10 soil microbiology
TRANSCRIPT
Soil Microbiology
Soil
Soils correspond to the surface layer of the Soils correspond to the surface layer of the
Earth's crust (lithosphere: litho = rock). Earth's crust (lithosphere: litho = rock).
They develop as a result of the weathering of They develop as a result of the weathering of
geological rock formations. geological rock formations.
Soil
Soil consist of Soil consist of
mineral particlesmineral particles (from the eroded rocks) and (from the eroded rocks) and
organic mattersorganic matters (from the remains of plants, (from the remains of plants, animals, and microorganisms). animals, and microorganisms).
Mineral and organic particles are intimately Mineral and organic particles are intimately mixed in soil, forming various types of soil mixed in soil, forming various types of soil aggregates.aggregates.
Soil microbiology
They are found in association with air (i.e. the soil They are found in association with air (i.e. the soil
atmosphere) and an aqueous phase (i.e. the soil atmosphere) and an aqueous phase (i.e. the soil
solution) in the pores existing between particles solution) in the pores existing between particles
and/or aggregates. and/or aggregates.
Air and water = limiting factorAir and water = limiting factor
Limit number and type of microorganismsLimit number and type of microorganisms
Oxygen level in sandy soil particle.O2
Microorganisms:The soil represents a favorable habitat for microorganisms and is inhabited by a wide range of microorganisms, including bacteria, fungi, algae, viruses and protozoa.
Microorganisms are found in large numbers in soil - usually between one and ten million microorganisms are present per gram of soil.
Microorganisms:
Bacteria and fungi being the most prevalent.
However, the availability of nutrients is often
limiting for microbial growth in soil and most soil
microorganisms may not be physiologically active
in the soil at a given time.
Microorganisms and their significance:
Almost every chemical transformation taking Almost every chemical transformation taking place in soil involves active contributions from soil place in soil involves active contributions from soil microorganisms. microorganisms.
Active role in soil fertility as a result of their Active role in soil fertility as a result of their involvement in the cycle of nutrients like carbon involvement in the cycle of nutrients like carbon and nitrogen, which are required for plant growth. and nitrogen, which are required for plant growth.
Microorganisms and their significance:
Soil microorganisms are responsible for the Soil microorganisms are responsible for the
decomposition of the organic matter entering the soil decomposition of the organic matter entering the soil
and therefore in the recycling of nutrients in soil. and therefore in the recycling of nutrients in soil.
Certain soil microorganisms such as mycorrhizal fungi Certain soil microorganisms such as mycorrhizal fungi
can also increase the availability of mineral nutrients can also increase the availability of mineral nutrients
(e.g. phosphorus) to plants. (e.g. phosphorus) to plants.
1. CO2 fixation by photoautotrophs and chemoautotrophs.
2. Methanogenesis from inorganic (CO2+H2) or organic matter, involves
various archaea methanogens (Methanobacterium, others). Global CH4
production ~1011 kg / yr (~85% biogenic)
Microorganisms in C cycle:
Carbon fixerCarbon fixer
PhotoautotrophsPhotoautotrophs
Anaerobic Anaerobic –– ChromatiumChromatium (purple, sulfur bacteria)(purple, sulfur bacteria)
Aerobic Aerobic –– cyanobacteriacyanobacteria
Chemoautotrophs Chemoautotrophs -- anaerobicanaerobic
Methanotrophs: Methanotrophs: MethylomonasMethylomonas
Sulfur oxidizer:Sulfur oxidizer: ThiobacillusThiobacillus
Microorganisms in C cycle:
Methanogenesis Methanogenesis –– anaerobic degradation of anaerobic degradation of carbon: strictly by microbes.carbon: strictly by microbes.
Anaerobic respiration involves the complete oxidation of Anaerobic respiration involves the complete oxidation of organic substancesorganic substances
(CH(CH22O)O)nn + X+ Xoxox ----------> CO> CO22 + X+ Xredred
XX = electron acceptor= electron acceptor
(NO(NO33--, SO, SO44
22--, S, S00, Fe, Fe3+3+))
Methanobacterium
Microorganisms in C cycle:Anaerobic decomposition of organic substances to COAnaerobic decomposition of organic substances to CO22
and CHand CH44 involving many different reactions and species of involving many different reactions and species of microorganisms. This is also called interspecies hydrogen microorganisms. This is also called interspecies hydrogen transfer [the gut,sediments, soils, and the rumen].transfer [the gut,sediments, soils, and the rumen].
a. Complex polymers a. Complex polymers →→monomersmonomers
b. The monomeric subunits b. The monomeric subunits →→ organic acidsorganic acids
c. Fermentations c. Fermentations →→ acetate, COacetate, CO22, and H, and H22
d. Methanogens produce methane (i.e. CHd. Methanogens produce methane (i.e. CH44))
1. Nitrogen fixation
2. NH3 assimilation
3. Ammonification
4. Nitrosification
5. Nitrification
6. Nitrate assimilation
7. Dissimilatory nitrate reduction
8. Denitrification
• Nitrogen fixation N2 → NH3 (aerobic)
• free-living: Azotobacter, cyanobacteria;
• symbiotic: Rhizobium, Frankia
• (anaerobic): Clostridium perfringens, purple & green sulfur phototrophs.
2. NH3 assimilation (aerobic & anaerobic)
3. Ammonification (organic N→ NH3)
4. Nitrosification (aerobic), Nitrosomonas
5. Nitrification (aerobic), Nitrobacter
6. Nitrate assimilation (NO3-→ NH3 → amino acids)
7. Dissimilatory nitrate reduction (NO3 -→ NO2
-)
8. Denitrification (NO3- → N2) Bacillus, Pseudomonas,
Biogeochemical Sulfur Cycle:
1. Sulfur oxidation (S°→ SO3-2→ SO4
-2): (aerobic) many
chemolithotrophs; (anaerobic) purple & green
photoautotrophs
2. Assimilatory sulfate reduction (SO4-2→ organic S)
3. Desulfurylation (organic S decomposition → H2S)
4. H2S oxidation (H2S → S°)
Aerobic: Thiobacillus, Beggiotoa (chemolithotrophs).
Anaerobic: Chlorobium, Chromatium
Biogeochemical Sulfur Cycle:5. Dissimilatory sulfate and sulfite reduction (solid purple
arrows) SO4
-2 or SO3-2 → H2S:
Desulfovibrio and related organisms6. Elemental sulfur reduction (S°→ H2S) Desulfuromonas,
thermophilic archaea, cyanobacteria in hypersaline sediments.
Microorganisms and their significance:
Other soil microorganisms can increase the Other soil microorganisms can increase the
amount of nutrients present in the soil. amount of nutrients present in the soil.
The microorganisms, which improve the fertility The microorganisms, which improve the fertility
status of the soil and contribute to plant growth, status of the soil and contribute to plant growth,
have been termed 'have been termed 'biofertilizersbiofertilizers‘‘..
Microorganisms and their significance:
Similarly, other soil microorganisms have been Similarly, other soil microorganisms have been
found to produce compounds (such as vitamins found to produce compounds (such as vitamins
and plant hormones) that can improve plant and plant hormones) that can improve plant
health and contribute to higher crop yield. health and contribute to higher crop yield.
These microorganisms (called 'phytostimulators') These microorganisms (called 'phytostimulators')
are currently studied for possible use as microbial are currently studied for possible use as microbial
inoculants to improve crop yield. inoculants to improve crop yield.
Microorganisms and their significance:
Some soil microorganisms are pathogenic to Some soil microorganisms are pathogenic to
plants. Large numbers are routinely found in the plants. Large numbers are routinely found in the
soil and many of them can infect the plant through soil and many of them can infect the plant through
the roots.the roots.
Microorganisms and their significance:
Some native microorganisms present in the soil are Some native microorganisms present in the soil are
antagonistic to the pathogens and can prevent the antagonistic to the pathogens and can prevent the
infection of crop plants. infection of crop plants.
Competition for nutrients and/or production of inhibitory Competition for nutrients and/or production of inhibitory
compounds such as secondary metabolites (antimicrobial compounds such as secondary metabolites (antimicrobial
metabolites and antibiotics) and extracellular enzymes. metabolites and antibiotics) and extracellular enzymes.
Microorganisms and their significance:
Other soil microorganisms produce compounds Other soil microorganisms produce compounds that stimulate the natural defense mechanisms of that stimulate the natural defense mechanisms of the plant and improve its resistance to pathogens. the plant and improve its resistance to pathogens.
The last two groups have been termed The last two groups have been termed 'biopesticides' (= biological control).'biopesticides' (= biological control).
Major groups of soil microorganisms :Bacteria:
Numerically abundant (109 cells/g soil) but most
non-culturable
Along with fungi, most important decomposers of
organic matter
Major groups of soil microorganisms :Bacteria:
Specialized groups participate in all biogeochemical cycles
Their extracellular polymers help bind soil particles into aggregates
Some form beneficial or pathogenic interactions with plants
Important group of bacteria
Actinomycetes sp. Rhizobium sp.
Pseudomonas aeroginosa Bacillus sp.
Major groups of soil microorganisms :Nitrogen fixing organisms: bacteria
Symbiotic with plants Free living
FrankiaAzospirillum
RhizobiumClostridium (some)Desulfovibrio
Purple sulphur bacteria*Purple non-sulphur bacteria*
Green sulphur bacteria*
AzotobacterBeijerinckia
Klebsiella (some)Cyanobacteria
(some)*
Other plantsLegumesAnaerobicAerobic
Examples of nitrogen-fixing bacteria (* denotes a photosynthetic bacterium)
Major groups of soil microorganisms :
Actinomycetes:specialized filamentous prokaryotesparticipate in decomposition of complex organic compoundsproduce many 2nd metabolites, e.g., antibiotics, geosmins (earth odor) that give soil its characteristic distinctive aroma
Major groups of soil microorganisms :
Fungi:the major component of microbial biomass in soilsmajor participants in decomposition of organic matterhyphal growth helps bind soil particles into stable aggregates
Ectomycorrhizae - sheath
Major groups of soil microorganisms :
Fungi:Some associate with plant roots: major plant pathogens,
Beneficial symbionts
increase nutrient uptake
and decrease disease incidence
Major groups of soil microorganisms :Protozoa:
major predators of soil bacteria,
grazing activities accelerate decomposition of organic matter in soil
Very abundant in well drained surface soils.
There are some 250 different species in soils
Major groups of soil microorganisms :
Cyanobacteria and algae (green algae, diatoms):
Photoautotrophs, form surface algal crusts important in
H2O retention
Some cyanobacteria carry out free-living and symbiotic
N2-fixation
Major groups of soil microorganisms :Viruses:
Numerically abundant, ecology not well defined
Both lytic and lysogenic bacteriophage (latter very common)
Persistance and migration of human enteroviruses pose serious health issues with land disposal of sewage and fecal wastes
Winogradsky column
Metagenomics method
Using 5S and 16S rRNA gene sequence analysis.Using 5S and 16S rRNA gene sequence analysis.
Can use to study uncultivated microbial majorityCan use to study uncultivated microbial majority
Main reason Main reason ––
cannot culture cannot culture –– nutrition and physiological nutrition and physiological
Nature of culture does not reflect natural behaviorNature of culture does not reflect natural behavior