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Chapter 25 ~ The History of Life on Earth

Chapter 25 ~ The History of Life on Earth. “…sparked by just the right combination of physical events & chemical processes…”. The Origin of Life is Hypothesis. Special Creation Was life created by a supernatural or divine force? not testable Extra-terrestrial Origin

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Chapter 25 ~ The History of Life on Earth

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  1. Chapter 25 ~ The History of Life on Earth • “…sparked by just the right combination of physical events & chemical processes…”

  2. The Origin of Life is Hypothesis • Special Creation • Was life created by a supernatural or divine force? • not testable • Extra-terrestrial Origin • Was the original source of organic (carbon) materials comets & meteorites striking early Earth? • testable • Spontaneous Abiotic Origin • Did life evolve spontaneously from inorganic molecules? • testable

  3. Conditions on early Earth • Reducing atmosphere • water vapor (H2O), CO2, N2, NOx, H2,NH3, CH4, H2S • lots of available H & its electron • no free oxygen • Energy source • lightning, UV radiation, volcanic low O2 = organic molecules do not breakdown as quickly What’s missingfrom thatatmosphere?

  4. Electrodes discharge sparks (lightning simulation) Water vapor Mixture of gases ("primitive atmosphere") Condenser Water Condensed liquid with complex, organic molecules Heated water ("ocean") Origin of Organic Molecules • Abiotic synthesis • 1920Oparin & Haldane propose reducing atmosphere hypothesis • 1953Miller & Ureytest hypothesis • formed organic compounds • amino acids • adenine CH4 H2 NH3

  5. Stanley Miller University of Chicago produced -amino acids -hydrocarbons -nitrogen bases -other organics Why was this experimentimportant??!

  6. The Origin of Life The 4-stage Origin of life Hypothesis: • 1- Abiotic synthesis of organic monomers • 2- Polymer formation • 3- Origin of Self-replicating molecules • 4- Molecule packaging (“protobionts”)

  7. Key Events in Origin of Life • Origin of Cells (Protobionts) • lipid bubbles  separate inside from outside  metabolism & reproduction • Origin of Genetics • RNA is likely first genetic material • multiple functions: encodes information (self-replicating), enzyme, regulatory molecule, transport molecule (tRNA, mRNA) • makes inheritance possible • makes natural selection & evolution possible • Origin of Eukaryotes • endosymbiosis

  8. The fossil record • Sedimentary rock: rock formed from sand and mud that once settled on the bottom of seas, lakes, and marshes • Dating: • 1- Relative~ geologic time scale; sequence of species • 2- Absolute~ radiometric dating; age using half-lives of radioactive isotopes

  9. Timeline • Key events in evolutionary history of life on Earth • 3.5–4.0 bya:life originated • 2.7 bya:free O2 = photosynthetic bacteria • 2 bya:first eukaryotes

  10. First Eukaryotes ~2 bya • Development of internal membranes • create internal micro-environments • advantage: specialization = increase efficiency • natural selection! nuclear envelope endoplasmicreticulum (ER) plasma membrane infolding of theplasma membrane nucleus DNA cell wall plasma membrane Prokaryotic cell Prokaryotic ancestor of eukaryotic cells Eukaryotic cell

  11. 2nd Endosymbiosis Eukaryotic cell with mitochondrion • Evolution of eukaryotes • origin of chloroplasts • engulfed photosynthetic bacteria, but did not digest them • mutually beneficial relationship • natural selection! photosyntheticbacterium chloroplast mitochondrion Endosymbiosis Eukaryotic cell with chloroplast & mitochondrion

  12. Lynn Margulis Theory of Endosymbiosis • Evidence • structural • mitochondria & chloroplasts resemble bacterial structure • genetic • mitochondria & chloroplasts have their own circular DNA, like bacteria • functional • mitochondria & chloroplasts move freely within the cell • mitochondria & chloroplasts reproduce independently from the cell

  13. Cambrian explosion • Diversification of Animals • within 10–20 million years most of the major phyla of animals appear in fossil record 543 mya

  14. Biogeography: the study of the past and present distribution of species • Pangaea-250 mya √ Permian extinction • Geographic isolation-180 mya √ African/South American reptile fossil similarities √ Australian marsupials

  15. Mass extinction • Permian(250 million years ago): 90% of marine animals; Pangea merge • Cretaceous(65 million years ago): death of dinosaurs, 50% of marine species; low angle comet

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