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 <sup>13</sup>C-labeled DIC with <sup>13</sup>C atom
fractions (<i>x</i>(<sup>13</sup>C)<sub>DIC</sub>) higher
than natural abundance (typically 2–50%). The produced CO<sub>2</sub> (<i>x</i>(<sup>13</sup>C) ≈ 1.11%) gradually
dilutes the initial <i>x</i>(<sup>13</sup>C)<sub>DIC</sub> allowing to quantify microbial mineralization using mass-balance
calculations. For <sup>13</sup>C-enriched CO<sub>2</sub> samples,
a newly developed isotope ratio mid-infrared spectrometer was introduced
with a precision of <i>x</i>(<sup>13</sup>C) < 0.006%.
As an example for extremely difficult and slowly degradable compounds,
CO<sub>2</sub> 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 <sup>13</sup>C. Thus, the RIL approach can be applied to sensitively monitor
biodegradation of various organic compounds under anoxic or oxic conditions.