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Susan H. Little

Researcher at University College London

Publications -  35
Citations -  1777

Susan H. Little is an academic researcher from University College London. The author has contributed to research in topics: Geotraces & Isotope fractionation. The author has an hindex of 16, co-authored 31 publications receiving 1237 citations. Previous affiliations of Susan H. Little include Royal School of Mines & Imperial College London.

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The GEOTRACES Intermediate Data Product 2017

Reiner Schlitzer, +313 more
- 20 Aug 2018 - 
TL;DR: The GEOTRACES Intermediate Data Product 2017 (IDP2017) as discussed by the authors is the second publicly available data product of the international GEOTrACES programme, and contains data measured and quality controlled before the end of 2016.
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The oceanic mass balance of copper and zinc isotopes, investigated by analysis of their inputs, and outputs to ferromanganese oxide sediments

TL;DR: In this paper, the authors investigated the biogeochemical cycling of copper (Cu) and zinc (Zn) isotopes in the ocean and presented estimates for the isotopic composition of the inputs to the oceans based on new data presented here and published data.
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Controls on trace metal authigenic enrichment in reducing sediments: Insights from modern oxygen-deficient settings

TL;DR: In this paper, the authors compare the authigenic enrichment patterns of these elements with a group whose behavior is not as well defined (Cd, Cu, Zn, and Ni) in three oxygen-poor settings: the Black Sea, the Cariaco Basin (Venezuela), and the Peru Margin.
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A modern framework for the interpretation of 238U/235U in studies of ancient ocean redox

TL;DR: In this paper, the authors focused on U isotopes in recent sediments from the two largest modern anoxic ocean basins, the Black Sea and the Cariaco Basin, with the aim of advancing the understanding of the U isotope systematics in reducing marine environments.
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Key role of continental margin sediments in the oceanic mass balance of Zn and Zn isotopes

TL;DR: In this paper, the authors present Zn isotope data for organic-rich and trace metal-rich continental margin sediments from the east Pacific margins that together provide the first observational evidence for the previously hypothesized burial of light Zn in such settings.