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Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.
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| one publication added to basket [209280] |
Morphology and environment of cold-water coral carbonate mounds on the NW European margin
Wheeler, A.J.; Beyer, A.; Freiwald, A.; de Haas, H.; Huvenne, V.A.I.; Kozachenko, M.; Olu-Le Roy, K.; Opderbecke, J. (2007). Morphology and environment of cold-water coral carbonate mounds on the NW European margin. Int. J. Earth Sci. 96(1): 37-56. dx.doi.org/10.1007/s00531-006-0130-6
In: International Journal of Earth Sciences. Springer: Berlin; Heidelberg. ISSN 1437-3254; e-ISSN 1437-3262, meer
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| Trefwoord |
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| Author keywords |
Carbonate mound; Cold-water coral; Morphology; Environmental setting; Seabed mapping |
| Auteurs | | Top |
- Wheeler, A.J., meer
- Beyer, A.
- Freiwald, A., meer
- de Haas, H., meer
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- Huvenne, V.A.I., meer
- Kozachenko, M.
- Olu-Le Roy, K.
- Opderbecke, J.
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| Abstract |
Cold-water coral carbonate mounds, owing their presence mainly to the framework building coral Lophelia pertusa and the activity of associated organisms, are common along the European margin with their spatial distribution allowing them to be divided into a number of mound provinces. Variation in mound attributes are explored via a series of case studies on mound provinces that have been the most intensely investigated: Belgica, Hovland, Pelagia, Logachev and Norwegian Mounds. Morphological variation between mound provinces is discussed under the premise that mound morphology is an expression of the environmental conditions under which mounds are initiated and grow. Cold-water coral carbonate mounds can be divided into those exhibiting “inherited” morphologies (where mound morphology reflects the morphology of the colonised features) and “developed” morphology (where the mounds assume their own gross morphology mainly reflecting dominant hydrodynamic controls). Finer-scale, surface morphological features mainly reflecting biological growth forms are also discussed. |
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