Chromium in Cascadia Basin, northeast Pacific Ocean
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Cr(VI) reduction has been observed in open-ocean oxygen-minimum zones, but its effect on water-column Cr isotope composition has not been shown in natural samples.
“although the reduction of Cr(VI) in open-ocean OMZ (oxygen-minimum zone) regions has been observed (Cranston and Murray, 1978;Cranston, 1983;Murray et al., 1983;Rue et al., 1997), the actual effect of this process on the Cr isotope composition in the water column has not been demonstrated in natural samples.”
From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Cranston, 1983
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- Authors
- Cranston, R. E.
- Affiliations
- Geological Survey of Canada (CA)
- Corresponding author
- Cranston, R.E.
- Venue
- Marine Chemistry
- Publisher
- Elsevier BV
- Published
- 1983-07
- Volume
- 13
- Issue
- 2
- Pages
- 109-125
- ISSN
- 0304-4203 (ISSN-L)
- OpenAlex
- W1975560893
- Cited by
- 59
- References
- 40
- Citations by year
- 2026: 1 · 2025: 1 · 2024: 1 · 2023: 2 · 2022: 1 · 2021: 11 · 2020: 4 · 2019: 1 · 2018: 2 · 2017: 1 · 2016: 3 · 2015: 1 · 2013: 1
- FWCI
- 2.07
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Marine Chemistry (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Environmental Science › Health, Toxicology and Mutagenesis › Chromium effects and bioremediation
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Keywords
- chromium, hexavalent chromium, dissolved chromium, Cascadia Basin, Northeast Pacific, silica, phosphate, continental margin, turbulent diffusion, advection, trace metal fluxes
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