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Dissolved iron (Fed) concentrations are reported for the Gulf of California oxygen minimum zone (OMZ), which was located in front of San Esteban sill, between Subtropical Subsurface Water (SSW) and Pacific Intermediate Water. Mean Fed concentration in the OMZ was 3.84 ± 2.48 nM, with minimum and maximum values of 1.48 and 10.02 nM. These concentrations are higher and are enriched in relation to the Tropical Northeast Pacific Ocean OMZ (0.25–1.2 nM), whose waters enter the gulf through SSW. Sediment resuspension and Fed-enriched waters cause the observed Fe increase at the stations located near San Esteban sill. On the other hand, the relatively lower Fed concentrations found at the stations farthest from the sill are the result of denitrification in the suboxic zone.   Se registran concentraciones de hierro disuelto (Fed) en la zona del minimo de oxigeno (ZMO) del golfo de California, que se ubico frente al relieve del umbral de San Esteban y entre el Agua Subsuperficial Subtropical (ASS) y el Agua Intermedia del Pacifico. La concentracion promedio de Fed en la ZMO fue de 3.84 ± 2.48 nM, con un valor minimo de 1.48 nM y un maximo de 10.02 nM. Estas concentraciones son mayores y estan enriquecidas (8:1) en relacion con las de la ZMO del oceano Pacifico Nororiental Tropical (0.25–1.2 nM), cuyas aguas ingresan al golfo de California mediante el ASS. La resuspension de sedimentos y aguas ricas en Fed provocan el incremento de este metal en las estaciones aledanas al umbral de San Esteban. Por otro lado, los valores relativamente menores son producto de la desnitrificacion en la zona suboxica en las estaciones mas alejadas del umbral de San Esteban

Concentration of dissolved iron in the oxygen minimum zone off San Esteban sill, Gulf of California