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Markéta Marečková e-mail: sagova @vurv.cz. Microorganisms in soil. S oil structure and its Soil ecosystem Trophic relationships Key processes Estimation, models and evaluation Soil is the most complex environment. E c osyst e m. Abiotic. Biotic. Func tion. Stru c tur e. - PowerPoint PPT Presentation
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Markéta Marečková
e-mail: [email protected]
Microorganisms in soil
• Soil structure and its • Soil ecosystem • Trophic relationships • Key processes• Estimation, models and evaluation
Soil is the most complex environment
Ecosystem
BioticAbiotic
Structure Function
Soil ecosystem
dominated by
heterotropic organisms
•bedrock•darkness
porous mixtureof solids, liquids and gases
•plant nutrition•decomposition of
OM
quantity & quality of C
predation
Methods of study
Solids
Porous material of solids, liquids and gasesBedrock : e.g. limestone,dolomite (neutral to alkaline), silicate (acidic)
Determines the basic soil pH.Humus: Humic acids are aromatic and aliphatic remains of lignin, aminoacids
and sugars. Humus is a product of decomposition, microbial or chemical. Humus is usually acid and is negatively charged.
Clay particles: large surface, together with humus influence ion exchange. Negatively charged.
\ Adsorbtion afinity: Al 3+ > Ca 2+ = Mg 2+ > K+ = NH3+ >Na+
Abiotic factors
Maier et al., 2000
Abiotic soil components
mineral particles
mineralparticles
mineralparticles pores pores pores
organic matter organic matter
sand silt gravel
Velikost porů, odpovídající procesy a organismy.
Na velikostní úrovni jílových částic (μm) se vyskytují pouze bakterie a houbová vlákna. Na úrovni prachu (0.063 mm) a písku (2 mm) se vyskytují kořenové vlášení, kořeny, prvoci, hlístice.
Struktura půdy
oživení porů
Meier et al., 2002
Water, liquids
Water is the main limiting factor in soilwater content is correlated to organic matter content
Pore size:
macropores > 0.08 mm, gravitation water, plants mesopores 0.08 -0.03 mm,capillary water micropores 0.03-0.005 mm,inside agregates, bacteriaultramicropores 0.005-0.0001mm,inside clay particles cryptopores < 0.0001mm, too small even for macromolecules
Abiotic factors
Maier et al., 2000
Water potential: force necessary for movement of a certain amount of water under a given pressure and material
Adhesion (binding force to solid surfaces – matrix potential, Ψm)Binding to ions (osmotic potencial, ΨS)Gravitation force (gravitation potencial, Ψg)
Reaches negative values because it is compared to free water. Given in pressure units.
Free and bound waterAbiotic soil components
surface forces, Ψm, - 31 až – 10000 atm
capillary forces, ΨS -0.1 až -30 atm
gravitation forces, Ψg 0 až -0.5 atm
Maier et al., 2000
Soil structure
examples of characteristics
pH vodivost Ca Mg Al Fe humus % organic
μS mg/kg mg/kg mg/kg mg/kg % %
Alpilles 7.54 256 5900 184 3.0 1.0 2.3 16.1
Bozi Dar 3.27 47 1290 106 5.3 1.4 40.6 95.7
Devin 7.87 200 6210 163 3.0 1.0 1.4 12.0
Kotyz 7.52 310 7600 191 3.0 1.2 3.7 26.6
Meluzina 5.03 86 2700 137 10.4 2.5 18.5 7.6
Nechranice 6.08 64 3470 618 3.0 1.0 7.2 11.6
Oblik 7.9 200 6090 307 3.0 1.0 0.5 21.5
Podyji 5.55 75 2010 404 4.1 2.9 3.2 10.2
Rynholec 6.31 53 2840 83 6.5 1.0 0.1 7.2
Saline Giraud 8.12 21350 3150 67 3.0 1.0 0.0 3.3
slanisko Nesyt 7.97 537 3390 1250 3.0 1.0 0.5 6.6
Srbsko 7.65 141 4740 141 3.0 1.0 0.5 8.2
Slepici vrch 4.57 24 100 29 3.0 1.0 0.7 1.5
Trebon 4.01 80 1160 289 3.4 4.4 3.8 9.1
Habitat of microorganisms: variable in space and time
stratified by physical and chemical forces and important
nutrients– C, organické látky, 02, N, P, S microhabitat
• soil particles• rhizosphere• air bubbles • sufaces of
organisms
Soil structure and life niches
life formactive cells, spores, fillaments, collonies, biofilms
(obydlí)
Viruses,phages
Living forms
Diversity of viruses in various soilsLiving forms
•Comparison of agricultural, forest and alpine soils.
•Highest diversity (Simpson index) was found in forest soils
•The highest percentage of viruses were bacteriophages
Proteobacteria: pseudomonads, myxobacteria, rhizobia AcidobacteriaActinobacteria: streptomycets, corynebacteriaVerrucomicrobiaFirmicutes: bacilli, clostridia, laktobacilliPlanctomycetes
Streptomyces
Chondromyces
Myxococcus Bacillus
Living forms
Bacteria
109 cells and thousands of species per gram soil. Culivativable part is only from tenths to tens of percent Aerobic dominate the anaerobic in regular soil several times. Spatial variability is enourmous.
Living forms
Molds
Aspergillus
Algae
Cryptomonas
Blue greens
Nostoc
Blue green algae and algae live only in top several cm of soil. They often make a crust or a biofilm and they are adapted to very dry environment even deserts.
Algae and Fungi
Living forms
AmoebasAcanthamoeba
Paranema
Heterotrophic flagellates
Protozoa
Living forms
Euplotes, Stylonychia
Cilliates
Nemathods
Springtails
Orchesella
Mites
Living forms
Mammals
Microtus arvalis
Oligochaetes
Lumbricullus variegatus
Živé složky půdy
Soil horizonsstructure
In soil, organic and anorganic material is layered to soil horizons. They are created byplant litter and water from rain and groundwater.
Abundance and biomass of soil populations
Scale analysis (A) Distribution of soil patches colonized by bacteria in a two-dimensional grid with an indication of the four sizes of microsamplesused. (B) Same distribution after the test for the presence of bacteria. The black and white elementary units represent positive and negative results, respectively. (C) Corresponding curves obtained after sampling, showing the percentages of positive microsamples as a function of the four microsample sizes. Different types of distribution of bacteria are shown in rows a, b, and c.
Grundmann et al.2004
Distribution by source
Resources occur in soil mostly at aggregates of different sizes. E.g. in upper soil there are larger pieces of OM than in the lower soil. Bacteria aggregate as site of sources.
structure
Example: The highest number of bacteria phylotypes occurred in the clay fraction. Protection from predation. Fertilization does not change this relationship. Also highest diversity in the smaller pores – association with particles is stronger than the nutrient exchange
Sessitch et al.2001
T-RFLP profiles in three fractions of differently treated soils
Inhabiting pore according to its size structurete
rmin
al f
rag
men
t le
ng
ht
Organic matter main factor influencing productivity of soil environment. ovlivňuje:•plant nutrition •community composition•water content•agregate stability•erosion control
The main source of OM is the higher plants. One part of plants is quickly mineralized to CO2, phosphates, sulfates, nitrates etc. and used by other organisms. the other part is decomposed only partly and makes up humus. The ration of both components differes between sites, the most important factors being pH and moisture. Clay component and humus are the source of soil fertility. Both processes mineralization and humification are driven by bacteria and fungi. Bacteria and fungi add to humus also by their bodies which make a biomass of 40-200 g m-2.
„Hot spots“ sites of highest mircorbial activity. 90% of activity goes on in 10% of soil volume. E.g. rhizosphere and burries of animals
structure Organic matter sources
Relationships between contents of C, N, bacteria and fungi in soil at 5 diffrent sites (beech, pine, meadow, organic field, convention field at 5 and 25 oC.
Sites differ by:fungi abundance but not that of bacteriaFungi quantity correlated with C and negatively with N. Bacteria correlate with temperature.
DOC dissolved organic carbon,DON dissolved organic nitrogen
Example
bacteria fungi
NH4+ NO3
-
DOC DON
Nutritionstructure
All processes are faster at higher temperature. Respiration is similar at all sites. Mineralization N, imobilization C and nitrification are the highest in a meadow and smalest in a forest
Example
Rate of soil processes function
mineralization
imobilization N nitrification
Soil bacteria according to the K-r selection
K organisms: slow metabolism, consumption of nutrients from small amoutns of poorly available sources, large genomes, filamentous forms, adaptation to harsh conditions (cold, deserts), stay at sites
r organisms: fast growing, fast reactions to a new source, consumption of available sources at good living conditions, coccal forms, fast growth, tolerate stress
Streptomyces, Micromonospora, Streptosporangium (podřády), myxobakterie
Burkholderia, Xanthomonas, Agrobacterium, entherobakterie
Nutrient consumptionstructure
C content in soil by source
microbial C total Cug/g %
arable land 70 - 720 1.0 - 3.8250 - 1080 3.0 - 6.0420 - 980 2.5 - 5.5
meadow 2670 2.9470 21120 1.9
forest 420 - 1770 0.9 - 2.6800 - 1670 1.2 - 6.0
1670 2.1subtropical forest 330 - 1090 0.9 - 1.8
200 - 790 0.7 - 1.3alpine meadow 1000 - 2750 1.7 - 2.8
structure
Examples of organic C content and microbial C content. In meadow ecosystems microbial content is higher.
•Soil trophic pyramid is not well known•Dominating process is decompostion Predation influences dynamics of the energy exchange processes •The best methods to describe are isotope probing •Limitation by C except in the rhizosphere (and by water as at all terrestrial ecosystems)
Trophic pyramidprocesses
secundary decomposers
PP
primary decomposers
predators I
predators II
nutrition
litter
shredded litter,microorganisms
decomposers, PP
predators I
chemolithotrophie
Trophic relationships in soil environment
natural meadow ecosystem
wheat monoculture
Agroecosystem is simplified,no mycorhiza, N2 fixation, limited nematods and increasing effect of cilliates
Trophic processesprocesses
Plant community
exudates litter
bacteria
protists
Carbon and other nutrients
ener
get
ic c
anal
bac
teri
al
fun
gal
Basic flows of energy and nutrients in soil ecosystems
Two basic types of food webs:
• based on exudates• based on litter
Food web in rhizosphere is fast. Production and biomass are several times higher than in the litter web. Interactions between plants, bacteria and protozoa are called a microbial loop. In this community, predators effectively control bacterial growth but the effect of secondary predators is low. Nutrients cycle locally and are not spread around. Plants give up to 40 % of assimilated carbon to rhizosphere microorganisms.
Bacterial food web is more typical for high pH , higher N, and lower soil moisture. Typical of fast overturn. Predators are protozoa and nematods. It is controlled by nutrients (bottom up).Fungal – oposite, controlled by predation(top down)
procesess Trophic relationships
Example:
A field with convention farming (full) and a field with organic farming (dashed) were followedduring a year.Biomass of bacteria and fungi correlated with temperature.Maximum of bacterial biomasswas reached in relationship to soil moisture. This demonstrates limitation with water in a soil community. Bacterivorous nematods were highest in winter, which shows high tolerance to T and avoiding of predators.
Trophic relationships
Bloem et al., 1994
predation predationpredation
grazingsubstrate processing
pore formationlitter fragmentation
bioturbation
Energy flow
Habitat formation
Function of organisms by body size organismů
Trophic interactions are fast while habitat formation is a long term process
Primary production
ChemolithotrophyFixace CO2
Energie: oxidace železa, amonných solí, sirníků, síry, kovů, dusitanů
Bernhart et al., 2007Jourdan et al., 2005
function
Zastoupení autotrophů podle qPCR Zastoupení autotrofů v průběhu tří let
Predation
soil predators: bakterivorous: protozoa, nematods, and bacterial predators phtophagous: mites, springtails
the main cause of bacterial mortality in soil
•no cyclic relationships•high redundancy causes high stability,•many prey species•fast nutrient cycle, mineralization
Predation in soil: consumption of heterotrophic organisms with detritus
Maier et al., 2000
Escape from predation:attachement to soil, small pores, pathogenicity, antibiosis, filaments, biofilm.
Protection from digestion: release of toxines, intracellular parazitism
Function
predation
Salinas et al., 2007
Movement of protozoa in soil: flagellates 2-4 cm, amoebas 3-6 cm, cilliates 1-2 cm
Consumption rate of bactria by prozoa. 5000 bacterial cells per min 800 kg of bacteria per ha per year
Predation
Ekelund et al., 2001
funkce
Correlation between the number of protozoaand bacteria at different sites in Danmark.The regular relationship on the figure demonstrates the possibility of bacteria control by protozoa at those sites.
Example:
Pisum sativum - Streptomyces lydicus – Rhizobium sp.
Streptomyces lydicus collonizes rhizosphere:
increases the number of nodules i.e. supports infections by nitrogen fixing Rhizobium sp.,increases the nodule surface, supports growth of rhizobia mostly by supplying Fe and other nutrients
Fe, other nutrients? Pisum sativum
S. lydicus Rhizobium sp.
nutrientsexudates, O2?
N source
Fe, other nutrients
N source ?
Tokala et al., Appl. Environ. Microbiol. 68, 2161-2171, 2002.
Mutualisms of three species
Tokala et al., Appl. Environ. Microbiol. 68, 2161-2171, 2002.
Nodes with a streptomycetes Nodes without streptomycetes
Nodes with streptomycetes have a large surface, which enables better nutrient utilization
Microorgansims are limited by specific requirements to moisture and temperature.They have limited or no capability to move. Microorganisms are dependent on dispersion by other organisms.
Everything is everywhere but the environment selects.
Limitation
Adaptation
Microorganisms are adapted to utilization of any organic substrate. Dispose of often large genomes, which contains pathways expresed under different conditions.Microorganisms grow quickly in the lab but very slowly in nature, one generationbetween 6 and 18 months, they are waiting for the ideal conditions to come. V laboratoři rostou velmi rychle, ale v přírodě je obrat mezi 6 a 18 měsíci.
Limitations of microbial processes function
Limitations of microbial processesfunction
Horizontal relationships – competition, comensalism, antibiosisNot well studies. Comensalisms occurs in C utilization. Cooperation in utilization of recalcitrant forms or in anaerobic conditions.
Example: „Disease supressive soils“
Use of antibiosis in agriculture. Disease suppressive soils are known for suppression of a specific pathogen, fungi, bacteria or nemathods. The most well known is disease suppression of take all wheat disease cause by mold Gauemanomyces graminis by antibiotics produced by pseudomonads.
• 11%
• 20%
• Inoculated• Not inoculated
• Inoculated• Not inoculated
• Suppressive• Conducive
Disease suppressive soilsexample Tievaliopsis basicola
microarray for identification of 1500 bacterial genera
differences in composition of communities in disease suppressive and conducive soils
conducive suppressive
Kyselkova et al., ISME 2009
Biodegradation
Microorganisms oxidating carbohydrates:bacteria, molds, yeasts, bluegreen algae, algae
Only aerobic processdependence on temperature, pH and sources of anorganic nutrients
Xenobiotics: (pesticids, polychlorinated bifenyls, explosives, tints, chlorinated solvents etc.)some are structurally related to natural compounds – slow degradation by existing enzymes
degradation of completely foreign compounds takes much longer, degradation pathways must be developed
Genomes of microorganisms – what is necessary
Glass et al.: Essential genes of a minimal bacterium
PNAS 2006;103;425-430
„minimal bacteria“ - Mycoplasma genitalium482 protein coding genes, since 2002 Nanoarchaeum equitans, 491 kb)
→ 382 from the total of 482 genes of M.genitalium are essential
Genomes of microorganisms – what is necessary
Haggblom et al.
Degradation of MTBE, methyl tert-butyl ether
One bacteria in 109 which can degrade it. Took 5 years to find it using enrichment cultivation.
Biodegradation of oil
Bacteria aggregate in high numbers at the edge between water and organic phase, or are present directly inside the organic phase
Biodegradation of oil
Functional metagenomic profiling of nine biomes
Nature 452, April 200815 milion od sequences were evaluateddivided by metabolisms and functions
9 bioms: underground, saline, sea, coral, freshwater, fish, terrestrial animals, microbial, and moskyto
Sekvence divided also by the originto viral and microbial
Separation of sequences by canonic ordination analysis
Microbial and viral set differes significantly
Processes dominating for microorganisms:cell wall building, sulfur, signalization, movement, respiration, building of proteins
Viral processes:membrane transport, potassium, phosphorus, cell division, DNA, virulence, sekundary metabolites, fatty acids
mikrobiální
virový
Climatic changes in relationship to soil microorganisms