铁氧化细菌的研究

Trevor J. Hancock
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引用次数: 0

摘要

铁氧化细菌是一种化学营养细菌,它们通过氧化溶解的亚铁来获得生存和繁殖所需的能量。已知它们在铁浓度低至0.1毫克/升的水中生长和增殖。然而,无论如何,需要0.3 ppm的分解氧来进行氧化。铁是生物体进行许多代谢反应所需的重要成分,如铁硫蛋白、血红蛋白和配位复合物等参与生化反应的蛋白质的形成。这种元素在地球上分布广泛,被认为是地壳、土壤和沉积物中最丰富的元素之一。铁是海洋环境中的微量元素之一。它在消化一些趋化养石生物中的作用可能是古老的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Study of Iron-Oxidizing Bacteria
Iron-oxidizing bacteria are chemotrophic bacteria that derive the energy they need to live and multiply by oxidizing dissolved ferrous iron. They are known to grow and proliferate in waters containing iron concentrations as low as 0.1 mg/L. However, at any rate 0.3 ppm of disintegrated oxygen is needed to carry out oxidation. Iron is a significant component required by living organisms to carry out numerous metabolic reactions such as formation of proteins involved in biochemical reactions, like iron-sulfur proteins, haemoglobin and coordination complexes. This element has a widespread distribution in the planet and is considered as one of the most abundant in the Earth's crust, soil and sediments. Iron is one of the trace elements in marine environments. Its role in the digestion of some chemolithotrophs is probably ancient.
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