Rhabdopleura normani Allman
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.10821331 |
persistent identifier |
https://treatment.plazi.org/id/0381104D-FFCD-B95C-EAF0-FA94F190FD4E |
treatment provided by |
Plazi |
scientific name |
Rhabdopleura normani Allman |
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Rhabdopleura normani Allman View in CoL in Norman, 1869
( Fig. 4A, B View FIGURE 4 )
Type locality. Outer Haaf, Unst, Shetland, U.K. at 93 fm (170 m) ( Norman 1869) or 90 fm (~ 165 m) on dead shell ( Allman 1869). Burdon-Jones (1954) cited the locality as c. 40 miles east of the Whalsay Skerries, i.e. c. 60.4° N, 0.48° E.
Key features. Inception of ringed erect tubes is indirect; blind-ending side branches comprise, for about half their length, an adherent portion that abruptly bends at a right angle upwards as an annulated tube ( Fig. 4B View FIGURE 4 ; see Andres 1977, fig. 1, interpretative). Allman (1869, p. 58) noted that adherent and erect parts of each side branch are of the same diameter ( Fig. 4A View FIGURE 4 ) and illustrated the median zigzag suture (ibid., pl. 8, fig. 4), which occupies only about a quarter of tube width. Measured from his drawing, zigzag angles are 54‒61°, mean 57°, with mode 55° (n = 11). Lankester (1884, pl. 39, fig. 1) also illustrated zigzag angles, having a larger range of 36‒60° owing to sinuous bending, with mean 47° and mode = 45° (n = 23), and also showed (ibid., pl. 41, fig. 2) a short ‘permanently closed’ chamber of creeping tube with zigzag angles 33‒43°, mean 40° and mode 40° (n = 8).
Comment. Allman’s material seems not to be represented by a type specimen. There is an unregistered slide in the collection of the Natural History Museum, London, labelled “ Rhabdopleura Normani, Allman. (fide A.M. Norman): no doubt from Shetland ”, with no other information (A. Waeschenbach, NHM, pers. comm., 9 Feb. 2024). The slide contains a dried piece of shell and is inadequate to establish that it represents the non-living material that Allman examined and illustrated. The species needs re-examining on the basis of topotypic material and a neotype established. Other slides (plus wet specimens) of putative R. normani from the NE Atlantic pertain to Hardanger Fjord, Norway. Lankester’s (1884) material, which has aways been regarded as R. normani , came from Hardanger Fjord (Lervik, Stordoe Island), at 40 fm (73 m) on Ascidia mentula . Lankester (1884, p. 623) noted that in 1879 A.M. Norman collected the species at 150 fm (274 m) from the same general locality on Desmophyllum pertusum coral (as Lophelia prolifera ). Unlike Allman, Lankester (1884, p. 630, pl. 38) was able to study the living animal, describing the zooid as having “black and orange-brown pigment, so as to give a spotted leopard-like appearance to the animal.” In comparing R. normani with Rhabdopleura mirabilis ( Sars, 1872) (see below), Lankester (1884, p. 626) concluded: “I do not think that Sars has given sufficient reason to lead to the conclusion that his Rh. Mirabilis is anything more than a variety of Rh. Normani .” Having said that, he did also admit that R. mirabilis does not “quite agree … since the polypide tubes are for no part of their course recumbent, but spring directly from the axis [creeping tube] at right angles to it.” He attributed this lack of correspondence in colony form to the different substratum.
Given its purported common distribution in the northeastern Atlantic (Burdon-Jones 1954), R. normani has been surprisingly little illustrated and redescribed. Maletz et al. (2016), however, photographed erect ringed tubes of R. normani in transparency, sourced from Bergen, Norway, with a scale bar indicating external tube diameter between fusellar collars as 143‒154 (148) μm (n = 10), and fusellus height 24‒41 (33) μm (n = 20).
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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