ORIGIN OF LIFE L4 Flashcards

I. Process of abiogenesis - CC requirements for life - CC abiotic synthesis hypothesis - SEQ abiogenesis II. History of life - SEQ timeline of life on earth

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1
Q

process of abiogenesis

A
  1. abiotic synthesis of monomers
  2. formation of organic macromolecules
  3. formation of protocells
  4. appearance of self replication
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2
Q

abiotic synthesis

A
  • first life developed from non living organic molecules

- those molecules had to form spontaneously

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3
Q

requirements for abiotic synthesis

A
  1. low O2
    - oxygen is reactive - breaks bonds
    - only forms 2 bonds - not conducive to building
  2. energy source
    - forming biological molecules - making bonds
    - making bonds = storing energy
  3. chemical building blocks
    - liquid water
    - dissolved inorganic molecules - ions
    - atmospheric CO2, H2O, CO, H2, N2
    - maybe NH3, H2S, CH4
  4. time
    - spontaneous chemical reactions are slow
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4
Q

Opain-Haldane hypothesis

A
  • life formed near earths surface - shallow water
  • tested using Miller-Urey experiment: found amino acids and other organic compounds, and more recently they found there were many molecules produced like DNA/RNA nucleic acid bases, all amino acids, several lipids and sugars, and ATP if phosphate is added
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5
Q

iron-sulfer world hypothesis

A
  • organic molecules at hydrothermal vents
  • hot H2O, CO, iron and nickel sulfides released
  • hot springs produce precursors to biological molecules
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6
Q

formation of organic macromolecules

A
  • can form on clay or rock surfaces
  • negative ions bind monomers
  • Zn, Fe catalyze polymerization
  • experimentally: polypeptides, polynucleotides, vesicles
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7
Q

formation of protocells

A
  • vesicle: fluid filled compartment surrounded by membrane like structure
  • forms from lipids in water
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8
Q

protocells

A
  • aggregates of abiotically produced organic macromolecules
  • exhibit attributes of living cells
  • electrical potential across surface
  • absorb materials leads to osmotic swelling
  • unique internal chemical environment
  • divide if sufficiently large
  • no mechanism of heredity
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9
Q

self replication

A
  • in living cells: genetic info stored in DNA, transmitted via mRNA, translated into protein
  • DNA then RNA then protein
  • thought that RNA was the first nucleic acid in living things
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10
Q

RNA world hypothesis

A
  • the first cells used RNA to store and copy genetic info

- DNA and proteins incorporated later

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11
Q

ribozymes

A
  • RNA molecules with enzymatic properties

- cleave RNA, catalyze RNA polymerization

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12
Q

protocells and self-replicating RNA

A
  • RNA polymers within vesicle leads to higher osmotic pressure which makes the vesicle grow
  • growing vesicles take up lipids, RNA from environment/other vesicles
  • RNA inside gets rewritten then vesicle continues to grow and eventually splits
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13
Q

DNA

A
  • thought that RNA came first - single stranded (ss)
  • became double stranded (ds) - more stable, better for storage
  • replaced by DNA - even more stable, better for storing over time
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14
Q

geological time scale

A
  • established via fossils, radiometric dating
  • based on major geologic climate and biological events
  • ex. mass extinctions often delineate periods
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15
Q

first cells

A
  • prokaryotes: no nucleus
  • anaerobic
  • heterotrophic
  • obtained organic molecules from environment
  • fermentation (how they got energy): no O2 required, relatively low yield
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16
Q

autotrophs

A
  • appeared after first cells
  • use energy from sunlight - made own food
  • 1st released S2
  • later released O2 by splitting H2O (cyanobacteria)
17
Q

oxygen apocalypse

A
  • 2.5 bya
  • rise in atmospheric O2 due to oxygenic photosynthesis
  • killed off most organisms
  • aerobes took over: dealt with O2 via aerobic respiration, higher ATP yield, common today
18
Q

eukaryotes

A
  • cells with membrane bound nucleus and organelles
  • appeared at least 1.8 bya
  • generated through endosymbiosis
  • all have mitochondria
19
Q

mitochondria and plastids

A
  • double membranes
  • similar size, enzymes, ribosomes to bacteria
  • DNA, sequences very similar to living bacteria
  • divide via binary fission
20
Q

multicellularity

A
  • 1.2 bya, may have been present
21
Q

Cambrian radiation

A
  • 40 million years
  • most extant animal groups appeared in fossil record
  • during Cambrian period: 542-488 mya
  • all in ocean
22
Q

colonization of land

A
  • 500 mya
  • plants and fungi first, animals later
  • adaptations to prevent desiccation