期刊
ENVIRONMENTAL SCIENCE & TECHNOLOGY
卷 48, 期 20, 页码 11926-11933出版社
AMER CHEMICAL SOC
DOI: 10.1021/es5020955
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资金
- ANR CESA
- International Program Fund of 985 Project, Sun Yatsen University
- Natural Science Foundation of China [41371315, 41225004]
- [ANR-10-LABX-21 (LABEX Ressources21)]
Until now, there has been little data on the isotope fractionation of nickel (Ni) in higher plants and how this can be affected by plant Ni and zinc (Zn) homeostasis. A hydroponic cultivation was conducted to investigate the isotope fractionation of Ni and Zn during plant uptake and translocation processes. The nonaccumulator Thlaspi arvense, the Ni hyperaccumulator Alyssum murale and the Ni and Zn hyperaccumulator Noccaea caerulescens were grown in low (2 mu M) and high (50 mu M) Ni and Zn solutions. Results showed that plants were inclined to absorb light Ni isotopes, presumably due to the functioning of low-affinity transport systems across root cell membrane. The Ni isotope fractionation between plant and solution was greater in the hyperaccumulators grown in low Zn treatments (Delta Ni-60(plant-solution) = -0.90 to -0.63 parts per thousand) than that in the nonaccumulator T. arvense (Delta Ni-60(plant-solution) = -0.21 parts per thousand), thus indicating a greater permeability of the low-affinity transport system in hyperaccumulators. Light isotope enrichment of Zn was observed in most of the plants (Delta Zn-66(plant-solution) = -0.23 to -0.10 parts per thousand), but to a lesser extent than for Ni. The rapid uptake of Zn on the root surfaces caused concentration gradients, which induced ion diffusion in the rhizosphere and could result in light Zn isotope enrichment in the hyperaccumulator N. caerulescens. In high Zn treatment, Zn could compete with Ni during the uptake process, which reduced Ni concentration in plants and decreased the extent of Ni isotope fractionation (Delta Ni-60(plant-solution) = -0.11 to -0.07 parts per thousand), indicating that plants might take up Ni through a low-affinity transport system of Zn. We propose that isotope composition analysis for transition elements could become an empirical tool to study plant physiological processes.
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