AnimaliaNot EvaluatedacceptedspeciesAccepted
Orectopora flabellum

Orectopora flabellum

Grischenko, Gordon & Melnik, 2018

GBIF:148403744

0year

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Descriptions(5)

Description. Colony erect, flabellate, subplanar and narrowly compressed, attached by short stalk (Fig. 6 A, C), white. Initially with single spreading fan of zooids, more or less bilaterally symmetrical, or shortly branching as 2 – 3 flattened lobes, entire fan gently concave frontally, convex abfrontally (Fig. 6 B, D, E). At inception, first major lobe (s) comprising bilaterally compressed fascicle (s) of 10 – 12 autozooids, before subdivision into smaller lobes (Fig. 8 E – O). Colony and lobes essentially 1 – 2 - layered, comprising, in transverse section, initially contiguous, but then laterally diverging, autozooidal tubes, backed by discontinuous series of smaller kenozooidal tubes (Figs 6 E, 7 A, C, F, 51 A, B, D, E). Surface of colony textured by series of thin sinuous growth lines (Figs 6 D, 7 B, E, H) and needle-like crystallites perpendicular to growth lines. Simple pseudopores opening externally, seemingly moderately sparse in SEM images, but more obvious and abundant in CT scans, more or less regularly distributed (Figs 7 B, E, 51 A – F). Autozooidal tubes mostly very long, with several running length of colony; other tubes shorter, originating by lateral budding in plane of colony as fascicles broaden (Fig. 51 A, C). Earliest-established peristomes more evident on colony faces by bulging of their longitudinal tubes, secondarily budded autozooids not bulging or less obviously so (Figs 6 A, E, 8 L). Openings of primary and secondary autozooidal tubes at colony margin evidenced by their circular to subcircular rims, some separated sublaterally by shafts of slightly smaller diameter (Fig. 7 A, B, D, F), interpreted to be proximal parts of differentiating autozooids. Interior surface of zooidal tubes lined by distally imbricated foliated fabric of wedge-shaped crystallites (Fig. 7 D, G, J). Kenozooids seen in transverse section at colony margin, 1 – 2 on abfrontal side of each autozooid (Fig. 7 A, C, F, I), with round to subtriangular rims. Interior surface ultrastructure as in autozooids. CT scans reveal kenozooids to be long, irregular structures descending behind or to the side of zooidal tubes (Fig. 51 B, D, E), occasionally communicating with neighbors via interzooidal pores, with more-numerous pseudopores to outer surface. Proximally, CT scans reveal kenozooidal chambers transition from elongate tubes to layers of squatter cushion- or amoeba-shapes (Fig. 51 A, B, F); each kenozooid communicating with neighbors above and below; those closer to outer surface with sparse pseudopores. Kenozooids also in axils between fascicle lobes. Gonozooid not seen. Ancestrula suberect, inclined at 45 – 55 ° angle to substratum (Fig. 8 B, N). Protoecium (Fig. 8 D) flared at base, with slightly smoother margin, continuous with peristome, surface with needle-like crystallites (interpreted as eroded planar-spherulitic fabric) and sparse pseudopores. Abfrontal sides of ancestrular zooid, one suberect zooid and base of erect fascicle of zooids supported by developing skirt of kenozooids and extrazooidal calcification (Fig. 8 B, E, N); skirt with scalloped margin depending on substratum (Fig. 8 P); exterior surface marked by vertical striae and ridges, and moderately sparse but evenly distributed pseudopores. Measurements (mm). Holotype, ZIRAS 1 / 50673 (Fig. 6): Colony height c. 2.07 (proximal end of largest colony broken), width 3.02; three main lobes (fascicles) length 0.48 – 1.01, width 0.43 – 1.51, thickness 0.09 – 0.16; ‘ stalk’ at point of breakage 0.33 × 0.17; ZL 1.308 – 1.853 (1.604 ± 0.198); PeL 0.043 – 0.163 (0.082 ± 0.035); PeD 0.123 – 0.154 (0.136 ± 0.009); ApL 0.094 – 0.105 (0.099 ± 0.003); ApW 0.086 – 0.098 (0.091 ± 0.004). Non-type specimen GLD 4 – 08, Stn 151 (Fig. 8 D): AnPeD 0.106 (n = 1).
Grischenko, Andrei V., Gordon, Dennis P., Melnik, Viacheslav 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. Zootaxa 4484 (1): 1-91, DOI: 10.11646/zootaxa.4484.1.1
Remarks. Orectopora flabellum n. gen., n. sp. is represented in the Russian-sector collection by 14 specimens having varied size and maturity. The novel features of this taxon defy inclusion in a named family and have required some interpretation to describe and explain them, facilitated by light microscopy, with and without staining, plus SEM and micro-CT. The form of the ancestrular zooid is similar to that in Pandanipora n. gen., and the initial colony form, comprising a short ascending series of zooids supporting an elevated structure, is reminiscent of that in Discantenna (Gordon & Taylor, 2010).
Grischenko, Andrei V., Gordon, Dennis P., Melnik, Viacheslav 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. Zootaxa 4484 (1): 1-91, DOI: 10.11646/zootaxa.4484.1.1
Distribution. Recorded from 14 stations within coordinates 12.65038 – 14.57215 ° N, 131.73948 – 134.71841 ° W, at depth range 4713 – 5275 m.
Grischenko, Andrei V., Gordon, Dennis P., Melnik, Viacheslav 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. Zootaxa 4484 (1): 1-91, DOI: 10.11646/zootaxa.4484.1.1
Etymology. Latin, flabellum, a fan, used as a noun in apposition.
Grischenko, Andrei V., Gordon, Dennis P., Melnik, Viacheslav 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. Zootaxa 4484 (1): 1-91, DOI: 10.11646/zootaxa.4484.1.1
Material examined. Holotype: ZIRAS 1 / 50673, colony detached from nodule, YMG R. V. Yuzhmorgeologiya cruise YMG 4 – 13, Stn 316, 3 August 2014, 13.09428 ° N, 132.37362 ° W, 4933 m. Paratype: NIWA 127723, colony detached from nodule, YMG R. V. Gelendzhik cruise GLD 4 – 12, Stn 258, 10 April 2013, 12.90213 ° N, 132.87047 ° W, 4713 m. Additional material: YMG 4 – 07, Stns 126, 136; GLD 4 – 08, Stns 145, 151; GLD 4 – 09, Stns 183, 198; GLD 4 – 11, Stns 219, 230; YMG 4 – 13, Stn 273; YMG 4 – 14, Stns 332, 363, 365. Total specimens examined 14.
Grischenko, Andrei V., Gordon, Dennis P., Melnik, Viacheslav 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. Zootaxa 4484 (1): 1-91, DOI: 10.11646/zootaxa.4484.1.1

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FIGURE 6. Orectopora flabellum n. gen., n. sp. Holotype, ZIRAS 1/50673. A, C, E, colony respectively seen in frontal, abfrontal and apical views; B, frontal view of left-hand lobe (fascicle) in A; D, oblique abfrontal view of right-hand lobe (fascicle) in C; F, base of broken colony stalk. Scale bars: A, C, E, 500 µm; B, D, 250 µm; F, 150 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.

FIGURE 7. Orectopora flabellum n. gen., n. sp. Details of colony morphology. A, B, E, H, holotype colony; C, D, F, G, I, J, specimen GLD4–08, Stn 151. A, B, E, apical, oblique-abfrontal and abfrontal views, respectively, of middle lobe (fascicle) in Fig. 7E, showing apparent roof forming in axil between what will become two fascicle lobes; note relatively large pseudopores in neanic calcification of abfrontal wall in B and E; C, F, two views of a small fascicle showing autozooidal apertures adjacent to concave frontal face of lobe (on right), between which are larger developing chambers (either autozooidal or reproductive), and, along convex abfrontal face (on left), a row of mostly kenozoidal openings (and perhaps some incipient autozooid buds); D, G, J, magnified sequence of images showing the largest developing chamber in C and F, and ultrastructural wall fabric; H, reversed (frontal) view of fascicle tip in E; I, frontal view of chamber in D, G, J. Scale bars: A, B, E, H, 200 µm; C, F, 150 µm; D, I, 50 µm; G, J, 20 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.

FIGURE 8. Orectopora flabellum n. gen., n. sp. Colonies at early stages of astogeny. A–D, rotational views of specimen GLD4–08, Stn 151, with ancestrular region more magnified in D; E, F, rotational views of specimen GLD4–08, Stn 145; G, H, specimen GLD4–11, Stn 230; I, J, specimen GLD4–11, Stn 219; K–P, rotational views of paratype specimen, NIWA 127723. Scale bars: A–C, E–H, 300 µm; D, P, 200 µm; I–O, 500 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.

FIGURE 51. Orectopora flabellum n. gen., n. sp. Micro-CT scans of paratype, NIWA 127723, as back-face isosurface renders showing colony interiors. A, colony curvature in lateral view showing part of abfrontal (left) and frontal (right) surfaces; note large cluster of kenozooidal chambers at lower left, becoming longer distally and near autozooidal tubes; B, like A, but from opposite side, showing more of abfrontal surface; note pseudopore density; C, en face view of colony frontal surface, with only the part in the square shown as backface isosurface render; note the kenozooids in the interior angle between two-right-hand fascicles (lobes); D, E, abfrontal side of colony, with that in D showing differentiating tip of middle lobe; note elongate kenozooids on either side of or abfrontal to autozooidal tubes; F, close-up of part of A showing variability of kenozooidal chambers. Scale bars: 100 µm.

Imageimage/png© Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.Grischenko, Andrei V.;Gordon, Dennis P.;Melnik, Viacheslav P.

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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

checklist

This dataset contains the digitized treatments in Plazi based on the original journal article Grischenko, Andrei V., Gordon, Dennis P., Melnik, Viacheslav 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. Zootaxa 4484 (1): 1-91, DOI: 10.11646/zootaxa.4484.1.1

Abstract

This work describes Bryozoa of the orders Cyclostomata and Ctenostomata found associated with polymetallic nodules collected by box-coring in the eastern part of the Russian exploration area of the Clarion-Clipperton Fracture Zone (CCFZ) under contract to Yuzhmorgeologiya. Scanning electron microscopic study of 358 cyclostome colonies and 14 ctenostome colonies from 4510–5280 m depth has resulted in the recognition of two new species of Ctenostomata, and 14 new species, nine new genera and two new families of Cyclostomata; three additional species of Cyclostomata are left in open nomenclature pending the discovery of missing reproductive characters. The taxonomic novelty is thus notable. One of the new Ctenostomata represents the first living example of the previously monotypic Late Cretaceous genus Pierrella. Twelve of the new cyclostome taxa have well-developed gonozooids, indicating that embryonic cloning (polyembryony) is normal in this deep-sea environment. On the other hand, one indeterminate tubuliporine and two rectangulates have dimorphic peristomes. In the latter two cases, enough mature colonies were found to suggest that this feature is normal, and that the dimorphic zooids are possibly female—in other words, capacious incubation chambers are apparently lacking, and therefore polyembryony would also be lacking or reduced. In one of these species, evidence is presented to suggest that the ancestrular zooid can reproduce precociously. Of the species reported here, only one has previously been found outside the exploration area, highlighting both the limited knowledge we have of bryozoans in the deep Pacific and/or a fauna that is largely endemic to the nodule environment. An additional 31 species of Cheilostomata have also been discovered that will be described in a subsequent publication. Most bryozoans are macrofaunal-sized, so are both inadequately determinable and overlooked in images obtained by remotely operated vehicles; yet, with 50 species, Bryozoa is the most speciose sessile macrofaunal phylum on the nodules. Nodules constitute hard substrata in an area otherwise mostly inhospitable for Bryozoa, hence mining would lead to loss of critical habitat. Further, as suspension-feeders, bryozoans are highly susceptible to smothering by suspended sediment, and non-mined areas closely adjacent to extraction zones would likely also be affected and their associated bryozoan fauna obliterated. More data are required on the distribution of the CCFZ bryozoan species elsewhere in the east Central Pacific to determine if mining would lead to local taxon extirpation or global extinction at both low and high taxonomic levels.

Grischenko A V, Gordon D P, Melnik V P, plazi (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. Plazi.org taxonomic treatments database. Checklist dataset https://doi.org/10.11646/zootaxa.4484.1.1 accessed via GBIF.org on 2026-06-14.

CC0Published 9/25/2018View dataset
GBIF Usage Key
148403744
Dataset Key
74b777c9-eae0-4770-8c86-dcbb10fb06b3
Origin
source
Backbone Key
10058247
Taxon ID
521587E4563C551509EEF914884FFBD0.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026