Part 1: Foundations of Environmental Science Ch 4 From Chemistry to Energy to Life PowerPoint® Slides prepared by Jay Withgott and Heidi Marcum Copyright © 2006 Pearson.
Download ReportTranscript Part 1: Foundations of Environmental Science Ch 4 From Chemistry to Energy to Life PowerPoint® Slides prepared by Jay Withgott and Heidi Marcum Copyright © 2006 Pearson.
Part 1: Foundations of Environmental Science Ch 4 From Chemistry to Energy to Life PowerPoint® Slides prepared by Jay Withgott and Heidi Marcum Copyright © 2006 Pearson Education, Inc., publishing as Benjamin Cummings Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings This lecture will help you understand: • The fundamentals of chemistry • The molecular building blocks of organisms: cell • Energy and energy flow • Photosynthesis, respiration, and chemosynthesis • Major hypotheses for life’s origins • Our knowledge of early life Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Exxon Valdez Oil Tanker In Prince William Sound, Alaska Central Case: Bioremediation of the Exxon Valdez Oil Spill • In 1989, 11 M gallons coated the Alaskan coastline The largest spill in U.S. history • Defiled the pristine environment • Tourism plummeted and jobs were lost • Bioremediation: pollution cleanup through enhanced natural biodegradation Some soil bacteria or fungi degrade Oil CmHn → C2H5OH + CO2 + H2O The recent BP Gulf Oil Spill (April ~ June, 2010): ~ 0.5 M gallons/day → ca. 50M gal , as of June 6, 2010. Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Chemistry is crucial for understanding: • How gases contribute to global climate change • How pollutants cause acid rain • The effects on health of wildlife and people • Water pollution • Wastewater treatment • Atmospheric ozone depletion • Energy issues Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Chemical building blocks • Matter : all material in the universe that has mass and occupies space - Can be transformed from one type of substance into others - But it cannot be destroyed or created which is… “The Law of Conservation of Matter” - the amount of matter stays constant - It is recycled in nutrient cycles and ecosystems Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Chemical building blocks • Matter : Mass Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Volume Chemical building blocks • Element : a fundamental type of matter, with a given set of properties (Table 4.1: Abundance) - Atoms : the smallest components that maintain an element’s chemical properties (J. Dalton, ~1805) Divisible ? - The atom’s nucleus has protons (positively charged particles) and neutrons (particles lacking electric charge) - Atomic number: the defined number of protons - Electrons : negatively charged particles surrounding the nucleus - Balances the positively charged protons Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings The structure of an atom Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Chemical building blocks • Isotopes : atoms with differing numbers of neutrons - Mass number : the combined number of protons and neutrons - Isotopes of an element behave differently - Some isotopes are radioactive and decay until they become nonradioactive stable isotopes - Emit high-energy radiation 6th Mtg end (9/4/08) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Radioactive decay (Natural Disintegration of R. Isotopes) very useful in dating materials • Half-life (t1/2) : the amount of time it takes for one-half of the atoms to disintegrate giving off radiation - Different radio-isotopes have different half-lives (ms~Gyrs) Short (Human) history 14C → 14N (5,730 y), organic matter (wood) Very Long (Geological) History 238U → 206Pb (4.47Gy), inorganic (rocks) 235U → 207Pb (0.704Gy), inorganic (rocks) 230Th → 226Ra (25ky), inorganic (oceanic sediment) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings 7th Mtg starts (9/9/08) Natural Disintegrations of Radiosotpopes (cont’d) The major source of geothermal energy (γ-ray) 40K → 238U → → → 226Ra → 222Rn 235U → → → 223Ra → 219Rn →→→ 207Pb (0.704 Gy) 232Th → → → 224Ra → 220Rn → → → 208Pb (14 Gy) 40Ar (1.28 Gy) → → → 206Pb (4.47G y) Artificial Disintegrations (“forced”) 235U + n → 91Kr + 142Ba +3n - Atomic Bomb (forced, uncontrolled) - Nuclear Power Plant (forced, controlled) Added(8/22/2013) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings 7th Mtg starts (9/9/08) Molecules & Compounds Molecules : Combinations of two or more atoms Oxygen gas (O2), Water(H2O), Sucrose (C12 H22O11) Compounds : A molecule composed of atoms of two or more different elements - Water : two hydrogen atoms bonded to one oxygen atom: H2O - Carbon dioxide : one carbon atom with two oxygen atoms: CO2 6th Mtg end (9/4/08) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Ions: eleectrically charged particles • Atoms (electrically neutral) may gain or lose electrons to become ions → electrically charged. • If loses e- → Cations (+) : Na+, Mg2+ • If gains e- →Anions (-): Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Cl-, O2- Atoms are held together with bonds • Covalent bond : atoms in a molecule share electrons - For example, the atoms that bond to form CH4. • Polar covalent bonds : Atoms share electrons unequally, with one atom exerting a greater pull The oxygen in a water molecule attracts electrons: H2O • Ionic bonds : an electron is transferred from one atom to another - Are not molecules, but are salts, such as table salt, NaCl • Solutions : mixture of substances w/o chemical bonding, eg.: wine, coca cola, oil, blood Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Water: the main reason life can exist • Hydrogen bond : oxygen from one water molecule attracts hydrogen atoms of another • Water’s strong cohesion allows nutrients and waste to be transported FOUR fellow neighbors for every water molecules in ice Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings • Water absorbs heat with only small changes in its temperature, which stabilizes systems Additional properties of water • Less dense ice floats on liquid water (Why less dense? ) • Water dissolves other molecules (excellent solvent) Density = mass/volume , d=m/V Dependence of density on temperature causes: →weather, wind, ocean currents, plate tectonics Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Water ionizes: H2O → H++ OH- Concentrations of H+ determine acidity of solutions • The pH scale ranges from 0 to 14 and quantifies the acidity of solutions: pH= -log[H+] - Acidic solutions: pH < 7 - Basic solutions: pH > 7 - Neutral solutions: pH = 7 [H+] = [OH-] = 10-7 M • A substance with pH of 6 contains 10 times as many H+ as a substance with pH of 7 7th Mtg end (9/9/08) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Drain Cleaner Organic Compounds • Organic Compounds : carbon atoms joined by covalent bonds and may include other elements - Such as nitrogen, oxygen, sulfur, and phosphorus • Hydrocarbons : contain only carbon and hydrogen - The simplest hydrocarbon is methane - Hydrocarbons can be a gas, liquid or solid Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Macromolecules: The building blocks of life large-size molecules often Polymers : long chains of repeated molecules - Three types of polymers are essential to life - Proteins - Nucleic acids - Carbohydrates - Lipids (are not polymers, but are also essential) → forms polymer like assembly water insoluble Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Proteins • Produce tissues, provide structural support, store & transport energy - Animals use proteins to generate skin, hair, muscles, and tendons - Some function as components of the immune system - They can serve as enzymes, molecules that promote certain chemical reactions Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings A special process involving proteins • Deoxyribonucleic acid (DNA) and Ribonucleic Acid (RNA) carry the hereditary information of organisms • - Long chains of nucleotides that contain sugar, phosphate, and a nitrogen base • Information in DNA is rewritten to RNA • RNA directs amino acid assembly into proteins that are synthesized (Ribosome) • Genes : regions of DNA that code for proteins that perform certain functions contained in Chromosomes. • Chromsome: made of DNA & Proteins coiled compact form of Chromatin • Genome: A complete set of chromosomes Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Carbohydrates and Lipids • Carbohydrates : consist of atoms of carbon, hydrogen, and oxygen (C, H & O) - Sugars : carbohydrate Glucose : provides energy for cells - Complex carbohydrates build structures and store energy (Natural Polymer) Starch : a complex carbohydrate of plant Cellulose: plant cell wall Glycogen: a complex carbohydrate of plant • Lipids : a chemically diverse group of compounds grouped together because they don’t dissolve in water cell membranes, structural support, and steroids • Lignin: Second most abundant macromolecule in plant (-> humic) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings We create synthetic polymers • Plastics : synthetic (human-made) polymers - Best known by their brand names (Nylon, Teflon, Kevlar) - Many are derived from petroleum hydrocarbons - Valuable because they resist chemical breakdown - Problematic because they cause long-lasting waste and pollution - Wildlife and health problems, water quality issues, harmful to marine animals - We must design less-polluting alternatives and increase recycling Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Organization of matter in living things • Cell : the basic unit of life’s organization • Prokaryotes : single-celled organisms lacking organelles and a nucleus • Eukaryotes : organisms containing complex cells with internal structures (organelles with membrane) Protists, Plants, Fungi, Animals - Ribosomes synthesize proteins - Mitrochondria extract energy from sugars and fats - Nucleus houses DNA - Chloroplast: Photosynthesis Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Hierarchy of matter in organisms Matter is organized in a hierarchy of levels, from atoms through cells through organ systems Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Characteristics of Living Organism (“Life”): (1) Organization: ordered (2) Exchange matter and energy with surroundings (environments) - consume matter & energy to maintain (& move) (3) Response to stimuli (4) Reproduction (5) Evolution: Undergo change to adapt to new environments which is changing all the time. Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Universe: consists of Matter and Energy “Law of Conservation of Mass & Energy” • Matter: Non-Living Matters: Inorganic Living Matters (Organism): “Life” (Organic) • Energy: Electromagnetic Energy(Light) Potential E., Kinetic E., Chemical E. • Living Organisms exchanges matter and energy with surroundings (environments) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Energy fundamentals • Energy : that which can change the position, physical composition or temperature of matter – ability to do a work (= Force x Distance) Potential energy (PE): energy of position Kinetic energy (KE): energy of motion Chemical energy (CE): potential energy held in the bonds • PE is changed into KE to produce motion, action, and heat Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Energy is conserved...but changes in quality • First law of thermodynamics = energy can change forms, but cannot be created or destroyed • Second law of thermodynamics = the nature of energy changes from a more-ordered to a less-ordered state - Entropy = an increasing state of disorder Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings The sun’s energy powers life • The sun releases radiation of the electromagnetic wave - Some is visible light, E= h (=hc/) - h=6.626x10-34 J.s (Planck’s constant), = frequency • Solar energy drives weather and climate, and powers plant growth Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Photosynthesis • Autotrophs (primary producers) : organisms such as green plants, algae and cyanobacteria produce their own food from the sun’s energy • Photosynthesis : the process of turning light energy from the sun into chemical energy - Carbon dioxide + water + sun’s energy is converted into sugars and high-quality energy Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Photosynthesis produces food (sugar) • Chloroplasts : organelles where photosynthesis occurs - Contain chlorophyll : a light-absorbing pigment - Light reaction : splits water by using solar energy - Calvin cycle : links carbon atoms from carbon dioxide into sugar (glucose) 6CO2 + 6H2O + sun light(energy) → C6H12O6 + 6O2 Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Cellular respiration releases chemical energy • Organisms use chemical energy from photosynthesis • Oxygen is used to convert glucose into water + carbon dioxide + energy • Heterotrophs: organisms that gain energy by feeding on others - Animals, fungi, many microbes C6H12O6 + 6O2 → Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings 6CO2 + 6H2O + Energy Early Earth:a very different place (Fig. 4.21, Tree of Life) • 4.5 billion years ago, Earth was a hostile place - Severe volcanic and tectonic activity - No oxygen (O2) existed in the atmosphere, until photosynthesis developed in microbes in a later stage CO2, CO, NH3, CH4, OH2, H2, Ar, He Escape Velocity: 12km/sec - Intense ultraviolet energy from the sun reaches Earth (b/c no O3 layer formed in the upper atmosphere) - No life existed • Life was only possible in the deep bottom of ocean, where sun’s radiation can’t reach Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Several hypotheses explain life’s origin • Primordial Soup (the Heterotrophic Hypothesis): life originated from a “primordial soup” of simple inorganic chemicals in the oceans - First life forms used organic compounds for energy • Life from the Depths (the Chemoautotrophic Hypothesis): life originated in deep-sea hydrothermal vents, with abundant sulfur - First organisms were chemoautrotrophs • “Seeds” from Space (the Panspermia Hypothesis): microbes from space traveled on meteorites to Earth - Cosmic Ansestory, Exogenesis Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Geothermal energy powers Earth’s systems • Hydrothermal vents: black smoker: underwater mini-volcano host entire communities that thrive in high temperature and pressure - Lack of sun prevents photosynthesis - Chemosynthesis: uses energy in hydrogen sulfide to produce sugar 6CO2 + 6H2O + 3H2S Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings C6H12O6 + 3H2SO4 Early Life: It’s the fossil record that teaches about earlier life on earth and its history • Single-celled bacteria occurred on Earth ~ 4 billion years ago Eukaryotes ~ 2 billion years • Fossil: an imprint in stone of a dead organism • Fossil record : gives information about the history of past life • Trilobites: Cambrian ~ Permian Period (540-250 M years ago): Extinct, probably with a Volcanic Eruption; • Dinosaurs: Triassic ~ Cretaceous Period (250~65 Mya) Extinct with an Asteroid Impact Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Brief history of Life on Earth: time before present (BP) 4.6G BP, Earth formed (CO2, CO, CH4, NH3, OH2, H2) 4.3~3.8G BP, Age of Bombardment, Chemical Evolution 3.8G BP, First Prokaryote (Archeo-Bacteria): Chemosynthetic Autotrophs 3.5G BP, Blue-green Algae, (O2 ~ 0.2%) : Photosynthetic Autotrophs 3.2G BP, Photosynthetic Bacteria produce O2, but used up 2.1G BP, First Eukaryotes, O2 started to buildup 1.5G BP, Multicellular organism (O2 ~ 3%) 800-550M BP, Cryogenic Era (-40oC): Snow Ball Earth 544M BP, Large, complex organisms (Cambrian Period starts: Explosion) 505M BP, Fish Paleozoic Era (540~251M, ~ Permian P.) 480M BP, Land plants 400M BP, Insects 380M BP, Amphibians 330M BP, Reptiles, Birds Mesozoic(251~65M, Triassic ~ CretaceousP.) 220M BP, Mammals Cenozoic (65M~ ) Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings 40M BP, Primates 5M BP, Hominids 2M BP, Homo Brief history of Mammals on Earth: 544M BP, Large, complex organisms (Cambrian Period starts) 505M BP, Fish Paleozoic (540~251M) 480M BP, Land plants Age of Fishes 400M BP, Insects 380M BP, Amphibians 330M BP, Reptiles, Birds 220M BP, Mammals 50M BP, Primates 5M BP, Hominids Mesozoic(251~65M) (Other Classes: Reptila, Amphibia) (Other Orders: Carnivora, Insectivora) (Other Families: Lemur, Monkeys) Age of Reptiles Cenozoic (65M~) Age of Mammals 2M BP, Genus Homo diverged from Australopithecines (Homo Hablis started to use Stone Tool) .25M BP, Homo Sapiens evolved replacing H. Erectus & H. Neanderthalensis (in Asia) (in Europe) 0.05M BP, culture develop more rapidly 0.01M BP, Neolithic Age (Domestication of Animals, Plants), First Town Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings 0.005 M BP, History started The fossil record shows that… • Earlier organisms evolved into later ones • Numbers of species increase over time in general • The vast majority of species are extinct • Earlier organisms were smaller and simpler • Several mass extinctions have occurred at every 50~150 M yrs, 5 major ones during last 500 M yrs • Large, complex organisms occurred 600 M years ago (since Cambrian Period) ~ 4G yrs after Earth formed. Early periods (87% of Earth Life) hade been rather quiet with extremely sluggish development of life forms Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings TREE of LIFE: Present-day organisms help decipher history Biologists use present-day organisms to get information about evolution The tree of life now consists of 3 prongs: bacteria, archaea, eukaryotes (Domains) Archea: single-celled prokaryotes very different from bacteria Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Tree of Life: Bacteria: large group of unicellular, prokaryote, microorganisms a few micrometres in length, shapes of spheres to rods & spirals. 40 million bacterial cells in a gram of soil and a million bacteria cells in a millilitre of fresh water; five nonillion (5×1030) on Earth. Protist: eg., Protozoa, protophita, slime mold, water mold. Eucaryote - Unicellular or Multicellular w/o specialized tissues Fungi: eg., Yeast, Mold, Mushroom Hetrotrophic organisms with chitinous (N-acetylglucosamine) cell wall Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings Conclusion • Life on Earth has flourished for over 3 billion years • Deciphering life’s origins depends on understanding - Energy - Energy flow - Chemistry • Chemistry can also help find solutions to environmental problems Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Review Which of the following part of an atom has a negative charge? a) Proton b) Neutron c) Electron d) Hydrogen Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Review Ionic bonds are bonds that …… a) Share electrons b) Occur when an electron is transferred from one atom to another c) Share electrons unequally d) Lose an electron Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Review Which of the following is NOT a reason water is essential for life? a) Water can absorb large amounts of heat without changing temperature b) Waste and nutrients can be transported in water c) Ice floats on liquid water, so fish survive cold winters d) Water usually cannot dissolve other molecules Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Review Of the following macromolecules, which one is NOT a polymer? a) Lipids b) Proteins c) Carbohydrates d) Nucleic acids Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Review Sugars, starches, and glucose are all: a) Lipids b) Proteins c) Carbohydrates d) Nucleic acids Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Review According to the second law of thermodynamics …? a) Energy cannot be created or destroyed b) Things tend to move toward a more disorderly state c) Matter can be created, but not energy d) Kinetic energy is the most efficient source of energy Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Review Which of the following organisms is an autotroph? a) Deep-sea tubeworm b) Horse c) Pine tree d) None of these Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Weighing the Issues Which hypothesis do you believe best explains the origin of life on Earth? a) The heterotrophic hypothesis (primordial soup) b) The panspermia hypothesis (“seeds” from space) c) The chemoautotrophic hypothesis (life from the ocean depths) d) None of these; life did not evolve Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Interpreting Graphs and Data A molecule of the hydrocarbon ethane contains…? a) 10 carbon atoms and 8 hydrogen atoms b) 8 carbon molecules and 10 hydrogen enzymes c) Carbon and hydrogen DNA d) Two different ions Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings QUESTION: Interpreting Graphs and Data Which is the most acidic material? a) Soft soap b) Rainwater c) Acid rain d) Lemon juice Copyright © 2008 Pearson Education, Inc., publishing as Benjamin Cummings