posted on 2017-09-14, 00:00authored byXiyang Dong, Maik A. Jochmann, Martin Elsner, Armin H. Meyer, Leonard E. Bäcker, Mona Rahmatullah, Daniel Schunk, Guido Lens, Rainer U. Meckenstock
Assessing
the biodegradation of organic compounds is a frequent
question in environmental science. Here, we present a sensitive, inexpensive,
and simple approach to monitor microbial mineralization using reverse
stable isotope labeling analysis (RIL) of dissolved inorganic carbon
(DIC). The medium for the biodegradation assay contains regular organic
compounds and 13C-labeled DIC with 13C atom
fractions (x(13C)DIC) higher
than natural abundance (typically 2–50%). The produced CO2 (x(13C) ≈ 1.11%) gradually
dilutes the initial x(13C)DIC allowing to quantify microbial mineralization using mass-balance
calculations. For 13C-enriched CO2 samples,
a newly developed isotope ratio mid-infrared spectrometer was introduced
with a precision of x(13C) < 0.006%.
As an example for extremely difficult and slowly degradable compounds,
CO2 production was close to the theoretical stoichiometry
for anaerobic naphthalene degradation by a sulfate-reducing enrichment
culture. Furthermore, we could measure the aerobic degradation of
dissolved organic carbon (DOC) adsorbed to granular activated carbon
in a drinking water production plant, which cannot be labeled with 13C. Thus, the RIL approach can be applied to sensitively monitor
biodegradation of various organic compounds under anoxic or oxic conditions.