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Hailstones: A Window into the Microbial and Chemical Inventory of a Storm Cloud

机译:冰雹:进入风暴云的微生物和化学资源清单的窗口

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摘要

Storm clouds frequently form in the summer period in temperate climate zones. Studies on these inaccessible and short-lived atmospheric habitats have been scarce. We report here on the first comprehensive biogeochemical investigation of a storm cloud using hailstones as a natural stochastic sampling tool. A detailed molecular analysis of the dissolved organic matter in individual hailstones via ultra-high resolution mass spectrometry revealed the molecular formulae of almost 3000 different compounds. Only a small fraction of these compounds were rapidly biodegradable carbohydrates and lipids, suitable for microbial consumption during the lifetime of cloud droplets. However, as the cloud environment was characterized by a low bacterial density (Me = 1973 cells/ml) as well as high concentrations of both dissolved organic carbon (Me = 179 µM) and total dissolved nitrogen (Me = 30 µM), already trace amounts of easily degradable organic compounds suffice to support bacterial growth. The molecular fingerprints revealed a mainly soil origin of dissolved organic matter and a minor contribution of plant-surface compounds. In contrast, both the total and the cultivable bacterial community were skewed by bacterial groups (γ-Proteobacteria, Sphingobacteriales and Methylobacterium) that indicated the dominance of plant-surface bacteria. The enrichment of plant-associated bacterial groups points at a selection process of microbial genera in the course of cloud formation, which could affect the long-distance transport and spatial distribution of bacteria on Earth. Based on our results we hypothesize that plant-associated bacteria were more likely than soil bacteria (i) to survive the airborne state due to adaptations to life in the phyllosphere, which in many respects matches the demands encountered in the atmosphere and (ii) to grow on the suitable fraction of dissolved organic matter in clouds due to their ecological strategy. We conclude that storm clouds are among the most extreme habitats on Earth, where microbial life exists.
机译:夏季,温带气候区经常形成暴风云。对这些无法进入且短暂的大气生境的研究很少。我们在此报告使用冰雹作为自然随机抽样工具对暴风云进行的首次全面生物地球化学研究。通过超高分辨率质谱对单个冰雹中的溶解有机物进行了详细的分子分析,揭示了近3000种不同化合物的分子式。这些化合物中只有一小部分是可快速生物降解的碳水化合物和脂质,适合在云滴的生命周期内消耗微生物。但是,由于云环境的特征是细菌密度低(Me = 1973细胞/ ml)以及高浓度的溶解有机碳(Me = 179 µM)和总溶解氮(Me = 30 µM),已经被痕量一定数量的易于降解的有机化合物足以支持细菌的生长。分子指纹图谱表明,土壤主要是溶解有机物的起源,而植物表面化合物的贡献很小。相反,全部细菌和可培养细菌群落均受细菌群体(γ-变形杆菌,鞘氨醇杆菌和甲基细菌)的偏斜影响,这表明植物表面细菌占主导地位。植物相关细菌群的富集指向云形成过程中微生物属的选择过程,这可能影响细菌在地球上的长距离迁移和空间分布。根据我们的结果,我们假设植物相关细菌比土壤细菌更有可能(i)由于对叶球生命的适应而在空气中存活,这在许多方面都与大气中遇到的需求相匹配,并且(ii)由于其生态策略,可以在云中溶解的有机物的适当比例上生长。我们得出的结论是,暴风云是地球上存在微生物生命的最极端的栖息地之一。

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