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Sulfide as a soil phytotoxin—a review

机译:硫化物作为土壤植物毒素的研究进展

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摘要

In wetland soils and underwater sediments of marine, brackish and freshwater systems, the strong phytotoxin sulfide may accumulate as a result of microbial reduction of sulfate during anaerobiosis, its level depending on prevailing edaphic conditions. In this review, we compare an extensive body of literature on phytotoxic effects of this reduced sulfur compound in different ecosystem types, and review the effects of sulfide at multiple ecosystem levels: the ecophysiological functioning of individual plants, plant-microbe associations, and community effects including competition and facilitation interactions. Recent publications on multi-species interactions in the rhizosphere show even more complex mechanisms explaining sulfide resistance. It is concluded that sulfide is a potent phytotoxin, profoundly affecting plant fitness and ecosystem functioning in the full range of wetland types including coastal systems, and at several levels. Traditional toxicity testing including hydroponic approaches generally neglect rhizospheric effects, which makes it difficult to extrapolate results to real ecosystem processes. To explain the differential effects of sulfide at the different organizational levels, profound knowledge about the biogeochemical, plant physiological and ecological rhizosphere processes is vital. This information is even more important, as anthropogenic inputs of sulfur into freshwater ecosystems and organic loads into freshwater and marine systems are still much higher than natural levels, and are steeply increasing in Asia. In addition, higher temperatures as a result of global climate change may lead to higher sulfide production rates in shallow waters.
机译:在海洋,咸淡水和淡水系统的湿地土壤和水下沉积物中,由于厌氧作用期间硫酸盐的微生物还原作用,强烈的植物毒素硫化物可能积累,其含量取决于普遍的营养条件。在这篇综述中,我们比较了有关这种还原的硫化合物在不同生态系统类型中的植物毒性作用的大量文献,并综述了硫化物在多种生态系统水平上的影响:单个植物的生态生理功能,植物-微生物协会和社区效应包括竞争和促进互动。关于根际中多种物种相互作用的最新出版物显示了更复杂的机理来解释抗硫化物性。结论是,硫化物是一种有效的植物毒素,在包括沿海系统在内的所有湿地类型中以及在几个层面上都深刻影响植物的适应能力和生态系统功能。传统的毒性试验(包括水耕法)通常忽略了根际效应,这使得很难将结果推算到实际的生态系统过程中。为了解释硫化物在不同组织水平上的不同作用,对生物地球化学,植物生理和生态根际过程的深入了解至关重要。这些信息甚至更加重要,因为人为地将硫输入淡水生态系统,并将有机负荷输入淡水和海洋系统仍然远远高于自然水平,并且在亚洲急剧增加。此外,由于全球气候变化而导致的较高温度可能导致浅水区较高的硫化物生产率。

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