AnimaliaNot EvaluatedacceptedspeciesAccepted
Anyuta anastema

Anyuta anastema

Grischenko, Gordon & Melnik, 2018

GBIF:148403736

0year

ABOUT

Descriptions(5)

Description. Colony erect, pedunculate and subcalyciform, with outwardly flaring capitulum of short branches (Fig. 39 A, B). Stalk (column) cylindrical, tapering proximally before expanding to form circular disk (Fig. 39 C, D). Branches of type colony disposed more or less in two clusters, each comprising two fascicles of zooids with associated structures. Length of outwardly inclined branches shorter than stalk. All surfaces interior-walled, with variably imbricating platy microstructure or the plate-like crystalline ‘ tablets’ commonly irregular and less angular (Fig. 40 C). Autozooidal tubes numbering 4 – 5 in each of the fascicles, the tubes indicated by their entire, round peristomial rims (Figs 39 C, D, 40 D – G, I, 41 A, E, I). Exterior skeletal surface of peristomial walls minutely irregular and uneven (Fig. 40 B, G), lightly textured, with variable expression of partial longitudinal and / or transverse ridges, striae and convexities. Pores simple, open, of variable shape, sparse. Peristomial rim even or slightly uneven, smooth or minutely granular. Skeletal ultrastructure of interior surface of peristomes similar to that of exterior but smoother and crystallites less discrete; no spinules or pustules. CT scans reveal that interzooidal communication pores are very sparse (Fig. 53 A, B). Center of sides of capitulum with alveolar / kenozooidal chambers (Figs 39 A, 40 A, 41 I, M, 53 A). Alveoli forming as low walls, typically arcuate, on upper surfaces. As these walls grow, the extrazooidal cavities they enclose become deeper, cupuliform, and kenozooid-like, filling in spaces between autozooidal peristomes, sometimes in stepwise series. Some alveoli very elongate, extending up frontal longitudinal faces of autozooidal peristomes (Figs 39 A, 40 A) and abfrontally as flattened alveoli / kenozooids (Fig. 53 A). Stalk with subparallel longitudinal ridges separating furrows in which are simple communication pores in generally linear series; ridges flare outward to circular base, giving appearance of pleated skirt (Fig. 40 J). CT scans reveal c. 18 highly elongate-triangular kenozooidal chambers in basal part of stalk; these wider basally, acicular distally, surrounding ancestrular protoecium in palisade arrangement (Fig. 53 D, E); these lacking porous communications with neighbors or exterior colony surface. In autozooidal clusters of mature colonies are smaller-diameter tubes with their openings encircled by subhorizontal subcircular flanges (Figs 39 A, B, D, 40 A, B, D – I), interpreted as gonozooids. Peristomial rim of smaller tubes somewhat inclined over opening (inferred ooeciopore), slightly reducing its diameter (Fig. 40 K). Encircling flange white, suggestive of different type of carbonate from rest of colony; a ring of tiny perforations around inner edge of flange against side of inferred ooeciostome (Fig. 40 K, L). Ancestrular zooid not seen in isolation; earliest growth stage encountered comprising three zooids (Fig. 41 A – D) — erect ancestrular peristome flanked laterofrontally by pair of daughter zooids budded from its base and concealing it frontally, its abfrontal surface coarsely ridged, with sparse pores. Peristomial tubes of ancestrular zooid and two daughters elongating and increasing in height and wall thickness. Developing colony becoming vasiform (Fig. 41 J – L, N – P); budding of additional zooids from distal abfrontal parts of autozooids, with ~ 3 walls forming sides of each bud (Fig. 41 I, M). Developing colony stem typically with longitudinal ridges and alveolar furrows, these less obvious with secondary calcification. Measurements (mm). Holotype, ZIRAS 1 / 50718 (Figs 39 – 40): Colony height 4.41; capitulum 3.28 × 2.80; base 1.03 × 0.95; stalk height 2.78; narrowest diameter 0.40 × 0.34; ZL 0.873 – 1.460 (1.147 ± 0.204); PeL 0.330 – 0.565 (0.448 ± 0.076); PeD 0.231 – 0.248 (0.241 ± 0.006); ApL 0.210 – 0.243 (0.228 ± 0.009); ApW 0.193 – 0.218 (0.202 ± 0.008). Dimorphic zooids (n = 4): GZH 0.152 – 0.211 (0.181 ± 0.024); GZD 0.251 – 0.325 (0.271 ± 0.036); GZFD 0.181 – 0.199 (0.188 ± 0.007); OpD 0.091 – 0.101 (0.094 ± 0.007).
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. Anyuta anastema n. gen., n. sp. is represented in the Russian-sector collection by twelve specimens. The capitulum of the smaller of the two largest colonies is skewed and less symmetrical than in the holotype colony and the alveoli are more open and elongate.
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 12 stations within coordinates 12.55602 – 14.32132 ° N, 129.11345 – 134.51190 ° W, at depth range 4690 – 5213 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. Greek, anastema, height, tallness, alluding to the elevated form of the colony with the branches lifted up, 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 / 50718, colony detached from nodule, YMG R. V. Gelendzhik cruise GLD 4 – 09, Stn 180, 26 December 2010, 13.03863 ° N, 133.39428 ° W, 4919 m. Paratype: NIWA 127725, 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, Stn 29; YMG 4 – 06, Stn 71; YMG 4 – 07, Stns 119, 133; GLD 4 – 08, Stn 144; GLD 4 – 11, Stn 227; YMG 4 – 13, Stns 281, 283; YMG 4 – 14, Stns 338, 360. Total specimens examined 12, two (the largest) with dimorphic zooids.
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 2. Colonies of some cyclostome bryozoans, in vivo, attached to polymetallic nodules. A–E, Pandanipora helix n. gen., n. sp.: A, specimen GLD4–09, Stn 190; B, specimen GLD4–12, Stn 262; C, specimen YMG4–07, Stn 143; D, specimen YMG4–13, Stn 295; E, specimen GLD 4–11, Stn 212. F, Tubuliporina sp. indet., specimen YMG18–01, Stn 7. G, H, Abyssoecia elevata n. gen., n. sp.: G, specimen GLD4–09, Stn 196; H, specimen GLD4–09, Stn 191. I, Discantenna metallica n. sp.: specimen GLD4–11, Stn 224. J, K, Frontohornera frontalis n. gen., n. sp.: J, specimen YMG4–07, Stn 124; K, specimen GLD4–11, Stn 210. L, Alyonushka hystricosa n. gen., n. sp.: specimen GLD4–09, Stn 199. M, Calyssopora volcano n. gen., n. sp.: specimen YMG18–01, Stn 33. N, O, Anyuta anastema n. gen., n. sp.: N, specimen GLD4–09, Stn 180; O, specimen YMG4–06, Stn 71. Scale bars: 1 mm.

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

FIGURE 39. Anyuta anastema n. gen., n. sp. A–D, holotype, ZIRAS 1/50718, in apical and lateral profiles; note the clusters of fascicles, at least three of which have dimorphic orifices with terminal flanges (dimorphic orifices arrowed). Scale bars: 500 µm.

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

FIGURE 40. Anyuta anastema n. gen., n. sp. Holotype, ZIRAS 1/50718. A, part of fascicle with autozooidal peristomes and two dimorphic peristomes with flanges; note large shallow alveoli on sides of peristomes; B, two peristomes, left one dimorphic; C, skeletal microstructure of part of peristome in L; D–G, subfascicles with both autozooidal and flanged dimorphic peristomes; H, close-up of squat flanged dimorphic peristome in E; note small alveoli on flanks of peristome; I, close-up of lower dimorphic peristome in F, showing it to be derived from an autozooidal peristome by its partial closure; J, base of column; K, L, close-ups of perforated flanges of dimorphic peristomes. Scale bars: A, B, D, F, 250 µm; G–J, 100 µm; K, L, 50 µm; C, 25 µm.

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

FIGURE 41. Anyuta anastema n. gen., n. sp. Progressive stages of development of young colonies. A–D, specimen YMG4–14, Stn 360, three-zooid stage; E–H, specimen YMG4–14, Stn 338, five–six-zooid stage; I–L, specimen YMG4–13, Stn 281, and M–P, specimen YMG4–06, Stn 71, showing later stages in which trabecular walls define spaces destined to become either autozooids or alveoli. Scale bars: 200 µm.

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

FIGURE 53. Anyuta anastema n. gen., n. sp. Micro-CT scans of paratype, NIWA 127725, as surface (C) and back-face isosurface renders showing colony interiors. A, view of colony from below; note absence of kenozooids from most of column; B, lateral abfrontal view of two small fascicles with entrance to dimorphic zooid indicated by arrowhead; note relative paucity of communication pores; C–E, exterior and interior views of colony base, showing lateral (C, D) and frontolateral (E) profiles with palisade of elongate-triangular kenozooidal chambers surrounding ancestrular protoecium (pr) and proximal part of its peristome (ap). 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
148403736
Dataset Key
74b777c9-eae0-4770-8c86-dcbb10fb06b3
Origin
source
Backbone Key
10339847
Taxon ID
521587E45609553B09EEFF1F884FFE9B.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026