Gray N D, Howarth R, Pickup R W, Jones J G, Head I M
Fossil Fuels and Environmental Geochemistry Postgraduate Institute (NRG), University of Newcastle, Newcastle upon Tyne NE1 7RU.
Appl Environ Microbiol. 1999 Nov;65(11):5100-6. doi: 10.1128/AEM.65.11.5100-5106.1999.
Microautoradiography was used to investigate substrate uptake by natural communities of uncultured bacteria from the genus Achromatium. Studies of the uptake of (14)C-labelled substrates demonstrated that Achromatium cells from freshwater sediments were able to assimilate (14)C from bicarbonate, acetate, and protein hydrolysate; however, (14)C-labelled glucose was not assimilated. The pattern of substrate uptake by Achromatium spp. was therefore similar to those of a number of other freshwater and marine sulfur-oxidizing bacteria. Different patterns of radiolabelled bicarbonate uptake were noted for Achromatium communities from different geographical locations and indicated that one community (Rydal Water) possessed autotrophic potential, while the other (Hell Kettles) did not. Furthermore, the patterns of organic substrate uptake within a single population suggested that physiological diversity existed in natural communities of Achromatium. These observations are consistent with and may relate to the phylogenetic diversity observed in Achromatium communities. Incubation of Achromatium-bearing sediment cores from Rydal Water with (35)S-labelled sulfate in the presence and absence of sodium molybdate demonstrated that this bacterial population was capable of oxidizing sulfide to intracellular elemental sulfur. This finding supported the role of Achromatium in the oxidative component of a tightly coupled sulfur cycle in Rydal Water sediment. The oxidation of sulfide to sulfur and ultimately to sulfate by Achromatium cells from Rydal Water sediment is consistent with an ability to conserve energy from sulfide oxidation.
运用显微放射自显影技术研究了无色菌属未培养细菌的自然群落对底物的摄取情况。对摄取(^{14}C)标记底物的研究表明,来自淡水沉积物的无色菌细胞能够从碳酸氢盐、乙酸盐和蛋白水解物中同化(^{14}C);然而,(^{14}C)标记的葡萄糖未被同化。因此,无色菌属对底物的摄取模式与其他一些淡水和海洋硫氧化细菌相似。来自不同地理位置的无色菌群落对放射性标记碳酸氢盐的摄取模式不同,这表明一个群落(瑞德尔湖)具有自养潜力,而另一个群落(地狱壶)则没有。此外,单一群体内有机底物的摄取模式表明,无色菌的自然群落中存在生理多样性。这些观察结果与在无色菌群落中观察到的系统发育多样性一致,并且可能与之相关。在有和没有钼酸钠的情况下,用(^{35}S)标记的硫酸盐培养来自瑞德尔湖含有无色菌的沉积物岩心,结果表明该细菌群体能够将硫化物氧化为细胞内的元素硫。这一发现支持了无色菌在瑞德尔湖沉积物紧密耦合的硫循环氧化部分中的作用。瑞德尔湖沉积物中的无色菌细胞将硫化物氧化为硫并最终氧化为硫酸盐,这与从硫化物氧化中保存能量的能力是一致的。