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dc.contributor.authorJohnson, Mark P.
dc.contributor.authorWhite, Martin
dc.contributor.authorWilson, Annette
dc.contributor.authorWürzberg, Laura
dc.contributor.authorSchwabe, Enrico
dc.contributor.authorFolch, Helka
dc.contributor.authorAllcock, A. Louise
dc.date.accessioned2018-09-20T16:12:07Z
dc.date.available2018-09-20T16:12:07Z
dc.date.issued2013-11-18
dc.identifier.citationJohnson, Mark P. White, Martin; Wilson, Annette; Würzberg, Laura; Schwabe, Enrico; Folch, Helka; Allcock, A. Louise (2013). A vertical wall dominated by acesta excavata and neopycnodonte zibrowii, part of an undersampled group of deep-sea habitats. PLoS ONE 8 (11),
dc.identifier.issn1932-6203
dc.identifier.urihttp://hdl.handle.net/10379/12101
dc.description.abstractWe describe a novel biotope at 633 to 762 m depth on a vertical wall in the Whittard Canyon, an extensive canyon system reaching from the shelf to the deep sea on Ireland's continental margin. We explored this wall with an ROV and compiled a photomosaic of the habitat. The assemblage contributing to the biotope was dominated by large limid bivalves, Acesta excavata (mean shell height 10.4 cm), and deep-sea oysters, Neopycnodonte zibrowii, at high densities, particularly at overhangs. Mean density of N. zibrowii increased with depth, with densities of the most closely packed areas of A. excavata also increasing with depth. Other taxa associated with the assemblage included the solitary coral Desmophyllum dianthus, cerianthid anemones, comatulid crinoids, the trochid gastropod Margarites sp., the portunid crab Bathynectes longispina and small fish of the family Bythitidae. The scleractinian coral Madrepora oculata, the pencil urchin Cidaris cidaris and a species of Epizoanthus were also common. Prominent but less abundant species included the flytrap anemone Actinoscyphia saginata, the carrier crab Paramola cuvieri, and the fishes Lepidion eques and Conger conger. Observations of the hydrography of the canyon system identified that the upper 500 m was dominated by Eastern North Atlantic Water, with Mediterranean Outflow Water beneath it. The permanent thermocline is found between 600 and 1000 m depth, i.e., in the depth range of the vertical wall and the dense assemblage of filter feeders. Beam attenuation indicated nepheloid layers present in the canyon system with the greatest amounts of suspended material at the ROV dive site between 500 and 750 m. A cross-canyon CTD transect indicated the presence of internal waves between these depths. We hypothesise that internal waves concentrate suspended sediment at high concentrations at the foot of the vertical wall, possibly explaining the large size and high density of filter-feeding molluscs.
dc.publisherPublic Library of Science (PLoS)
dc.relation.ispartofPLoS ONE
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Ireland
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/ie/
dc.subjectocean margin exchange
dc.subjectinternal waves
dc.subjectbenthic fauna
dc.subjectcoral-reefs
dc.subjectpropagation
dc.subjectbiscay
dc.subjectslope
dc.subjectatlantic
dc.subjectcanyon
dc.subjectbay
dc.titleA vertical wall dominated by acesta excavata and neopycnodonte zibrowii, part of an undersampled group of deep-sea habitats
dc.typeArticle
dc.identifier.doi10.1371/journal.pone.0079917
dc.local.publishedsourcehttps://doi.org/10.1371/journal.pone.0079917
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