

DIAGNOSIS. — Reticulate colonies with relatively wide and thick branches and relatively thin dissepiments. Autozooecia arranged in two rows on the branches. Autozooecia triangular in mid tangential section, triangular to pentagonal proximal to bifurcations. Narrow keel with single row of nodes developed.

OCCURRENCE. — Lower Devonian – Upper Permian.

COMPARISON

Spinofenestella Termier &Termier, 1971 View in CoL differs from the genus Rectifenestella Morozova, 1974 View in CoL by the triangular shape of the autozooecia in mid tangential section.

Spinofenestella major ( Nikiforova, 1933) View in CoL comb. nov. ( Fig. 21 View FIG E-I; Appendix)

Fenestella major Nikiforova, 1933: 16 . — Schulga-Nesterenko 1951: 93, 94, pl. 17, fig. 3, pl. 18, fig. 2.

Fenestella donaica – Nikiforova 1927: 250, pl. 12, figs 8, 9.

Fenestella donaica var. major Nikiforova, 1933: 16 , pl. 16, figs 4, 5. — Nekhoroshev 1948: 28, pl. 2, fig. 3, pl. 10, fig. 5.

Alternifenestella major View in CoL – Gorjunova 2013: 576, 577, pl. 5, fig. 2.

MATERIAL. — SMF 21.899.

OCCURRENCE. — Carboniferous, Mississippian (upper Visean); Roque Redonde (Montagne Noire, southern France). Carboniferous, Mississippian; Ukraine, Donetz Basin. Carboniferous, Mississippian (Serpukhovian); Russian Platform. Middle Carboniferous; Kazakhstan.

EXTERIOR DESCRIPTION

Reticulate colony formed by straight branches joined by narrow dissepiments. Fenestrules oval to rectangular, about twice as long as wide. Autozooecia arranged in two rows on branches. Autozooecial apertures circular, with low smooth peristome; 3 to 5 apertures spaced per fenestrule length. Median keel low, narrow, containing small elliptical nodes. Nodes 0.03-0.05 mm in diameter, spaced 0.14-0.18 mm from centre to centre.

INTERIOR DESCRIPTION

Autozooecia short, triangular to trapezoid in mid tangential section; with short to moderately long vestibule in longitudinal section. Axial wall between autozooecial rows strongly zigzag; aperture positioned at distal end of chamber. Superior hemisepta present, long, curved proximally; inferior hemisepta absent. External laminated skeleton well-developed on both obverse and reverse sides. Heterozooecia not observed.

COMPARISON

Spinofenestella major ( Nikiforova, 1933) View in CoL comb. nov. differs from Spinofenestella donaica ( Lebedev, 1924) View in CoL in longer fenestrules (0.77-1.02 mm vs 0.55-0.65 mm in S. donaica View in CoL ). Spinofenestella major View in CoL comb. nov. differs from S. donaiciformis (Schulga-Nesterenko, 1951) in smaller and more closely spaced nodes on the median keel (distance between node centres 0.14-0.18 mm vs 0.30-0.42 mm in S. donaiciformis ).

Spinofenestella cf. simplaris ( Trizna, 1961) View in CoL ( Figs 22H View FIG ; 23 View FIG A-C; Appendix)

Fenestella simplaris Trizna, 1961: 75 , 76, pl. 8, figs 3, 4, text-fig. 27.

MATERIAL. — SMF 21.906- SMF 21.910.

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

EXTERIOR DESCRIPTION

Reticulate colony formed by straight branches joined by wide dissepiments. Fenestrules oval to rectangular, long, narrow. Autozooecia arranged in two rows on branches. Autozooecial apertures circular, with low smooth peristome; 3 to 4 apertures spaced per fenestrule length. Large elliptical nodes on the low keel, widely and irregularly spaced.

INTERIOR DESCRIPTION

Autozooecia short, triangular to trapezoid in mid tangential section; with short to moderately long vestibule in longitudinal section. Axial wall between autozooecial rows strongly zigzag; aperture positioned at distal end of chamber. Superior hemisepta weakly developed; inferior hemisepta absent. External laminated skeleton well-developed on both obverse and reverse sides. Heterozooecia not observed.

COMPARISON

The present material is similar to Spinofenestella simplaris ( Trizna, 1961) from the Mississippian of Urals. However, the present material has significantly longer fenestrules (0.83-1.02 mm vs 0.55-0.75 mm in S. simplaris ). The present material differs from Spinofenestella plebeia ( M’Coy, 1844) from the Lower Carboniferous of Ireland, in wider branches (average branch width 0.38 mm vs 0.29 mm in S. plebeia ), and wider dissepiments (average dissepiment width 0.23 mm vs 0.17 mm in S. plebeia ). It differs from S. triangularis ( Nekhoroshev, 1953) from the Mississippian of Kazakhstan in wider branches (branch width 0.35-0.42 mm vs 0.15-0.20 mm in S. triangularis ).

SMF

Forschungsinstitut und Natur-Museum Senckenberg

Kingdom

Animalia

Phylum

Bryozoa

Class

Stenolaemata

Order

Fenestrida

Family

Fenestellidae

Loc

Spinofenestella Termier & Termier, 1971

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

Alternifenestella major

GORJUNOVA R. V. 2013: 576
2013
Loc

Alternifenestella

TERMIER H. & TERMIER G. 1971: 42
1971
Loc

Fenestella simplaris

TRIZNA V. B. 1961: 75
1961
Loc

Fenestella major

NIKIFOROVA A. I. 1933: 16
1933
Loc

Fenestella donaica var. major

NEKHOROSHEV V. P. 1948: 28
NIKIFOROVA A. I. 1933: 16
1933
Loc

Fenestella donaica

NIKIFOROVA A. I. 1927: 250
1927
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