Rhamphostomella cellata ( O’Donoghue & O’Donoghue, 1923 )

Grischenko, Andrei V., Gordon, Dennis P., Taylor, Paul D., Kuklinski, Piotr, Denisenko, Nina V., Spencer-Jones, Mary E. & Ostrovsky, Andrew N., 2022, Taxonomy, ecology and zoogeography of the Recent species of Rhamphostomella Lorenz, 1886 and Mixtoscutella n. gen. (Bryozoa, Cheilostomata), Zootaxa 5131 (1), pp. 1-115 : 46-49

publication ID

https://doi.org/ 10.11646/zootaxa.5131.1.1

publication LSID

lsid:zoobank.org:pub:CF550031-D6A9-48A3-A953-A1BD40C72F5E

DOI

https://doi.org/10.5281/zenodo.6520693

persistent identifier

https://treatment.plazi.org/id/03892374-0B1A-330D-FF73-AA771C22FE41

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Plazi

scientific name

Rhamphostomella cellata ( O’Donoghue & O’Donoghue, 1923 )
status

 

Rhamphostomella cellata ( O’Donoghue & O’Donoghue, 1923) View in CoL

( Fig. 13 View FIGURE 13 )

Smittina cellata O’Donoghue & O’Donoghue, 1923, p. 43 , pl. 4, fig. 31.

Smittina cellata: O’Donoghue & O’Donoghue 1926, p. 68 .

Rhamphostomella cellata: Osburn 1952, p. 431 View in CoL , pl. 52, fig. 9.

Not Rhamphostomella cellata: Hansen 1962, p. 39 View in CoL .

Smittina torquata O’Donoghue & O’Donoghue, 1923, p. 43 , pl. 4, fig. 32.

Smittina torquata: O’Donoghue & O’Donoghue 1926, p. 68 .

Material examined. Lectotype: NHMUK 1964.1 View Materials .2.9, single colony detached from bivalve mollusc shell, fractured into nine fragments (mounted on seven SEM stubs), C.H. O’Donoghue Collection, Pacific coast of North America (presumably Vancouver Island , British Columbia).

Measurements. NHMUK 1964.1.2.9, Pacific coast of North America ( Fig. 13A–L View FIGURE 13 ). ZL, 0.65–1.23 (0.89 ± 0.14). ZW, 0.32–0.55 (0.44 ± 0.06). ZD, 0.30–0.33 (n = 2). OrL, 0.15–0.25 (0.21 ± 0.02). OrW, 0.20–0.28 (0.23 ± 0.02). OeL, 0.25–0.33 (0.29 ± 0.02) (n = 22). OeW, 0.35–0.43 (0.38 ± 0.02) (n = 22). Av(s)L, 0.07–0.16 (0.11 ± 0.02). P(m)N, 17–27 (22).

Description. Colonies encrusting, multiserial, unilaminar ( Fig. 13A View FIGURE 13 ), more or less circular, attaining 22 mm in maximal dimension, light brown when dry. Zooids large, oblong-hexagonal to oval, or pyriform ( Fig. 13A, D, F, G View FIGURE 13 ), arranged in checkered pattern, demarcated by fine sutures between lateral and transverse zooidal walls; sutures visible in both young and old parts of colony.

Frontal shield umbonuloid ( Fig. 13A, D, G, I View FIGURE 13 ), thin, inflated to slightly convex, smooth to dimpled, with reticulate appearance in young zooids( Fig.13A,B,D View FIGURE 13 )and smoothly tuberculate in older zooids( Fig.13E–G View FIGURE 13 );with numerous deep circulartoovalareolaealongmargins,separatedbyshort,narrowinterareolarridges.Umbonuloidcomponentoccupying about40%oflengthoffrontalshield,withparallellineationandaccretionarybanding( Fig.13I,K View FIGURE 13 ).Ringscardiscrete( Fig. 13I,K View FIGURE 13 ),formingregularboundarybetweenumbonuloidexteriorwallandextra-umbonuloidinteriorwallmicrostructure.

Primary orifice ( Fig. 13B, C, E View FIGURE 13 ) broadly circular to transversely oval; distal and lateral margins formed by upper terminal part of distal transverse wall incidentally bearing ill-defined rim ( Fig. 13C View FIGURE 13 ). Distal margin of orifice rounded, proximal margin concave with median bifid lyrula having acute tips directed distolaterally, and distinct triangular process on each side with acute or round tip, occasionally strongly reduced. Condyles and oral spines absent.

Secondary orifice irregularly circular to oval, cormidial ( Fig. 13C–H View FIGURE 13 ), distally and distolaterally restricted by elevated vertical walls of distal and lateral zooids; proximally formed by slightly elevated peristomial outgrowth of frontal shield, incorporating asymmetrically positioned cystid of suboral avicularium. In ovicellate zooids, lateral peristomial lappets connected to proximolateral corners of ooecium ( Fig. 13F–H View FIGURE 13 ), conferring circular or sometimes irregularly triangular (because of avicularium) outline to secondary orifice.

Cystid of suboral avicularium small, low, asymmetrically situated proximolateral to zooidal orifice on left or right side, with dimpled surface and one small communication pore. Frontal surface (rostral/postmandibular areas) of avicularium concave, to one side of zooidal midline, facing obliquely frontally. Rostrum lodged within rim of peristome, slightly curving inward to conform to it, directed obliquely distolaterally and frontally ( Fig. 13C, D, E, H View FIGURE 13 ). Palatal foramen lingulate to semioval and roundly triangular, conforming to shape of rostrum, opesia semioval to lingulate. Crossbar complete.

No adventitious avicularia.

Although all ooecia were broken in material studied, ovicells are clearly hyperstomial, with ooecia free of secondary calcification ( Fig. 13F–H View FIGURE 13 ). Ooecium formed by distal autozooid, its coelomic cavity connected with visceral coelom via communication canal that opens on underside of proximal part of frontal shield of distal zooid as chevron-shaped communication slit about midway between transverse wall and ring scar ( Fig. 13I View FIGURE 13 ). Remnants of ectooecium bear circular pseudopores in one specimen ( Fig. 13F View FIGURE 13 ). Proximal margin of ooecium very weakly concave.

Zooids interconnected by three mural pore chambers in each distolateral wall ( Fig. 13L View FIGURE 13 ) and two multiporous septula in basal half of transverse walls. In some zooids, transverse walls with two shallow recesses separated by medial buttress.

Basal walls of zooids entirely calcified ( Fig. 13J View FIGURE 13 ), smooth, flat, without white spots or protuberances. Boundaries between zooids indicated basally by fine sutures.

Ancestrula and early astogeny not observed.

Remarks. The fragments examined have zooids with partially to fully damaged ovicells. One zooid shows the incomplete roof of an ovicell with two circular pseudopores and the remnants of a third laterally. In their original description, O’Donoghue & O’Donoghue (1923, p. 43) described the surface of ovicells as being “perforated by a series of large irregular pores” (their fig. 31 shows 10–12 oval to irregular pseudopores).

O’Donoghue & O’Donoghue (1923) described Smittina cellata and S. torquata from Vancouver Island. Osburn (1952, p. 431) synonymized these species, treating the former as the senior synonym of the latter and placing it in Rhamphostomella .

The surface of the frontal shield of R. cellata is dimpled, conferring a reticulate appearance similar to that in R. curvirostrata and R. townsendi . The former species clearly differs from the latter two in having the suboral avicularium located within the rim of peristome, slightly curving inwards to conform to it. While the suboral avicularium in the latter two species is connected with the peristome, both the rostrum and frontal surface differ from R. cellata in position, shape and orientation.

The Canadian Museum of Nature contains some material identified by O’Donoghue from British Columbia (24 items), including a dried specimen of R. cellata (Cat. No. – CMNI 1988-0135, Northumberland Channel). Unfortunately, there are no images, and the specimen is not mentioned as a type in the On-line Collection Data of the Museum. Accordingly, we selected a lectotype from C.H. O’Donoghue Collection deposited in the Natural History Museum, London. Although a precise locality was not written on the label, these specimens likely came from the waters around Vancouver Island, British Columbia.

Ecology. Rhamphostomella cellata is known only from the depth range 1.8–9.1 m. Colonies encrust mollusc shells.

Distribution. This little-known species was first described from Northumberland Channel and Gabriola Passage (about 49°52.0ʹ N, 123°72.0ʹ W), Vancouver Island, British Columbia ( O’Donoghue & O’Donoghue 1923). O’Donoghue & O’Donoghue (1926) recorded it from numerous localities in British Columbia (Namu, Port Simpson, off Round Island, Houston Channel, Brotchie Ledge, Victoria, off Point Caution, off Breakwater Island, Cowichan Gap) and near the San Juan Islands in Puget Sound. The specimens examined by Osburn were collected from Middle Bank, Puget Sound ( Osburn 1952). Records of the species from Baffin Bay and Davis Strait ( Hansen 1962) are doubtful. From these distributional data, R. cellata is an Eastern Pacific boreal, sublittoral species.

Kingdom

Animalia

Phylum

Bryozoa

Class

Gymnolaemata

Order

Cheilostomatida

Family

Umbonulidae

Genus

Rhamphostomella

Loc

Rhamphostomella cellata ( O’Donoghue & O’Donoghue, 1923 )

Grischenko, Andrei V., Gordon, Dennis P., Taylor, Paul D., Kuklinski, Piotr, Denisenko, Nina V., Spencer-Jones, Mary E. & Ostrovsky, Andrew N. 2022
2022
Loc

Rhamphostomella cellata:

Hansen, B. K. 1962: 39
1962
Loc

Rhamphostomella cellata:

Osburn, R. C. 1952: 431
1952
Loc

Smittina cellata: O’Donoghue & O’Donoghue 1926 , p. 68

O'Donoghue, C. H. & O'Donoghue, E. 1926: 68
1926
Loc

Smittina torquata: O’Donoghue & O’Donoghue 1926 , p. 68

O'Donoghue, C. H. & O'Donoghue, E. 1926: 68
1926
Loc

Smittina cellata O’Donoghue & O’Donoghue, 1923 , p. 43

O'Donoghue, C. H. & O'Donoghue, E. 1923: 43
1923
Loc

Smittina torquata O’Donoghue & O’Donoghue, 1923 , p. 43

O'Donoghue, C. H. & O'Donoghue, E. 1923: 43
1923
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