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

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.