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A guide to the deep-water sponges of - NMFS Scientific Publications ...

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46 Pr<strong>of</strong>essional Paper <strong>NMFS</strong> 12<br />

30. Poecillastra tenuilaminaris (Sollas, 1886)<br />

Description. This sponge is polymorphic but typically<br />

has a plate-like or lamellar growth form. The surface <strong>of</strong><br />

<strong>the</strong> sponge is smooth <strong>to</strong> <strong>the</strong> unaided eye but microscopically<br />

hispid. Small oscula occur on one side only. The<br />

consistency is firm, incompressible, and fragile. Size is<br />

highly variable but attains a length and height exceeding<br />

more than 1 m. Color in life is whitish <strong>to</strong> light brown,<br />

<strong>of</strong>ten with a dark fringe at <strong>the</strong> distal edge.<br />

Skeletal structure. The choanosome consists <strong>of</strong> an<br />

unorganized mix <strong>of</strong> calthrops and oxeas: calthrops<br />

(320–540 × 35–48 µm per ray), occasionally triods with<br />

rays <strong>of</strong> <strong>the</strong> same size, oxeas (1240–2650 × 32–47 µm).<br />

Microscleres are streptasters (14–28 µm) and acanthose<br />

microxeas (117–157 × 3–5 µm) that are always bent in<br />

<strong>the</strong> middle.<br />

Zoogeographic distribution. Common. In Alaska –<br />

Bering Sea (Zhemchug Canyon) and eastern Gulf <strong>of</strong><br />

Alaska. May reach densities up <strong>to</strong> 19 per m 2 in eastern<br />

Gulf <strong>of</strong> Alaska habitats. Elsewhere – holotype described<br />

from Sea <strong>of</strong> Japan, also reported from along <strong>the</strong> California<br />

Coast and <strong>the</strong> Gulf <strong>of</strong> California. Present records<br />

strongly suggest a circumboreal distribution in <strong>the</strong><br />

North Pacific. However, morphological differences do<br />

exist between populations, suggesting some genetic<br />

isolation (see Remarks).<br />

Habitat. In Alaska – attached <strong>to</strong> bedrock at depths<br />

between 149 and 486 m in <strong>the</strong> Bering Sea and attached<br />

<strong>to</strong> bedrock, boulders, and cobbles at depths between<br />

71 and 255 m in <strong>the</strong> eastern Gulf <strong>of</strong> Alaska. Elsewhere<br />

– reported at depths <strong>to</strong> 74 m.<br />

Remarks. Previously known as Normania tenuilaminaris<br />

Sollas 1886, P. tenuilaminaris was originally described as<br />

having straight acanthose microxeas. The microxeas we<br />

examined from <strong>the</strong> Bering Sea specimens were consistently<br />

bent but this is <strong>the</strong> only difference between <strong>the</strong><br />

specimens and in our opinion not sufficient <strong>to</strong> separate<br />

<strong>the</strong> specimens at <strong>the</strong> species level. However, it is probable<br />

that <strong>the</strong> Bering Sea population is genetically isolated<br />

and may have developed different morphological<br />

characters, such as <strong>the</strong> bent microxeas. This species is<br />

preyed upon by <strong>the</strong> sea stars Hippasteria spp., Poraniopsis<br />

inflata, Pteraster tesselatus, Ceramaster patagonicus, and<br />

possibly Henricia longispina. We have observed a very<br />

similar sponge in <strong>the</strong> central Aleutian Islands at depths<br />

between 142 and 1386 m but we would need <strong>to</strong> collect<br />

a specimen <strong>to</strong> confirm conspecificity.<br />

Pho<strong>to</strong>s. 1) Fragments <strong>of</strong> specimen collected at a depth<br />

<strong>of</strong> 175 m in <strong>the</strong> eastern Gulf <strong>of</strong> Alaska. Note <strong>the</strong> hydroids<br />

growing on <strong>the</strong> fringe. Grid marks are 1 cm 2 . 2) Same<br />

specimen as in pho<strong>to</strong> 1 in situ. 3) Specimen collected<br />

at a depth <strong>of</strong> 486 m in Zhemchug Canyon, Bering Sea.<br />

Grid marks are 1 cm 2 .

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