Әуедегі ұса микроорганизмдер және олардың таралуы

Tiny lifeforms floating and drifting in the air, carried by the wind

Aeroplankton (or aerial plankton) are tiny lifeforms that float and drift in the air, carried by wind. Most of the living things that make up aeroplankton are very small to microscopic in size, and many can be difficult to identify because of their tiny size. Scientists collect them for study in traps and sweep nets from aircraft, kites or balloons. The study of the dispersion of these particles is called aerobiology. Aeroplankton is made up mostly of microorganisms, including viruses, about 1,000 different species of bacteria, around 40,000 varieties of fungi, and hundreds of species of protists, algae, mosses, and liverworts that live some part of their life cycle as aeroplankton, often as spores, pollen, and wind scattered seeds. Additionally, microorganisms are swept into the air from terrestrial dust storms, and an even larger amount of airborne marine microorganisms are propelled high into the atmosphere in sea spray. Aeroplankton deposits hundreds of millions of airborne viruses and tens of millions of bacteria every day on every square meter around the planet. Small, drifting aeroplankton are found everywhere in the atmosphere, reaching concentration up to 106 microbial cells per cubic metre. Processes such as aerosolization and wind transport determine how the microorganisms are distributed in the atmosphere. Air mass circulation globally disperses vast numbers of the floating aerial organisms, which travel across and between continents, creating biogeographic patterns by surviving and settling in remote environments. As well as the colonization of pristine environments, the globetrotting behaviour of these organisms has human health consequences. Airborne microorganisms are also involved in cloud formation and precipitation, and play important roles in the formation of the phyllosphere, a vast terrestrial habitat involved in nutrient cycling.

The atmosphere is the least understood biome on Earth despite its critical role as a microbial transport medium. and that they might be metabolically active. Different processes, such as aerosolisation, might be important in selecting which microorganisms exist in the atmosphere. In the case of microorganisms, air mass circulation disperses vast amounts of individuals and interconnects remote environments. Airborne microorganisms can travel between continents, survive and settle on remote environments, which creates biogeographic patterns. and antibiotic resistances, cloud formation and precipitation, involved in nutrient cycling. Previous studies investigating bioaerosols using amplicon sequencing predominantly focussed on the bacterial fraction of the air microbiome, while fungal and plant pollen fractions frequently remained understudied. Airborne microbial organisms also impact agricultural productivity, as bacterial and fungal species distributed by air movement act as plant blights. Furthermore, atmospheric processes, such as cloud condensation and ice nucleation events were shown to depend on airborne microbial particles. Therefore, understanding the dynamics of microbial organisms in air is crucial for insights into the atmosphere as an ecosystem, but also will inform on human wellbeing and respiratory health. In recent years, next generation DNA sequencing technologies, such as metabarcoding as well as coordinated metagenomics and metatranscriptomics studies, have been providing new insights into microbial ecosystem functioning, and the relationships that microorganisms maintain with their environment. There have been studies in soils, the ocean, the human gut, and elsewhere. In the atmosphere, though, microbial gene expression and metabolic functioning remain largely unexplored, in part due to low biomass and sampling difficulties. and targeted genomics and transcriptomics towards ribosomal genes has supported earlier findings about the maintenance of metabolic activity in aerosols and in clouds. An efficient transfer of the pollen guarantees successful reproduction in flowering plants. No matter how pollen is dispersed, the male female recognition is possible by mutual contact of stigma and pollen surfaces. Cytochemical reactions are responsible for pollen binding to a specific stigma. There is a body of evidence suggesting that allergic reactions induced by pollen are on the increase, particularly in highly industrial countries.]]

Fungi, a major element of atmospheric bioaerosols, are capable of existing and surviving in the air for extended periods of time. Both the spores and the mycelium may be dangerous for people suffering from allergies, causing various health issues including asthma. Apart from their negative impact on human health, atmospheric fungi may be dangerous for plants as sources of infection. Moreover, fungal organisms may be capable of creating additional toxins that are harmful to humans and animals, such as endotoxins or mycotoxins. Considering this aspect, aeromycological research is considered capable of predicting future symptoms of plant diseases in both crops and wild plants. Notably, the presence of numerous fungal organisms pathogenic to plants has been determined in mountainous regions. Intriguing are reports of thunderstorm asthma. In a now classic study from the United Kingdom, an outbreak of acute asthma was linked to increases in Didymella exitialis ascospores and Sporobolomyces basidiospores associated with a severe weather event. Thunderstorms are associated with spore plumes: when spore concentrations increase dramatically over a short period of time, for example from 20,000 spores/m3 to over 170,000 spores/m3 in 2 hours. However, other sources consider pollen or pollution as causes of thunderstorm asthma. Transoceanic and transcontinental dust events move large numbers of spores across vast distances and have the potential to impact public health, and similar correlative evidence links dust blown off the Sahara with pediatric emergency room admissions on the island of Trinidad. Fungal spores usually rank first among bioaerosol constituents due to their count numbers which can reach to between , while pollen grains and fern spores can each reach to between .]] Many small animals, mainly arthropods (such as insects and spiders), are also carried upwards into the atmosphere by air currents and may be found floating several thousand feet up. Aphids, for example, are frequently found at high altitudes. Ballooning, sometimes called kiting, is a process by which spiders, and some other small invertebrates, move through the air by releasing one or more gossamer threads to catch the wind, causing them to become airborne at the mercy of air currents. A spider (usually limited to individuals of a small species), or spiderling after hatching, will climb as high as it can, stand on raised legs with its abdomen pointed upwards ("tiptoeing"), and then release several silk threads from its spinnerets into the air. These automatically form a triangular shaped parachute which carries the spider away on updrafts of winds where even the slightest of breezes will disperse the arachnid. Even atmospheric samples collected from balloons at altitude and ships mid ocean have reported spider landings. Mortality is high. Enough lift for ballooning may occur, even in windless conditions, if an electrostatic charge gradient is present in the atmosphere.

Nematodes (roundworms), the most common animal taxon, are also found among aeroplankton. Accordingly, nematodes can be readily dispersed by wind. However, as reported by Vanschoenwinkel et al., Some microorganisms are swept up from terrestrial dust storms, but most originate from marine microorganisms in sea spray. In 2018, scientists reported that hundreds of millions of viruses and tens of millions of bacteria are deposited daily on every square meter around the planet. The presence of airborne cyanobacteria and microalgae as well as their negative impacts on human health have been documented by many researchers worldwide. However, studies on cyanobacteria and microalgae are few compared with those on other bacteria and viruses. Research is especially lacking on the presence and taxonomic composition of cyanobacteria and microalgae near economically important water bodies with much tourism. Research on airborne algae is especially important in tourist areas near water bodies. Sunbathers are exposed to particularly high quantities of harmful cyanobacteria and microalgae. Additionally, harmful microalgae and cyanobacteria blooms tend to occur in both marine and freshwater reservoirs during summer. Previous work has shown that the Mediterranean Sea is dominated by the picocyanobacteria Synechococcus sp. and Synechocystis sp., which are responsible for the production of a group of hepatotoxins known as microcystins. Because most tourism occurs in summer, many tourists are exposed to the most extreme negative impacts of airborne microalgae.]] Airborne bacteria are emitted by most Earth surfaces (plants, oceans, land, and urban areas) to the atmosphere via a variety of mechanical processes such as aeolian soil erosion, sea spray production, or mechanical disturbances including anthropogenic activities. and carried by wind to long distances. As a consequence, bacteria are present in the air up to at least the lower stratosphere. Given that the atmosphere is a large conveyor belt that moves air over thousands of kilometers, microorganisms are disseminated globally. Depending on their size, airborne cyanobacteria and microalgae can be inhaled by humans and settle in different parts of the respiratory system, leading to the formation or intensification of numerous diseases and ailments, e. g., allergies, dermatitis, and rhinitis. According to Wiśniewska et al.,

Airborne microalgae and cyanobacteria are the most poorly studied organisms in aerobiology and phycology. However, it was shown in 2012 that the average quantity of atmospheric algae is between 100 and 1000 cells per cubic meter of air. Cyanobacteria and microalgae end up in the air as a consequence of their emission from soil, buildings, trees, and roofs. Among these, microorganisms are of particular interest in fields as diverse as epidemiology, including phytopathology, bioterrorism, forensic science, and public health, and environmental sciences, like microbial ecology, meteorology and climatology. More precisely concerning the latter, airborne microorganisms contribute to the pool of particles nucleating the condensation and crystallization of water and they are thus potentially involved in cloud formation and in the triggering of precipitation. The constant flux of bacteria from the atmosphere to the Earth's surface due to precipitation and dry deposition can also affect global biodiversity, but they are rarely taken into account when conducting ecological surveys. As stressed by these studies attempting to decipher and understand the spread of microbes over the planet, concerted data are needed for documenting the abundance and distribution of airborne microorganisms, including at remote and altitudes sites. ), dispersal units (e. g., fungal spores and plant pollen), and various fragments or excretions (e. g., plant debris and brochosomes). Bioaerosol particle diameters range from nanometers up to about a tenth of a millimeter. The upper limit of the aerosol particle size range is determined by rapid sedimentation, i. e., larger particles are too heavy to remain airborne for extended periods of time. Bioaerosols include living and dead organisms as well as their fragments and excrements emitted from the biosphere into the atmosphere. Historically, the first investigations of the occurrence and dispersion of microorganisms and spores in the air can be traced back to the early 19th century. Since then, the study of bioaerosols has come a long way, and air samples collected with aircraft, balloons, and rockets have shown that bioaerosols released from land and ocean surfaces can be transported over long distances and up to very high altitudes, i. e., between continents and beyond the troposphere. and the potential for dispersal determines the distribution, abundance, and thus, the community dynamics of species at different sites. A new habitat must first be reached before filters such as organismal abilities and adaptations, the quality of a habitat, and the established biological community determine the colonization efficiency of a species. While larger animals can cover distances on their own and actively seek suitable habitats, small (<2 mm) organisms are often passively dispersed, While active dispersal accounts for rather predictable distribution patterns, passive dispersal leads to a more randomized immigration of organisms. A propagule is any material that functions in propagating an organism to the next stage in its life cycle, such as by dispersal. The propagule is usually distinct in form from the parent organism. Propagules are produced by plants (in the form of seeds or spores), fungi (in the form of spores), and bacteria (for example endospores or microbial cysts). Often cited as an important requirement for effective wind dispersal is the presence of propagules (e. g., resting eggs, cysts, ephippia, juvenile and adult resting stages), which also enables organisms to survive unfavorable environmental conditions until they enter a suitable habitat. These dispersal units can be blown from surfaces such as soil, moss, and the desiccated sediments of temporary or intermittent waters. The passively dispersed organisms are typically pioneer colonizers. with the weight and form of the propagules, and therefore, the wind speed required for their transport, determining the dispersal distance. For example, in nematodes, resting eggs are less effectively transported by wind than other life stages, while organisms in anhydrobiosis are lighter and thus more readily transported than hydrated forms. Because different organisms are, for the most part, not dispersed over the same distances, source habitats are also important, with the number of organisms contained in air declining with increasing distance from the source system. The distances covered by small animals range from a few meters, Freshwater organisms that must "cross the dry ocean" While these have been qualitatively well studied, accurate estimates of their dispersal rates are lacking. Microorganisms might undergo a selection process during their way up into the troposphere and the stratosphere. and 40 to 8 × 104 cells per cubic metre in the highest part of the troposphere called the free troposphere. The troposphere is the most dynamic layer in terms of chemistry and physics of aerosols and harbors complex chemical reactions and meteorological phenomena that lead to the coexistence of a gas phase, liquid phases (i. e., cloud, rain, and fog water) and solid phases (i. e., microscopic particulate matter, sand dust). The various atmospheric phases represent multiple biological niches. seasons, surface conditions

Microorganisms attached to aerosols can travel intercontinental distances, survive, and further colonize remote environments. Airborne microbes are influenced by environmental and climatic patterns that are predicted to change in the near future, with unknown consequences. Airborne microbial communities play significant roles in public health and meteorological processes, so it is important to understand how these communities are distributed over time and space. Given that cultivable organisms represent about 1% of the entire microbial community, culture independent techniques and especially metagenomic studies applied to atmospheric microbiology have the potential to provide additional information on the selection and genetic adaptation of airborne microorganisms. This observed correlation of microbial community functional potential and the physical and chemical characteristics of their environments could have resulted from genetic modifications (microbial adaptation

The presence of a specific microbial functional signature in the atmosphere has not been investigated yet. and might behave differently than bacterial cells. Still, the proportion and nature (i. e., fungi versus bacteria) of microbial cells that are resistant to the harsh atmospheric conditions within airborne microbial communities are unknown. and several studies have demonstrated diverse microbial biosignatures are recoverable from the atmosphere. Microbial transport has been shown to occur across inter continental distances above terrestrial habitats. which have potential human health consequences. Severe particulate matter pollution is associated with chronic obstructive pulmonary disease and asthma, as well as risks for early death. While the chemical components of particulate matter pollution and their impacts on human health have been widely studied, the potential impact of pollutant associated microbes remains unclear. Airborne microbial exposure, including exposure to dust associated organisms, has been established to both protect against and exacerbate certain diseases. Understanding the temporal dynamics of the taxonomic and functional diversity of microorganisms in urban air, especially during smog events, will improve understanding of the potential microbe associated health consequences. The data suggest that potential pathogen and antibiotic resistance burden increases with increasing pollution levels and that severe smog events promote the exposure. In addition, the particulate matter also contained several bacteria that harbored antibiotic resistant genes flanked by mobile genetic elements, which could be associated with horizontal gene transfer. Many of these bacteria were typical or putative members of the human microbiome.]] The outdoor atmosphere harbors diverse microbial assemblages composed of bacteria, fungi and viruses whose functioning remains largely unexplored. in general the vast majority of airborne microbes originate from natural environments like soil or plants, with large spatial and temporal variations of biomass and biodiversity. Once ripped off and aerosolized from surfaces by mechanical disturbances such as those generated by wind, raindrop impacts or water bubbling, a time long enough for being transported across oceans and continents and ice nuclei. provided that they survive their journey from emission to deposition. Bacterial survival is indeed naturally impaired during atmospheric transport, but a fraction remains viable. At high altitude, the peculiar environments offered by cloud droplets are thus regarded in some aspects as temporary microbial habitats, providing water and nutrients to airborne living cells. In addition, the detection of low levels of heterotrophy raises questions about microbial functioning in cloud water and its potential influence on the chemical reactivity of these complex and dynamic environments. Marine aerosols consist of a complex mixture of sea salt, non sea salt sulfate and organic molecules and can function as nuclei for cloud condensation, influencing the radiation balance and, hence, climate. For example, biogenic aerosols in remote marine environments (for example, the Southern Ocean) can increase the number and size of cloud droplets, having similar effects on climate as aerosols in highly polluted regions. Specifically, phytoplankton emit dimethylsulfide, and its derivate sulfate promotes cloud condensation. Understanding the ways in which marine phytoplankton contribute to aerosols will allow better predictions of how changing ocean conditions will affect clouds and feed back on climate. After the tantalizing detection of phosphine (PH3) in the atmosphere of the planet Venus, and in the absence of a known and plausible chemical mechanism to explain the formation of this molecule, Greaves et al. speculated in 2020 that microorganisms might be present in suspension in the Venusian atmosphere. They have formulated the hypothesis of the microbial formation of phosphine, envisaging the possibility of a liveable window in the Venusian clouds at a certain altitude with an acceptable temperature range for microbial life.

While the physical and chemical properties of airborne particulate matter have been extensively studied, their associated airborne microbiome remains largely unexplored. Microbiomes are defined as characteristic microbial communities, which include prokaryotes, fungi, protozoa, other micro eukaryotes and viruses, that occupy well defined habitats. The term microbiome is broader than other terms, for example, microbial communities, microbial population, microbiota or microbial flora, as microbiome refers to both its composition (the microorganisms involved) and its functions (their members' activities and interactions with the host/environment), which contribute to ecosystem functions. Throughout Earth's history, microbial communities have changed the climate, and climate has shaped microbial communities. Microorganisms can modify ecosystem processes or biogeochemistry on a global scale, and we start to uncover their role and potential involvement in changing the climate. However, the effects of climate change on microbial communities (i. e., diversity, dynamics, or distribution) are rarely addressed. In the case of fungal aerobiota, its composition is likely influenced by dispersal ability, rather than season or climate. Indeed, the origin of air masses from marine, terrestrial, or anthropogenic impacted environments, mainly shapes the atmospheric air microbiome. This evidence suggests that climatic conditions may act as an environmental filter for the aeroplankton, selecting a subset of species from the regional pool, and raises the question of the relative importance of the different factors affecting both bacterial and eukaryal aeroplankton.

In 2021, researchers demonstrated that environmental DNA (eDNA) can be collected from air and used to identify mammals. In 2023, scientists developed a specialized sampling probe and aircraft surveys to assess biodiversity of multiple taxa, including mammals, using air eDNA.