Seawater chemistry.
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Parameters of the seawater carbonate chemistry were sampled at the beginning (n = 1) and the end of the experiment (n = 3; mean ±1 s.d.). Total dissolved Fe measurements in abiotic control treatments after 0.2 µm filtration as measured by voltammetry (n = 2; mean ± 1 s.d.). The decreased dissolved Fe concentration in the +Fe treatment can be attributed to precipitation/absorption of colloidal iron. pCO2 was calculated from TA and pHtotal at 3°C and a salinity of 34 using CO2SYS [27], using average final nutrient concentrations of 1 and 60 µmol kg−1 for phosphate and silicate, respectively.
创建时间：
2015-12-02
