High levels of primary biogenic organic aerosols are
driven by only a few plant-associated microbial taxa

Abdoulaye Samaké, Aurélie Bonin, Jean-Luc Jaffrezo, Pierre Taberlet, Samuel Weber, Gaëlle Uzu, Véronique Jacob, Sébastien Conil, Jean M.F. Martins

► To cite this version:

Abdoulaye Samaké, Aurélie Bonin, Jean-Luc Jaffrezo, Pierre Taberlet, Samuel Weber, et al. High levels of primary biogenic organic aerosols are driven by only a few plant-associated microbial taxa. Atmospheric Chemistry and Physics, 2020, 20 (9), pp.5609-5628. 10.5194/acp-20-5609-2020. hal-03038657

HAL Id: hal-03038657

https://hal.science/hal-03038657

Submitted on 12 Mar 2021

**HAL** is a multi-disciplinary open access
archive for the deposit and dissemination of sci-
entific research documents, whether they are pub-
lished or not. The documents may come from
teaching and research institutions in France or
abroad, or from public or private research centers.

L'archive ouverte pluridisciplinaire HAL, est
destinée au dépôt et à la diffusion de documents
scientifiques de niveau recherche, publiés ou non,
émanant des établissements d'enseignement et de
recherche français ou étrangers, des laboratoires
publics ou privés.

<figure><img src="image_1.png" /></figure>
<figure><img src="image_2.png" /></figure>

# High levels of primary biogenic organic aerosols are driven by only a few plant-associated microbial taxa

Abdoulaye Samaké<fnref n="1" />, Aurélie Bonin<fnref n="2" />, Jean-Luc Jaffrezo<fnref n="1" />, Pierre Taberlet<fnref n="2" />, Samuël Weber<fnref n="1" />, Gaëlle Uzu<fnref n="1" />, Véronique Jacob<fnref n="1" />, Sébastien Conil<fnref n="3" />, and Jean M. F. Martins<fnref n="1" />

**Correspondence:** Abdoulaye Samaké (abdoulaye.samake2@univ-grenoble-alpes.fr) and Jean Martins (jean.martins@univ-grenoble-alpes.fr)

Received: 15 December 2019 – Discussion started: 9 January 2020
Revised: 11 March 2020 – Accepted: 14 April 2020 – Published: 13 May 2020

**Abstract.** Primary biogenic organic aerosols (PBOAs) represent a major fraction of coarse organic matter (OM) in air. Despite their implication in many atmospheric processes and human health problems, we surprisingly know little about PBOA characteristics (i.e., composition, dominant sources, and contribution to airborne particles). In addition, specific primary sugar compounds (SCs) are generally used as markers of PBOAs associated with bacteria and fungi, but our knowledge of microbial communities associated with atmospheric particulate matter (PM) remains incomplete. This work aimed at providing a comprehensive understanding of the microbial fingerprints associated with SCs in PM₁₀ (particles smaller than 10 µm) and their main sources in the surrounding environment (soils and vegetation). An intensive study was conducted on PM₁₀ collected at a rural background site located in an agricultural area in France. We combined high-throughput sequencing of bacteria and fungi with detailed physicochemical characterizations of PM₁₀, soil, and plant samples and monitored meteorological and agricultural activities throughout the sampling period. Results show that in summer SCs in PM₁₀ are a major contributor of OM in air, representing 0.8% to 13.5% of OM mass. SC concentrations are clearly determined by the abundance of only a few specific airborne fungal and bacterial taxa. The temporal fluctuations in the abundance of only four predominant fungal genera, namely *Cladosporium*, *Alternaria*, *Sporobolomyces*, and *Dioszegia*, reflect the temporal dynamics in SC concentrations. Among bacterial taxa, the abundance of only *Massilia*, *Pseudomonas*, *Frigoribacterium*, and *Sphingomonas* is posi-

tively correlated with SC species. These microbes are significantly enhanced in leaf over soil samples. Interestingly, the overall community structure of bacteria and fungi are similar within PM₁₀ and leaf samples and significantly distinct between PM₁₀ and soil samples, indicating that surrounding vegetation is the major source of SC-associated microbial taxa in PM₁₀ in this rural area of France.

## 1 Introduction

Airborne particulate matter (PM) is the subject of high scientific and political interest mainly because of its important effects on climate and public health (Boucher et al., 2013; Fröhlich-Nowoisky et al., 2016; Fuzzi et al., 2006). Numerous epidemiological studies have significantly related both acute and chronic exposures to ambient PM with respiratory impairments, heart diseases, asthma, and lung cancer, as well as increased risk of mortality (Kelly and Fussell, 2015; Lecours et al., 2017; Pope and Dockery, 2006). PM can also affect directly or indirectly the climate by absorbing and/or diffusing both the incoming and outgoing solar radiation (Boucher et al., 2013; Fröhlich-Nowoisky et al., 2016). These effects are modulated by highly variable physical characteristics (e.g., size, specific surface, concentrations) and the complex chemical composition of PM (Fröhlich-Nowoisky et al., 2016; Fuzzi et al., 2015). PM consists of a complex mixture of inorganic trace elements and carbonaceous matter (organic carbon and elemental carbon), with organic mat-

<footnote n="1">¹Université Grenoble Alpes, CNRS, IRD, INP-G, IGE (UMR 5001), Grenoble, 38000, France</footnote>

<footnote n="2">²Université Grenoble Alpes, CNRS, LECA (UMR 5553), BP 53, Grenoble, 38041, France</footnote>

<footnote n="3">³ANDRA DRD/OPE Observatoire Pérenne de l'Environnement, 55290 Bure, France</footnote>
ter (OM) generally being the major but poorly characterized
constituent of PM (Boucher et al., 2013; Bozzetti et al., 2016;
Fortenberry et al., 2018). A quantitative understanding of
OM sources is critically important to develop efficient guide-
lines for both air-quality control and abatement strategies. So
far, considerable efforts have been undertaken to investigate
OM associated with anthropogenic and secondary sources,
but much less is known about emissions from primary bio-
genic sources (Bozzetti et al., 2016; China et al., 2018; Yan
et al., 2019).

Primary biogenic organic aerosols (PBOAs) are a subset
of organic PM that are directly emitted by processes in-
volving the biosphere (Boucher et al., 2013; Elbert et al.,
2007). PBOAs typically refer to biologically derived mate-
rials, notably including living organisms (e.g., bacteria, fun-
gal spores, Protozoa, viruses), nonliving biomass (e.g., mi-
crobial fragments), and other types of biological materials
like pollen or plant debris (Amato et al., 2017; Elbert et al.,
2007; Fröhlich-Nowoisky et al., 2016). PBOAs are gaining
increasing attention notably because of their ability to affect
human health by causing infectious, toxic, and hypersensi-
tivity diseases (Fröhlich-Nowoisky et al., 2016; Huffman et
al., 2019). For instance, PBOA components, especially fun-
gal spores and bacterial cells, have recently been shown to
cause significant oxidative potential (Samaké et al., 2017).
However, to date, the precise role of PBOA components and
interplay regarding mechanisms of diseases are remarkably
misunderstood (Coz et al., 2010; Hill et al., 2017). Specific
PBOA components can also participate in many relevant at-
mospheric processes like cloud condensation and ice nucle-
ation, thereby directly or indirectly affecting the Earth's hy-
drological cycle and radiative balance (Boucher et al., 2013;
Fröhlich-Nowoisky et al., 2016; Hill et al., 2017). These di-
verse impacts are effective at a regional scale due to the
transport of PBOAs (Dommergue et al., 2019; Yu et al.,
2016). Moreover, PBOAs are a major component of OM
found in particles less than 10 µm in aerodynamic diameter
(PM₁₀) (Bozzetti et al., 2016; Coz et al., 2010; Samaké et
al., 2019b). For instance, Bozzetti et al. (2016) have shown
that PBOAs equal the contribution of secondary organic
aerosols (SOAs) to OM in PM₁₀ collected at a rural back-
ground site in Switzerland during both the summer and win-
ter periods. However, current estimates of global terrestrial
PBOA emissions are very uncertain and range between 50
and 1000 Tg yr⁻¹ (Boucher et al., 2013; Coz et al., 2010; El-
bert et al., 2007), underlining the critical gap in the under-
standing of this significant OM fraction.

The recent application of fluorescent technics, such as
the ultraviolet aerodynamic particle sizer, the wideband in-
tegrated bioaerosol sensor (Bozzetti et al., 2016; Gosselin
et al., 2016; Huffman and Santarpia, 2017; Huffman et al.,
2019), and scanning electron microscopy (Coz et al., 2010),
has provided very insightful information on the abundance
of size-segregated ambient PBOAs. Atmospheric sources of
PBOAs are numerous and include agricultural activities, leaf

abrasion, and soil resuspension (Coz et al., 2010; Medeiros
et al., 2006; Pietrogrande et al., 2014). To date, the detailed
constituents of PBOAs, their predominant sources, and their
atmospheric emission processes, as well as their contribu-
tions to total airborne particles, remain poorly documented
and quantified (Bozzetti et al., 2016; Coz et al., 2010; Elbert
et al., 2007). Such information would be important for inves-
tigating the properties and atmospheric impacts of PBOAs, as
well as for a future optimization of source-resolved chemical
transport models (CTMs), which are still generally unable to
accurately simulate important OM fractions (Ciarelli et al.,
2016; Heald et al., 2011; Kang et al., 2018).

Primary sugar compounds (SCs, defined as sugar alcohols and saccharides) are ubiquitous water-soluble compounds found in atmospheric PM (Gosselin et al., 2016; Medeiros et al., 2006; Pietrogrande et al., 2014; Jia et al., 2010b). SC species are emitted from biologically derived sources (Medeiros et al., 2006; Verma et al., 2018) and have sometimes been detected in aerosols taken from air masses influenced by smoke from biomass burning (Fu et al., 2012; Yang et al., 2012). However, recent studies conducted at several sites across France revealed a weak correlation between daily concentrations of SC and levoglucosan in PM<sub>2.5</sub> and PM<sub>10</sub> collected throughout the year (Golly et al., 2018; Samaké et al., 2019a). This suggests that the open burning of biomass is not a significant source of SCs in the environments studied here. In this context, specific SC species are still extensively viewed as powerful markers for tracking sources and estimating PBOA contributions to OM mass (Bauer et al., 2008; Gosselin et al., 2016; Jia et al., 2010b; Medeiros et al., 2006). For example, glucose is the most common monosaccharide in vascular plants, and it has been predominantly used as an indicator of plant material (such as pollen or plant debris) from several areas around the world (Jia et al., 2010b; Medeiros et al., 2006; Pietrogrande et al., 2014; Verma et al., 2018). Trehalose (a.k.a. mycose) is a common metabolite of various microorganisms, serving as an osmoprotectant accumulating in a cell's cytosol during harsh conditions (e.g., dehydration and heat) (Bougouffa et al., 2014). It has been proposed as a generic indicator of soil-borne microbiota (Jia et al., 2010b; Medeiros et al., 2006; Pietrogrande et al., 2014; Verma et al., 2018). Similarly, mannitol and arabitol are two very common sugar alcohols (also called polyols), serving as storage and transport solutes in fungi (Gosselin et al., 2016; Medeiros et al., 2006; Verma et al., 2018). Their atmospheric concentration levels have frequently been used to investigate fungal spore contributions to PBOA mass in different environments (urban, rural, costal, and polar) around the world (Barbaro et al., 2015; Gosselin et al., 2016; Jia et al., 2010b; Verma et al., 2018; Weber et al., 2018).

Despite the relatively vast literature using the atmospheric
concentration levels of SCs as potential suitable markers of
PBOAs associated with bacteria and fungi, our understand-
ing of associated airborne microbial communities (i.e., di-
versity and community composition) remains poor. This is
due in particular to the lack of high-resolution (i.e., daily) data sets characterizing how well the variability of these microbial communities may be related to that of primary sugar species. Such information is of paramount importance to better understand the dominant atmospheric sources of SCs (and then PBOAs), as well as their relevant effective environmental drivers, which are still poorly documented (Bozzetti et al., 2016).

Our recent works discussed the size distribution features and the spatial and temporal variability in atmospheric particulate SC concentrations in France (Golly et al., 2018; Samaké et al., 2019a, b). As a continuation, in this study we present the first daily temporal-concurrent characterization of ambient SC species concentrations and both bacterial and fungal community compositions for PM₁₀ collected at a rural background site located in an intensive agricultural area. The aim of this study was to use a DNA metabarcoding approach (Taberlet et al., 2018) to investigate PM₁₀-associated microbial communities, which can help answer the following research questions. (i) What are the microbial community structures associated with PM₁₀? (ii) Is the temporal dynamics of SC concentrations related to changes in the airborne microbial community composition? (iii) What are the predominant sources of SC-associated microbial communities at a continental rural field site? Since soil and vegetation are currently believed to be the dominant sources of airborne microorganisms in most continental areas (Bowers et al., 2011; Jia et al., 2010a; Rathnayake et al., 2016), our study focused on these two potential sources.

# 2 Material and methods

## 2.1 Site description

The Observatoire Pérenne de l'Environnement (OPE) is a continental rural background observatory located about 230 km east of Paris at an altitude of 392 m (Fig. 1). This French critical zone observatory (CZO) is part of a long-term multidisciplinary project monitoring the state of environmental variables, including among others fluxes, abiotic and biotic variables, and their functions and dynamics (http://ope.andra.fr/index.php?lang=en, last access: 10 December 2019). It is largely impacted by agricultural activities. It is also characterized by a low population density (less than 22 per square kilometer within an area of 900 km²) with no industrial activities or surrounding major transport roads. The air monitoring site itself lies in a "reference sector" of 240 km² in the middle of a field crop area (tens of kilometers in all directions). This reference sector is composed of vast farmlands interspersed with wooded areas. The area is further defined by a homogeneous soil type with a predominantly superficial clay–limestone composition. The daily agricultural practices and meteorological data (including wind speed and direction, temperature, rainfall level, and

relative humidity) within the reference sector are recorded and made available by ANDRA (Agence nationale pour la gestion des déchets radioactifs). The agricultural fields of the area are generally submitted to a 3-year crop-rotation system. The major crops during the campaign period were pea and oilseed rape.

## 2.2 Sample collection

An intensive field campaign was conducted at this site for the sake of the present study. The aerosol sampling campaign period lasted from 12 June to 21 August 2017, covering the summer period in France. During this period, ambient PM₁₀ was collected daily (from 09:00 UTC to 09:00 UTC the next day) onto prebaked quartz fiber filters (Pall Tissuquartz 2500QAT-UP, Ø = 150 mm) using high-volume samplers (Aerosol Sampler DHA-80, DIGITEL; 24 h at 30 m³ h⁻¹). After collection, all filter samples were wrapped in aluminum foil, sealed in zipper plastic bags, and stored at <4 °C until further analysis. More details on the preparation, storage, and handling of these filter samples can be found in Samaké et al. (2019b). A total of 69 samples and 6 field blanks were collected.

Surface soil samples (0–5 cm depth, 15 cm × 15 cm area) were simultaneously collected from two fields within the pea and oilseed rape growing areas. The fields are located in the immediate vicinity of the PM₁₀ sampler and under the prevailing wind directions (Fig. 1). To represent as closely as possible the local soil microbial communities, we randomly collected five subsamples (about 100 g per sampling unit) within each parcel and pooled them. Topsoil sampling took place on a weekly basis during the campaign period. After collection and homogenization, 15 g of each subsample was stored in airtight containers (sterile bottles, Schott, GL45, 100 mL) containing the same weight of sterile silica gel (around 15 g). Such a soil desiccation method is a straightforward approach to prevent any microbial growth and change in community over time at room temperature (Taberlet et al., 2018). A total of eight topsoil samples were collected for each parcel.

Finally, leaf samples were collected from the major types of vegetation within the reference sector. These include leaves of oilseed rape, pea, oak, maple, beech, and herbs (Fig. 1). A total of eight leaf samples were analyzed. These samples were also stored in airtight containers (sterile bottles, Schott, GL45, 100 mL) containing 15 g of silica gel. It should be noted that leaf samples were collected only once, 4 weeks after the end of PM and soil sampling, while the major crops were still on site.

## 2.3 Chemical analyses

Daily PM₁₀ samples were analyzed for various chemical species using subsampled fractions of the collection filters and a large array of analytical methods. Detailed information
<figure><img src="image_3.png" /><figcaption>**Figure 1.** Overview of the sampling area at the OPE site (France). (a) Location of sampling units and (b) wind conditions (speed and direction) during the field-sampling campaign period.</figcaption></figure>

<figure><img src="image_4.png" /></figure>

on all the chemical-analysis procedures has been reported previously (Golly et al., 2018; Samaké et al., 2019b; Waked et al., 2014). Briefly, SCs (i.e., polyols and saccharides) and water-soluble ions (including Ca²⁺) were systematically analyzed in all samples, using respectively high-performance liquid chromatography with pulsed amperometric detection (HPLC-PAD) and ionic chromatography (IC; Thermo Fisher ICS 3000, USA). Free-cellulose concentrations were determined using an optimized enzymatic hydrolysis (Samaké et al., 2019a) and the subsequent analysis method of the resultant glucose units using HPLC-PAD (Golly et al., 2018; Samaké et al., 2019b; Waked et al., 2014). Organic and elemental carbon (OC, EC) were analyzed using a Sunset thermal-optic instrument and the EUSAAR2 protocol (Cavalli et al., 2010). This analytical method requires a high temperature, thereby constraining the choice of quartz as the sampling filter material. OM content in PM₁₀ samples was then estimated using an OM-to-OC conversion factor of 1.8: OM = 1.8 × OC (Samaké et al., 2019a, b). This value of 1.8 for the OM/OC ratio was chosen on the basis of previous studies carried out in France (Samaké et al., 2019b, and references therein)

## 2.4 Biological analyses: DNA extraction in PM₁₀ samples

Aerosol samples typically contain very low DNA concentrations, and the DNA-binding properties of the quartz fibers of aerosol collection filters make its extraction with traditional protocols challenging (Dommergue et al., 2019; Jiang et al., 2015; Luhung et al., 2015). In the present study, we were also constrained by the limited daily collection filter surface for the simultaneous chemical and microbiological analyses of the same filters. To circumvent issues of low efficiency during genomic DNA extraction, several technical improvements have been made to optimize the extraction of

high-quality DNA from PM₁₀ samples (Dommergue et al., 2019; Jiang et al., 2015; Luhung et al., 2015). This includes thermal water bath sonication helping the lysis process in thick cell walls (e.g., fungal spores and Gram-positive bacteria), which might not be effectively lysed solely by means of bead beating (Luhung et al., 2015). Some consecutive (2 d at maximum) quartz filter samples with low OM concentrations were also pooled when necessary. Detailed information regarding the resultant composite samples (labeled A1 to A36) is presented in Table S1 in the Supplement. Figure S1 in the Supplement presents the average concentration levels of SC species in each sample. The results clearly show that air samples can be categorized from low (background, from A1 to A4 and A21 to A36) to high (peak, from A5 to A20) PM₁₀-SC concentration levels.

In terms of DNA extraction, one-quarter (about 38.5 cm²) of each filter sample was used. First, filter aliquots were aseptically inserted into individual 50 mL Falcon tubes filed with sterilized saturated phosphate buffer (Na₂HPO₄, NaH₂PO₄, 0.12 M; pH ≈ 8). PM₁₀ was desorbed from the filter samples by gentle shaking for 10 min at 250 rpm. This pretreatment allows the separation of the collected particles from the quartz filters thanks to the high competing interaction between the saturated phosphate buffer and the charged biological materials (Jiang et al., 2015; Taberlet et al., 2018). After gentle vortex mixing, the subsequent resuspension was filtered with a polyethersulfone membrane disk filter (Supor® PES 47 mm 200, 0.2 µm, Pall, USA). We repeated this desorbing step three times to enhance the recovery of the biological material from the quartz filters. Each collection PES membrane was then shredded into small pieces and used for DNA extractions using the DNeasy PowerWater kit (Qiagen, Germantown, MD, USA). The standard protocol of the supplier was followed with only minor modifications: 30 min of thermal water bath sonication at 65 °C (EMAG, Emmi-60 HC, Germany; 50% efficiency) and 5 min of bead beating
before and after sonication were added. Finally, DNA was eluted in 50 µL of EB buffer. Such an optimized protocol has been recently shown to produce a 10-fold increase in DNA extraction efficiency (Dommergue et al., 2019; Luhung et al., 2015), thereby allowing high-throughput sequencing of air samples. Note that all the steps mentioned above were performed under laminar flow hoods and that materials (filter funnels, forceps, and scissors) were sterilized prior to use.

## 2.4.1 Biological analyses: DNA extraction from soil and leaf samples

The soil sample pretreatment and the extracellular DNA extraction were achieved following an optimized protocol proposed elsewhere (Taberlet et al., 2018). Briefly, this protocol involves thoroughly mixing and extracting 15 g of soil in 15 mL of sterile saturated phosphate buffer for 15 min. About 2 mL of the resulting extracts was centrifuged for 10 min at 10 000 g, and 500 µL of the resulting supernatant was used for DNA extraction using the NucleoSpin Soil Kit (Macherey-Nagel, Düren, Germany) following the manufacturer's original protocol after skipping the cell lysis step. Finally, DNA was eluted with 100 µL of SE buffer.

To extract DNA from either endophytic or epiphytic microorganisms, aliquots of leaf samples (about 25–30 mg) were extracted with the DNeasy Plant Mini Kit (QIAGEN, Germany) according to the supplier's instructions with the following minor modifications: after the resuspension of powdered samples in 400 µL of AP1 buffer, the samples were incubated for 45 min at 65 °C with RNase A. Finally, DNA was eluted with 100 µL of AE buffer.

## 2.4.2 Biological analyses: polymerase chain reaction amplification and sequencing

Bacterial and fungal community compositions were surveyed using, respectively, the Bact02 (Forward 5'-KGCCAGCMGCCGCGGTAA-3' and Reverse 3'-GGACTACCMGGGTATCTAA-5') and Fung02 (Forward 5'-GGAAGTAAAAGTCGTAACAAGG-3' and Reverse 3'-CAAGAGATCCGTTGYTGAAAGTK-5') published primer pairs (see Taberlet et al., 2018, for details on these primers). The primer pair Bact02 targets the V4 region of the bacterial 16S rDNA region while the Fung02 primer pair targets the nuclear ribosomal internal transcribed spacer region 1 (ITS1). Four independent PCR (polymerase chain reaction) replicates were carried out for each DNA extract. Eight nucleotide tags were added to both primer ends to uniquely identify each sample, ensuring that each PCR replicate was labeled by a unique combination of forward and reverse tags. The tag sequences were created with the oligotag command within the open-source OBITools software suite (Boyer et al., 2016) so that all pairwise tag combinations were differentiated by at least five different base pairs (Taberlet et al., 2018).

DNA amplification was performed in a 20 µL total volume solution containing 10 µL of AmpliTaq Gold 360 Master Mix (Applied Biosystems, Foster City, CA, USA), 0.16 µL of 20 mg mL⁻¹ bovine serum albumin (BSA; Roche Diagnostics, Basel, Switzerland), 0.2 µM of each primer, and 2 µL of diluted DNA extract. DNA extracts from soil and filters were diluted eight times, while DNA extracts from leaves were diluted four times. Amplifications were performed using the following thermocycling program: an initial activation of DNA polymerase for 10 min at 95 °C; x cycles of 30 s denaturation at 95 °C, 30 s annealing at 53 °C and 56 °C for bacteria and fungi, respectively, and 90 s elongation at 72 °C; and a final extension at 72 °C for 7 min. The number of cycles x was determined by qPCR and set at 40 for all markers and DNA extract types, except for the Bact02 amplification of soil and leaf samples (30 cycles) and the Fung02 amplification of filter samples (42 cycles). After amplification, about 10 % of amplification products were randomly selected and verified using a QIAxcel Advanced device (QIAGEN, Hilden, Germany) equipped with a high-resolution cartridge for separation.

After amplification, PCR products from the same marker were pooled in equal volumes and cleaned with the MinElute PCR purification kit (Qiagen, Hilden, Germany), following the manufacturer's instructions. The two pools were sent to Fasteris SA (Geneva, Switzerland; https://www.fasteris.com/dna/, last access: 10 December 2019) for library preparation and MiSeq Illumina 2 × 250 bp paired-end sequencing. The two sequencing libraries (one per marker) were prepared according to the PCR-free MetaFast protocol (https://www.fasteris.com/dna/?q=content/metastar-protocol-amplicon-metagenomic-analysis, last access: 10 May 2020), which aims at limiting the formation of chimeras.

To monitor any potential false positives inherent to tag jumps and contamination (Schnell et al., 2015), the sequencing experiment included both extraction and PCR negatives, as well as unused tag combinations.

## 2.4.3 Bioinformatic analyses of raw reads

The Illumina raw sequence reads were processed separately for each library using the OBITools software suite (Boyer et al., 2016), specifically dedicated to metabarcoding data processing. First, the raw paired-ends were assembled using the illumina paired-end program, and the sequences with a low alignment score (fastq average quality score <40) were discarded. The aligned sequences were then assigned to the corresponding PCR replicates with the program ngsfilter by allowing zero and two mismatches on tags and primers, respectively. Strictly identical sequences were dereplicated using the program obuniq, and a basic filtration step was performed with the obligrep program to select sequences within the expected range length (i.e., longer than 65 and 39 bp for fungi and bacteria, respectively, excluding tags and primers), with-
out ambiguous nucleotides, and observed at least 10 times in
at least one PCR replicate.

The remaining unique sequences were grouped and as-
signed to molecular operational taxonomic units (MOTUs)
with a 97% sequence identity using the Sumatra and
Sumaclust programs (Mercier et al., 2013). The Sumatra
algorithm computes pairwise similarities among sequences
based on the length of the longest common subsequence, and
the Sumaclust program uses these similarities to cluster the
sequences (Mercier et al., 2013). An abundance of sequences
belonging to the same cluster was summed up, and the cluster
center was defined as the MOTU representative of the cluster
(Mercier et al., 2013).

The taxonomic classification of each MOTU was per-
formed using the ecotag program (Boyer et al., 2016), which
uses full-length metabarcodes as references. The ecoPCR
program (Ficetola et al., 2010) was used to build the metabar-
code reference database for each marker. Briefly, ecoPCR
performs an in silico amplification within the EMBL public
database (release 133), using the Fung02 and Bact02 primer
pairs and allowing a maximum of three mismatches per
primer. The resultant reference database was further refined
by keeping only sequence records assigned at the species,
genus, and family levels.

After taxonomic assignment, data sets were acquired, and
further processing with the open-source R software (RStu-
dio interface, version 3.4.1) was performed to filter out
chimeras, potential contaminants, and failed PCR replicates.
More specifically, MOTUs that were highly dissimilar to
any reference sequence (sequence identity <0.95) were con-
sidered chimeras and discarded. Secondly, MOTUs whose
abundance was higher in extraction and PCR negatives were
also excluded. Finally, PCR replicates inconstantly distant
from the barycenter of the four PCR replicates correspond-
ing to the same sample were considered dysfunctional and
discarded. The remaining PCR replicates were summed up
per sample.

## 2.5 Data analysis

Unless specified otherwise, all exploratory statistical anal-
yses were achieved with R. Rarefaction and extrapolation
curves were obtained with the iNEXT 2.0-12 package (Hsieh
et al., 2016) to investigate the gain in species richness as we
increased the sequencing depth for each sample. Alpha di-
versity estimators including Shannon and Chao1 were cal-
culated with the phyloseq 1.22-3 package (McMurdie and
Holmes, 2013) on data rarefied to the same sequencing depth
per sample type (see Table S2 for details on the rarefaction
depths). Nonmetric multidimensional scaling (NMDS) ordi-
nation analysis was performed to decipher the temporal pat-
terns in airborne microbial community structures (phylum
or class taxonomic group) in air samples. These analyses
were achieved with the metaMDS function within the vegan
package (Oksanen et al., 2019) with the number of random

starts set to 500. The NMDS ordinations were obtained us-
ing pairwise dissimilarity matrices based on Bray-Curtis in-
dex. The envfit function implemented in vegan was used to
assess the airborne microbial communities, which could ex-
plain the temporal dynamics of ambient SC species concen-
trations. Pairwise analysis of similarity (ANOSIM) was per-
formed to assess similarity between groups of PM₁₀ aerosol
samples. This was achieved using the anosim function of ve-
gan (Oksanen et al., 2019) with the number of permutations
set to 999. Spearman's rank correlation analysis was used to
investigate further the relationship between airborne micro-
bial communities and SC species.

To gain further insight into the dominant source of SC-
associated microbial communities, NMDS analysis based on
Horn distance was performed to compare the microbial com-
munity composition similarities between PM₁₀ aerosol, soil,
and leaf samples.

## 3 Results

### 3.1 Primary sugar compounds and relative
contributions to OM mass

Temporal dynamics of daily PM₁₀ carbonaceous components (e.g., primary sugar compounds, cellulose, and OM) are presented in Fig. 2. Nine SCs including seven polyols and two saccharide compounds have been quantified in all ambient PM₁₀ collected at the study site. Ambient SC concentration levels peaked on 8 August 2017 in excellent agreement with the daily harvest activities around the study site (Fig. 2a). The average concentration (average ± SD) of total SCs during the campaign is 259.8 ± 253.8 ng m⁻³ with a range of 26.6 to 1679.5 ng m⁻³, contributing on average to 5.7 ± 3.2% of total OM mass in PM₁₀ with a range of 0.8–13.5% (Fig. 2b). The total measured polyols present an average concentration of 26.3 ± 54.4 ng m⁻³. Among all the measured polyols, arabitol (67.4 ± 83.1 ng m⁻³) and mannitol (68.1 ± 75.3 ng m⁻³) are the predominant species, followed by lesser amounts of sorbitol (10.9 ± 7.6 ng m⁻³), erythritol (7.0 ± 8.8 ng m⁻³), inositol (2.3 ± 2.0 ng m⁻³), and xylitol (2.3 ± 3.0 ng m⁻³). Glycerol was also observed in our samples but with concentrations frequently below the quantification limit. The average concentration of saccharide compounds is 51.2 ± 45.0 ng m⁻³. Trehalose (55.8 ± 51.9 ng m⁻³) is the most abundant saccharide species, followed by glucose (46.9 ± 37.1 ng m⁻³). The average concentration of calcium is 251.1 ± 248.4 ng m⁻³.

A Spearman's rank correlation analysis based on the daily
dynamics was used to examine the relationships between
SC species. As shown in Table 1, sorbitol and inositol are
well-correlated linearly (R = 0.57, p<0.001). Herein, sor-
bitol (R = 0.59, p<0.001) and inositol (R = 0.64, p<0.001)
are significantly correlated to Ca²⁺. It can also be noted that
all other SC species are highly correlated with each other
<figure><img src="image_5.png" /><figcaption>**Figure 2.** Ambient concentrations of carbonaceous components in PM₁₀. (a, c–f) Daily variations in SC and calcium concentrations along with daily agricultural activities around the site. (b) Contribution of SCs to organic matter mass. Results for 9-week daily measurements indicate that SCs together represent a large fraction of OM, contributing to between 0.8 % to 13.5 % of OM mass in summer. Glycerol is not presented because its concentration was generally below the quantification limit.</figcaption></figure>

($p<0.001$) and that they are weakly correlated to the temporal dynamics of sorbitol and inositol (Table 1).

## 3.2 Microbial characterization of samples, richness and diversity

The structures of bacterial and fungal communities were generated for the 62 collected samples, consisting of 36 aerosol, 18 surface soil, and 8 leaf samples. After paired-end assembly of sequence reads, sample assignment, filtering based on sequence length and quality, and discarding rare sequences, we are left with 2 575 857 and 1 647 000 reads respectively for fungi and bacteria, corresponding to 4762 and 5852

unique sequences, respectively. After the clustering of high-quality sequences, potential contaminants, and chimeras, the final data sets (all samples pooled) consist respectively of 597 and 944 MOTUs for fungi and bacteria, with 1 959 549 and 901 539 reads. The average number of reads (average ± SE) per sample is 31 607 ± 2072 and 14 563 ± 1221 for fungi and bacteria, respectively. The rarefaction curves of MOTU diversity showed common logarithmic shapes approaching a plateau in all cases (Fig. S2). This indicates an overall sufficient sequencing depth to capture the diversity of sequences occurring in the different types of samples. To compare the microbial community diversity and species richness, data normalization was performed by randomly selecting from
<table><caption>**Table 1.** Relationships between SCs and calcium in PM₁₀ from the study site. Spearman's rank correlation analyses are based on the daily dynamics of chemical species (n = 69).</caption><thead><tr><th></th><th>Arabitol</th><th>Mannitol</th><th>Glucose</th><th>Trehalose</th><th>Erythritol</th><th>Xylitol</th><th>Sorbitol</th><th>Inositol</th><th>Ca<sup>2+</sup></th></tr></thead><tbody><tr><td>Arabitol</td><td>1.00</td><td></td><td></td><td></td><td></td><td></td><td></td><td></td><td></td></tr><tr><td>Mannitol</td><td>0.94***</td><td>1.00</td><td></td><td></td><td></td><td></td><td></td><td></td><td></td></tr><tr><td>Glucose</td><td>0.90***</td><td>0.90***</td><td>1.00</td><td></td><td></td><td></td><td></td><td></td><td></td></tr><tr><td>Trehalose</td><td>0.93***</td><td>0.96***</td><td>0.87***</td><td>1.00</td><td></td><td></td><td></td><td></td><td></td></tr><tr><td>Erythritol</td><td>0.69***</td><td>0.51***</td><td>0.57***</td><td>0.56***</td><td>1.00</td><td></td><td></td><td></td><td></td></tr><tr><td>Xylitol</td><td>0.84***</td><td>0.84***</td><td>0.80***</td><td>0.79***</td><td>0.65***</td><td>1.00</td><td></td><td></td><td></td></tr><tr><td>Sorbitol</td><td>0.22</td><td>0.26*</td><td>0.35**</td><td>0.15</td><td>0.21</td><td>0.24*</td><td>1.00</td><td></td><td></td></tr><tr><td>Inositol</td><td>0.39**</td><td>0.24</td><td>0.34**</td><td>0.25*</td><td>0.71***</td><td>0.39**</td><td>0.57***</td><td>1.00</td><td></td></tr><tr><td>Ca<sup>2+</sup></td><td>0.12</td><td>0.11</td><td>0.11</td><td>0.09</td><td>0.30*</td><td>0.27*</td><td>0.59***</td><td>0.64***</td><td>1.00</td></tr></tbody></table>

Note: * p<0.1, ** p<0.01, *** p<0.001

each sample 4287 fungal sequence reads and 2865 bacterial sequence reads. The Chao1 values of fungi are higher for aerosol samples than for soil and leaf samples (p<0.05), indicating higher richness in airborne PM₁₀ (Fig. S3a). In contrast, PM₁₀ and soil samples showed higher values of Shannon index (p<0.05), indicating a higher fungal diversity in these ecosystems. The soil harbors higher bacterial richness and diversity than PM₁₀ (p<0.05), which in turn harbors greater richness and diversity compared to leaf samples (p<0.05) (Fig. S3b).

## 3.3 Taxonomic composition of airborne PM₁₀

### 3.3.1 Fungal communities

The statistical assignment of airborne PM₁₀ fungal MOTUs at different taxonomic levels reveals 3 phyla, 17 classes, 58 orders, and 160 families (Fig. 3). Interestingly, fungal MOTUs are dominated by two common phyla: Ascomycota (accounting for an average of 76 ± 20.4% (average ± SD) of fungal sequences across all air samples), followed by Basidiomycota (23.9 ± 20.4%). The remaining sequences correspond to Mucoromycota (<0.01%) and to unclassified sequences (approximately 0.03%). As evidenced in Fig. 3, the predominant (>1%) fungal classes are Dothideomycetes (70.0%), followed by Agaricomycetes (16.0%), Tremellomycetes (5.0%), Sordariomycetes (2.6%), Microbotryomycetes (2.2%), Leotiomycetes (1.8%), and Eurotiomycetes (1.4%). The predominant orders include Pleosporales (35.5%) and Capnodiales (34.4%), which belong to Ascomycota. Likewise, the dominant orders in Basidiomycota are Polyporales (7.5%), followed by Russulales (4.2%), Tremellales (2.8%), Hymenochaetales (2.6%), and Sporidiobolales (2.2%). At the genus level, about 327 taxa are characterized across all air samples, among which *Cladosporium* (32.9%), *Alternaria* (15.0%), *Epicoccum* (15.0%), *Peniophora* (2.7%), *Sporobolomyces* (2.2%), *Phlebia* (2.0%), and *Pyrenophora* (1.9%) are the most abundant communities.

### 3.3.2 Bacterial communities

For bacterial communities, the Bact02 marker allowed 17 phyla, 43 classes, 91 orders, and 182 families to be identified (Fig. 3). Predominant phyla include Proteobacteria (55.3 ± 8.6%), followed by Bacteroidetes (22.1±4.1%), Actinobacteria (14.2±2.2%), and Firmicutes (6±5.9%), with less than 1.8% of the total bacterial sequence reads being unclassified. At the class level, the predominant bacteria are Alphaproteobacteria (29.4%), Actinobacteria (13.8%), Gammaproteobacteria (12.1%), Betaproteobacteria (11.4%), Cytophagia (8.3%), Flavobacteriia (6.3%), Sphingobacteriia (5.9%), Bacilli (3.5%), and Clostridia (2.2%). As many as 392 genera were detected in all aerosol samples, although many sequences (22.8%) could not be taxonomically assigned at the genus level. The most abundant (>2%) genera are *Sphingomonas* (20.0%), followed by *Massilia* (8.4%), *Hymenobacter* (5.5%), *Pseudomonas* (5.1%), *Pedobacter* (3.3%), *Flavobacterium* (2.8%), *Chryseobacterium* (2.8%), *Frigoribacterium* (2.5%), and *Methylobacterium* (1.9%).

## 3.4 Relationship between airborne microbial community abundances and PM₁₀ SC species

The NMDS (nonmetric multidimensional scaling) ordination exploring the temporal dynamics of microbial community beta diversity among all PM₁₀ aerosol samples revealed significant temporal shifts in community structure for both fungi and bacteria (Fig. 4).

An NMDS (two dimensions, stress = 0.15) based on fungal class-level compositions (Fig. 4a) results in three distinct clusters of PM₁₀ samples. With one exception (A23), all air samples with higher SC concentration levels (A5 to A20, see Table S2 and Fig. S1) are clustered together and are distinct from those with background levels of atmospheric SC concentrations. This pattern is further confirmed with the analysis of similarity, which shows a significant separation of clusters of samples (ANOSIM, R = 0.31, p<0.01). As evidenced in Fig. 4a, this difference is
<figure><img src="image_6.png" /><figcaption>**Figure 3.** Taxonomic and phylogenetic trees of fungal and bacterial community structures in PM₁₀ at the study site. Phylogenetic trees are analyzed with the Environment for Tree Exploration (ETE3) package implemented in Python (Huerta-Cepas et al., 2016). The circle from the inner to the outer layer represents classification from kingdom to order successively. Further details on fungal and bacterial taxa at genus level are provided in Fig. S4. The node size represents the average relative abundance of taxa. Only nodes with relative abundance ≥ 1 are highlighted in bold.</figcaption></figure>

mainly explained by the NMDS1 axis, which results from
the predominance of only a few class-level fungi in PM₁₀
samples, including *Dothideomycetes*, *Tremellomycetes*, *Mi-
crobotryomycetes*, and *Exobasidiomycetes*. Vector fitting of

chemical time series data to the NMDS ordination plot indi-
cates that the latter four fungal community assemblages best
correlate with individual SC species. Mannitol (R² = 0.37,
p<0.01), arabitol (R² = 0.36, p<0.01), trehalose (R² =
0.41, p<0.01), glucose (R² = 0.33, p<0.01), xylitol (R² =
0.45, p<0.01), erythritol (R² = 0.40, p<0.01), and inositol
(R² = 0.24, p = 0.01) are significantly positively correlated
to the fungal assemblage ordination solution.

For bacterial phylum-level compositions (Fig. 4b), an
NMDS ordination (two dimensions, stress = 0.07) analysis
differentiates the PM₁₀ samples into two distinct clusters ac-
cording to their SC concentration levels. All air samples with
higher SC concentration levels except two (A23 and A24)
are clustered separately from those with ambient background
concentration levels. ANOSIM analysis (R = 0.69, p<0.01)
further confirms the significant difference between the two
clusters of samples. Proteobacteria constitute the most dom-
inant bacterial phylum during the SC peak over the sam-
pling period. Interestingly, changes in individual SC profiles
are significantly correlated with bacterial community tempo-
ral shifts (Fig. 4b). Mannitol (R² = 0.25, p<0.01), arabitol
(R² = 0.24, p<0.01), trehalose (R² = 0.32, p<0.01), glu-
cose (R² = 0.32, p<0.01), xylitol (R² = 0.38, p<0.01), and
erythritol (R² = 0.27, p<0.01) are mainly positively corre-
lated to the bacterial community dissimilarity.

Given the distinct clustering patterns of airborne PM₁₀ mi-
crobial beta diversity structures according to SC concentra-
tion levels, a Pearson’s rank correlation analysis has been
performed to further examine the relationship between indi-
vidual SC profiles and airborne microbial community abun-
dance at phylum and class levels. This analysis reveals that
for class-level fungi, the abundances of Dothideomycetes,
Tremellomycetes, and Microbotryomycetes are highly pos-
itively correlated (p<0.05) to the temporal evolutions of
the individual SC species concentration levels (Fig. S5a).
Likewise, ambient SC species concentration levels are sig-
nificantly correlated (p<0.05) to the Proteobacteria phylum
(Fig. S5b). To gain further insight into the airborne micro-
bial fingerprints associated with ambient SC species, cor-
relation analyses were also performed at a finer taxonomic
level. These analyses show that the temporal dynamics of
SC species primarily correlates best (p<0.05) with the *Cla-
dosporium*, *Alternaria*, *Sporobolomyces*, and *Dioszegia* fun-
gal genera (Fig. 5a). Similarly, the time series of SC species
are primarily positively correlated (p<0.05) with *Massilia*,
*Pseudomonas*, *Frigoribacterium*, and to a lesser degree (non-
significant) with the *Sphingomonas* bacterial genus (Fig. 5b).

3.5 Sources of airborne microbial communities at the study site

As shown in Fig. 6, the airborne microbial genera most
positively correlated with SC species are also distributed in
the surrounding environmental samples of surface soils and
leaves. In addition, microbial taxa of PM₁₀ associated with
<figure><img src="image_7.png" /><figcaption>**Figure 4.** Main airborne microbial communities associated with atmospheric concentrations of SC species. NMDS ordination plots are used to show the relationship among time series of aerosol samples. The stress values indicate an adequate two-dimensional picture of sample distribution. Ellipses represent 95 % confidence intervals for the cluster centroid. NMDS analyses are performed directly on taxonomically assigned quality-filtered sequence tables at class and phylum level for fungi (a) and bacteria (b), respectively. Ambient primary sugar concentration levels in PM₁₀ appear to be highly influenced by the airborne microbial community structure and abundance. Similar results are obtained with taxonomically assigned MOTU tables, highlighting the robustness of our methodology.</figcaption></figure>

SC species are generally more abundant in the leaf than in the topsoil samples (Fig. 6). In order to further explore and visualize the similarity of species compositions across local environment types, we conducted an NMDS ordination analysis (Fig. 7). As evidenced in Fig. 7, the beta diversities of fungal and bacterial MOTUs are more similar within the same habitat (PM₁₀, plant, or soil) and are grouped across habitats as expected. Interestingly, the beta diversities of fungal and bacterial MOTUs in leaf samples and those in airborne PM₁₀ are generally not readily distinguishable, with similarity becoming more prominent during atmospheric peaks of SC concentration levels (Fig. 6). However, the overall beta diversities in airborne PM₁₀ and in leaf samples are significantly different from those from topsoil samples (ANOSIM, R = 0.89 and 0.80 and *p*<0.01 for fungal and bacterial communities, respectively), without any overlap regardless of whether or not harvesting activities are performed around the sampling site.

This observation is also confirmed by an unsupervised hierarchical cluster analysis, which reveals a pattern similar to that observed in the NMDS ordination, where taxa from leaf samples and airborne PM₁₀ are clustered together regardless of whether ambient concentration levels of SC peaked or not. They are clustered separately from those of topsoil samples (Fig. S7).

## 4 Discussion

Very few studies exist on the interactions between the air microbiome and PM chemical profiles (Cao et al., 2014; Elbert et al., 2007). In this study, we used a comprehensive multidisciplinary approach to produce for the first time airborne microbial fingerprints associated with SC species in PM₁₀ and to identify the dominant sources of SCs in an extensively cultivated, continental rural area.
<figure><img src="image_8.png" /><figcaption>**Figure 5.** Heatmap of Spearman's rank correlation between SCs and abundance of airborne communities at the study site. (a) Fungal genera and (b) bacterial genera. Only genera with relative abundance ≥ 1 are shown.</figcaption></figure>

## 4.1 SCs as a major source of organic matter in PM₁₀

SC species have recently been reported to be ubiquitous in PM₁₀ collected in several areas in France (Golly et al., 2018; Samaké et al., 2019b). In this study, the total SCs presented an average concentration of 259.8 ± 253.8 ng m⁻³ with a range of 26.6 to 1679.5 ng m⁻³ in all air samples. These concentration values are on average 5 times higher than those typically observed in urban areas in France (average values during summer 48.5 ± 43.6 ng m⁻³) (Golly et al., 2018; Samaké et al., 2019a, b). However, these concentration levels are in agreement with a previous study conducted in a similar environment, i.e., continental rural sites located in large crop fields (Yan et al., 2019).

The total concentrations of SCs quantified in atmospheric PM₁₀ over our study site accounted for 0.8% to 13.5% of the daily OM mass. This is remarkable considering that less than 20% of total particulate OM mass can generally be identified at the molecular level. Hence, our results for a 9-week-long period indicate that SC could be a major identified molecular fraction of OM for agricultural areas during summer, which is in agreement with several previous studies

conducted worldwide (Jia et al., 2010b; Verma et al., 2018; Yan et al., 2019). Further, it has been shown (Samaké et al., 2019a) that the identified polyols probably represent only a small fraction of the emission flux from this PBOA source and that a large fraction of the co-emitted organic material remains unknown. Hence, the PBOA source can potentially represent, for part of the year, a major source of atmospheric OM unaccounted for in CTMs.

## 4.2 Composition of airborne fungal and bacterial communities

In this study, 597 (39–132 MOTUs per sample) and 944 (31–129 MOTUs per sample) MOTUs were obtained for the functional and bacterial libraries, respectively, reflecting the high richness of airborne microbial communities associated with ambient PM₁₀ in this rural agricultural zone in France. Airborne fungi were dominated by Ascomycota (AMC) followed by Basidiomycota (BMC) phyla, consistent with the natural feature of many Ascomycota, whose single-celled or hyphal forms are small enough to be rapidly aerosolized, in contrast to many Basidiomycota that are typically too large
<figure><img src="image_9.png" /></figure>

**Figure 6.** Abundance of SC-species-associated microbial taxa. (a) Fungal genera and (b) bacterial genera in the airborne PM₁₀ samples and surrounding environmental samples. Black markers inside each box indicate the mean abundance value, while the top, middle, and bottom lines of the box represent the 75th, median, and 25th percentiles, respectively. The whiskers at the top and bottom of the box extend from the 95th to the 5th percentiles. Data were rarefied at the same minimum sequencing depth.

<figure><img src="image_10.png" /></figure>

**Figure 7.** Compositional comparison of sample types in a NMDS scaling ordination. NMDS plots are constructed from a Horn distance matrix of MOTUs abundances for fungi (a) and bacteria (b). Data sets are rarefied at the same sequencing depth. The stress values indicate an adequate two-dimensional picture of sample distribution. Ellipses represent 95% confidence intervals for the cluster centroids. Circular and triangular shapes highlight air PM₁₀ samples with background and peak SC concentrations, respectively.

to be easily aerosolized (Moore et al., 2011; Womack et al., 2015). Many members of AMC and BMC are known to actively eject ascospores and basidiospores, as well as aqueous jets and droplets containing a mixture of carbohydrates and inorganic solutes, into the atmosphere (Elbert et al., 2007; Womack et al., 2015). The prevalence of Ascomycota and Basidiomycota is consistent with results from previous studies also indicating that the Dikarya subkingdom (Ascomy-

cota and Basidiomycota) represents about 98% of known species in the biological kingdom of Eumycota (i.e., fungi) in the atmosphere (Elbert et al., 2007; James et al., 2006; Womack et al., 2015; Xu et al., 2017).

Airborne bacteria in this study belonged mainly to the Proteobacteria, Bacteroidetes, Actinobacteria, and Firmicutes phyla, consistent with previous studies (Liu et al., 2019; Maron et al., 2005; Wei et al., 2019b). Gram-negative
Proteobacteria constitute a major taxonomic group among prokaryotes (Itävaara et al., 2016; Yadav et al., 2018), including bacterial taxa which are very diverse, important in agriculture, and capable of fixing nitrogen in symbiosis with plants (Itävaara et al., 2016; Yadav et al., 2018). Proteobacteria can survive under conditions with very low nutrient content, which explains their atmospheric versatility (Itävaara et al., 2016; Yadav et al., 2018). These results are similar to those observed in previous studies conducted in different environments around the world, where Proteobacteria, Actinobacteria, and Firmicutes have also been reported as dominant bacterial phyla (Liu et al., 2019; Maron et al., 2005; Wei et al., 2019a). In particular, the most frequent Gram-negative (Proteobacteria and Bacteroidetes) and Gram-positive (Actinobacteria and Firmicutes) bacteria and filamentous fungi (Ascomycota and Basidiomycota) have been previously linked to raw straw handling activities. For instance, it has been suggested that straw combustion during agricultural activities could be a major source of airborne microorganisms in PM<sub>2.5</sub> in the northern plains of China (Wei et al., 2019a, b). However, in our study, SC species are not correlated (R = −0.09, *p* = 0.46; Fig. S7) with levoglucosan during the campaign period, confirming that biomass burning is not an important source of airborne microbial taxa associated with SCs in our PM<sub>10</sub> series. Bubble bursting associated with sea spray could also potentially be a source of bacteria, fungi, and water-soluble organic species, along with sea salts, to PM<sub>10</sub> (Prather et al., 2013; Zhu et al., 2015). However, SC species were not found to be significantly related to Cl<sup>-</sup> (R = −0.14, *p* = 0.28) or Na<sup>+</sup> (R = −0.18, *p* = 0.16), which are two inorganic tracers typical of marine sources, nor did they correlate with methanesulfonic acid (R = −0.05, *p* = 0.69), a well-known tracer of biogenic marine activity (Arndt et al., 2017; Gaston et al., 2010). It therefore seems unlikely that the sources of SCs from marine environments were significant at this site. This point is further discussed in Sect. 4.4.

## 4.3 Atmospheric concentration levels of SC species in PM₁₀ are associated with the abundance of a few specific airborne taxa of fungi and bacteria

SCs are widely produced in large quantities by many microorganisms to cope with environmental stress conditions (Medeiros et al., 2006). SC species are known to accumulate in high concentrations in microorganisms at low water availability to reduce intracellular water activity and prevent enzyme inhibition due to dehydration (Hrynkiewicz et al., 2010). In addition, the temporal dynamics of ambient polyol concentrations has been suggested as an indicator to follow the general seasonal trend in airborne fungal spore counts (Bauer et al., 2008; Gosselin et al., 2016). Although this strategy has allowed the introduction of conversion ratios between specific polyol species (i.e., arabitol and mannitol) and airborne fungal spores in general (Bauer et al., 2008),

the structure of the airborne microbial community associated with SC species has not yet been studied. Our results provide culture-independent evidence that the airborne microbiome structure and the combined bacterial and fungal communities largely determine the SC species concentration levels in PM₁₀.

Temporal fluctuations in the abundance of only a few specific fungal and bacterial genera reflect the temporal dynamics of ambient SC concentrations. For fungi, genera that show a significant positive correlation (p<0.05) with SC species include *Cladosporium*, *Alternaria*, *Sporobolomyces*, and *Dioszegia*. *Cladosporium* and *Alternaria* are fungal genera that contribute on average to 47.9% of total fungal sequence reads in our air samples series. These are asexual fungal genera that produce spores by dry-discharge mechanisms, wherein spores are detached from their parent colonies and easily dispersed by the ambient airflow or other external forces (e.g., raindrops, elevated temperature), as opposed to actively discharged spores with liquid jets or droplets in the air (Elbert et al., 2007; Wei et al., 2019b; Womack et al., 2015). Our results are consistent with the well-known seasonal behavior of airborne fungal spores with levels of *Cladosporium* and *Alternaria* which have been shown to reach their maximum from early to midsummer in a rural agricultural area of Portugal (Oliveira et al., 2009).

Similarly, bacterial genera positively correlated with SC species are *Massilia*, *Pseudomonas*, *Frigoribacterium*, and *Sphingomonas*. Although it is the prevalent bacterial genus at the study site, *Sphingomonas* is indeed not significantly positively correlated with SC species. The genus *Sphingomonas* is known to include numerous metabolically versatile species capable of using carbon compounds usually present in the atmosphere (Cáliz et al., 2018). The atmospheric abundance of species affiliated with *Massilia* has already been linked to the change in the stage of plant development (Ofek et al., 2012), which can be attributed to the capacity of *Massilia* to promote plant growth through the production of indoleacetic acid (Kuffner et al., 2010) and siderophores (Hrynkiewicz et al., 2010), which makes it antagonistic towards *Phytophthora infestans* (Weinert et al., 2010).

As far as we know, this is the first study evaluating microbial fingerprints with SC species in atmospheric PM; hence, it is not possible to compare our correlation results with those of previous works. However, it has already been suggested that types and quantities of SC species produced by fungi under culture conditions are specific to microbial species and external conditions such as carbon source, drought, heat, etc. (Hrynkiewicz et al., 2010). In future studies, we intend to apply a culture-dependent method to directly characterize the SC contents of some species amongst the dominant microbial taxa identified in this study after growth under several laboratory chambers, reproducing controlled environmental conditions in terms of temperature, water vapor, and carbon sources.
## 4.4 Local vegetation as a major source of airborne microbial taxa of PM₁₀ associated with SC species

There are still many challenging questions on the emission processes leading to fungi and bacteria being introduced into the atmosphere together with their chemical components. In particular, the potential influence of soil and vegetation and their respective roles in structuring airborne microbial communities are still debated (Lymeropoulou et al., 2016; Rathnayake et al., 2016; Womack et al., 2015), especially since this knowledge is particularly essential for the precise modeling of PBOA emissions processes to the atmosphere within chemical transport models.

The characterization of the temporal dynamics of SC species concentrations could provide important information on PBOA sources in terms of composition, environmental drivers, and impacts. The results obtained over a 9-week period of daily PM₁₀ SC measurements clearly show that the temporal dynamics of sorbitol (R = 0.59, p<0.001) and inositol (R = 0.64, p<0.001) are well-correlated linearly with that of calcium, a typical inorganic water-soluble ion from crustal material. This indicates a common atmospheric origin for these chemicals. Sorbitol and inositol are well-known reduced sugars that serve as a carbon source for microorganisms when other carbon sources are limited (Ng et al., 2018; Xue et al., 2010). In microorganisms, sorbitol and inositol are mainly produced by the reduction of intracellular glucose by aldose reductase in the cytoplasm (Ng et al., 2018; Welsh, 2000; Xue et al., 2010). Moreover, significant concentrations of both sorbitol and inositol have already been measured in surface-soil samples from five cultivated fields in the San Joaquin Valley, USA (Jia et al., 2010b; Medeiros et al., 2006). Therefore, sorbitol and inositol are most likely associated with microorganisms from soil resuspension.

With the exception of sorbitol and inositol, all other SC species measured in air samples at our sampling site are strongly correlated with each other, indicating a common origin. Daily calcium concentration peaks are not systematically associated with those of these other SC species. Interestingly, the highest atmospheric levels of these SC species occurred on 8 August 2017, coinciding well with daily harvesting activities around the site. This is also consistent with the multi-year monitoring of the dominant SCs in PM₁₀ at this site, where ambient SCs showed a clear seasonal trend with higher values recorded in early August and in good agreement with harvesting activities around the study area every year from 2012 to 2017 (Samaké et al., 2019a). This suggests that the processes responsible for the dynamics of atmospheric concentrations of SCs are replicated annually and are most likely effective over large areas of field crop (Golly et al., 2018; Samaké et al., 2019a). Interestingly, glucose – the most common monosaccharide present in vascular plants and microorganism – has already been proposed as a molecular indicator of biota emitted into the atmosphere by vascular plants and/or by the resuspension of soil from

agricultural land (Jia et al., 2010b; Pietrogrande et al., 2014). Therefore, all other SC species measured in our series can be considered to be most likely the result of the mechanical resuspension of crop residues (e.g., leaf debris) and microorganisms attached to them. Other confirmations of this interpretation stem from the excellent daily covariations observed in the PM₁₀ between SC species levels and ambient cellulose, which is widely considered a reliable indicator of plant debris sources in PM studies (Bozzetti et al., 2016; Hiranuma et al., 2019).

Microbial abundance and community structure in samples from the surrounding environment can provide further useful information on source apportionment and importance. Our data indicate that the airborne microbial genera most positively correlated to SC species are also distributed in the surrounding environmental samples of both surface soils and leaves, suggesting a dominant influence of the local environment for microbial taxa associated with SC species as opposed to long-range transport. This observation makes sense since actively discharged ascospores and basidiospores are generally relatively large airborne particles with a short atmospheric residence time (Elbert et al., 2007; Womack et al., 2015), limiting the possibilities of long-range dissemination. Accordingly, the majority of previous studies investigating the potential sources of air microbes identified local surface environments (e.g., leaves, soils) as having more important effects on the airborne microbiome structure in field crop areas (Bowers et al., 2011; Wei et al., 2019b; Womack et al., 2015). This is all the more the case in our study with homogeneous crop activities for tens to hundreds of kilometers around the site.

In the present study, microbial diversity and richness observed in the surface soils are generally higher than those on leaf surfaces. Microbial taxa which most positively correlated with PM₁₀ SC species are generally more abundant in leaf than in topsoil samples. These results were unexpected and show the possible importance of leaf surfaces in structuring the airborne taxa associated with SC species. Considering the general grouping of leaf samples and airborne PM₁₀ regardless of harvesting activities around the study site and in addition to the separate assemblies of rarefied MOTUs in airborne PM₁₀ and topsoil samples, it can be argued that the aerial parts of plants are the major source of microbial taxa associated with SC species. Such an observation is most likely related to increased vegetative surfaces (e.g., leaves) in summer that provides sufficient nutrient resources for microbial growth (Rathnayake et al., 2016). By reviewing previous studies, *Alternaria* and *Epicoccum*, which made up 30% of total fungal sequence reads in all air samples in this study, have been shown to be common saprobes or weak pathogens of leaf surfaces (Andersen et al., 2009). Similarly, *Cladosporium*, which accounted for 32.9% of total fungal genera in all air samples, has also been shown to be a common saprotrophic fungus, inhabiting decayed tree or plant debris (Wei et al., 2019b). The high relative abundance of *Sphingomonas*
and *Massilia*, accounting for 28.4 % of total bacterial genera in all air samples, is also noticeable. These two phyllosphere-inhabiting bacterial genera are well-known for their plant protective potential against phytopathogens (Aydogan et al., 2018; Rastogi et al., 2013).

Altogether, these observations support our interpretation that leaves are the major direct source of airborne fungi and bacteria during the summer months at this site of high agricultural activity. Endophytes and epiphytes can be dispersed in the air and transported vertically as particles by air currents, much faster and more widely than by other mechanisms, such as direct dissemination from surface soil, which is generally controlled by soil moisture (Jocteur Monrozier et al., 1993). The most wind-dispersible soil constituents are indeed the smallest soil particles (i.e., clay-size fraction), which contain the largest number of microorganisms (Jocteur Monrozier et al., 1993) and can only be released into the atmosphere under conditions of prolonged drought. This interpretation is also consistent with previous studies (Bowers et al., 2011; Liu et al., 2019; Lymperopoulou et al., 2016; Mhuireach et al., 2016), which also show the extent to which endophytes and epiphytes can serve as quantitatively important sources of airborne microbes during summertime when vegetation density is highest. For example, Lymperopoulou et al. (2016) observed that bacteria and fungi suspended in the air are generally 2 to more than 10 times more abundant in air that passed over 50 m of a vegetative surface than in air that is immediately upwind of the same vegetative surface. However, the relative abundance of taxa associated with SCs in surface soils in this study could also be indicative of a feedback loop, in which the soil may serve as a source of microbial endophytes and epiphytes for plants, while the local vegetation in turn may serve as a source and sink of microbes for local soils during leaf senescence.

## 5 Conclusions

Primary biogenic organic aerosols (PBOAs) affect human health, climate, agriculture, etc. However, the details of microbial communities associated with the temporal and spatial variations in atmospheric concentrations of SC, which are tracers of PBOAs, remain unknown. The present study aimed at identifying the airborne fungi and bacteria associated with SC species in PM₁₀ and their major sources in the surrounding environment (soils and vegetation). To that end, we combined high-throughput sequencing of bacteria and fungi with detailed physicochemical characterizations of PM₁₀ soil and leaf samples collected at a continental rural background site located in a large agricultural area in France.

The main results demonstrate that the identified SC species are a major contributor of OM in summer, accounting together for 0.8 % to 13.5 % of OM mass in air. The atmospheric concentration peaks of SC coincide with the daily harvest activities around the sampling site, pointing towards direct resuspension of biological materials, i.e., crop residues and associated microbiota as an important source of SC in our PM₁₀ series. Furthermore, we have also discovered that the temporal evolutions of SC in PM₁₀ are associated with the abundance of only a few specific airborne fungal and bacterial taxa. These microbial taxa are significantly enhanced in the surrounding environmental samples of leaves over surface soils. Finally, the excellent correlation of SC species and cellulose, a marker of plant materials, implies that local vegetation is likely the most important source of fungal and bacterial taxa associated with SC in PM₁₀ at rural locations directly influenced by agricultural activities in France.

Our findings are a first step in the understanding of the processes leading to the emission of these important chemical species and the large OM fraction of PM in the atmosphere, and in the parametrization of these processes for their introduction in CTMs. They could also be used for planning efforts to reduce both the PBOA source strengths and the spreading of airborne microbial and derivative allergens such as endotoxins and mycotoxins. However, it remains to be investigated how well different climate patterns and sampling site specificities, in terms of land use and vegetation cover, could affect our main conclusions.

*Data availability.* The sequencing data files are available from the DRYAD repository (https://doi.org/10.5061/dryad.2fqz612m4, Samaké et al., 2020). All relevant chemical and environmental data sets are archived at the IGE (Institut des Géosciences de l'Environnement) and are available upon request from the co-author (Jean-Luc Jaffrezo).

*Supplement.* The supplement related to this article is available online at: https://doi.org/10.5194/acp-20-5609-2020-supplement.

*Author contributions.* JLJ, JMFM, and GU supervised the thesis of AS, and JLJ, JMFM, GU, and AS designed the research project. PT gave advice for soil and leaf sampling. SC supervised the sample collections and provided the agricultural activity records. VJ developed the analytical techniques for SC species and cellulose measurements. AS and AB performed the experiments. AB performed the bioinformatic analyses. AS performed statistical analyses and wrote the original draft. SW produced the circular phylogenetic trees. All authors reviewed and edited the final paper.

*Competing interests.* The authors declare that they have no conflict of interest.
*Acknowledgements.* We acknowledge the work of many engineers in the lab at the Institut des Géosciences de l'Environnement for the analyses (Anthony Vella, Vincent Lucaire). The authors would like to kindly thank the dedicated efforts of many other people at the sampling site and in the laboratories for collecting and analyzing the samples.

The PhD of Abdoulaye Samaké is funded by the government of Mali. We gratefully acknowledge the LEFE-CHAT and EC2CO programs of the CNRS for financial supports of the CAREM-BIOS multidisciplinary project, with ADEME funding. Chemical and microbiological analytical aspects were supported at IGE by the Air-O-Sol and MOME platforms, respectively, within Labex OSUG@2020 (ANR10 LABX56).

*Review statement.* This paper was edited by Alex Huffman and reviewed by two anonymous referees.

## References

Amato, P., Brisebois, E., Draghi, M., Duchaine, C., Fröhlich-Nowoisky, J., Huffman, J. A., Mainelis, G., Robine, E., and Thibaudon, M.: Main biological aerosols, specificities, abundance, and diversity, in Microbiology of Aerosols, pp. 1–21, John Wiley & Sons, Ltd., https://doi.org/10.1002/9781119132318, 2017.

Andersen, G. L., Frisch, A. S., Kellogg, C. A., Levetin, E., Lighthart, B., and Paterno, D.: Aeromicrobiology/air quality, in Encyclopedia of Microbiology (Third Edition), pp. 11–26, Academic Press, Oxford., https://doi.org/10.1016/B978-012373944-5.00166-8, 2009.

Arndt, J., Sciare, J., Mallet, M., Roberts, G. C., Marchand, N., Sartelet, K., Sellegri, K., Dulac, F., Healy, R. M., and Wenger, J. C.: Sources and mixing state of summertime background aerosol in the north-western Mediterranean basin, Atmos. Chem. Phys., 17, 6975–7001, https://doi.org/10.5194/acp-17-6975-2017, 2017.

Aydogan, E. L., Moser, G., Müller, C., Kämpfer, P., and Glaeser, S. P.: Long-term warming shifts the composition of bacterial communities in the phyllosphere of galium album in a permanent grassland field-experiment, Front. Microbiol., 9, 144, https://doi.org/10.3389/fmicb.2018.00144, 2018.

Barbaro, E., Kirchgeorg, T., Zangrando, R., Vecchiatto, M., Piazza, R., Barbante, C., and Gambaro, A.: Sugars in Antarctic aerosol, Atmos. Environ., 118, 135–144, https://doi.org/10.1016/j.atmosenv.2015.07.047, 2015.

Bauer, H., Claeys, M., Vermeylen, R., Schueller, E., Weinke, G., Berger, A., and Puxbaum, H.: Arabitol and mannitol as tracers for the quantification of airborne fungal spores, Atmos. Environ., 42, 588–593, https://doi.org/10.1016/j.atmosenv.2007.10.013, 2008.

Boucher, O., Randall, D., Artaxo, P., Bretherton, C., Feingold, G., Forster, P., Kerminen, V.-M., Kondo, Y., Liao, H., and Lohmann, U.: Clouds and aerosols, in: Climate change 2013: the physical science basis, Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, 571–657, Cambridge University Press, https://doi.org/10.1017/CBO9781107415324.016, 2013.

Bougouffa, S., Radovanovic, A., Essack, M., and Bajic, V. B.: DEOP: a database on osmoprotectants and associated pathways, Database, 2014, https://doi.org/10.1093/database/bau100, 2014.

Bowers, R. M., Sullivan, A. P., Costello, E. K., Collett, J. L., Knight, R., and Fiereri, N.: Sources of bacteria in outdoor air across cities in the Midwestern United States, Appl. Environ. Microbiol., 77, 6350–6356, https://doi.org/10.1128/AEM.05498-11, 2011.

Boyer, F., Mercier, C., Bonin, A., Le Bras, Y., Taberlet, P., and Coissac, E.: OBITOLS: a UNIX-inspired software package for DNA metabarcoding, Mol. Ecol. Resour., 16, 176–182, https://doi.org/10.1111/1755-0998.12428, 2016.

Bozzetti, C., Daellenbach, K. R., Hueglin, C., Fermo, P., Sciare, J., Kasper-Giebl, A., Mazar, Y., Abbaszade, G., El Kazzi, M., Gonzalez, R., Shuster-Meiseles, T., Flasch, M., Wolf, R., Képelová, A., Canonaco, F., Schnelle-Kreis, J., Slowik, J. G., Zimmermann, R., Rudich, Y., Baltensperger, U., El Haddad, I., and Prévôt, A. S. H.: Size-resolved identification, characterization, and quantification of primary biological organic aerosol at a European rural site, Environ. Sci. Technol., 50, 3425–3434, https://doi.org/10.1021/acs.est.5b05960, 2016.

Cáliz, J., Triadó-Margarit, X., Camarero, L., and Casamayor, E. O.: A long-term survey unveils strong seasonal patterns in the airborne microbiome coupled to general and regional atmospheric circulations, P. Natl. Acad. Sci., 115, 12229, https://doi.org/10.1073/pnas.1812826115, 2018.

Cao, C., Jiang, W., Wang, B., Fang, J., Lang, J., Tian, G., Jiang, J., and Zhu, T. F.: Inhalable microorganisms in Beijing’s PM₂.₅ and PM₁₀ pollutants during a severe smog event, Environ. Sci. Technol., 48, 1499–1507, https://doi.org/10.1021/es4048472, 2014.

Cavalli, F., Viana, M., Yttri, K. E., Genberg, J., and Putaud, J.-P.: Toward a standardised thermal-optical protocol for measuring atmospheric organic and elemental carbon: the EUSAAR protocol, Atmos. Meas. Tech., 3, 79–89, https://doi.org/10.5194/amt-3-79-2010, 2010.

China, S., Burrows, S. M., Wang, B., Harder, T. H., Weis, J., Tanarhte, M., Rizzo, L. V., Brito, J., Cirino, G. G., Ma, P.-L., Cliff, J., Artaxo, P., Gilles, M. K., and Laskin, A.: Fungal spores as a source of sodium salt particles in the Amazon basin, Nat. Commun., 9, 4793, https://doi.org/10.1038/s41467-018-07066-4, 2018.

Ciarelli, G., Aksoyoglu, S., Crippa, M., Jimenez, J.-L., Nemitz, E., Sellegri, K., Äijälä, M., Carbone, S., Mohr, C., O’Dowd, C., Poulain, L., Baltensperger, U., and Prévôt, A. S. H.: Evaluation of European air quality modelled by CAMx including the volatility basis set scheme, Atmos. Chem. Phys., 16, 10313–10332, https://doi.org/10.5194/acp-16-10313-2016, 2016.

Coz, E., Artíñano, B., Clark, L. M., Hernandez, M., Robinson, A. L., Casuccio, G. S., Lersch, T. L., and Pandis, S. N.: Characterization of fine primary biogenic organic aerosol in an urban area in the northeastern United States, Atmos. Environ., 44, 3952–3962, https://doi.org/10.1016/j.atmosenv.2010.07.007, 2010.

Dommergue, A., Amato, P., Tignat-Perrier, R., Magand, O., Thollot, A., Joly, M., Bouvier, L., Sellegri, K., Vogel, T., Sonke, J. E., Jaffrezo, J.-L., Andrade, M., Moreno, I., Labuschagne, C., Martin, L., Zhang, Q., and Larose, C.: Methods to investigate the global atmospheric microbiome, Front. Microbiol., 10, 243, https://doi.org/10.3389/fmicb.2019.00243, 2019.

Elbert, W., Taylor, P. E., Andreae, M. O., and Pöschl, U.: Contribution of fungi to primary biogenic aerosols in the atmosphere: wet
and dry discharged spores, carbohydrates, and inorganic ions, Atmos. Chem. Phys., 7, 4569–4588, https://doi.org/10.5194/acp-7-4569-2007, 2007.

Ficetola, G., Coissac, E., Zundel, S., Riaz, T., Shehzad, W., Bessière, J., Taberlet, P., and Pompanon, F.: An in silico approach for the evaluation of DNA barcodes, BMC Genomics, 11, 434, https://doi.org/10.1186/1471-2164-11-434, 2010.

Fröhlich-Nowoisky, J., Kampf, C. J., Weber, B., Huffman, J. A., Pöhlker, C., Andreae, M. O., Lang-Yona, N., Burrows, S. M., Gunthe, S. S., Elbert, W., Su, H., Hoor, P., Thines, E., Hoffmann, T., Després, V. R., and Pöschl, U.: Bioaerosols in the earth system: climate, health, and ecosystem interactions, Atmos. Res., 182, 346–376, https://doi.org/10.1016/j.atmosres.2016.07.018, 2016.

Fu, P., Kawamura, K., Kobayashi, M., and Simoneit, B. R.: Seasonal variations of sugars in atmospheric particulate matter from Gosan, Jeju Island: Significant contributions of airborne pollen and Asian dust in spring, Atmos. Environ., 55, 234–239, https://doi.org/10.1029/2003JD003697, 2012.

Fuzzi, S., Andreae, M. O., Huebert, B. J., Kulmala, M., Bond, T. C., Boy, M., Doherty, S. J., Guenther, A., Kanakidou, M., Kawamura, K., Kerminen, V.-M., Lohmann, U., Russell, L. M., and Pöschl, U.: Critical assessment of the current state of scientific knowledge, terminology, and research needs concerning the role of organic aerosols in the atmosphere, climate, and global change, Atmos. Chem. Phys., 6, 2017–2038, https://doi.org/10.5194/acp-6-2017-2006, 2006.

Fuzzi, S., Baltensperger, U., Carslaw, K., Decesari, S., Denier van der Gon, H., Facchini, M. C., Fowler, D., Koren, I., Langford, B., Lohmann, U., Nemitz, E., Pandis, S., Riipinen, I., Rudich, Y., Schaap, M., Slowik, J. G., Spracklen, D. V., Vignati, E., Wild, M., Williams, M., and Gilardoni, S.: Particulate matter, air quality and climate: lessons learned and future needs, Atmos. Chem. Phys., 15, 8217–8299, https://doi.org/10.5194/acp-15-8217-2015, 2015.

Gaston, C. J., Pratt, K. A., Qin, X., and Prather, K. A.: Real-time detection and mixing state of methanesulfonate in single particles at an inland urban location during a phytoplankton bloom, Environ. Sci. Technol., 44, 1566–1572, https://doi.org/10.1021/es902069d, 2010.

Golly, B., Waked, A., Weber, S., Samaké, A., Jacob, V., Conil, S., Rangognio, J., Chrétien, E., Vagnot, M.-P., Robic, P.-Y., Besombes, J.-L., and Jaffrezo, J.-L.: Organic markers and OC source apportionment for seasonal variations of PM₂.₅ at 5 rural sites in France, Atmos. Environ., 198, 142–157, https://doi.org/10.1016/j.atmosenv.2018.10.027, 2018.

Gosselin, M. I., Rathnayake, C. M., Crawford, I., Pöhlker, C., Fröhlich-Nowoisky, J., Schmer, B., Després, V. R., Engling, G., Gallagher, M., Stone, E., Pöschl, U., and Huffman, J. A.: Fluorescent bioaerosol particle, molecular tracer, and functional spore concentrations during dry and rainy periods in a semi-arid forest, Atmos. Chem. Phys., 16, 15165–15184, https://doi.org/10.5194/acp-16-15165-2016, 2016.

Heald, C. L., Coe, H., Jimenez, J. L., Weber, R. J., Bahreini, R., Middlebrook, A. M., Russell, L. M., Jolleys, M., Fu, T.-M., Alkan, J. D., Bower, K. N., Capes, G., Crosier, J., Morgan, W. T., Robinson, N. H., Williams, P. I., Cubison, M. J., DeCarlo, P. F., and Dunlea, E. J.: Exploring the vertical profile of atmospheric organic aerosol: comparing 17 aircraft field campaigns

with a global model, Atmos. Chem. Phys., 11, 12673–12696, https://doi.org/10.5194/acp-11-12673-2011, 2011.

Hill, T. C. J., DeMott, P. J., Conen, F., and Möhler, O.: Impacts of bioaerosols on atmospheric ice nucleation Processes, in Microbiology of Aerosols, pp. 195–219, John Wiley & Sons, Ltd., https://doi.org/10.1002/9781119132318, 2017.

Hiranuma, N., Adachi, K., Bell, D. M., Belosi, F., Beydoun, H., Bhaduri, B., Bingemer, H., Budke, C., Clemen, H.-C., Conen, F., Cory, K. M., Curtius, J., DeMott, P. J., Eppers, O., Grawe, S., Hartmann, S., Hoffmann, N., Höhler, K., Jantsch, E., Kiselev, A., Koop, T., Kulkarni, G., Mayer, A., Murakami, M., Murray, B. J., Nicosia, A., Petters, M. D., Piazza, M., Polen, M., Reicher, N., Rudich, Y., Saito, A., Santachiara, G., Schiebel, T., Schill, G. P., Schneider, J., Segev, L., Stopelli, E., Sullivan, R. C., Suski, K., Szakáll, M., Tajiri, T., Taylor, H., Tobo, Y., Ullrich, R., Weber, D., Wex, H., Whale, T. F., Whiteside, C. L., Yamashita, K., Zelenyuk, A., and Möhler, O.: A comprehensive characterization of ice nucleation by three different types of cellulose particles immersed in water, Atmos. Chem. Phys., 19, 4823–4849, https://doi.org/10.5194/acp-19-4823-2019, 2019.

Hrynkiewicz, K., Baum, C., and Leinweber, P.: Density, metabolic activity, and identity of cultivable rhizosphere bacteria on Salix viminalis in disturbed arable and landfill soils, J. Plant Nutr. Soil Sci., 173, 747–756, https://doi.org/10.1002/jpln.200900286, 2010.

Hsieh, T. C., Ma, K. H., and Chao, A.: iNEXT: an R package for rarefaction and extrapolation of species diversity (Hill numbers), Methods Ecol. Evol., 7, 1451–1456, https://doi.org/10.1111/2041-210X.12613, 2016.

Huerta-Cepas, J., Serra, F., and Bork, P.: ETE 3: Reconstruction, analysis, and visualization of Phylogenomic Data, Mol. Biol. Evol., 33, 1635–1638, https://doi.org/10.1093/molbev/msw046, 2016.

Huffman, J. A. and Santarpia, J.: Online techniques for quantification and characterization of biological aerosols, in Microbiology of Aerosols, pp. 83–114, John Wiley & Sons, Ltd., https://doi.org/10.1002/9781119132318, 2017.

Huffman, J. A., Perring, A. E., Savage, N. J., Clot, B., Crouzy, B., Tummon, F., Shoshanim, O., Damit, B., Schneider, J., Sivaprakasam, V., Zawadowicz, M. A., Crawford, I., Gallagher, M., Topping, D., Doughty, D. C., Hill, S. C., and Pan, Y.: Real-time sensing of bioaerosols: review and current perspectives, Aerosol Sci. Technol., 54, 465–495, https://doi.org/10.1080/02786826.2019.1664724, 2019.

Itävaara, M., Salavirta, H., Marjamaa, K., and Ruskeeniemi, T.: Geomicrobiology and metagenomics of Terrestrial Deep Subsurface Microbiomes, Adv. Appl. Microbiol., 94, 1–77, https://doi.org/10.1016/bs.aambs.2015.12.001, 2016.

James, T. Y., Kauff, F., Schoch, C. L., Matheny, P. B., Hofstetter, V., Cox, C. J., Celio, G., Gueidan, C., Fraker, E., Miadlikowska, J., Lumbsch, H. T., Rauhut, A., Reeb, V., Arnold, A. E., Amtoft, A., Stajich, J. E., Hosaka, K., Sung, G.-H., Johnson, D., O'Rourke, B., Crockett, M., Binder, M., Curtis, J. M., Slot, J. C., Wang, Z., Wilson, A. W., Schüßler, A., Longcore, J. E., O'Donnell, K., Mozley-Standridge, S., Porter, D., Letcher, P. M., Powell, M. J., Taylor, J. W., White, M. M., Griffith, G. W., Davies, D. R., Humber, R. A., Morton, J. B., Sugiyama, J., Rossman, A. Y., Rogers, J. D., Pfister, D. H., Hewitt, D., Hansen, K., Hambleton, S., Shoemaker, R. A., Kohlmeyer, J., Volkmann-Kohlmeyer, B.,
Spotts, R. A., Serdani, M., Crous, P. W., Hughes, K. W., Matsuura, K., Langer, E., Langer, G., Untereiner, W. A., Lücking, R., Büdel, B., Geiser, D. M., Aptroot, A., Diederich, P., Schmitt, I., Schultz, M., Yahr, R., Hibbett, D. S., Lutzoni, F., McLaughlin, D. J., Spatafora, J. W., and Vilgalys, R.: Reconstructing the early evolution of Fungi using a six-gene phylogeny, Nature, 443, 818–822, https://doi.org/10.1038/nature05110, 2006.

Jia, Y., Bhat, S., and Fraser, M. P.: Characterization of saccharides and other organic compounds in fine particles and the use of saccharides to track primary biologically derived carbon sources, Atmos. Environ., 44, 724–732, https://doi.org/10.1016/j.atmosenv.2009.10.034, 2010a.

Jia, Y., Clements, A. L., and Fraser, M. P.: Saccharide composition in atmospheric particulate matter in the southwest US and estimates of source contributions, J. Aerosol Sci., 41, 62–73, https://doi.org/10.1016/j.jaerosci.2009.08.005, 2010b.

Jiang, W., Liang, P., Wang, B., Fang, J., Lang, J., Tian, G., Jiang, J., and Zhu, T. F.: Optimized DNA extraction and metagenomic sequencing of airborne microbial communities, Nat. Protoc., 10, 768–779, https://doi.org/10.1038/nprot.2015.046, 2015.

Jocteur Monrozier, L., Guez, P., Chalamet, A., Bardin, R., Martins, J., and Gaudet, J. P.: Distribution of microorganisms and fate of xenobiotic molecules in unsaturated soil environments, Sci. Total Environ., 136, 121–133, https://doi.org/10.1016/0048-9697(93)090302-M, 1993.

Kang, M., Ren, L., Ren, H., Zhao, Y., Kawamura, K., Zhang, H., Wei, L., Sun, Y., Wang, Z., and Fu, P.: Primary biogenic and anthropogenic sources of organic aerosols in Beijing, China: insights from saccharides and n-alkanes, Environ. Pollut., 243, 1579–1587, https://doi.org/10.1016/j.envpol.2018.09.118, 2018.

Kelly, F. J. and Fussell, J. C.: Air pollution and public health: emerging hazards and improved understanding of risk, Environ. Geochem. Health, 37, 631–649, https://doi.org/10.1007/s10653-015-9720-1, 2015.

Kuffner, M., De Maria, S., Puschenreiter, M., Fallmann, K., Wieshammer, G., Gorfer, M., Strauss, J., Rivelli, A. R., and Sesitsch, A.: Culturable bacteria from Zn- and Cd-accumulating Salix caprea with differential effects on plant growth and heavy metal availability, J. Appl. Microbiol., 108, 1471–1484, https://doi.org/10.1111/j.1365-2672.2010.04670.x, 2010.

Liu, H., Hu, Z., Zhou, M., Hu, J., Yao, X., Zhang, H., Li, Z., Lou, L., Xi, C., Qian, H., Li, C., Xu, X., Zheng, P., and Hu, B.: The distribution variance of airborne microorganisms in urban and rural environments, Environ. Pollut., 247, 898–906, https://doi.org/10.1016/j.envpol.2019.01.090, 2019.

Luhung, I., Wu, Y., Ng, C. K., Miller, D., Cao, B., and Chang, V. W.-C.: Protocol improvements for low concentration DNA-based bioaerosol sampling and analysis, PLOS ONE, 10, e0141158, https://doi.org/10.1371/journal.pone.0141158, 2015.

Lymeropoulou, D. S., Adams, R. I., and Lindow, S. E.: Contribution of vegetation to the microbial composition of nearby outdoor air, Appl. Environ. Microbiol., 82, 3822–3833, https://doi.org/10.1128/AEM.00610-16, 2016.

Maron, P.-A., Lejon, D. P. H., Carvalho, E., Bizet, K., Lemanceau, P., Ranjard, L., and Mougel, C.: Assessing genetic structure and diversity of airborne bacterial communities by DNA fingerprinting and 16S rDNA clone library, Atmos. Environ., 39, 3687–3695, https://doi.org/10.1016/j.atmosenv.2005.03.002, 2005.

McMurdie, P. J. and Holmes, S.: phyloseq: An R package for reproducible interactive analysis and graphics of microbiome sensus Data, PLoS ONE, 8, e61217, https://doi.org/10.1371/journal.pone.0061217, 2013.

Medeiros, P. M., Conte, M. H., Weber, J. C., and Simoneit, B. R. T.: Sugars as source indicators of biogenic organic carbon in aerosols collected above the howland experimental forest, Maine, Atmos. Environ., 40, 1694–1705, https://doi.org/10.1016/j.atmosenv.2005.11.001, 2006.

Mercier, C., Boyer, F., Kopylova, E., Taberlet, P., Bonin, A., and Coissac, E.: SUMATRA and SUMACLUST: fast and exact comparison and clustering of sequences. Programs and Abstracts of the SeqBio, Workshop, pp. 27–29, 2013.

Mhuireach, G., Johnson, B. R., Altrichter, A. E., Ladau, J., Meadow, J. F., Pollard, K. S., and Green, J. L.: Urban greenness influences airborne bacterial community composition, Sci. Total Environ., 571, 680–687, https://doi.org/10.1016/j.scitotenv.2016.07.037, 2016.

Moore, D., Robson, G. D., and Trinci, A. P. J.: 21st century guidebook to fungi, Cambridge University Press, Cambridge, https://doi.org/10.1017/CBO9780511977022, 2011.

Ng, T. W., Ip, M., Chao, C. Y. H., Tang, J. W., Lai, K. P., Fu, S. C., Leung, W. T., and Lai, K. M.: Differential gene expression in Escherichia coli during aerosolization from liquid suspension, Appl. Microbiol. Biotechnol., 102, 6257–6267, https://doi.org/10.1007/s00253-018-9083-5, 2018.

Ofek, M., Hadar, Y., and Minz, D.: Ecology of root colonizing massilia (oxalobacteraceae), PLoS ONE, 7, e40117, https://doi.org/10.1371/journal.pone.0040117, 2012.

Oksanen, J., Blanchet, F. G., Friendly, M., Kindt, R., Legendre, P., McGlinn, D., R. Minchin, P. R., O'Hara, R. B., Simpson, G. L., Solymos, Peter, Stevens, M. H. H., Szoecs, E., and Wagner, H.: Vegan: community ecology package, available at: https://cran.r-project.org (last access: 7 May 2020) and https://github.com/vegandevs/vegan (last access: 7 May 2020), 2019.

Oliveira, M., Ribeiro, H., Delgado, J. L., and Abreu, I.: The effects of meteorological factors on airborne fungal spore concentration in two areas differing in urbanisation level, Int. J. Biometeorol., 53, 61–73, https://doi.org/10.1007/s00484-008-0191-2, 2009.

Prather, K. A., Bertram, T. H., Grassian, V. H., Deane, G. B., Stokes, M. D., DeMott, P. J., Aluwihare, L. I., Palenik, B. P., Azam, F., Seinfeld, J. H., Moffet, R. C., Molina, M. J., Cappa, C. D., Geiger, F. M., Roberts, G. C., Russell, L. M., Ault, A. P., Baltrusaitis, J., Collins, D. B., Corrigan, C. E., Cuadra-Rodriguez, L. A., Ebben, C. J., Forestieri, S. D., Guasco, T. L., Hersey, S. P., Kim, M. J., Lambert, W. F., Modini, R. L., Mui, W., Pedler, B. E., Ruppel, M. J., Ryder, O. S., Schoepp, N. G., Sullivan, R. C., and Zhao, D.: Bringing the ocean into the laboratory to probe the chemical complexity of sea spray aerosol, P. Natl. Acad. Sci. USA, 110, 7550–7555, https://doi.org/10.1073/pnas.1300262110, 2013.

Pietrogrande, M. C., Bacco, D., Visentin, M., Ferrari, S., and Casali, P.: Polar organic marker compounds in atmospheric aerosol in the Po valley during the Supersito campaigns – part 2: seasonal variations of sugars, Atmos. Environ., 97, 215–225, https://doi.org/10.1016/j.atmosenv.2014.07.056, 2014.

Pope, C. A. and Dockery, D. W.: Health effects of fine particulate air pollution: lines that connect, J. Air Waste Manag. Assoc., 56, 709–742, 2006.
Rastogi, G., Coaker, G. L., and Leveau, J. H. J.: New insights into the structure and function of phyllosphere microbiota through high-throughput molecular approaches, FEMS Microbiol. Lett., 348, 1–10, https://doi.org/10.1111/1574-6968.12225, 2013.

Rathnayake, C. M., Metwali, N., Baker, Z., Jayarathne, T., Kostle, P. A., Thorne, P. S., O'Shaughnessy, P. T., and Stone, E. A.: Urban enhancement of PM₁₀ bioaerosol tracers relative to background locations in the midwestern United States, J. Geophys. Res.-Atmos., 121, 5071–5089, https://doi.org/10.1002/2015JD024538, 2016.

Samaké, A., Uzu, G., Martins, J. M. F., Calas, A., Vince, E., Parat, S., and Jaffrezo, J. L.: The unexpected role of bioaerosols in the Oxidative Potential of PM, Sci. Rep., 7, 10978, https://doi.org/10.1038/s41598-017-11178-0, 2017.

Samaké, A., Jaffrezo, J.-L., Favez, O., Weber, S., Jacob, V., Canete, T., Albinet, A., Charron, A., Riffault, V., Perdrix, E., Waked, A., Golly, B., Salameh, D., Chevrier, F., Oliveira, D. M., Besombes, J.-L., Martins, J. M. F., Bonnaire, N., Conil, S., Guillaud, G., Mesbah, B., Rocq, B., Robic, P.-Y., Hulin, A., Le Meur, S., Descheemaeker, M., Chretien, E., Marchand, N., and Uzu, G.: Arabinol, mannitol, and glucose as tracers of primary biogenic organic aerosol: the influence of environmental factors on ambient air concentrations and spatial distribution over France, Atmos. Chem. Phys., 19, 11013–11030, https://doi.org/10.5194/acp-19-11013-2019, 2019a.

Samaké, A., Jaffrezo, J.-L., Favez, O., Weber, S., Jacob, V., Albinet, A., Riffault, V., Perdrix, E., Waked, A., Golly, B., Salameh, D., Chevrier, F., Oliveira, D. M., Bonnaire, N., Besombes, J.-L., Martins, J. M. F., Conil, S., Guillaud, G., Mesbah, B., Rocq, B., Robic, P.-Y., Hulin, A., Le Meur, S., Descheemaeker, M., Chretien, E., Marchand, N., and Uzu, G.: Polyols and glucose particulate species as tracers of primary biogenic organic aerosols at 28 French sites, Atmos. Chem. Phys., 19, 3357–3374, https://doi.org/10.5194/acp-19-3357-2019, 2019b.

Samaké, A., Bonin, A., Jaffrezo, J.-L., Taberlet, P., Weber, S., Uzu, G., Jacob, V., Conil, S., and Martins, J. M. F.: Sequencing data from: High levels of primary biogenic organic aerosols are driven by only a few plant-associated microbial taxa, v2, Dryad, Dataset, https://doi.org/10.5061/dryad.2fqz612m4, 2020.

Schnell, I. B., Bohmann, K., and Gilbert, M. T. P.: Tag jumps illuminated – reducing sequence-to-sample misidentifications in metabarcoding studies, Mol. Ecol. Resour., 15, 1289–1303, https://doi.org/10.1111/1755-0998.12402, 2015.

Taberlet, P., Bonin, A., Zinger, L., and Coissac, E.: Environmental DNA: for biodiversity research and monitoring, Oxford University Press, Oxford, New York, https://doi.org/10.1093/oso/9780198767220.001.0001, 2018.

Verma, S. K., Kawamura, K., Chen, J., and Fu, P.: Thirteen years of observations on primary sugars and sugar alcohols over remote Chichijima Island in the western North Pacific, Atmos. Chem. Phys., 18, 81–101, https://doi.org/10.5194/acp-18-81-2018, 2018.

Waked, A., Favez, O., Alleman, L. Y., Piot, C., Petit, J.-E., Delainay, T., Verlinden, E., Golly, B., Besombes, J.-L., Jaffrezo, J.-L., and Leoz-Garziandia, E.: Source apportionment of PM₁₀ in a north-western Europe regional urban background site (Lens, France) using positive matrix factorization and including primary biogenic emissions, Atmos. Chem. Phys., 14, 3325–3346, https://doi.org/10.5194/acp-14-3325-2014, 2014.

Weber, S., Uzu, G., Calas, A., Chevrier, F., Besombes, J.-L., Charon, A., Salameh, D., Ježek, I., Močnik, G., and Jaffrezo, J.-L.: An apportionment method for the oxidative potential of atmospheric particulate matter sources: application to a one-year study in Chamonix, France, Atmos. Chem. Phys., 18, 9617–9629, https://doi.org/10.5194/acp-18-9617-2018, 2018.

Wei, M., Xu, C., Xu, X., Zhu, C., Li, J., and Lv, G.: Characteristics of atmospheric bacterial and fungal communities in PM₂.₅ following biomass burning disturbance in a rural area of North China Plain, Sci. Total Environ., 651, 2727–2739, https://doi.org/10.1016/j.scitotenv.2018.09.399, 2019a.

Wei, M., Xu, C., Xu, X., Zhu, C., Li, J., and Lv, G.: Size distribution of bioaerosols from biomass burning emissions: characteristics of bacterial and fungal communities in submicron (PM₁₀) and fine (PM₂.₅) particles, Ecotoxicol. Environ. Saf., 171, 37–46, https://doi.org/10.1016/j.ecoenv.2018.12.026, 2019b.

Weinert, N., Meincke, R., Gottwald, C., Radl, V., Dong, X., Schloter, M., Berg, G., and Smalla, K.: Effects of genetically modified potatoes with increased zeaxanthin content on the abundance and diversity of rhizobacteria with in vitro antagonistic activity do not exceed natural variability among cultivars, Plant Soil, 326, 437–452, https://doi.org/10.1007/s11107-009-0024-z, 2010.

Welsh, D. T.: Ecological significance of compatible solute accumulation by micro-organisms: from single cells to global climate, FEMS Microbiol. Rev., 24, 263–290, https://doi.org/10.1111/j.1574-6976.2000.tb00542.x, 2000.

Womack, A. M., Artaxo, P. E., Ishida, F. Y., Mueller, R. C., Saleska, S. R., Wiedemann, K. T., Bohannan, B. J. M., and Green, J. L.: Characterization of active and total fungal communities in the atmosphere over the Amazon rainforest, Biogeosciences, 12, 6337–6349, https://doi.org/10.5194 bg-12-6337-2015, 2015.

Xu, C., Wei, M., Chen, J., Zhu, C., Li, J., Lv, G., Xu, X., Zheng, L., Sui, G., Li, W., Chen, B., Wang, W., Zhang, Q., Ding, A., and Mellouki, A.: Fungi diversity in PM₂.₅ and PM₁ at the summit of Mt. Tai: abundance, size distribution, and seasonal variation, Atmos. Chem. Phys., 17, 11247–11260, https://doi.org/10.5194/acp-17-11247-2017, 2017.

Xue, C., Liu, T., Chen, L., Li, W., Liu, I., Kronstad, J. W., Seyfang, A., and Heitman, J.: Role of an expanded inositol transporter repertoire in cryptococcus neoformans sexual reproduction and virulence, 1, e00084-10, https://doi.org/10.1128/mBio.00008-10, 2010.

Yadav, A. N., Verma, P., Sachan, S. G., Kaushik, R., and Saxena, A. K.: Psychrotrophic microbiomes: molecular diversity and beneficial role in plant growth promotion and soil health, in Microorganisms for Green Revolution, vol. 7, pp. 197–240, Springer Singapore, Singapore, https://doi.org/10.1007/978-981-10-7146-1_11, 2018.

Yan, C., Sullivan, A. P., Cheng, Y., Zheng, M., Zhang, Y., Zhu, T., and Collett, J. L.: Characterization of saccharides and associated usage in determining biogenic and biomass burning aerosols in atmospheric fine particulate matter in the North China Plain, Sci. Total Environ., 650, 2939–2950, https://doi.org/10.1016/j.scitotenv.2018.09.325, 2019.

Yang, Y., Chan, C., Tao, J., Lin, M., Engling, G., Zhang, Z., Zhang, T., and Su, L.: Observation of elevated fungal tracers due to biomass burning in the Sichuan Basin at Chengdu City, China, Sci. Total Environ., 431, 68–77, 2012.
Yu, X., Wang, Z., Zhang, M., Kuhn, U., Xie, Z., Cheng, Y., Pöschl, U., and Su, H.: Ambient measurement of fluorescent aerosol particles with a WIBS in the Yangtze River Delta of China: potential impacts of combustion-related aerosol particles, Atmos. Chem. Phys., 16, 11337–11348, https://doi.org/10.5194/acp-16-11337-2016, 2016.

Zhu, C., Kawamura, K., and Kunwar, B.: Organic tracers of primary biological aerosol particles at subtropical Okinawa Island in the western North Pacific Rim: organic biomarkers in the north Pacific, J. Geophys. Res.-Atmos., 120, 5504–5523, 2015.