Fistulipora prolifica Ulrich, 1884

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 : 158

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-F757-FFA8-A001-FE45E197F855

treatment provided by

Felipe

scientific name

Fistulipora prolifica Ulrich, 1884
status

 

Fistulipora prolifica Ulrich, 1884 View in CoL

( Figs 6 View FIG A-D; 7A, B; Appendix)

Fistulipora prolifica Ulrich, 1884: 45 View in CoL , 46, pl. 3, fig. 2, 2a. — Trizna 1958: 41, 42, pl. 3, figs 5, 6.

MATERIAL. — SMF 23.112- SMF 23.118 (thin sections); SMF 23.119 (free colony).

OCCURRENCE. — Carboniferous, Mississippian (Visean); USA (Kentucky). Carboniferous, lower Visean; Kuznets Basin, Russia. Carboniferous, Mississippian (upper Visean); Roque Redonde (Montagne Noire, southern France).

DESCRIPTION

Encrusting, multilayered colony. Separate sheets in multilayered colony 1.05-4.30 mm thick. Autozooecia growing from thin epitheca, bending at their bases towards the colony surface. Basal diaphragms common to abundant, often inclined, concentrated usually in proximal parts of autozooecia. Autozooecial apertures circular to oval. Lunaria weakly developed. Vesicles moderately large, separating autozooecia usually in a single row, locally in 2 rows, 6-10 surrounding each autozooecia aperture, with rounded to flat roofs, polygonal in tangential section. Autozooecial walls granular prismatic, 0.010 -0.015 mm thick. Maculae present, consisting of vesicular skeleton, 0.9-2.4 mm in diameter, slightly elevated.

COMPARISON

Fistulipora prolifica Ulrich, 1884 View in CoL differs from F. incrustans ( Phillips, 1836) View in CoL from the Mississippian of British Isles in larger autozooecial apertures (average aperture width 0.39 mm vs 0.32 mm in F. incrustans View in CoL ). Fistulipora prolifica View in CoL differs from F. parvilabrum Schulga-Nesterenko, 1955 View in CoL in larger and widely spaced autozooecial apertures (average autozooecial width 0.39 mm vs 0.29 mm in F. parvilabrum View in CoL ; average autozooecial spacing 0.74 mm vs 0.56 mm in F. parvilabrum View in CoL ).

Fistulipora cf. tubulosa Nikiforova, 1933 View in CoL ( Fig. 7 View FIG C-F; Appendix)

Fistulipora tubulosa Nikiforova, 1933: 6 View in CoL , pl. 1, figs 6, 7; 1948: 9, 10, pl. 1, figs 1, 2. — Nekhoroshev 1956: 9, 10, pl. 1, figs 1, 2. — Trizna 1958: 36, 37, pl. 1, figs 1-5.

MATERIAL. — SMF 23.120- SMF 23.130, TCD.60337.

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

DESCRIPTION

Encrusting colony, 1.5-2.3 mm thick. Autozooecia growing from thin epitheca, bending in the early exozone to the colony surface. Basal diaphragms absent or common, up to 5 in autozooecia, thin, concentrated usually in proximal parts of autozooecia. Autozooecial apertures circular to oval. Lunaria well-developed, triangular to horseshoe-shaped; ends of lunaria not indenting autozooecia.Vesicles moderately large, separating autozooecia in 1-2 rows, 7-14 surrounding each autozooecia aperture, with rounded roofs, polygonal in tangential section. Autozooecial walls granular prismatic, 0.010 -0.015 mm thick. Maculae present, consisting of vesicular skeleton.

COMPARISON

The present species is similar to Fistulipora tubulosa Nikiforova, 1933 from the Lower Carboniferous of Kazakhstan and Russia. The only difference is that the species from Montagne Noire was not found to produce a tubular colony like in previous records. However, tubular colonies are usually produced by encrusting of ephemeral substrates, which decay after death, and so such colonies are potentially encrusting also other kinds of substrate. Fistulipora tubulosa Nikiforova, 1933 described by Nikiforova (1948) (this work was finished by Nekhoroshev) has unusually small and abundant vesicles, 15-17 surrounding each autozooecial aperture (vs 7-14 in present material and 9-12 in the holotype). Fistulipora tubulosa is similar to F.djebaglinica Nikiforova, 1933 from the Mississippian of Turkestan, but differs from it in larger autozooecial apertures (aperture width 0.24-0.43 mm vs 0.25-0.28 mm in F. djebaglinica ).

Fistulipora parvilabrum Schulga-Nesterenko, 1955 ( Fig. 8 View FIG A-C; Appendix)

Fistulipora parvilabrum Schulga-Nesterenko, 1955: 61-64 View in CoL , pl. 2, figs 1, 2.

MATERIAL. — SMF 21.770- SMF 21.772, TCD.60333, 60338, 60345.

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

DESCRIPTION

Encrusting to submassive colony, 1.56-3.35 mm thick. Autozooecia growing from thin epitheca, bending in the early exozone to the colony surface. Basal diaphragms common, 4-6 in each autozooecium, concentrated usually in proximal parts of autozooecia. Autozooecial apertures circular to oval. Lunaria well-developed, horseshoe-shaped; ends of lunaria not indenting autozooecia. Vesicles moderately large, separating autozooecia in 1-2 rows, 7-11 surrounding each autozooecia aperture, with rounded roofs, polygonal in tangential section. Autozooecial walls granular prismatic, 0.005 -0.010 mm thick.

COMPARISON

Fistulipora parvilabrum Schulga-Nesterenko, 1955 View in CoL differs from F.incrustans ( Phillips, 1836) View in CoL in smaller autozooecial apertures (average aperture width 0.29 mm vs 0.32 mm in F.incrustans View in CoL ).

SMF

Forschungsinstitut und Natur-Museum Senckenberg

Kingdom

Animalia

Phylum

Bryozoa

Class

Stenolaemata

Order

Cystoporida

Family

Fistuliporidae

Genus

Fistulipora

Loc

Fistulipora prolifica Ulrich, 1884

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

Fistulipora tubulosa

TRIZNA V. B. 1958: 36
NEKHOROSHEV V. P. 1956: 9
NIKIFOROVA A. I. 1933: 6
1933
Loc

Fistulipora prolifica

TRIZNA V. B. 1958: 41
ULRICH E. O. 1884: 45
1884
Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF