AnimaliaNot EvaluatedacceptedspeciesAccepted

Rallocytus ridiculus

Rallocytus ridiculus

Grischenko, Gordon & Melnik, 2018

GBIF:9945174

0year

PROFILE

Species Profile

Habitat

Marine

Characteristics

Extant

ABOUT

Descriptions(5)

Description. Colony erect, pedunculate, with autozooidal peristomes radiating outwards around periphery of capitulum; maximum of nine autozooidal peristomes and one dimorphic peristome (Fig. 42 A – D), or seven autozooidal peristomes and two dimorphic peristomes (Fig. 43 A – C), in single uneven whorl. Column relatively short, flaring proximally to skirt-like base (Fig. 43 C), distally to wider capitulum. Entire colony surface strongly malleate, each dimple surrounded by distinct angular ridge (Figs 42 F, H, 43 D – H, 54 A); pores simple, sparse, more evident in CT scans (Fig. 54 B). Surface ultrastructure generally of imbricated platy crystallites (Fig. 43 I), in places irregularly arranged and lacking preferred growth direction. Capitulum broadly and shallowly calyciform, calyx center with few to several shallow alveoli and other smaller such openings at surface (Figs 42 A, B, 43 A); CT scans indicate these appear as flattened chambers in optical section (Fig. 54 C). Autozooidal peristomes in single subregular series, skeletal surface like that of column, with very sparse pores. Peristomial apertures mostly slightly irregular (Figs 42 A – D, 43 A – G). Inner surface of peristome tubes typically weakly corrugated, smooth to lightly textured, no pustules or spinules (Figs 42 G, 43 K). Dimorphic peristomes 1 – 2 in calyx whorl, evident from their smaller apertures, chamber size as in ordinary zooids; dimorphism sometimes pertaining to ancestrular peristome (Fig. 54 A, B). Capacious gonozooid (s) not seen. Dimorphic apertures inferred to be female, facing frontalwards (Fig. 42 A, B, D – G) or inclined towards calyx center (Fig. 43 A – G; one of the two such apertures). Dimorphic zooids seen as early as four-zooid stage colony (Fig. 44 E – L) or lacking in young colony (Fig. 44 M – P). Ancestrula not seen in isolation, but obviously erect judging from smallest (three-zooid) colony stage seen (Fig. 44 A – D), which lacks expanded base; CT scans confirm that ancestrular peristome originates from center of dome-like protoecium (Fig. 54, right image). First daughter zooid budded from ancestrular peristome soon after development to achieve two-zooid colony; third zooid develops between these (Fig. 44 A). Medium-sized colonies with central space (Fig. 44 E) filling with alveoli as capitulum expands radially (Fig. 44 E, 54 C). Measurements (mm). Holotype, ZIRAS 1 / 50723 (Fig. 42): Colony height 1.24; capitulum 1.23 × 0.88; ZL 0.440 – 0.598 (0.524 ± 0.051) (n = 9); PeL 0.085 – 0.242 (0.167 ± 0.054) (n = 9); PeD 0.163 – 0.202 (0.185 ± 0.013) (n = 9); ApL 0.118 – 0.151 (0.136 ± 0.012) (n = 9); ApW 0.113 – 0.142 (0.126 ± 0.009) (n = 9). Dimorphic zooid (n = 1): ZL 0.553; PeL 0.218; PeD 0.213; OpL 0.083; OpW 0.092.

Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

Remarks. Rallocytus ridiculus n. sp. is striking for its malleated surface texture (seen also in Calyssopora vasiformis n. sp.) and the dimorphic zooids within the calyx whorl. There are significant implications attached to a potential female reproductive function for the dimorphic zooids. First, a CT scan of one mature colony in which a dimorphic peristome appears in the calyx whorl shows this zooid to be the ancestrula (Fig. 54 A – C). Can this mean that the dimorphic peristomes seen in several juvenile colonies (e. g. Fig. 44 E – H, I – L) also pertain to the ancestrula? We cannot be sure; another mature colony had two dimorphic peristomes (Fig. 43 A – E), and either one, or neither, was ancestrular. But, if so, then it would seem to pose an energetic problem for early colony development, unless the dimorphic ancestrular zooid also has a feeding polypide, as seems likely. Alternatively (or additionally), the timing of budding of the first daughter zooid (from the ancestrular peristome, not the protoecium) may be such as to ensure that at least one feeding zooid is contemporaneous with a non-feeding ancestrula. A zooid pair in Fig. 44 A indicates simultaneity of development of the first two zooids (apparent autozooids, in this case). Second, if a dimorphic peristome occurs in a juvenile colony (as in Fig. 44 E – H, I – L), how is this peristome maintained as the zooid grows upwards? Or is the modified peristomial aperture shed and regrown during polypide recycling? Such a thing has never been reported. The fact that at least one cyclostome species in this fauna has multiple brown bodies (i. e. in Pandanipora helix; Fig. 5 E) shows that polypide recycling can happen in this stable environment, so perhaps peristomial shape might be labile. Indeed, conventional gonozooids begin as normal autozooids, modifying during further growth. Third, the lack of a capacious incubation chamber in any of the numerous specimens of Rallocytus ridiculu s n. gen., n. sp. (and Anyuta anastema n. gen., n. sp.) suggests that embryonic cloning (polyembryony) might be secondarily suppressed (wholly or partly) in these taxa — the dimorphic zooid, being the same size as an ordinary autozooid, would have little volume for cloning (unlike in Cinctiporidae). If the ancestrular zooid can produce eggs precociously in R. ridiculu s, then the apparent strategy could be that of reproducing one or a few larvae early and several times therafter, instead of producing a capacious gonozooid for the delayed mass production of embryos, either during a very narrow time period or, as in Filicrisia geniculata (Jenkins et al. 2017), over an extended period of time.

Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

Distribution. Recorded from 21 stations within coordinates 12.65742 – 14.41137 ° N, 129.08067 – 134.56370 ° W, at depth range 4640 – 5213 m.

Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

Etymology. Latin, ridiculus, absurd, alluding to the dimorphic zooid (s), which can sometimes include / comprise the ancestrular zooid.

Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

Material examined. Holotype: ZIRAS 1 / 50723, colony detached from nodule, YMG R. V. Yuzhmorgeologiya cruise YMG 4 – 06, Stn 79, 16 August 2006, 13.23973 ° N, 134.39873 ° W, 4810 m. Paratype 1: ZIRAS 2 / 50724, colony detached from nodule, YMG R. V. Yuzhmorgeologiya cruise YMG 4 – 07, Stn 130, 4 August 2007, 13.22832 ° N, 134.56370 ° W, 4830 m. Paratype 2: NIWA 127726, colony detached from nodule, YMG R. V. Yuzhmorgeologiya cruise YMG 4 – 14, Stn 359, 19 January 2016, 14.08687 ° N, 131.78558 ° W, 5122 m. Additional material: YMG 18 – 01, Stns 6, 31, 34; YMG 4 – 06, Stn 83; YMG 4 – 07, Stn 116; GLD 4 – 08, Stns 155, 159; GLD 4 – 09, Stns 173, 183, 196; GLD 4 – 11, Stns 206, 223; GLD 4 – 12, Stn 262; YMG 4 – 13, Stn 283; YMG 4 – 14, Stns 323, 328, 338, 340. Total specimens examined 23, 18 with dimorphic orifices.

Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

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CLASSIFICATION

Taxonomic Classification Tree

AnimaliaBryozoaStenolaemataCyclostomatidaAnyutidaeRallocytusRallocytus ridiculus

K

Animalia

Animalia2,981,931

P

Bryozoa

C

Stenolaemata

Stenolaemata14,358

O

Cyclostomatida

Cyclostomatida3,672

F

Anyutidae

G

Rallocytus

S

Rallocytus ridiculus

Rallocytus ridiculus

RELATED

Related Name Usages(5)

Matching names from other GBIF-indexed checklists and datasets.

Rallocytus ridiculusGrischenko, Gordon & Melnik, 2018

acceptedspecies

Rallocytus ridiculusGrischenko, Gordon & Melnik, 2018

acceptedspecies

Rallocytus ridiculusGrischenko, Gordon & Melnik, 2018

acceptedspecies

Rallocytus ridiculusGrischenko, Gordon & Melnik, 2018

acceptedspecies

Rallocytus ridiculusGrischenko, Gordon & Melnik, 2018

acceptedspecies

MULTIMEDIA

Media Files(5)

FIGURE 5. Pandanipora helix n. gen., n. sp. A, K, specimen YMG4–13, Stn 289; B, C, specimen YMG4–13, Stn 308; D, specimen YMG4–07, Stn 143; E, specimen GLD4–11, Stn 219; F, specimen YMG4–14, Stn 330; G–I, specimen YMG4–14, Stn 326; J, specimen GLD4–12, Stn 258; L, specimen YMG4–13, Stn 321. A–D, F, prop morphology: A, vertical and oblique columnar props attached to nodule by expanded tips; B, curved props attached to nodule irregularities by expanded tips with complex outlines; C, same, close-up; D, single elongated prop from its inception in the zooid basal wall to its distal expansion; E, light micrograph of colony showing successively overlapping zooids with their coelomic cavities continuing into the props with no intervening septum or pore, as well as 2–5 brown bodies located centrally to proximally in several zooids; F, prop tip showing opening towards substratum and internal surface with wedge-shaped crystallites, structurally analogous to peristome; G–I, ancestrula and daughter zooid budded from peristome; J–L, ancestrula and postancestrular zooids. Scale bars: A, B, E, 500 µm; C, D, J–L, 250 µm; F, 50 µm; G–I, 100 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

FIGURE 42. Rallocytus ridiculus n. gen., n. sp. Holotype, ZIRAS 1/50723. A–D, apical and oblique-lateral rotational views of colony with single dimorphic zooid, its smaller aperture (arrowed) facing frontalwards; E–G, peristomes and apertures of dimorphic zooid and adjacent autozooids; H, malleated colony surface at junction of capitulum and column. Scale bars: A–D, 250 µm; E–H, 100 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

FIGURE 43. Rallocytus ridiculus n. gen., n. sp. Paratype 1, ZIRAS 2/50724. A–D, apical and oblique views of fertile colony with two dimorphic zooids (arrowed), one with its aperture facing frontalwards, the other peristome turned slightly toward calyx center; E, F, peristomes, including a smaller frontally facing dimorphic one; G, two autozooidal peristomes with incurved dimorphic peristome between; H, base of column; I, skeletal microstructure; J, K, showing dimorphic and autozooidal apertures, respectively. Scale bars: A–C, 250 µm; D–H, 100 µm; J, K, 50 µm; I, 25 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

FIGURE 44. Rallocytus ridiculus n. gen., n. sp. Progressive stages of development of ancestrulate colonies. A–D, specimen YMG4–14, Stn 340, at three-zooid stage, with no distinction among peristomes; E–H, specimen GLD4–09, Stn 183, with four functional zooids, one dimorphic; I–L, specimen GLD4–08, Stn 159, with six functional zooids, one dimorphic; M–P, specimen GLD4–11, Stn 206, five functional zooids, none dimorphic. Scale bars: A, E, 150 µm; B–D, F–P, 200 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

FIGURE 54. Rallocytus ridiculus n. gen., n. sp. Micro-CT scans of paratype 2, NIWA 127726, as surface (A) and back-face isosurface renders showing colony interiors. A, surface and interior views of seven-zooid colony with dimorphic ancestrular zooid (daz) colored purple in the right-hand image; note small cluster of flattened kenozooidal chambers surrounding protoecium but absent from sides of column; B, lateral view, with entire dimorphic ancestrular zooid seen in left half; C, apical view of calyx, showing flattened kenozooidal/alveolar chambers filling center, dimorphic peristome at right indicated by arrowhead. Scale bars: 100 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion - Clipperton Fracture Zone, eastern Pacific Ocean-taxon novelty and implications of mining

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CITATIONS

References(1)

1

Grischenko, A. V.; Gordon, D. P.; Melnik, V. P. (2018). Bryozoa (Cyclostomata and Ctenostomata) from polymetallic nodules in the Russian exploration area, Clarion–Clipperton Fracture Zone, eastern Pacific Ocean—taxon novelty and implications of mining. <em>Zootaxa.</em> 4484(1): 1.

original descriptionWorld Register of Marine Species