Lesson 7: Origins of Life on Earth

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16 Terms

1
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Spontaneous Generation

Belief that life arises regularly from non-life.

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Biogenesis

Life only comes from lifeand cannot arise from non-living matter.

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Earth’s formation

4.6bya

Condensing from vast cloud of dust and rocks that surrounded the sun

  • No life yet and was bombarded with ice and rocks

  • the heat from collision so intense, water was evaporated from ice


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The first atmosphere formation

3.9bya

  • Reducing atmosphere (no oxygen O2)

  • lots of water vapour and the compounds of volcanic eruptions, (N2, CO2, CH4,NH3,H2,H2S)

  • Earth started to cool, oceans formed as water vapour condensed, most H2 escaped to space


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The Theory of the Origin of Life

  1. Abiotic (non-living) synthesis of small organic molecules

  2. Synthesis of monomers into polymers (macromolecules)

  3. Packaging of molecules into protocells → first membrane bonded vesicles

  4. origin of self-replicating molecules


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Abiotic synthesis of small organic molecules

The spontaneous formation of organic monomers from inorganic compounds without the presence of living organisms.

  • Key conditions: Required inorganic gases (H2OH2​O, CH4CH4​, NH3NH3​, H2H2​) and energy from volcanic activity, lightning, or UV radiation

  • Experimental support: The Miller-Urey experiment demonstrated that amino acids and other organic compounds could form under simulated early-Earth conditions

  • Proposed locations: reducing atmosphere and deep-sea volcanic vents, and meteorites


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Synthesis of monomers into polymers (macromolecules)

  • Dripping amino acids (liquid form) or RNA nucleotides onto hot rocks/sand → molecules would spontaneously form polymers

    • Polymers were not the complex organic molecules in present day, but could function as a protein as catalyst for chem rxn


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Packaging of molecules into protocells

The process by which organic molecules aggregate to form enclosed structures resembling cells (protocells), allowing for internal environments to develop. These protocells may have provided a platform for biochemical reactions leading to more complex life forms.

  • vesicles can reproduce and divide on their own

  • can grow without diluting their contents

  • can absorb montmorillonite (clay produced from weathered volcanic ash) particles which may contain RNA

  • Some can perform metabolic reactions using external source (hot rocks) of reactants


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Origin of self-replicating molecules

  • First genetic material is RNA (less stable), NOT DNA

  • Ribozymes (basic RNA) can catalyze chem rxn

  • An RNA world existence for a long time in which small RNA molecules were able to replicate and store info about the vesicles that carried them

  • Eventually DNA produced → MORE STABLE molecule


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Prokaryotes origin time

3.9 bya

  • first single celled organisms


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When the first real evidence of prokaryotes in Fossil Record appeared

3.5 bya - 2.1 bya

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Time period when beginning of Oxidized atmosphere → reducing atmosphere changing

2.7 bya

  • Oxy increased in water due to cyanobacteria spitting water molecules during photosynthesis

  • Oxy reacts with dissolved iron, creating rust in ocean sediments and leading to a significant increase in atmospheric oxygen.


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Eukaryotes appearance time period

2.1bya LOTS OF PROKARYOTES DIED OFF

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Where did Eukaryotes come from?

  • Endosymbiont theory suggests that eukaryotes originated from symbiotic relationships between different species of prokaryotes, where certain prokaryotic cells engulfed others but did not digest them, leading to a mutualistic relationship.


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Multicellular Organisms time period

1.2 bya → when multicellular organisms first appeared on Earth, marking a significant evolution in complexity.

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Larger multicellular organisms appearance time

575 mya