4.7 Article

Uranium isotope geochemistry in modern coastal sediments: Insights from Toulon Bay, France

Journal

CHEMICAL GEOLOGY
Volume 481, Issue -, Pages 133-145

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.chemgeo.2018.01.032

Keywords

Uranium; Coastal sediments; Diagenesis; Uranium isotope composition; Redox-sensitive elements

Funding

  1. CARTOCHIM research program (Toulon-Provence-Mediterranee (TPM))
  2. CARTOCHIM research program (Region PACA)
  3. CARTOCHIM research program (l'Agence de l'Eau Rhone-Mediterranee et Corse)
  4. CARTOC research program (Toulon-Provence-Mediterranee (TPM))
  5. CARTOC research program (Region PACA)
  6. CARTOC research program (l'Agence de l'Eau Rhone-Mediterranee et Corse)
  7. PREVENT research program (Toulon-Provence-Mediterranee (TPM))
  8. PREVENT research program (Region PACA)
  9. PREVENT research program (l'Agence de l'Eau Rhone-Mediterranee et Corse)
  10. METFLUX research program (Toulon-Provence-Mediterranee (TPM))
  11. METFLUX research program (Region PACA)
  12. METFLUX research program (l'Agence de l'Eau Rhone-Mediterranee et Corse)
  13. SE.D.RI.PORT (Interreg Marittimo) research program (Toulon-Provence-Mediterranee (TPM))
  14. SE.D.RI.PORT (Interreg Marittimo) research program (Region PACA)
  15. SE.D.RI.PORT (Interreg Marittimo) research program (l'Agence de l'Eau Rhone-Mediterranee et Corse)
  16. French Ministry of National Education, Higher Education and Research
  17. NSERC-CRD (Natural Sciences and Engineering Research Council of Canada - Collaborative Research and Development)

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By assessing U geochemistry in marine sediments of Toulon Bay (NW Mediterranean Sea), authigenic U accumulation was found to be tightly linked to that of Mo and V with slight differences in accumulation rate depending on sediment redox conditions. In sediments collected on a transect along a river plume, the authigenic accumulation of these redox-sensitive elements appears to be linked to sediment grain size which probably drives the redox status of the sediments. A typical U loss in re-oxidized sediments was observed in sediments that had been previously disturbed. However, the dissolved U profiles do not show a simple and typical depletion trend but rather a depletion in the top 10 cm followed by release in deeper pore waters that could be linked to a potential reoxidation/mobilization of authigenic U(IV). The released U could be further scavenged as a U-P precipitate. The U isotopic data (delta U-238), which are the first reported for the coastal hypoxic sediments of Toulon Bay, average -0.12 +/- 0.12% in surface sediments. However, sediments situated in front of river mouths show higher values of delta U-238 (up to +0.75%); these high values are reported for the first time in sediments below an oxic water column.

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