Fig. 3.
Box plot showing data distribution for estimates of dissolved phosphorus in Archean seawater with 0.67 mM of Si from 3.8 to 2.6 Ga from measured and literature P/Fe ratios (2, 16–22). Average dissolved P concentration for Archean is shown, while one standard deviation is illustrated by the shaded area. Modern seawater is shown for comparison (11). The right panel summarizes the previous estimates of P concentrations in the Archean ocean (e.g. (1) Jones et al. (7); (2) Planavsky et al. (5); (3) Rasmussen et al. (8)). The range of P concentration of Archean seawater increases when assuming that the sediments experienced a 50% loss during early diagenesis.

Box plot showing data distribution for estimates of dissolved phosphorus in Archean seawater with 0.67 mM of Si from 3.8 to 2.6 Ga from measured and literature P/Fe ratios (2, 16–22). Average dissolved P concentration for Archean is shown, while one standard deviation is illustrated by the shaded area. Modern seawater is shown for comparison (11). The right panel summarizes the previous estimates of P concentrations in the Archean ocean (e.g. (1) Jones et al. (7); (2) Planavsky et al. (5); (3) Rasmussen et al. (8)). The range of P concentration of Archean seawater increases when assuming that the sediments experienced a 50% loss during early diagenesis.

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