Zinc isotope fractionation during high‐affinity and low‐affinity zinc transport by the marine diatom Thalassiosira oceanica
By S. John, Robin Geis, Mak A. Saito, E. Boyle. 2007
203 citations recorded by the source corpus.
Subfields: Geochemistry and Petrology, Industrial and Manufacturing Engineering, Oceanography
View Paper: https://www.semanticscholar.org/paper/c3fb0d372f3be10b1d10ea5fe4af5d190df3c99f
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Citations in the corpus
- Isotopic fractionation and transport mechanisms of Zn in plants (2009, unknown): “The light δ66Zn values measured in bamboo leaves are very unlikely resulting from external pollution becausemost of the terrestrial values recorded to date have positive δ66Zn (Maréchal et al., 1999; Weiss et al., 2007; John et al., 2007b; Cloquet et al., 2008).”
- A Review of the Stable Isotope Bio-geochemistry of the Global Silicon Cycle and Its Associated Trace Elements (2018, background): “…into diatoms appears to be determined by whether the diatom is utilizing a high or low-affinity Zn transport mechanism, in addition to ambient free Zn2+ concentrations, and is also heavily influenced by surface adsorption and organic matter incorporation (John et al., 2007; Zhao et al., 2014).”
- Zinc Homeostasis and isotopic fractionation in plants: a review (2017, unknown): “Early work in diatoms suggested that plasma membrane transporters discriminate between Zn isotopes (Gélabert et al. 2006; John et al. 2007).”