Hippothoa peristomata Gordon, 1984
Gordon, Dennis P., 2020, New Hippothoidae (Bryozoa) from Australasia, Zootaxa 4750 (4), pp. 451-476 : 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.3717944 |
persistent identifier |
https://treatment.plazi.org/id/6262878C-FFFD-FFFF-FF3E-FD07A468FA70 |
treatment provided by |
Plazi |
scientific name |
Hippothoa peristomata Gordon, 1984 |
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Hippothoa peristomata Gordon, 1984 View in CoL
( Fig. 10B, C, E, F View FIGURE 10 )
Hippothoa peristomata Gordon, 1984: 111 View in CoL , text-fig. 10E, pl. 43E–G; Gordon et al. 2009: 291.
Material examined. Holotype: NIWA 7429 View Materials (H-330), Kermadec Ridge (no data) . Other material: NIWA 22948 View Materials , 35.7415° S, 178.4983° E, 312 m GoogleMaps ; NIWA 76400 View Materials , 37.6152° S, 177.0957° E, 165–170 m GoogleMaps ; NIWA 93782 View Materials , 120856, 36.9078° S, 169.8463° W, 1013 m GoogleMaps .
Remarks. The species was named for the extremely elevated orificial region ( Fig. 10B View FIGURE 10 ), shown here in profile for the first time ( Fig. 10E View FIGURE 10 ). The ooecium of the terminal ovicell is relatively large and globular, and a little wider than the maternal zooid ( Fig. 10C View FIGURE 10 ). The holotype colony had unusual kenozooids and it appears that these were not anomalous as they also occur in a sample from the Louisville Seamount Chain. They are almost the same size and shape as autozooids but instead of a tall elevated orifice there is only a smooth rounded convexity ( Fig. 10F View FIGURE 10 ); this does not appear to be a reparative feature.
Only one ancestrula has been found and it is kenozooidal.
Hippothoa peristomata was first discovered in a sample from the Kermadec Ridge but the label with station data was lost. Further, the type material lacked an ancestrula. The species has subsequently been identified three times in later-collected samples—from the outer continental shelf south of White Island, Bay of Plenty, at 165–170 m, on the southern Kermadec Ridge near Rumble III Seamount at 312 m, and on the Louisville Seamount Chain at 1013 m. The substratum is volcanic rock.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Hippothoa peristomata Gordon, 1984
Gordon, Dennis P. 2020 |
Hippothoa peristomata
Gordon, D. P. & Taylor, P. D. & Bigey, F. P. 2009: 291 |
Gordon, D. P. 1984: 111 |