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Thermophilic fermentative bacteria from a deep borehole in granitic rock in Sweden

机译:瑞典花岗岩中深层钻孔的热敏发酵细菌

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A borehole drilled to a final depth of 6779 m in granitic rock in Gravberg, Sweden, was sampled and examined for the presence and activity of anaerobic bacteria. The application of anaerobic enrichment and isolation techniques resulted in pure cultures of various fermenting bacteria. Growth in enrichment cultures was observed only in those cultures inoculated from water samples from a depth of 3500 m. Pure cultures of anaerobic, fermenting bacteria were obtained with the following substrates: glucose, starch, xylane, ethanol, and lactate. All isolated bacteria were so far undiscribed bacteria by means of their physiological properties. One strain of the glucose fermenting bacteria was further characterized concerning its phylogenetic position and was found to be closest related to Clostridium thermohydrosulfuricum. However, by means of its characteristic metabolism, it was clearly separated from C. thermohydrosulfuricum. No sulfate-reducing or methanogenic bacteria were found in any of the samples. Fermentative bacteria growing in the presence of hematite often reduced the iron and induced the formation and deposition of insoluble iron sulfides.
机译:对瑞典格贝格的花岗岩岩石中钻到6779米的最终深度的钻孔,并检测厌氧细菌的存在和活性。厌氧富集和分离技术的应用导致各种发酵细菌的纯培养物。仅在从3500米的水样中接种的那些培养物中观察到富集培养物的生长。用以下底物获得纯胰腺,发酵细菌:葡萄糖,淀粉,二甲苯,乙醇和乳酸。所有孤立的细菌都是通过其生理特性到目前为止的细菌。一种葡萄糖发酵细菌的一种菌株进一步表征其有关其系统发育位置,并被发现与梭菌热氢核素相关。然而,通过其特征性代谢,它显然将其与C. Thermohoshosulcumum分离。在任何样品中发现不含硫酸盐或甲状腺细菌。在赤铁矿存在下生长的发酵细菌通常还原铁并诱导不溶性硫化铁的形成和沉积。

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