Mycale (Aegogropila) sulevoidea Sollas, 1902

Figs 11 a–e, 12a–g, 13a–g, 14, Table 2

Esperella sulevoidea Sollas, 1902: 213, pl. XV fig. 10.

Mycale sulevoidea; Hentschel 1912: 325, pl. 13 fig. 6, pl. 18 fig. 14; Barnes & Bell 2002 a: table 1 (listed only).

? Mycale sulevoidea; Burton 1934: 548; Burton 1959: 228; Vacelet & Vasseur 1971: 86 (no adequate descriptions).

Not: Lévi (1961a: 16); Pulitzer-Finali (1993: 290) = M. (Ae.) orientalis .

Carmia sulevoidea; Thomas 1968: 256, figs 3–4.

Mycale (Aegogropila) sulevoidea; Lim et al. 2008: 102.

Material examined. ZMA Por. 01594, Indonesia, Indonesia, Nusa Tenggara, Solor Islands, Lamakera, 8.4237°S 123.1502°E, depth 20 m, coll. Siboga Expedition, stat. 061, field nr. SE 527 II, 1 May 1899; ZMA Por. 02891, Indonesia, Papua, Aru Islands, Pearl Banks, anchorage off Pulau Jedan, 5.4134°S 134.6677°E, depth 13 m, coll. Siboga Expedition, stat. 273, field nr. SE 144.1, 23 December 1899 ; ZMA Por. 07989, Indonesia, Nusa Tenggara, Sumba, NE coast, reef flat off Melolo, 9.16668°S 120.75°E, depth 1–4 m, coll . R. W.M. van Soest, snorkeling, Indonesian-Dutch Snellius II Expedition stat. 052, field nr. 052 / II/34, red crust on Acropora, 14 September 1984 ; ZMA Por. 08964, Indonesia, Sulawesi, SE Sulawesi, SW Salayar, reef NE of Pulau Bahuluang, 6.45°S 120.43°E, depth 10–15 m, coll . R. W.M. van Soest, SCUBA, Indonesian-Dutch Snellius II Expedition stat. 169, field nr. 169 / IV/35, 30 September 1984 (red crust); ZMA Por. 09555, Singapore, Raffles Lighthouse, 1.2884°N 103.7563°E, littoral, depth 0–2 m, coll. H. Moll, snorkeling, 5 January 1978 (blood-red crust) ; ZMA Por. 12459, Indonesia, Sulawesi, SE Sulawesi, Salayar anchorage and surroundings, 6.0963°S 120.4481°E, depth 0–35 m, coll. Siboga Expedition, stat. 213, field nr. SE 1753I, 26 September 1899 ; ZMA Por. 17808, Kenya, Shimoni Channel, 4. 6667°S 39.3833°E, depth 8–11, coll. Y. Benayahu , SCUBA, field nr. PO 25395, 3 February 2003; ZMA Por. 21702a, Singapore, Pulau Hantu, coll. H. Moll, 21 September 1978 .

Description (Figs 11 a–c). Encrusting, consolidating dead coral rubble. The type was described as creeping with disc-like attachment. Our specimens are similarly patchy, but may also be somewhat thicker forming cushions. Oscules are usually slightly raised above the surface. Sizes usually do not exceed several cm 2. Surface smooth but irregular. Consistency soft. Color where recorded red or blood-red (cf. photo in Lim et al. 2008).

Skeleton (Figs 11 d–e). The ectosomal aegogropila-type skeleton is fairly robust, with intercrossing spicule tracts 30–70 µm in diameter made up of 5–8 spicules in cross section, delimiting triangular meshes of 300–600 µm in size. Variability among the various specimens is large. Several specimens tend to have the ectosomal tracts aligned with sigma I microscleres, but this is not always the case. Rosettes of anisochelae I measure 95–150 µm in diameter and are concentrated near the crossing points of the spicule tracts. Choanosomal tracts in the inner parts of the sponge are separated at approximately 500–800 µm and have a maximum thickness of 120–180 µm. Towards the surface they subdivide into thinner tracts as thin as 40 µm, carrying the surface skeleton. Microscleres are evenly distributed in the ectosomal region, but become scarcer in the interior.

Spicules (Figs 11e, 12 a–g, 13a–g). Mycalostyles, anisochelae in three categories, sigmas in two categories, toxas.

Mycalostyles (Figs 12a,a 1, 13a,a 1), robust, with elongated head and only slightly constricted neck, 286– 370.9 – 465 x 7– 9.2 – 17 µm.

Anisochelae I (Figs 12b, 13b), well-developed alae, including broad upper and lower frontal alae, with shaft approximately 40% of its length free, in side view, the upper frontal alae are flaring outwards, 39– 51.1 – 63 µm.

Anisochelae II (Figs 12c,c 1,c 2, 13c), characteristically duck-bill shaped in side-view (terminology cf. Hajdu et al. 1995 for similar anisochelae in their species Brazilian M. (Ae.) escarlatei); narrow elongated upper alae, with upper frontal alae tapering from distally broad to proximally narrower, curved outwards at the lower rim, causing a curved duckbill-like outline in side view (this varies somewhat among the specimens); free part of the shaft quite short; in dorsal view the spicule is violin-shaped due to upper lateral alae narrow from being expanded distally to become barely thinner than the shaft proximally and subsequently swelling again in the lower alae; spicules robust in comparison with anisochelae II of M. (Ae.) orientalis and they are on average longer in the present species; length quite variable within and among specimens, 24– 34.4 – 47 µm.

Anisochelae III (Figs 12d, 13d,d 1), possibly occurring in two overlapping shapes and sizes; both types are narrow in shape, the larger may be resembling small anisochelae II, the smaller approaching the compact shape found in M. (Ae.) gravelyi and M. (Ae.) orientalis with slightly longer shaft; separation in two distinct spicule types is not quite clear, so we treat them both as growth forms of the same anisochela III, length 11– 16.2 – 24 µm.

Sigmas I (Figs 12e, 13e), robust, with strongly curved apices, length variable among specimens, 76– 102.3 – 130 µm, thickness up to 12 µm.

Sigmas II (Figs 12f, 13f), thin, strongly curved, 17– 25.8 – 35 µm.

Toxas (Figs 12g, 13g), predominantly deeply curved, but more shallow-curved shapes also occur; large variation in size, 22– 93.5 – 240 µm, thickness up to 1.5 µm, almost invariably thinner than the toxas of M. (Ae.) orientalis; in some specimens the toxas were rare.

Distribution and ecology. (Fig. 14) Indonesia, Singapore, Malaysia, India, Kenya, possibly Mozambique, Madagascar and Red Sea, from shallow water down to 20–35 m depth.

Remarks. The assignment to I. Sollas’ Esperella sulevoidea is based especially on the small drawing she presented in pl. XV fig. 10 of the middle-sized category of anisochelae. The type description does not mention presence of sigmas II, but these spicules may often be easily overlooked. Hentschel’s (1912) description of material from the Aru Islands does contain measurements of sigmas II as well as a good description of the characteristic anisochela II. His measurements of the mycalostyles exceed those of Sollas’ and our own measurements (up to 576 µm), but overlaps with our data, and we are confident Hentschel’s material belongs to the present species. This also applies to Thomas’ (1968) record from Palk Bay, India, who provides an excellent description of a ‘brick-red’ specimen collected at 1–2 m depth.

We refrained from distinguishing different discrete types of anisochelae III, which was suggested by Hajdu et al. 1995, as anisochelae III and IV, for the present species. Although we acknowledge that shapes of anisochelae III in M. (Ae.) sulevoidea are more variable than is usual in other species of Mycale, we could not confirm the clear distinctness. In various specimens the variation usually overlapped, both in size and shape. These tiny spicules may likely depend for their shape of a number of factors such as silica content of the environment or growth process.

Burton’s (1934) record of three ‘flagelliform’ specimens of 35 x 1.5 cm from the Great Barrier Reef remains dubious without further information. Such habitus forms have not been encountered in our material. Their shape reminds of Mycale (Zygomycale) parishi (q.v.). Likewise, Burton’s (1959) record of the species from the Red Sea is uncertain due to lack of description.

We made SEM images of 6 specimens, but a detailed comparison of regional specimens is not presented as our specimens were all from the West Pacific except the single specimen from Kenya. This has smaller and thinner mycalostyles, some diversity in shape of anisochelae III, and the toxas were rare. However, the single specimen precludes regional conclusions .

The present species is very similar to M. (Ae.) orientalis, and we compared the two species including spicule sizes (cf. Table 2). The comparison yielded the following differences: (1) the subtly different shape of the upper alae of the anisochelae II (cf. Figs 12c,c 1,c 2), which in the present species are curved abruptly outwards in the lower part of the median alae, whereas these are gradually curved in M.(Ae.) orientalis; moreover in dorsal view the anisochelae differ in the violin-shaped narrowing of the lateral alae in M. (Ae.) sulevoidea opposed to the normal shaped lateral alae in M. (Ae.) orientalis (cf. Figs 5d,d 1), (2) in the larger size of the anischelae II (Table 2), and (3) in the longer and thicker mycalostyles (Table 2). Less clear is the difference in color. M. (Ae.) orientalis is reported to have an orange live color, against the present species reported as red, blood-red or brick-red, but there are currently no live images to further prove this. The here cited alleged differences require further confirmation.

Additional Mycale (Aegogropila) species from the region

Remark. Most of the species listed here have not been examined by us (excepting Mycale (Aegogropila) cavernosa Bergquist, 1965), so their properties can only be derived from the original description and if present subsequent records. It is not certain that they are all valid species. As stated above, we limit the listing to the considered region stretching from the West Pacific Islands in the east, the coasts of East Africa in the west, South China and the Philippines in in the north and northeastern, northern and southwestern parts of Australia.