G4 Earth Evolution: Life Lecture 1: Origin of life and complex life. Myth marketing and hype. Lecture 2: Proterozoic life and metazoans Lecture 3: The

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G4 Earth Evolution: Life Lecture 1: Origin of life and complex life. Myth marketing and hype. Lecture 2: Proterozoic life and metazoans Lecture 3: The Phanerozoic record and exceptional preservation Lecture 4: Effects of life on Earth and non-Uniformitarianism Slide 2 Lecture 1: Origin of life and complex life. Myth marketing and hype. 1. What can be known about the evolution of life? 2. Establishing a list of events 3. Establishing a possible chronology 4. Archaean life 5. Evolution of complexity Slide 3 1. What can be known about the evolution of life? Lazcano, 2001 Of necessity, work on the origin of life should be regarded as enquiring and explanatory rather than definitive and conclusive .the issue should be addressed conjecturally in an attempt to construct a coherent historical narrative. Hence influenced by scientific and cultural fashions, for example, the possibility of life originating on Mars early heterotrophy in a Dog-eat-Dog social climate. Is a scientist allowed to not know something? Slide 4 2. Establishing a list of events Assumed steps Common ancestor to all modern life DNA based Evidence or reasoning DNA sequencing Slide 5 2. Establishing a list of events Assumed steps Darwins warm little pond Common ancestor to all modern life DNA based Evidence or reasoning Oparin and Haldanes theories, 1920s Miller experiments (eg 1993) - electrical discharges for 1 week over a mixture of CH 4, NH 3, H 2 and H 2 O produced organic molecules including amino acids and urea. Importance of HCN - polymers denature to produce amino acids, purines, and adenine. Evidence from the Murchison Meteorite - 4.6 Ga, includes array of protein and non-protein amino acids, purines, pyramidines, hydrocarbons and evidence of liquid water. Slide 6 2. Establishing a list of events Assumed steps Darwins warm little pond Common ancestor to all modern life DNA based Evidence or reasoning Oparin and Haldanes theories, 1920s Miller experiments (eg 1993) - electrical discharges for 1 week over a mixture of CH 4, NH 3, H 2 and H 2 O produced organic molecules including amino acids and urea. Importance of HCN - polymers denature to produce amino acids, purines, and adenine. Evidence from the Murchison Meteorite - 4.6 Ga, includes array of protein and non-protein amino acids, purines, pyramidines, hydrocarbons and evidence of liquid water. Most primitive modern organisms are hyperthermophiles However, rapid decay of most organic molecules at high temperatures makes this unlikely for the pond. Slide 7 2. Establishing a list of events Assumed steps Darwins warm little pond Appearance of anaerobic heterotrophs using surrounding molecules for growth and reproduction Common ancestor to all modern life DNA based Evidence or reasoning Heterotrophs chemically simple, but need a convincing method of carrying information through time. RNA? But ribose and phosphate esters chemically unlikely in chemical soup. Maybe modified nucleic acid sugar- phosphate backbones, maybe another self-replicating molecule, maybe something like prions. Slide 8 2. Establishing a list of events Slide 9 Assumed steps Darwins warm little pond Appearance of anaerobic heterotrophs using surrounding molecules for growth and reproduction Transition to RNA world Common ancestor to all modern life DNA based Evidence or reasoning RNA is catalytic and encoding. Used in primitive reproduction today. Slide 10 2. Establishing a list of events Assumed steps Darwins warm little pond Appearance of anaerobic heterotrophs using surrounding molecules for growth and reproduction Transition to RNA world Darwinian evolution towards dominance of DNA Common ancestor to all modern life DNA based Evidence or reasoning This is what we see today. Better fidelity of information carriage Slide 11 2. Establishing a list of events Assumed steps Darwins warm little pond Appearance of anaerobic heterotrophs using surrounding molecules for growth and reproduction Transition to RNA world Darwinian evolution towards dominance of DNA Evolution of primitive cells Common ancestor to all modern life DNA based Evidence or reasoning Margulis minimum cell. Slide 12 2. Establishing a list of events Assumed steps Darwins warm little pond Appearance of anaerobic heterotrophs using surrounding molecules for growth and reproduction Transition to RNA world Darwinian evolution towards dominance of DNA Evolution of primitive cells Evolution of autotrophy Common ancestor to all modern life DNA based Evidence or reasoning Necessary for sustainability. Most primitive life does it. Slide 13 2. Establishing a list of events Assumed steps Darwins warm little pond Appearance of anaerobic heterotrophs using surrounding molecules for growth and reproduction Transition to RNA world Darwinian evolution towards dominance of DNA Evolution of primitive cells Evolution of autotrophy Common ancestor to all modern life DNA based Evidence or reasoning All molecular trees show a single, common root to the tree of life. Slide 14 3. Establishing a possible chronology Assumed steps Darwins warm little pond Appearance of anaerobic heterotrophs using surrounding molecules for growth and reproduction Transition to RNA world Darwinian evolution towards dominance of DNA Evolution of primitive cells Evolution of autotrophy Common ancestor to all modern life DNA based Evidence or reasoning During and after meteorite bombardment. Murchison Meteorite - 4.6 Ga After 3.8 Ga . .. . Carbon isotopes go light very early - around 3.8 Ba. Stromatolites. (Oldest fossils disputed, oldest definite fossils 2.5 Ba from Transvaal Supergroup) Slide 15 3. Establishing a possible chronology Slide 16 4. Archaean life Slide 17 Lecture 2: Proterozoic life and metazoans 1. Prokaryotes and eukaryotes 2. Evolution of eukaryotes 3. Eukaryote radiations 4. Evolution of metazoans 5. PreCambrian-Cambrian boundary Slide 18 1. Prokaryotes and eukaryotes Slide 19 2. Evolution of eukaryotes Slide 20 3. Eukaryotic radiations Biologically: probably split off at 3.5 Ba Palaeontologically: oldest ?2.1 Ba from Michigan BIF large cells common since 2 Ba Acritarchs: unequivocal eukaryotes, probably dinoflagellate cysts from 1.7 Ba common from 1 Ba Slide 21 4. Origin of metazoans Slide 22 Slide 23 5. The PreCambrian-Cambrian boundary Slide 24