Clathria (Axosuberites) nidificata ( Kirkpatrick, 1907 )

Schejter, Laura, Cristobo, Javier & Ríos, Pilar, 2024, New records of demosponges (Porifera) from the South Orkney Islands (Antarctica) with a checklist for the region, Zootaxa 5403 (4), pp. 401-430 : 409

publication ID

https://doi.org/ 10.11646/zootaxa.5403.4.1

publication LSID

lsid:zoobank.org:pub:C2EAB19C-07CB-4013-9C93-D25259EA2673

DOI

https://doi.org/10.5281/zenodo.10562140

persistent identifier

https://treatment.plazi.org/id/03D687FD-C503-8251-FF45-FD986DC5BAFA

treatment provided by

Plazi

scientific name

Clathria (Axosuberites) nidificata ( Kirkpatrick, 1907 )
status

 

Clathria (Axosuberites) nidificata ( Kirkpatrick, 1907) View in CoL

( Fig. 3k–n View FIGURE 3 )

Restricted synonymy: Ophlitaspongia nidificata Kirkpatrick, 1907 ; Axociella nidificata ( Kirkpatrick, 1907) .

Material examined: 4 small specimens collected at station 11 ( SOI; 60°53'S, 42°35'W; 487 m; 10/3/2014; MACN-In 44362; IEO-CSIC Col.) GoogleMaps .

Description: Small sponges shrub-like, 3 to 4 cm in height. The living specimens were light brown ( Figure 3k View FIGURE 3 ). Spicules are two categories of styles and toxas. The skeleton of the branches is constituted of a central axis of styles II, echinated by styles I mostly ( Figure 3n View FIGURE 3 ). The styles I are straight and measure 750–1510 / 10–50 μm ( Figure 3l View FIGURE 3 ); styles II are also straight but thinner, 400–590 / 5–10 μm; toxas are numerous and measure 170–600 μm, usually with spined tips ( Figure 3l–n View FIGURE 3 ).

Remarks: Some specimens were epibiotic on dead Caryophyllia corals ( Figure 3k View FIGURE 3 ), that are common corals in the area ( Schejter et al. 2016a), and on pebbles. The specimens here studied were morphologically similar to Artemisima plumosa , but unlike this species, they lack chelae. Clathria (A.) nidificata is well known from Antarctic waters ( Campos et al. 2007; Ríos 2006, Koltun 1964, Fernández et al. 2021), sub-Antarctic regions such as South Georgias Islands ( Koltun 1964), Burdwood bank ( Schejter et al. 2017), and deep sea Argentinean waters ( Burton 1940). This represents the first record for the SOI.

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