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Updated: Jul 16, 2026

DNA Stable-Isotope Probing (DNA-SIP)
Published on: August 2, 2010
Insights into the fate of a 13C labelled phenol pulse for stable isotope probing (SIP) experiments
Mike Manefield1, Rob Griffiths, Niall P McNamara
1Centre for Marine Biofouling and Bioinnovation, University of New South Wales, Sydney, 2052, Australia. manefield@unsw.edu.au
Abstract:
Stable isotope probing (SIP) using DNA or RNA as a biomarker has proven to be a useful method for attributing substrate utilisation to specific microbial taxa. In this study we followed the transfer of a (13)C(6)-phenol pulse in an activated sludge micro-reactor to examine the resulting distribution of labelled carbon in the context of SIP. Most of the added phenol was metabolically converted within the first 100 min after (13)C(6)-phenol addition, with 49% incorporated into microbial biomass and 6% respired as CO(2). Less than 1% of the total (13)C labelled carbon supplied was incorporated into microbial RNA and DNA, with RNA labelling 6.5 times faster than DNA. The remainder of the added (13)C was adsorbed and/or complexed to suspended solids within the sludge. The (13)C content of nucleic acids increased beyond the initial consumption of the (13)C-phenol pulse. This study confirms that RNA labels more efficiently than DNA and reveals that only a small proportion of a pulse is incorporated into nucleic acids. Evidence of continued (13)C incorporation into nucleic acids suggests that cross-feeding of the SIP substrate was rapid. This highlights both the benefits of using a biomarker that is rapidly labelled and the importance of sampling within appropriate timescales to avoid or capture the effects of cross-feeding, depending on the goal of the study.
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