Publication Date:
2022-05-26
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.
Description:
With 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.
Description:
The 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.
Repository Name:
Woods Hole Open Access Server
Type:
Article
Format:
application/pdf
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