Abstract
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.
Highlights
Oxygen minimum zones (OMZ) or suboxic layers are characterized by having oxygen concentrations of
The Gulf of California OMZ is attributed to high rates of primary productivity (Álvarez-Borrego and Lara-Lara 1991) and consequent high respiration rates (Thunell 1998, Delgadillo-Hinojosa et al 2006)
Four hydrographic stations (24, 28, 34, and 38) were considered to study the OMZ because its boundary was located off San Esteban sill (SES)
Summary
Oxygen minimum zones (OMZ) or suboxic layers are characterized by having oxygen concentrations of
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