Fig. 4From: Isotope ratio-based quantification of carbon assimilation highlights the role of plastidial isoprenoid precursor availability in photosynthesisNet carbon assimilation values (A) obtained from isotope ratio mass spectrometry (IRMS) of 13C labeled plant tissue are quantitatively similar to those obtained by gas exchange measurements. a Two methods to calculate A in time course labeled Arabidopsis plants adapted to different light intensities (80–500 PAR, n = 107 plants). Gas exchange measurements of cuvette enclosed plants were taken continuously during the 30–45 min pre-labeling adaptation phase, and reported values represent the average A in normal air for the 3 min prior to introducing the 13CO2-containing atmosphere. For each plant, the analogous IRMS-based carbon assimilation estimate was calculated from the raw IRMS data (μg 13C mg−1 D.W.) and converted to μmol 13CO2 m−2 s−1 based on their individual leaf surface areas, rosette dry weights, and labeling times. Outliers were identified by the interquartile range rule. b The correlation between surface area and dry mass of Arabidopsis rosettes is weak and insufficient to establish a general rule used in gas exchange and 13C labeling experiments. Surface area was estimated by comparison to a calibrated size standard as described in methods. Mass was determined following lyophilization of the intact rosette. Each point represents a single rosette stage Arabidopsis plant 50–70 days old. Outliers were removed according to the interquartile range ruleBack to article page