Course review

A2.1 Origins of cells

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A2.1.1—Conditions on early Earth

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• Early Earth had volcanic gases, high CO₂, methane, water vapour, and little free oxygen • Lack of ozone allowed intense UV radiation at Earth's surface • Prebiotic chemistry may have formed amino acids, bases, sugars, fatty acids, and nucleotides

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A2.1.2—Cells as smallest units of life

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• Cells are self-sustaining units with membranes, genetic material, and metabolism • Life requires heredity, variation, compartmentalization, and Darwinian evolution • Viruses contain genetic material but lack independent cellular metabolism

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A2.1.3—Spontaneous origin of cells

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• First cells had to arise from non-living materials by self-assembly • Required steps include organic synthesis, polymerization, self-replication, and membranes • Competing hypotheses include protocell-first, gene-first, and metabolism-first models

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A2.1.4—Evidence for origin of carbon compounds

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• Miller-Urey produced amino acids from methane, ammonia, hydrogen, and water vapour • Later experiments used different gases and energy sources, including UV and ionizing radiation • Results support abiotic synthesis of amino acids, fatty acids, sugars, bases, and simple polymers

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A2.1.5—Spontaneous formation of vesicles

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• Amphipathic fatty acids can spontaneously form monolayers, bilayers, and vesicles • Microspheres could enclose polymers and monomers, creating internal chemistry • Fatty acids likely preceded more complex phospholipid membranes

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A2.1.6—RNA as presumed first genetic material

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• RNA can store genetic information and fold into catalytic ribozymes • RNA world hypothesis proposes RNA acted before DNA and protein enzymes • Evidence includes ribosomal RNA catalysis, RNA primers, and ribose forming under prebiotic conditions

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A2.1.7—Evidence for last universal common ancestor (LUCA)

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• LUCA links the abiotic phase of Earth history to all later cellular life • Universal genetic code, shared biochemistry, and conserved genes support common ancestry • Genomic studies found shared gene families likely inherited from LUCA

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A2.1.8—Dating first cells and LUCA

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• Fossils and surrounding rocks can be dated by radiometric methods • Molecular clocks use DNA or protein changes to estimate divergence times • LUCA may have existed around 4 billion years ago

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A2.1.9—Evolution near hydrothermal vents

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• Nuvvuagittuq haematite tubes provide fossil evidence from ancient hydrothermal vents • Conserved genes suggest LUCA was anaerobic, CO₂-fixing, H₂-dependent, N₂-fixing, and thermophilic • Hydrothermal vents supplied hydrogen, carbon dioxide, iron, heat, and chemosynthetic energy

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