By Ana Ramos*, José Luis Sanz, Fran Ramil and Moustapha Bouzouma
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3D preliminary image obtained with multibeam |
A 3D seismic survey, carried out in 1999-2000 by Woodside Energy Ltd during the exploration of offshore hydrocarbon deposits, revealed the presence of deep-water carbonate mound systems off Mauritania. The system, described by Colman et al. (2005), covers a linear extent of at least 190 km at 450-550 m depth on the continental slope, and could be one of the largest carbonate mounds so far discovered. |
The structure, almost two km wide and 100 meters high over the seabed, runs parallel to the shelf break, always at 450-550 m depth, between two channels 50 meters deep which runs east and west of the main formation. Rough extension of coral-reef from Mauritanian Continental margin (Author: Javier Rey) |
Living exemplaires of deep-water coral together with sessil epifauna at southern reef boundary, near Senegal (Photo: Ana Ramos) |
Samples study suggests that the reef is mostly constituted by death coral (mainly Lophelia pertusa), soaked in an abundant fine and compacted mud; moreover the coral surface was almost devoid of sessile epifauna. Except for its southern part, where some fragments of living L. pertusa were collected (400 gr wet weight!!), the coral seems more eroded and “older” towards the north, being almost fossilized at some places. |
Detail on a living coral with sessil epifauna at southern reef boundary, near Senegal (Photo: Ana Ramos) => |
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<= Sample of death corals mixed with fine mud (Photo: Ana Ramos) |
Fossilized corals (Photo: Ana Ramos) => |
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<= Compacted rock with coral and bivalves shells (Photo: Ana Ramos) |
* Contact:
Ana Ramos Martos
Instituto Español de Oceanografía
Cabo Estai, Canido
E-36200, Vigo (Pontevedra)
Phone: +34 986 492111
ana.ramos@vi.ieo.es






