Aliquots (1 ml) were filtered onto precombusted GF filters (0.45 µm pore size), which were frozen at −20 °C until EA-IRMS analysis. Carbon isotopic ratios (R =
13C/
12C) were determined on filters folded into tin capsules, using a CHN analyzer (ThermoFinnigan 1112 Series) interfaced with a mass spectrometer (ThermoFinnigan
MAT Delta Plus) via a Conflow III open split interface. Abundances were calculated in relation to Vienna Pee Dee Belemnite-limestone (V-PDB), using in-house casein standards calibrated against IAEA-600 and IAEA-CH-6 international standards.
Bulk carbon assimilation was calculated as atom percent excess (APE) as follows:
where
Rf and
Ri are the
13C isotope ratio at the final and initial sampling time, respectively.
Bulk carbon incorporation rates (
Fbulk) were calculated as follows:
where
KA is the fraction of assimilated carbon (calculated as described in Supplementary Methods),
ρC is the amount of carbon per cell,
A is the final cell abundance estimated through flow cytometry and
t is the incubation time. We considered a range of
ρC = 10–280 fg C cell
−1 [50 (
link)].
Thomas F., Le Duff N., Wu T.D., Cébron A., Uroz S., Riera P., Leroux C., Tanguy G., Legeay E, & Guerquin-Kern J.L. (2021). Isotopic tracing reveals single-cell assimilation of a macroalgal polysaccharide by a few marine Flavobacteria and Gammaproteobacteria. The ISME Journal, 15(10), 3062-3075.