Nitrogen Isotope Fractionation During Nitrate and Ammonium Uptake in Maize: Hydroponic Evidence and Implications for Ecological Investigations
Priscillia Semaoune, Joëlle Templier, Sylvie Derenne, R. Dave Evans, Mathieu Sebilo

TL;DR
This study examines how maize plants fractionate nitrogen isotopes during nitrate and ammonium uptake, offering insights into ecological interpretations of nitrogen isotope data.
Contribution
The study provides new evidence on concentration-dependent isotope fractionation during nitrate and ammonium uptake in maize.
Findings
Nitrate uptake shows low and concentration-independent nitrogen isotope fractionation.
Ammonium uptake exhibits higher and concentration-dependent nitrogen isotope fractionation.
An isotope mixing model indicates that nitrate efflux contributes to isotope enrichment in solution.
Abstract
Understanding nitrogen (N) isotopic fractionation during plant uptake is critical for interpreting δ15N variations in terrestrial ecosystems. We investigated isotopic discrimination during ammonium (NH4 +) or nitrate (NO3 −) uptake in maize (Zea mays) grown hydroponically under controlled conditions with 0.2 and 2 mM to represent high and low affinity transport systems, respectively. Nitrogen (15ε) and oxygen (18ε) isotopic fractionation during NO3 − uptake were determined. NO3 − uptake exhibited low and concentration‐independent 15ε values (0.2 mM: 15ε = −2‰; 2 mM: 15ε = −1.7‰). In contrast, 18ε was lower at high concentrations (0.2 mM: 18ε = −5.3‰; 2 mM: 18ε = −2.1‰). For NH4 + uptake, 15ε was higher and increased with concentration (0.2 mM: 15ε = −5.7‰; 2 mM: 15ε = −8.5‰). An isotope mixing model suggests a small NO3 − efflux contributes to 15N and 18O enrichment in solution due to…
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Taxonomy
TopicsPlant nutrient uptake and metabolism · Soil Carbon and Nitrogen Dynamics · Plant Water Relations and Carbon Dynamics
