The stable chromium (Cr) isotope system is an emerging paleoredox proxy. Interpretation of sedimentary and seawater δ53Cr (53Cr/52Cr relative to SRM 979) hinges on our understanding of the isotopic fractionations during Cr sequestration from seawater to sediments. Seawater δ53Cr values reported thus far are for total dissolved Cr. This study reports the δ53Cr of both dissolved Cr (III) and dissolved Cr (VI) across the oxygen minimum zone in the eastern tropical North Pacific off Manzanillo, Mexico. Dissolved Cr (III) accounts for 48% to 54% total dissolved Cr in this region. There are no correlations between O2 and Cr concentrations, or O2 concentrations and δ53Cr throughout the water column. The δ53Cr of Cr (III) is lower than that of Cr (VI) by a relatively constant offset (0.42 ± 0.15‰, 1σ, n = 5) and is also uncorrelated with dissolved O2 concentration. These observations provide part of the foundation for using δ53Cr of the authigenic Cr in organic‐rich shales to reconstruct seawater δ53Cr. A survey of growing literature Cr concentration and δ53Cr data suggests that the Cr isotope fractionation factor in the global ocean is likely more complex than previously thought. More future species‐dependent Cr isotope studies could shed new light on the biogeochemical processes controlling the oceanic Cr isotope fractionation.

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