Role of Near-Bottom Currents in the Distribution of Sediments within the Southern Bay of Campeche, Gulf of Mexico

• Published in: Journal of coastal research Vol. 24; no. 6; pp. 1487 - 1494
• Main Authors: Salas-de-León, David Alberto, Monreal-Gómez, María Adela, Díaz-Flores, Miguel Angel, Salas-Monreal, David, Velasco-Mendoza, Habacuc, Riverón-Enzástiga, Mayra Lorena, Ortiz-Zamora, Glicinia
• Format: Journal Article
• Language: English
• Published: Fort Lauderdale Coastal Education and Research Foundation (CERF) 01.11.2008; Allen Press Inc
• Subjects: Bahía de Campeche; Bay of Campeche; Bottom currents; Bottom sediments; Boundaries; Brackish; Carbonates; Charts; Coastal; Coastal currents; Coasts; corrientes costeras; corrientes de fondo; Data analysis; Dinámica de procesos sedimentarios; Doppler effect; Eddies; Freshwater; Grain size; Gulf of Mexico; Gulfs; Lagoons; Linear equations; Magnetic permeability; Marine; Mathematical models; Ocean currents; Oceanography; River deltas; River discharge; River flow; Rivers; Sediment distribution; Sediment dynamic process; Sediment transport; Sediments; Velocity; ASW, Mexico, Campeche; Mexico, Campeche
• ISSN: 0749-0208; 1551-5036
• DOI: 10.2112/07-0857.1

The sediment distribution in the southern Bay of Campeche is mainly governed by wind-induced currents and mesoscale cyclonic eddies. An increase in sediment grain size toward the sea is attributed to the presence of a convergence zone that sorts the sediments from heavier to lighter. A small anticyclonic eddy near the coast leads to a concentration of sediments westward of the Grijalva-Usumacinta River. We combined current profiles and charts of the distribution of magnetic susceptibility within sediments with a hydrodynamic numerical model to elucidate the distribution of the major sedimentary units in the Southern Bay of Campeche, Gulf of Mexico. Acoustic Doppler current profiles and geostrophic velocity data were used to set the water velocity at the open boundaries of the applied numerical model. The model was forced by the dominant winds. Sediment on the southeastern side of the bay is dominated by carbonates because of a lack of river discharge and other systems that contribute terrigenous sediments. In the southernmost side of the bay, where the major rivers are located, the bottom sediments are mainly of terrigenous origin.