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Deep water bioherms of the scleractinian coral Lophelia pertusa(L.) at 64° n on the Norwegian shelf: Structure and associated megafauna
Abstract
Megafauna on bioherms (large biological structures) of the scleractinian coral Lophelia pertusa at 240-290 m depth in the Haltenbanken- Fmyabanken area was investigated by video-recording. Sixteen transects from soft bottom with scattered patches of stones below bioherms to top of bioherms were analysed. Fauna patterns were related to the near-bottom currents. The orientation of the gorgonianParamuricea placomus was used as an indicator of the direction of the main currents at the bioherms. The bioherms were 2 to 31 m high, and had a basal area ranging from 1 500 to 50 600 m2. 36 taxa were identified, of which five taxa only occurred on the bioherms, and five only on the soft bottom with scattered stones. The diversity, H', was highest in the zone of dead Lophelia, and lowest on the silty clay. None of the 26 taxa observed on stones were spesific for this habitat, but occurred also on the bioherms or the soft bottom. The area with Lophelia rubble, near the basis of the bioherms, had the lowest number of taxa (15), but the highest average density of individuals (7.92 ind./1Om2). Different sponges, gorgonians (Paragorgia arborea, Paramuricea placomus, Primnoa resedaeformis), squat lobsters (Munida sarsi), redfish (Sebastes spp.) and saithe (Pollachius virens) dominated in terms of individuals per area. Diversity, density of sponges and density of gorgonians were highest on the down-current side of the bioherms. Saithe were observed with highest densities near the basis of the bioherms, on the up-current side, while redfish had highest densities on the parallel-current side of the bioherm top. These results indicate that near bottom currents and turbulence are factors affecting the fauna on Lophelia bioherms.
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Cited by
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Ramirez-Llodra, E., Brandt, A., Danovaro, R., De Mol, B., Escobar, E., German, C. R., Levin, L. A., Martinez Arbizu, P., Menot, L., Buhl-Mortensen, P., et al. (2010) · Biogeosciences · doi:10.5194/bg-7-2851-2010 · Cited by 913
Self-citationRogers, A. D. (1999) · International Review of Hydrobiology · doi:10.1002/iroh.199900032 · Cited by 435
Large deep-water coral banks in the Porcupine Basin, southwest of Ireland
De Mol, B., Van Rensbergen, P., Pillen, S., Van Herreweghe, K., Van Rooij, D., McDonnell, A., Huvenne, V, Ivanov, M., Swennen, R., & Henriet, J. P. (2002) · Marine Geology · doi:10.1016/s0025-3227(02)00281-5 · Cited by 313
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Metadata
- Authors
- Mortensen, P. B., Hovland, M., Brattegard, T., & Farestveit, R.
- Venue
- Sarsia
- Publisher
- Informa UK Limited
- Published
- 1995-11-07
- Volume
- 80
- Issue
- 2
- Pages
- 145-158
- ISSN
- 0036-4827 (ISSN-L)
- OpenAlex
- W2316193362
- Cited by
- 238
- References
- 0
- FWCI
- 2.16
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: Deep water bioherms of the scleractinian coral Lophelia pertusa(L.) at 64° n on the Norwegian shelf: Structure and associated megafauna. https://app.cochat.ai/papers/10.1080/00364827.1995.10413586
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- Mortensen, P. B., Hovland, M., Brattegard, T., & Farestveit, R. (1995). Deep water bioherms of the scleractinian coral Lophelia pertusa(L.) at 64° n on the Norwegian shelf: Structure and associated megafauna. Sarsia. https://doi.org/10.1080/00364827.1995.10413586
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