Fig. 5: Concentrations of ascorbate-extractable Fe (FeA) and dissolved iron over sediment depth at three stations within the transects. | Nature Communications

Fig. 5: Concentrations of ascorbate-extractable Fe (FeA) and dissolved iron over sediment depth at three stations within the transects.

From: Potentially bioavailable iron produced through benthic cycling in glaciated Arctic fjords of Svalbard

Fig. 5

The three frames show the amount of FeA and the concentration of dissolved iron (dFe(II)) in the pore water versus sediment depth at a stations closest to the fjord head (Kongsfjorden (KFa) = KFa1, Lilliehöökfjorden (LF) = LF1, Dicksonfjorden (DF) = DF1); b mid-fjord stations (KFa = KFa5, LF = LF5, DF = DF3); and c: stations closest to the fjord mouth (KFa = KFa7, LF = LF8, DF = DF5).

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