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Hailstones: A Window into the Microbial and Chemical Inventory of a Storm Cloud
被引:172
作者:
Santl-Temkiv, Tina
[1
,2
,3
]
Finster, Kai
[2
,3
]
Dittmar, Thorsten
[4
]
Hansen, Bjarne Munk
[1
]
Thyrhaug, Runar
[5
]
Nielsen, Niels Woetmann
[6
]
Karlson, Ulrich Gosewinkel
[1
]
机构:
[1] Aarhus Univ, Dept Environm Sci, Roskilde, Denmark
[2] Aarhus Univ, Dept Biosci, Microbiol Sect, Aarhus, Denmark
[3] Aarhus Univ, Dept Phys & Astron, Stellar Astrophys Ctr, Aarhus, Denmark
[4] Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm, Max Planck Res Grp Marine Geochem, D-26111 Oldenburg, Germany
[5] Univ Bergen, Dept Biol, Bergen, Norway
[6] Danish Meteorol Inst, Copenhagen, Denmark
来源:
PLOS ONE
|
2013年
/
8卷
/
01期
基金:
欧洲研究理事会;
新加坡国家研究基金会;
关键词:
DISSOLVED ORGANIC-MATTER;
MOLECULAR CHARACTERIZATION;
WATER;
MASS;
CARBON;
ENUMERATION;
CHEMISTRY;
BACTERIA;
COMMUNITIES;
VARIABILITY;
D O I:
10.1371/journal.pone.0053550
中图分类号:
O [数理科学和化学];
P [天文学、地球科学];
Q [生物科学];
N [自然科学总论];
学科分类号:
07 ;
0710 ;
09 ;
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 mu M) and total dissolved nitrogen (Me = 30 mu M), 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 (gamma-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.
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