Francisco José Lobo Sánchez, Francisco Javier Hernández Molina, Andrés Maldonado López, Jesús Galindo Zaldívar, Fernando Bohoyo Muñoz, Yasmina M. Martos Martín, Lara F. Pérez Miguel, José Rodríguez Fernández, Juan Tomás Vázquez
Multibeam bathymetry and parametric echo-sounder profiles show the nature of the surficial morphology and the most recent sub-surface sediment record of Scan Basin, a key area to track the path of bottom waters from Weddell Sea to Scotia Sea. We particularly focus in the southern part of the basin, where the identification of a number of channel-like features records the inception of the Weddell Sea Deep Water (WSDW) in the basin. A clear morphological distinction is observed between channels located at both sides of the basin, which most likely suggest a different degree of interaction between oceanographic and tectonic factors.
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