Reconstructing the seafloor environment during sapropel formation using benthic foraminiferal trace metals, stable isotopes, and sediment composition

@article{Fhlaithearta2010ReconstructingTS,
  title={Reconstructing the seafloor environment during sapropel formation using benthic foraminiferal trace metals, stable isotopes, and sediment composition},
  author={Shauna N{\'i} Fhlaithearta and Gert‐Jan Reichart and Frans J. Jorissen and Christophe Fontanier and Eelco J. Rohling and John Thomson and Gert J. Lange},
  journal={Paleoceanography},
  year={2010},
  volume={25}
}
The evolution of productivity, redox conditions, temperature, and ventilation during the deposition of an Aegean sapropel (S1) is independently constrained using bulk sediment composition and high-resolution single specimen benthic foraminiferal trace metal and stable isotope data. The occurrence of benthic foraminifer, Hoeglundina elegans (H. elegans), through a shallow water (260 m) sapropel, permits for the first time a comparison between dissolved and particulate concentrations of Ba and Mn… 

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