In order to understand the hydrothermal input of barium (Ba) to the ocean interior and the changes of Ba in the hydrothermal plume, we measured dissolved (<0.2 μm) and...
University of Cambridge Department of Earth Sciences. Authorship was originally taken from the JGOFS CDs (Lowry & BODC) and was changed by request of the BODC.
The Baltic Sea is largely anoxic and sulfidic at depth but periodically oxygenated by the inflow of oxic seawater from the North Sea. This present an ideal natural laboratory to...
The distribution of dissolved rare earth elements (REEs) and neodymium isotopes (εNd) in the open ocean traces water mass mixing and provides information on lithogenic inputs to the source regions of
