铁锰氧化细菌胆氏细螺旋体SP-6的表面反应性

Maicon Araujo, Daniela Gutierrez Rueda, Yuhao Li, Janice Kenney, Daniel Alessi, Kurt Konhauser
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引用次数: 0

摘要

原核细胞的表面对水溶液中金属的吸附和自生矿物的形成起着重要的作用(Konhauser 2006)。尽管大多数研究集中在细胞壁上,但众所周知,许多细菌合成细胞外的多糖和蛋白质层,包括被称为鞘的物质。研究表明,蓝细菌Calothrix sp.产生的鞘在环中性pH值下具有中性电荷,并且假设这种鞘可能允许蓝细菌在高硅化率的地热环境中生存(Phoenix et al. 2002)。具体来说,钙思鞘表面羟基位点的优势促进了与水性二氧化硅的氢键,诱导了鞘上无定形二氧化硅的沉淀,从而保护了下面的细胞(Phoenix et al. 2002)。胆氏细螺旋体是一种被护套的铁和锰氧化细菌,经常栖息在矿物质渗漏中,其中铁2+和锰2+排放到含氧地表水中(Spring et al. 1996)。因此,鞘层被铁(III)和锰(IV)氢氧化物包裹,而下面的细胞受到保护,免受矿化(Emerson和Ghiorse 1992, Emerson et al. 2010)。然而,与钩丝虱不同的是,钩丝虱的鞘成分表明,它在环中性pH下的行为可能不同(Emerson和giorse 1993)。为了研究钩螺旋体鞘和细胞壁的表面反应性,我们分析了分离的L. cholodnii SP-6鞘、无鞘细胞和完整的细丝。我们使用电位滴定、ζ电位、cd吸附和傅里叶变换红外(FTIR)光谱来研究这些成分,以阐明细胞壁和鞘之间表面电荷的变化。对于分离的鞘和完整的细丝,采用两点质子化模型拟合滴定数据,得到的pKa值分别为6.05(±0.29)和9.34(±0.11);分别为7.77(±0.17)和10.50(±0.20)。对于无鞘细胞,采用三位点质子化模型拟合最佳,得到的pKa值分别为5.40(±0.59)、8.11(±1.64)和10.73(±0.45)。与完整的细丝相比,分离鞘中的总质子活性位点浓度较低。此外,在环中性的pH下,与完整的细丝和分离的鞘相比,无鞘细胞的净负电荷更低(图1)。这一信息与三种材料的Cd吸附行为一致(图2)。因此,我们的初步结果表明,细刺虫的鞘比完整的细丝在环中性的pH下反应性更低,这使我们假设最外层会隔离相对较少的阳离子,包括Mn 2+。从溶液中,可能会保护下层细胞免受有害的矿化。除此之外,反应性较低的鞘表面也有助于细胞附着,这对溪流中常见的物种很重要(Phoenix et al. 2002, Emerson et al. 2010)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Surface reactivity of the iron and manganese-oxidizing bacterium Leptothrix cholodnii SP-6
Surfaces of prokaryotic cells play a significant role in the adsorption of metals from aqueous solution and the formation of authigenic minerals (Konhauser 2006). Although most studies focus on the cell wall, it is known that many bacteria synthesise an extracellular layer of polysaccharides and proteins, including what are known as sheaths. It has been shown that the cyanobacterium Calothrix sp. produces as sheath which is neutrally charged at circumneutral pH values, and it was hypothesized that such a sheath might allow the cyanobacterium to survive in geothermal settings with high silicification rates (Phoenix et al. 2002). Specifically, the dominance of hydroxyl sites on Calothrix ’s sheath surface facilitates hydrogen bonding with aqueous silica species, inducing the precipitation of amorphous silica on the sheath and thus protecting the underlying cell (Phoenix et al. 2002). Leptothrix cholodnii is a sheathed, iron and manganese-oxidizing bacterium that frequently inhabits minerals seeps, where Fe 2+ and Mn 2+ discharge into oxygenated surface waters (Spring et al. 1996). As a result, the sheath becomes encrusted with Fe(III) and Mn(IV) oxyhydroxides while the underlying cells are protected from mineralization (Emerson and Ghiorse 1992, Emerson et al. 2010). However, unlike Calothrix, Leptothrix’ s sheath composition suggests that it might behave differently at circumneutral pH (Emerson and Ghiorse 1993). To investigate the surface reactivity of Leptothrix 's sheath and cell wall we analyzed isolated sheaths, sheathless cells, and intact filaments of L. cholodnii SP-6. We studied these components using potentiometric titration, zeta-potential, Cd-adsorption, and Fourier transform infrared (FTIR) spectroscopy to elucidate changes in surface charge between the cell wall and sheath. For the isolated sheaths and intact filaments, titration data were fit using a two-site protonation model, resulting in the following pKa values: 6.05 (±0.29) and 9.34 (±0.11); and 7.77 (±0.17) and 10.50 (±0.20), respectively. For the sheathless cells, the best fit was obtained by using a three-site protonation model, resulting in the following pKa values: 5.40 (±0.59), 8.11 (±1.64) and 10.73 (±0.45). Total proton-active site concentrations were lower in isolated sheaths compared to intact filaments. Additionally, at circumneutral pH, net negative charge was lower for sheathless cells compared to intact filaments and isolated sheaths (Fig. 1). This information agrees with the Cd adsorption behaviour found for the three materials (Fig. 2). Thus, our preliminary results suggest that Leptothrix ’s sheath is less reactive than the intact filaments at circumneutral pH, leading us to hypothesize that the outermost layer would sequester relatively lower amounts of cations, including Mn 2+ , from solution and potentially would protect the underlaying cell from deleterious mineralization. In addition to that, the less reactive sheath’s surface would also contribute to cell attachment, which is important for a species commonly found in streams (Phoenix et al. 2002, Emerson et al. 2010).
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