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美国东部三种拟金属植物C4草的原位元素吸收差异

Differential elemental uptake in three pseudo-metallophyte C grasses in situ in the eastern USA.

作者信息

Gonneau Cédric, Mohanty Sanjay K, Dietterich Lee H, Hwang Wei-Ting, Willenbring Jane K, Casper Brenda B

机构信息

Department of Biology, University of Pennsylvania, Philadelphia, PA 19104, USA.

Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104, USA.

出版信息

Plant Soil. 2017 Jul;416(1-2):149-163. doi: 10.1007/s11104-017-3198-9. Epub 2017 Feb 10.

Abstract

BACKGROUND AND AIMS

Elemental uptake in serpentine floras in eastern North America is largely unknown. The objective of this study was to determine major and trace element concentrations in soil and leaves of three native pseudo-metallophyte C grasses in situ at five sites with three very different soil types, including three serpentine sites, in eastern USA.

METHODS

Pseudo-total and extractible concentrations of 15 elements were measured and correlated from the soils and leaves of three species at the five sites.

RESULTS

Element concentrations in soils of pseudo-metallophytes varied up to five orders of magnitude. Soils from metalliferous sites exhibited higher concentrations of their characteristic elements than non-metalliferous. In metallicolous populations, elemental concentrations depended on the element. Concentrations of major elements (Ca, Mg, K) in leaves were lower than typical toxicity thresholds, whereas concentrations of Zn were higher.

CONCLUSIONS

In grasses, species can maintain relatively low metal concentrations in their leaves even when soil concentrations are richer. However, in highly Zn-contaminated soil, we found evidence of a threshold concentration above which Zn uptake increases drastically. Finally, absence of main characteristics of serpentine soil at one site indicated the importance of soil survey and restoration to maintain serpentinophytes communities and avoid soil encroachment.

摘要

背景与目的

北美东部蛇纹石植物区系中的元素吸收情况在很大程度上尚不明确。本研究的目的是在美国东部五个具有三种截然不同土壤类型(包括三个蛇纹石土壤地点)的位点,原位测定三种本土假金属植物C草的土壤和叶片中的主要元素和微量元素浓度。

方法

测定了五个位点三种植物的土壤和叶片中15种元素的假全量和可提取浓度,并进行相关性分析。

结果

假金属植物土壤中的元素浓度变化高达五个数量级。含金属土壤中其特征元素的浓度高于不含金属的土壤。在含金属种群中,元素浓度取决于元素种类。叶片中主要元素(钙、镁、钾)的浓度低于典型毒性阈值,而锌的浓度较高。

结论

对于草类植物,即使土壤中元素浓度较高,物种仍可在叶片中维持相对较低的金属浓度。然而,在锌污染严重的土壤中,我们发现存在一个阈值浓度,高于该浓度锌的吸收会急剧增加。最后,一个位点缺乏蛇纹石土壤的主要特征表明了土壤调查和恢复对于维持蛇纹石植物群落以及避免土壤侵蚀的重要性。

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