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UNIT V Chapter 17 The History Of Life III. The History of Life A. The Fossil Record 1. Fossils and Ancient Life- fossils provide evidence about the history of life on Earth and how different groups have changed. a. Paleontologist- scientist who study fossils b. 99% of all species that ever lived are extinct 2. Interpreting Fossil Evidence a. Most fossils form in sedimentary rock 3. Relative Dating- age of fossil determined by comparing its placement with that of fossils in other layers of rock. youngest oldest 4. Radioactive dating- use radioactive decay to assign absolute ages to rocks. Age calculated by calculating amount of radioactive decay it contains B. Geologic Time Scaleevolutionary time based on boundaries in fossil record marked by mass extinctions and explosive radiations of new life forms C. Earth’s Early History 1. Formation of Earth- formed about 4.6 billion a. Early atmosphereyears ago contained hydrogen cyanide, carbon dioxide, carbon monoxide, nitrogen, hydrogen sulfide, and water. No oxygen! b. Earth cooled enough to allow first solid rocks c. 3.8 billion years agocooled enough for water to condense (formation of first sedimentary rocks) 2. First organic molecules a. Oparin-Haldane hypothesis- said conditions on primitive Earth synthesized organic compounds from inorganic compounds b. Miller and Urey- conducted experiment to determine if conditions would produce organic compounds. Scientists now know that Miller and Urey’s original simulations of Earth’s early atmosphere were not acurate. However, similar experiments based on more current knowledge of Earth’s early atmosphere have also produced organic compounds D. How Did Life Begin 1. Formation of microspheres- under certain conditions large organic molecules form tiny bubbles called proteinoid microspheres. Have some characteristics of living things. (storing and releasing energy) Microspheres are not cells, but they have some characteristics of living systems. Like cells, they have selectively permeable membranes through which water molecules can pass. 2. Evolution of RNA and DNA- puzzle not solved yet. Think that RNA existed first and could grow and duplicate themselves. May then have DNA-directed protein synthesis that now exists. 3. Free oxygen- from original anaerobic prokaryotes (bacteria) eventually photosynthetic bacteria evolved and began to produce oxygen (about 2.2 billion years ago) a. Rise in oxygen led to extinctions of some organisms b. Also led to rise in new life forms using oxygen in metabolic pathways 4. Origin of Eukaryotic cells (about 2 billion years ago) a. Endosymbiotic theory- proposes eukaryotic cells arose from living comunities formed by several organisms b. Some cell organelles have features of free-living bacteria 1). Mitochondria and chloroplasts contain DNA and ribosomes similar to bacteria’s DNA and ribosomes 2). Mitochondria and chloroplasts reproduce by binary fission when cells containing them divide by mitosis 5. Sexual reproduction and multicellularity a. Sexual reproductionarose soon after eukaryotic cells- led to increase in genetic variation and evolutionary change in species due to natural selection b. Multicellular cells- few hundred million years after sexual reproduction Ancient jellyfish, an early multicellular animal from Precambrian time D. Patterns of Evolution- six major patterns account for large scale evolutionary changes (macroevolution) 1. Mass Extinctions- led to disappearance of huge number of species. Often led to burst of evolution and new species 2. Adaptive Radiation- single species or small group of species has evolved into several different forms that live in different ways. Like Darwin’s finches. 3. Convergent Evolution- natural selection molds similar body structures in unrelated organisms. Convergent Evolution and analogous structures. The ocotillo of Southwestern North America (left) looks remarkably similar to the alluidia (right) found in Madagascar. The plants are not closely related and owe their resemblance to analogous adaptations that evolved independently in response to similar environmental pressures 4. Coevolution- evolutionary change in one organism may also be followed by corresponding change in another organism. Example: orchid has unusually long spur containing supply of nectar. The hawk moth has equally long feeding tube enabling it to feed on nectar 5. Punctuated Equilibrium- long stable periods interrupted by brief periods of more rapid change. Can occur for several reasons- genetic drift, conditions following mass extinctions 6. Developmental genes and body plans- the changes in timing of certain genes during embryonic development can contribute to genetic variation Fossil evidence shows that some ancient insects had no wings, but others had wing-like structures on many body segments. In modern insects (bottom), genes may turn off wing Hox genes in all except development one or two body segments. Chapter 17 The History Of Life What proportion of all species that ever lived has become extinct? a. less than 1 percent b. approximate one-half c. more than 99 percent d. It is impossible to estimate. What proportion of all species that ever lived has become extinct? a. less than 1 percent b. approximate one-half c. more than 99 percent d. It is impossible to estimate. Most fossils form in a. peat bogs. b. tar pits. c. sedimentary rock. d. the sap of ancient trees. Most fossils form in a. peat bogs. b. tar pits. c. sedimentary rock. d. the sap of ancient trees. The length of time required for half of the radioactive atoms in a sample to decay is its a. half-life. b. relative date. c. radioactive date. d. none of the above The length of time required for half of the radioactive atoms in a sample to decay is its a. half-life. b. relative date. c. radioactive date. d. none of the above How would you date a sample of rock that you suspect as being one of the earliest on Earth? a. Use a radioactive isotope with a short half-life. b. Use a radioactive isotope with a long half-life. c. Use an index fossil. d. It is impossible to date very early rocks. How would you date a sample of rock that you suspect as being one of the earliest on Earth? a. Use a radioactive isotope with a short half-life. b. Use a radioactive isotope with a long halflife. c. Use an index fossil. d. It is impossible to date very early rocks. The levels of division of the geologic time scale, from smallest to largest are a. eras, periods, and epochs. b. epochs, periods, and eras. c. periods, eras, and epochs. d. periods, epochs, and eras. The levels of division of the geologic time scale, from smallest to largest are a. eras, periods, and epochs. b. epochs, periods, and eras. c. periods, eras, and epochs. d. periods, epochs, and eras. The Mesozoic is often called the Age of a. Invertebrates. b. Vertebrates. c. Dinosaurs. d. Mammals. The Mesozoic is often called the Age of a. Invertebrates. b. Vertebrates. c. Dinosaurs. d. Mammals. Earth's most recent era is the a. Paleozoic. b. Mesozoic. c. Cenozoic. d. Precambrian. Earth's most recent era is the a. Paleozoic. b. Mesozoic. c. Cenozoic. d. Precambrian. Why did oceans not exist on Earth nearly 4 billion years ago? a. No water was present. b. Water remained a gas because Earth was very hot. c. Water existed as ice because Earth was very cold. d. none of the above Why did oceans not exist on Earth nearly 4 billion years ago? a. No water was present. b. Water remained a gas because Earth was very hot. c. Water existed as ice because Earth was very cold. d. none of the above Miller and Urey's experiments attempted to simulate the conditions a. of Earth's early seas. b. of Earth's early atmosphere. c. of Earth before liquid water existed. d. deep inside Earth. Miller and Urey's experiments attempted to simulate the conditions a. of Earth's early seas. b. of Earth's early atmosphere. c. of Earth before liquid water existed. d. deep inside Earth. A necessary condition for the evolution of life on Earth was a. the existence of DNA. b. free oxygen. c. the formation of the ozone layer. d. liquid water. A necessary condition for the evolution of life on Earth was a. the existence of DNA. b. free oxygen. c. the formation of the ozone layer. d. liquid water. What do proteinoid microspheres have in common with cells? a. They can store and release energy. b. They contain DNA. c. They contain RNA. d. They are communities of organisms. What do proteinoid microspheres have in common with cells? a. They can store and release energy. b. They contain DNA. c. They contain RNA. d. They are communities of organisms. The endosymbiont theory proposes that eukaryotic cells arose from a. single prokaryotic cells. b. multicellular prokaryotes. c. communities of prokaryotes inside a larger cell. d. communities of eukaryotes inside a larger cell. The endosymbiont theory proposes that eukaryotic cells arose from a. single prokaryotic cells. b. multicellular prokaryotes. c. communities of prokaryotes inside a larger cell. d. communities of eukaryotes inside a larger cell. What was the response of various groups of early organisms when oxygen levels rose in the atmosphere? a. extinction b. a move into airless habitats c. the evolution of metabolic pathways that used oxygen for respiration d. all of the above What was the response of various groups of early organisms when oxygen levels rose in the atmosphere? a. extinction b. a move into airless habitats c. the evolution of metabolic pathways that used oxygen for respiration d. all of the above The first organisms were a. prokaryotes. b. eukaryotes. c. proteinoid microspheres. d. microfossils The first organisms were a. prokaryotes. b. eukaryotes. c. proteinoid microspheres. d. microfossils A very large mass extinction occurred at the end of the a. Precambrian. b. Cambrian Period. c. Paleozoic Era d. Quaternary Period. A very large mass extinction occurred at the end of the a. Precambrian. b. Cambrian Period. c. Paleozoic Era d. Quaternary Period. The process by which two species evolve in response to each other, for example, a flower having a structure compatible with the body structure of its pollinator, is an example of a. convergent evolution. b. adaptive radiation. c. coevolution. d. punctuated equilibrium. The process by which two species evolve in response to each other, for example, a flower having a structure compatible with the body structure of its pollinator, is an example of a. convergent evolution. b. adaptive radiation. c. coevolution. d. punctuated equilibrium. A mass extinction would encourage the rapid evolution of surviving species a. by changing developmental genes. b. by opening ecological niches. c. because it killed all organisms that had coevolved. d. because it spared all organisms that had evolved convergently. A mass extinction would encourage the rapid evolution of surviving species a. by changing developmental genes. b. by opening ecological niches. c. because it killed all organisms that had coevolved. d. because it spared all organisms that had evolved convergently. A single species that has evolved into several different forms that live in different ways has undergone a. adaptive radiation. b. coevolution. c. punctuated equilibrium. d. mass extinction. A single species that has evolved into several different forms that live in different ways has undergone a. adaptive radiation. b. coevolution. c. punctuated equilibrium. d. mass extinction. Two patterns of macroevolution that involve very rapid response to environmental pressures are a. convergent evolution and changes in developmental genes. b. coevolution and convergent evolution. c. adaptive radiation and changes in developmental genes. d. punctuated equilibrium and mass extinction. Two patterns of macroevolution that involve very rapid response to environmental pressures are a. convergent evolution and changes in developmental genes. b. coevolution and convergent evolution. c. adaptive radiation and changes in developmental genes. d. punctuated equilibrium and mass extinction.