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Extremophilic microorganisms and the physico-chemical limits of life Helga Stan-Lotter, University of Salzburg, Austria New classification of organisms - Bacteria, Archaea and Eukarya Extreme environments: their physico-chemical parameters Molecular adaptations to extreme environments Growth versus survival Origin of Life ? Prokaryote World Multi-cell Life 1 Man First Eukaryotes 0.01 First Invertebrates 2 PO (atm) 0.1 0.001 0.0001 0.00001 4.5 4 3.5 3 2.5 2 1.5 Time before Present (Ga) 1 0.5 0 Eukaryotes - Prokaryotes (1931) / Eubacteria (Bacteria) \ Archaebacteria (1977) (Archaea) Prokaryote World Multi-cell Life 1 Man First Eukaryotes 0.01 First Invertebrates 2 PO (atm) 0.1 0.001 0.0001 0.00001 4.5 4 3.5 3 2.5 2 1.5 Time before Present (Ga) 1 0.5 0 Venus Mars Viking lander approaching Mars (painting) 1996 Staphylococcus aureus Vibrio cholerae Cyanobacteria Spirulina species Amoeba (protozoon) Unicellular algae (unicellular diatom) Extreme environments are hostile to human life and were thought to be uninhabitable by other organisms. (Richard Johnson) Extreme habitats are environments with a restricted species diversity and the absence of some taxonomic groups (Thomas D. Brock) Extreme physico-chemical factors: Temperature - high, low Pressure - high pH value - high; low Salinity - high Water activity - low Ionizing radiation - high Toxic substances - high concentrations Nutrients (carbon, other) - low concentrations Survival versus Growth Spores, endospores, cysts, seeds (resting stages): Unicellular bodies, produced by plants, fungi, and some microorganisms. Often a resting stage is encased in a protective coat, adapted to resist heat, desiccation, or other unfavorable environmental conditions. Hot environments on Earth Thermophiles and Hyperthermophiles Adaptations Hot spring (Yellowstone) Solfatara field in Yellowstone (USA) Grand Prismatic Spring (Yellowstone) Sulfur spring, pH 1.8-2.2 S-layer (surface) Solfatara field on Kraffla mountain (Iceland) Mud geysir (Iceland) Solfatara field (Iceland) Pyrodictium occultum Self-heating coal refuse piles (Habitat of Thermoplasma acidophilum) Black smokers and hydrothermal vents Many hyperthermophilic Archaea are chemolithotrophic. Their energy sources are anorganic substances, e.g. H2, So, FeS2, FeCO3 Scheme of the universal lipid bilayer membrane Membrane lipids of hyperthermophiles often consist of isoprenoid tetraether structures; these are more resistant to heat and acid than ester bonds and fatty acids Psychrophiles Temperature and growth Salty environments on Earth (high salinity, low water activity) Halophilic and halotolerant prokaryotes Adaptations Swakopmund salterns (Namibia) Permian salt sediments Bore cores from salt sediments (600 m below surface) Haloarchaeal colonies on M2 agar Halococcus salifodinae, an archaeal isolate from Permian salt High radiation; high concentrations of toxic substances Radiation resistant metallo-tolerant, toxitolerant Adaptations Biologically efficient radiation dosis (in Gray): 1 Gy = 1 Joule absorbed energy per kg of tissue Lethal dosis Humans Salmonella, Bacillus sp. Deinococcus radiodurans 5-10 Gy 2.000 - 6.000 Gy > 30.000 Gy Deinococcus radiodurans possesses an extremely efficient DNA repair system; can excise and repair misincorporated bases; can repair breaks in single- or double-stranded DNA; can reassemble its chromosome from fragments. Metallo-tolerant, toxi-tolerant microorganisms: Efflux pumps (ATPases) Low concentrations of nutrients: Deep subsurface Oligotroph, thermotolerant, metallo-tolerant Deep terrestrial subsurface Bacterial endospore Tardigrade, moving Tardigrade, dry Tardigrades: up to 2.3 % of dry weight: Trehalose Relevance for the origin of life ...? (Hypothesis paper by Cleaves II & Chalmers, Extremophiles may be irrelevant to the origin of life. Astrobiology 4: 1, 2004) Summary Microorganisms thrive in extreme environments which once were believed entirely hostile to life Extreme environments are characterized by one or several physico-chemical parameters Extremophilic microorganisms survive exposure to space conditions, desiccation, and low nutrient environments - all this perhaps for millions of years. They may therefore survive also space travel. However, many extreme environmental parameters are not compatible with ideas about the origin and early evolution of life (see Cleaves and Chalmers, 2004).