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Origin of Life Hypotheses
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I. Earth History 4.5 bya: Earth Forms
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I. Earth History - Earliest Atmosphere - probably of volcanic origin Gases produced were probably similar to those created by modern volcanoes (H2O, CO2, SO2, CO, S2, Cl2, N2, H2) and NH3 and CH4
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I. Earth History 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks
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I. Earth History 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.5 bya: Oldest Fossils
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I. Earth History 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.5 bya: Oldest Fossils Stromatolites - communities of layered 'bacteria'
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I. Earth History bya: Oxygen in Atmosphere 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.4 bya: Oldest Fossils
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I. Earth History bya: Oxygen 1.8 bya: first eukaryote 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.4 bya: Oldest Fossils
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I. Earth History bya: Oxygen 1.8 bya: first eukaryote 0.9 bya: first animals 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.4 bya: Oldest Fossils
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I. Earth History bya: Oxygen 1.8 bya: first eukaryote 0.9 bya: first animals 0.5 bya: Cambrian 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.4 bya: Oldest Fossils
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I. Earth History bya: Oxygen 1.8 bya: first eukaryote 0.9 bya: first animals 0.5 bya: Cambrian 0.24 bya:Mesozoic 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.4 bya: Oldest Fossils
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I. Earth History bya: Oxygen 1.8 bya: first eukaryote 0.9 bya: first animals 0.5 bya: Cambrian 0.24 bya:Mesozoic 0.065 bya:Cenozoic 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.4 bya: Oldest Fossils
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I. Earth History 4.5 million to present (1/1000th of earth history) bya: Oxygen 1.8 bya: first eukaryote 0.9 bya: first animals 0.5 bya: Cambrian 0.24 bya:Mesozoic 0.065 bya:Cenozoic 4.5 bya: Earth Forms 4.0 bya: Oldest Rocks 3.4 bya: Oldest Fossils
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II. Origin of Life Hypotheses
- Oparin-Haldane Hypothesis (1924): - in a reducing atmosphere, biomonomers would form spontaneously Aleksandr Oparin ( ) J.B.S. Haldane ( )
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II. Origin of Life Hypotheses
- Oparin-Haldane Hypothesis (1924): - in a reducing atmosphere, biomonomers would form spontaneously - Miller-Urey (1953) all biologically important monomers have been produced by these experiments, even while changing gas composition and energy sources
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II. Origin of Life Hypotheses
- Oparin-Haldane Hypothesis (1924): - in a reducing atmosphere, biomonomers would form spontaneously - Miller-Urey (1953) - Sydney Fox polymerized protein microspheres
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II. Origin of Life Hypotheses
- Oparin-Haldane Hypothesis (1924): - in a reducing atmosphere, biomonomers would form spontaneously - Miller-Urey (1953) - Sydney Fox polymerized protein microspheres - Cairns-Smith ( ) - clays as templates for non-random polymerization Murcheson meteorite - amino acids present; some not found on Earth. To date, 74 meteoric AA's. Szostak - clays could catalyze formation of RNA's
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III. Acquiring the Characteristics of Life
A. Three Primary Attributes: - Barrier (phospholipid membrane) - Metabolism (reaction pathways) - Genetic System
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III. Acquiring the Characteristics of Life
B. Barrier (phospholipid membrane) - form spontaneously in aqueous solutions
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A B C D E III. Acquiring the Characteristics of Life
C. Metabolic Pathways - problem: how can pathways with useless intermediates evolve? These represent 'maladaptive valleys', don't they? A B C D E How do you get from A to E, if B, C, and D are non-functional?
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A B C D E III. Acquiring the Characteristics of Life
C. Metabolic Pathways - Solution - reverse evolution A B C D E
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E III. Acquiring the Characteristics of Life C. Metabolic Pathways
- Solution - reverse evolution suppose E is a useful molecule, initially available in the env. E
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E III. Acquiring the Characteristics of Life C. Metabolic Pathways
- Solution - reverse evolution suppose E is a useful molecule, initially available in the env. As protocells gobble it up, the concentration drops. E
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D E III. Acquiring the Characteristics of Life C. Metabolic Pathways
- Solution - reverse evolution Anything that can absorb something else (D) and MAKE E is at a selective advantage... D E
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D E III. Acquiring the Characteristics of Life C. Metabolic Pathways
- Solution - reverse evolution Anything that can absorb something else (D) and MAKE E is at a selective advantage... but over time, D may drop in concentration... D E
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C D E III. Acquiring the Characteristics of Life C. Metabolic Pathways
- Solution - reverse evolution So, anything that can absorb C and then make D and E will be selected for... C D E
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A B C D E III. Acquiring the Characteristics of Life
C. Metabolic Pathways - Solution - reverse evolution A B C D E and so on until a complete pathway evolves.
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