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At the first lecture it was clear that many of you understood little of what I said.
Two problems are :
(i) English
(ii) New words, new concepts, that make you stumble ...
But other problems could be :
(i) If you are a first year student then you are not sure yet of what is expected of you as a student.
(ii) You have prior expectations of what you will learn in this General Education course, and these expectations are different to what you are getting. Such an attitude will prevent you from learning.
There is a solution !
1. Stop being a high school student and start being a university student.
2. Think with flexibility.
3. Accept that you may not understand a concept now, but that you may later.
4. If you come across a word or concept that you don’t understand, then do not stumble at that word or concept, but step over it and continue to listen. You can come back to it later. If you get stuck at one place then you cannot learn anything.
5. READ AS MUCH AS POSSIBLE. It is your duty to start reading and to continue to read the rest of your life.
6. We cannot teach you to learn, you must learn by yourself.
7. The best students are those driven by CURIOSITY.
8. The best students do not expect an answer to all of their questions; and yet expect many answers to one question.
9. Expect to be educated very widely at ICU, but also expect the opportunity to learn some things at great depth. Above all, broaden your horizons by learning about many things. A broad knowledge of many things, and a specialised knowledge of some will help you in later life. But the most important is learning how to learn.
10.Expect to increase your vocabulary by 100%, that is to double your vocabulary in your four years as a student.
11. All the same, you can also expect to get a great deal of enjoyment from the university environment, and make many friends. However, never forget your duty to learn and do well.
Now a thought test !
I want to see how much you are aware of your surroundings, especially the biosphere, because what I will introduce next relates to the biosphere.
Gas (Symbol) Percentage
Nitrogen (N) 78.03
Oxygen (O) 20.99
Argon (Ar) .94
Carbon dioxide (CO2). .035 -.04
Hydrogen (H) .01
Neon (Ne) .012
Helium (He) .0005
Krypton (Kr) .0001
Ozone (O3) .00006
Xenon (Xe) .000009
3. TODAY: Biogeochemical cycling. The four 3. TODAY: Biogeochemical cycling. The four
important elements in the biosphere related to life. important elements in the biosphere related to life.
Why N is an important macronutrient.Why N is an important macronutrient.
4. Next Wednesday: The phenomenon of the 4. Next Wednesday: The phenomenon of the
RhizobiumRhizobium/legume symbiosis/legume symbiosis
5. Next Friday: How plant cells work, the biology of 5. Next Friday: How plant cells work, the biology of
the root hairthe root hair
6. The following Monday: Experiments with root 6. The following Monday: Experiments with root
hairshairs
7. The following Tuesday: 7. The following Tuesday: AgrobacteriumAgrobacterium and and
sciencescience
Biogeochemical Cycling: movement of elements within or between ecosystems caused by organisms, by geological, hydrological, and atmospheric forces, and by chemical reactions
Elements within a cycle can move as: Solids, Liquids, or Gases
The chemical form of an element can vary among physical states or within a physical state
(e.g., Nitrogen as NH4+, NH3, N2)
Elements involved in cycling can also have different chemical forms (e.g., Carbon as CO2 (carbon dioxide)
or CO (carbon monoxide)
There are two basic terms used in cycling:
Pools: the amount of an element within a physical location or component of a cycle (sinks)
e.g.: tree, ocean, atmosphere, soil
Fluxes: the rate of movement of an element between pools
e.g.: evaporation, burning, dissolution of a rock, river carrying materials from land to the ocean
Residence Time
The length of time that an atom or molecule of a particular element spends in a particular location or component of a cycle
Mean Residence Time
Altering cycling rates can alter mean residence times and have the potential to lead to either depletion or pollution
Recycle Time
Basics of nutrient cycling
• Short-term: fixed stock available for organisms; question of turnover time
• Long-term: exchange between short-term pools and minerals/fossils
• Anthropogenic perturbations of nutrient cycling, local and global
Local and global cycling
• Local vs. global feedbacks in nutrient dynamics (recycling vs. one-way flow) depend on physics: gaseous phases mix, solid/liquid phases stay– one-way: energy, water– partly recycled: carbon, nitrogen– mostly recycled: phosphorus
• Humans have long affected local landscapes, but only recently affected global biogeochemical cycles
Dynamics of recycled nutrients
• cycling: available, temporarily unavailable, incorporated
• amount of biomass in plants = biomass:nutrient ratio (approx. 2:1 for carbon, varies more for other nutrients)
• fast cycling can be good for organisms (lots of available nutrient), but can also lead to long-term nutrient losses
organisms
unavailable(organic)
available(mineralized)
death
decomposition/mineralization
uptake
The water cycle
• water goes through biological systems on essentially a one-way trip
• cycle is fairly quick (except for aquifers, deep ocean circulation)
Let’s consider four biogeochemical cycles of elements required by organisms for life
CarbonPhosphorusSulphurNitrogen
Major pools of the carbon cycle in billions of tons of carbon.
The oceans contain the largest pool of carbon.
Carbon cycle• Central “nutrient”:
– closely bound to energy
– bound to N
– makes up structure of most organisms: 50% of dry biomass
• Major carbon storage, or sinks:– slow-decomposing compounds in soil– bicarbonate in the ocean– fossil fuels– wood
Carbon (2)
• Gaseous phase: well-mixed. Atmospheric concentration 350 ppm (pre-industrial 250 ppm)
• Aqueous phase: dissolves in ocean water (bicarbonate buffer).
• Solid phase: residence times of carbon in soil, and in plants, from weeks to centuries
Phosphorus• Extremely local recycling (no
gaseous phase)
• Long-term weathering/erosion cycle
• Most important/limiting in aquatic ecosystems, tropical terrestrial habitats
Dimethylsulfide (DMS) is released by phytoplankton, is then oxidized to sulfur dioxide and ultimately sulfate in the atmosphere.
Sulfate can cause clouds to form by having water droplets condense on it.
Nitrogen• Nitrogen: used for proteins, RUBISCO
• only nitrates (and some ammonium) available to plants: N mineralization by decomposers
• long-term loss/gain of N: deposition, leaching, volatilization
Nitrogen (2)
• Nitrogen dynamics depend on plant chemistry (C:N ratio, pH, decomposability), carbon dynamics, microbial community
• Short-cuts for plants: N-fixing organisms, mycorrhizae, direct uptake of organic N (?)
• Human nitrogen loading: fertilizer runoff (overflows from previously almost-closed cycles)
What’s so important about Nitrogen cycling?
essential nutrient (fertilizers, growing legumes as crops) –changes in native species composition of ecosystem
atmospheric pollutant (burning fuels)
groundwater pollutant
Nitrogen Cycle
ASSIMILATORY orDISSIMILATORYNO3
- REDUCTION
N2
Organic N NH4+
NO3-
DENITRIFICATION
NONSYMBIOTICN2 FIXATION SYMBIOTIC
N2 FIXATION
DECOMPOSITION
NITRIFICATION
AMMONIFICATION
IMMOBILIZATION
PLANT UPTAKE
Forms of Organic N
Protein &peptide N
Labile N
HydrolyzableUnknown N
AcidInsoluble N
Aminosugar N
Nucleicacid N
Major Inorganic N Compounds
Compound Formula Oxidation state
Form in soil
Ammonium NH4+ -3 Fixed in clay lattice, dissolved,
as gaseous ammonia (NH3)
Hydroxylamine
Dinitrogen
Nitrous oxide
Nitric oxide
Nitrite
Nitrate
NH2OH
N2
N2O
NO
NO2-
NO3-
-1
0
+1
+2
+3
+5
Not detected
Gas
Gas, dissolved
Gas, dissolved
Dissolved
Dissolved
Nitrogen Fixation The nodules on the rootsof this bean plant contain bacteria called Rhizobium that help convert nitrogen in the soil to a form the plant can utilize.
Dinitrogen Fixation
Treatment Yield (g)
Oats Peas
No N added
Non-inoculated
Inoculated with legume soil
Inoculated with sterile soil
0.6
0.7
—
0.8
16.4
0.9
112 mg NO3-–N per pot added
Non-inoculated
Inoculated with legume soil
12.0
11.6
12.9
15.3Hellriegel and Wilfarth (1888)
The alder, whose fat shadow nourisheth–Each plant set neere him long flourisheth. –William Browne (1613), Brittania’s Pastorals, Book I, Song 2
Types of Biological Nitrogen Fixation
Free-living (asymbiotic)• Cyanobacteria
• Azotobacter
Associative• Rhizosphere–Azospirillum
• Lichens–cyanobacteria
• Leaf nodules
Symbiotic• Legume-rhizobia
• Actinorhizal-Frankia
Free-living N2 Fixation
Energy• 20-120 g C used to fix 1 g N
Combined Nitrogen• nif genes tightly regulated
• Inhibited at low NH4+ and NO3
- (1 μg g-1 soil, 300 μM)
Oxygen• Avoidance (anaerobes)
• Microaerophilly
• Respiratory protection
• Specialized cells (heterocysts, vesicles)
• Spatial/temporal separation
• Conformational protection
Associative N2 Fixation
• Phyllosphere or rhizosphere (tropical grasses)
• Azosprillum, Acetobacter
• 1 to 10% of rhizosphere population
• Some establish within root
• Same energy and oxygen limitations as free-living
• Acetobacter diazotrophicus lives in internal tissue of sugar cane, grows in 30% sucrose, can reach populations of 106 to 107 cells g-1 tissue, and fix 100 to 150 kg N ha-1 y-1
Estimated Average Rates of Biological N2 Fixation
Organism or system N2 fixed (kg ha-1 y-1)
Free-living microorganismsCyanobacteria Azotobacter Clostridium pasteurianum
250.3
0.1-0.5
Grass-Bacteria associative symbiosesAzospirillum 5-25
Cyanobacterial associationsGunnera AzollaLichens
10-20300
40-80
Leguminous plant symbioses with rhizobia
Grain legumes (Glycine, Vigna, Lespedeza, Phaseolus)
Pasture legumes (Trifolium, Medicago, Lupinus)
50-100
100-600
Actinorhizal plant symbioses with Frankia
Alnus
Hippophaë
Ceanothus
Coriaria
Casuarina
40-300
1-150
1-50
50-150
50
• Nitrogen Fixation
• Almost all N is in the atmosphere
• 90-190 Tg N fixed by terrestrial systems
• 40-200 Tg N fixed by aquatic systems
• 3-10 Tg N fixed by lightning
• 32-53 Tg N fixed by crops
Some biogeochemical cycling key points:
• cycling occurs at local to global scales
• biogeochemical cycles have 2 basic parts: pools and fluxes
• elements are recycled among the biosphere, atmosphere, lithosphere and hydrosphere
• cycles of each element differ (chemistry, rates, pools, fluxes,interactions)
• cycling is important because it can affect many other aspects of the environment and the quality of our lives
Plant Nutrition
• Plant metabolism is based on sunlight and inorganic elements present in water, air, and soil.
• C, H, and O and energy are used to generate organic molecules via photosynthesis.
• Other chemical elements, such as mineral nutrients, are also absorbed from soil.
Plant Nutrients
• Plants absorb many elements, some of which they do not need.
• An element is considered an essential nutrient if it meets three criteria:• It is necessary for complete, normal plant
development through a full life cycle.• It itself is necessary; no substitute can be
effective.• It must be acting within the plant, not outside it.
• Many roles in plant metabolism.
Types of Essential Nutrients
• Nine essential nutrients, called macronutrients, are needed in very large amounts
• Eight other essential nutrients, called micronutrients, are needed only in small amounts.
Essential Nutrients to Most Plants
Macronutrient
% Dry Weight Component/Function
Carbon (C ) 45.0 Organic compounds
Oxygen (O) 45.0 Organic compounds
Hydrogen (H) 6.0 Organic compounds
Nitrogen (N) 1.0-4.0 Amino acids; nucleic acids, chlorophyll
Potassium (K) 1.0 Amino acids; regulates stomata opening/closing
Calcium (Ca) 0.5 Enzyme cofactor; influences cell permeability
Phosphorus (P) 0.2 ATP; proteins; nucleic acids; phosphoplipids
Magnesium (Mg) 0.2 Chlorophyll; enzyme activator
Sulfur (S) 0.1 CoA; amino acids
Essential Nutrients to Most Plants
Micronutrient Component/Function
Iron (Fe) Cytochromes; chlorophyll synthesis
Chlorine (Cl) Osmosis; water-splitting in photosynthesis
Copper (Cu) Plastocyanin; enzyme activator
Manganese (Mn) Enzyme activator; component of chlorophyll
Zinc (Zn) Enzyme activator
Molybdenum (Mo) Nitrogen fixation
Boron (B) Cofactor in chlorophyll synthesis
Nickel (Ni) Cofactor for enzyme functioning in nitrogen metabolism
Nitrogen: An Essential Macronutrient
• N is not present in rock, but is abundant in the atmosphere as a gas, N2.
• The process of converting N2 to chemically active forms of N is nitrogen metabolism.
• Nitrogen metabolism consists of 3 stages:
• Nitrogen Fixation (N2 -> NO3-)
• Nitrogen Reduction (NO3- -> NO2
- -> NH3 -> NH4
+)
• Nitrogen Assimilation (transfer of NH2 groups)
• Runoff, leaching, denitrification, and harvested crops reduce soil nitrogen.
Nitrogen Cycling Processes
Nitrogen Fixation – bacteria convert nitrogen gas (N2) to ammonia (NH3).
Decomposition – dead nitrogen fixers release N-containing compounds.
Ammonification – bacteria and fungi decompose dead plants and animals and release excess NH3 and ammonium ions (NH4
+).
Nitrification – type of chemosynthesis where NH3 or NH4
+ is converted to nitrite (NO2-); other bacteria
convert NO2- to nitrate (NO3
-).
Denitrification – bacteria convert NO2- and NO3
- to N2.
Means of Nitrogen Fixation
1) Human manufacturing of synthetic fertilizers
2) Lightning
3) Nitrogen-fixing bacteria and cyanobacteria
• Some are free-living in soil (E.g., Nostoc, Azotobacter); others live symbiotically with plants (E.g., Frankia, Rhizobium).
• These organisms have nitrogenase, an enzyme that uses N2 as a substrate.
• N2 + 8e- + 8H+ + 16ATP -> 2NH3 + H2 + 16ADP + 16Pi
• NH3 is immediately converted to NH4+.• Bacterial enzymes sensitive to O2. • Leghemoglobin binds to O2 and protects enzymes.• Symbiotic fixation rate depends on plant stage.
Nitrogen Fixing Bacteria and Cyanobacteria
Natural Sources of Organic N
Source % N
Dried blood 12
Peruvian guano 12
Dried fish meal 10
Peanut meal 7
Cottonseed meal 7
Sludge from sewer treatment plant 6
Poultry manure 5
Bone meal 4
Cattle manure 2
Symbiotic Nitrogen Fixation
• Nitrogen-fixing bacteria fix N (E.g., Rhizobium)
• Plants fix sugars (E.g.,legumes).• Plants form swellings that house
N-fixing bacteria, called root nodules.
• Mutualistic association.
• Excess NH3 is released into soil.
• Crop rotation maintains soil fertility.
Development of a Root Nodule• Bacteria enter the
root through an infection thread.
• Bacteria are then released into cell and assume form called bacteroids, contained within vesicles.
Symbiotic Nitrogen Fixation
The Rhizobium-legume association
Bacterial associations with certain plant families, primarily legume species, make the largest singlecontribution to biological nitrogen fixation in the biosphere
When this association is not present or functional, weapply nitrogen-containing fertilizers to replace reducednitrogen removed from the soil during repeated cycles of crop production. This practice consumes fossil fuels, both in fertilizer production and application.
Biological nitrogen fixation is the reduction of
atmospheric nitrogen gas (N2) to ammonium ions (NH4+)
by the oxygen-sensitive enzyme, nitrogenase. Reducing power is provided by NAPH/ferredoxin, via an Fe/Mocentre.
Even within the bacteria, only certain free-living bacteria (Klebsiella, Azospirillum, Azotobacter), blue-green bacteria (Anabaena) and a few symbiotic Rhizobial species are known nitrogen-fixers.
Plant genomes lack any genes encoding this enzyme,which occurs only in prokaryotes (bacteria).
Another nitrogen-fixing association exists betweenan Actinomycete (Frankia spp.) and alder (Alnus spp.)
The enzyme nitrogenase catalyses the conversion of atmospheric, gaseous dinitrogen (N2) and dihydrogen (H2) to ammonia (NH3), as shown in the chemical equation below:
N2 + 3 H2 2 NH3
The above reaction seems simple enough and the atmosphere is 78% N2, so why is this enzyme so important?
The incredibly strong (triple) bond in N2 makes this reaction very difficult to carry out efficiently. In fact, nitrogenase consumes ~16 moles of ATP for every molecule of N2 it reduces to NH3, which makes it one of the most energy-expensive processes known in Nature.
Biological NH3 creation (nitrogen fixation) accounts for an estimated 170 x 109 kg of ammonia every year. Human industrial production amounts to some 80 x 109
kg of ammonia yearly.
The industrial process (Haber-Bosh process) uses an Fe catalyst to dissociate molecules of N2 to atomic nitrogen on the catalyst surface, followed by reaction with H2 to form ammonia. This reaction typically runs at ~450º C and 500 atmospheres pressure.
These extreme reaction conditions consume a huge amount of energy each year, considering the scale at which NH3 is produced industrially.
If a way could be found to mimic nitrogenase catalysis(a reaction conducted at 0.78 atmospheres N2 pressure and ambient temperatures), huge amounts of energy
(and money) could be saved in industrial ammonia production.
If a way could be found to transfer the capacity to form N-fixing symbioses
from a typical legume host to an important non-host crop species such as corn or wheat,
far less fertilizer would be needed to be produced and applied
in order to sustain crop yields
The Dream…..
Because of its current and potential economic importance, the interaction between Rhizobia and leguminous plants has been intensively studied.
Our understanding of the process by which these twosymbionts establish a functional association is still not complete, but it has provided a paradigm for manyaspects of cell-to-cell communication between microbesand plants (e.g. during pathogen attack), and even between cells within plants (e.g. developmental signals; fertilization by pollen).
Symbiotic Rhizobia are classified in two groups:
Fast-growing Rhizobium spp. whose nodulation functions(nif, fix) are encoded on their symbiotic megaplasmids (pSym)
Slow-growing Bradyrhizobium spp. whose N-fixation and nodulation functions are encoded on their chromosome.
There are also two types of nodule that can be formed:
determinate and
indeterminateThis outcome is controlled by the plant host
Formed on tropical legumes by Rhizobium and Bradyrhizobium
Meristematic activity not persistent - present only during early stage of nodule formation; after that, cells simply expand rather than divide, to form globose nodules.
Nodules arise just below epidermis; largely internal vascular system
Determinate nodules
Uninfected cells dispersed throughout nodule; equipped to assimilate NH4
+ as ureides (allantoin and allantoic acid)
allantoin allantoic acid
Indeterminate nodules
Formed on temperate legumes (pea, clover, alfalfa);typically by Rhizobium spp.
Cylindrical nodules with a persistent meristem;nodule growth creates zones of different developmentalstages
Nodule arises near endodermis, and nodule vasculature clearly connected with root vascular system
Typical Associations (cross-inoculation groups)
Rhizobium leguminosarum biovar phaseolicolonizes bean (Phaseolus spp.)(tropical; determinate nodules)
R.l. biovar trifoliicolonizes clover (Trifolium spp.)(temperate; indeterminate nodules)
R.l. biovar viciaecolonizes pea (Pisum spp.) and vetch(temperate; indeterminate nodules)
Rhizobium meliloticolonizes alfalfa (Medicago sativa)temperate; indeterminate nodules
Rhizobium frediicolonizes soybean (Glycine max)tropical; determinate nodules
Bradyrhizobium japonicumcolonizes soybeantropical; determinate nodules
Rhizobium NGR 234colonizes Parasponia and tropicals;very broad host range
Nodule development process
1. Bacteria encounter root; they are chemotactically attracted toward specificplant chemicals (flavonoids) exuding from root tissue,especially in response to nitrogen limitation
daidzein (an isoflavone)
naringenin(a flavanone)
2. Bacteria attracted to the root attach themselves to the root hair surface and secrete specific oligosaccharidesignal molecules (nod factors).
nod factor
3. In response to oligosaccharide signals, the root hair becomes deformed and curls at the tip; bacteria becomeenclosed in small pocket.
Cortical cell division is induced within the root.
4. Bacteria then invade the root hair cell and move along an internal, plant-derived “infection thread”, multiplying, and secreting polysaccharides that fill the channel.
5. Infection thread penetrates through several layers of cortical cells and then ramifies within the cortex. Cells in advance of the thread divide and organize themselves into a nodule primordium.
6. The branched infection thread enters the nodule primordium zone and penetrates individual primordium cells.
7. Bacteria are released from the infection thread into the cytoplasm of the host cells, but remain surrounded by the peribacteroid membrane. Failure to form the PBM results in the activation of host defenses and/or the formation of ineffective nodules.
8. Infected root cells swell and cease dividing. Bacteria within the swollen cells change form to become endosymbiotic bacteroids, which begin to fix nitrogen.
The nodule provides an oxygen-controlled environment (leghemoglobin = pink nodule interior) structured to facilitate transport of reduced nitrogen metabolites from the bacteroids to the plant vascular system, and of photosynthate from the host plant to the bacteroids.
Types of bacterial functions involved innodulation and nitrogen fixation
nod (nodulation) and nol (nod locus) genesmutations in these genes block nodule formation oralter host rangemost have been identified by transposon mutagenesis, DNA sequencing and protein analysis, in R. meliloti, R. leguminosarum bv viciae and trifolii
fall into four classes: nodDnodA, B and C (common nod genes)hsn (host-specific nod genes)other nod genes
F G H I N D1 A B C I J Q P G E F H D3 E K D H A B C
(nol) (nod) (nif) (fix)
Gene clusters on R. meliloti pSym plasmid
N M L R E F D A B C I J T C B A H D K E N
Gene clusters on R. leguminosarum bv trifolii pSym plasmid
- - - D2 D1 Y A B C S U I J - - -
Gene cluster on Bradyrhizobium japonicum chromosome
Nod D (the sensor)the nod D gene product recognizes molecules (phenylpropanoid-derived flavonoids)produced by plant roots and becomes activated as a resultof that binding
activated nodD protein positively controls the expression of the other genes in the nod gene“regulon” (signal transduction)
different nodD alleles recognize various flavonoidstructures with different affinities, and respond withdifferential patterns of nod gene activation
naringenin(a flavanone)
Common nod genes - nod ABC
mutations in nodA,B or C completely abolish the ability of the bacteria to nodulate the host plant; they are found as part of the nod gene “regulon” in all Rhizobia ( common)
products of these genes are required for bacterial induction of root cell hair deformation and root cortical cell division
The nod ABC gene products are enzymes responsible for synthesis of diffusible nod factors, whcih are sulfated and acylated beta-1,4-oligosaccharides of glucosamine
(other gene products, e.g. NodH, may also be needed for special modifications)
[ 1, 2 or 3 ][C16 or C18 fatty acid]
SO3=
nod factors are active on host plants at very low concentrations (10-8 to 10-11 M) but have no effect on non-host species
mutations in these genes elicit abnormal root reactions on their usual hosts, and sometimes elicit root hair deformation reactions on plants that are not usually hosts
Host-specific nod genes
Example: loss of nodH function in R. meliloti results in synthesis of a nod factor that is no longer effective on alfalfa but has gained activity on vetch
The nodH nod factor is now more hydrophobic than the normal factor - no sulfate group on the oligosaccharide.
The role of the nodH gene product is therefore to add a specific sulfate group, and thereby change host specificity
Other nod genes
May be involved in the attachment of the bacteria to the plant surface, or in export of signal molecules, orproteins needed for a successful symbiotic relationship
exo (exopolysaccharide) genes
In Rhizobium-legume interactions that lead to indeterminate nodules, exo mutants cannot invade theplant properly. However, they do provoke the typical plant cell division pattern and root deformation, and can even lead to nodule formation, although these areoften empty (no bacteroids). In interactions that usually produce determinate nodules, exo mutations tend to have no effect on the process.
Exopolysaccharides may provide substrate for signal production, osmotic matrix needed during invasion, and/or a recognition or masking function during invasion
Encode proteins needed for exopolysaccharide synthesisand secretion
nif (nitrogen fixation) genes
Gene products are required for symbiotic nitrogen fixation, and for nitrogen fixation in free-living N-fixingspeciesExample: subunits of nitrogenase
fix (fixation) genes
Gene products required to successfully establish afunctional N-fixing nodule. No fix homologues have been identified in free-living N-fixing bacteria.
Example: regulatory proteins that monitor and controloxygen levels within the bacteroids
FixL senses the oxygen level; at low oxygen tensions, itacts as a kinase on FixJ, which regulates expression of two more transcriptional regulators: NifA, the upstream activator of nif and some fix genes; FixK, the regulator of fixN (another oxgen sensor?)
This key transducing protein, FixL, is a novel hemoprotein kinase with a complex structure. It has an N-terminal membrane-anchoring domain, followed by the heme binding section, and a C-terminal kinase catalytic domain. Result?Low oxygen tension activates nif gene transcription and permits the oxygen-sensitive nitrogenase to function.
Metabolic genes and transporters
Dicarboxylic acid (malate) transport and metabolism
Genes for other functions yet to be identified….
Proteomic analysis of bacteroids and peribacteroid membrane preparations
DNA microarray analysis of gene expression patterns
Host plant role in nodulation
1. Production and release of nod gene inducers - flavonoids
2. Activation of plant genes specifically required for successful nodule formation - nodulins
3. Suppression of genes normally involved in repelling microbial invaders - host defense genes
Nodulins
Bacterialattachment
Root hairinvasion
Bacteroiddevelopment
Nitrogenfixation
Nodulesenescence
early nodulins
latenodulins
Nodulins?
Pre-infectionInfection and noduleformation
Nodulefunction andmaintenance
Nodulesenescence
Early nodulins
At least 20 nodule-specific or nodule-enhanced genesare expressed in plant roots during nodule formation;most of these appear after the initiation of the visiblenodule.
Five different nodulins are expressed only in cells containing growing infection threads. These may encode proteins that are part of the plasmalemma surrounding the infection thread, or enzymes needed to make or modify other molecules
Twelve nodulins are expressed in root hairs and incortical cells that contain growing infection threads.They are also expressed in host cells a few layers ahead of the growing infection thread.
Late nodulins
The best studied and most abundant late nodulin isthe protein component of leghemoglobin. The heme component of leghemoglobin appears to be synthesized by the bacteroids.
Treatment of Lotus japonicus roots with nod factorfrom Mesorhizobium loti (NF), or infection with wt M. loti,(+) or an ineffective nodC strain of M. loti (-)
Other late nodulins are enzymes or subunits of enzymesthat function in nitrogen metabolism (glutaminesynthetase; uricase) or carbon metabolism (sucrosesynthase). Others are associated with the peribacteroidmembrane, and probably are involved in transportfunctions. These late nodulin gene products are usually not unique to nodule function, but are found in otherparts of the plant as well. This is consistent with thehypothesis that nodule formation evolved as a specialized form of root differentiation.
There must be many other host gene functions that are needed for successful nodule formation.
Example: what is the receptor for the nod factor?
These are being sought through genomic and proteomicanalyses, and through generation of plant mutantsthat fail to nodulate properly
The full genome sequencing of Medicago truncatulaand Lotus japonicus , both currently underway, will greatly speed up this discovery process.
A plant receptor-like kinase required for
both bacterial and fungal symbiosis S. Stracke et al Nature 417:959 (2002)
Screened mutagenized populations of the legumeLotus japonicus for mutants that showed an inabilityto be colonized by VAM Mutants found to also be affected in their ability to be colonized by nitrogen-fixing bacteria (“symbiotic mutants”)
Inhibitor of nodulation
Inducers of nodulation in Rhizobium leguminosarum bv viciae
luteolin eriodictyol
genistein
Figure 19.70
Genetics of Nitrogenase
Gene Properties and function
nifH
nifDK
nifA
nifB
nifEN
nifS
fixABCX
fixK
fixLJ
fixNOQP
fixGHIS
Dinitrogenase reductase
Dinitrogenase
Regulatory, activator of most nif and fix genes
FeMo cofactor biosynthesis
FeMo cofactor biosynthesis
Unknown
Electron transfer
Regulatory
Regulatory, two-component sensor/effector
Electron transfer
Transmembrane complex
Nitrogenase
FeMo Cofactor
N2 + 8H+
2NH3 + H2
8e-
4C2H2 + 8H+ 4C2H2
DinitrogenaseDinitrogenasereductase
Fd(red)
Fd(ox)
nMgATP
nMgADP + nPi
N2 + 8H+ + 8e- + 16 MgATP 2NH3 + H2 + 16MgADP
Taxonomy of Rhizobia
Genus Species Host plantRhizobium leguminosarum bv. trifolii
“ bv. viciae “ bv. phaseolitropicietli
Trifolium (clovers)Pisum (peas), Vicia (field beans), Lens (lentils), LathyrusPhaseolus (bean)Phaseolus (bean), LeucaenaPhaseolus (bean)
Sinorhizobium melilotifrediisaheliteranga
Melilotus (sweetclover), Medicago (alfalfa), TrigonellaGlycine (soybean)Sesbania Sesbania, Acacia
Bradyrhizobium japonicumelkaniiliaoningense
Glycine (soybean)Glycine (soybean)Glycine (soybean)
Azorhizobium caulinodans Sesbania (stem nodule)
‘Meso rhizobium’ lotihuakuiiciceritianshanensemediterraneum
Lotus (trefoil)Astragalus (milkvetch)Cicer (chickpea)
Cicer (chickpea)
[Rhizobium] galegae Galega (goat’s rue), Leucaena
Photorhizobium spp. Aeschynomene (stem nodule)
Nitrogen Fixation
• Energy intensive process :
• N2 + 8H+ + 8e- + 16 ATP = 2NH3 + H2 + 16ADP + 16 Pi
• Performed only by selected bacteria and actinomycetes
• Performed in nitrogen fixing crops (ex: soybeans)
Role of Root Exudates
General• Amino sugars, sugars
Specific• Flavones (luteolin), isoflavones
(genistein), flavanones, chalcones
• Inducers/repressors of nod genes
• Vary by plant species
• Responsiveness varies by rhizobia species
Infection Process
• Attachment• Root hair curling• Localized cell wall
degradation• Infection thread• Cortical cell
differentiation• Rhizobia released into
cytoplasm• Bacterioid differentiation
(symbiosome formation)• Induction of nodulins
Nodule Metabolism
Oxygen metabolism• Variable diffusion barrier• Leghemoglobin
Nitrogen metabolism• NH3 diffuses to cytosol• Assimilation by GOGAT• Conversion to organic-N for
transport
Carbon metabolism• Sucrose converted to
dicarboxylic acids• Functioning TCA in
bacteroids• C stored in nodules as starch
Sources
• Lightning• Inorganic fertilizers• Nitrogen Fixation• Animal Residues• Crop residues• Organic fertilizers
Forms of Nitrogen
• Urea CO(NH2)2
• Ammonia NH3 (gaseous)• Ammonium NH4
• Nitrate NO3
• Nitrite NO2
• Atmospheric Dinitrogen N2
• Organic N
Global Nitrogen ReservoirsNitrogen Reservoir
Metric tons nitrogen
Actively cycled
Atmosphere 3.9*1015 No
Ocean soluble salts
Biomass6.9*1011
5.2*108
YesYes
Land organic matter Biota
1.1*1011
2.5*1010
SlowYes
Roles of Nitrogen
• Plants and bacteria use nitrogen in the form of NH4
+ or NO3-
• It serves as an electron acceptor in anaerobic environment
• Nitrogen is often the most limiting nutrient in soil and water.
Nitrogen is a key element for
• amino acids• nucleic acids (purine, pyrimidine) • cell wall components of bacteria
(NAM).
Nitrogen Cycles
• Ammonification/mineralization• Immobilization• Nitrogen Fixation • Nitrification• Denitrification
Mineralization or Ammonification
• Decomposers: earthworms, termites, slugs, snails, bacteria, and fungi
• Uses extracellular enzymes initiate degradation of plant polymers
• Microorganisms uses:• Proteases, lysozymes, nucleases to
degrade nitrogen containing molecules
• Plants die or bacterial cells lyse release of organic nitrogen
• Organic nitrogen is converted to inorganic nitrogen (NH3)
• When pH<7.5, converted rapidly to NH4
• Example:
Urea NH3 + 2 CO2
Immobilization
• The opposite of mineralization• Happens when nitrogen is limiting in the
environment• Nitrogen limitation is governed by C/N ratio• C/N typical for soil microbial biomass is 20• C/N < 20 Mineralization• C/N > 20 Immobilization
Microorganisms fixing
• Azobacter• Beijerinckia• Azospirillum• Clostridium• Cyanobacteria
• Require the enzyme nitrogenase
• Inhibited by oxygen
• Inhibited by ammonia (end product)
Rates of Nitrogen Fixation
N2 fixing system Nitrogen Fixation (kg N/hect/year)
Rhizobium-legume 200-300
Cyanobacteria- moss
30-40
Rhizosphere associations
2-25
Free- living 1-2
Bacterial Fixation
• Occurs mostly in salt marshes• Is absent from low pH peat of
northern bogs• Cyanobacteria found in
waterlogged soils