2020
DOI: 10.3390/atmos11080802
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Airborne Bacterial and Eukaryotic Community Structure across the United Kingdom Revealed by High-Throughput Sequencing

Abstract: Primary biological aerosols often include allergenic and pathogenic microorganisms posing potential risks to human health. Moreover, there are airborne plant and animal pathogens that may have ecological and economic impact. In this study, we used high-throughput sequencing techniques (Illumina, MiSeq) targeting the 16S rRNA genes of bacteria and the 18S rRNA genes of eukaryotes, to characterize airborne primary biological aerosols. We used a filtration system on the UK Facility for Airborne Atmospheric Measur… Show more

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Cited by 6 publications
(5 citation statements)
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“…Gusareva et al [ 1 ] also found that the plant-associated reads in the tropical air ecosystem collapsed at the level of Viridiplantae, according to 18S rRNA gene sequencing, but in this case the Fungi RA was on average more than 30 times greater than the mean Viridiplantae RA. Song et al [ 14 ] also applied 18S rRNA gene sequencing to PM samples collected across the United Kingdom, reporting that Fungi and Plantae (Phragmoplastophyta phylum) contributed on average 48.3% and 37.4%, respectively. Findings from our research, which are partially contrasting with those from the above-cited studies, may be ascribed to the strong dependence of the eukaryotic kingdom emission sources on the geographical characteristics of the monitoring region/country, and its corresponding atmospheric factors.…”
Section: Resultsmentioning
confidence: 99%
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“…Gusareva et al [ 1 ] also found that the plant-associated reads in the tropical air ecosystem collapsed at the level of Viridiplantae, according to 18S rRNA gene sequencing, but in this case the Fungi RA was on average more than 30 times greater than the mean Viridiplantae RA. Song et al [ 14 ] also applied 18S rRNA gene sequencing to PM samples collected across the United Kingdom, reporting that Fungi and Plantae (Phragmoplastophyta phylum) contributed on average 48.3% and 37.4%, respectively. Findings from our research, which are partially contrasting with those from the above-cited studies, may be ascribed to the strong dependence of the eukaryotic kingdom emission sources on the geographical characteristics of the monitoring region/country, and its corresponding atmospheric factors.…”
Section: Resultsmentioning
confidence: 99%
“…The phylum Microsporidia is a large group of eukaryotic obligate intracellular parasites that can only complete their life cycle within an infected eukaryotic host cell [ 26 ]. Ascomycota and Basidiomycota are the two largest fungal phyla, widespread in many environments, including the atmosphere [ 14 ], and were further analysed in this study since they were the most abundant and pervasive ones in the collected PM10 samples. The predominance of Ascomycota in airborne particles, as compared to Basidiomycota Fungi, was reported in many studies performed worldwide [ 16 , 25 , 27 ].…”
Section: Resultsmentioning
confidence: 99%
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“…The BIOARC project (Towards a UK Airborne Bioaerosol Climatology) aimed to evaluate the airborne concentrations of BioPM in the UK via targeted aircraft and groundbased sampling; early emerging results from the aircraft campaign were presented by Song et al [18] who demonstrated that Cladosporium was a major component in the boundary layer via PCR analysis. In this study, we present an overview and synthesis of the UKbased ground site UV-LIF bioaerosol spectrometer datasets collected during BIOARC.…”
Section: Aims and Objectivesmentioning
confidence: 99%
“…Primary ice formation at temperatures warmer than −38 • C requires the presence of a catalyst ice nuclei (IN) particle via heterogeneous processes [14,15], where certain species of BioPM have been identified as potent IN in the critical −15 to 0 • C warm regime owing to the presence of ice nucleating proteins. Fungi such as Fusarium have displayed ice activity as warm as −3.5 • C [16], and such fungi have been observed in the upper atmosphere and free tropospheric cloud water samples [17][18][19]. Significantly, only small quantities (~0.01 L −1 ) of such warm temperature IN are needed to induce rapid mixed-phase cloud glaciation via secondary ice processes, resulting in reduced cloud lifetime and reflectivity, ultimately impacting the radiation budget [20].…”
Section: Introductionmentioning
confidence: 99%