AnimaliaNot EvaluatedacceptedspeciesAccepted
Calyssopora clarionensis

Calyssopora clarionensis

Grischenko, Gordon & Melnik, 2018

GBIF:148403739

0year

ABOUT

Descriptions(5)

Description. Colony erect, compact (Fig. 33) relative to other species, with apron-like base, vasiform; column topped by capitulum comprising peripheral autozooidal peristomes surrounding central concavity. Skeletal surface irregularly textured with minute dimples and granules except for base of column. Pores tiny, simple, sparse. Autozooids in well-developed infertile colonies in single whorl of 6 – 7 (Fig. 35 I – P), with incipient zooid bud developing frontally at lower level between each pair; apertures bilaterally symmetrical, with raised, granular, arcuate lateral rims and concave frontal and abfrontal rims (Figs 33 A, 34 A – F, M), hence somewhat mitriform in profile. Wall interiors densely covered by prickle-like granules (Fig. 34 N, P). Alveoli rare between peristome bases abfrontally. Autozooids in mature brooding colonies with c. 8 peristomes in primary whorl and c. 7 slightly smaller peristomes at lower level (Fig. 34 A). Gonozooid single, developing from female zooid in central concavity of capitulum, ventricose in vicinity of ooeciostome only, occupying part or all of concavity, ooeciostome strongly curved and hood-like (Figs 33 A, 34 A, B, G, H, J), its surface granular-tubercular, ooeciopore concealed from frontal view. Sparse, relatively large alveoli adjacent to gonozooid within concavity (Fig. 34 A, C). Ancestrular zooid erect, not seen in isolation; earliest growth stage encountered comprising three very similar zooids (Fig. 35 A – D) such that it is not clear which is ancestrular; protoecium not obvious. Elongation and outward curving of peristomes resulting in small vasiform colony (Fig. 35 F – H) with budding of additional zooids lateroabfrontally between peristomes (Fig. 35 M, N). Measurements (mm). Holotype, ZIRAS 1 / 50719 (Fig. 33 A): Colony height 1.94; capitulum 1.28 × 1.22; base at substratum 0.75 × 0.83; column diameter 0.47 – 0.76; ZL 0.653 – 0.882 (0.784 ± 0.088) (n = 8); PeL 0.221 – 0.303 (0.255 ± 0.026) (n = 8); PeD 0.203 – 0.233 (0.218 ± 0.011) (n = 8); ApL 0.196 – 0.228 (0.211 ± 0.011) (n = 8); ApW 0.155 – 0.192 (0.168 ± 0.013) (n = 8). Gonozooid (n = 1): GZL 0.483; GLW 0.491; OsL 0.348; OsW 0.226; OsH 0.207. Paratype 2, ZIRAS 3 / 50721 (Fig. 33 C): OpL 0.091 (n = 1); OpW 0.108 (n = 1). Paratype 3, ZIRAS 4 / 50722 (Fig. 33 D): OpL 0.098 (n = 1); OpW 0.124 (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. Calyssopora clarionensis n. sp. differs most obviously from the type species in having a gonozooid with a curved ooeciostome and prickled zooidal interiors.
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 13 stations within coordinates 12.84500 – 14.33668 ° N, 129.07338 – 134.46597 ° W, at depth range 4690 – 5222 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. Pertaining to the Clarion Fracture, which defines the northern margin of the potential mining area.
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 / 50719, colony attached to nodule particle, YMG R. V. Gelendzhik cruise GLD 4 – 11, Stn 220, 30 April 2012, 12.88593 ° N, 133.18168 ° W, 4916 m. Paratype 1: ZIRAS 2 / 50720, colony attached to nodule particle, YMG R. V. Yuzhmorgeologiya cruise YMG 4 – 13, Stn 291, 27 July 2014, 13.00083 ° N, 132.49723 ° W, 4865 m. Paratype 2: ZIRAS 3 / 50721, colony attached to nodule particle, YMG R. V. Gelendzhik cruise GLD 4 – 09, Stn 186, 1 January 2011, 13.45140 ° N, 133.53807 ° W, 4872 m. Paratype 3: ZIRAS 4 / 50722, detached colony, YMG R. V. Gelendzhik cruise GLD 4 – 12, Stn 246, 3 April 2013, 13.00578 ° N, 132.95280 ° W, 4935 m. Additional material: YMG 18 – 01, Stn 24; YMG 4 – 07, Stn 134; GLD 4 – 08, Stns 144, 150; GLD 4 – 11, Stn 209; YMG 4 – 13, Stns 287, 290; YMG 4 – 14, Stns 327, 339. Total specimens examined 13.
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

Export occurrence data

Darwin Core Archive (ZIP)

CLASSIFICATION

Taxonomic Classification Tree

MULTIMEDIA

Media Files(3)

FIGURE 33. Calyssopora clarionensis n. gen., n. sp. General view of holotype and paratype colonies. A, holotype, ZIRAS 1/ 50719, with fully hooded ooeciostome; B, paratype 1, ZIRAS 2/50720, with mostly hooded ooecostome; C, paratype 2, ZIRAS 3/50721, with ooeciopore visible; D, paratype 3, ZIRAS 4/50722, with partially developed ooeciostome not yet concealing ooeciopore. Scale bars: 250 µm.

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

FIGURE 34. Calyssopora clarionensis n. gen., n. sp. A, D, G, J, holotype, ZIRAS 1/50719, respectively showing an apical view of the fertile colony and profiles of the hooded ooeciostome; B, E, H, K, paratype 2, ZIRAS 3/50721, respectively showing an apical view of the gonozooid and profiles of a more-truncated ooeciostome; C, F, I, L, paratype 3, ZIRAS 4/50722, similar views of a colony with a more-open ooeciostome; M, specimen YMG4–13, Stn 287, mitriform shape of autozooecial orifice when seen in oblique lateral view; N, specimen GLD4–11, Stn 209, oblique view of autozooidal peristome and aperture showing spinose granulation of interior and exterior surfaces; O, P, paratype 1, ZIRAS 2/50720, respectively showing trabecula joining two peristomes and vertical view of autozooidal aperture. Scale bars: A–F, 200 µm; G–I, 100 µm; J–P, 50 µm.

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

FIGURE 35. Calyssopora clarionensis n. gen., n. sp. Progressive stages of development of ancestrular and young colonies. A–D, specimen YMG18–01, Stn 24, three-zooid colony; E–H, specimen GLD4–08, Stn 144, four–five-zooid stage; I–L, specimen YMG4–07, Stn 134, seven-zooid stage with central cavity presumably representing incipient incubation chamber; M–P, specimen GLD4–11, Stn 209, eight-zooid stage with paired central cavities. Scale bars: 200 µm.

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

IMAGES

Gallery(3)

See Gallery

Occurrences with images

Source Information

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 2026-06-15.

CC0Published 9/25/2018View dataset
GBIF Usage Key
148403739
Dataset Key
74b777c9-eae0-4770-8c86-dcbb10fb06b3
Origin
source
Backbone Key
10494706
Taxon ID
521587E45600553109EEFA53884FFB88.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026