AnimaliaacceptedgenusAccepted
Pandanipora

Pandanipora

Grischenko, Gordon & Melnik, 2018

GBIF:148403741

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Descriptions(4)

Diagnosis. Colony uniserial, linear to helicospiral, semi-erect to erect, supported above substratum by proplike extensions, generally one per zooid. Autozooids comprising continuous proximal portions that form axis of colony, plus erect peristomial tubes. Zooidal budding via symmetrical median partition originating from floor of axial part of parent zooid; proximal parts of zooids frontally overlapping. Autozooidal pseudopores tiny, simple, sparse. Gonozooid unknown. Ancestrula erect, tubiform, with swollen, squat, imperforate protoecium, its distal peristome curving.
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. Pandanipora n. gen. differs from typical stomatoporiform tubuliporines in being wholly non-adnate and supported above the substratum by props, typically one per zooid, as well as strictly uniserial and either unbranching or with a rare short bifurcation near the colony origin. Stomatopora Bronn, 1825 and related encrusting genera have an adnate ancestrula. Insofar as the ancestrula of Pandanipora n. gen. is erect and tubiform, it resembles that of Peristomatopora Moyano, 1991, which has the same form, i. e. a small swollen, squat protoecium, plus a curving erect peristome. On this basis, Peristomatopora would seem to be unrelated to Stomatopora, but the phylogenetic relationships of these and associated genera are poorly known. Taylor (1993) retained use of the family Stomatoporidae Pergens & Meunier, 1887, whereas Ross & Ross (1996) merged Stomatoporidae in the later-named Diastoporidae Gregory, 1899, itself based on a genus of controversial status in which the gonozooid is typical of that in the Plagioeciidae Canu, 1918 (Taylor & Wilson, 1999). Hayward & Ryland (1985) and Moyano (1991) included Stomatopora and / or associates in Oncousoeciidae Canu, 1918. Hayward & Ryland (1985, p. 18) illustrated a gonozooid in extant Stomatopora gingrina Jullien, 1882 that has the same form as that illustrated in Peristomatopora by Moyano (1991), which begs the question, which character is phylogenetically more significant — the form of the ancestrula or the incubation chamber? The gonozooid in Pandanipora is so far unknown. Do skeletal ultrastructural characters provide a clue? Moyano (1991) gave no such information concerning his new stomatoporine taxa. Taylor & Weedon (2000) reported that “ Stomatopora ” sp. (with an adnate ancestrula) and all studied articulates (with an erect ancestrula) apart from Crisulipora have a fabric suite that includes hexagonal semi-nacre, which is not found in Pandanipora n. gen. Instead, Pandanipora exhibits a predominantly distally imbricated foliated fabric typical of rectangulates, some cerioporines and some tubuliporines. The question remains open, but Pandanipora appears distant from articulates and stomatoporines (the latter admittedly based on limited data) and is probably closer to some other tubuliporines.
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 angiosperm genus Pandanus Parkinson, in which branches are characteristically supported by vertical prop roots, plus - pora, a common suffix for cyclostome bryozoans. Gender feminine.
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
Type species. Pandanipora helix n. sp.
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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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 2026-06-14.

CC0Published 9/25/2018View dataset
GBIF Usage Key
148403741
Dataset Key
74b777c9-eae0-4770-8c86-dcbb10fb06b3
Origin
source
Backbone Key
10409480
Taxon ID
521587E45635550F09EEFA40892FFC92.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026