Dactylocalyx pumiceus Stutchbury, 1841

Moser, Julia, Moraes, Fernando C., Castello-Branco, Cristiana, Pequeno, Carolline B. & Muricy, Guilherme, 2022, Manned submersible dives reveal a singular assemblage of Hexactinellida (Porifera) off the Amazon River mouth, Northern Brazil, Zootaxa 5105 (1), pp. 105-130 : 113-119

publication ID	https://doi.org/ 10.11646/zootaxa.5105.1.4
publication LSID	lsid:zoobank.org:pub:B5C60031-4303-4CBA-A59C-22AE34B73631
DOI	https://doi.org/10.5281/zenodo.6335982
persistent identifier	https://treatment.plazi.org/id/03A687C1-FFE5-1379-B1B1-F9EE4E152E2B
treatment provided by	Plazi
scientific name	Dactylocalyx pumiceus Stutchbury, 1841
status

Treatment

Dactylocalyx pumiceus Stutchbury, 1841 View in CoL

( Figs 6–9 View FIGURE 6 View FIGURE 7 View FIGURE 8 View FIGURE 9 )

Synonymy: Dactylocalyx pumiceus Stutchbury, 1841: 87 ; Gray 1867: 506; Carter 1873: 357; Sollas 1879: 123; Schulze 1887: 348; Reid 1957: 821; Mothes de Moraes 1977: 42; van Soest & Stentoft 1988: 10; Alcolado 2002: 55; Reiswig 2002a: 1296; Mothes et al. 2003: 63; Lopes et al. 2005: 50; Mothes et al. 2006: 58; Muricy et al. 2006: 145; Lopes 2007: 50; Hajdu & Lopes 2007: 354; Vieira et al. 2010: 21; Muricy et al. 2011: 180.

Dactylocalyx ingalli Bowerbank, 1869: 78 .

Dactylocalyx pumiceus var. stutchburyi Sollas, 1879: 131 .

Dactylocalyx subglobosus, Schmidt 1880: 53 ; Schulze 1887: 349 (non Dactylocalyx subglobosus Gray, 1867 ).

Diplacodium mixtum Schmidt, 1880: 57 .

Dactylocalyx patella Schulze, 1886: 85 .

Dactylocalyx potatorum Schmidt, 1880: 53 .

Material examined. MNRJ 21299 View Materials , Brazil, off Pará State, upper slope, 01°31.321’N – 046°44.231’W, 260 m depth, coll. F. Moraes / MV Alucia, submersible Deep Rover, 18.vii.2017 GoogleMaps . MNRJ 21284 View Materials , Brazil, off Maranhão State, upper slope, 00°27.224’S – 043°59.429’W, 210 m depth, coll. R. Moura / MV Alucia, submersible Deep Rover, 15.vii.2017 GoogleMaps .

Material examined for comparison. Dactylocalyx pumiceus USNM 1409958, Dominica, 197 m depth, coll. B. Hoeksema, A. Schrier, B. Brandt & T. Devine, 11.iii.2016. USNM 5424 About USNM , Barbados, 225 m depth, coll. A. Agassiz & C. Sigsbee, 10.iii.1879 .

Diagnosis. Dactylocalyx with thick dictyonal skeleton and fused hexactins; dense small tubule network ramified and irregularly anastomosed. Megascleres asymmetrical pentactins and hexactins, both regular or with long, sinuous, filamentous rays. Microscleres discohexasters, onychohexasters and rare oxyhexasters.

Description. Basiphytous, cup- to barrel or vase-shaped, plate-like or calyciform sponge measuring 22–53 cm long by 17–30 cm wide and 23 mm thick ( Fig. 6A–F View FIGURE 6 ). Surface microhispid, irregular, grooved in both internal and external sides and perforated by small caliber tubules ( Fig. 6G View FIGURE 6 ). Grooves up to 3–30 mm wide and 8–50 mm deep ( Fig. 6F, H View FIGURE 6 ). Color in vivo white, cream or greenish-yellow, becoming white or cream in ethanol. Consistency firm but friable.

Skeleton ( Fig. 7 View FIGURE 7 ): Dictyonal skeleton thick, stout to thin and fragile, tuberculated, forming polygonal meshes (mainly triangular and quadrangular with rounded corners), and with connections tip-to-tip and tip-to-node ( Fig. 7A–D View FIGURE 7 ). Network of small tubules dense, ramified, irregularly anastomosed. Siliceous prominences project through the surface ( Fig. 7A View FIGURE 7 ). Dermalia with fused hexactins, diactins and discohexasters.Atrialia with spined hexactins and pentactins, free or fused to the dictyonalia, diactins, and free hexasters in variable abundance ( Fig. 7D View FIGURE 7 ).

Spicules: Megascleres are fused hexactins and free large diactins, asymmetrical pentactins and hexactins. Microscleres are discohexasters, onychohexasteres and rare oxyhexasters ( Figs 7E–F View FIGURE 7 , 8 View FIGURE 8 , 9 View FIGURE 9 ; Table 2 View TABLE 2 ).

Fused hexactins irregular, asymmetrical, with straight, microspined actins 55–96 µm long by 7–10 µm thick, club-shaped, with expanded, rounded endings ( Fig. 7E–F View FIGURE 7 ).

Large diactins smooth, crossing transversally the skeleton, always broken (not shown). Length> 350 µm, width 10.0–42.9–90.0 µm.

Pentactins asymmetrical, microspined, with tangential rays straight to curved and spines densely distributed along the rays; ends sometimes club-shaped to rounded ( Fig. 8A View FIGURE 8 ). Longer tangential rays 58.0–148.9–390.0 µm in length and shorter tangential rays 30.0–98.0–220.0 µm in length; proximal ray 53.0–276.4–900.0 µm in length. All rays 2.5–3.2–6.3 µm thick. Some pentactins have very long, contorted rays, sometimes branching and forming long, sinuous silica filaments that may connect to the dtctyonalia (present only in MNRJ 21284; Fig. 8B View FIGURE 8 ).

Hexactins asymmetrical, spined, with long, straight to curved rays, that may also branch forming long sinuous filaments ( Fig. 8B View FIGURE 8 ). Ends can be spherical to rounded ( Fig. 8C View FIGURE 8 ). Some spicules have seven actins (heptactins; Fig. 8D View FIGURE 8 ). Longer tangential rays 73.0–175.8–600.0 µm in length; shorter tangential rays 23.0–111.8–360.0 µm long. Proximal ray 85.0–264.6–730.0 µm in length; distal ray 13.0–105.9–600.0 µm in length. All rays 2.5–3.8–10.0 µm thick.

Discohexasters abundant, with short spined primary rays branching in spined secondary rays that end up in umbrellas; diameter 25.0–55.0–80.0 µm ( Fig. 9A View FIGURE 9 ).

Onychohexasters common, with short, spined primary rays branching on spined secondary rays that end up in anchors with two or three v-shaped teeth; diameter 25.0–45.9–68.0 µm ( Fig. 9B View FIGURE 9 ).

Oxyhexasters rare, with short microspined primary rays and long microspined secondary rays, terminating in acerate ends ( Fig. 9C, D View FIGURE 9 ); diameter 43.0–62.0–78.0 µm (n=16).

Geographical and Bathymetric Distribution. Atlantic Ocean: Portugal ( Schulze 1886, 1887 as Dactylocalyx patella ), Bermuda ( Schulze 1887), Florida, USA ( Schmidt 1880 as Diplacodium mixtum ), Cuba ( Schmidt 1880 as Diplacodium mixtum ), Barbados ( Stutchbury 1841; Schulze 1879; van Soest and Stentoft 1988), Northern Brazil (new record), Southeastern Brazil ( Lopes et al. 2005), and Southern Brazil ( Mothes-de-Moraes 1977), from 91 to 1966 m depth. The present record in Northern Brazil fills part of the large gap between the southernmost Caribbean records and Southeastern Brazilian specimens, noted by Lopes et al. (2005).

Ecology. Polychaetes were found associated to the sponge, which was sampled on rocky outcrop and hard carbonate bottoms at 210–260 m depth.

Taxonomic remarks. The genus Dactylocalyx contains only two species, Dactylocalyx pumiceus from Barbados and D. subglobosus Gray, 1867 , probably from the West Indies, exact location unknown ( Reiswig 2002a; de Voogd et al. 2021) They are very similar except by a pear-shaped body and two classes of discohexasters in D. subglobosus versus one class in D. pumiceus ; onychohexasters, oxyhexasters, and irregular pentactins and hexactins with long, sinuous, filamentous rays are absent both in D. subglobosus and in most specimens of D. pumiceus (e.g., Gray 1867; Schulze 1877; Sollas 1879; Mothes-de-Moraes 1977; Reiswig 2002a; Lopes et al. 2005; Tabachnick et al. 2009). Their status as two distinct species needs verification through revision of spicule variability in the many specimens of D. pumiceus that are deposited in zoological collections worldwide ( Reiswig 2002a) and additional collections for molecular studies.

The two populations studied here from Northern Brazil showed variations in body shape, color, substrate and abundance. Specimens sampled off Pará State were white in vivo, large cup- to barrel-shaped, sparse, uncommon (only three individuals were observed), and fixed to the rocky substrate by a large portion of the base or side ( Fig. 6A, B View FIGURE 6 ). In contrast, off Maranhão State, specimens are cream to greenish-yellow in color, have lower cup- to funnel- or plate shape, are fixed on the substrate by a small area or a short peduncle, and are very abundant on hard substrates covered by a thin layer of carbonate sediments ( Fig. 6 View FIGURE 6 C-E). Irregular pentactins and hexactins with long filamentous rays and heptactins are present in MNRJ 21284 from off Maranhão State and absent in MNRJ 21299 from off Pará State, but we cannot extrapolate these characteristics to the whole populations without additional collections. Together, these differences could indicate that our specimens belong to two distinct species, but we described them as conspecific because they fall within the range of variation reported for D. pumiceus in the literature ( Sollas 1879; Mothes-de-Moraes 1977; Reiswig 2002a; Lopes et al. 2005). Additional collections are required to further investigate this issue. We agree with Reiswig (2002a) and Tabachnick et al. (2009) that a comprehensive morphological revision of D. pumiceus is greatly needed, preferably complemented with genetic data.