Publication Date:
2024-06-18
Description:
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).
Keywords:
Arabian_Sea; Area/locality; Bermuda; b - physiological parameter; Carbon dioxide, aquatic; carbon isotope fractionation; Central_Equatorial_Pacific; Coccolithophores; DEPTH, water; East_Equatorial_Pacific; Event label; Florisphaera profunda; Group; growth rate; Growth rate, cell divison per day; Growth rate, required; Isotopic fractionation, during photosynthis; LATITUDE; LONGITUDE; North_East_Pacific; Peru_Upwelling_North; Peru_Upwelling_South; Phosphate; photic zone; Phytoplankton; Pruned model (Hernandez-Almeida et al., 2020); Radiation, photosynthetically active; Reference/source; Residual of isotopic fractionation, during photosynthis; Sea surface temperature; Shallow-intermediate planktic foraminifera ratio; SO; South_Atlantic; South_East_Pacific; Sta_Monica; Surface sediments; Type; δ18O gradient, planktic foraminifera
Type:
Dataset
Format:
text/tab-separated-values, 1432 data points
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