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Iron-Oxidizing Bacteria Are Associated with Ferric Hydroxide Precipitates (Fe-Plaque) on the Roots of Wetland Plants

机译:铁氧化细菌与湿地植物根系上的氢氧化铁沉淀(铁斑)相关

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摘要

The presence of Fe-oxidizing bacteria in the rhizosphere of four different species of wetland plants was investigated in a diverse wetland environment that had Fe(II) concentrations ranging from tens to hundreds of micromoles per liter and a pH range of 3.5 to 6.8. Enrichments for neutrophilic, putatively lithotrophic Fe-oxidizing bacteria were successful on roots from all four species; acidophilic Fe-oxidizing bacteria were enriched only on roots from plants whose root systems were exposed to soil solutions with a pH of <4. In Sagittaria australis there was a positive correlation (P < 0.01) between cell numbers and the total amount of Fe present; the same correlation was not found for Leersia oryzoides. These results present the first evidence for culturable Fe-oxidizing bacteria associated with Fe-plaque in the rhizosphere.
机译:在不同的湿地环境中研究了四种不同湿地植物的根际中铁氧化细菌的存在,这些环境的Fe(II)浓度范围为每升数十至数百微摩尔,pH范围为3.5至6.8。在所有四个物种的根部成功富集了嗜中性的,嗜盐性的铁氧化性铁细菌。嗜酸性铁氧化细菌仅富集在植物的根上,该植物的根系暴露于pH <4的土壤溶液中。在南方人参中,细胞数量与Fe的总量呈正相关(P <0.01)。未发现米曲霉具有相同的相关性。这些结果为根际中与铁斑相关的可培养铁氧化细菌提供了第一个证据。

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