The Moira Mounds, small cold-water coral banks in the Porcupine Seabight, NE Atlantic: Part A an early stage growth phase for future coral carbonate mounds?

Type Article
Date 2011-03
Language English
Author(s) Wheeler A. J.1, 2, Kozachenko M.3, Henry L. -A.4, Foubert A.5, de Haas H.6, Huvenne V. A. I.7, Masson D.C.7, Olu KarineORCID8
Affiliation(s) 1 : Univ Coll, Dept Geol, Cork, Ireland.
2 : Univ Coll, Environm Res Inst, Cork, Ireland.
3 : Univ Coll Cork, Coastal & Marine Resources Ctr, Environm Res Inst, Cobh, Cork, Ireland.
4 : Scottish Assoc Marine Sci, Oban PA37 1QA, Argyll, Scotland.
5 : Katholieke Univ Leuven, Dept Earth & Environm Sci, B-3001 Heverlee, Belgium.
6 : Royal Netherlands Inst Sea Res NIOZ, NL-1790 AB Den Burg, Netherlands.
7 : Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England.
8 : IFREMER, Ctr Brest, F-29280 Plouzane, France
Source Marine Geology (0025-3227) (Elsevier Science Bv), 2011-03 , Vol. 282 , N. 1-2 , P. 53-64
DOI 10.1016/j.margeo.2010.08.006
WOS© Times Cited 24
Keyword(s) cold-water coral, coral carbonate mound, benthic processes, biogeological processes, marine geology, NE Atlantic
Abstract This paper presents a comprehensive overview of the Moira Mounds in the Porcupine Seabight, combining a review of currently published material with new data and interpretations. The Moira Mounds are circular to ovoid-shaped individual or clustered coral banks (referred to as "scleractinian spaced cluster macroreefs") located in the Belgica (carbonate) mound province, Porcupine Seabight, west of Ireland. They are up to 10 m high and 20 to 35 m in diameter. For the first time, a map showing the complete extent and location of the Moira Mounds is published, revealing 256 examples grouped into four areas mainly between 800 and 1100 m water depth. ROV groundtruthing revealed the importance of bedload sand transport in Moira Mound formation and development processes through sediment entrapment by coral frameworks (Lophelia pertusa and Madrepora oculata). New estimated growth rates for the Moira Mounds are comparable to those measured for much larger Irish coral carbonate mounds but an order of magnitude lower than rates from comparably sized reefs offshore Norway. As well as the framework corals. 26 macrobenthic invertebrate species were identified from a single box core that were similar to those communities found in adjacent off-mound habitats. It is proposed that the Moira Mounds are an example of the early stage growth phase of nearby giant coral carbonate mounds and represent a westward extension of the zone of active cold-water coral mound growth and therefore a deepening of the zone of cold-water coral growth over recent climate cycles. (C) 2010 Elsevier B.V. All rights reserved.
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Wheeler A. J., Kozachenko M., Henry L. -A., Foubert A., de Haas H., Huvenne V. A. I., Masson D.C., Olu Karine (2011). The Moira Mounds, small cold-water coral banks in the Porcupine Seabight, NE Atlantic: Part A an early stage growth phase for future coral carbonate mounds? Marine Geology, 282(1-2), 53-64. Publisher's official version : https://doi.org/10.1016/j.margeo.2010.08.006 , Open Access version : https://archimer.ifremer.fr/doc/00035/14633/