sunlight does not penetrate beyond the top few centimeters of the soil surface
phototropic microorganisms are therefore limited to the top few centimeters of soil
e.g. algae, lichen
Biotic stresses are caused by living organisms such as pathogens, insects, weeds, animals, birds, rodents, nematodes, fungi, bacteria, viruses, protozoa, parasites, etc.
algae
grows on stagnant water
2. soil moisture
availability of water is critical for microbial activity
optimal microbial activity occurs at -0.1 atm, which is the transition between capillary water and free water
fungi are most desiccation resistant, followed by actinomycetes and finally the bacteria
3. soil temperature
psychrophilic (prefer <20C)
mesophilic (prefer 20C - 45C)
thermophilic (45C-90C)
hyperthermophilic (>90C)
most soil organisms are mesophilic because of the buffering effect of soil on soil temperature, particularly at depths beneath the soil surface
4. soilpH
undisturbed soils usually have soil pH values within the range of 6-8, and most soil organisms have pHoptima within this range
acidithiobacillusthiooxidans, an organism that oxidizes to sulfur to sulfuric acid has a pH optimum of 2-3
autotrophic microorganism
gumagawa ng sariling environment/nutrients to proliferate
5. soiltexture
all soils contain microbial communities regardless of the soil texture
soils with mixture of sand, silt, and clay particles offer a more favorable habitat for organisms because they hold more nutrients, water, and air flow than do pure sands or clays
6. soilnutrients
carbon and nitrogen are generally the most important limiting nutrients that are found in soils
major exception to this is the plant
7. redox potential
measurement of the tendency of an environment to oxidize or reduce substrates
source of natural product and antibiotics e.g. steptomycin
produce geosmin, the compound which gives soil and water a characteristic earthy odor
capable of degradation of complex organic molecules
capable of biological nitrogen fixation with species of the non-legume-associated frankia
3. archaea
acrhaea contribute to multiple soil processes including the biogeochemical cycling of C, N and S
ammonia oxidizing archaeans (AOA) in general, AOA appear to be more important to ammonia oxidation in environments that have lower levels of N such as natural ecosystems
4. Fungi
despite their lower numbers compared with bacteria, fungi usually contribute to a higher proportion of the total soil microbial biomass
beneficial fungi
penicillium and aspergillus - involved in nutrient recycling; important in the development of the soil structure because they physically entrap soil particles with fungal hyphae
phanerochaete chrysosporium - can also degrade a variety of pollutant molecules
5. algae
are typically phototropic and thus would be expected to survive and metabolize in the presence of light and CO2
algal metabolism is critical soil formation in two ways:
detrimental algae
chlamydomonas- most common algae found in acidic soils
diatoms - found primarily in neutral and alkaline soil
in temperate soils, the relative abundance of the major algal group follows the order of green algae>diatoms> red algae
protozoa
there are three major categories of protozoa: the flagellates, the amoebae and the ciliates
there is an evidence that they may also be involved to some extent, int the decomposition of soil organic matter
protozoan population of a soil is often correlated with the bacterial population which is the major food source present
II. aeromicrobiology
atmosphere is an inhospitable climate for microorganisms mainly because of desiccation stress
limited time frame in which microbes can remain biologically active
spore-forming bacteria, molds, fungi, and cyst-forming protozoa have specific mechanisms that protect them from harsh environment
relative humidity
relative water content of the air
in general, most G- bacteria associated with aerosols tend to survive for longer periods at low to mid relative levels of humidities, with enhanced decay at the relative humidities above 80%
opposite tends to be true for gram-positive bacteria, which tend to remain viable longer in association with high relative humidities
2. temperature
high temperatures promote inactivation, mainly associated with desiccation and protein denature, and lower temperatures promote longer survival times
when temperatures approachfreezing, however, some microorganism lose viability because of the formation of ice crystals on their surface
radiation
dienococcuss radiodurans - soil bacterium that is considered the most highly radiation-resistant organism, has the ability to enzymatically repair damage to chromosomal DNA
4. oxygen, open air factors (oafs) and ions
oxygen toxicity is important in the inactivation of microorganisms when O2 is converted to more reactive forms (Superoxide radicals, hydrogen peroxide, and hydroxide radicals)
OAF is term coined to describe an environmental effect that cannot be replicated in laboratory experimental setthings
aerosolization of indigenous soil pathogens
spores can potentially be aerosolized and cause human infections
important fungal geo-indigenous pathoens include coccidioides immitis and histoplasma capsulatum
bacillus anthracis is a bacterial geo-indigenous pathogen that causes lethal disease in humans via pulmonary, gastrointestinal or cutaneous modes of infections
microbiology in the clouds
some microorganisms, called ice nucelators, efficiently catalyze ice formation and may play a role in the formation and precipitation in the clouds
agriculture
contamination of crops and animals via bioaerosols has a large worldwide economic impact
rice and wheat are two of the major staple crops that are paramount to world food security
agriculture
airborne spread of pathogenic microorganisms is also highly important in the animal husbandry industry
occurence of foot-and-mouth disease is an example of bioaerosols
important airborne toxins
clostridium botulinum (botulinum A toxin) - potential biological warfare agent; lethal dose for botulinum toxin by inhalation is 0.3 microg, with death occurring 12 hours after exposure
Environmental microbiology
study of microbes within all habitats and their detrimental and beneficial impacts on health and welfare
water treatment
water
waterborne disease reduction
norovirus and legionella
food consumption
food
foodborne disease
clostridium botulinum, E. coli O157:H7
indoor activities
fomites
respiratory disease
rhinovirus
breathing
air
legionellosis
legionella pneumophila
enhanced microbial antibiotic resistance
hospitals
antibiotic-resistant microbial infections
methicillin-resistant staphylococcus aureus
nutrient cycling
soil
maintenance of biogeochemical cycling
soil heterotrophic bacteria
rhizosphere/plant interactions
soil
enhanced plant growth
rhizobia mycorrhizal fungi
bioremediation
soil
degradation of toxic organics
pseudomonas spp.
freshwater type
microorganisms thrive more here than in the deep sea due to highsalinity content in the sea, very richsoil and as well as other microorganisms used as nutrients
emerging environmentally transmitted microbial pathogens and biological agents
studied to reduce their detrimentaleffects on people
physical and chemical components/characteristics are also studied to know how to eradicatethem