The family Myriotrochidae Théel (Echinodermata: Holothurioidea) in the deep northeast Atlantic Ocean

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Recent sampling in the Rockall Trough, Porcupine Seabight and Porcupine Abyssal Plain, in the NE Atlantic, has yielded 200 specimens of apodous holothurians belonging to seven species of the family Myriotrochidae Théel from depths between 1000 and 4310 m. These include the type species of a new genus and two new species of existing genera. Parvotrochus belyaevi gen. et sp. nov. is described from some minute specimens from the Rockall Trough that possess both exceptionally small wheel-like deposits and numerous, large curved rods in the body wall and tentacles. Myriotrochus clarki sp. Nov. has affinities to M. vitreus (M. Sars) but shows differences in the shape of the plates of the calcareous ring and in having larger, frequently abnormally formed, wheels. Siniotrochus myriodontus sp. Nov. is similar to the type species of this genus, S. phoxus, Pawson, but differs in the arrangement of the teeth on the wheels. A single small specimen of Prototrochus Belyaev et Mironov from the Whittard Canyon, northern Bay of Biscay, is similar to P. minutus (Östergren), a species known only from the Sea of Japan, but differs in some characteristics of the wheels and tentacles. A new subspecies, P. zenkevitchi rockallensis subsp. nov., is proposed for a form of P. zenkevitchi (Belyaev) that was the most common myriotrochid encountered. P. zenkevitchi was known previously only from a few localities in the Pacific and S Atlantic deep-sea trenches. Similarly, two species previously known only from the NE Pacific, Myriotrochus bathybius H. L. Clark and M. giganteus H. L. Clark, are also recorded from the N Atlantic for the first time. The synonymy of M. giganteus and M. sp. ex gr. macquariensis-giganteus Belyaev et Mironov is proposed. The greatest number both of specimens and species came from the areas most intensively sampled. The present records show that several species have world-wide distributions. The wide geographic separation of many records is the result of both poor sampling effort in the deep sea, particularly with fine-meshed gear, and the difficulties in sampling infaunal animals in the deep sea. Box core samples in the Rockall Trough suggest that the myriotrochids are more common in this area than would be supposed from epibenthic sledge data. Hence, myriotrochids may be more prevalent in the deep sea than previously thought.