Published carbon isotope fractionation (Ɛp) and environmental data for photic zone and surface sediment samples

References of the studies in which b has been calculated from Ɛp values from alkenones, together with the coordinates, in-situ and estimated (if in-situ was not available) [CO2]aq, PO43-, SST, PAR and modeled coccolithophore growth rate using the global model [Krumhardt et al., 2017]. Interpolated micropaelontological datasets to the locations of the surface sediment samples: planktonic foraminifera intermediate-surface ratio, relative abundance of Florisphaera profunda and offset in d18O between shallow and deep planktonic foraminifera used in Fig. 8. Calculations of the required growth rate and residuals of the pruned model (CO2aq + size) (Fig. 9).