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首页> 外文期刊>Environmental microbiology >Fungal oxidative dissolution of the Mn(II)-bearing mineral rhodochrosite and the role of metabolites in manganese oxide formation
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Fungal oxidative dissolution of the Mn(II)-bearing mineral rhodochrosite and the role of metabolites in manganese oxide formation

机译:含锰(II)的矿物菱锰矿的真菌氧化溶解及代谢产物在氧化锰形成中的作用

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Microbially mediated oxidation of Mn(II) to Mn(III/IV) oxides influences the cycling of metals and remineralization of carbon. Despite the prevalence of Mn(II)-bearing minerals in nature, little is known regarding the ability of microbes to oxidize mineral-hosted Mn(II). Here, we explored oxidation of the Mn(II)-bearing mineral rhodochrosite (MnCO_3) and characteristics of ensuing Mn oxides by six Mn(II)-oxidizing Ascomycete fungi. All fungal species substantially enhanced rhodochrosite dissolution and surface modification. Mineral-hosted Mn(II) was oxidized resulting in formation of Mn(III/IV) oxides that were all similar to δ-MnO_2 but varied in morphology and distribution in relation to cellular structures and the MnCO_3 surface. For four fungi, Mn(II) oxidation occurred along hyphae, likely mediated by cell wall-associated proteins. For two species, Mn(II) oxidation occurred via reaction with fungal-derived superoxide produced at hyphal tips. This pathway ultimately resulted in structurally unique Mn oxide clusters formed at substantial distances from any cellular structure. Taken together, findings for these two fungi strongly point to a role for fungal-derived organic molecules in Mn(III) complexation and Mn oxide templation. Overall, this study illustrates the importance of fungi in rhodochrosite dissolution, extends the relevance of biogenic superoxide-based Mn(II) oxidation and highlights the potential role of mycogenic exudates in directing mineral precipitation.
机译:微生物介导的Mn(II)氧化为Mn(III / IV)氧化物会影响金属的循环和碳的再矿化。尽管自然界中普遍存在含Mn(II)的矿物质,但关于微生物氧化矿物承载的Mn(II)的能力知之甚少。在这里,我们探讨了含锰(II)的矿物菱锰矿(MnCO_3)的氧化作用以及随后被六种锰(II)氧化的子囊真菌所产生的锰氧化物的特性。所有真菌种类都大大增强了菱锰矿的溶解和表面改性。矿物承载的Mn(II)被氧化,导致形成Mn(III / IV)氧化物,这些氧化物均与δ-MnO_2相似,但在形态和分布方面与细胞结构和MnCO_3表面有关。对于四种真菌,Mn(II)氧化沿菌丝发生,可能是由细胞壁相关蛋白介导的。对于两种物种,Mn(II)氧化是通过与菌丝尖端产生的真菌衍生的超氧化物反应而发生的。该途径最终导致在距任何细胞结构相当远的距离处形成的结构独特的Mn氧化物簇。综上所述,这两种真菌的发现强烈指出了真菌衍生的有机分子在Mn(III)络合和Mn氧化物模板中的作用。总的来说,这项研究说明了真菌在菱锰矿溶解中的重要性,扩展了基于生物超氧化物的Mn(II)氧化的相关性,并强调了致真菌分泌物在指导矿物沉淀中的潜在作用。

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