Isotope fractionation during root water uptake by Acacia caven is enhanced by arbuscular mycorrhizas

Aim A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular mycorrhizal fungi (AMF) on the isotopic composition of Acacia caven xylem water. As the most common plant-fungal association, AMF might expla...

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Published in	Plant and soil Vol. 441; no. 1/2; pp. 485 - 497
Main Authors	Poca, María, Coomans, Olivia, Urcelay, Carlos, Zeballos, Sebastián R., Bodé, Samuel, Boeckx, Pascal
Format	Journal Article
Language	English
Published	Cham Springer Science + Business Media 01.08.2019 Springer International Publishing Springer Springer Nature B.V
Subjects	Acacia Acacia caven Aquaporins Arbuscular mycorrhizas Biomedical and Life Sciences Composition Depletion deuterium Distillation Distilled water Ecology Fractionation Fungi irrigation Irrigation water Isotope fractionation Isotopes Life Sciences Moisture content mycorrhizal fungi oxygen Plant Physiology Plant Sciences REGULAR ARTICLE roots Seedlings Soil moisture soil sampling Soil Science & Conservation Soil water stable isotopes vesicular arbuscular mycorrhizae Water Water transport Water uptake xerophytes Xylem Argentina Ecohydrology Isotope fractionation Plant-soil-water interactions Aquaporins Stable isotopes Mycorrhiza
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ISSN	0032-079X 1573-5036
DOI	10.1007/s11104-019-04139-1

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Abstract	Aim A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular mycorrhizal fungi (AMF) on the isotopic composition of Acacia caven xylem water. As the most common plant-fungal association, AMF might explain this isotopic mismatch. Methods Seedlings were grown with and without AMF and irrigated with the same water. After 120 days, stem and soil samples were collected and following cryogenic distillation, H and O isotopic composition of xylem and soil water, as well as irrigation water, was measured. Results Xylem water of non-mycorrhizal seedlings was significantly depleted in 2 H compared to soil water (differences up to −15.6‰). When AMF were present, the depletion was significantly higher and appeared for both H and O (differences up to −24.6‰ for δ 2 H and − 2.9‰ for δ 18 O between soil and xylem water). Conclusions Results suggest that isotopic fractionation occurred during water uptake in this xerophytic species. To explain this, we propose an aquaporin-driven mechanism mediating water transport via transmembrane passage. Furthermore, we show for the first time, that AMF enhance the observed discrimination against heavy isotopes, probably by enforcing water passage through aquaporins. Given their ubiquity, AMF could question the fractionation-free assumption during root water uptake.
AbstractList	Aim A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular mycorrhizal fungi (AMF) on the isotopic composition of Acacia caven xylem water. As the most common plant-fungal association, AMF might explain this isotopic mismatch. Methods Seedlings were grown with and without AMF and irrigated with the same water. After 120 days, stem and soil samples were collected and following cryogenic distillation, H and O isotopic composition of xylem and soil water, as well as irrigation water, was measured. Results Xylem water of non-mycorrhizal seedlings was significantly depleted in 2 H compared to soil water (differences up to −15.6‰). When AMF were present, the depletion was significantly higher and appeared for both H and O (differences up to −24.6‰ for δ 2 H and − 2.9‰ for δ 18 O between soil and xylem water). Conclusions Results suggest that isotopic fractionation occurred during water uptake in this xerophytic species. To explain this, we propose an aquaporin-driven mechanism mediating water transport via transmembrane passage. Furthermore, we show for the first time, that AMF enhance the observed discrimination against heavy isotopes, probably by enforcing water passage through aquaporins. Given their ubiquity, AMF could question the fractionation-free assumption during root water uptake. AIM: A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular mycorrhizal fungi (AMF) on the isotopic composition of Acacia caven xylem water. As the most common plant-fungal association, AMF might explain this isotopic mismatch. METHODS: Seedlings were grown with and without AMF and irrigated with the same water. After 120 days, stem and soil samples were collected and following cryogenic distillation, H and O isotopic composition of xylem and soil water, as well as irrigation water, was measured. RESULTS: Xylem water of non-mycorrhizal seedlings was significantly depleted in ²H compared to soil water (differences up to −15.6‰). When AMF were present, the depletion was significantly higher and appeared for both H and O (differences up to −24.6‰ for δ²H and − 2.9‰ for δ¹⁸O between soil and xylem water). CONCLUSIONS: Results suggest that isotopic fractionation occurred during water uptake in this xerophytic species. To explain this, we propose an aquaporin-driven mechanism mediating water transport via transmembrane passage. Furthermore, we show for the first time, that AMF enhance the observed discrimination against heavy isotopes, probably by enforcing water passage through aquaporins. Given their ubiquity, AMF could question the fractionation-free assumption during root water uptake. Aim A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular mycorrhizal fungi (AMF) on the isotopic composition of Acacia caven xylem water. As the most common plant-fungal association, AMF might explain this isotopic mismatch. Methods Seedlings were grown with and without AMF and irrigated with the same water. After 120 days, stem and soil samples were collected and following cryogenic distillation, H and O isotopic composition of xylem and soil water, as well as irrigation water, was measured. Results Xylem water of non-mycorrhizal seedlings was significantly depleted in .sup.2H compared to soil water (differences up to -15.6â°). When AMF were present, the depletion was significantly higher and appeared for both H and O (differences up to -24.6â° for [delta].sup.2H and - 2.9â° for [delta].sup.18O between soil and xylem water). Conclusions Results suggest that isotopic fractionation occurred during water uptake in this xerophytic species. To explain this, we propose an aquaporin-driven mechanism mediating water transport via transmembrane passage. Furthermore, we show for the first time, that AMF enhance the observed discrimination against heavy isotopes, probably by enforcing water passage through aquaporins. Given their ubiquity, AMF could question the fractionation-free assumption during root water uptake. AimA growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular mycorrhizal fungi (AMF) on the isotopic composition of Acacia caven xylem water. As the most common plant-fungal association, AMF might explain this isotopic mismatch.MethodsSeedlings were grown with and without AMF and irrigated with the same water. After 120 days, stem and soil samples were collected and following cryogenic distillation, H and O isotopic composition of xylem and soil water, as well as irrigation water, was measured.ResultsXylem water of non-mycorrhizal seedlings was significantly depleted in 2H compared to soil water (differences up to −15.6‰). When AMF were present, the depletion was significantly higher and appeared for both H and O (differences up to −24.6‰ for δ2H and − 2.9‰ for δ18O between soil and xylem water).ConclusionsResults suggest that isotopic fractionation occurred during water uptake in this xerophytic species. To explain this, we propose an aquaporin-driven mechanism mediating water transport via transmembrane passage. Furthermore, we show for the first time, that AMF enhance the observed discrimination against heavy isotopes, probably by enforcing water passage through aquaporins. Given their ubiquity, AMF could question the fractionation-free assumption during root water uptake.
Audience	Academic
Author	Poca, María Zeballos, Sebastián R. Bodé, Samuel Urcelay, Carlos Coomans, Olivia Boeckx, Pascal
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Snippet	Aim A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular... Aim A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular... AimA growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular... AIM: A growing number of studies show a discrepancy between the isotopic composition of xylem water and plant water sources. We tested the effect of arbuscular...
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SubjectTerms	Acacia Acacia caven Aquaporins Arbuscular mycorrhizas Biomedical and Life Sciences Composition Depletion deuterium Distillation Distilled water Ecology Fractionation Fungi irrigation Irrigation water Isotope fractionation Isotopes Life Sciences Moisture content mycorrhizal fungi oxygen Plant Physiology Plant Sciences REGULAR ARTICLE roots Seedlings Soil moisture soil sampling Soil Science & Conservation Soil water stable isotopes vesicular arbuscular mycorrhizae Water Water transport Water uptake xerophytes Xylem
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Title	Isotope fractionation during root water uptake by Acacia caven is enhanced by arbuscular mycorrhizas
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