AnimaliaNot EvaluatedacceptedspeciesAccepted
Haywardozoon pacificum

Haywardozoon pacificum

Grischenko, Gordon & Melnik, 2018

GBIF:148403707

0year

ABOUT

Descriptions(5)

Description. Colony encrusting, diffuse, comprising up to c. 12 large zooids, partly uniserially arranged and disjunct (Figs 47, 48), adjacent zooids connected distally and laterally by very small contact points; highly transparent and apparently colorless in life. Zooids generally mostly elongated, their lateral outlines weakly convex to subparallel or even slightly diverging; bilaterally symmetrical or one side extending outwards as a triangular skirt. Daughter zooids budded distolaterally. Membranous frontal wall gently rising to highest point of zooid at orifice (Fig. 47 G). Orifice wider than long (Figs 47 I, J, 48 G), having slightly thickened cuticularized rim with two components — proximal rim more or less transversely C-shaped, concave on inner side; distal rim more or less straight but produced proximally as D-shaped flap that superficially resembles operculum and fits into concavity of proximal rim; edge of flap slightly thickened (Figs 48 G, H). Vestibule more or less parallel-sided, a little longer than broad, 28 – 33 % polypide length, with strongly developed parieto-diaphragmatic musculature at proximolateral corners (Fig. 47 I, J). Vestibule 0.097 – 0.123 mm long; retracted tentacle crown 0.265 – 0.311 mm long, tentacle number not determined. No stomach gizzard. Small brown bodies or fragments of brown bodies retained in cystid (Fig. 47 I, J). Anchor point of polypide retractor muscles not clearly seen. One very small oval zooid encountered that may be ancestrula, very close to proximal curved ‘ tail’ of large zooid that may have budded from it (Fig. 48 I). Orifice of small zooid (Fig. 48 J) identical in form to that of large zooids). Measurements (mm). Holotype, ZIRAS 1 / 50726 (Figs 47, 48): ZL 0.703 – 1.450 (1.048 ± 0.211); ZW 0.438 – 0.852 (0.714 ± 0.117); OrL 0.088 – 0.140 (0.120 ± 0.018); OrW 0.150 – 0.203 (0.172 ± 0.019). Ancestrula (n = 1): AnL 0.322; AnW 0.221; AnOrL 0.027; AnOrW 0.059.
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. We follow Jebram (1986) in including Haywardozoidae in superfamily Hislopioidea, and Reverter- Gil et al. (2016) concerning the emended spelling of the family name. Our material conforms to the overall characters of the two described Atlantic species of Haywardozoon, especially H. inarmatum, which has a similar budding pattern and zooid shape, but from which it differs in details of the orifice. D’Hondt (1983) characterized the polypide of Haywardozoon species as “ minute … inhabiting only a very small portion of the zoecial cavity ”, which is not the case in H. pacificum n. sp. The CCZ colonies were found only on tubes of serpulid polychaetes attached to nodules.
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 eight stations within coordinates 12.26676 – 13.61415 ° N, 130.82158 – 134.59811 ° W, at depth range 4741 – 5050 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. Alluding to the first description of the genus in the Pacific Ocean.
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 / 50726, colony encrusting tube of serpulid polychaete detached from nodule, YMG R. V. Yuzhmorgeologiya cruise YMG 4 – 04, Stn 39, 16 August 2005, 13.61415 ° N, 130.82158 ° W, 5017 m. Additional material: YMG 4 – 07, Stns 134, 143; GLD 4 – 11, Stns 214, 220; GLD 4 – 12, Stns 245, 267; YMG 4 – 14, Stn 322. Total specimens examined eight.
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 47. Haywardozoon pacificum n. sp. Specimens stained in Rose Bengal. A, specimen GLD4–11, Stn 214, zooids on a serpulid tube; B–G, holotype, ZIRAS 1/50726, different views of zooids on a serpulid tube; H–J, specimen GLD4–12, Stn 245, respectively showing very lightly stained zooids on serpulid tube and two zooids seen in transmitted light. Abbreviations: bb, brown body; d, diaphragm; dmd, dilator muscles of diaphragm; g, gut; olf, operculum-like flap; rmtc, retractor muscles of tentacle crown; t, tentacle cluster; v, vestibule. Scale bars: A–H, 500 µm; I, J, 100 µm.

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

FIGURE 48. Haywardozoon pacificum n. sp. Holotype, ZIRAS 1/50726. A–F, autozooids disposed on serpulid tube, all slightly collapsed through drying; G, H, orificial region showing operculum-like flap; I, autozooid, with dwarf ancestrular at lower right; J, close-up of ancestrula. Scale bars: A, F, 500 µm; B–E, I, 250 µm; G, 200 µm; H, I, 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 2026-06-16.

CC0Published 9/25/2018View dataset
GBIF Usage Key
148403707
Dataset Key
74b777c9-eae0-4770-8c86-dcbb10fb06b3
Origin
source
Backbone Key
10276805
Taxon ID
521587E45676554E09EEFAFF8958FCB0.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026