Evidence map›Paper›PMID 40798946›Full record

ArticleAnnals of botany2025

Root mucilage enhances plant water use under combined soil and atmospheric drought.

Asegidew Akale, Mohanned Abdalla, Tina Koehler, Anna M Sauer, Efstathios Diamantopoulos, Mutez A Ahmed

Abstract read
In one paragraph

Article in Annals of botany, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

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0cells of the map it votes in
1citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

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2 · The registry

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3 · Its place in the literature

Who cites it

1 citing paper in PubMed.

  1. Article
4 · The record

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5 · Who and what money

Authors and funding

6 authors.

Asegidew AkaleRoot-Soil Interaction, School of Life Sciences, Technical University of Munich, Freising, 85354, Germany.ORCID 0009-0003-3439-7421
Mohanned AbdallaRoot-Soil Interaction, School of Life Sciences, Technical University of Munich, Freising, 85354, Germany.ORCID 0000-0002-4220-8761
Tina KoehlerRoot-Soil Interaction, School of Life Sciences, Technical University of Munich, Freising, 85354, Germany.ORCID 0000-0002-6423-6835
Anna M SauerRoot-Soil Interaction, School of Life Sciences, Technical University of Munich, Freising, 85354, Germany.
Efstathios DiamantopoulosSoil Physics, University of Bayreuth, Bayreuth, 95447, Germany.
Mutez A AhmedRoot-Soil Interaction, School of Life Sciences, Technical University of Munich, Freising, 85354, Germany.ORCID 0000-0002-7402-1571

Funding

Deutsche Forschungsgemeinschaft
6 · The paper itself

Abstract

BACKGROUND AND

aimsPlants have evolved various root adaptive traits to enhance their ability to access soil water in stressful conditions. Although root mucilage has been suggested to facilitate root water uptake in drying soils, its impact during combined edaphic and atmospheric stress remains unknown. We hypothesized that mucilage decreases the saturated soil hydraulic conductivity, and consequently, a genotype with high mucilage production will exhibit lower maximum soil-plant hydraulic conductance and restrict transpiration at relatively low vapour pressure deficit (VPD). On the contrary, in drying soil, mucilage attenuates the gradients in matric potential at the root-soil interface and thus facilitates root water uptake, especially at high VPD.

methodsWe compared two cowpea genotypes with contrasting mucilage production rates and subjected them to three consecutively increasing levels of VPD (1.04, 1.8 and 2.8 kPa) while the soil was left to dry out. We measured the transpiration rate and soil and leaf water potentials and estimated canopy and plant hydraulic conductance during soil drying. KEY

resultsIn wet soil conditions, the high-mucilage genotype restricted transpiration rate at lower VPD (1.46 kPa) compared with the low-mucilage genotype (1.58 kPa). Likewise, the initial slope of transpiration rate in response to VPD (the maximum conductance) was significantly lower in the high- compared with the low-mucilage genotype. During soil drying, the transpiration rate declined earlier in the low- compared with the high-mucilage genotype, supporting the hypothesis that mucilage helps to maintain the hydraulic continuity between roots and soil at lower water potentials in the high-mucilage genotype.

conclusionsRoot mucilage is a promising trait that reduces water use in wet soil conditions, thereby conserving soil moisture for critical phases (e.g. flowering and grain filling), both on a daily basis (increasing VPD) and on a seasonal time scale (soil drying).

Indexed as

DroughtsPlant MucilagePlant RootsSoilVignaWaterAtmosphereGenotypePlant LeavesPlant TranspirationVapor PressurePlant MucilageSoilWaterCowpeasoil dryingsoil hydraulic conductivityvapour pressure deficit

Identifiers

PMID40798946
PMCPMC12682819

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.