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Explore the historical experiments of Redi, Spallanzani, and Pasteur that debunked the concept of spontaneous generation and introduced the theory of biogenesis. Learn about the Earth's formation and evolution, from organic compounds to cell-like structures. Watch the educational video for a comprehensive understanding of life's origin and evolution on our planet.
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Origin of Life • Biogenesis • Earth’s History • The First Life-forms
Biological Evolution • To View Video: • Move mouse cursor over slide title-link • When hand appears, click once • ASX Video plays about 20 min • A 10 Question Video Quiz is included in the presentation
Biogenesis • The Concept of Spontaneous Generation • Redi’s Experiment • Spallanzani’s Experiment • Pasteur’s Experiment
Learning Objectives • TSW… • Define spontaneous generation, & list some of the observations that led people to think that life could arise from nonliving things • Summarize the results of experiments by Redi & by Spallanzani that tested the hypothesis of spontaneous generation • Describe how Pasteur’s experiment disproved the hypothesis of spontaneous generation
Spontaneous Generation • Concept that living things could arise from non-living things • Examples • Maggots appear on rotting meat • Fish & tadpoles appear in formerly dry ponds • Biogenesis • All living things arise from other living things • Cell theory
Redi’s ExperimentFrancesco Redi (1626 – 1697) • Problem • How do maggot life arise in rotting meat? • Observation • Flies land on rotting meat • Maggots appear in rotting meat • Hypothesis • Maggots arise from the eggs of flies
Redi’s Experiment:1668 • Investigation • Control group – meat in open jars: exposed to flies • Experimental group – meat in muslin sealed jars: no contact w/ flies • Data • Meat in open jars – developed maggots • Meat in sealed jars – no maggots appear • Conclusion • Maggots hatch from fly eggs laid on rotten meat • Criticism • Did not address microorganisms
Spallanzani’s ExperimentLazzaro Spallanzani (1729 – 1799) • Problem • Where do microorganisms come from? • Observation • Broth exposed to air develops microorganisms & spoils • Microorganisms can be carried into the air on dust • Hypothesis • Microorganisms arise from other microorganisms
Spallanzani’s Experiment:1768 • Investigation • Control group – boiled broth left in open flask: exposed to dustin air • Experimental group – boiled broth in sealed flask: no exposure to dust • Data • Broth in open flasks – developed microbes • Broth in sealed flasks – no microbes appear • Conclusion • Microorganisms arise from other microorganisms • Criticism –Sealed flasks deprived of a vital force
Pasteur’s ExperimentLouis Pasteur (1822 – 1895) • Problem • Where do microorganisms come from? • Observation • Broth exposed to air develops microorganisms & spoils • Microorganisms can be carried into the air on dust • Hypothesis • Microorganisms arise from other microorganisms
Pasteur’s Experiment:1859 • Investigation • Control group – boiled broth left in open curve-necked flask: dustin air is trapped by neck • Experimental group – boiled broth is exposed by breaking necks: exposure to dust • Data • Broth in open flasks – developed no microbes for 1 year • Broth in flasks w/ broken neck – microbes appear right away • Conclusion • Microorganisms arise from other microorganisms • No Criticism – Vital force concept abandoned
Earth’s History • The Formation of the Earth • The First Organic Compounds • From Molecules to Cell-like Structures
Learning Objectives • TSW… • Outline the modern scientific understanding of the formation of Earth • Summarize the concept of half-life • Describe the production of organic compounds in the Miller-Urey experiments • Summarize the possible importance of cell-like structures produced in the laboratory
The Formation of the Earth • 5 by – Solar system is swirling mass of gas & dust • Inward collapse of most material: sun forms • Planets form from remainder • 4.6 by – Earth formed • 400 million year period of collisions of planetesimals • Earth is molten due to release of heat energy from collisions • Evidence from moon rocks & meteorites
Earth’s AgeVolcanism • 4 by – Planetesimal collisions subside • Volcanic activity begins to form primitive atmosphere • 3.8 by – Oldest known Earth rocks • Ancient atmosphere is neither oxidizing nor reducing • Gasses: CO2; N2; H2O vapor
Earth’s AgeLava Flow • 3.2 by – Earth cools as collisions & volcanic activity subside • Atmosphere forms from out gassing from rocks & gas capture • Oceans form from condensation of H2O from cooling surface & comet capture • 2.2 by – Earth has continents & oceans like today • Ancient atmosphere is neither oxidizing nor reducing • Gasses: CO2; N2; H2O vapor
Radioactive Dating • # Protons (p+) – constant for each element • Atomic number • Examples: C = 6; H = 1 • # Neutrons (n0) – variable for each element • Atomic mass number = #p+ + #n0 • Examples: C may be 12C, 13C, or 14C; H may be 1H, 2H (deuterium), or 3H (tritium)
Radioactive Dating • Radioactive isotopes – radioisotopes • Elements w/ unstable nuclei that undergo radioactive decay– particles are released • Half-life • Length of time for ½ of any sample of a radioisotope to decay • Half-life can vary from a fraction of a second to billions of years • Used inabsolute dating • Specific time of existence
Dating with Index Fossils • Index fossils • Extinct wide-spread species whose fossils can be found all over the world • Usually marine organisms • Carried world wide on ocean currents • Used inrelative dating • Fossils of a species found & dated in one region of the Earth are assumed to be the same relative age as those of the same species found in another region Extinct brachiopods
Experimental Synthesis: Organic Compounds • Miller-Urey Experiment (1953) • Tested Oparin’s hypothesis • Circulated H2O vapor & other gasses through chamber w/ electric sparking device • Condensed vapor into liquid water • Analyzed condensate for organic compounds • Results • Some amino acids & other organic compounds formed
Miller-Urey Experiment • To View Video: • Move mouse cursor over slide title-link • When hand appears, click once • ASF Video plays about 3 min
Experimental Synthesis: Organic Compounds • Further Experiments (1960s-1980s) • Tested Oparin’s hypothesis • Used a variety of gasses • Used a variety of energy sources • Results • All 20 amino acids • Simple mono- & di-saccharides • Fatty acids • ATP • RNA & DNA nucleotides
Modern StudiesSuggest Thermal Vents • Further Experiments (1990s) • Ancient atmosphere neither reducing nor oxidizing • Gasses: CO2; N2; H2O vapor • Energy sources: hot minerals • Synthesis of organics– near undersea erupting volcanoes or thermal vents • Rich in sulfur & iron compounds • Reducing conditions – H2S
Life at Hydrothermal Vents • To View Video: • Move mouse cursor over slide title-link • When hand appears, click once • ASF Video plays about 5 min
Organic Compounds from Beyond Earth • Organic compounds are abundant w/in our galaxy • Form in giant dust clouds in space • Organic compounds can be carried to earth by comets & meteorites • May have accumulated in oceans over millions of years during formation of the Earth
The First Organic Compounds • Oparin’s Hypothesis (1923) • Early Earth atmosphere • Reducing gasses present • NH3(ammonia); H2(hydrogen gas); H2O (water vapor); CH4(methane) • Energy source – lightning & UV radiation • Scenario: • Simple organic compounds form in atmosphere • Compounds rained into oceans • Complex organic compounds form from chemical reactions in presence of lightning & UV radiation
From Molecules toCell-like Structures • Protobionts • Form spontaneously in laboratory conditions from abiotically produced organic compounds • Have some life-like properties • Reproduce by budding • Exhibit metabolic ability • Microspheres • Proteins organized into a membrane • Coacervates • Linked amino acids & sugars organized into a droplet
The First Life-forms • The Origin of Heredity • The Roles of RNA • The First Prokaryotes • The First Eukaryotes
Learning Objectives • TSW… • Explain the importance of the chemistry of RNA in relation to the origin of life • List 3 inferred characteristics that describe the first forms of cellular life on Earth • Name 2 types of autotrophy & describe the difference btw them • Define endosymbiosis, & explain why it is important in the history of eukaryotes
HeredityReview:Transcription&Translation • Heredity & Phenotype • DNA RNA PROTEIN • Proteins give us our individual physical appearance & physiology • Q.Why is RNA necessary? • DNA is also a template • Why not make proteins directly from DNA? • A.It probably evolved 1st • RNA is simpler & readily produced by aboitic processes • Many viruses reproduce using RNA
BIG-TIME QUESTION!!!Replication requires a hereditary substance. Also, replication requires proteins to catalyze the replication process. Origin of Heredity Conundrum!!!Proteins cannot be formed w/out nucleic acids. Mmmmm…but nucleic acids cannot be formed w/out proteins!
Heredity & RNA • Roles of RNA • Transcription & translation (per earlier chapter) • Ribozyme– RNA molecule: • Acts as an enzyme • Replicates itself • The 1st life-form MAY have been a protobiont-like “cell” w/ ribozyme-like RNA enclosed • It would contain a “genetic code” • It could replicate its hereditary material • It could evolve via natural selection • It could catalyze the synthesis of proteins • What’s not to like?
The First ProkaryotesSimilar to Archaebacteria • Bacteria-like Organisms (3.8+ by) • Anaerobic metabolism • Did not use O2 • Heterotrophy • Took in organic molecules from the environment • Autotrophic Life • Chemoautotrophy –chemosynthesis • Use CO2 as C source (like photoautotrophy) • Use inorganic molecules (H2S) as energy source (not sunlight)
Later Forms:Bacteria & Cyanobacteria • Cyanobacteria (3.8 by ?) • Photosynthesis • Uses CO2 as C source • Uses sunlight as energy source • Produces O2 as a byproduct: “Oxygen Revolution” • First fossils – 3.5 by • Look like modern cyanobacteria • Aerobic Metabolism • Evolved to absorb poisonous O2 from photosynthesizing cells • Uses O2 to “burn” sugar & produce ATP energy
The First Eukaryotes • Eukaryotes (2 – 1.5 by) • Endosymbiosis • Small prokaryotes invade larger prokaryote • Mutualism: symbiotic relationship begins • Membrane Infolding • Regions of prokaryote cell membrane loop inward & pinch off into cell interior • Membranes are metabolically dedicated to specific tasks
The GeologicTime Scale Time Periods • Eons(ex. Phanerozoic) • Eras(ex. Cenozoic) • Periods(ex. Quaternary) • Epoch (ex. Holocene)