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Trace element concentrations in ostracod shells are a vital tool for paleoenvironmental reconstructions. The most common approach used to measure trace element concentrations in ostracod shells is batch dissolution followed by analysis of the resulting solution. However, oxide coatings, secondary carbonate crusts, or adhering clay minerals can contaminate their surface with significant quantities...
Stable isotopes and trace elements in ostracod shells have been used widely in paleolimnological investigations of past lake hydrochemistry and climate because they provide insights into past water balance and solute evolution of lakes. Regional differences in lake characteristics and species-specific element fractionation, however, do not permit generalization of results from other regions or ostracod...
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