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Microbial and biochemical alterations due to storage of deep-sea sediments under ambient tropical conditions

机译:在热带环境下深海沉积物的储存导致微生物和生化变化

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Response of indigenous bacteria to incubation at normal pressure and tropical temperature (28 +/- 2 degrees C), were examined in four deep-sea sediments from polymetallic-nodule fields in Central Indian Basin (CIB). Sediments were stored in sterile air-tight polythene containers. Changes in microbial and biochemical parameters were monitored once in every two months for a year. Bacterial counts and ATP decreased from similar to 10(8) to similar to 10(7) g-(1) and similar to 10(1) to similar to 10(1) ng g(-1) dry sediment respectively, within 8-10 months before stabilization. Protein: carbohydrate ratio fluctuated considerably. The four samples responded distinctively to storage, suggesting dependence of variations on inherent sedimentary properties. Though bacteriologically and biochemically altered, the integrity of metals in sediments changed only marginally. Sediment properties evolved from a non-steady phase to a steady phase.
机译:在印度中部盆地(CIB)多金属结核田的四个深海沉积物中,研究了土著细菌对在常压和热带温度(28 +/- 2摄氏度)下孵化的响应。沉积物存储在无菌的不透气聚乙烯容器中。一年中每两个月监测一次微生物和生化参数的变化。细菌计数和ATP分别在8内从类似于10(8)降至类似于10(7)g-(1)和类似于10(1)类似于类似于10(1)ng g(-1)的干沉物。稳定前-10个月。蛋白质:碳水化合物的比例波动很大。这四个样品对储层的响应明显不同,表明变化对固有沉积特性的依赖性。尽管在细菌学和生物化学方面发生了变化,但沉积物中金属的完整性仅发生了少量变化。沉积物性质从非稳定阶段发展到稳定阶段。

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