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Kathleen Scheiderich

Researcher at United States Geological Survey

Publications -  16
Citations -  683

Kathleen Scheiderich is an academic researcher from United States Geological Survey. The author has contributed to research in topics: Isotope fractionation & Water column. The author has an hindex of 8, co-authored 14 publications receiving 580 citations. Previous affiliations of Kathleen Scheiderich include University of Delaware & Commonwealth Scientific and Industrial Research Organisation.

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Copper speciation and isotopic fractionation in plants: uptake and translocation mechanisms.

TL;DR: The lack of isotopic discrimination in oat plants suggests that Cu uptake and translocation are not redox selective, and the presence of isotopically light Cu in tomatoes is attributed to a reductive uptake mechanism, andThe isotopic shifts within various tissues are attributed to redox cycling during translocation.
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Global variability of chromium isotopes in seawater demonstrated by Pacific, Atlantic, and Arctic Ocean samples

TL;DR: In this article, the authors presented multiple sites in the Arctic Ocean, and three locations in the Atlantic and Pacific Oceans, where the highest δ53Cr values occur in Pacific-sourced waters, which also have the lowest Cr concentration.
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Copper Isotope Fractionation during Equilibration with Natural and Synthetic Ligands

TL;DR: The results show that complexation of Cu by organic ligands can affect the isotopic signature of the free Cu ion, which is considered the most bioavailable species, and highlight the importance of understanding fractionation processes in the uptake medium when using Cu isotopes to study the uptake mechanisms of organisms.
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Molybdenum isotope, multiple sulfur isotope, and redox-sensitive element behavior in early Pleistocene Mediterranean sapropels

TL;DR: In a recent study as mentioned in this paper, the same authors used geochemical redox proxies (Re, Mo, Mo isotopes, V, Fe/Al, and multiple S isotopes) in 8 sapropels from the Pleistocene to confirm water column euxinic conditions of varying intensity during sapropel deposition.