Phenolic acid-degrading Paraburkholderia prime decomposition in forest soil

Abstract

AbstractPlant-derived phenolic acids are metabolized by soil microorganisms whose activity may enhance the decomposition of soil organic carbon (SOC). We characterized whether phenolic acid-degrading bacteria would enhance SOC mineralization in forest soils when primed with 13C-labeled p-hydroxybenzoic acid (PHB). We further investigated whether PHB-induced priming could explain differences in SOC content among mono-specific tree plantations in a 70-year-old common garden experiment. The activity of Paraburkholderia and Caballeronia dominated PHB degradation in all soils regardless of tree species or soil type. We isolated the principal PHB-degrading phylotype (Paraburkholderia madseniana RP11T), which encoded numerous oxidative enzymes, including secretion signal-bearing laccase, aryl-alcohol oxidase and DyP-type peroxidase, and confirmed its ability to degrade phenolics. The addition of PHB to soil led to significant enrichment (23-fold) of the RP11T phylotype (RP11ASV), as well as enrichment of other phylotypes of Paraburkholderia and Caballeronia. Metabolism of PHB primed significant loss of SOC (3 to 13 µmols C g-1 dry wt soil over 7 days). In contrast, glucose addition reduced SOC mineralization (−3 to -8 µmols C g-1 dry wt soil over 7 days). RP11ASV abundance and the expression of PHB monooxygenase (pobA) correlated with PHB respiration and were inversely proportional to SOC content in the field. We propose that plant-derived phenolics stimulate the activity of phenolic acid-degrading bacteria thereby causing soil priming and SOC loss. We show that Burkholderiaceae dominate soil priming in diverse forest soils and this observation counters the prevailing view that priming phenomena are a generalized non-specific response of community metabolism.