FINAL Week 8 Microbial Evolution, Biogeochem and Elemental Cycles Flashcards

1
Q

Metabolic phenotype of first primitive cells

A
  1. Strictly Anaerobes (fermentation of anaerobic respiration)
  2. Chemolithotrophic or methanogenic
  3. Inhospitable surface conditions –> may have lived on subsurface habitats
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2
Q

Deep Ocean Hydrothermal Vent Hypothesis

A
  1. Supply of reduced inorganic compounds (e- donors)
    > AA, nitrogen bases, sugars react within carbonaceous silicate and clay mound matrix
  2. Mineral rich (metals, elements, nutrients)
    > Fe3+, H+, Ni2+, CO2, PO4, Fe2+ and macromolecules&cofactors from prebiotic soup emerge to support DNA/RNA/proteins
  3. Minerals, pH and redox –> biological molecule formation
    > Divergence of bacteria and archaea and global dispersal to new habitats/cell wall biochem/lipid biosynthesis
  4. Primordial catalytic RNA
    > LUCA: organization into self-inclosed micelle structure
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3
Q

Microbial Life on Early Earth

A
  1. Stromatolites from ancient anoxygenic phototrophic microbes (green non-sulfur)
  2. Banded iron formation:
    > evidence for atmospheric oxygenation (Cyanobacteria)
    > Dark bands: Fe3+ oxides; O2 is then free to accumulate in air

**Later: Populations –> guilds –> communities
> Species composition of habitat (niche) determined by redox material, nutrient and physical property availability

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4
Q

Organo-lithotrophic redox cycling
d = donor
a = acceptor

A
  1. Chemorgano:
    » CH2O (d) –> CO2
    » NO3, Mn(IV), Fe(III) (a) –> NH4, Mn(II), Fe(II) (d)
  2. Chemolitho:
    » Opposite for 2nd one
    » O2, NO3, Mn(IV) (a) –> H2O, N2, Mn(I), H+ (d)
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5
Q

Global Carbon Cycle

A
  1. Majority CO2 release from microbial decomposition
  2. Net CO2 fixation (photosynthesis) and respiration
    > Major sources from Earth’s crust, soils, oceans and fossil fuels
    > Keeling Curve: increase in CO2 proportional to increase in temperature
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6
Q

Paper #2: Microbial Nanowires

A

Electrically conductive bacteria by Shewanella oneidensis strain MR-1
> Less microbial culture formation in excess e- acceptor culture, but more in limited culture
> Nutrients have to be in close proximity for microbes to take in via motility, but nanowires make it easier (usually patchily distributed and soluble)
> Pili-like appendages: proteinaceous EC filament; current ACROSS nanowires (not along) measured via Scanning Tunnel Microscopy (STM) and contacting with nanofabricated Pt electrodes

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7
Q

Nanowire: more EC e- transfer

A
  1. Provide Silica Hydrous Ferric oxide (solid Fe3+) as e- acceptor (metal reducing)
    > Reduction produces nanocrystalline magnetite (Fe3O4)
    > Genetic basis: decaheme c-type cytochrome (ETC)
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