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Kolb, S.

Publications and source records attributed to Kolb, S..

2 recordsLinked to original sources

Elucidating the systemic response of wheat plants under waterlogging based on transcriptomic and metabolic approaches

Extreme weather conditions lead to significant imbalances in crop productivity, which in turn affect food security. Flooding events cause serious problems to many crop species such as wheat. Although metabolic readjustments under flooding are important for plant regeneration, underlying processes remain poorly understood. Here, we investigated the systemic response of wheat to waterlogging using metabolomics and transcriptomics. A 12-day exposure to excess water triggered nutritional imbalances and disruption of metabolite synthesis and translocation, reflected by reduction of plant biomass and growth performance. Metabolic and transcriptomic profiling in roots, xylem, and leaves indicated anaerobic fermentation processes as a local response occurring in roots. Differentially expressed genes and ontological categories revealed that carbohydrate metabolism plays an important role as a systemic response. Analysis of the translocation rate of specific compounds in the xylem showed how waterlogging alters the composition of xylem exudates and thus the root to shoot communication. Interestingly, among all metabolites determined in our study, alanine was the most abundant transported in the xylem. Our results suggest an important role of this amino acid not only as amino-nitrogen source but also as the major root-to-shoot translocated and systemically acting metabolite crucial for balancing C/N between roots and shoots during waterlogging. The relevance of this study relies on the basis to characterize the important role of alanine as HighlightMetabolic and transcriptomic changes in wheat highlight alanine as the major root-to-shoot translocated and systemically acting metabolite crucial for balancing C/N between roots and shoots.

physiology↗

Transcriptional dynamics of methane-cycling microbiomes are linked to seasonal CH4 fluxes in two hydromorphic and organic-rich grassland soils

Soil CH4 fluxes are driven by CH4-producing and -consuming microorganisms that determine whether soils are sources or sinks of this potent greenhouse gas. Using quantitative metatranscriptomics, we linked CH4-cycling microbiomes to net surface CH4 fluxes throughout a year in two drained peatland soils differing in grassland land-use intensity and physicochemical properties. CH4 fluxes were highly dynamic; both soils were net CH4 sources in autumn and winter and sinks in spring and summer. Despite similar net CH4 emissions, methanogen and methanotroph loads, as determined by small subunit rRNA transcripts per gram soil, differed strongly between sites. In contrast, mRNA transcript abundances were similar in both soils and correlated well with CH4 fluxes. The methane monooxygenase to methanogenesis mRNA ratio was higher in spring and summer, when the soils were net CH4 sinks. CH4 uptake was linked to an increased proportion of USC and {gamma} and pmoA2 pmoA transcripts. We assume that methanogen transcript abundance may be useful to approximate changes in net surface CH4 emissions from drained peat soils; high methanotroph to methanogen ratios would indicate CH4 sink properties. Our study shows the strength of quantitative metatranscriptomics; mRNA transcript abundance holds promising indicator to link soil microbiome functions to ecosystem-level processes.

microbiology↗