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dc.contributor.authorHebbeln, Dierk  Concept link
dc.contributor.authorWienberg, Claudia  Concept link
dc.contributor.authorWintersteller, P.  Concept link
dc.contributor.authorFreiwald, Andre  Concept link
dc.contributor.authorBecker, M.  Concept link
dc.contributor.authorBeuck, Lydia  Concept link
dc.contributor.authorDullo, C.  Concept link
dc.contributor.authorEberli, G. P.  Concept link
dc.contributor.authorGlogowski, S.  Concept link
dc.contributor.authorMatos, L.  Concept link
dc.contributor.authorForster, N.  Concept link
dc.contributor.authorReyes-Bonilla, H.  Concept link
dc.contributor.authorTaviani, Marco  Concept link
dc.date.accessioned2014-05-29T20:06:26Z
dc.date.available2014-05-29T20:06:26Z
dc.date.issued2014-04-07
dc.identifier.citationBiogeosciences 11 (2014): 1799-1815en_US
dc.identifier.urihttps://hdl.handle.net/1912/6688
dc.description© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeosciences 11 (2014): 1799-1815, doi:10.5194/bg-11-1799-2014.en_US
dc.description.abstractWith an extension of > 40 km2 the recently discovered Campeche cold-water coral province located at the northeastern rim of the Campeche Bank in the southern Gulf of Mexico belongs to the largest coherent cold-water coral areas discovered so far. The Campeche province consists of numerous 20–40 m-high elongated coral mounds that are developed in intermediate water depths of 500 to 600 m. The mounds are colonized by a vivid cold-water coral ecosystem that covers the upper flanks and summits. The rich coral community is dominated by the framework-building Scleractinia Enallopsammia profunda and Lophelia pertusa, while the associated benthic megafauna shows a rather scarce occurrence. The recent environmental setting is characterized by a high surface water production caused by a local upwelling center and a dynamic bottom-water regime comprising vigorous bottom currents, obvious temporal variability, and strong density contrasts, which all together provide optimal conditions for the growth of cold-water corals. This setting – potentially supported by the diel vertical migration of zooplankton in the Campeche area – controls the delivering of food particles to the corals. The Campeche cold-water coral province is, thus, an excellent example highlighting the importance of the oceanographic setting in securing the food supply for the development of large and vivid cold-water coral ecosystems.en_US
dc.description.sponsorshipThe research leading to these results has received support from the Deutsche Forschungsgemeinschaft (DFG) through funding of the WACOM – West Atlantic Cold-water Coral Ecosystems projects, grants HE 3412/17-1 and DU 129/47-1, and through providing ship time. A. Freiwald received funds from the Hessian LOEWE BiK-F Project A3.10, and G. P. Eberli acknowledges the donors of the American Chemical Society Petroleum Research Fund (grant no. 49017-ND8) for partial support of this research and the industrial associates of the CSL – Center for Carbonate Research at the University of Miami for additional funding. L. Matos has been supported by the FCT scholarship SFRH/BD/72149/2010.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherCopernicus Publications on behalf of the European Geosciences Unionen_US
dc.relation.urihttps://doi.org/10.5194/bg-11-1799-2014
dc.rightsAttribution 3.0 Unported*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/
dc.titleEnvironmental forcing of the Campeche cold-water coral province, southern Gulf of Mexicoen_US
dc.typeArticleen_US
dc.identifier.doi10.5194/bg-11-1799-2014


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