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Abstract:
It is well established that soil microorganisms play an important role in respiration of newly fixed plant
carbon. Recent results show that they also contribute significantly to soil organic matter (SOM) formation.
We hypothesized that different molecular size classes of compounds in soil microbial biomass
(SMB) have variable turnover time and in consequence influence SOM formation differentially. Here we
used natural differences in carbon stable isotope signatures (d13C values) after C3eC4 vegetation change
to track newly fixed C4 plant carbon into SMB molecular size classes. SMB was obtained by chloroform
fumigation extraction (SFE) and d13C values of its size classes were measured using size exclusion
chromatography coupled online to liquid chromatography‒isotope ratio mass spectrometry (SECeLC
eIRMS). Resolved SMB was assigned to 5 size classes of 1800e9800, 800e1800, 380e800, 180e380 and
50e180 Da respectively. The contribution of recent C4 plant carbon to size classes of SMB decreased with
increasing molecular weight (MW). It ranged from 77 19% in the lowest MW size class size class to
41 14% in the highest MW size class in a sandy soil and from 59 18% in the lowest MW size class to
8 15% in the highest MW size class in a clayey soil. A decreasing carbon turnover of compounds in SMB
extracts along a continuum of molecular size from small to large implies that low molecular weight
microbial compounds are rapidly metabolized products that link to fast respiratory carbon fluxes,
whereas high molecular weight ones could be products of microbial synthesis like structural compounds
that have slower turnover rates and link to slower SOM formation. Our methods help avoid contamination
of CFE extracts and the results help explain why SMB turnover is faster in CFE extracts when compared to calculations using membrane lipids (e.g. PLFA-based).
