Poecillastra ducitriaena Kelly & Cárdenas sp. nov.

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Figs 1, 4, 6

Etymology

Named for the possession of triaenes in addition to the apparent spiculation of Lamellomorpha, and their guide to the phylogenetic origins of this species (‘ duci -’ in the sense of a guide).

Type material

Holotype NEW ZEALAND • Subantarctic region of New Zealand, east of Snares Island Platform, NIWA Station TRIP3072/8; 48.5° S, 168.0° E; depth 125–213 m; 21 Oct. 2010; NIWA 61944 leg.; fish bottom trawl; UPSZTY 178604 (a small piece of the holotype preserved in 70% ethanol, as well as a spicule preparation), NIWA.

Type locality

Subantarctic region of New Zealand, Snares Island Platform, depth 125– 213 m.

Description

Multilamellate, foliose, fan sponge (Fig. 4A), 160 mm high, 104 mm wide, with a short thick stalk about 2 cm thick. Lamella up to 2 cm thick in places, attenuating to curled margins. Oscules were not visible on the holotype. Cribriporal pore areas are widespread between parallel tangential tracts of oxeas; individual pores 80–160 µm in diameter, on both sides of the lamella. Texture firm, compressible, flexible, granular and smooth to the touch. Colour in preservative tan.

Skeleton

Choanosome composed of huge swathes of long straight oxeas, radiating through the lamella, terminating below the surface (Fig. 6E). Contort oxeas are found in the stalk. Ectosome, relatively thick, packed with microxeas and perforated by ostia.

Spicules

MEGASCLERES (Fig. 4 B–C)

Oxeas with long fine attenuated tips, 1725(1150‾2271) × 16(8‾22) µm; contort oxeas in the stalk, 1801(1095‾2671) × 13(5‾17) µm; short-shafted triaenes, relatively uncommon, rhabd straight, attenuating, 290(260‾300) µm, clads curved or acutely bent, occasionally with bifurcating tips, 232(200‾250) µm, cladome width 400‾500 µm long.

MICROSCLERES (Fig. 4 D–F)

Microxeas, heavily microspined, sometimes faintly centrotylote and acutely centrally bent, sharp ended, abundant, 38(28‾46) × 3(2‾4) µm; metaster- to amphiaster-like streptasters with long, microspined rays, rare, 8(5‾12) µm long; spirasters with dense, short rays, rare, 5‾7 µm long.

Distribution

East of Snares Island Platform.

Substrate, depth range and ecology

Attached by a thick stalk to sediment covered rocky substrate, depth 125‾ 213 m.

DNA barcodes

COI. Holotype (MK033626); 28 bp difference with the COI of L. strongylata; 24 bp difference with the COI of Poecillastra compressa (Bowerbank, 1866) (HM592675). 28S (C1-C2). Holotype (MK 033144); 5 bp difference with the 28S (C1-C2) of L. strongylata; 3 bp difference with the 28S (C1-C2) of Poecillastra compressa (HM592757).

Remarks

This remarkable sponge was first identified as a third species of Lamellomorpha, as it appeared to have an almost identical form (stalked, multilamellar fan), a megasclere complement of straight and contort oxeas (more or less restricted to the stalk), small centrotylote microxeas, and metasters (albeit rare). Because the short-shafted triaenes were relatively uncommon, it was initially hypothesised that this was a species of Lamellomorpha with rudimentary triaenes that ‘showed the way’ to the true affinity of the genus with other triaene-bearing Tetractinellida . However, molecular sequencing consistently linked Poecillastra ducitriaena sp. nov. with other Poecillastra species (Fig. 7). Despite its consistency with two independent markers, we note that this grouping is not supported (bootstrap of 60 for COI, of 10 with 28S). This may be due to the absence of other subantarctic Poecillastra species in our sampling which Poecillastra ducitriaena sp. nov. may be closer to (P. Cárdenas, unpublished results).

Although not fully documented (Kelly et al. 2009), our knowledge of Poecillastra in the New Zealand region is reasonable and includes what we consider to be Poecillastra laminaris (Sollas, 1886) (Zeng et al. 2016) and Poecillastra schulzei (Sollas, 1886) . While several undescribed species are known from the New Zealand EEZ, no specimens are known that contain the characteristic contort oxeas of Poecillastra ducitriaena sp. nov.