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Origin and History of Life
Chapter 18
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QOD: evolution FRQs Answer FRQ # 10 in your notebook, while I check your CH packet (this can be before or after #1-2) Continue with #1 and #2 if finished (Numbers 1, 2, and 10 are required, the rest are optional, but I would look over them as a way to study for your test)
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A. The Early Earth 1. The earth is about 4.6 BYA
2. Some chemicals present during early earth: - water vapor - nitrogen - carbon dioxide - hydrogen - methane - ammonia
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These chemicals exist within the "soup" of earth's early atmosphere
These chemicals exist within the "soup" of earth's early atmosphere. This atmosphere was inhospitable to life. Also, with no atmosphere, the earth was being hit by asteroids and other space debris.
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Monomers Evolve Miller /Urey Virtual Miller/Urey
an experiment that simulated the conditions thought at the time to be present on the early Earth, and tested for the occurrence of chemical origins of life methane (CH4), ammonia (NH3), hydrogen (H2), and water (H2O) electric current through the system, to simulate lightning storms believed to be common on the early earth, after several days, some molecules were combined monomers, (amino acids) Miller's experiment showed that organic compounds such as amino acids, which are essential to cellular life, could be made easily under the conditions that scientists believed to be present on the early earth
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Vents like this one can convert N2 to NH3 (ammonia) Ammonia is necessary for the formation or organic molecules NH4
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C. Polymers Evolve Microspheres - cell like, composed of protein (repeating units of amino acids).
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Fun Fact.. Glass microspheres (manufacured) are primarily used as a filler and volumizers, reflectors for highway safety, additive for cosmetics and adhesives, with limited applications in medical technology.
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The Protocell Evolves In water, organic chemicals do not necessarily remain uniformly dispersed but may separate out into layers or droplets. If the droplets which form contain a colloid, rich in organic compounds and are surrounded by a tight skin of water molecules, then they are known as coacervates: tiny spherical droplet of assorted organic molecules. Abiogenesis or biopoiesis is the natural process by which life arose from non-living matter such as simple organic compounds Coacervates were famously proposed by Alexander Oparin as crucial in first theory of abiogenesis (origin of life)
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A coacervate is a tiny spherical droplet of assorted organic molecules (specifically, lipid molecules) which is held together by hydrophobic forces from a surrounding liquid. Think of the way oil beads in water.
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E. Self Replication System Evolves DNA --> RNA --> Protein
Droplets of organic molecules are interesting, the fact that some even have a double membrane is even more exciting. To truly be a living organism, these structures must be able to reproduce. How did DNA (or RNA) get inside a coacervate?
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Hypotheses for Self Replicating Systems
1. RNA - First Hypothesis - the first genes were RNA, which was used as a template to make DNA 2. Protein - First Hypothesis - enzymes came first as they were needed to drive the synthesis of DNA 3. Polypeptide and RNA evolved simultaneously - this hypothesis eliminates the "chicken and egg" question.
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Once the protocell was capable of reproduction, it became a true cell
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Quick Review of the Steps that Would Give Rise to the First Cell 1
Quick Review of the Steps that Would Give Rise to the First Cell 1. Monomers Evolve 2. Macromolecules 3. Plasma membrane 4. Self Replication
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19.2 - The History of Life A. Fossils Tell a Story
remains of past life Paleontology - study of fossils and the history of life
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Sedimentation and Stratum - visible in layers of rock - sequence indicates age
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B. Relative Dating of Fossils Geologists discovered that strata of the same age contain the same fossils index fossils Index fossils can be used for the relative dating of strata.
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Absolute Dating of Fossils
1. Absolute dating relies on radioactive dating to determine the actual age of fossils. - also called numerical dating 2. Radioactive isotopes have a half-life, the time it takes for half of a radioactive isotope to change into a stable element. M&M Activity on Half Life
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Another explanation of why carbon is used to estimate time.
Another explanation of why carbon is used to estimate time. Ratios of carbon and nitrogen in fossils give a good estimate of how long something has been dead.
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Carbon 14 (14C)is a radioactive isotope
The stable molecule is Carbon 12 (12C) Half of Carbon 14 will change to Nitrogen every 5,730 years. The ratio of nitrogen to carbon 14 gives us an estimate of the age of the rock.
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EARTH’s TIMELINE
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ERAS & PERIODS 1. Precambrian Era -First cells - Bacteria - Algae
- invertebrates
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Cambrian (invertebrates) Ordovician (arthropods)
ERAS & PERIODS 2. Paleozoic Era Cambrian (invertebrates) Ordovician (arthropods)
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CAMBRIAN
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Silurian (plants) Devonian (amphibians, fish) Carboniferous (amphibians) Permian (mass extinction) Mass Extinctions mark an ERA change......next up: Mesozoic Era
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Carboniferous
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MESOZOIC ERA – THE AGE OF REPTILES
Triassic Period First small mammals Pangaea begins to separate Dinosaurs
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Figure 19.14
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Jurassic Period (213 MYA) Dinosaurs dominate earth First birds
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Figure 19A
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Jurassic Period
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Cretaceous Period Flowering Plants appear Mass Extinction of dinosaurs
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CENOZOIC ERA - The Age of Mammals
Tertiary Period (65 MYA) Birds and mammals flourish Continents move into current positions
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Cenozoic Era
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Quaternary Period Extinction of the giant mammals (mammoth) Ice Age
First Hominids
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Figure 19.6b
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Cenozoic Era
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19.3 Factors that Influence Evolution
A. Continential Drift -- biogeography - caused by plate tectonics B. Mass Extinctions (Permian, Triassic...)
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Related Videos Youtube - The Cambrian Explosion (13 Min) Nova Science Now - Permian Mass Extinction PBS - Extinction of the Dinosaurs History - Armageddon: What Killed the Dinosaurs Fox News - What Killed the Dinosaurs (3.15 min)
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AP Biology 2010 Fossil Project
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