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ORIGINAL RESEARCH article

Front. Plant Physiol.
Sec. Environmental Interactions
Volume 2 - 2024 | doi: 10.3389/fphgy.2024.1457037
This article is part of the Research Topic Alternative plant water uptake pathways under a changing environment View all articles

Foliar water uptake and phyllosphere microbe colonization increase under higher soil nitrogen availability

Provisionally accepted
  • 1 Instituto de Biociencias de la Patagonia INBIOP-CONICET-UNPSJB, Comodoro Rivadavia, Argentina
  • 2 University of Buenos Aires, Buenos Aires, Buenos Aires, Argentina

The final, formatted version of the article will be published soon.

    Leaf water uptake (FWU) represents an alternative pathway to plant water acquisition that can have positive effects on water and carbon balance. Leaf surface traits including the phyllosphere microbes can affect the leaf wetness capacity and FWU. These functional and structural leaf traits could change depending on soil resources availability. The aim of this study was to evaluate the responses of FWU and leaf surface traits such as contact angle, water drop adhesion (LWA) and phyllosphere-associated microbiota to soil nitrogen addition. Three dominant plant species, Azorella prolifera, Senecio filaginoides, and Papostippa speciosa, of an arid steppe in Patagonia exposed to nitrogen (+N) and nitrogen plus water (+NW) addition for ten years were selected. Leaf contact angle did not exhibit statistical differences among treatments within species. LWA was higher in all treatments with respect to the control (C) for shrub A. prolifera and grass P. speciosa. Nitrogen addition increased significantly FWU in A. prolifera and in P. speciosa with respect to C. Colonyforming units of culturable microorganisms (CFU) on leaf surface responded to N addition, but the changes were statistically significant in S. filaginoides and P. speciosa in +NW, increasing three and eight times, respectively, in relation to the C. A positive linear relationship was found between FWU and LWA across species and treatments. On the other hand, CFU of phyllosphere was negative and exponentially correlated with LWA and FWU, across species and treatments. The results suggest that soil N enrichment could affect functional leaf traits and phyllosphere microbiota in a way that may confer a higher potential to cope with drought by facilitating the use of alternative water sources. On the other hand, we suggested that species with leaves more colonized have less surface exposed for FWU and could have lower wettability depending on the hydrophobicity degree of microbes. However, a higher cover of epiphyte's microorganisms could compensate the effects of lower FWU by avoiding the leaf dehydration. This study contributes to a better understanding of plant leaf-microbe interactions under higher N atmospheric deposition and intensive fertilization as global agricultural production is expected to increase.

    Keywords: Foliar water uptake, phyillosphere microbiota, Patagonian steppe, water drop adhesion; wettability, Nitrogen, Plant-Microbe Interactions

    Received: 30 Jun 2024; Accepted: 13 Nov 2024.

    Copyright: © 2024 Arias, Palmeri, Parra, Carbonell-Silletta, Silva, Goldstein, SCHOLZ and Bucci. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

    * Correspondence: Nadia Soledad Arias, Instituto de Biociencias de la Patagonia INBIOP-CONICET-UNPSJB, Comodoro Rivadavia, Argentina

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