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Aerobiology of Plant Pathogens:
Mechanisms, Gradients and Spatial Patterns
Pravin Kumar Bagaria
L-2018-A-58-D
• Aerobiology (Greek: aēr = “air” + bios = “life” + logia = “to study”)
- a branch of biology that studies organic particles, such as bacteria, fungal
spores, very small insects, pollen grains and viruses, which are passively
transported by the air (Anonymous, 2017).
- the study of airborne biological particles and their movement and impact on
human, animal and plant health.
- a scientific multidisciplinary biological science, which deals with the source,
release, dispersion, and deposition of different micro-organisms found in the air
and their impact on the ecosystem or life of plants, animals and human beings
(Edmonds, 1979).
• 1935 - Term "Aerobiology" by F.C. Meier (USA)
• 1952 - Term 'Air Spora' by P.H. Gregory published in Nature which describe the
airborne pollen grains and fungal spores as:
“The population of air-borne particles of plant or animal origin, which will
here be called the air ‘spora’ (taking the Greek σπορ′α as a word of similar
usage to ‘flora’ and ‘fauna’), contains spores and pollens of various shapes
ranging in size from 100 μm in diameter for some tree pollens to 3-5 μm
with some of the smallest fungus spores” (Gregory, 1952).
Spores collected from air of Calcutta
by Cunningham in 1873.
(Figure collected from the book “The Air Spora” by Maureen E. Lacey and
Jonathan S. West, Springer Pub.2006)
• 1873 - In India, first aerobiological study by D.D.
Cunningham (British physician at Calcutta). The
book entitled, ‘Microscopic examination of air’.
• 1933-52 - Prof. K. C. Mehta collected
uredospores of three rusts of wheat and barley.
Reported the presence of teleutospores, smut
spores, Alternaria and different species of
Puccinia.
Aerobiological Triangle
https://shodhganga.inflibnet.ac.in
Isard et al 2005
• According to geometry, inoculum source can be classified as
Point source
Individuals or small groups of infected plants;
A diameter of less than 1% of the length of the gradient
Line source
Hedges containing infected alternative host plants or
Strips of a susceptible cultivar
Area source
Infected fields
Although such area sources may become point sources if the distance over which
the gradient is measured is kilometres rather than metres
• According to vertical position, inoculum source may be
Above ground level
Ground level sources
McCartney et al 2006
Source of Inoculum
Spore liberation/ discharge (Take off)
(process of detachment of spores from the spore-bearing structure)
I. Active Spore Discharge in Fungi: Spores may be violently discharged by the
mechanisms like:
(i) Bursting of spore-producing structures
(ii) Sudden changes in shape of turgid spores or of turgid structures associated with
the spores;
(iii) Rapid twisting movements produced as a result of drying in filamentous
sporangiophores or by hygroscopic movement;
(iv) Sudden breaking of tensile water in conidia or conidiophores, distorted on drying,
which are thereby permitted to return to their original form; and
(v) Impaction
II. Passive Spore Liberation:
(i) Liberation of Dry Spores - Through rain drop and winds (Mechanical momentum
and Blowing away:- Rust uredospore)
(ii) Liberation of Slime Spores- Through rain drop
• Spores may also be removed from the leaf surface by puffing action of raindrops
• Occurs when the first raindrops fall
• Release of puffball spores from the mature fruiting bodies has a similar action
• Strong gusts of wind or contact with animals can also result in spore puffs
I. Active Spore Discharge in Fungi:
A-C - Trigger device in Sphaerobolus sp.
D-H – Syringe device, D-E in Sphaerotheca sp., F-J in
Pilobolus sp.
Drop-excretion mechanism
A - Basidiospore discharge.
B-E – Successive stage in the fluid drop excretion
and basidiospore discharge
I. Active Spore Discharge in Fungi:
A-B – Change in condition of turgid structures in Sclerospora sp.
C-F – Hygroscopic movements of sporangiophores in
Peronospora tabacina.
G-K – Gas bubble mechanism in Deightoniella torulosa
Spore liberation mechanism by impact of rain
A-F – In Niduriales
G-J – Lycoperdon sp.
Dispersal of Plant Pathogen
• Transport of spores or infectious bodies, acting as inoculum, from one host to
another host at various distances resulting in the spread of the disease
OR
• Displacement of a plant pathogen from its place of production or origin to a
suitable place where it can grow/ established
• Fundamental step for repeated cycles of infection and multiplication
• Dependent on the method of discharge by individual taxa as well as
environmental factors, such as temperature, humidity, and wind speed
• Strong gusts disperse spores even when the average wind speeds are too low
• Wind dispersal is promoted by warm and dry weather
• Peak during afternoon hours, when humidity is low and wind speeds are
increased
McCartney et al 2006; Levetin, 2016
Mechanism of Spore Dispersion
• Active dispersion
• Passive dispersion:-
Dispersion by Wind
High temperatures & low relative humidity
Long range dissemination – b/w fields or regions
Dispersion by Rain splash
Also provides moisture required for germination
Short range dissemination – within plant or nearby
plants
Movement in the Atmosphere
• Wind is the major factor, with gusts and lulls affecting
take off, transport, and deposition
• In a crop, spores have to pass from the laminar layer
close to the leaf surface into the turbulent layer
within the crop
• Gusts and turbulence enhance spore removal from
leaves by sweeping away the layer of slow-moving air
next to the leaf surface
• Spores must pass through the crop boundary layer
surrounding the crop
Levetin 2016
The ground is black.
Above ground is thin layer of laminar air (L)
and on top of this turbulent air (T).
Discharged spores are disseminated by wind.
• Carried by wind, spores are transported both horizontally and vertically
• Horizontally, spores carried for thousands of kilometers, dispersing pathogens into new
areas
• Vertically, carried upward by convective activity or thermals and have been recovered
from altitudes higher than 5,000 m
• Rain splash can also propel spores into the atmosphere, and it is second to wind in
importance as a means of pathogen dispersal
• Splash-borne spores or bacteria are usually produced in mucilage which inhibits their
direct removal by wind
• The first raindrops dissolve the mucilage and leave a spore suspension available for splash
dispersal by additional raindrops
Levetin 2016
Survival in the Atmosphere
• Fungal spores are more resistant to environmental stress compared to parent hyphae.
• Exposure to harmful radiation, extremes of temperature and humidity can decrease the
viability.
• Changes in relative humidity, often caused by changing wind speeds, may affect survival,
especially for thin-walled spores, which may easily plasmolyze.
• Desiccation risks are more during the daytime and close to the ground.
• At night and at high altitudes, conditions are less stressful.
• Thin-walled colorless spores may be more vulnerable compared to pigmented spores.
• Low temperatures in the upper atmosphere may be preservative and protect spores
from UV damage
Levetin 2016
Scale of spore/ disease spread
Microscale,
Mesoscale, or
Synoptic scale Levetin, 2016
Scales of Pathogen Dispersal Scales of air turbulence
Mahaffee and Stoll, 2016
Microscale spread
• Limited to less than a few hundred meters within one field and occurs within one
growing season
• Roughly corresponds to a zero-order epidemic
• The focus begins with a single successful propagule causing an infection and creating a
lesion
• After several generations of localized pathogen spread for polycyclic diseases, which
produce many generations of inocula and many cycles of infection during a single growing
season, the focus may reach a detectable size
• In an annual crop, these are about 1 m in diameter around the initial source of infection
• If growing conditions are unsuitable for the pathogen, the focus may stop expanding or
even disappear with new growth in the canopy. Levetin, 2016
Mesoscale spread
• However, when conditions are favorable for the pathogen, the disease will spread
• As the primary focus continues to expand, secondary foci and later tertiary foci appear.
• This continued focal spread over a larger area is considered mesoscale spread and
corresponds to a first-order epidemic
• This may be restricted to one field but may spread over many fields or up to an area
several hundred square kilometers or even over part of a continent during a single
growing season
Levetin, 2016
Synoptic or Macroscale spread
• Synoptic or macroscale spread occurs when the epidemic progresses for several years and
spreads over an area of several thousand square kilometers
• This is also referred to as a second-order epidemic.
• This pandemic may cover a whole continent after a certain number of years
Spore Landing (Deposition)
• Sedimentation
• Impaction
• Inpingement
• Filtration
• Boundary layer exchange & turbulence
• Rain deposition
• While airborne – spores touch wet surfaces – get
trapped
Spore movement is influenced by
• Gravity
• Brownian motion
• Electric charge
• Temperature
• Inertial precipitation and impaction
• Periodicity of wind
Diurnal
Nocturnal
• Turbulence in air
Levetin 2016
Dispersal by wind/ rain-splash and spore deposition gradients
• Individual spores released from the same source under the same wind conditions follow
different paths and travel different distances.
• With disperse downwind, spore concentrations in the air decrease referred to as
‘concentration gradients’.
• The turbulent nature of wind causes a dilution in the concentration of a spore plume.
• Consequently, dispersal gradients for splash-dispersed spores are generally much shorter
than those for wind-dispersed spores.
• Crop canopy structure affects the deposition of splashed droplets and the potential for
spread by secondary splash.
• Thus, duration of exposure to rain and rain intensity may modify ‘primary splash’
gradients.
• Primary dispersal is dominant at the beginning of a rain shower.
• However, as rain duration continues, secondary spread may begin to be important.
• If the rain persists for sufficient time to deplete the source, inoculum deposited may be
lost by wash-off.
McCartney et al 2006
SPORE DEPOSITION AND DISEASE GRADIENTS
• For both wind and splash-dispersed plant pathogen inoculum, deposition rates decrease with
distance away from the inoculum source
• The disease pattern that develops will also show a decrease in disease with increasing distance
away from the source, i.e. a disease gradient
• Disease gradients can also result from gradients in host or environmental factors
• Background inoculum from a large number of distant sources produces a uniform distribution of
disease with distance across a crop
• Vertical disease gradients can also be observed when inoculum sources are at ground level
• Disease gradients produced by splash-dispersed inoculum are usually steeper than those
produced by wind-dispersed inoculum
• Secondary spore dispersal can flatten primary spore dispersal and disease gradients with time
McCartney et al 2006
• Monocyclic diseases produce only primary disease gradients
• Over long periods of time the disease gradients gradually become less steep
• Disease gradients with polycyclic diseases are first observed in a crop as primary disease
foci resulting from a single lesion
• Initially disease gradients are steep but spores which escape from the crop canopy soon
establish secondary foci
• Primary disease gradients become more shallow as foci expand and, with the expansion
of secondary foci
• Initial horizontal gradients are caused by wind-dispersed primary inoculum but
subsequent horizontal spread and vertical spread up the crop canopy is achieved by
splash-dispersed secondary inoculum
• Gradients from sources above ground level are generally less steep than those from
ground level sources
• The same spore dispersal mechanism could account for steep gradients close to a
source and shallow gradients farther away McCartney et al 2006
Measurement of gradients (spore dispersal or disease gradient)
Spore numbers per m3 (spore concentration gradient) or
Spore numbers per m2 (spore deposition gradient) (C) or
Disease incidence or severity (Y ) at different distances (x)
• Spore numbers can be estimated with artificial samplers
• Spore deposition gradients can be measured by passive samplers (horizontal slides under
rain-shields for wind-dispersed spores) or beakers for splash-dispersed spores
• Concentration gradients can be measured with volumetric samplers
• The disease component of disease gradients has been measured as numbers of lesions,
numbers of infected leaves, numbers of infected plants, the percentage leaf area affected or
the percentage of the population of plants which is affected
McCartney et al 2006
Spatial patterns
• Spatial patterns of disease may be quite different from the spore dispersal
patterns
• Because spore dispersal is a short term phenomenon compared to most other
stages of disease development
• Spatial patterns are the result of many individual dispersal events from many
sources over periods of days or even weeks
• Disease patterns and epidemic size are strongly influenced by dispersal patterns
• Spatial patterns foci are often circular but strongly affected by wind, may become
comet- or V-shaped.
• Foci generally have a constant radial expansion, with the rate varying with the
scale of the infection from a few centimeters per day for a localized infection to
hundreds of kilometers per year for a pandemic
McCartney et al 2006
• Trajectory analysis - a standard tool in the study of air movement and it tracks the
movement of air parcels using information on wind fields and atmospheric temperature
structures
• Potential long distance aerial transport uses air parcel trajectory analysis to establish links
between source and receptor regions
• Backward trajectory analysis is frequently used to trace the previous movement of a
spore-laden parcel of air and locate the inoculum source
• Once the source is identified, forward trajectories are used to indicate further potential
areas of fallout.
• Various dispersion models have been used to trace the movement of spores from
dissemination at a source to deposition at a sink by calculating trajectories based on upper
air winds, temperature, and other parameters.
McCartney et al 2006; Levetin 2016
NASA’S Balloon Missions
Exposing Microorganisms in the Stratosphere 1 (E-MIST 1) - 2014
• For studying bacteria in Earth’s stratosphere (about 10 to 31 miles)
at NASA’s Kennedy Space Center, Florida
• A radiation-tolerant strain of bacteria (Bacillus pumilus) was
carried inside the E-MIST payload (mounted on large balloon, New
Mexico)
• Purpose: To expose bacterium to harsh conditions of the
stratosphere (5 hours)
• Result: Data could be collected within the stratosphere
Exposing Microorganisms in the Stratosphere 2 (E-MIST 2) – 2015 October
• Exposed bacterium to Mars surface-like conditions (extremely cold, dry air, harsh ultraviolet
radiation and low air pressure) to test how well they could survive
• Result: After 8 hours of exposure, 99.999% of the bacteria were dead, damaged, or destroyed
beyond the point of being able to regrow (19 miles above sea level)
Microbes in Atmosphere for Radiation, Survival and Biological Outcomes Experiment (MARSBOx) –
2019, Sept
• This aerobiology research experiment was flown on a NASA scientific balloon mission launched from
Fort Sumner, New Mexico (6.5 hours and altitude of 110,000 feet)
• Purpose: To measure effect of ionizing radiation conditions in the stratosphere
Carried 9 different types of microorganisms (bacteria & fungi) in dormant state
• Results: most of bacteria died, but fungal spores were able to better withstand the harsh
environment at >20 miles up
Aircraft Bioaerosol Collector (ABC) - (installed NASA’s C-20A aircraft)
• ABC - an instrument, custom built at NASA’s Armstrong Flight Research Center
• Purpose:
To capture and seal up bioaerosol samples in troposphere and in lower stratosphere
(as high as 8.5 miles)
To tackle difficult challenge of sampling and studying microorganisms at extreme
altitudes during ascent, descent and sustained cruises
To discover airborne bacterial diversity at different levels
• Result: a similar distribution of bacteria in the atmosphere at all altitudes
Periodicity of airborne concentration of
Botrytis cinerea conidia above a
strawberry field monitored using rotating
arm sampler and a qPCR assay for
quantification of conidia
Carisse 2016
Dynamics of B. cinerea airborne conidia monitored in raspberry
(a), strawberry (b), and grape (c) plantings in Canada (2010)
Progress of Botrytis fruit rot in strawberry plantings with various
cultivars at the Agriculture and Agri-Food Canada experimental
farm in 2010 Carisse, 2016
Fungal spores were identified and quantified in the air of Bratislava during the 1-year
period (2016) using a Burkard 7-day volumetric aerospore trap.
Spore calendar for Bratislava Exponential classes (spores/m3):
a 1–5, b 6–10, c 11–25, d 26–50, e 51–100, f 101–500, g 501–1000, h
> 1000
Relative contributions (% of total spore
concentration) of the major spore types in
the air of Bratislava
Annual total spore count (spores/m3)-
836,418 fungal spores belonging to 53
spore types in Bratislava during 2016
Scevkova and Kovac 2019
Monthly variations in the spore concentrations of the major
fungal taxa and total fungal spores in the air of Bratislava
Prevailing weather conditions (mean, maximum and
minimum air temperature, absolute air humidity and
rainfall)
Scevkova and Kovac, 2019
Airborne spores of Cladosporium spp. were sampled on the roof, 21 m above sea level in
Viborg during 115 days, 31 May–22 September 2015, on the 48 × 14 mm slides using a
Hirst-type spore trap
Olsen et al 2019a
Daily average concentrations of Cladosporium spp. at
Viborg station during 31 May- 22 September 2015 (n =
115), mean daily average concentration over the period:
1897 spores m-3. Red vertical lines confine the longest
period of high concentrations. Peak daily average
concentration occurred on 16 August (13,553 Spores m-3)
Cladosporium spp. diurnal distribution at Viborg
station on the days with daily average
concentrations: above 3000 Spores m-3 (green line,
n = 21), above 3000 Spores m-3 without considering
14 August and 16 August (red line, n = 19), below
3000 Spores m-3 (blue line, n = 94)
The episode of 13–25 August 2015:
a 3-h time series of Cladosporium spp. concentrations at Viborg (blue) and Copenhagen (red) stations, daily
precipitation at Foulum station (green) ;
b Lines represent 48-h back trajectories for the period of 13–25 August: green on 13 August and 25 August, red
on the day with maximal concentration, i.e. on 16 August, black on the other days within the period;
Olsen et al 2019a
Burkard volumetric spore sampler.
Compared the concentrations of airborne Alternaria spores and the patterns of air mass
transport using HYSPLIT model between Copenhagen and Viborg with the main focus on
the days with daily average spore concentrations >100 s m-3 (high concentration days).
Monthly spore integrals of airborne Alternaria spores
(2012–2015) for all days and for high concentration days
(with daily average concentration > 100 s m-3); CPH
Copenhagen, VIB Viborg
Daily time-series of airborne Alternaria spp. At
Copenhagen and Viborg stations (2012–2015)
Olsen et al 2019b
Clusters and cluster means of 48-h back-trajectories for the Copenhagen station on the days with daily average
concentration:
a > 100 s m-3 (high days) and b <100 s m-3 (low days)
Olsen et al 2019b
Clusters and cluster means of 48-h back-trajectories for the Viborg station on the days with daily average
concentration:
a > 100 s m-3 (high days) and b <100 s m-3 (low days)
Olsen et al 2019b
Air samples were collected using settle plate method. Petri plates containing potato
dextrose agar (PDA), Martins rose bengal agar (MRBA) and Czapek’s Dox agar medium
supplemented with chloramphenicol (250 mg/ml) were used for collecting the air samples.
The rhizosphere, air and phylloplane were dominated by Rhizopus stolonifer.
Pestalotiopsis disseminata is one of the major pathogens of Som and was found highest in
aerosphere followed by phyllosphere.
Fungal diversity in air in the Som plantation area
Ray et al 2019
Common population among the four environments:
rhizosphere, non-rhizosphere, air and phylloplane
Two qPCR TaqMan assays were developed to detect pathogen DNA: the first used a generic
probe to detect Phytophthora spp., and the second was based on a specific probe for
detecting P. ramorum and P. lateralis.
All samples tested positive for the genus Phytophthora, although P. ramorum and P.
lateralis were not detected.
Migliorini et al 2019
Seasonal variation in DNA quantities
(pg/µl) of Phytophthora species
(black line) shown with
meteorological variables, i.e.
rainfall (mm, a);
relative humidity (%, b);
maximum, minimum and mean air
temperature (°C, c); and
extremes of air temperature (°C, d)
Conclusion
• A wide variety of plant pathogens, including viruses, bacteria, oomycetes, and fungi, are
dispersed through the atmosphere
• When conidia are produced on a source near the ground or in the lower canopy, they are
exposed to slow wind speeds, low turbulence, and rapid rates of sedimentation,
conditions that are conducive to short-distance transport
• When they are deposited on a susceptible host, infection can
occur, and when environmental conditions are favorable, the resulting disease spread
may lead to widespread crop loss
• Measurement of disease or spore gradients can be extremely important for identifying
sources of disease, for identifying inoculum dispersal mechanisms, for assessing the
effectiveness of some disease control strategies and for interpreting the results of field
experiments
• Long range dispersal favours more widespread epidemics and increases the likelihood of
disease persistence
• A thorough understanding of the role of the aerobiological pathway in pathogen
dispersal is necessary for the management and control of disease
• Knowledge of aerobiology can help researchers and farmers to assess, predict and
decrease the effects of epidemic pathogens
Aerobiology of Plant Pathogens........................pptx

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Aerobiology of Plant Pathogens........................pptx

  • 1. Aerobiology of Plant Pathogens: Mechanisms, Gradients and Spatial Patterns Pravin Kumar Bagaria L-2018-A-58-D
  • 2. • Aerobiology (Greek: aēr = “air” + bios = “life” + logia = “to study”) - a branch of biology that studies organic particles, such as bacteria, fungal spores, very small insects, pollen grains and viruses, which are passively transported by the air (Anonymous, 2017). - the study of airborne biological particles and their movement and impact on human, animal and plant health. - a scientific multidisciplinary biological science, which deals with the source, release, dispersion, and deposition of different micro-organisms found in the air and their impact on the ecosystem or life of plants, animals and human beings (Edmonds, 1979).
  • 3. • 1935 - Term "Aerobiology" by F.C. Meier (USA) • 1952 - Term 'Air Spora' by P.H. Gregory published in Nature which describe the airborne pollen grains and fungal spores as: “The population of air-borne particles of plant or animal origin, which will here be called the air ‘spora’ (taking the Greek σπορ′α as a word of similar usage to ‘flora’ and ‘fauna’), contains spores and pollens of various shapes ranging in size from 100 μm in diameter for some tree pollens to 3-5 μm with some of the smallest fungus spores” (Gregory, 1952).
  • 4. Spores collected from air of Calcutta by Cunningham in 1873. (Figure collected from the book “The Air Spora” by Maureen E. Lacey and Jonathan S. West, Springer Pub.2006) • 1873 - In India, first aerobiological study by D.D. Cunningham (British physician at Calcutta). The book entitled, ‘Microscopic examination of air’. • 1933-52 - Prof. K. C. Mehta collected uredospores of three rusts of wheat and barley. Reported the presence of teleutospores, smut spores, Alternaria and different species of Puccinia.
  • 6. Isard et al 2005
  • 7. • According to geometry, inoculum source can be classified as Point source Individuals or small groups of infected plants; A diameter of less than 1% of the length of the gradient Line source Hedges containing infected alternative host plants or Strips of a susceptible cultivar Area source Infected fields Although such area sources may become point sources if the distance over which the gradient is measured is kilometres rather than metres • According to vertical position, inoculum source may be Above ground level Ground level sources McCartney et al 2006 Source of Inoculum
  • 8. Spore liberation/ discharge (Take off) (process of detachment of spores from the spore-bearing structure) I. Active Spore Discharge in Fungi: Spores may be violently discharged by the mechanisms like: (i) Bursting of spore-producing structures (ii) Sudden changes in shape of turgid spores or of turgid structures associated with the spores; (iii) Rapid twisting movements produced as a result of drying in filamentous sporangiophores or by hygroscopic movement; (iv) Sudden breaking of tensile water in conidia or conidiophores, distorted on drying, which are thereby permitted to return to their original form; and (v) Impaction
  • 9. II. Passive Spore Liberation: (i) Liberation of Dry Spores - Through rain drop and winds (Mechanical momentum and Blowing away:- Rust uredospore) (ii) Liberation of Slime Spores- Through rain drop • Spores may also be removed from the leaf surface by puffing action of raindrops • Occurs when the first raindrops fall • Release of puffball spores from the mature fruiting bodies has a similar action • Strong gusts of wind or contact with animals can also result in spore puffs
  • 10. I. Active Spore Discharge in Fungi: A-C - Trigger device in Sphaerobolus sp. D-H – Syringe device, D-E in Sphaerotheca sp., F-J in Pilobolus sp. Drop-excretion mechanism A - Basidiospore discharge. B-E – Successive stage in the fluid drop excretion and basidiospore discharge
  • 11. I. Active Spore Discharge in Fungi: A-B – Change in condition of turgid structures in Sclerospora sp. C-F – Hygroscopic movements of sporangiophores in Peronospora tabacina. G-K – Gas bubble mechanism in Deightoniella torulosa Spore liberation mechanism by impact of rain A-F – In Niduriales G-J – Lycoperdon sp.
  • 12. Dispersal of Plant Pathogen • Transport of spores or infectious bodies, acting as inoculum, from one host to another host at various distances resulting in the spread of the disease OR • Displacement of a plant pathogen from its place of production or origin to a suitable place where it can grow/ established • Fundamental step for repeated cycles of infection and multiplication • Dependent on the method of discharge by individual taxa as well as environmental factors, such as temperature, humidity, and wind speed • Strong gusts disperse spores even when the average wind speeds are too low • Wind dispersal is promoted by warm and dry weather • Peak during afternoon hours, when humidity is low and wind speeds are increased McCartney et al 2006; Levetin, 2016
  • 13. Mechanism of Spore Dispersion • Active dispersion • Passive dispersion:- Dispersion by Wind High temperatures & low relative humidity Long range dissemination – b/w fields or regions Dispersion by Rain splash Also provides moisture required for germination Short range dissemination – within plant or nearby plants
  • 14. Movement in the Atmosphere • Wind is the major factor, with gusts and lulls affecting take off, transport, and deposition • In a crop, spores have to pass from the laminar layer close to the leaf surface into the turbulent layer within the crop • Gusts and turbulence enhance spore removal from leaves by sweeping away the layer of slow-moving air next to the leaf surface • Spores must pass through the crop boundary layer surrounding the crop Levetin 2016 The ground is black. Above ground is thin layer of laminar air (L) and on top of this turbulent air (T). Discharged spores are disseminated by wind.
  • 15. • Carried by wind, spores are transported both horizontally and vertically • Horizontally, spores carried for thousands of kilometers, dispersing pathogens into new areas • Vertically, carried upward by convective activity or thermals and have been recovered from altitudes higher than 5,000 m • Rain splash can also propel spores into the atmosphere, and it is second to wind in importance as a means of pathogen dispersal • Splash-borne spores or bacteria are usually produced in mucilage which inhibits their direct removal by wind • The first raindrops dissolve the mucilage and leave a spore suspension available for splash dispersal by additional raindrops Levetin 2016
  • 16. Survival in the Atmosphere • Fungal spores are more resistant to environmental stress compared to parent hyphae. • Exposure to harmful radiation, extremes of temperature and humidity can decrease the viability. • Changes in relative humidity, often caused by changing wind speeds, may affect survival, especially for thin-walled spores, which may easily plasmolyze. • Desiccation risks are more during the daytime and close to the ground. • At night and at high altitudes, conditions are less stressful. • Thin-walled colorless spores may be more vulnerable compared to pigmented spores. • Low temperatures in the upper atmosphere may be preservative and protect spores from UV damage Levetin 2016
  • 17. Scale of spore/ disease spread Microscale, Mesoscale, or Synoptic scale Levetin, 2016 Scales of Pathogen Dispersal Scales of air turbulence Mahaffee and Stoll, 2016
  • 18. Microscale spread • Limited to less than a few hundred meters within one field and occurs within one growing season • Roughly corresponds to a zero-order epidemic • The focus begins with a single successful propagule causing an infection and creating a lesion • After several generations of localized pathogen spread for polycyclic diseases, which produce many generations of inocula and many cycles of infection during a single growing season, the focus may reach a detectable size • In an annual crop, these are about 1 m in diameter around the initial source of infection • If growing conditions are unsuitable for the pathogen, the focus may stop expanding or even disappear with new growth in the canopy. Levetin, 2016
  • 19. Mesoscale spread • However, when conditions are favorable for the pathogen, the disease will spread • As the primary focus continues to expand, secondary foci and later tertiary foci appear. • This continued focal spread over a larger area is considered mesoscale spread and corresponds to a first-order epidemic • This may be restricted to one field but may spread over many fields or up to an area several hundred square kilometers or even over part of a continent during a single growing season Levetin, 2016 Synoptic or Macroscale spread • Synoptic or macroscale spread occurs when the epidemic progresses for several years and spreads over an area of several thousand square kilometers • This is also referred to as a second-order epidemic. • This pandemic may cover a whole continent after a certain number of years
  • 20. Spore Landing (Deposition) • Sedimentation • Impaction • Inpingement • Filtration • Boundary layer exchange & turbulence • Rain deposition • While airborne – spores touch wet surfaces – get trapped Spore movement is influenced by • Gravity • Brownian motion • Electric charge • Temperature • Inertial precipitation and impaction • Periodicity of wind Diurnal Nocturnal • Turbulence in air Levetin 2016
  • 21. Dispersal by wind/ rain-splash and spore deposition gradients • Individual spores released from the same source under the same wind conditions follow different paths and travel different distances. • With disperse downwind, spore concentrations in the air decrease referred to as ‘concentration gradients’. • The turbulent nature of wind causes a dilution in the concentration of a spore plume. • Consequently, dispersal gradients for splash-dispersed spores are generally much shorter than those for wind-dispersed spores. • Crop canopy structure affects the deposition of splashed droplets and the potential for spread by secondary splash. • Thus, duration of exposure to rain and rain intensity may modify ‘primary splash’ gradients. • Primary dispersal is dominant at the beginning of a rain shower. • However, as rain duration continues, secondary spread may begin to be important. • If the rain persists for sufficient time to deplete the source, inoculum deposited may be lost by wash-off. McCartney et al 2006
  • 22. SPORE DEPOSITION AND DISEASE GRADIENTS • For both wind and splash-dispersed plant pathogen inoculum, deposition rates decrease with distance away from the inoculum source • The disease pattern that develops will also show a decrease in disease with increasing distance away from the source, i.e. a disease gradient • Disease gradients can also result from gradients in host or environmental factors • Background inoculum from a large number of distant sources produces a uniform distribution of disease with distance across a crop • Vertical disease gradients can also be observed when inoculum sources are at ground level • Disease gradients produced by splash-dispersed inoculum are usually steeper than those produced by wind-dispersed inoculum • Secondary spore dispersal can flatten primary spore dispersal and disease gradients with time McCartney et al 2006
  • 23. • Monocyclic diseases produce only primary disease gradients • Over long periods of time the disease gradients gradually become less steep • Disease gradients with polycyclic diseases are first observed in a crop as primary disease foci resulting from a single lesion • Initially disease gradients are steep but spores which escape from the crop canopy soon establish secondary foci • Primary disease gradients become more shallow as foci expand and, with the expansion of secondary foci • Initial horizontal gradients are caused by wind-dispersed primary inoculum but subsequent horizontal spread and vertical spread up the crop canopy is achieved by splash-dispersed secondary inoculum • Gradients from sources above ground level are generally less steep than those from ground level sources • The same spore dispersal mechanism could account for steep gradients close to a source and shallow gradients farther away McCartney et al 2006
  • 24. Measurement of gradients (spore dispersal or disease gradient) Spore numbers per m3 (spore concentration gradient) or Spore numbers per m2 (spore deposition gradient) (C) or Disease incidence or severity (Y ) at different distances (x) • Spore numbers can be estimated with artificial samplers • Spore deposition gradients can be measured by passive samplers (horizontal slides under rain-shields for wind-dispersed spores) or beakers for splash-dispersed spores • Concentration gradients can be measured with volumetric samplers • The disease component of disease gradients has been measured as numbers of lesions, numbers of infected leaves, numbers of infected plants, the percentage leaf area affected or the percentage of the population of plants which is affected McCartney et al 2006
  • 25. Spatial patterns • Spatial patterns of disease may be quite different from the spore dispersal patterns • Because spore dispersal is a short term phenomenon compared to most other stages of disease development • Spatial patterns are the result of many individual dispersal events from many sources over periods of days or even weeks • Disease patterns and epidemic size are strongly influenced by dispersal patterns • Spatial patterns foci are often circular but strongly affected by wind, may become comet- or V-shaped. • Foci generally have a constant radial expansion, with the rate varying with the scale of the infection from a few centimeters per day for a localized infection to hundreds of kilometers per year for a pandemic McCartney et al 2006
  • 26. • Trajectory analysis - a standard tool in the study of air movement and it tracks the movement of air parcels using information on wind fields and atmospheric temperature structures • Potential long distance aerial transport uses air parcel trajectory analysis to establish links between source and receptor regions • Backward trajectory analysis is frequently used to trace the previous movement of a spore-laden parcel of air and locate the inoculum source • Once the source is identified, forward trajectories are used to indicate further potential areas of fallout. • Various dispersion models have been used to trace the movement of spores from dissemination at a source to deposition at a sink by calculating trajectories based on upper air winds, temperature, and other parameters. McCartney et al 2006; Levetin 2016
  • 27. NASA’S Balloon Missions Exposing Microorganisms in the Stratosphere 1 (E-MIST 1) - 2014 • For studying bacteria in Earth’s stratosphere (about 10 to 31 miles) at NASA’s Kennedy Space Center, Florida • A radiation-tolerant strain of bacteria (Bacillus pumilus) was carried inside the E-MIST payload (mounted on large balloon, New Mexico) • Purpose: To expose bacterium to harsh conditions of the stratosphere (5 hours) • Result: Data could be collected within the stratosphere Exposing Microorganisms in the Stratosphere 2 (E-MIST 2) – 2015 October • Exposed bacterium to Mars surface-like conditions (extremely cold, dry air, harsh ultraviolet radiation and low air pressure) to test how well they could survive • Result: After 8 hours of exposure, 99.999% of the bacteria were dead, damaged, or destroyed beyond the point of being able to regrow (19 miles above sea level)
  • 28. Microbes in Atmosphere for Radiation, Survival and Biological Outcomes Experiment (MARSBOx) – 2019, Sept • This aerobiology research experiment was flown on a NASA scientific balloon mission launched from Fort Sumner, New Mexico (6.5 hours and altitude of 110,000 feet) • Purpose: To measure effect of ionizing radiation conditions in the stratosphere Carried 9 different types of microorganisms (bacteria & fungi) in dormant state • Results: most of bacteria died, but fungal spores were able to better withstand the harsh environment at >20 miles up Aircraft Bioaerosol Collector (ABC) - (installed NASA’s C-20A aircraft) • ABC - an instrument, custom built at NASA’s Armstrong Flight Research Center • Purpose: To capture and seal up bioaerosol samples in troposphere and in lower stratosphere (as high as 8.5 miles) To tackle difficult challenge of sampling and studying microorganisms at extreme altitudes during ascent, descent and sustained cruises To discover airborne bacterial diversity at different levels • Result: a similar distribution of bacteria in the atmosphere at all altitudes
  • 29. Periodicity of airborne concentration of Botrytis cinerea conidia above a strawberry field monitored using rotating arm sampler and a qPCR assay for quantification of conidia Carisse 2016
  • 30. Dynamics of B. cinerea airborne conidia monitored in raspberry (a), strawberry (b), and grape (c) plantings in Canada (2010) Progress of Botrytis fruit rot in strawberry plantings with various cultivars at the Agriculture and Agri-Food Canada experimental farm in 2010 Carisse, 2016
  • 31. Fungal spores were identified and quantified in the air of Bratislava during the 1-year period (2016) using a Burkard 7-day volumetric aerospore trap.
  • 32. Spore calendar for Bratislava Exponential classes (spores/m3): a 1–5, b 6–10, c 11–25, d 26–50, e 51–100, f 101–500, g 501–1000, h > 1000 Relative contributions (% of total spore concentration) of the major spore types in the air of Bratislava Annual total spore count (spores/m3)- 836,418 fungal spores belonging to 53 spore types in Bratislava during 2016 Scevkova and Kovac 2019
  • 33. Monthly variations in the spore concentrations of the major fungal taxa and total fungal spores in the air of Bratislava Prevailing weather conditions (mean, maximum and minimum air temperature, absolute air humidity and rainfall) Scevkova and Kovac, 2019
  • 34. Airborne spores of Cladosporium spp. were sampled on the roof, 21 m above sea level in Viborg during 115 days, 31 May–22 September 2015, on the 48 × 14 mm slides using a Hirst-type spore trap
  • 35. Olsen et al 2019a Daily average concentrations of Cladosporium spp. at Viborg station during 31 May- 22 September 2015 (n = 115), mean daily average concentration over the period: 1897 spores m-3. Red vertical lines confine the longest period of high concentrations. Peak daily average concentration occurred on 16 August (13,553 Spores m-3) Cladosporium spp. diurnal distribution at Viborg station on the days with daily average concentrations: above 3000 Spores m-3 (green line, n = 21), above 3000 Spores m-3 without considering 14 August and 16 August (red line, n = 19), below 3000 Spores m-3 (blue line, n = 94)
  • 36. The episode of 13–25 August 2015: a 3-h time series of Cladosporium spp. concentrations at Viborg (blue) and Copenhagen (red) stations, daily precipitation at Foulum station (green) ; b Lines represent 48-h back trajectories for the period of 13–25 August: green on 13 August and 25 August, red on the day with maximal concentration, i.e. on 16 August, black on the other days within the period; Olsen et al 2019a
  • 37. Burkard volumetric spore sampler. Compared the concentrations of airborne Alternaria spores and the patterns of air mass transport using HYSPLIT model between Copenhagen and Viborg with the main focus on the days with daily average spore concentrations >100 s m-3 (high concentration days).
  • 38. Monthly spore integrals of airborne Alternaria spores (2012–2015) for all days and for high concentration days (with daily average concentration > 100 s m-3); CPH Copenhagen, VIB Viborg Daily time-series of airborne Alternaria spp. At Copenhagen and Viborg stations (2012–2015) Olsen et al 2019b
  • 39. Clusters and cluster means of 48-h back-trajectories for the Copenhagen station on the days with daily average concentration: a > 100 s m-3 (high days) and b <100 s m-3 (low days) Olsen et al 2019b
  • 40. Clusters and cluster means of 48-h back-trajectories for the Viborg station on the days with daily average concentration: a > 100 s m-3 (high days) and b <100 s m-3 (low days) Olsen et al 2019b
  • 41. Air samples were collected using settle plate method. Petri plates containing potato dextrose agar (PDA), Martins rose bengal agar (MRBA) and Czapek’s Dox agar medium supplemented with chloramphenicol (250 mg/ml) were used for collecting the air samples. The rhizosphere, air and phylloplane were dominated by Rhizopus stolonifer. Pestalotiopsis disseminata is one of the major pathogens of Som and was found highest in aerosphere followed by phyllosphere.
  • 42. Fungal diversity in air in the Som plantation area Ray et al 2019 Common population among the four environments: rhizosphere, non-rhizosphere, air and phylloplane
  • 43. Two qPCR TaqMan assays were developed to detect pathogen DNA: the first used a generic probe to detect Phytophthora spp., and the second was based on a specific probe for detecting P. ramorum and P. lateralis. All samples tested positive for the genus Phytophthora, although P. ramorum and P. lateralis were not detected.
  • 44. Migliorini et al 2019 Seasonal variation in DNA quantities (pg/µl) of Phytophthora species (black line) shown with meteorological variables, i.e. rainfall (mm, a); relative humidity (%, b); maximum, minimum and mean air temperature (°C, c); and extremes of air temperature (°C, d)
  • 45. Conclusion • A wide variety of plant pathogens, including viruses, bacteria, oomycetes, and fungi, are dispersed through the atmosphere • When conidia are produced on a source near the ground or in the lower canopy, they are exposed to slow wind speeds, low turbulence, and rapid rates of sedimentation, conditions that are conducive to short-distance transport • When they are deposited on a susceptible host, infection can occur, and when environmental conditions are favorable, the resulting disease spread may lead to widespread crop loss • Measurement of disease or spore gradients can be extremely important for identifying sources of disease, for identifying inoculum dispersal mechanisms, for assessing the effectiveness of some disease control strategies and for interpreting the results of field experiments • Long range dispersal favours more widespread epidemics and increases the likelihood of disease persistence • A thorough understanding of the role of the aerobiological pathway in pathogen dispersal is necessary for the management and control of disease • Knowledge of aerobiology can help researchers and farmers to assess, predict and decrease the effects of epidemic pathogens

Notas del editor

  1. Aerobiology (from Greek ἀήρ, aēr, "air"; βίος, bios, "life"; and -λογία, -logia) is a branch of biology that studies organic particles, such as bacteria, fungal spores, very small insects, pollen grains and viruses, which are passively transported by the air.[1] Aerobiologists have traditionally been involved in the measurement and reporting of airborne pollen and fungal spores as a service to allergy sufferers.[1] The first finding of airborne algae took place in Germany in 1910.[2]
  2. 1935 - The term "Aerobiology" by F.C. Meier (USA) for the studies of air spora like airborne fungal spores, pollen grains and other microorganisms. 1952 - Term 'Air Spora' by P.H. Gregory published in Nature which describe the airborne pollen grains and fungal spores as: 1873 - In India, first aerobiological study was carried out by D.D. Cunningham, a British physician at, Calcutta. This was the first report on aerobiological work in India, was published in the book entitled, „Microscopic examination of air‟. 1933-52 - Prof. K. C. Mehta collected uredospores of three rusts of wheat and barley from 62 different parts of country in different altitude. He reported the presence of teleutospores, smut spores, Alternaria and different species of Puccinia.
  3. Most of the aerobiological work is carried out with reference to the Aerobiological Triangle described by a pathway of five main steps viz.,
  4. Chapter 9:- General aerobiological process diagram (Isard et al. Principles of the atmospheric pathway for invasive species applied to soybean rust. 2005. Copyright, American Institute of Biological Sciences). Isard SA, Russo JM, Ariatti A. 2007. The Integrated Aerobiology Modeling System applied to the spread of soybean rust into the Ohio River valley during September 2006. Aerobiologia 23:271–282. Isard, S. A., Gage, S. H., Comtois, P. and Russo, J. M., 2005: Principles of the atmospheric pathway for invasive species applied to soybean rust. BioScience 55, pp. 851-861.
  5. Conidia of Blumeria (Erysiphe) graminis f.sp. hordei (cause of barley powdery mildew), which form in chains above the leaf surface, were released by wind speeds greater than 0.5 m s (Hammett and Manners, 1974) and conidia of Drechslera maydis (cause of southern leaf blight of maize) were removed only by wind speeds of more than 5 m s (Aylor, 1975). The wind intermittency observed in crop canopies probably plays an important role in spore removal because it is only in gusts that wind speeds are large enough to remove spores However, Aylor (1987) suggests that deposition will determine the shape of concentration gradients only when wind speeds in the canopy are low and when turbulence is slight. Thus, for spores released in gusts the effects of enhanced turbulence on diffusion may be much greater than the enhanced deposition by inertial impaction.
  6. Conidia of Blumeria (Erysiphe) graminis f.sp. hordei (cause of barley powdery mildew), which form in chains above the leaf surface, were released by wind speeds greater than 0.5 m s (Hammett and Manners, 1974) and conidia of Drechslera maydis (cause of southern leaf blight of maize) were removed only by wind speeds of more than 5 m s (Aylor, 1975). The wind intermittency observed in crop canopies probably plays an important role in spore removal because it is only in gusts that wind speeds are large enough to remove spores However, Aylor (1987) suggests that deposition will determine the shape of concentration gradients only when wind speeds in the canopy are low and when turbulence is slight. Thus, for spores released in gusts the effects of enhanced turbulence on diffusion may be much greater than the enhanced deposition by inertial impaction.
  7. I. Active Spore Discharge in Fungi: Spores may be violently discharged by the mechanisms like: (i) The bursting of spore-producing structures; (ii) Sudden chan­ges in shape of turgid spores or of turgid structures associated with the spores; (iii) Rapid twisting movements produced as a result of drying in filamentous sporangiophores or by hygroscopic movement; (iv) Sudden breaking of tensile water in conidia or conidiophores, distorted on drying, which are thereby permitted to return to their original form; and (a) by impaction. The distance of projection of spore discharge depends on the initial velocity of the projective and on its size, shape and density.
  8. Active Spore Discharge in Fungi: Spores may be violently discharged by the mechanisms like: (i) The bursting of spore-producing structures; (ii) Sudden chan­ges in shape of turgid spores or of turgid structures associated with the spores; (iii) Rapid twisting movements produced as a result of drying in filamentous sporangiophores or by hygroscopic movement; (iv) Sudden breaking of tensile water in conidia or conidiophores, distorted on drying, which are thereby permitted to return to their original form; and (a) by impaction. The distance of projection of spore discharge depends on the initial velocity of the projective and on its size, shape and density. The active discharge of basidiospores of Hymenomycetes is associated with the secretion of a small drop of liquid and the spores are discharged by drop-excretion mechanism (Fig. 259).
  9. CHAPTER 6 DISPERSAL OF FOLIAR PLANT PATHOGENS: MECHANISMS, GRADIENTS AND SPATIAL PATTERNS. H.A. McCARTNEY, B.D.L. FITT AND J.S. WEST B. M. Cooke, D. Gareth Jones and B. Kaye (eds.), The Epidemiology of Plant Diseases, 2nd edition, 159–192. © 2006 Springer. Printed in the Netherlands
  10. Although still vulnerable to certain types of environmental damage while airborne ; spores have even been reported to germinate in the clouds Spores may also serve as condensation nuclei for rain. Because of the erosion of the ozone layer in the upper atmosphere, the effects of UV radiation on fungal spores have been the focus of several studies. Scientists are interested in possible decreases in spore germination, mycelium development, and spore formation caused by the radiation (53, 54). Despite environmental hazards, many spores are able to survive long-range transport, but the percentage of viable spores that actually reach a target and cause infection is low.
  11. Levetin, 2016 Aerobiology of Agricultural Pathogens
  12. Levetin, 2016 Aerobiology of Agricultural Pathogens
  13. Levetin, 2016 Aerobiology of Agricultural Pathogens
  14. However, the proportion of conidia that escape the canopy, assuming that the source is within it, depends on the equilibrium between deposition and turbulent transport and on the vertical position of the inoculum source. When conidia are produced on a source near the ground or in the lower canopy, they are exposed to slow wind speeds, low turbulence, and rapid rates of sedimentation, conditions that are conducive to short-distance transport.Spores can be deposited on the crop surface by sedimentation, impaction, boundary layer exchange, turbulence, or electrostatic deposition and through raindrops Loss of viability may occur due to desiccation
  15. Winds are highly variable in both time and space. This variability or turbulence causes individual spores, released from the same source under the same wind conditions, to follow different paths and travel different distances. Therefore, as spore plumes disperse downwind from sources their concentrations in the air decrease. The decreases in concentration are frequently referred to as ‘concentration gradients’. Mean wind speed characteristics above crops are fairly well understood; wind speeds increase with height depending on the nature of the crop (height, architecture, density) and the stability of the atmosphere (temperature profile). For example, in neutrally stratified atmospheres when buoyancy effects can be neglected, over open terrain with uniform vegetation, wind speed u(z) increases logarithmically with height z : The wind profile is logarithmic only with well formed surface boundary layers over large uniform areas. Wind profiles near obstructions such as hedges or near changes in terrain, for example woodland boundaries, may be more complex
  16. Monocyclic diseases produce only primary disease gradients, in which all the lesions arise from the same inoculum source. For example, gradients of the phoma leaf spot stage of stem canker (causal agent Leptosphaeria maculans) can be produced by the wind-borne ascospores in winter oilseed rape crops in the autumn (Gladders and Musa, 1980). However, spores of pathogens causing monocyclic diseases may be released over long periods of time so that the disease gradients gradually become less steep as the growing season progresses. This may explain why gradients of wheat eyespot in inoculated winter wheat plots became less steep with successive observations, although removal of inoculum suggested that there was no secondary disease spread (Rowe and Powelson, 1973).
  17. Many economically important crop diseases are caused by foliar fungal pathogens, for which the main routes of dispersal are wind-borne or splash-borne spores. The scale of dispersal by these processes ranges from a few centimetres for some the wind. For foliar pathogens, disease spread is the direct consequence of spore dispersal, although spatial patterns of disease may be quite different from the spore dispersal patterns which cause them. This is partly because spore dispersal is a short term phenomenon compared to most other stages of disease development. Disease patterns are often the result of many individual dispersal events from many sources over periods of days or even weeks. For example, conidia of Pyrenopeziza brassicae, the cause of light leaf spot on oilseed rape (Brassica napus ssp. oleifera), take about 18 hours to germinate under optimum conditions, while splash dispersal of conidia over typical distances of 20-30 cm takes less than one second and wind dispersal of ascospores of P. brassicae over 100 m takes 1-2 minutes. Even for long distance dispersal, such as for tobacco blue mould (www.ces.ncsu.edu/depts/pp/bluemold/) that can spread from Cuba to the southern USA (Aylor, 1999) or cereal rusts in the USA or India (Hamilton and Stakman, 1967; Nagarajan and Singh, 1990), dispersal events (hours or days) may be short compared with infection processes.
  18. The HYSPLIT (hybrid single-particle Lagrangian integrated trajectory) model has been widely and successfully used to track the movement of several pathogens and predict the occurrence of disease outbreaks Back-trajectory analysis revealed long distance dispersal of exotic Bacillus bacteria 1800 km from the black sea to Sweden, where the species was isolated from red pigmented snow. Trajectory modelling account for large scale movement of air parcels due to wind direction changes and track air movements over large distances. Several studies of potential long distance aerial transport of plant pathogens have used air parcel trajectory analysis to establish links between source and receptor regions. Trajectory analysis is a standard tool in the study of air pollutant movement and it tracks the movement of air parcels using information on wind fields and atmospheric temperature structures. Back-trajectory analysis of wind contributed to evidence for long distance dispersal of exotic Bacillus bacteria 1800 km from the black sea to Sweden, where the species was isolated from red pigmented snow. Trajectory modelling can account for large scale movement of air parcels due to wind direction changes and track air movements over large distances.
  19. A radiation-tolerant strain of bacteria called Bacillus pumilus was carried inside the E-MIST payload, which was equipped with power, a control board for self-controlled operations, customizable electronics, environmental controls and sensors. The second Exposing Microorganisms in the Stratosphere mission, E-MIST 2, exposed the bacterium Bacillus pumilus SAFR-032 to Mars surface-like conditions to test how well they could survive. The E-MIST 2 payload was launched from New Mexico on a NASA high-altitude balloon and spent eight hours within the stratosphere at close to 19 miles above sea level. Samples were parachuted back to Earth for analysis, and the science team found that, after the eight hours of exposure, 99.999% of the bacteria were dead, damaged, or destroyed beyond the point of being able to regrow. The undamaged few showed small variations in DNA compared to samples of the same bacteria that stayed on the ground. Fully understanding the implications of these results will require further study, but the initial discoveries from the mission have provided significant insights for aerobiology, Earth ecology and astrobiology. The E-MIST 2 mission launched in October 2015.
  20. The MARSBOx experiment for aerobiology research was flown on a NASA scientific balloon mission launched from Fort Sumner, New Mexico, on Sept. 23, 2019. The mission lasted 6.5 hours and reached a sustained altitude of 110,000 feet. MARSBOx measured the ionizing radiation conditions in the stratosphere using onboard instruments. It also carried nine different types of microorganisms, including bacteria and fungi, in a dormant state that can protect them from many tough environmental conditions. Preliminary results from the flight show that most of the bacteria died, but the fungal spores were able to better withstand the harsh environment at more than 20 miles up. Aircraft Bioaerosol Collector (ABC) The Aircraft Bioaerosol Collector, or ABC, is an instrument that was custom built at NASA’s Armstrong Flight Research Center to capture and seal up bioaerosol samples from upstream air flowing around a moving aircraft. The ABC can collect samples while flying as high as 8.5 miles, and tackles the difficult challenge of sampling and studying microorganisms afloat at extreme altitudes. The first mission to use the instrument, ABC-1, was led by members of the Aerobiology Lab at NASA Ames and was designed to discover the types of airborne bacteria present at different levels in the troposphere, the lowest layer of Earth’s atmosphere, and in the lower stratosphere, the layer above the troposphere. The research team installed the ABC on NASA’s C-20A aircraft. The research jet was then flown over regions of California and the western U.S., and the ABC collected air samples during ascent, descent and sustained cruises at altitudes up to almost 7.5 miles. Scientists were surprised to discover a similar distribution of bacteria in the atmosphere at all altitudes studied.
  21. Chapter 7 Epidemiology and Aerobiology of Botrytis spp. By Odile Carisse © Her Majesty the Queen Right of Canada 2016 The release of Botrytis conidia from conidiating material is influenced by wind speed, and the removal of conidia generally increases with increasing wind speed. The release of conidia is regulated by a hygroscopic mechanism as well as by leaf vibrations, air movements, and rain splashes (Jarvis 1962a, b, c, 1980b; Sutton 1990; Thomas et al. 1988). For most Botrytis spp., there is a circadian periodicity in airborne conidia concentration: the maximum occurs at about midday, which corresponds to the highest wind speed and turbulence near the ground (Fig. 7.5). In general, this periodicity is correlated positively with increasing temperature and wind velocity and negatively with increasing percentage of relative humidity (RH) and the presence of dew. S. Fillinger, Y. Elad (eds.), Botrytis – the Fungus, the Pathogen and its Management in Agricultural Systems, DOI 10.1007/978-3-319-23371-0_7
  22. In flower-infecting Botrytis pathosystems, the seasonal progress of airborne B. cinerea in berry plantings is characterized generally by an airborne conidia concentration that is initially low but then increases during fruit ripening and until the last fruit harvest
  23. Fungal spores were identified and quantified in the air of Bratislava during the 1-year period (2016) using a Burkard 7-day volumetric aerospore trap. Spectrum and quantity of fungal spores were measured from January to December 2016 by Hirst type volumetric aerospore trap (Burkard model). The sampler was placed on the roof of the Department of Botany, Comenius University in Bratislava, in northwest part of the city at the height of 10 m above ground level.
  24. Jana Scevkova and Jozef Kovac, 2019 Aerobiologia Fungal spores were identified and quantified in the air of Bratislava during the 1-year period (2016) using a Burkard 7-day volumetric aerospore trap. The total annual spore concentration recorded during this period was 836,418 spores/m3, belonging to 53 fungal spore types. The fungal taxa contributing the highest concentration of spores were Cladosporium (71.88% of the total), Coprinus (8.84%), Leptosphaeria (3.88%), Ganoderma (3.43%) and Alternaria (2.79%). Fungal spores peaked during summer and autumn months (June–October) and declined from November to March. The maximum monthly total spore concentration (153,342 spores/m3) was recorded in July, while the minimum (1381 spores/m3) in January. Spore concentrations of most analysed airborne fungal taxa were positively associated with air temperature and/or negatively associated with relative air humidity either throughout the year or only in summer. Cladosporium spore concentration was positively related with the wind speed, whereas the association between Ganoderma spore concentration and wind speed was negative. Spores of Leptosphaeria showed significant positive association with relative air humidity and significant negative association with sunshine duration in summer. Knowledge of seasonal patterns of the type and number of spores in the air
  25. Airborne spores of Cladosporium spp. were sampled by the Asthma and Allergy Association on the roof of Regionshospitalet, 21 m above sea level in Viborg (56270N 9240E) during 115 days, 31 May–22 September 2015, on the 48 9 14 mm slides using a Hirst-type spore trap
  26. Yulia Olsen et al 2019 Aerobiologia (2019) 35:373–378 Daily average concentrations of Cladosporium spp. at Viborg station during 31 May- 22 September 2015 (n = 115), mean daily average concentration over the period: 1897 spores m3. Red vertical lines confine the longest period of high concentrations. Peak daily average concentration occurred on 16 August (13,553 Spores m3) The diurnal cycle of Cladosporium spores (Fig. 3) on the days with daily average concentrations above 3000 Spores m-3 had a maximum between 08:00 and 10:00. However, after excluding the high concentrations on 14 August and 16 August, the diurnal distribution reflected elevated concentrations between 06:00 and 20:00 (Fig. 3).
  27. Elevated day time concentrations in Viborg on the days with daily average concentrations exceeding the threshold also indicate the local character of the sources. Eighteen (out of 21) days with daily average concentration above 3000 Spores m-3 occurred in August, contributing up to 80% of August SIn. The peak daily average and 3-h concentrations were measured on 16 August. During the 11 days, 14–24 August, the air masses were arriving from the East and South East, i.e. originating in the areas in Poland, the Baltic countries, and north-west Russia, passing over the Baltic sea and southern Sweden (Fig. 2b). Conversely, on 13 August and on 25 August, the wind directions were distinctively different with the air masses arriving from the North–West and South–West (Fig. 2b). In the course of those 11 days, the corresponding daily average concentrations at the Copenhagen station were lower than at the Viborg station.
  28. High airborne Alternaria spore concentrations measured in eastern Denmark have been associated with local agricultural sources. However, the density of agricultural areas is highest in western Denmark. This is the first report of airborne Alternaria spore concentrations obtained with Burkard volumetric spore sampler in western Denmark, Viborg. We compared the concentrations of airborne Alternaria spores and the patterns of air mass transport using HYSPLIT model between Copenhagen and Viborg for the seasons 2012–2015, with the main focus on the days with daily average Alternaria spore concentrations C 100 s m-3 (high concentration days). local sources cause the main load of airborne Alternaria spore concentrations in Denmark; We found increased shares of trajectories coming from SouthEast on the high concentration days and increased shares of trajectories coming from the West and North-West on the days with concentrations below 100 s m-3 for both stations. July and August had the highest spore integrals matching the periods of grain harvesting in Denmark.
  29. Muga silkworm is endemic to North-East India. The quality of primary host plant, i.e. Som. (Persea bombycina Kost.), greatly affects the quality of cocoon and silk production. Som is susceptible to different foliar diseases caused by fungi, which can reduce the yield of leaf from 13.8 to 41.6% annually Air samples were collected using settle plate method described by Aneja (2012). Petri plates containing potato dextrose agar (PDA), Martins rose bengal agar (MRBA) and Czapek’s Dox agar medium supplemented with chloramphenicol (250 mg/ml) were used for collecting the air samples. The rhizosphere, air and phylloplane were dominated by Rhizopus stolonifera. Pestalotiopsis disseminata is one of the major pathogens of Som and was found highest in aerosphere followed by phyllosphere.
  30. Ray et al 2019 Aerobiologia
  31. In this study, spore trap monitoring was applied to provide a proof of concept for the use of qPCR to detect Phytophthora in aerial samples and provide valuable information for epidemiological studies in nurseries. Two qPCR TaqMan assays were developed to detect pathogen DNA: the first used a generic probe to detect Phytophthora spp., and the second was based on a specific probe for detecting P. ramorum and P. lateralis. All samples tested positive for the genus Phytophthora, although P. ramorum and P. lateralis were not detected. In late spring and in autumn, two main peaks of Phytophthora sporulation were observed. Peaks were preceded by rainfall, high relative humidity, and mild temperature. From midMay to the end of August, Phytophthora DNA detected in the air increased with relative humidity, while it decreased with increasing mean temperature. There was also a positive correlation between Phytophthora DNA detected and rainfall in the same period. No significant correlations between Phytophthora DNA and temperature or rainfall were found from the end of August to December. Our results are in agreement with those obtained with classical diagnostic methods based on microscopy, but the approach used here enabled rapid detection and relative quantification of the target organisms, thus assisting in the implementation of disease management strategies
  32. Migliorini et al 2019 Aerobiologia (2019) 35:201–214