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Biofilm adaptation to iron availability in the presence of biotite and consequences for chemical weathering

机译:在黑云母存在下生物膜对铁有效性的适应及其对化学风化的影响

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摘要

Bacteria in nature often live within biofilms, exopolymeric matrices that provide a favorable environment that can differ markedly from their surroundings. Biofilms have been found growing on mineral surfaces and are expected to play a role in weathering those surfaces, but a clear understanding of how environmental factors, such as trace-nutrient limitation, influence this role is lacking. Here, we examine biofilm development by Pseudomonas putida in media either deficient or sufficient in Fe during growth on biotite, an Fe rich mineral, or on glass. We hypothesized that the bacteria would respond to Fe deficiency by enhancing biotite dissolution and by the formation of binding sites to inhibit Fe leaching from the system. Glass coupons acted as a no-Fe control to investigate whether biofilm response depended on the presence of Fe in the supporting solid. Biofilms grown on biotite, as compared to glass, had significantly greater biofilm biomass, specific numbers of viable cells (SNVC), and biofilm cation concentrations of K, Mg, and Fe, and these differences were greater when Fe was deficient in the medium. Scanning electron microscopy (SEM) confirmed that biofilm growth altered the biotite surface, smoothing the rough, jagged edges of channels scratched by hand on the biotite, and dissolving away small, easy-to-access particles scattered across the planar surface. High-resolution magic angle spinning proton nuclear magnetic resonance (HRMAS H-1 NMR) spectroscopy showed that, in the Fe-deficient medium, the relative amount of polysaccharide nearly doubled relative to that in biofilms grown in the medium amended with Fe. The results imply that the bacteria responded to the Fe deficiency by obtaining Fe from biotite and used the biofilm matrix to enhance weathering and as a sink for released cation nutrients. These results demonstrate one mechanism by which biofilms may help soil microbes overcome nutrient deficiencies in oligotrophic systems.
机译:自然界中的细菌通常生活在生物膜(共聚基质)中,生物膜提供了与其周围环境明显不同的有利环境。已经发现生物膜生长在矿物表面上,并有望在使这些表面风化中发挥作用,但缺乏对环境因素(例如微量营养素限制)如何影响该作用的清晰理解。在这里,我们研究了恶臭假单胞菌在黑云母,富含铁的矿物或玻璃上生长过程中,铁缺乏或足够的培养基中生物膜的发育。我们假设该细菌将通过增强黑云母溶解和通过形成结合位点来抑制铁从系统中的浸出而对铁缺乏做出反应。玻璃样片用作无铁对照,以研究生物膜响应是否取决于支撑固体中铁的存在。与玻璃相比,在黑云母上生长的生物膜具有更大的生物膜生物量,活细胞的特定数量(SNVC)以及K,Mg和Fe的生物膜阳离子浓度,当铁在培养基中缺乏时,这些差异会更大。扫描电子显微镜(SEM)证实,生物膜的生长改变了黑云母的表面,使用手在黑云母上划伤的通道的粗糙,锯齿状的边缘变得光滑,并溶解了分散在整个平面上的小且易于接近的颗粒。高分辨率魔角旋转质子核磁共振波谱(HRMAS H-1 NMR)光谱显示,在缺铁培养基中,多糖的相对量比在用Fe修饰的培养基中生长的生物膜中的相对含量几乎翻倍。结果表明,细菌通过从黑云母中获取铁来应对铁缺乏症,并利用生物膜基质增强了耐候性并用作释放阳离子养分的汇。这些结果证明了生物膜可以帮助土壤微生物克服贫营养系统中营养缺乏的一种机制。

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