Figure 2: Comparison of observations and model output of inorganic phosphate uptake during 33P-phosphate pulse and 32P-phosphate chase experiments. | Nature Communications

Figure 2: Comparison of observations and model output of inorganic phosphate uptake during 33P-phosphate pulse and 32P-phosphate chase experiments.

From: Dominant oceanic bacteria secure phosphate using a large extracellular buffer

Figure 2

Observations (black circles) and model output (blue lines) of traced inorganic phosphate (33Pi and 32Pi) in cells during six pulse–chase experiments (top row of plots) at two contrasting sites: least productive waters of the gyre centre and more productive tropical waters. Seawater samples with bioassayed ambient 31Pi were pulsed with 0.8 or 2.4 nmol l−1 31Pi labelled with 0.05 nmol l−1 33Pi and chased after 1 h incubation with 80 or 800 nmol l−1 and 240 or 2,400 nmol l−1 of 31Pi labelled with 0.01 nmol l−1 32Pi. Note that observations and model output values are normalized to the maximum uptake measure (counts per minute per ml) in a time course in each experiment to lie between 0 and 100%. dil, dilution.

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