Suberites cebriones Morozov et al. 2019
publication ID |
https://doi.org/ 10.11646/zootaxa.5357.1.2 |
publication LSID |
lsid:zoobank.org:pub:B9D8C271-2781-43D7-A9CB-629CCC0EF7FC |
DOI |
https://doi.org/10.5281/zenodo.10012509 |
persistent identifier |
https://treatment.plazi.org/id/03D17677-FFCE-194D-B78F-FF61F51D2BDD |
treatment provided by |
Plazi |
scientific name |
Suberites cebriones Morozov et al. 2019 |
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Suberites cebriones Morozov et al. 2019 View in CoL
( Fig. 3a–h View FIGURE 3 )
Material analyzed. Laptev Sea, MMBI trawl survey 2014, st. A-66 (77.2316N, 137.065E), depth 33 m (1 specimen; KFU-LH-2/006); GoogleMaps st. A-24 (76.2616N, 139.0433E), depth 15 m (1 specimen; KFU-LH-2/007); GoogleMaps st. L-19 (75.1983N, 128.4633E), depth 45 m (1 specimen; KFU-LH-2/008) GoogleMaps .
Description. Sponge has the shape of a shallow cup, up to 3.5 by 4 cm, with walls about 1.5 cm thick and the depression around 1 cm deep ( Fig. 3h View FIGURE 3 ). Body is attached by a weak, ill-developed stalk to the substrate, usually enveloping a polychaete tube or small pebbles. Surface smooth and even. Texture firm and almost incompressible, easily cut. Oscula in young specimens are inconspicuous. In adult specimens there is a sieve pore area at the bottom of depression. Colour beige.
Spicules. Megascleres fall into three distinct categories, viz. choanosomal subtylostyles and ectosomal tylostyles, with some specimens additionally containing stocky strongyles. The latter are never very abundant, usually 10–15 spicules per microscopic slide. Thus, a careful examination is required.
Large cylindrical subtylostyles ( Fig. 3a–a View FIGURE 3 1 View FIGURE 1 ) with only barely visible basal swelling, straight or slightly curved, rather short-pointed: 334–418±46–527 × 6.9–8.6±1.3–10.5 (n = 60) µm. Small tylostyles ( Fig. 3b–b View FIGURE 3 1 View FIGURE 1 ), slightly fusiform, short-pointed: 173–273±58–458 × 5–7±1.5–9.7 (n = 50) µm. Large, stocky strongyles ( Fig. 3c View FIGURE 3 ), occasionally tylostrongyles: 79–166±48–300 × 10.6–13±2–18 (n = 30). Microscleres are exclusively microspined, ranging in shape from microstrongyles to microstyles and microxeas ( Fig. 3d–f View FIGURE 3 ). Dimensions: microstrongyles, 11– 18.3±5.8–36.8 (n = 80) µm; microxeas, 30–41±8.4–57 (n = 140) µm; microstyles, 16–25.2±3.8–35 (n = 30) µm.
Skeleton. Choanosomal skeleton is a confused, almost halichondroid reticulation of large subtylostyles, cemented by a dense mass of microrhabds. In the ectosome there are well-defined bouquets of tylostyles, reinforced with a thick (up to ~ 100 µm) layer of microrhabds.
Remarks. Koltun (1966) recognized two morphotypes of S. domuncula var. ficus (= S. lutkenii ) from the Barents and Laptev Seas (see Koltun 1966, Pl. XXXIV, figs. 1–3). Recently Morozov et al. (2019) recognized the same two morphotypes in the Laptev Sea, which they differentiated into separate species, viz. S. montalbidus (= S. lutkenii ) and S. cebriones . Apart from differences in gross morphologies (fig-shaped vs. cup-shaped forms; corrugated vs. smooth surfaces) there are skeletal characters that are useful in species identification: as opposed to S. lutkenii , microrhabds in S. cebriones are distributed throughout both ectosome and choanosome in abundance. Additionally, microxeas in S. cebriones are much more stocky: a ratio of length to width in S. cebriones on average is 30% lower, compared to that of S. lutkenii (p value <0.001).
Suberites cebriones is an eastern-Arctic species, whose geographic range limits to the west are confined to the New Siberian Shoal area at the border between Laptev and East-Siberian Seas. It’s currently unknown how far eastwards along the Siberian coasts this species can be found, yet it apparently has a close relative, S. mineri ( Laubenfels 1935) , from the North Pacific.
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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