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Depth-related distribution and abundance of seastars (Echinodermata: Asteroidea) in the Porcupine Seabight and Porcupine Abyssal Plain,N.E. Atlantic
Institution:1. Department of Biology, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA;2. Life Sciences, The Natural History Museum, Cromwell Road, London, SW7 5BD, UK;3. School of Ocean and Earth Sciences, University of Southampton, Southampton, United Kingdom;4. Minderoo-UWA Deep-Sea Research Centre, School of Biological Sciences and Oceans Institute, The University of Western Australia (M090), 35 Stirling Highway, Perth, WA, 6009, Australia;5. British Geological Survey, Lyell Centre, Research Avenue South, Edinburgh, EH14 4AP, UK;6. School of Energy, Geoscience, Infrastructure and Society, Institute of Life and Earth Sciences, Heriot-Watt University, Edinburgh, UK, EH14 4AS, UK;1. Key Laboratory of Marine Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China;2. School of Oceanography, Shanghai Jiao Tong University, Shanghai, China;3. Centre de Recherche en Paléontologie – Paris, Sorbonne Université, 4 place Jussieu, 75005 Paris, France;4. Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC, USA;5. Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution, Washington, DC, USA;6. Départment Origines et Évolution, Muséum National d''Histoire Naturelle, Paris, France;7. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China
Abstract:The depth-related distribution of seastar (Echinodermata: Asteroidea) species between 150 and 4950 m in the Porcupine Seabight and Porcupine Abyssal Plain is described. 47 species of asteroid were identified from ~14,000 individuals collected. The bathymetric range of each species is recorded. What are considered quantitative data, from an acoustically monitored epibenthic sledge and supplementary data from otter trawls, are used to display the relative abundance of individuals within their bathymetric range. Asteroid species are found to have very narrow centres of distribution in which they are abundant, despite much wider total adult depth ranges. Centres of distribution may be skewed. This might result from competition for resources or be related to the occurrence of favourable habitats at particular depths. The bathymetric distributions of the juveniles of some species extend outside the adult depth ranges. There is a distinct pattern of zonation with two major regions of faunal change and six distinct zones. An upper slope zone ranges from 150 to ~700 m depth, an upper bathyal zone between 700 and 1100 m, a mid-bathyal zone from 1100 to1700 m and a lower bathyal zone between 1700 and 2500 m. Below 2500 m the lower continental slope and continental rise have a characteristic asteroid fauna. The abyssal zone starts at about 2800 m. Regions of major faunal change are identified at the boundaries of both upper and mid-bathyal zones and at the transition of bathyal to abyssal fauna. Diversity is greatest at ~1800 m, decreasing with depth to ~2600 m before increasing again to high levels at ~4700 m.
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