41 st SaasFee course from Planets to Life 39 April 2011 Lecture 2: - - PowerPoint PPT Presentation

41 st saas fee course from planets to life 3 9 april 2011
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41 st SaasFee course from Planets to Life 39 April 2011 Lecture 2: - - PowerPoint PPT Presentation

41 st SaasFee course from Planets to Life 39 April 2011 Lecture 2: The top down approach to understanding the origin of life cont. Understanding the characterisFcs of the organisms close to the root of the tree Most are


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41st Saas‐Fee course from Planets to Life 3‐9 April 2011

Lecture 2: The “top down” approach to

understanding the origin of life – cont.

  • Understanding the characterisFcs of the
  • rganisms close to the root of the tree

– Most are extremophiles (grow at high temperatures, high and low pH, high salt, etc) – The origin of metabolism – The “RNA” world – The possible role of viruses in the origin of life – The possible importance of “biofilms” in the early evoluFon of life

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CharacterisFc differences between the three domains of life: Archaea, Bacteria and Eukarya

Characteristics* Archaea Bacteria Eukarya

Cells with membrane-bound nucleus and other organelles No No Yes DNA circular1 Yes Yes No Ribosome size 70S 70S 80S Membrane lipids Ether linked Ester linked Ester linked Cell walls No PDG2 PDG No Histone proteins Yes No Yes Operons in DNA Yes Yes No Ribosome structure distinct distinct Archaeal-like Antibiotic sensitivity No Yes No Photosynthesis No Yes Yes Growth at temperatures >80°C Yes Yes No

*There are many physiological characterisFcs that are found only in bacteria and

  • archaea. 1There are some excepFons. 2PDG is pepFdoglycan; Archaea do not have

PDG but do have at least 7 different cell surface layers (protein, lipid, etc)

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SLIDE 3

Longitudinal secFon through the flagella area The kinetosome (basil body) that is the anchoring site for a flagellum

The endoplasmic reFculum is an interconnected network

  • f tubules, vesicles and is

involved in the synthesis

  • f proteins, lipidss, sugar

metabolism, etc

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Limits of Life and Limits of Diversity

  • Are their limits to evolutionary diversity of life as we

know it?

  • What environmental conditions limit where life can

exist?

What did Darwin have to say that is germane to these questions?

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SLIDE 6

Darwin's most famous book, was published in 1859. Within 20 years it convinced most of the internaFonal scienFfic community that evoluFon was a fact.

Quotes from The Origin

  • f Species

In reference to natural selec.on: “I can see no limit to this power, in slowly and beautifully adapting each form to the most complex relations of life” Darwin’s ending paragraph: “…from so simple a beginning endless forms most beautiful and most wonderful have been, and are being evolved”

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The blobfish (Psychrolutes marcidus) is found at depths greater than 5000 m off the coast

  • f Australia and Tasmania. To remain

buoyant, the flesh of the blobfish is a gelaFnous mass with a density slightly less than water. This allows the fish to float above the sea floor without expending energy on

  • swimming. The relaFve lack of muscle is not

a disadvantage as it primarily swallows edible macer that floats by in front it (adult blobfish ~30 cm long). This crustacean invades a fishes mouth, devours its tongue, and takes the tongues place. It then acts like a tongue; the fish can use it to grip and swallow prey ‐ the parasite gets first dibs at the food. (From: Carl Zimmer, Parasite Rex, Simon & Schuster)

“I can see no limit to this power etc”

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“there are no limits” ‐ The water bear (Tardigrade) could easily survive on Mars and in the ice of Europa

TarFgrades are between 0.05 and 1.2 mm in length, have feet with claws like bears and walk like bears. They are found everywhere including hot springs, in a 5m layer of solid ice, on the top of the Himalayas, stone walls etc but mostly live in moss. They could survive on Mars because:

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The water bear is capable of surviving for more than 12 years in a completely dry state called the “tun” state or in “cysts”. In the “tun”state they will survive in liquid helium, absolute alcohol or even ether and

  • brine. Just add water and they come

back to life ‐ just like instant coffee

Dry form “tun” Asphyi.c state ‐O2 coming back to life

with addi.on of water

“gummy bear”

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SLIDE 10

41st Saas‐Fee course from Planets to Life 3‐9 April 2011

The “top down” approach to understanding the origin of life

  • Understanding the characterisFcs of the
  • rganisms close to the root of the tree

– Most are extremophiles (grow at high temperatures, high and low pH, high salt, etc)

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SLIDE 11

The Universal PhylogeneFc Tree: Origin of Life and EvoluFon ImplicaFons

What does this tree tell us about the evolu8on of organisms?

1. There are three domains of life 2. All extant life arose from a common ancestor 3. Bacteria and Archaea thought to be part of the same group of organisms (prokaryotes, Monera etc) are disFnctly different 7. The Eukarya evolved from the archaea 8. The deepest rooted organisms are thermophiles (hyperthermophiles)

  • 11. The proFsts are polyphyleFc (see

diplomonads and ciliates)

  • 12. The cyanobacteria (the mother of all
  • xygen producing photosyntheFc
  • ganisms) are not deeply rooted

Universal Phylogenetic Tree

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The microbial world, its limits and

  • ur search for life elsewhere

EXTREMOPHILES – Organisms that live in the most extreme environmental condiFons (Temperature, salinity, pH, pressure, radiaFon, heavy metals, low water acFvity, and combinaFon of extremes) Important note: There is sFll much we don’t understand about Earth life and the limits of evoluFon of carbon‐based life to live under extreme condiFons

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EvoluFonary innovaFons observed in Earth organisms

THERE IS STILL MUCH TO BE DISCOVERED

  • During the past 10 years the Census of Marine

Life has discovered thousands of new species of animals and plants

  • This is even more pronounced for marine

microorganisms and it is estimated that more than 99% of the microbes in the ocean are uncharacterized new species

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SLIDE 14

The microbial world, its limits and

  • ur search for life elsewhere

EXTREMOPHILES – Organisms that live in the most extreme environmental condiFons (Temperature, salinity, pH, pressure, radiaFon, heavy metals, low water acFvity, and combinaFon of extremes)

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Why study extremophiles?

  • Limits of carbon‐based life
  • Some extremophiles deeply rooted in global

phylogeneFc trees (parFcularly thermophiles)

  • The range of habitat condiFons for extremophiles

may be analogous to environmental condiFons on

  • ther planets and moons
  • Paleomicrobiology (metabolic history) and the

changing environmental condiFons throughout Earth history

  • “Top down” approaches to studying the origin of

life

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Parameter Extreme range on Earth Extreme level for growth

  • f organisms

Temperature

~-50 - >1200°C Lowest Temperature -15°C Highest Temperature - 122°C Eukaryotes to 62°C ;metazoans to ~50°C

pH

0 - 14 Bacteria, Archaea and fungi at pH 0 - 13

Water activity (Aw)

Distilled H2O to total dryness Highest salt - 35% NaCl (many microbes and animals can survive desiccation)

Radiation

Generally less than 1 kGy Some microbes survive levels 10X higher than found naturally on Earth

Heavy metals

Depends on environments and specific metals (>10mM) Bacteria and algae grow in 2-5mM Cd, Zn, Ni etc

Pressure

<1 to ~1,100 atm (subseafloor habitas possibly to >6 km in the crust) High diversity of bacteria, invertebrates and fish in ocean trenches

Limits of Life

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Limits: Some key environmental variables regulaFng life processes

  • Temperature and Pressure: Together they determine

the boundary condiFons for liquid water

  • Salinity: relates to the availability of water and in

combinaFon with pressure or low temperature can result in added stress to cells

  • pH: in most cases organisms evolve mechanisms to

maintain pH’s near neutrality inside the cell

  • Organic solvents: destroys lipid membranes
  • Other combina.ons: dryness, radiaFon, redox

condiFons, heavy metals, etc in combinaFon with T, P, S, and pH

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What are the limits for C‐based life?

Only temperature and availability of water limit Earth life

Note: toxic levels of metals, radiaFon, etc can kill life

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Enzyme acFvity in water/organic solvent mixture (Bragger et al., 2000)

(Modified from Deming and Eiken, 2007)

Temperature range for microbial growth and survival: 1. Microbial growth at ‐15°C and up to at least 122°C 2. Enzyme acFvity at low temperature depends on liquid solvent 3. Salts and extracellular polysaccharides (EPS) can protect cells; some hyperthermophiles have >4M K at high temperatures 4. Bacterial spores and vegetaFve cells have been observed from million year ice cores 5. Anaerobes including methanogens (along with methane) in ice cores 6. Anaerobic methane oxidizing archaea associated with methane hydrates

(122°C)

Maximum growth T for eukaryotes (70°C) Maximum growth T for metazoans (~50°C) Viable microbes observed at 250°C

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Temperature Classes of Microorganisms

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Hyperthermophile (Temp. OpFmum >80°C) – Early microbiology studies pioneered by Thomas Brock in the 1970’s

Boulder Spring, Yellowstone NaFonal Park

Octobus Springs, Yellowstone NaFonal Park (The site where Thermus aqua;cus was

  • isolated. T aqua;cus provides the

polymerize enxyme used in the Polymerase Chain ReacFon)

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Hydrothermal vents discovered 1977, black smokers, 1979

Juan deFuca Ridge – NE Pacific (2,500 m depth,

350°C hot fluid)

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Different Edifice Morphologies, Endeavour

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Highest Temperature Organism on Earth from Finn (Mothra) 2 m

Highest Temperature Organism on Earth from Finn

3 days growth 1.03 m

121°C organism grown under anaerobic condiFons with acetate, FeIII forms magneFte, doubles 24 hrs

Kashefi et al., Science 2003

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Pyrolobus fumarii* (Tmax = 113ºC, Topt= 106ºC,

Tmin= 90ºC)

A Pyrodic8um species has been described (Science 301:934, 2001) that can grow up to 121ºC, and a strain of Methanopyrus kandleri has been shown to grow up to 122ºC (PNAS 105:10949, 2008)

FISH staining of vent chimney TEM, P. fumarii cell

(Reinhard Rachel)

Red, Archaea; Green, Bacteria (Chris.an Jeanthon)

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Even hyperthermophiles have parasites

Nanoarchaeum Nanoarchaeum genome (PNAS 100:12984, 2003; J. Bacteriol. 190:1743, 2008)

  • a. Circular, 0.49 Mbp–smallest genome of any species of Archaea.
  • b. Contains no recognizable genes encoding biosyntheFc enzymes for

amino acids, nucleoFdes, or coenzymes.

  • c. Lacks genes encoding proteins for major catabolic pathways (e.g.,

glycolysis).

  • d. Missing genes for some ATPase subunits.
  • e. Most gene dense genome of any cell (99% of genes encode proteins).

Red, Nanoarchaeum Green, Ignicoccus 0.4 µm

Photos by Reinhard Rachel

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Problems Solutions

  • 1. Protein Denaturation

Heat-stable proteins; heat- shock proteins (chaperones)

  • 2. DNA Denaturation

Reverse DNA gyrase; introduces positive supercoiling into the chromosome, which raises the melting point; stabilizing proteins

  • 3. Membrane Melting

Tetra-ether lipid monolayer membranes; covalent bonds adjoining membrane halves resist membrane peeling

  • 4. Low Solubility of O2 at High Temperatures

Diverse anaerobic energy metabolisms; S0- and H2- based metabolisms

Hyperthermophiles: Overcoming the negaFve effects of high temperature

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Eukaryotes that live at high temperatures

  • Upper temperature for growth of a single‐cell

eukaryotes is 62°C (fungi)

  • Upper temperature for growth of a metazoan

is 50°C (polychaete worm from deep‐sea hydrothermal vents)

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Alvinella pompejana “Pompei worm” (A heat‐loving metazoan)

Size: up to 150 mm Distribu.on: East Pacific Rise from 21°N to 23°S Biology: Dwells inside organic tubes in acFve chimney walls. Temperature growth range 20‐50°C but can tolerate exposure to temperatures >100°C; Feeds on bacteria;

  • uter surface colonized by filamentous bacteria
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Inferno Palm worms – Axial Volcano

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Alvinella pompejana Worm

Photograph of a video taken from DSRV Alvin in hydrothermal vents at 21°N, East Pacific Rise, showing an Alvinella pompejana worm standing

  • n a substrate measured at 105°C.

Sketch to clarify the posiFon of the worm and the temperature probe

Nature 1992

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Alvinella pompejana (East Pacific Rise)

Scanning electron micrograph ‐ head size is 3 cm

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Cary et al., Nature 391:545‐546 (1998)

There is an ongoing “discussion” as to the upper temperature for growth

  • f the Alvinella worms that live on

acFve sulfide structures. This report by Cary and colleagues demonstrated that the rear part of the tube where Alvinella pompejana resides reaches temperatures close to 80°C. Some of the biochemistry data on these worms indicate that 40‐50°C may be the hocest temperature for these animals.It is clear, however, that Alvinella can survive exposure to temperatures approaching 100°C.

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Science 312:231 (2006)

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Schema.c of the thermal gradient aquarium. Chamber consisted of : (A) aluminum reinforcement plate; (B) clear polycarbonate window; (C) PEEK ouwlow tubing; (D) holes drilled into the block to within 2.5 mm of the slot containing animals for inserFon of temperature probe; (E) )‐ring face seal; (F) slot to contain animals; (G)PEEK inflow tubing; and (H) an anodized aluminum block with a slot to contain animals.

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SLIDE 36

DistribuFon of P. sulfincola and P. palmiformis worms in temperature‐gradient experiments. Worms were uniformly dispersed within the aquaria before establishing the temperature

  • gradient. (A to C) Plots of P. sulfincola

distribuFons over Fme within a 20° to 61°C gradient; N = 5, 9 and 4 individuals, respecFvely. (D) Plot of P. palmformis distribuFons over Fme within a 20° to 55°C gradient; N = 8 individuals.

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Scale Worm (Polychaete) living on the edge Juan deFuca Ridge NE Pacific (320°C fluid)

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(Deming, 2009)

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Psychrophiles

  • Lowest temperature for growth ‐12°C, acFve

metabolism <‐22°C.

  • Evidence for survival at temperatures as low

as ‐80°C (liquid nitrogen)

  • Spores found in ice cores that are >1 million

years old

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Psychrophiles: Tempmax < 20ºC

←Photos by Jim Staley→

Polaromonas Topt = +4ºC

Losest temperature for growth:

Psychromonas ingrahami Topt= +4°C, Tmin= –12°C, Tmax= +10°C

Marine sea ice

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Cultured phage‐bacterial host systems acFve at –1°C

Middelboe et al., 2002 (seawater) Borriss et al., 2003 (sea ice) Wells and Deming, 2006 (both)

Colwellia psychrerythraea strain 34H

3 µm 3 µm 3 µm

(Borriss et al., 2003) (Wells and Deming, 2006)

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Problems and Solutions: Psychrophiles

Problems

Prevent ice-crystal formation and cell death Enable protein activity: enzymes must maintain significant catalytic activity at low temperature Maintain membrane function: the

  • rganism must maintain

significant levels of nutrient transport at low temperature

Solutions

Live in a briny habitat, produce compatible solutes and/or exopolysaccharides (EPS) Make more flexible proteins (higher α-helix; lower β- sheet content) Make more polar and less hydrophobic proteins, with fewer weak bonds (ionic, hydrogen) Make lipids with greater content

  • f short-chained, branched,

and unsaturated fatty acids

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The Antarc;c ice‐fish (Channichthyidae) are the only known vertebrates without

  • hemoglobin. Consequently, their blood is transparent. Their metabolism relies on the
  • xygen dissolved in the liquid blood and is absorbed directly through the skin from the
  • water. This works because of the increased solubility of oxygen in cold water and is an

adaptaFon to life at temperatures that are less than 0°C (icefish size 25 cm long) (Wikipedia)

“I can see no limit to this power

etc” (Darwin referring to natural selecFon”

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Summary – Temperature and life

  • To date, the lowest temperature for growth is

‐12°C and the maximum temperature for growth is 122°C

  • Low temperature microbes (psychrophiles) do

not have ancient lineages

– Spore‐forming psychrophilic bacteria are of concern regarding planetary protecFon issues to icy planetary bodies

  • High temperature microbes (hyperthermophiles)

have ancient lineages

– Hyperthermophiles are of interest regarding the origin

  • f life and the origin of metabolism and eukaryotes

– The highest temperature for growth of a eukaryote is >60°C lower than the maximum temperature for a microbe