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Additional porewater, bottom water and solid phase geochemical and Ni isotope...
The reactivity and isotope fractionation of Ni is strongly influenced by biological and redox-related processes in the ocean, giving the isotope system (expressed as δ60 Ni)... -
Salt- corrected chemical compounds, elemental concentrations and Ni isotope d...
The reactivity and isotope fractionation of Ni is strongly influenced by biological and redox-related processes in the ocean, giving the isotope system (expressed as δ60 Ni)... -
Ni and P elemental concentrations in suspended particulate matter of bottom w...
The reactivity and isotope fractionation of Ni is strongly influenced by biological and redox-related processes in the ocean, giving the isotope system (expressed as δ60 Ni)... -
Bottom Water (collected with the benthic trace profiler (BTP)) geochemical an...
The reactivity and isotope fractionation of Ni is strongly influenced by biological and redox-related processes in the ocean, giving the isotope system (expressed as δ60 Ni)... -
Porewater geochemical and Ni isotope data for sediment cores collected during...
The reactivity and isotope fractionation of Ni is strongly influenced by biological and redox-related processes in the ocean, giving the isotope system (expressed as δ60 Ni)...
