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van Dusschoten, D.

Publications and source records attributed to van Dusschoten, D..

2 recordsLinked to original sources

Integrating Orthology and Cross-Species Transcriptomics to Unravel Root Drought Responses in Faba Bean and Maize

During soil drying, roots in upper and deeper soil layers experience different hydraulic environments, yet the molecular programs that accompany and potentially drive depth-specific changes in root water uptake capacity remain poorly understood. Here, we address this gap by coupling depth-resolved RNA-seq with previously measured hydraulic uptake profiles in pot-grown faba bean (Vicia faba) and maize (Zea mays), two crop species with contrasting root architecture, sampled from upper (drying) and lower (comparatively wet) root zones at the onset and after four days of soil drying. Differential expression analysis revealed strongly top-region of the roots dominated transcriptional responses in both species, consistent with the steeper hydraulic challenge in drying upper layers. Maize displayed a TIP- and dehydrin-dominated drought response, whereas faba bean induced NIP-like aquaporins and a broader LEA repertoire, suggesting divergent strategies for root water and cellular stress protection. To compare transcriptome responses across these distally related species, we grouped orthologous genes across 26 species using OrthoFinder. With this approach, we identified 905 drought-responsive orthogroups, of which only 17% were shared between species despite broadly convergent gene onthology (GO) enrichment profiles. Phylogenetic tracing showed that 95.7% of faba bean-specific and 90.3% of maize-specific drought-responsive orthogroups are conserved across monocot and dicot lineages, indicating that species-specific drought transcriptomes arise primarily through differential recruitment of ancestral gene families rather than lineage-specific innovation. These findings define a molecular framework linking root hydraulic architecture to gene regulation under drought and identify conserved transcriptional regulatory hubs as targets for broad-spectrum abiotic stress improvement in both faba bean and maize.

plant biology↗

Development and calibration of the FSPM CPlantBox to represent the interactions between water and carbon fluxes in the soil-plant-atmosphere continuum

A plants development is strongly linked to the water and carbon flows in the soil-plant-atmosphere continuum. Expected climate shifts will alter the water and carbon cycles and will affect plant phenotypes. Comprehensive models which simulate mechanistically and dynamically the feedback loops between a plants three-dimensional development and the water and carbon flows are useful tools to evaluate the sustainability of genotype-environment-management combinations which do not yet exist. In this study, we present the latest version of the open-source three-dimensional Functional-Structural Plant Model CPlantBox with PiafMunch and DuMux coupling. We simulated semi-mechanistically the development of generic C3 monocots from 10 to 25 days after sowing and undergoing an atmospheric dry spell of one week (no precipitation). We compared the results for dry spells starting on different days (day 11 or 18) and with different climates (wetter and colder against drier and warmer atmospheric and initial soil conditions). Compared with the wetter and colder climate, the dry spell with the drier and warmer climate led to a lower instantaneous water use efficiency. Moreover, the lower symplasm turgor for the drier and warmer climate limited the growth, which made the sucrose available for other processes, such as maintenance respiration. Both of these effects were stronger for the later dry spell compared with the early dry spell under the drier and warmer climate. We could thus use CPlantBox to simulate diverging emerging processes (like carbon partitioning) defining the plants phenotypic plasticity response to their environment.

plant biology↗