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Copyright © 2009 Pearson Education Inc., publishing as Pearson Benjamin Cummings
Brock Biology of Microorganisms, Twelfth Edition – Madigan / Martinko / Dunlap / Clark
752-4001-00L Mikrobiologie
Julia Vorholt Lecture 8: Nov 12, 2012
Copyright © 2009 Pearson Education Inc., publishing as Pearson Benjamin Cummings
Brock Biology of Microorganisms, Twelfth Edition – Madigan / Martinko / Dunlap / Clark
1) Nutrients and microbial growth 2) Introduction to principles of metabolism 3) Chemoorganotrophy 4) Chemolithotrophy 5) Phototrophy 6) Autotrophy, nitrogen fixation 7) Global carbon, nitrogen, sulfur cycles
Copyright © 2009 Pearson Education Inc., publishing as Pearson Benjamin Cummings
Glycolysis and Citric Acid Cycle
Fig. 4.14
Glucose
Pyruvate
2 Pyruvate
2 lactate
Substrate-level-phosphorylation
Electron transport-coupled phosphorylation
Pyruvate (three carbons)
Acetyl-CoA
Oxalacetate2
Malate2
Fumarate2
Succinate2
Succinyl-CoA
Citrate3
Aconitate3
Isocitrate3
-Ketoglutarate2
C2
C4
C5
C6
Electron transport-coupled
phosphorylation
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Aerobic Respiration
Complex I (NADH:quinone oxidoreductase) NADH donates e- to FMN FMN donates e- to quinone
Complex II (succinate dehydrogenase complex) Bypasses Complex I Feeds e- and H+ from FADH directly to quinone pool
Complex III (cytochrome bc1 complex)
Transfers e- from quinones to cytochrome c Cytochrome c shuttles e- to cytochromes a and a3
Complex IV (cytochromes a and a3) Terminal oxidase; reduces O2 to H2O
Electron transport process in the membrane of
Paracoccus denitrificans
Chap. 4.10 Fig. 4.19
CYTOPLASMENVI
RONM
ENT
Complex IISuccinate
Fumarate
Q cycle
0.22
0.0
0.1
0.36
0.39
E0(V)
E0(V)
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Aerobic Respiration
Electron transport process in the membrane of
Escherichia coli
Fig. 14.13a Chap. 4.11
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Anaerobic Respiration
The use of electron acceptors other than oxygen
Examples include nitrate (NO3-), ferric iron (Fe3+), sulfate
(SO42-), carbonate (CO3
2-), certain organic compounds
Less energy released compared to aerobic respiration
Energy released from redox reactions can be determined by comparing reduction potentials of each electron acceptor
Dependent on electron transport, generation of a proton motive force, and ATPase activity
Chap. 4.12, 14.6
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Major Forms of Anaerobic Respiration
Thermodynamic hierarchy of
electron acceptors
Organisms: (many) Pseudomonas
Paracoccus
Organisms: Enterobacteria,
e.g. E. coli
Chap. 14.6 Fig. 14.11
0.42
0.3
0.27
0.25
0.22
0
0.2
0.3
0.4
0.75
0.82
Anoxic
Oxic(oxygenpresent)
Anoxic Proton reduction;Pyrococcus furiosus,obligate anaerobe
E0(V)
Carbonate respiration;acetogenic bacteria,obligate anaerobes
Sulfur respiration;facultative aerobes andobligate anaerobes
Carbonate respiration;methanogenic Archaea;obligate anaerobes
Sulfate respiration(sulfate reduction);obligate anaerobes(SO4
2- SO32-, E0 0.52)
Fumarate respiration;facultative aerobes
Iron respiration; facultativeaerobes and obligateanaerobes
Reductive dechlorination;facultative aerobes andobligate anaerobes
Nitrate respiration;facultative aerobes (somereduce NO3
- to NH4)
Denitrification;facultative aerobes
Manganese reduction;facultative aerobes
Aerobic respiration;obligate andfacultative aerobes
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Dissimilative Reduction of Nitrate
-> Denitrification is a biological source of gaseous N2
Chap. 14.7 Fig. 14.12
Nitrate
Nitrite
Nitric oxide
Nitrous oxide
Dinitrogen
Gases
Nitratereduction (Escherichiacoli)
Denitrification (Pseudomonasstutzeri)
NO3
NO2
NO
N2O
N2
Nitrate reductase
Nitrite reductase
Nitric oxide reductase
Nitrous oxide reductase
NH4+
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Respiration and Anaerobic Respiration
Chap. 14.7 Fig. 14.13
Periplasm
Q cycle
Cytoplasm
Aerobic respiration
Denitrification
Nitrate reduction
Periplasm
Q cycle
Cytoplasm
Nitrate reductase complex
Nitr
ate
re
duct
ase
Nitr
ate
re
duct
ase
Nitr
ic o
xide
re
duct
ase
Periplasm Nitrate reductase complex
Q cycle
Cytoplasm
N2O reductase
NO2
reductase
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Major Forms of Anaerobic Respiration
Chap. 14.6 Fig. 14.11
0.42
0.3
0.27
0.25
0.22
0
0.2
0.3
0.4
0.75
0.82
Anoxic
Oxic(oxygenpresent)
Anoxic Proton reduction;Pyrococcus furiosus,obligate anaerobe
E0(V)
Carbonate respiration;acetogenic bacteria,obligate anaerobes
Sulfur respiration;facultative aerobes andobligate anaerobes
Carbonate respiration;methanogenic Archaea;obligate anaerobes
Sulfate respiration(sulfate reduction);obligate anaerobes(SO4
2- SO32-, E0 0.52)
Fumarate respiration;facultative aerobes
Iron respiration; facultativeaerobes and obligateanaerobes
Reductive dechlorination;facultative aerobes andobligate anaerobes
Nitrate respiration;facultative aerobes (somereduce NO3
- to NH4)
Denitrification;facultative aerobes
Manganese reduction;facultative aerobes
Aerobic respiration;obligate andfacultative aerobes
Organisms: Shewanella Geobacter
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Microbial Fuel Cell
www.microbialfuelcell.org
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Electricigens – Potential mechanisms for electron transfer
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Major Forms of Anaerobic Respiration
Chap. 14.6 Fig. 14.11
0.42
0.3
0.27
0.25
0.22
0
0.2
0.3
0.4
0.75
0.82
Anoxic
Oxic(oxygenpresent)
Anoxic Proton reduction;Pyrococcus furiosus,obligate anaerobe
E0(V)
Carbonate respiration;acetogenic bacteria,obligate anaerobes
Sulfur respiration;facultative aerobes andobligate anaerobes
Carbonate respiration;methanogenic Archaea;obligate anaerobes
Sulfate respiration(sulfate reduction);obligate anaerobes(SO4
2- SO32-, E0 0.52)
Fumarate respiration;facultative aerobes
Iron respiration; facultativeaerobes and obligateanaerobes
Reductive dechlorination;facultative aerobes andobligate anaerobes
Nitrate respiration;facultative aerobes (somereduce NO3
- to NH4)
Denitrification;facultative aerobes
Manganese reduction;facultative aerobes
Aerobic respiration;obligate andfacultative aerobes
Organisms: Methanosarcina
Methanobacterium Methanococcus Methanopyrus
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Methanogenesis and Acetogenesis
at 1-10 Pa H2: G‘ = - 17 kJ/mol)
Some methanogens also use acetate or methanol as substrate
Chap. 14.10 Fig. 14.16
Proton or sodium motive force (plus
substrate-level phosphorylation for
acetogens)
Methanogenesis ( G0 136 kJ)
Acetogenesis ( G0 105 kJ)
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Methanogenesis
Methanogenesis is the only way that methanogenic archaea can obtain energy for growth. => Specialization
Methanogens are the only organisms known to produce methane (CH4) as a catabolic end product.
They are strict anaerobes.
Atmospheric concentrations of methane have doubled since 200 years.
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Anoxic Decomposition
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Rumen and Gastrointestinal System of a Cow
Chap. 24.10 Fig. 24.27
The rumen contains 1010-1011
microbes/g of rumen constituents
Microbial fermentation in the rumen is mediated by celluloytic microbes that hydrolyze cellulose to free glucose that is then fermented, producing volatile fatty acids (e.g., acetic, propionic, butyric) and the CH4 and CO2
Fatty acids pass through rumen wall into bloodstream and are utilized by the animal as its main energy source
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Biochemical Reactions in the Rumen
Rumen microbes also synthesize amino acids and vitamins for their animal host
Rumen microbes themselves can serve as a source of protein to their host when they are directly digested
Chap. 24.10 Fig. 24.28
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Rumen and Gastrointestinal System of a Cow
Chap. 25.7 Fig. 25.26
The rumen contains 1010-1011
microbes/g of rumen constituents
Microbial fermentation in the rumen is mediated by celluloytic microbes that hydrolyze cellulose to free glucose that is then fermented, producing volatile fatty acids (e.g., acetic, propionic, butyric) and the CH4 and CO2
Fatty acids pass through rumen wall into bloodstream and are utilized by the animal as its main energy source
Copyright © 2009 Pearson Education Inc., publishing as Pearson Benjamin Cummings
Biochemical Reactions in the Rumen
Rumen microbes also synthesize amino acids and vitamins for their animal host
Rumen microbes themselves can serve as a source of protein to their host when they are directly digested
Chap. 25.7 Fig. 25.27
FEED, HAY, etc.
Cellulose, starch, sugars
Fermentation Fermentation
Cellulolysis, amylolysis
Formate
Pyruvate Succinate
Lactate Propionate CO2
Removed byeructation toatmosphere
Acetate
Rum
inan
t blo
odst
ream
Rum
en w
all
VFAs
AcetatePropionateButyrate
Overall stoichiometry of rumen fermentation:
SUGARS
Copyright © 2009 Pearson Education Inc., publishing as Pearson Benjamin Cummings
Brock Biology of Microorganisms, Twelfth Edition – Madigan / Martinko / Dunlap / Clark
1) Nutrients and microbial growth 2) Introduction to principles of metabolism 3) Chemoorganotrophy 4) Chemolithotrophy 5) Phototrophy 6) Autotrophy, nitrogen fixation 7) Global carbon, nitrogen, sulfur cycles
Copyright © 2009 Pearson Education Inc., publishing as Pearson Benjamin Cummings
Chemolithotrophy: Beggiatoa
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Sergej Winogradsky: Concept of Chemolithotrophy 1887
Drawings made by Winogradsky of Beggiatoa. Fig. 1. The tip of a filament of Beggiatoa alba: (a) in sulfurous [sulfide-containing] water, (b) after 24 h in water nearly depleted in H2S, (c) after 48 h in water without H2S. Fig. 2. The tip of a filament of Beggiatoa media. Fig. 3. The tip of a filament of Beggiatoa minima. From Winogradsky, S. 1949. Microbiologie du Sol. Masson, Paris.
Sulfur oxidizers
Fig. 1.2
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Chemolithotrophy
Chemolithotrophs are organisms that obtain energy
from the oxidation of inorganic compounds
Most chemolithotrophs obtain their carbon from CO2 (autotrophs)
Many sources of reduced molecules exist in the
environment
The oxidation of different reduced compounds yields
varying amounts of energy
Chap. 13.6
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Chemolithotrophic processes
Chap. 13.6
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Energy Yields from Oxidation of Inorganic Electron Donors
Chap. 13.6
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Hydrogen Oxidizers (aerobic) / Knallgas bacteria
Chap. 13.7
> Large amounts of hydrogen are formed during the anaerobic biological degradation of organic material.
> Low amounts are also released during geochemical processes and are found in vulcanic gases.
H2 + 0.5 O2 -> H2O (G°‘ = - 237 kJ/mol) Key enzyme: Hydrogenase (Fe, S) (Ni, Fe) „Knallgasbakterien“ – aerobic hydrogen oxidizing microorganisms: Ralstonia eutropha (Alcaligenes), Paracoccus (usually facultative chemolithotroph)
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Hydrogenases of Aerobic Hydrogen oxidizing Bacteria
Chap. 13.7 Fig. 13.20
Membrane-integrated hydrogenase
Cytoplasmic hydrogenase
Cell material
Out
In
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Nitrification
NH3 and NO2- are oxidized by nitrifying bacteria (and archaea) during the process of nitrification
Two groups of bacteria work in concert to fully oxidize ammonia to nitrate
The nitrifiers are widespread in soil and water. They can be found in nature wherever ammonium is liberated and oxygen is available.
Like many other chemolithotrophs, the nitrifiers are particularly active at the oxic/anoxic interface of sediments and water bodies.
Only small energy yields from this reaction
=> Growth of nitrifying bacteria is very slow
Nitrite-oxidizing
Ammonium-oxidizing
Chap. 13.10
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Oxidation of Ammonia by Ammonia-Oxidizing Bacteria
Chap. 13.10 Fig. 13.26
AMO, ammonia monooxygenase
HAO, hydroxylamine oxidoreductase
Cyt aa3, terminal cyt c oxidase (complex IV)
Oxidation ofhydroxylamine
Out
Oxidation ofammonia
Reductionof oxygen
In
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Oxidation of Nitrite to Nitrate by Nitrifying Bacteria
Chap. 13.10 Fig. 13.27
NXR, nitrite oxidoreductase
Cyt aa3, terminal cyt c oxidase (complex IV)
Periplasm
Cytoplasm
Oxidation of nitrite
Reductionof oxygen
Reverse e flowto make NADH
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Degradation of limestone
NH3 NO2- NO3
-
Salpeter- säure
Nitric acid
salpetrige Säure
Nitrous acid
Agriculture
Ca(CO3)2
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Nitrifiers in waste-water treatment
The chemolithoautotrophic ammonium- and nitrite-oxidizing bacteria play a vital role in modern waste-water treatment for nitrogen removal.
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Anammox
Chap. 13.11 Fig. 13.28
Anammox: anoxic ammonia oxidation (to N2 gas)
NH4+ + NO2
- -> N2 + H2O Performed by unusual group of
obligate aerobic bacteria (Plantomycetes)
Anammoxosome is compartment where anammox reactions occur
Protects cell from reactions occuring during anammox
Hydrazine (H2N-NH2) is an intermediate of anammox
Anammox is very beneficial in the treatment of wastewater Anammoxosome
membraneElectrontransport
Out In