• Assessment of C, N, and Si Isotopes as Tracers of Past Ocean Nutrient and Carbon Cycling 

      Farmer, J. R.ORCIDiD; Hertzberg, J. E.ORCIDiD; Cardinal, D.ORCIDiD; Fietz, S.; Hendry, K.ORCIDiD; Jaccard, S. L.ORCIDiD; Paytan, A.ORCIDiD; Rafter, P. A.ORCIDiD; Ren, H.; Somes, C. J.ORCIDiD; Sutton, J. N.ORCIDiD; GEOTRACES PAGES Biological Productivity Working Group Members (Global Biogeochemical Cycles, 2021-07-02)
      Biological productivity in the ocean directly influences the partitioning of carbon between the atmosphere and ocean interior. Through this carbon cycle feedback, changing ocean productivity has long been hypothesized as ...
    • Iron Exports From Catchments Are Constrained by Redox Status and Topography 

      Tittel, JörgORCIDiD; Büttner, OlafORCIDiD; Friese, KurtORCIDiD; Lechtenfeld, Oliver J.ORCIDiD; Schuth, Stephan; von Tümpling, Wolf; Musolff, AndreasORCIDiD (Global Biogeochemical Cycles, 2022-01-18)
      Fe(III) hydroxides stabilize organic carbon (OC) and P in soils. Observations of rising stream Fe concentrations are controversially posited to result from a flushing of iron‐rich deeper soil layers or a decrease of competing ...
    • Past and Future Climate Variability Uncertainties in the Global Carbon Budget Using the MPI Grand Ensemble 

      Loughran, T. F.ORCIDiD; Boysen, L.ORCIDiD; Bastos, A.ORCIDiD; Hartung, K.ORCIDiD; Havermann, F.ORCIDiD; Li, H.ORCIDiD; Nabel, J. E. M. S.ORCIDiD; Obermeier, W. A.ORCIDiD; Pongratz, J.ORCIDiD (Global Biogeochemical Cycles, 2021-08-21)
      Quantifying the anthropogenic fluxes of CO2 is important to understand the evolution of carbon sink capacities, on which the required strength of our mitigation efforts directly depends. For the historical period, the ...