Title: Lecture 6' Microbial Adaptations 1
1Lecture 6. Microbial Adaptations 1
- Extremophilic micro-organisms
- Adaptive stresses
- Thermophiles
- Macromolecular stability
- Psychrophiles
- Halophiles
- Acidophiles
2Extremophiles
3Adaptive stresses
- Thermophiles
- Psychrophiles
- Halophiles
- Acidophiles
- Alkalophiles
- Barophiles
- Radiophiles
- Oligotrophy
- Denaturation and chemical destruction of macro-
and small molecules membrane hyperfluidity - Membrane hypofluidity Slow reaction kinetics
- Hyperosmotic stress
- Chemical stability membrane potentials
- Proton pumping against a negative pH gradient
- Unfavourable reaction equilibria reaction
kinetics - Molecular damage
- Nutrient deficiency and uptake affinity
4Thermophiles to Hyperthermophiles
5Thermophilic biotopes and organisms
Bacillus stearothermophilus Thermus
aquaticus Thermotoga spp. Sulfolobus spp.
Pyrococcus spp. Pyrodictium spp. Methanococcus
Terrestrial and deep sea hydrothermal systems
Methanococcus jannaschii
6Hyperthermophiles in the Tree of Life
BACTERIA
ARCHAEA
EUKARYA
7Living at high temperatures Problems and
Solutions
- Proteins denature at high temperatures.
- Many essential small molecules (e.g., ATP, NADH
etc) are unstable at high temperatures. - Membranes become more fluid at high temperatures.
- Reaction rates increase with temperature
metabolic overrun?
- Thermodynamic stability of proteins is increased.
- Not known exactly metabolic channeling may be
important. - Membrane lipid compositions change to reduce
fluidity. - Enzyme conformational mobility and expression
levels control metabolic rates
8Comparative stability of b-glycosidases
9Molecular mechanisms of protein stability
- Proteins are stabilised by weak intramolecular
interactions (h? lt H-bonds lt ionic bonds) and
protein-solvent interactions. - Comparisons of 3D x-ray structures of homologous
proteins from different thermal sources show - gt Intramolecular packing
- lt External loops
- More helix-forming aas
- Stabilised helix dipoles
- gt Proline residues
- lt Asn residues
- Salt bridge networks
Higher protein stability
10Protein stability a balance between the net
free energy of the folded and denatured states
- N ? D model
- DG comprises enthalpy and entropy components
- Maximum enthalpy from intramolecular bonds
- Minimum entropy
- Folded proteins have high entropy
- Solvent entropy is minimised in folded state
DG Free energy of denaturation
Unfolded
Folded
11Stabilising lipids and reducing membrane fluidity
- Increase hydrophobic interactions between lipids
- Reduced fatty acid branching
- Increased fatty acid chain length
- Cyclisation
- Stabilise chemically sensitive ester bonds
- Ether-linked lipids in Archaea only
- Reduce lateral mobility of lipids
- C40 monolayer lipids in Archaea only
12Psychrophiles living at low temperatures
Arctic, Antarctic, deep Marine and alpine
regions
13Organisms at low temperatures
- Psychrophiles Topt, 15oC, Tmax lt 20oC, Tmin ,
lt0oC - Psychrotolerants (psychrotrophs) Topt, 20oC,
Tmax gt 20oC, Tmin , gt3oC - Very wide species diversity of Bacteria, Fungi,
Algae - E.g., Planococcus, Staphylococcus, Nostoc,
Actinomyetes - Limited diversity of Archaea
- Methanogens, uncultured crenarchaeota
14PsychrophilesProblems and Solutions
- Low metabolic rates
- Membrane rigidity
- Protein flexibility
- Cytoplasmic freezing
- Grow slowly
- Adapt membrane fluidity
- gt Unsaturation
- lt Chain length
- gt Methyl branching
- Increase conformational flexibility
- Reduce intramolecular bonding
- Accumulation of solutes (freeze prevention)
- Ice-nucleating proteins (freeze control)
15Extreme halophiles
- Living at very high salt concentrations
- Vertebrates lt 1.5M
- Halobacteria 1.5 3M
- Haloarchaea 3 5.2M
16Examples of moderate and extreme halophiles
- Bacteria
- Microccus
- Bacillus
- Flavobacterium
- Halomonas
- Vibrio
- Alteromonas
- Pseudomonas
- Eukaryotes
- Artemia
- Dunaliella
- Archaea
- Halobacterium
- Halorubrum
- Haloferax
- Haloarcula
- Halococcus
17Extreme halophiles in the tree of life
18Extreme halophilesProblems and Solutions
- Osmoregulation
- Protein stability
- Archaea
- Accumulation of intracellular salts (5M KCl)
- Bacteria
- Accumulation of low molecular weight solutes
(osmolytes) with osmotic potential - Increases in acidic a.a.s
19Osmolytes
- Glycerol (algae, fungi)
- Sugars, polyols and derivatives
- Glycine betaine
- a-amino acids (P, E)
- Ectoine, Hydroxyectoine
- Charged or hydroxylated compounds
- which H-bond with water molecules
20Protein stability in Halophiles
- High ionic strength (salt concentration)
denatures proteins - Dissociation of salt bridges
- Removal of protein water shell
- Halophilic proteins have increased surface
charged amino acids - Stabilised by K salt networks
- Increased water shell
- Many halophilic proteins require molar KCl for
stability
21Acidophiles
- Geothermal areas
- Acid mine drainage
pH 0 3
2So 3 O2 2 H2O à 2 H2SO4
4 FeS2 15 O2 14 H2O à 4 Fe(OH)3 8 H2SO4
22Acidophiles are phylogenetically diverse
- Eukaryotes
- Fungi (numerous)
- Algae (Cyanidium)
- Protozoa (flagellates, ciliates, amoebae)
- Bacteria
- Heterotrophs (Alicyclobacillus, Acidiphilium,
Sulfobacillus) - Autotrophs (Acidithiobacillus)
- Archaea
- Numerous heterotrophs and autotrophs, many
thermophilic (Thermoplasma, Sulfolobus,
Acidianus, Metallosphaera)
23Chemoautotrophic metabolism in acidophiles
- Sulfolobus
- Acidianus
- Stygioglobus
- Aquifex
- Sulfobacillus
- Aerobic sulphur oxidation (So ? SO4-2 O2 ?
H2O) - Aerobic sulphide oxidation (S-2 ? SO4-2 O2 ?
H2O) - Anaerobic hydrogen oxidation (H2 So ? H2S)
- Aerobic hydrogen oxidation (H2 1/2O2 ? H2O)
- Aerobic iron oxidation (FeII ? FeIII O2
? H2O)
24AcidophilesProblems and Solutions
- pH homeostasis
- Molecular stability
- Intracellular pH trans-membrane potentials
- Internal pH is maintained at 5-7 by maintained
by proton pumping high external proton drives
chemiosmotic ATP synthesis - Acid stable proteins
- Stabilised by increase in charged amino acids