AnimaliaacceptedgenusAccepted
Rallocytus

Rallocytus

Grischenko, Gordon & Melnik, 2018

GBIF:148403733

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Descriptions(4)

Diagnosis. Colony erect, pedunculate, autozooidal peristomes radiating around infundibuliform calyx in single irregular whorl; interior surface of peristome lacking spinules or pustules. Dimorphic zooids 1 – 2 per colony within zooidal whorl, not occupying colony center, inferred to be female, each with reduced opening (presumed ooeciopore); appearing as early as four-zooid stage of colony growth, with reduced opening pertaining to ancestrula. Ancestrula erect, its peristome placed centrally on protoecium.
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. Rallocytus n. gen. is presently monogeneric. In general aspect, the form of the colony resembles that in Calyssopora n. gen., but differs strikingly in that the colony center is not occupied by a capacious incubation chamber. Rather, as evidenced by early colony stages, a dimorphic zooid can occur within a single zooid whorl of four zooids, three of them autozooids; Micro-CT scans of one such colony revealed that the dimorphic zooid, distinguished only by the smaller size of its aperture, is the ancestrular zooid. On the other hand, one of the largest colonies (a paratype) has up to ten peristomes in a single whorl, two of them dimorphic, both with their apertures facing upwards or towards the colony center, rather than outwards like autozooidal peristomial apertures. Since a colony cannot have two ancestrulae, the implication is that the ancestrula, being the oldest still-functional zooid in the colony, is capable of precocious reproduction — assuming that our inference of a reproductive function for the dimorphic zooids is correct. Note that not every ancestrular peristome is dimorphic — we have submature colonies in which it resembles that of ordinary zooids. It is thus highly unlikely that the dimorphic zooids are primary or secondary nanozooids, such as are found in the tubuliporine genus Diplosolen Canu, 1918 and some species of Plagioecia and Favosipora (Gordon & Taylor 2001). These small zooids in Diplosolen have very tiny apertures with a single emergent tentacle (Silén & Harmelin 1974) that seems to have a cleaning function, and occur only in two-dimensionally encrusting colonies, unlike the situation in erect Rallocytus ridiculus n. gen., n. sp. An ancestrula would not be expected to have a nanozooid function, whereas a reproductive function cannot be ruled out.
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 rallus, thin, and Latinized Greek cytus, container, alluding to the cystid of dimorphic zooids inferred to be fertile. Gender masculine.
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. Rallocytus ridiculus 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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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
148403733
Dataset Key
74b777c9-eae0-4770-8c86-dcbb10fb06b3
Origin
source
Backbone Key
10343140
Taxon ID
521587E4560D553809EEFF1F8B49FBF2.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026