B11J-0580
Plant-Microbial Interactions Define Potential Mechanisms of Organic Matter Priming in the Rhizosphere

Monday, 14 December 2015
Poster Hall (Moscone South)
Kateryna Zhalnina1,2, Heejung Cho1, Zhao Hao1, Nasim Mansoori3, Ulas Karaoz4, Stefan Jenkins1, Richard A. White III5, Mary Suzanne Lipton5, Kai Deng3, Jizhong Zhou6, Jennifer Pett-Ridge7, Trent Northen1, Mary K Firestone2 and Eoin Brodie1, (1)Lawrence Berkeley National Laboratory, Berkeley, CA, United States, (2)University of California Berkeley, Berkeley, CA, United States, (3)Joint BioEnergy Institute, Emeryville, CA, United States, (4)Lawrence Berkeley National Lab, Berkeley, CA, United States, (5)Pacific Northwest National Laboratory, Richland, WA, United States, (6)Univ Oklahoma, Norman, OK, United States, (7)Lawrence Livermore National Laboratory, Chemical Sciences Division, Livermore, CA, United States
Abstract:
In the rhizosphere, metabolic processes of plants and microorganisms are closely coupled, and together with soil minerals, their interactions regulate the turnover of soil organic C (SOC). Plants provide readily assimilable metabolites for microorganisms through exudation, and it has been hypothesized that increasing concentrations of exudate C may either stimulate or suppress rates of SOC mineralization (rhizosphere priming). Both positive and negative rhizosphere priming has been widely observed, however the underlying mechanisms remain poorly understood.

To begin to identify the molecular mechanisms underlying rhizosphere priming, we isolated a broad range of soil bacteria from a Mediterranean grassland dominated by annual grass. Thirty-nine heterotrophic bacteria were selected for genome sequencing and both rRNA gene analysis and metagenome coverage suggest that these isolates represent naturally abundant strain variants. We analyzed their genomes for potential metabolic traits related to life in the rhizosphere and the decomposition of polymeric SOC. While the two dominant groups, Alphaproteobacteria and Actinobacteria, were enriched in polymer degrading enzymes, Alphaproteobacterial isolates contained greater gene copies of transporters related to amino acid, organic acid and auxin uptake or export, suggesting an enhanced metabolic potential for life in the root zone.

To verify this metabolic potential, we determined the enzymatic activities of these isolates and revealed preferences of strains to degrade certain polymers (xylan, cellulose or lignin). Fourier Transform Infrared spectroscopy is being used to determine which polymeric components of plant roots are targeted by specific strains and how exudates may impact their degradation. To verify the potential of isolates to assimilate root exudates and export key metabolites we are using LC-MS/MS based exometabolomic profiling.

The traits hypothesized and verified here (transporters, enzymes, exudate uptake and degradation of plant polymers) provide a mechanistic basis of rhizosphere microbial succession and SOC priming and will contribute to our overarching goal of developing predictive models of the rhizosphere.