“…Coastal upwelling is not only an important source of nutrient-rich waters to the RC, but it is also a source of trace metals, particularly of those with a nutrient-type distribution, such as cadmium (Bruland et al, 1978). Previous studies carried out along the CCS have shown that upwelling is the principal mechanism delivering cadmium to superficial waters off the coast of Washington (van Geen and Husby, 1996), Oregon (Takesue and van Geen, 2002) the northern CCS (Bruland, 1980;, and Baja California in the southern part of the CCS (Sañudo-Wilhelmy and Flegal, 1991;Segovia-Zavala et al, 1998;Takesue et al, 2004). In the upwelling area off the coast of California and Oregon (USA), for example, dissolved cadmium (Cd d ) has been proposed as a tracer of upwelled waters (van Geen et al, 1992;van Geen and Husby, 1996;Takesue and van Geen, 2002); however, it is not known how Cd concentrations are modified once these Cd-rich upwelled waters enter o remain within a RC, especially in those centers where this "confinement" results in increased phytoplankton growth and, in consequence, biological removal of nutrients and trace metals.…”