1979
DOI: 10.1128/aem.37.5.924-927.1979
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Evidence that bacteria can form new cells in airborne particles

Abstract: Serratia marcescens incubated for 8 h at 31 degrees C in a chemically defined medium contained in shake flasks was aerosolized into rotating-drum aerosol chambers at 30 degrees C and saturated humidity. Cells furnished tryptone (Difco) and glycerol just before aerosolization increased (in viable numbers and countable cells) almost twofold within 1 to 2 h after becoming airborne, whereas cells not furnished additional tryptone decreased in viable numbers at a faster rate than the number of particles removed by … Show more

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Cited by 47 publications
(11 citation statements)
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“…The majority of isolates from the atmosphere are usually bacteria of high guanine (G) and cytosine (C) content DNA, which is more resistant to UV damage compared to low G/C content, and/or with pigmented cell walls, which enhance their UV blocking capacity [76,77]. Air microbiota can also suffer from dehydration and desiccation, but their incorporation into clouds and fog droplets can protect them and sustain their viability and activity [78][79][80]. Viable bacteria, fungi and yeasts have been observed in fogs, super-cooled cloud droplets, and snow samples [10,11,81].…”
Section: The Atmosphere As a Source Of Beneficial Microbes In The Viementioning
confidence: 99%
“…The majority of isolates from the atmosphere are usually bacteria of high guanine (G) and cytosine (C) content DNA, which is more resistant to UV damage compared to low G/C content, and/or with pigmented cell walls, which enhance their UV blocking capacity [76,77]. Air microbiota can also suffer from dehydration and desiccation, but their incorporation into clouds and fog droplets can protect them and sustain their viability and activity [78][79][80]. Viable bacteria, fungi and yeasts have been observed in fogs, super-cooled cloud droplets, and snow samples [10,11,81].…”
Section: The Atmosphere As a Source Of Beneficial Microbes In The Viementioning
confidence: 99%
“…The question of whether airborne cells are actively growing in aerosols was answered first by Dimmick et al (1979), who demonstrated that bacteria could divide on airborne particles, increasing from 7.3 × 10 5 to 1.4 × 10 6 cells L −1 within 6 h. However, considering the fact that different cloud types can persist for several days or weeks in the atmosphere before dissolving and being precipitated, respectively, it would be more accurate to see microorganisms as transients. Here, the huge challenge would be to survive and reproduce if the niche to which they are already adapted is present at the site of deposition, readapt to the new ecological niche upon deposition or remain dormant pending some future change in the environment.…”
Section: Aerial Growth and Survivalmentioning
confidence: 99%
“…It is assumed that the liquid and super‐cooled water from which the free tropospheric clouds are composed provides a better temporary habitat for living airborne cells than dry air, where desiccation can be a limiting factor for growth. Thus cloud droplets may provide a medium in which these cells can divide, as suggested by Dimmick et al (1979), Fuzzi et al (1997) and Sattler et al (2001). However, cloud water presents some specific characteristics such as acidic pH (generally from 3 to 7), high oxidative capacity, the presence of toxic compounds such as formaldehyde, high light (including UV) exposure, and relatively low temperatures (from −15 to 10°C at Puy de Dôme – see http://wwwobs.univ-bpclermont.fr/observ/chimie/DATA/pdd_Choix.html).…”
Section: Introductionmentioning
confidence: 99%