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

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

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16 Professional Paper NMFS 12 4. Farrea kurilensis ssp. nov. Reiswig and Stone, in preparation Description. Lace-like mass has large-caliber (2-cm diameter), short, branching, and anastomosing tubes increasing in size (of the mass) by lateral growth, conforming, and attaching at multiple sites to the hard substrate and not growing erect. Surface of the mass is labyrinthic, but that of individual tube elements is smooth. Open terminal ends of tubes are effectively oscula. Consistency is flexible but brittle due to fusion of the very thin primary skeleton. Individuals observed in situ have a diameter of 170 cm. Color in life is translucent light blue to white. Skeletal structure. The primary framework is a fused farreoid lattice of hexactins forming a network of square meshes with sides 439–750 µm long; it is continuous throughout the specimen. Loose megascleres include dermal and atrial pentactins, often with knobs or very short distal rays (170–375 µm tangential ray length, 211–422 µm proximal ray length); very large anchorate clavules with completely smooth shafts (302–1243 µm length); moderate-sized uncinates (1.03–2.99 mm length); very rare choanosomal hexactins (208–239 µm ray length). Microscleres consist of two size classes of stellate discohexasters (30–89 µm and 91–293 µm in diameter). Zoogeographic distribution. Locally common and abundant in some areas. In Alaska – central Aleutian Islands. Elsewhere – not reported. Habitat. Attached to bedrock, mudstone, boulders, cobbles, and hexactinellid sponge skeletons at depths between 300 and 2249 m. Remarks. Farrea kurilensis presently has two subspecies: F. k. kurilensis, which occurs near the Kuril Islands and in the Sea of Okhotsk, has smooth pileate clavules, while F. k. beringiana, which also occurs near the Kuril Islands, has all clavules with spines. The new Aleutian subspecies differs from these in having anchorate clavules with smooth shafts and an alternate microsclere combination. Photos. 1) Preserved (frozen then dried) fragment of a specimen collected at a depth of 2105 m in the central Aleutian Islands. Grid marks are 1 cm 2 . 2) The same specimen as in photo 1 in situ.

5. Farrea occa occa Bowerbank, 1862 Description. Lace-like hemispheric mass has largecaliber (1.5 to 2-cm diameter), short, branching and anastomosing tubes increasing in size (of the mass) by lateral growth, attached to hard substrate at central origin and at multiple lateral contact sites. Surface of the mass is labyrinthic with open ends of tubes functioning as oscula, but external and internal surfaces of individual tube elements are smooth. Consistency is flexible but brittle and fragile due to breakage of the very thin fused primary skeleton. An individual mass from a single settled larva may reach 3 m in diameter and over 1 m in height. Color in life is translucent white to pale yellow. Skeletal structure. SEM images of spicules are shown in Appendix IV. The primary framework is a fused farreoid lattice of hexactins forming a network of square meshes with sides 79–494 µm long; it is continuous throughout the specimen. Loose megascleres include dermal and atrial pentactins (190–305 µm tangential ray length, 78–280 µm proximal ray length); pileate and anchorate clavules usually with smooth shafts, rarely with one or two large spines (196–308 µm length); moderatesized uncinates (0.89–2.64 mm length). Microscleres are mainly oxyhexasters with relatively long primary rays (57–111 µm in diameter). There may be a very few discohexasters or onychohexasters. Zoogeographic distribution. Locally common and abundant in some areas. In Alaska – eastern Gulf of Alaska. Elsewhere – cosmopolitan, but the previous known northern limit of the subspecies was 55.4°N in northern British Columbia; the new Alaska collections extend the northern limit to 58.2°N. Habitat. In Alaska – attached to bedrock, boulder, and cobbles at depths between 91 and 238 m. Elsewhere – attached to cobbles, bedrock, shell, coral skeletons, and hexactinellid sponge skeletons at depths between 86 and 1360 m. Remarks. This may be the largest species of sponge in the North Pacific Ocean, with a diameter reaching 3 m. This sponge provides much refuge habitat for small fish and micro-invertebrates that may be forage species for larger fish and crabs. Photos. 1) Fragment of a specimen collected at a depth of 168 m in the eastern Gulf of Alaska. Grid marks are 1 cm 2 . 2) Specimen at a depth of 165 m in the eastern Gulf of Alaska. 17

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

4. Farrea kurilensis ssp. nov. Reiswig and S<strong>to</strong>ne, in preparation<br />

Description. Lace-like mass has large-caliber (2-cm<br />

diameter), short, branching, and anas<strong>to</strong>mosing tubes<br />

increasing in size (<strong>of</strong> <strong>the</strong> mass) by lateral growth, conforming,<br />

and attaching at multiple sites <strong>to</strong> <strong>the</strong> hard<br />

substrate and not growing erect. Surface <strong>of</strong> <strong>the</strong> mass<br />

is labyrinthic, but that <strong>of</strong> individual tube elements is<br />

smooth. Open terminal ends <strong>of</strong> tubes are effectively<br />

oscula. Consistency is flexible but brittle due <strong>to</strong> fusion<br />

<strong>of</strong> <strong>the</strong> very thin primary skele<strong>to</strong>n. Individuals observed<br />

in situ have a diameter <strong>of</strong> 170 cm. Color in life is translucent<br />

light blue <strong>to</strong> white.<br />

Skeletal structure. The primary framework is a fused<br />

farreoid lattice <strong>of</strong> hexactins forming a network <strong>of</strong> square<br />

meshes with sides 439–750 µm long; it is continuous<br />

throughout <strong>the</strong> specimen. Loose megascleres include<br />

dermal and atrial pentactins, <strong>of</strong>ten with knobs or very<br />

short distal rays (170–375 µm tangential ray length,<br />

211–422 µm proximal ray length); very large anchorate<br />

clavules with completely smooth shafts (302–1243<br />

µm length); moderate-sized uncinates (1.03–2.99 mm<br />

length); very rare choanosomal hexactins (208–239<br />

µm ray length). Microscleres consist <strong>of</strong> two size classes<br />

<strong>of</strong> stellate discohexasters (30–89 µm and 91–293 µm in<br />

diameter).<br />

Zoogeographic distribution. Locally common and<br />

abundant in some areas. In Alaska – central Aleutian<br />

Islands. Elsewhere – not reported.<br />

Habitat. Attached <strong>to</strong> bedrock, muds<strong>to</strong>ne, boulders,<br />

cobbles, and hexactinellid sponge skele<strong>to</strong>ns at depths<br />

between 300 and 2249 m.<br />

Remarks. Farrea kurilensis presently has two subspecies:<br />

F. k. kurilensis, which occurs near <strong>the</strong> Kuril Islands<br />

and in <strong>the</strong> Sea <strong>of</strong> Okhotsk, has smooth pileate clavules,<br />

while F. k. beringiana, which also occurs near <strong>the</strong> Kuril<br />

Islands, has all clavules with spines. The new Aleutian<br />

subspecies differs from <strong>the</strong>se in having anchorate clavules<br />

with smooth shafts and an alternate microsclere<br />

combination.<br />

Pho<strong>to</strong>s. 1) Preserved (frozen <strong>the</strong>n dried) fragment <strong>of</strong><br />

a specimen collected at a depth <strong>of</strong> 2105 m in <strong>the</strong> central<br />

Aleutian Islands. Grid marks are 1 cm 2 . 2) The same<br />

specimen as in pho<strong>to</strong> 1 in situ.

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