Fig. 2: Physiological measurements associated with the incubations. | Nature Communications

Fig. 2: Physiological measurements associated with the incubations.

From: Short-term acidification promotes diverse iron acquisition and conservation mechanisms in upwelling-associated phytoplankton

Fig. 2: Physiological measurements associated with the incubations.

a Nitrate (NO3, black), phosphate (PO4 x 10, white), and silicate (H4SiO4, gray) concentrations (µmol L−1). The initial (T0) concentrations are those before amending at the concentrations shown in Table 1. b Chlorophyll a concentrations (µmol L−1) from every 24 h interval for the 400 (red), 800 (blue), and 1200 ppm CO2 treatments (green). At Experiment 1, the 800 ppm and 1200 ppm treatments are significantly different (P = 0.026) after 72 h. At Experiment 3, the 400 ppm treatment is significantly different from both the 800 ppm (P = 0.018) and 1200 ppm treatments (P = 0.010) after 96 h. c Ratios of particulate organic carbon (POC) to particulate organic nitrogen (PON). The expected Redfield ratio (106:16) is denoted with horizontal dashed line. d Short-term iron-59 uptake rates normalized to chlorophyll a (µmol Fe mol C−1 hr−1) (pmol Fe µg Chl−1 hr−1) for inorganic iron (FeCl3, black, left y-axis) and organically-complexed iron as ferrioxamine B (Fe-DFB, white, right y-axis). At Experiment 3, the FeCl3 uptake rates are significantly different between the 400 and 1200 ppm treatments (P = 0.016). Both pCO2 treatments and time points in hours are denoted on the x-axis in (a, c, d). Error bars represent the standard deviation of the mean (n = 3 biologically independent samples or field replicate samples for T0 except the Experiment 4800 ppm samples where n = 2). Significant differences (P < 0.05, Two-way ANOVA with Tukey’s HSD test) are denoted with an asterisk (*).

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