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A flow cytometric method to measure prokaryotic records in ice cores: an example from the West Antarctic Ice Sheet Divide drilling site

机译:一种流式细胞术方法,用于测量冰芯中的原核记录:西南南极冰盖分钻场的示例

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摘要

Microorganisms were the earliest inhabitants on our planet that occupy nearly every environment, and play a major role in biogeochemical cycles. Despite their global importance, there remains a paucity of data on microbial responses to long-term environmental and climatic changes. Microorganisms are known to be immured in glacial ice, but no high-resolution temporal records of their density exist, owing in large part to the lack of appropriate clean methodology that allows for rapid analysis of samples over depth. We describe a clean and time efficient method that can produce a high-temporal resolution record of prokaryotic density archived in ice cores. The method combines acquisition of discrete samples using a continuous ice-core melting system coupled with flow cytometry (FCM) of DNA-stained samples. Specifically, we evaluate the performance of the FCM measurement technique in terms of specificity, precision, accuracy and minimum detection limits. Examples from the West Antarctic Ice Sheet Divide ice core are included to show the efficacy of the method.
机译:微生物是我们这个星球上最早的居民,占据了几乎每一个环境,并在生物地球化学周期中发挥重要作用。尽管其全球重要性,但仍然存在关于长期环境和气候变化的微生物反应数据。已知微生物在冰川冰中浸泡,但没有存在密度的高分辨率时间记录,因此由于缺乏适当的清洁方法,允许快速分析水平的水平。我们描述了一种清洁和时间的有效方法,可以在冰芯中归档的原核密度的高时间分辨率记录。该方法使用与DNA染色样品的流式细胞术(FCM)联接的连续冰芯熔化系统相结合了离散样品。具体而言,我们在特异性,精度,准确度和最小检测限度方面评估FCM测量技术的性能。包括西南极冰片划分冰芯的实例,以显示该方法的功效。

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