Stable silicon isotope signatures of marine pore waters – Biogenic opal dissolution versus authigenic clay mineral formation

Ehlert, Claudia, Doering, Kristin, Wallmann, Klaus, Scholz, Florian, Sommer, Stefan, Grasse, Patricia, Geilert, Sonja, Frank, Martin·2016·Geochimica et Cosmochimica Acta
DOI 10.1016/j.gca.2016.07.022

Cited by (124)

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  8. Supplementary material to "Impact of ambient conditions on the Si isotope fractionation in marine pore fluids during early diagenesis"
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  9. Reply on RC2
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  10. Reply on RC1
    James Ward · 2022 · Biogeosciences
  11. Comment on bg-2022-51
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  12. Geochemistry of pore water
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  14. Data for solid phase (biogenic opal bSi), d30SibSi, porosity, Al, K and porosity-corrected K concentrations and pore waters (silicic acid (Si), d30SiPW, dissolved K and Cl concentations for core M77/14491
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    Kristin Doering · 2008 · Figshare
  16. Data for solid phase (biogenic opal bSi), d30SibSi, porosity, Al, K and porosity-corrected K concentrations and pore waters (silicic acid (Si), d30SiPW, dissolved K and Cl concentations for core M77/14701
    Kristin Doering · 2008 · Figshare
  17. Age model and sedimentation rate of sediment core M77/1_549-1
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  20. Silicon isotope-based assessments of biogenic and dissolved silica content determination in marine sediments
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  23. Constraining marine silicate alteration in volcanic material-rich continental margin sediments since the last Glacier Maximum evidenced by stable Si isotopes
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  24. An assessment of the Zr/Hf ratio as a proxy of marine clay authigenesis
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