Rhabdopleura annulata Norman, 1921
publication ID |
https://doi.org/10.11646/zootaxa.5424.3.3 |
publication LSID |
lsid:zoobank.org:pub:524CF65D-F877-42E1-B983-EDC7D3ED1623 |
DOI |
https://doi.org/10.5281/zenodo.10821347 |
persistent identifier |
https://treatment.plazi.org/id/0381104D-FFCA-B95A-EAF0-FECAF5B6FC4A |
treatment provided by |
Plazi (2024-03-15 11:05:36, last updated 2024-11-26 22:49:03) |
scientific name |
Rhabdopleura annulata Norman, 1921 |
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Rhabdopleura annulata Norman, 1921 View in CoL ( Fig. 5B View FIGURE 5 )
Type locality. Western Three Kings Shelf , northernmost New Zealand, 34.4833° S, 172.0500° E, 549 m depth on a stone GoogleMaps .
Key features. Inception of ringed erect tubes is direct. Erect tubes arise directly from the upper surface of primary creeping tubes, having the same width/diameter (erect-tube diameter 169‒213 μm—adding together Norman’s dimensions for internal tube diameter and wall thickness between collars). Erect-tube spacing was described as variable, being close together or 3‒8 mm distant from each other. Very widely transverse zigzag fusellar sutures occur on the creeping tube, with zigzag angles extending onto the flat lateral margins. Mean fusellus height was stated to be 50 μm.
Comment. Gordon et al. (2023, fig. 3a, 6a, b) illustrated and measured a tiny part of the holotype specimen (SEM and LM images), determining that erect tubes were 167‒200 μm diameter (mean 180 μm) between collars, with fusellus height 38‒54 μm (mean 45 μm) and zigzag angles on creeping tubes were 25‒46° (mean 34°). Johnston’s (1937) record of R. annulata from Port Willunga, south of Adelaide, South Australia, was not illustrated and Shepherd (1997) did not cite the provenance of his illustrations of Rhabdopleura in a handbook on marine invertebrates of southern Australia, including Tasmania, so no firm conclusion can be drawn on the identity of southern Australian material. Johnston stated that tube diameter was 265 μm, larger than reported for the New Zealand type locality. Ramírez-Guerrero et al. (2020) recorded R. annulata from Heron Island, Great Barrier Reef.
Gordon, D. P., Quek, Z. B. R., Orr, R. J. S., Waeschenbach, A., Huang, D., Strano, F., Ramsfjell, M. H. & Liow, L. H. (2023) Morphological diversity and a ribosomal phylogeny of Rhabdopleura (Hemichordata: Graptolithina) from the Western Pacific (Singapore and New Zealand), with implications for a re-evaluation of rhabdopleurid species diversity. Marine Biodiversity, 53 (4), 1 - 18. https: // doi. org / 19.1007 / s 12526 - 022 - 01310 - 3
Johnston, T. H. (1937) A note on the occurrence of Rhabdopleura annulata in South Australian waters. Records of the South Australian Museum, 6, 105 - 107.
Norman, J. R. (1921) Rhabdopleura. British Antarctic Terra Nova Expedition Natural History Reports, Zoology, 4, 95 - 102.
Ramirez-Guerrero, G. M., Kocot, K. M. & Cameron, C. B. (2020) Zooid morphology and molecular phylogeny of the graptolite Rhabdopleura annulata (Hemichordata, Pterobranchia) from Heron Island, Australia. Canadian Journal of Zoology, 98, 844 - 849. https: // doi. org / 10.1139 / cjz- 2020 - 0049
FIGURE 5. Original illustrations of three described species of Rhabdopleura characterized by direct-frontal inception of ringed erect tubes (A‒C). Erect-tube inception in R. compacta (D‒F) appears to be a form of indirect erect-tube inception. Note that the direction of zooid budding is the same in A to C. A, Rhabdopleura mirabilis (from Sars 1872, pl. 1, fig. 5). B, Rhabdopleura annulata (from Norman 1921, fig. 4). C, Rhabdopleura recondita (after Beli et al. 2018, fig. 2C). D‒F, Rhabdopleura compacta (respectively after Hincks 1880, pl. 72, fig. 8; Stebbing 1970b, fig. 1; Stebbing 1970a, fig. 3).
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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Graptolithina |
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