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Microbial activity and phylogeny in ice cores retrieved of Lake Paula, a newly detected freshwater lake in Antarctica

机译:南极洲新发现的淡水湖保拉湖的冰芯中的微生物活性和系统发育

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A permanent ice covered water body, called Lake Paula, was detected in Patriot Hills in the West Antarctic and sampled for the first time ever for microbial life. The ice sheet measured approximately 2,5m thickness and the water body has a depth of about 10m. The lake is situated near a moraine which partly ablates from snow and provides meltwater from the slopes to the lake during austral summer. These running waters which are kept liquid by the heating up of the dark soil are penetrating the lower ice cover and thus softening up the lakeside part if the ice core. It is inoculated by nutrients, active microbes and diatoms of terrestrial origin. A distinct gradient concerning bacterial numbers, biomass and production which is 10 fold at the ice-water interface compared to the exposed part is observable. Temperature sensitivity of the embedded microbes reflect the gradient as well: Bacteria isolated from the upper part showed growth optima at 10℃, the lower part at 25℃, phylogenetic properties done by 16s rDNA reveal distinct communities depending on their vertical position, some clones are similar to those retrieved in Lake Vostok ice cores. These results offer the conclusion that even in this harsh environment like the Antarctic continent a dynamic system like microbial ice aggregates can be sustained as long as the supply of liquid water which is essential for an active bacterial metabolism is provided at least for a small time frame.
机译:在南极西部的爱国者丘陵地区发现了一个永久性的冰盖水域,称为保拉湖,并首次进行了微生物生命取样。冰盖的厚度约为2.5m,水体的深度约为10m。该湖位于冰ora附近,在夏季,部分冰被雪消融,并从山坡向湖中提供融水。这些由于深色土壤的加热而保持液态的自来水渗入下部冰盖,从而软化了冰芯(如果是冰芯)。它是由营养,活跃的微生物和陆生硅藻接种的。可以观察到与细菌​​数量,生物量和产生量有关的明显梯度,在冰水界面处,与暴露部分相比,梯度是其十倍。包埋的微生物的温度敏感性也反映了梯度:从上部分离的细菌在10℃时显示最佳生长,在25℃的下部时显示最佳生长,通过16s rDNA完成的系统发育特性根据其垂直位置显示出不同的群落,有些克隆是类似于在沃斯托克湖冰芯中发现的那些。这些结果提供了这样的结论,即,即使在诸如南极洲这样的严酷环境中,只要至少在很短的时间内就提供了对细菌主动代谢至关重要的液态水,就可以维持诸如微生物冰团块之类的动力系统。 。

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