Hippothoa pacifica Gordon, 1984

Gordon, Dennis P., 2020, New Hippothoidae (Bryozoa) from Australasia, Zootaxa 4750 (4), pp. 451-476 : 468-469

publication ID

https://doi.org/ 10.11646/zootaxa.4750.4.1

publication LSID

lsid:zoobank.org:pub:AE9FDD46-5471-44B3-97FB-11C4BD45C59B

DOI

https://doi.org/10.5281/zenodo.3717946

persistent identifier

https://treatment.plazi.org/id/6262878C-FFFE-FFFF-FF3E-F9E7A6D2FD6E

treatment provided by

Plazi

scientific name

Hippothoa pacifica Gordon, 1984
status

 

Hippothoa pacifica Gordon, 1984

( Fig. 10A, D View FIGURE 10 )

Hippothoa divaricata pacifica Gordon, 1984: 111 View in CoL , text-fig. 10C, F, pl. 43A, B; Gordon et al. 2009: 291.

Material examined. Holotype: NIWA 1279 View Materials (H-282), 30.5533° S, 178.5267° W, 125 m. GoogleMaps Paratype: NIWA 1280 View Materials (P-567), same data as holotype GoogleMaps . Other material: NIWA 73295 View Materials , 34.2685° S, 173.0248° E, 168 m GoogleMaps ; NIWA 98914 View Materials , 46.7250° S, 165.7750° E, 286 m GoogleMaps ; NIWA 144794 View Materials , 33.9875° S, 171.7508° E, 170–174 m GoogleMaps ; NIWA 26694 View Materials , 26696 View Materials , 98202 View Materials , 98214 View Materials , 98215 View Materials , 42.8292° S, 177.4218° W, 826 m. GoogleMaps

Remarks. Gordon & Ryland (1977) noted the close similarity between European and New Zealand specimens of Hippothoa divaricata , treating them as conspecific. Differences appeared trivial, including “the autozooidal sinus, which is more U-shaped, and the pore-chambers which are more triangular” in the New Zealand form. Gordon (1984) described the latter as a new subspecies, H. divaricata pacifica , further noting more-elongate zooeciules, fewer pore-chambers and a kenozooidal ancestrula, but was not able to illustrate the ovicell in the type specimens, noting, however (in remarks on Hippothoa calciophilia Gordon, 1984, p. 110 ), that the apex of the ovicell in H. divaricata pacifica was bimucronate.

The new material gives information on the ovicell, of which the ooecium is indeed bimucronate ( Fig. 10A View FIGURE 10 ), appearing as a pair of converging, rimmed, drop-shaped tubular (elevated) pseudopores in non-eroded specimens. De Blauwe (2009) has illustrated by SEM Belgian material of H. divaricata —the sole ovicell shown has an ooecium with more-widely separated elevations, each with a small excavation in it. The specimen additionally shows that the autozooids are proportionally narrower and more-strongly carinate than in the New Zealand form, which is here raised to full species rank. Moyano’s (1986) illustrations of H. divaricata from Chile resemble H. pacifica but the ancestrula has an orifice and operculum.

Hippothoa pacifica ranges throughout New Zealand from the vicinity of Raoul Island to southern South Island (c. 29– 47° S), where it seems to be restricted to calcareous substrata. It occurs from shallow coastal water to 826 m depth.

Kingdom

Animalia

Phylum

Bryozoa

Class

Gymnolaemata

Order

Cheilostomatida

Family

Hippothoidae

Genus

Hippothoa

Loc

Hippothoa pacifica Gordon, 1984

Gordon, Dennis P. 2020
2020
Loc

Hippothoa divaricata pacifica

Gordon, D. P. & Taylor, P. D. & Bigey, F. P. 2009: 291
Gordon, D. P. 1984: 111
1984
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